﻿PT	AU	BA	BE	GP	AF	BF	CA	TI	SO	SE	BS	LA	DT	CT	CY	CL	SP	HO	DE	ID	AB	C1	C3	RP	EM	RI	OI	FU	FP	FX	CR	NR	TC	Z9	U1	U2	PU	PI	PA	SN	EI	BN	J9	JI	PD	PY	VL	IS	PN	SU	SI	MA	BP	EP	AR	DI	DL	D2	EA	PG	WC	WE	SC	GA	PM	OA	HC	HP	DA	UT
J	Dalseg, TS; Nakrem, HA; Smelror, M				Dalseg, Thine Sanne; Nakrem, Hans Arne; Smelror, Morten			Organic-walled microfossils and palynodebris in cold seep carbonate deposits: The Upper Jurassic-Lower Cretaceous Agardhfjellet Formation on Svalbard (Arctic Norway)	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Mesozoic; seeps; carbonates; palynomorphs; palynofacies; Svalbard; Arctic	CENTRAL SPITSBERGEN; HYDROCARBON SEEP; GAS HYDRATE; AUTHIGENIC CARBONATES; JANUSFJELLET SUBGROUP; SLOTTSMOYA MEMBER; CONTINENTAL-SLOPE; SEA; GULF; PALEOENVIRONMENTS	This study gives the first detailed report of palynomorphs from Mesozoic cold hydrocarbon seep deposits. The organic-walled microfossils and palynodebris comprise ex situ fossil material in the seep deposits of the Upper Jurassic-Lower Cretaceous Agardhfjellet Formation, and consist of both specimens that originated during the time of deposition and a few fossils reworked from older strata. The palynomorphs from the Agardhfjellet Formation carbonate seep deposits in Central Spitsbergen, Svalbard, are better preserved than the palynological material in the shale deposits in the same formation. This is due to early authigenic precipitation of carbonate, which led to a relatively rapid cementation of the sediments, preventing flattening of the fossils. The Non-metric Multidimensional Scaling (NMDS) of the dinoflagellate cyst assemblages in the studied succession shows an age-specific trend, rather than being environmentally controlled, while the NMDS of the palynofacies shows that the content of palynodebris in the samples is more environmental-specific than age-specific.	[Dalseg, Thine Sanne] BakerHughes, Tanangerveien 501, NO-4056 Tananger, Norway; [Nakrem, Hans Arne] Univ Oslo, Nat Hist Museum, POB 1172, NO-0318 Oslo, Norway; [Smelror, Morten] Geol Survey Norway, POB 6215, NO-7491 Trondheim, Norway	University of Oslo; Geological Survey of Norway	Dalseg, TS (通讯作者)，BakerHughes, Tanangerveien 501, NO-4056 Tananger, Norway.	thinesd@gmail.com		Smelror, Morten/0000-0002-9593-648X	Norwegian Research Council; Norwegian Petroleum Directorate; Spitsbergen Travel; ExxonMobil; Fugro; Statoil; OMV; Powercontrols and Hydro; National Geographic Society	Norwegian Research Council(Research Council of Norway); Norwegian Petroleum Directorate; Spitsbergen Travel; ExxonMobil(Exxon Mobil Corporation); Fugro; Statoil; OMV; Powercontrols and Hydro; National Geographic Society(National Geographic Society)	We acknowledge the Norwegian Research Council, Norwegian Petroleum Directorate, Spitsbergen Travel, ExxonMobil, Fugro, Statoil, OMV, Powercontrols and Hydro and the National Geographic Society for financing our fieldwork in the years 2007-2012. The authors are also grateful to all the volunteers and students from the Svalbard Jurassic Research Group for their participation in the joint fieldwork. Constructive comments on the manuscript by Henning Dypvik and an anonymous reviewer greatly improved the final paper.	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Geol.		2016	96	2					135	146		10.17850/njg96-2-01	http://dx.doi.org/10.17850/njg96-2-01			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EA3ZD		gold, Green Submitted			2025-03-11	WOS:000386546900005
J	Smelror, M; Larssen, GB				Smelror, Morten; Larssen, Geir Birger			Are there Upper Cretaceous sedimentary rocks preserved on Sorkapp Land, Svalbard?	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Paleogene; Cretaceous; stratigraphy; dinoflagellates; Sorkapp; Svalbard; Arctic	SEQUENCE STRATIGRAPHY; LOWER PALEOGENE; BARENTS SEA; BASIN; SPITSBERGEN; BIOSTRATIGRAPHY; SUCCESSION; GREENLAND	Paleogene formations on eastern Sorkapp Land contain common, reworked, Middle and Late Cretaceous terrestrial and marine microfloras. This observation questions the Late Cretaceous age reported for the Firkanten Formation in the Oyrlandet Graben on western Sorkapp Land, as the pollen and spores reported from this graben may not be in situ. The present palynostratigraphic data from the eastern Sorkapp Land suggest that the Firkanten and Basilika formations were deposited in a relatively short time-period during the Early to Mid Thanetian. The youngest Cretaceous deposits documented from the Carolinefjellet Formation in eastern Sorkapp Land are of Late Albian age.	[Smelror, Morten] Geol Survey Norway NGU, N-7491 Trondheim, Norway; [Larssen, Geir Birger] Lundin Norway AS, POB 794, N-9488 Harstad, Norway	Geological Survey of Norway	Smelror, M (通讯作者)，Geol Survey Norway NGU, N-7491 Trondheim, Norway.	morten.smelror@ngu.no						[Anonymous], TERTIARY FOLD AND TH; [Anonymous], 1996, P ODP SCI RESULTS; [Anonymous], 1991, Rapport Gronlands geologiske Undersogelse, DOI DOI 10.34194/BULLGGU.V160.6716; BALKWILL HR, 1983, PHANEROZOIC GEOLOGY, P1; Cepek P., 2001, INTRO CONTINENTAL FO, P551; Cepek Pavel, 2001, Geologisches Jahrbuch Reihe B, V91, P535; Dallmann W.K., 1999, Lithostratigraphic lexicon of Svalbard: review and recommendations for nomenclature use: Upper Palaeozoic to Quaternary bedrock; Dypvik H, 2011, PALAEOGEOGR PALAEOCL, V302, P156, DOI 10.1016/j.palaeo.2010.12.025; FALEIDE JI, 1993, MAR PETROL GEOL, V10, P186, DOI 10.1016/0264-8172(93)90104-Z; FEYLING-HANSSEN R W, 1984, Polar Research, V2, P77, DOI 10.1111/j.1751-8369.1984.tb00487.x; Harding IC, 2011, EARTH PLANET SC LETT, V303, P97, DOI 10.1016/j.epsl.2010.12.043; Head M. J., 1984, 6TH INT PAL C CALG, P61; HELLANDHANSEN W, 1990, AAPG BULL, V74, P260; Krutzsch W., 2001, IntraContinental Fold Belts, V91, P693; MANUM S., 1960, NYTT MAG BOT, V8, P17; MANUM S B, 1986, Polar Research, V4, P103, DOI 10.1111/j.1751-8369.1986.tb00526.x; Manum S. B., 1962, NORSK POLARINSTUTT S, V125; Matthiessen J., 1986, THESIS U KIEL; Mudge DC, 2001, MAR PETROL GEOL, V18, P577, DOI 10.1016/S0264-8172(00)00074-X; Mudge DC, 1996, MAR PETROL GEOL, V13, P295, DOI 10.1016/0264-8172(95)00066-6; Nagy J, 2005, PALAEOGEOGR PALAEOCL, V222, P161, DOI 10.1016/j.palaeo.2005.03.014; Nagy J., 1970, Skr. norsk Polarinst., VNo. 152, P1; Nagy Jeno, 2000, Grzybowski Foundation Special Publication, V7, P333; Nagy Jeno, 2004, V8, P359; Nohr-Hansen H, 2000, GFF, V122, P115, DOI 10.1080/11035890001221115; Nohr-Hansen H., 1993, Dinoflagellate cyst stratigraphy of the Barremian to Albian, Lower Cretaceous, North-East Greenland, P1; Nohr-Hansen H, 2012, REV PALAEOBOT PALYNO, V178, P59, DOI 10.1016/j.revpalbo.2012.03.009; Nohr-Hansen H, 2011, GEOL SURV DEN GREENL, P61; PARKER JR, 1967, GEOL MAG, V104, P487, DOI 10.1017/S0016756800049220; Powell A.J., 1992, P155; Radmacher W, 2014, MAR PETROL GEOL, V57, P109, DOI 10.1016/j.marpetgeo.2014.04.008; Radmacher W, 2014, REV PALAEOBOT PALYNO, V201, P29, DOI 10.1016/j.revpalbo.2013.10.003; Smelror M., 1996, 252450000196 IKU; Smelror Morton, 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P83	34	7	7	0	0	GEOLOGICAL SOC NORWAY	TRONDHEIM	C/O NGU, 7491 TRONDHEIM, NORWAY	0029-196X			NORW J GEOL	Norw. J. Geol.		2016	96	2					147	158		10.7850/njg96-2-05	http://dx.doi.org/10.7850/njg96-2-05			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EA3ZD					2025-03-11	WOS:000386546900006
J	Dodsworth, P				Dodsworth, Paul			Palynostratigraphy and palaeoenvironments of the Eagle Ford Group (Upper Cretaceous) at the Lozier Canyon outcrop reference section, west Texas, USA	PALYNOLOGY			English	Article						Eagle Ford Group; Lozier Canyon; Cenomanian-Turonian boundary events; dinoflagellate cysts; prasinophyte phycomata; shale oil; geosteering; Texas	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; TURONIAN BOUNDARY EVENT; INTERIOR SEAWAY; NANNOFOSSIL PALEOECOLOGY; STRATOTYPE SECTION; STRATIGRAPHY; DINOCYST; RECORD; BASIN; ASSEMBLAGES	This study describes the detailed palynology of the Eagle Ford Group at Lozier Canyon, its principal outcrop reference section in west Texas. Prominent marine phytoplankton assemblages are consistent with a proposed depositional setting for Lozier Canyon on a submarine platform within the Cretaceous Western Interior Seaway (KWIS) of the USA. The Lower Eagle Ford Formation (middle to upper Cenomanian) was deposited under restricted marine conditions with oxygen-deficient, probably anoxic bottom waters, as indicated by the black, organic-rich (ca. 1 to > 6% total organic carbon) shale lithology. The formation comprises two fourth-order stratigraphical sequences, each showing sedimentary evidence of increasing water depth during deposition. Palynomorph assemblages from the sequences are dominated by green algal prasinophyte phycomata in the lower parts and peridinioid dinoflagellate cysts in the upper parts. The productivity of these marine phytoplankton groups may have been stimulated by availability of ammonium (prasinophytes) and nitrite (peridinioids) from upwelling, or vertical expansion of the oxygen-minimum zone. The transition from prasinophyte- to peridinioid-dominated assemblages may reflect elevation of the photic zone to a level less regularly encroached by deeper, ammonium-enriched waters of the denitrification zone. The overlying Upper Eagle Ford Formation (upper Cenomanian to upper Turonian or Coniacian) was deposited under deeper, relatively open marine conditions, as indicated by a decrease in organic carbon content and an increase in carbonate content. This is supported by the presence of diversified dinoflagellate cyst assemblages, including inter-regional (high- to mid-latitude) marker events; in the upper Cenomanian, base and acme Cyclonephelium compactum-membraniphorum, top consistent and frequent Litosphaeridium siphoniphorum, and top Adnatosphaeridium tutulosum; in the middle to upper Turonian, range bases of Heterosphaeridium difficile and Senoniasphaera rotundata. The stratigraphical resolution offered by palynology indicates potential application to wellsite geosteering' of commercial shale oil and shale gas wells drilled in the Eagle Ford Group.	[Dodsworth, Paul] StrataSolve Ltd, 42 Gaskell St, Warrington WA4 2UN, Cheshire, England		Dodsworth, P (通讯作者)，StrataSolve Ltd, 42 Gaskell St, Warrington WA4 2UN, Cheshire, England.	dodsworth@stratasolve.com		Dodsworth, Paul/0000-0002-8895-9472				Akyuz I, 2015, PALYNOLOGY TURONIAN; [Anonymous], 1993, SPEC PUBL NUMBER; [Anonymous], 1985, FINE GRAINED DEPOSIT; Bloch JD, 1999, GEOL SURV CANADA B, V531; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Brown C.W., 1962, AAPG BULL, V46, P2133, DOI [DOI 10.1306/BC743957-16BE-11D7-8645000102C1865D, 10.1306/BC743957-16BE-11D7-8645000102C1865D]; Burnett J.A., 1998, P132; Burnett JA, 1999, P YORKS GEOL SOC, V52, P371, DOI 10.1144/pygs.52.4.371; CHRISTOPHER RA, 1982, J PALEONTOL, V56, P525; Clarke R. F. 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J	Schioler, P				Schioler, Poul			<i>Bianchina hieroglyphica</i> gen. et sp nov., a new dinoflagellate cyst with a unique archaeopyle type and ornament from the mid-Cretaceous of the East Coast Basin, New Zealand	PALYNOLOGY			English	Article						fossil dinoflagellates; mid-Cretaceous; biostratigraphy; archaeopyle type; East Coast Basin; New Zealand		The new dinoflagellate cyst Bianchina hieroglyphica gen. et sp. nov. with the unique combination of archaeopyle type 3Ia3Pa(3-5'') and a characteristic penitabular, hieroglyph-like surface ornament is described from rocks of Late Aptian to Middle Cenomanian age (mid-Cretaceous) from the New Zealand East Coast Basin.	[Schioler, Poul] Morgan Goodall Palaeo Pty Ltd, Unit 1, Arvida St, Malaga, WA 6090, Australia; [Schioler, Poul] GNS Sci, POB 30-368, Lower Hutt 5040, New Zealand	GNS Science - New Zealand	Schioler, P (通讯作者)，Morgan Goodall Palaeo Pty Ltd, Unit 1, Arvida St, Malaga, WA 6090, Australia.; Schioler, P (通讯作者)，GNS Sci, POB 30-368, Lower Hutt 5040, New Zealand.	poul.schioler@mgpalaeo.com.au			GNS Science Direct Crown Funded programme Global Change Though Time, Biostratigraphy and Time Scales [GCT8]; Ministry of Science and Innovation programme, Petroleum Source Rocks and Fluids [C050x905]	GNS Science Direct Crown Funded programme Global Change Though Time, Biostratigraphy and Time Scales; Ministry of Science and Innovation programme, Petroleum Source Rocks and Fluids	The author is grateful for support from the GNS Science Direct Crown Funded programme Global Change Though Time, Biostratigraphy and Time Scales (GCT8), and the Ministry of Science and Innovation programme C050x905, Petroleum Source Rocks and Fluids. Permission from East Coast Ventures Ltd. to publish biostratigraphical data from the Ranui-2 well is greatly appreciated. Roger Tremain and Sonja Fry (GNS Science) are thanked for preparing the samples. The author is grateful to Dan Mantle (Morgan Goodall Palaeo) for useful comments on the manuscript, and is likewise grateful to two journal reviewers, one anonymous and Martin A. Pearce, Evolution Applied, as well as to the journal Editor for providing useful suggestions for improvement of the manuscript.	Batten D.J., 1999, FOSSIL PLANTS SPORES, P15; Cohen K M., 2014, International Chronostratigraphic Chart - v 2014/10; Evitt W.R., 1985, SPOROPOLLENIN DINOFL, P1; Fensome R.A., 2008, DINOFLAJ2, Version 1; Field B.D., 1997, I GEOLOGICAL NUCL SC, V19, P1; Kiel S, 2013, PALAEOGEOGR PALAEOCL, V390, P17, DOI 10.1016/j.palaeo.2012.10.033; Morgan R., 1980, PALAEONTOLOGY, V18, P1; Raine JI., 2015, 201239 GNS; SchiOler P., 2012, 201282LR GNS	9	1	1	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2016	40	3					411	417		10.1080/01916122.2015.1092479	http://dx.doi.org/10.1080/01916122.2015.1092479			7	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	DZ7LN					2025-03-11	WOS:000386047200010
J	Kozlowska, M; Barski, M; Mieszkowski, R; Antoszewska, K				Kozlowska, Malgorzata; Barski, Marcin; Mieszkowski, Radoslaw; Antoszewska, Katarzyna			A new Triassic-Jurassic section in the southern part of the Holy Cross Mts. (Poland) - implications for palaeogeography	GEOLOGICAL QUARTERLY			English	Article						Middle Jurassic transgression; dinoflagellate cysts; stratigraphy; electrical resistivity tomography (ERT)	ELECTRICAL-RESISTIVITY TOMOGRAPHY; DEPOSITIONAL SYSTEMS; BASIN; MOUNTAINS	Sedimentological, stratigraphical and geophysical studies across a new Triassic-Jurassic transition section in the Holy Cross Mts., Poland have revealed a large sedimentary hiatus embracing the entire latest Triassic Early Jurassic earliest Middle Jurassic time interval and yielded new data on the Triassic fluvial system and on Middle Jurassic shallow marine sedimentation. The presence of organic-walled dinoflagellate cysts allowed a precise age assignment of the black clay facies. Regional discussions and comparisons may be made with other areas with a similar depositional environment in Poland. For the first time a counterpart of the "Kokieliskie Beds" lithostratigraphic unit is proposed to exist in the Holy Cross Mts. area.	[Kozlowska, Malgorzata; Barski, Marcin; Mieszkowski, Radoslaw; Antoszewska, Katarzyna] Univ Warsaw, Inst Geol, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland	Polish Geological Institute - National Research Institute; University of Warsaw	Kozlowska, M (通讯作者)，Univ Warsaw, Inst Geol, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	mmkozlowska@uw.edu.pl		Kozlowska, Malgorzata/0000-0002-1904-6098; Mieszkowski, Radoslaw/0000-0002-4021-4965; Barski, Marcin/0000-0002-4102-3538	Institute of Geology, Faculty of Geology, University of Warsaw	Institute of Geology, Faculty of Geology, University of Warsaw	We would like to thank the reviewers of this paper: Prof. P. Tucholka, Dr. hab. G. Pienkowski and one anonymous reviewer for their constructive comments. We would like to express warmest acknowledgements to Prof. B.A. Matyja for his many and very helpful discussions during the research. Special thanks go to Dr. W. Kozlowski for reporting the newly exposed Wolica section and later for many perceptive discussions during the preparation of the manuscript. This work was supported by the internal grants system of the Institute of Geology, Faculty of Geology, University of Warsaw.	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Q.		2016	60	2					365	384		10.7306/gq.1259	http://dx.doi.org/10.7306/gq.1259			20	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DV8XI					2025-03-11	WOS:000383219600009
J	Gedl, P				Gedl, Przemyslaw			<i>Homotryblium</i>-dominated Eocene dinoflagellate cyst assemblages from Middle Miocene (Badenian) glauconitic sands at Lipowiec (Rortocze, SE Poland)	GEOLOGICAL QUARTERLY			English	Article						Eocene; Miocene; reworking; palaeoenvironment; Rortocze; SE Poland	CARPATHIAN FOREDEEP; ADJACENT SEAS; NORTH; OLIGOCENE; BIOSTRATIGRAPHY; BASIN; SEDIMENTS; PALEOGENE; PALEOENVIRONMENT; GREENLAND	A section over 20 m thick of the basal Middle Miocene succession exposed at Lipowiec (Rortocze, SE Poland) was studied for palynology. Thirteen samples were collected from quartz and glauconitic-quartz sands and thin clay layers. Sand samples were barren but clay samples yielded dinoflagellate cysts. Their assemblages consist of reworked Paleogene specimens dominated by the Homotryblium floripes complex (H. floripes and morphologically similar H. plectilum and H. vellum). The presence of reworked Paleogene specimens indicates intense erosion of marine Paleogene strata during initial stages of the Middle Miocene transgression at Rortocze. Analysis of stratigraphical ranges of reworked dinoflagellate cysts and comparison with their occurrences in known epicontinental Paleogene sites of SE Poland suggest an Upper Eocene age of the washed-out strata. The taxonomic composition of the assemblages described suggests that the Upper Eocene deposits accumulated in a near-shore, lagoonal embayment characterized presumably by oligotrophic waters of slightly increased salinity. A high proportion of the Homotryblium floripes complex is also characteristic of reworked assemblages found in younger Miocene strata of neighbouring exposures in Rortocze, which indicates widespread Eocene lagoonal environments in this part of Rortocze. Coeval Eocene strata from the eastern part of Rortocze and from the Carpathian Foredeep show different taxonomic compositions suggesting varied sedimentary settings during Eocene transgression in this region. These differences reflect variable amounts of freshwater influence resulting in a range of environments that ranged from oligotrophic to brackish.	[Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl						[Anonymous], 1996, Palynology: principles and applications; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Buraczyriski J., 1994, GEOL Q, V38, P739; Czepiec I., 1996, Kwart. 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H., 1986, PAPERS 1 S NEOGENE D, V17, P169; Wysocka A., 2004, POLISH GEOLOGICAL I, V13, P137; Wysocka A., 2002, ACTA GEOL POL, V52, P535	62	3	3	0	3	POLISH GEOLOGICAL INST	WARSAW	RAKOWIECKA 4, BLDG A, ROOM 434, PL-00-975 WARSAW, POLAND	1641-7291	2082-5099		GEOL Q	Geol. Q.		2016	60	2					461	472		10.7306/gq.1289	http://dx.doi.org/10.7306/gq.1289			12	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DV8XI		gold			2025-03-11	WOS:000383219600016
J	Gedl, P; Peryt, D; Peryt, TM				Gedl, Przemyslaw; Peryt, Danuta; Peryt, Tadeusz Marek			Foraminiferal and palynological organic matter records of the Upper Badenian (Middle Miocene) deposits at Anadoly (marginal part of the Ukrainian Carpathian Foredeep Basin)	GEOLOGICAL QUARTERLY			English	Article						Paratethys; Carpathian Foredeep; Upper Badenian; foraminifers; dinoflagellate cysts; palaeoenvironment	NORTH-ATLANTIC OCEAN; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; CENTRAL PARATETHYS; SALINITY CRISIS; PLANKTONIC-FORAMINIFERA; ENVIRONMENTAL-CHANGES; OXYGEN INDEX; NEOGENE; SEDIMENTS	The Badenian section of Anadoly near Kamyanets Podilskyy (Ukrainian Carpathian Foredeep Basin) consists of the Tyras Fm. (gypsum and Ratyn Limestone) and the Ternopil Mb. of the Kosiv Fm. The latter are 5.3 m thick and are composed of dark grey mudstones with limestone intercalations. This study indicates the occurrence of over 54 species of benthic foraminifers and 10 species of planktonics. Benthic foraminifera are represented mainly by calcareous forms; agglutinated tests are very rare. Planktonic foraminifera appear in the upper part of the succession studied. Five benthic foraminiferal assemblages are recognized: A (Elphidium/Lobatula/Astrononion) B (Hauerinidae), C (Cibicidoides/Lobatula), D (Porosononion) and E (Uvigerina/Bulimina). The foraminiferal record indicates deposition in a shallow subtidal environment (20 m depth) of normal marine salinity and temperate waters followed by gradual deepening of the basin to >50 m. Analysis of foraminiferal assemblages indicates that bottom waters were highly oxygenated during deposition of the lower and middle parts of the Anadoly sequence. During deposition of the upper part of the sequence the oxygenation of bottom water gradually decreased, as expressed by a large decrease in the proportion of oxic species and an increase in dysoxic ones. The same set of samples yielded low amounts of palynological organic matter represented by dominant black opaque phytoclasts; bisaccate pollen grains and dinoflagellate cysts are rare. Taxonomically impoverished assemblages of the latter consist of dominant Polysphaeridium and Cleistosphaeridium placacanthum associated with Lingulodinium machaerophorum and a few other taxa. The taxonomically richest assemblage was found in the topmost sample. These changes were interpreted as indicative for increased salinity in the surface water layer, with its maximum in the middle part of the section; the assemblage from the topmost part is characteristic for normal marine salinity.	[Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, Senacka 1, PL-31002 Krakow, Poland; [Peryt, Danuta] Polish Acad Sci, Inst Paleobiol, Twarda 51-55, PL-00818 Warsaw, Poland; [Peryt, Tadeusz Marek] Polish Geol Inst, Natl Res Inst, Rakowiecka 4, PL-00975 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; Polish Geological Institute - National Research Institute	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl	Peryt, Tadeusz/F-9289-2019; Peryt, Danuta/F-9988-2019	Peryt, Tadeusz/0000-0002-8017-1701; Peryt, Danuta/0000-0002-5821-1084	Committee on Scientific Research [6 P04D 009 11]; Ministry of Science and Higher Education [Ukraina/193/2006]	Committee on Scientific Research; Ministry of Science and Higher Education	The fieldwork was supported by research grant No. 6 P04D 009 11 (Committee on Scientific Research) to T.M. Peryt, and the analyses by special grant No. Ukraina/193/2006 (Ministry of Science and Higher Education) to M. Kotarba. We thank M. Jasionowski and A.V. Poberezhskyy for their help in the field, and the journal reviewers: N. Hudackova, M.A. Kaminski and B. Slodkowska for their helpful comments.	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Bull, V23, P1; Van der Zwaan G.J., 1983, UTRECHT MICROPALEONT, V30, P49; Van der Zwaan GJ, 1999, EARTH-SCI REV, V46, P213, DOI 10.1016/S0012-8252(99)00011-2; van Hinsbergen DJJ, 2005, PALAEOGEOGR PALAEOCL, V221, P245, DOI 10.1016/j.palaeo.2005.02.013; Verhallen P.J.J.M., 1991, Utrecht Micropaleontological Bulletins, P1; Vjalov O.S., 1981, HIST GEOLOGIC DEV UK; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wall D., 1973, Geoscience Man, V7, P95; Williams G.L., 1977, P1231; Wysocka A., 2002, ACTA GEOL POL, V52, P535	94	7	8	0	2	POLISH GEOLOGICAL INST	WARSAW	RAKOWIECKA 4, BLDG A, ROOM 434, PL-00-975 WARSAW, POLAND	1641-7291	2082-5099		GEOL Q	Geol. Q.		2016	60	2					517	536		10.7306/gq.1300	http://dx.doi.org/10.7306/gq.1300			20	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DV8XI		gold			2025-03-11	WOS:000383219600019
J	Luo, ZH; You, XJ; Mertens, KN; Gu, HF				Luo, Zhaohe; You, Xuejing; Mertens, Kenneth Neil; Gu, Haifeng			Morphological and molecular characterization of <i>Tovellia</i> cf. <i>aveirensis</i> (Dinophyceae) from Jiulong River, China	NOVA HEDWIGIA			English	Article						Cyst; freshwater dinoflagellate; Gymnodinium dodgei; type C eyespot; Woloszynskia	SP-NOV DINOPHYCEAE; GEN. NOV; ALEXANDRIUM DINOPHYCEAE; ELECTRON-MICROSCOPY; LAKE TOVEL; PHYLOGENY; ULTRASTRUCTURE; GENERA; CYSTS; CONVERGENCE	The dinoflagellate genus Tovellia is exclusively freshwater and characterized by the presence of an extraplastidial eyespot (Type C sensu Moestrup & Daugbjerg), a straight apical line of narrow plates (ALP) and a bipolar cyst with axial horns. Here we establish a Tovellia strain TSJL01 through incubation of a cyst with a pronounced paracingulum and bearing long, hollow and tapering processes collected from Jiulong River (China). The morphology of motile cells and cysts was investigated using light microscopy, scanning electron microscopy and transmission electron microscopy. Cells of strain TSJLO1 possess a long ALP on the apex, with 10 or 11 narrow elongated vesicles lined at each side. The amphiesma has many pentagonal or hexagonal latitudinal vesicles, with 7-10 series on the epicone, 4-5 on the hypocone and 2 in the cingulum. Thin sections reveal a type C eyespot, and numerous chloroplasts radiating from a central pyrenoid complex. Cysts produced in culture differ from those observed in the field in the shape of their processes. Phylogenetic analyses based on large subunit ribosomal DNA (LSU rDNA) support that TSJL01 is nested within the genus Tovellia, and is closely related to T. aveirensis. The Chinese strain differs from T aveirensis mainly in the number of elongated plates surrounding ALP and thus was tentatively identified as T. cf. aveirensis. Another closely related species, Gymnodinium dodgei, is transferred to Tovellia based on the eyespot and cyst morphology.	[Luo, Zhaohe; You, Xuejing; Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Luo, Zhaohe] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China; [You, Xuejing] Fujian Normal Univ, Fuzhou 350007, Peoples R China; [Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France	Third Institute of Oceanography, Ministry of Natural Resources; Jinan University; Fujian Normal University; Ifremer	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Mertens, Kenneth/AAO-9566-2020; Luo, Zhaohe/ITT-7163-2023; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Luo, Zhaohe/0000-0001-8662-2414; Gu, Haifeng/0000-0002-2350-9171; Mertens, Kenneth/0000-0003-2005-9483	National Natural Science Foundation of China [41376170, 41306171]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This project was supported by National Natural Science Foundation of China (41376170, 41306171). 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J	Xu, JZ; Wu, XH; Yang, YJ; Xu, S; Kang, YH; Fu, XL; Yue, H; Shi, JQ; Wu, ZX				Xu, Jinzhu; Wu, XingHua; Yang, Yanjun; Xu, Sha; Kang, Yuanhao; Fu, Xiaoli; Yue, Hong; Shi, Junqiong; Wu, Zhongxing			Changes in growth, photosynthesis and chlorophyll fluorescence in the freshwater dinoflagellate <i>Peridinium umbonatum</i> (Peridiniales, Pyrrophyta) in response to different temperatures	PHYCOLOGIA			English	Article						Chlorophyll; Fluorescence; OJIP curve; Peridinium umbonatum; Photosynthesis; Temperature	HARMFUL ALGAL BLOOMS; PHOTOSYSTEM-II; BROWN TIDE; ANOPHAGEFFERENS; ECOSYSTEMS; IRRADIANCE; MULTIPLE	Peridinium umbonatum causes harmful algal blooms in freshwater ecosystems; however, environmental conditions that promote accelerated growth and blooming of this organism have not been resolved. Increasing global temperatures has been suggested as a possible factor for shifts in phytoplankton composition to more harmful species. Therefore, this study investigated the physiological responses of this freshwater dinoflagellate to different temperatures, a factor that will strongly be affected by future climate change scenarios. Specific growth rates of P. umbonatum were markedly lower at 10 degrees C and 14 degrees C than at 18 degrees C, 25 degrees C and 30 degrees C, with the highest growth rate measured at 18 degrees C. Cell mobility was significantly inhibited at 10 degrees C and 14 degrees C. The maximum photochemical efficiency (Fv/Fm) of photosystem II and maximum relative electron transport rate decreased significantly at temperatures below 14 degrees C. However, nonphotochemical quenching significantly increased at 10 degrees C and 14 degrees C. Variable fluorescence at phase J increased in chlorophyll a fluorescence transients for P. umbonatum grown at 10 degrees C and 14 degrees C. The density of reaction centres and quantum energy flux ratios increased with increasing temperature, whereas the absorption and trapping energy flux, as well as the relative variable fluorescence intensity at the J-step, decreased with increasing temperature. These results suggest that low temperatures inhibit photosynthesis in P. umbonatum, resulting in low specific growth rates and increased cell immobility. This finding suggests that exposure to a temperature of 18 degrees C plays an important role in the growth and cyst germination of Peridinium, implying that increasing temperature might promote dinoflagellate Peridinium blooms.	[Xu, Jinzhu; Yang, Yanjun; Xu, Sha; Kang, Yuanhao; Fu, Xiaoli; Yue, Hong; Shi, Junqiong; Wu, Zhongxing] Southwest Univ, Key Lab Ecoenvironm Three Gorges Reservoir Reg, Minist Educ,Sch Life Sci, Chongqing Key Lab Plant Ecol & Resources Res Thre, Chongqing 400715, Peoples R China; [Wu, XingHua] Hubei Acad Environm Sci, Wuhan 430000, Hubei, Peoples R China	Southwest University - China	Wu, ZX (通讯作者)，Southwest Univ, Key Lab Ecoenvironm Three Gorges Reservoir Reg, Minist Educ,Sch Life Sci, Chongqing Key Lab Plant Ecol & Resources Res Thre, Chongqing 400715, Peoples R China.	wuzhx@swu.edu.cn	sha, xu/LOS-6846-2024	wu, zhong xing/0000-0002-2789-2200	National Natural Science Foundation of China [41301097, 31170372]; Fundamental Research Funds for the Central Universities [XDJK2016C111]; National science and technology major project on water pollution control and treatment [2012X07104-002]; Doctoral Found Project of China SWU [SWU110065]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Fundamental Research Funds for the Central Universities(Fundamental Research Funds for the Central Universities); National science and technology major project on water pollution control and treatment; Doctoral Found Project of China SWU	We are grateful to anonymous reviewers for helpful comments and suggestions on the manuscript. The study was supported by the National Natural Science Foundation of China (41301097 and 31170372), Fundamental Research Funds for the Central Universities (XDJK2016C111), National science and technology major project on water pollution control and treatment (2012X07104-002) and the Doctoral Found Project of China SWU (SWU110065).	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J	Caramés, A; Amenábar, CR; Concheyro, A				Carames, Andrea; Amenabar, Cecilia R.; Concheyro, Andrea			UPPER CRETACEOUS FORAMINIFERA AND PALYNOMORPHS FROM EKELOF COAST SECTION, EKELOF POINT, EASTERN JAMES ROSS ISLAND, ANTARCTIC PENINSULA	AMEGHINIANA			English	Article						Foraminifera; Palynomorphs; Upper Cretaceous; James Ross Island; Antarctic Peninsula	SANTA-MARTA FORMATION; MARAMBIO GROUP; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; CONTINENTAL-SHELF; HUMPS-ISLAND; BASIN; STRATIGRAPHY; PALEOGENE; MEMBER	A micropaleontological analysis of foraminifera and palynomorphs obtained from a partial sedimentary section cropping out at Ekelof Point, eastern James Ross Island, Antarctic Peninsula, is presented. The section, named Ekelof Coast, includes the lowest levels of the Upper Cretaceous Hamilton Point Member of the Snow Hill Island Formation. Among the foraminifera, 18 benthic taxa including 10 agglutinated and eight calcareous are recognized. Palynomorphs include continental and marine species. The continental assemblage contains 44 spore and pollen species. The marine assemblage consists of 10 peridinioid dinoflagellate cysts species, dominating in number of specimens, and 10 gonyaula-coids. Although the palynomorph assemblage supports a late Campanian age for the section, an earliest Maastrichtian age is not excluded. The paleoenvironmental interpretation based on the distribution of foraminiferal morphogroups indicates an outer shelf-upper bathyal environment in agreement with sedimentological data. The paleoenvironmental inference based on the S/D ratio (sporomorph versus dinoflagellate cysts) and the P/G ratio (peridinioid versus gonyaulacoid cysts) suggest a coastal to inner neritic setting with a continuous continental supply from the continent to the marine environment, evidenced by the slight dominance of the peridionoids over gonyaulacoids cysts. The discrepancy observed between palynological and micropaleontological-sedimentological data may be linked to the development of a narrow continental shelf during the Late Cretaceous. In such continental shelf, terrestrial palynomorphs and peridinoid cysts would quickly run down the slope and would be deposited in the deep marine environment together with gonyaulacoid cysts.	[Carames, Andrea; Amenabar, Cecilia R.; Concheyro, Andrea] Univ Buenos Aires, CONICET, Dept Ciencias Geol, Inst Estudios Andinos Don Pablo Groeber, Intendente Guiraldes 2160,Ciudad Univ,C1428EGA, Buenos Aires, DF, Argentina; [Amenabar, Cecilia R.; Concheyro, Andrea] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Buenos Aires, DF, Argentina; [Amenabar, Cecilia R.; Concheyro, Andrea] Inst Antartico Argentino, 25 Mayo 1151,3er Piso, RA-1650 San Martin, Buenos Aires, Argentina	University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; Instituto Antartico Argentino	Caramés, A (通讯作者)，Univ Buenos Aires, CONICET, Dept Ciencias Geol, Inst Estudios Andinos Don Pablo Groeber, Intendente Guiraldes 2160,Ciudad Univ,C1428EGA, Buenos Aires, DF, Argentina.	carames@gl.fcen.uba.ar; amenabar@gl.fcen.uba.ar; andrea@gl.fcen.uba.ar		AMENABAR, CECILIA R./0000-0003-1280-3903	 [PICTO DNA 2010-00112]		The authors are indebted to J. m. Lirio (Instituto Antartico Argentino) and A. Mackern for their help during sampling and geological observations at Ekelof Point and to the Direccion Nacional del Antartico-Instituto Antartico Argentino and the logistics facilities of the Fueza Aerea argentina for their assistance during the argentine Summer antarctic expedition 2008. We are grateful to P. Alvarez for the foraminifera samples preparation and to the instituto Tecnologico de Micropaleontologia (ITT FOSSIL-UNISINOS, Brasil) for the preparation of palynological samples. We also thank the Centro de Microscopia Avanzada (CMA) of the Facultad de Ciencias Exactas y naturales de la Universidad de Buenos Aires for the SEM foraminifera photographs. We would like to thank Dr. Eduardo Olivero (CADIC-CONICET, argentina) and Dr. Brian T. Huber (Smithsonian institution, USA) for their constructive suggestions and remarks which helped improve the manuscript. We also thank m. Reguero (MLP, argentina) and E. Olivero for their invite regarding the presentation of this paper for the Special number of Ameghiniana. This paper corresponds to contribution number R-175 of the Instituto de Estudios Andinos 'Don Pablo Groeber' (IDean). This work was supported by grant PICTO DNA 2010-00112.	Alekseychik-Mitskevich L.S., 1973, Trudy vsesoyuznogo neftyanogo nauchnoissledovatel'skogo geologorazvedochnogoinstituta (VNIGRI), V343, P12; [Anonymous], ADAMS ESSAYS MICROSC; [Anonymous], 1938, CONTRIBUTIONS CUSHMA; [Anonymous], 1992, GEOLOGIA ISLA J ROSS; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Avnimelech M., 1952, Contributions from the Cushman Foundation, V3, P60; BERRY E. 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J	Balkis, N; Balci, M; Giannakourou, A; Venetsanopoulou, A; Mudie, P				Balkis, Neslihan; Balci, Muharrem; Giannakourou, Antonia; Venetsanopoulou, Amalia; Mudie, Petra			Dinoflagellate resting cysts in recent marine sediments from the Gulf of Gemlik (Marmara Sea, Turkey) and seasonal harmful algal blooms	PHYCOLOGIA			English	Article						Dinoflagellates; Marine sediment; Marmara Sea; Toxic and nontoxic cysts	LATE QUATERNARY CORES; SP-NOV DINOPHYCEAE; BLACK-SEA; SURFACE SEDIMENTS; PHYTOPLANKTON COMMUNITY; PROTOCERATIUM-RETICULATUM; DISTRIBUTION PATTERNS; TOKYO-BAY; IZMIR BAY; EUTROPHICATION	Thirty-four dinoflagellate cyst taxa were found in surface sediment (0-2 cm) at five stations (60-100-m water depth) in the Gulf of Gemlik, Marmara Sea, during four seasons from August 2011 to May 2012. Lingulodinium machaerophorum, Operculodinium centrocarpum and Selenopemphix quanta dominated cyst assemblages in the polluted gulf, where nutrient-rich surface water was stratified during most seasons and bottom water was hypoxic. Twelve cyst taxa were incubated and produced motile cells that reproduced and survived 14-15 days. Highest cyst species number (33) occurred in summer; maximum number of cysts (living and empty) per cm 3 wet sediment was in spring, with the annual range from 1520 (fall) to 108,000 (spring). Nine taxa (Brigantedinium simplex, L. machaerophorum, O. centrocarpum, S. quanta, Spiniferites mirabilis, Spiniferites ramosus, cysts of Alexandrium sp., Scrippsiella trifida and S. trochoidea) were found in all seasons at all stations. The harmful dinoflagellates L. machaerophorum and cysts of S. trochoidea and Alexandrium sp. were the most abundant species. The cyst of the toxic species, Cochlodinium sp., is reported for the first time from Turkey. Other HAB species included A. tamarense, Protoceratium reticulatum, Heterocapsa triquetra and Gymnodinium catenatum/nolleri. Relative abundance of potentially toxic dinoflagellates (74%-92% of total cysts cm(-3)) was always higher than nontoxic species, and percentage abundance of cysts cm(-3) produced by autotrophs (19/34 total species) almost always exceeded those of heterotrophs. Although distributions of the resting cyst taxa were significantly influenced by surface temperature, dissolved oxygen and total water depth, surface salinity was the strongest predictor for cyst occurrences.	[Balkis, Neslihan] Istanbul Univ, Dept Biol, Fac Sci, TR-34134 Istanbul, Turkey; [Balci, Muharrem] Bursa Tech Univ, Dept Bioengn, Fac Nat Sci Architecture & Engn, Osmangazi, Bursa, Turkey; [Giannakourou, Antonia; Venetsanopoulou, Amalia] HCMR, 46km Athinon Souniou, Athens, Greece; [Mudie, Petra] Geol Survey Canada Atlantic, Box 1006, Dartmouth, NS B2Y 4A2, Canada	Istanbul University; Bursa Technical University; Hellenic Centre for Marine Research; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Balkis, N (通讯作者)，Istanbul Univ, Dept Biol, Fac Sci, TR-34134 Istanbul, Turkey.	neslbalk@istanbul.edu.tr	Balkis-Ozdelice, Neslihan/AAG-5490-2019; BALCI, Muharrem/V-9411-2017	BALKIS-OZDELICE, NESLIHAN/0000-0001-8030-7480; Giannakourou, Antonia/0000-0003-3897-0339; BALCI, Muharrem/0000-0001-9373-6647	Joint Research and Technology Program Greece-Turkey [TUBITAK 109Y385, GSRT10TUR/130 2 EYDE ETAK 1438]; NSERC (Canada)	Joint Research and Technology Program Greece-Turkey; NSERC (Canada)(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work was supported by the Joint Research and Technology Program Greece-Turkey (TUBITAK 109Y385 and GSRT10TUR/130 2 EYDE ETAK 1438 awarded to N. Balkis and A. Giannakourou). An earlier study received funding support for P. Mudie from the NSERC (Canada) Discovery Grant Program. Thanks to Dr Kazumi Matsuoka from Nagasaki University for his valuable contribution to identification of some cyst species. We also thank two anonymous reviewers for their detailed comments and suggestions for improving the clarity of our objectives and reported results.	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J	Carvalho, MD; Bengtson, P; Lana, CC				Carvalho, Marcelo de A.; Bengtson, Peter; Lana, Cecilia C.			Late Aptian (Cretaceous) paleoceanography of the South Atlantic Ocean inferred from dinocyst communities of the Sergipe Basin, Brazil	PALEOCEANOGRAPHY			English	Article						Aptian; Cretaceous; dinocysts; paleoceanography; dysoxic-anoxic event; Sergipe Basin; Brazil	DINOFLAGELLATE CYST ASSEMBLAGES; SEDIMENTARY ORGANIC-MATTER; SEA-LEVEL CHANGES; WESTERN INTERIOR BASIN; PALEOENVIRONMENTAL ANALYSIS; ENVIRONMENTAL-CHANGES; TERTIARY BOUNDARY; ALBIAN SUCCESSION; PALYNOFACIES; STRATIGRAPHY	The late Aptian (Early Cretaceous) is a crucial time interval for understanding the paleoceanographic changes in the Southern Hemisphere. Oceanographic changes in the emerging South Atlantic Ocean during this interval are reflected in the stratigraphic distribution of dinoflagellate communities recorded in the Muribeca and Riachuelo formations of the Sergipe Basin in northeastern Brazil. The Subtilisphaera community, in the lower and middle parts of the section, appears to be related to the Subtilisphaera Ecozone and suggests the onset of Tethyan influence in the central South Atlantic, in a restricted to inner-neritic environment. The succeeding Spiniferites community, in the middle part of the section, represents the first significant transgression, probably of eustatic origin. The Cyclonephelium-Exochosphaeridium community, in the upper part of the section, appears to be related to an oceanic event characterized by intermittent dysoxic-anoxic conditions. The uppermost part of the section is dominated by the Spiniferites community, related to a progressive regional transgression and culminating in an open-marine, fully Tethyan environment in the central part of the widening South Atlantic.	[Carvalho, Marcelo de A.] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Rio De Janeiro, Brazil; [Bengtson, Peter] Heidelberg Univ, Inst Geowissensch, Heidelberg, Germany; [Lana, Cecilia C.] Petrobras SA, CENPES, Gerencia Bioestratig & Paleoecol, Rio De Janeiro, Brazil	Universidade Federal do Rio de Janeiro; Ruprecht Karls University Heidelberg; Petrobras	Carvalho, MD (通讯作者)，Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Rio De Janeiro, Brazil.	mcarvalho@mn.ufrj.br	Carvalho, Marcelo/G-8463-2015; LANA, CRISTIANO/AAI-4176-2020		Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)) [302064/2010-9]; Research Support Foundation of Rio de Janeiro State (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Rio de Janeiro (FAPERJ)) [E-26/103.028/2008]; Brazilian Research Funding Organization (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)) [BEX 11616/13-0]; German Academic Exchange Service (DAAD) [A/13/03339]	Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq))(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Research Support Foundation of Rio de Janeiro State (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Rio de Janeiro (FAPERJ)); Brazilian Research Funding Organization (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); German Academic Exchange Service (DAAD)(Deutscher Akademischer Austausch Dienst (DAAD))	We are grateful to Javier Helenes Escamilla (CICESE, Ensenada, Mexico) and an anonymous reviewer, who improved this paper significantly with suggestions and critical comments. We also thank Susanne Feist-Burkhardt (SFB Geological Consulting and Services, Ober-Ramstadt, Germany) for additional palynological analyses of the GTP-24 well (unpublished Petrobras report), which provide a more precise age assessment for the section. We thank especially Marta Claudia Viviers (Petrobras, Rio de Janeiro, Brazil), who kindly analyzed the calcareous microfauna in several samples of the studied section. We express our thanks to Petrobras for giving M.A. Carvalho the opportunity to study the material. This study was funded mainly by the Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), grant no. 302064/2010-9), the Research Support Foundation of Rio de Janeiro State (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Rio de Janeiro (FAPERJ), grant no. E-26/103.028/2008), the Brazilian Research Funding Organization (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), grant no. BEX 11616/13-0), and the German Academic Exchange Service (DAAD), grant no. A/13/03339). The data used in this study can be accessed at http://archiv.ub.uniheidelberg.de/volltextserver/1586/1/marcelo.pdf.	AbdelKireem MR, 1996, J AFR EARTH SCI, V22, P93, DOI 10.1016/0899-5362(95)00125-5; [Anonymous], 1966, TXB POLLEN ANAL; [Anonymous], 1977, J. 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J	Eynaud, F; Londeix, L; Penaud, A; Sanchez-Goni, MF; Oliveira, D; Desprat, S; Turon, JL				Eynaud, Frederique; Londeix, Laurent; Penaud, Aurelie; Sanchez-Goni, Maria-Fernanda; Oliveira, Dulce; Desprat, Stephanie; Turon, Jean-Louis			Dinoflagellate cyst population evolution throughout past interglacials: Key features along the Iberian margin and insights from the new IODP Site U1385 (Exp 339)	GLOBAL AND PLANETARY CHANGE			English	Article						Dinocysts; Interglacials; Biodiversity and climate shifts; Southern Iberian margin	WESTERN MEDITERRANEAN SEA; RED TIDE DINOFLAGELLATE; SMALL-SCALE TURBULENCE; NORTH-ATLANTIC; SHACKLETON SITE; ORGANIC-MATTER; LIVING FOSSILS; CLIMATE; OCEAN; SEDIMENTS	IODP 339 Site U1385 ("Shackleton site", e.g. Hodell et al., 2013a), from the SW Iberian margin, offers the opportunity to study marine microfossil population dynamics by comparing several past interglacials and to test natural shifts of species that occurred across these warm periods, in a subtropical context. Here, more specifically, we present results obtained for the dinoflagellate cyst (dinocyst) population integrated at a regional scale thanks to the addition of data from proximal sites from southern Iberian margin. When possible, observations made using the dinocyst bio-indicator are compared to additional proxies from the same records in order to test the synchronicity of the marine biota response. Pollen data available for some of the compiled marine sequences also offer the opportunity to directly compare marine biota with terrestrial ecosystem responses. This spatio-temporal compilation reveals that, over the last 800 ka, surface waters around Iberia were tightly coupled to (rapid) climate changes and were characterised by coherent dinocyst assemblage patterns, highlighting a permanent connection between Atlantic and Mediterranean waters as evidenced through a continuous exchange of dinocyst populations. Some index species well illustrate the evolution of the regional hydrographic context along time, as for instance Spiniferites and Impagidinium species, together with Lingulodinium machaerophorum, Bitectatodinium tepikiense and heterotrophic brown cysts. They constitute key bio-indicators in context of natural environmental shifts at long and short timescales. (C) 2015 Elsevier B.V. All rights reserved.	[Eynaud, Frederique; Londeix, Laurent; Sanchez-Goni, Maria-Fernanda; Oliveira, Dulce; Desprat, Stephanie; Turon, Jean-Louis] Univ Bordeaux, CNRS, UMR EPOC 5805, Allee Geoffroy St Hilaire, F-33615 Pessac, France; [Penaud, Aurelie] Univ Brest UBO, IUEM, Lab Domaines Ocean, UMR 6538,CNRS, Pl Nicolas Copernic, Plouzane, France; [Sanchez-Goni, Maria-Fernanda; Oliveira, Dulce; Desprat, Stephanie] EPHE, CNRS, UMR EPOC 5805, F-33615 Pessac, France; [Oliveira, Dulce] IPMA, Div Geol & Georecursos Marinhos, Ave Brasilia 6, P-1449006 Lisbon, Portugal; [Oliveira, Dulce] CIMAR, Associate Lab, Oporto, Portugal	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; 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); Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Instituto Portugues do Mar e da Atmosfera; Universidade do Porto	Eynaud, F (通讯作者)，Univ Bordeaux, CNRS, UMR EPOC 5805, Allee Geoffroy St Hilaire, F-33615 Pessac, France.	f.eynaud@epoc-u-bordeaux1.fr	Sanchez Goñi, Maria Fernanda/R-3699-2019; Oliveira, Dulce/H-9855-2018; Penaud, Aurelie/F-2485-2011; Desprat, Stephanie/N-7637-2013	Oliveira, Dulce/0000-0002-3016-532X; Penaud, Aurelie/0000-0003-3578-4549; Sanchez Goni, Maria Fernanda/0000-0001-8238-7488; Eynaud, Frederique/0000-0003-1283-7425; Desprat, Stephanie/0000-0003-4400-679X	INSU (OA-LEFE-IMAGO) French CNRS programmes; INSU (TS-INTERRVIE) French CNRS programmes	INSU (OA-LEFE-IMAGO) French CNRS programmes; INSU (TS-INTERRVIE) French CNRS programmes	The crews, together with the scientific and technical staffs of the RV JOIDES Resolution are thanked for work accomplished during the IODP leg 339 and the recovery of site U1385. This study was conducted in the frame of the INSU (OA-LEFE-IMAGO and TS-INTERRVIE) French CNRS programmes within the "IceBioRAM", "Warmclim" & "Pulse" projects and grants which supported palynological analyses of the IODP339 U1385 site. We wish to thank L Devaux for preparing the samples and MC Gasparotto for her help on MIS 11 data acquisition. We gratefully acknowledge reviewers, whose anonymous comments have contributed to increase the quality of this manuscript. This is an UMR-EPOC contribution.	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J	Jung, JH; Choi, JM; Coats, DW; Kim, YO				Jung, Jae-Ho; Choi, Jung Min; Coats, D. Wayne; Kim, Young-Ok			<i>Euduboscquella costata</i> n. sp (Dinoflagellata, Syndinea), an Intracellular Parasite of the Ciliate <i>Schmidingerella arcuata</i>: Morphology, Molecular Phylogeny, Life Cycle, Prevalence, and Infection Intensity	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						18S ribosomal RNA; marine intracellular parasite; plankton; Syndinean dinoflagellate; tintinnid	DUBOSCQUELLA-CACHONI; FAVELLA-PANAMENSIS; DIVERSITY	The syndinean dinoflagellate Euduboscquella costata n. sp., an intracellular parasite of the tintinnid ciliate Schmidingerella arcuata, was discovered from Korean coastal water in November of 2013. Euduboscquella costata parasitized in about 62% of the host population, with infection intensity (- number of trophonts in a single host cell) ranging from 1 to 8. Based on morphology and nuclear 18S ribosomal RNA gene sequences, the parasite is new to science. Euduboscquella costata n. sp. had an infection cycle typical of the genus, but had morphological and developmental features that distinguished it from congeneric species. These features include: (1) episome of the trophont with 2540 grooves converging toward the center of the shield; (2) a narrow, funnel-shaped lamina pharyngea extending from the margin of the episomal shield to the nucleus; (3) persistence of grooves during extracellular development (sporogenesis); (4) a single food vacuole during sporogenesis; (5) separation of sporocytes early in sporogenesis, regardless of type of spore formed; and (6) dinospore size (ca. 14 mu m in length) and shape (bulbous episome with narrower, tapering hyposome). After sporogenesis, E. costata produced four different types of spore that showed completely identical 18S rRNA gene sequences. The gene sequence was completely identical with a previously reported population, Euduboscquella sp. ex S. arcuata, from Assawoman Bay, USA, indicating that the two populations are likely conspecific. Favella ehrenbergii, a widely recorded tintinnid known to host Euduboscquella spp., co-occurred with S. arcuata, but was not infected by E. costata in field samples or during short-term, cross-infection experiments.	[Jung, Jae-Ho; Choi, Jung Min; Kim, Young-Ok] Korea Inst Ocean Sci & Technol, Jangmok Myon 656834, Geoje, South Korea; [Coats, D. Wayne] Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA	Korea Institute of Ocean Science & Technology (KIOST); Smithsonian Institution; Smithsonian Environmental Research Center	Kim, YO (通讯作者)，Korea Inst Ocean Sci & Technol, 41 Jangmok 1, Jangmok Myon 656834, Geoje, South Korea.	yokim@kiost.ac	KIM, YOUNG JIN/E-9374-2011; Jung, Jae-Ho/L-2849-2016; Jung, Jae-Ho/G-2084-2011	Choi, Jung Min/0000-0003-4902-8453; Coats, D Wayne/0000-0002-0636-189X; Jung, Jae-Ho/0000-0001-5497-8678	KIOST project [PE99193]	KIOST project	This research was supported by KIOST projects (PE99193).	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Eukaryot. Microbiol.	JAN-FEB	2016	63	1					3	15		10.1111/jeu.12231	http://dx.doi.org/10.1111/jeu.12231			13	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	DA9LZ	25963420				2025-03-11	WOS:000368131600001
J	Richerol, T; Fréchette, B; Rochon, A; Pienitz, R				Richerol, Thomas; Frechette, Bianca; Rochon, Andre; Pienitz, Reinhard			Holocene climate history of the Nunatsiavut (northern Labrador, Canada) established from pollen and dinoflagellate cyst assemblages covering the past 7000years	HOLOCENE			English	Article						dinocysts; fjord; Holocene; Nunatsiavut; paleoclimate; palynology	SEA-SURFACE CONDITIONS; LATE QUATERNARY; QUANTITATIVE RECONSTRUCTION; ATMOSPHERIC CIRCULATION; PALYNOLOGICAL EVIDENCE; ENVIRONMENTAL-CHANGE; MARINE-SEDIMENTS; ATLANTIC CANADA; FJORDS LABRADOR; DEGLACIATION	This study documents the past similar to 7000years of Holocene climatic history for Labrador and Nunatsiavut, using a sedimentary sequence of more than 8m retrieved in Nachvak fjord, one of the northernmost fjords of Nunatsiavut. Using a multi-proxy approach combining a solid Accelerator Mass Spectrometry (AMS)-C-14 chronology and the fossil assemblages of pollen grains and dinoflagellate cysts (dinocysts), we were able to compare terrestrial and marine records in an effort to obtain a better understanding of the mid- to late-Holocene climate history of the Nunatsiavut. Records begin at the end of the deglaciation and showed a general delay in the sequence of climate events which followed, both in terrestrial and marine realms. The presence of Pentapharsodinium dalei in great abundance in Nachvak Fjord revealed a strong influence of the North Atlantic Ocean and the Labrador Sea until similar to 3000yr BP. Afterward, its rather fast disappearance marked the increased influence of Arctic waters. The last 1000years show climate stability in the region over the marine realm and a cooling trend over terrestrial landscapes.	[Richerol, Thomas; Pienitz, Reinhard] Univ Laval, Ctr Etud Nord, Lab Paleoecol Aquat, Quebec City, PQ G1V 0A6, Canada; [Richerol, Thomas; Pienitz, Reinhard] Univ Laval, Dept Geog, Quebec City, PQ G1V 0A6, Canada; [Frechette, Bianca] Univ Quebec Montreal, Ctr Rech Geochim & Geodynam Geotop, Montreal, PQ, Canada; [Rochon, Andre] Univ Quebec Rimouski, Inst Sci Mer ISMER, Lab Palynol Marine, Rimouski, PQ, Canada	Laval University; Laval University; University of Quebec; University of Quebec Montreal; University of Quebec; Universite du Quebec a Rimouski	Richerol, T (通讯作者)，Univ Laval, Ctr Etud Nord, Lab Paleoecol Aquat, 2405 Rue Terrasse,Pavillon Abitibi Price, Quebec City, PQ G1V 0A6, Canada.	thomas_richerol@yahoo.fr	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); Network of Centers of Excellence program ArcticNet; Nunatsiavut Government; Natural Sciences and Engineering Research Council of Canada [170043]	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Network of Centers of Excellence program ArcticNet; Nunatsiavut Government; Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	This work was funded through grants from the Natural Sciences and Engineering Research Council of Canada (NSERC) and the Network of Centers of Excellence program ArcticNet awarded to Reinhard Pienitz and Andre Rochon, as well as through funding from the Nunatsiavut Government. 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J	Bringué, M; Pospelova, V; Calvert, SE; Enkin, RJ; Lacourse, T; Ivanochko, T				Bringue, Manuel; Pospelova, Vera; Calvert, Stephen E.; Enkin, Randolph J.; Lacourse, Terri; Ivanochko, Tara			High resolution dinoflagellate cyst record of environmental change in Effingham Inlet (British Columbia, Canada) over the last millennium	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Primary productivity reconstructions; Warming in the second half of the 20th century; Little Ice Age; Medieval Climate Anomaly; Laminated sediments; Paleoseismicity	SEA-SURFACE TEMPERATURE; PROCESS LENGTH VARIATION; PACIFIC COASTAL FJORD; SANTA-BARBARA BASIN; VANCOUVER-ISLAND; WEST-COAST; CLIMATE VARIABILITY; NORTH PACIFIC; ICE-AGE; PROTOCERATIUM-RETICULATUM	We present a high resolution sedimentary record of dinoflagellate cysts spanning the last similar to 900 years recovered from Effingham Inlet, a glacial fjord on the west coast of Vancouver Island, Canada. The combination of seasonal coastal upwelling supporting high levels of marine primary productivity in surface waters, together with restricted bottom water circulation in the silled fjord, fosters the preservation of laminated sediments in the inner basin of Effingham Inlet. Geochemical data are used to assess the sedimentary fades of the core, which is composed primarily of laminated units (50.2%) occasionally interrupted by "seismites" (39.5%) and homogenous units (102%). The chronology of the similar to 2 m-long core is based on varve counting and fifteen C-14 dates, and is anchored by a seismite previously dated at AD 1946. The dinoflagellate cyst assemblages are diverse (total of 47 taxa), abundant (average concentrations of 102,900 cyst g(-1) of dry sediment), and characterized by a proportionally equal contribution of autotrophic and heterotrophic cyst taxa in most samples. Overall, cyst assemblages are characterized by Operculodinium centrocarpum (362%) accompanied by Brigantedinium spp. (18.0%) and Dubridinium spp. (6.6%). Multivariate analyses are used to extract the dominant patterns of variability in autotrophic and heterotrophic dinoflagellate cyst assemblages separately, and help in identifying the temperature and primary productivity gradients encoded in the cyst sedimentary record in this particular estuary. Specific intervals identified in the dinoflagellate cyst record are interpreted to represent the local expression of the "Medieval Climate Anomaly" (from the base of the record, similar to AD 1090 to 1230), the "Little Ice Age" (similar to AD 1230 to late 19th century) and warming in the second half of the 20th century. The timing of these intervals are consistent with the regional paleoclimate and help constrain past climatic and oceanographic variability on the west coast of Vancouver Island. The origin of homogenous units in the sedimentary record of Effingham Inlet and paleoseismicity in the region are also discussed. (C) 2015 Elsevier B.V. All rights reserved.	[Bringue, Manuel; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada; [Calvert, Stephen E.; Ivanochko, Tara] Univ British Columbia, Dept Earth Ocean & Atmospher Sci, Vancouver, BC V5Z 1M9, Canada; [Enkin, Randolph J.] Geol Survey Canada Pacific, Sidney, BC, Canada; [Lacourse, Terri] Univ Victoria, Dept Biol, Victoria, BC V8W 2Y2, Canada	University of Victoria; University of British Columbia; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Victoria	Bringué, M (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada.	mbringue@uvic.ca	Lacourse, Terri/G-5647-2012; Bringue, Manuel/KIH-8224-2024	Bringue, Manuel/0000-0003-4460-8344; Pospelova, Vera/0000-0003-4049-8133; Lacourse, Terri/0000-0002-7559-5374	Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT); University of Victoria Bob Wright; Commander Peter Chance MASC Graduate Fellowship	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)); University of Victoria Bob Wright; Commander Peter Chance MASC Graduate Fellowship	We are grateful to the officers and crew of the CCGS John P. Tully for their help during the sampling. Financial support for this research was provided by a Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery grant (224236) to V. Pospelova and the Canadian Foundation for Climate and Atmospheric Research (CFCAS) to S.E. Calvert. M. Bringue was supported by the Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) B2 doctoral fellowship, the University of Victoria Bob Wright Graduate Scholarship, and Commander Peter Chance MASC Graduate Fellowship. We also wish to thank M. Soon (University of British Columbia) for supervising the C, N, carbonate C and opal determinations, as well as Z. Sandwith and A. Lew for their help in processing the samples and mounting the microscope slides, and C. Nittrouer (University of Washington) for the loan of the Kasten corer. We are grateful to Dr. Fabienne Marret and one anonymous reviewer for their constructive comments that helped improve the manuscript	Allen S. 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Paleoclimatol. Paleoecol.	JAN 1	2016	441		4				787	810		10.1016/j.palaeo.2015.10.026	http://dx.doi.org/10.1016/j.palaeo.2015.10.026			24	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	CZ5AG					2025-03-11	WOS:000367113900014
J	van Helmond, NAGM; Sluijs, A; Papadomanolaki, NM; Plint, AG; Gröcke, DR; Pearce, MA; Eldrett, JS; Trabucho-Alexandre, J; Walaszczyk, I; van de Schootbrugge, B; Brinkhuis, H				van Helmond, Niels A. G. M.; Sluijs, Appy; Papadomanolaki, Nina M.; Plint, A. Guy; Groecke, Darren R.; Pearce, Martin A.; Eldrett, James S.; Trabucho-Alexandre, Joao; Walaszczyk, Ireneusz; van de Schootbrugge, Bas; Brinkhuis, Henk			Equatorward phytoplankton migration during a cold spell within the Late Cretaceous super-greenhouse	BIOGEOSCIENCES			English	Article							CENOMANIAN-TURONIAN BOUNDARY; OCEANIC ANOXIC EVENT; DINOFLAGELLATE CYST ASSEMBLAGES; CARBON-ISOTOPE STRATIGRAPHY; SEA-LEVEL CHANGE; WESTERN INTERIOR; PALEOENVIRONMENTAL ANALYSIS; KASKAPAU FORMATION; DINOCYST; BASIN	Oceanic Anoxic Event 2 (OAE2), a similar to 600 kyr episode close to the Cenomanian Turonian boundary (ca. 94 Ma), is characterized by relatively widespread marine anoxia and ranks amongst the warmest intervals of the Phanerozoic. The early stages of OAE2 are, however, marked by an episode of widespread transient cooling and bottom water oxygenation: the Plenus Cold Event. This cold spell has been linked to a decline in atmospheric pCO(2), resulting from enhanced global organic carbon burial. To investigate the response of phytoplankton to this marked and rapid climate shift we examined the biogeographical response of dinoflagellates to the Plenus Cold Event. Our study is based on a newly generated geochemical and palynological data set from a high-latitude Northern Hemisphere site, Pratts Landing (western Alberta, Canada). We combine these data with a semi-quantitative global compilation of the stratigraphic distribution of dinoflagellate cyst taxa. The data show that dinoflagellate cysts grouped in the Cyclonephelium compactum membraniphorum morphological plexus migrated from high to mid-latitudes during the Plenus Cold Event, making it the sole widely found (micro)fossil to mark this cold spell. In addition to earlier reports from regional metazoan migrations during the Plenus Cold Event, our findings illustrate the effect of rapid climate change on the global biogeographical dispersion of phytoplankton.	[van Helmond, Niels A. G. M.; Sluijs, Appy; Papadomanolaki, Nina M.; van de Schootbrugge, Bas; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Plint, A. Guy] Univ Western Ontario, Dept Earth Sci, London, ON N6A 5B7, Canada; [Groecke, Darren R.; Trabucho-Alexandre, Joao] Univ Durham, Dept Earth Sci, S Rd, Durham DH1 3LE, England; [Pearce, Martin A.] Evolut Appl Ltd, 50 Mitchell Way, Cheltenham GL54 2PL, Glos, England; [Eldrett, James S.] Shell Int Explorat & Prod Inc, Kesslerpk 1, NL-2288 GS Rijswijk, Netherlands; [Trabucho-Alexandre, Joao] Univ Utrecht, Fac Geosci, Dept Earth Sci, Comparat Sedimentol Grp, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Walaszczyk, Ireneusz] Univ Warsaw, Fac Geol, Inst Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland; [Brinkhuis, Henk] Royal Netherlands Inst Sea Res, NIOZ, POB 59, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; Western University (University of Western Ontario); Durham University; Royal Dutch Shell; Utrecht University; Polish Geological Institute - National Research Institute; University of Warsaw; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	van Helmond, NAGM (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands.	n.vanhelmond@uu.nl	Alexandre, João/AAT-5878-2020; Brinkhuis, Henk/IUO-8165-2023; Walaszczyk, Ireneusz/ABE-7229-2021; Sluijs, Appy/B-3726-2009; Grocke, Darren R./F-4799-2015	Walaszczyk, Ireneusz/0000-0002-6037-8860; Brinkhuis, Henk/0000-0003-0253-6610; van Helmond, Niels/0000-0003-0024-7217; Eldrett, James/0000-0001-5196-3112; Sluijs, Appy/0000-0003-2382-0215; Trabucho Alexandre, Joao/0000-0003-1997-027X; Grocke, Darren R./0000-0003-2296-7530; Pearce, Martin/0000-0001-7856-1076	Utrecht University; Statoil; European Research Council (ERC) under the European Union [259627]; Natural Sciences and Engineering Research Council of Canada (NSERC); UK Natural Environment Research Council (NERC) [NE/H021868/1]; NERC [NE/H021868/1] Funding Source: UKRI	Utrecht University; Statoil; European Research Council (ERC) under the European Union(European Research Council (ERC)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); UK 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 paper used data generated on sediments recovered and curated by the International Ocean Discovery Program (IODP). We thank Paul Dodsworth, Poul Schioler and an anonymous reviewer for helpful comments and suggestions and J. van Tongeren and N. Welters for laboratory assistance. Utrecht University supported this research with a "Focus en Massa" program grant to Henk Brinkhuis. Statoil provided additional financial support. The European Research Council (ERC) under the European Union's Seventh Framework Program provided funding for this work by ERC Starting Grant 259627 to Appy Sluijs. Regional studies of Cretaceous strata in western Canada were supported by a Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant to A. Guy Plint. Darren R. Grocke acknowledges funding by a UK Natural Environment Research Council (NERC) Standard Grant (NE/H021868/1). This work was carried out under the program of the Netherlands Earth System Science Centre (NESSC).	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J	Dallanave, E; Bachtadse, V; Crouch, EM; Tauxe, L; Shepherd, CL; Morgans, HEG; Hollis, CJ; Hines, BR; Sugisaki, S				Dallanave, Edoardo; Bachtadse, Valerian; Crouch, Erica M.; Tauxe, Lisa; Shepherd, Claire L.; Morgans, Hugh E. G.; Hollis, Christopher J.; Hines, Benjamin R.; Sugisaki, Saiko			Constraining early to middle Eocene climate evolution of the southwest Pacific and Southern Ocean	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						early-middle Eocene; Southwest Pacific Ocean; magnetostratigraphy; biochronology; climate evolution; early Eocene climatic optimum	SEA TEMPERATURES; MEAD STREAM; NEW-ZEALAND; PALEOCENE; BIOCHRONOLOGY; TRANSITION; SEDIMENTS	Studies of early Paleogene climate suffer from the scarcity of well-dated sedimentary records from the southern Pacific Ocean, the largest ocean basin during this time. We present a new magnetostratigraphic record from marine sediments that outcrop along the mid-Waipara River, South Island, New Zealand. Fully oriented samples for paleomagnetic analyses were collected along 45 m of stratigraphic section, which encompasses magnetic polarity Chrons from C23n to C21n (similar to 51.5-47 Ma). These results are integrated with foraminiferal, calcareous nannofossil, and dinoflagellate cyst (dinocyst) biostratigraphy from samples collected in three different expeditions along a total of similar to 80 m of section. Biostratigraphic data indicates relatively continuous sedimentation from the lower Waipawan to the upper Heretaungan New Zealand stages (i.e., lower Ypresian to lower Lutetian, 55.5 to 46 Ma). We provide the first magnetostratigraphically-calibrated age of 48.88 Ma for the base of the Heretaungan New Zealand stage (latest early Eocene). To improve the correlation of the climate record in this section with other Southern Ocean records, we reviewed the magnetostratigraphy of Ocean Drilling Program (ODP) Site 1172 (East Tasman Plateau) and Integrated Ocean Drilling Program (IODP) Site 131356 (Wilkes Land Margin, Antarctica). A paleomagnetic study of discrete samples could not confirm any reliable magnetic polarity reversals in the early Eocene at Site 1172. We use the robust magneto-biochronology of a succession of dinocyst bioevents that are common to mid-Waipara, Site 1172, and Site U1356 to assist correlation between the three records. A new integrated chronology offers new insights into the nature and completeness of the southern high-latitude climate histories derived from these sites. (C) 2015 Elsevier B.V. All rights reserved.	[Dallanave, Edoardo; Bachtadse, Valerian] Univ Munich, Dept Earth & Environm Sci, D-80333 Munich, Germany; [Crouch, Erica M.; Shepherd, Claire L.; Morgans, Hugh E. G.; Hollis, Christopher J.; Hines, Benjamin R.] GNS Sci, Lower Hutt 5040, New Zealand; [Tauxe, Lisa; Sugisaki, Saiko] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; [Shepherd, Claire L.; Hines, Benjamin R.] Victoria Univ Wellington, Sch Geog Environm & Earth Sci, Wellington 6140, New Zealand	University of Munich; GNS Science - New Zealand; University of California System; University of California San Diego; Scripps Institution of Oceanography; Victoria University Wellington	Dallanave, E (通讯作者)，Univ Munich, Dept Earth & Environm Sci, D-80333 Munich, Germany.	dallanave@geophysik.uni-muenchen.de	Crouch, Erica/C-2820-2013; Dallanave, Edoardo/AAS-6344-2020; Hollis, Christopher/D-3560-2011; Bachtadse, Valerian/E-3457-2010	Hines, Benjamin/0000-0001-6177-7137; Dallanave, Edoardo/0000-0003-4673-1792; Hollis, Christopher John/0000-0001-8840-9852; Bachtadse, Valerian/0000-0002-1226-2986; Shepherd, Claire/0000-0003-0990-7592	Deutsche Forschungsgemeinschaft (DFG) [Ba1210/19-1, Ba1210/19-2]; New Zealand Government through the GNS Science Global Change through Time Program [540GCT62]	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); New Zealand Government through the GNS Science Global Change through Time Program	This research has been supported by grants Ba1210/19-1 and Ba1210/19-2 of the Deutsche Forschungsgemeinschaft (DFG) to V. Bachtadse and by the New Zealand Government through the GNS Science Global Change through Time Program (540GCT62). We thank Cor Langereis and three anonymous reviewers for the comments that greatly improved the manuscript.	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Sci. Lett.	JAN 1	2016	433						380	392		10.1016/j.epsl.2015.11.010	http://dx.doi.org/10.1016/j.epsl.2015.11.010			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	CZ5CP		Green Submitted			2025-03-11	WOS:000367120300038
J	Fernández-Herrera, LJ; Band-Schmidt, CJ; López-Cortés, DJ; Hernández-Guerrero, CJ; Bustillos-Guzmán, JJ; Núñez-Vázquez, E				Fernandez-Herrera, Leyberth J.; Band-Schmidt, Christine J.; Lopez-Cortes, David J.; Hernandez-Guerrero, Claudia J.; Bustillos-Guzman, Jose J.; Nunez-Vazquez, Erick			Allelopathic effect of <i>Chattonella marina</i> var. <i>marina</i> (Raphidophyceae) on <i>Gymnodinium catenatum</i> (Dinophycea)	HARMFUL ALGAE			English	Article						Allelopathy; Chattonella marina; Gymnodinium catenatum; Mortality; Temporary cysts	GULF-OF-CALIFORNIA; RED-TIDE; DINOFLAGELLATE ALEXANDRIUM; TOXIC DINOFLAGELLATE; LIFE-CYCLE; MEXICAN PACIFIC; PHYTOPLANKTON; GROWTH; MECHANISMS; MICROALGAE	The allelopathic effect of the raphidophyte Chattonella marina var. marina on the dinoflagellate Gymnodinium catenatum was determined. Both species are harmful algal bloom forming algae, produce toxic metabolites, and can co-exist in the environment. In general, raphidophytes tend to dominate over dinoflagellates, which may indicate an allelopathic effect of the former algae. Strains of C. marina var. marina and G. catenatum isolated from Bahia de La Paz were cultured in bi-algal cultures with and without cell contact. Additionally, cultures of G. catenatum were exposed to cell-free culture filtrates of the raphidophyte to test whether soluble allelopathic molecules are active. During late stationary phase, both species were cultivated in mixed cultures for 72 h using the following cell abundance proportions: 20 x 10(3) cells L-1:20 x 10(3) cells L-1 (1:1; G. catenatum: C. marina); 10 x 10(3) cells L-1:20 x 10(3) cells L-1 (1:2), and 20 x 10(3) cells L-1:10 x 10(3) cells L-1 (2:1). Cells of G. catenatum were also exposed to different volumes of cell filtrates of C. marina (10, 20, and 50 mL) using the same cell abundance proportions for 24 h. Samples were taken daily for cell counts and microscopic observations. Growth inhibition was higher when there was cell contact between both species, however mortality of G. catenatum was also observed without direct cell contact, indicating that toxic metabolites are liberated to the culture medium. Changes in cell morphology of G. catenatum occurred in the presence of cells and filtrates of C. marina, such as loss of flagella and motility, swelling, loss of girdle and sulci, prominent nucleus, rupture of cell membrane, and cell lysis. Induction of temporary cysts was also observed. These results suggest that toxic metabolites are liberated to the medium by C. marina, affecting G. catenatum by inhibiting its growth and causing changes in its life history, providing new insights of interactions between raphidophytes and dinoflagellates that could happen in the natural environment when both species are present. (C) 2015 Elsevier B.V. All rights reserved.	[Fernandez-Herrera, Leyberth J.; Band-Schmidt, Christine J.; Hernandez-Guerrero, Claudia J.] Ctr Interdisciplinario Ciencias Marinas CICIMAR I, Dept Plancton & Ecol Marina, Apartado Postal 592, La Paz 23000, Bcs, Mexico; [Lopez-Cortes, David J.; Bustillos-Guzman, Jose J.; Nunez-Vazquez, Erick] Ctr Invest Biol Noroeste CIBNOR, Calle IPN 195, La Paz 23096, Bcs, Mexico	CIBNOR - Centro de Investigaciones Biologicas del Noroeste	Band-Schmidt, CJ (通讯作者)，Ctr Interdisciplinario Ciencias Marinas CICIMAR I, Dept Plancton & Ecol Marina, Apartado Postal 592, La Paz 23000, Bcs, Mexico.	cbands@ipn.mx	Hernandez-Guerrero, Claudia/AAD-9442-2020	Band-Schmidt, Christine Johanna/0000-0002-8251-9820; Nunez Vazquez, Erick Julian/0000-0003-1257-731X	Consejo Nacional de Ciencia y Tecnologia [CONACYT-SEP 178227]; CONACYT [267363, PIFI 1296, 2277, 1145];  [SIP 2015-1381];  [PC0.11];  [PC0.12]	Consejo Nacional de Ciencia y Tecnologia(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); ; ; 	We thank Ira Fogel for editing services. This project was funded by institutional projects (SIP 2015-1381, PC0.11, and PC0.12), and by the Consejo Nacional de Ciencia y Tecnologia (CONACYT-SEP 178227). C.J.B.S. and C.J.H.G. are COFFA-IPN and EDI-IPN fellows. L.J.F.H. is a recipient of student fellowships (CONACYT 267363, PIFI 1296, 2277, and 1145).[SS]	Anglès S, 2012, HARMFUL ALGAE, V16, P20, DOI 10.1016/j.hal.2011.12.008; [Anonymous], 1974, MODELS ECOLOGY; [Anonymous], DRAINAGE BASIN NUTR; Arzul G, 1999, J EXP MAR BIOL ECOL, V232, P285, DOI 10.1016/S0022-0981(98)00120-8; Band-Schmidt CJ, 2012, HYDROBIOLOGIA, V693, P81, DOI 10.1007/s10750-012-1088-y; Band-Schmidt C, 2006, J PHYCOL, V42, P757, DOI 10.1111/j.1529-8817.2006.00234.x; Band-Schmidt CJ, 2010, MAR DRUGS, V8, P1935, DOI 10.3390/md8061935; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; BRAVO I, 1986, Investigacion Pesquera (Barcelona), V50, P313; Bustillos-Guzmán JJ, 2015, FOOD ADDIT CONTAM A, V32, P381, DOI 10.1080/19440049.2014.1000978; Cai ZP, 2014, OCEANOLOGIA, V56, P639, DOI 10.5697/oc.56-3.639; Cembella AD, 2003, PHYCOLOGIA, V42, P420, DOI 10.2216/i0031-8884-42-4-420.1; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Figueroa RI, 2008, AQUAT MICROB ECOL, V52, P13, DOI 10.3354/ame01206; 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; Garate-Lizarraga I., 2009, CICIMAR Oceanides, V24, P15; GENTIEN P, 1990, J MAR BIOL ASSOC UK, V70, P571, DOI 10.1017/S0025315400036596; GLEASON FK, 1984, ARCH MICROBIOL, V138, P273, DOI 10.1007/BF00402134; Glibert P.M., 2005, OCEANOGRAPHY, V18, P132; Glibert PM, 2006, BIOGEOCHEMISTRY, V77, P441, DOI 10.1007/s10533-005-3070-5; Graneli E, 2005, DRAINAGE BASIN NUTR, P99; Granéli E, 2008, HARMFUL ALGAE, V8, P94, DOI 10.1016/j.hal.2008.08.011; Gross EM, 2003, CRIT REV PLANT SCI, V22, P313, DOI 10.1080/713610859; Hallegraeff GM, 2012, HARMFUL ALGAE, V14, P130, DOI 10.1016/j.hal.2011.10.018; Hallegraeff G.M., 1995, MANUAL HARMFUL MARIN, P365; Hattenrath-Lehmann TK, 2011, HARMFUL ALGAE, V11, P106, DOI 10.1016/j.hal.2011.08.005; HUNTLEY M, 1986, MAR ECOL PROG SER, V28, P105, DOI 10.3354/meps028105; Ianora A, 2006, ESTUAR COAST, V29, P531, DOI 10.1007/BF02784281; Ianora A, 2011, MAR DRUGS, V9, P1625, DOI 10.3390/md9091625; IVES JD, 1987, J EXP MAR BIOL ECOL, V112, P131, DOI 10.1016/0022-0981(87)90113-4; López-Cortés DJ, 2011, HIDROBIOLOGICA, V21, P185; Jugnu R, 2009, INDIAN J MAR SCI, V38, P77; Kim D, 2007, J PLANKTON RES, V29, P241, DOI 10.1093/plankt/fbm011; Kim Daekyung, 2010, P245; Kim M., 2010, 14 INT C HARMF ALG B; Kuroda A, 2005, COMP BIOCHEM PHYS C, V141, P297, DOI 10.1016/j.cca.2005.07.009; Legrand C, 2003, PHYCOLOGIA, V42, P406, DOI 10.2216/i0031-8884-42-4-406.1; Marshall JA, 2005, MAR BIOL, V147, P541, DOI 10.1007/s00227-005-1597-6; Matsuyama Y., 2000, Bull. 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J	Bastianini, M; Totti, C; Penna, A; De Lazzari, A; Montresor, M				Bastianini, M.; Totti, C.; Penna, A.; De Lazzari, A.; Montresor, M.			Dinoflagellate cyst production in the north-western Adriatic Sea	MEDITERRANEAN MARINE SCIENCE			English	Article						Dinoflagellates; cysts; sediment traps; NW Adriatic Sea; Scrippsiella; Biecheleria	SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; RECENT MARINE-SEDIMENTS; SP-NOV DINOPHYCEAE; SURFACE SEDIMENTS; RESTING CYSTS; TIME-SERIES; ALEXANDRIUM-CATENELLA; ENVIRONMENTAL-FACTORS; GONYAULAX-TAMARENSIS; MEDITERRANEAN SEA	A sediment trap study was conducted in the Gulf of Venice, north-western Adriatic Sea, from April to December 2005 to assess relationships between planktonic dinoflagellates and cyst production. Every month, CTD profiles and discrete samplings for phytoplankton, nutrients and particulate matter were conducted. Cyst fluxes spanned from 90 to 127,600 cysts m(-2) d(-1) and major peaks were due to a small cyst attributed to cf. Biecheleria and to calcareous cysts of Scrippsiella trochoidea. A good correspondence between cyst fluxes in sediment traps and the presence of the corresponding vegetative cells in the water column was detected for Lingulodinium polyedrum, and species of the genera Gonyaulax and Protoperidinium. A PCR method applied to surface sediment samples allowed the identification of a number of potentially harmful dinoflagellate cysts (Alexandrium minutum, A. taylorii, Lingulodinium polyedrum and Protoceratium reticulatum).	[Bastianini, M.; De Lazzari, A.] CNR, Ist Sci Marine, Castello 2737-F Arsenale Tesa 104, I-30122 Venice, Italy; [Totti, C.] Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, Via Brecce Bianche, I-60131 Ancona, Italy; [Penna, A.] Univ Urbino, Dipartimento Sci Biomol, Viale Trieste 296, I-61100 Pesaro, PU, Italy; [Montresor, M.] Stn Zool Anton Dohrn, I-80121 Naples, Italy	Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR); Marche Polytechnic University; University of Urbino; Stazione Zoologica Anton Dohrn	Bastianini, M (通讯作者)，CNR, Ist Sci Marine, Castello 2737-F Arsenale Tesa 104, I-30122 Venice, Italy.	mauro.bastianini@ismar.cnr.it	; TOTTI, Cecilia Maria/A-9178-2016	Bastianini, Mauro/0000-0001-6758-4192; Montresor, Marina/0000-0002-2475-1787; TOTTI, Cecilia Maria/0000-0002-1532-6009; DE LAZZARI, AMELIA/0000-0002-5915-5918	Italian Flagship Project RITMARE (Ricerca ITaliana per il MARE)	Italian Flagship Project RITMARE (Ricerca ITaliana per il MARE)	C. Totti and M. Montresor have contributed equally to this work. This research has been partly funded by the Italian Flagship Project RITMARE (Ricerca ITaliana per il MARE) and has been conducted in the framework of the LTER activities of the Northern Adriatic site. We thank the crews of R/V U. D'Ancona and M/B Litus. We thank Tiziana Romagnoli for the SEM images. We also thank Alfredo Boldrin and Alessandra Pugnetti for their critical reviews of this paper.	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Sci.		2016	17	3					751	765		10.12681/mms.1770	http://dx.doi.org/10.12681/mms.1770			15	Fisheries; Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Geology; Marine & Freshwater Biology; Oceanography	EI2KS		gold, Green Published			2025-03-11	WOS:000392316700014
B	Saraswati, PK; Srinivasan, MS	Saraswati, PK; Srinivasan, MS			Saraswati, P. K.; Srinivasan, M. S.	Saraswati, PK; Srinivasan, MS		Organic-Walled Microfossils	MICROPALEONTOLOGY: PRINCIPLES AND APPLICATIONS			English	Article; Book Chapter							DINOFLAGELLATE CYSTS; INDICATORS; MICROSCOPY; MORPHOLOGY; SEA		[Saraswati, P. K.] Indian Inst Technol, Dept Earth Sci, Bombay, Maharashtra, India; [Srinivasan, M. S.] Banaras Hindu Univ, Dept Geol, Varanasi, Uttar Pradesh, India	Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Bombay; Banaras Hindu University (BHU)	Saraswati, PK (通讯作者)，Indian Inst Technol, Dept Earth Sci, Bombay, Maharashtra, India.							[Anonymous], 1974, FOSSIL LIVING DINOFL; [Anonymous], 1980, PALEOBIOLOGY PLANT P; [Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1996, PALYNOLOGY PRINCIPLE; Crouch EM, 2003, PALAEOGEOGR PALAEOCL, V194, P387, DOI 10.1016/S0031-0182(03)00334-1; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; Dorning K.J., 2005, Encyclopedia of Geology, P418; Dutta S, 2006, J EARTH SYST SCI, V115, P99, DOI 10.1007/BF02703028; Dutta S, 2007, ORG GEOCHEM, V38, P1625, DOI 10.1016/j.orggeochem.2007.06.014; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Evitt W. R., 1961, Micropaleontology, V7, P385, DOI 10.2307/1484378; Jansonius J., 1978, Introduction to marine micropalaeontology, P341; Jones RobertWynn., 2006, Applied Palaeontology; Paris F., 2005, ENCY GEOLOGY, P428; Reichart GJ, 2003, MAR MICROPALEONTOL, V49, P303, DOI 10.1016/S0377-8398(03)00050-1; SARJEANT WAS, 1987, MICROPALEONTOLOGY, V33, P1, DOI 10.2307/1485525; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; Strother PK, 2002, AM ASS STRATIGRAPHIC, P81; Talyzina NM, 2000, REV PALAEOBOT PALYNO, V108, P37, DOI 10.1016/S0034-6667(99)00032-9; Traverse A., 2007, Paleopalynology, VSecond; Williams D.B., 1971, MICROPALAEONTOLOGY O, P91; Zhou CM, 2001, PALAEONTOLOGY, V44, P1157	22	0	0	0	0	SPRINGER INTERNATIONAL PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND			978-3-319-14574-7; 978-3-319-14573-0				2016							139	154		10.1007/978-3-319-14574-7_9	http://dx.doi.org/10.1007/978-3-319-14574-7_9	10.1007/978-3-319-14574-7		16	Paleontology	Book Citation Index– Science (BKCI-S)	Paleontology	BK3AQ					2025-03-11	WOS:000434628800010
J	Gradstein, FM; Waters, CN; Charnock, M; Munsterman, D; Hollerbach, M; Brunstad, H; Hammer, O; Vergara, L				Gradstein, Felix M.; Waters, Colin N.; Charnock, Mike; Munsterman, Dirk; Hollerbach, Michelle; Brunstad, Harald; Hammer, Oyvind; Vergara, Luis			Stratigraphic Guide to the Cromer Knoll, Shetland and Chalk Groups, North Sea and Norwegian Sea	NEWSLETTERS ON STRATIGRAPHY			English	Article							CRETACEOUS STRATIGRAPHY; BENTHIC FORAMINIFERA; FRONTIER BASINS; MID-NORWAY; BIOSTRATIGRAPHY; RESERVOIRS; ATLANTIC; EVENTS; MARGIN; DINOFLAGELLATE	This guide provides a major revision and update of the stratigraphy of the Cromer Knoll, Shetland and Chalk Groups for the UK and Norwegian sectors in the North Sea, and of the Cromer Knoll and Shetland Groups in the Norwegian Sea. The first chapters deal with the paleoceanographic and geologic settings and updated biostratigraphy, followed by the chapters with the new and improved lithostratigraphy. The Cretaceous biostratigraphy calculated for the microfossil record in 37 Norwegian wells integrates over 100 foraminifer, dinoflagellate cyst, diatom and miscellaneous events in nineteen zones, numbered from NCF1 through NCF 19 (North Sea Cretaceous Micro Fossil Zones 1-19). A literature based Dinoflagellate Cyst Zonation (DCZ), linked to the NCF zones, is also presented with eleven zones and thirty-nine subzones for Cretaceous marine strata in the North Sea. Both zonations are optimized for industrial applications with ditch cuttings samples. The lithostratigraphy of the North Sea, unified for the UK and Norwegian sectors describes 3 groups, 30 formation units and one member. The Cretaceous lithostratigraphy for the Norwegian Sea describes 2 groups, 17 formations and 14 members. This (long overdue) update alleviates misnaming and incidental use of unique names for reservoir units, without documentation and lack of biostratigraphic and correlative insight. The internet site www.nhm2.uio.no/norlex and the CD inserted with this publication provide core archives for the lithostratigraphic units.	[Gradstein, Felix M.; Hammer, Oyvind] Univ Oslo, Geol Museum, NO-0318 Oslo, Norway; [Waters, Colin N.] British Geol Survey, Keyworth NG12 5GG, Notts, England; [Charnock, Mike; Brunstad, Harald] Lundin Petr AS Norway, NO-1366 Lysaker, Norway; [Munsterman, Dirk] TNO, Geol Survey Netherlands, Utrecht, Netherlands; [Hollerbach, Michelle] Appl Petr Technol, Ovre Banegate 28, N-4014 Stavanger, Norway; [Vergara, Luis] Apache Egypt, 11 Rd 281, Cairo, Egypt	University of Oslo; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Netherlands Organization Applied Science Research	Gradstein, FM (通讯作者)，Univ Oslo, Geol Museum, NO-0318 Oslo, Norway.	felix.gradstein@gmail.com	Hammer, Øyvind/A-6319-2017		Norwegian operation of Chevron; Norwegian operation of DONG; Norwegian operation of ENI; Norwegian operation of VNG; Norwegian operation of RWE-DEA; Norwegian operation of Statoil; Norwegian operation of Idemitsu; Norwegian operation of Lundin Petroleum; Norwegian operation of ConocoPhillips; Norwegian operation of Norske Shell; DISKOS Consortium of oil companies operating offshore Norway; Norwegian Petroleum Directorate; 'The Force' Project; Norlex; NERC [bgs05001] Funding Source: UKRI	Norwegian operation of Chevron; Norwegian operation of DONG; Norwegian operation of ENI; Norwegian operation of VNG; Norwegian operation of RWE-DEA; Norwegian operation of Statoil; Norwegian operation of Idemitsu; Norwegian operation of Lundin Petroleum; Norwegian operation of ConocoPhillips; Norwegian operation of Norske Shell; DISKOS Consortium of oil companies operating offshore Norway; Norwegian Petroleum Directorate; 'The Force' Project; Norlex; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	NORLEX has received support by the Norwegian operations of Chevron, DONG, ENI, Endeavour Energy (now in VNG), RWE-DEA, Norsk Hydro (now Statoil), Idemitsu, Lundin Petroleum, ConocoPhillips, and Norske Shell. Norlex was also supported by the DISKOS Consortium of oil companies operating offshore Norway, the Norwegian Petroleum Directorate and 'The Force' Project. The International Commission on Stratigraphy (ICS) provides long term guidance and important advice regarding the use and applicability of the International Stratigraphic Guide. Advice was received from the local Norwegian Stratigraphic Committee and the Norwegian Petroleum Directorate. The Stratigraphical Commission of the Geological Society (London, UK) has been truly keen to provide advice, help and support Norlex. For this we are grateful.	Abbots I.L., 1991, PETROLEUM GEOLOGY N, P785; Andrews I.J., 1990, UK OFFSHORE REGIONAL; [Anonymous], 1987, PETROLEUM GEOLOGY N; [Anonymous], ZITTELIANA; [Anonymous], 1991, Proceedings of the Yorkshire Geological Society; [Anonymous], 1999, A Joint Chalk Stratigraphic Framework. 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Stratigr.	JAN	2016	49	1					71	280		10.1127/nos/2016/0071	http://dx.doi.org/10.1127/nos/2016/0071			208	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DE4II		Green Accepted			2025-03-11	WOS:000370592000005
J	Riding, JB; Lucas-Clark, J				Riding, James B.; Lucas-Clark, Joyce			The life and scientific work of William R. Evitt (1923-2009)	PALYNOLOGY			English	Biographical-Item						acritarchs; biography; dinoflagellates and dinoflagellate cysts; history; palaeontological techniques; trilobites; United States; William R. Evitt		Occasionally (and fortunately), circumstances and timing combine to allow an individual, almost singlehandedly, to generate a paradigm shift in his or her chosen field of inquiry. William R. (Bill') Evitt (1923-2009) was such a person. During his career as a palaeontologist, Bill Evitt made lasting and profound contributions to the study of both dinoflagellates and trilobites. He had a distinguished, long and varied career, researching first trilobites and techniques in palaeontology before moving on to marine palynomorphs. Bill is undoubtedly best known for his work on dinoflagellates, especially their resting cysts. He worked at three major US universities and spent a highly significant period in the oil industry. Bill's early profound interest in the natural sciences was actively encouraged both by his parents and at school. His alma mater was Johns Hopkins University where, commencing in 1940, he studied chemistry and geology as an undergraduate. He quickly developed a strong vocation in the earth sciences, and became fascinated by the fossiliferous Lower Palaeozoic strata of the northwestern United States. Bill commenced a PhD project on silicified Middle Ordovician trilobites from Virginia in 1943. His doctoral research was interrupted by military service during World War II; Bill served as an aerial photograph interpreter in China in 1944 and 1945, and received the Bronze Star for his excellent work. Upon demobilisation from the US Army Air Force, he resumed work on his PhD and was given significant teaching duties at Johns Hopkins, which he thoroughly enjoyed. He accepted his first professional position, as an instructor in sedimentary geology, at the University of Rochester in late 1948. Here Bill supervised his first two graduate students, and shared a great cameraderie with a highly motivated student body which largely comprised World War II veterans. At Rochester, Bill continued his trilobite research, and was the editor of the Journal of Paleontology between 1953 and 1956. Seeking a new challenge, he joined the Carter Oil Company in Tulsa, Oklahoma, during 1956. This brought about an irrevocable realignment of his research interests from trilobites to marine palynology. He undertook basic research on aquatic palynomorphs in a very well-resourced laboratory under the direction of one of his most influential mentors, William S. "Bill' Hoffmeister. Bill Evitt visited the influential European palynologists Georges Deflandre and Alfred Eisenack during late 1959 and, while in Tulsa, first developed several groundbreaking hypotheses. He soon realised that the distinctive morphology of certain fossil dinoflagellates, notably the archaeopyle, meant that they represent the resting cyst stage of the life cycle. The archaeopyle clearly allows the excystment of the cell contents, and comprises one or more plate areas. Bill also concluded that spine-bearing palynomorphs, then called hystrichospheres, could be divided into two groups. The largely Palaeozoic spine-bearing palynomorphs are of uncertain biological affinity, and these were termed acritarchs. Moreover, he determined that unequivocal dinoflagellate cysts are all Mesozoic or younger, and that the fossil record of dinoflagellates is highly selective. Bill was always an academic at heart and he joined Stanford University in 1962, where he remained until retiring in 1988. Bill enjoyed getting back into teaching after his six years in industry. During his 26-year tenure at Stanford, Bill continued to revolutionise our understanding of dinoflagellate cysts. He produced many highly influential papers and two major textbooks. The highlights include defining the acritarchs and comprehensively documenting the archaeopyle, together with highly detailed work on the morphology of Nannoceratopsis and Palaeoperidinium pyrophorum using the scanning electron microscope. Bill supervised 11 graduate students while at Stanford University. He organised the Penrose Conference on Modern and Fossil Dinoflagellates in 1978, which was so successful that similar meetings have been held about every four years since that inaugural symposium. Bill also taught many short courses on dinoflagellate cysts aimed at the professional community. Unlike many eminent geologists, Bill actually retired from actively working in the earth sciences. His full retirement was in 1988; after this he worked on only a small number of dinoflagellate cyst projects, including an extensive paper on the genus Palaeoperidinium.	[Riding, James B.] British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England; [Lucas-Clark, Joyce] Clark Geol Serv, 1023 Old Canyon Rd, Fremont, CA 94536 USA	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk			NERC [bgs05002, bgs05016] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		ALBERT N R, 1990, Palynology, V14, P209; ALBERT NR, 1988, THESIS, P481; Alberti G., 1961, Palaeontographica, V116, P1; ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ARTZNER D, 1979, SYSTEMATIC ILLUSTRAT, P119; BACHMAN SB, 1982, TRENCH FOREARC GEOLO, V10, P401; BAILEY EH, 1964, BULLETIN CALIFORNIAN, V183, P177; Baker G., 1955, AUSTR J SCI, V17, P133; Balme B.E., 1952, T I MIN ENG LONDON, V111, P870; Barnes Lawrence G., 2013, Contributions in Science (Los Angeles), P51; BARS MS, 1973, GEOLOGICAL SURVEY CA, P25; BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; BATTEN D J, 1988, Cretaceous Research, V9, P337, DOI 10.1016/0195-6671(88)90007-9; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BELOW R, 1981, PALAEONTOGR ABT B, V1, P145; BELOW R, 1990, PALAEONTOGR ABT B, V1, P96; BERKLAND JO, 1973, GEOL SOC AM BULL, V84, P2389, DOI 10.1130/0016-7606(1973)84<2389:RVOSOC>2.0.CO;2; BERKLAND JO, 1972, AM ASSOC PETR GEOL B, V56, P2295; BEROZA GC, 1991, B SEISMOL SOC AM, V81, P1603; BINT A N, 1983, Palynology, V7, P171; BINT A N, 1986, Palynology, V10, P135; BINT AN, 1984, THESIS, P373; Blake M.C., 1974, Modern and Ancient Geosynclinal Sedimentation: Society of Economic Paleontologists and Mineralogists Special Publication, V19, P345, DOI [10.2110/pec.74.19.0345, DOI 10.2110/PEC.74.19.0345, 10.2110/pec.74.19]; EVITT WR, PUBLICATION LIST	26	15	15	1	7	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2016	40			1	SI		2	131		10.1080/01916122.2016.1147792	http://dx.doi.org/10.1080/01916122.2016.1147792			130	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	DK4KH		Green Accepted, hybrid, Green Submitted			2025-03-11	WOS:000374886400002
J	Servals, T; Martin, RE; Nützel, A				Servals, Thomas; Martin, Ronald E.; Nuetzel, Alexander			The impact of the terrestrialisation process' in the late Palaeozoic: <i>p</i>CO<sub>2</sub>, <i>p</i>O<sub>2</sub>, and the 'phytoplankton blackout'	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Phytoplankton; Acritarchs; Dinoflagellates; Carboniferous; Permian; Planktotrophy	PHANEROZOIC TAXONOMIC DIVERSITY; KINETIC-MODEL; ORDOVICIAN BIODIVERSIFICATION; MACROEVOLUTIONARY PATTERNS; GLOBAL DIVERSITY; ATMOSPHERIC CO2; REVISED MODEL; FOSSIL RECORD; LAND PLANTS; EVOLUTION	With few exceptions, the impact of the evolution of the terrestrial biosphere on the evolution of the marine sphere has been largely ignored. So too has the resulting complementary role of marine photosynthesis and primary productivity in the evolution of atmospheric and oceanic pCO(2) and pO(2) in response to land-sea interactions. The Early-Middle Palaeozoic invasion of the continents by plants is considered to be responsible for major changes in the carbon cycle and changing values of pO(2) and pCO(2) in the atmosphere. Some authors have also related the 'terrestrialisation process' to the rapid Late Devonian decline of organic-walled phytoplankton (acritarch) diversity. The stratigraphical interval between the Carboniferous and early Triassic, i.e., the late Palaeozoic-Early Mesozoic, is a time period with a very low diversity of organic-walled phytoplankton, and this period was therefore considered by some authors as corresponding to a 'Phytoplankton Blackout.' It has been argued that the marine food web during this interval was related to the invasion of land by plants, suggesting that a reduced nutrient input to the ocean by runoff decreased the number of acritarchs and primary production in the marine realm. Subsequently, it has also been suggested that the Phanerozoic phytoplankton record can be correlated with models of pCO(2) with high acritarch diversities corresponding to periods of high pCO(2). Conversely, the spread of terrestrial forests may have increased weathering rates via deeper rooting, releasing increased amounts of nutrients to the oceans while also increasing atmospheric pCO(2). The present paper critically reviews the proposed scenarios and discusses the possible relations between terrestrial and marine ecosystems, in particular the possible impact of the terrestrialisation process on marine phytoplankton. The known Palaeozoic fossil record of the phytoplankton is incomplete to a high degree. It consists almost entirely on the organic-walled fraction, because calcareous and siliceous phytoplankton remain almost unrecorded. In addition, the fossil record solely provides information about the diversity of cysts, but not necessarily precise data of the number and quality of the cyst-producing phytoplanktonic organisms. Taking into consideration that only few modern phytoplankton taxa produce cysts, the absence of cysts in the fossil record does not necessarily imply the absence of phytoplankton. In contrast, the presence of planktotrophic larvae of marine invertebrate organisms indicates that phytoplankton must have been present in the Late Palaeozoic oceans, and the marine trophic web did indeed not collapse in the Late Devonian. The presence and abundance of filter feeding and suspension feeding benthic organisms such as brachiopods, crinoids, sponges and corals also suggest sufficient primary production in the Lite Palaeozoic seas. It can be concluded that, although the phytoplankton is largely absent from the fossil record, a 'phytoplankton blackout' is unrealistic. A major remaining question is to understand why the cyst production decreased after the Late Devonian and why this might be correlated to changes of pCO(2). (C) 2015 Elsevier B.V. All rights reserved.	[Servals, Thomas] Univ Lille, CNRS, UMR 8198, Evo Eco Paleo, F-59655 Villeneuve Dascq, France; [Martin, Ronald E.] Univ Delaware, Dept Geol Sci, Newark, DE 19716 USA; [Nuetzel, Alexander] GeoBio Ctr LMU, Palaeontol & Geobiol, Dept Earth & Environm Sci, SNSB Bayer Staatssammlung Palaontol & Geol, D-80333 Munich, Germany	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite de Lille; University of Delaware; University of Munich	Servals, T (通讯作者)，Univ Lille, CNRS, UMR 8198, Evo Eco Paleo, F-59655 Villeneuve Dascq, France.	thomas.servais@univ-lille1.fr	Servais, Thomas/S-8045-2019; Nützel, Alexander/ABB-6301-2020; Servais, Thomas/I-2115-2018	Nutzel, Alexander/0000-0002-8852-7688; Servais, Thomas/0000-0002-4089-7874	Agence Nationale de Recherche (ANR) project [ANR-10-BLAN-0607]; Agence Nationale de la Recherche (ANR) [ANR-10-BLAN-0607] Funding Source: Agence Nationale de la Recherche (ANR)	Agence Nationale de Recherche (ANR) project(Agence Nationale de la Recherche (ANR)); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	The idea to produce the present paper initiated at a scientifical congress at Erlangen (Germany), where the three authors met. Several colleagues are thanked for providing useful elements of discussion over the years that helped to draft this manuscript, including Alain Blieck (Lille, France), Yukio Isozaki (Tokyo, Japan), Gary Mullins (Llandudno, UK), Axel Munnecke (Erlangen, Gemany), Robert Riding (Knoxville, USA), Lorenz Schwark (Kiel, Germany) and Paul Strother (Boston, USA) and others. We are particularly grateful to the two reviewers of the papers, Gerard Versteegh (Bremen, Germany) and Paul Strother (Boston, USA). This is a contribution to the Agence Nationale de Recherche (ANR) project "Terrestrialisation" (ANR-10-BLAN-0607). Ron Martin benefited from an "invited professorship" at the University of Lille.	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S	Feist-Burkhardt, S; Götz, AE		Montenari, M		Feist-Burkhardt, S.; Goetz, A. E.			Ultra-High-Resolution Palynostratigraphy of the Early Bajocian Sauzei and Humphriesianum Zones (Middle Jurassic) from Outcrop Sections in the Upper Rhine Area, Southwest Germany	STRATIGRAPHY & TIMESCALES, VOL 1	Stratigraphy and Timescales		English	Article; Book Chapter							NORTH-WEST SHELF; DINOFLAGELLATE CYSTS; HAUPTROGENSTEIN; RADIATION	Marine and terrestrial palynomorphs of the Middle Jurassic, Early Bajocian are documented from three outcrop sections in the Upper Rhine area, southwest Germany. The studied part of the sections corresponds to the Early Bajocian Sauzei and Humphriesianum zones and is independently age dated down to ammonite subzone level. Palynomorph assemblages are quantitatively studied and detailed data are provided. The palynomorph assemblages are discussed and a succession of dinoflagellate cyst stratigraphical events is proposed. The dinoflagellate cyst assemblages are characterized by many first occurrences of known taxa and many new taxa left in open nomenclature. Most of them belong to the family of the Gonyaulacaceae that typically shows very fast evolution at this time. The findings are compared to coeval assemblages from Europe and Australasia. The study provides detailed data on the dinoflagellate cyst succession in a poorly studied time interval at a much finer scale than previously known. It will add valuable information to improve Middle Jurassic palynostratigraphical schemes.	[Feist-Burkhardt, S.] SFB Geol Consulting & Serv, Ober Ramstadt, Germany; [Feist-Burkhardt, S.] Univ Geneva, Geneva, Switzerland; [Goetz, A. E.] Keele Univ, Keele, Staffs, England	University of Geneva; Keele University	Feist-Burkhardt, S (通讯作者)，SFB Geol Consulting & Serv, Ober Ramstadt, Germany.; Feist-Burkhardt, S (通讯作者)，Univ Geneva, Geneva, Switzerland.	feistburkhardt@gmail.com	Feist-Burkhardt, Susanne/B-1522-2009; Götz, Annette/AAJ-5873-2020	Feist-Burkhardt, Susanne/0000-0001-6019-6242; Gotz, Annette E./0000-0002-7467-3617				[Anonymous], 2015, TIMESCALE CREATOR; [Anonymous], 2016, STRATABUGS; [Anonymous], 2016, LANDESAMT GEOLOGIE R; Bloos G, 2005, NEWSL STRATIGR, V41, P263, DOI 10.1127/0078-0421/2005/0041-0263; Bloos G., 2005, NEWSL STRATIGR, V41, P1; Burkhalter RM, 1997, ECLOGAE GEOL HELV, V90, P269; Butler N, 2005, MICROPALEAEONTOLOGIC, P43; Dietze V., 2011, TEIL BAJOCIUM JH GES, V167, P49; Dietze Volker, 2015, Palaeodiversity, V8, P31; Dietze Volker, 2013, Palaeodiversity, P29; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; Drugg W.S., 1978, PALAEONTOGRAPHICA AB, V168, P61; Evitt W. 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Abh., V119, P113; Gonzalez R, 1996, ECLOGAE GEOL HELV, V89, P695; Gonzalez R, 1996, SEDIMENT GEOL, V102, P111, DOI 10.1016/0037-0738(95)00059-3; Gowland S., 1991, Proceedings of the Yorkshire Geological Society, V48, P375; Gradstein F., 2004, A Geological Time Scale; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P1; Hostettler B., 2016, SWISS J GEOS INPRESS; Kommission Deutsche Stratigraphische, 2002, DTSCH STRATIGRAPHISC; Mantle DJ, 2012, REV PALAEOBOT PALYNO, V180, P41, DOI 10.1016/j.revpalbo.2012.03.005; Ohmert W., 1988, Jahreshefte des Geologischen Landesamtes Baden-Wuerttemberg, V30, P315; OHMERT W., 1994, GEOBIOS, V17, P359; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Riding J.B., 1992, P7; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; Riding James B., 2001, Memoir of the Association of Australasian Palaeontologists, V24, P33; Riding JB, 2010, REV PALAEOBOT PALYNO, V162, P543, DOI 10.1016/j.revpalbo.2010.07.008; Riding James B., 1991, Palynology, V15, P115; Rioult M., 1997, BULL CENT RECH ELF E, V17, P41; van de Schootbrugge B, 2005, PALEOBIOLOGY, V31, P73, DOI 10.1666/0094-8373(2005)031<0073:EJCCAT>2.0.CO;2; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Woollam R., 1983, Report Institute of Geological Sciences, P1; [No title captured]	48	6	7	0	0	ACADEMIC PRESS LTD-ELSEVIER SCIENCE LTD	LONDON	125 LONDON WALL, LONDON EC2Y 5AS, ENGLAND	2468-5178		978-0-12-811550-3; 978-0-12-811549-7	STRATIGR TIMESCALE			2016	1						325	392		10.1016/bs.sats.2016.10.001	http://dx.doi.org/10.1016/bs.sats.2016.10.001			68	Geology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Paleontology	BI6LG					2025-03-11	WOS:000413437000006
J	Machalski, M; Vellekoop, J; Dubicka, Z; Peryt, D; Harasimiuk, M				Machalski, Marcin; Vellekoop, Johan; Dubicka, Zofia; Peryt, Danuta; Harasimiuk, Marian			Late Maastrichtian cephalopods, dinoflagellate cysts and foraminifera from the Cretaceous-Paleogene succession at Lechowka, southeast Poland: Stratigraphic and environmental implications	CRETACEOUS RESEARCH			English	Article						Ammonites; Nautilids; Dinocysts; Foraminifera; K-Pg boundary; Central Europe	SEA-LEVEL CHANGE; ANOXIC EVENT 1B; TERTIARY BOUNDARY; BENTHIC FORAMINIFERA; STEVNS KLINT; CALCAREOUS NANNOFOSSIL; PLANKTIC FORAMINIFERA; AMMONITES; EXTINCTION; END	The Lechowka section comprises the most complete Cretaceous Paleogene (K-Pg) boundary succession in Poland and is among 29 sites worldwide with the youngest ammonite record. Here, cephalopods (ammonites and nautilids), organic-walled dinoflagellates (dinocysts) and foraminifera from the uppermost Maastrichtian interval are studied. In terms of ammonite biostratigraphy, the upper Maastrichtian Hoploscaphites constrictus crassus Zone is documented up to a level 120 cm below the K-Pg boundary. There is no direct, ammonite-based evidence of the highest Maastrichtian H. constrictus johnjagti Zone. However, the predominance of the dinocyst marker taxon Palynodinium grallator suggests the presence of the equivalent of the uppermost Maastrichtian Thalassiphora pelagica Subzone, which is correlatable with the H. c. johnjagti ammonite Zone. The planktonic foraminiferal assemblage is coeval with that from the H. c. johnjagti Zone as well. These data indicate that the top of the Maastrichtian at Lechowka is complete within the limits of biostratigraphic resolution, albeit slightly condensed. The dinocyst and foraminiferal assemblages are dominated by taxa that are characteristic of high-energy, marginal marine environments. A reduction in test size among the calcareous epifaunal benthic foraminifera is observed at a level 50 cm below the K-Pg boundary, which is possibly related to environmental stress associated with Deccan volcanism. (C) 2015 Elsevier Ltd. All rights reserved.	[Machalski, Marcin; Peryt, Danuta] Inst Paleobiol PAN, PL-00818 Warsaw, Poland; [Vellekoop, Johan] Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Palaeoceanog,Lab Palaeobotany &, NL-3584 CD Utrecht, Netherlands; [Dubicka, Zofia] Univ Warsaw, Fac Geol, PL-02089 Warsaw, Poland; [Harasimiuk, Marian] Marie Curie Sklodowska Univ, Fac Earth Sci & Spatial Management, PL-20718 Lublin, Poland	Polish Academy of Sciences; Institute of Paleobiology of the Polish Academy of Sciences; Utrecht University; University of Warsaw; Maria Curie-Sklodowska University	Machalski, M (通讯作者)，Inst Paleobiol PAN, Ul Twarda 51-55, PL-00818 Warsaw, Poland.	mach@twarda.pan.pl	Vellekoop, Johan/L-1805-2019; Dubicka, Zofia/ABB-3388-2020; Vellekoop, Johan/F-6466-2017; Peryt, Danuta/F-9988-2019; Machalski, Marcin/AAX-1074-2020	Harasimiuk, Marian/0000-0003-1260-7881; Dubicka, Zofia/0000-0003-1105-4111; Vellekoop, Johan/0000-0001-6977-693X; Peryt, Danuta/0000-0002-5821-1084; Machalski, Marcin/0000-0002-1121-4093	Netherlands Organization for Scientific Research (NWOopen competition grant) [ALWPJ/09047]	Netherlands Organization for Scientific Research (NWOopen competition grant)	Michai Andziak, Waldemar Jezierski, Adam Zaremba and Zbigniew Lis are acknowledged for assistance during fieldwork at Lechowka. Norbert Keutgen is thanked for help in complementing nautilid literature and Neil Landman for providing a photograph of the artificial wax mould of Recent Nautilus. Grzegorz Racki is acknowledged for inspiring discussions on the Lechowka section and K-Pg extinctions. Neil Landman and two anonymous, reviewers are thanked for their reviews of the earlier versions of this paper. John W.M. Jagt is thanked for linguistic correction of the final version of this text. Funding for this research to JV was provided by the Netherlands Organization for Scientific Research (NWO open competition grant ALWPJ/09047).	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Res.	JAN	2016	57						208	227		10.1016/j.cretres.2015.08.012	http://dx.doi.org/10.1016/j.cretres.2015.08.012			20	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	CW5SA		Green Published			2025-03-11	WOS:000365055700018
J	Guilbaud, J; Massé, A; Wolff, FC; Jaouen, P				Guilbaud, Julie; Masse, Anthony; Wolff, Francois-Charles; Jaouen, Pascal			Porous membranes for ballast water treatment from microalgae-rich seawater	MARINE POLLUTION BULLETIN			English	Article						Ship; Ballast water; Alga; Membrane; Microfiltration; Techno-economic	UF PRETREATMENT PRIOR; REVERSE-OSMOSIS; ULTRAFILTRATION MEMBRANE; DINOFLAGELLATE CYSTS; SWRO-DESALINATION; RO MEMBRANES; FILTRATION; TEMPERATURE	The ballast waters from ships pose a major threat to oceans, notably because of the spread of microorganisms. The present study evaluates the techno-economic feasibility of implementing the membrane process to remove microalgae from seawater to be ballasted in a single step during planktonic bloom. The optimal conditions for the microfiltration of complex and reproducible synthetic seawater are a permeate flux and specific filtered volume of 100 L.h(-1).m(-2) and 75 L.m(-2).cycle(-1), respectively. Recovery of the membrane process represents about 76.6% and 62.7% of the annual cost for a cruise ship (5400 passengers) and liquefied natural gas (LNG) carrier (75,000 m(3) of liquid natural gas), followed by the membrane replacement cost (13.4% and 21.9%, respectively). The treatment costs are competitive with conventional treatments, even when the membrane process is more feasible for cruise ships due to its smaller capital cost and footprint. (C) 2015 Elsevier Ltd. All rights reserved.	[Guilbaud, Julie; Masse, Anthony; Jaouen, Pascal] Univ Nantes, LUNAM, GEPEA, CNRS,UMR 6144, F-44602 St Nazaire, France; [Wolff, Francois-Charles] Univ Nantes, LUNAM, LEMNA, EA 4272, F-44322 Nantes 3, France	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute for Engineering & Systems Sciences (INSIS); Nantes Universite; Nantes Universite	Massé, A (通讯作者)，Univ Nantes, LUNAM, GEPEA, CNRS,UMR 6144, 37 Bd Univ,BP 406, F-44602 St Nazaire, France.	anthony.masse@univ-nantes.fr	anthony, masse/JVM-9157-2024					AFNOR, 2000, 872 AFNOR NF EN; AFNOR, 1997, 1484 AFNOR NF EN; AFNOR, 1999, 90117 AFNOR NFT; Aminot A., 2004, METHODES ANAL MILIEU; [Anonymous], 2007, FILTR SEPARAT, V44, P36; Bacchin P, 2006, J MEMBRANE SCI, V281, P42, DOI 10.1016/j.memsci.2006.04.014; Bessiere Y, 2005, J MEMBRANE SCI, V264, P37, DOI 10.1016/j.memsci.2005.04.018; Bolch CJS, 2007, HARMFUL ALGAE, V6, P465, DOI 10.1016/j.hal.2006.12.008; Brehant A, 2002, DESALINATION, V144, P353, DOI 10.1016/S0011-9164(02)00343-0; Bu-Rashid KA, 2007, DESALINATION, V203, P229, DOI 10.1016/j.desal.2006.04.010; Casana A., 2012, INT C DES SUST EDS C; Castaing JB, 2010, DESALINATION, V253, P71, DOI 10.1016/j.desal.2009.11.031; Castaing J.B., 2011, THESIS; Cheryan M., 1998, ULTRAFILTRATION MICR, DOI 10.1201/9781482278743; Denis C, 2009, SEP PURIF TECHNOL, V69, P37, DOI 10.1016/j.seppur.2009.06.017; Doblin MA, 2006, MAR POLLUT BULL, V52, P259, DOI 10.1016/j.marpolbul.2005.12.014; Dobroski N., 2007, ASSESSMENT EFFICACY; Gille D, 2005, DESALINATION, V182, P301, DOI 10.1016/j.desal.2005.03.020; Glucina K, 1998, DESALINATION, V118, P205, DOI 10.1016/S0011-9164(98)00131-3; Gollasch S., 2002, Ballast water management in the North-East Atlantic: Report to aid decision making on ballast water in OSPAR BDC; Gollasch S, 2007, HARMFUL ALGAE, V6, P585, DOI 10.1016/j.hal.2006.12.009; Gregg MD, 2007, HARMFUL ALGAE, V6, P567, DOI 10.1016/j.hal.2006.08.009; Guilbaud J, 2013, DESALIN WATER TREAT, V51, P416, DOI 10.1080/19443994.2012.714890; Guillard R. 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Pollut. Bull.	DEC 30	2015	101	2					612	617		10.1016/j.marpolbul.2015.10.044	http://dx.doi.org/10.1016/j.marpolbul.2015.10.044			6	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	CZ4XY	26517940				2025-03-11	WOS:000367107600018
J	Limoges, A; de Vernal, A; Ruiz-Fernández, AC				Limoges, Audrey; de Vernal, Anne; Ruiz-Fernandez, Ana-Carolina			Investigating the impact of land use and the potential for harmful algal blooms in a tropical lagoon of the Gulf of Mexico	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Sediment samples; Dinocysts; Algal bloom; Deforestation; Southwestern Gulf of Mexico; Lagoon	DINOFLAGELLATE CYSTS; PYRODINIUM-BAHAMENSE; POPULATION-DYNAMICS; SOUTHWESTERN GULF; ALVARADO LAGOON; 1ST REPORT; LONG-TERM; RED TIDE; SEDIMENTS; VARIABILITY	Palynological and geochemical analyses were carried out on a sediment core collected in the shallow Alvarado lagoon (Veracruz, Southwestern Gulf of Mexico) in order to evaluate the impact of the significant decline in the surrounding native coastal vegetation on phytoplankton assemblages. The sedimentary sequence encompasses the last millennium and provides information on pre-industrial phytoplankton assemblages. Results highlight a recent increase of freshwater-sourced organic matter relative to marine organic matter in line with reduced total concentrations of cyst-producing dinoflagellates. These changes appear to be synchronous to the extensive conversion of wetlands into agricultural areas, with consequences on the stability and water retention capacity of the soils bordering the lagoon system. The data also show that Polysphaeridium zoharyi, a cyst produced by the potentially toxic dinoflagellate Pyrodinium bahamense, is present in high abundance in the dinoflagellate population of the lagoon. Consequently, the modern cyst bank of P. bahamense in sediment has the potential to initiate harmful blooms since surface sediments are prone to resuspension events related to strong seasonal winds and human activities. (c) 2015 Elsevier Ltd. All rights reserved.	[Limoges, Audrey; de Vernal, Anne] Univ Quebec, Geotop, Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada; [Ruiz-Fernandez, Ana-Carolina] Univ Nacl Autonoma Mexico, Unidad Acad Mazatlan, Inst Ciencias Mar & Limnol, Mazatlan 82000, Mexico	University of Quebec; University of Quebec Montreal; Universidad Nacional Autonoma de Mexico	Limoges, A (通讯作者)，Univ Quebec, Geotop, Succ Ctr Ville, CP 8888, Montreal, PQ H3C 3P8, Canada.	limoges.audrey@courrier.uqam.ca; devernal.anne@uqam.ca; caro@ola.icmyl.unam.mx	de Vernal, Anne/D-5602-2013; Ruiz-Fernández, Ana Carolina/ABG-6985-2020	Limoges, Audrey/0000-0002-4587-3417; RUIZ-FERNANDEZ, ANA CAROLINA/0000-0002-2515-1249	Fonds de Recherche Nature et Technologies of Quebec; Mexico-Quebec [CONA CYT-00005-2013-01/0196813]	Fonds de Recherche Nature et Technologies of Quebec; Mexico-Quebec	This study was possible through the financial support of Fonds de Recherche Nature et Technologies of Quebec, and the bilateral project Mexico-Quebec CONA CYT-00005-2013-01/0196813. We would like to thank Yves Gelinas, Marianne Ellegaard, Claude Hillaire-Marcel and Nicolas Van Nieuwenhove for helpful comments. We also want to thank Francis Kercichof and Michael A. Poirrier for providing details about the preferred habitat of Rangia sp.	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J	Salgado, P; Vázquez, JA; Riobó, P; Franco, JM; Figueroa, RI; Kremp, A; Bravo, I				Salgado, Pablo; Vazquez, Jose A.; Riobo, Pilar; Franco, Jose M.; Figueroa, Rosa I.; Kremp, Anke; Bravo, Isabel			A Kinetic and Factorial Approach to Study the Effects of Temperature and Salinity on Growth and Toxin Production by the Dinoflagellate <i>Alexandrium ostenfeldii</i> from the Baltic Sea	PLOS ONE			English	Article							PARALYTIC SHELLFISH TOXINS; LACTIC-ACID BACTERIA; GENUS ALEXANDRIUM; SACCHAROMYCES-CEREVISIAE; SPIROLIDE PRODUCTION; PERUVIANUM BALECH; MENDIOLA BALECH; CYST FORMATION; DINOPHYCEAE; BLOOM	Alexandrium ostenfeldii is present in a wide variety of environments in coastal areas worldwide and is the only dinoflagellate known species that produces paralytic shellfish poisoning (PSP) toxins and two types of cyclic imines, spirolides (SPXs) and gymnodimines (GYMs). The increasing frequency of A. ostenfeldii blooms in the Baltic Sea has been attributed to the warming water in this region. To learn more about the optimal environmental conditions favoring the proliferation of A. ostenfeldii and its complex toxicity, the effects of temperature and salinity on the kinetics of both the growth and the net toxin production of this species were examined using a factorial design and a response-surface analysis (RSA). The results showed that the growth of Baltic A. ostenfeldii occurs over a wide range of temperatures and salinities (12.5-25.5 degrees C and 5-21, respectively), with optimal growth conditions achieved at a temperature of 25.5 degrees C and a salinity of 11.2. Together with the finding that a salinity > 21 was the only growth-limiting factor detected for this strain, this study provides important insights into the autecology and population distribution of this species in the Baltic Sea. The presence of PSP toxins, including gonyautoxin (GTX)-3, GTX-2, and saxitoxin (STX), and GYMs (GYM-A and GYM-B/-C analogues) was detected under all temperature and salinity conditions tested and in the majority of the cases was concomitant with both the exponential growth and stationary phases of the dinoflagellate's growth cycle. Toxin concentrations were maximal at temperatures and salinities of 20.9 degrees C and 17 for the GYM-A analogue and > 19 degrees C and 15 for PSP toxins, respectively. The ecological implications of the optimal conditions for growth and toxin production of A. ostenfeldii in the Baltic Sea are discussed.	[Salgado, Pablo] Inst Fomento Pesquero IFOP, Dept Medio Ambiente, Div Invest Acuicultura, Punta Arenas, Chile; [Vazquez, Jose A.] CSIC, IIM, Grp Reciclado & Valorizac Mat Residuales REVAL, Vigo, Spain; [Riobo, Pilar; Franco, Jose M.] CSIC, IIM, Vigo, Spain; [Salgado, Pablo; Figueroa, Rosa I.; Bravo, Isabel] Ctr Oceanog Vigo, IEO, Vigo, Spain; [Kremp, Anke] Finnish Environm Inst SYKE, Ctr Marine Res, Helsinki, Finland	Instituto de Fomento Pesquero (Valparaiso); Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Spanish Institute of Oceanography; Finnish Environment Institute	Salgado, P (通讯作者)，Inst Fomento Pesquero IFOP, Dept Medio Ambiente, Div Invest Acuicultura, Punta Arenas, Chile.	pablo.salgado@ifop.cl	Bravo, Isabel/D-3147-2012; Salgado, Pablo/KMA-0636-2024; Vazquez Alvarez, Jose Antonio/K-5938-2014; Figueroa, Rosa/M-7598-2015; Riobo, Pilar/K-1945-2017	Vazquez Alvarez, Jose Antonio/0000-0002-1122-4726; Figueroa, Rosa/0000-0001-9944-7993; Bravo, Isabel/0000-0003-3764-745X; Salgado, Pablo/0000-0002-4168-3675; Riobo, Pilar/0000-0002-1921-6229	CCVIEO project; Ministry of Economy and Competitiveness [CICAN-2013-40671-R]	CCVIEO project; Ministry of Economy and Competitiveness	This work is a contribution of the Unidad Asociada "Microalgas Nocivas" (CSIC-IEO) and was financially supported by the CCVIEO project and CICAN-2013-40671-R (Ministry of Economy and Competitiveness). P. Salgado is a researcher at IFOP, which has provided financial support for his doctoral stay.	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J	Uddandam, P; Prasad, V; Rai, J; Joshi, H				Uddandam, Premraj; Prasad, Vandana; Rai, Jyotsana; Joshi, Hema			A STUDY OF THE DISTRIBUTION PATTERN OF DINOFLAGELLATE CYSTS FROM THE BAY OF BENGAL	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Dinoflagellates; Organic-walled dinoflagellate cysts; Gonyaulacoid; Protoperidinioids; and western Bay of Bengal	SEA-SURFACE CONDITIONS; BIOLOGICAL PRODUCTIVITY; ARABIAN SEA; SEDIMENTS; QUATERNARY; ASSEMBLAGES; ATLANTIC; HOLOCENE; NORTH; SALINITY	Dinoflagellates are one of the major phytoplankton groups of the marine system. The onshore-offshore trends exhibited by dinoflagellate cysts are important criteria to decipher palaoenvironmental and palaeo-oceanographic changes. Several studies have been carried out on the organic-walled dinoflagellate cyst distribution pattern in surface sediments of various marine regions of mid-high latitudes with very few studies from the tropical oceans. In the present study, dinoflagellate cyst distribution pattern was studied in proximal-distal transect of the western Bay of Bengal at a water depth of 25m to 2500m. Distribution of different species of protoperidinioid and gonyaulacoid dinoflagellate cysts were studied. Four major types of dinoflagellate cyst associations, which are characteristic of inner neritic (Inner shelf), outer neritic (outer shelf), slope and oceanic zones, have been recognized. With the exception of gonyaulacoid dinoflagellate cyst Bitectatodinium spongium, coastal inner and outer neritic regions of the Bay of Bengal are dominated by protoperidinioid dinoflagellate cysts (heterotrophic forms). The oceanic assemblages are characterized by a low diversity of gonyalaucoid dinoflagellate cysts (autotrophic forms) represented by Spiniferites species. The heterotrophic dinoflagellate cyst species, predominant in the inner, outer and slope regions, show considerable variation in the species composition in coastal to distal region of the Bay of Bengal. Diversity and abundance of protoperidinioid dinoflagellate cysts point to a high-nutrient loading and eutrophic environmental conditions of marine waters stretching as far as the slope regions of the Bay of Bengal. Based on the present study, it is deciphered that high nutrient supply and salinity fluctuations due to river runoff activity determine the distribution pattern of dinoflagellate cyst in coastal to distal parts of the Bay of Bengal.	[Uddandam, Premraj; Prasad, Vandana; Rai, Jyotsana] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India; [Joshi, Hema] Kumaun Univ, Dept Bot, Almora, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Kumaun University	Prasad, V (通讯作者)，Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India.	premrajuddandam@gmail.com; prasadvan@gmail.com			Ministry of Earth Science (MoES), India [SIBER/NIO/RN/11]	Ministry of Earth Science (MoES), India	We are thankful to the Director, Birbal Sahni Institute of Palaeobotany (BSIP), India for providing facilities. This study is carried out as a part of Ministry of Earth Science (MoES), India funded project SIBER/NIO/RN/11 entitled "High resolution palaeoclimatic studies from the bay of Bengal". Authors thanks. Dr. Rajiv Nigam and Dr. Rajeev Saraswat for valuable suggestions and the excellent support during sample collection. Present publication bears BSIP permission number 85/2014-2015.	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Palaeontol. Soc. India	DEC	2015	60	2					11	19						9	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DB0PG					2025-03-11	WOS:000368209400002
J	Thakur, B; Srivastava, J; Uddandam, P; Manoj, M; Prasad, V				Thakur, Biswajeet; Srivastava, Jyoti; Uddandam, Premraj; Manoj, Mc; Prasad, Vandana			ROLE OF SEDIMENTARY PROCESSES AND ENVIRONMENTAL FACTORS IN DETERMINING THE DISTRIBUTION PATTERN OF DIATOMS AND MARINE/TERRESTRIAL PALYNOMORPHS IN A TROPICAL COASTAL WETLAND	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Vembanad wetland; Pollen; Diatoms; Palynofacies; Dinoflagellate cysts; Depositional environment	DINOFLAGELLATE CYST DISTRIBUTION; COCHIN BACKWATER; VEMBANAD LAKE; WEST-COAST; INDIA; RECONSTRUCTION; CARBONATE; IGNITION; ESTUARY; SEA	Factors controlling the distribution of marine and terrestrial palynomorphs in a coastal ecosystem were studied from surface sediments of 17 stations of Vembanad wetland, Kerala. Marine and terrestrial organic matter, mangrove and terrestrial pollen, dinoflagellate cysts, diatoms, Total organic carbon, percentage of sand, silt and clay, total dissolved solids and salinity were recorded in the sediment samples from each station. Based on the study, three depositional zones were identified in the Vembanad wetland i) flood tidal basin, ii) Central tidal basin, and iii) fluvial basin. The constant composition of terrestrial and mangrove pollen in the 8 stations of the northern Vembanad ecosystem from Munambaom-Barmouth points to tidal influence. Low percentage of dinocysts and pollen but high percentage of diatoms in Munambaom, Cherai beach, and Midway to Cherai stations of the central part of Vembanad is probably due to prevalence of high energy and an oxidizing environment of deposition. Abundance of terrestrial pollen as well as fresh water diatoms, but extremely low representatives of marine dinocyst in the southern stations Kochi Shipyard-Kumarakaom indicate high fluvial supply and proximal setting with respect to the terrestrial source. This study helped to elucidate the role of different factors, i.e. proximal-distal trend, tidal flushing, hydrodynamic conditions, climate and redox state of the depositional environment in determining the distribution of marine and terrestrial palynomorphs in a coastal environment.	[Thakur, Biswajeet; Srivastava, Jyoti; Uddandam, Premraj; Manoj, Mc; Prasad, Vandana] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Prasad, V (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	prasad.van@gmail.com	Srivastava, Jyoti/AAB-1612-2020; Manoj, M/AAR-1882-2020	Manoj, M C/0000-0001-8112-6315; Srivastava, Jyoti/0000-0002-5264-7995				Abdulla Bava K., 1996, THESIS; Anirudhan T. S., 1988, THESIS; [Anonymous], DEV PALEOENVIRONMENT; [Anonymous], ENV SCI TECHNOLOGY; [Anonymous], 2010, The Diatoms: Applications for the Environmental and Earth Sciences, DOI DOI 10.1017/CBO9780511763175; Ansari Z. A., 1974, MAHASAGAR, V7, P3; Balachandran K. 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J	Sachsenhofer, RF; Hentschke, J; Bechtel, A; Coric, S; Gratzer, R; Gross, D; Horsfield, B; Rachetti, A; Soliman, A				Sachsenhofer, R. F.; Hentschke, J.; Bechtel, A.; Coric, S.; Gratzer, R.; Gross, D.; Horsfield, B.; Rachetti, A.; Soliman, A.			Hydrocarbon potential and depositional environments. of Oligo-Miocene rocks in the Eastern Carpathians (Vrancea Nappe, Romania)	MARINE AND PETROLEUM GEOLOGY			English	Article						Oligocene; Dysodile; Menilite; Paratethys; Source rock; Organic geochemistry; Palynofacies	ALPINE FORELAND BASIN; OLIGOCENE DINOFLAGELLATE CYSTS; FLYSCH CARPATHIANS; MENILITE FORMATION; MOLDAVIDIAN BASIN; PETROLEUM SYSTEMS; ORGANIC-MATTER; MOLASSE BASIN; BLACK SHALES; SEDIMENTS	The Oligocene to early Miocene fine-grained succession in the Eastern Carpathians includes, from base to top the Lower Menilite (LMM), Bituminous Marl (BMM), Lower Dysodilic Shale (LDSM), and Upper Dysodilic Shale (UDSM) members. These stratigraphic units, constituting the main hydrocarbon source rocks in the Eastern Carpathians, have been studied in an outcrop section to determine its depositional environment and hydrocarbon potential. The LMM contains high amounts of TOC, but because of low thickness its source potential is limited. The organic matter of the overlying BMM is mainly derived from autochthonous marine organisms including bacterial biomass. TOC contents are moderate because of dilution by carbonate minerals. Calcareous nannoplankton dates the BMM into nannoplankton zones NP21-22. Salinity and redox conditions varied from reduced to slightly enhanced and from strictly anoxic to dysoxic. The LDSM contains carbonate-free black shale and sandstone beds deposited in a depositional lobe under anoxic conditions. Despite of high HI values, land plants form a significant part of the organic matter. Channel fill sediments form the top of the LDSM. The lower part of the early Miocene UDSM accumulated in a lobe, whereas its upper part represents a basin plain setting. MITC ratios reflect a trend from slightly enhanced to slightly decreased normal marine salinity. The presence of aryl-isoprenoids suggests a temporary photic zone anoxia controlled by salinity variations. Both marine and terrestrial biomass contributed to the organic matter. A major change towards oxic conditions occurred at the boundary between the UDSM and the overlying Gura Soimului Formation. The studied succession can generate 6 t of hydrocarbons per square meter. All members are oil prone, but yield oil with different biomarker characteristics. This allows the identification of oil generated from different lithostratigraphic units. (C) 2015 Elsevier Ltd. All rights reserved.	[Sachsenhofer, R. F.; Hentschke, J.; Bechtel, A.; Gratzer, R.; Gross, D.] Univ Leoben, Dept Appl Geosci & Geophys, A-8700 Leoben, Austria; [Coric, S.] Geol Survey Austria, A-1030 Vienna, Austria; [Horsfield, B.] Geoforschungszentrum Potsdam, Sect 4 3, D-14473 Potsdam, Germany; [Rachetti, A.] Univ Leoben, Dept Gen & Analyt Chem, A-8700 Leoben, Austria; [Soliman, A.] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt	University of Leoben; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; University of Leoben; Egyptian Knowledge Bank (EKB); Tanta University	Sachsenhofer, RF (通讯作者)，Univ Leoben, Dept Appl Geosci & Geophys, Peter Tunner Str 5, A-8700 Leoben, Austria.	reinhard.sachsenhofer@unileoben.ac.at	Bechtel, Achim/A-9885-2011; Soliman, Ali/R-1583-2018; Sachsenhofer, Reinhard/KFA-6113-2024	Bechtel, Achim/0000-0002-3937-8209; Gross, Doris/0000-0001-7442-5093; Sachsenhofer, Reinhard/0000-0002-6616-5583; Soliman, Ali/0000-0001-7366-4607				Algeo TJ, 2004, CHEM GEOL, V206, P289, DOI 10.1016/j.chemgeo.2003.12.009; Amadori ML, 2012, INT J EARTH SCI, V101, P1599, DOI 10.1007/s00531-011-0744-1; Batten DJ, 2005, T GEOBIOL, V23, P203; Bechtel A, 2012, MAR PETROL GEOL, V35, P55, DOI 10.1016/j.marpetgeo.2012.02.017; Bechtel A, 2014, ORG GEOCHEM, V71, P43, DOI 10.1016/j.orggeochem.2014.04.005; Bechtel A, 2013, ORG GEOCHEM, V62, P74, DOI 10.1016/j.orggeochem.2013.07.008; Belayouni H, 2009, INT J EARTH SCI, V98, P157, DOI 10.1007/s00531-007-0226-7; BERNER RA, 1984, GEOCHIM COSMOCHIM AC, V48, P605, DOI 10.1016/0016-7037(84)90089-9; BRAY EE, 1961, GEOCHIM COSMOCHIM AC, V22, P2, DOI 10.1016/0016-7037(61)90069-2; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brinkhuis H., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P219; Calvert SE, 1996, ECON GEOL BULL SOC, V91, P36, DOI 10.2113/gsecongeo.91.1.36; Curtis JB, 2004, ORG GEOCHEM, V35, P1573, DOI 10.1016/j.orggeochem.2004.06.018; DAMSTE JSS, 1989, ORG GEOCHEM, V14, P555; DAMSTE JSS, 1987, GEOCHIM COSMOCHIM AC, V51, P2393, DOI 10.1016/0016-7037(87)90292-4; DEAN WE, 1989, AM J SCI, V289, P708, DOI 10.2475/ajs.289.6.708; Demaison G, 1994, AAPG MEMOIR, V60, P73; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; DIDYK BM, 1978, NATURE, V272, P216, DOI 10.1038/272216a0; EGLINTON TI, 1990, ACS SYM SER, V429, P529; Fensome R.A., 2008, DINOFLAJ2, Version 1; Francu J., 2010, AAPG M 18 OCT 2010 K; FU J, 1986, ORG GEOCHEM, V10, P119; Gheta N., 1986, DARI SEAME I GEOLOGI, P289; GOOSSENS H, 1984, NATURE, V312, P440, DOI 10.1038/312440a0; Gratzer R, 2011, MAR PETROL GEOL, V28, P1171, DOI 10.1016/j.marpetgeo.2011.03.001; Grossi V, 2004, PHYTOCHEMISTRY, V65, P3049, DOI 10.1016/j.phytochem.2004.09.002; Guerrera F, 2012, GEOL CARPATH, V63, P463, DOI 10.2478/v10096-012-0036-0; Hofmann P, 2000, PALAEOGEOGR PALAEOCL, V163, P97, DOI 10.1016/S0031-0182(00)00147-4; HORSFIELD B, 1989, GEOCHIM COSMOCHIM AC, V53, P891, DOI 10.1016/0016-7037(89)90033-1; Horsfield B., 1997, The bulk composition of first-formed petroleum in source rocks, P335, DOI 10.1007/978-3-642-60423-27; Köster J, 1998, ORG GEOCHEM, V29, P543, DOI 10.1016/S0146-6380(98)00059-X; Köster J, 1998, ORG GEOCHEM, V29, P649, DOI 10.1016/S0146-6380(98)00182-X; Kotarba MJ, 2007, ORG GEOCHEM, V38, P1431, DOI 10.1016/j.orggeochem.2007.03.012; Kotarba M.J., 2006, AAPG Memoir, V84, P395, DOI DOI 10.1306/985614M843074; Lafargue E, 1998, REV I FR PETROL, V53, P421, DOI 10.2516/ogst:1998036; LANGFORD FF, 1990, AAPG BULL, V74, P799; Lebenzon C., 1973, DARI SEAMA ALE I GEO, VLIX/4, P101; Lüning S, 2003, J PETROL GEOL, V26, P153, DOI 10.1111/j.1747-5457.2003.tb00023.x; Mackenzie A.S., 1984, ADV PETROLEUM GEOCHE, V1, P115, DOI DOI 10.1016/B978-0-12-032001-1.50008-0; Matenco L, 2000, TECTONOPHYSICS, V316, P255, DOI 10.1016/S0040-1951(99)00261-9; Melinte MC, 2005, STUD GEOL POLON, V124, P341; Melinte-Dobrinescu M.C., 2008, Acta Palaeontol. 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DEC	2015	68		A				269	290		10.1016/j.marpetgeo.2015.08.034	http://dx.doi.org/10.1016/j.marpetgeo.2015.08.034			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DA4GE					2025-03-11	WOS:000367757300017
J	Kretschmann, J; Filipowicz, NH; Owsianny, PM; Zinssmeister, C; Gottschling, M				Kretschmann, Juliane; Filipowicz, Natalia H.; Owsianny, Pawel M.; Zinssmeister, Carmen; Gottschling, Marc			Taxonomic Clarification of the Unusual Dinophyte <i>Gymnodinium</i> <i>limneticum</i> WOlOSZ. (Gymnodiniaceae) from the Tatra Mountains	PROTIST			English	Article						Cyst; dinoflagellate; epitype; morphology; phylogeny; taxonomy	FRESH-WATER DINOFLAGELLATE; WESTERN KOREA MORPHOLOGY; GEN. NOV DINOPHYCEAE; RDNA-BASED PHYLOGENY; COMB. NOV; SPINIFERODINIUM-GALEIFORME; MOLECULAR CHARACTERIZATION; SCRIPPSIELLA-TROCHOIDEA; ELECTRON-MICROSCOPY; SPECIES BOUNDARIES	The Gymnodiniaceae -even in a strict sense-comprise a vast diversity of dinophytes regarding morphology and ecology. Taxonomy and nomenclature of their constituent species remain problematic, although crucial to fully explore the biology of the group. Here, we present the rarely documented dinophyte Gymnodinium limneticum from its type locality at Lake Morskie Oko in Poland, for which we established strains and made extensive morphological studies. The species was unusual in exhibiting capsoid cells as predominant life-history stage, which were embedded and dividing in extensive mucilage leading to an enkaptic pseudocolonial system. We also generated ribosomal RNA sequences that were included in a comprehensive molecular phylogeny. Our species was clearly identified as a member of the Gymnodiniaceae s.str. but within the lineage, it was only distantly related to the type species of Gymnodinium, G. fuscum. Rather, it constituted a monophyletic group together with species assigned to Spiniferodinium and as a nomenclatural result, we propose two new combinations (i.e., Sp. limneticum comb. nov., Sp. palustre comb. nov.). As Spiniferodinium now includes dinophyte species inhabiting marine or freshwater environments as well, our investigations may provide evidence for an evolutionary scenario with corresponding transitions being more frequent than considered before. (C) 2015 Elsevier GmbH. All rights reserved.	[Kretschmann, Juliane; Gottschling, Marc] Univ Munich, GeoBioctr, Dept Biol Systemat Bot & Mykol, D-80638 Munich, Germany; [Filipowicz, Natalia H.] Med Univ Gdansk, Dept Biol & Pharmaceut Bot, PL-80416 Gdansk, Poland; [Owsianny, Pawel M.] Adam Mickiewicz Univ, Fac Geog & Geol Sci, Inst Geoecol & Geoinformat, PL-61680 Poznan, Poland; [Owsianny, Pawel M.] Adam Mickiewicz Univ, Didact & Sci Branch Pila, PL-64920 Pila, Poland; [Zinssmeister, Carmen] German Ctr Marine Biodivers Res DZMB, Senckenberg Meer, D-26382 Wilhelmshaven, Germany	University of Munich; Fahrenheit Universities; Medical University Gdansk; Adam Mickiewicz University; Adam Mickiewicz University; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN)	Gottschling, M (通讯作者)，Univ Munich, GeoBioctr, Dept Biol Systemat Bot & Mykol, Menzinger Str 67, D-80638 Munich, Germany.	gottschling@bio.lmu.de	Gottschling, Marc/K-2186-2014; Filipowicz, Natalia/KYO-9817-2024	Owsianny, Pawel Michal/0000-0003-0517-5881	Munchener Universitatsgesellschaft; National Sciences Centre, Poland (NCN) [N N305 273840]	Munchener Universitatsgesellschaft; National Sciences Centre, Poland (NCN)	Field work in the area of the Tatra National Park was done with the permission of the Ministry of Environment of the Republic of Poland (no. DOPpn-4102-995/49867/11/RS), as part of research supported by the National Sciences Centre, Poland (NCN no. N N305 273840). We thank Katharina Puchler (Munich) for assistance in the molecular lab, Malte Elbrachter (List / Sylt) for helpful comments on a previous version of our manuscript, and Werner Greuter (Palermo, Berlin) for providing advice to the taxonomic paragraph. Financial support was provided by the Munchener Universitatsgesellschaft and is gratefully acknowledged here. We are thankful to the jury, which awarded the Lehre@LMU-research prize to the first author's Master thesis. Polish Academy of Learning (Polska Akademia Umiejetnosci, Krakow) is thanked for permission to reproduce drawings from Woloszynska (1935).	Allman GJ, 1855, Q J MICROSC SCI S, Vs1-3, P21; ALLMANN G.J., 1854, Proc. Roy. Irish Acad, V6, P118; [Anonymous], INFUSIONSTHIERCHEN V INFUSIONTHIERCHEN VO; BALVAY G, 1992, ARCH SCI, V45, P135; Bergh R. 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J	Takahashi, K; Moestrup, O; Jordan, RW; Iwataki, M				Takahashi, Kazuya; Moestrup, Ojvind; Jordan, Richard W.; Iwataki, Mitsunori			Two New Freshwater Woloszynskioids <i>Asulcocephalium miricentonis</i> gen. et sp nov and <i>Leiocephalium pseudosanguineum</i> gen. et sp nov (Suessiaceae, Dinophyceae) Lacking an Apical Furrow Apparatus	PROTIST			English	Article						Apical furrow; dinoflagellate; eyespot; Asulcocephalium miricentonis; Leiocephalium pseudosanguineum; Suessiaceae	ELECTRON-MICROSCOPY; COASTAL WATERS; LAKE TOVEL; COMB. NOV; DINOFLAGELLATE; ULTRASTRUCTURE; MORPHOLOGY; PHYLOGENY; CINCTA; LIGHT	Two new woloszynskioid dinoflagellates, Asulcocephalium miricentonis gen. et sp. nov. and Leiocephalium pseudosanguineum gen. et sp. nov., are described from Japanese freshwater ponds on the basis of bright field and fluorescence light microscopy, scanning and transmission electron microscopy, and molecular phylogeny inferred from rDNA sequences. Asulcocephalium miricentonis has a spherical anterior nucleus and chloroplast with a pyrenoid penetrated by the cytoplasm. This species has 9-12 latitudinal series of amphiesmal vesicles (AVs), including an apparently large AV on the right ventral side of the epicone. Leiocephalium pseudosanguineum has a U-shaped nucleus in the epicone and chloroplasts without a pyrenoid. This species has at least 24 latitudinal series of AVs. The characteristic features of both species were brick-like material ( type E) in the eyespot and the lack of an apical furrow. These features coincide with those of Polarella glacialis, but the two species differ in cell shape, number and arrangement of AVs, shape of resting cysts, and habitats; i.e., P. glacialis has been reported only from marine cold waters. Molecular phylogeny revealed that A. miricentonis and L. pseudosanguineum were positioned in the Suessiaceae and closely related to Piscinoodinium sp., but their relationship to Polarella and other reported taxa was not supported. (C) 2015 Elsevier GmbH. All rights reserved.	[Takahashi, Kazuya] Yamagata Univ, Grad Sch Sci & Engn, Yamagata 9908560, Japan; [Moestrup, Ojvind] Univ Copenhagen, Sect Phycol, Inst Biol, DK-2100 Copenhagen K, Denmark; [Jordan, Richard W.] Yamagata Univ, Fac Sci, Yamagata 9908560, Japan; [Iwataki, Mitsunori] Univ Tokyo, Asian Nat Environm Sci Ctr, Bunkyo Ku, Tokyo 1138657, Japan	Yamagata University; University of Copenhagen; Yamagata University; University of Tokyo	Iwataki, M (通讯作者)，Univ Tokyo, Asian Nat Environm Sci Ctr, Bunkyo Ku, 1-1-1 Yayoi, Tokyo 1138657, Japan.	iwataki@anesc.u-tokyo.ac.jp	Iwataki, Mitsunori/H-9640-2019; Takahashi, Kazuya/LCD-6164-2024	Iwataki, Mitsunori/0000-0002-5844-2800; Takahashi, Kazuya/0000-0003-1349-1120; Jordan, Richard/0000-0002-8997-7349	Yamagata University Green Science Network;  [24580258]; Grants-in-Aid for Scientific Research [15H04533, 25304029] Funding Source: KAKEN	Yamagata University Green Science Network; ; 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 appreciate Dr. Shuhei Ota and Ms. Mizuho Sugasawa of the University of Tokyo and Ms. Chihiro Sarai of Yamagata University for their help during sampling in Kenmin-no-mori, Yamagata. 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J	Bouchouicha-Smida, D; Bates, SS; Lundholm, N; Lambert, C; Mabrouk, HH; Hlaili, AS				Bouchouicha-Smida, Donia; Bates, Stephen S.; Lundholm, Nina; Lambert, Christophe; Mabrouk, Hassine Hadj; Hlaili, Asma Sakka			Viability, growth and domoic acid toxicity of the diatom <i>Nitzschia bizertensis</i> following filtration by the mussel <i>Mytilus</i> sp.	MARINE BIOLOGY			English	Article							HARMFUL ALGAL BLOOMS; ALEXANDRIUM-CATENELLA; GUT PASSAGE; DINOFLAGELLATE CYSTS; POPULATIONS; PACIFIC; DINOPHYCEAE; TRANSPORT; SURVIVAL; OYSTERS	The diatom Nitzschia bizertensis was recently discovered in Bizerte Lagoon (Tunisia, SW Mediterranean Sea), where it was shown to produce the amnesic shellfish poisoning toxin, domoic acid (DA). This diatom was previously found to be widespread in both time and space throughout the lagoon. The present study was carried out to test the hypothesis that N. bizertensis is able to survive after being filtered and ejected as biodeposits (faeces plus pseudofaeces) by mussels. N. bizertensis cultures (strains BD4 and BD8), at natural bloom concentrations, were fed to mussels (Mytilus sp.). The stomach contents (after 1 h) and biodeposits (after 48 h) were observed for the presence and viability of N. bizertensis cells. Light microscopy revealed intact and partial cells of N. bizertensis in both the stomach contents and biodeposits of the mussels. Incubation of the biodeposits resulted in the regrowth of N. bizertensis. This provides evidence that transplanted mussels have the potential to serve as vectors for the transport of N. bizertensis. Furthermore, cells regrown from the biodeposits contained DA, but at levels lower than those in pre-filtered cells (up to 11.9 fg cell(-1)). Thus, regrown cells remain toxigenic. The results suggest that one must guard against spreading N. bizertensis and other DA producers via the transfer of shellfish from contaminated to pristine areas.	[Bouchouicha-Smida, Donia; Mabrouk, Hassine Hadj; Hlaili, Asma Sakka] Univ Carthage, Fac Sci Bizerte, Dept Sci Vie, Lab Cytol Vegetale & Phytoplanctonol, Zarzouna 7021, Bizerte, Tunisia; [Bates, Stephen S.] Fisheries & Oceans Canada, Gulf Fisheries Ctr, Moncton, NB E1C 9B6, Canada; [Lundholm, Nina] Univ Copenhagen, Nat Hist Museum Denmark, DK-1307 Copenhagen K, Denmark; [Lambert, Christophe] Inst Univ Europeen Mer, UMR CNRS 6539, Lab Sci Environm Marin, F-29280 Plouzane, France	Universite de Carthage; Fisheries & Oceans Canada; University of Copenhagen; Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM)	Bouchouicha-Smida, D (通讯作者)，Univ Carthage, Fac Sci Bizerte, Dept Sci Vie, Lab Cytol Vegetale & Phytoplanctonol, Zarzouna 7021, Bizerte, Tunisia.	bouchouichadonia15@yahoo.fr	Lundholm, Nina/AAY-6249-2020; HLAILI, Asma/AAD-9610-2019; Lundholm, Nina/A-4856-2013	Lambert, Christophe/0000-0002-5885-467X; Lundholm, Nina/0000-0002-2035-1997				Anderson DM, 2012, ANNU REV MAR SCI, V4, P143, DOI 10.1146/annurev-marine-120308-081121; BARDOUIL M, 1993, J SHELLFISH RES, V12, P417; Barillé L, 2000, DIATOM RES, V15, P11; BATES SS, 1991, CAN J FISH AQUAT SCI, V48, P1136, DOI 10.1139/f91-137; Bouchouicha-Smida D, 2015, ESTUAR COAS IN PRESS; BRICELJ VM, 1993, DEV MAR BIO, V3, P371; Briski E, 2013, LIMNOL OCEANOGR, V58, P1361, DOI 10.4319/lo.2013.58.4.1361; Carriker Melbourne R., 1992, Journal of Shellfish Research, V11, P507; Daguin C, 2001, HEREDITY, V86, P342, DOI 10.1046/j.1365-2540.2001.00832.x; DGPA Direction Generale de la Peche et de l'Aquaculture, 2013, PLAN DIR AQ TUN PROG; Guéguen M, 2008, AQUAT LIVING RESOUR, V21, P21, DOI 10.1051/alr:2008018; Guillard R. 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Biol.	DEC	2015	162	12					2513	2519		10.1007/s00227-015-2758-x	http://dx.doi.org/10.1007/s00227-015-2758-x			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	CX6DE					2025-03-11	WOS:000365790600017
J	Skupien, P; Pavlus, J; Falahatgar, M; Javidan, M				Skupien, Petr; Pavlus, Jan; Falahatgar, Mostafa; Javidan, Mojtaba			Middle Jurassic organic-walled dinoflagellate cysts and palynofacies from Telma-Dareh, south of Sari, northern Iran	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						Northern Iran; Middle Jurassic; Aalenian/Bajocian boundary; Dinoflagellate cyst; Palynofacies	SHEMSHAK GROUP; ALBORZ; PALEOENVIRONMENTS; LITHOSTRATIGRAPHY; BAJOCIAN; FRANCE; BASIN	Analyses of organic-walled dinoflagellates and palynofacies from the marly Unit 3 of the Dalichai Formation in the Telma-Dareh section of the Central Alborz Mountains, northern Iran, have been carried out. Our palynological study has revealed diverse and well-preserved dinoflagellate cyst assemblages, comprising 49 taxa. Based on the first and last appearance datums of dinoflagellate index species, this marly part can be correlated with the northwest European Nannoceratopsis gracilis Biozone of Aalenian to early Bajocian age. Dinoflagellate cyst assemblage data allow the placement of the Aalenian/Bajocian boundary and correlation with the range of the belemnite Brevibelus breviformis. The Aalenian age of the Dalchai Formation at Telma-Dareh contrasts to the Bajocian age attribution by previous authors. Similarities of dinoflagellate cyst assemblages to those from northwest Europe and the northwest Tethys indicate marine connections between the two areas. The palynofacies predominance of land-derived phytoclasts reflects deposition on a proximal oxic shelf with high terrestrial and freshwater influx. Dinoflagellate cyst assemblages that are dominated by representatives of Nannoceratopsis presumably reflect brackish conditions. (C) 2015 Elsevier B.V. All rights reserved.	[Skupien, Petr; Pavlus, Jan] VSB Tech Univ Ostrava, Inst Geol Engn, Ostrava 70833, Czech Republic; [Falahatgar, Mostafa] Payame Noor Univ, Dept Geol, Tehran 3697, Iran; [Javidan, Mojtaba] Islamic Azad Univ, Dept Geol, Shahrood Branch, Shahrood, Iran	Technical University of Ostrava; Payame Noor University; Islamic Azad University	Skupien, P (通讯作者)，VSB Tech Univ Ostrava, Inst Geol Engn, 17 Listopadu 15, Ostrava 70833, Czech Republic.	petr.skupien@vsb.cz; mostafa.mo2@gmail.com	Falahatgar, Mostafa/Q-5753-2018; Skupien, Petr/G-8767-2019	Javidan, Mojtaba/0009-0004-1599-3751; Skupien, Petr/0000-0001-9158-466X; FALAHATGAR, MOSTAFA/0000-0002-6919-1306	Ministry of Education, Youth and Sports of the Czech Republic [SP2014/10]; "Research and Development of Innovations" Operational Programme - Structural Funds of the European Union [CZ.1.05/2.1.00/03.0082]; state budget of the Czech Republic	Ministry of Education, Youth and Sports of the Czech Republic(Ministry of Education, Youth & Sports - Czech Republic); "Research and Development of Innovations" Operational Programme - Structural Funds of the European Union; state budget of the Czech Republic	The research of PS and JP was supported by grant SP2014/10 from the Ministry of Education, Youth and Sports of the Czech Republic. This paper has been written within the framework of the project "Institute of clean technologies of mining and utilisation of raw materials for energy use", registration number CZ.1.05/2.1.00/03.0082, as supported by the "Research and Development of Innovations" Operational Programme, financed by Structural Funds of the European Union and the state budget of the Czech Republic. We wish to thank anonymous reviewers for commenting critically on an earlier type-script. We thank J. W. M. Jagt (Natuurhistorisch Museum Maastricht, Netherlands) for linguistic help.	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Palaeobot. Palynology	DEC	2015	223						128	137		10.1016/j.revpalbo.2015.09.009	http://dx.doi.org/10.1016/j.revpalbo.2015.09.009			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	CW5TY					2025-03-11	WOS:000365060700012
J	Deng, YY; Hu, ZX; Zhan, ZF; Ma, ZP; Tang, YZ				Deng, Yunyan; Hu, Zhangxi; Zhan, Zifeng; Ma, Zhaopeng; Tang, Yingzhong			Differential expressions of an <i>Hsp70</i> gene in the <i>dinoflagellate Akashiwo sanguinea</i> in response to temperature stress and transition of life cycle and its implications	HARMFUL ALGAE			English	Article						Akashiwo sanguinea; Cyst; Dinoflagellate; Harmful algal blooms; Heat shock protein 70 gene (Hsp70); Temperature response	HEAT-SHOCK PROTEINS; ALGAL BLOOMS; HEAT-SHOCK-PROTEIN-70 GENES; MOLECULAR CHAPERONES; TRANSPORT; CLONING; MARINE; GROWTH	The unarmoured dinoflagellate Akashiwo sanguinea is a cosmopolitan species frequently causing harmful algal blooms in temperate to tropical estuaries and marine coasts. While resting cyst production and wide temperature tolerance have been well documented as two adaptive strategies for HAB-forming dinofiagellates, little attention has been paid to the molecular mechanisms, such as the functional genes and their expressions relevant to these ecological processes. Here, the cloning of the gene Hsp70, a gene putatively involved in the process of temperature stress responses, in A. sanguinea and its differential expressions in response to temperature stress and transition of life cycle stages were reported. Based on homologous cloning and the rapid amplification of cDNA ends (RACE), the full-length cDNA sequence (2171 bp) of an Hsp70 gene from A. sanguinea (AsHsp70) was obtained (Accession No. KJ755185), with an open reading frame of 1950 bp. The deduced 649 amino acids (aa) possessed an ATPase domain of 399 aa, a substrate peptide binding domain of 124 aa and a C-terminus domain of 126 aa. The highly conserved motifs of Hsp70 family identified in AsHsp70 suggest conservative function of Hsp70. Real-time quantitative PCR revealed that AsHsp70 expression (20 C-maintained) was dramatically up-regulated by both low (15 degrees C, 10 degrees C, 5 degrees C) and high (25 degrees C, 30 degrees C) temperature shocks. Rapid and significant increase of AsHsp70 expression could be detected within 10 min after exposure to lower temperature stress (10 degrees C). Compared with the stepwise increases or decreases in temperature (+/- 5 degrees C each step), one-step shocks (+/- 10 degrees C) elicited markedly higher AsHsp70 transcripts. In addition, AsHsp70 transcription varied with growth stage and life cycle, peaking in immature cysts undergoing morphogenesis and returning to lower levels in cysts when morphogenesis was completed. The results together strongly suggest that A. sanguinea is more tolerant to gradual than drastic temperature stress and that AsHsp70 may be involved in the adaptation of A. sanguinea to varying temperatures. It is also suggested that Hsp70 might play roles in the encystment of dinoflagellates, which, however, needs more solid evidence for confirmation. (C) 2015 Elsevier B.V. All rights reserved.	[Deng, Yunyan; Hu, Zhangxi; Zhan, Zifeng; Ma, Zhaopeng; Tang, Yingzhong] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Ma, Zhaopeng] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023	Hu, Zhangxi/0000-0002-4742-4973	China Postdoctoral Science Foundation [2014M551969, 2015180754]; NSFC-Shandong Joint Fund [U1406403]; Fund for Creative Research Groups by NSFC [41121064]	China Postdoctoral Science Foundation(China Postdoctoral Science Foundation); NSFC-Shandong Joint Fund; Fund for Creative Research Groups by NSFC	We acknowledge financial support from the Project funded by China Postdoctoral Science Foundation (no. 2014M551969 and no. 2015180754), the NSFC-Shandong Joint Fund (no. U1406403) and the Fund for Creative Research Groups by NSFC (no. 41121064). We are also grateful of Dr. Fred C. 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J	Jauzein, C; Evans, AN; Erdner, DL				Jauzein, Cecile; Evans, Andrew N.; Erdner, Deana L.			The impact of associated bacteria on morphology and physiology of the dinoflagellate <i>Alexandrium tamarense</i>	HARMFUL ALGAE			English	Article						Algal-bacterial interactions; Dinoflagellate; Growth; Photosynthesis; Toxin	GYMNODINIUM-CATENATUM DINOPHYCEAE; TOXIN COMPOSITION VARIATIONS; MICROBIAL COMMUNITY; ALGICIDAL BACTERIA; MARINE-BACTERIA; CYST FORMATION; HIROSHIMA BAY; ALGAL BLOOMS; GROWTH; FUNDYENSE	Despite their potential impact on phytoplankton dynamics and biogeochemical cycles, biological associations between algae and bacteria are still poorly understood. The aim of the present work was to characterize the influence of bacteria on the growth and function of the dinoflagellate Alexandrium tamarense. Axenic microalgal cultures were inoculated with a microbial community and the resulting cultures were monitored over a 15-month period, in order to allow for the establishment of specific algal-bacterial associations. Algal cells maintained in these new mixed cultures first experienced a period of growth inhibition. After several months, algal growth and cell volume increased, and indicators of photosynthetic function also improved. Our results suggest that community assembly processes facilitated the development of mutualistic relationships between A. tamarense cells and bacteria. These interactions had beneficial effects on the alga that may be only partly explained by mixotrophy of A. tamarense cells. The potential role of organic exudates in the establishment of these algal-bacterial associations is discussed. The present results do not support a role for algal-bacterial interactions in dinoflagellate toxin synthesis. However, variations observed in the toxin profile of A. tamarense cells during culture experiments give new clues for the understanding of biosynthetic pathways of saxitoxin, a potent phycotoxin. (C) 2015 Elsevier B.V. All rights reserved.	[Jauzein, Cecile; Erdner, Deana L.] Univ Texas Dallas, Inst Marine Sci, Port Aransas, TX USA; [Evans, Andrew N.] Univ So Mississippi, Dept Coastal Sci, Ocean Springs, MS USA	University of Texas System; University of Texas Dallas; University of Southern Mississippi	Jauzein, C (通讯作者)，Univ Paris 06, Sorbonne Univ, Lab Oceanog Villefranche, INSU CNRS, Villefranche Sur Mer, France.	cjauzein@gmail.com	Erdner, Deana/C-4981-2008	Erdner, Deana/0000-0002-1736-8835; Jauzein, Cecile/0000-0001-6291-6821	National Oceanic and Atmospheric Administration Center for Sponsored Coastal Ocean Research [NA09NOS4780166]; ECOHAB program [8394]	National Oceanic and Atmospheric Administration Center for Sponsored Coastal Ocean Research(National Oceanic Atmospheric Admin (NOAA) - USA); ECOHAB program	We would like to thank Dr. D.M. Anderson and D. Kulis for providing Alexandrium tamarense cultures and for processing toxin samples. This article is a result of research funded by the National Oceanic and Atmospheric Administration Center for Sponsored Coastal Ocean Research under award no. 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J	Gibb, OT; Steinhauer, S; Fréchette, B; de Vernal, A; Hillaire-Marcel, C				Gibb, Olivia T.; Steinhauer, Sarah; Frechette, Bianca; de Vernal, Anne; Hillaire-Marcel, Claude			Diachronous evolution of sea surface conditions in the Labrador Sea and Baffin Bay since the last deglaciation	HOLOCENE			English	Article						Baffin Bay; Davis Strait; dinoflagellate cysts; Labrador Sea; last deglaciation; sea surface conditions	WALLED DINOFLAGELLATE CYSTS; NORTHERN NORTH-ATLANTIC; HOLOCENE CLIMATE-CHANGE; DISKO-BUGT; HUDSON STRAIT; WEST GREENLAND; YOUNGER DRYAS; FRESH-WATER; ICE COVER; CANADIAN ARCHIPELAGO	Assessing changes in sea surface conditions due to the effects of past freshwater outflow through Baffin Bay and Davis Strait to the Labrador Sea, hereafter referred to as the Baffin Bay corridor, is relevant in understanding the variability in Labrador Sea Water (LSW) formation. Here, regional changes in oceanographic circulation and sea surface conditions are reconstructed based on organic-walled dinoflagellate cyst (dinocyst) assemblages from four cores collected from deep, central sites of the Baffin Bay corridor. All cores exhibit a major shift in dinocyst assemblages since the late glacial period. This shift consists of a change from a polar-subpolar heterotrophic species assemblage tolerating cold and near permanent ice-covered conditions, to assemblages characterized by a higher diversity and the occurrence of phototrophic taxa associated with mild conditions. Sea surface reconstructions from the modern analogue technique display a shift from harsh, quasi-perennial ice cover to warmer summer sea surface temperatures and a seasonal sea ice. South of the Davis Strait sill, this regime shift occurred at ca. 11.9 cal ka BP due to the influence of North Atlantic waters. Baffin Bay, however, remained densely sea ice covered until about 7.4 cal ka BP, when these warmer waters penetrated into Baffin Bay and mixed with the West Greenland Current (WGC). This mixing was facilitated by the retreat of the Greenland and Laurentide Ice Sheet (LIS) margins. A major change in Labrador Sea surface conditions occurred nearly at about the same time (similar to 7.6 cal ka BP) when the strong stratification of surface waters weakened because of the reduction in meltwater supplies from the LIS that allowed winter convection and the inception of LSW formation. All these new records demonstrate large amplitude fluctuations in sea surface conditions tightly controlled by the relative strengths and shifts of the warmer WGC and colder Baffin Island Current.	[Gibb, Olivia T.; Steinhauer, Sarah; Frechette, Bianca; de Vernal, Anne; Hillaire-Marcel, Claude] GEOTOP Res Ctr, Montreal, PQ H3C 3P8, Canada		Gibb, OT (通讯作者)，GEOTOP Res Ctr, CP 8888 Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.	oliviagibb@gmail.com	de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/H-1441-2012; Hillaire-Marcel, Claude/C-9153-2013	Hillaire-Marcel, Claude/0000-0002-3733-4632	Ministere du Developpement Economique, Innovation et Exportation (MDEIE); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT); Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Resources Canada (NRCan); Natural Sciences and Engineering Research Council of Canada (NSERC) [HU2008029]	Ministere du Developpement Economique, Innovation et Exportation (MDEIE); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Resources Canada (NRCan)(Natural Resources CanadaCanadian Forest Service); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	Support from the Ministere du Developpement Economique, Innovation et Exportation (MDEIE) and Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT) is acknowledged. Special thanks to the Canadian Foundation for Climate and Atmospheric Sciences (CFCAS), Natural Resources Canada (NRCan), and the Natural Sciences and Engineering Research Council of Canada (NSERC) for their financial support of the HU2008029 expedition in the Labrador Sea.	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Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	CW8NI					2025-03-11	WOS:000365256000003
J	Figueroa, RI; Dapena, C; Bravo, I; Cuadrado, A				Figueroa, Rosa I.; Dapena, Carlos; Bravo, Isabel; Cuadrado, Angeles			The Hidden Sexuality of <i>Alexandrium Minutum</i>: An Example of Overlooked Sex in Dinoflagellates	PLOS ONE			English	Article							LIFE-CYCLES; GONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; CYST FORMATION; CELL-CYCLE; DINOPHYCEAE; DNA; REPRODUCTION; ORGANIZATION; SEGREGATION	Dinoflagellates are haploid eukaryotic microalgae in which rapid proliferation causes dense blooms, with harmful health and economic effects to humans. The proliferation mode is mainly asexual, as the sexual cycle is believed to be rare and restricted to stressful environmental conditions. However, sexuality is key to explaining the recurrence of many dinoflagellate blooms because in many species the fate of the planktonic zygotes (planozygotes) is the formation of resistant cysts in the seabed (encystment). Nevertheless, recent research has shown that individually isolated planozygotes in the lab can enter other routes besides encystment, a behavior of which the relevance has not been explored at the population level. In this study, using imaging flow cytometry, cell sorting, and Fluorescence In Situ Hybridization (FISH), we followed DNA content and nuclear changes in a population of the toxic dinoflagellate Alexandrium minutum that was induced to encystment. Our results first show that planozygotes behave like a population with an "encystment-independent" division cycle, which is light-controlled and follows the same Light: Dark (L:D) pattern as the cycle governing the haploid mitosis. Resting cyst formation was the fate of just a small fraction of the planozygotes formed and was restricted to a period of strongly limited nutrient conditions. The diploid-haploid turnover between L:D cycles was consistent with two-step meiosis. However, the diel and morphological division pattern of the planozygote division also suggests mitosis, which would imply that this species is not haplontic, as previously considered, but biphasic, because individuals could undergo mitotic divisions in both the sexual (diploid) and the asexual (haploid) phases. We also report incomplete genome duplication processes. Our work calls for a reconsideration of the dogma of rare sex in dinoflagellates.	[Figueroa, Rosa I.] Lund Univ, Aquat Ecol, S-22362 Lund, Sweden; [Figueroa, Rosa I.; Dapena, Carlos; Bravo, Isabel] IEO, Vigo 36390, Spain; [Cuadrado, Angeles] Univ Alcala UAH, Dept Biomed & Biotecnol, Alcala De Henares 28801, Spain	Lund University; Spanish Institute of Oceanography; Universidad de Alcala	Figueroa, RI (通讯作者)，Lund Univ, Aquat Ecol, Biol Bldg, S-22362 Lund, Sweden.	rosa.figueroa@biol.lu.se	Bravo, Isabel/D-3147-2012; Cuadrado, Angeles/H-3470-2015; Figueroa, Rosa/M-7598-2015	Bravo, Isabel/0000-0003-3764-745X; Cuadrado, Angeles/0000-0003-0089-5249; Figueroa, Rosa/0000-0001-9944-7993	FORMAS (Sweden) [Formas 215-2010-824]; Spanish National Project CICAN [CGL2013-40671-R]; CCVIEO project	FORMAS (Sweden)(Swedish Research Council Formas); Spanish National Project CICAN; CCVIEO project	The present work was funded by a FORMAS (Sweden) project to RF (Formas 215-2010-824), the Spanish National Project CICAN (CGL2013-40671-R) to IB and RF and the CCVIEO project. The present work was funded by a FORMAS (Sweden) project to RF (Formas 215-2010-824), the Spanish National Project CICAN (CGL2013-40671-R) to IB and RF and the CCVIEO project. We thank Isabel Ramilo for technical support.	ADAMICH M, 1976, PLANTA, V130, P1, DOI 10.1007/BF00390837; Alpermann TJ, 2010, J PHYCOL, V46, P18, DOI 10.1111/j.1529-8817.2009.00767.x; Alverca E, 2007, CYTOGENET GENOME RES, V116, P224, DOI 10.1159/000098191; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Bell G., 1982, The Masterpiece of Nature: The Evolution and Genetics of Sexuality, DOI 10.4324/9780429322884; BHAUD Y, 1988, J CELL SCI, V89, P197; Biecheler B., 1952, Bull. Biol. Fr. 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A., 1972, B SOC BOT FR S1, V1972, P201, DOI DOI 10.1080/00378941.1972.10839089; TaroncherOldenburg G, 1997, LIMNOL OCEANOGR, V42, P1178, DOI 10.4319/lo.1997.42.5_part_2.1178; Tillmann U, 2013, J PHYCOL, V49, P298, DOI 10.1111/jpy.12037; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; Wisecaver JH, 2011, ANNU REV MICROBIOL, V65, P369, DOI 10.1146/annurev-micro-090110-102841	64	42	44	1	35	PUBLIC LIBRARY SCIENCE	SAN FRANCISCO	1160 BATTERY STREET, STE 100, SAN FRANCISCO, CA 94111 USA	1932-6203			PLOS ONE	PLoS One	NOV 23	2015	10	11							e0142667	10.1371/journal.pone.0142667	http://dx.doi.org/10.1371/journal.pone.0142667			21	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	CX7AW	26599692	Green Published, Green Submitted, gold			2025-03-11	WOS:000365853900035
J	Lin, SJ; Cheng, SF; Song, B; Zhong, X; Lin, X; Li, WJ; Li, L; Zhang, YQ; Zhang, H; Ji, ZL; Cai, MC; Zhuang, YY; Shi, XG; Lin, LX; Wang, L; Wang, ZB; Liu, X; Yu, S; Zeng, P; Hao, H; Zou, Q; Chen, CX; Li, YJ; Wang, Y; Xu, CY; Meng, SS; Xu, X; Wang, J; Yang, HM; Campbell, DA; Sturm, NR; Dagenais-Bellefeuille, S; Morse, D				Lin, Senjie; Cheng, Shifeng; Song, Bo; Zhong, Xiao; Lin, Xin; Li, Wujiao; Li, Ling; Zhang, Yaqun; Zhang, Huan; Ji, Zhiliang; Cai, Meichun; Zhuang, Yunyun; Shi, Xinguo; Lin, Lingxiao; Wang, Lu; Wang, Zhaobao; Liu, Xin; Yu, Sheng; Zeng, Peng; Hao, Han; Zou, Quan; Chen, Chengxuan; Li, Yanjun; Wang, Ying; Xu, Chunyan; Meng, Shanshan; Xu, Xun; Wang, Jun; Yang, Huanming; Campbell, David A.; Sturm, Nancy R.; Dagenais-Bellefeuille, Steve; Morse, David			The <i>Symbiodinium kawagutii</i> genome illuminates dinoflagellate gene expression and coral symbiosis	SCIENCE			English	Article							SMALL RNAS; HOST; GLUCOSE; SID-1; ALGAE	Dinoflagellates are important components of marine ecosystems and essential coral symbionts, yet little is known about their genomes. We report here on the analysis of a high-quality assembly from the 1180-megabase genome of Symbiodinium kawagutii. We annotated protein-coding genes and identified Symbiodinium-specific gene families. No whole-genome duplication was observed, but instead we found active (retro) transposition and gene family expansion, especially in processes important for successful symbiosis with corals. We also documented genes potentially governing sexual reproduction and cyst formation, novel promoter elements, and a microRNA system potentially regulating gene expression in both symbiont and coral. We found biochemical complementarity between genomes of S. kawagutii and the anthozoan Acropora, indicative of host-symbiont coevolution, providing a resource for studying the molecular basis and evolution of coral symbiosis.	[Lin, Senjie; Lin, Xin; Li, Ling; Zhang, Yaqun; Shi, Xinguo; Lin, Lingxiao; Wang, Lu; Meng, Shanshan] Xiamen Univ, State Key Lab Marine Environm Sci & Marine Biodiv, Xiamen 361101, Peoples R China; [Lin, Senjie; Lin, Xin; Li, Ling; Zhang, Yaqun; Shi, Xinguo; Lin, Lingxiao; Wang, Lu; Meng, Shanshan] Xiamen Univ, Global Change Res Ctr, Xiamen 361101, Peoples R China; [Lin, Senjie; Zhang, Huan; Zhuang, Yunyun] Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA; [Cheng, Shifeng; Song, Bo; Zhong, Xiao; Li, Wujiao; Wang, Zhaobao; Liu, Xin; Yu, Sheng; Zeng, Peng; Chen, Chengxuan; Li, Yanjun; Wang, Ying; Xu, Chunyan; Xu, Xun; Wang, Jun; Yang, Huanming] Beijing Genom Inst BGI Shenzhen, Shenzhen 518083, Peoples R China; [Cheng, Shifeng] Univ Hong Kong, Hong Kong Univ HKU BGI Bioinformat Algorithms & C, Dept Comp Sci, Hong Kong, Hong Kong, Peoples R China; [Cheng, Shifeng] Univ Hong Kong, Sch Biol Sci, Pokfulam, Hong Kong, Peoples R China; [Ji, Zhiliang; Cai, Meichun; Zou, Quan] Xiamen Univ, Sch Life Sci, State Key Lab Stress Cell Biol, Xiamen 361101, Peoples R China; [Hao, Han] Agcy Sci Technol & Res, Bioinformat Inst, Singapore, Singapore; [Wang, Jun] Univ Copenhagen, Dept Biol, DK-2200 Copenhagen, Denmark; [Wang, Jun; Yang, Huanming] King Abdulaziz Univ, Princess Al Jawhara Ctr Excellence Res Hereditary, Jeddah 21413, Saudi Arabia; [Yang, Huanming] James D Watson Inst Genome Sci, Hangzhou, Zhejiang, Peoples R China; [Campbell, David A.; Sturm, Nancy R.] Univ Calif Los Angeles, David Geffen Sch Med, Dept Microbiol Immunol & Mol Genet, Los Angeles, CA 90095 USA; [Dagenais-Bellefeuille, Steve; Morse, David] Univ Montreal, Dept Sci Biol, Inst Rech Biol Vegetale, Montreal, PQ H3C 3J7, Canada	Xiamen University; Xiamen University; University of Connecticut; Beijing Genomics Institute (BGI); University of Hong Kong; University of Hong Kong; Xiamen University; Agency for Science Technology & Research (A*STAR); A*STAR - Bioinformatics Institute (BII); University of Copenhagen; King Abdulaziz University; University of California System; University of California Los Angeles; University of California Los Angeles Medical Center; David Geffen School of Medicine at UCLA; Universite de Montreal	Lin, SJ (通讯作者)，Xiamen Univ, State Key Lab Marine Environm Sci & Marine Biodiv, Xiamen 361101, Peoples R China.	senjie.lin@uconn.edu	Liu, Xin/ABJ-9485-2022; Wang, Jun/A-7261-2013; li, lin/KEJ-1056-2024; Zou, Quan/A-7801-2015; Li, Zilin/AAB-1216-2019; Xu, Xun/AAI-6763-2020; Song, Bo/AAU-6535-2021; Lin, Senjie/A-7466-2011; Chen, Chengxuan/HCH-3606-2022; Yang, Huanming/C-6513-2013	Dagenais Bellefeuille, Steve/0000-0001-5281-5971; Xu, Xun/0000-0002-5338-5173; Yang, Huanming/0000-0002-0858-3410; Chen, Chengxuan/0000-0002-9650-1437; Liu, Xin/0000-0003-3256-2940; Morse, David/0000-0003-4131-4367	Natural Science Foundation of China [K16110, K16044]; U.S. National Science Foundation [OCE-0854719]; U.S. NIH [AI056034, AI073806]; National Science and Engineering Research Council of Canada [171382-03]	Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); U.S. National Science Foundation(National Science Foundation (NSF)); U.S. NIH(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USA); National Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work was supported by Natural Science Foundation of China grants K16110 and K16044 (to S.L.), U.S. National Science Foundation grant OCE-0854719 (to S.L. and H.Z.), U.S. NIH awards AI056034 and AI073806 (to D.A.C. and N.R.S.), National Science and Engineering Research Council of Canada grant 171382-03 (to D.M.), and various funds to BGI-Shenzhen, Shenzhen [State Key Laboratory of Agricultural Genomics, Guangdong Provincial Key Laboratory of core collection of crop genetic resources research and application (2011A091000047), Shenzhen Engineering Laboratory of Crop Molecular design breeding, and China National GeneBank-Shenzhen]. The genomic sequences and the annotated genes of S. kawagutii, as well as RNA sequencing data (unigenes), are available in our Symka Genome Database in Xiamen University: http://bioinf.xmu.edu.cn/symka_new; these data have also been deposited into the National Center for Biotechnology Information Short Read Archive (SRA) under accession number SRA148697.	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J	Mertens, KN; Takano, Y; Yamaguchi, A; Gu, H; Bogus, K; Kremp, A; Bagheri, S; Matishov, G; Matsuoka, K				Mertens, Kenneth Neil; Takano, Yoshihito; Yamaguchi, Aika; Gu, Haifeng; Bogus, Kara; Kremp, Anke; Bagheri, Siamak; Matishov, Gennady; Matsuoka, Kazumi			The molecular characterization of the enigmatic dinoflagellate <i>Kolkwitziella acuta</i> reveals an affinity to the <i>Excentrica</i> section of the genus <i>Protoperidinium</i>	SYSTEMATICS AND BIODIVERSITY			English	Article						brackish water; Caspian Sea; Finland; FTIR; phylogeny; single-cell PCR	CYST-THECA RELATIONSHIP; HETEROTROPHIC DINOFLAGELLATE; PHYLOGENETIC POSITIONS; SP-NOV; DINOPHYCEAE; PERIDINIALES; SEDIMENTS; EMPHASIS; SYSTEM; BROWN	Kolkwitziella acuta is a cyst-forming dinoflagellate with a unique tabulation, occurring in freshwater to brackish environments of Eurasia and the USA. Based on the unique thecal plate arrangement, this species was previously interpreted as a missing link in the evolution between the genus Protoperidinium and the Diplopsalioideae. We isolated living K. acuta cysts from the south-western Caspian Sea and the central Baltic (Finland), and re-established the cyst-theca relationship. The cysts had a distinctive polar and dorsoventral compression and a characteristic wrinkly texture. The plate formula of the thecate stage was Po, X, 4, 2a, 7, 3c+t, ?s, 5, 1. Large subunit (LSU) and small subunit (SSU) ribosomal DNA sequences obtained through single-cell PCR of these cysts reveal that this species is close to Protoperidinum excentricum which belongs to the Excentrica section of the genus Protoperidinium. We suggest that it evolved from the genus Diplopsalis through a split of the apical and anterior intercalary plates. Furthermore, that the split of the antapical plates occurred several times independently in the evolution of Protoperidinium and Diplopsalioideae and is therefore a polyphyletic trait. The cyst of Kolkwitziella is considered an indicator of low salinities, specifically between 0 and 22 psu. Geochemical analysis of the cyst walls suggests a heterotrophic mode of nutrition.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Takano, Yoshihito; Matsuoka, Kazumi] Inst East China Sea Res ECSER, Nagasaki, Japan; [Yamaguchi, Aika] Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 6578501, Japan; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA; [Kremp, Anke] Finnish Environm Inst, Ctr Marine Res, FI-00251 Helsinki, Finland; [Bagheri, Siamak] Iranian Fisheries Res Org, Inland Waters Aquaculture Inst, Anzali 66, Iran; [Matishov, Gennady] Russian Acad Sci, Southern Sci Ctr, Rostov Na Donu 344006, Russia	Ghent University; Kobe University; Third Institute of Oceanography, Ministry of Natural Resources; Texas A&M University System; Texas A&M University College Station; Finnish Environment Institute; Russian Academy of Sciences; Southern Scientific Center, Russian Academy of Sciences	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be	Mertens, Kenneth/AAO-9566-2020; Bagheri, Siamak/S-2035-2016; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Gu, Haifeng/0000-0002-2350-9171; Bagheri, Siamak/0000-0002-4645-7634; Bogus, Kara/0000-0003-4690-0576; Matishov, Gennady/0000-0003-4430-5220; Mertens, Kenneth/0000-0003-2005-9483	Kakenhi [22-00805]; National Science Foundation of China [41376170];  [RFMEFI60414x0129]	Kakenhi(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); National Science Foundation of China(National Natural Science Foundation of China (NSFC)); 	K.N.M. is a postdoctoral fellow of FWO Belgium and this research was partly conducted at Nagasaki University and supported by a Kakenhi grant 22-00805. H. Gu was supported by National Science Foundation of China (41376170). Gennady Matishov at SSC RAS was supported by Project RFMEFI60414x0129. Veijo Kinnunen and Magnus Lindstrom are thanked for sampling Sallvik. Jaana Koistinen is thanked for help with shipping samples from Finland to Japan. Samples from Lake Terkos and Buyucekmece used in this project were provided by the National Lacustrine Core Repository. Peta Mudie is thanked for providing samples from the Black Sea. Vera Pospelova is gratefully acknowledged for processing samples from Lake Terkos and Buyucekmece. Martin J. Head is thanked for advice on taxonomy and Malte Elbrachter and Yuri Okolodkow are thanked for providing access to obscure literature. The comments of two anonymous reviewers have been appreciated.	Abe T. 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Biodivers.	NOV 2	2015	13	6					829	844		10.1080/14772000.2015.1078855	http://dx.doi.org/10.1080/14772000.2015.1078855			16	Biodiversity Conservation; Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Life Sciences & Biomedicine - Other Topics	CX4NE					2025-03-11	WOS:000365676800001
J	Noorbergen, LJ; Lourens, LJ; Munsterman, DK; Verreussel, RMCH				Noorbergen, L. J.; Lourens, L. J.; Munsterman, D. K.; Verreussel, R. M. C. H.			Stable isotope stratigraphy of the early Quaternary of borehole Noordwijk, southern North Sea	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	International Field Symposium of the INQUA-Peribaltic-Working-Group (INQUA TERPRO Commission)	JUN 25-30, 2013	LITHUANIA	INQUA Peribalt Working Grp, TERPRO Commiss		Early Quaternary; Southern North Sea; Borehole Noordwijk; Benthic foraminifera; Stable isotope stratigraphy; Palynostratigraphy	DINOFLAGELLATE CYSTS; FORAMINIFERA; TERRESTRIAL; SEDIMENTS; DEPOSITS; BASIN	Between 2.58 Ma and 2.4 Ma, most of the present onshore sector of the Netherlands was an epicontinental sea. Previous studies suggest the occurrence of multiple cold and warm phases in shallow marine successions of the Maassluis Formation in conjunction with the first prominent Northern Hemisphere ice sheet expansions. Nevertheless, correlation with deep marine isotope stages is tentative and relies on relative dating as absolute dating techniques are difficult to apply. Here, we present for the first time an early Quaternary, high-resolution benthic stable isotope record from the onshore sector of the Netherlands, taken from borehole Noordwijk. We tune our record to MIS 100-94 using the characteristic delta O-18 signature and complementary biostratigraphic data. This new high resolution isotope chronology is providing important insights on stratigraphy and palaeoenvironmental development of the southern North Sea area during the early Quaternary. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.	[Noorbergen, L. J.; Lourens, L. J.] Univ Utrecht, Dept Earth Sci, Fac Geosci, NL-3584 CD Utrecht, Netherlands; [Munsterman, D. K.; Verreussel, R. M. C. 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J	Accoroni, S; Percopo, I; Cerino, F; Romagnoli, T; Pichierri, S; Perrone, C; Totti, C				Accoroni, Stefano; Percopo, Isabella; Cerino, Federica; Romagnoli, Tiziana; Pichierri, Salvatore; Perrone, Cesira; Totti, Cecilia			Allelopathic interactions between the HAB dinoflagellate <i>Ostreopsis</i> cf. <i>ovata</i> and macroalgae	HARMFUL ALGAE			English	Article						Ostreopsis; Macroalgae; Allelopathy; Harmful algae; Growth inhibition; Cysts	HARMFUL ALGAL BLOOMS; ULVA-LINZA CHLOROPHYTA; NORTHERN ADRIATIC SEA; MEDITERRANEAN SEA; COASTAL WATERS; CORALLINA-PILULIFERA; POSIDONIA-OCEANICA; FEEDING-DETERRENTS; ALGICIDAL ACTIVITY; PRYMNESIUM-PARVUM	Intense blooms of the toxic benthic dinoflagellate Ostreopsis cf. ovata have been a recurrent phenomenon along several Mediterranean coasts during summer in the last few years. These blooms are often associated with noxious effects on humans and deaths of benthic invertebrates. Previous studies carried out on the Conero Riviera (northern Adriatic Sea) highlighted that Ostreopsis abundances recorded on rocks were significantly higher than on the surface of seaweeds, suggesting that some allelopathic interactions might occur between Ostreopsis and macroalgal substrates. In this study we investigated under experimental conditions the interactions between O. cf. ovata and three of the most common macroalgae in this area: Dictyota dichotoma (brown alga), Rhodymenia pseudopalmata (red alga) and Ulva rigida (green alga). Three different experiments were set up: O. cf. ovata was grown (i) together with fresh macroalgal tissues, (ii) in media in which macroalgae were previously cultured, and (iii) in media with the addition of dry macroalgal powder at different concentrations. The results indicated that all the investigated seaweeds exerted negative effects toward the benthic dinoflagellate O. cf. ovata. D. dichotoma inhibited the growth of O. cf. ovata in all tested experimental conditions; U. rigida had inhibitory effect both in form of fresh thalli and dry powder but not as growth medium filtrate, suggesting that either Ulva does not release any allelopathic compound in the medium in absence of O. cf. ovata or the alleged released allelochemicals are rapidly degradable. Neither the fresh thalli of R. pseudopalmata or the filtrate of its culture medium showed any inhibitory effects, while a negative effect was only observed at high concentrations of dry thallus powder. With the exception of D. dichotoma co-culture experiment, a complete algicidal effect was never observed partly because O. cf. ovata produced a large amount of resting stages, which permitted its survival. (C) 2015 Elsevier B.V. All rights reserved.	[Accoroni, Stefano; Percopo, Isabella; Cerino, Federica; Romagnoli, Tiziana; Pichierri, Salvatore; Totti, Cecilia] Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, I-60131 Ancona, Italy; [Perrone, Cesira] Univ Bari, Dipartimento Biol, I-70124 Bari, Italy	Marche Polytechnic University; Universita degli Studi di Bari Aldo Moro	Accoroni, S (通讯作者)，Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, Via Brecce Blanche, I-60131 Ancona, Italy.	s.accoroni@univpm.it	; TOTTI, Cecilia Maria/A-9178-2016; Accoroni, Stefano/F-5818-2014	Romagnoli, Tiziana/0009-0009-5181-987X; Cerino, Federica/0000-0002-9191-9957; TOTTI, Cecilia Maria/0000-0002-1532-6009; Accoroni, Stefano/0000-0002-1134-7849	ISPRA - Italian Ministry of the Environment	ISPRA - Italian Ministry of the Environment	This research was partially funded by ISPRA - Italian Ministry of the Environment. The authors wish to gratefully thank Rossella Pistocchi and Franca Guerrini for their useful indications about the experimental design and Mauro Marini for the nutrient analysis. 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J	Brosnahan, ML; Velo-Suárez, L; Ralston, DK; Fox, SE; Sehein, TR; Shalapyonok, A; Sosik, HM; Olson, RJ; Anderson, DM				Brosnahan, Michael L.; Velo-Suarez, Lourdes; Ralston, David K.; Fox, Sophia E.; Sehein, Taylor R.; Shalapyonok, Alexi; Sosik, Heidi M.; Olson, Robert J.; Anderson, Donald M.			Rapid growth and concerted sexual transitions by a bloom of the harmful dinoflagellate <i>Alexandrium fundyense</i> (Dinophyceae)	LIMNOLOGY AND OCEANOGRAPHY			English	Article							NAUSET MARSH SYSTEM; GONYAULAX-TAMARENSIS; CYST FORMATION; CELL-CYCLE; RED-TIDE; CAPE-COD; TEMPERATURE; DYNAMICS; PHYTOPLANKTON; SALINITY	Transitions between life cycle stages by the harmful dinoflagellate Alexandrium fundyense are critical for the initiation and termination of its blooms. To quantify these transitions in a single population, an Imaging FlowCytobot (IFCB), was deployed in Salt Pond (Eastham, Massachusetts), a small, tidally flushed kettle pond that hosts near annual, localized A. fundyense blooms. Machine-based image classifiers differentiating A. fundyense life cycle stages were developed and results were compared to manually corrected IFCB samples, manual microscopy-based estimates of A. fundyense abundance, previously published data describing prevalence of the parasite Amoebophrya, and a continuous culture of A. fundyense infected with Amoebophrya. In Salt Pond, a development phase of sustained vegetative division lasted approximately 3 weeks and was followed by a rapid and near complete conversion to small, gamete cells. The gametic period (approximate to 3 d) coincided with a spike in the frequency of fusing gametes (up to 5% of A. fundyense images) and was followed by a zygotic phase (approximate to 4 d) during which cell sizes returned to their normal range but cell division and diel vertical migration ceased. Cell division during bloom development was strongly phased, enabling estimation of daily rates of division, which were more than twice those predicted from batch cultures grown at similar temperatures in replete medium. Data from the Salt Pond deployment provide the first continuous record of an A. fundyense population through its complete bloom cycle and demonstrate growth and sexual induction rates much higher than are typically observed in culture.	[Brosnahan, Michael L.; Sehein, Taylor R.; Shalapyonok, Alexi; Sosik, Heidi M.; Olson, Robert J.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Velo-Suarez, Lourdes] IFREMER, Dept Dynam Environm Cotier, Plouzane, France; [Ralston, David K.] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA; [Fox, Sophia E.] Natl Pk Serv, Cape Cod Natl Seashore, Wellfleet, MA USA	Woods Hole Oceanographic Institution; Ifremer; Woods Hole Oceanographic Institution; United States Department of the Interior; US National Park Service	Brosnahan, ML (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	mbrosnahan@whoi.edu	Velo-Suárez, Lourdes/C-2664-2009; Sehein, Taylor/HJI-8995-2023	Brosnahan, Michael/0000-0002-2620-7638; Sosik, Heidi/0000-0002-4591-2842	National Science Foundation [OCE-0430724, OCE-0911031, OCE-1314642]; National Institutes of Health through the Woods Hole Center for Oceans and Human Health [NIEHS-1P50-ES021923-01]; National Park Service (NPS) [H238015504]; Gordon and Betty Moore Foundation [2649]; Access to the Sea program at the Woods Hole Oceanographic Institution; Marie Curie International Outgoing Fellowship [MOHAB PIOF-GA-252260]; Directorate For Geosciences; Division Of Ocean Sciences [1314642] Funding Source: National Science Foundation	National Science Foundation(National Science Foundation (NSF)); National Institutes of Health through the Woods Hole Center for Oceans and Human Health; National Park Service (NPS); Gordon and Betty Moore Foundation(Gordon and Betty Moore Foundation); Access to the Sea program at the Woods Hole Oceanographic Institution; Marie Curie International Outgoing Fellowship(European Union (EU)); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	Special thanks to Bruce Keafer, Kerry Norton, David Kulis, Yan Gao and other staff and student members of D. Anderson's laboratory for assistance in sample collection and preparation of cultures, to Micheil Boesel for technical assistance during the design and construction of the IFCB support raft, to Krista Lee and staff at the Cape Cod National Seashore Salt Pond Visitor Center for assistance in setting up the raft communication system, and to Linda Amaral-Zettler, Leslie Murphy, and Julie Reveillaud who assisted with Amoebphrya surveys at Salt Pond. This work was supported by the National Science Foundation (OCE-0430724, OCE-0911031, and OCE-1314642) and National Institutes of Health (NIEHS-1P50-ES021923-01) through the Woods Hole Center for Oceans and Human Health, by National Park Service (NPS) Cooperative Agreement H238015504, by the Gordon and Betty Moore Foundation (Grant #2649 to HMS), and by an award from the Access to the Sea program at the Woods Hole Oceanographic Institution. Additional support was provided through a Marie Curie International Outgoing Fellowship to L. Velo-Suarez (IOF; grant agreement: MOHAB PIOF-GA-252260).	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Oceanogr.	NOV	2015	60	6					2059	2078		10.1002/lno.10155	http://dx.doi.org/10.1002/lno.10155			20	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	CU9TO	27667858	Green Published, hybrid			2025-03-11	WOS:000363888400015
J	Paredes, JM; Foix, N; Guerstein, GR; Guler, MV; Irigoyen, M; Moscoso, P; Giordano, S				Paredes, Jose M.; Foix, Nicolas; Raquel Guerstein, G.; Guler, Maria V.; Irigoyen, Martin; Moscoso, Pablo; Giordano, Sergio			A late eocene-early Oligocene transgressive event in the Golfo San Jorge basin: Palynological results and stratigraphic implications	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						El Huemul formation; Pre-patagoniense transgression; Late eocene to early Oligocene; dinoflagellate cysts; Golfo San Jorge basin; Patagonia	TIERRA-DEL-FUEGO; LAND MAMMAL AGE; MIDDLE EOCENE; DINOFLAGELLATE CYSTS; COASTAL-PLAIN; NEW-JERSEY; PATAGONIA; ARGENTINA; PALEOCENE; DEPOSITS	A new Cenozoic dataset in the subsurface of the South Flank of the Golfo San Jorge Basin (Santa Cruz province) allowed to identify a non-previously recognized transgressive event of late Eocene to early Oligocene age. Below of a marine succession containing a dinoflagellate cyst assemblage that characterizes the C/G palynological zone of the Chenque Formation (early Miocene), a 80-110 m thick marine succession contains a palynological assemblage integrated by Gelatia inflata, Diphyes colligerum and Reticulatosphaera actinocoronata supporting the occurrence of a marine incursion in the basin during the Eocene Oligocene transition (EOT). The new lithostratigraphic unit - here defined as El Huemul Formation covers in sharp contact to the Sarmiento Formation, and become thinner from East to West; the unit has been identified in about 1800 well logs covering up to 3500 km(2), and its subsurface distribution exceed the boundaries of the study area. The El Huemul Formation consists of a thin lag of glauconitic sandstones with fining-upward log motif, followed by a mudstone-dominated succession that coarsening-upward to sandstones, evidencing a full T-R cycle. Preservation of the El Huemul Formation in the subsurface of the South Flank has been favored by the reactivation of WNW-ESE late Cretaceous normal faults, and by the generation of N-S striking normal faults of Paleocene-Eocene age. Flexural loading associated to igneous intrusions of Paleocene?- middle Eocene age also promoted the increase of subsidence in the South Flank of the basin prior to the transgression. (C) 2015 Elsevier Ltd. All rights reserved.	[Paredes, Jose M.; Foix, Nicolas] Univ Natl Patagonia San Juan Bosco, Dept Geol FCN, RA-9005 Comodoro Rivadavia, Chubut, Argentina; [Foix, Nicolas; Raquel Guerstein, G.; Guler, Maria V.] CONICET Consejo Invest Cient & Tecn, Buenos Aires, DF, Argentina; [Raquel Guerstein, G.; Guler, Maria V.] Univ Nacl Sur, Dept Geol, INGEOSUR Inst Geol Sur, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Irigoyen, Martin; Moscoso, Pablo; Giordano, Sergio] SINOPEC ARGENTINA Explorat & Prod Inc, Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Paredes, JM (通讯作者)，Univ Natl Patagonia San Juan Bosco, Dept Geol FCN, Ruta Prov S-N,Km 4, RA-9005 Comodoro Rivadavia, Chubut, Argentina.	paredesj@unpata.edu.ar	Paredes, Jose/S-4679-2019	Guerstein, G. 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J	Wells, ML; Trainer, VL; Smayda, TJ; Karlson, BSO; Trick, CG; Kudela, RM; Ishikawa, A; Bernard, S; Wulff', A; Anderson, DM; Cochlan, WP				Wells, Mark L.; Trainer, Vera L.; Smayda, Theodore J.; Karlson, Bengt S. O.; Trick, Charles G.; Kudela, Raphael M.; Ishikawa, Akira; Bernard, Stewart; Wulff, Angela; Anderson, Donald M.; Cochlan, William P.			Harmful algal blooms and climate change: Learning from the past and present to forecast the future	HARMFUL ALGAE			English	Article						Harmful algal blooms; HAB; Climate change	DOMOIC ACID PRODUCTION; PHYTOPLANKTON COMMUNITY STRUCTURE; PARALYTIC SHELLFISH TOXINS; DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; NITZSCHIA SPP. BACILLARIOPHYCEAE; CO2 CONCENTRATING MECHANISMS; INORGANIC CARBON ACQUISITION; SETO INLAND SEA; PSEUDO-NITZSCHIA; MARINE-PHYTOPLANKTON	Climate change pressures will influence marine planktonic systems globally, and it is conceivable that harmful algal blooms may increase in frequency and severity. These pressures will be manifest as alterations in temperature, stratification, light, ocean acidification, precipitation-induced nutrient inputs, and grazing, but absence of fundamental knowledge of the mechanisms driving harmful algal blooms frustrates most hope of forecasting their future prevalence. Summarized here is the consensus of a recent workshop held to address what currently is known and not known about the environmental conditions that favor initiation and maintenance of harmful algal blooms. There is expectation that harmful algal bloom (HAB) geographical domains should expand in some cases, as will seasonal windows of opportunity for harmful algal blooms at higher latitudes. Nonetheless there is only basic information to speculate upon which regions or habitats HAB species may be the most resilient or susceptible. Moreover, current research strategies are not well suited to inform these fundamental linkages. There is a critical absence of tenable hypotheses for how climate pressures mechanistically affect HAB species, and the lack of uniform experimental protocols limits the quantitative cross-investigation comparisons essential to advancement. A HAB "best practices" manual would help foster more uniform research strategies and protocols, and selection of a small target list of model HAB species or isolates for study would greatly promote the accumulation of knowledge. Despite the need to focus on keystone species, more studies need to address strain variability within species, their responses under multifactorial conditions, and the retrospective analyses of long-term plankton and cyst core data; research topics that are departures from the norm. Examples of some fundamental unknowns include how larger and more frequent extreme weather events may break down natural biogeographic barriers, how stratification may enhance or diminish HAB events, how trace nutrients (metals, vitamins) influence cell toxicity, and how grazing pressures may leverage, or mitigate HAB development. There is an absence of high quality time-series data in most regions currently experiencing HAB outbreaks, and little if any data from regions expected to develop HAB events in the future. A subset of observer sites is recommended to help develop stronger linkages among global, national, and regional climate change and HAB observation programs, providing fundamental datasets for investigating global changes in the prevalence of harmful algal blooms. Forecasting changes in HAB patterns over the next few decades will depend critically upon considering harmful algal blooms within the competitive context of plankton communities, and linking these insights to ecosystem, oceanographic and climate models. From a broader perspective, the nexus of HAB science and the social sciences of harmful algal blooms is inadequate and prevents quantitative assessment of impacts of future HAB changes on human wellbeing. These and other fundamental changes in HAB research will be necessary if HAB science is to obtain compelling evidence that climate change has caused alterations in HAB distributions, prevalence or character, and to develop the theoretical, experimental, and empirical evidence explaining the mechanisms underpinning these ecological shifts. (C) 2015 Elsevier B.V. All rights reserved.	[Wells, Mark L.] Univ Maine, Sch Marine Sci, Orono, ME 04469 USA; [Trainer, Vera L.] NOAA, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Marine Biotoxins Program, Seattle, WA 98112 USA; [Smayda, Theodore J.] Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA; [Karlson, Bengt S. O.] SMHI Res & Dev, Oceanog, S-42671 Vastra Frolunda, Sweden; [Trick, Charles G.] Univ Western Ontario, Dept Biol, London, ON N6A 5B7, Canada; [Kudela, Raphael M.] Univ Calif Santa Cruz, Ocean Sci, Santa Cruz, CA 95064 USA; [Ishikawa, Akira] Mie Univ, Grad Sch Bioresources, Lab Biol Oceanog, Tsu, Mie 5148507, Japan; [Bernard, Stewart] CSIR NRE Ctr High Performance Comp, Earth Syst Earth Observat, ZA-7700 Cape Town, South Africa; [Wulff, Angela] Univ Gothenburg, Dept Biol & Environm Sci, SE-40530 Gothenburg, Sweden; [Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Cochlan, William P.] San Francisco State Univ, Romberg Tiburon Ctr Environm Studies, Tiburon, CA 94920 USA	University of Maine System; University of Maine Orono; National Oceanic Atmospheric Admin (NOAA) - USA; University of Rhode Island; Swedish Meteorological & Hydrological Institute; Western University (University of Western Ontario); University of California System; University of California Santa Cruz; Mie University; University of Gothenburg; Woods Hole Oceanographic Institution; California State University System; San Francisco State University	Wells, ML (通讯作者)，Univ Maine, Sch Marine Sci, Orono, ME 04469 USA.	mlwells@maine.edu; vera.l.trainer@noaa.gov; tsmayda@uri.edu; Bengt.Karlson@smhi.se; trick@uwo.ca; kudela@ucsc.edu; ishikawa@bio.mie-u.ac.jp; sbernard@csir.co.za; angela.wulff@bioenv.gu.se; danderson@whoi.edu; cochlan@sfsu.edu	Karlson, Bengt/AAG-1747-2020; Trainer, Vera/AAE-9306-2022	Karlson, Bengt/0000-0002-7524-3504; Bernard, Stewart/0000-0001-6537-3682; , Vera/0009-0005-9585-6753	PICES; GEOHAB; U.S. National Office for Marine Biotoxins and Harmful Algal Blooms, Woods Hole Oceanographic Institution; SCOR-IOC GEOHAB; National Science Foundation (NSF) [OCE-1131657, OCE 1130748, OCE-1128041, OCE-1314642]; NOAA NCCOS grants [NA10NOS4780161, NA10NOS4780160]; Woods Hole Center for Oceans and Human Health; National Institute of Environmental Health Sciences (NIEHS) [1-P50-ES021923-01]; California Sea Grant; California Ocean Protection Council [R/OPCCONT-12 A 10]; National Aeronautics and Space Administration grant [NNX13AL28G]; NOAA award [NA11NOS4780030]; Grants-in-Aid for Scientific Research [25450256] Funding Source: KAKEN; NASA [470051, NNX13AL28G] Funding Source: Federal RePORTER; Division Of Ocean Sciences; Directorate For Geosciences [1314642, 1131657] Funding Source: National Science Foundation	PICES; GEOHAB; U.S. National Office for Marine Biotoxins and Harmful Algal Blooms, Woods Hole Oceanographic Institution; SCOR-IOC GEOHAB; National Science Foundation (NSF)(National Science Foundation (NSF)); NOAA NCCOS grants(National Oceanic Atmospheric Admin (NOAA) - USA); Woods Hole Center for Oceans and Human Health; 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)); California Sea Grant; California Ocean Protection Council; National Aeronautics and Space Administration grant; NOAA award(National Oceanic Atmospheric Admin (NOAA) - USA); 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)); NASA(National Aeronautics & Space Administration (NASA)); Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	Support for the workshop organized under the auspices of PICES and GEOHAB and endorsed by ICES was provided by the North Pacific Marine Science Organization (PICES), the U.S. National Office for Marine Biotoxins and Harmful Algal Blooms, Woods Hole Oceanographic Institution and SCOR-IOC GEOHAB. Additional support for MLW, CGT, and WPC was from the National Science Foundation (NSF) Grants OCE-1131657 and OCE 1130748 and NOAA NCCOS grants NA10NOS4780161 and NA10NOS4780160, respectively. Support for DMA was provided through the Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF) Grants OCE-1128041 and OCE-1314642; and National Institute of Environmental Health Sciences (NIEHS) Grant 1-P50-ES021923-01. Support for RMK was provided through California Sea Grant and California Ocean Protection Council award R/OPCCONT-12 A 10, National Aeronautics and Space Administration grant NNX13AL28G, and the NOAA award NA11NOS4780030. We express our sincere appreciation to G. Hallegraeff, S. Moore, and an anonymous reviewer for their contributions that improved this work. 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J	Cheng, JH; Zhou, CM; He, CQ; Shi, TM; Amuti, A				Cheng, Jinhui; Zhou, Chunmei; He, Chengquan; Shi, Tianming; Amuti, Aliya			New Eocene dinoflagellate cysts from the southern edge of the Junggar Basin, Xinjiang, China	GRANA			English	Article						marine; dinoflagellate cyst; Eocene; Junggar Basin; Anjihaihe Formation		The Anjihaihe Formation in the southern edge of the Junggar Basin was previously considered a series of freshwater lacustrine depositions. However, abundant marine dinoflagellate cysts were recently recovered from the middle to upper part of the middle member of the formation. Two new genera, six new species and one new subspecies among the abundant dinoflagellate cysts are described and illustrated, i.e. Circulodinium? laeve sp. nov., Kaiwaradinium abbreviatum sp. nov., Spiniferites adnatus subsp. latispinus subsp. nov., Oligosphaeropsis accreta gen. et. sp. nov., Oligosphaeropsis complex gen. et. sp. nov., Oligosphaeropsis megaprocessa gen. et. sp. nov. and Tianshandinium biconicum gen. et. sp. nov. They are rare to common constituents of the dinoflagellate assemblage in the Anjihaihe Formation and may prove useful for regional biostratigraphic correlation and palaeoenvironment re-establishment.	[Cheng, Jinhui; He, Chengquan] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China; [Zhou, Chunmei; Shi, Tianming; Amuti, Aliya] PetroChina Xinjiang Oilfield Co, Explorat & Dev Res Inst, Karamay, Xinjiang, Peoples R China	Chinese Academy of Sciences; Sinopec; China National Petroleum Corporation	Cheng, JH (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, 39 East Beijing Rd, Nanjing 210008, Jiangsu, Peoples R China.	jhcheng@nigpas.ac.cn	Zhou, Chunmei/JEP-0374-2023	cheng, jin hui/0000-0002-3560-3667	National Natural Science Foundation of China [41102019, 41272014]; Exploration and Development Research Institute of PetroChina Xinjiang Oilfield Company [K10-36]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Exploration and Development Research Institute of PetroChina Xinjiang Oilfield Company	This work was supported by the National Natural Science Foundation of China [41102019,41272014]; the Exploration and Development Research Institute of PetroChina Xinjiang Oilfield Company [K10-36].	[Anonymous], 1993, SPEC PUBL NUMBER; [Anonymous], 1980, SP PAP PALAEONTOL; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region, 1999, STRAT LITH XINJ UYG; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; MacRae RA, 1996, CAN J BOT, V74, P1687, DOI 10.1139/b96-205; [齐雪峰 QI Xue-feng], 2009, [新疆石油地质, Xinjiang Petroleum Geology], V30, P289; Regional Stratigraphic Chart Compiling Group of Xinjiang Regional Stratigraphic Chart, 1981, REG STRAT CHART N W; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; Sun MR, 1990, PERMIAN TERTIARY STR, P122; Tang, 1993, W CHINA MED J, V8, P140; Williams G.L., 2000, American Association of Stratigraphic Palynologists Contributions Series, V37, P1; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zhou Chun-mei, 2012, Journal of Stratigraphy, V36, P723	15	0	2	2	13	TAYLOR & FRANCIS AS	OSLO	KARL JOHANS GATE 5, NO-0154 OSLO, NORWAY	0017-3134	1651-2049		GRANA	Grana	OCT 2	2015	54	4					294	304		10.1080/00173134.2015.1096300	http://dx.doi.org/10.1080/00173134.2015.1096300			11	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	CV4LV					2025-03-11	WOS:000364239500005
J	Benzaggagh, M; Homberg, C; Schnyder, J; Razgallah, S; Hssaida, T				Benzaggagh, Mohamed; Homberg, Catherine; Schnyder, Johann; Razgallah, Saloua; Hssaida, Touria			Importance of calcareous dinoflagellate cysts and of the pelagic biomicrofacies in dating the Upper Jurassic-Lowermost Berriasian deposits in the western tethyan realm	ANNALES DE PALEONTOLOGIE			French	Article						Calcareous dinoflagellate cysts; Calpionellids; Microfacies; Upper Jurassic; Lowermost Berriasian; Western Tethys	JURASSIC/CRETACEOUS BOUNDARY; STRATIGRAPHIC DISTRIBUTION; INTERNAL PRERIF; AMMONITE; RIF; MESORIF; CALPIONELLIDS; MOUNTAINS; MOROCCO; UMBRIA	The study of several hundreds of thin sections from dozen outcrops in three different paleogeographic basins: the External Rif Range (Morocco), the Vocontian Basin (Southeastern France) and the northern Tunisia, has confirmed the importance of pelagic microfaunal associations to date the Upper Jurassic deposits. Among those palaeontological groups, crinoid saccocomids, which appear in the Middle Oxfordian, are thriving noticeably in the three basins at the base of the lower Tithonian substage (Hybonotum ammonite zone). Calcareous dinoflagellate cysts (two new species) were also used to characterize 10 biozones, 7 at least have a general value in the Tethyan realm. Protoglobigerines, abundant in the Upper Oxfordian and at the base of the Kimmeridgian (Platynota zone), are rare or absent in younger strata. In the external Rif and in northern Tunisia, microfilaments show two levels of abundance, respectively in the Divisum and the Beckeri zones. They disappear at the top of the latter zone. Chitinoidellids were used to characterize the Lower Tithonian (Ponti zone)-Upper Tithonian (zone Microcanthum) boundary. Calpionellids, appearing at the top of the Microcanthum zone, are still abundant within the Durangites zone. Globochaete, often present, are really abundant only from the base of the Lower Tithonian and higher up throughout the Tithonian. Radiolarians show random stratigraphic distributions. Combining all these various fossil groups and their abundance, we define 13 biozones of concurrent range, which are well-correlated with ammonite zones. It corresponds respectively to the Upper Oxfordian-basal Kimmeridgian (Platynota zone), the Hypselocyclum zone, the Divisum zone, the Acanthicum-Eudoxus zones, the Beckeri zone, the Hybonotum zone, the Darwini-Semiforme zones, the Fallauxi zone, the Ponti zone, the Microcanthum pro parte zone, the upper part of the Microcanthum zone-lower part of the Durangites zone, the upper part of the Durangites zone and the lower part of the Euxinus zone. The present work aims to contribute towards to a better and more practical biostratigraphical zonation of the Upper Jurassic-lowermost Berriasian deposits in the western tethyan basins. (C) 2015 Elsevier Masson SAS. All rights reserved.	[Benzaggagh, Mohamed] Univ Moulay Ismail, Fac Sci, Dept Geol, BP 11-102, Zitoune, Meknes, Morocco; [Homberg, Catherine] CNRS, UMR 7193, Inst Sci Terre Paris, F-75005 Paris, France; [Schnyder, Johann] Univ Paris 06, UMR 7193, ISTeP, Sorbonne Univ, F-75005 Paris, France; [Razgallah, Saloua] Univ Tunis El Manar, Fac Sci, Dept Sci Terre, Tunis 1060, Tunisia; [Hssaida, Touria] Univ Hassan II Mohammedia, Fac Sci Ben MSik, Casablanca, Morocco	Moulay Ismail University of Meknes; Sorbonne Universite; 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); Universite de Tunis-El-Manar; Faculte des Sciences de Tunis (FST); Hassan II University of Casablanca	Benzaggagh, M (通讯作者)，Univ Moulay Ismail, Fac Sci, Dept Geol, BP 11-102, Zitoune, Meknes, Morocco.	benzaggagh@gmail.com	Schnyder, Johann/IQV-5253-2023	Homberg, Catherine/0000-0003-3821-7304				Aubouin J., 1980, EUROPE CHAINES PERIM, P62; AUBRY MP, 1988, GEOBIOS-LYON, V21, P709, DOI 10.1016/S0016-6995(88)80089-5; Ben Abdesselam-Mandaoui S, 2011, CR PALEVOL, V10, P527, DOI 10.1016/j.crpv.2011.05.006; BENABDESSELAMMAHDAOUI S, 2010, GEO-ECO-TROP, V34, P113; Benzaggagh M, 1996, CR ACAD SCI II A, V322, P661; BENZAGGAGH M, 1995, CR ACAD SCI II A, V321, P681; BENZAGGAGH M, 1995, CR ACAD SCI II, V320, P227; Benzaggagh M, 1997, NEWSL STRATIGR, V35, P127; BENZAGGAGH M., 1988, THESIS; Benzaggagh M., 2015, ANN PALEONTOLOGIE, V101; Benzaggagh M., 2000, DOCUMENTS LAB GEOLOG; Benzaggagh M, 2012, ANN PALEONTOL, V98, P253, DOI 10.1016/j.annpal.2012.07.001; Benzaggagh M, 2006, NEWSL STRATIGR, V42, P115, DOI 10.1127/0078-0421/2006/0042-0115; Benzaggagh M, 2010, PALAEONTOL Z, V84, P301, DOI 10.1007/s12542-009-0045-1; Bonet F., 1956, B ASOC MEX GEOL PET, V8, P389; Borza K., 1986, ACTA GEOLOGICA HUNGA, V291, P133; BORZA K, 1984, GEOLGICKYZBORNIK GEO, V3, P539; Borza K., 1969, MIKROFACIES MIKROFOS; Borza K., 1964, GEOL SBOR, V15, P189; Caracuel JE, 1997, PALAEOGEOGR PALAEOCL, V135, P163, DOI 10.1016/S0031-0182(97)00030-8; CECCA F, 1991, CR ACAD SCI II, V313, P1441; CECCA F., 1989, DOCUMENTS LAB GEOLOG, V107; Colom G., 1935, ASS ETUDE GEOLOGIE M, V3, P1; Colom G., 1994, REV ESPAGNOLA MICROP, VXXVI, P5; de Lapparent J, 1924, B SOC GEOLOGIQUE FRA, P615; DROMART G, 1988, COMPTES RENDUS AC 2A, V312, P617; Durand-Delga M., 1957, PUBL SERV CARTE GEOL, V13, P153; Enay R., 1975, MEMOIRE BUREAU RECHE, V10, P261; Grandesso P., 1977, MEMOIRES SCI GEOLOGI MEMOIRES SCI GEOLOGI, V32, P3; Homberg C, 2013, B SOC GEOL FR, V184, P501, DOI 10.2113/gssgfbull.184.4-5.501; Housa V, 2004, CRETACEOUS RES, V25, P771, DOI 10.1016/j.cretres.2004.07.001; Housa V, 1999, CRETACEOUS RES, V20, P699, DOI 10.1006/cres.1999.0177; Keupp H., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V122, P497, DOI 10.2973/odp.proc.sr.122.189.1992; Lakova I, 1999, GEOL CARPATH, V50, P151; NAGY I, 1986, Acta Geologica Hungarica, V29, P45; Nagy I., 1966, Foldtani Kozlony, V96, P86; Nowak W., 1968, Rocznik Polskiego Towarzystwa Geologicznego, V38, P275; Petrova Silviya, 2012, Geologica Balcanica, V41, P53; POP G, 1997, CR HEBD ACAD SCI, V322, P661; Pop G., 1998, ROMANIAN J STRATIGRA, V77, P3; REHAKOVA D, 2005, VOLUMINA JURASSICA, V3, P15; Rehakova Daniela, 2000, Mineralia Slovaca, V32, P79; Rehanek J., 1985, Casopis pro Mineralogii a Geologii, V30, P367; REHANEK J, 1982, Geologicky Zbornik, V33, P219; Rehanek Jan, 1993, Revue de Micropaleontologie, V36, P143; Remane J., 1963, TRAVAUX LABORATOIRE, V39, p25?82; Remane J., 1971, Ann Guebhard, V47, P1; Sallouhi H, 2011, CR PALEVOL, V10, P641, DOI 10.1016/j.crpv.2011.08.003; Wanner J., 1940, PALEONT, V22, P75, DOI [10.1007/BF03041716, DOI 10.1007/BF03041716]; Weinkauf M.F.G., 2013, Documenta Naturae, V192, P241; Wendler J, 2002, CRETACEOUS RES, V23, P213, DOI 10.1006/cres.2002.0311	51	11	12	0	3	MASSON EDITEUR	MOULINEAUX CEDEX 9	21 STREET CAMILLE DESMOULINS, ISSY, 92789 MOULINEAUX CEDEX 9, FRANCE	0753-3969	1778-3666		ANN PALEONTOL	Ann. Paleontol.	OCT-DEC	2015	101	4					251	263		10.1016/j.annpal.2015.04.006	http://dx.doi.org/10.1016/j.annpal.2015.04.006			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DL6ED					2025-03-11	WOS:000375731500001
J	Jiang, XW; Wang, J; Gao, Y; Chan, LL; Lam, PKS; Gu, JD				Jiang, Xi-Wen; Wang, Jing; Gao, Yue; Chan, Leo Lai; Lam, Paul Kwan Sing; Gu, Ji-Dong			Relationship of proteomic variation and toxin synthesis in the dinoflagellate <i>Alexandrium tamarense</i> CI01 under phosphorus and inorganic nitrogen limitation	ECOTOXICOLOGY			English	Article						Alexandrium tamarense; PSTs; Cell cycle; Nutrient condition; Toxin synthesis protein	PHOSPHATASE GENE SEQUENCE; BACILLUS-SUBTILIS; TRANSCRIPTIONAL REGULATION; C2 TOXIN; SAXITOXIN; DINOPHYCEAE; IDENTIFICATION; BIOSYNTHESIS; TOXICITY; MINUTUM	Paralytic shellfish toxins (PSTs) are originated from cyanobacteria and dinoflagellates, including Alexandrium tamarense, the common dinoflagellate species. In this study, a toxic dinoflagellate strain of A. tamarense CI01 was selected for studying the PSTs' concentration and the related protein variation during the whole cell cycle under different nutrient conditions. High-performance liquid chromatography, 2-D DIGE and Western blotting were used collectively for protein profiling and identification. Results showed that the toxin content was suppressed under nitrogen limiting condition, but enhanced in phosphorous limiting medium. Based on the results of proteomics analysis, 7 proteins were discovered to be related to the PSTs biosynthesis of A. tamarense CI01, including S-adenosylhomocysteine hydrolase, ornithine cyclodeaminase, argininosuccinate synthase, methyluridine methyltransferase cystine ABC transporter, phosphoserine phosphatase, argininosuccinate synthase and acyl-CoA dehydrogenase, which corresponds to the metabolism of the methionine, cysteine, ornithine, arginine and proline. Moreover, some photosynthesis relating proteins also increased their expression during PST synthesis period in A. tamarense CI01, such as phosphoenolpyruvate carboxylase, chloroplast phosphoglycerate kinase, peridininchlorophyll alpha-binding protein, Mg2+ transporter protein and chloroplast phosphoglycerate kinase. The above findings are in support of our hypothesis that these proteins are involved in toxin biosynthesis of A. tamarense CI01, but cause-and-effect mechanisms need to be investigated in further studies.	[Jiang, Xi-Wen; Wang, Jing; Gu, Ji-Dong] Univ Hong Kong, Sch Biol Sci, Hong Kong, Hong Kong, Peoples R China; [Jiang, Xi-Wen] Hong Kong Polytech Univ, Dept Hlth Technol & Informat, Kowloon, Hong Kong, Peoples R China; [Wang, Jing] Tianjin Univ Sci & Technol, Coll Marine Sci & Engn, Tianjin 300457, Peoples R China; [Gao, Yue] Xiamen Univ, State Key Lab Marine Environm Sci, Environm Sci Res Ctr, Xiamen 361005, Peoples R China; [Chan, Leo Lai] City Univ Hong Kong, Shenzhen Key Lab Sustainable Use Marine Biodivers, Res Ctr Oceans & Human Heath, Shenzhen Res Inst, Shenzhen, Peoples R China; [Chan, Leo Lai; Lam, Paul Kwan Sing] City Univ Hong Kong, State Key Lab Marine Pollut, Kowloon, Hong Kong, Peoples R China; [Chan, Leo Lai] City Univ Hong Kong, Dept Biomed Sci, Kowloon, Hong Kong, Peoples R China; [Lam, Paul Kwan Sing] City Univ Hong Kong, Dept Biol & Chem, Kowloon, Hong Kong, Peoples R China	University of Hong Kong; Hong Kong Polytechnic University; Tianjin University Science & Technology; Xiamen University; City University of Hong Kong; Shenzhen Research Institute, City University of Hong Kong; City University of Hong Kong; City University of Hong Kong; City University of Hong Kong	Gu, JD (通讯作者)，Univ Hong Kong, Sch Biol Sci, Pokfulam Rd, Hong Kong, Hong Kong, Peoples R China.	jdgu@hku.hk	Gu, Ji-Dong/AAF-2291-2019; Chan, Leo/F-6943-2011; /D-3086-2009; LAM, Kwan Sing Paul/B-9121-2008	/0000-0002-7082-9784; LAM, Kwan Sing Paul/0000-0002-2134-3710; CHAN, Lai Leo/0000-0002-2755-3268	Hong Kong RGC GRF Grant [HKU7655/07M]	Hong Kong RGC GRF Grant	This work was supported by the Hong Kong RGC GRF Grant No. HKU7655/07M (J-DG). Mrs. Jessie Lai was thanked for the laboratory assistance.	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J	Hartkopf-Fröder, C; Königshof, P; Littke, R; Schwarzbauer, J				Hartkopf-Froeder, Christoph; Koenigshof, Peter; Littke, Ralf; Schwarzbauer, Jan			Optical thermal maturity parameters and organic geochemical alteration at low grade diagenesis to anchimetamorphism: A review	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Review						Vitrinite; Conodonts; Palynomorphs; Invertebrates; Thermal maturity; Organic geochemical alteration	CONODONT COLOR ALTERATION; ORDOVICIAN SOURCE ROCKS; ALTERATION INDEX CAI; VITRINITE REFLECTANCE; PALEOZOIC ROCKS; HYDROCARBON GENERATION; DINOFLAGELLATE CYSTS; MOLECULAR TAPHONOMY; BURIAL HISTORY; WALLED MICROFOSSILS	Sedimentary organic matter derives from biological precursor material which undergoes systematic, irreversible changes upon burial which mainly reflect increasing diagenetic temperatures, although other factors have also an influence. Several parameters have been established in the last decades to determine the palaeotemperature history of sedimentary rocks based on geochemical or petrographical methods. Organic matter is the most temperature-sensitive solid constituent in sedimentary rocks and vitrinite reflectance (VR), miospore and conodont colour alteration are among the most widely used optical maturity parameters. Despite tremendous interest in estimating maturity parameters in the oil generation zone as well as for high grade diagenesis and metamorphism and despite decades of research only a few of these methods have been well established and compared to each other by now. The focus of this review is on some new aspects with respect to organic matter maturation and optical palaeotemperature parameters, especially for high grade diagenesis and anchimetamorphism. Such a discussion might be a prerequisite for a better understanding of palaeotemperature assessments in different sedimentological and/or geotectonic settings and useful for different fields in applied sciences. Furthermore, suggestions for further research are discussed. (C) 2015 Elsevier B.V. All rights reserved.	[Hartkopf-Froeder, Christoph] Geol Survey North Rhine Westphalia, De Greiff Str 195, D-47803 Krefeld, Germany; [Koenigshof, Peter] Senckenberg Res Inst, D-60325 Frankfurt, Germany; [Koenigshof, Peter] Nat Hist Museum, D-60325 Frankfurt, Germany; [Littke, Ralf; Schwarzbauer, Jan] Rhein Westfal TH Aachen, Inst Geol & Geochem Petr & Coal, Energy & Mineral Resources Grp EMR, D-52056 Aachen, Germany	Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); RWTH Aachen University	Hartkopf-Fröder, C (通讯作者)，Geol Survey North Rhine Westphalia, De Greiff Str 195, D-47803 Krefeld, Germany.	hartkopf-froeder@gd.nrw.de; Peter.Koenigshof@senckenberg.de; ralf.littke@emr.rwth-aachen.de; jan.schwarzbauer@emr.rwth-aachen.de	Hartkopf-Froder, Christoph/ACK-0770-2022; Schwarzbauer, Jan/C-6682-2015; Littke, Ralf/A-6701-2016	Hartkopf-Froder, Christoph/0000-0002-1835-577X; Schwarzbauer, Jan/0000-0001-7307-9491; Littke, Ralf/0000-0003-0421-8720				Ainsworth N.R., 1987, Geological Survey of Ireland Bulletin, V4, P41; AINSWORTH NR, 1990, MAR PETROL GEOL, V7, P288, DOI 10.1016/0264-8172(90)90006-3; Al Sandouk-Lincke NA, 2013, ORG GEOCHEM, V59, P22, DOI 10.1016/j.orggeochem.2013.03.006; al Sandouk-Lincke NA, 2014, J ANAL APPL PYROL, V107, P211, DOI 10.1016/j.jaap.2014.03.004; Al-Ameri TK, 2010, ARAB J GEOSCI, V3, P155, DOI 10.1007/s12517-009-0060-2; Alabusheva A.V., 1990, INT GEOL REV, V32, P1166; Aldridge RJ, 1998, BIOLOGY OF HAGFISHES, P15; Allen K, 1999, J MICROPALAEONTOL, V18, P183, DOI 10.1144/jm.18.2.183; Allen Kathryn, 2000, Grzybowski Foundation Special Publication, V7, P1; Alpern B., 1987, MEM SOC GEOL FR, V151, P55; Amijaya H, 2006, INT J COAL GEOL, V66, P271, DOI 10.1016/j.coal.2005.07.008; [Anonymous], FOSSIL PLANTS SPORES; [Anonymous], THESIS; [Anonymous], 1980, Eclogae Geologicae Helvetiae, DOI DOI 10.5169/SEALS-164949; [Anonymous], PALAEONTOLOGIA ELECT; [Anonymous], 1964, CONODONTS; [Anonymous], 1991, GOTTINGER ARB GEOL P; Araujo CV, 2014, INT J COAL GEOL, V130, P89, DOI 10.1016/j.coal.2014.05.002; Arkai P, 2002, SCHWEIZ MINER PETROG, V82, P273; Armstrong H.A., 1987, P203; Armstrong H. 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J. Coal Geol.	OCT 1	2015	150						74	119		10.1016/j.coal.2015.06.005	http://dx.doi.org/10.1016/j.coal.2015.06.005			46	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Geology	CW5SF					2025-03-11	WOS:000365056200007
J	Triki, HZ; Laabir, M; Daly-Yahia, OK				Triki, Habiba Zmerli; Laabir, Mohamed; Daly-Yahia, Ons Kefi			LIFE HISTORY, EXCYSTMENT FEATURES, AND GROWTH CHARACTERISTICS OF THE MEDITERRANEAN HARMFUL DINOFLAGELLATE <i>ALEXANDRIUM PSEUDOGONYAULAX</i>	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium pseudogonyaulax; excystment; germling cell; growth rate; irradiance; life cycle; resting cysts; salinity	TOXIC DINOFLAGELLATE; CYST FORMATION; GONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; COASTAL WATERS; RESTING CYSTS; DINOPHYCEAE; GERMINATION; SALINITY; BLOOM	Studies considering the biology and ecology of the toxic bloom-forming species, Alexandrium pseudogonyaulax, are rare. Our results highlight five features not described before in A. pseudogonyaulax life cycle: (i) A. pseudogonyaulax gametes showed two modes of conjugation, anisogamy and isogamy, (ii) sexual conjugation occurs either in the dark or in the light phase by engulfment or a fusion process, (iii) the presence of planozygote and newly formed cysts in monoclonal culture suggests homothallism, (iv) newly formed cysts have very dark vesicular content and are mostly unparatabulated when observed under light microscope and (v) natural resting cysts are able to give either a planomeiocyte or two vegetative cells. Cyst viability was enhanced after 5 months of cold storage (4 degrees C), with excystment rate reaching 97% after 3 d of incubation. Excystment rate was highest (43%-79%) in Enriched Natural Sea Water diluted culture medium, whereas few germling cells were able to survive without the culture medium (0%-13%). Salinity-irradiance experiments revealed that the highest cell concentrations occur at high irradiances for all the tested salinities. Vegetative growth rates generally increased with increasing irradiance, and were less dependent on salinity variations. The relatively low growth rate, low cell densities in the laboratory, and the notable capacity of producing cysts along growth phases of A. pseudogonyaulax could explain the occurrence of high resting cysts densities in the sediment of Bizerte lagoon and the relatively low abundances of vegetative cells in the water column.	[Triki, Habiba Zmerli; Daly-Yahia, Ons Kefi] IRESA Carthage Univ, Tunisian Natl Agron Inst INAT, Tunis 1082, Tunisia; [Laabir, Mohamed] Univ Montpellier, CNRS, IFREMER,IRD, Ctr Marine Biodivers Exploitat & Conservat MARBEC, F-34095 Montpellier 5, France	Universite de Montpellier; Institut de Recherche pour le Developpement (IRD); Ifremer; Centre National de la Recherche Scientifique (CNRS)	Triki, HZ (通讯作者)，IRESA Carthage Univ, Tunisian Natl Agron Inst INAT, 43 Ave Charles Nicolle, Tunis 1082, Tunisia.	bibarouma@hotmail.fr		Kefi Daly Yahia, Ons/0000-0001-9532-8989	JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program - IRD (Institut Francais pour la Recherche et le Developpement); TOTAL Foundation	JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program - IRD (Institut Francais pour la Recherche et le Developpement); TOTAL Foundation(Total SA)	This study benefitted from financial supports of the JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program funded by IRD (Institut Francais pour la Recherche et le Developpement) and from LAGUNOTOX project funded by TOTAL Foundation. 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Phycol.	OCT	2015	51	5					980	989		10.1111/jpy.12337	http://dx.doi.org/10.1111/jpy.12337			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	CU1ET	26986892				2025-03-11	WOS:000363263500013
J	Gu, HF; Luo, ZH; Mertens, KN; Price, AM; Turner, RE; Rabalais, NN				Gu, Haifeng; Luo, Zhaohe; Mertens, Kenneth Neil; Price, Andrea Michelle; Turner, Robert Eugene; Rabalais, Nancy N.			CYST-MOTILE STAGE RELATIONSHIP, MORPHOLOGY, ULTRASTRUCTURE, AND MOLECULAR PHYLOGENY OF THE GYMNODINIOID DINOFLAGELLATE <i>BARRUFETA RESPLENDENS</i> COMB. NOV., FORMERLY KNOWN AS <i>GYRODINIUM RESPLENDENS</i>, ISOLATED FROM THE GULF OF MEXICO	JOURNAL OF PHYCOLOGY			English	Article						Barrufeta bravensis; cyst; Gymnodinium; Gyrodinium resplendens; LSU rDNA	LSU RDNA SEQUENCES; ALEXANDRIUM DINOPHYCEAE; ELECTRON-MICROSCOPY; MEDITERRANEAN SEA; COASTAL WATERS; MIXED MODELS; GEN. NOV.; LIGHT; SP.	In the present study, we redescribed Gyrodinium resplendens through incubation of process bearing cysts extracted from sediment collected in the northern Gulf of Mexico. The morphology and ultrastructure of the motile stage and cyst stage were examined using light microscopy, scanning electron microscopy, and transmission electron microscopy and this revealed that the species should be transferred to the genus Barrufeta. This genus differs from other gymnodinioid genera in possessing a Smurf-cap apical structure complex (ASC) and currently encompasses only one species, Barrufeta bravensis. B. resplendens shows a Smurf-cap ASC that consists of three rows of elongated vesicles with small knobs in the middle one. B. resplendens is very similar to B. bravensis in cell morphology, but can be separated using the ultrastructure such as the shape and location of nucleus and pyrenoids, which highlights the importance of ultrastructure at inter-specific level in the genus Barrufeta. The unique cysts of B. resplendens are brown and process bearing, and have a tremic archeopyle with a zigzag margin on the dorsal side of the epicyst, and not polar as in cysts of Polykrikos. The cysts do not survive the palynological treatment used here and probably have a wide distribution. Maximum-likelihood and Bayesian inference were carried out based on partial large subunit ribosomal DNA (LSU rDNA) sequences. Molecular phylogeny supports that the genus Barrufeta is monophyletic, and that the genus Gymnodinium is polyphyletic. Our results suggest that details of the ASC together with ultrastructure are potential features to subdivide the genus Gymnodinium.	[Gu, Haifeng; Luo, Zhaohe] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Price, Andrea Michelle] McGill Univ, Dept Geog, Montreal, PQ H3A OB9, Canada; [Turner, Robert Eugene] Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA; [Rabalais, Nancy N.] Louisiana Univ Marine Consortium, Chauvin, LA 70344 USA	Third Institute of Oceanography, Ministry of Natural Resources; Ghent University; Louisiana State University System; Louisiana State University	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Mertens, Kenneth/AAO-9566-2020; Luo, Zhaohe/ITT-7163-2023; Rabalais, Nancy/GQA-6087-2022; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022	Luo, Zhaohe/0000-0001-8662-2414; Price, Andrea/0000-0002-5359-053X; Mertens, Kenneth/0000-0003-2005-9483; Gu, Haifeng/0000-0002-2350-9171; Rabalais, Nancy N./0000-0002-1514-837X	National Natural Science Foundation of China [41376170]; Natural Science and Engineering Research Council of Canada (NSERC); National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research [NA09NOS4780204, NA09NOS4780230]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research(National Oceanic Atmospheric Admin (NOAA) - USA)	Haifeng Gu was supported by National Natural Science Foundation of China (41376170). Kenneth Neil Mertens is a post-doctoral fellow of FWO Belgium. Andrea M. Price was supported by a Natural Science and Engineering Research Council of Canada (NSERC) graduate scholarship. Sample collection was supported by the National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research, under awards NA09NOS4780204 to Louisiana Universities Marine Consortium and award NA09NOS4780230 to Louisiana State University. Anne de Vernal is acknowledged to let us use the facilities at GEOTOP (Montreal). We thank two anonymous reviewers for constructive suggestions that improved the manuscript.	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OCT	2015	51	5					990	999		10.1111/jpy.12342	http://dx.doi.org/10.1111/jpy.12342			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	CU1ET	26986893				2025-03-11	WOS:000363263500014
J	Candel, MS				Soledad Candel, Maria			First record of <i>Palaeostomocystis</i> <i>subtilitheca</i> in Holocene marine sediments from the Beagle Channel, southern Tierra del Fuego, Argentina	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Acritarch; Marine environment; Holocene; Beagle Channel; Southern Hemisphere	BAHIA-BLANCA ESTUARY; DINOFLAGELLATE CYSTS; PALYNOFACIES ANALYSIS; BUENOS-AIRES; ACRITARCHS; SEA; PALYNOLOGY	This study documents the occurrence of Palaeostomocystis subtilitheca in Holocene sediments from the Beagle Channel area, southern Argentina, and represents the first record of this acritarch in high latitudes of the Southern Hemisphere. P. subtilitheca is considered as an indicator for polar to subpolar environments with high planktonic productivity and nutrient-rich waters and can probably be associated with low-salinity stratified waters. The Beagle Channel presents environmental characteristics similar to those reported by other authors in Central West Greenland and the Faroe Islands, characterized by high concentrations of nutrients in the surface waters. The Beagle Channel constitutes a favourable environment for the development of this species in subpolar regions of the Southern Hemisphere. (C) 2015 Elsevier B.V. All rights reserved.	Ctr Austral Invest Cient CADIC CONICET, RA-9410 Ushuaia, Tierra Del Fueg, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Candel, MS (通讯作者)，Ctr Austral Invest Cient CADIC CONICET, Bernardo Houssay 200, RA-9410 Ushuaia, Tierra Del Fueg, Argentina.	soledadcandel@cadic-conicet.gob.ar			CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas) [PIP 02787/02, PIP 11220100100041]	CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET))	The author is grateful to Dr. Mirta Quattrocchio and Dr. Ana Maria Borromei (INGEOSUR-CONICET, Universidad Nacional del Sur) for the critical reading on an earlier version of the manuscript. I wish to thank too Dr. Shinya Sugita and two anonymous reviewers for their constructive comments that helped to improve the final version of the manuscript. This study was supported by CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas), PIP 02787/02 and PIP 11220100100041 grants to Dr. Mirta Quattrocchio and Dr. Ana Maria Borromei, respectively.	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J	Olde, K; Jarvis, I; Ulicny, D; Pearce, MA; Trabucho-Alexandre, J; Cech, S; Gröcke, DR; Laurin, J; Svábenická, L; Tocher, BA				Olde, Kate; Jarvis, Ian; Ulicny, David; Pearce, Martin A.; Trabucho-Alexandre, Joao; Cech, Stanislav; Grocke, Darren R.; Laurin, Jiri; Svabenicka, Lilian; Tocher, Bruce A.			Geochemical and palynological sea-level proxies in hemipelagic sediments: A critical assessment from the Upper Cretaceous of the Czech Republic	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Sea-level change; Cretaceous; Chemostratigraphy; Palynology; Dinoflagellate cysts	WESTERN INTERIOR BASIN; CENOMANIAN-TURONIAN BOUNDARY; CARBON-ISOTOPE STRATIGRAPHY; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SEQUENCE STRATIGRAPHY; PALEOENVIRONMENTAL CHANGE; PELAGIC CARBONATES; CONTINENTAL-MARGIN; TERTIARY BOUNDARY; SHALLOW-MARINE	Geochemical and palynological records are presented for an expanded Turonian-Coniacian hemipelagic succession in the central Bohemian Cretaceous Basin. A high-resolution stratigraphic framework is provided by biostratigraphy and organic carbon stable-isotope (delta C-13(org)) chemostratigraphy. A short-term (100 kyr) sea-level curve has been derived from high-resolution transgressive/regressive maxima / shore-proximity data established from basin-wide sediment geometries. The viability of geochemical and palynological parameters as potential sea-level proxies is tested against this independently derived sea-level record. Elemental chemostratigraphy is demonstrated to offer a reliable means of identifying medium- to long-term (0.4-2.4 Myr) sea-level trends. Manganese maxima are associated with periods of high sea level, and troughs with intervals of low sea level. Falling Mn contents accompany regression and rising values transgression. Major transgressive events associated with medium-term sea-level change are marked by sharp increases in Ti/Al ratios, but short-term (100 kyr) sea-level cycles are not consistently identified. Long-term delta C-13(org) variation and dinoflagellate cyst species richness are positively correlated and show similarities to the sea-level curve. Baseline trends have a cycle duration close to the 2.4 Myr long-eccentricity cycle. Dinocyst species richness closely follows short-term changes in sea level, with marked increases in dinocyst diversity coincident with most short-term flooding events. Periods of rapid sea-level rise caused an influx of a more diverse 'outer shelf' assemblage into the study area, together with the addition of shallower water species, some of which may have been transported into the central basin by hypopycnal flows. Changes in the proportion and abundance of peridinioid dinoflagellate cysts (principally Palaeohystrichophora infusorioides) were controlled principally by changing nutrient levels. Proximity proxies derived from geochemical and palynological data are not always consistent with the independent sea-level model. This exemplifies the need to understand all factors influencing elemental geochemical and palynological proxies before making simplistic sea level interpretations. (C) 2015 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).	[Olde, Kate; Jarvis, Ian] Kingston Univ London, Sch Geog Geol & Environm, Ctr Earth & Environm Sci Res, Kingston Upon Thames KT1 2EE, Surrey, England; [Ulicny, David; Laurin, Jiri] Acad Sci Czech Republ, Inst Geophys, CR-14131 Prague, Czech Republic; [Pearce, Martin A.] Evolut Appl Ltd, Cheltenham GL54 2PL, Glos, England; [Trabucho-Alexandre, Joao] Univ Durham, Dept Earth Sci, Durham DH1 3LE, England; [Trabucho-Alexandre, Joao; Grocke, Darren R.] Inst Earth Sci, NL-3584 CD Utrecht, Netherlands; [Cech, Stanislav; Svabenicka, Lilian] Czech Geol Survey, Prague 11821, Czech Republic; [Tocher, Bruce A.] STATOIL, Houston, TX 77042 USA	Kingston University; Czech Academy of Sciences; Institute of Geophysics of the Czech Academy of Sciences; Durham University; Czech Geological Survey; Equinor	Jarvis, I (通讯作者)，Kingston Univ London, Sch Geog Geol & Environm, Ctr Earth & Environm Sci Res, Kingston Upon Thames KT1 2EE, Surrey, England.	i.jarvis@kingston.ac.uk	Alexandre, João/AAT-5878-2020; Uličný, David/H-6412-2014; Laurin, Jiri/H-6396-2014; Jarvis, Ian/A-1637-2008; Grocke, Darren R./F-4799-2015	Pearce, Martin/0000-0001-7856-1076; Laurin, Jiri/0000-0001-6674-1117; Trabucho Alexandre, Joao/0000-0003-1997-027X; Jarvis, Ian/0000-0003-3184-3097; Ulicny, David/0000-0002-0331-4174; Grocke, Darren R./0000-0003-2296-7530	Statoil Petroleum AS [4501936147]; Kingston University London; UK Natural Environment Research Council (NERC) [NE/H020756/1, NE/H021868/1]; Czech Science Foundation (GACR) [P210/10/1991]; Academy of Sciences of the Czech Republic [AV0Z30120515]; NERC [NE/H021868/1, NE/H020756/1] Funding Source: UKRI	Statoil Petroleum AS; Kingston University London; UK Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Czech Science Foundation (GACR)(Grant Agency of the Czech Republic); Academy of Sciences of the Czech Republic(Czech Academy of Sciences); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	Insightful reviews by Finn Surlyk and an anonymous referee enabled improved presentation of this work. KO was supported by Statoil Petroleum AS contract 4501936147 and Kingston University London. IJ and DRG acknowledge funding by UK Natural Environment Research Council (NERC) grants NE/H020756/1 and NE/H021868/1. This research was supported by the Czech Science Foundation (GACR) grant P210/10/1991 and research programme AV0Z30120515 of the Academy of Sciences of the Czech Republic.	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Paleoclimatol. Paleoecol.	OCT 1	2015	435						222	243		10.1016/j.palaeo.2015.06.018	http://dx.doi.org/10.1016/j.palaeo.2015.06.018			22	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	CP5ZG		Green Accepted, Green Published, hybrid			2025-03-11	WOS:000359963500020
J	Narale, DD; Naidu, PD; Anil, AC; Godad, SP				Narale, Dhiraj Dhondiram; Naidu, Pothuri Divakar; Anil, Arga Chandrashekar; Godad, Shital P.			Evolution of productivity and monsoonal dynamics in the eastern Arabian Sea during the past 68 ka using dinoflagellate cyst records	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Eastern Arabian Sea; Monsoons; Productivity; Marine isotopic stages; Dinoflagellate cyst	SURFACE SEDIMENTS; INDIAN-OCEAN; QUATERNARY; GULF; PRESERVATION; TEMPERATURE; VARIABILITY; INDICATORS; SALINITY; DENITRIFICATION	For the first time here we report the dinoflagellate cyst assemblage response to the monsoon variability over the last 68 ka from the Eastern Arabian Sea (EAS). Based on the cyst assemblage, five dinoflagellate cyst zones were established, corresponding to four Marine Isotopic Stages (MIS 1-4). An increased abundance of autotrophic Gonyaulacoid species (especially Spiniferites) during glacials (MIS 2 and 4) and late MIS 3 (similar to 41.67 to 25.3 ka) reflects high productivity driven by strong winter convection during the Northeast monsoon. In contrast, their decreased abundance during MIS 1 and early MIS 3 (similar to 58.6 to 42.87 ka) reveals decrease in productivity due to strong stratification caused by intense monsoon precipitation induced runoff from the Western Ghats and reduced light penetration driven by cloud cover. The variation in heterotrophic Protoperidinium species abundance could be related to variation in the Oxygen Minimum Zone (OMZ) intensity, with better preservation during intense OMZ in MIS 3 and the late Holocene (similar to 3 ka onwards). Therefore, it is proposed here that the abundance of Protoperidinium can be used as an index of OMZ in the LAS. (C) 2015 Elsevier B.V. All rights reserved.	[Narale, Dhiraj Dhondiram; Naidu, Pothuri Divakar; Anil, Arga Chandrashekar; Godad, Shital P.] CSIR Natl Inst Oceanog, Panaji 403004, Goa, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO)	Naidu, PD (通讯作者)，CSIR Natl Inst Oceanog, Panaji 403004, Goa, India.	divakar@nio.org	Naidu, Pothuri/AAH-1613-2019		CSIR	CSIR(Council of Scientific & Industrial Research (CSIR) - India)	We are grateful to the Director, CSIR-National Institute of Oceanography (NI), India for his support. We thank Dr. Paropakari, CSIR-NIO, India for sharing the core samples; Dr. Kenneth Neil Mertens, Ghent University, Belgium and Dr. Malte Elbrachter, AWI, Germany for the dinoflagellate cyst identification training course and for providing taxonomic literature. D.D.N. is grateful to CSIR for awarding the Senior Research Fellowship (SRF) and DST-SERB for International Travel Support Scheme. This is a NIO contribution (no. 5770).	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OCT 1	2015	435						193	202		10.1016/j.palaeo.2015.06.006	http://dx.doi.org/10.1016/j.palaeo.2015.06.006			10	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	CP5ZG					2025-03-11	WOS:000359963500017
J	Antonioli, L; Távora, VD; Dino, R				Antonioli, Luzia; de Araujo Tavora, Vladimir; Dino, Rodolfo			Palynology of carcinolites and limestones from the Baunilha Grande Ecofacies of the Pirabas Formation (Miocene of Para state, northeastern Brazil)	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Brazil; Carcinolites; Miocene; Palynology; Pirabas Formation	DECAPOD CRUSTACEA; COMMUNITIES; TERTIARY; AMAZONIA; FACIES; BASIN	The Pirabas Formation records important transgressive/regressive marine events in northern Brazil during the Miocene. Here, we present the results of a palynological analysis of four samples from finely stratified gray limestone and associated carbonate concretions bearing decapod crustacean remains. These sampled strata are representatives of the Baunilha Grande Ecofacies, and our analysis enhances the knowledge of local biostratigraphy and paleoecology. The palynoflora is dominated by taxa typical of Neogene tropical areas, such as Zonocostites ramonae (the most common species), together with Retitricolpites and Retitricolporites genera. Commonly represented are the smooth and apiculate trilete/monolete spores (Polypodiisporites, Verrucosisporites, Magnastriatites, and Deltoidospora), in conjunction with some freshwater algae (Ovoidites and Botryococcus). Gymnosperm pollen grains were absent. Marine microplankton (dinoflagellate cysts, acritarchs and foraminiferal test linings) are scarce, although present in all samples. The presence of the index species, Malvacipolloides maristellae and Pachydermites diederixii, co-occurring with Zonocostites ramonae and Lanagiopollis crassa, suggests that these sediments and concretions belong to the "T-13 Malvacipolloides matistellae" palynozone (Jaramillo et al., 2011), considered as late-Early Miocene in age. Palynological and sedimentological evidence further points to a predominantly continental depositional environment with a weak marine influence, as indicated by the persistent presence of sparse dinoflagellate cysts, acritarchs and foraminiferal test linings, typical of a mangrove environment. (c) 2015 Elsevier Ltd. All rights reserved.	[Antonioli, Luzia; Dino, Rodolfo] Univ Estado Rio de Janeiro, Dept Stratig & Paleontol, BR-20550900 Rio De Janeiro, RJ, Brazil; [de Araujo Tavora, Vladimir] Fed Univ Para, Dept Geol, BR-66059 Belem, Para, Brazil; [Dino, Rodolfo] Petrobras Cenpes PDEDS, BR-21941598 Rio De Janeiro, RJ, Brazil	Universidade do Estado do Rio de Janeiro; Universidade Federal do Para	Antonioli, L (通讯作者)，Univ Estado Rio de Janeiro, Dept Stratig & Paleontol, Rua Sao,Francisco Xavier 524, BR-20550900 Rio De Janeiro, RJ, Brazil.	luziaa@uerj.br; vtavora@orm.com.br; dino@petrobras.com.br	Dino, Rodolfo/AAD-2105-2021; Antonioli, Luzia/AAC-9679-2021					Aguilera Orangel, 2013, Swiss Journal of Palaeontology, V132, P99, DOI 10.1007/s13358-013-0051-5; Amador E.S., 1982, C BRAS GEOL 23 SLAV, V23, P1451; [Anonymous], [No title captured]; [Anonymous], 1974, B TEC PETROBRAS; [Anonymous], [No title captured]; [Anonymous], [No title captured]; Arai M., 1994, S GEOL AM BEL SBG NA, V4, P185; Bistrichi C.A., 2007, Paleontologia: Cenarios de Vida, P689; BRITO IM, 1971, AN ACAD BRAS CIENC, V43, P489; BRITO IM, 1972, AN ACAD BRAS CIENC, V44, P95; CONCHEYRO GA, 1992, AN ACAD BRAS CIENC, V64, P421; Costa J. 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Queen., P51; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zalan P.V., 2007, Geociencias da Petrobras, V15, P341	88	18	18	0	12	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811			J S AM EARTH SCI	J. South Am. Earth Sci.	OCT	2015	62						134	147		10.1016/j.jsames.2015.05.005	http://dx.doi.org/10.1016/j.jsames.2015.05.005			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CN5IF					2025-03-11	WOS:000358462300010
J	Genovesi, B; Berrebi, P; Nagai, S; Reynaud, N; Wang, JH; Masseret, E				Genovesi, Benjamin; Berrebi, Patrick; Nagai, Satoshi; Reynaud, Nathalie; Wang, Jinhui; Masseret, Estelle			Geographic structure evidenced in the toxic dinoflagellate <i>Alexandrium pacificum</i> Litaker (<i>A</i>. <i>catenella</i> - group IV (Whedon & Kofoid) Balech) along Japanese and Chinese coastal waters	MARINE POLLUTION BULLETIN			English	Article						Alexandrium pacificum (A. catenella - group IV); Toxic dinoflagellate; Harmful algal blooms; Invasive species distribution; Temperate Asian coasts; Microsatellites markers	HARMFUL ALGAL BLOOMS; SHELLFISH POISONING TOXINS; SETO-INLAND-SEA; MICROSATELLITE MARKERS; GENETIC DIFFERENTIATION; TAMARENSE DINOPHYCEAE; SPATIAL-DISTRIBUTION; RESTING CYSTS; POPULATION; BAY	The intra-specific diversity and genetic structure within the Alexandrium pacificum Litaker (A. catenella - Group IV) populations along the Temperate Asian coasts, were studied among individuals isolated from Japan to China. The UPGMA dendrogram and FCA revealed the existence of 3 clusters. Assignment analysis suggested the occurrence of gene flows between the Japanese Pacific coast (cluster-1) and the Chinese Zhejiang coast (cluster-2). Human transportations are suspected to explain the lack of genetic difference between several pairs of distant Japanese samples, hardly explained by a natural dispersal mechanism. The genetic isolation of the population established in the Sea of Japan (cluster-3) suggested the existence of a strong ecological and geographical barrier. Along the Pacific coasts, the South North current allows limited exchanges between Chinese and Japanese populations. The relationships between Temperate Asian and Mediterranean individuals suggested different scenario of large-scale dispersal mechanisms. (C) 2015 Published by Elsevier Ltd.	[Genovesi, Benjamin; Nagai, Satoshi; Reynaud, Nathalie] Res Ctr Environm Conservat, Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan; [Genovesi, Benjamin; Berrebi, Patrick; Reynaud, Nathalie] Univ Montpellier, Inst Sci Evolut, UMR UM CNRS IRD 5554, F-34095 Montpellier 05, France; [Nagai, Satoshi] Natl Res Inst Fisheries Sci, Aquat Genom Res Ctr, Kanazawa Ku, Yokohama, Kanagawa 2368648, Japan; [Wang, Jinhui] East China Sea Environm Monitoring Ctr, Shanghai 200137, Peoples R China; [Masseret, Estelle] Univ Montpellier, UMR MARBEC IRD Ifremer UM CNRS 9190, F-34095 Montpellier 5, France	Japan Fisheries Research & Education Agency (FRA); Universite de Montpellier; Japan Fisheries Research & Education Agency (FRA); Universite de Montpellier; Ifremer	Masseret, E (通讯作者)，Univ Montpellier, UMR MARBEC IRD Ifremer UM CNRS 9190, Cc93,Pl Eugene Bataillon, F-34095 Montpellier 5, France.	estelle.masseret@univ-montp2.fr	Nagai, Satoshi/HOA-8686-2023; jinhui, wang/JMC-9435-2023	Nagai, Satoshi/0000-0001-7510-0063; Masseret, Estelle/0000-0001-6856-8637	Japan Society for the Promotion of Science (JSPS) [19380116, PE08002]; Region Languedoc-Roussillon; Programme National d'Environnement Coder (PNEC-France); Grants-in-Aid for Scientific Research [19380116] Funding Source: KAKEN	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); Region Languedoc-Roussillon(Region OccitanieRegion Ile-de-France); Programme National d'Environnement Coder (PNEC-France); 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 supported by a Grant-in-Aid for Scientific Research (Kiban-B, No. 19380116) from the Japan Society for the Promotion of Science (JSPS) and a post-doctoral fellowship from the JSPS (No. PE08002). The Region Languedoc-Roussillon (through a Ph.D. fellowship granted to GB) and the Programme National d'Environnement Cotier (PNEC-France) have financially supported sampling in France in 2004. Authors thank IFREMER Sete LER/LR for its assistance and logistic support at sea in France. The authors specially thank Daniel Grzebyk for his valuable support for the submission of the post-doctoral project to the JSPS and his helpful comments on an early version of the manuscript. Finally, we are gratefull to the anonymous reviewer who helped us to improve this manuscript.	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Pollut. Bull.	SEP 15	2015	98	1-2					95	105		10.1016/j.marpolbul.2015.07.009	http://dx.doi.org/10.1016/j.marpolbul.2015.07.009			11	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	CS5QW	26188429				2025-03-11	WOS:000362134100023
J	Zonneveld, KAF; Pospelova, V				Zonneveld, Karin A. F.; Pospelova, Vera			A determination key for modern dinoflagellate cysts	PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; late Quaternary; identification key	SEDIMENTS; DINOPHYCEAE; THECA	The first online modern organic-walled dinoflagellate cyst determination key has been launched at www.marum.de/dinocystkey.html. This key is based on easily recognisable morphological features of dinoflagellate cysts that can be observed using standard transmitted light microscopy. To date, the key includes 96 cyst species that can be found in late Quaternary marine sediments. This key is free of charge to users, and will be continuously updated and improved by the authors. For each individual species of dinoflagellate cyst, the website provides information on its defining morphological characteristics and the cyst-motile stage relationship. It gives a comparison with other morphologically similar taxa, links to publications with original cyst descriptions and outlines their modern global distribution where this information is available. All species descriptions are illustrated by line drawings showing their most distinctive characteristics, and accompanied by high-quality bright-field photomicrographs. The key is compatible with all major computing platforms (including smartphones) and software.	[Zonneveld, Karin A. F.] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, Victoria, BC, Canada	University of Bremen; University of Victoria	Zonneveld, KAF (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, FB 5 Geowissensch,Postfach 330440, D-28334 Bremen, Germany.			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 the MARUM Information Technology (IT) services team who made the online posting of this key possible, and for their technical support. We are very grateful to Martin Head, Ian Harding and James Riding for their constructive comments and suggestions. Partial funding for this work was provided to VP by the Natural Sciences and Engineering Research Council of Canada (NSERC).	Bravo Isabel, 2014, Microorganisms, V2, P11; Casas-Monroy O, 2013, AQUAT CONSERV, V23, P254, DOI 10.1002/aqc.2310; Dale B, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; Hoppenrath M., 2009, KL SENCKENBERG-REIHE, V49, P264; Kawami H, 2009, PHYCOL RES, V57, P259, DOI 10.1111/j.1440-1835.2009.00545.x; Krepakevich A, 2010, CONT SHELF RES, V30, P1924, DOI 10.1016/j.csr.2010.09.002; Lewis J, 2013, GLOBAL MEDIA APOCALYPSE: PLEASURE, VIOLENCE AND THE CULTURAL IMAGININGS OF DOOM, P1; Lundholm N, 2011, PHYCOLOGIA, V50, P629, DOI 10.2216/11-16.1; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Mertens KN, 2012, MAR MICROPALEONTOL, V96-97, P48, DOI 10.1016/j.marmicro.2012.08.002; Mertens KN, 2012, REV PALAEOBOT PALYNO, V184, P74, DOI 10.1016/j.revpalbo.2012.06.012; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Price AM, 2014, PALYNOLOGY, V38, P101, DOI 10.1080/01916122.2013.864341; Ribeiro S, 2010, PHYCOLOGIA, V49, P48, DOI 10.2216/09-11.1; Rochon A, 1999, AM ASS STRATIGR PALY, V35; Satta CT, 2010, DEEP-SEA RES PT II, V57, P256, DOI 10.1016/j.dsr2.2009.09.013; Shin HH, 2010, MAR POLLUT BULL, V60, P1243, DOI 10.1016/j.marpolbul.2010.03.019; Taylor FJR, 2008, BIODIVERS CONSERV, V17, P407, DOI 10.1007/s10531-007-9258-3; Verleye TJ, 2011, MAR MICROPALEONTOL, V78, P65, DOI 10.1016/j.marmicro.2010.10.001; Zonneveld KAF, 1997, REV PALAEOBOT PALYNO, V97, P319, DOI 10.1016/S0034-6667(97)00002-X; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003; Zonneveld KAF, 2012, MAR POLLUT BULL, V64, P114, DOI 10.1016/j.marpolbul.2011.10.012	22	129	133	0	22	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	SEP 2	2015	39	3					387	409		10.1080/01916122.2014.990115	http://dx.doi.org/10.1080/01916122.2014.990115			23	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	CT1HU					2025-03-11	WOS:000362550100005
J	Thomas, ML; Pocknall, DT; Warny, S; Bentley, SJ; Droxler, AW; Nittrouer, CA				Thomas, Marie Louise; Pocknall, David T.; Warny, Sophie; Bentley, Samuel J., Sr.; Droxler, Andre W.; Nittrouer, Charles A.			Assessing palaeobathymetry and sedimentation rates using palynomaceral analysis: a study of modern sediments from the Gulf of Papua, offshore Papua New Guinea	PALYNOLOGY			English	Article						Gulf of Papua; Quaternary; palynomacerals; principal component analysis (PCA); southeast Asia; tropics; sedimentation	WALLED DINOFLAGELLATE CYSTS; PALYNOFACIES ANALYSIS; HOLOCENE SEDIMENTS; FLY RIVER; MARGIN; BASIN; PALYNOSTRATIGRAPHY; RECONSTRUCTION; PRESERVATION; MISSISSIPPI	Palynologists interested in better understanding the sedimentation and energy of depositional environments have often included studies of palynomaceral fragments, particularly when performing palynofacies analyses. Due to the difficult nature of classifying these fragments, researchers have developed numerous, often overlapping, classification schemes. These different schemes make it difficult to compare and contrast between research projects. Determining the appropriate scheme to apply when counting these fragments can be confusing, and application of these schemes can yield inconclusive results, especially when sedimentation and energy are in constant flux. A scheme of five categories, including brown wood (palynomaceral 1-2), leaf cuticle (palynomaceral 3), black debris (palynomaceral 4), structureless organic matter (SOM) and resin, is utilised here. It is applied to the analysis of 64 modern samples from the top 0-4 cm of sediment collected throughout the Gulf of Papua, Papua New Guinea. These samples span a suite of common marine depositional environments: river mouths and deltas, the proximal portion of the continental shelf dominated by a large clinoform, and turbidite and hemipelagic/pelagic deposits on the slope and in the deep ocean basin. Principal component analysis (PCA) confirms this simplified classification scheme provides an indirect means of assessing distance from shore and shelf-slope break, overall water depth and sediment accumulation rate, but other factors, such as processing technique, marine productivity, sediment source, time in transport and residence and bioturbation, are taken into account to fully explain distribution.	[Thomas, Marie Louise; Bentley, Samuel J., Sr.] Louisiana State Univ, Geol & Geophys, Baton Rouge, LA 70803 USA; [Pocknall, David T.] Hess Corp, Technol & Excellence, Houston, TX 77010 USA; [Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA; [Droxler, Andre W.] Rice Univ, Dept Earth Sci, Houston, TX 77005 USA; [Nittrouer, Charles A.] Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA	Louisiana State University System; Louisiana State University; Hess Corporation; Louisiana State University System; Louisiana State University; Rice University; University of Washington; University of Washington Seattle	Thomas, ML (通讯作者)，Louisiana State Univ, Geol & Geophys, E235 Howe Russell Geosci Complex, Baton Rouge, LA 70803 USA.	mlthomas716@yahoo.com	Warny, Sophie/A-8226-2013	Bentley, Samuel/0000-0001-5826-7689; Warny, Sophie/0000-0002-3451-040X	National Science Foundation (NSF); Marathon GeoDE (Geoscience Diversity Enrichment) Fellowship; AASP-The Palynological Society; Encana	National Science Foundation (NSF)(National Science Foundation (NSF)); Marathon GeoDE (Geoscience Diversity Enrichment) Fellowship; AASP-The Palynological Society; Encana	The samples for this work were obtained through the MARGINS Source-to-Sink (S2S) Focus Initiative funded by the National Science Foundation (NSF). The Marathon GeoDE (Geoscience Diversity Enrichment) Fellowship provided funding for this project, including travel to core curation sites, sample processing, and analysis. The authors would also like to thank AASP-The Palynological Society and Encana for additional scholarships supporting this research. We would also like to thank the reviewers for their in-depth reviews which helped improve the paper.	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J	Williams, GL; Damassa, SP; Fensome, RA; Guerstein, GR				Williams, Graham L.; Damassa, Sarah P.; Fensome, Robert A.; Guerstein, G. Raquel			<i>Wetzeliella</i> and its allies - the 'hole' story: a taxonomic revision of the Paleogene dinoflagellate subfamily Wetzelielloideae	PALYNOLOGY			English	Article						biostratigraphy; dinoflagellate cysts; evolution; Paleogene; taxonomy; wetzelielloideans	EOCENE; CYSTS; BIOSTRATIGRAPHY; PALEOCENE; EISENACK; ENGLAND	Fossil dinoflagellate cysts of the Paleogene peridiniacean subfamily Wetzelielloideae have a stable tabulation pattern similar to that of other fossil peridiniaceans, but distinguished by a four-sided (quadra) rather than a six-sided (hexa) 2a plate. Aside from tabulation, wetzelielloideans show great morphological variability, especially in ornamentation and horn development, but also in wall structure. This diversity has distracted attention from the morphological variation of the archeopyle, which, although always formed through loss of the 2a plate only, shows variations that we consider critical in unravelling the group's phylogeny. Important factors are the shape and relative dimensions of the archeopyle and whether the operculum is attached (adnate) or detached. These parameters allow us to define five archeopyle types: equiepeliform, hyperepeliform, hypersoleiform, latiepeliform and soleiform. Based primarily on archeopyle type and secondarily on wall morphology and ornamentation, we recognise six genera with an equiepeliform archeopyle, four with a hyperepeliform archeopyle, five with a latiepeliform archeopyle, five with a soleiform archeopyle and one with a hypersoleiform archeopyle. The earliest known wetzelielloideans, which occur around the Paleocene-Eocene boundary, have an equiepeliform archeopyle. Other archeopyle types evolved rapidly: taxa with hyperepeliform, latiepeliform and hypersoleiform types are known from the Ypresian. Latiepeliform and hyperepeliform types are restricted to the Ypresian and Lutetian. Forms with the soleiform archeopyle appeared in the late Lutetian, but were rare until the Bartonian, when they became the dominant type, and they were the only type in Priabonian and younger strata. Wetzelielloideans became extinct in the middle Oligocene. We make numerous taxonomic proposals, including the following new genera: Castellodinium, Dolichodinium, Epelidinium, Kledodinium, Michouxdinium, Petalodinium, Piladinium, Rhadinodinium, Sagenodinium, Sophismatia, Stenodinium, Stichodinium and Vallodinium. We emend the diagnoses of Charlesdowniea, Dracodinium and Wilsonidium, and erect the species Kledodinium filosum, Petalodinium sheppeyense and Sagenodinium franciscanum.	[Williams, Graham L.; Fensome, Robert A.] Bedford Inst Oceanog, Nat Resources Canada, Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Guerstein, G. Raquel] Univ Nacl Sur, Dept Geol, Lab Palinol INGEOSUR, RA-8000 Bahia Blanca, Buenos Aires, Argentina	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Fensome, RA (通讯作者)，Bedford Inst Oceanog, Nat Resources Canada, Geol Survey Canada Atlantic, POB 1006, Dartmouth, NS B2Y 4A2, Canada.	rfensome@nrcan.gc.ca		Guerstein, G. Raquel/0000-0003-1623-1084	Geological Survey of Canada, part of the Earth Sciences Sector (ESS) of Natural Resources Canada [20140222]	Geological Survey of Canada, part of the Earth Sciences Sector (ESS) of Natural Resources Canada(Natural Resources Canada)	A paper of this kind relies on support from many colleagues, and to this end, we are grateful for the help provided, especially in the provision of images, by Graham Dolby, Alina Iakovleva, Dan Michoux, Henrik Nohr-Hansen and Jo Prebble. GLW is also grateful to colleagues who have shared images with him over the years. We thank Bill MacMillan for his expert help with the drafting of some of the figures, and Nelly Koziel for technical assistance. Jen Galloway and Peta Mudie read early versions of the manuscript and provided suggestions for its improvement, for which we are grateful. We greatly appreciate the input of reviewers Chris Clowes and Alina Iakovleva, who provided perceptive insights that resulted in considerable improvements to the manuscript. We are additionally grateful to Alina for providing information on zonations involving wetzeliellioideans published in Russian. We are appreciative of helpful suggestions from Martin Pearce. Last but not least, thanks to editor Jim Riding for his advice and encouragement. GLW and RAF are grateful for the support of the Geological Survey of Canada, part of the Earth Sciences Sector (ESS) of Natural Resources Canada, for support. 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J	Estebenet, MSG; Guerstein, GR; Casadío, S				Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.; Casadio, Silvio			BIOSTRATIGRAPHIC AND PALEOENVIRONMENTAL STUDY OF RIO TURBIO FORMATION (MIDDLE-UPPER EOCENE) IN SOUTHWEST OF PATAGONIA (ARGENTINA) BASED ON DINOFLAGELLATE CYSTS	REVISTA BRASILEIRA DE PALEONTOLOGIA			Spanish	Article						dinoflagellate cysts; middle-late Eocene; Drake Passage; biostratigraphy; paleoenvironment	SANTA-CRUZ PROVINCE; TIERRA-DEL-FUEGO; SOUTHERN-OCEAN; DRAKE PASSAGE; SEA; RECONSTRUCTIONS; STRATIGRAPHY; CIRCULATION; ANTARCTICA; GREENHOUSE	During the middle and late Eocene the Austral Basin, in southern Patagonia (Argentina), was flooded by an Atlantic Ocean transgression, which was responsible for the deposition of the upper member of the Rio Turbio Formation. We have analyzed the dinoflagellate cyst assemblages from this stratigraphic section in order to provide a biostratigraphic framework and reconstruct the paleogeographic and paleoceanographic conditions in this area. Dinoflagellate cyst events recorded were compared and interpreted based taking into account other records recognized for the South Pacific Ocean. The comparison allowed us to suggest an age between 45.5 Ma (mid-Lutetian) and 33.5 Ma (Priabonian) for the upper member of the Rio Turbio Formation. We recognized three zones of dinoflagellate cysts. Zone I presents an alternating dominance between Enneadocysta dictyostila, Deflandrea antarctica and Vozzhennikovia apertura indicating two sea level rises. Zone II is dominated by V apertura suggesting high trophic levels and cool waters in a shallow-marine coastal environment. The lower part of the Zone III shows a high abundance of Turbiosphaera filosa with different morphotypes, which may correspond to physicochemical changes in the water column. The uppermost part of the Zone III is characterized by Protoperidinaceae and typical forms of T. filosa suggesting an oceanic environment influenced by upwelling processes. Zones I and II are defined by the dominance of middle Eocene endemic-Antarctic assemblage, while Zone III shows a significant replacement of these taxa by cosmopolitan species. This turnover seems to be forced by the deepening of the Southern Atlantic Ocean gateways and the changes in the ocean circulation patterns.	[Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.] Univ Nacl Sur, CONICET, Dept Geol, Inst Geol Sur, San Juan 670,B80001CN Bahia Blanca, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Casadio, Silvio] Univ Nacl Rio Negro, CONICET, RA-8332 General Roca, Rio Negro, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Estebenet, MSG (通讯作者)，Univ Nacl Sur, CONICET, Dept Geol, Inst Geol Sur, San Juan 670,B80001CN Bahia Blanca, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	sol.gonzalezestebenet@uns.edu.ar; raquel.guerstein@uns.edu.ar; scasadio@conicet.gov.ar						ARCHANGELSKY S, 1969, Ameghiniana, V6, P181; Archangelsky S., 1968, Ameghiniana, V5, P406; Arguijo M. H., 1981, ACT 8 C GEOL ARG, V4, P691; Biddle K., 1986, Assoc. 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Paleontol.	SEP-DEC	2015	18	3					429	442		10.4072/rbp.2015.3.08	http://dx.doi.org/10.4072/rbp.2015.3.08			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DC3LY		Green Published, Bronze			2025-03-11	WOS:000369122000008
J	Popescu, SM; Dalibard, M; Suc, JP; Barhoun, N; Melinte-Dobrinescu, MC; Bassetti, MA; Deaconu, F; Head, MJ; Gorini, C; Do Couto, D; Rubino, JL; Auxietre, JL; Floodpage, J				Popescu, Speranta-Maria; Dalibard, Mathieu; Suc, Jean-Pierre; Barhoun, Nadia; Melinte-Dobrinescu, Mihaela-Carmen; Bassetti, Maria Angela; Deaconu, Florina; Head, Martin J.; Gorini, Christian; Do Couto, Damien; Rubino, Jean-Loup; Auxietre, Jean-Luc; Floodpage, Jonathan			Lago Mare episodes around the Messinian-Zanclean boundary in the deep southwestern Mediterranean	MARINE AND PETROLEUM GEOLOGY			English	Article						High-resolution micropaleontology; Messinian-Zanclean boundary; Marine reflooding; Lago Mare events; Deposition of the Upper Evaporitic Unit	BASIN SE SPAIN; MIOCENE-PLIOCENE BOUNDARY; SALINITY CRISIS; ALBORAN SEA; TECTONIC EVOLUTION; DEPOSITS; NEOGENE; PROGRESSION; CHRONOLOGY; INSIGHTS	We present a high-resolution analysis of planktonic foraminifers, calcareous nannofossils, ostracods, dinoflagellate cysts and pollen grains in four sequences from DSDP-ODP holes in the southwestern Mediterranean Alboran and Balearic basins (976B, 977A, 978A and 134B) encompassing the previously defined Messinian-Zanclean boundary. The study focuses on (1) the marine reflooding, which closed the Messinian Salinity Crisis prior to the Zanclean GSSP; (2) the nature of the Lago Mare in the deep basins (indicated by Paratethyan dinoflagellate cysts), which appears to comprise several Paratethyan influxes without climatic control; and (3) the depositional context of the youngest Messinian evaporites which accumulated in a marine environment relatively close to the palaeoshoreline. Isolation of the Aegean Basin during the paroxysmic second step of the crisis is considered to have stored Paratethyan waters, which may then have poured into the Mediterranean central basins after deposition of the evaporitic sequence. (C) 2015 Elsevier Ltd. All rights reserved.	[Popescu, Speranta-Maria; Dalibard, Mathieu; Deaconu, Florina] GeoBioStratData Consulting, F-69140 Rillieux La Pape, France; [Suc, Jean-Pierre; Gorini, Christian] Univ Paris 06, Sorbonne Univ, UMR 7193, Inst Sci Terre Paris iSTeP, F-75005 Paris, France; [Suc, Jean-Pierre; Gorini, Christian] Inst Sci Terre Paris iSTeP, CNRS, UMR 7193, F-75005 Paris, France; [Barhoun, Nadia] Univ Hassan II Mohammedia, Fac Sci Ben MSik, Casablanca, Morocco; [Melinte-Dobrinescu, Mihaela-Carmen] Natl Inst Marine Geol & Geoecol, Bucharest 70318, Romania; [Bassetti, Maria Angela] Univ Perpignan, CEFREM, F-66860 Perpignan 9, France; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Do Couto, Damien] Univ Geneva, Sect Earth & Environm Sci, CH-1205 Geneva, Switzerland; [Rubino, Jean-Loup] CSTJF, TG ISS, TOTAL, F-64018 Pau, France; [Auxietre, Jean-Luc; Floodpage, Jonathan] PN BTF, TOTAL, F-92400 Paris, 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); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite; Hassan II University of Casablanca; National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Universite Perpignan Via Domitia; Brock University; University of Geneva; Total SA; Centre Scientifique et Technique Jean Feger (CSTJF); Total SA	Popescu, SM (通讯作者)，GeoBioStratData Consulting, 385 Route Mas Rillier, F-69140 Rillieux La Pape, France.	speranta.popescu@gmail.com	Bassetti, Maria-Angela/AAD-5998-2022; Mihaela, mihaela/AAF-5894-2021; DO COUTO, Damien/W-9543-2018	Bassetti, Maria Angela/0000-0003-3092-0046; DO COUTO, Damien/0000-0003-0589-208X	French CNRS/INSU Program "Actions Marges" (MedOc); TOTAL/Univ. Paris 6 GRI Mediterranee	French CNRS/INSU Program "Actions Marges" (MedOc); TOTAL/Univ. Paris 6 GRI Mediterranee	These investigations have been supported by the French CNRS/INSU Program "Actions Marges" (MedOc) and the TOTAL/Univ. Paris 6 GRI Mediterranee. We thank the Integrated Ocean Drilling Program (IODP) and the Curator of the Bremen Core Repository and its staff for facilities in providing the requested samples. S. Warny and an anonymous referee are thanked for the improvements suggested to our manuscript.	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Pet. Geol.	SEP	2015	66		1				55	70		10.1016/j.marpetgeo.2015.04.002	http://dx.doi.org/10.1016/j.marpetgeo.2015.04.002			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CW5SB		Green Submitted			2025-03-11	WOS:000365055800005
J	Suc, JP; Gillet, H; Çagatay, MN; Popescu, SM; Lericolais, G; Armijo, R; Melinte-Dobrinescu, MC; Sen, S; Clauzon, G; Sakinç, M; Zabci, C; Ucarkus, G; Meyer, B; Çakir, Z; Karakas, Ç; Jouannic, G; Macalet, R				Suc, Jean-Pierre; Gillet, Herve; Cagatay, M. Namik; Popescu, Speranta-Maria; Lericolais, Gilles; Armijo, Rolando; Melinte-Dobrinescu, Mihaela Carmen; Sen, Sevket; Clauzon, Georges; Sakinc, Mehmet; Zabci, Cengiz; Ucarkus, Gulsen; Meyer, Bertrand; Cakir, Ziyadin; Karakas, Cagil; Jouannic, Gwenael; Macalet, Rodica			The region of the Strandja Sill (North Turkey) and the Messinian events	MARINE AND PETROLEUM GEOLOGY			English	Article						Mediterranean-Paratethys connection; Onshore-offshore stratigraphy; Messinian Salinity Crisis; Erosion; Fluvial network	LATE MIOCENE; BLACK-SEA; ANATOLIAN FAULT; SALINITY CRISIS; THRACE BASIN; LAGO-MARE; PALEOGEOGRAPHIC EVOLUTION; EASTERN PARATETHYS; MEDITERRANEAN SEA; MARMARA	The two sides of the Strandja Sill show a highly discontinuous stratigraphic succession since the Late Oligocene. This area, together with the Sea of Marmara Basin, is usually proposed as the gateway for the Paratethyan freshwaters and organisms that constituted the Lago Mare fades in the Mediterranean Sea during the Messinian Salinity Crisis (MSC). Our investigations involving new field observations and datings, together with previous studies, suggest that the sill has possibly experienced such a connection at around 8 Ma, i.e. significantly before the crisis. The proposal of a sea-level drop of the Black Sea before 7 Ma is not supported by our data on dinoflagellate cysts. Consistency of calcareous nannofossil succession at DSDP Site 380 is reinforced, allowing to reassert that subaerial erosion impacted both the southwestern Black Sea and the central Marmara - Dardanelles area during the peak of the MSC. At that time, this region was crossed by two oppositely directed fluvial networks, further supporting the absence of a marine gateway through the Strandja Sill. It is concluded that none of the Lago Mare events recorded in the Mediterranean during the MSC were the consequence of the passage of Paratethyan waters and organisms through this area. In the Black Sea, the well-dated Messinian fluvial erosion can be followed offshore. The overlying prograding deltaic deposits attest to a fast marine reflooding after the crisis. This constitutes a comprehensive - erosion sedimentation model in an area intensively explored for hydrocarbons. (C) 2015 Elsevier Ltd. All rights reserved.	[Suc, Jean-Pierre; Meyer, Bertrand] Univ Paris 06, Sorbonne Univ, UMR 7193, iSTeP, F-75005 Paris, France; [Suc, Jean-Pierre; Meyer, Bertrand] iSTeP, CNRS, UMR 7193, F-75005 Paris, France; [Gillet, Herve] Univ Bordeaux 1, EPOC, F-33405 Talence, France; [Cagatay, M. Namik; Sakinc, Mehmet; Zabci, Cengiz; Cakir, Ziyadin] Istanbul Tech Univ, Fac Mines, Dept Geol Engn, TR-34469 Istanbul, Turkey; [Popescu, Speranta-Maria] GeoBioStratData Consulting, F-69140 Rillieux La Pape, France; [Lericolais, Gilles] IFREMER, F-92138 Issy Les Moulineaux, France; [Armijo, Rolando; Karakas, Cagil] Inst Phys Globe Paris, CNRS, Tecton & Mecan Lithosphere, UMR 7154, F-75238 Paris 05, France; [Melinte-Dobrinescu, Mihaela Carmen] Natl Inst Marine Geol & Geoecol, Bucharest 70318, Romania; [Sen, Sevket] Museum Natl Hist Nat, CNRS, UMR 7207, Ctr Rech Paleobiodiversite & Paleoenvironm, Paris, France; [Clauzon, Georges] Aix Marseille Univ, CNRS, IRD, CEREGE UM34, F-13545 Aix En Provence, France; [Ucarkus, Gulsen] Istanbul Tech Univ, Eurasia Inst Earth Sci, TR-34469 Istanbul, Turkey; [Jouannic, Gwenael] Cerema, DTer Est, Lab Reg Pants & Chaussees Nancy, F-54510 Tomblaine, France; [Macalet, Rodica] Natl Inst Hydrol & Water Management, Bucharest 013686, Romania	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); Sorbonne Universite; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); Istanbul Technical University; Ifremer; Universite Paris Cite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Sorbonne Universite; Museum National d'Histoire Naturelle (MNHN); Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite PSL; College de France; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Istanbul Technical University	Suc, JP (通讯作者)，iSTeP, CNRS, UMR 7193, F-75005 Paris, France.	jeanpierre.suc@gmail.com	Armijo, Rolando/P-5123-2019; Mihaela, mihaela/AAF-5894-2021; Ucarkus, Gulsen/X-7308-2019; Lericolais, Gilles/AAX-1662-2021; Sen, Sevket/HTS-0602-2023; Cagatay, M./S-6736-2016; Meyer, Bertrand/E-6903-2011; Jouannic, Gwenael/ABG-7687-2020; Cakir, Ziyadin/C-3594-2008; Zabci, Cengiz/X-3048-2018	GILLET, Herve/0000-0003-4589-1030; Jouannic, Gwenael/0000-0003-3399-389X; Cakir, Ziyadin/0000-0003-3050-5619; Armijo, Rolando/0000-0002-8258-2862; Zabci, Cengiz/0000-0003-0814-0422; Lericolais, Gilles/0000-0002-8159-9187				Armijo R, 2002, TERRA NOVA, V14, P80, DOI 10.1046/j.1365-3121.2002.00397.x; Armijo R, 1999, GEOLOGY, V27, P267, DOI 10.1130/0091-7613(1999)027<0267:WPOTNA>2.3.CO;2; Bache F, 2012, BASIN RES, V24, P125, DOI 10.1111/j.1365-2117.2011.00521.x; Band J., 2009, GEOCHEM GEOPHY GEOSY, V10; Çagatay MN, 2006, SEDIMENT GEOL, V188, P171, DOI 10.1016/j.sedgeo.2006.03.004; Chaput E., 1938, B SOC GEOL FR SER, V5, P363; Clauzon G, 2005, BASIN RES, V17, P437, DOI 10.1111/j.1365-2117.2005.00269.x; Do Couto D, 2014, MAR PETROL GEOL, V52, P57, DOI 10.1016/j.marpetgeo.2014.01.018; 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Pet. Geol.	SEP	2015	66		1				149	164		10.1016/j.marpetgeo.2015.01.013	http://dx.doi.org/10.1016/j.marpetgeo.2015.01.013			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CW5SB		Green Submitted, Green Published			2025-03-11	WOS:000365055800010
J	Suc, JP; Popescu, SM; Do Couto, D; Clauzon, G; Rubino, JL; Melinte-Dobrinescu, MC; Quillévéré, F; Brun, JP; Dumurzanov, N; Zagorchev, I; Lesic, V; Tomic, D; Sokoutis, D; Meyer, B; Macalet, R; Rifelj, H				Suc, Jean-Pierre; Popescu, Speranta-Maria; Do Couto, Damien; Clauzon, Georges; Rubino, Jean-Loup; Melinte-Dobrinescu, Mihaela Carmen; Quillevere, Frederic; Brun, Jean-Pierre; Dumurzanov, Nikola; Zagorchev, Ivan; Lesic, Vesna; Tomic, Dragana; Sokoutis, Dimitrios; Meyer, Bertrand; Macalet, Rodica; Rifelj, Helena			Marine gateway vs. fluvial stream within the Balkans from 6 to 5 Ma	MARINE AND PETROLEUM GEOLOGY			English	Article						Mediterranean; Paratethys connections; Messinian Salinity Crisis; Marine microfossils; Fluvial erosion; Balkans corridor	MESSINIAN SALINITY CRISIS; LATE MIOCENE; LATE NEOGENE; DACIC BASIN; SOUTHWESTERN BULGARIA; EASTERN PARATETHYS; CENOZOIC EXTENSION; MEDITERRANEAN SEA; SOUTHERN RHODOPE; PANNONIAN BASIN	Since the discovery of calcareous nannofossils, dinoflagellate cysts and planktonic foraminifers in deposits from the Dacic Basin, intensive research has been performed in order to evidence which gateway this microplankton used to connect Paratethys and the Mediterranean prior and after the Messinian Salinity Crisis (MSC). Such a gateway is also to be regarded at the origin of successive influxes of Paratethyan organisms (molluscs, ostracods, dinoflagellates) into the Mediterranean Basin ("Lago Mare" events). Observing that the Istanbul area, usually proposed for this purpose, was inefficient, we examine the succession of marine well-dated pre-MSC and post-MSC deltaic deposits through the Balkans, from northern Greece to southern Romania, that constitutes a reliable candidate for such a marine corridor, the origin of which was caused by the regional tectonic extension. The reconstructed palaeogeography for high sea level episodes that encompassed the MSC clarifies the context of the so-called North Aegean Lake. This marine gateway probably evolved as a powerful river during the peak of the MSC, contributing to the deposition of clastics in the hydrocarbon Prinos Field. A tectonically controlled subsidence to the north and south of the Skopje region caused the closure of such a gateway. (C) 2015 Elsevier Ltd. All rights reserved.	[Suc, Jean-Pierre; Meyer, Bertrand] Univ Paris 06, UMR 7193, Inst Sci Terre Paris iSTeP, Sorbonne Univ, F-75005 Paris, France; [Suc, Jean-Pierre; Meyer, Bertrand] CNRS, UMR 7193, Inst Sci Terre Paris iSTeP, F-75005 Paris, France; [Popescu, Speranta-Maria] GeoBioStratData Consulting, F-69140 Rillieux La Pape, France; [Do Couto, Damien] Univ Geneva, Sect Earth & Environm Sci, CH-1205 Geneva, Switzerland; [Clauzon, Georges] Aix Marseille Univ, CNRS, IRD, CEREGE UM34, F-13545 Aix En Provence, France; [Rubino, Jean-Loup] TOTAL, TG ISS, CSTJF, F-64018 Pau, France; [Melinte-Dobrinescu, Mihaela Carmen] Natl Inst Marine Geol & Geoecol, Bucharest 70318, Romania; [Quillevere, Frederic] Univ Lyon 1, Lab Geol Lyon, Terres, Planetes,Environm,UMR CNRS 5276, F-69622 Villeurbanne, France; [Brun, Jean-Pierre] Univ Rennes 1, Geosci Rennes, UMR 6118, F-35042 Rennes, France; [Dumurzanov, Nikola] Sts Cyril & Methodius Univ, Fac Min & Geol, Stip 2000, Macedonia; [Zagorchev, Ivan] Bulgarian Acad Sci, Inst Geol, BU-1113 Sofia, Bulgaria; [Lesic, Vesna; Tomic, Dragana] Geodet Author, Dept Geomagnetism & Aeron, Belgrade, Serbia; [Sokoutis, Dimitrios] Univ Utrecht, Dept Earth Sci, Fac Geosci, NL-3508 Utrecht, Netherlands; [Sokoutis, Dimitrios] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; [Macalet, Rodica] Natl Inst Hydrol & Water Management, Bucharest 013686, Romania; [Rifelj, Helena] Geol Survey Slovenia, Ljubljana 1000, Slovenia	Sorbonne Universite; 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); University of Geneva; Universite PSL; College de France; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Total SA; Centre Scientifique et Technique Jean Feger (CSTJF); National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Ecole Normale Superieure de Lyon (ENS de LYON); Universite de Rennes; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Saints Cyril & Methodius University of Skopje; Bulgarian Academy of Sciences; Utrecht University; University of Oslo	Suc, JP (通讯作者)，Univ Paris 06, UMR 7193, Inst Sci Terre Paris iSTeP, F-75005 Paris, France.	jeanpierre.suc@gmail.com	Mihaela, mihaela/AAF-5894-2021; Quillévéré, Frédéric/C-8317-2012; Meyer, Bertrand/E-6903-2011; DO COUTO, Damien/W-9543-2018	Quillevere, Frederic/0000-0002-6248-0447; DO COUTO, Damien/0000-0003-0589-208X	ANR-EGEO Project	ANR-EGEO Project(Agence Nationale de la Recherche (ANR))	Georges Clauzon, who passed away in March, 2013, actively participated to the field trips in the region with most of us. M. Bohme and A. Ilg are acknowledged for information on fossil fishes from the Prosilio section and for arousing our interest in erosional surfaces in this sedimentary succession. A. Di Stefano analysed our samples from the Akropotamos section. The main part of fieldwork and micropalaeontological analyses was realized during the ANR-EGEO Project that provided a significant financial support. Two anonymous referees significantly contributed to improve this manuscript.	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Pet. Geol.	SEP	2015	66		1				231	245		10.1016/j.marpetgeo.2015.01.003	http://dx.doi.org/10.1016/j.marpetgeo.2015.01.003			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CW5SB		Green Submitted			2025-03-11	WOS:000365055800015
J	Silva, WG; Zerfass, GSA; Souza, PA; Helenes, J				Silva, Wagner G.; Zerfass, Geise S. A.; Souza, Paulo A.; Helenes, Javier			Biochronostratigraphy and paleoenvironment analysis of Neogene deposits from the Pelotas Basin (well 2-TG-96-RS), Southernmost Brazil	ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS			English	Article						Micropaleontology; Biostratigraphy; Neogene; Pelotas Basin	GRANDE-DO-SUL; BIOSTRATIGRAPHY; STRATIGRAPHY; FORAMINIFERA; EVOLUTION; HOLOCENE; STRATA; BAY	This paper presents the integration of micropaleontological (palynology and foraminifera) and isotopic (Sr-87/Sr-86) analysis of a selected interval from the well 2-TG-96-RS, drilled on the onshore portion of the Pelotas Basin, Rio Grande do Sul, Brazil. A total of eight samples of the section between 140.20 and 73.50 m in depth was selected for palynological analysis, revealing diversified and abundant palynomorph associations. Species of spores, pollen grains and dinoflagellate cysts are the most common palynomorphs found. Planktic and benthic calcareous foraminifera were recovered from the lowest two levels of the section (140.20 and 134.30 m). Based on the stratigraphic range of the species of dinoflagellate cysts and sporomorphs, a span age from Late Miocene to Early Pliocene is assigned. The relative age obtained from the Sr-87/Sr-86 ratio in shells of calcareous foraminifers indicates a Late Miocene (Messinian) correspondence, corroborating the biostratigraphic positioning performed with palynomorphs. Paleoenvironmental interpretations based on the quantitative distribution of organic components (palynomorphs, phytoclasts and amorphous organic matter) throughout the section and on foraminiferal associations indicate a shallow marine depositional environment for the section. Two palynologicals intervals were recognized based on palynofacies analysis, related to middle to outer shelf (140.20 to 128.90 m) and inner shelf (115.75 to 73.50 m) conditions.	[Silva, Wagner G.] Inst Fed Educ Ciencia & Tecnol Rio Grande Sul, IFRS, BR-95520000 Osorio, RS, Brazil; [Silva, Wagner G.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Lab Palinol Marleni Marques Toigo, Inst Geociencias, BR-91540000 Porto Alegre, RS, Brazil; [Zerfass, Geise S. A.] Ilha Fundao, BPA PDGEO CENPES PETROBRAS, BR-21941915 Rio De Janeiro, RJ, Brazil; [Souza, Paulo A.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, BR-91540000 Porto Alegre, RS, Brazil; [Helenes, Javier] CICESE, Div Ciencias Tierra, Dept Geol, Ensenada 22860, Baja California, Mexico	Instituto Federal do Rio Grande do Sul (IFRS); Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Silva, WG (通讯作者)，Inst Fed Educ Ciencia & Tecnol Rio Grande Sul, IFRS, Campus Osorio,Rua Santos Dumont 2127, BR-95520000 Osorio, RS, Brazil.	wagner.guimaraes.silva@gmail.com	Alves de Souza, Paulo/O-9779-2018; Helenes, Javier/J-5033-2016	Alves de Souza, Paulo/0000-0001-9844-1530; Helenes, Javier/0000-0002-0135-1879	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [132470/2010-1, 310727/2014-6]; Agencia Nacional do Petroleo, Gas Natural e Biocombustiveis (ANP); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [1012119]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Agencia Nacional do Petroleo, Gas Natural e Biocombustiveis (ANP); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS))	The authors would like to thank the Companhia de Pesquisa de Recursos Minerais (CPRM) for providing the samples and Petrobras for the SEM images. We are grateful to the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq proc. 132470/2010-1, 310727/2014-6), Agencia Nacional do Petroleo, Gas Natural e Biocombustiveis (ANP) and Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS proc. 1012119) for their financial support.	Anjos G.S., 2004, Revista Brasileira de Paleontologia, V7, P127; Anjos-Zerfass G.S., 2008, Rev. Bras. Geociencias, V38, P47; [Anonymous], 1996, Palynology: principles and applications; ARAI M., 2006, 7 S CRET BRAS SERR N, V12; ASMUS HE, 1983, EPISODES, P3, DOI 10.18814/epiiugs/1983/v6i4/001; Bauermann S. G., QUATERNARIO RIO GRAN, P81; Blow W.H., 1969, Proceedings of the International Conference on Planktonic Microfossils, V1, P199; Bolli H.M., 1985, P155; Bueno G.V., 2007, Bol. 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Assoc. Strat. Palynologists Contribution Series, V17, P169; Yassini I., 1995, FORAMINIFERIDA OSTRA	69	9	9	0	1	ACAD BRASILEIRA DE CIENCIAS	RIO JANEIRO	RUA ANFILOFIO DE CARVALHO, 29, 3 ANDAR, 20030-060 RIO JANEIRO, BRAZIL	0001-3765	1678-2690		AN ACAD BRAS CIENC	An. Acad. Bras. Cienc.	SEP	2015	87	3					1565	1582		10.1590/0001-3765201520140584	http://dx.doi.org/10.1590/0001-3765201520140584			18	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	CS1QI	26312424	Green Submitted, Green Published, gold			2025-03-11	WOS:000361842000008
J	Castro, SP; Carvalho, MA				Castro, Susan P.; Carvalho, Marcelo A.			Santonian dinocyst assemblages of the Santa Marta Formation, Antarctic Peninsula: Inferences for paleoenvironments and paleoecology	ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS			English	Article						Santonian dinocysts; Antarctica; Cretaceous; Santa Marta Formation; dinocyst blooms	JAMES-ROSS-ISLAND; DINOFLAGELLATE CYSTS; BASIN; STRATIGRAPHY; EVOLUTION	To better understand the paleoenvironments of the lower-middle Santonian, dinocyst data were obtained from the Santa Marta Formation, Larsen Basin, James Ross Island, Antarctic Peninsula. This study provides the first available quantitative dinocyst data for the Santa Marta Formation, which should more clearly reflect detailed changes in paleoenvironments, as recorded by fluctuations in diversity and abundance. To record the Santonian dinocyst assemblages from the Larsen Basin, 30 samples from an outcrop of the Lachman Crags Member (LC section) were analyzed. These assemblages are dominated by peridiniacean dinocysts typical of the Isabelidinium flora. A lower-middle Santonian age was determined after the recognition of Odontochitina porifera and Isabelidinium cretaceum zones. Cluster analysis based on quantitative data, yielded five dinocyst assemblages: Manumiella, Heterosphaeridium, Chlamydophorella, Isabelidinium and Odontochitina. Two Santonian blooms, Isabelidinium and Odontochitina, recognized in other regions were also recorded in the studied section. The stratigraphic distribution shows an alternation between the assemblages, distinguishing in the section six intervals. The high abundance of the Manumiella assemblage at the uppermost interval of the section represents the shallower setting, whereas the high abundance of Odontochitina at the middle part of the section represents the deepest setting.	[Castro, Susan P.; Carvalho, Marcelo A.] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Lab Paleoecol Vegetal, BR-22040040 Rio De Janeiro, RJ, Brazil; [Castro, Susan P.] Univ Fed Rio de Janeiro, Ilha Fundao, Inst Geociencias, Programa Posgrad, BR-21949900 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro	Castro, SP (通讯作者)，Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Lab Paleoecol Vegetal, Quinta Boa Vista S-N, BR-22040040 Rio De Janeiro, RJ, Brazil.	susanpcastro@yahoo.com.br	Carvalho, Marcelo/G-8463-2015		Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [301573/2013-1]; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/103.028/2008]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	This study was supported by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) scholarship to S.P. Castro, by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) grant no. 301573/2013-1 to M. Carvalho, the Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) grant no. E-26/103.028/2008 to M. Carvalho. We thank Petrobras geologist Dr. Mitsuru Arai for his valuable suggestions about dinocyst ecology. We thank the anonymous reviewers for their valuable suggestions.	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Acad. Bras. Cienc.	SEP	2015	87	3					1583	1597		10.1590/0001-3765201520140651	http://dx.doi.org/10.1590/0001-3765201520140651			15	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	CS1QI	26312427	gold, Green Submitted			2025-03-11	WOS:000361842000009
J	Sassenhagen, I; Sefbom, J; Godhe, A; Rengefors, K				Sassenhagen, Ingrid; Sefbom, Josefin; Godhe, Anna; Rengefors, Karin			Germination and colonization success of <i>Gonyostomum semen</i> (Raphidophyceae) cysts after dispersal to new habitats	JOURNAL OF PLANKTON RESEARCH			English	Article						cyst germination; Gonyostomum semen; invasion; life cycle; local adaptation; microalgae	DINOFLAGELLATE; DIFFERENTIATION; BLOOMS	Colonization of new habitats through dispersal of phytoplankton cysts might be limited, if resident populations out-compete invaders during germination. We reciprocally transferred Gonyostomum semen (Raphidophyceae) cysts from three lakes into native and foreign waters originating from the respective habitats. Germination rate and germling growth were impacted by water origin, but there was no preference for native water. Gonyostomum semen's ability to germinate in different conditions might explain its expansion in northern Europe.	[Sassenhagen, Ingrid; Rengefors, Karin] Lund Univ, Aquat Ecol, S-22362 Lund, Sweden; [Sefbom, Josefin; Godhe, Anna] Univ Gothenburg, Dept Biol & Environm Sci, S-40530 Gothenburg, Sweden	Lund University; University of Gothenburg	Sassenhagen, I (通讯作者)，Lund Univ, Aquat Ecol, Solvegatan 37, S-22362 Lund, Sweden.	ingrid.sassenhagen@biol.lu.se	Rengefors, Karin/K-5873-2019	Rengefors, Karin/0000-0001-6297-9734; Sassenhagen, Ingrid/0000-0002-5969-2289	Swedish Research Council FORMAS [215-2010-751]	Swedish Research Council FORMAS(Swedish Research Council Formas)	The research was supported by a grant of the Swedish Research Council FORMAS to K.R. (215-2010-751). Funding to pay the Open Access publication charges for this article was provided by the Swedish Research Council Formas (215-2010-751).	ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1985, J PHYCOL, V21, P200; CRONBERG G, 1988, HYDROBIOLOGIA, V161, P217, DOI 10.1007/BF00044113; De Meester L, 2002, ACTA OECOL, V23, P121, DOI 10.1016/S1146-609X(02)01145-1; Drouet F, 1935, BIOL BULL-US, V68, P422, DOI 10.2307/1537563; Figueroa RI, 2006, J PHYCOL, V42, P859, DOI 10.1111/j.1529-8817.2006.00240.x; Findlay DL, 2005, HYDROBIOLOGIA, V533, P243, DOI 10.1007/s10750-004-2962-z; Fryxell G.A., 1983, SURVIVAL STRATEGIES; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; Imai I, 2012, HARMFUL ALGAE, V14, P46, DOI 10.1016/j.hal.2011.10.014; Lebret K, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0082510; Lebret K, 2012, ENVIRON MICROBIOL, V14, P2395, DOI 10.1111/j.1462-2920.2012.02769.x; Peczula W, 2015, HYDROBIOLOGIA, V744, P177, DOI 10.1007/s10750-014-2075-2; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rengefors K, 1996, J PLANKTON RES, V18, P1753, DOI 10.1093/plankt/18.9.1753; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; Rengefors K, 2012, HARMFUL ALGAE, V18, P65, DOI 10.1016/j.hal.2012.04.005; Sassenhagen I, 2015, ENVIRON MICROBIOL, V17, P5063, DOI 10.1111/1462-2920.12987; Sassenhagen I, 2015, HARMFUL ALGAE, V41, P38, DOI 10.1016/j.hal.2014.11.001; van Gremberghe I, 2009, ENVIRON MICROBIOL, V11, P2564, DOI 10.1111/j.1462-2920.2009.01981.x	20	4	4	1	18	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	SEP-OCT	2015	37	5					857	861		10.1093/plankt/fbv067	http://dx.doi.org/10.1093/plankt/fbv067			5	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	CS3RY	26412910	Green Submitted, hybrid, Green Published			2025-03-11	WOS:000361993700002
J	Abadie, E; Kaci, L; Berteaux, T; Hess, P; Sechet, V; Masseret, E; Rolland, JL; Laabir, M				Abadie, Eric; Kaci, Lamia; Berteaux, Tom; Hess, Philipp; Sechet, Veronique; Masseret, Estelle; Rolland, Jean Luc; Laabir, Mohamed			Effect of Nitrate, Ammonium and Urea on Growth and Pinnatoxin G Production of <i>Vulcanodinium rugosum</i>	MARINE DRUGS			English	Article						Vulcanodinium rugosum; pinnatoxin G; Ingril lagoon; growth; nitrogen source	HARMFUL ALGAL BLOOMS; RED TIDE DINOFLAGELLATE; ALEXANDRIUM-CATENELLA; SOUTHERN FRANCE; THAU LAGOON; MEDITERRANEAN WATERS; SCRIPPSIELLA-HANGOEI; TOXIC DINOFLAGELLATE; NITROGEN-SOURCES; PHYTOPLANKTON	Vulcanodinium rugosum, a recently described dinoflagellate species producing a potent neurotoxin (pinnatoxin G), has been identified in French Mediterranean lagoons and was responsible for recurrent episodes of shellfish toxicity detected by mouse bioassay. Until now, the biology and physiology of V. rugosum have not been fully investigated. We studied the growth characteristics and toxicity of a V. rugosum strain (IFR-VRU-01), isolated in the Ingril lagoon in June 2009 (North-Western French Mediterranean Sea). It was cultivated in Enriched Natural Sea Water (ENSW) with organic (urea) and inorganic (ammonium and nitrate) nitrogen, at a temperature of 25 degrees C and irradiance of 100 mol/m(2)s(-1). Results showed that ammonium was assimilated by cells more rapidly than nitrate and urea. V. rugosum is thus an osmotrophic species using urea. Consequently, this nitrogen form could contribute to the growth of this dinoflagellate species in the natural environment. There was no significant difference (Anova, p = 0.856) between the growth rate of V. rugosum cultivated with ammonium (0.28 +/- 0.11 day(-1)), urea (0.26 +/- 0.08 day(-1)) and nitrate (0.24 +/- 0.01 day(-1)). However, the production of chlorophyll a and pinnatoxin G was significantly lower with urea as a nitrogen source (Anova, p < 0.027), suggesting that nutritional conditions prevailing at the moment of the bloom could determine the cellular toxicity of V. rugosum and therefore the toxicity measured in contaminated mollusks. The relatively low growth rate (0.28 day(-1)) and the capacity of this species to continuously produce temporary cysts could explain why cell densities of this species in the water column are typically low (20,000 cells/L).	[Abadie, Eric; Kaci, Lamia; Berteaux, Tom] IFREMER, Lab Environm Ressources Languedoc Roussillon, Ctr Marine Biodivers Exploitat & Conservat MARBEC, Sete 3, France; [Hess, Philipp; Sechet, Veronique] IFREMER, Dept ODE UL PHYC, F-44311 Nantes 3, France; [Masseret, Estelle; Laabir, Mohamed] Univ Montpellier, Ctr Marine Biodivers Exploitat & Conservat MARBEC, CNRS, IRD, F-34095 Montpellier 5, France; [Rolland, Jean Luc] Univ Montpellier, Univ Perpignan, IFREMER, Interact Hotes Pathogenes Environm,UMR 5244, F-34095 Montpellier, France	Ifremer; Ifremer; Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); Ifremer; Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite Perpignan Via Domitia; Ifremer; Universite de Montpellier	Abadie, E (通讯作者)，IFREMER, Lab Environm Ressources Languedoc Roussillon, Ctr Marine Biodivers Exploitat & Conservat MARBEC, CS30171, Sete 3, France.	eric.abadie@ifremer.fr; kaci_lamia@hotmail.fr; tom.berteaux@ifremer.fr; philipp.hess@ifremer.fr; veronique.sechet@ifremer.fr; estelle.masseret@univ-montp2.fr; jean.luc.rolland@ifremer.fr; mohamed.laabir@univ-montp2.fr	; Hess, Philipp/G-1761-2010	ABADIE, Eric/0000-0001-9431-2010; Hess, Philipp/0000-0002-9047-1345; sechet, veronique/0000-0002-7085-3215; Rolland, jean-luc/0000-0001-9823-6588; Masseret, Estelle/0000-0001-6856-8637	LAGUNOTOX project - Fondation TOTAL; l'Agence de l'Eau Rhone Mediterranee Corse (AERMC); IRD (Institut National pour la Recherche et le Developpement); LMI COYS-MED; Pays de la Loire Regional Council	LAGUNOTOX project - Fondation TOTAL; l'Agence de l'Eau Rhone Mediterranee Corse (AERMC); IRD (Institut National pour la Recherche et le Developpement); LMI COYS-MED; Pays de la Loire Regional Council(Region Pays de la Loire)	This work was supported by the LAGUNOTOX project funded by Fondation TOTAL. We would also like to thank l'Agence de l'Eau Rhone Mediterranee Corse (AERMC) for their financial help. Thanks to IRD (Institut National pour la Recherche et le Developpement) for funding Mohamed Laabir's stay in Tunisia and to LMI COYS-MED for supporting his research. Contributions from Philipp Hess and Veronique Sechet were part of the COSELMAR project (partly funded by the Pays de la Loire Regional Council). Thanks to Yves Collos for his help.	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Drugs	SEP	2015	13	9					5642	5656		10.3390/md13095642	http://dx.doi.org/10.3390/md13095642			15	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	CS2HZ	26404325	Green Published, gold			2025-03-11	WOS:000361891700009
J	Singh, H; Prasad, M; Kumar, K; Singh, SK				Singh, Hukam; Prasad, Mahesh; Kumar, Kishor; Singh, Sanjai K.			Early Eocene macroflora and associated palynofossils from the Cambay Shale Formation, western India: Phytogeographic and palaeoclimatic implications	PALAEOWORLD			English	Article						Palaeoflora; Palaeoclimate; Vastan Lignite Mine; Cambay Shale Formation; Eocene; India	VASTAN LIGNITE MINE; FOSSIL WOOD; SP-NOV; FRUITS; GUJARAT; MIOCENE; SEDIMENTS; BASIN; ANACARDIACEAE; PALYNOLOGY	A diverse assemblage of plant macrofossils and the associated representative palynofloral elements are documented from the early Eocene subsurface beds of the Cambay Shale Formation exposed in an open cast lignite mine at Vastan Village in the Surat District, western India. The Vastan mine succession is cyclic, each cycle representing a transgressive burial event terminating in the low energy lagoonal conditions. The higher energy cycle begins with sandy lenses having rich biotic remains, followed by mudstones and molluscan shell beds and ends with lignite seams. The dominantly muddy facies and the associated biota demonstrate predominantly low energy near shore or coastal plain depositional setting with conditions varying from dominantly marine (shallow) through brackish to fresh water. The Vastan mine is a well dated fossil locality with a rich and diverse biota of mammals, birds, snakes, lizards, fish, insects, molluscs, foraminifers, dinoflagellates, and plants. The plants comprise leaf and fruit impressions, seeds, fruits, wood fragments, mangrove rooting structures, fungal thalli and spores, pteridophytic spores, and angiosperm pollen grains. Thirteen macrofossil species, including several morphotaxa, are represented by the families Calophyllaceae, Rutaceae, Anacardiaceae, Rubiaceae, Combretaceae, Lythraceae, Sapindaceae, Malvaceae, and Ebenaceae. The palynological assemblage representing fourteen taxa includes the new species, Notothyrites undulatus, Callimothallus semicircularis, and Carallioipollenites integerrimoides. Habitat and distribution of modern taxa comparable with the fossil assemblage from Vastan suggest a terrestrial lowland environment. The macrofossil taxa are indicative of mesophytic, mixed forest growing under tropical to subtropical climate with sufficient humidity. The occurrence of dipterocarp elements along with taxa such as Swintonia, Pterospermum and Diospyros, etc. seems to suggest the presence of a tropical rain forest in the vicinity of Vastan. (C) 2015 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.	[Singh, Hukam; Prasad, Mahesh; Singh, Sanjai K.] Birbal Sahni Inst Paleobot, Lucknow 226001, Uttar Pradesh, India; [Kumar, Kishor] Wadia Inst Himalayan Geol, Dehra Dun 248001, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Department of Science & Technology (India); Wadia Institute of Himalayan Geology (WIHG)	Kumar, K (通讯作者)，Wadia Inst Himalayan Geol, 33 Gen Mahadeo Singh Rd, Dehra Dun 248001, Uttar Pradesh, India.	kumark@wihg.res.in	KUMAR, Kishor/H-7232-2013; Singh, Sarvesh Kumar/AHC-3896-2022		BSIP, Lucknow; Wadia Institute of Himalayan Geology Dehradun	BSIP, Lucknow; Wadia Institute of Himalayan Geology Dehradun(Department of Science & Technology (India))	We thank Prof. Ashok Sahni (Lucknow University) for his overall guidance and suggestions for improvement of the manuscript, to Dr. K. Ambwani (BSIP) for his valuable suggestions and help in identifying the palynomorphs, and to Prof. R.S. Rana for help in a multiple ways. We also thank Dr. John G. Conran (University of Adelaide) and two anonymous reviewers for offering numerous valuable suggestions that helped improve the manuscript greatly. We are thankful to the Director, BSIP, Lucknow and Director, Wadia Institute of Himalayan Geology Dehradun for providing the necessary funds and field and laboratory facilities for this work.	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J	Wiese, F; Zobel, K; Keupp, H				Wiese, Frank; Zobel, Kerstin; Keupp, Helmut			Calcareous dinoflagellate cysts and the Turonian nutrient crisis - Data from the upper Turonian of the Lower Saxony Basin (northern Germany)	CRETACEOUS RESEARCH			English	Review						Calcareous dinoflagellate cysts; Pithonella spp.; Nutrient crisis; Late Turonian; Late Cretaceous	NW GERMANY; EQUATORIAL ATLANTIC; QUATERNARY EASTERN; BOUNDARY INTERVAL; STRATIGRAPHY; WESTERN; OCEAN; RECONSTRUCTION; EUROPE; CHALK	Little information exists on the distribution of calcareous dinoflagellate cysts from the Turonian (Upper Cretaceous) of Germany, and the first taxonomic assessment of late Turonian calcareous dinoflagellate cysts from the Salder Formation (NW Germany, Lower Saxony Basin) is a first step to close this gap. Ca. 11.000 calcareous dinoflagellate cysts were considered for this study, representing seven taxa only. The dominant taxon is Pithonella, mainly represented by Pithonella sphaerica and Pithonella ovalis, while Pithonella cardiiformis and Pithonella discoidea are rare. The species Pithonella spiralis n. sp. is newly described. Non-pithonellid c-dinocysts are represented by Normandia circumperforata and Pirumella sp. The late Turonian c-dinocyst diversity of the NW German shelf sea is extremely low compared with the Early Cretaceous species richness in the same area. The diversity drop is explained to result from a Turonian nutrient crisis, caused by the drowning of source areas of nutrient input during the early Late Cretaceous sea-level highstand. (C) 2015 Elsevier Ltd. All rights reserved.	[Wiese, Frank] Univ Gottingen, Geosci Ctr Univ, Dept Geobiol, D-37077 Gottingen, Germany; [Zobel, Kerstin; Keupp, Helmut] Free Univ Berlin, Inst Geol Sci, Sect Paleontol, D-12249 Berlin, Germany	University of Gottingen; Free University of Berlin	Wiese, F (通讯作者)，Univ Gottingen, Geosci Ctr Univ, Dept Geobiol, Goldschmidtstr 3, D-37077 Gottingen, Germany.	fwiese1@gwdg.de		Wiese, Frank/0000-0002-6910-2166	German Research Foundation DFG [Wi 1656/7-1]	German Research Foundation DFG(German Research Foundation (DFG))	We are highly indebted to two anonymous reviewers for their very detailed and keen reviews, which improved the manuscript considerably. We thank Maike Glos and Marc Barlage (Berlin), for sample preparation and thin-sections. Gwen Other (Asche) is thanked for the desperate work to measure dimensions of thousands of calcareous dinoflagellates cysts in thin-section. We thank the German Research Foundation DFG for financial support (Wi 1656/7-1).	ADAMS T. 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J	Shields, JD; Sullivan, SE; Small, HJ				Shields, Jeffrey D.; Sullivan, Shelley E.; Small, Hamish J.			Overwintering of the parasitic dinoflagellate <i>Hematodinium perezi</i> in dredged blue crabs (<i>Callinectes sapidus</i>) from Wachapreague Creek, Virginia	JOURNAL OF INVERTEBRATE PATHOLOGY			English	Article						Hibernation; Life cycle; Seasonality; Infection; Parasite; Crustacea; Decapoda	LOBSTER NEPHROPS-NORVEGICUS; IN-VITRO CULTIVATION; CHIONOECETES-OPILIO; EXPERIMENTAL INFECTIONS; ORCHITOPHRYA-STELLARUM; DEVELOPMENTAL CYCLE; AMERICAN LOBSTER; CONCEPTION BAY; DISEASE; MORTALITY	Parasitic dinoflagellates in the genus Hematodinium cause disease and mortality in several commercially important marine decapod crustaceans. One species, Hematodinium perezi, occurs in blue crabs, Callinectes sapidus, along the eastern seaboard and Gulf coast of the USA. The parasite infects blue crabs, other decapods, and amphipods in the high salinity waters of coastal bays. Epizootics of the parasite often reach prevalence levels of 75-80% during outbreaks with diseased crabs dying from the infection. Prevalence of the parasite is bimodal, with a minor peak in late spring or summer, and a major peak in fall, and declining rapidly to nearly zero in late November and December. The rapid decline in infections in the late fall brings up the question of whether the parasite overwinters in crabs or whether it uses an unidentified resting stage, such as a cyst. We report observations on the prevalence of the parasite from winter dredge surveys undertaken in 2011 and 2012. Crabs were examined via hemolymph smears, histology, and PCR diagnosis for the presence of H. perezi and other pathogens. Active infections were observed from January through March in 2011 and 2012, indicating the parasite can overwinter in blue crabs. However, several crabs that were positive by PCR had presumptive effete infections that were difficult to diagnose in histological slides and hemolymph smears. These infections did not appear to be active and may have been in subsidence. Dredged crabs with light and moderate active infections were held at 15 degrees C to determine if the parasite was capable of rapid progression. In 8 cases, infections exhibited logarithmic growth progressing rapidly over 8-12 days. We present evidence that overwintering of H. perezi occurs in the blue crab hosts, that infections are capable of responding rapidly to increases in temperatures, and that overwintering provides a reservoir of infected animals for transmission to occur in the spring. (C) 2015 Elsevier Inc. All rights reserved.	[Shields, Jeffrey D.; Sullivan, Shelley E.; Small, Hamish J.] Virginia Inst Marine Sci, Coll William & Mary, Gloucester Point, VA 23062 USA	William & Mary; Virginia Institute of Marine Science	Shields, JD (通讯作者)，Virginia Inst Marine Sci, Coll William & Mary, POB 1346, Gloucester Point, VA 23062 USA.	jeff@vims.edu		Shields, Jeffrey D./0000-0002-2658-4572; Small, Hamish/0009-0007-7450-8447	National Science Foundation's Ecology of Infectious Diseases (EID) program [OCE BE-UF0723662]	National Science Foundation's Ecology of Infectious Diseases (EID) program	We thank Tom Dolan, Pattie O'Leary, Sean Fate, Edward Smith, and Mike Sanderson for their help in dredging crabs and processing samples in the laboratory. This research was supported by National Science Foundation's Ecology of Infectious Diseases (EID) program (OCE BE-UF0723662). This is VIMS contribution #3482.	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Invertebr. Pathol.	SEP	2015	130						124	132		10.1016/j.jip.2015.07.013	http://dx.doi.org/10.1016/j.jip.2015.07.013			9	Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Zoology	CR3UO	26232044				2025-03-11	WOS:000361258800018
J	Fertouna-Bellakhal, M; Dhib, A; Fathalli, A; Bellakhal, M; Chomérat, N; Masseret, E; Laabir, M; Turki, S; Aleya, L				Fertouna-Bellakhal, Mouna; Dhib, Amel; Fathalli, Afef; Bellakhal, Meher; Chomerat, Nicolas; Masseret, Estelle; Laabir, Mohamed; Turki, Souad; Aleya, Lotfi			<i>Alexandrium</i> <i>pacificum</i> Litaker sp nov (Group IV): Resting cyst distribution and toxin profile of vegetative cells in Bizerte Lagoon (Tunisia, Southern Mediterranean Sea)	HARMFUL ALGAE			English	Article						Alexandrium pacificum Litaker sp nov (Alexandrium catenella-group IV (Whedon & Kofoid) Balech); Cysts; Vegetative cells; Ribotype; Toxin profile; Mapping	SPECIES COMPLEX DINOPHYCEAE; MODERN DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; CATENELLA DINOPHYCEAE; SPATIAL-DISTRIBUTION; BALLAST WATER; TOKYO-BAY; SHELLFISH; DYNAMICS; HARMFUL	A high spatial resolution sampling of Alexandrium pacificum cysts, along with sediment characteristics (% H2O, % organic matter (OM), granulometry), vegetative cell abundance and environmental factors were investigated at 123 study stations in Bizerte Lagoon (Tunisia). Morphological examination and ribotyping of cells obtained from a culture called ABZ1 obtained from a cyst isolated in lagoon sediment confirmed that the species was A. pacificum. The toxin profile from the ABZ1 culture harvested during exponential growth phase was simple and composed of the N-sulfocarbamoyl toxins C1 (9.82 pg toxin cell(-1)), the GTX6 (3.26 pg toxin cell(-1)) and the carbamoyl toxin Neo-STX (0.38 pg toxin cell(-1)).The latter represented only 2.8% of the total toxins in this strain. High abundance of A. pacificum cysts correlated with enhanced percentages of water and organic matter in the sediment. In addition, sediment fractions of less than 63 mu m were examined as a favorable potential seedbed for initiation of future blooms and outbreaks of A. pacificum in the lagoon. A significant difference in the cyst distribution pattern was recorded among the lagoon's different zones, with the higher cyst abundance occurring in the inner waters. Also, no correlation due to the specific hydrodynamics of the lagoon was observed in the spatial distribution of A. pacificurn cysts and vegetative cells. (C) 2015 Elsevier B.V. All rights reserved.	[Fertouna-Bellakhal, Mouna; Dhib, Amel; Aleya, Lotfi] Univ Bourgogne Franche Comte, Lab Chrono Environm, CNRS, UMR 6249, F-6249 Besancon, France; [Fertouna-Bellakhal, Mouna; Fathalli, Afef; Bellakhal, Meher] Inst Super Peche & Aquaculture Bizerte, Unite Rech Exploit Milieux Aquat, Bizerte 7080, Tunisia; [Fertouna-Bellakhal, Mouna; Turki, Souad] Ctr Goulette, Inst Natl Sci & Technol Mer, Lab Milieu Marin, La Goulette, Tunisia; [Fertouna-Bellakhal, Mouna] FSB, Bizerte 7021, Tunisia; [Chomerat, Nicolas] IFREMER, Stn Biol Marine, F-29900 Concarneau, France; [Masseret, Estelle; Laabir, Mohamed] Univ Montpellier, UMR MARBEC 9190 IRD Ifremer UM CNRS, F-34095 Montpellier 5, France	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite de Franche-Comte; Institut National des Sciences et Technologies de la Mer; Ifremer; Universite de Montpellier	Aleya, L (通讯作者)，Univ Bourgogne Franche Comte, Lab Chrono Environm, CNRS, UMR 6249, F-6249 Besancon, France.	lotfi.aleya@univ-fcomte.fr		Masseret, Estelle/0000-0001-6856-8637; Chomerat, Nicolas/0000-0001-9691-6344	French National Programme Ecosphere Continentale et Cotiere - EC2CO; Fondation pour la Recherche sur la Biodiversite - INVALEX project [AAPIN-2009-036]	French National Programme Ecosphere Continentale et Cotiere - EC2CO; Fondation pour la Recherche sur la Biodiversite - INVALEX project	This study was conducted by Mouna Fertouna-Bellakhal as a part of her PhD research, co-directed at the University of Bourgogne Franche-Comte, the French National Center for Scientific Research (CNRS 6249), Besancon, France, and at the Tunisian National Institute of Sciences and Sea Technologies (INSTM), la Goulette, Tunisia. Sampling, isolation and cultivation of the ABZ1 A. catenella strain studied were supported by grants from the French National Programme Ecosphere Continentale et Cotiere - EC2CO and from the Fondation pour la Recherche sur la Biodiversite - INVALEX project (AAPIN-2009-036). We thank Dr. Zouher Amzil and Veronique Savar from the Laboratoire Phycotoxines - Ifremer Nantes (France) for the toxins analysis and Dr. Yves Collos and all the members of the UMR ECOSYM (MARBEC since January 2015), University of Montpellier for their help and kindness. We also thank all the members of the Faculty of Sciences of Bizerte, the High Institute of Fisheries and Aquaculture of Bizerte and the CNRS 6249 Laboratory of Chrono-Environment, Besancon.	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J	Silva, T; Caeiro, MF; Costa, PR; Amorim, A				Silva, Teresa; Caeiro, Maria F.; Costa, Pedro Reis; Amorim, Ana			<i>Gymnodinium catenatum</i> Graham isolated from the Portuguese coast: Toxin content and genetic characterization	HARMFUL ALGAE			English	Article						Gymnodinium catenatum; Intra-specific variability; PST profile; Strain origin; Single nucleotide polymorphism; Portugal	PARALYTIC SHELLFISH TOXINS; SAXITOXIN ANALOGS; LIQUID-CHROMATOGRAPHY; MEXICAN PACIFIC; BALLAST WATER; RIBOSOMAL DNA; DINOFLAGELLATE; DINOPHYCEAE; PROFILES; CYSTS	The bloom forming marine dinoflagellate Gymnodinium catenatum Graham has been linked to paralytic shellfish poisoning (PSP) outbreaks in humans. Along the Portuguese coast (NE Atlantic), G. catenatum shows a complex bloom pattern, raising questions about the origin and affinities of each bloom population. In this work, the variability within six cultured strains of G. catenatum isolated from Portuguese coastal waters (S coast, W coast and NW coast), between 1999 and 2011, was investigated. The strains were analyzed for toxin profiling and intra-specific genetic diversity. Regarding the toxin profile, differences recorded between strains could not be assigned to the time of isolation or geographical origin. The parameter that most influenced the toxin profile was the life-cycle stage that originated the culture: vegetative cell versus hypnozygote (resting cyst). At the genetic level, all strains showed similar sequences for the D1-D2 region of the large subunit (LSU) of the nuclear ribosomal DNA (rDNA) and shared complete identity with strains from Spain, Algeria, China and Australia. Conversely, we did not find a total identity match for the ITS-5.8S nuclear rDNA fragment. After sequence analysis, two guanine/adenine (R) single nucleotide polymorphisms (SNP 1 and 2) were detected for all strains, in the ITS1 region. This species has been reported to present very conservative LSU and ITS-5.8S rDNA regions, though with few SNP, including SNP1 of this study, already attributed to strains from certain locations. The SNP here described characterize G. catenatum populations from Portuguese waters and may represent valuable genetic markers for studies on the phylogeography of this species. (C) 2015 Elsevier B.V. All rights reserved.	[Silva, Teresa; Amorim, Ana] Univ Lisbon, Fac Ciencias, MARE Marine & Environm Sci Ctr, P-1749016 Lisbon, Portugal; [Caeiro, Maria F.; Amorim, Ana] Univ Lisbon, Fac Ciencias, Dept Biol Vegetal, P-1749016 Lisbon, Portugal; [Caeiro, Maria F.] Univ Aveiro, CESAM Ctr Environm & Marine Studies, P-3810193 Aveiro, Portugal; [Costa, Pedro Reis] CCMAR Ctr Marine Sci, IPMA Portuguese Inst Ocean & Atmosphere, P-1449006 Lisbon, Portugal	Universidade de Lisboa; Universidade de Lisboa; Universidade de Aveiro; Instituto Portugues do Mar e da Atmosfera	Silva, T (通讯作者)，Univ Lisbon, Fac Ciencias, MARE Marine & Environm Sci Ctr, P-1749016 Lisbon, Portugal.	teresalsilva@fc.ul.pt	; Amorim, Ana/AAA-2615-2020; Reis Costa, Pedro/N-1908-2019; Caeiro, Maria/C-1200-2014	Lopes Silva, Teresa/0000-0003-4785-5383; Amorim, Ana/0000-0002-9612-4280; Reis Costa, Pedro/0000-0001-6083-470X; Caeiro, Maria/0000-0003-0559-6344	Portuguese Foundation for Science and Technology (FCT) [PEst-OE/MAR/UI0199/2011, HABSPOT - PTDC/MAR/100348/2008]; FCT Investigator Program [IF/00271/2013]	Portuguese Foundation for Science and Technology (FCT)(Fundacao para a Ciencia e a Tecnologia (FCT)); FCT Investigator Program(Fundacao para a Ciencia e a Tecnologia (FCT))	This study was supported by the Portuguese Foundation for Science and Technology (FCT) through the research projects HABSPOT - PTDC/MAR/100348/2008 and PEst-OE/MAR/UI0199/2011). Pedro R. Costa was supported through the FCT Investigator Program (IF/00271/2013). The authors wish to thank colleagues from project HABSPOT for fruitful discussions and help in sample collection during the oceanographic cruises. We also acknowledge the technical assistance and enthusiasm of the crew of R/V Mytillus, Vera Veloso for the skilled assistance regarding culture maintenance and J. Lino Costa for advice on the statistical approach. 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J	Paul, S; Sharma, J; Singh, BD; Saraswati, PK; Dutta, S				Paul, Swagata; Sharma, Jyoti; Singh, Bhagwan D.; Saraswati, Pratul K.; Dutta, Suryendu			Early Eocene equatorial vegetation and depositional environment: Biomarker and palynological evidences from a lignite-bearing sequence of Cambay Basin, western India	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article						Early Eocene; Biomarkers; Angiosperms; Tropical climate	VASTAN LIGNITE; ORGANIC-MATTER; TRITERPENOID HYDROCARBONS; AROMATIC-HYDROCARBONS; DIAGENETIC FATE; SEDIMENTS; COALS; MINE; GUJARAT; MIOCENE	An investigation of palaeofloral distribution with depositional environment and palaeoclimatic condition of western Indian subcontinent during Early Eocene period has been carried out from a lignite-bearing succession of Cambay Basin, western India. The study of biomarkers, palynological remains and petrography is taken as proxies for providing supportive evidence for our inference. The petrographic results reveal that the sediments are thermally immature and coalification was extended up to the lignitic stage (low rank B). The palynological results show the dominance of angiosperms, mainly members belonging to the Arecaceae family, throughout the studied section. Triterpenoids with oleanane, ursane and lupane structure in extractable organic matter are derived from angiosperm wax. Pollen grains (Spinizonocolpites, Proxapertites, Dipterocarpuspollenites, Albertipollenites, Retipollenites, Arengapollenites, Lakiapollis and Longapertites) with pteridophyte spores and fungal fruiting bodies confirm the prevalence of tropical to subtropical climate during the deposition of the sediments. Sesquiterpenoids like longifolene-12, methanoazulene, cadinane and 8-selinene together with amyrin derivatives are the indicator of Dipterocarpaceae family that grows in the extant tropical rain forests in SE Asia. Appearance of dinoflagellate cysts and the predominance of lower molecular weight part in n-alkane series with the signature of submerged/floating vegetation in the shale horizon indicate marine influence in the younger part of the mine section. The presence of mangrove pollen such as Spinizonocolpites, Proxapertites and Acanthotricolpites further suggests that the lignite-bearing sequence was deposited in marshy marginal marine environment. (C) 2015 Elsevier BM. All rights reserved.	[Paul, Swagata; Sharma, Jyoti; Saraswati, Pratul K.; Dutta, Suryendu] Indian Inst Technol, Dept Earth Sci, Mumbai 400076, Maharashtra, India; [Singh, Bhagwan D.] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Bombay; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Paul, S (通讯作者)，Indian Inst Technol, Dept Earth Sci, Mumbai 400076, Maharashtra, India.	swagata@iitb.ac.in; s.dutta@iitb.ac.in	Paul, Swagata/G-6064-2019; Dutta, Suryakanti/JXM-1340-2024	Dutta, Suryendu/0000-0003-2969-116X	Oil Industry Development Board (OIDB) [4/27/2009-OIDB DT.2/2/2011]; Department of Science and Technology (DST)	Oil Industry Development Board (OIDB); Department of Science and Technology (DST)(Department of Science & Technology (India))	We would like to express our gratitude to Oil Industry Development Board (OIDB) (4/27/2009-OIDB DT.2/2/2011) for the financial support for organic geochemical study. 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J	Petrick, BF; McClymont, EL; Marret, F; van der Meer, MTJ				Petrick, Benjamin F.; McClymont, Erin L.; Marret, Fabienne; van der Meer, Marcel T. J.			Changing surface water conditions for the last 500 ka in the Southeast Atlantic: Implications for variable influences of Agulhas leakage and Benguela upwelling	PALEOCEANOGRAPHY			English	Article							LONG-CHAIN ALKENONES; HYDROGEN ISOTOPIC COMPOSITION; WIND-DRIVEN CIRCULATION; NORTH-ATLANTIC; INDIAN-OCEAN; CLIMATE VARIABILITY; EAST ATLANTIC; SEA; MIDPLEISTOCENE; SALINITY	The Southeast Atlantic Ocean is an important component of global ocean circulation, as it includes heat and salt transfer into the Atlantic through the Agulhas leakage as well as the highly productive Benguela upwelling system. Here we reconstruct sea surface temperatures (SSTs) from Ocean Drilling Program (ODP) Site 1087 in the Southeast Atlantic to investigate surface ocean circulation patterns during the late Pleistocene (0-500 ka). The U-37(K)' index and dinoflagellate cyst assemblages are used to reconstruct SSTs, delta D-alkenone is used to reconstruct changes in sea surface salinity, and mass accumulation rates of alkenones and chlorine pigments are quantified to detect changing marine export productivity. The greatest amplitude of SST warming precedes decreases in benthic delta O-18 and therefore occurs early in the transition from glacials to interglacials. The dDalkenone, as a salinity indicator, increases before SSTs, suggesting that the pattern of Agulhas leakage is more complex than suggested by SST proxies. Marine isotope stage (MIS) 10 shows an anomalous pattern: it is marked by a pronounced increase in chlorine concentration, which may be related to enhanced/expanded Benguela upwelling reaching the core site. We find no evidence of an absence of Agulhas leakage throughout the record, suggesting that there is no Agulhas cutoff even during MIS 10. Finally, the ODP Site 1087 record shows an increasing strength of Agulhas leakage towards the present day, which may have impacted the intensity of the Atlantic meridional overturning circulation. As a result, the new analyses from ODP Site 1087 demonstrate a complex interaction between influences of the Benguela upwelling and the Agulhas leakage through the late Pleistocene, which are inferred here to reflect changing circulation patterns in the Southern Ocean and in the atmosphere.	[Petrick, Benjamin F.] Newcastle Univ, Sch Geog Polit & Sociol, Newcastle Upon Tyne NE1 7RU, Tyne & Wear, England; [McClymont, Erin L.] Univ Durham, Dept Geog, Durham, England; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 3BX, Merseyside, England; [van der Meer, Marcel T. J.] NIOZ Royal Netherlands Inst Sea Res, Den Burg, Texel, Netherlands	Newcastle University - UK; Durham University; University of Liverpool; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Petrick, BF (通讯作者)，Newcastle Univ, Sch Geog Polit & Sociol, Newcastle Upon Tyne NE1 7RU, Tyne & Wear, England.	benjamin.petrick@newcastle.ac.uk	Petrick, Benjamin/JWP-5723-2024; McClymont, Erin/AAX-3657-2020; van der Meer, Marcel/L-3450-2013; McClymont, Erin/K-2153-2012	van der Meer, Marcel/0000-0001-6454-1752; Petrick, Benjamin/0000-0002-4211-0625; McClymont, Erin/0000-0003-1562-8768; Marret-Davies, Fabienne/0000-0003-4244-0437	School of Geography, Politics and Sociology (Newcastle University) by a PhD studentship; Dutch Organisation for Scientific Research (NWO) through a VIDI grant	School of Geography, Politics and Sociology (Newcastle University) by a PhD studentship; Dutch Organisation for Scientific Research (NWO) through a VIDI grant(Netherlands Organization for Scientific Research (NWO))	This research used samples provided by the Integrated Ocean Drilling Program. Funding for this research was provided by the School of Geography, Politics and Sociology (Newcastle University) by a PhD studentship (B.F.P.). We also thank Catherine Pierre, Jacques Giraudeau, Dick Kroon, Thibaut Caley, and Gema Martinez-Mendez for the provision of data and Aurora Elmore, Rebecca Payne, Andrew Henderson, Richard Pancost, and James Petrick for their constructive comments on an earlier draft of the manuscript. Marcel van der Meer was funded by the Dutch Organisation for Scientific Research (NWO) through a VIDI grant. Finally, we would like to thank anonymous reviewers for their helpful and constructive comments. 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J	Bijl, PK; Brinkhuis, H				Bijl, Peter K.; Brinkhuis, Henk			A new genus and two new species of dinoflagellate cysts from lower Eocene marine sediments of the Wilkes Land Margin, Antarctica	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Antarctic Margin; Early Eocene; Organic walled dinoflagellate cyst taxonomy; Biostratigraphy	SOUTH-PACIFIC; NEW-ZEALAND; CLIMATE; SECTOR; OCEAN	Integrated Ocean Drilling Program (IODP) Expedition 318 recovered lower Eocene sediments in Hole U1356A from the continental rise of the Wilkes Land Margin, Antarctica. These sediments yielded a new genus of organic-walled dinoflagellate cysts (Adeliesphaera gen. nov.). We tentatively place this new genus within the suborder Gonyaulacineae, family Areoligeraceae, based on the obligate apical archeopyle, the asymmetric antapical geometry and the left-side offset sulcal notch. We herein describe the type species of Adeliesphaera gen. nov., Adeliesphaera ohanlonii sp. nov., as well as a new species of Turbiosphaera, Turbiosphaera guersteinae sp. nov. The short stratigraphic range of both species (53.7-53.4 Ma and 53.1-52.9 Ma, respectively) qualifies them as potentially important regional Southern Ocean stratigraphic markers for high-resolution age control. (C) 2015 Elsevier B.V. All rights reserved.	[Bijl, Peter K.; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Paleobot & Palyn, NL-3508 TC Utrecht, Netherlands; [Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Paleobot & Palyn, POB 80-115, NL-3508 TC Utrecht, Netherlands.	p.k.bijl@uu.nl	Brinkhuis, Henk/IUO-8165-2023	Bijl, Peter/0000-0002-1710-4012; Brinkhuis, Henk/0000-0003-0253-6610	U.S. National Science Foundation; Dutch National Science Foundation (NWO) [866.10.110, 863.13.002]	U.S. National Science Foundation(National Science Foundation (NSF)); Dutch National Science Foundation (NWO)(Netherlands Organization for Scientific Research (NWO))	We thank Chris Clowes and one anonymous reviewer for their helpful comments, which really improved the manuscript. This research used samples from the Integrated Ocean Drilling Program (IODP). IODP was sponsored by the U.S. National Science Foundation and participating countries under management of Joined Oceanographic Institutions inc. Both authors thank the Dutch National Science Foundation (NWO; NPP Grant 866.10.110 to H.B.; VENI Grant 863.13.002 to P.K.B) for financial support. Natasja L.D. Welters is thanked for sample processing and slide preparation. Gea Zijlstra, Rob Fensome and Graham Williams are thanked for help with taxonomy and nomenclature.	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Palaeobot. Palynology	SEP	2015	220						88	97		10.1016/j.revpalbo.2015.05.004	http://dx.doi.org/10.1016/j.revpalbo.2015.05.004			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	CM1KC		Green Published			2025-03-11	WOS:000357438800007
J	Silva, RL; Duarte, LV				Silva, Ricardo L.; Duarte, Luis V.			Organic matter production and preservation in the Lusitanian Basin (Portugal) and Pliensbachian climatic hot snaps	GLOBAL AND PLANETARY CHANGE			English	Article						Elemental geochemistry; Black shales; Paleoceanography; Pliensbachian; Lusitanian Basin	OCEANIC ANOXIC EVENT; BASQUE-CANTABRIAN BASIN; WATER MASS-EXCHANGE; CARBONATE PRODUCTION; ATMOSPHERIC CO2; REVISED MODEL; SOURCE-ROCK; NORTHERN; GEOCHEMISTRY; STRATIGRAPHY	The Pliensbachian (Early Jurassic) hemipelagic carbonate series of the Lusitanian Basin (Portugal) are of major importance as this basin is located at a key position between the Tethyan and Boreal (North European) realms. One of the most conspicuous features of this basin is the organic-rich nature of most of the Margaritatus Chronozone hemipelagic deposits, with the occurrence of several well-defined regional black shales. The analysis of selected redox sensitive elements (V, Cr, Co, Ni, Mo, and U) from the worldwide reference section of Peniche indicates that in this basin most of the organic-rich fades of the Ibex-Margaritatus chronozones were deposited under an oxic-dysoxic regime, while the rare centimetre thick well-defined black shales were deposited and preserved under suboxic-anoxic, intermittently euxinic conditions. Based on the integration of sedimentological, biostratigraphical, geochemical, and organic petrographic evidence we suggest that these basinwide black shales, corresponding to widespread mucilage and microbial outbreaks, were driven by extreme climate warming coupled with high oceanic productivity and intermittently stratified epeiric seas. Regionally, these "hot snaps" may have promoted the observed rapid but short-lived expansion of Tethyan ammonites into Boreal domains or led to decrease benthic diversity. Ensuing cooling during the Margaritatus Chronozone was accompanied by southwards influx of northwards ammonite fauna or radiation of cyst forming dinoflagellates. Worldwide preservation of organic matter during the Late Pliensbachian seems to have resulted in decreased atmospheric CO2 levels through geological storage of carbon, triggering and/or amplifying the Spinatum Chronozone icehouse event. Ultimately, this cooling event may have led to the occurrence of permafrost and/or methane gas hydrates in locations easily disturbed by the subsequent Early Toarcian warming, or/and volcanic activity driven by crustal unloading due to deglaciation. (C) 2015 Elsevier B.V. All rights reserved.	[Silva, Ricardo L.] Dalhousie Univ, Basin & Reservoir Lab, Dept Earth Sci, Halifax, NS B3H 4J1, Canada; [Duarte, Luis V.] Univ Coimbra, MARE Marine & Environm Sci Ctr, Fac Sci & Technol, P-3030790 Coimbra, Portugal	Dalhousie University; Universidade de Coimbra	Silva, RL (通讯作者)，Dalhousie Univ, Basin & Reservoir Lab, Dept Earth Sci, Halifax, NS B3H 4J1, Canada.	ricardo.silva@dal.ca; lduarte@dct.uc.pt	Duarte, Luis/F-5282-2013; Silva, Ricardo L./G-2183-2010	Duarte, Luis/0000-0002-9025-5896; Silva, Ricardo L./0000-0002-4361-8455	FCT-MCTES [SFRH/BD/47362/2008]; ExxonMobil Canada Proprieties (Sable Offshore Energy Project) through the Petroleum Geoscience Research Grant; FCT-Portugal [PTDC/CTE-GIX/098968/2008]; COMPETE-FEDER [PTDC/CTE-GIX/098968/2008]; Fundação para a Ciência e a Tecnologia [PTDC/CTE-GIX/098968/2008, SFRH/BD/47362/2008] Funding Source: FCT	FCT-MCTES(Fundacao para a Ciencia e a Tecnologia (FCT)); ExxonMobil Canada Proprieties (Sable Offshore Energy Project) through the Petroleum Geoscience Research Grant(Exxon Mobil Corporation); FCT-Portugal(Fundacao para a Ciencia e a Tecnologia (FCT)); COMPETE-FEDER(European Union (EU)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	Ricardo L. Silva thanks the FCT-MCTES for funding through a PhD fellowship (SFRH/BD/47362/2008), the ExxonMobil Canada Proprieties (on behalf of the Sable Offshore Energy Project) for financial support through the Petroleum Geoscience Research Grant to Dalhousie University (Basin and Reservoir Lab), and the Industry partners of the Consortium Source Rock and Geochemistry of the Central Atlantic Margins. This work has been partially supported by project PTDC/CTE-GIX/098968/2008 - "High resolution stratigraphy of the Lower Jurassic organic-rich marine series in the Lusitanian Basin" (FCT-Portugal and COMPETE-FEDER).	Aberhan M, 2003, GEOLOGY, V31, P1077, DOI 10.1130/G19938.1; Algeo TJ, 2009, CHEM GEOL, V268, P211, DOI 10.1016/j.chemgeo.2009.09.001; ALLDREDGE AL, 1993, DEEP-SEA RES PT I, V40, P1131, DOI 10.1016/0967-0637(93)90129-Q; Alves TM, 2002, MAR PETROL GEOL, V19, P727, DOI 10.1016/S0264-8172(02)00036-3; [Anonymous], 1990, Deposition of Organic Facies; [Anonymous], 1988, Jahrb. Geol. 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J	Craveiro, SC; Daugbjerg, N; Moestrup, O; Calado, AJ				Craveiro, Sandra C.; Daugbjerg, Niels; Moestrup, Ojvind; Calado, Antonio J.			Fine-structural characterization and phylogeny of <i>Peridinium polonicum</i>, type species of the recently described genus <i>Naiadinium</i> (Dinophyceae)	EUROPEAN JOURNAL OF PROTISTOLOGY			English	Article						ITS rDNA; Naiadinium polonicum; Phylogeny; Pusule; Scrippsiella; Ultrastructure	FRESH-WATER DINOFLAGELLATE; RDNA-BASED PHYLOGENY; SP-NOV DINOPHYCEAE; FLAGELLAR APPARATUS; MARINE DINOFLAGELLATE; HETEROTROPHIC DINOFLAGELLATE; CALCAREOUS CYSTS; ULTRASTRUCTURE; THORACOSPHAERACEAE; TAXONOMY	Peridinium polonicum is a freshwater peridinioid with an unusual tabulation that includes one or two anterior intercalary plates in the mid-dorsal axis, and in such a low position that it seems inset in precingular Plate 4. Although the species has been classified in both Peridinium and Peridiniopsis, evidence from nucleotide sequences consistently shows that its closest relatives are within the Scrippsiella group. The genus Naiadinium Carty has been recently described with P. polonicum as its type species. However, Naiadinium was separated from other peridinioids only on the basis of shape and plate arrangements and these characters do not allow reliable determination of its closest phylogenetic relatives. Serial section fine-structural analysis revealed the presence of a small peduncle supported by a conspicuous microtubular basket that extended far into the cell; a complex pusular system that included a collecting chamber from which about 70 pusular tubes radiated; a flagellar apparatus with general peridinioid characters but with an unusually large distance of nearly 700 nm between basal bodies. An ITS1-5.8S-ITS2 rDNA-based phylogenetic analysis grouped, with high statistical support, Naiadinium polonicum with three species currently placed in Scrippsiella, viz. S. irregularis, S. precaria and S. ramonii. (C) 2015 Elsevier GmbH. All rights reserved.	[Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; [Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, GeoBioTec Res Unit, P-3810193 Aveiro, Portugal; [Daugbjerg, Niels; Moestrup, Ojvind] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-2100 Copenhagen O, Denmark	Universidade de Aveiro; Universidade de Aveiro; University of Copenhagen	Craveiro, SC (通讯作者)，Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal.	scraveiro@ua.pt	Calado, Sandra Carla/A-6791-2016; Daugbjerg, Niels/D-3521-2014; Calado, Antonio Jose/D-6263-2015	Calado, Sandra Carla/0000-0002-2738-7626; Daugbjerg, Niels/0000-0002-0397-3073; Calado, Antonio Jose/0000-0002-9711-0593	QREN - POPH - Tipologia 4.1 - Formacao Avancada [SFRH/BPD/68537/2010]; European Social Funding (FSE); Portuguese Ministry of Education and Science (MEC);  [PEst-OE/CTE/UI4035/2014]; Fundação para a Ciência e a Tecnologia [PEst-OE/CTE/UI4035/2014, SFRH/BPD/68537/2010] Funding Source: FCT	QREN - POPH - Tipologia 4.1 - Formacao Avancada; European Social Funding (FSE)(European Social Fund (ESF)); Portuguese Ministry of Education and Science (MEC); ; Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	SCC was supported by a grant (SFRH/BPD/68537/2010) from the financing program "QREN - POPH - Tipologia 4.1 - Formacao Avancada" and by the European Social Funding (FSE) and the Portuguese Ministry of Education and Science (MEC). GeoBioTec was funded by PEst-OE/CTE/UI4035/2014.	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J	Segit, T; Matyja, BA; Wierzbowski, A				Segit, Tomasz; Matyja, Bronislaw A.; Wierzbowski, Andrzej			The Middle Jurassic succession in the central sector of the Pieniny Klippen Belt (Sprzycne Creek): implications for the timing of the Czorsztyn Ridge development	GEOLOGICA CARPATHICA			English	Article						Middle Jurassic; Pieniny Klippen Belt; Magura Basin; "black flysch"; stratigraphy; dinoflagellate cysts	BLACK FLYSCH; DINOFLAGELLATE CYSTS; BAJOCIAN; AGE; CARPATHIANS; EVOLUTION; DEPOSITS; MTS.	In this study, we revisit the stratigraphic age and discuss sedimentary characteristics of the lower Middle Jurassic turbidite deposits ("black flysch") of the Szlachtowa Formation, as well as the under- and overlying members of the Sprzycne Creek section situated in the central sector of the Pieniny Klippen Belt (Poland). We show that the succession captures the lower Middle Jurassic marine sediments of the pre-Late Albian Magura Basin, located to the north of an ancient submarine swell (Czorsztyn Ridge). The turbidite deposits of the Szlachtowa Formation and marly shales of the Opaleniec Formation yield dinoflagellate cysts indicative of the latest Aalenian or learliest Bajocian to Early Bathonian. The character of these deposits, and their location below the overthrusted Subpieniny Nappe show that this succession does not belong to the successions of the Oravicum domain, located on the southern side of the Czorsztyn Ridge. The Szlachtowa Formation is underlain by the Skrzypny Formation, which is reported for the first time outside the Oravicum domain. It suggests that the pre-Late Albian Magura Basin came into existence not earlier than during the latest Aalenian, following the rising of the Czorsztyn Ridge. The marly shales assigned here to the Opaleniec Formation of Late Bajocian-Bathonian age and younger marly deposits of Cretaceous age were distinguished in the past as the so-called "Sprzycne beds" of Cretaceous age. However, the combination of these two rock units into a single lithostratigraphic unit is unsuitable because they represent two separated stratigraphical intervals and their contact is tectonic.	[Segit, Tomasz; Matyja, Bronislaw A.] 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	Segit, T (通讯作者)，Univ Warsaw, Inst Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	t.segit@uw.edu.pl; matyja@uw.edu.pl; andrzej.wierzbowski@pgi.gov.pl		Segit, Tomasz/0000-0003-2952-6332	Institute of Geology (Faculty of Geology, University of Warsaw) [BST 160600/2]	Institute of Geology (Faculty of Geology, University of Warsaw)	This research was supported by an internal Grant from the Institute of Geology (Faculty of Geology, University of Warsaw) No. BST 160600/2. We are grateful to Zofia Dubicka, PhD (Dept. of Palaeontology, Institute of Geology, University of Warsaw) for planktonic foraminiferal dating of samples. We wish to thank three reviewers for their insightful feedback and dr. E. Jurewicz for fruitful discussions on the topic of this paper. R. Nawrot is gratefully acknowledged for help and fieldwork assistance.	[Anonymous], 2012, Miner Slovaca; Aubrecht Roman, 1994, Geologica Carpathica, V45, P211; Aubrecht Roman, 2004, Mineralia Slovaca, V36, P1; Barski M, 2012, GEOL Q, V56, P391, DOI 10.7306/gq.1030; BIRKENMAJER K, 1977, Acta Geologica Polonica, V27, P387; Birkenmajer K., 1963, Annales de la Societe Geologique de Pologne, V33, P415; Birkenmajer K., 1965, Annales de la Societe Geologique de Pologne, V35, P327; Birkenmajer K., 1953, B ACAD POL SCI, V1, P271; Birkenmajer K., 1986, STUDIA GEOLOGICA POL, V88, P7; Birkenmajer K., 1977, Stud. Geol. 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Pol. Tow. Geol, V4, P221; Sikora W., 1971, 43 M POL GEOL SOC KR, P241; Traverse A., 2007, Topics in Geobiology Series, American Association of Stratigraphic Palynologists Foundation, V28, P1; Uchman A., 2006, PALAEOTECTONIC EVOLU, P85; Underhill J. R., 1994, Siliciclastic Sequence Stratigraphy: Recent Developments and Applications, V58, P449, DOI DOI 10.1306/M58581C18; Wierzbowski A., 1999, STUD GEOL POL, V74, P237	57	16	18	0	3	SLOVAK ACAD SCIENCES GEOLOGICAL  INST	BRATISLAVA	DUBRAVSKA CESTA 9, BRATISLAVA, 840 05, SLOVAKIA	1335-0552	1336-8052		GEOL CARPATH	Geol. Carpath.	AUG	2015	66	4					285	302		10.1515/geoca-2015-0026	http://dx.doi.org/10.1515/geoca-2015-0026			18	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CR0IH		Green Submitted, gold			2025-03-11	WOS:000361001400003
J	Krock, B; Borel, CM; Barrera, F; Tillmann, U; Fabro, E; Almandoz, GO; Ferrario, M; Cardona, JEG; Koch, BP; Alonso, C; Lara, R				Krock, Bernd; Marcela Borel, C.; Barrera, Facundo; Tillmann, Urban; Fabro, Elena; Almandoz, Gaston O.; Ferrario, Martha; Garzon Cardona, John E.; Koch, Boris P.; Alonso, Cecilia; Lara, Ruben			Analysis of the hydrographic conditions and cyst beds in the San Jorge Gulf, Argentina, that favor dinoflagellate population development including toxigenic species and their toxins	JOURNAL OF MARINE SYSTEMS			English	Article						Coastal water masses; Southwest Atlantic; Planktonic community; Toxins; Alexandrium tamarense; Protoceratium reticulatum; LC-MS/MS; Dinoflagellate bloom; Dinoflagellate cysts	DIARRHEIC SHELLFISH TOXINS; SOUTHERN PATAGONIAN SHELF; BUENOS-AIRES PROVINCE; ALEXANDRIUM-TAMARENSE; VERTICAL MIGRATION; PHYTOPLANKTON BLOOMS; CHLOROPHYLL; SEA; VARIABILITY; AMERICA	The overlay of cooler nutrient enriched Beagle-Magellan water with warmer nutrient depleted shelf water and a strong stratification of the water column in the San Jorge Gulf region, Argentina, coincided with relatively high dinoflagellate abundances in April 2012, up to 34,000 cells L-1. This dinoflagellate proliferation was dominated by Ceratium spp., but environmental conditions also favored to a lesser amount the occurrence of toxigenic dinoflagellates, such as Atexandrium tamarense and Protoceratium reticulatum, whose toxins were hardly detected in any other areas along the expedition transect of the R/V Puerto Deseado between 38 and 56 degrees S (Ushuaia-Mar del Plata) in March/April 2012. Generally vegetative cells of A. tamarense and P. reticulatum co-occurred with their respective phycotoxins in the water column and their cysts in the upper sediment layers. Two strains of A. tamarense were isolated from the bloom sample and morphologically characterized. Their PSP toxin profiles consisted of C1/2, gonyautoxins 1/4 and to a lesser amount of neosaxitoxin and confirmed earlier data from this region. The ratios between autotrophic picoplankton and heterotrophic bacteria were higher in shelf waters in the north than in Beagle-Magellan waters in the south of San Jorge Gulf. (C) 2015 Elsevier B.V. All rights reserved.	[Krock, Bernd; Tillmann, Urban; Koch, Boris P.] Alfred Wegener Inst Polar & Marine Res, Helmholtz Zentrum Polar & Meeresforsch, Chem Okol, D-27570 Bremerhaven, Germany; [Marcela Borel, C.] Univ Nacl Sur, CONICET, Inst Geol Sur, Dept Geol,Lab Palinol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Barrera, Facundo; Garzon Cardona, John E.; Lara, Ruben] Consejo Nacl Invest Cient & Tecn, IADO, Biogeoquim Marina, Bahia Blanca, Buenos Aires, Argentina; [Fabro, Elena; Almandoz, Gaston O.; Ferrario, Martha] Univ Nacl La Plata, Fac Ciencias Nat & Museo, Div Ficol, RA-1900 La Plata, Buenos Aires, Argentina; [Marcela Borel, C.; Barrera, Facundo; Fabro, Elena; Almandoz, Gaston O.; Ferrario, Martha; Garzon Cardona, John E.; Lara, Ruben] Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina; [Koch, Boris P.] Univ Appl Sci, D-27568 Bremerhaven, Germany; [Alonso, Cecilia] Univ Republ, Ctr Univ Reg Este, Rocha 27000, Uruguay	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of La Plata; Museo La Plata; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad de la Republica, Uruguay	Krock, B (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Helmholtz Zentrum Polar & Meeresforsch, Chem Okol, Handelshafen 12, D-27570 Bremerhaven, Germany.	bernd.krock@awi.de	Krock, Bernd/ABB-7541-2020; Alonso, Cecilia/IWU-9937-2023; Koch, Boris/B-2784-2009	Borel, C. Marcela/0000-0001-5772-4534; Koch, Boris/0000-0002-8453-731X; Almandoz, Gaston O./0000-0001-7931-582X; Alonso, Cecilia/0000-0003-3869-4418	Binational project MINCyT-BMBF [AL/11/03-ARG 11/021]; EU project IMCONet (FP7 IRSES) [319718]; HGF (Helmholtz Association of German Research Centres) through the research programme PACES; PIP CONICET [11420100100234, 11420100100173]	Binational project MINCyT-BMBF; EU project IMCONet (FP7 IRSES); HGF (Helmholtz Association of German Research Centres) through the research programme PACES; PIP CONICET(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET))	This work was financed by the Binational project MINCyT-BMBF (AL/11/03-ARG 11/021). Additional funding was provided in the frames of the EU project IMCONet (FP7 IRSES, action no. 319718) and the HGF (Helmholtz Association of German Research Centres) through the research programme PACES. 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Mar. Syst.	AUG	2015	148						86	100		10.1016/j.jmarsys.2015.01.006	http://dx.doi.org/10.1016/j.jmarsys.2015.01.006			15	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	CK9FQ		Green Published			2025-03-11	WOS:000356546400008
J	Eldrett, JS; Ma, C; Bergman, SC; Ozkan, A; Minisini, D; Lutz, B; Jackett, SJ; Macaulay, C; Kelly, AE				Eldrett, James S.; Ma, Chao; Bergman, Steven C.; Ozkan, Aysen; Minisini, Daniel; Lutz, Brendan; Jackett, Sarah-Jane; Macaulay, Calum; Kelly, Amy E.			Origin of limestone-marlstone cycles: Astronomic forcing of organic-rich sedimentary rocks from the Cenomanian to early Coniacian of the Cretaceous Western Interior Seaway, USA	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Cretaceous; Cenomanian-Turonian; OAE-2; Milankovitch cycles; paleoclimate; Eagle Ford Group	WALLED DINOFLAGELLATE CYSTS; BOUNDARY EVENT; TRACE-METALS; CARBONATE; PRESERVATION; PROXIES; BASIN; PALEOPRODUCTIVITY; BIODIVERSITY; GREENHOUSE	We present an integrated multidisciplinary study of limestone-marlstone couplets from a continuously cored section including parts of the upper Buda Limestone, the entire Eagle Ford Group (Boquillas Formation) and lower Austin Chalk from the Shell Iona-1 research borehole (Texas, USA), which provides a >8 million year (myr) distal, clastic sediment-starved, intrashelf basin record of the early Cenomanian to the earliest Coniacian Stages. Results show that despite variable yet minimal diagenetic overprints, several unambiguous primary environmental signals are preserved and support greater water-mass ventilation and current activity promoting increased silica/carbonate productivity during the deposition of limestone beds compared to deposition of marlstone beds which reflect greater organic matter productivity and preservation. Furthermore, our astronomical analyses demonstrate that the limestone-marlstone couplets in the Iona-1 core reflect climatic forcing driven by solar insolation resulting from integrated Milankovitch periodicities. In particular, we propose that obliquity and precession forcing on the latitudinal distribution of solar insolation may have been responsible for the observed lithological and environmental variations through the Cenomanian, Turonian and Coniacian in this mid-latitude epicontinental sea setting. Our data also suggests that rhythmic lithological alternations deposited in Greenhouse periods, in general, may simply reflect climate-driven cycles related to Earth-Sun dynamics without the need to invoke significant sea-level variations. (C) 2015 Elsevier B.V. All rights reserved.	[Eldrett, James S.; Ma, Chao; Bergman, Steven C.; Ozkan, Aysen; Minisini, Daniel; Lutz, Brendan; Jackett, Sarah-Jane; Macaulay, Calum; Kelly, Amy E.] Shell Int Explorat & Prod Inc, Houston, TX 77082 USA; [Ma, Chao] Univ Wisconsin, Dept Geosci, Madison, WI 53706 USA; [Lutz, Brendan; Jackett, Sarah-Jane] Shell Explorat & Prod Inc, Houston, TX 77079 USA	Royal Dutch Shell; University of Wisconsin System; University of Wisconsin Madison	Eldrett, JS (通讯作者)，Shell Int Explorat & Prod Inc, 3333 Highway 6 South, Houston, TX 77082 USA.	james.eldrett@shell.com	Ma, Chao/AAC-8569-2020; MacAulay, Calum/K-1795-2016; Bergman, Steven/AAZ-2256-2020	bergman, steven/0000-0002-1292-6535; Ma, Chao/0000-0002-0122-5696; Eldrett, James/0000-0001-5196-3112	Shell International Exploration and Production Inc.	Shell International Exploration and Production Inc.	We acknowledge analytical contributions of Bob Gregory and Kurt Ferguson (the Stable Isotope Laboratory at Southern Methodist University, USA) and colleagues at Shell, in particular lain Prince and Ru Smith for internal reviews, Aaron Shunk for astrochronology discussions, and David Lavallee and Nick Howes for writing Mat Lab code enabling the isolation and removal of core cracks from the grayscale data. We acknowledge the contribution of Paul Dodsworth, Petros Hardas, John Gregory and Mark Phipps for biostratigraphic insights. We would also like to thank Brad Sageman and an anonymous journal reviewer for excellent suggestions which greatly improved the manuscript. This research was conducted and funded by Shell International Exploration and Production Inc., and we thank our Shell leadership for permission to publish.	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Sci. Lett.	AUG 1	2015	423						98	113		10.1016/j.epsl.2015.04.026	http://dx.doi.org/10.1016/j.epsl.2015.04.026			16	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	CK3LG					2025-03-11	WOS:000356117000010
J	Kretschmann, J; Elbräzchter, M; Zinssmeister, C; Soehner, S; Kirsch, M; Kusber, WH; Gottschling, M				Kretschmann, Juliane; Elbraezchter, Malte; Zinssmeister, Carmen; Soehner, Sylvia; Kirsch, Monika; Kusber, Wolf-Henning; Gottschling, Marc			Taxonomic clarification of the dinophyte <i>Peridinium acuminatum</i> Ehrenb., <i>Scrippsiella acuminata, comb. nov</i>. (Thoracosphaeraceae, Peridiniales)	PHYTOTAXA			English	Article						calcareous dinoflagellates; epitypification; Goniodoma; molecular systematics; morphology; nomenclature; taxonomy	DINOFLAGELLATE RESTING CYSTS; GENERIC NAMES; KIEL BIGHT; TROCHOIDEA; CLASSIFICATION; MORPHOLOGY; DIVERSITY; SEDIMENTS; GENUS	Peridinium acuminatum (Peridiniales, Dinophyceae) was described in the first half of the 19th century, but the name has been rarely adopted since then. It was used as type of Goniodoma, Heteraulacus and Yesevius, providing various sources of nomenclatural and taxonomic confusion. Particularly, several early authors emphasised that the organisms investigated by C.G. Ehrenberg and S.F.N.R. von Stein were not conspecific, but did not perform the necessary taxonomic conclusions. The holotype of P. acuminatum is an illustration dating back to 1834, which makes the determination of the species ambiguous. We collected, isolated, and cultivated Scrippsiella acuminata, comb. nov. (strain GeoB 427) from the type locality off Kiel, Germany (Baltic Sea). We barcoded the species of the Thoracosphaeraceae using rRNA sequences and investigated the morphology of the strain using light and electron microscopy. As taxonomic result, we designate an epitype for Peridinium acuminatum, as no conflict with C.G. Ehrenberg's protologue can be stated. It is indistinguishable from Scrippsiella trochoidea (likewise described from the Kiel Fjord) that we consider a later heterotypic synonym. Our study contributes to the disentanglement of dinophyte taxonomy in a very challenging case, and we trust that C.G. Ehrenberg and S.F.N.R. von Stein investigated different species under the epithet 'acuminatum'. The complex nomenclature and taxonomy of Goniodoma, and its type species Goniodoma acuminatum, is discussed in the Electronic Supplement. We consider Pyrrhotriadinium, with the type species Pyrrhotriadinium polyedricum (Gonyaulacales), well suited to harbour all gonyaulacalean taxa so far assigned to Goniodoma and Heteraulacus as well.	[Kretschmann, Juliane; Zinssmeister, Carmen; Soehner, Sylvia; Gottschling, Marc] Univ Munich, Dept Biol, GeoBio Ctr, Dept Biol Systemat Bot & Mykol, D-80638 Munich, Germany; [Elbraezchter, Malte] Helmholtz Zentrum Polar & Meeresforschung, Wattenmeerstat Sylt Alfred Wegener Inst, D-25992 List Auf Sylt, Germany; [Zinssmeister, Carmen] German Ctr Marine Biodivers Res DZMB, Senckenberg Meer, D-26382 Wilhelmshaven, Germany; [Kirsch, Monika] Univ Bremen, Fachbereich Geowissensch Fachrichtung Hist Geol, D-28359 Bremen, Germany; [Kusber, Wolf-Henning] Free Univ Berlin, Botan Garten, D-14195 Berlin, Germany; [Kusber, Wolf-Henning] Free Univ Berlin, Botan Museum Berlin Dahlem, D-14195 Berlin, Germany	University of Munich; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); University of Bremen; Free University of Berlin; Free University of Berlin	Gottschling, M (通讯作者)，Univ Munich, Dept Biol, GeoBio Ctr, Dept Biol Systemat Bot & Mykol, Menzinger Str 67, D-80638 Munich, Germany.	gottschling@bio.lmu.de	Gottschling, Marc/K-2186-2014		Deutsche Forschungsgemeinschaft [KE 322/36, RI 1738/5, WI 725/2]; Munchener Universitatsgesellschaft	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); Munchener Universitatsgesellschaft	Eva Facher and Martina Silber (both Munich) supported our lab work that is gratefully acknowledged here. We are thankful to Andrea Krone (Berlin) for providing us with high resolution scans of Ehrenberg's published prints. ME thanks the Alfred-Wegener-Institut (List / Sylt) for the continued use of research facilities. Financial support was provided by the Deutsche Forschungsgemeinschaft (grants KE 322/36, RI 1738/5, and WI 725/25) and the Munchener Universitatsgesellschaft. We acknowledge valuable and constructive comments from five anonymous reviewers.	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J	Pospelova, V; Price, AM; Pedersen, TF				Pospelova, Vera; Price, Andrea M.; Pedersen, Thomas F.			Palynological evidence for late Quaternary climate and marine primary productivity changes along the California margin	PALEOCEANOGRAPHY			English	Article							WALLED DINOFLAGELLATE CYSTS; SANTA-BARBARA BASIN; SEA-SURFACE TEMPERATURE; NORTHERN NORTH-ATLANTIC; NE PACIFIC; HETEROTROPHIC DINOFLAGELLATE; SELECTIVE PRESERVATION; ESTUARINE SEDIMENTS; HIGH-LATITUDES; CURRENT SYSTEM	A high-resolution sedimentary record of dinoflagellate cysts from Ocean Drilling Program Hole 1017E (off Point Conception, California margin) reflects how marine primary productivity has changed in response to major shifts in climate and ocean circulation along the California margin over the past 42 kyr. Throughout the studied sequence, dinoflagellate cyst assemblages are dominated by upwelling-related taxa, signifying the continued presence of coastal upwelling on the margin during the late Quaternary. The cyst record suggests that marine primary productivity was enhanced during the Holocene and Bolling, and to a lesser extent, during the late glacial and most Dansgaard-Oeschger events, while an apparent reduction in primary productivity can be seen during the Younger Dryas. The best analogue technique, based on a modern dinoflagellate cyst assemblage database from the northeast Pacific, was used for quantitative reconstruction of past sea surface conditions. It points to dynamic changes in annual marine primary productivity (similar to 235-331 g Cm-2 yr(-1)) and sea surface temperature (similar to 10.1-12.6 degrees C in winter; similar to 13.1-14.3-degrees C in summer), while sea surface salinity appears to be confined to a narrower range (similar to 32.9-33.4 in summer). Our results also indicate noticeable climate variability during the Holocene in this region.	[Pospelova, Vera; Price, Andrea M.; Pedersen, Thomas F.] Univ Victoria, Sch Earth & Ocean Sci, OEASB, Victoria, BC, Canada; [Price, Andrea M.] McGill Univ, Dept Geog, Montreal, PQ, Canada	University of Victoria	Pospelova, V (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, OEASB, Victoria, BC, Canada.	vpospe@uvic.ca		Price, Andrea/0000-0002-5359-053X; Pospelova, Vera/0000-0003-4049-8133	Natural Science and Engineering Research Council of Canada (NSERC) [312305]; NSERC Graduate Fellowship	Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); NSERC Graduate Fellowship(Natural Sciences and Engineering Research Council of Canada (NSERC))	Sediment samples were provided by the Integrated Ocean Drilling Program (IODP). We thank B. Conard, J. Firth, B. Horan, and P. Rumford (IODP) for their assistance in subsampling the sediments. We gratefully acknowledge R. Behl, W. Berger, E. Emmer, I. Hendy, T. Hill, T. Ivanochko, J. Kennett, D. Pak, B. Thunell, and O. Seki for kindly allowing us access to their data. The data are available to anyone upon request to the corresponding author. Funding for this research was provided by the Natural Science and Engineering Research Council of Canada (NSERC) to V.P. (discovery grant 312305). A. P. was supported by the NSERC Graduate Fellowship. We are grateful to the Editor (C. Charles) and two anonymous reviewers for their constructive suggestions which improved this manuscript.	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J	Feifel, KM; Fletcher, SJ; Watson, LR; Moore, SK; Lessard, EJ				Feifel, K. M.; Fletcher, S. J.; Watson, L. R.; Moore, S. K.; Lessard, E. J.			<i>Alexandrium</i> and <i>Scrippsiella</i> cyst viability and cytoplasmic fullness in a 60-cm sediment core from Sequim Bay, WA	HARMFUL ALGAE			English	Article						Alexandrium; Scrippsiella; Dinoflagellate cysts; Germination success; Viability; Resuspension	SPECIES COMPLEX DINOPHYCEAE; RESTING CYSTS; TROCHOIDEA DINOPHYCEAE; PUGET-SOUND; GERMINATION; RESUSPENSION; CATENELLA; EXCYSTMENT; GROWTH; GULF	Many marine protists produce a benthic resting stage during their life history. This non-motile cyst stage can either germinate near the sediment surface to provide the inoculum for subsequent blooms or, be buried by sediment deposits over time and entrained into the sedimentary record. Buried cysts can be resuspended into the water column by mixing events (e.g., storms) or other disturbances (e.g., dredging). It is not clear how long cysts can survive while buried in the sediments and still be capable of germinating given favorable conditions. Here, the germination success of cysts produced by the potentially toxic dinoflagellate genus Alexandrium and the non-toxic dinoflagellate genus Scrippsiella is reported from a 60-cm sediment core collected in Sequim Bay, WA, in December 2011. Cysts of Alexandrium spp. and Scrippsiella spp. were isolated from 2-cm sections of the core, placed in individual wells of a 96-well plate with growth medium, imaged, incubated at favorable conditions and monitored for germination. An image analysis program, DinoCyst, was used to quantitatively measure the amount of granular storage products, presumed energy stores, inside the cytoplasm to test the hypothesis that older cysts located deeper in the sediment core will have fewer energy stores available and will be less likely to germinate. An index of the area of the cytoplasm occupied with granular storage products relative to cyst size, termed 'cytoplasmic fullness', and age, based on Pb-210 dating of surrounding sediments, was compared with germination success or failure. This research indicates that cysts of Alexandrium spp. and Scrippsiella spp. can remain viable in sediments for 60 years or longer, show little visual evidence of cytoplasmic deterioration over this timescale (as measured by cytoplasmic fullness), and that germination success is statistically similar for cysts isolated from 0-60 cm deep in the sediment core. These results suggest that a cyst's cytoplasmic fullness is not indicative of viability and that cysts located as deep as 60 cm in the sediments are as likely to germinate as surface cysts given favorable conditions. (C) 2015 Elsevier B.V. All rights reserved.	[Feifel, K. M.; Fletcher, S. J.; Lessard, E. J.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA; [Watson, L. R.] CALTECH, Pasadena, CA 91125 USA; [Moore, S. K.] NOAA, Natl Marine Fisheries Serv, Seattle, WA 98122 USA	University of Washington; University of Washington Seattle; California Institute of Technology; National Oceanic Atmospheric Admin (NOAA) - USA	Feifel, KM (通讯作者)，Univ Washington, Sch Oceanog, Box 357940, Seattle, WA 98195 USA.	kfei04@uw.edu			NSF GK-12 OASIS program; University of Washington Pacific Northwest Center for Human Health and Oceans Studies; National Park Service George Melendez Wright Climate Change Fellowship	NSF GK-12 OASIS program(National Science Foundation (NSF)); University of Washington Pacific Northwest Center for Human Health and Oceans Studies; National Park Service George Melendez Wright Climate Change Fellowship	This research was funded by the NSF GK-12 OASIS program, University of Washington Pacific Northwest Center for Human Health and Oceans Studies, University of Washington Integrative Graduate Education and Research Traineeship (IGERT) on Ocean Change and had research support from the National Park Service George Melendez Wright Climate Change Fellowship. We are grateful for the technical assistance from Garfield High School (Seattle, WA) students L. Aasen, A. Maloney-Bertelli, K. Vesteins-son, and H. Xie used to develop the DinoCyst program. Thanks to C. Nittrouer, R. Hale, K. Boldt and the crew of the R/V Barnes for help obtaining and processing the sediment core. 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J	Trivedi, GK; Ranhotra, PS				Trivedi, G. K.; Ranhotra, P. S.			Palynofloral Evidence for Palaeoecology and Depositional Environment of the Kopili Formation (Late Eocene), Jaintia Hills, Meghalaya	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						Palynofloral assemblage; Kopili Formation; Late Eocene; Palaeoecology; Depositional environment; Jaintia Hills; Meghalaya; India	INDIA	A rich and diversified palynofloral assemblage has been recovered from the Kopili Formation exposed at 136 km post on Jowai-Badarpur Road, Jaintia Hills, Meghalaya, India. Besides the gymnospermous and angiospermous pollen and pteridophytic spores, the palynofloral assemblage also contains dinoflagellate cysts, fungal remains, bryophytic spores and reworked Gondwana palynofossils in good amount. Based on the distribution and habitat of the extant counterparts of recovered palynofossils, eight plant complexes have been recognized. Most families represented in the assemblage are presently distributed in the tropical to sub-tropical regions indicating almost similar climatic conditions during the deposition of Kopili sediments. The palynofloral assemblage indicates coastal to marine depositional environment with minor oscillations of sea, having fresh water connections with swamps and ponding conditions nearby.	[Trivedi, G. K.; Ranhotra, P. S.] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Trivedi, GK (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	gktrivedi19@rediffmail.com; ranhotra.p@gmail.com						[Anonymous], 1989, PALAEOBOTANIST; Baksi S.K., 1962, B GEOL MIN METALL SO, V26, P1; Banerjee D., 1973, PALEOBOTANIST, V20, P1; DAS P.K., 2001, HIMAL GEOL, V22, P55; Dasgupta A. B., 1964, 22 INT GEOL C NEW DE; DUTTA S K, 1980, Biological Memoirs, V5, P56; DUTTA S K, 1976, Geophytology, V6, P65; Dutta S.K., 1982, J PALAEONT SOC IND S, P65; MATHUR L.P., 1964, 22 SESSION, P1; Mehrotra N.C., 2000, B OIL NAT GAS COMM, V37, P145; SAH SCD, 1968, PALEOBOTANIST, V16, P177; Salujha SK, 1974, PALAEOGENES KHASI JA, V21, P267; Saxena R.K., 1982, PALEOBOTANIST, V39, P34; Saxena Ramesh K., 2009, Acta Palaeobotanica, V49, P253; Schull B.J., 1966, T GULF COAST ASS GEO, V16, P81; Sein M.K., 1974, SPEC PUBL B SAHNI I, V3, P99; SELKIRK D R, 1975, Proceedings of the Linnean Society of New South Wales, V100, P70; Singh HP., 1987, PALAEOBOTANIST, V35, P301; TRIPATHI S K M, 1985, Geophytology, V15, P164; Tripathi S.K.M., 1984, SPEC PUBL PALAEOBOTA, P316; Tripathi SKM., 1984, PALAEOBOTANIST, V32, P153; Trivedi G.K., 2000, PALAEOBOTANIST, V49, P269; Trivedi GK., 2005, APPL BOT, P183; Trivedi GK., 1991, GEOPHYTOLOGY, V20, P66; Trivedi GK., 1985, J INDIAN BOT SOC, V64, P66; Trivedi Gyanendra K., 2009, Sbornik Narodniho Muzea v Praze Rada B Prirodni Vedy, V65, P9	26	4	4	0	5	SPRINGER INDIA	NEW DELHI	7TH FLOOR, VIJAYA BUILDING, 17, BARAKHAMBA ROAD, NEW DELHI, 110 001, INDIA	0016-7622	0974-6889		J GEOL SOC INDIA	J. Geol. Soc. India	JUL	2015	86	1					33	40		10.1007/s12594-015-0278-4	http://dx.doi.org/10.1007/s12594-015-0278-4			8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CN0VX					2025-03-11	WOS:000358133200004
J	Cirilli, S; Buratti, N; Gugliotti, L; Frixa, A				Cirilli, Simonetta; Buratti, Nicoletta; Gugliotti, Luigi; Frixa, Alfredo			Palynostratigraphy and palynofacies of the Upper Triassic Streppenosa Formation (SE Sicily, Italy) and inference on the main controlling factors in the organic rich shale deposition	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Triassic; Palynofacies; Palynostratigraphy; Organic matter; Sicily; Streppenosa Formation	ST-AUDRIES BAY; JURASSIC BOUNDARY; TRIASSIC/JURASSIC BOUNDARY; PALYNOLOGICAL CHARACTERIZATION; DINOFLAGELLATE CYSTS; MEDITERRANEAN AREA; VEGETATION HISTORY; MASS EXTINCTION; CLIMATE-CHANGE; SOUTHERN ALPS	This paper focuses on the Upper Triassic Streppenosa Formation, penetrated by the Pachino 4 on-shore well, (Southern Sicily, Italy) in order to find stratigraphic age constrains and to reconstruct the paleoenvironmental evolution of this basin within the Upper Triassic palaeogeographic scenario of the western Tethys. Pachino 4 is one of the wells drilled by Eni Exploration and Production in the south-eastern Hyblean plateau with the purpose to better define the time and space distribution of reservoirs and source rocks in an area characterized by considerable subsidence and strong tectonic activity, balanced by high sedimentation rate. The Streppenosa Formation depocenter consists of a thick sequence (>2500 m) of organic rich shales, turbiditic limestones and manly limestones, grouped into three members (Lower, Middle and Upper). The well diversified microflora assemblages allow the dating of the upper part of the Lower Member and the Middle Member as Norian and the Upper Member as Rhaetian. The palynofacies variations across the Streppenosa Formation show significative changes in the relative abundances of the organic debris that, associated with the lithological and sedimentological features, allowed a reconstruction of the depositional facies successions and a hypothesis for the forcing mechanisms driving the black shale deposition. We considered that the deposition of the Streppenosa Formation occurred in an epeiric basin, under oxygen-depleted bottom waters, with different depth that varied through time in response to the sedimentation rates, eustatic sea level changes, and basin subsidence. The integration of palynofacies and lithofacies data suggests a crucial role for river runoff, responsible for water stratification and for primary productivity increase in the water column. The process was triggered by warmer and wetter climate conditions as documented in many Upper Triassic successions of the western Tethys realm. (C) 2015 Elsevier B.V. All rights reserved.	[Cirilli, Simonetta; Buratti, Nicoletta] Univ Perugia, Dipartimento Fis & Geol, I-06123 Perugia, Italy; [Gugliotti, Luigi; Frixa, Alfredo] Eni E&P, Milan, Italy	University of Perugia; Eni SpA	Cirilli, S (通讯作者)，Univ Perugia, Dipartimento Fis & Geol, Via Pascoli, I-06123 Perugia, Italy.	simonetta.cirilli@unipg.it			Sedimentary Organic Matter Laboratory [CONLABSSOR-000934]	Sedimentary Organic Matter Laboratory	The authors gratefully acknowledge Eni E&P Management for permission to study the cuttings and core samples of the Pachino 4 borehole and to publish the results. We are grateful to Amalia Spina for the useful discussions and help and to Giulia Panfili for her assistance in the laboratory. We are deeply in debt with M. H. Stephenson for his accurate review that surely improved the quality of the paper. This study was supported by the funds of the Sedimentary Organic Matter Laboratory (Grant number: CONLABSSOR-000934), directed by S. Cirilli (Perugia University, Italy).	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J	Verhoeven, K; Louwye, S				Verhoeven, Koen; Louwye, Stephen			The Pleistocene palaeoenvironment and stratigraphy of Flatey island (northern Iceland): a preliminary assessment based on palynomorphs	BOREAS			English	Article							DINOFLAGELLATE CYST STRATIGRAPHY; PLIOCENE; TJORNES; PALEOECOLOGY; SEDIMENTS; PLIOPLEISTOCENE; RECONSTRUCTION; ASSEMBLAGES; RECORD; SHELF	For the first time, palynological data (pollen, spores and dinoflagellate cysts) from Pleistocene outcrop and core deposits from Flatey, off northern Iceland, are presented. The study provides a reconnaissance stratigraphical assessment of the deposits, the correlation between the Pleistocene of Flatey and the well-known Tjornes section on the mainland, and the reconstruction of the Pleistocene palaeoenvironment. The preservation of the assemblages is poor to moderate, whereas the diversity and richness are moderate to high. The pollen and spores indicate vegetation composed mainly of sedges and heath, comparable to the vegetation in the Tjornes area during deposition of the Pleistocene Breidavik Group. Analysis of dinoflagellate cyst assemblages from an outcrop sample allowed their assignment to the Lower Pleistocene dinoflagellate cyst zone DAZ5, previously defined in the Tjornes section. A core sample yielded a dinoflagellate cyst assemblage unknown from the Tjornes area. The dinoflagellate cyst data combined with the palaeomagnetic record, the radiometric dating of lavas, and the position of the diamictites and tuff layers allowed refinement of the previously proposed stratigraphical correlations between the Tjornes area and the Flatey core. The deposition of the sequence from the Flatey core took place during the Matuyama, i.e. between 2.59 and 0.78Ma, and several hiatuses are postulated. The Lower Pleistocene dinoflagellate cyst assemblages from the outcrop sample bear similarities to those recovered from fully marine subsurface samples on the northern shelf of Iceland within the Polar Front realm. Similar oceanographical conditions influenced by the Irminger Current and the East Icelandic Current can be inferred for Early Pleistocene times.	[Verhoeven, Koen; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Ghent University	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	stephen.louwye@ugent.be	Verhoeven, Koen/IZP-9609-2023; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				Akhmetiev M.A., 1978, T ACAD SCI USSR; Albertsson K. J., 1989, JOKULL, V13, P55; Bardarson G. 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J	Rubiolo, JA; Vale, C; Martín, V; Fuwa, H; Sasaki, M; Botana, LM				Rubiolo, J. A.; Vale, C.; Martin, V.; Fuwa, H.; Sasaki, M.; Botana, L. M.			Potassium currents inhibition by gambierol analogs prevents human T lymphocyte activation	ARCHIVES OF TOXICOLOGY			English	Article						Gambierol; Heptacyclic analog of gambierol; Tetracyclic analog of gambierol; Voltage-gated potassium channels; Human T lymphocytes; Ciguatoxin; Autoimmune diseases	DINOFLAGELLATE GAMBIERDISCUS-TOXICUS; ION CHANNELS; BIOLOGICAL EVALUATION; AUTOIMMUNE-DISEASES; GENE-EXPRESSION; MESSENGER-RNA; UP-REGULATION; K+ CHANNELS; KV1.3; ASTHMA	Gambierol is a marine polycyclic ether toxin, produced along with ciguatoxin congeners by the dinoflagellate Gambierdiscus toxicus. We have recently reported that two truncated skeletal analogs of gambierol comprising the EFGH- and BCDEFGH-rings of the parent compound showed similar potency to gambierol on voltage-gated potassium channels (Kv) inhibition in neurons. Gambierol and its truncated analogs share the main crucial elements for biological activity, which are the C28=C29 double bond within the H-ring and the unsaturated side chain. Since Kv channels are critical for the regulation of calcium signaling, proliferation, secretion and migration in human T lymphocytes, we evaluated the activity of both the tetracyclic and heptacyclic analogs of gambierol on potassium currents in resting T lymphocyte and their effects on interleukin-2 (IL-2) release and gene expression in activated T lymphocytes. The results presented in this work clearly demonstrate that both truncated analogs of gambierol inhibit Kv channels present in resting T lymphocytes (Kv1.3) and prevented lymphocyte activation by concanavalin A. The main effects of the heptacyclic and tetracyclic analogs of gambierol in human T cells are: (1) inhibition of potassium channels in resting and concanavalin-activated T cells in the nanomolar range, (2) inhibition of IL-2 release from concanavalin-activated T cells and (3) negatively affect the expression of genes involved in cell proliferation and immune response observed in concanavalin-activated lymphocytes. These results together with the lack of toxicity in this cellular model, indicates that both analogs of gambierol have additional potential for the development of therapeutic tools in autoimmune diseases.	[Rubiolo, J. A.; Vale, C.; Martin, V.; Botana, L. M.] Univ Santiago de Compostela, Fac Vet, Dept Farmacol, Lugo 27003, Spain; [Fuwa, H.; Sasaki, M.] Tohoku Univ, Grad Sch Life Sci, Sendai, Miyagi 980, Japan	Universidade de Santiago de Compostela; Tohoku University	Vale, C (通讯作者)，Univ Santiago de Compostela, Fac Vet, Dept Farmacol, Lugo 27003, Spain.	mdelcarmen.vale@usc.es; Luis.Botana@usc.es	López, Luis/AAJ-7111-2021; Vale, Carmen/L-5287-2014; Fuwa, Haruhiko/D-1773-2010; Rubiolo Gaytan, Juan Andres/A-8732-2014	Vale, Carmen/0000-0002-9842-6223; Botana, Luis M/0000-0003-2153-6608; Martin Vazquez, Victor/0000-0001-6841-3803; Fuwa, Haruhiko/0000-0001-5343-9023; Rubiolo Gaytan, Juan Andres/0000-0002-7820-7365	FEDER; CDTI and Technological Funds; Ministerio de Economia y Competitividad [AGL2012-40185-CO2-01]; Conselleria de Cultura, Educacion e Ordenacion Universitaria [GRC2013-016]; Axencia Galega de Innovacion, Spain [ITC-20133020 SINTOX, IN852A 2013/16-3 MYTIGAL]; CDTI under ISIP Programme, Spain [IDI-20130304 APTAFOOD]; European Union [265409 muAQUA, 315285 CIGUATOOLS, 312184 PHARMASEA]; Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan [24102507, 23102016]; Grants-in-Aid for Scientific Research [23102016, 24102507, 26102708, 25282228] Funding Source: KAKEN	FEDER(European Union (EU)Spanish Government); CDTI and Technological Funds; Ministerio de Economia y Competitividad(Spanish Government); Conselleria de Cultura, Educacion e Ordenacion Universitaria; Axencia Galega de Innovacion, Spain; CDTI under ISIP Programme, Spain; European Union(European Union (EU)); Ministry of Education, Culture, Sports, Science and Technology (MEXT), 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))	The research leading to these results has received funding from the following FEDER co-funded grants. From CDTI and Technological Funds, supported by Ministerio de Economia y Competitividad, AGL2012-40185-CO2-01 and Conselleria de Cultura, Educacion e Ordenacion Universitaria, GRC2013-016, and through Axencia Galega de Innovacion, Spain, ITC-20133020 SINTOX, IN852A 2013/16-3 MYTIGAL. From CDTI under ISIP Programme, Spain, IDI-20130304 APTAFOOD. From the European Union's Seventh Framework Programme managed by REA - Research Executive Agency (FP7/2007-2013) under grant agreement Nos. 265409 mu AQUA, 315285 CIGUATOOLS and 312184 PHARMASEA. Grants-in-Aid for Scientific Research on Priority Areas "Chemical Biology of Natural Products": (Nos. 24102507 and 23102016) from the Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan.	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Toxicol.	JUL	2015	89	7					1119	1134		10.1007/s00204-014-1299-2	http://dx.doi.org/10.1007/s00204-014-1299-2			16	Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Toxicology	CK3EQ	25155189				2025-03-11	WOS:000356099800011
J	Levac, E; Lewis, M; Stretch, V; Duchesne, K; Neulieb, T				Levac, Elisabeth; Lewis, Michael; Stretch, Vanessa; Duchesne, Katie; Neulieb, Thomas			Evidence for meltwater drainage via the St. Lawrence River Valley in marine cores from the Laurentian Channel at the time of the Younger Dryas	GLOBAL AND PLANETARY CHANGE			English	Article						Younger Dryas; Paleoceanography; Dinocyst; Meltwater drainage; Microfossils; Laurentian Channel	SEA-SURFACE CONDITIONS; GLACIAL LAKE AGASSIZ; ATLANTIC THERMOHALINE CIRCULATION; LATE QUATERNARY DEGLACIATION; NORTH-ATLANTIC; ICE-SHEET; CHAMPLAIN SEA; PALEOCEANOGRAPHIC CHANGES; CONTINENTAL-MARGIN; LABRADOR CURRENT	Debate is ongoing about the source(s) and paths of meltwater that drained into the North Atlantic Ocean at the time of the Younger Dryas (YD), especially the eastern route from glacial Lake Agassiz and predecessor lakes of the Laurentian Great Lakes located along the southeastern edge of the Laurentide Ice Sheet. Here, evidence is presented for meltwater drainage via the St. Lawrence eastern route from five new sediment cores from Cabot Strait, Laurentian Channel and Scotian Shelf at the time of the YD. Palynological analyses are used to reconstruct sea surface conditions based on dinoflagellate cyst records, and pollen data are used for additional correlation. The reconstructions show distinct drops in salinity and temperature and increased sea ice cover duration within the YD period. In addition to these new records, we present a re-examination of original data and paleoceanographic interpretation of surface waters based on a new analysis of dinoflagellate cyst zonation in combination with an updated chronology supported by new radiocarbon dates and refined calibrations. The results clearly define the YD core intervals which contain strong evidence of lowered salinity, thereby re-establishing the St. Lawrence drainage system as a significant route for inflow of YD meltwater to the North Atlantic. This inflow does not exclude the possibility for another source of freshwater, as suggested by geographical differences in the duration of cold, low salinity conditions west and east of Laurentian Channel associated with the YD climatic event. (C) 2015 Elsevier B.V. All rights reserved.	[Levac, Elisabeth; Duchesne, Katie] Bishops Univ, Dept Environm Studies & Geog, Sherbrooke, PQ J1M 1Z7, Canada; [Lewis, Michael] Nat Resources Canada, Geol Survey Canada Atlantic, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; [Stretch, Vanessa] Univ Guelph, Dept Geog, Guelph, ON N1G 2W1, Canada; [Neulieb, Thomas] McGill Univ, Dept Geog, Montreal, PQ H3A 0G, Canada	Bishops University; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography; University of Guelph	Levac, E (通讯作者)，Bishops Univ, Dept Environm Studies & Geog, 2600 Coll, Sherbrooke, PQ J1M 1Z7, Canada.	elevac@ubishops.ca; Michael.Lewis@NRCan-RNCan.gc.ca; vstretch@uoguelph.ca; kduchesne2@gmail.com; tneulieb@gmail.com			Natural Sciences and Engineering Research Council, Canada [RGPIN/341997-2007]; Bishop's University; Natural Resources Canada Earth Sciences Sector Offshore Geoscience	Natural Sciences and Engineering Research Council, Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Bishop's University; Natural Resources Canada Earth Sciences Sector Offshore Geoscience(Natural Resources Canada)	We acknowledge and appreciate improvements to the paper suggested by P. Mudie and D. Forbes for the Geological Survey of Canada, and by two anonymous reviewers for the journal. We thank Lorna Murison, Vanessa Asselin and Eric Fortier from Bishop's University, and F. McCarthy, Brock University and her students for assistance in the processing of samples. We thank Gail Chmura for use of her palynology lab and discussions. We are indebted to Dr. D.J.W. Piper (Geological Survey of Canada Atlantic) for assistance in the selection and dating of cores for this study. We appreciate Dr. A.A.L. Miller (Marine Geos, Wolfville, NS) for expert discussion and selection of foraminifera for dating. We acknowledge and thank the scientific personnel, officers, and crew of the CCGS Hudson for core collection, and I. Hardy and K. Jarrett and staff at Geological Survey of Canada Atlantic for core curation and assistance with sampling. Descriptions of the study cores were made by J. Kennedy, K. Jenner, G. Vilks, L. Aquilina, I. Hardy and C. Rodrigues. We thank G. St-Onge and F. Barletta at the University of Quebec at Rimouski for chronological assistance and advice. Funding from Natural Sciences and Engineering Research Council, Canada (RGPIN/341997-2007) (Discovery Grant to E.L.), Senate Research Committee grants from Bishop's University, and support of the Natural Resources Canada Earth Sciences Sector Offshore Geoscience program are acknowledged. This is a contribution of the Earth Sciences Sector of Natural Resources Canada.	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J	Hoins, M; Van de Waal, DB; Eberlein, T; Reichart, GJ; Rost, B; Sluijs, A				Hoins, Mirja; Van de Waal, Dedmer B.; Eberlein, Tim; Reichart, Gert-Jan; Rost, Bjoern; Sluijs, Appy			Stable carbon isotope fractionation of organic cyst-forming dinoflagellates: Evaluating the potential for a CO<sub>2</sub> proxy	GEOCHIMICA ET COSMOCHIMICA ACTA			English	Article							GROWTH-RATE; MARINE-PHYTOPLANKTON; PHOTOSYNTHETIC FRACTIONATION; C-13; TEMPERATURE; ACQUISITION; CULTURE; WATER; DISCRIMINATION; CARBOXYLATION	Over the past decades, significant progress has been made regarding the quantification and mechanistic understanding of stable carbon isotope fractionation (C-13 fractionation) in photosynthetic unicellular organisms in response to changes in the partial pressure of atmospheric CO2 (pCO(2)). However, hardly any data is available for organic cyst-forming dinoflagellates while this is an ecologically important group with a unique fossil record. We performed dilute batch experiments with four harmful dinoflagellate species known for their ability to form organic cysts: Alexandrium tamarense, Scrippsiella trochoidea, Gonyaulax spinifera and Protoceratium reticulatum. Cells were grown at a range of dissolved CO2 concentrations characterizing past, modern and projected future values (similar to 5-50 mu mol L-1), representing atmospheric pCO(2) of 180, 380, 800 and 1200 mu atm. In all tested species, C-13 fractionation depends on CO2 with a slope of up to 0.17& (mu mol L)(-1). Even more consistent correlations were found between C-13 fractionation and the combined effects of particulate organic carbon quota (POC quota; pg C cell(-1)) and CO2. Carbon isotope fractionation as well as its response to CO2 is species-specific. These results may be interpreted as a first step towards a proxy for past pCO(2) based on carbon isotope ratios of fossil organic dinoflagellate cysts. However, additional culture experiments focusing on environmental variables other than pCO(2), physiological underpinning of the recorded response, testing for possible offsets in C-13 values between cells and cysts, as well as field calibration studies are required to establish a reliable proxy. (C) 2015 Elsevier Ltd. All rights reserved.	[Hoins, Mirja; Reichart, Gert-Jan; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Hoins, Mirja; Eberlein, Tim; Rost, Bjoern] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Marine Biogeosci, D-27570 Bremerhaven, Germany; [Van de Waal, Dedmer B.] Netherlands Inst Ecol NIOO KNAW, Dept Aquat Ecol, NL-6708 PB Wageningen, Netherlands; [Reichart, Gert-Jan] Royal Netherlands Inst Sea Res NIOZ, NL-1797 SZ T Horntje, Texel, Netherlands	Utrecht University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Royal Netherlands Academy of Arts & Sciences; Netherlands Institute of Ecology (NIOO-KNAW); Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Hoins, M (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	M.Hoins@uu.nl	Van de Waal, Dedmer/B-8002-2012; Rost, Bjoern/B-4447-2015; Sluijs, Appy/B-3726-2009; KNAW, NIOO-KNAW/A-4320-2012; Reichart, Gert-Jan/N-6308-2018	Sluijs, Appy/0000-0003-2382-0215; Rost, Bjorn/0000-0001-5452-5505; KNAW, NIOO-KNAW/0000-0002-3835-159X; Van de Waal, Dedmer/0000-0001-8803-1247; Reichart, Gert-Jan/0000-0002-7256-2243	Darwin Centre for Biogeosciences [3021]; European Research Council under the European Community [259627, 205150]; German Ministry of Education and Research	Darwin Centre for Biogeosciences; European Research Council under the European Community(European Research Council (ERC)); German Ministry of Education and Research(Federal Ministry of Education & Research (BMBF))	This research was funded through Darwin Centre for Biogeosciences Grant 3021, awarded to GJR and AS, and the European Research Council under the European Community's Seventh Framework Program through ERC Starting Grants #259627 to AS and #205150 to BR. DBvdW and BR thank BIOACID, financed by the German Ministry of Education and Research. We thank Urban Tillmann (Alfred Wegener Institute) and Karin Zonneveld (Marum, Bremen University) for providing dinoflagellate strains Alex5 and GeoB 267, respectively, and Ulrike Richter, Laura Wischnewski, Jana Holscher (Alfred Wegener Institute) and Arnold van Dijk (Utrecht University) for technical support.	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J	Mertens, KN; Aydin, H; Uzar, S; Takano, Y; Yamaguchi, A; Matsuoka, K				Mertens, Kenneth Neil; Aydin, Hilal; Uzar, Serdar; Takano, Yoshihito; Yamaguchi, Aika; Matsuoka, Kazumi			RELATIONSHIP BETWEEN THE DINOFLAGELLATE CYST <i>SPINIFERITES PACHYDERMUS</i> AND <i>GONYAULAX ELLEGAARDIAE</i> SP NOV FROM IZMIR BAY, TURKEY, AND MOLECULAR CHARACTERIZATION	JOURNAL OF PHYCOLOGY			English	Article						18S rDNA; 28S rDNA; Aegean Sea; Gonyaulax spinifera; Incubation	HETEROTROPHIC DINOFLAGELLATE; THECA RELATIONSHIP; RECENT SEDIMENTS; DINOPHYCEAE; MORPHOLOGY; GENUS; SEA	Here, we established the cyst-motile stage relationship for Spiniferites pachydermus through incubation of cysts with a characteristically microreticulate/perforate surface isolated from Izmir Bay in the eastern Aegean Sea of the eastern Mediterranean. The morphology of the motile stage was similar to Gonyaulax spinifera but had a different size, overhang, displacement and reticulations. Based on the distinct morphology of the cyst and morphological differences in motile cells, we assigned S. pachydermus from Izmir Bay to the new species Gonyaulax ellegaardiae. We elucidate the phylogenetic relationship of G. ellegaardiae through large and small subunit ribosomal DNA and show that it forms a clade with other species that belong to the G. spinifera complex.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Aydin, Hilal; Uzar, Serdar] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Manisa, Turkey; [Takano, Yoshihito; Matsuoka, Kazumi] Inst East China Sea Res ECSER, Nagasaki 8512213, Japan; [Yamaguchi, Aika] Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 6578501, Japan	Ghent University; Celal Bayar University; Kobe University	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be	Mertens, Kenneth/AAO-9566-2020; UZAR, SERDAR/G-9956-2014; Mertens, Kenneth/C-3386-2015	UZAR, SERDAR/0000-0002-9477-7413; Mertens, Kenneth/0000-0003-2005-9483	Higher Education Council of Turkey	Higher Education Council of Turkey(Ministry of National Education - Turkey)	K.N.M. is a postdoctoral fellow of FWO Belgium. H.A. was partly supported by the Higher Education Council of Turkey. We thank Martin J. Head and Rob Fensome for advice on nomenclature. The comments of Andre Rochon, Barrie Dale and one anonymous reviewer have been appreciated.	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Assoc. Strat. Palynologists Contribution Series, V17, P169; Yamaguchi A, 2005, PHYCOL RES, V53, P30; Yamaguchi A, 2006, PHYCOL RES, V54, P317, DOI 10.1111/j.1440-1835.2006.00438.x; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003; Zwickl D.J., 2006, GARLI GENETIC ALGORI	63	25	26	1	34	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	JUN	2015	51	3					560	573		10.1111/jpy.12304	http://dx.doi.org/10.1111/jpy.12304			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	CL0IZ	26986670				2025-03-11	WOS:000356627000014
J	Zarei, E; Ghasemi-Nejad, E				Zarei, Elahe; Ghasemi-Nejad, Ebrahim			Sequence stratigraphy of the Gurpi Formation (Campanian-Paleocene) in southwest of Zagros, Iran, based on palynomorphs and foraminifera	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Sequence stratigraphy; Foraminifera; Dinocyst indices; Depositional environment; Campanian-Paleocene; Zagros	CRETACEOUS-TERTIARY BOUNDARY; DINOFLAGELLATE CYSTS; SEA-LEVEL; ORGANIC-MATTER; SEDIMENTS; PALYNOFACIES; PALEOBATHYMETRY; ASSEMBLAGES; CARBONATES; FRAMEWORK	The Gurpi Formation is a well-known source rock in the Zagros basin, which stretches from northeast to southwest Iran. Sequence stratigraphy was done based on the integration of evidence derived from palynological proxies and foraminiferal data. According to sequence stratigraphy, seven time lines including four sequence boundaries of type II and three maximum flooding surfaces with a resolution varying from 1 to 5 MY and three complete third-order sequences and one transgressive systems tract (TST) were differentiated. Maximum flooding surface of the first sequence in middle Campanian probably equates the 70-Ma maximum flooding surface (MFS) K175 of Sharland et al. (GeoArabia P: 371, 2001), andMFS of the second sequence in early Maastrichtian is correlated with the marked 68-Ma MFS (MFS K180) of Sharland et al. (GeoArabia P: 371, 2001) that is recorded in many parts of the Arabian Plate. Correlation with the Haq global eustatic curve, though uncertain because of the effect of local tectonics over the relative sea level changes, however, could be possible with the 69.5 Ma. Also, purple shales of the base of the Pabdeh Formation with a Thanetian age are defined as a MFS, correlation of which with the marked 58-Ma MFS (MFS Pg10) of Sharland et al. (GeoArabia P: 371, 2001) and with 56.5-Ma MFS of Haq seems likely. The relative sea level curve resulted in this study is not well in accord with the existing eustasy curves for the middle Campanian-late Paleocene indicating effect of tectonic on relative sea level changes during this period.	[Zarei, Elahe; Ghasemi-Nejad, Ebrahim] Univ Tehran, Dept Geol, Fac Sci, Tehran, Iran	University of Tehran	Zarei, E (通讯作者)，Univ Tehran, Dept Geol, Fac Sci, Enghelab Ave, Tehran, Iran.	zarei@khayam.ut.ac.ir; eghasemi@khayam.ut.ac.ir	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068; zaeri, faezeh/0000-0002-6652-8989				Alavi M, 2004, AM J SCI, V304, P1, DOI 10.2475/ajs.304.1.1; Alsharhan AS., 1997, Sedimentary Basins and Petroleum Geology of the Middle East, DOI DOI 10.1016/B978-044482465-3/50003-6; [Anonymous], 1990, BIOL TAPHONOMY; Batten D., 1996, Palynology: principles and applications, P1011; Batten DJ, 2005, T GEOBIOL, V23, P203; BERGER WH, 1988, MAR GEOL, V81, P15, DOI 10.1016/0025-3227(88)90014-X; 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; Buceflo Palliani R, 1998, J MICROPALE IN PRESS, V17; DAVEY R.J., 1971, P 2 PLANKTONIC C, VI., P331; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; Downie C.E.A., 1971, PALYNOLOGICAL INVEST; Ellis AC, 1996, PETROL GEOSCI, V2, P29, DOI 10.1144/petgeo.2.1.29; Flugel E., 2004, MICROFACIES ANAL LIM; GIBSON TG, 1989, MAR MICROPALEONTOL, V15, P29, DOI 10.1016/0377-8398(89)90003-0; Goff J.C., 1995, MIDDLE E PETROLEUM G, V1, P402; GORIN GE, 1991, PALAEOGEOGR PALAEOCL, V85, P303, DOI 10.1016/0031-0182(91)90164-M; Guasti E, 2005, MAR MICROPALEONTOL, V55, P1, DOI 10.1016/j.marmicro.2005.01.001; Guasti E, 2006, MAR MICROPALEONTOL, V59, P210, DOI 10.1016/j.marmicro.2006.02.008; HABIB D, 1989, PALAEOGEOGR PALAEOCL, V74, P23, DOI 10.1016/0031-0182(89)90018-7; HABIB D, 1992, GEOLOGY, V20, P165, DOI 10.1130/0091-7613(1992)020<0165:DACNRT>2.3.CO;2; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Harris AJ, 2003, MAR MICROPALEONTOL, V48, P127, DOI 10.1016/S0377-8398(03)00002-1; HART G F, 1986, Palynology, V10, P1; Helenes J, 1999, CRETACEOUS RES, V20, P447, DOI 10.1006/cres.1999.0160; Hemmati-Nasab M, 2008, THESIS U TEHRAN; Holbourn A, 2001, PALAEOGEOGR PALAEOCL, V170, P171, DOI 10.1016/S0031-0182(01)00223-1; Homke S, 2009, GEOL SOC AM BULL, V121, P963, DOI 10.1130/B26035.1; Islam M., 1984, Tertiary Res, V6, P11; James G.A, 1965, STRATIGRAPHIC NOMENC; Jassim SZ, 2006, GEOLOGY OF IRAQ; JOLLEY DW, 1992, REV PALAEOBOT PALYNO, V74, P207, DOI 10.1016/0034-6667(92)90008-5; Jones R., 1994, MICROPALEONTOLOGY HY, P273; Karim K.H., 2005, Jou. 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J. Geosci.	JUN	2015	8	6					4011	4023		10.1007/s12517-014-1443-6	http://dx.doi.org/10.1007/s12517-014-1443-6			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CJ2TG					2025-03-11	WOS:000355336800053
J	Ivanova, EV; Marret, F; Zenina, MA; Murdmaa, IO; Chepalyga, AL; Bradley, LR; Schornikov, EI; Levchenko, OV; Zyryanova, MI				Ivanova, Elena V.; Marret, Fabienne; Zenina, Maria A.; Murdmaa, Ivar O.; Chepalyga, Andrey L.; Bradley, Lee R.; Schornikov, Eugene I.; Levchenko, Oleg V.; Zyryanova, Maria I.			The Holocene Black Sea reconnection to the Mediterranean Sea: New insights from the northeastern Caucasian shelf	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Ostracods; Molluscs; Foraminifers; Dinoflagellate cysts; Palaeoenvironment; Sedimentation	LATE PLEISTOCENE; ENVIRONMENTAL-CHANGES; DINOFLAGELLATE CYSTS; SURFACE CONDITIONS; MARMARA SEA; LEVEL; SALINITY; INDICATORS; WATER; AGE	Recent findings about the evolution of palaeogeographic conditions of the Black Sea during the Holocene have significantly improved our understanding of the profound environmental changes that took place around 9 ka ago, when the Neoeuxinian Lake reconnected to the global ocean. In contrast to the western and southeastern regions where numerous studies have been recently performed, the northeast region remains relatively under investigated. We carried out the first multi-proxy continuous study of a sediment core (Ak-2575) from the northeastern Black Sea shelf that includes benthic calcareous fossils (ostracods, molluscs and foraminifers), dinoflagellate cysts (dinocysts) and sedimentology, thus providing reconstructions of surface and bottom-water conditions. The age model of the core is based on 10 AMS-C-14 dates. Calibrated ages are used throughout the manuscript. The first appearance of Mediterranean elements is documented at 9.6 cal. ka BP. Our data provide evidence of sustained cohabitation of benthic species of Caspian and Mediterranean origins, represented by different ontogenetic stages, from at least similar to 7.8 (or even 8.8) to 6.7 cal. ka BP with the gradual disappearance of brackish species suggesting a gradual increase in salinity and most likely a change in the salt composition. Dinocyst assemblages show species succession that is coherent across the Black Sea basin, with brackish taxa dominating until similar to 8.5 cal. ka BP and being slowly replaced by euryhaline species. The occurrences of authigenic gypsum crystals, especially abundant at similar to 7.4 and 6.5 cal. ka BP, suggest the temporal appearance of hydrogen sulphide at the shelf edge which during certain periods appears to reduce the abundance of benthic fauna. (C) 2015 Elsevier B.V. All rights reserved.	[Ivanova, Elena V.; Zenina, Maria A.; Murdmaa, Ivar O.; Levchenko, Oleg V.; Zyryanova, Maria I.] Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia; [Marret, Fabienne; Bradley, Lee R.] Univ Liverpool, Sch Environm Sci, Liverpool L69 3BX, Merseyside, England; [Chepalyga, Andrey L.] Russian Acad Sci, Inst Geog, Moscow V71, Russia; [Zenina, Maria A.; Schornikov, Eugene I.] RAS, Far East Div, AV Zhirmunsky Inst Marine Biol, Vladivostok, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology; University of Liverpool; Russian Academy of Sciences; Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Ivanova, EV (通讯作者)，Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia.	e_v_ivanova@ocean.ru; f.marret@liverpool.ac.uk; maria_zenina@mail.ru; murdmaa@mail.ru; tchepalyga@mail.ru; l.r.bradley@liverpool.ac.uk; eschornikov@yandex.ru; olevses@rambler.ru; zyryanova.maria@mail.ru	Tchepalyga, Andrey/AAF-9790-2021; Murdmaa, Ivar/T-3538-2017; Ivanova, Elena/B-3775-2016; Bradley, Lee/AAA-6818-2019	Tchepalyga, Andrey/0000-0001-8654-1614; Marret-Davies, Fabienne/0000-0003-4244-0437; Bradley, Lee/0000-0003-0833-9351	European project Marie Curie [CLIMSEAS-PIRSES-GA-2009-247512]; Russian Science Foundation [14-50-00095]	European project Marie Curie(European Union (EU)); Russian Science Foundation(Russian Science Foundation (RSF))	Our paper is a contribution to CLIMSEAS the European project Marie Curie, CLIMSEAS-PIRSES-GA-2009-247512: "Climate Change and Inland Seas: Phenomena, Feedback and Uncertainties. The Physical Science Basis". The crew of RV Aquanavt and the scientific party of the cruise are acknowledged for the assistance in collecting the core Ak 2575. We thank Guillaume Soulet for providing the reservoir effect estimates, Olga Dara for performing two XRD analyses of gypsum crystals, Lisa Wright (Univ. of Liverpool) for processing samples for dinocyst analyses and Anastasiya Zavrajnova for sieving the core samples. We gratefully appreciate the constructive comments from the editor Thierry Correge and the reviewers, Suzanne Leroy and Andre Rochon. This study was partly funded by the Russian Science Foundation grant 14-50-00095 (El and IM) and the Leverhulme Trust (FM and LB, project "The Black Sea enviommental condtions during the meso- and neolithic period"). We acknowledge Scottish Universities Environmental Research Centre and Poznan Radiocarbon Laboratory for performing AMS <SUP>14</SUP>C analyses.	Agalarova D. 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Paleoclimatol. Paleoecol.	JUN 1	2015	427						41	61		10.1016/j.palaeo.2015.03.027	http://dx.doi.org/10.1016/j.palaeo.2015.03.027			21	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	CI2PW					2025-03-11	WOS:000354590500004
J	Chen, TT; Liu, Y; Song, SQ; Li, CW; Tang, YZ; Yu, ZM				Chen, Tiantian; Liu, Yun; Song, Shuqun; Li, Caiwen; Tang, Ying Zhong; Yu, Zhiming			The effects of major environmental factors and nutrient limitation on growth and encystment of planktonic dinoflagellate <i>Akashiwo sanguinea</i>	HARMFUL ALGAE			English	Article						Dinoflagellate; Cysts; Harmful algal blooms; Nitrogen; Phosphorus; Nutrient limitation	HARMFUL ALGAL BLOOMS; RED-TIDE; CYST FORMATION; GONYAULAX-TAMARENSIS; SEXUAL REPRODUCTION; PERIDINIUM-CINCTUM; NITROGEN-SOURCES; CHLOROPHYLL-A; LIFE-CYCLE; DINOPHYCEAE	The bloom-forming dinoflagellate Akashiwo sanguinea is commonly observed in estuarine and coastal waters around the world. Annually recurrent blooms of this species have been observed in the coastal waters of China, particularly in the Sishili Bay, Yantai since 2004. However, limited studies have been conducted on the recurrence mechanism of A. sanguinea other than periodical monitoring of its population dynamics and associated environmental variables. Thus, to further explore the bloom and succession mechanisms of A. sanguinea in the field, we studied the effects cif major nutritional components on the growth and encystment of A. sanguinea, as well as the effects of key environmental factors on the growth of A sanguinea through a series of laboratory trials. Our results indicated that A sanguinea was able to grow well within the temperature range of 20-25 degrees C, salinity range of 20 - 30, with the maximum laboratory irradiance of 78.14 mu E m(-2) s(-1) , and was able to survive and grow in low nutrient. However, lower concentrations of nutrients (e.g., nitrate, phosphate) and higher ammonium exerted different degrees of limiting effects on the growth of A sanguinea, and induced 2.3-21.24% of vegetative cells to form resting cysts simultaneously in laboratory cultures. On the other hand, very limited or no cyst formation was observed in nutrient-replete or extremely low nutrient cultures, indicating the threshold effect of nutritional stress on the encystment of A. sanguinea. The physiological strategy of encystment of A sanguinea in nutrient-limiting environment facilitates the survival and succession of A sanguinea species in fluctuating seawaters, and provides seed sources for reoccurring algal blooms under favorable environmental conditions. (C) 2015 Elsevier B.V. All rights reserved.	[Chen, Tiantian; Liu, Yun; Song, Shuqun; Li, Caiwen; Tang, Ying Zhong; Yu, Zhiming] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Chen, Tiantian; Tang, Ying Zhong] Univ Chinese Acad Sci, Beijing 10039, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Li, CW (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	caiwenli@live.com	Liu, Yun/Q-1757-2019; Chen, Tiantian/KFR-4471-2024	Li, Caiwen/0000-0003-3974-2522; Yu, Zhiming/0000-0003-0377-1129	China youth project [41206145]; NSFC -Shandong Joint Fund for Marine Science Research Centers [U1406403]; Foundation of innovation group projects of the National Natural Science Foundation of China (NNSFC) [41121064]; 100 Talents Program of the Chinese Academy of Sciences	China youth project; NSFC -Shandong Joint Fund for Marine Science Research Centers; Foundation of innovation group projects of the National Natural Science Foundation of China (NNSFC)(National Natural Science Foundation of China (NSFC)); 100 Talents Program of the Chinese Academy of Sciences(Chinese Academy of Sciences)	We thank Prof. Dongyan Liu (CAS) for her laboratory and field assistance during isolation of the dinoflagellate species and field sampling at Sishili Bay, Yantai, China, and thanks to Dr. Jie Xiao (SOA) for her comments and suggestions to the manuscript. We are also highly grateful of the insightful comments and suggestions of the two anonymous reviewers. This study was financially supported by the China youth project (Grant no. 41206145), the NSFC -Shandong Joint Fund for Marine Science Research Centers (Grant no. U1406403), and Foundation of innovation group projects (Grant no. 41121064) of the National Natural Science Foundation of China (NNSFC), and the 100 Talents Program of the Chinese Academy of Sciences. [SS]	Anderson D.M., 1998, PHYSL ECOLOGY HARMFU, P19; Anderson DM, 1997, NATURE, V388, P513, DOI 10.1038/41415; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; Anderson DM, 2009, OCEAN COAST MANAGE, V52, P342, DOI 10.1016/j.ocecoaman.2009.04.006; Beam C. 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J	Bati, Z				Bati, Zuhtu			Dinoflagellate cyst biostratigraphy of the upper Eocene and lower Oligocene of the Kirmizitepe Section, Azerbaijan, South Caspian Basin	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cyst; Upper Eocene; Lower Oligocene transition; Biostratigraphy; South Caspian Basin; Azerbaijan	LOWER MIOCENE; PRODUCTIVE SERIES; EASTERN ANATOLIA; MUS BASIN; BLACK-SEA; STRATIGRAPHY; NORTHERN; EVOLUTION; PALEOGEOGRAPHY; DEPRESSION	The South Caspian Basin is a deep Cenozoic basin located in eastern Paratethys along the northern margin of the Arabia-Eurasia collision zone. The basin, with its proven oil and gas reserves, has been the subject of numerous biostratigraphic studies, but most of these studies have concentrated on the Pliocene reservoir rocks. Precise chronological correlations between Paratethyan sedimentary successions and Mediterranean stages have not yet been achieved, although detailed local foraminiferal and non-foraminiferal biostratigraphic studies allow chronostratigraphic division and accurate regional correlations. As a pioneering work, this paper provides a detailed dinoflagellate cyst biostratigraphy of the upper Eocene and lower Oligocene deposits in the South Caspian Basin. A total of 127 dinoflagellate cyst taxa have been studied for the first time from the Eocene Koun Formation and the Oligocene part of the Maykop Formation exposed in the Kirmizitepe Section, Azerbaijan. Three dinoflagellate cyst biozones known from classic areas in central Italy are recognizable in the South Caspian Basin. One (Aal zone) is uppermost Eocene and two (Gse and Adi zones) are lower Oligocene. Thus, although some dinoflagellate cyst species from the studied section have stratigraphic ranges different from those of mid and higher latitudes, others provide correlations with previously defined biozones and dinoflagellate cyst events in the Tethyan realm and northwestern Europe. Dinoflagellate cyst assemblages indicate shallow marine depositional conditions for the latest Eocene. Deeper conditions prevailed during the earliest part of the early Oligocene, succeeded by a pronounced shallowing later in the early Oligocene. (C) 2015 Elsevier B.V. All rights reserved.	Turkish Petr Corp, Explorat Dept, TR-06100 Ankara, Turkey	Turkish Petroleum Corporation (TPAO); Ministry of Energy & Natural Resources - Turkey	Bati, Z (通讯作者)，Turkish Petr Corp, Explorat Dept, 2180 Cadde 10, TR-06100 Ankara, Turkey.	bati@tpao.gov.tr						Abdullayev NR., 2012, AAPG MEMOIR, V95, P71, DOI DOI 10.1306/13291385M953446; Abrams MA, 1997, MAR PETROL GEOL, V14, P451, DOI 10.1016/S0264-8172(97)00011-1; Abreu V., 2000, 1 AAPGS IN REG INT C; Akgun F., 1987, B GEOL SOC TURK, V29, P13; Akkiraz S., 2000, THESIS DOKUZ EYLUL U; Aleksandrova GN, 2011, STRATIGR GEO CORREL+, V19, P310, DOI 10.1134/S0869593811030014; Artyushkov EV, 2007, RUSS GEOL GEOPHYS+, V48, P1002, DOI 10.1016/j.rgg.2007.11.007; Baganz OW, 2012, AAPG MEMOIR, V95, P57, DOI DOI 10.1306/13291384M953444; Bati Z., 2009, 3470 TPAO; Bati Z., 2007, STRAT KOM CAL 22 23, P5; Bati Z, 2007, MICROPALEONTOLOGY, V53, P249, DOI 10.2113/gsmicropal.53.4.249; BERBERIAN M, 1983, CAN J EARTH SCI, V20, P163, DOI 10.1139/e83-015; 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; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 1995, SOC ECON PALEONT MIN, V54, P295; Brinkhuis H., 1992, HIGH RESOLUTION DINO, P219; Brunet MF, 2003, SEDIMENT GEOL, V156, P119, DOI 10.1016/S0037-0738(02)00285-3; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Bujak J.P., 1994, Journal of Micropalaeontology, V13, P119; Bujak J.P., 1980, SPEC PAP PALAEONTOL, V24; BUJAK JP, 1976, MAR MICROPALEONTOL, V1, P101, DOI 10.1016/0377-8398(76)90007-4; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Chateauneuf J.J., 1980, Memorie du Bureau de Recherches Geologiques et Minieres, V116, P1; Chateauneuf J.-J., 1978, Bull. 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Palaeobot. Palynology	JUN	2015	217						9	38		10.1016/j.revpalbo.2015.03.002	http://dx.doi.org/10.1016/j.revpalbo.2015.03.002			30	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	CH6OK					2025-03-11	WOS:000354155700002
J	Aydin, H; Yürür, EE; Uzar, S; Küçüksezgin, F				Aydin, Hilal; Yurur, Emine Erdem; Uzar, Serdar; Kucuksezgin, Filiz			Impact of industrial pollution on recent dinoflagellate cysts in Izmir Bay (Eastern Aegean)	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cyst; Metals; Industrial pollution; Sediment type; Izmir Bay (Eastern Aegean)	STREAM-SUBSURFACE EXCHANGE; HEAVY-METAL POLLUTION; SURFACE SEDIMENTS; ALEXANDRIUM-CATENELLA; SPATIAL-DISTRIBUTION; RESTING STAGES; SEA; EUTROPHICATION; ASSEMBLAGES; NUTRIENT	The spatial distribution of dinoflagellate cysts was studied to understand the impact of industrial pollution on the surface sediment of Izmir Bay, Turkey. Forty two dinoflagellate cyst morphotypes belonging to 12 genera were identified and qualified at 12 sampling points. The cyst of Gymnodinium nolleri dominated the bay and had the highest abundance in most of the stations, following Spiniferites bulloideus and Linguloclinium machaerophorum. The highest cyst concentration was recorded in the inner part of the bay. Cyst concentration ranged between 384 and 9944 cyst g(-1) dry weight of sediment in the sampling area. Sediment metal concentrations were determined. Heavy metal levels in Izmir Inner Bay were higher than the Middle and Outer Bay. L. machaerophorum, Dubridinium caperatum and Polykrikos kofoidii showed significant positive correlation with some metals (Cd, Pb, Cu, Zn) and organic carbon content. However, there was no significant correlation between dinoflagellate cyst abundance and sediment type. (C) 2015 Elsevier Ltd. All rights reserved.	[Aydin, Hilal; Yurur, Emine Erdem; Uzar, Serdar] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Manisa, Turkey; [Kucuksezgin, Filiz] Dokuz Eylul Univ, Inst Marine Sci & Technol, TR-35340 Izmir, Turkey	Celal Bayar University; Dokuz Eylul University	Aydin, H (通讯作者)，Celal Bayar Univ, Fac Sci & Arts, Dept Biol, Muradiye Campus, TR-45140 Manisa, Turkey.	hilalaydin66@gmail.com	Kucuksezgin, Filiz/P-3788-2019; UZAR, SERDAR/G-9956-2014	UZAR, SERDAR/0000-0002-9477-7413; Kucuksezgin, Filiz/0000-0001-9030-5227	Scientific and Technical Research Council of Turkey (TUBITAK) [113Y006]	Scientific and Technical Research Council of Turkey (TUBITAK)(Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK))	This study was partly supported by the Scientific and Technical Research Council of Turkey (TUBITAK) (Project No. 113Y006) and within the framework of the "IMTS-199 Izmir Bay Marine Research Project". This study also contains part of the PhD dissertation of Serdar Uzar from Celal Bayar University. The authors are grateful to the Marine Chemistry Laboratory of Dokuz Eylul University Institute of Marine Science and Technology for their assistance with the analysis. The authors also thank the crew of R/V K. Piri Reis for their assistance during fieldwork.	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Pollut. Bull.	MAY 15	2015	94	1-2					144	152		10.1016/j.marpolbul.2015.02.038	http://dx.doi.org/10.1016/j.marpolbul.2015.02.038			9	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	CJ3BC	25817312				2025-03-11	WOS:000355357400027
J	Vellekoop, J; Smit, J; van de Schootbrugge, B; Weijers, JWH; Galeotti, S; Damsté, JSS; Brinkhuis, H				Vellekoop, Johan; Smit, Jan; van de Schootbrugge, Bas; Weijers, Johan W. H.; Galeotti, Simone; Damste, Jaap S. Sinninghe; Brinkhuis, Henk			Palynological evidence for prolonged cooling along the Tunisian continental shelf following the K-Pg boundary impact	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Elles section; Cretaceous-Palaeogene boundary; Dinoflagellate cysts; Climate change; Sea level	CRETACEOUS-TERTIARY BOUNDARY; DINOFLAGELLATE CYST ASSEMBLAGES; GLYCEROL TETRAETHER LIPIDS; SEA-LEVEL FLUCTUATIONS; MASS EXTINCTION; CHICXULUB IMPACT; MEMBRANE-LIPIDS; EL KEF; PALEOGENE; PALEOCENE	The Cretaceous-Palaeogene (K-Pg) boundary mass extinction event is related to major global environmental changes resulting from a large extraterrestrial impact. Organic-walled cyst-producing marine dinoflagellates (dinocysts) survived the K-Pg mass-extinction relatively unscathed, making them ideally suited for reconstructing these environmental changes. So far, one of the best dinocyst records available is from the K-Pg boundary Global Stratotype Section and Point (GSSP) at El Kef (NW Tunisia). There, the dinocyst record shows major fluctuations across the boundary, likely reflecting strong responses to environmental changes. These fluctuations have so far not been confirmed by other studies. Therefore, in this study we performed a high-resolution marine palynological study on a closely spaced sample set from the Elles section, some 75 km south of El Kef, in order to generate a palaeoenvironmental and palaeoclimatic record across the K-Pg boundary to allow verification and refinement of earlier reported environmental changes. To better constrain the reconstructions based on qualitative biotic proxies we employed the quantitative sea surface temperature proxy TEX86. Unfortunately, the TEX86 proxy record of the studied section is compromised because of post-depositional oxidation. However, the diverse dinocyst assemblages at Riles show strong fluctuations similar to the El Kef record, therefore confirming the earlier recorded signals, showing rapid, regionally consistent changes. These records imply that the latest Cretaceous was characterized by a gradual cooling trend and the onset of relative sea level fall. Within the immediate post-extinction interval, in the first thousands of years after the impact, dinocyst assemblages reveal multiple incursions of higher-latitude dinocyst species implying repeated pulses of cooling. These results signify that the earliest Danian climatic and environmental conditions were relatively unstable across the Tunisian shelf. (C) 2015 Elsevier B.V. All rights reserved.	[Vellekoop, Johan; van de Schootbrugge, Bas; Brinkhuis, Henk] Univ Utrecht, Dept Earth Sci, Lab Palaeobot & Palynol, Marine Palynol & Paleoceanog,Geosci, NL-3584 CD Utrecht, Netherlands; [Smit, Jan] Vrije Univ Amsterdam, Dept Sedimentol & Marine Geol, Eventstratig, NL-1018 HV Amsterdam, Netherlands; [Weijers, Johan W. H.; Damste, Jaap S. Sinninghe] Univ Utrecht, Dept Earth Sci, Geochem, Geosci, NL-3584 CD Utrecht, Netherlands; [Galeotti, Simone] Univ Urbino Carlo Bo, Dept Earth Life & Environm Sci, I-61029 Urbino, Italy; [Damste, Jaap S. Sinninghe; Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, NL-1797 SZ T Horntje, Texel, Netherlands	Utrecht University; Vrije Universiteit Amsterdam; Utrecht University; University of Urbino; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Vellekoop, J (通讯作者)，KU Leuven Univ, Dept Earth & Environm Sci, Div Geol, Celestijnenlaan 200E, B-3001 Louvain, Belgium.	johan.vellekoop@ees.kuleuven.be	Vellekoop, Johan/L-1805-2019; Brinkhuis, Henk/IUO-8165-2023; Vellekoop, Johan/F-6466-2017; Sinninghe Damste, Jaap/F-6128-2011	Galeotti, Simone/0000-0001-9636-9344; Vellekoop, Johan/0000-0001-6977-693X; Sinninghe Damste, Jaap/0000-0002-8683-1854; Brinkhuis, Henk/0000-0003-0253-6610	Utrecht University; Netherlands Organization for Scientific Research [ALWPJ/09047]	Utrecht University; Netherlands Organization for Scientific Research(Netherlands Organization for Scientific Research (NWO))	We thank N. Welters, J. van Tongeren and J. Ossebaar for analytical assistance. We thank the editor, Prof. Finn Surlyk and the two anonymous reviewers for their comments and suggestions. Funding for this research was provided by Utrecht University and the Netherlands Organization for Scientific Research (open competition grant ALWPJ/09047 to Brinkhuis and Sinninghe-Damste).	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Paleoclimatol. Paleoecol.	MAY 15	2015	426						216	228		10.1016/j.palaeo.2015.03.021	http://dx.doi.org/10.1016/j.palaeo.2015.03.021			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	CG8ZA		Green Published			2025-03-11	WOS:000353603000018
J	Bisconti, M				Bisconti, Michelangelo			Anatomy of a new cetotheriid genus and species from the Miocene of Herentals, Belgium, and the phylogenetic and palaeobiogeographical relationships of Cetotheriidae s.s. (Mammalia, Cetacea, Mysticeti)	JOURNAL OF SYSTEMATIC PALAEONTOLOGY			English	Article						Cetacea; Cetotheriidae s.s; Herentalia nigra; Mysticeti; palaeobiogeography; phylogeny	NORTH-SEA BASIN; BALEEN WHALE; DINOFLAGELLATE CYSTS; BALAENOPTERID WHALE; EARLY-PLIOCENE; MORPHOLOGY; EVOLUTION; STRATIGRAPHY; HISTORY; FOSSIL	Herentalia nigra gen. et sp. nov. is described and compared to other mysticetes. It belongs to Cetotheriidae s.s. and represents one of the best-preserved cetotheriid skulls from the southern border of the North Sea. A comprehensive phylogenetic analysis revealed that it is closely related to Nannocetus and to a Japanese Herpetocetus, suggesting that it belongs to the subfamily Herpetocetinae. The phylogenetic analysis performed tests the recent hypothesis that Caperea marginata belongs to Cetotheriidae. However the present results confirm that the pygmy right whale cannot be considered a member of Cetotheriidae. The phylogenetic analysis was used as the basis for a cladistic palaeobiogeographical analysis of Cetotheriidae that revealed that the family originated in the Pacific basin during the Burdigalian and subsequently underwent a sequence of dispersal and vicariance events that allowed its members to enter other ocean basins. The evolution of Cetotheriidae diversity was punctuated by two distinct phases of species originations (one in the Burdigalian and the other in the Tortonian) that broadly correspond to a massive increase of food availability in the ocean trophic webs.http://zoobank.org/urn:lsid:zoobank.org:pub:DB1647B0-53E9-4014-B31A-F8B063923EB4	San Diego Nat Hist Museum, San Diego, CA 92101 USA		Bisconti, M (通讯作者)，San Diego Nat Hist Museum, 1588 El Prado, San Diego, CA 92101 USA.	michelangelobisconti@gmail.com	Bisconti, Michelangelo/ITR-9582-2023	Bisconti, Michelangelo/0000-0002-0281-4863	Italian Ministry of University and Scientific Research; Synthesys 2 grant - European Community Research Infrastructure Action under the FP 7 (NL-TAF Project) [1730]	Italian Ministry of University and Scientific Research(Ministry of Education, Universities and Research (MIUR)); Synthesys 2 grant - European Community Research Infrastructure Action under the FP 7 (NL-TAF Project)	I want to express my gratitude to Klaas Post (Natuurhistorisch Museum, Rotterdam, the Netherlands) who brought the existence of this specimen to my knowledge in 2001 and organized my visits to Dutch institutions to study fossil mysticetes. Collaboration with Peter Van Bree was very useful, and he provided a lot of assistance during my visit at the Zoological Museum in Amsterdam in 2001. Reinier Van Zelst and John De Vos were of great help during my visit to Naturalis, Leiden, in 2012 to re-study the specimen. Annelise Folie, Olivier Lambert and Mark Bosselaers (all at the Royal Belgian Institute of Natural Sciences, Brussels, Belgium), Klaas Post (Natural History Museum, Rotterdam) and Rene Fraaye (The Groene Port, Boxtel, Holland) provided very kind assistance and help during my numerous visits to the Belgian and Dutch collections and made several specimens available for my comparative study. Many thanks are due to Olivier Lambert who provided data on the stratigraphy of Herenthals. Dave Bohaska (National Museum of Natural History, Smithsonian Institution) gave me access to the Metopocetus skulls that are used here. Rodolfo Salas Gismondi (Museo de Historia Natural, Universidad Nacional Mayor de San Marcos, Lima) warranted access to specimens of Piscobalaena nana. Many thanks are due to Mark Uhen, Tom Demere and Adrian Lister (Associate Editor of the Journal of Systematic Palaeontology), who greatly improved the quality of the manuscript. My 2001 visit was funded by the Italian Ministry of University and Scientific Research, being a contribution of the Pisa Unit (unit coordinator Walter Landini, Dipartimento di Scienze della Terra, University of Pisa) to the research project 'Palaeobiogeography of Central Mediterranean from Miocene to Quaternary' (national coordinator Danilo Torre, Dipartimento di Scienze della Terra, University of Florence). My 2012 visit was funded by a Synthesys 2 grant (Synthesys Project http://www.synthesys.info/), which was financed in 2012 by the European Community Research Infrastructure Action under the FP 7 (NL-TAF Project n. 1730). 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Jr, 2008, Virginia Museum of Natural History Special Publication, V14, P141	52	39	41	0	13	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	1477-2019	1478-0941		J SYST PALAEONTOL	J. Syst. Palaeontol.	MAY 4	2015	13	5					377	395		10.1080/14772019.2014.890136	http://dx.doi.org/10.1080/14772019.2014.890136			19	Evolutionary Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Evolutionary Biology; Paleontology	CG8PL					2025-03-11	WOS:000353570900001
J	Guler, V; Berbach, L; Archangelsky, A; Archangelsky, S				Guler, Veronica; Berbach, Lorena; Archangelsky, Ana; Archangelsky, Sergio			QUISTES DE DINOFLAGELADOS Y POLEN ASOCIADO DEL CRETACICO INFERIOR (FORMACION SPRINGHILL) DE LA CUENCA AUSTRAL, PLATAFORMA CONTINENTAL ARGENTINA	REVISTA BRASILEIRA DE PALEONTOLOGIA			Spanish	Article						dinoflagellate cysts; angiosperms; Early Cretaceous; Austral Basin; Argentina	PATAGONIA; STRATIGRAPHY; SECTION; POLLEN	DINOFLAGELLATE CYSTS AND ASSOCIATED POLLEN FROM LOWER CRETACEOUS (SPRINGHILL FORMATION) IN THE AUSTRAL BASIN, ARGENTINA CONTINENTAL SHELF. Well preserved and moderately diverse, early Cretaceous dinoflagellate cyst assemblages were recovered from the Springhill Formation at wells MLD3 and MLD4, of southeastern Argentina. The relative dating of the sequences is based on the first and last occurrences of age-diagnostic dinoflagellate cysts taxa. These bioevents are, in ascending order: last occurrence of Kleithriasphaeridium fasciatum, first occurrence of Prolixosphaeridium parvispinum, last occurrence of Phoberocysta neocomica, first occurrence of Herendeenia postprojecta, first occurrence of Odontochitina operculata, last occurrence of Cassiculosphaeridia magna and last occurrence of Kaiwaradinium scrutillinum and support a late Barremian age for both stratigraphical sequences. The last occurrence of K. fasciatum and the first occurrence of P.. parvispinum recorded at the lower part of the marine interval in the MLD3 well and the upper part of the MLD4 well, constrain the age of the beginning of the transgressive episode around the early/late Barremian transition, not younger than the early late Barremian. In these intervals, the upper part of the Australian Muderongia testudinaria Zone Helby can be indirectly recognized. The top of the Muderongia australis Zone was recognized at the uppermost marine part of the MLD3 well, assigned to the late Barremian. First occurrences of primitive angiosperm pollen grains like cf. Clavatipollenites, Spinizonocolpites sp., Arecipites sp., Asteropollis, Foveomonocolpites and Tricolpites were recorded too in both wells.	[Guler, Veronica] Univ Nacl Sur, Dept Geol, Inst Geol Sur, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Berbach, Lorena] Museo Municipal Ciencias Nat Carlos Darwin, RA-8109 Buenos Aires, DF, Argentina; [Archangelsky, Ana; Archangelsky, Sergio] Museo Argentino Ciencias Nat Bernardino Rivadavia, Div Paleobot, RA-1405 Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN)	Guler, V (通讯作者)，Univ Nacl Sur, Dept Geol, Inst Geol Sur, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	vguler@criba.edu.ar; lberbach@yahoo.com; sarchangelsky@gmail.com; aarchangelsky@yahoo.com.ar						[Anonymous], MEMOIRS; Arbe H.A., 2002, Geologia y Recursos Naturales de Santa Cruz: Relatorio del XV Congreso Geologico Argentino, El Calafate, P103; Archangelsky S., 1984, Ameghiniana, V21, P15; Archangelsky Sergio, 2002, Revista del Museo Argentino de Ciencias Naturales Nueva Serie, V4, P25; Archangelsky S, 2013, INT J PLANT SCI, V174, P559, DOI 10.1086/668693; Baldoni A.M., 1983, REV ESP MICROPALEONT, V15, P47; Biddle K., 1986, Assoc. 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D., 1981, B CEN RECH EXPLOR PR, V5, P1; Robbiano J.A., 1996, CONGRESO GEOL OGI CO, P323; Schwarz E, 2011, MAR PETROL GEOL, V28, P1218, DOI 10.1016/j.marpetgeo.2010.11.003; Stover L.E., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P261; WISEMAN JF, 1974, INIT REPTS DSDP, V27, P915	37	7	8	0	1	SOC BRASILEIRA PALEONTOLOGIA	SAO LEOPOLDO	PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL	1519-7530	2236-1715		REV BRAS PALEONTOLOG	Rev. Bras. Paleontol.	MAY-AUG	2015	18	2					307	324		10.4072/rbp.2015.2.10	http://dx.doi.org/10.4072/rbp.2015.2.10			18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	CW7AK		Bronze, Green Published			2025-03-11	WOS:000365150100010
J	Accoroni, S; Glibert, PM; Pichierri, S; Romagnoli, T; Marini, M; Totti, C				Accoroni, Stefano; Glibert, Patricia M.; Pichierri, Salvatore; Romagnoli, Tiziana; Marini, Mauro; Totti, Cecilia			A conceptual model of annual <i>Ostreopsis</i> cf. <i>ovata</i> blooms in the northern Adriatic Sea based on the synergic effects of hydrodynamics, temperature, and the N:P ratio of water column nutrients	HARMFUL ALGAE			English	Article						Ostreopsis; N:P ratio; Temperature; Harmful algae; Benthic dinoflagellates; Cysts	PALYTOXIN-LIKE COMPOUNDS; HARMFUL ALGAL BLOOMS; COASTAL WATERS; MEDITERRANEAN SEA; GONYAULAX-TAMARENSIS; ENVIRONMENTAL-CONDITIONS; POSIDONIA-OCEANICA; GENUS OSTREOPSIS; TOXIN PROFILE; AEGEAN SEA	The ecology of Ostreopsis cf. ovata blooms in the Conero Riviera (N Adriatic Sea) was investigated based on sampling carried out from 2007 to 2012, in order to assess the role of environmental factors associated with blooms. Generally, the temporal trend of blooms showed the first cell appearance at the end of July/early August, the maximum abundances in late-summer at end of September/early October reaching up to 10(6) cells g(-1), fw on macrophyte samples, and the decline of the blooms at end October/early November. Calm conditions appeared to be a prerequisite for blooms. When suitable hydrodynamic conditions exist, O. cf. ovate blooms appear to be triggered by a combination of optimal temperature and available nutrients. A water temperature threshold of 25 degrees C plays a key role in the germination of O. cf. ovate cysts and therefore in bloom onset, and an N:P ratio around Redfield value is a necessary condition to allow cell proliferation. The synergy of higher temperatures and optimal N:P ratios resulted in a higher net growth rate of O. cE ovate cells. After the onset, blooms can be maintained at temperature values even below 20 degrees C and at N:P ratios that are in excess of the Redfield ratio. Once the bloom has started it may be maintained not necessarily through high growth rates, but likely through other physiological mechanisms. Bloom decline occurred when temperatures dropped below 18 degrees C. The net effect of the synergy between local hydrodynamic conditions, temperature, and N and P availability may help to explain why blooms in the northern Adriatic Sea occur differently from those in other Mediterranean regions. (C) 2015 Elsevier B.V. All rights reserved.	[Accoroni, Stefano; Pichierri, Salvatore; Romagnoli, Tiziana; Totti, Cecilia] Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, I-60131 Ancona, Italy; [Accoroni, Stefano; Glibert, Patricia M.] Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA; [Marini, Mauro] CNR, Inst Marine Sci, I-60125 Ancona, Italy	Marche Polytechnic University; University System of Maryland; University of Maryland Center for Environmental Science; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR)	Accoroni, S (通讯作者)，Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, Via Brecce Bianche, I-60131 Ancona, Italy.	s.accoroni@univpm.it	glibert, patricia/G-1026-2013; Marini, Mauro/AAE-9399-2020; TOTTI, Cecilia Maria/A-9178-2016; Accoroni, Stefano/F-5818-2014	Romagnoli, Tiziana/0009-0009-5181-987X; Marini, Mauro/0000-0002-9674-7197; TOTTI, Cecilia Maria/0000-0002-1532-6009; Accoroni, Stefano/0000-0002-1134-7849	MURST; ISPRA-Italian Ministry of the Environment; ENPI M3-HABs project	MURST(Ministry of Education, Universities and Research (MIUR)); ISPRA-Italian Ministry of the Environment; ENPI M3-HABs project	The authors wish to thank Federica Colombo, Giacomo Ciampi and Angela Pastore for field and laboratory assistance. This research was partly funded by MURST (PRIN 2007), ISPRA-Italian Ministry of the Environment and ENPI M3-HABs project. 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J	Akselman, R; Krock, B; Alpermann, TJ; Tillmann, U; Borel, CM; Almandoz, GO; Ferrario, ME				Akselman, Rut; Krock, Bernd; Alpermann, Tilman J.; Tillmann, Urban; Marcela Borel, C.; Almandoz, Gaston O.; Ferrario, Martha E.			<i>Protoceratium reticulatum</i> (Dinophyceae) in the austral Southwestern Atlantic and the first report on YTX-production in shelf waters of Argentina	HARMFUL ALGAE			English	Article						Protoceratium reticulatum; Dinoflagellates; Southwestern Atlantic; Phylogeny; Yessotoxins; Cysts	HARMFUL ALGAL BLOOMS; DINOFLAGELLATE CYSTS; PHYLOGENETIC-RELATIONSHIPS; YESSOTOXINS PROFILE; GONYAULAX-SPINIFERA; MARINE-SEDIMENTS; LARGE SUBUNIT; NORTH; COMPLEX; SHELLFISH	Protoceratium reticulatum is a dinoflagellate with a life cycle that includes a motile planktonic stage and a resting cyst stage in benthic habitat, both with a wide geographical distribution, including southern South America. P. reticulatum produces yessotoxins (YTX) - these can be accumulated in shellfish and show potent cytotoxicity, posing a risk to human health if contaminated shellfish is consumed. YTX have been reported from coastal shellfish of many localities, but until now it was unknown if they were present in the austral Southwestern Atlantic and also if local populations of P. reticulatum have the ability to produce these toxins. In this study we report the presence of YTX in plankton samples and its production in culture by two P. reticulatum strains isolated from the San Jorge Gulf (SJG). In addition, we describe the geographical distribution and seasonal abundance of this species based on data collected over the past two decades. The YTX cell quotas calculated from net hauls (similar to 10 pg cell(-1)) are in the same range as the toxin cell quotas observed in these two isolates. The phylogenetic analysis of sequences of the hypervariable region of the large subunit (LSU) 28S rDNA showed that the two clonal strains from the SJG were part of a monophyletic clade that subdivides P. reticulatum into two well-supported, divergent sub-clades. The sequences of the two strains of P. reticulaturn from the SJG fell in the same clade as the majority of sequences of P. reticulatum, which belong to a geographically widely distributed evolutionary clade. P. reticulatum was occasionally observed from about 35 degrees S in Uruguayan shelf waters up to 530 S on the Patagonian shelf and north of Tierra del Fuego, and it was present from coastal areas up to the shelf break zone. We recorded P. reticulatum in plankton samples during spring, summer and autumn but invariably in low abundance (maximum: 560 cells L-1). Viable cysts of the species in surface sediments also showed a wide geographical distribution. Together, the high total abundances and high relative numerical contribution to planktonic dinoflagellate assemblages near frontal areas, emphasize the necessity to pay attention to the dynamics of this species in areas of potential risk of harmful algal bloom development. (C) 2015 Elsevier B.V. All rights reserved.	[Akselman, Rut] Inst Nacl Invest & Desarrollo Pesquero INIDEP, Mar Del Plata, Buenos Aires, Argentina; [Krock, Bernd; Tillmann, Urban] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; [Alpermann, Tilman J.] Senckenberg Res Inst, D-60325 Frankfurt, Germany; [Alpermann, Tilman J.] Nat Hist Museum, D-60325 Frankfurt, Germany; [Marcela Borel, C.] CONICET Univ Nacl Sur, Inst Geol Sur INGEOSUR, Bahia Blanca, Buenos Aires, Argentina; [Almandoz, Gaston O.; Ferrario, Martha E.] Fac Ciencias Nat & Museo, RA-1900 La Plata, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National Fisheries Research & Development Institute (INIDEP); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); National University of La Plata; Museo La Plata	Akselman, R (通讯作者)，Inst Nacl Invest & Desarrollo Pesquero INIDEP, V Ocampo 1,Escollera Norte,B7602HSA, Mar Del Plata, Buenos Aires, Argentina.	rutaks@inidep.edu.ar	Krock, Bernd/ABB-7541-2020; Alpermann, Tilman/JGE-0512-2023	Borel, C. Marcela/0000-0001-5772-4534; Almandoz, Gaston O./0000-0001-7931-582X	HGF through the research program PACES of the Alfred Wegener Institute (AWI); binational project MINCyT-BMBF [AL/11/03-ARG 11/021]; GEF-PNUD [ARG 02/18]; GEF-PNUD (FREPLATA) [RLA/99/G31]; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET) [PIP 01734, PIP 00173]; European Commission under the 7th Framework Program through the Action - IMCONet (FP7 IRSES) [319718]	HGF through the research program PACES of the Alfred Wegener Institute (AWI); binational project MINCyT-BMBF; GEF-PNUD; GEF-PNUD (FREPLATA); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); European Commission under the 7th Framework Program through the Action - IMCONet (FP7 IRSES)(European Union (EU)Marie Curie Actions)	This work was partially financed by the HGF through the research program PACES of the Alfred Wegener Institute (AWI) and the binational project MINCyT-BMBF (AL/11/03-ARG 11/021). It was also supported by grants GEF-PNUD ARG 02/18, GEF-PNUD RLA/99/G31 (FREPLATA) and Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET) PIP 01734 and by PIP 00173 (CONICET) grant and by the European Commission under the 7th Framework Program through the Action - IMCONet (FP7 IRSES, action no. 319718). We thank P. Sarmiento from the MEB service (Museo de La Plata), R. Reta, A.D. Cucchi Colleoni and M. Carignan (INIDEP) for technical assistance, and crews of the RVs of INIDEP and CONICET-MINDEF, Argentina, for onboard collaboration; L. Rhodes and K. Smith (Cawthron Institute, Nelson, New Zealand) are kindly acknowledged for providing LSU sequences of strains of P. reticulatum from New Zealand. This is Contribution No. 1929 of the Instituto Nacional de Investigacion y Desarrollo Pesquero (INIDEP), Mar del Plata, Argentina.[SS].	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WALL D., 1967, PALAEONTOLOGY, V10, P95; Walsh D, 1998, BIOCHEM SYST ECOL, V26, P495, DOI 10.1016/S0305-1978(98)00006-4; Wang L, 2014, HARMFUL ALGAE, V31, P100, DOI 10.1016/j.hal.2013.10.013; Woloszynska H.J., 1928, ARCHWM HYDROBIOL RYB, V3, P155; Yasumoto T, 1997, BIOSCI BIOTECH BIOCH, V61, P1775, DOI 10.1271/bbb.61.1775	105	28	30	1	19	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	MAY	2015	45						40	52		10.1016/j.hal.2015.03.001	http://dx.doi.org/10.1016/j.hal.2015.03.001			13	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	CN0IV		Green Published			2025-03-11	WOS:000358098200005
J	Neves, RAF; Valentin, JL; Figueiredo, GM; Hégaret, H				Neves, Raquel A. F.; Valentin, Jean Louis; Figueiredo, Gisela M.; Hegaret, Helene			Responses of the common periwinkle <i>Littorina littorea</i> to exposure to the toxic dinoflagellate <i>Alexandrium minutum</i>	JOURNAL OF MOLLUSCAN STUDIES			English	Article							VEGETATIVE CELLS; CYSTS; MICROALGAE; BLOOM; BAY		[Neves, Raquel A. F.] Univ Fed Rio de Janeiro, Inst Biol, Dept Ecol, Programa Posgrad Ecol, Rio De Janeiro, Brazil; [Valentin, Jean Louis] Univ Fed Rio de Janeiro, Inst Biol, Dept Biol Marinha, Lab Zooplancton Marinho, Rio De Janeiro, Brazil; [Figueiredo, Gisela M.] Univ Fed Rio de Janeiro, Inst Biol, Dept Biol Marinha, Lab Ecol Trof, Rio De Janeiro, Brazil; [Hegaret, Helene] Univ Bretagne Occidentale, IFREMER, Lab Sci Environm Marin, Inst Univ Europeen Mer,CNRS,UMR 6539,IRD, F-29280 Plouzane, France	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); CNRS - Institute of Ecology & Environment (INEE); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM)	Neves, RAF (通讯作者)，Univ Fed Rio de Janeiro, Inst Biol, Dept Ecol, Programa Posgrad Ecol, Rio De Janeiro, Brazil.	neves.raf@hotmail.com	VALENTIN, JEAN/I-9403-2012; Hegaret, Helene/B-7206-2008; A. F. Neves, Raquel/D-5128-2015; Figueiredo, Gisela/G-9280-2015	Hegaret, Helene/0000-0003-4639-9013; A. F. Neves, Raquel/0000-0002-2627-9666; Figueiredo, Gisela/0000-0002-0842-2289	Brazilian Capes fellowship [BEX 17644/12-7]; FAPERJ; CNPq	Brazilian Capes fellowship; FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported by the Brazilian Capes fellowship no BEX 17644/12-7 to RAF Neves (Programa de Doutorado Sanduiche no Exterior) and partially supported by FAPERJ and CNPq grants. We also wish to acknowledge Gary H. Wikfors, Sandra E. Shumway, Janet Reid and two anonymous reviewers for their constructive comments on the manuscript and English corrections.	Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Bricelj VM, 2012, HARMFUL ALGAE, V16, P27, DOI 10.1016/j.hal.2012.01.001; Bricelj V.M., 1996, HARMFUL TOXIC ALGAL, P405; Bricelj V. Monica, 1998, Reviews in Fisheries Science, V6, P315, DOI 10.1080/10641269891314294; Bricelj VM, 2005, NATURE, V434, P763, DOI 10.1038/nature03415; CHAPELLE A., 2013, ETUDE PROLIFERATION, V1; Davies MS, 1999, MAR ECOL PROG SER, V179, P247, DOI 10.3354/meps179247; Deeds JR, 2008, MAR DRUGS, V6, P308, DOI [10.3390/md20080015, 10.3390/md6020308]; ERARDLEDENN E, 1993, DEV MAR BIO, V3, P109; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Haberkorn H, 2011, MAR POLLUT BULL, V62, P1191, DOI 10.1016/j.marpolbul.2011.03.034; Hillebrand H, 1999, J PHYCOL, V35, P403, DOI 10.1046/j.1529-8817.1999.3520403.x; Ito K, 2004, MAR POLLUT BULL, V48, P1116, DOI 10.1016/j.marpolbul.2003.12.020; Laabir M, 2007, AQUAT LIVING RESOUR, V20, P51, DOI 10.1051/alr:2007015; MacQuarrie SP, 2008, MAR ECOL PROG SER, V366, P59, DOI 10.3354/meps07538; Menden-Deuer S, 2000, LIMNOL OCEANOGR, V45, P569, DOI 10.4319/lo.2000.45.3.0569; Moore H. B., 1937, Journal of the Marine Biological Association Plymouth NS, V21, P721; NORTON TA, 1990, HYDROBIOLOGIA, V193, P117, DOI 10.1007/BF00028071; OHMAN MD, 1991, BIOL BULL, V181, P500, DOI 10.2307/1542370; Perez KO, 2009, J EXP MAR BIOL ECOL, V369, P79, DOI 10.1016/j.jembe.2008.09.019; Persson A, 2008, MALACOLOGIA, V50, P341, DOI 10.4002/0076-2997-50.1-2.341; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; Persson A, 2012, HARMFUL ALGAE, V19, P101, DOI 10.1016/j.hal.2012.06.006; Prakash A, 1971, Bull Fish Res Bd Can, V177, P1; Shumway Sandra E., 1995, Reviews in Fisheries Science, V3, P1; Sommer U, 1999, AQUAT BOT, V63, P11, DOI 10.1016/S0304-3770(98)00108-9	28	3	3	1	14	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0260-1230	1464-3766		J MOLLUS STUD	J. Molluscan Stud.	MAY	2015	81		2				308	311		10.1093/mollus/eyu092	http://dx.doi.org/10.1093/mollus/eyu092			4	Marine & Freshwater Biology; Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Zoology	CJ2MD		Green Published			2025-03-11	WOS:000355318000016
J	Radmacher, W; Mangerud, G; Tyszka, J				Radmacher, Wieslawa; Mangerud, Gunn; Tyszka, Jaroslaw			Dinoflagellate cyst biostratigraphy of Upper Cretaceous strata from two wells in the Norwegian Sea	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palynostratigraphy; Upper Cretaceous; Dinoflagellate cyst; Voring Basin; Norwegian Sea	VORING BASIN; CONTINENTAL-MARGIN; FAN SYSTEM; EVOLUTION; NORWAY; PALYNOLOGY; SANDSTONES	Rich assemblages of dinoflagellate cysts from two sections in the Norwegian Sea provide a solid basis for a palynostratigraphic framework for the upper Albian to upper Maastrichtian succession in this area. The framework is based on a unique composite section combining samples from the shallow stratigraphic core 6711/4-U-1 and core-samples from well 6707/10-1, the latter filling in data from the intervals represented by hiatuses in core 6711/4-U-1. Seven previously described, and one new palynostratigraphic zone, are recognised. These are based on the relative abundances of prominent taxa together with top and base occurrences of selected age-diagnostic dinoflagellate cyst taxa. The zones and their ages in ascending order from the oldest to youngest comprise: the intra late Albian to intra early Cenomanian Subtilisphaera kalaalliti Interval Zone sensu Nohr-Hansen (1993a); the intra early Cenomanian to intra late Cenomanian Palaeohystrichophora infusorioides-Palaeohystrichophora palaeoinfusa Interval Zone sensu Radmacher et al. (2014b); the Turonian to ?intra early Coniacian Heterosphaeridium diffi cile Interval Zone sensu Nohr-Hansen (2012); the ?intra early Coniacian to late Santonian Dinopterygium alatum Interval Zone sensu Radmacher et al. (2014b); the early Campanian Palaeoglenodinium cretaceum Interval Zone sensu Radmacher et al. (2014b); the new intra Campanian Hystrichosphaeridium dowlingii-Heterosphaeridium spp. Interval Zone; the intra late Campanian Chatangiella bondarenkoi Interval Zone sensu Radmacher et al. (2014b) and the intra late Maastrichtian Wodehouseia spinata Range Zone sensu Nohr-Hansen (1996). Comparison of the palynological events with records in adjacent regions enables correlation across similar paleolatitudes in the Northern Hemisphere. (C) 2015 Elsevier B.V. All rights reserved.	[Radmacher, Wieslawa; Tyszka, Jaroslaw] Polish Acad Sci, ING PAN Inst Geol Sci, Res Ctr Krakow, BioGeoLab, PL-31002 Krakow, Poland; [Mangerud, Gunn] Univ Bergen, Dept Earth Sci, NO-5020 Bergen, Norway	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; University of Bergen	Radmacher, W (通讯作者)，Polish Acad Sci, Inst Geol Sci, Krakow Res Ctr, Ul Senacka 1, PL-31002 Krakow, Poland.	ndkrol@cyf-kr.edu.pl; Gunn.Mangerud@geo.uib.no; ndtyszka@cyf-kr.edu.pl	Radmacher, Wiesława/ABH-7042-2020; Mangerud, Gunn/ABD-2588-2020	Radmacher, Wieslawa/0000-0001-7316-3693	Research Council of Norway; University of Bergen, Norway	Research Council of Norway(Research Council of Norway); University of Bergen, Norway	The authors would like to thank the Norwegian Petroleum Directorate for providing palynological slides from well 6707/10-1, and SINTEF for providing core-samples from well 6711/4-U-1. We greatly appreciate the help of the Laboratory of Palaeobotany and Palynology in Utrecht (The Netherlands). We are grateful to Atle Mork, Robert Williams and Jeno Nagy for help with providing palynological samples and slides. WR would like to thank Graham Bell, Martin Pearce, Mike Kaminski, Eiichi Setoyama and Michal Radmacher for their scientific and technical assistance. The authors also wish to thank the reviewers and the editor for detailed and helpful comments on the manuscript. The project has received support from The Research Council of Norway through the mobility programme "Yggdrasil", providing a six months research fellowship for the first author at the University of Bergen, Norway.	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Palaeobot. Palynology	MAY	2015	216						18	32		10.1016/j.revpalbo.2014.12.007	http://dx.doi.org/10.1016/j.revpalbo.2014.12.007			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	CG6QK					2025-03-11	WOS:000353426800002
J	Tabara, D; Pacton, M; Makou, M; Chirila, G				Tabara, Daniel; Pacton, Muriel; Makou, Matthew; Chirila, Gabriel			Palynofacies and geochemical analysis of Oligo-Miocene bituminous rocks from the Moldavidian Domain (Eastern Carpathians, Romania): Implications for petroleum exploration	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						Palynology; Palynofacies; Organic geochemistry; Oligo-Miocene; Eastern Carpathians	SEDIMENTARY ORGANIC-MATTER; WALLED DINOFLAGELLATE CYSTS; ADJACENT SEAS; BASIN; MIOCENE; FRANCE; NORTH; NAPPE; PALEOENVIRONMENTS; DEPOSITS	A palynological, palynofacies and geochemical investigation conducted on Oligo-Miocene bituminous rocks of the Lower Dysodilic Shale Formation and the Upper Dysodilic Shale Formation (Eastern Carpathians) has allowed recovery of pollen and spore assemblages associated with marine palynofossils (dinoflagellates and prasinophyte algae) and phytoclasts. The general composition of the assemblages suggests an anoxic depositional environment from a distal basin to a highly proximal shelf. The palynological assemblage identified in the Lower Dysodilic Shale Formation exhibits an abundance of dinoflagellate cysts and prasinophyte algae, with some taxa, such as Wetzeliella gochtii, Rhombodinium draco and Cordosphaeridium gracile, indicating a Rupelian early Chattian age for these deposits. In contrast, the Upper Dysodilic Shale Formation displays diverse assemblages of palynomorphs (more pollen and spores) and its age is older than middle Aquitanian. Geochemical (Total Organic Carbon content and Rock-Eval pyrolysis) and palynofacies (optical and scanning electron microscopy) analyses performed on samples from the Lower Dysodilic Shale Formation suggest that it contains type II kerogen (oil prone), consisting of abundant amorphous organic matter (ACM), extracellular polymeric substances (EPS) and coccoid bodies (bacteria or algae). This kerogen comes from a marine source (derived from phytoplankton and bacteria), and likely accumulated in a distal suboxic-anoxic basin. The Total Organic Carbon (TOC) content suggests good to excellent petroleum potential, especially for generating mixed oil and gas. The level of kerogen maturation (inferred from the Thermal Alteration Index, Tr a and prasinophyte algae fluorescence) lies at the boundary between immature and mature phases. The Upper Dysodilic Shale Formation is abundant in translucent and opaque phytoclasts, suggesting a continental organic matter source and type III kerogen, and thus would yield mainly gas. This organic matter was principally deposited in a highly proximal shelf setting. (C) 2015 Elsevier B.V. All rights reserved.	[Tabara, Daniel; Chirila, Gabriel] Alexandru Ioan Cuza Univ, Dept Geol, Iasi 700505, Romania; [Pacton, Muriel; Makou, Matthew] Univ Lyon 1, Labo Geol Lyon Terre Planetes Environm, CNRS, UMR 5276, F-69622 Villeurbanne, France; [Pacton, Muriel] ETH, Inst Geol, CH-8092 Zurich, Switzerland; [Chirila, Gabriel] Halliburton Energy Serv Romania, Bucharest, Romania	Alexandru Ioan Cuza University; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Claude Bernard Lyon 1; Ecole Normale Superieure de Lyon (ENS de LYON); Swiss Federal Institutes of Technology Domain; ETH Zurich; Halliburton	Tabara, D (通讯作者)，Alexandru Ioan Cuza Univ, Dept Geol, 20A Carol I Blvd, Iasi 700505, Romania.	dan.tabara@yahoo.com	Tabara, Daniel/C-6630-2015; Chirila, Gabriel/F-4167-2011; Chirila, Gabriel/A-9361-2010	Tabara, Daniel/0000-0003-1235-6963; Chirila, Gabriel/0000-0002-8253-9848				Alberti G., 1961, Palaeontographica, V116, P1; Amadori ML, 2012, INT J EARTH SCI, V101, P1599, DOI 10.1007/s00531-011-0744-1; Badescu D., 2005, Evolutia tectono-stratigrafica (Mezozoica si Neozoica) a Carpatilor Orientali; BALTES N, 1969, 1 INT C PLANKT MICR, V1, P26; Balteș N., 1983, ANN LINSTITUT GEOL G, V60, P265; Bancila I., 1958, GEOLOGIA CARPATILOR; Barski M, 2010, GEOL CARPATH, V61, P121, DOI 10.2478/v10096-010-0005-4; Batten D.J., 1999, FOSSIL PLANTS SPORES, P15; Batten D.J., 1983, PETROLEUM GEOCHEMIST, P275; Belayouni H, 2009, INT J EARTH SCI, V98, P157, DOI 10.1007/s00531-007-0226-7; Bombardiere L, 2000, SEDIMENT GEOL, V132, P177, DOI 10.1016/S0037-0738(00)00006-3; Carvalho MD, 2006, SEDIMENT GEOL, V192, P57, DOI 10.1016/j.sedgeo.2006.03.017; Charles J.J., 2009, THESIS BANGOR U UK; COMBAZ A., 1980, KEROGEN INSOLUBLE OR, P55; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; Courtinat B, 2003, GEOBIOS-LYON, V36, P13, DOI 10.1016/S0016-6995(02)00074-8; Davey R.J., 1966, STUDIES MESOZOIC CAI, P53; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P263, DOI 10.2307/1485875; Drugg W.S., 1967, Tulane Studies in Geology, V5, P181; Durand B., 1980, Kerogen: Insoluble Organic Matter from Sedimentary Rocks, Institut Francais du Petrole, P35; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; Eisenack A., 1938, Schriften der Physikalisch-Okonomischen Gesellschaft zu Konigsberg, V70, P181; Eisenack A., 1960, Neues Jahrb. 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Palaeobot. Palynology	MAY	2015	216						101	122		10.1016/jsevpalbo.2015.02.002	http://dx.doi.org/10.1016/jsevpalbo.2015.02.002			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	CG6QK					2025-03-11	WOS:000353426800008
J	M'Hamdi, A; Slimani, H; Louwye, S; Soussi, M; Ben Ismail-Lattrache, K; Ben Ali, W				M'Hamdi, Amel; Slimani, Hamid; Louwye, Stephen; Soussi, Mohamed; Ben Ismail-Lattrache, Kmar; Ben Ali, Walid			Dinoflagellates cysts and palynofacies from Maastrichtian-Danian transition at the stratotye El kef (Tunisia)	COMPTES RENDUS PALEVOL			French	Article						Cretaceous-Paleogene boundary; Dinoflagellate cysts; Palynofacies; Stratotype El kef	CRETACEOUS-TERTIARY BOUNDARY; OULED HADDOU; PALEOGENE BOUNDARY; CALCAREOUS NANNOFOSSIL; PLANKTIC FORAMINIFERA; EXTERNAL RIF; BIOSTRATIGRAPHY; EXTINCTION; PALEOCENE; STRATIGRAPHY	A palynological study of the Cretaceous-Paleogene (K-Pg) boundary deposits at the stratotype El kef, Tunisia, showed an exceptional richness of palynomorphs. Dinoflagellate cysts (dinocysts) are abundant, diversified and well preserved. The K-Pg boundary lies right after the last appearance of the Cretaceous species, Dinogymnium cretaceum, Dinogymnium acuminatum and Pterodinium cretaceum, and directly below the first appearance of the species markers of the basal Danian, such as Damassadinium californicum, Membranilarnacia? tenella, Senoniasphaera inornata, Carpatella cornuta, Eisenackia circumtabulata and Lanternosphaeridium reinhardtii. The age determined for these levels based on dinocysts is in agreement with that determined using planktonic foraminifera. The palynofacies study showed an organic matter dominated by marine palynomorphs, essentially dinoflagellate cysts, the sporomorphs are rare. Continental palynomorphs (Sporomorphs) and Amorphous Organic Matter (AOM) are present in all samples. The microplankton is dominated by peridinoid dinocysts with a progressive enrichment at Danian, mainly the Senegalinium group. The Total Organic Carbon (TOC) content is generally less than 0.6 wt %. The TOC, Rock-Eval pyrolysis and palynofacies analyses indicate that the El Haria Formation presents immature organic matter of types II and III and a low Thermal Alteration Index (TAI). (C) 2015 Published by Elsevier Masson SAS on behalf of l'Academie des sciences.	[M'Hamdi, Amel; Soussi, Mohamed; Ben Ismail-Lattrache, Kmar; Ben Ali, Walid] Univ Tunis El Manar, Fac Sci Tunis, Unite Rech, UR 11,ES 15,Dept Geol, El Manar 2092 11, Tunisia; [Slimani, Hamid] Univ Mohammed 5, URAC 46, Lab Geol & Teledetect, Inst Sci,Dept Sci Terre, Rabat, Morocco; [Louwye, Stephen] Univ Ghent, Unite Rech Paleontol, B-9000 Ghent, Belgium	Universite de Tunis-El-Manar; Faculte des Sciences de Tunis (FST); Mohammed V University in Rabat; Ghent University	M'Hamdi, A (通讯作者)，Univ Tunis El Manar, Fac Sci Tunis, Unite Rech, UR 11,ES 15,Dept Geol, Campus Univ, El Manar 2092 11, Tunisia.	mhamdiame25@yahoo.fr	Slimani, Hamid/AAL-4055-2020; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Slimani, Hamid/0000-0001-6392-1913; Soussi, Mohamed/0000-0001-7819-2231				Alberti G., 1959, Mitteilungen aus dem Geologischen Staatsinstitut in Hamburg, V28, P91; ALEGRET L, 1999, TEM GEOL MIN I TECNO, V26, P142; [Anonymous], 9210 GEOL SURV CAN; [Anonymous], 1980, Special Papers in Palaeontology; [Anonymous], 1976, BEDFORD I OCEANOGRAP; Arenillas I, 2000, MICROPALEONTOLOGY, V46, P31; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Batten D.J., 1983, PETROLEUM GEOCHEMIST, P275; Batten D.J., 1982, J. 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R. Acad. Sci. Ser. IIA Earth Planet. Sci., V331, P141, DOI [10.1016/S1251, DOI 10.1016/S1251]	87	17	18	1	11	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	ISSY-LES-MOULINEAUX	65 RUE CAMILLE DESMOULINS, CS50083, 92442 ISSY-LES-MOULINEAUX, FRANCE	1631-0683	1777-571X		CR PALEVOL	C. R. Palevol	APR-MAY	2015	14	3					167	180		10.1016/j.crpv.2015.01.008	http://dx.doi.org/10.1016/j.crpv.2015.01.008			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DB1ZP		Green Published			2025-03-11	WOS:000368308400001
J	Mertens, KN; Takano, Y; Gu, HF; Yamaguchi, A; Pospelova, V; Ellegaard, M; Matsuoka, K				Mertens, Kenneth Neil; Takano, Yoshihito; Gu, Haifeng; Yamaguchi, Aika; Pospelova, Vera; Ellegaard, Marianne; Matsuoka, Kazumi			Cyst-theca relationship of a new dinoflagellate with a spiny round brown cyst, <i>Protoperidinium lewisiae</i> sp nov., and its comparison to the cyst of <i>Oblea acanthocysta</i>	PHYCOLOGICAL RESEARCH			English	Article						Bohai Sea; Changle Harbor; East China Sea; Jinzhou Harbor; Lake Saroma; large subunit rDNA; San Pedro Harbor; small subunit rDNA	MOTILE STAGE RELATIONSHIPS; LATE QUATERNARY; SEQUENCE DATA; DINOPHYCEAE; PERIDINIALES; GENUS; PHYLOGENY; SEA; ULTRASTRUCTURE; IDENTIFICATION	Round spiny brown cysts with apiculocavate processes were isolated from sediments of Lake Saroma, Japan, Changle Harbor, East China Sea, China, Jinzhou Harbor, Bohai Sea, China, and San Pedro Harbor, California, USA. Superficially similar round spiny brown cysts of the species, Oblea acanthocysta were, for comparison, restudied through light microscopy and scanning electron microscopy (SEM) and by sequencing of small subunit (SSU) and large subunit (LSU) rDNA obtained through a single cyst from Lake Saroma. These morphological measurements and SEM observations showed that the new cysts can be discriminated from O.acanthocysta by the archeopyle, number of processes, shape of process bases and its apiculocavate processes. Based on LSU sequences, the most closely related species was Protoperidinium monovelum, for which no cyst stage has been described so far. However, the thecal morphology of the specimens found in this study differed from P.monovelum in details of the sulcal plates and shape of apical pore and 2a plate. We therefore describe Protoperidinium lewisiae sp. nov., which can be found in estuarine subtropical to temperate waters of the Pacific Ocean.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Takano, Yoshihito; Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res ECSER, Nagasaki 852, Japan; [Yamaguchi, Aika] Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 657, Japan; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen, Peoples R China; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC, Canada; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg, Denmark	Ghent University; Nagasaki University; Kobe University; Third Institute of Oceanography, Ministry of Natural Resources; University of Victoria; University of Copenhagen	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be	Mertens, Kenneth/AAO-9566-2020; Ellegaard, Marianne/H-6748-2014; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022	Ellegaard, Marianne/0000-0002-6032-3376; Pospelova, Vera/0000-0003-4049-8133; Mertens, Kenneth/0000-0003-2005-9483; Gu, Haifeng/0000-0002-2350-9171	Kakenhi Grant [22-00805]; Natural Science and Engineering Research Council of Canada (NSERC) [224236]; National Natural Science Foundation of China [41376170]	Kakenhi Grant(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	KNM 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 Natural Science and Engineering Research Council of Canada (NSERC) is acknowledged for partial funding of this project (VP Discovery Grant 224236). Haifeng Gu was supported by the National Natural Science Foundation of China (41376170). Hiromi Saitoh and Kimihiko Maekawa are thanked for assistance during sampling of Saroma Lake. Aya Morinaga is thanked for sampling Omura Bay. Carrie Wolfe, Adam Willingham, and Dennis Dunn from the Southern California Marine Institute, http://www.scmi.net/ are thanked for their help with sampling in San Pedro Harbor. Martin J. Head is acknowledged for sharing published measurements. Two anonymous reviewers and the editors, Mitsunobu Kamiya and Mona Hoppenrath, are thanked for helpful comments that significantly improved the manuscript.	Abe T. 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Res.	APR	2015	63	2					110	124		10.1111/pre.12083	http://dx.doi.org/10.1111/pre.12083			15	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	CG5OA		Bronze			2025-03-11	WOS:000353340200005
J	Liu, TT; Mertens, KN; Ribeiro, S; Ellegaard, M; Matsuoka, K; Gu, HF				Liu, Tingting; Mertens, Kenneth Neil; Ribeiro, Sofia; Ellegaard, Marianne; Matsuoka, Kazumi; Gu, Haifeng			Cyst-theca relationships and phylogenetic positions of Peridiniales (Dinophyceae) with two anterior intercalary plates, with description of <i>Archaeperidinium bailongense</i> sp nov and <i>Protoperidinium fuzhouense</i> sp nov.	PHYCOLOGICAL RESEARCH			English	Article						Archaeperidinium constrictum; Archaeperidinium minutum; cyst-theca relationship; dinoflagellate cysts; LSU rDNA; Protoperidinium abei; Protoperidinium avellana; Protoperidinium excentricum; Protoperidinium stellatum	WALLED DINOFLAGELLATE CYSTS; MOTILE STAGE RELATIONSHIPS; HETEROTROPHIC DINOFLAGELLATE; MOLECULAR PHYLOGENY; GENUS; QUATERNARY	Protoperidinium species with two anterior intercalary plates were originally classified by Jorgensen in the subgenus Archaeperidinium and assigned to the sections Excentrica, Avellana and Archaeperidinium by Taylor, on the basis of the relative size of anterior intercalary plates and the extent of cingulum displacement. Phylogenetic relationships among these three sections have not been fully explored. Recently, Archaeperidinium was reinstated as a genus, but several species fitting the emended description have not been transferred formally as molecular data were not available. In the present study we examined the cyst-theca relationship of seven species with two anterior intercalary plates: four species assigned to Protoperidinium and three to Archaeperidinium, from the China Sea. Partial large subunit ribosomal DNA sequences were obtained from these seven species by single-cell polymerase chain reaction, and for the cyst of Protoperidinium stellatum from France. Two new species, Archaeperidinium bailongense and Protoperidinium fuzhouense, were described based on both theca and cyst morphology, and the cyst-theca relationships of A.constrictum and P.abei var. rotunda were established for the first time. Maximum-likelihood and Bayesian inference analyses revealed that P.fuzhouense was nested within the Protoperidinium sensu stricto clade despite having only six postcingular plates, and sections Excentrica, Avellana and the genus Archaeperidinium were all monophyletic. Our results suggest that the presence/absence of a sulcal fin and antapical horns and the displacement of the cingulum are the most stable characteristics of the motile stages within the respective clades.	[Liu, Tingting; Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen, Peoples R China; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Ribeiro, Sofia] Geol Survey Denmark & Greenland, Dept Marine Geol & Glaciol, Copenhagen, Denmark; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg, Denmark; [Matsuoka, Kazumi] Nagasaki Univ, Nagasaki 852, Japan	Third Institute of Oceanography, Ministry of Natural Resources; Ghent University; Geological Survey Of Denmark & Greenland; University of Copenhagen; Nagasaki University	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen, Peoples R China.	guhaifeng@tio.org.cn	Ribeiro, Sofia/AAZ-2782-2021; Mertens, Kenneth/AAO-9566-2020; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015; Ribeiro, Sofia/G-9213-2018; Ellegaard, Marianne/H-6748-2014	Gu, Haifeng/0000-0002-2350-9171; Mertens, Kenneth/0000-0003-2005-9483; Ribeiro, Sofia/0000-0003-0672-9161; Ellegaard, Marianne/0000-0002-6032-3376	National Science Foundation of China [41376170]	National Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank the editor (Mitsunori Iwataki) and Karin Zonneveld for constructive suggestions that improved the manuscript. This project was supported by National Science Foundation of China (41376170). K.N.M. is a postdoctoral fellow of FWO Belgium. K.N.M. would like to thank J. P. Debenay for sampling Estuaire de la Vie.	Abe T. H., 1936, Science Reports of the Tohoku University (4), V10, P639; Abe T. H., 1981, PUBLICATIONS SETO MA, V6, P1; ABE TOHRU HIDEMITI, 1927, SCI REPT TOHOKU IMP UNIV 4TH SER BIOL, V2, P383; Alix B, 2012, NUCLEIC ACIDS RES, V40, pW573, DOI 10.1093/nar/gks485; [Anonymous], 1995, Marine ecological processes; [Anonymous], 1993, SPEC PUBL NUMBER; Balech E., 1978, Neotropica (La Plata), V24, P3; BALECH E., 1964, BOL INST BIOL MAR MAR DEL PLATA, V4, P1; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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Res.	APR	2015	63	2					134	151		10.1111/pre.12081	http://dx.doi.org/10.1111/pre.12081			18	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	CG5OA					2025-03-11	WOS:000353340200007
J	Ghourchaei, S; Ghasemi-Nejad, E; Vahidinia, M; Ashouri, A				Ghourchaei, Shemshad; Ghasemi-Nejad, Ebrahim; Vahidinia, Mohammad; Ashouri, Alireza			Paleoenvironmental reconstruction of the upper Cretaceous succession (Abtalkh Formation) of the Kopeh-Dagh Basin, northeastern Iran based on foraminiferal and palynological analyses	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Foraminifera; Paleoenvironment; Organic facies; Kopeh-Dagh basin; Iran	BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; TERTIARY BOUNDARY; PLANKTONIC-FORAMINIFERA; TECTONIC EVOLUTION; ORGANIC-MATTER; SOUTH ATLANTIC; SEA; ENVIRONMENTS; PALEOECOLOGY	In order to reconstruct sea surface water productivity and sea floor oxygenation during late Campanian-Maastrichtian, planktonic and benthic foraminiferal assemblages, and organofacies, studies were carried out on a succession of strata in west of Kopeh-Dagh basin of northeastern Iran. Six distinct planktonic (P-types 1-6) and five benthic foraminiferal assemblages (B-types1-5) and five organic assemblages (O-types 1-5) were distinguished in the studied sequence. The changes in composition of assemblages along the section are correlated with variations in surface productivity and water aeration. The changes indicate transition from mesotrophic to oligotrophic conditions.	[Ghourchaei, Shemshad; Vahidinia, Mohammad; Ashouri, Alireza] Ferdowsi Univ Mashhad, Dept Geol, Fac Sci, Mashhad, Iran; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Dept Geol, Fac Sci, Tehran, Iran	Ferdowsi University Mashhad; University of Tehran	Ghourchaei, S (通讯作者)，Ferdowsi Univ Mashhad, Dept Geol, Fac Sci, Mashhad, Iran.	shemshadg@gmail.com	Vahidinia, Mohammad/AAB-7110-2020; Ghasemi-Nejad, Ebrahim/AAF-6087-2020; ghourchaei, shemshad/S-3283-2016	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068; Ashouri, Ali Reza/0000-0002-2913-4913				Abramovich S, 2003, PALAEOGEOGR PALAEOCL, V202, P1, DOI 10.1016/S0031-0182(03)00572-8; Abramovich S, 2003, MAR MICROPALEONTOL, V48, P225, DOI 10.1016/S0377-8398(03)00021-5; Abramovich S, 2002, PALAEOGEOGR PALAEOCL, V178, P145, DOI 10.1016/S0031-0182(01)00394-7; Abramovich S, 2010, PALEOCEANOGRAPHY, V25, DOI 10.1029/2009PA001843; Afshar Harb A., 1969, B IRAN PET I, V37, P86; Afshar-Harb A, 1994, GEOLOGY KOPEH DAGH; Afshar-Harb A, 1979, THESIS U LONDON NO I; Aghanabati A, 2004, GEOLOGY IRAN GEOLOGI; Alavi M, 1997, GEOL SOC AM BULL, V109, P1563, DOI 10.1130/0016-7606(1997)109<1563:TTAARO>2.3.CO;2; Alegret L, 2005, PALAEOGEOGR PALAEOCL, V224, P53, DOI 10.1016/j.palaeo.2005.03.031; Alegret L, 2001, MICROPALEONTOLOGY, V47, P269, DOI 10.2113/47.4.269; Alegret L, 2001, GEOLOGY, V29, P891, DOI 10.1130/0091-7613(2001)029<0891:BFATCT>2.0.CO;2; ALMOGILABIN A, 1990, NATO ADV SCI I C-MAT, V327, P565; ALMOGILABIN A, 1993, PALEOCEANOGRAPHY, V8, P671, DOI 10.1029/93PA02197; [Anonymous], UTRECHT MICROPALAEON; [Anonymous], 2007, Paleopalynology; Ashckenazi-Polivoda S, 2011, PALAEOGEOGR PALAEOCL, V305, P93, DOI 10.1016/j.palaeo.2011.02.018; Ashckenazi-Polivoda S, 2010, PALAEOGEOGR PALAEOCL, V289, P134, DOI 10.1016/j.palaeo.2010.02.028; Barrera E, 1990, PALEOCEANOGRAPHY, V5, P867, DOI 10.1029/PA005i006p00867; Batten D.J., 1983, PETROLEUM GEOCHEMIST, P275; BERBERIAN M, 1981, CAN J EARTH SCI, V18, P210, DOI 10.1139/e81-019; BERGGREN WA, 1975, PALAEOGEOGR PALAEOCL, V18, P73, DOI 10.1016/0031-0182(75)90025-5; BERNHARD JM, 1986, J FORAMIN RES, V16, P207, DOI 10.2113/gsjfr.16.3.207; Bernhard JM, 1997, J FORAMIN RES, V27, P301, DOI 10.2113/gsjfr.27.4.301; Bombardiere L, 2000, SEDIMENT GEOL, V132, P177, DOI 10.1016/S0037-0738(00)00006-3; BOULTER MC, 1986, SEDIMENTOLOGY, V33, P871, DOI 10.1111/j.1365-3091.1986.tb00988.x; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; BRINKHUIS H, 1988, REV PALAEOBOT PALYNO, V56, P5, DOI 10.1016/0034-6667(88)90071-1; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; CARON M, 1983, MAR MICROPALEONTOL, V7, P453, DOI 10.1016/0377-8398(83)90010-5; COCCIONI R, 1994, GEOLOGY, V22, P779, DOI 10.1130/0091-7613(1994)022<0779:KTBEGI>2.3.CO;2; Conan SMH, 2000, DEEP-SEA RES PT II, V47, P2207, DOI 10.1016/S0967-0645(00)00022-9; DHONDT S, 1995, PALEOCEANOGRAPHY, V10, P123, DOI 10.1029/94PA02671; Erbacher J, 1998, CRETACEOUS RES, V19, P805, DOI 10.1006/cres.1998.0134; Fakouri GA, 1996, THESIS U SHAHID BEHE; Frank TD, 2005, PALEOCEANOGRAPHY, V20, DOI 10.1029/2004PA001052; Friedrich O, 2006, MAR MICROPALEONTOL, V58, P135, DOI 10.1016/j.marmicro.2005.10.005; Friedrich O, 2005, J FORAMIN RES, V35, P228, DOI 10.2113/35.3.228; Friedrich O., 2009, PARADOX REV MICROPAL, V53, P175; Ghoorchaei S, 2012, GEOPERSIA, V2, P25; Golonka J, 2004, TECTONOPHYSICS, V381, P235, DOI 10.1016/j.tecto.2002.06.004; Habib D, 2007, PALAEOGEOGR PALAEOCL, V255, P87, DOI 10.1016/j.palaeo.2007.02.043; Hammer O., 2005, PALAEONTOL ELECTRON, V4, P1; HART MB, 1980, NATURE, V286, P252, DOI 10.1038/286252a0; Hemleben C., 1989, MODERN PLANKTONIC FO, DOI [10.1007/978-1-4612-3544-6, DOI 10.1007/978-1-4612-3544-6]; Hoek RP, 1996, MICROPALEONTOLOGY, V42, P125, DOI 10.2307/1485866; Holbourn A, 2001, J FORAMIN RES, V31, P60, DOI 10.2113/0310060; Holbourn A, 1999, GEOL SOC SPEC PUBL, V153, P195, DOI 10.1144/GSL.SP.1999.153.01.13; Holbourn A, 1999, NEUES JAHRB GEOL P-A, V212, P335, DOI 10.1127/njgpa/212/1999/335; JAMINSKI J, 1995, REV PALAEOBOT PALYNO, V87, P43, DOI 10.1016/0034-6667(94)00141-6; Jorissen FJ, 1999, MAR GEOL, V153, P91, DOI 10.1016/S0025-3227(98)00088-7; KAIHO K, 1994, GEOLOGY, V22, P719, DOI 10.1130/0091-7613(1994)022<0719:BFDOIA>2.3.CO;2; KAIHO K, 1992, MAR MICROPALEONTOL, V18, P229, DOI 10.1016/0377-8398(92)90014-B; Kalantary A., 1987, BIOFACIES RELATIONSH; Keller G, 2004, MAR MICROPALEONTOL, V53, P83, DOI 10.1016/j.marmicro.2004.04.012; KOUTSOUKOS EAM, 1990, PALAEOGEOGR PALAEOCL, V77, P145, DOI 10.1016/0031-0182(90)90130-Y; KROON D, 1990, MAR MICROPALEONTOL, V16, P25, DOI 10.1016/0377-8398(90)90027-J; Kuhnt Wolfgang, 1996, Revue de Micropaleontologie, V39, P271, DOI 10.1016/S0035-1598(96)90119-1; Leckie R.M., 1998, STRATIGRAPHY PALEOEN, V6, P101; LECKIE RM, 1987, MICROPALEONTOLOGY, V33, P164, DOI 10.2307/1485491; Li LQ, 1999, MAR GEOL, V161, P171, DOI 10.1016/S0025-3227(99)00078-X; Loeblich Jr A. 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P. C. M., 1986, Bulletin des Centres de Recherches ExplorationProduction ElfAquitaine, V11, P1; Waveren I, 1994, PALAEOGEOGR PALAEOCL, V112, P85; Widmark JGV, 1997, PALAIOS, V12, P354, DOI 10.2307/3515335; Widmark JGV, 1997, MAR MICROPALEONTOL, V31, P135, DOI 10.1016/S0377-8398(97)00008-X; Widmark JGV, 2000, CRETACEOUS RES, V21, P367, DOI 10.1006/cres.1999.0193	84	6	6	0	7	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	APR	2015	8	4					2153	2168		10.1007/s12517-014-1276-3	http://dx.doi.org/10.1007/s12517-014-1276-3			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CF6BH					2025-03-11	WOS:000352640900026
J	Cruz-López, R; Maske, H				Cruz-Lopez, Ricardo; Maske, Helmut			A non-amplified FISH protocol to identify simultaneously different bacterial groups attached to eukaryotic phytoplankton	JOURNAL OF APPLIED PHYCOLOGY			English	Article						Fluorescence in situ hybridization; Epiphytic bacteria; Phytoplankton cells	IN-SITU HYBRIDIZATION; OLIGONUCLEOTIDE PROBES; CYST FORMATION; EPIFLUORESCENCE MICROSCOPY; HIROSHIMA BAY; SP NOV.; DINOPHYCEAE; IDENTIFICATION; DIATOMS; GROWTH	Eukaryotic phytoplankton and bacteria form complex trophic interactions in nature and cultures. The interaction will depend on the spatial arrangement but the architecture of these arrangements has been little investigated. Here we modified a protocol to identify and localize multiple bacterial taxa attached to phytoplankton cells in culture and natural samples, including sensitive dinoflagellates. Samples were embedded in agarose and hybridized simultaneously with different probes of distinct fluorescence properties. Embedding avoided losses or damage of host cells and preserved the attached bacteria during hybridization and washing. Embedding still allowed efficient hybridization and identification of intact host cells. After fluorescence in situ hybridization of the bacteria the phytoplankton host cells, including dinoflagellates were still intact. Digital image stacks taken with a wide field epifluorescence microscope using different excitation-emission wavelength combinations allow the location of the different bacterial groups on the host cell surface and the spatial relationship of the different bacterial groups.	[Cruz-Lopez, Ricardo; Maske, Helmut] CICESE, Dept Biol Oceanog, Ensenada 22860, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Cruz-López, R (通讯作者)，CICESE, Dept Biol Oceanog, Carretera Tijuana Ensenada 3918, Ensenada 22860, Baja California, Mexico.	ricardo.crlp@gmail.com		Maske, Helmut/0000-0002-8047-6484; Cruz-Lopez, Ricardo/0000-0002-4782-7625	Consejo Nacional de Ciencia y Tecnologia [CB-2008-01 106003]	Consejo Nacional de Ciencia y Tecnologia(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	This work was supported by Consejo Nacional de Ciencia y Tecnologia project CB-2008-01 106003 (to H.M.) and a PhD fellowship (to R.C-L.). We thank Michael Latz (Scripps Institute of Oceanography) for providing L. polyedrum strain and the 'Microalgae-Biology and Culture laboratory' (Centro de Investigacion Cientifica y Educacion Superior de Ensenada) for providing the G. angulosa strain.	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Appl. Phycol.	APR	2015	27	2					797	804		10.1007/s10811-014-0379-2	http://dx.doi.org/10.1007/s10811-014-0379-2			8	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	CF3KA					2025-03-11	WOS:000352446200017
J	Avila, M; De Zarate, C; Clement, A; Carbonell, P; Pérez, F				Avila, Marcela; De Zarate, Constanza; Clement, Alejandro; Carbonell, Pamela; Perez, Felipe			Effect of abiotic factors in vegetative growth of <i>Alexandrium catenella</i> from cysts in laboratory	REVISTA DE BIOLOGIA MARINA Y OCEANOGRAFIA			Spanish	Article						Alexandrium catenella; growth rate; temporal and dormant cysts; temperature; photoperiod; policlonal culture	KOFOID BALECH 1985; SOUTHERN CHILE; TOXIN CONTENT; DINOPHYCEAE; WHEDON; TEMPERATURE; STRAINS; SALINITY; TOXICITY; OUTBREAK	Alexandrium catenella is a toxic dinoflagellate that causes harmful algal blooms in the marine inland sea of southern Chile. To gain an insight about the effect of temperature, salinity, photoperiod and nutrient levels in culture medium growth vegetative polyclonal cells of A. catenella (strain ACO90610 QUE-Q) from sediment cysts (Quellon, Chile) were cultivated. The strain was studied in different experiments by cells count using the Utermohl method, every 2 days during 56 days. Effect of salinity (15, 20, 25, 30) using as control seawater with 31 of salinity; temperature (10, 15 and 20 degrees C) photoperiod (12: 12, 16: 08 and 8: 16 L: D) and was determinated nutrients, with L1 medium at different proportions of NaNO3 and NaHPO4. The results showed that cells of A. catenella grew in all range of salinities tested, showing a greater growth rate at 30 (3788 cells mL(-1) on day 26; mu= 0.18 div d(-1)). At 20 degrees C, temperature decrease the growth rate (<1500 cells mL(-1); mu = 0.11 div d(-1)) while at 10 degrees C and 15 degrees C stimulate the growth (> 3000 cells mL(-1); mu = 0.12 div d(-1)). The culture medium without nitrates and phosphates inhibit growth rates, while L1 and L1/ 2 support growth (> 2800 cells. L-1; mu = 0.08 and 0.06 div d(-1), respectively). Different photo-period treatments have similar results (mu = 0.05, 0.07 and 0.08 div d(-1)) reaching 2000 cells mL(-1) at the end of the experiment. These results suggest that the cultured strain responded to changes in temperature, photoperiod and differ ent nutrient concentrations.	[Avila, Marcela; De Zarate, Constanza] Univ Arturo Prat, ICYT, Puerto Montt, Chile; [Avila, Marcela; De Zarate, Constanza; Clement, Alejandro; Carbonell, Pamela; Perez, Felipe] Corporac Desarrollo Univ Arturo Prat, CORDUNAP, Iquique, Chile	Universidad Arturo Prat	Avila, M (通讯作者)，Univ Arturo Prat, ICYT, Ejercito 443, Puerto Montt, Chile.	mavila@unap.cl		CLEMENT, ALEJANDRO/0009-0006-2495-7087				Aguilera-Belmonte A, 2013, HARMFUL ALGAE, V23, P55, DOI 10.1016/j.hal.2012.12.006; Aguilera-Belmonte A, 2011, HARMFUL ALGAE, V12, P105, DOI 10.1016/j.hal.2011.09.006; Alves-De-Souza C, 2008, BOT MAR, V51, P399, DOI 10.1515/BOT.2008.052; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; Bustamante J, 2003, HARMFUL ALGAE, V2, P207, DOI 10.1016/S1568-9883(03)00022-2; Uribe Juan Carlos, 2010, Anales Instituto Patagonia (Chile), V38, P103; Carrasco C, 2007, TALL RES CRUC CIMAR, P35; Cassis David, 2002, Rev. biol. mar. oceanogr., V37, P43; Clement A., 1988, THESIS OREGON STATE; Collos Y, 2004, J PHYCOL, V40, P96, DOI 10.1046/j.1529-8817.2004.03034.x; Cordova Jose Luis, 2002, Harmful Algae, V1, P343, DOI 10.1016/S1568-9883(02)00066-5; Cox AM, 2008, HARMFUL ALGAE, V7, P379, DOI 10.1016/j.hal.2007.01.006; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; Fuentes C., 2006, INT SOC STUD HARMF A, P183; Garrido Cristián, 2012, Anales Instituto Patagonia (Chile), V40, P155, DOI 10.4067/S0718-686X2012000200015; Garrido Cristián, 2012, Anales Instituto Patagonia (Chile), V40, P113, DOI 10.4067/S0718-686X2012000200010; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Guzman L., 1975, AN I PATAGONIA, V6, P209; Guzman L, 1975, ANS I PAT PUNTA AREN, V6, P173; Iriarte JL, 2007, ESTUAR COAST SHELF S, V74, P471, DOI 10.1016/j.ecss.2007.05.015; Laabir M, 2011, J PLANKTON RES, V33, P1550, DOI 10.1093/plankt/fbr050; Lembeye G., 2006, AVANCES CONOCIMIENTO, P99; Lembeye G, 1998, SEGUIMIENTO TOXICIDA, P1; Mardones J., 2010, Harmful Algae News, V41, P8; Matsuoka K., 2000, GUIA TECNICA ESTUDIO; Molinet C, 2003, REV CHIL HIST NAT, V76, P681; Munoz Pablo, 1992, Revista de Biologia Marina, V27, P187; Navarro JM, 2006, HARMFUL ALGAE, V5, P762, DOI 10.1016/j.hal.2006.04.001; Seguel M, 2006, DISTRIBUCION QUISTES, P51; Seguel M, 2010, RES CRUC CIMAR 10 FI, P71; Seguel Miriam, 2010, Ciencia y Tecnologia del Mar, V33, P59; Siu GKY, 1997, HYDROBIOLOGIA, V352, P117, DOI 10.1023/A:1003042431985; Varela D, 2012, HARMFUL ALGAE, V15, P8, DOI 10.1016/j.hal.2011.10.029	33	6	6	2	29	UNIV VALPARAISO	VINA DEL MAR	FACULTAD CIENCIAS MAR RECURSOS NATURALES, CASILLA 5080 - RENACA, VINA DEL MAR, 00000, CHILE	0717-3326	0718-1957		REV BIOL MAR OCEANOG	Rev. Biol. Mar. Oceanogr.	APR	2015	50			1	SI		177	185		10.4067/S0718-19572015000200004	http://dx.doi.org/10.4067/S0718-19572015000200004			9	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	CF3VZ		Green Submitted, hybrid			2025-03-11	WOS:000352478300004
J	Tang, YZ; Gobler, CJ				Tang, Ying Zhong; Gobler, Christopher J.			SEXUAL RESTING CYST PRODUCTION BY THE DINOFLAGELLATE <i>AKASHIWO SANGUINEA</i>: A POTENTIAL MECHANISM CONTRIBUTING TO THE UBIQUITOUS DISTRIBUTION OF A HARMFUL ALGA	JOURNAL OF PHYCOLOGY			English	Article						Akashiwo sanguinea; geographic distribution; germination; harmful algal bloom; life cycle; resting cyst	RED TIDE; GYMNODINIUM-CATENATUM; MICRORETICULATE CYST; GONYAULAX-TAMARENSIS; SURFACE SEDIMENTS; CHESAPEAKE BAY; COASTAL LAGOON; BALLAST WATER; LIFE-HISTORY; BLOOMS	The dinoflagellate Akashiwo sanguinea is a well known, cosmopolitan harmful microalga that frequently forms harmful algal blooms (HABs) in marine estuaries from temperate to tropical waters, and has posed a severe threat to fish, shellfish, and sea birds. Therefore, it is important to understand the ecology of this species, particularly the mechanisms regulating its ubiquitous geographic distribution and frequent recurrence of. To date, the mechanisms regulating distribution and recurrence of HABs by this species have been poorly understood. While resting cyst production can play a central role in the geographic expansion and initiation of HABs, studies of the life cycle of this alga, including cyst production, have been lacking. Here, we demonstrate that A. sanguinea produces sexual resting cysts homothallically. We present evidence for cell pairs in sexual mating, biflagellated planozygote formation, and cysts of different morphologies, and we describe time series for germination of cysts to germlings with two longitudinal flagella, along with studies of possible factors affecting cyst production. Phylogenetic analysis of large sub-unit rDNA sequences revealed a monophyly of this species and thus possibly a recent common ancestor for all global populations. The discovery of resting cyst production by A. sanguinea suggests its frequent recurrence of blooms and global distribution may have been facilitated by the natural and anthropogenic transport of resting cysts.	[Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Shandong, Peoples R China; [Tang, Ying Zhong; Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA	Chinese Academy of Sciences; Institute of Oceanology, CAS; State University of New York (SUNY) System; Stony Brook University	Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, 7 Nanhai Rd, Qingdao 266071, Shandong, Peoples R China.	yingzhong.tang@qdio.ac.cn; christopher.gobler@stonybrook.edu	Gobler, Christopher/JOZ-2924-2023		Suffolk County Department of Health Services, Office of Ecology; New Tamarind Foundation; Fund for Creative Research Groups by NSFC [41121064]	Suffolk County Department of Health Services, Office of Ecology; New Tamarind Foundation; Fund for Creative Research Groups by NSFC	We acknowledge support from the Suffolk County Department of Health Services, Office of Ecology, and the New Tamarind Foundation. This study was also funded by the Fund for Creative Research Groups by NSFC (41121064). We thank Theresa Hattenrath for isolating the Northport Bay cultures of Akashiwo sanguinea, Mathew J. Harke for the phylogenetic analyses, and Dr. Ning Xu from Jinan University, China for sharing the sequences of A. sanguinea from Chinese coastal waters. We are also highly grateful of the constructive comments of the three anonymous reviewers and the Associate Editor, A. Michelle Wood. We claim that there is no conflict of interest regarding the work presented in this article.	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Phycol.	APR	2015	51	2					298	309		10.1111/jpy.12274	http://dx.doi.org/10.1111/jpy.12274			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	CF5SO	26986525				2025-03-11	WOS:000352617500010
J	Vasiliev, I; Reichart, GJ; Grothe, A; Damsté, JSS; Krijgsman, W; Sangiorgi, F; Weijers, JWH; van Roij, L				Vasiliev, Iuliana; Reichart, Gert-Jan; Grothe, Arjen; Damste, Jaap S. Sinninghe; Krijgsman, Wout; Sangiorgi, Francesca; Weijers, Johan W. H.; van Roij, Linda			Recurrent phases of drought in the upper Miocene of the Black Sea region	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Black Sea; Miocene; Hydrogen isotopes; Carbon isotopes; Alkenones; n-Alkanes; TEX86; SSTs; Palynology	MESSINIAN SALINITY CRISIS; DINOFLAGELLATE CYST RECORD; LONG-CHAIN ALKENONES; INDIVIDUAL N-ALKANES; DELTA-D VALUES; HYDROGEN ISOTOPES; TETRAETHER LIPIDS; CLIMATE VARIABILITY; EMILIANIA-HUXLEYI; MEMBRANE-LIPIDS	Since the Miocene the Black Sea proved to be highly sensitive to fluctuations in the hydrological cycle because of its recurrent restricted connections with the open ocean and the location between the dry Mediterranean and more humid higher northern latitudes. Although the Black Sea formed one of the foci of the 1975 Deep Sea Drilling Project Leg 42B, robust tools to reconstruct past changes in its hydrological cycle were lacking at that time. Here we revisit the sedimentary succession (Hole 380A) and determined compound-specific carbon (delta C-13) hydrogen isotope ratios (delta D) of terrestrial and aquatic biomarkers to investigate changes in the hydrological budget of the Black Sea during the late Miocene. The delta C-13 and delta D isotopic composition of n-alkanes as well as alkenones and palynology indicate large environmental changes in the Black Sea and/or in the sources of the water entering the Black Sea during the late Miocene. The delta D of alkenones, showing an enrichment of more than 80 parts per thousand at the end of the Miocene, implies a major shift in basin hydrology, possibly resulting in severely increased salinity. These changes in delta D composition of the alkenones coincide with both with sharp shifts in reconstructed sea surface temperature and palynological assemblages. Two intervals with negative water budget were identified, most likely caused by enhanced evaporation. The older and longer dry/evaporative phase predates the Maeotian/Pontian boundary (regional stages) at similar to 6.1 Ma. The younger drying phase corresponds to the Messinian Salinity Crisis. This shift to highly evaporative conditions is related to a similar shift previously observed in a Messinian (Pontian) sedimentary succession from the Taman Peninsula (Russia). These recurrent dry phases likely reflect regional climatic shifts over a significantly larger area around the Black Sea area during the upper Miocene. (C) 2015 Elsevier B.V. All rights reserved.	[Vasiliev, Iuliana; Reichart, Gert-Jan; Damste, Jaap S. Sinninghe; Weijers, Johan W. H.; van Roij, Linda] Univ Utrecht, Dept Earth Sci, Organ Geochem, NL-3584 CD Utrecht, Netherlands; [Vasiliev, Iuliana; Krijgsman, Wout] Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands; [Reichart, Gert-Jan; Krijgsman, Wout] Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands; [Grothe, Arjen; Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, Lab Palaeobot & Palynol, Marine Palynol & Paleoceanog, NL-3584 CD Utrecht, Netherlands	Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Vasiliev, I (通讯作者)，Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands.	i.vasiliev@uu.nl	Reichart, Gert-Jan/N-6308-2018; Sinninghe Damste, Jaap/F-6128-2011	Reichart, Gert-Jan/0000-0002-7256-2243; Krijgsman, Wout/0000-0002-1472-1074; Vasiliev, Iuliana/0000-0002-1024-6966; Sinninghe Damste, Jaap/0000-0002-8683-1854; Sangiorgi, Francesca/0000-0003-4233-6154	Netherlands Earth and Life Sciences Foundation (ALW); Netherlands Organization for Scientific Research (NWO) via the Veni grant [863.09.006]	Netherlands Earth and Life Sciences Foundation (ALW); Netherlands Organization for Scientific Research (NWO) via the Veni grant	We are grateful to the IODP Bremen Core Repository. We thank M. Stoica and C. Van Baak for inspiring discussions on Black Sea hydrological changes, and Y.R. Mulders and T. Donders for help with palynological work. This research was financially supported by the Netherlands Earth and Life Sciences Foundation (ALW) with support from The Netherlands Organization for Scientific Research (NWO) via the Veni grant, number 863.09.006 of IV.	Andersen N, 2001, GEOLOGY, V29, P799, DOI 10.1130/0091-7613(2001)029<0799:LARCVD>2.0.CO;2; [Anonymous], 2005, Rev. 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Paleoclimatol. Paleoecol.	APR 1	2015	423						18	31		10.1016/j.palaeo.2015.01.020	http://dx.doi.org/10.1016/j.palaeo.2015.01.020			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	CE4KD		Green Published			2025-03-11	WOS:000351798600002
J	Sildever, S; Andersen, TJ; Ribeiro, S; Ellegaard, M				Sildever, Sirje; Andersen, Thorbjorn Joest; Ribeiro, Sofia; Ellegaard, Marianne			Influence of surface salinity gradient on dinoflagellate cyst community structure, abundance and morphology in the Baltic Sea, Kattegat and Skagerrak	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						sea-surface salinity (SSS); dinoflagellate cysts; species diversity; Operculodinium centrocarpum; process length; Baltic Sea	PROCESS LENGTH VARIATION; PROTOCERATIUM-RETICULATUM; RECENT SEDIMENTS; LIFE-CYCLE; WEST-COAST; GERMINATION; FJORD; EUTROPHICATION; PRESERVATION; ASSEMBLAGES	Changes in dinoflagellate cyst forming species composition, abundance and morphology along the surface salinity gradient in the Baltic Sea, Kattegat and Skagerrak were investigated and compared with detailed surface salinity data. A strong positive correlation was found between species diversity and surface salinity (R-2 = 0.94; n = 7) in the Baltic Sea-Kattegat-Skagerrak system. The most pronounced decrease in dinoflagellate cyst diversity occurred between Kattegat and the Arkona basin, where the surface salinity also steeply declined. Overall, the total cyst abundance decreased along the salinity gradient. However, in the Gotland and particularly in the Northern Central basin cyst concentrations were elevated compared to the surrounding basins and the cyst community was dominated by heterotrophic cyst-producing dinoflagellate species. Possible factors behind this observation are discussed, with increased nutrient supply as the most likely primary cause. In addition, surface salinity was also confirmed to influence process length development of Operculodinium centrocarpum (R-2 = 0.86; n = 145), which was the most abundant species in this study. (C) 2015 Elsevier Ltd. All rights reserved.	[Sildever, Sirje; Ellegaard, Marianne] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-1353 Frederiksberg K, Denmark; [Andersen, Thorbjorn Joest] Univ Copenhagen, Dept Geosci & Nat Resource Management, Sect Geog, DK-1350 Copenhagen K, Denmark; [Ribeiro, Sofia] Geol Survey Greenland & Denmark, Marine Geol & Glaciol, DK-1350 Copenhagen K, Denmark	University of Copenhagen; University of Copenhagen; Geological Survey Of Denmark & Greenland	Ellegaard, M (通讯作者)，Univ Copenhagen, Dept Plant & Environm Sci, Thorvaldsensvej 40, DK-1871 Frederiksberg C, Denmark.	me@plen.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Andersen, Thorbjorn Joest/N-7560-2014; Ellegaard, Marianne/H-6748-2014; Sildever, Sirje/G-6674-2017; Ribeiro, Sofia/G-9213-2018	Andersen, Thorbjorn Joest/0000-0001-5032-9945; Ellegaard, Marianne/0000-0002-6032-3376; Sildever, Sirje/0000-0002-4847-936X; Ribeiro, Sofia/0000-0003-0672-9161	European Commission 7th Framework Programme (FP) [217246]; Estonian Ministry of Education and Research [IUT 19-6]	European Commission 7th Framework Programme (FP); Estonian Ministry of Education and Research(Ministry of Education & Research Tartu)	J. Laanemets, M.J. Lilover and S.VM. Tesson are thanked for the scientific discussion. Surface sediment samples used in this study were collected within the INFLOW (The Holocene Saline Water Inflow Changes into the Baltic Sea) project, funded by the European Commission 7th Framework Programme (FP/2007-2013) under Grant agreement No. 217246. Writing of the manuscript was supported by the institutional research funding (IUT 19-6) of the Estonian Ministry of Education and Research.	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Coast. Shelf Sci.	MAR 20	2015	155						1	7		10.1016/j.ecss.2015.01.003	http://dx.doi.org/10.1016/j.ecss.2015.01.003			7	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	CF6OI					2025-03-11	WOS:000352675600002
J	Deprez, A; Tesseur, S; Stassen, P; D'haenens, S; Steurbaut, E; King, C; Claeys, P; Speijer, RP				Deprez, Arne; Tesseur, Steven; Stassen, Peter; D'haenens, Simon; Steurbaut, Etienne; King, Christopher; Claeys, Philippe; Speijer, Robert P.			Early Eocene environmental development in the northern Peri-Tethys (Aktulagay, Kazakhstan) based on benthic foraminiferal assemblages and stable isotopes (O, C)	MARINE MICROPALEONTOLOGY			English	Article						Early Eocene; Benthic foraminifera; Paleoecology; Kazakhstan; Oxygen deficiency; Trophic conditions	THERMAL MAXIMUM; LATE PALEOCENE; DINOFLAGELLATE CYSTS; CARBON ISOTOPES; SEA-LEVEL; OXYGEN; BIOSTRATIGRAPHY; ATLANTIC; DABABIYA; SECTION	The Aktulagay section in Kazakhstan provides an expanded northern Tethyan record of the middle Ypresian (calcareous nannoplankton zones NP11-13, similar to 54-50 Ma), including the Early Eocene Climatic Optimum (EECO). The marl sequence features a series of sapropel beds, observed throughout the Peri-Tethys, indicative of the basin-wide occurrence of episodic hypoxic events. In order to unravel the paleoenvironmental evolution at Aktulagay during this period of global warming, we investigated the benthic foraminiferal record by means of a detailed multivariate analysis of the >63 mu m fraction, as well as through stable isotopic (C, O) investigations on excellently preserved benthic foraminiferal specimens. The Alashen Formation (NP11 to lower NP12; similar to 54 to 52.5 Ma), in the lower part of the sequence, contains a diverse assemblage of deep outer neritic (similar to 200-250 m) benthic foraminifera, with common Pulsiphonina prima and Paralabamina lunata. The seafloor conditions are interpreted as initially (54 Ma) well-ventilated and oligo-to mesotrophic, gradually changing to more eutrophic and oxygen-limited, culminating in more permanent low oxygen conditions and eutrophy in the sapropel-bearing Aktulagay BI unit (middle NP12; similar to 52.5-52 Ma). The latter conclusion is corroborated by the dominance of Anomalinoides acutus and Bulimina aksuatica and the lower diversity. Also the upward migration of endobenthic species to the sediment-water interface, as suggested by rising delta C-13(endobenthic) values, supports this interpretation. A transgression, which flooded lowlands, might have caused this development. In the Aktulagay B2 unit (top NP12-NP13; similar to 52-50 Ma), benthic foraminiferal assemblages dominated by Epistominella minute suggest an oligotrophic environment, with transient pulses of phytodetritus and moderate ventilation. The Aktulagay B2 unit coincides with the peak temperature interval of the EECO, as indicated by its position close to the base of NP13 and rising delta C-13(epibenthic) values. Large river plumes, episodically reaching the area, in a monsoonal climatic context, might explain this basin development. Although it is not unlikely that some of the observed patterns are related to long-term climate change, it can currently not be excluded that changing paleogeography and variable connections to the Tethys, Atlantic and the Arctic Ocean were responsible for the long-term period with dysoxia and anoxia during deposition of the sapropel beds at the Peri-Tethyan seafloor. The evolution of the basin as observed in Aktulagay shows similarities to the evolution of the North Sea Basin as observed in Denmark, suggesting that these basins were connected during the Early Eocene. (C) 2014 Elsevier B.V. All rights reserved.	[Deprez, Arne; Tesseur, Steven; Stassen, Peter; D'haenens, Simon; Steurbaut, Etienne; Speijer, Robert P.] Katholieke Univ Leuven, Dept Earth & Environm Sci, B-3001 Heverlee, Belgium; [Steurbaut, Etienne] Royal Belgian Inst Nat Sci, OD Earth & Hist Life, B-1000 Brussels, Belgium; [Claeys, Philippe] Vrije Univ Brussel, Earth Syst Sci, B-1050 Brussels, Belgium	KU Leuven; Royal Belgian Institute of Natural Sciences; Vrije Universiteit Brussel	Deprez, A (通讯作者)，Katholieke Univ Leuven, Dept Earth & Environm Sci, Celestijnenlaan 200E, B-3001 Heverlee, Belgium.	arne.deprez@ees.kuleuven.be; steven_tesseur@msn.com; petenstassen@ees.kuleuven.be; simon.dhaenens@yale.edu; etienne.steurbaut@naturalsciences.be; chrldng@globalnet.co.uk; phclaeys@vub.ac.be; robertspeijer@ees.kuleuven.be	Speijer, Robert/H-5073-2016; Claeys, Philippe/B-4895-2008; Stassen, Peter/P-8837-2015; D'haenens, Simon/IST-6502-2023	Claeys, Philippe/0000-0002-4585-7687; Stassen, Peter/0000-0002-2663-2781; D'haenens, Simon/0000-0003-1248-3188	KU Leuven Research Fund; Research Foundation Flanders (FWO) [G0422-10]; Synthesis project - EU-Research Infrastructure Action under the FP7 "Capacities" Specific Program [SE-TAF-2732]	KU Leuven Research Fund(KU Leuven); Research Foundation Flanders (FWO)(FWO); Synthesis project - EU-Research Infrastructure Action under the FP7 "Capacities" Specific Program	This manuscript benefited significantly from constructive reviews by two anonymous reviewers and by Sev Kender and two anonymous reviewers on an earlier version of this manuscript. Financial support was provided by the KU Leuven Research Fund and the Research Foundation Flanders (FWO) grant G0422-10 to RPS, PC and ES. PC thanks the Hercules Foundation Flanders for the upgrade of the VUB Stable Isotope laboratory. This work benefited from Synthesis project SE-TAF-2732 to PS, which was financed by the EU-Research Infrastructure Action under the FP7 "Capacities" Specific Program.	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Micropaleontol.	MAR	2015	115						59	71		10.1016/j.marmicro.2014.11.003	http://dx.doi.org/10.1016/j.marmicro.2014.11.003			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	CF7PU					2025-03-11	WOS:000352749600004
J	Moore, SK; Bill, BD; Hay, LR; Emenegger, J; Eldred, KC; Greengrove, CL; Masura, JE; Anderson, DM				Moore, Stephanie K.; Bill, Brian D.; Hay, Levi R.; Emenegger, Jennifer; Eldred, Kiara C.; Greengrove, Cheryl L.; Masura, Julie E.; Anderson, Donald M.			Factors regulating excystment of <i>Alexandrium</i> in Puget Sound, WA, USA	HARMFUL ALGAE			English	Article						Alexandrium; Puget Sound; Excystment; Cysts; Harmful algal bloom; Red tide	RESTING CYSTS; TAMARENSE; DINOPHYCEAE; GERMINATION; CATENELLA; TEMPERATURE; WASHINGTON; DORMANCY; DARKNESS; BLOOMS	Factors regulating excystment of a toxic dinoflagellate in the genus Alexandrium were investigated in cysts from Puget Sound, Washington State, USA. Experiments were carried out in the laboratory using cysts collected from benthic seedbeds to determine if excystment is controlled by internal or environmental factors. The results suggest that the timing of germination is not tightly controlled by an endogenous clock, though there is a suggestion of a cyclical pattern. This was explored using cysts that had been stored under cold (4 degrees C), anoxic conditions in the dark and then incubated for 6 weeks at constant favorable environmental conditions. Excystment occurred during all months of the year, with variable excystment success ranging from 31-90%. When cysts were isolated directly from freshly collected sediments every month and incubated at the in situ bottom water temperature, a seasonal pattern in excystment was observed that was independent of temperature. This pattern may be consistent with secondary dormancy, an externally modulated pattern that prevents excystment during periods that are not favorable for sustained vegetative growth. However, observation over more annual cycles is required and the duration of the mandatory dormancy period of these cysts must be determined before the seasonality of germination can be fully characterized in Alexandrium from Puget Sound. Both temperature and light were found to be important environmental factors regulating excystment, with the highest rates of excystment observed for the warmest temperature treatment (20 degrees C) and in the light. (C) 2015 Elsevier B.V. All rights reserved.	[Moore, Stephanie K.] Univ Corp Atmospher Res, Joint Off Sci Support, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr,NOAA, Seattle, WA 98112 USA; [Bill, Brian D.] NOAA, Environm & Fisheries Sci Div, NW Fisheries Sci Ctr, Natl Marine Fisheries Serv, Seattle, WA 98112 USA; [Hay, Levi R.; Emenegger, Jennifer; Eldred, Kiara C.] Univ Washigton, NW Fisheries Sci Ctr, Natl Marine Fisheries Serv, NOAA, Seattle, WA 98112 USA; [Greengrove, Cheryl L.; Masura, Julie E.] Univ Washington Tacoma, Tacoma, WA 98402 USA; [Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	National Center Atmospheric Research (NCAR) - USA; National Oceanic Atmospheric Admin (NOAA) - USA; National Oceanic Atmospheric Admin (NOAA) - USA; National Oceanic Atmospheric Admin (NOAA) - USA; University of Washington; University of Washington Tacoma; Woods Hole Oceanographic Institution	Moore, SK (通讯作者)，Univ Corp Atmospher Res, Joint Off Sci Support, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr,NOAA, 2725 Montlake Blvd E, Seattle, WA 98112 USA.	stephanie.moore@noaa.gov	Masura, Julie/AAA-6153-2019	Eldred, Kiara/0000-0002-4067-8639	NOAA ECOHAB [NA10NOS4780158]; Woods Hole Oceanographic Institution [NA10NOS4780159]; Washington Sea Grant, University of Washington [NA10OAR4170057, R/OCEH-9]; NOAA ECOHAB through the Woods Hole Center for Oceans and Human Health, National Science Foundation Grant [OCE-1314642]; National Institute of Environmental Health Sciences Grant [1-P01-ES021923-01]; Division Of Ocean Sciences; Directorate For Geosciences [1314642] Funding Source: National Science Foundation	NOAA ECOHAB(National Oceanic Atmospheric Admin (NOAA) - USA); Woods Hole Oceanographic Institution; Washington Sea Grant, University of Washington(University of Washington); NOAA ECOHAB through the Woods Hole Center for Oceans and Human Health, National Science Foundation Grant; National Institute of Environmental Health Sciences Grant; Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	The authors thank the Captain and crew of the R/V Clifford A. Barnes; D. Kulis, B. Keafer and J. Kleindinst at Woods Hole Oceanographic Institution; V. Trainer at the National Oceanic and Atmospheric Administration (NOAA) Northwest Fisheries Science Center; and K. Rickerson from the Sound Toxins program. This research was supported in part by NOAA ECOHAB funding to the NOAA Northwest Fisheries Science Center, University of Washington (NA10NOS4780158) and Woods Hole Oceanographic Institution (NA10NOS4780159); and a grant from Washington Sea Grant, University of Washington, pursuant to NOAA Award No. NA10OAR4170057, Project R/OCEH-9, to the University of Washington, Tacoma. The views expressed herein are those of the authors and do not necessarily reflect the views of NOAA or any of its sub-agencies. Support for D. M. Anderson was provided by NOAA ECOHAB through the Woods Hole Center for Oceans and Human Health, National Science Foundation Grant OCE-1314642 and National Institute of Environmental Health Sciences Grant 1-P01-ES021923-01. This is ECOHAB contribution number 793.[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, 2006, LIMNOL OCEANOGR, V51, P860, DOI 10.4319/lo.2006.51.2.0860; 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, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; Anglès S, 2012, HARMFUL ALGAE, V16, P20, DOI 10.1016/j.hal.2011.12.008; Anglès S, 2012, HARMFUL ALGAE, V16, P1, DOI 10.1016/j.hal.2011.12.006; [Anonymous], CAN TECH REP FISH AQ; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; [Anonymous], ALGAL TOXINS SEAFOOD; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; County King, 2014, QUATERMASTER H UNPUB; CRAIB J. 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B., 1969, Bulletin Fisheries Research Board of Canada, VNo. 168, P1; Rathaille AN, 2011, HARMFUL ALGAE, V10, P629, DOI 10.1016/j.hal.2011.04.015; Tobin ED, 2011, HARMFUL ALGAE, V10, P216, DOI 10.1016/j.hal.2010.10.002; Trainer VL, 2003, J SHELLFISH RES, V22, P213; Vancouver G., 1798, VOYAGE DISCOVERY N P, V2, P260; Vleeshouwers LM, 1995, J ECOL, V83, P1031, DOI 10.2307/2261184; Wang L, 2014, HARMFUL ALGAE, V31, P100, DOI 10.1016/j.hal.2013.10.013; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	40	26	31	2	37	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	MAR	2015	43						103	110		10.1016/j.hal.2015.01.005	http://dx.doi.org/10.1016/j.hal.2015.01.005			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	CE6SQ	26109923	Green Accepted			2025-03-11	WOS:000351968900010
J	Neves, RAF; Figueiredo, GM; Valentin, JL; Scardua, PMD; Hégaret, H				Neves, Raquel A. F.; Figueiredo, Gisela M.; Valentin, Jean Louis; da Silva Scardua, Patricia Mirella; Hegaret, Helene			Immunological and physiological responses of the periwinkle <i>Littorina littorea</i> during and after exposure to the toxic dinoflagellate <i>Alexandrium minutum</i>	AQUATIC TOXICOLOGY			English	Article						Harmful algal bloom (HAB); Alexandrium; Toxin accumulation; Hemocytes; Histopathology; Gastropod	PARALYTIC SHELLFISH TOXINS; FLOW-CYTOMETRIC ANALYSIS; SCALLOP CHLAMYS-NOBILIS; CRASSOSTREA-VIRGINICA; EASTERN OYSTERS; IMMUNE-RESPONSE; HEMOCYTES; GASTROPODA; BIOTRANSFORMATION; HISTOPATHOLOGY	Species of the dinoflagellate genus Alexandrium produce phycotoxins responsible for paralytic shellfish poisoning. Blooms of Alexandrium minutum reach very high concentrations of vegetative cells in the water column; and when these blooms occur, large numbers of toxic cysts can be produced and deposited on sediments becoming available to benthic species. The present study investigated the potential effect of exposure to toxic cysts of A. minutum on the periwinkle Littorina littorea. Snails were exposed for nine days to pellicle cysts of toxic and non-toxic dinoflagellates, A. minutum and Heterocapsa triquetra, respectively, followed by six days of depuration while they were fed only H. triquetra. Toxin accumulation, condition index, immune and histopathological responses were analyzed. Histological alterations were also monitored in snails exposed to a harmful A. minutum bloom, which naturally occurred in the Bay of Brest. Snails exposed to toxic cysts showed abnormal behavior that seems to be toxin-induced and possibly related to muscle paralysis. Periwinkles accumulated toxins by preying on toxic cysts and accumulation appeared dependent on the time of exposure, increasing during intoxication period but tending to stabilize during depuration period. Toxic exposure also seemed to negatively affect hemocyte viability and functions, as ROS production and phagocytosis. Histological analyses revealed that toxic exposure induced damages on digestive organs of snails, both in laboratory and natural systems. This study demonstrates that an exposure to the toxic dinoflagellate A. minutum leads to sublethal effects on L. littorea, which may alter individual fitness and increase the susceptibility of snails to pathogens and diseases. (C) 2015 Elsevier B.V. All rights reserved.	[Neves, Raquel A. F.; Valentin, Jean Louis] Univ Fed Rio de Janeiro, Inst Biol, Dept Ecol, Programa Posgrad Ecol, Rio De Janeiro, Brazil; [Figueiredo, Gisela M.] Univ Fed Rio de Janeiro, Inst Biol, Dept Biol Marinha, Lab Ecol Trof, Rio De Janeiro, Brazil; [Valentin, Jean Louis] Univ Fed Rio de Janeiro, Inst Biol, Dept Biol Marinha, Lab Zooplancton Marinho, Rio De Janeiro, Brazil; [da Silva Scardua, Patricia Mirella] Univ Fed Paraiba, Ctr Ciencias Exatas & Nat, Dept Biol Mol, Lab Imunol & Patol Invertebrados, BR-58059900 Joao Pessoa, Paraiba, Brazil; [Hegaret, Helene] Inst Univ Europeen Mer, Lab Sci Environm Marin, UMR CNRS UBO IRD IFREMER 6539, F-29280 Plouzane, France; [Hegaret, Helene] GDR 3569 PHYCOTOX, Microalgues Risques Homme & Ecosyst, F-29280 Plouzane, France	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal da Paraiba; Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM)	Neves, RAF (通讯作者)，Univ Fed Estado Rio de Janeiro, Dept Ecol & Recursos Marinhos, Ave Pasteur,458 Sala 314-B Urca, BR-22290240 Rio De Janeiro, Brazil.	neves.raf@hotmail.com; gmandali@biologia.ufrj.br; jlv@biologia.ufrj.br; mirella_dasilva@hotmail.com; helene.hegaret@univ-brest.fr	VALENTIN, JEAN/I-9403-2012; Neves, Raquel/D-5128-2015; da Silva, Patricia/A-5115-2018; Figueiredo, Gisela/G-9280-2015; Hegaret, Helene/B-7206-2008	Figueiredo, Gisela/0000-0002-0842-2289; Hegaret, Helene/0000-0003-4639-9013; da Silva, Patricia Mirella/0000-0001-9687-0235	Brazilian Capes fellowship [BEX 17644/12-7]; FAPERJ; CNPq (PELD-Guanabara); Bilateral Cooperation CNPq/CNRS [24712, 490559/2010-7]	Brazilian Capes fellowship; FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); CNPq (PELD-Guanabara)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)); Bilateral Cooperation CNPq/CNRS	The authors are grateful to Malwenn Lassudrie and Marc Long for their help during the experiment, to Christophe Lambert and Nelly Le Goic for assistance with sample preparation, and to Janet Reid for English revision. We thank IFREMER Pelagos for providing information regarding A. minutum densities during the natural bloom. R.A.F Neves was supported by the Brazilian Capes fellowship No. BEX 17644/12-7 and partially supported by grants from FAPERJ and CNPq (PELD-Guanabara). P.M. da Silva was supported by the Bilateral Cooperation CNPq/CNRS (research project nos. 24712 and 490559/2010-7).	[Anonymous], 1998, PHYSL ECOLOGY HARMFU; Auffret Michel, 1995, Fish Immunology Technical Communications, V4, P55; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Bricelj VM, 2012, HARMFUL ALGAE, V16, P27, DOI 10.1016/j.hal.2012.01.001; Bricelj VM, 2011, MAR ECOL PROG SER, V430, P35, DOI 10.3354/meps09111; Bricelj V. 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Toxicol.	MAR	2015	160						96	105		10.1016/j.aquatox.2015.01.010	http://dx.doi.org/10.1016/j.aquatox.2015.01.010			10	Marine & Freshwater Biology; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Toxicology	CD2WZ	25621399				2025-03-11	WOS:000350941000010
J	Green, L; Fong, P				Green, Lauri; Fong, Peggy			A small-scale test of the species-energy hypothesis in a southern California estuary	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						Diversity; Infauna; Macroalgae; Microphytobenthos; Productivity; Species-energy hypothesis	GREEN ALGAL MATS; SALT-MARSH; NUTRIENT ENRICHMENT; ENTEROMORPHA-INTESTINALIS; COMPLEX INTERACTIONS; COMMUNITY RESPONSES; MACROALGAL DETRITUS; TEMPORAL-CHANGES; COASTAL WATERS; DIVERSITY	Theoretical predictions of a direct positive association between productivity and diversity (P/D) have received considerable empirical support in marine systems, although this relationship tends to break down at smaller scales (<25 km). Another theory commonly advanced in terrestrial systems, the species-energy hypothesis (SEH), relates productivity (=energy) to diversity indirectly through an increase in population abundances, which then reduces the likelihood of localized extinction and therefore enhances richness. The SEH has been supported on both global and local scales but has not been experimentally tested in estuarine systems or at the scale of a patch. We tested whether the predictions of the SEH (increased abundance and diversity) or the P/D hypothesis (increased diversity, no predictions for abundance) described the relationship between macroalgal productivity and the abundance and diversity of infauna and site-attached epifauna (hereafter macrofauna) and the microphytobenthos (MPB) in an estuarine benthic community. We conducted a single-factor experiment comparing the effects over time of three treatments comprised of two levels of macroalgae as an added energy source and a plastic mimic as a control that provided structure and habitat but no energy. Contrary to predictions of both the SEH and the P/D hypothesis, there were no measurable differences in taxonomic richness among treatments. However, in partial support of the SEH, we found that total macrofaunal abundance was 50% higher in both macroalgal treatments compared to the mimic and these were largely comprised of detritivores such as spionid polychaetes and oligochaetes. Phaeopigments increased in macroalgal plots but not the mimic, suggesting that added productivity decomposed, supplying more food for detritivores. As this taxonomic group is present in all plots, although in differing abundances, increasing energy flow through this pathway did not enhance taxonomic richness. Macroalgae stimulated the MPB (measured as chl a) more than did the mimic, and elevated chl b in macroalgal treatments indicated the increase was due to sporeling green macroalgae. However, benthic diatoms and dinoflagellates (estimated from chl c) were not affected by treatment. Thus, we found that at the patch level, neither the SEH nor the P/D hypothesis predicted patterns of diversity for estuarine macrofauna; rather, in this system, increased productivity simply supported higher abundances within the same taxonomic groups that occurred at all productivity levels. (C) 2015 Elsevier B.V. All rights reserved.	[Green, Lauri; Fong, Peggy] Univ Calif Los Angeles, Los Angeles, CA 90095 USA	University of California System; University of California Los Angeles	Green, L (通讯作者)，US EPA, 2030 SE Marine Sci Dr, Newport, OR 97365 USA.	ruiz-green.lauri@epa.gov; pfong@biology.ucla.edu		Green, Lauri/0000-0001-9179-1749	Vavra Research; UCLA Department of Ecology and Evolutionary Biology Funds	Vavra Research; UCLA Department of Ecology and Evolutionary Biology Funds	We acknowledge the lives of the organisms that were lost during the course of this research. We thank the US Navy for use of the Mugu Lagoon study site and Martin Ruane at the Naval Base Ventura County for his help and support on this project. Maria Lopez was instrumental in her tireless efforts in the processing of macrofaunal samples. We also thank Christina Phung for analyzing sediment chlorophyll samples and assisting in the field. Field support was contributed by Sarah Bryson, Sarah Hogan, Tonya Kane, Cameron Pospisi, and Claudia Ruiz-Green. This manuscript was improved due to the helpful comments of Richard Ambrose, Daniel Blumstein, Rachel Kennison, and two helpful reviewers. Financial support came from the Vavra Research and UCLA Department of Ecology and Evolutionary Biology Funds awarded to L Green. 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Exp. Mar. Biol. Ecol.	MAR	2015	464						35	43		10.1016/j.jembe.2014.12.012	http://dx.doi.org/10.1016/j.jembe.2014.12.012			9	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	CB6IK					2025-03-11	WOS:000349730500005
J	Koutsodendris, A; Brauer, A; Zacharias, I; Putyrskaya, V; Klemt, E; Sangiorgi, F; Pross, J				Koutsodendris, Andreas; Brauer, Achim; Zacharias, Ierotheos; Putyrskaya, Victoria; Klemt, Eckehard; Sangiorgi, Francesca; Pross, Joerg			Ecosystem response to human- and climate-induced environmental stress on an anoxic coastal lagoon (Etoliko, Greece) since 1930 AD	JOURNAL OF PALEOLIMNOLOGY			English	Article						Varve microfacies; Palynomorphs; mu-XRF scanning; Human impact; North Atlantic Oscillation; Eastern Mediterranean	DINOFLAGELLATE CYSTS; EUTROPHICATION; PHYTOPLANKTON; ASSEMBLAGES; MARINE; IMPACT; RECORD; REGION; BASIN; SEA	To better constrain the effects of anthropogenic impact on coastal wetlands with respect to natural variability, we here analyze annually laminated sediments from Etoliko lagoon (western Greece, Mediterranean Sea) spanning the last 80 years. Sub-decadal-scale palynomorph (pollen and dinoflagellate cyst) and seasonal-scale palynomorph (microfacies and mu-XRF) analyses were carried out to investigate the evolution of the aquatic environment and the surrounding terrestrial ecosystem. Based on a robust age model, which was developed using varve counting and Cs-137 dating, our results indicate that land-use changes have altered the vegetation dynamics and led to eutrophication of the aquatic environment particularly from the early 1980s onwards. In agreement with instrumental data and reports of fish mass mortality events, our varve composition and high-resolution element scanning data suggest that the ecosystem has been under unprecedented pressure since 1990 AD. In particular, the enhancement of anoxic conditions due to human-induced eutrophication is linked to high accumulation rates of organic matter, an increased presence of bacteria in sediment microfacies, and a decrease in the Fe/Mn ratio in the sediment. In addition, a change in varve type from calcite- to aragonite-dominated in 1983 and a higher Sr concentration during the 1990s indicate an increasingly saline aquatic environment. Comparison with meteorological data suggests that lower precipitation during a persistent positive North Atlantic Oscillation mode along with a gradual increase in mean summer temperature since the 1980s may have enhanced the saline conditions. These findings demonstrate that climate change can intensify the human impact on aquatic ecosystems. In conclusion, our analytical approach provides a valuable tool for evaluating the degree of degradation of Etoliko lagoon and the effectiveness of implemented management plans on the aquatic ecosystem, indicating that the efforts to restore its water circulation have only weakly contributed towards an environmental recovery.	[Koutsodendris, Andreas; Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, D-69120 Heidelberg, Germany; [Brauer, Achim] German Res Ctr Geosci, Sect Climate Dynam & Landscape Evolut 5 2, D-14473 Potsdam, Germany; [Zacharias, Ierotheos] Univ Patras, Dept Environm & Nat Resources Management, Agrinion 30100, Greece; [Putyrskaya, Victoria; Klemt, Eckehard] Univ Appl Sci, Hsch Ravensburg Weingarten, D-88250 Weingarten, Germany; [Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, Fac Geosci, NL-3548 CD Utrecht, Netherlands	Ruprecht Karls University Heidelberg; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; University of Patras; Utrecht University	Koutsodendris, A (通讯作者)，Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, Neuenheimer Feld 234, D-69120 Heidelberg, Germany.	Andreas.Koutsodendris@geow.uni-heidelberg.de	Zacharias, Ierotheos/R-9672-2017; Koutsodendris, Andreas/G-8966-2013	Zacharias, Ierotheos/0000-0001-8410-6862; Brauer, Achim/0000-0002-6655-9451; Sangiorgi, Francesca/0000-0003-4233-6154; Koutsodendris, Andreas/0000-0003-4236-7508				Albanakis K, 1995, P 4 PANH GEOGR C ATH, P27; Appleby PG, 2002, DEV PALEOENVIRON RES, V1, P171; Ariztegui D, 2010, GLOBAL PLANET CHANGE, V71, P183, DOI 10.1016/j.gloplacha.2009.11.016; Avramidis P, 2015, ENVIRON EARTH SCI, V73, P5687, DOI 10.1007/s12665-014-3824-2; Avramidis P, 2013, ENVIRON EARTH SCI, V70, P383, DOI 10.1007/s12665-012-2134-9; BACHHUBER H, 1982, NUCL TECHNOL, V59, P291, DOI 10.13182/NT82-A33032; Barbier EB, 2011, ECOL MONOGR, V81, P169, DOI 10.1890/10-1510.1; Brauer A.H., 2004, The Climate in Historical Times. 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Paleolimn.	MAR	2015	53	3					255	270		10.1007/s10933-014-9823-1	http://dx.doi.org/10.1007/s10933-014-9823-1			16	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	CB9SA					2025-03-11	WOS:000349971500001
J	Colpaert, W; Bosselaers, M; Lambert, O				Colpaert, Wouter; Bosselaers, Mark; Lambert, Olivier			Out of the Pacific: A second fossil porpoise from the Pliocene of the North Sea Basin	ACTA PALAEONTOLOGICA POLONICA			English	Editorial Material						Mammalia; Cetacea; Odontoceti; Phocoenidae; Pliocene; North Sea Basin; Belgium	DINOFLAGELLATE CYST STRATIGRAPHY; PHYLOGENETIC-RELATIONSHIPS; UPPER MIOCENE; CETACEA; ODONTOCETI; JAPAN; DELPHINOIDEA; PHOCOENIDAE; HOKKAIDO; MAMMALIA	Although modern porpoises (Phocoenidae, Odontoceti, Cetacea) occupy most oceanic regions of the world, their fossil record outside the Pacific Ocean remains extremely scarce. Based on a partial skull from lower Pliocene layers (Kattendijk Formation, Zanclean, 5-4.4 Ma) of the Antwerp harbour, a new genus and species of fossil phocoenid, Brabocetus gigaseorum gen. et sp. nov., is described. The new taxon is diagnosed by a unique combination of characters including an anterolateraly widely-open antorbital notch, the anteromedial sulcus being shorter than the posteromedial sulcus, the frontal boss being longer than wide, pronounced asymmetry of the vertex, and the possible presence of an additional longitudinal sulcus across the premaxillary eminence. The phylogenetic analysis indicates that B. gigaseorum is not closely related to extant phocoenids; it is included in a clade comprising most north-west Pacific fossil species, two north-east Pacific fossil species, and the only previously described North Sea fossil species Septemtriocetus bosselaersi. Considering the paleobiogeographic distribution of phocoenids, an early Pliocene arrival from the North Pacific to the North Sea may be correlated to the early opening of the Bering Strait and migration via the Arctic. The presence of S. bosselaersi in younger deposits (Piacenzian) of the southern margin of the North Sea Basin could be the result of either a second dispersal event, or of local speciation in the North Sea, whereas an additional trans-Arctic migration from the North Pacific lead to the present occupation of the North Atlantic and North Sea by the phylogenetically distantly related harbor porpoise Phocoena phocoena.	[Colpaert, Wouter] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Bosselaers, Mark; Lambert, Olivier] Inst Royal Sci Nat Belgique, DO Terre & Hist Vie, B-1000 Brussels, Belgium	Ghent University	Lambert, O (通讯作者)，Inst Royal Sci Nat Belgique, DO Terre & Hist Vie, Rue Vautier 29, B-1000 Brussels, Belgium.	wouterjcolpaert@gmail.com; mark.bosselaers@telenet.be; olivier.lambert@naturalsciences.be	Lambert, Olivier/AEN-2469-2022	Lambert, Olivier/0000-0003-0740-5791				[Anonymous], 2011, MESQUITE MODULAR SYS; Barnes L.G., 1984, PaleoBios, V42, P1; Barnes Lawrence G., 2008, Natural History Museum of Los Angeles County Science Series, P99; BARNES LG, 1985, MAR MAMMAL SCI, V1, P149, DOI 10.1111/j.1748-7692.1985.tb00003.x; Bianucci G., 2009, International Conference on Vertebrate Palaeobiogeography and Continental Bridges across Tethys, Mesogea, and Mediterranean Sea, P9; Bianucci G, 2002, GEOBIOS-LYON, V35, P19, DOI 10.1016/S0016-6995(02)00045-1; Bianucci G, 2013, J VERTEBR PALEONTOL, V33, P722, DOI 10.1080/02724634.2013.744757; Bianucci G, 2011, GEOBIOS-LYON, V44, P549, DOI 10.1016/j.geobios.2011.02.009; Bianucci Giovanni, 1996, Palaeontographia Italica, V83, P73; Boessenecker RW, 2013, GEODIVERSITAS, V35, P815, DOI 10.5252/g2013n4a5; Brisson M.J., 1762, QUADRUPEDUM SCILICET; de Muizon C, 2002, ZOOL J LINN SOC-LOND, V134, P423, DOI 10.1046/j.1096-3642.2002.00015.x; de Muizon C., 1985, Travaux de l'Institut Francais d'Etudes Andines, V27, P1; de Muizon C., 1988, Annales de Paleontologie, V74, P159; De Schepper S, 2009, GEOL MAG, V146, P92, DOI 10.1017/S0016756808005438; Deméré TA, 2003, B AM MUS NAT HIST, P32, DOI 10.1206/0003-0090(2003)279<0032:C>2.0.CO;2; Fajardo-Mellor L, 2006, MAR MAMMAL SCI, V22, P910, DOI 10.1111/j.1748-7692.2006.00080.x; FLOWER W.H., 1867, The Transactions of the Zoological Society of London, V6, P87, DOI DOI 10.1111/J.1096-3642.1867.TB00572.X; Fordyce R.E., 2001, Secondary Adaptation of Tetrapods to Life in Water, P169; FRASER F. 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J	Prauss, ML				Prauss, M. L.			Marine palynology of the Oceanic Anoxic Event 3 (OAE3, Coniacian - Santonian) at Tarfaya, Morocco, NW Africa - transition from preservation to production controlled accumulation of marine organic carbon	CRETACEOUS RESEARCH			English	Article						OAE3; Palynology; Dinocysts; Coniacian; Santonian; Tarfaya; NW Africa	BLACK-SHALE DEPOSITION; EASTERN TROPICAL ATLANTIC; DINOFLAGELLATE CYSTS; BOUNDARY EVENT; PALEOENVIRONMENTAL ANALYSIS; CLIMATE VARIABILITY; IVORY-COAST; SEDIMENTS; BURIAL; STRATIFICATION	The paper presented is the first comprehensive, fully quantitative, high resolution study of marine palynology from an OAE3 black-shale environment. It is based on 175 m core spanning the upper Turonian to lower Santonian at Tarfaya, Morocco, NW Africa, which has been sampled from centimetre to 3 m intervals. The results are integrated and discussed with lithology and geochemistry data to (I) distinguish between potential changes in production and preservation of total organic carbon (TOC) accumulation and (2) constrain the stratigraphic position of the Oceanic Anoxic Event 3 (OAE3). The succession is characterized by increased total organic carbon (TOC), varying between 1% and 19% (average about 6%). Distinct black-shale horizons of variable thickness appear episodically throughout the succession, with higher frequency in the late Turonian. Higher TOC contents do not strictly correlate to lithologic black-shales or peaks of a specific taxon of organic-walled algae. The palynomorph spectrum is strongly dominated by organic-walled algae, with the ratio of terrigenous sporomorphs to organic-walled algae (t/m index) varying between zero and 0.05 (average 0.01). The dominance of algal organic matter is corroborated by the prevalence of Type I kerogen identified using Rock-Eval pyrolysis. Dinocyst diversity is low, with the absolute taxa number varying from 7 to 27 between single samples. The peridinioid/gonyaulacoid ratio of dinocysts (p/g ratio) shows strong fluctuations, varying between 1 and 283 (average of about 100). The upper Turonian interval is dominated by Bosedinia spp., a dinocyst taxon formerly described as abundant only in lacustrine sediments from the Oligocene and Miocene of SE Asia. This dominance is episodically modified by the increase of the warm-temperate waters dinocysts fraction, here mainly represented by the genera Alterbidinium, Isabelidinium and Spinidinium. Within the Coniacian-Santonian, black-shale horizons are limited in number and are concentrated within the upper Coniacian to lower Santonian interval. The dinocysts show alternating, prominent peak abundances of Palaeohystrichophora spp. and the warm-temperate water dinocysts fraction, here mainly represented by the genera Trithyrodinium and Chatangiella. However, a final episode of increased proportions of Bosedinia spp. is confined to a 5 m thick black-shale horizon closely spanning the Coniacian-Santonian boundary. Changes in the ratio of total sulphur to total organic carbon (TS/TOC) reflect fluctuating oxygen contents of bottom waters throughout the late Turonian to Santonian. These are significantly parallelled by the alternation of dinocysts assemblages suggestive of enhanced upwelling and water column stratification respectively, probably reflecting changes in the mode of TOC accumulation. Accordingly, preservation largely prevails during the late Turonian interval and changes towards increased production within the Coniacian-Santonian. However, a final preservation-event is probably represented by the black-shale horizon closely spanning the Coniacian-Santonian boundary (top Dicarinella concavata foraminifera zone), which may reflect an episodic shutdown of a major upwelling cell. It is thus proposed, that the "culmination" of the OAE3 at Tarfaya may represent intermittent preservation of TOC within an otherwise high productivity environment related to a global cooling trend. (C) 2014 Elsevier Ltd. All rights reserved.	Freie Univ, Inst Geosci, Sect Paleontol, D-12249 Berlin, Germany	Free University of Berlin	Prauss, ML (通讯作者)，Freie Univ, Inst Geosci, Sect Paleontol, Malteser Str 74-100, D-12249 Berlin, Germany.	mprauss@zedatfu-berlin.de			Deutsche Forschungsgemeinschaft, DFG [KE 322/39-2]	Deutsche Forschungsgemeinschaft, DFG(German Research Foundation (DFG))	Sample material was provided by Wolfgang Kuhnt, lithology and biostratigraphy by Mohamed Aquit and Ann Holbourn, all Christian Albrechts University, Kiel, Germany. Language improvement of the paper has been kindly supported by Ryan Pereira, University New Castle, United Kingdom. The project has been supported by a research grant from the Deutsche Forschungsgemeinschaft, DFG, grant number KE 322/39-2.	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J	Al-Ameri, TK; Al-Nagshbandi, SF				Al-Ameri, Thamer K.; Al-Nagshbandi, Srood F.			Age assessments and palynofacies of the Jurassic oil source rocks succession of North Iraq	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						North Iraq; Palynomorphs; Age; Palynofacies; Source rocks; Jurassic Formations	HYDROCARBONS; KEROGENS	Palynomorps of mainly dinoflagellate cysts are used in this study to assess age of Middle Jurassic (Bajocian-Bathonian) Sargelu, Upper Jurassic (Upper Callovian-Lower Oxfordian) Naokelekan, Upper Jurassic (Kimeridgian and Oxfordian) Gotnia and Barsarine, and Upper Jurassic-Lower Cretaceous (Beriassian-Tithonian) Chia Gara source rock Formations. Materials used for this palynological study are 85 core and cutting samples of five oil exploratory wells of Bj-1, Tk-3, Aj-8, K-109 and Tq-1 of selected North Iraqi oil fields. Palynofacies assessments are performed for this studied succession by ternary kerogen plots of the phytoclast, amorphous organic matters and palynomorphs. Accordingly, Chia Gara and Sargelu Formations are both deposited in distal suboxic to anoxic basin and can be correlated with kerogens classified microscopically as Type A and Type B, which comprised principally brazinophyte algae, dinoflagellate cysts, spores, pollen, foraminifera test linings and phytoclasts that could indicate affect of upwelling current. These deposits 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 of 2.7-3.0 for the Chia Gara Formation and 2.9-3.1 for the Sargelu Formation.	[Al-Ameri, Thamer K.] Univ Baghdad, Dept Geol, Coll Sci, Jadiriyah, Iraq; [Al-Nagshbandi, Srood F.] Univ Salahuddin, Dept Geol, Coll Sci, Erbil, Iraq	University of Baghdad	Al-Nagshbandi, SF (通讯作者)，Univ Salahuddin, Dept Geol, Coll Sci, Erbil, Iraq.	thamer_alameri@yahoo.com; geothamer@scbaghdad.com						Al-Ameri TK, 2011, J PETROL GEOL, V34, P199, DOI 10.1111/j.1747-5457.2011.00501.x; Al-Ameri TK, 1999, CRETACEOUS RES, V20, P359, DOI 10.1006/cres.1999.0157; Al-Ameri TK, 2006, P AAPG C HOUST TEX; Al-Haba Yahya Kasim, 1989, GEOCHEMICAL STUDIES, V15; Alsharhan AS., 1997, Sedimentary Basins and Petroleum Geology of the Middle East, DOI DOI 10.1016/B978-044482465-3/50003-6; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Davey R.J., 1982, GEOL SURV DENMARK, V6, P1; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; Dunnington H.V., 1958, HABITAT OIL AAPG S, P1194, DOI DOI 10.1306/SV18350C49; Espetalie J, 1977, REV I 3, V41, P75; Helby R, 1987, STUDIES AUSTR MESOZO, P1; Hunt JM, 1997, PETROLEUM GEOCHEMIST, P743; Milliod MA, 1974, CONTRIBUTION SERIES, V4; RAHMAN M, 1995, J PETROL GEOL, V18, P91, DOI 10.1111/j.1747-5457.1995.tb00743.x; Riding JB, 1987, PALYNOLOGY, V7, P197; SARJEANT WAS, 1975, CONTRIBUTIONS SERIES, V4, P51; Sharland P.R., 2001, GEO ARABIA SPECIAL P, V2; 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; Thusu B, 1995, J MICROPALAEONTOL, V4, P113; Traverse A, 2008, PALEOPALYNOLOGY, V28, P813; 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 RC, 1959, LEXIQUE STRATIGRAPHQ, VIII; Welte D.H., 1984, PETROLEUM FORMATION; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P817	27	4	4	0	3	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	FEB	2015	8	2					759	771		10.1007/s12517-013-1245-2	http://dx.doi.org/10.1007/s12517-013-1245-2			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CC6PZ					2025-03-11	WOS:000350489900013
J	Rabbani, J; Ghasemi-Nejad, E; Ashori, A; Vahidinia, M				Rabbani, Javad; Ghasemi-Nejad, Ebrahim; Ashori, Alireza; Vahidinia, Mohammad			Quantitative palynostratigraphy and palaeoecology of Tethyan Paleocene-Eocene red beds in north of Zagros sedimentary basin, Iran	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Palynostratigraphy; Paleoecology; Paleocene-Eocene; Red beds; Zagros; Iran	DINOFLAGELLATE CYSTS; PALYNOFACIES; STRATIGRAPHY; BELT	Biostratigraphic and quantitative characteristics of dinocyst assemblages and palynofacies have been used to interpret the paleoecology and sea level changes of Paleocene-Eocene red beds in north of Zagros sedimentary basin, Iran. One hundred forty-eight species and 69 genera of dinoflagellate cysts are recorded from 32 rock samples collected from the 153-m-thick outcrop section. Three dinocyst zones comparable to North Hemisphere midlatitude zonation are established and described. Three palynofacies differentiated-VI: proximal suboxic-anoxic shelf, VIII: distal dysoxic-anoxic shelf, and IX: distal suboxic-anoxic basin-suggest a suboxic-anoxic proximal-distal shelf and distal basin for the strata under investigation. The sequence stratigraphy events have been documented on the basis of palynological asset recorded such as palynofacies, SOM/MP ratio, dinocyst abundance and diversity, peridinioid/gonyaulacoid (P/G) ratio, proximochorate and cavate cysts ratio, and specific inner neritic, outer neritic, and oceanic taxa trends). The record of sea level changes for the Paleocene-Eocene red beds shows a third-order sequence with one sequence boundary (type II). The P/G ratio shows increasing upward trend of paleoproductivity in this sequence.	[Rabbani, Javad; Ashori, Alireza; Vahidinia, Mohammad] Ferdowsi Univ Mashhad, Dept Geol, Fac Sci, Mashhad, Iran; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Dept Geol, Fac Sci, Tehran, Iran	Ferdowsi University Mashhad; University of Tehran	Rabbani, J (通讯作者)，Ferdowsi Univ Mashhad, Dept Geol, Fac Sci, Mashhad, Iran.	javad_rabbani80@yahoo.com	Ghasemi-Nejad, Ebrahim/AAF-6087-2020; Rabbani, Javad/R-9337-2019; Vahidinia, Mohammad/AAB-7110-2020; Ashori, Alireza/AAC-8198-2022	Rabbani, Javad/0000-0001-9026-0831; Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068; Ashori, Alireza/0000-0003-0946-1965				ALAVI M, 1994, TECTONOPHYSICS, V229, P211, DOI 10.1016/0040-1951(94)90030-2; Alavi M, 2004, AM J SCI, V304, P1, DOI 10.2475/ajs.304.1.1; Carvalho MD, 2006, SEDIMENT GEOL, V192, P57, DOI 10.1016/j.sedgeo.2006.03.017; Egger Hans, 2003, Geological Society of America Special Paper, V369, P133; Ghasemi-Nejad E, 2001, IRANIAN INT J SCI, V2; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Hardenbol J., 1998, SEPM SPECIAL PUBLICA; Jaramillo CA, 1999, PALAEOGEOGR PALAEOCL, V145, P259, DOI 10.1016/S0031-0182(98)00126-6; Radi T, 2007, AM GEOPH UN FALL M; Sangiorgi F, 2002, PALAEOGEOGR PALAEOCL, V186, P199, DOI 10.1016/S0031-0182(02)00450-9; Scott RW, 2006, INT S CRET MAJ GEOL; Skupien P, 2008, B GEOSCI, V83, P207, DOI 10.3140/bull.geosci.2008.02.207; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; Tyson R.V., 1993, Applied Micropalaeontology, P153, DOI [10.1007/978-94-017-0763-35, DOI 10.1007/978-94-017-0763-35]; Vallejo C, 2002, CRETACEOUS RES, V23, P845, DOI 10.1006/cres.2002.1028; Ziegler MA., 2001, GEOARABIA, V6, P445, DOI [DOI 10.2113/GEOARABIA0603445, 10.1016/s0302-4598(97)00093-7, DOI 10.1016/S0302-4598(97)00093-7]	16	5	5	0	3	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	FEB	2015	8	2					827	838		10.1007/s12517-013-1164-2	http://dx.doi.org/10.1007/s12517-013-1164-2			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CC6PZ					2025-03-11	WOS:000350489900018
J	Moshirfar, Y; Mahdavi, M; Ghasemi-Nejad, E; Ashouri, A				Moshirfar, Yavar; Mahdavi, Masoumeh; Ghasemi-Nejad, Ebrahim; Ashouri, Alireza			Eocene climatic events recorded in dinoflagellate cyst assemblages from the Kopeh-Dagh Basin, NE Iran; a statistical approach	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						EECO; MECO; Dinocyst assemblages; Kopeh-Dagh Basin; Iran	PALEOCENE; SEAS	To evaluate the climate events of the Eocene, a section of the Khangiran Formation, dated Early-Middle Eocene based on Planktonic foraminifera (P6-P11 zones) was selected in the Kopeh-Dagh Basin of Northeastern Iran and sampled systematically for palynological studies. Statistical notions such as Detrended Correspondence Analyses and Canonical Correspondence Analyses were practiced on the data gathered. Results were plotted and drawn as statistical diagrams for abundance of climate proxy genera and environmental parameters. These suggests a shift from a warm, high-nutrient, low-oxygen environment of inner neritic setting to a relatively colder, less nutrient and high-oxygen outer neritic environment from the Early to the Middle Eocene.	[Moshirfar, Yavar; Ashouri, Alireza] Ferdowsi Univ Mashhad, Dept Geol, Fac Sci, Mashhad, Iran; [Mahdavi, Masoumeh] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Dept Geol, Fac Sci, Tehran, Iran	Ferdowsi University Mashhad; Brock University; University of Tehran	Ghasemi-Nejad, E (通讯作者)，Univ Tehran, Dept Geol, Fac Sci, Tehran, Iran.	eghasemi@khayam.ut.ac.ir	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068; Ashouri, Ali Reza/0000-0002-2913-4913				Afshar-Harb A., 1969, B IRANIAN PETROLEOUM, V37, P86; Aghanabati Ali, 2006, GEOLOGY IRAN; Bijl PK, 2011, PALEOCEANOGRAPHY, V26, DOI 10.1029/2009PA001905; Bijl PK, 2011, LPP CONTRIBUTION SER, V34; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Ghasemi-Nejad E, 1999, KOMMISION SCHWEIZ PA, V119, P69; GUASTI E, 2005, THESIS U BREMEN; HILL MO, 1980, VEGETATIO, V42, P47, DOI 10.1007/BF00048870; Leps J., 2007, Multivariate Analysis of Ecological Data Using CANOCO, VThird, DOI [DOI 10.1017/CBO9780511615146.006, DOI 10.1017/CBO9780511615146]; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; Pearson PN, 2000, NATURE, V413, P481; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; Pross J, 2001, PALAEOGEOGR PALAEOCL, V166, P369, DOI 10.1016/S0031-0182(00)00219-4; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; Salahi A, 2011, THESIS FERDOWSI U MA; Shin HH, 2012, MAR MICROPALEONTOL, V94-95, P72, DOI 10.1016/j.marmicro.2012.06.005; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; Sluijs A, 2009, BIOGEOSCIENCES, V6, P1755, DOI 10.5194/bg-6-1755-2009; Smith RY, 2010, PALAEOGEOGR PALAEOCL, V293, P120, DOI 10.1016/j.palaeo.2010.05.006; Taylor FJR, 1987, BOT MONOGR, V21, P785; TERBRAAK CJF, 1986, ECOLOGY, V67, P1167; Traverse A., 2007, PALEOPALYNOLOGY, V28; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7; Zachos JC, 2010, EARTH PLANET SC LETT, V299, P242, DOI 10.1016/j.epsl.2010.09.004	25	3	3	0	6	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	FEB	2015	8	2					867	876		10.1007/s12517-013-1184-y	http://dx.doi.org/10.1007/s12517-013-1184-y			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CC6PZ					2025-03-11	WOS:000350489900021
J	Li, Z; Han, MS; Matsuoka, K; Kim, SY; Shin, HH				Li, Zhun; Han, Myung Soo; Matsuoka, Kazumi; Kim, So Young; Shin, Hyeon Ho			IDENTIFICATION OF THE RESTING CYST OF <i>COCHLODINIUM POLYKRIKOIDES</i> MARGALEF (DINOPHYCEAE, GYMNODINIALES) IN KOREAN COASTAL SEDIMENTS	JOURNAL OF PHYCOLOGY			English	Article						Cochlodinium polykrikoides; morphology; resting cyst; reticulate ornament; sediment	UNARMORED DINOFLAGELLATE; MORPHOLOGY; MODELS; SEA	This study provides the first morphological features of resting cysts of Cochlodinium polykrikoides collected from Korean coastal sediments. Evidence for the existence of resting cysts of C. polykrikoides is based on the morphological and molecular phylogenetic data of the germinated cells and a resting cyst. The morphology of the resting cysts differed from that reported previously in sediments and culture experiments. The distinct feature is that the cyst body was covered by the reticulate ornaments and spines.	[Li, Zhun; Han, Myung Soo] Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; [Li, Zhun; Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, Geoje 656830, South Korea; [Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, Nagasaki 8512213, Japan; [Kim, So Young] Korea Polar Res Inst, Arctic Res Ctr, Inchon 406840, South Korea	Hanyang University; Korea Institute of Ocean Science & Technology (KIOST); Nagasaki University; Korea Polar Research Institute (KOPRI); Korea Institute of Ocean Science & Technology (KIOST)	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Geoje 656830, South Korea.	shh961121@kiost.ac	LI, ZHUN/GLT-3478-2022; Kim, So-Young/JFS-7698-2023	LI, ZHUN/0000-0001-8961-9966; Shin, Hyeon Ho/0000-0002-9711-6717	Public Welfare & Safety Research Program through the National Research Foundation of Korea (NRF) - Ministry of Science, ICT & Future Planning [PN65760]	Public Welfare & Safety Research Program through the National Research Foundation of Korea (NRF) - Ministry of Science, ICT & Future Planning	This research was supported by the Public Welfare & Safety Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Science, ICT & Future Planning (Development of autonomous microalgal identification system and feasibility analyses of developed HAB control technologies: PN65760).	Darriba D, 2012, NAT METHODS, V9, P772, DOI 10.1038/nmeth.2109; Guindon S, 2010, SYST BIOL, V59, P307, DOI 10.1093/sysbio/syq010; Iwataki M, 2007, PHYCOL RES, V55, P231, DOI 10.1111/j.1440-1835.2007.00466.x; Jeanmougin F, 1998, TRENDS BIOCHEM SCI, V23, P403, DOI 10.1016/S0968-0004(98)01285-7; 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; Kokinos John P., 1995, Palynology, V19, P143; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Matsuoka K, 2008, HARMFUL ALGAE, V7, P261, DOI 10.1016/j.hal.2007.12.002; Matsuoka K, 2010, HARMFUL ALGAE, V9, P548, DOI 10.1016/j.hal.2010.04.003; Matsuoka K, 2009, REV PALAEOBOT PALYNO, V154, P79, DOI 10.1016/j.revpalbo.2008.12.013; Mertens KN, 2009, MAR MICROPALEONTOL, V70, P54, DOI 10.1016/j.marmicro.2008.10.004; Morse RE, 2013, HARMFUL ALGAE, V28, P71, DOI 10.1016/j.hal.2013.05.013; NFRDI, 2012, ANN REP NAT FISH RES; NFRDI, 2014, HARMF ALG BLOOMS KOR; Orlova TY, 2004, BOT MAR, V47, P184, DOI 10.1515/BOT.2004.019; Park J.C., 2007, THESIS CHONNAM NATL; Park TG, 2010, HARMFUL ALGAE, V9, P59, DOI 10.1016/j.hal.2009.08.002; Pospelova V, 2010, MAR MICROPALEONTOL, V76, P37, DOI 10.1016/j.marmicro.2010.04.003; Reñé A, 2013, HARMFUL ALGAE, V25, P39, DOI 10.1016/j.hal.2013.02.004; Richlen ML, 2010, HARMFUL ALGAE, V9, P163, DOI 10.1016/j.hal.2009.08.013; Ronquist F, 2003, BIOINFORMATICS, V19, P1572, DOI 10.1093/bioinformatics/btg180; Sarai C, 2013, REV PALAEOBOT PALYNO, V192, P103, DOI 10.1016/j.revpalbo.2012.12.007; Shin HH, 2013, HARMFUL ALGAE, V28, P37, DOI 10.1016/j.hal.2013.05.011; Takano Y, 2006, J PHYCOL, V42, P251, DOI 10.1111/j.1529-8817.2006.00177.x; Takano Y, 2004, PHYCOL RES, V52, P107, DOI 10.1111/j.1440-183.2004.00332.x; Tang YZ, 2012, HARMFUL ALGAE, V20, P71, DOI 10.1016/j.hal.2012.08.001	28	40	42	2	22	WILEY-BLACKWELL	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	2015	51	1					204	210		10.1111/jpy.12252	http://dx.doi.org/10.1111/jpy.12252			7	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	CB1PU	26986269				2025-03-11	WOS:000349400900016
J	Limoges, A; Mertens, KN; Ruíz-Fernández, AC; de Vernal, A				Limoges, Audrey; Mertens, Kenneth Neil; Carolina Ruiz-Fernandez, Ana; de Vernal, Anne			FIRST REPORT OF FOSSILIZED CYSTS PRODUCED BY THE BENTHIC <i>BYSMATRUM SUBSALSUM</i> (DINOPHYCEAE) FROM A SHALLOW MEXICAN LAGOON IN THE GULF OF MEXICO	JOURNAL OF PHYCOLOGY			English	Article						Alvarado Lagoon; dinosporin; palynology; red tide; resting cyst	NOV DINOPHYCEAE; DINOFLAGELLATE; SCRIPPSIELLA; MORPHOLOGY; ECOLOGY	Cysts belonging to the benthic dinoflagellate Bysmatrum subsalsum were recovered from palynologically treated sediments collected in the Alvarado Lagoon (southwestern Gulf of Mexico). The cysts are proximate, reflecting the features of the parent thecal stage, and their autofluorescence implies a dinosporin composition similar to the cyst walls of phototrophic species. This finding is important for our understanding of B. subsalsum life cycle transitions and ecology. Encystment may play an important role in the bloom dynamics of this species as it can enable the formation of a sediment cyst bank that allows reinoculation of the water column when conditions become favorable. This is the first report of a fossilized cyst produced by a benthic dinoflagellate recovered from sub-recent sediments.	[Limoges, Audrey; de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Carolina Ruiz-Fernandez, Ana] Univ Nacl Autonoma Mexico, Unidad Acad Mazatlan, Inst Ciencias Mar & Limnol, Mazatlan 82000, Mexico	University of Quebec; University of Quebec Montreal; Ghent University; Universidad Nacional Autonoma de Mexico	Limoges, A (通讯作者)，Univ Quebec, Geotop, CP 8888,Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.	limoges.audrey@gmail.com	Mertens, Kenneth/AAO-9566-2020; de Vernal, Anne/D-5602-2013; Ruiz-Fernández, Ana Carolina/ABG-6985-2020; Mertens, Kenneth/C-3386-2015	Limoges, Audrey/0000-0002-4587-3417; Mertens, Kenneth/0000-0003-2005-9483; RUIZ-FERNANDEZ, ANA CAROLINA/0000-0002-2515-1249	 [PAPIIT-DGAPA IN105009]		Mona Hoppenrath, Carmen Zinnsmeister, Maria Faust, and Ojvind Moestrup are acknowledged for help with identification. Special thanks go to Nicolas Van Nieuwenhove for helpful comments. Raynald Lapointe and Maryse Henry are acknowledged for their help with SEM preparation. Support for sampling activities was provided through grant PAPIIT-DGAPA IN105009. The helpful comments by two anonymous reviewers were greatly appreciated.	Anderson D., 2004, Manual on Harmful Marine Microalgae, Monographs on Oceanographic Methodology, VVolume 11, P165; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Bogus K, 2014, J PHYCOL, V50, P254, DOI 10.1111/jpy.12170; Bravo Isabel, 2014, Microorganisms, V2, P11; Bravo I, 2012, HARMFUL ALGAE, V18, P24, DOI 10.1016/j.hal.2012.04.001; Brenner WW, 2001, NEUES JAHRB GEOL P-A, V219, P229, DOI 10.1127/njgpa/219/2001/229; de Vernal A., 1996, Les cahiers du GEOTOP, V3, P16; Faust MA, 1998, PHYCOLOGIA, V37, P47, DOI 10.2216/i0031-8884-37-1-47.1; Faust MA, 1996, J PHYCOL, V32, P669, DOI 10.1111/j.0022-3646.1996.00669.x; FAUST MA, 1992, J PHYCOL, V28, P94; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Gottschling M, 2012, PROTIST, V163, P15, DOI 10.1016/j.protis.2011.06.003; Head M.J., 1996, Palynology: Principles and Applications, P1197; Hoppenrath M, 2013, HARMFUL ALGAE, V27, P1, DOI 10.1016/j.hal.2013.03.006; HORIGUCHI T, 1988, J PHYCOL, V24, P426; HORIGUCHI T, 1983, BOT MAG TOKYO, V96, P351, DOI 10.1007/BF02488179; Jeong Hae Jin, 2012, Ocean Science Journal, V47, P1, DOI 10.1007/s12601-012-0001-y; LESSARD EJ, 1986, J PLANKTON RES, V8, P1209, DOI 10.1093/plankt/8.6.1209; LOMBARD EH, 1971, J PHYCOL, V7, P188, DOI 10.1111/j.1529-8817.1971.tb01500.x; Murray S, 2006, PHYCOLOGIA, V45, P161, DOI 10.2216/05-05.1; Ostenfeld C. H., 1908, WISSENSCHAFTLICHE ER, V8, P123; Satta CT, 2013, HARMFUL ALGAE, V24, P65, DOI 10.1016/j.hal.2013.01.007; Sekida Satoko, 1999, Hikobia, V13, P65; STEIDINGER K A, 1977, Phycologia, V16, P69, DOI 10.2216/i0031-8884-16-1-69.1; Steidinger Karen A., 1996, P387, DOI 10.1016/B978-012693015-3/50006-1; Versteegh GJM, 2012, ORG GEOCHEM, V43, P92, DOI 10.1016/j.orggeochem.2011.10.007	26	13	13	0	11	WILEY-BLACKWELL	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	2015	51	1					211	215		10.1111/jpy.12257	http://dx.doi.org/10.1111/jpy.12257			5	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	CB1PU	26986270				2025-03-11	WOS:000349400900017
J	Konoki, K; Suga, Y; Fuwa, H; Yotsu-Yamashita, M; Sasaki, M				Konoki, Keiichi; Suga, Yuto; Fuwa, Haruhiko; Yotsu-Yamashita, Mari; Sasaki, Makoto			Evaluation of gambierol and its analogs for their inhibition of human K<sub>v</sub>1.2 and cytotoxicity	BIOORGANIC & MEDICINAL CHEMISTRY LETTERS			English	Article						Gambierol; Voltage-gated potassium channels; Cytotoxicity	DINOFLAGELLATE GAMBIERDISCUS-TOXICUS; NONSELECTIVE CATION CHANNEL; POTENT MARINE TOXIN; PARTIAL STEREOCHEMICAL ASSIGNMENTS; GATED POTASSIUM CHANNELS; RED TIDE DINOFLAGELLATE; ALGA PRYMNESIUM-PARVUM; PTYCHODISCUS-BREVIS; SODIUM-CHANNELS; ANTIFUNGAL SUBSTANCES	Gambierol and its heptacyclic and tetracyclic analogs were tested for inhibitory activity against the human voltage-gated potassium channel Kv1.2 (hKv1.2), which was stably expressed in Chinese hamster ovary (CHO) cells. Gambierol, the heptacyclic analog, and the tetracyclic analog inhibited the potassium current evoked by a step pulse from -80 mV to 40 mV. The IC50 values for the three compounds were 0.75 +/- 0.15 nM, 7.6 +/- 1.2 nM, and 28 +/- 4.0 nM (the mean +/- SEM, n = 3), respectively. The cytotoxic activity was examined in order to assess a relationship between cytotoxicity and inhibition of the hKv1.2. The IC50 values for gambierol, the heptacyclic analog, and the tetracyclic analog in the wild-type CHO cells were 95 +/- 7.1 lM, 6.5 +/- 0.8 lM(the mean +/- SEM, n = 3), and > 100 lM (n = 3), respectively, whereas those in the CHO cells stably expressing hKv1.2 were 78 +/- 5.8 lM, 6.0 +/- 1.0 lM (the mean +/- SEM, n = 3), and > 100 lM (n = 3). These results suggested that cytotoxicity is not triggered by inhibition of the human Kv1.2. The electrophysiological recording at the resting potential in the presence of gambierol, the heptacyclic analog, and the tetracyclic analog revealed the dose-dependent leak current, which was largest when the heptacyclic analog was administered to the cells. We thus propose that the leak current induced by these compounds might cause a fatal effect on the cultured cells. (C) 2014 Elsevier Ltd. All rights reserved.	[Konoki, Keiichi; Yotsu-Yamashita, Mari] Tohoku Univ, Grad Sch Agr Sci, Aoba Ku, Sendai, Miyagi 9818555, Japan; [Suga, Yuto; Fuwa, Haruhiko; Sasaki, Makoto] Tohoku Univ, Grad Sch Life Sci, Aoba Ku, Sendai, Miyagi 9808577, Japan	Tohoku University; Tohoku University	Konoki, K (通讯作者)，Tohoku Univ, Grad Sch Agr Sci, Aoba Ku, 1-1 Tsutsumidori Amamiyamachi, Sendai, Miyagi 9818555, Japan.	konoki@m.tohoku.ac.jp; masasaki@m.tohoku.ac.jp	Sasaki, Makoto/AAE-5204-2019; Yotsu-Yamashita, Mari/ABZ-1205-2022; KONOKI, Keiichi/U-2249-2019; Fuwa, Haruhiko/D-1773-2010	Fuwa, Haruhiko/0000-0001-5343-9023; Konoki, Keiichi/0000-0001-5788-5426	ERATO Murata Lipid Active Structure Project; Grants-in-Aid for Scientific Research [26292057, 25282228, 23102015, 26660094, 23102016] Funding Source: KAKEN	ERATO Murata Lipid Active Structure Project; 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))	The research studies were funded by the ERATO Murata Lipid Active Structure Project, Japan Science and Technology Agency, a Grant-in-Aid for Scientific Research on Innovative Areas ` Chemical Biology of Natural Products' from the Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan64 (M. S., and K. K.), and the Japan Society for the Promotion of Science for Funding Program for the Next Generation World-Leading Researchers (LS012) (M. Y. Y.). We thank Takayuki Oka and Masato Nishio of Bio Research Center Co. Ltd and Atsushi Otsuki of Nanion Technologies GmbH for providing technical support for the electrophysiological recording with Port-A-Patch ~. We thank RIKEN Bioresource Center through the National Bio-Resource Project of the MEXT, Japan, for providing the human embryonic kidney cell line 293T (RCB2202) and the Chinese hamster ovary cell line CHO-K1 (RCB0285).	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Med. Chem. Lett.	FEB 1	2015	25	3					514	518		10.1016/j.bmcl.2014.12.022	http://dx.doi.org/10.1016/j.bmcl.2014.12.022			5	Chemistry, Medicinal; Chemistry, Organic	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy; Chemistry	AY9XT	25556093	Bronze			2025-03-11	WOS:000347901700017
J	Olde, K; Jarvis, I; Pearce, M; Ulicny, D; Tocher, B; Trabucho-Alexandre, J; Gröcke, D				Olde, Kate; Jarvis, Ian; Pearce, Martin; Ulicny, David; Tocher, Bruce; Trabucho-Alexandre, Joao; Groecke, Darren			A revised northern European Turonian (Upper Cretaceous) dinoflagellate cyst biostratigraphy: Integrating palynology and carbon isotope events	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palynology; Dinoflagellate cyst; Czech Republic; Chalk; Turonian; Carbon isotope event	SEA-LEVEL CHANGES; SHALLOW-MARINE; BOUNDARY EVENT; ANOXIC EVENT; STRATIGRAPHY; BASIN; DINOCYST; GERMANY; CONIACIAN; CHALK	Organic walled dinoflagellate cyst (dinocyst) assemblage data are presented for a new Turonian regional reference core (Bch-1) drilled at Bechary in the Bohemian Cretaceous Basin, east-central Czech Republic. The detailed stratigraphic framework for the section is summarised based on calcareous nannofossil and macrofossil biostratigraphy, regional e-log correlation, sequence stratigraphy and carbon isotope chemostratigraphy. Dinocyst results obtained for 196 samples from the 405 m long core offer the highest resolution (similar to 22 kyr) stratigraphically well-constrained data set available to date for the Turonian Stage, 93.9-89.8 Ma. A dinocyst biostratigraphic framework is presented based on the evolutionary first and last occurrence, first common occurrence, and acmes of key species. Published dinocyst data from English Turonian Chalk successions in East Sussex, Berkshire, Kent and Norfolk are reviewed within a stratigraphic framework provided by macrofossil records and carbon isotope event (CIE) chemostratigraphy. Critical analysis of existing published Turonian dinocyst zonation schemes shows them to be untenable. Correlation of the English Chalk data to Bch-1 provides a basis for defining a regional dinocyst event stratigraphy with 22 datum levels, and a revised dinocyst zonation scheme constrained within a chemostratigraphic framework of 10 major CIEs. The new zones consist of a Cenomanian Litosphaeridium siphoniphorum Zone, followed by the Cauveridinium membraniphorum Zone spanning the uppermost Cenomanian to Lower Coniacian. This is subdivided into: Senoniasphaera turonica (Lower-mid-Middle Turonian); and Raetiaedinium truncigerum (mid-Middle Turonian-mid-Lower Coniacian) subzones. The Oligosphaeridium pulcherrimum Zone (Senonisphaera rotundata Subzone) characterises the Lower Coniacian. The new stratigraphy offers a basis for improved correlation and dating of Upper Cretaceous successions. (C) 2014 Elsevier B.V. All rights reserved.	[Olde, Kate; Jarvis, Ian] Kingston Univ London, Sch Geog Geol & Environm, Ctr Earth & Environm Sci Res, Kingston Upon Thames KT1 2EE, Surrey, England; [Pearce, Martin] Evolut Appl Ltd, Cheltenham GL54 2PL, Glos, England; [Ulicny, David] Acad Sci Czech Republ, Inst Geophys, CR-14131 Prague, Czech Republic; [Tocher, Bruce] STATOIL, Houston, TX 77042 USA; [Trabucho-Alexandre, Joao; Groecke, Darren] Univ Durham, Dept Earth Sci, Durham DH1 3LE, England; [Trabucho-Alexandre, Joao] Inst Earth Sci Utrecht, NL-3584 CD Utrecht, Netherlands	Kingston University; Czech Academy of Sciences; Institute of Geophysics of the Czech Academy of Sciences; Equinor; Durham University	Jarvis, I (通讯作者)，Kingston Univ London, Sch Geog Geol & Environm, Penrhyn Rd, Kingston Upon Thames KT1 2EE, Surrey, England.	kateolde@gmail.com; i.jarvis@kingston.ac.uk; info@evolutionapplied.com; ulicny@ig.cas.cz; bruce@statoil.com; j.trabucho@uu.nl; d.r.grocke@durham.ac.uk	Alexandre, João/AAT-5878-2020; Uličný, David/H-6412-2014; Grocke, Darren R./F-4799-2015; Jarvis, Ian/A-1637-2008	Trabucho Alexandre, Joao/0000-0003-1997-027X; Pearce, Martin/0000-0001-7856-1076; Grocke, Darren R./0000-0003-2296-7530; Jarvis, Ian/0000-0003-3184-3097; Ulicny, David/0000-0002-0331-4174	Kingston University London PhD studentship; Statoil Petroleum AS [4501936147]; UK Natural Environment Research Council (NERC) [NE/H020756/1, NE/H021868/1]; Academy of Sciences of the Czech Republic [RVO: 67985530]; Czech Science Foundation (GACR) [P210/10/1991]; NERC [NE/H021868/1, NE/H020756/1] Funding Source: UKRI	Kingston University London PhD studentship; Statoil Petroleum AS; UK Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Academy of Sciences of the Czech Republic(Czech Academy of Sciences); Czech Science Foundation (GACR)(Grant Agency of the Czech Republic); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	KO acknowledges receipt of a Kingston University London PhD studentship and support by Statoil Petroleum AS contract 4501936147. IJ and DG were funded by UK Natural Environment Research Council (NERC) grants NE/H020756/1 and NE/H021868/1, respectively. DU acknowledges support from research programme RVO: 67985530 of the Academy of Sciences of the Czech Republic. The Bch-1 coring project was funded by Czech Science Foundation (GACR) grant P210/10/1991 to DU.	[Anonymous], ANN PALEONTOL; Bell DG, 1997, J MICROPALAEONTOL, V16, P30, DOI 10.1144/jm.16.1.30; Bloch J.D., 1999, GEOL SURV CAN BULL, V531, P1; BRIDEAUX WW., 1977, GEOL SURV CAN BULL, V281, P1; BUJAK J P, 1978, Geological Survey of Canada Bulletin, P1; Burnett J.A., 1998, P132; Cech S., 1989, P657; Cech Stanislav, 2005, Bulletin of Geosciences, V80, P321; Clarke R. F. A., 1967, Verb K ned Akad Wet Amst, V24, P1; Costa L. 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Palynology	FEB	2015	213						1	16		10.1016/j.revpalbo.2014.10.006	http://dx.doi.org/10.1016/j.revpalbo.2014.10.006			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	CA8VF		Green Accepted			2025-03-11	WOS:000349198300001
J	Peczula, W; Suchora, M; Zukowska, G				Peczula, Wojciech; Suchora, Magdalena; Zukowska, Grazyna			The influence of glucose and peat extract additions on the spring recruitment of <i>Gonyostomum semen</i> from the sediments	HYDROBIOLOGIA			English	Article						Gonyostomum semen; Dissolved organic carbon; Recruitment; Cyst germination; Lake sediments	DISSOLVED ORGANIC-CARBON; CLIMATE-CHANGE; TOXIC DINOFLAGELLATE; HUMIC SUBSTANCES; MASS DEVELOPMENT; RESTING CYSTS; FOREST LAKES; GERMINATION; GROWTH; PHYTOPLANKTON	The effect of two various forms of DOC on the Gonyostomum semen recruitment from sediments was conducted under experimental laboratory conditions. We tested the hypothesis that DOC is a factor enhancing spring recruitment of the species by exposing sediments from a humic lake with a 17-year bloom history, to three various DOC additions (two solutions of glucose and one solution of a peat extract). Sediments and lake water were incubated for 14 days at 16A degrees C, in 14:10 h light:dark cycle, with germling and adult cell abundance ascertained in the water every third day, and water parameters every seventh day. Our important findings were that (1) Gonyostomum recruitment was uneven and the period of germination was relatively short; (2) all treatments significantly affected germling occurrence; however, sugar-derived DOC seemed to suppress the recruitment, whereas peat extract improved it. Due to the additional phosphorus load in peat treatment (against phosphorus-free sugar treatments), it is likely that it played a major role in the observed differences, however, our results did not exclude the potential role of peat-derived DOC forms. In conclusion, we proposed that Gonyostomum expansion is supported by enhanced recruitment from sediment seed banks related to water chemistry alterations, driven by the climate change.	[Peczula, Wojciech; Suchora, Magdalena] Univ Life Sci Lublin, Dept Hydrobiol, Lublin, Poland; [Zukowska, Grazyna] Univ Life Sci Lublin, Inst Soil Sci Environm Engn & Management, Lublin, Poland	University of Life Sciences in Lublin; University of Life Sciences in Lublin	Peczula, W (通讯作者)，Univ Life Sci Lublin, Dept Hydrobiol, Lublin, Poland.	wojciech.peczula@up.lublin.pl	Suchora, Magdalena/AAI-1229-2019; Peczula, Wojciech/T-6681-2018; Suchora, Magdalena/R-6910-2016; , Grazyna Zukowska/X-1809-2018	Peczula, Wojciech/0000-0002-6760-4189; Suchora, Magdalena/0000-0002-3210-8492; , Grazyna Zukowska/0000-0002-8189-6675				Agrawal SC, 2009, FOLIA MICROBIOL, V54, P273, DOI 10.1007/s12223-009-0047-0; Agrawal SC, 2002, FOLIA MICROBIOL, V47, P527, DOI 10.1007/BF02818793; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2006, LIMNOL OCEANOGR, V51, P860, DOI 10.4319/lo.2006.51.2.0860; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; 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SAKO Y, 1985, B JPN SOC SCI FISH, V51, P267; Schindler DW, 1997, BIOGEOCHEMISTRY, V36, P1, DOI 10.1023/A:1005768527751; SCHINDLER DW, 1992, HYDROBIOLOGIA, V229, P1, DOI 10.1007/BF00006987; Sousa AI, 2007, J EXP MAR BIOL ECOL, V341, P142, DOI 10.1016/j.jembe.2006.09.020; vanDok W, 1997, J PHYCOL, V33, P12; Vollenweider R.A., 1969, A Manual on Methods for Measuring Primary Productivity in Aquatic Environment; Vuorenmaa J, 2006, SCI TOTAL ENVIRON, V365, P47, DOI 10.1016/j.scitotenv.2006.02.038; WETZEL RG, 1992, HYDROBIOLOGIA, V229, P181, DOI 10.1007/BF00007000; Whitehead PG, 2009, HYDROLOG SCI J, V54, P101, DOI 10.1623/hysj.54.1.101; Willén E, 2003, HYDROBIOLOGIA, V502, P315, DOI 10.1023/B:HYDR.0000004289.92343.39; Worrall F, 2004, SCI TOTAL ENVIRON, V326, P95, DOI 10.1016/j.scitotenv.2003.11.022	62	3	4	2	27	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0018-8158	1573-5117		HYDROBIOLOGIA	Hydrobiologia	FEB	2015	744	1					177	186		10.1007/s10750-014-2075-2	http://dx.doi.org/10.1007/s10750-014-2075-2			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	AW3JH		hybrid			2025-03-11	WOS:000346182100013
J	van Helmond, NAGM; Hennekam, R; Donders, TH; Bunnik, FPM; de Lange, GJ; Brinkhuis, H; Sangiorgi, F				van Helmond, Niels A. G. M.; Hennekam, Rick; Donders, Timme H.; Bunnik, Frans P. M.; de Lange, Gert J.; Brinkhuis, Henk; Sangiorgi, Francesca			Marine productivity leads organic matter preservation in sapropel S1: palynological evidence from a core east of the Nile River outflow	QUATERNARY SCIENCE REVIEWS			English	Article						Eastern Mediterranean; Holocene; Sapropel S1; Dinocysts; Pollen and spores; Productivity; Preservation; Nile discharge	WALLED DINOFLAGELLATE CYSTS; HOLOCENE-LATE PLEISTOCENE; MEDITERRANEAN-SEA; LATE QUATERNARY; SURFACE SEDIMENTS; AEGEAN SEA; CARBONATE DIAGENESIS; AFRICAN MONSOON; NORTH-ATLANTIC; POLLEN	The formation of Eastern Mediterranean organic matter rich deposits known as sapropels is the results of two mechanisms: (enhanced) marine productivity and preservation of organic material at depth. However, their relative contribution and their leads and lags with respect to each other remain elusive. Here, we address these questions by studying sediments deposited prior to, during, and after the most recent sapropel (S1, similar to 10-6 calibrated ka before present, BP) with an integrated marine and terrestrial palynological approach, combined with existing and newly generated geochemical data. The studied core was retrieved from an area under strong influence of the Nile outflow and has high average sediment accumulation rates allowing a high temporal resolution (of several decades to centuries). Marine productivity, as reconstructed with total dinocyst accumulation rates (ARs) and biogenic CaCO3 content, starts to increase similar to 1 ka prior to sapropel formation. A shift in the dinocyst taxa contributing to the productivity signal at sapropel onset indicates the rapid development of (seasonal) water column stratification. Pollen and spore ARs also increase prior to sapropel onset, but a few centuries after the increase in marine productivity. Hence, the first shift to a high marine productivity system before sapropel deposition may have been mostly favoured by the injection of nutrients via shoaling of the nutricline with a minor contribution of nutrients from land via river input and flooding of the shelves. Pollen assemblages indicate a gradual change across the sapropel onset from a savanna-like, through coastal marsh expansion, toward an open woodland assemblage, which is consistent with enhanced Nile influence and delta development. At sapropel onset a marked shift in pollen ARs could suggest increased preservation under anoxia. However, major shifts in pollen assemblages and signs of selective- or partial decomposition of terrestrial palynomorphs are absent. We therefore suggest that the high pollen ARs largely result from an increased influx of pollen by enhanced Nile discharge and extension of the freshwater plume. Three centuries after the sapropel onset, dinocyst ARs and CaCO3 content indicate that marine productivity starts to decrease, while sapropel deposition continued. Organic carbon content decreased only later and less dramatically. This may be explained by a shift in the dominance of the organisms contributing to marine productivity, to an enhanced preservation of organic matter, or a combination of both. (C) 2014 Elsevier Ltd. All rights reserved.	[van Helmond, Niels A. G. M.; Brinkhuis, Henk; Sangiorgi, Francesca] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Hennekam, Rick; de Lange, Gert J.] Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Donders, Timme H.; Bunnik, Frans P. M.] Univ Utrecht, Fac Geosci, Dept Phys Geog, NL-3584 CD Utrecht, Netherlands; [Donders, Timme H.; Bunnik, Frans P. M.] TNO, Energy Petroleum Geosci, NL-3584 CB Utrecht, Netherlands; [Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; Utrecht University; Utrecht University; Netherlands Organization Applied Science Research; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	van Helmond, NAGM (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	n.vanhelmond@uu.nl	Brinkhuis, Henk/IUO-8165-2023; Donders, Timme/J-5044-2012; De Lange, Gert/B-9639-2014	Brinkhuis, Henk/0000-0003-0253-6610; De Lange, Gert/0000-0002-9420-3022; van Helmond, Niels/0000-0003-0024-7217; Hennekam, Rick/0000-0002-8823-4519; Sangiorgi, Francesca/0000-0003-4233-6154; Donders, Timme/0000-0003-4698-3463	NWO, PASS2-project; Utrecht University; "Focus & Massa" program grant; PALM-project; Statoil	NWO, PASS2-project; Utrecht University; "Focus & Massa" program grant; PALM-project; Statoil	The sediment samples used for this study were recovered during the PASSAP cruise in May 2000 with the RV Pelagia, which was funded by NWO as a part of the PASS2-project. We thank the captain, crew and scientific participants of that cruise. Jan van Tongeren is thanked for sample processing. The manuscript benefited greatly from the comments and suggestions of three anonymous reviewers. Utrecht University supported this research with a "Focus & Massa" program grant to Henk Brinkhuis and Caroline Slomp. NWO is acknowledged for funding of the PALM-project. Statoil provided additional financial support.	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Sci. Rev.	JAN 15	2015	108						130	138		10.1016/j.quascirev.2014.11.014	http://dx.doi.org/10.1016/j.quascirev.2014.11.014			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	CA5PJ		Green Published			2025-03-11	WOS:000348960000009
J	Aydin, H; Yürür, EE; Uzar, S; Küçüksezgin, F				Aydin, Hilal; Yurur, Emine Erdem; Uzar, Serdar; Kucuksezgin, Filiz			Modern Dinoflagellate Cyst Assemblages of Aliaga and Nemrut Bay: Influence of Industrial Pollution	TURKISH JOURNAL OF FISHERIES AND AQUATIC SCIENCES			English	Article						Resting cyst; heavy metals; sediment; Eastern Mediterranean	HEAVY-METAL POLLUTION; SURFACE SEDIMENTS; IZMIR BAY; AEGEAN SEA; ALEXANDRIUM-CATENELLA; SPATIAL-DISTRIBUTION; TRACE-METALS; EUTROPHICATION; TURKEY; COAST	The spatial distribution of modern dinoflagellate cysts was studied, with the purpose of understanding the impact from industrial pollution and sediment characteristics. Eight surface sediment samples were collected to analysis of the spatial distribution of dinoflagellate cysts from two industrially polluted areas: Aliaga and Nemrut Bay (Eastern Mediterranean). A total of 42 dinoflagellate cyst morphotype were identified and total cyst abundance ranged between 11 and 2543 cyst g(-1) dry weight sediment at sampling points. The cyst assemblages were represented by cyst of Gymnodinium nolleri, Alexandrium affine type and Lingulodiniumma chaerophorum. The higher cyst concentration was recorded at mostly Aliaga Bay stations however the higher cyst diversity was found at Nemrut Bay stations. Total cyst concentration and autotrophic cyst concentration indicated metal pollution in the sampling areas whereas total number of cysts had no correlation with any metal levels in the sediment except Cr. The distribution of dinoflagellate cysts also showed correlation with sediment structure in Aliaga and Nemrut Bay.	[Aydin, Hilal; Yurur, Emine Erdem; Uzar, Serdar; Kucuksezgin, Filiz] Celal Bayar Univ, Dept Biol, Fac Sci & Arts, Campus Muradiye, TR-45140 Manisa, Turkey	Celal Bayar University	Aydin, H (通讯作者)，Celal Bayar Univ, Dept Biol, Fac Sci & Arts, Campus Muradiye, TR-45140 Manisa, Turkey.	hilalaydin66@gmail.com	Uzar, Serdar/G-9956-2014; Kucuksezgin, Filiz/P-3788-2019	Kucuksezgin, Filiz/0000-0001-9030-5227				[Anonymous], 1985, UNEP Regional Seas Reports and Studies, V56; Aydin H, 2014, FRESEN ENVIRON BULL, V23, P1795; Aydin H, 2014, J ENVIRON BIOL, V35, P413; Aydin H, 2011, MAR MICROPALEONTOL, V80, P44, DOI 10.1016/j.marmicro.2011.03.004; BRULAND KW, 1991, LIMNOL OCEANOGR, V36, P1555, DOI 10.4319/lo.1991.36.8.1555; Christophoridis C, 2009, J HAZARD MATER, V168, P1082, DOI 10.1016/j.jhazmat.2009.02.154; D'Silva MS, 2013, MAR POLLUT BULL, V66, P59, DOI 10.1016/j.marpolbul.2012.11.012; Dale B., 1983, P69; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dale B, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; Duruibe JO, 2007, INT J PHYS SCI, V2, P112; Esen E., 2010, 39 CIESM VEN IT, P249; Esen E, 2010, ENVIRON MONIT ASSESS, V160, P257, DOI 10.1007/s10661-008-0692-9; Folk R.L, 1980, PETROLOGY SEDIMENARY, P26; Gencay H.A., 2006, J FISH AQUAT SCI, V23, P43; Ghani S. 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J. Fish. Quat. Sci.		2015	15				SI		543	554		10.4194/1303-2712-v15_2_42	http://dx.doi.org/10.4194/1303-2712-v15_2_42			12	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	DD3TL		Bronze			2025-03-11	WOS:000369845700020
J	Aydin, H; Balci, M; Uzar, S; Balkis, N				Aydin, Hilal; Balci, Muharrem; Uzar, Serdar; Balkis, Neslihan			DINOFLAGELLATE CYST ASSEMBLAGES IN SURFACE SEDIMENTS OF SOUTHWESTERN BLACK SEA AND CANAKKALE STRAIT (DARDANELLES)	FRESENIUS ENVIRONMENTAL BULLETIN			English	Article						Dinoflagellate cyst; surface sediment; Canakkale Strait; Black Sea	SPATIAL-DISTRIBUTION; AEGEAN SEA; IZMIR BAY; MARMARA; WESTERN; GERMINATION; QUATERNARY; ABUNDANCE; COAST	In order to document the distribution of dinoflagellate cyst assemblages, eight surface sediment samples were collected in surface sediments from southwestern Black Sea and Canakkale Strait. A total of 25 cyst types and 1 unknown cyst type were identified. Samples displays low total cyst concentrations with values ranging from 8 to 346 cyst g(-1) dry weight sediment. Autotrophic dinoflagellates highly and significantly contributes (p<0.01) to the total cyst concentration. Lingulodinium machaerophorum, cyst type of Alexandrium minutum and Spiniferites bulloideus were dominant at the sampling points. Higher cyst concentration and diversity observed at stations in Black Sea could be linked to the type of sediment. Small-sized sediment (sand-silt) were mostly dominant at the Black Sea stations compare to the more sandy type sediment of Canakkale Strait. Present study provides the first modern dinoflagellate cyst records from surface sediments of southwestern Black Sea and Canakkale Strait.	[Aydin, Hilal; Uzar, Serdar] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Muradiye, Manisa, Turkey; [Balci, Muharrem] Bursa Tech Univ, Fac Nat Sci, Dept Bioengn, Arch,Engn, Osmangazi, Bursa, Turkey; [Balkis, Neslihan] Istanbul Univ, Fac Sci, Dept Biol, Istanbul, Turkey	Celal Bayar University; Bursa Technical University; Istanbul University	Aydin, H (通讯作者)，Celal Bayar Univ, Fac Sci & Arts, Dept Biol, Campus Muradiye, TR-45140 Muradiye, Manisa, Turkey.	hilalaydin66@gmail.com	Balkis-Ozdelice, Neslihan/AAG-5490-2019; UZAR, SERDAR/G-9956-2014; BALCI, Muharrem/V-9411-2017	UZAR, SERDAR/0000-0002-9477-7413; BALCI, Muharrem/0000-0001-9373-6647; BALKIS-OZDELICE, NESLIHAN/0000-0001-8030-7480				Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; Aydin H., 2013, Journal of Fisheries and Aquatic Sciences (Su Urunleri Dergisi), V30, P109, DOI 10.12714/egejfas.2013.30.3.04; Aydin H., 2014, FRESEN ENVIRON BULL, V23, P1; Aydin H, 2014, J ENVIRON BIOL, V35, P413; Aydin H, 2011, MAR MICROPALEONTOL, V80, P44, DOI 10.1016/j.marmicro.2011.03.004; 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Bull.		2015	24	12C					4789	4798						10	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	DA3LQ					2025-03-11	WOS:000367699500012
J	You, XJ; Luo, ZH; Su, YP; Gu, L; Gu, HF				You, Xuejing; Luo, Zhaohe; Su, Yuping; Gu, Li; Gu, Haifeng			<i>Peridiniopsis jiulongensis</i>, a new freshwater dinoflagellate with a diatom endosymbiont from China	NOVA HEDWIGIA			English	Article						cyst; Jiulong River; Peridiniopsis; P. kevei; P. niei; P. penardii	SP-NOV DINOPHYCEAE; FLAGELLAR APPARATUS; SERIAL REPLACEMENT; MIXED MODELS; PERIDINIALES; PHYLOGENY; GEN.; PENARDII; MARINE	Detailed study on Peridiniopsis species using modern techniques is still limited. Here we report a new Peridiniopsis species isolated from the Jiulong River, China, which was described as jiulongensis H. Gu sp. nov. Vegetative cells of P. jiulongensis were subjected to detailed examination by light microscopy, scanning electron microscopy and transmission electron microscopy. P. jiulongensis has a plate pattern of Po, X, 3', la, 6 '', 5C, 5S, 5''',, 2 '''' and harbors a dinokaryotic and a eukaryotic nucleus. The eyespot of P. jiulongensis was bounded by triple envelopes and thus classified as type D. Molecular phylogeny based on dinoflagellate small subunit ribosomal DNA (SSU rDNA) sequences revealed that dinoflagellates with a diatom endosymbiont were monophyletic and P. jiulongensis was grouped together with Peridiniopsis cf. kevei, P niei and P. penardii. Molecular phylogeny based on endosymbiont SSU rDNA sequences showed that P. jiulongensis, P. cf. kevei, and P. penardii formed a well resolved group and were close to Thalassiosira species.	[You, Xuejing; Su, Yuping] Fujian Normal Univ, Fuzhou 350007, Peoples R China; [You, Xuejing; Luo, Zhaohe; Gu, Li; Gu, Haifeng] Third Inst Oceanog, Xiamen 361005, Peoples R China	Fujian Normal University; Third Institute of Oceanography, Ministry of Natural Resources	Gu, HF (通讯作者)，Third Inst Oceanog, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com	Su, Yu-Ping/J-7534-2012; Luo, Zhaohe/ITT-7163-2023; Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171; Luo, Zhaohe/0000-0001-8662-2414	National Science Foundation of China [41101060, 41376170]; special foundation of non-profit research institutes of Fujian province [2011R1004-2]; young visiting scholars foundation of State Key Laboratory of Coastal and Marine Environment of Xiamen University [MELRS1103]	National Science Foundation of China(National Natural Science Foundation of China (NSFC)); special foundation of non-profit research institutes of Fujian province; young visiting scholars foundation of State Key Laboratory of Coastal and Marine Environment of Xiamen University	We thank two anonymous reviewers for constructive suggestions. This project was supported by National Science Foundation of China (41101060, 41376170), special foundation of non-profit research institutes of Fujian province (2011R1004-2), young visiting scholars foundation of State Key Laboratory of Coastal and Marine Environment of Xiamen University (MELRS1103).	Alix B, 2012, NUCLEIC ACIDS RES, V40, pW573, DOI 10.1093/nar/gks485; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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J	Li, Z; Matsuoka, K; Shin, HH; Kobayashi, S; Shin, K; Lee, T; Han, MS				Li, Zhun; Matsuoka, Kazumi; Shin, Hyeon Ho; Kobayashi, Satori; Shin, Kyungsoon; Lee, TaeHee; Han, Myung-Soo			<i>Brigantedinium majusculum</i> is the cyst of <i>Protoperidinium sinuosum</i> (Protoperidiniaceae, Dinophyceae)	PHYCOLOGIA			English	Article						Brigantedinium majusculum; cyst-theca relationship; Protoperidinium pentagonum; Protoperidinium sinuosum	DINOFLAGELLATE RESTING CYSTS; RECENT MARINE-SEDIMENTS; THECA RELATIONSHIP; COASTAL WATERS; SP-NOV; PERIDINIALES; AUSTRALIA; MODELS; GENUS; PARK	Two morphologically distinct species, Brigantedinium majusculum and Trinovantedinium applanatum, have been suggested as a cyst stage of Protoperidinium pentagonum; however, the cyst-theca relationships are still virtually undefined. In this study, we re-examined the motile stage of B. majusculum via thecal plate analysis together with a molecular phylogenetic analysis based on partial large-subunit ribosomal DNA gene sequences. The morphological features of motile cells germinated from B. majusculum were identical to those of Pr. sinuosum, and the molecular phylogenetic analysis showed that the germinated cells and B. majusculum are closely related to Pr. pentagonum and Pr. latissimum as a sister group. Additionally, high sequence divergences were observed between the germinated cells and B. majusculum as well as Pr. pentagonum and Pr. latissimum (18.0-19.5% according to P-values and 20.7-22.9% according to Kimura two-parameter values). On the basis of these results, our study indicates that B. majusculum should be accepted as the cyst of Pr. sinuosum.	[Li, Zhun; Han, Myung-Soo] Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; [Li, Zhun; Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656834, South Korea; [Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, Nagasaki 8512213, Japan; [Kobayashi, Satori] Tokyo Kyuei Co Ltd, Kawaguchi, Saitama 3330866, Japan; [Shin, Kyungsoon] Korea Inst Ocean Sci & Technol, Ballast Res Ctr, South Sea Res Inst, Geoje 656834, South Korea; [Lee, TaeHee] Korea Inst Ocean Sci & Technol, Maritime Secur Res Ctr, Ansan 426744, South Korea	Hanyang University; Korea Institute of Ocean Science & Technology (KIOST); Nagasaki University; Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST)	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656834, South Korea.	shh961121@kiost.ac.kr; hanms@hanyang.ac.kr	LI, ZHUN/GLT-3478-2022	Shin, Hyeon Ho/0000-0002-9711-6717; LI, ZHUN/0000-0001-8961-9966	Marine Biotechnology Program, and Construction test, evaluation, and certification systems for US Coast Guard phase II standard - Ministry of Oceans and Fisheries, Korea [PM58580]	Marine Biotechnology Program, and Construction test, evaluation, and certification systems for US Coast Guard phase II standard - Ministry of Oceans and Fisheries, Korea	This work was supported by grants from Marine Biotechnology Program, and Construction test, evaluation, and certification systems for US Coast Guard phase II standard (PM58580) funded by Ministry of Oceans and Fisheries, Korea.	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J	Hallegraeff, GM				Hallegraeff, Gustaaf M.			Transport of harmful marine microalgae via ship's ballast water: Management and mitigation with special reference to the Arabian Gulf region	AQUATIC ECOSYSTEM HEALTH & MANAGEMENT			English	Article; Proceedings Paper	International Conference on Marine Invasive Species: Management of Ballast Water and Other Vectors	FEB 17-19, 2014	Muscat, OMAN			ballast water management; Alexandrium; Cochlodinium; Noctiluca; ballast water exchange; ballast water heat treatment	ALEXANDRIUM-CATENELLA; DINOPHYCEAE; DISPERSAL; DIATOM; TIME; BACILLARIOPHYCEAE; ORGANISMS; TAXONOMY; PACIFIC; COMPLEX	The potential for transport of non-indigenous marine microalgae via ship's ballast water has been amply demonstrated, and nearly all known harmful algal bloom species have been documented in viable form from ship's ballast water. Ballast water uptake needs to be strongly discouraged during harmful algal bloom events. Efficacy of ballast water exchange in removing harmful microalgal cells is limited, since this nearly always leaves behind a viable inoculum. The precise location of ballast water exchange needs to be carefully chosen, and retention of dinoflagellate cysts and diatom spores in ballast tank sediments is of special concern. The only fully effective ballast water treatment for microalgae is the application of biocides, but heat treatment also offers considerable promise especially in subtropical and tropical waters. To manage harmful algal blooms, other key environmental drivers such as eutrophication and climate change also need to be addressed. Effective monitoring for harmful algal species and their toxins remains the critical tool to protect human health, fisheries, aquaculture and desalination industries. Challenges and opportunities for ballast water management in the Arabian Gulf region are discussed.	Univ Tasmania, Inst Marine & Antarct Studies, Hobart, Tas 7001, Australia	University of Tasmania	Hallegraeff, GM (通讯作者)，Univ Tasmania, Inst Marine & Antarct Studies, Private Bag 129, Hobart, Tas 7001, Australia.	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Health Manag.		2015	18	3			SI		290	298		10.1080/14634988.2015.1027138	http://dx.doi.org/10.1080/14634988.2015.1027138			9	Ecology; Environmental Sciences; Marine & Freshwater Biology; Water Resources	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Water Resources	CR6XL					2025-03-11	WOS:000361491600006
J	Pszczólkowski, A				Pszczolkowski, Andrzej			APTIAN AGE OF THE "SPOTTED LIME STONE" (PIENINY LIMESTONE FORMATION) IN GRAJCAREK STREAM (PIENINY KLIPPEN BELT, POLAND)	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						Cretaceous; biostratigraphy; microfacies; calcareous microfossils; Pieniny Klippen Belt; Poland	CRETACEOUS PLANKTONIC-FORAMINIFERA; CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; CHAMBERED REPRESENTATIVES; INTEGRATED STRATIGRAPHY; PRE-GUITTARD; TETHYS; FRANCE; STRATOTYPE; BOUNDARY; SECTION	Planktonic foraminifera, calcareous dinocysts and nannofossils have been identified in thin sections of the "spotted lime stone", exposed in the Grajcarek Stream at Szlachtowa and as signed to the Pieniny Lime stone Formation in the Magura Succession, Pieniny Klippen Belt (south ern Poland). The new data indicate that the "spotted lime stone" is older than was suggested in previous reports (Albian or Cenomanian?). The foraminiferal taxa belong mainly to the upper part of the Lower Aptian. The calcareous nannofossils may cor respond to the Aptian NC6(?)-NC7 zones, whereas the assemblage of calcareous dinoflagellate cysts is less conclusive (Late Barremian-Aptian).	[Pszczolkowski, Andrzej] Polish Acad Sci, Inst Geol Sci, Res Ctr Warszawa, PL-00818 Warsaw, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Pszczólkowski, A (通讯作者)，Mozarta 6 M 1103, PL-02736 Warsaw, Poland.	pszczolkowski@yahoo.com						Aguado R, 1999, CRETACEOUS RES, V20, P663, DOI 10.1006/cres.1999.0176; Ando A, 2013, CRETACEOUS RES, V45, P275, DOI 10.1016/j.cretres.2013.05.002; [Anonymous], [No title captured], DOI DOI 10.1029/GM077P0005; ANTONOVA ZA, 1964, T VSESOYUZ NEFTAGAZI, V12, P3; Banner F.T., 1993, Bulletin of the Natural History Museum Geology Series, V49, P1; Banner F.T., 1988, Journal of Micropalaeontology, V7, P143; Bignot G., 1964, Revue de Micropaleontologie, V7, P138; BIRKENMAJER K, 1987, Studia Geologica Polonica, V92, P87; BIRKENMAJER K, 1987, Studia Geologica Polonica, V92, P107; Birkenmajer K, 1979, PRZEWODNIK GEOLOGICZ, P1; Birkenmajer K., 2001, 12 M ASS EUR GEOL SO, P127; Birkenmajer K., 1965, ROCZNIK POLSKIEGO TO, V35, P379; Birkenmajer K., 1958, PRZEWODNIK GEOLOGICZ, P1; Birkenmajer K., 1977, Stud. 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J	Gedl, P; Józsa, S				Gedl, Przemyslaw; Jozsa, Stefan			EARLY?-MIDDLE JURASSIC DINOFLAGELLATE CYSTS AND FORAMINIFERA FROM THE DARK SHALE OF THE PIENINY KLIPPEN BELT BETWEEN JARABINA AND LITMANOVA (SLOVAKIA): AGE AND PALAEONVIRONMENT	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						Dinoflagellate cysts; foraminifera; Jurassic; biostratigraphy; palynofacies; palaeoenvironment; Pieniny Klippen Belt	BENTHIC FORAMINIFERA; SHELF DEPOSITS; BAJOCIAN; ASSEMBLAGES; MORPHOGROUPS	The results presented are a part of the biostratigraphical and palaeoenvironmental studies of the authors on the microfauna and organic-walled dinoflagellate cysts from the Mesozoic dark deposits of the Pieniny Klippen Belt. The authors present the latest results from the Lower-Middle Jurassic strata, including the Szlachtowa and the Skrzypny Shale formations in the Slovak part of the Pieniny Klippen Belt near the villages of Jarabina, Kamienka and Litmanova. Material for the present study comes from exposures along the Maly Lipnik, Vel'ky Lipnik and Riecka Streams, and from the Jar-1 bore hole, near Jarabina. The authors document the microfaunal and phytoplanctonic content of these rocks that contain over 50 foraminifera and 20 dinoflagellate cyst species. Their Middle Toarcian?-Aalenian to Bajocian-Bathonian ages are proposed and discussed. Quantitative and qualitative variations of both microfossil groups are interpreted as reflecting various sedimentary settings, related mainly to the variable intensity of in flux of terrestrial matter into marine basins, leading to different bottom-water living conditions.	[Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, PL-31002 Krakow, Poland; [Jozsa, Stefan] Comenius Univ, Fac Sci, Dept Geol & Paleontol, SK-84215 Bratislava, Slovakia	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Comenius University Bratislava	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl; jozsa@fns.uniba.sk		Jozsa, Stefan/0000-0002-8563-3039; Jozsa, Stefan/0000-0001-5089-2121	 [APVV-0112-12];  [VEGA 2/0094/14]	; 	The second author is grateful for financial support to APVV-0112-12 and VEGA 2/0094/14. Special thanks go to Jan Schlogl for remarks on ammonites, to Mike Kaminski for critical reading the manuscript and constructive remarks on the agglutinated foraminifera, to Anton Waltschew for determining the ostracods shown in the photodocumentation and to Frank Simpson for linguistic correction. Marcin Barski is acknowledged for critical reading the manuscript and comments.	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OLEANDRY 2A, KRAKOW, POLAND	0208-9068			ANN SOC GEOL POL	Ann. Soc. Geol. Pol.		2015	85	1					91	122						32	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CK1BQ					2025-03-11	WOS:000355940800005
J	Gedl, P				Gedl, Przemyslaw			DINOFLAGELLATE CYSTS FROM THE PALAEOGENE OF THE LUKOWA-4 BOREHOLE (CARPATHIAN FOREDEEP, SE POLAND): BIOSTRATIGRAPHY AND PALAEOENVIRONMENT	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						Dinoflagellate cysts; Eocene; Palaeogene; biostratigraphy; palaeoenvironment; Carpathian Foredeep	CENOZOIC DYNAMIC EVOLUTION; LATE EOCENE; DEPOSITS; MAGNETOSTRATIGRAPHY; MIOCENE	This paper documents the presence of Eocene marine strata in the Carpathian Foredeep area in Poland. Assemblages of marine dinoflagellate cysts have been found in sands penetrated by the Lukowa-4 bore hole be low the Miocene succession of the foredeep. Their age is interpreted as Late Eocene. The presence of marine strata of this age in this area sheds new light on the palaeogeography of the Carpathian foreland during the Late Eocene. The dinoflagellate cysts described are compared with coeval Carpathian and epicontinental assemblages; possible connections between these two basins are discussed. Phytogenetic deposits that occur above the marine sands of the Lukowa-4 bore hole contain freshwater palynomorphs, indicating their swamp and lacustrine origins. The overlying sand contains impoverished dinoflagellate cyst assemblages; their age is discussed.	Polish Acad Sci, Res Ctr Krakow, 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, Res Ctr Krakow, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl						Andreyeva-Grigorovich A, 2011, ATLAS PALEOGENE DINO; [Anonymous], 1989, P OC DRIL PROGR SCI; [Anonymous], 1980, PALEOBIOLOGY PLANT P; [Anonymous], 1996, Palynology: principles and applications; BATTEN D.J., 1996, PALYNOLOGY PRINCIPLE, V1, P205; 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; 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; Brugman W. 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OLEANDRY 2A, KRAKOW, POLAND	0208-9068			ANN SOC GEOL POL	Ann. Soc. Geol. Pol.		2015	85	1					285	308						24	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CK1BQ					2025-03-11	WOS:000355940800014
J	Liu, TT; Mertens, KN; Gu, HF				Liu, Tingting; Mertens, Kenneth Neil; Gu, Haifeng			Cyst-theca relationship and phylogenetic positions of the diplopsalioideans (Peridiniales, Dinophyceae), with description of <i>Niea</i> and <i>Qia gen</i>. <i>nov</i>.	PHYCOLOGIA			English	Article						Boreadinium breve; Cyst; Diplopelta globula; Diplopsalis lenticula; Diplopsalopsis ovata; Lebouraia pusilla; Oblea acanthocysta; Oblea rotunda; Oblea torta; Qia lebouriae	OBLEA-ROTUNDA DIPLOPSALIDACEAE; DINOFLAGELLATE CYSTS; MIXED MODELS; PROTOPERIDINIUM; SEDIMENTS; REVISION; GENERA; PLATES; RDNA	Nine genera have been assigned to the subfamily Diplopsalioideae, but since most have not been characterized molecularly and their cyst-theca relationships are largely unknown, the phylogenetic relationships among these genera are not well understood. Here we established the cyst-theca relationships of 11 species (Boreadinium breve, Diplopelta globula, Diplopsalis lenticula, Diplopsalopsis ovata, Lebouraia pusilla, Niea acanthocysta, Niea chinensis, Niea torta, Oblea rotunda, Preperidinium cf. meunieri and Qia lebouriae) belonging to nine genera by incubating cysts collected along the coast of China. In addition, we obtained 22 large-subunit ribosomal DNA sequences from the germinated motile cells of these 11 species by single-cell polymerase chain reaction. A new genus, Niea, was erected to encompass species with a plate formula identical to that of Oblea, that is, Po, X, 3', 1a, 6 '', 3C+t, 5''', 2'''', but with an ortho 1'. Niea chinensis was described based on both theca and cyst morphology. The genus Oblea was emended to incorporate only species with a meta 1'. As a consequence, Oblea acanthocysta and O. torta were transferred to the newly erected genus Niea. A second new genus, Qia, was established to encompass Diplopsalis lebouriae, and the genus Diplopsalis was emended, differing from Qia in the shape of the anterior intercalary (1a) plate. Phylogenetic analyses were carried out using maximum likelihood and Bayesian inference. Molecular phylogeny revealed that the diplopsalioideans were not monophyletic and were subdivided into three clades. From our results, the shape of the first apical and anterior intercalary plates and the number of apical, anterior intercalary and antapical plates were useful characteristics to distinguish the diplopsalioideans at the genus level.	[Liu, Tingting; Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Third Institute of Oceanography, Ministry of Natural Resources; Ghent University	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022	Mertens, Kenneth/0000-0003-2005-9483; Gu, Haifeng/0000-0002-2350-9171	National Natural Science Foundation of China [41376170]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This project was supported by National Natural Science Foundation of China (41376170). K.N.M. is a postdoctoral fellow of FWO Belgium. Two anonymous reviewers and the editor are thanked for constructive comments that significantly improved the article.	Abe T. 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J	Li, Z; Shin, HH; Han, MS				Li, Zhun; Shin, Hyeon Ho; Han, Myung-Soo			Morphology and phylogeny of a new woloszynskioid dinoflagellate <i>Tovellia paldangensis</i> sp nov (Dinophyceae)	PHYCOLOGIA			English	Article						Cyst; Dinoflagellates; Freshwater; Sediment; Tovellia	LAKE TOVEL; GEN. NOV; ULTRASTRUCTURE; SCRIPPSIELLA; MODELS; CYSTS; SEA	The genus Tovellia contains approximately eight described species. A new species, Tovellia paldangensis sp. nov. was observed by incubation of a cyst from sediment collected in the Paldang Dam Lake in Korea. The vegetative cells of this new species were 20.0-27.0 mu m long, 18.0-23.0 mu m wide, and 17.0-20.5 mu m thick. The cingulum was displaced by one cingulum width, the nucleus was located in the posterior part of the cell, and the chloroplasts were numerous and in yellow-green in color. A prominent red body was present on each side of the cingulum. The amphiesma had numerous thin polygonal plates that were arranged in three to four latitudinal series on the epicone and in two to three series on the hypocone. A narrow apical line of plates (ALP) extended over the anterior part of the cell, approximately in a 3/4 of the ventral side and 1/4 of the dorsal side of the epicone. The antapical plate was usually hexagonal. T. paldangensis was clearly differentiated from the other species of Tovellia by the morphology of its vegetative cell (two red bodies, and the ALP lines on each side separated by a row of four to five elongate plates) and the resting cyst (typically covered with numerous short solid spines). Phylogenetic analysis based on partial large subunit ribosomal RNA gene sequences indicated that T. paldangensis was most closely related to T. coronata, T. sanguinea, and T. aveirensis.	[Li, Zhun; Han, Myung-Soo] Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; [Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656830, South Korea	Hanyang University; Korea Institute of Ocean Science & Technology (KIOST)	Han, MS (通讯作者)，Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea.	hanms@hanyang.ac.kr	LI, ZHUN/GLT-3478-2022	Shin, Hyeon Ho/0000-0002-9711-6717; LI, ZHUN/0000-0001-8961-9966	Korea Ministry of Environment [2013001470001]	Korea Ministry of Environment(Ministry of Environment (ME), Republic of Korea)	This project was supported by the Korea Ministry of Environment (2013001470001).	BEAKES GW, 1988, CAN J BOT, V66, P1054, DOI 10.1139/b88-151; Calado AJ, 2006, J PHYCOL, V42, P434, DOI 10.1111/j.1529-8817.2006.00195.x; Calado AJ, 2011, PHYCOLOGIA, V50, P641, DOI 10.2216/11-21.1; CHRISTEN H. 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J	Mertens, KN; Wolny, J; Carbonell-Moore, C; Bogus, K; Ellegaard, M; Limoges, A; de Vernal, A; Gurdebeke, P; Omura, T; Al-Muftah, A; Matsuoka, K				Mertens, Kenneth Neil; Wolny, Jennifer; Carbonell-Moore, Consuelo; Bogus, Kara; Ellegaard, Marianne; Limoges, Audrey; de Vernal, Anne; Gurdebeke, Pieter; Omura, Takuo; Al-Muftah, Abdulrahman; Matsuoka, Kazumi			Taxonomic re-examination of the toxic armored dinoflagellate <i>Pyrodinium bahamense</i> Plate 1906: Can morphology or LSU sequencing separate <i>P</i>. <i>bahamense</i> var. <i>compressum</i> from var. <i>bahamense</i>?	HARMFUL ALGAE			English	Article						Biometry; Cyst; Theca; Thermophile; LSU; Saxitoxins	SURFACE SEDIMENTS; FT-IR; DINOPHYCEAE; CYSTS; NOV; PHYLOGENIES; FLORIDA	Pyrodinium bahamense Plate 1906 is a tropical to subtropical dinoflagellate that can cause paralytic shellfish poisoning (PSP). Based on differences in the morphology of the motile stage, as well as geographic distribution, this species was separated into two varieties, the toxic var. compressum and the non-toxic var. bahamense by Steidinger et al. (1980). Thereafter, Balech (1985) carefully reinvestigated the two varieties and concluded there were no significant morphological differences between them. We re-examined the motile cell and cyst morphology of these two varieties, concurring with the arrangement of the sulcal plates, but demonstrating the plate overlap for the first time. The observed size-frequency spectra of cell body diameter, cyst body diameter and cyst process length were unimodal. Overall, we agree with Balech (1985) that there is no consistent criterion to unequivocally separate both varieties based on morphology. We therefore recommend ceasing the use of these varieties (and forma). In addition, we suggest that observations of both varieties in a single plankton sample should be interpreted as the occurrence of different life stages at the sampling time. However, the phylogenetic analysis using partial LSU rDNA sequence data revealed two clearly separated ribotypes within the Pyrodinium clade, an Indo-Pacific and Atlantic-Caribbean ribotype, suggesting that Pyrodinium bahamense is a species complex. The genetic distance between these ribotypes is short, which suggests a late Quaternary separation. Geochemical analyses of the cyst walls also show differences between specimens from both geographical regions. (C) 2014 Elsevier B.V. All rights reserved.	[Mertens, Kenneth Neil; Gurdebeke, Pieter] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Wolny, Jennifer] Univ S Florida, Fish & Wildlife Res Inst, St Petersburg, FL 33701 USA; [Carbonell-Moore, Consuelo] Oregon State Univ, Dept Bot & Plant Pathol, Coll Agr Sci, Corvallis, OR 97331 USA; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA; [Bogus, Kara] Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77845 USA; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Fac Sci, DK-1871 Frederiksberg C, Denmark; [Limoges, Audrey; de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Omura, Takuo] Lab Aquat Sci Consultant Co LTD LASC, Ota Ku, Tokyo 1450064, Japan; [Al-Muftah, Abdulrahman] Qatar Univ, Dept Biol & Environm Sci, Doah, Qatar; [Matsuoka, Kazumi] Inst East China Sea Res ECSER, Nagasaki 8528521, Japan	Ghent University; Florida Fish & Wildlife Conservation Commission; State University System of Florida; University of South Florida; Oregon State University; Texas A&M University System; Texas A&M University College Station; Texas A&M University System; Texas A&M University College Station; University of Copenhagen; University of Quebec; University of Quebec Montreal; Qatar University	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be; Jennifer.Wolny@maryland.gov; carbonem@onid.orst.edu; bogus@iodp.tamu.edu; me@plen.ku.dk; limoges.audrey@gmail.com; devemal.anne@uqam.ca; pieter.gurdebeke@ugent.be; omura@lasc.co.jp; aralmuftah@qu.edu.qa; kazu-mtk@nagasaki-u.ac.jp	de Vernal, Anne/D-5602-2013; Gurdebeke, Pieter/AAY-7059-2020; Mertens, Kenneth/AAO-9566-2020; Ellegaard, Marianne/H-6748-2014; Mertens, Kenneth/C-3386-2015	Gurdebeke, Pieter R./0000-0003-1425-8515; Wolny, Jennifer L./0000-0002-3556-5015; Ellegaard, Marianne/0000-0002-6032-3376; Limoges, Audrey/0000-0002-4587-3417; Mertens, Kenneth/0000-0003-2005-9483; Bogus, Kara/0000-0003-4690-0576				Abbott JP, 2009, HARMFUL ALGAE, V8, P343, DOI 10.1016/j.hal.2008.07.005; AI-Muftah A. 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J	Barrón, E; Peyrot, D; Rodríguez-López, JP; Meléndez, N; del Valle, RL; Najarro, M; Rosales, I; Comas-Rengifo, MJ				Barron, Eduardo; Peyrot, Daniel; Pedro Rodriguez-Lopez, Juan; Melendez, Nieves; Lopez del Valle, Rafael; Najarro, Maria; Rosales, Idoia; Jose Comas-Rengifo, Ma			Palynology of Aptian and upper Albian (Lower Cretaceous) amber-bearing outcrops of the southern margin of the Basque-Cantabrian basin (northern Spain)	CRETACEOUS RESEARCH			English	Article						Palynology; Amber; Aptian; Upper Albian; Basque-Cantabrian basin; Spain	ANGIOSPERM DIVERSIFICATION; POTOMAC GROUP; EL SOPLAO; DEPOSITS; POLLEN; RECORDS; SYSTEM; UNIT	The Lower Cretaceous deposits of the southern margin of the Basque-Cantabrian basin (northern Spain) are characterised by continental deposits interbedded with amber-bearing marine-influenced facies. These facies crop out in various localities and have yielded well-preserved palynological assemblages. The palynoflora is dominated by gymnosperm pollen grains, and shows relatively diversified spore content but scarce dinoflagellate cysts. The palynofloral evidence and regional geological setting indicate that the studied successions are dated as Aptian (Montoria-La Mina outcrop) and late Albian (Periacerrada 1 and 2 and Salinillas de Buradon outcrops, and the Pancorbo site). Angiosperm pollen does not constitute a significant part of the Aptian assemblages but becomes diversified and numerically abundant in those dated as late Albian. Although broadly similar to contemporaneous palynofloras from eastern Spain, the Aptian assemblages of Montoria-La Mina do not yield tricolpate angiosperm pollen. Conversely, the inferred late Albian assemblages show a high content in polyaperturate angiosperm pollen grains, as occurs in other localities in Portugal, Western Europe and North America. The studied palynoflora shows significant differences from published assemblages located further north, in western France and Canada. (C) 2014 Elsevier Ltd. All rights reserved.	[Barron, Eduardo; Najarro, Maria; Rosales, Idoia] Inst Geol & Minero Espana, E-28003 Madrid, Spain; [Peyrot, Daniel] Robertson UK Ltd, Tyn Y Coed, Llandudno LL30 1SA, Gwynedd, Wales; [Pedro Rodriguez-Lopez, Juan; Melendez, Nieves] Univ Complutense Madrid, Fac Ciencias Geol, Dept Estratig, E-28040 Madrid, Spain; [Pedro Rodriguez-Lopez, Juan] Saudi Arabian Oil Co, Dhahran, Saudi Arabia; [Lopez del Valle, Rafael] Museo Ciencias Nat Alava, E-01001 Vitoria, Spain; [Jose Comas-Rengifo, Ma] Univ Complutense Madrid, Fac Ciencias Geol, Dept Paleontol, E-28040 Madrid, Spain	Complutense University of Madrid; Saudi Aramco; Complutense University of Madrid	Barrón, E (通讯作者)，Inst Geol & Minero Espana, Rios Rosas 23, E-28003 Madrid, Spain.	e.barron@igme.es	peyrot, Daniel/AAI-6091-2020; Barrón, Eduardo/L-4726-2014; Rosales, Idoia/F-2287-2011; Najarro, Maria/S-1007-2018; Comas-Rengifo, Maria Jose/H-8373-2015	Rosales, Idoia/0000-0003-4381-2917; Barron, Eduardo/0000-0003-4979-1117; Najarro, Maria/0000-0002-2642-4544; peyrot, Daniel/0000-0002-3897-6733; Comas-Rengifo, Maria Jose/0000-0002-6593-3798; Comas Rengifo, Maria Jose/0000-0002-3529-8439; melendez, nieves/0000-0002-9476-740X	Spanish Ministry of Economy and Competitiveness [CGL2011-23948, CGL2011-23717, CGL2011-24546, CGL2011-25894]	Spanish Ministry of Economy and Competitiveness(Spanish Government)	This work is a contribution of the DGI projects CGL2011-23948, CGL2011-23717, CGL2011-24546 and CGL2011-25894 financed by the Spanish Ministry of Economy and Competitiveness. Daniel Peyrot publishes with the approval of the board of Robertson (UK) Ltd. We thank Xavier Delclos (University of Barcelona), Enrique Penalver and Pepa Torres (IGME), Jim Fenton (Robertson), Paulo R. Trincao (Botanical Garden of the University of Coimbra) and Jesus Alonso (Natural History Museum of Alava) for their inestimable assistance. We wish also to thank Dr. E. Koutsoukos (Editor in Chief) and the two anonymous referees who provided valuable suggestions for the improvement of the manuscript.	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Res.	JAN	2015	52		A				292	312		10.1016/j.cretres.2014.10.003	http://dx.doi.org/10.1016/j.cretres.2014.10.003			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	AY6GY					2025-03-11	WOS:000347666300023
J	van Helmond, NAGM; Sluijs, A; Damsté, JSS; Reichart, GJ; Voigt, S; Erbacher, J; Pross, J; Brinkhuis, H				van Helmond, N. A. G. M.; Sluijs, A.; Damste, J. S. Sinninghe; Reichart, G. -J.; Voigt, S.; Erbacher, J.; Pross, J.; Brinkhuis, H.			Freshwater discharge controlled deposition of Cenomanian-Turonian black shales on the NW European epicontinental shelf (Wunstorf, northern Germany)	CLIMATE OF THE PAST			English	Article							OCEANIC ANOXIC EVENT; DINOFLAGELLATE CYST ASSEMBLAGES; STRATIGRAPHIC REFERENCE SECTION; GLYCEROL TETRAETHER LIPIDS; SEA-SURFACE TEMPERATURES; ORGANIC-CARBON BURIAL; MARINE-SEDIMENTS; CRETACEOUS CLIMATE; MEMBRANE-LIPIDS; SOUTH-ATLANTIC	Global warming, changes in the hydrological cycle and enhanced marine primary productivity all have been invoked as having contributed to the occurrence of widespread ocean anoxia during the Cenomanian-Turonian oceanic anoxic event (OAE2; similar to 94 Ma), but disentangling these factors on a regional scale has remained problematic. In an attempt to separate these forcing factors, we generated palynological and organic geochemical records using a core spanning the OAE2 from Wunstorf, Lower Saxony Basin (LSB; northern Germany), which exhibits cyclic black shale-marl alternations related to the orbital precession cycle. Despite the widely varying depositional conditions complicating the interpretation of the obtained records, TEX86H indicates that sea-surface temperature (SST) evolution in the LSB during OAE2 resembles that of previously studied sites throughout the proto-North Atlantic. Cooling during the so-called Plenus Cold Event interrupted black shale deposition during the early stages of OAE2. However, TEX86 does not vary significantly across black shale-marl alternations, suggesting that temperature variations did not force the formation of the cyclic black shale horizons. Relative (i.e., with respect to marine palynomorphs) and absolute abundances of pollen and spores are elevated during phases of black shale deposition, indicative of enhanced precipitation and run-off. High abundances of cysts from inferred heterotrophic and euryhaline dinoflagellates supports high run-off, which likely introduced additional nutrients to the epicontinental shelf resulting in elevated marine primary productivity. We conclude that orbitally forced enhanced precipitation and run-off, in tandem with elevated marine primary productivity, were critical in cyclic black shale formation on the northern European epicontinental shelf and potentially for other OAE2 sections in the proto-Atlantic and Western Interior Seaway at similar latitudes as well.	[van Helmond, N. A. G. M.; Sluijs, A.; Brinkhuis, H.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Palaeobot & Paly, NL-3584 CD Utrecht, Netherlands; [Damste, J. S. Sinninghe; Reichart, G. -J.] Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Damste, J. S. Sinninghe; Reichart, G. -J.; Brinkhuis, H.] Royal Netherlands Inst Sea Res, NIOZ, NL-1790 AB Den Burg, Texel, Netherlands; [Voigt, S.] Goethe Univ Frankfurt, Inst Geosci, D-60438 Frankfurt, Germany; [Erbacher, J.] Bundesanstalt Geowissensch & Rohstoffe, D-30641 Hannover, Germany; [Pross, J.] Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, D-69120 Heidelberg, Germany	Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Goethe University Frankfurt; Ruprecht Karls University Heidelberg	van Helmond, NAGM (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Palaeobot & Paly, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	n.vanhelmond@uu.nl	Brinkhuis, Henk/IUO-8165-2023; Voigt, Silke/G-7270-2017; Reichart, Gert-Jan/N-6308-2018; Sluijs, Appy/B-3726-2009; Sinninghe Damste, Jaap/F-6128-2011	Voigt, Silke/0000-0002-2560-5933; Reichart, Gert-Jan/0000-0002-7256-2243; van Helmond, Niels/0000-0003-0024-7217; Erbacher, Jochen/0000-0003-2793-0307; Sluijs, Appy/0000-0003-2382-0215; Sinninghe Damste, Jaap/0000-0002-8683-1854; Brinkhuis, Henk/0000-0003-0253-6610	NWO [834.11.006]; Focus and Massa project of Utrecht University; Statoil; European Research Council (ERC) under the European Union [259627]	NWO(Netherlands Organization for Scientific Research (NWO)); Focus and Massa project of Utrecht University; Statoil; European Research Council (ERC) under the European Union(European Research Council (ERC))	The Wunstorf Coring Scientific Drilling Party is thanked for providing the chance to work on their exceptionally well-recovered core. We thank Itzel Ruvalcaba Baroni and Walter Hale for sampling support, and Dominika Kasjaniuk, Arnold van Dijk, Natasja Welters, Jan van Tongeren (Utrecht University), and Anchelique Mets (NIOZ) for analytical assistance and sample preparation. Andrew Gale and David Naafs are thanked for their constructive reviews. We acknowledge NWO for funding the purchase of the HPLC-MS (grant no. 834.11.006) used for the GDGT analysis presented in this study. This research was supported by the Focus and Massa project of Utrecht University granted to Henk Brinkhuis and Caroline Slomp, and additional financial support by Statoil. The European Research Council (ERC) under the European Union Seventh Framework Program provided funding for this work by ERC Starting Grant no. 259627 to Appy Sluijs.	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Past.		2015	11	3					495	508		10.5194/cp-11-495-2015	http://dx.doi.org/10.5194/cp-11-495-2015			14	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	CE9JJ		gold, Green Submitted, Green Published			2025-03-11	WOS:000352159900008
J	Açikalin, S; Vellekoop, J; Ocakoglu, F; Yilmaz, IÖ; Smit, J; Altiner, SÖ; Goderis, S; Vonhof, H; Speijer, RP; Woelders, L; Fornaciari, E; Brinkhuis, H				Acikalin, Sanem; Vellekoop, Johan; Ocakoglu, Faruk; Yilmaz, I. Omer; Smit, Jan; Altiner, Sevinc O.; Goderis, Steven; Vonhof, Hubert; Speijer, Robert P.; Woelders, Lineke; Fornaciari, Eliana; Brinkhuis, Henk			Geochemical and palaeontological characterization of a new K-Pg Boundary locality from the Northern branch of the Neo-Tethys: Mudurnu - Goynuk Basin, NW Turkey	CRETACEOUS RESEARCH			English	Article						K-Pg Boundary; Mudurnu-Goynuk Basin; Carbon isotope record; Siderophile trace element record; Organic dinoflagellate cysts; Planktic foraminifera	CRETACEOUS-TERTIARY BOUNDARY; PALEOENVIRONMENTAL CHANGES; PLANKTIC FORAMINIFERA; DINOFLAGELLATE CYSTS; CHICXULUB IMPACT; EXTINCTION; IDENTIFICATION; STRATIGRAPHY; EVOLUTION; ZONATION	A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-Goynuk basin in northwestern Turkey. To characterize the K-Pg transition in this basin, two stratigraphic sections were measured and sampled at high resolution: the Okcular and the Goynuk North sections. These sections were analysed for siderophile trace elements, including Ir and other platinum group elements (PGE: Ru, Rh, Pd, Ir, Pt), bulk stable carbon isotopes, calcareous nannofossils, planktic foraminifera and organic-walled dinoflagellate cysts (dinocysts). In this basin, the upper Maastrichtian consists of monotonous grey mudstones, mostly intercalated with turbidites and the basal Danian is characterised by grey mudstones, that are overlain by a rhythmic alternation of limetones and mudstones. The K-Pg boundary is marked by a thin, reddish ejecta layer, characterized by an enrichment of PGE and an abrupt negative shift in bulk delta C-13. This ejecta layer is followed by 15-17 cm of thick darker, clayey mudstone, the so-called boundary clay. The upper Maastrichtian to lower Danian interval displays a succession of biostratigraphic events, such as the globally recognized spike of the dinocyst taxon Manumiella druggii in the Maastrichtian, followed by the extinction of Cretaceous planktic foraminifera at the K-Pg boundary, and a subsequent rapid succession of First Occurrences (FOs) of dinocysts, such as Senoniasphaera inornata, Membranilarnacia? tenella and Damassadinium californicum and planktic foraminifera, including Parvularugoglobigerina eugubina and Subbotina triloculinoides in the lower Danian. Overall the sedimentological and palaeontological data suggest that the studied sites in the Mudurnu-Goynuk basin were deposited under normal marine conditions, likely in an outer neritic to upper bathyal environment. Our geochemical and biostratigraphic characterization of the K-Pg boundary transition in the Mudurnu-Goynuk basin provides a new K-Pg boundary record in the Northern branch of the Neo-Tethys and allows a detailed comparison with K-Pg boundary sections worldwide. (C) 2014 Elsevier Ltd. All rights reserved.	[Acikalin, Sanem] Badley Ashton & Associates Ltd, Horncastle, Leics, England; [Vellekoop, Johan; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Utrecht, Netherlands; [Ocakoglu, Faruk] Eskisehir Osmangazi Univ, Dept Geol Engn, Eskisehir, Turkey; [Yilmaz, I. Omer; Altiner, Sevinc O.] Middle E Tech Univ, Dept Geol Engn, TR-06531 Ankara, Turkey; [Smit, Jan; Vonhof, Hubert] Vrije Univ Amsterdam, Fac Earth & Life Sci, Amsterdam, Netherlands; [Goderis, Steven] Vrije Univ Brussel, Brussels, Belgium; [Goderis, Steven] Univ Ghent, Dept Analyt Chem, B-9000 Ghent, Belgium; [Speijer, Robert P.; Woelders, Lineke] KU Leuven Univ, Div Geol, Dept Earth & Environm Sci, Leuven, Belgium; [Fornaciari, Eliana] Univ Padua, Dept Geosci, Padua, Italy	Utrecht University; Eskisehir Osmangazi University; Middle East Technical University; Vrije Universiteit Amsterdam; Vrije Universiteit Brussel; Ghent University; KU Leuven; University of Padua	Açikalin, S (通讯作者)，Badley Ashton & Associates Ltd, Winceby House, Horncastle, Leics, England.	sanemacikalin@gmail.com	Brinkhuis, Henk/IUO-8165-2023; Speijer, Robert/H-5073-2016; , OMER/AAZ-9186-2020; Vellekoop, Johan/L-1805-2019; ALTINER, Sevinç/ABA-2728-2020; Vellekoop, Johan/F-6466-2017; FORNACIARI, ELIANA/ACJ-1340-2022; Goderis, Steven/F-9908-2011; Ocakoglu, Faruk/C-9485-2009	Vellekoop, Johan/0000-0001-6977-693X; FORNACIARI, ELIANA/0000-0001-7369-9535; Goderis, Steven/0000-0002-6666-7153; Vonhof, Hubert/0000-0002-0897-8244; Acikalin, Sanem/0000-0001-7700-3363; Brinkhuis, Henk/0000-0003-0253-6610; Ocakoglu, Faruk/0000-0002-4619-5865; Smit, Jan/0000-0002-6070-4865	Commision for Scientific Research Projects, Eskisehir Osmangazi University (ESOGU-BAP) [200715024]; Scientific and Technological Research Council of Turkey (TUBITAK) [104Y153]; Netherlands Organisation for Scientific Research (NWO open competition grant) [ALWPJ/09047]; Research Foundation Flanders (FWO grant) [G.0B85.13, G009113]	Commision for Scientific Research Projects, Eskisehir Osmangazi University (ESOGU-BAP); Scientific and Technological Research Council of Turkey (TUBITAK)(Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK)); Netherlands Organisation for Scientific Research (NWO open competition grant)(Netherlands Organization for Scientific Research (NWO)); Research Foundation Flanders (FWO grant)(FWO)	This study is supported by Commision for Scientific Research Projects, Eskisehir Osmangazi University (ESOGU-BAP; Project no: 200715024), The Scientific and Technological Research Council of Turkey (TUBITAK; Project no:104Y153), the Netherlands Organisation for Scientific Research (NWO open competition grant ALWPJ/09047) and the Research Foundation Flanders (FWO grant G.0B85.13 and G009113). S.G.is a postdoctoral fellow of the Reserach Foundation Flanders (FWO). The authors would like to acknowledge field and laboratory assistance of Osman Kir, Matthieu Cartigny and Tjerk Veenstra. We would like to thank to two anonymous reviewers and the Editor in Chief, Eduardo Koutsoukos for their constructive comments.	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Res.	JAN	2015	52		A				251	267		10.1016/j.cretres.2014.07.011	http://dx.doi.org/10.1016/j.cretres.2014.07.011			17	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	AY6GY		Green Accepted			2025-03-11	WOS:000347666300020
J	Li, Z; Shin, HH; Lee, T; Han, MS				Li, Zhun; Shin, Hyeon Ho; Lee, Taehee; Han, Myung-Soo			Resting stages of freshwater algae from surface sediments in Paldang Dam Lake, Korea	NOVA HEDWIGIA			English	Article						resting-stage algae; morphology; freshwater; surface sediment	DINOFLAGELLATE CYSTS; AKINETE DIFFERENTIATION; VEGETATIVE POPULATION; GERMINATION; CRYPTOPHYCEAE; SEQUENCES; RESERVOIR; PATTERNS; ECOLOGY; LIGHT	Although the studies on marine cysts are quite frequent, information on resting stages of freshwater algae are rather scarce. The present study focused on the identification of resting-stage algae from freshwater sediments in Paldang Dam Lake, an important source of water for South Korea. We examined the morphological characteristics of resting-stage specimens and identified them by germination experiments or DNA analysis. Surface sediment samples were collected from 12 sites in Paldang Dam Lake from July 2009 to June 2010. Thirty-five resting stage morphotypes were identified: 19 chlorophytes, 6 dinoflagellates, 5 diatoms, 2 cyanobacteria, 2 euglenoids and 1 cryptophyte. Resting-stage and vegetative cells of five chlorophyte morphotypes could not be identified by morphology. These specimens were identified by molecular sequence analysis based on the nuclear-encoded SSU rDNA sequences of Polyedriopsis, Oogamochlamys and Chlamydomonas. Our samples included resting-stage of the potentially toxic species Cylindrospennum stagnale, the first recorded sighting in Korea. Resting-stage assemblages were dominated by diatoms, which ranged from 560 to 2750 cells g(-1). Resting-stage of diatoms and cyanobacteria were abundant along the eastern shore toward the southern part of Paldang Dam Lake, where there have been periodic algal blooms.	[Li, Zhun; Han, Myung-Soo] Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; [Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656830, South Korea; [Lee, Taehee] Korea Inst Ocean Sci & Technol, Maritime Secur Res Ctr, Ansan 426744, South Korea	Hanyang University; Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST)	Han, MS (通讯作者)，Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea.	hanms@.hanyang.ac.kr	LI, ZHUN/GLT-3478-2022	Shin, Hyeon Ho/0000-0002-9711-6717; LI, ZHUN/0000-0001-8961-9966	Korea Ministry of Environment [2013001470001]	Korea Ministry of Environment(Ministry of Environment (ME), Republic of Korea)	This study has been supported by Korea Ministry of Environment (2013001470001).	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A., 1973, BRIT PHYCOL J, V8, P105, DOI DOI 10.1080/00071617300650141; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Wall D., 1971, Geoscience Man, V3, P1; Wood SA, 2007, TOXICON, V50, P292, DOI 10.1016/j.toxicon.2007.03.025	59	8	9	5	35	GEBRUDER BORNTRAEGER	STUTTGART	JOHANNESSTR 3A, D-70176 STUTTGART, GERMANY	0029-5035			NOVA HEDWIGIA	Nova Hedwigia		2015	101	3-4					475	500		10.1127/nova_hedwigia/2015/0284	http://dx.doi.org/10.1127/nova_hedwigia/2015/0284			26	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	CW5WI					2025-03-11	WOS:000365066900016
J	Boonstra, M; Ramos, MIF; Lammertsma, EI; Antoine, PO; Hoorn, C				Boonstra, M.; Ramos, M. I. F.; Lammertsma, E. I.; Antoine, P. -O.; Hoorn, C.			Marine connections of Amazonia: Evidence from foraminifera and dinoflagellate cysts (early to middle Miocene, Colombia/Peru)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Pebas; Marginal marine; Neogene; Micropaleontology; Marine palynomorphs	CHACO FORELAND BASIN; MADRE-DE-DIOS; PALEOENVIRONMENTAL RECONSTRUCTION; MORPHOLOGICAL ABNORMALITIES; NORTHWESTERN AMAZONIA; PERUVIAN AMAZONIA; YECUA FORMATION; CLIMATE-CHANGE; ADRIATIC SEA; RIVER	Species composition in the present-day Amazonian heartland has an imprint of past marine influence. The exact nature, timing and extent of this marine influence, however, are largely unresolved. Here we use calcareous tests of foraminifera and marine palynomorphs from Miocene sediments in northwestern Amazonia to extend on current estimates for salinity ranges, paleoenvironments and paleogeography. Our samples mostly contain tests and/or organic linings of euryhaline (tolerant to a wide range of salinity) foraminifera of the genera Ammonia, Trochammina and Elphidium, with Ammonia being by far the dominant genus at all locations. Organic-walled dinoflagellate cysts (dinocysts), such as Spiniferites, Brigantedinium and Tuberculodinium vancampoae, are also common at a number of sites. This association of foraminifera and dinocyst taxa points at varying salinities, with aberrant forms of Ammonia indicating lower limits of 0-10 psu (practical salinity units) whereas dinocyst associations suggest more marine conditions. Such regional heterogeneity is common at the interface of shallow marine to freshwater environments, like estuaries. We conclude that during the early and middle Miocene marginal marine conditions reached at least 2000 km inland from the Caribbean portal. Global high sea level and fast subsidence in the sub-Andean zone are thought to be the controlling mechanisms of the marine incursions. Lowering of global sea level and a change in tectonic regime terminated the incursions in the course of the Plio-Pleistocene. (C) 2014 Elsevier B.V. All rights reserved.	[Boonstra, M.; Lammertsma, E. I.; Hoorn, C.] Univ Amsterdam, IBED, NL-1090 GE Amsterdam, Netherlands; [Ramos, M. I. F.] CCTE, Museu Paraense Emilio Goeldi, BR-66077830 Belem, PA, Brazil; [Antoine, P. -O.] Univ Montpellier 2, CNRS, IRD, Inst Sci Evolut,CC064, F-34095 Montpellier, France	University of Amsterdam; Museu Paraense Emilio Goeldi; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier	Hoorn, C (通讯作者)，Univ Amsterdam, IBED, POB 94248, NL-1090 GE Amsterdam, Netherlands.	M.C.Hoorn@uva.nl	Hoorn, Carina/A-9372-2015	Hoorn, Carina/0000-0001-5402-6191; ANTOINE, Pierre-Olivier/0000-0001-9122-1818	CLIM-AMAZON [295091]	CLIM-AMAZON	We are very grateful for the help we received from Suzette Flantua (map) and Jan van Arkel (photos). We thank Hubert Vonhof for the discussion and for sharing sample material; Simon Troelstra and Peter Frenzel for the advice on the classification of organic linings; Waldemar Herngreen for the initial assessment of dinocysts; Roel Verreussel for retrieving samples from the TNO repository. Roel Verreussel, Alexander Houben and Francesca Sangiorgi are acknowledged for sharing their dinocyst expertise. Francisco Parra and Rosa Navarrete have identified microfossils from Contamana, Peru. We acknowledge CLIM-AMAZON (www.clim-amazon.eu), a joint Brazilian-European facility for climate and geodynamic research on the Amazon River Basin sediment, for partially funding this work (E.L. grant 295091 and C.H. travel funds). Willem Renema, Frank Wesselingh and two anonymous reviewers are kindly thanked for their comments, which helped us to substantially improve the manuscript.	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Paleoclimatol. Paleoecol.	JAN 1	2015	417						176	194		10.1016/j.palaeo.2014.10.032	http://dx.doi.org/10.1016/j.palaeo.2014.10.032			19	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AY9HY					2025-03-11	WOS:000347862400017
J	Gu, HF; Liu, TT; Mertens, KN				Gu, Haifeng; Liu, Tingting; Mertens, Kenneth Neil			Cyst-theca relationship and phylogenetic positions of <i>Protoperidinium</i> (Peridiniales, Dinophyceae) species of the sections <i>Conica</i> and <i>Tabulata</i>, with description of <i>Protoperidinium shanghaiense</i> sp nov.	PHYCOLOGIA			English	Article						Brigantedinium majusculum; LSU rDNA; Protoperidinium biconicum; Protoperidinium conicum; Protoperidinium divaricatum; Protoperidinium humile; Protoperidinium latissimum; Protoperidinium pentagonum; Trinovantedinium applanatum	RIBOSOMAL-RNA GENE; HETEROTROPHIC DINOFLAGELLATE GENUS; RECENT SEDIMENTS; RESTING CYSTS; MIXED MODELS; SEQUENCES; JORGENSEN; PLATES	The genus Protoperidinium has been divided into several sections based on the shape of the first apical plate, the number/shape of anterior intercalary plates and the presence/absence of antapical horns/spines; however, phylogenetic relationships among these sections have not been fully explored. We examined the cyst-theca relationships of seven Protoperidinium species isolated from sediments along the Chinese coast. Ten partial nuclear-encoded large subunit ribosomal DNA (LSU rDNA) sequences were obtained by single-cell polymerase chain reaction (PCR) for seven species belonging to the Conica and Tabulata sections of the genus. New cyst-theca relationships were established for Protoperidinium biconicum and Protoperidinium humile, and the former was restricted to warmer waters. Brigantedinium majusculum was identified as the cyst of Protoperidinium pentagonum; whereas, Trinovantedinium applanatum corresponded to Protoperidinium shanghaiense sp. nov. Phylogenetic analyses based on LSU rDNA sequences were carried out using maximum likelihood and Bayesian inference and revealed that the theca-based section Conica was polyphyletic, and Tabulata was monophyletic. Surprisingly, some cyst-based genera (e.g. Brigantedinium, Selenopemphix) proved to be polyphyletic.	[Gu, Haifeng; Liu, Tingting] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Third Institute of Oceanography, Ministry of Natural Resources; Ghent University	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Mertens, Kenneth/AAO-9566-2020; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Gu, Haifeng/0000-0002-2350-9171; Mertens, Kenneth/0000-0003-2005-9483	National Natural Science Foundation of China [41376170]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank Associate Editor Ken Ishida and two anonymous reviewers for constructive suggestions that improved the manuscript. This project was supported by National Natural Science Foundation of China (41376170). Kenneth Neil Mertens is a postdoctoral fellow of FWO Belgium.	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J	Li, Z; Shin, HH; Lim, WA; Lee, T; Yoon, YH; Han, MS				Li, Zhun; Shin, Hyeon Ho; Lim, Wol-Ae; Lee, Taehee; Yoon, Yang Ho; Han, Myung-Soo			Morphology and phylogeny of <i>Pentapharsodinium jinhaense sp nov.</i> (Dinophyceae) producing a calcareous resting cyst	PHYCOLOGIA			English	Article						Dinoflagellates; Jinhae-Masan Bay; Pentapharsodinium; Resting cyst	SCRIPPSIELLA DINOPHYCEAE; MARINE DINOFLAGELLATE; THECA RELATIONSHIPS; PERIDINIALES; CALCIODINELLOIDEAE; CLASSIFICATION; TROCHOIDEA; SEDIMENTS	A new species, Pentapharsodinium jinhaense sp. nov., was established by incubating resting cysts, which were collected from trap samples from Jinhae-Masan Bay, Korea. The resting cysts of P. jinhaense were spherical or ovoidal, with a large reddish pigment body and a thick wall covered by numerous needle-shaped calcareous crystals. The size, shape and plate tabulation of motile cells that germinated from the resting cysts were similar to those of Pentapharsodinium tyrrhenicum and Ensiculifera carinata; however, the motile cells had a spine located in the anterior sulcal plate and many pores and spines on the thecal surface. Molecular phylogenetic analysis using internal transcribed spacer and 5.8s rDNA showed that P. jinhaense was closely related to P. tyrrhenicum. Large subunit ribosomal DNA sequences also revealed that P. jinhaense was nested within Pentapharsodinium and formed a strongly supported clade with Pentapharsodinium dalei and P. tyrrhenicum.	[Li, Zhun; Han, Myung-Soo] Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; [Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656830, South Korea; [Lim, Wol-Ae] Natl Fisheries Res & Dev Inst, Busan 619705, South Korea; [Lee, Taehee] Korea Inst Ocean Sci & Technol, Maritime Secur Res Ctr, Ansan 426744, South Korea; [Yoon, Yang Ho] Chonnam Natl Univ, Fac Marine Technol, Dundeok Dong 550749, Yeosu, South Korea	Hanyang University; Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); Chonnam National University	Shin, HH (通讯作者)，Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea.	shh961121@kiost.ac.kr; hanms@hanyang.ac.kr	LI, ZHUN/GLT-3478-2022	Shin, Hyeon Ho/0000-0002-9711-6717; LI, ZHUN/0000-0001-8961-9966	Korea Institute of Ocean Science and Technology [PE9931A, PE99305]; Construction test, evaluation and certification systems for USCG phase II standard - Ministry of Oceans and Fisheries, Korea [PM58580]	Korea Institute of Ocean Science and Technology; Construction test, evaluation and certification systems for USCG phase II standard - Ministry of Oceans and Fisheries, Korea	This work was supported by a grant from Korea Institute of Ocean Science and Technology (PE9931A and PE99305), and Construction test, evaluation and certification systems for USCG phase II standard (PM58580) funded by Ministry of Oceans and Fisheries, Korea.	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L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; Guindon S, 2010, SYST BIOL, V59, P307, DOI 10.1093/sysbio/syq010; INDELICATO S R, 1986, Japanese Journal of Phycology, V34, P153; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; Jeanmougin F, 1998, TRENDS BIOCHEM SCI, V23, P403, DOI 10.1016/S0968-0004(98)01285-7; Keupp H., 1991, P267; KOBAYASHI S, 1995, J PHYCOL, V31, P147, DOI 10.1111/j.0022-3646.1995.00147.x; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Li Z, 2015, PHYCOLOGIA, V54, P67, DOI 10.2216/14-080.1; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATSUOKA K, 1990, Bulletin of Plankton Society of Japan, V37, P127; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; Matsuoka K., 2000, TECHNICAL GUIDE MODE; 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, 1988, PHYCOLOGIA, V27, P387, DOI 10.2216/i0031-8884-27-3-387.1; MONTRESOR M, 1995, PHYCOLOGIA, V34, P87, DOI 10.2216/i0031-8884-34-1-87.1; MONTRESOR M, 1993, J PHYCOL, V29, P223, DOI 10.1111/j.0022-3646.1993.00223.x; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Pospelova V, 2010, MAR MICROPALEONTOL, V76, P37, DOI 10.1016/j.marmicro.2010.04.003; Ronquist F, 2003, BIOINFORMATICS, V19, P1572, DOI 10.1093/bioinformatics/btg180; Shin HH, 2014, HARMFUL ALGAE, V39, P175, DOI 10.1016/j.hal.2014.07.012; Shin HH, 2013, HARMFUL ALGAE, V28, P37, DOI 10.1016/j.hal.2013.05.011; Shin HH, 2012, MAR MICROPALEONTOL, V94-95, P72, DOI 10.1016/j.marmicro.2012.06.005; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; 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; Takano Y, 2006, J PHYCOL, V42, P251, DOI 10.1111/j.1529-8817.2006.00177.x; WALL D, 1968, Journal of Paleontology, V42, P1395; White TJ., 1990, PCR PROTOCOLS GUIDE, P315; Zinssmeister C, 2012, J PHYCOL, V48, P1107, DOI 10.1111/j.1529-8817.2012.01182.x	45	6	6	2	17	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia		2015	54	6					566	577		10.2216/15-50.1	http://dx.doi.org/10.2216/15-50.1			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	CX8ZT					2025-03-11	WOS:000365995200003
J	Coelho, ACMQ; Antonioli, L; Dino, R; Portela, HA				Meirelles Quintanilha Coelho, Ana Cristina; Antonioli, Luzia; Dino, Rodolfo; Portela, Helena Antunes			Evaluation of the potential generator Aptian-Albian oil section of the Sergipe Basin, integrating palynofacies and organic geochemistry analyses	BRAZILIAN JOURNAL OF GEOLOGY			Portuguese	Article						Sergipe Basin; organic geochemistry; petrography; palynofacies; petroleum geology; hydrocarbons		Data presented in this investigation refer to studies integrating palynofacies and organic geochemistry analyses that were performed on 51 samples of PEC-41-SE-9 well, located in the Sergipe Basin, Eastern Brazilian continental margin. It was evaluated the potential for oil generation, identifying the type and degree of maturation of the organic matter. Optical analyzes show that the organic matter is composed in greater proportion by amorphous organic matter in good preservation, with high fluorescence. It also presents a 67% average concerning the total composition of the kerogen. The phytoclasts usually are well preserved in almost all the section. The palynomorphs are composed of an association, predominantly, of spores and pollen grains of genus Classopollis, featuring a predominantly arid to semi-arid climate environment at deposition time. Presence of the dinoflagellate in the upper section displays the first marine ingressions that happened in the end of Aptian. Based on the qualitative and quantitative results of kerogen, it was possible to characterize three distinct palynofacies, in which the palynofacies I had the best features for quality and preservation of organic matter. The results show total organic carbon values up to 6.39% and Rock-Eval pyrolysis data pointed to the type II kerogen rich in organic matter suitable for the formation of hydrocarbon accumulations. The hydrogen index is found between 200 and 550 mg HC/g of total organic carbon, which shows good potential for oil and gas generation. Spore color index data conclude that the organic matter is found predominantly on the immature maturation phase, with SCI values of 4.0 to 4.5, corroborating with data of maximum temperature, of up to 432 degrees C.	[Meirelles Quintanilha Coelho, Ana Cristina] Univ Estado Rio De Janeiro, Fac Geol, Programa Posgrad Analise Bacias & Faixas Moveis, Rio De Janeiro, RJ, Brazil; [Antonioli, Luzia; Dino, Rodolfo] Univ Estado Rio De Janeiro, Fac Geol, Rio De Janeiro, RJ, Brazil; [Dino, Rodolfo] Pesquisa Desenvolvimento Gas Energia & Desenvolvi, Petrobras Ctr Pesquisas & Desenvolvimento Leopold, Rio De Janeiro, RJ, Brazil; [Portela, Helena Antunes] Univ Estado Rio De Janeiro, Fac Formacao Professores, Rio De Janeiro, RJ, Brazil	Universidade do Estado do Rio de Janeiro; Universidade do Estado do Rio de Janeiro; Universidade do Estado do Rio de Janeiro	Coelho, ACMQ (通讯作者)，Univ Estado Rio De Janeiro, Fac Geol, Programa Posgrad Analise Bacias & Faixas Moveis, Rio De Janeiro, RJ, Brazil.	anacoelho.ep@gmail.com; luantonioli@ig.com.br; dino@petrobras.com.br; helenaportela@gmail.com	Dino, Rodolfo/AAD-2105-2021; Coelho, Ana/E-4606-2012; Antonioli, Luzia/AAC-9679-2021					[Anonymous], JB GEOLOGISCHEN BUND; [Anonymous], THESIS U FEDERAL RIO; Aquino G.S., 1990, B GEOCIENCIAS PETROB, V4, P75; Bernard P.C., 1981, Organic Maturation Studies and Fossil Fuel Exploration, P337; BRENNER G J, 1968, Pollen et Spores, V10, P341; Cainelli C., 1998, AAPG INT C EXH SHO 2; COMBAZ A., 1964, REV MICROPALDONTOL, V7, P205; COMBAZ A., 1980, KEROGEN INSOLUBLE OR, P55; Cookson I. C., 1947, BA NZ ANTARCTIC RES, V2, P127; COUPER R. A., 1953, NEW ZEALAND GEOL SURV PALEONTOL BULL, V22, P1; de Lima M.R., 1980, Ameghiniana, V17, P15; DETTMANN M.E., 1963, P ROY SOC VICTORIA, V77, P1; Dino R., 1992, Tese de Doutorado; DINO R., 1994, Boletim de Geociencias da Petrobras, V8, P257; ESPITALIE J, 1985, REV I FR PETROL, V40, P563, DOI 10.2516/ogst:1985035; Espitalie J., 1977, REV I FRANC PETROLE, V32, P32; Habib D., 1969, MICROPALEONTOLOGY, V16, P345; HOROWITZ A, 1970, ISRAEL J EARTH SCI, V19, P153; Hunt J.M., 1995, PETROLEUM GEOCHEMIST, V2; Jarvie D.M., 1991, TREATISE PETROLEUM G, P113; Mendonca Filho J.G., 2009, PALINOLOGIA; Mendonca Filho J.G., 2001, 8 C BRAS GEOQ CUR PA; Miner E.L., 1935, American Midland naturalist, V16, P616; PFLUG H. D., 1953, PALAEONTOGRAPHICA, V95 B, P60; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; SRIVASTAVA SK, 1972, PALAEONTOGR ABT B, V139, P1; Szatmari P., 1980, ANAIS 31 CONGRESSE B, V1, P455; 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, Palynofacies Analysis, P153; Uesugui N., 1979, Boletim Tecnico da Petrobras, V22, P229; Welte D.H., 1984, PETROLEUM FORMATION; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	32	2	2	0	6	SOC BRASILEIRA GEOLOGIA	SAO PAULO	CAIXA POSTAL 11348, SAO PAULO, SP 05422-970, BRAZIL	2317-4889	2317-4692		BRAZ J GEOL	Braz. J. Geol.	DEC	2014	44	4					579	595		10.5327/Z23174889201400040005	http://dx.doi.org/10.5327/Z23174889201400040005			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CM6KO		Green Published, gold			2025-03-11	WOS:000357797600006
J	Sarkar, S; Saxena, RK; Sarkar, S				Sarkar, Samir; Saxena, R. K.; Sarkar, Suivian			PALYNOLOGY OF THE EOCENE SEDIMENTS OF THE WEST GARO HILLS, MEGHALAYA, NE INDIA: BIOSTRATIGRAPHIC AND PALAEOENVIRONMENTAL IMPLICATIONS	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Palynofossils; Palaeoenvironment; Benthic Foraminifera; Eocene; Meghalaya; India	NORTH CACHAR HILLS; ASSAM	The present paper deals with the palynofloral assemblages recovered from the Tura, Siju and Rewak Formations (early to late Eocene) exposed along the Tura-Dalu road, West Garo Hills, Meghalaya. The palynoflora recorded from the Tura Formation is qualitatively poor and consists mainly of pteridophyte spores, gymnospermous pollen and fungal remains. The overlying Siju Formation is dominated by dinoflagellate cysts, whereas the topmost Rewak Formation is mainly represented by pteridophytic spores and angiosperm pollen. Four distinct palynozones have been recognized on the basis of abundance and distribution of stratigraphically significant palynofossils, in ascending order. The present palynofloral data supported by benthic foraminiferal record suggest that the Siju Formation was deposited in a transgressive phase of a shallow sea. The dominance of terrestrial elements and decrease in dinocyst and benthic foraminifera populations in the overlying Rewak Formation clearly indicate the onset of a regressive phase during the sedimentation of the Rewak Formation. The Siju Formation is predominantly marine, whereas the Rewak Formation represents sediments deposited in a coastal swamp environment. The palynoflora has been compared with the Eocene assemblages recorded from other sedimentary basins of India, and based on the characteristic pollen, middle and late Eocene age have been assigned for the Siju and Rewak Formations respectively. The modern distribution of the extant counterparts of the palynotaxa indicates the prevalence of a tropical (warm-humid) climate during deposition of the Eocene rocks in the area of investigation.	[Sarkar, Samir; Saxena, R. K.; Sarkar, Suivian] 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			Council of Scientific and Industrial Research, New Delhi for the SRF (NET) fellowship [091528(0016)/2009-EMR-I]	Council of Scientific and Industrial Research, New Delhi for the SRF (NET) fellowship	The authors are thankful to the Director, Birbal Sahni Institute of Palaeobotany, Lucknow for encouragement and kind permission to publish this paper. We are very thankful to Dr. M. Shanmukhappa and Dr. Marcela Svobodova for their constructive suggestions. Suman Sarkar is also indebted to the Council of Scientific and Industrial Research, New Delhi for the SRF (NET) fellowship (Grant No. 091528(0016)/2009-EMR-I).	Ambwani K., 1993, Phytomorphology, V43, P153; [Anonymous], 1972, P SEM PAL IND STRAT; [Anonymous], 2000, Palaeobot; [Anonymous], 1962, Bulletin of the Geological Mining and Metallurgical Society of India, V25, P1; Bakshi S.K., 1974, ASPECTS APPRAISAL IN, P502; Baksi S.K., 1962, B GEOL MIN METALL SO, V26, P1; Banerjee D., 1964, B GEOL MINING METAL, V32, P1; CHAKRABORTY A., 1972, Quart. Jour. Geol. Min. Met. Soc. India, V44, P109; Chakraborty A., 1972, B ONGC, V9, P133; Chatterjee N. N., 1963, Q J GEOLOGICAL MININ, V34, P147; DUTTA S K, 1980, Biological Memoirs, V5, P56; Dutta S.K., 1970, PALAEONTOGRAPH ABTEI, V11, P1; Evans P., 1932, Trans Mining Geol. Inst. India, V27, p, P155; Ghosh A.M.N., 1954, Rec. GSI, V83, P423; Ghosh T. K., 1969, SEN MEMORIAL VOLUME, P123; HERON A. 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D., 1977, P 4 C IND MICR STRAT, p[134, 1974]; Sah SCD., 1970, POLLEN BORE HOLES JH, V18, P127; SALUJHA SK, 1972, P S PAL IND STRAT CA, P265; Salujha SK, 1974, PALAEOGENES KHASI JA, V21, P267; SAMANTA BK, 1971, J GEOL SOC INDIA, V12, P318; Santapau, 1969, J SEN MEMORIAL VOLUM, P109; SARKAR S, 1988, Palaeontographica Abteilung B Palaeophytologie, V209, P29; Sarkar S, 1997, INDIAN J PETROLEUM G, V6, P99; Sarkar Samir, 2000, Journal of the Palaeontological Society of India, V45, P137; Sarkar Samir, 2000, Himalayan Geology, V21, P167; Saxena R.K., 2000, Palaeobotanist (Lucknow), V49, P253; Saxena R.K., 1996, GEOPHYTOLOGY, V26, P19; Saxena Ramesh K., 2009, Acta Palaeobotanica, V49, P253; Sein MK, 1974, SPEC PUBL J L B SMIT, V3, P99; Singh H.P., 1992, GEOPHYTOLOGY, V22, P181; Singh H. P., 1976, J PALYNOL, V11, P43; Singh H.P., 1978, HIMAL GEOL, V8, P33; Singh HP., 1987, PALAEOBOTANIST, V35, P301; Singh R. Y., 1978, PALEOBOTANIST, V25, P475; Singh RY., 1977, Palaeobot, V23, P189; Singh RY., 1977, Palaeobot, V24, P1; Tewari B.S., 1984, J PALAEONTOLOGICAL S, V29, P43; TRIPATHI S K M, 1985, Geophytology, V15, P164; Tripathi S K M, 1984, SPECIAL PUBLICATION, P316; Trivedi GK., 1985, J INDIAN BOT SOC, V64, P66; Trivedi Gyanendra K., 2009, Sbornik Narodniho Muzea v Praze Rada B Prirodni Vedy, V65, P9; Venkatachala B.S., 1984, P 10 IND C MICR STRA, P95; VENKATACHALA B.S., 1968, Palaeobotanist, V17, P179; WALL D., 1967, PALAEONTOLOGY, V10, P95	59	8	8	0	2	PALAEONTOLOGICAL SOC INDIA	LUCKNOW	LUCKNOW UNIV, GEOLOGY DEPT, LUCKNOW, INDIA	0552-9360			J PALAEONTOL SOC IND	J. Palaeontol. Soc. India	DEC	2014	59	2					199	212						14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	AZ5FF					2025-03-11	WOS:000348245100005
J	Estebenet, MSG; Guerstein, GR; Raising, MER				Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.; Rodriguez Raising, Martin E.			Middle Eocene dinoflagellate cysts from Santa Cruz Province, Argentina: Biostratigraphy and paleoenvironment	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cyst; Middle Eocene; Southern Ocean; Paleoenvironment; Biostratigraphy	SOUTHERN-OCEAN; SEA; SEDIMENTOLOGY; STRATIGRAPHY; ANTARCTICA; GREENHOUSE; CARBON	The upper member of the Rio Turbio Formation is a well-exposed marine Eocene unit at high latitudes in Patagonia, Argentina. It holds important information helpful to reconstruct regional climate and oceanographic patterns in an area adjacent to the Drake Passage. Knowledge on the paleoenvironmental and paleoceanographic evolution of the southwestern Atlantic Ocean during the Paleogene is hindered by the lack of precise tools to date and correlate the sedimentary units. In this paper we present the dinoflagellate cyst assemblages from the upper member of the Rio Turbio Formation and compare the stratigraphic distribution of their species with the ranges proposed in the Paleogene Southern Pacific Ocean dinoflagellate cyst zonation. The abundance of Enneadocysta dictyostila, the first occurrence of Impagidinium parvireticulatum and the presence of Vozzhennikovia apertura all allow us to propose a mid-Lutetian to mid-Priabonian age (44.6 to 34 Ma) for the upper member of the Rio Turbio Formation. The study section is characterized by a middle Eocene endemic-Antarctic dinocyst assemblage. According to the dinocyst assemblages the analyzed section can be divided into four zones. Zone I is dominated by E. dictyostila, which points to a distal setting in an inner shelf environment. Zone II exhibits a high abundance of V. apertura, thus suggesting high trophic levels and cool waters in a shallow-marine, coastal environment. Zone III is dominated by I. parvireticulatum and a lower abundance of E. dictyostila, both species indicating a possible deepening of the depositional area with increasing influence of oceanic waters. Finally, Zone IV is dominated by V. apertura, indicating shallow marine waters. Our data suggest that V. apertura could have been produced by a stress-tolerant dinoflagellate species. Toward the top of the section, the samples are dominated exclusively by sporomorphs and zygospores of fresh-water green algae, which indicate a transition from a tide-dominated deltaic to a continental environment (C) 2014 Elsevier B.V. All rights reserved.	[Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.; Rodriguez Raising, Martin E.] Univ Nacl Sur, Inst Geol Sur, Dept Geol, Bahia Blanca, Buenos Aires, Argentina; [Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.] Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Estebenet, MSG (通讯作者)，Univ Nacl Sur, Inst Geol Sur, Dept Geol, San Juan 670,B8000ICN, Bahia Blanca, Buenos Aires, Argentina.	sol.gonzalezestebenet@uns.edu.ar; raquel.guerstein@uns.edu.ar; martin_rodriguezraising@yahoo.com.ar		Guerstein, G. Raquel/0000-0003-1623-1084	Agencia Nacional de Promocion Cientifica y Tecnologica [PICT 89/09]; Consejo Nacional de Investigaciones Cientificas y Tecnicas [PIP: 112-201101-00566]; Universidad Nacional del Sur [PGI 24/H101]	Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); Consejo Nacional de Investigaciones Cientificas y Tecnicas(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Universidad Nacional del Sur	The authors thank O. Cardenas for palynological technical assistance. R. Fensome and P.K. Bijl helped to considerably improve a preliminary version of the manuscript with their comments. We thank J. Cornago for the linguistic improvement of the manuscript. J. Blackford (RPP Editor), J. Pross and an anonymous reviewer critically evaluated and improved this research paper. This study was funded by grants from the Agencia Nacional de Promocion Cientifica y Tecnologica (PICT 89/09), from Consejo Nacional de Investigaciones Cientificas y Tecnicas (PIP: 112-201101-00566) and from Universidad Nacional del Sur (PGI 24/H101).	[Anonymous], 2010, Estratigrafia secuencial de los depositos marinos y continentales del Eoceno-Oligoceno temprano de la cuenca Austral, suroeste de la provincia de Santa Cruz; ARCHANGELSKY S, 1969, Ameghiniana, V6, P181; Archangelsky S., 1968, Ameghiniana, V5, P406; Arguijo M. 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Palynology	DEC	2014	211						55	65		10.1016/j.revpalbo.2014.09.002	http://dx.doi.org/10.1016/j.revpalbo.2014.09.002			11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AX8BX		Green Published			2025-03-11	WOS:000347136600004
J	Schreck, M; Matthiessen, J				Schreck, Michael; Matthiessen, Jens			<i>Batiacasphaera bergenensis</i> and <i>Lavradosphaera elongata</i> - New dinoflagellate cyst and acritarch species from the Miocene of the Iceland Sea (ODP Hole 907A)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cyst; Acritarch; Biostratigraphy; Miocene; Iceland Sea	MIDDLE MIOCENE; PLIOCENE; OCEAN; CIRCULATION; ONSET	A detailed palynological investigation of the almost continuous middle through upper Miocene sediment sequence of ODP Hole 907A in the Iceland Sea revealed the presence of a new species of the dinoflagellate cyst genus Batiacasphaera, and a new species of the acritarch genus Lavradosphaera. Batiacasphaera bergenensis sp. nov. and Lavradosphaera elongata sp.,nov. are both morphologically distinctive and have well-defined stratigraphic range tops that are independently constrained by the pristine paleomagnetic record of Hole 907A. Both species disappeared within a narrow interval across the middle to late Miocene boundary, when small-scale glaciations on Greenland were large enough to reach sea level. The distinct morphology of the proposed species and their highest occurrence in this critical interval highlights their potential for future biostratigraphic application in the Miocene of the high northern latitudes, an area important for understanding the Late Cenozoic transition into a bipolar glaciated world. (C) 2014 Elsevier B.V. All rights reserved.	[Schreck, Michael] Korea Polar Res Inst, Inchon 406860, South Korea; [Matthiessen, Jens] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, D-27568 Bremerhaven, Germany	Korea Institute of Ocean Science & Technology (KIOST); Korea Polar Research Institute (KOPRI); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Schreck, M (通讯作者)，Korea Polar Res Inst, 26 Songdomirae Ro, Inchon 406860, South Korea.	Michael.Schreck@kopri.re.kr		Matthiessen, Jens/0000-0002-6952-2494	German Research Foundation (DFG MA) [3913/2]; K-Polar project - Korea Polar Research Institute [PP13030]; Basic Research Program - Korea Polar Research Institute [PE14062]	German Research Foundation (DFG MA)(German Research Foundation (DFG)); K-Polar project - Korea Polar Research Institute; Basic Research Program - Korea Polar Research Institute	The Ocean Drilling Project provided samples used within this study. We thank Walter Hale and Alex Wulbers for technical support while sampling at the IODP Core Repository (Bremen), and Ute Bock for technical support in the SEM facility at AWI-Bremerhaven. Discussions with Stijn De Schepper (University of Bergen) and Martin J. Head (Brock University) were greatly welcomed, and the helpful comments of two anonymous reviewers are appreciated. We acknowledge the German Research Foundation (DFG) for financial support (DFG MA 3913/2), and MS is additionally grateful to funding by the K-Polar project (No. PP13030) and the Basic Research Program (No. PE14062), both supported by the Korea Polar Research Institute.	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Palaeobot. Palynology	DEC	2014	211						97	106		10.1016/j.revpalbo.2014.07.002	http://dx.doi.org/10.1016/j.revpalbo.2014.07.002			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AX8BX		Green Published			2025-03-11	WOS:000347136600008
J	Díaz, PA; Molinet, C; Seguel, M; Díaz, M; Labra, G; Figueroa, RI				Diaz, Patricio A.; Molinet, Carlos; Seguel, Miriam; Diaz, Manuel; Labra, Gissela; Figueroa, Rosa I.			Coupling planktonic and benthic shifts during a bloom of <i>Alexandrium catenella</i> in southern Chile: Implications for bloom dynamics and recurrence	HARMFUL ALGAE			English	Article						Alexandrium catenella; Dinoflagellate cysts; Resting cysts; Bloom encystment/excystment; Chilean Inland Sea	HARMFUL ALGAL BLOOMS; RECENT MARINE-SEDIMENTS; DINOFLAGELLATE SCRIPPSIELLA-HANGOEI; RESTING CYSTS; SURFACE SEDIMENTS; FUNDYENSE POPULATIONS; ENVIRONMENTAL-FACTORS; SPATIAL-DISTRIBUTION; DINOPHYCEAE; GULF	Cell abundances and distributions of Alexandrium catenella resting cysts in recent sediments were studied along time at two locations in the Chilean Inland Sea exposed to different oceanographic conditions: Low Bay, which is much more open to the ocean than the more interior and protected Ovalada Island. The bloom began in interior areas but maximum cyst concentrations were recorded in locations more open to the ocean, at the end of the Moraleda channel. Our results showed a time lapse of around 3 months from the bloom peak (planktonic population) until the number of resting cysts in the sediments reached a maximum. Three months later, less than 10% of the A. catenella cysts remained in the sediments. Maximum cyst numbers in the water column occurred one month after the planktonic peak, when no cells were present. The dinoflagellate assemblage at both study sites was dominated by heterotrophic cysts, except during the A. catenella bloom. CCA analyses of species composition and environmental factors indicated that the frequency of A. catenella blooms was associated with low temperatures, but not with salinity, chlorophyll a concentration, and predator presence (measured as clam biomass). However, resting cyst distribution was only related to cell abundance and location. The occurrence of A. catenella cysts was also associated with that of cysts from the toxic species Protoceratium reticulatum. By shedding light on the ecological requirements of A. catenella blooms, our observations support the relevance of encystment as a mechanism of bloom termination and show a very fast depletion of cysts from the sediments (<3 months), which suggest a small role for resting cyst deposits in the recurrence of A. catenella blooms in this area. (C) 2014 The Authors. Published by Elsevier B.V.	[Diaz, Patricio A.; Molinet, Carlos; Diaz, Manuel] Univ Austral Chile, Programa Invest Pesquera, Puerto Montt, Chile; [Diaz, Patricio A.; Molinet, Carlos; Diaz, Manuel] Univ Austral Chile, Inst Acuicultura, Puerto Montt, Chile; [Seguel, Miriam; Labra, Gissela] Univ Austral Chile, Ctr Reg Anal Recursos & Med Ambiente CERAM, Puerto Montt, Chile; [Diaz, Patricio A.; Figueroa, Rosa I.] Ctr Oceanog Vigo, IEO, Vigo 36390, Spain; [Figueroa, Rosa I.] Lund Univ, Dept Biol, S-22362 Lund, Sweden	Universidad Austral de Chile; Universidad Austral de Chile; Universidad Austral de Chile; Spanish Institute of Oceanography; Lund University	Díaz, PA (通讯作者)，Univ Austral Chile, Programa Invest Pesquera, Pinos S-N, Puerto Montt, Chile.	patriciodiaz@uach.cl	Menendez Gonzalez, Manuel/GSJ-2393-2022; Diaz, Patricio/B-8128-2018; Figueroa, Rosa/M-7598-2015	Diaz, Patricio/0000-0002-9403-8151; Figueroa, Rosa/0000-0001-9944-7993	FONDEF Project [MR07I1007]; BECAS-CHILE Program of the National Commission for Scientific and Technological Research (CONICYT); Formas (Sweden)	FONDEF Project(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDEF); BECAS-CHILE Program of the National Commission for Scientific and Technological Research (CONICYT); Formas (Sweden)(Swedish Research Council Formas)	We thank the Chilean Monitoring Program for monthly reports on phytoplankton distributions in Southern Chile. Jonathan Aguilar participated in field sampling. This work was funded by FONDEF Project MR07I1007 from the 2nd Program on Red Tides. P.A. Diaz is the recipient of a Ph.D. student fellowship from the BECAS-CHILE Program of the National Commission for Scientific and Technological Research (CONICYT). R.I. 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J	Drljepan, M; McCarthy, FMG; Hubeny, JB				Drljepan, Matea; McCarthy, Francine M. G.; Hubeny, J. Bradford			Natural and cultural eutrophication of Sluice Pond, Massachusetts, USA, recorded by algal and protozoan microfossils	HOLOCENE			English	Article						aridity; dinoflagellate cysts; eutrophication; Holocene; lake level; thecamoebians	DINOFLAGELLATE PERIDINIUM-GATUNENSE; THECAMOEBIANS TESTATE AMEBAS; EASTERN NORTH-AMERICA; ARCELLACEANS THECAMOEBIANS; VEGETATION DYNAMICS; WATER-QUALITY; LEVEL CHANGES; NOVA-SCOTIA; LAKE-ERIE; CYSTS	Microfossil studies from Sluice Pond, Massachusetts, identified two environmental perturbations that impacted algal and protozoan communities: (1) natural eutrophication and water column mixing driven by the mid-Holocene drought and (2) cultural eutrophication, increasing bottom water anoxia, and toxicity accompanying human settlement. SP09 KC2 from the deep basin of this partially meromictic pond has an abundant and diverse record of dinoflagellate cysts spanning 11,400 years. Bottom water anoxia appears to have prevented benthic protozoans from colonizing until lake levels fell throughout New England during the mid-Holocene drought. Lower lake levels allowed mixing of the water column and a thecamoebian fauna rich in centropyxids, Pontigulasia compressa, and Difflugia oblonga to flourish in SP09 KC2. This lowstand is marked by an unconformity spanning the mid-Holocene hemlock minimum (5400-3500 cal. BP) in SP07 PC4 and by an increase in nutrients in the water column allowing mesotrophic-eutrophic dinoflagellate taxa (Peridinium cf. gatunense and Peridinium willei) to increase at the expense of Peridinium wisconsinense. Rising lake levels in response to the warm, wet climate are recorded by increasing abundances of protozoa tolerant of lower dissolved oxygen (DO) throughout Sluice Pond similar to 2200 cal. BP - the thecamoebians Arcella vulgaris, Difflugia protaeiformis, and Cucurbitella tricuspis and the ciliate Codonella cratera. Subsequent decline in lake level associated with late Holocene aridity allowed a diverse thecamoebian community to thrive until around 300 years ago when a more intense phase of eutrophication resulted from human impact. Bottom water anoxia due to enhanced biochemical oxygen demand (BOD) is recorded by the dominance of C. tricuspis in sediments rich in ragweed pollen and other weedy plants. Peak cyst concentrations in this interval in SP07 PC4 reflect cultural eutrophication leading to high primary productivity and low DO, promoting cyst preservation. Low microfossil concentrations in the surface sediments are attributed to low DO and toxicity.	[Drljepan, Matea; McCarthy, Francine M. G.] Brock Univ, St Catharines, ON L2S 3A1, Canada; [Hubeny, J. Bradford] Salem State Univ, Salem, MA 01970 USA	Brock University; Massachusetts System of Public Higher Education; Salem State University	Drljepan, M (通讯作者)，Brock Univ, Dept Earth Sci, 500 Glenridge Ave, St Catharines, ON L2S 3A1, Canada.	md08tz@brocku.ca			Brock University Graduate Studies Research Fellowship	Brock University Graduate Studies Research Fellowship	This research was supported by the Brock University Graduate Studies Research Fellowship.	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J	Zhao, J; Wan, XQ; Xi, DP; Jing, X; Li, W; Huang, QH; Zhang, JY				Zhao Jing; Wan XiaoQiao; Xi DangPeng; Jing Xia; Li Wei; Huang QingHua; Zhang JinYan			Late Cretaceous palynology and paleoclimate change: Evidence from the SK1 (South) core, Songliao Basin, NE China	SCIENCE CHINA-EARTH SCIENCES			English	Article						Late Cretaceous; Songliao Basin; spores and pollen; dinoflagellate; paleoclimate		Cretaceous climate was warmer than today. The Songliao Basin contains one of the most important Late Cretaceous non-marine deposits in China for the research of the paleoenvironment and paleoclimate. This research is based on core samples from the SK1(S) borehole. The strata sampled are the upper part of the Quantou Formation to member 2 of the Nenjiang Formation, where spores, pollen, dinoflagellates, and other microfossils are abundantly preserved. Based on analysis of the spores and pollen fossils from the core samples, the following six fossil assemblage zones have been recognized in ascending order: The Cicatricosisporites-Cyathidites-Pinuspollenites, Schizaeoisporites-Cyathidites-Classopollis, Cyathidites-Schizaeoisporites, Schizaeoisporites-Cyathidites-Proteacidites, Proteacidites-Cyathidites-Dictyotriletes, and the Lythraites-Callistipollenites-Schizaeoisporites zones. The six fossil zones range from the late Cenomanian to early Campanian. The Late Cretaceous dinoflagellate cysts in the Songliao Basin are of high abundance and low diversity. Specific phytoplankton types reflect salinity changes of the Songliao Lake. Paleoecology of the dinoflagellates suggests that sediments of members 2 and 3 of the Yaojia Formation (K-2 y (2+3)) were deposited in a freshwater environment, whereas members 2 and 3 of the Qingshankou Formation (K-2 q (2+3)) and members 1 and 2 of the Nenjiang Formation (K-2 n (1+2)) were deposited in freshwater to brackish water environments. Combined with the paleoecology of dinoflagellates and the palynomorph biozones, valuable information of the paleoclimate was provided. The quantitative analyses of spores and pollen fossils, such as vegetation type, climate type, and humidity type, diversity and dominance, indicate a relatively sub-humid, mid-subtropical paleoclimate, with slight climatic fluctuation and/or temporal change.	[Zhao Jing; Wan XiaoQiao; Xi DangPeng; Li Wei] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Beijing 100083, Peoples R China; [Zhao Jing; Zhang JinYan] Huabei Oil Field Corp Ltd, Explorat & Dev Res Inst, Renqiu 062552, Peoples R China; [Jing Xia] Guangzhou Marine Geol Survey, Guangzhou 510075, Guangdong, Peoples R China; [Huang QingHua] Daqing Oil Field Corp Ltd, Explorat & Dev Res Inst, Daqing 163712, Peoples R China	China University of Geosciences; Sinopec; China Geological Survey; Guangzhou Marine Geological Survey; Sinopec	Wan, XQ (通讯作者)，China Univ Geosci, State Key Lab Biogeol & Environm Geol, Beijing 100083, Peoples R China.	wanxq@cugb.edu.cn			National Basic Research Program of China [2012CB822002]; National Natural Science Foundation of China [41172037]; China Geological Survey [1212011120145]; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) [123111]; Fundamental Research Funds for the Central Universities [2012011]	National Basic Research Program of China(National Basic Research Program of China); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); China Geological Survey(China Geological Survey); State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS)(Chinese Academy of Sciences); Fundamental Research Funds for the Central Universities(Fundamental Research Funds for the Central Universities)	This study was supported by National Basic Research Program of China (Grant No. 2012CB822002), National Natural Science Foundation of China (Grant No. 41172037), China Geological Survey (Grant No. 1212011120145), State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) (Grant No. 123111), and Fundamental Research Funds for the Central Universities (Grant No. 2012011). We are indebted to Profs. Wang Daning, Li Jianguo, Li Jie, and Dr. Lu Yuanzheng for their guidance in fossil identification. Special thanks go to the reviewers for the valuable advice. We acknowledge help of Dr. Robert W. Scott, the University of Tulsa, who helped with the English in the manuscript. Field and technical laboratory work was provided by the Research Institute of Petroleum Exploration and Development.	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China-Earth Sci.	DEC	2014	57	12					2985	2997		10.1007/s11430-014-4975-4	http://dx.doi.org/10.1007/s11430-014-4975-4			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AW3FE					2025-03-11	WOS:000346170700012
J	Bringué, M; Pospelova, V; Field, DB				Bringue, Manuel; Pospelova, Vera; Field, David B.			High resolution sedimentary record of dinoflagellate cysts reflects decadal variability and 20th century warming in the Santa Barbara Basin	QUATERNARY SCIENCE REVIEWS			English	Article						California Current System; Last century warming; Pacific Decadal Oscillation; El Nino-Southern Oscillation; Upwelling; Primary productivity; Lingulodinium machaerophorum; Laminated sediments	CALIFORNIA CURRENT SYSTEM; SEA-SURFACE TEMPERATURE; NORTH PACIFIC; EL-NINO; SOUTHERN CALIFORNIA; CLIMATE VARIABILITY; HYDROGRAPHIC CONDITIONS; HIGH-LATITUDES; SP NOV.; OCEAN	We present a continuous record of dinoflagellate cysts from a core of laminated sediments collected in the Santa Barbara Basin (SBB), off Southern California. The core spans the last similar to 260 years and is analysed at biennial (two-year) resolution. Variations in dinoflagellate cyst assemblages are compared with 20th century historical changes, and are used to examine changes in primary productivity and species composition, which are bound to the variability in upwelling and sea-surface temperature (SST) in the region. Cysts produced by heterotrophic dinoflagellates dominate the assemblages. In particular, Brigantedinium spp. (on average 64.2% of the assemblages) are commonly associated with high levels of primary productivity, typically observed under active upwelling conditions, when nutrient supply is higher. Other heterotrophic taxa such as cysts of Protoperidinium americanum, Protoperidinium fukuyoi, Protoperidinium minutum and Archaeperidinium saanichi, all Echinidinium species, Quinquecuspis concreta and Selenopemphix undulata are more abundant in the early part of the record (similar to 1750s-1870s). These taxa are generally associated with high primary productivity and are observed predominantly during intervals marked by relatively variable conditions of SST, stratification and nutrient loading. The 20th century is marked by an increase in several species of autotrophic affinity, primarily Lingulodinium machaerophorum and Spiniferites ramosus. In recent surface sediments from the region, these species are more abundant in the Southern California Bight, and they are associated with conditions of relaxed upwelling in the SBB (typically observed during summer and fall), when SST is higher and nutrient supply is moderate. Their increasing concentrations since the early 20th century reflect warmer SST and possibly stronger stratification during the warmest season. Taken together, the changes in cyst assemblages provide further evidence that persistently warmer conditions in the SBB began affecting marine populations by the late 1920s. Decadal-scale variations in primary productivity are encoded in the heterotrophic dinoflagellate cyst record, with higher (lower) concentrations of heterotrophic taxa occurring during "cool" ("warm") phases of the Pacific Decadal Oscillation (PDO) index. Wavelet analysis of heterotrophic taxa concentrations suggests a weaker influence of the PDO on biota of the region during the 19th century. (C) 2014 Elsevier Ltd. All rights reserved.	[Bringue, Manuel; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, Victoria, BC V8W 2Y2, Canada; [Field, David B.] Hawaii Pacific Univ, Coll Nat Sci, Kaneohe, HI 96744 USA	University of Victoria; Hawaii Pacific University	Bringué, M (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada.	mbringue@uvic.ca	Bringue, Manuel/KIH-8224-2024	Bringue, Manuel/0000-0003-4460-8344; Pospelova, Vera/0000-0003-4049-8133	Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery grant [224236]; Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) B2 fellowship; University of Victoria Bob Wright Graduate Scholarship	Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) B2 fellowship; University of Victoria Bob Wright Graduate Scholarship	This research was funded by a Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery grant (224236) to V. Pospelova. M. Bringue was supported by the Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) B2 fellowship and the University of Victoria Bob Wright Graduate Scholarship. We are grateful to Z. Gedalof (University of Guelph) for providing the Gedalof and Smith (2001) reconstructed PDO index data. We also wish to thank D. Dahn for his help in processing the samples. Finally, our thanks go to two anonymous reviewers whose comments helped improve the manuscript.	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J	Estrada, N; Ascencio, F; Shoshani, L; Contreras, RG				Estrada, Norma; Ascencio, Felipe; Shoshani, Liora; Contreras, Ruben G.			Apoptosis of hemocytes from lions-paw scallop <i>Nodipecten subnodosus</i> induced with paralyzing shellfish poison from <i>Gymnodinium catenatum</i>	IMMUNOBIOLOGY			English	Article						Apoptosis; Gonyautoxin 2/3 epimers (GTX 2/3 epimers); Gymnodinium catenatum; Hemocyte; Nodipecten subnodosus; Paralyzing shellfish poisons	INHIBITOR OKADAIC ACID; MUSSEL MYTILUS-EDULIS; ALEXANDRIUM-FUNDYENSE; CRASSOSTREA-VIRGINICA; INDIVIDUAL CELLS; EASTERN OYSTERS; DINOFLAGELLATE; EXPOSURE; HISTOPATHOLOGY; MAINTENANCE	The toxic dinoflagellate Gymnodinium catenatum produces paralyzing shellfish poisons (PSPs) that are consumed and accumulated by bivalves. Previously, we recorded a decrease in hemocytes 24 h after injection of PSPs (gonyautoxin 2/3 epimers, GTX2/3) in the adductor muscle in the lions-paw scallop Nodipecten subnodosus. In this work, qualitative and quantitative analyses, in in vivo and in vitro experiments, revealed that the lower count of hemocytes results from cells undergoing typical apoptosis when exposed to GTX 2/3 epimers. This includes visible morphological alterations of the cytoplasmic membrane, damage to the nuclear membrane, condensation of chromatin, DNA fragmentation, and release of DNA fragments into the cytoplasm. Induction of apoptosis was accompanied by phosphatidylserine exposure to the outer cell membrane and activation of cysteine-aspartic proteases, caspase 3 and caspase 8. Addition of an inhibitor of caspase to the medium suppressed activation in hemocytes exposed to the toxins, suggesting that cell death was induced by a caspase-dependent apoptotic pathway. The results are important for future investigation of the scallop's immune system and should provide new insights into apoptotic processes in immune cells of scallops exposed to PSPs. (C) 2014 Elsevier GmbH. All rights reserved.	[Estrada, Norma; Ascencio, Felipe] SC CIBNOR, Ctr Invest Biol Noroeste, La Paz 23096, Bcs, Mexico; [Shoshani, Liora; Contreras, Ruben G.] CINVESTAV, IPN, Ctr Invest & Estudios Avanzados, Mexico City 07300, DF, Mexico	CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Telefonica SA; Instituto Politecnico Nacional - Mexico; CINVESTAV - Centro de Investigacion y de Estudios Avanzados del Instituto Politecnico Nacional	Estrada, N (通讯作者)，SC CIBNOR, Ctr Invest Biol Noroeste, Calle IPN 195, La Paz 23096, Bcs, Mexico.	norma.estrada.munoz@gmail.com; rcontrer@fisio.cinvestav.mx	Contreras, Ruben G./F-2309-2018	Contreras, Ruben G./0000-0001-7311-1615	CIBNOR [AC 3.0]; Consejo Nacional de Ciencia y Tecnologia of Mexico fellowship (CONACYT) [172583]	CIBNOR; Consejo Nacional de Ciencia y Tecnologia of Mexico fellowship (CONACYT)(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	We thank Carmen Rodriguez and Eulalia Meza Chavez of the Laboratorio de Histologia e Histoquimica of Centro de Investigaciones Biologicas del Noroeste, S.C.(CIBNOR) for technical assistance and Ira Fogel of CIBNOR for valuable editorial services. Financial support was provided by CIBNOR grant AC 3.0. N.A.E. is a recipient of a Consejo Nacional de Ciencia y Tecnologia of Mexico fellowship (CONACYT 172583).	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J	Srivastava, DK; Garg, R				Srivastava, D. K.; Garg, Rahul			RECORD OF <i>EUPATAGUS</i> L. AGASSIZ, 1847 (ECHINOIDEA) FROM THE SIJU FORMATION, GARO HILLS, MEGHALAYA, INDIA	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Brissid echinoid; Eupatagus; Siju Formation; Eocene (Bartonian); Garo Hills; Meghalaya; India	PALEOGENE; EOCENE	A brissid echinoid is recorded and described from the Siju Formation exposed at about 7 km southeast of Adugiri village (along Dilni River), Garo Hills, Meghalaya, India and placed under the genus Eupatagus L. Agassiz, 1847. It is characterized by a large, oval test with mild frontal sinus; convex aboral surface; anteriorly eccentric ethmolytic apical system; long, petaloid ambulacral petals and imperforate, non crenulated tubercles. Calcareous nannofossils and dinoflagellate cysts indicate lower Bartonian age for the echinoid-bearing level of the Siju Formation.	[Srivastava, D. K.] Univ Lucknow, Dept Geol, Ctr Adv Study, Lucknow 226007, Uttar Pradesh, India; [Garg, Rahul] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Lucknow University; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Srivastava, DK (通讯作者)，Univ Lucknow, Dept Geol, Ctr Adv Study, Lucknow 226007, Uttar Pradesh, India.	deardrdk@gmail.com; rahulbsip@gmail.com						[Anonymous], MEMOIRS MUS COMP ZOO; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BERGGREN WA, 1988, MICROPALEONTOLOGY, V34, P362, DOI 10.2307/1485604; CHAKRABORTY A., 1972, Quart. Jour. Geol. Min. Met. Soc. India, V44, P109; Chakraborty A., 1972, B ONGC, V9, P133; Donovan SK, 2000, J PALEONTOL, V74, P654, DOI 10.1666/0022-3360(2000)074<0654:SEFTEO>2.0.CO;2; Duncan P. M., 1883, PAL IND, V14 1, P104; Fischer A.G., 1966, Treatise on Invertebrate Paleontology, V3, pU543; Geological Survey of India, 1976, KNOW YOUR DISTR S GA; Hottinger L., 1983, Utrecht Micropaleontological Bulletins, V30, P239; Jauhri AK, 2001, PALAEOGEOGR PALAEOCL, V168, P187, DOI 10.1016/S0031-0182(00)00255-8; Khowaja-Ateequzzaman, 2007, 21 IND C MICR STRAT, P96; McGowran B., 1991, MEMOIR GEOLOGICAL SO, V20, P21; Medlicott H.B., 1874, RECORDS GEOLOGICAL S, V7, P58; Medlicott H. B., 1868, RECORDS GEOLOGICAL S, V1, P11; Nagappa Y., 1959, Micropaleontology, v, V5, P141; Oldham T., 1863, Q J GEOL SOC, V19, P524; Rai J., 2009, P IGCP 2007 INT C GE, P275; Rai J., 2007, PALEOBOTANIST, V29, P29; SAMANTA B K, 1969, Micropaleontology (New York), V15, P325, DOI 10.2307/1484930; SAMANTA BK, 1968, GEOL MAG, V105, P124, DOI 10.1017/S0016756800052493; Serra-Kiel I, 1998, SEPM SPEC PUBLICATIO, V60; Sinha N.K., 1982, Records of the Geological Survey of India, V112, P66; Smith A.B., 2011, ECHINOID DIRECTORY; Spengler E., 1923, Palaeontologia Indica, V8, P1; Srivastava D.K., 2004, Journal of the Palaeontological Society of India, V49, P125; Srivastava D. K., 2008, EARTH SCI INDIA, V1, P83; SRIVASTAVA DK, 1981, J PALAEONTOLOGICAL S, V25, P38; Srivatava Dinesh Kumar, 2008, Revue de Paleobiologie, V27, P511; Varol O., 1998, P200	30	3	3	0	0	PALAEONTOLOGICAL SOC INDIA	LUCKNOW	LUCKNOW UNIV, GEOLOGY DEPT, LUCKNOW, INDIA	0552-9360			J PALAEONTOL SOC IND	J. Palaeontol. Soc. India	DEC	2014	59	2					227	230						4	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	AZ5FF					2025-03-11	WOS:000348245100008
J	Limoges, A; de Vernal, A; Van Nieuwenhove, N				Limoges, Audrey; de Vernal, Anne; Van Nieuwenhove, Nicolas			Long-term hydrological changes in the northeastern Gulf of Mexico (ODP-625B) during the Holocene and late Pleistocene inferred from organic-walled dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Gulf of Mexico; Last interglacial; Holocene; Dinoflagellate cysts; Paleoceanographic reconstructions	SEA-SURFACE CONDITIONS; LAST GLACIAL MAXIMUM; FRESH-WATER INPUT; NORTH-ATLANTIC; HIGH-LATITUDES; CLIMATE-CHANGE; LOOP CURRENT; ICE; VARIABILITY; MELTWATER	Palynological analyses are used in conjunction with oxygen isotopes and Mg/Ca ratios in foraminifers in order to document the response of dinoflagellate cysts (dinocysts) assemblages to changing climate conditions in the northeastern Gulf of Mexico over the Holocene and late Pleistocene. During MIS 6, but also during the cooler phases of MIS 5, lmpagidinium species and Operculodinium centrocarpum were dominating the assemblages. By contrast, during the last interglacial (LIG) and the Holocene, assemblages were mainly composed of Spiniferites taxa and characterized by high relative abundance of Spiniferites mirabilis-hyperacanthus. Operculodinium israelianum and/or Polysphaeridium zoharyi. These two periods exhibit similar to 1-2 degrees C difference in temperature as inferred from Mg/Ca ratios and show significantly distinct assemblages, with higher percentages of S. mirabilis during the LIG and higher percentages of P. zoharyi during the Holocene. This likely denotes important differences in the hydrogeographical conditions (e.g. surface circulation, bathymetric configuration) between the present and last interglacial. The importance of environmental parameters other than temperature and salinity for dinocyst assemblage dynamics is furthermore illustrated. (C) 2014 Elsevier B.V. All rights reserved.	[Limoges, Audrey; de Vernal, Anne; Van Nieuwenhove, Nicolas] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Limoges, A (通讯作者)，Univ Quebec, Geotop, CP 8888,Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.	limoges.audrey@gmail.com; devernal.anne@uqam.ca; nvannieuwenhove.geotop@gmail.com	Van Nieuwenhove, Nicolas/IAQ-1532-2023; de Vernal, Anne/D-5602-2013	Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Limoges, Audrey/0000-0002-4587-3417	Fonds de Recherche Nature et Technologies of Quebec	Fonds de Recherche Nature et Technologies of Quebec	This study was possible through the financial support of Fonds de Recherche Nature et Technologies of Quebec. We gratefully acknowledge Jean-Francois Helie, Andre Poirier and Maryse Henry for their technical and scientific support with isotopic, trace element and palynological analyses. We also thank Charlene Manceau for her help with foraminifer picking. Helpful comments by two anonymous reviewers and the associate editor Thierry Correge are thankfully acknowledged.	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Paleoclimatol. Paleoecol.	NOV 15	2014	414						178	191		10.1016/j.palaeo.2014.08.019	http://dx.doi.org/10.1016/j.palaeo.2014.08.019			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AT8SO					2025-03-11	WOS:000345202500014
J	Grosfjeld, K; De Schepper, S; Fabian, K; Husum, K; Baranwal, S; Andreassen, K; Knies, J				Grosfjeld, Kari; De Schepper, Stijn; Fabian, Karl; Husum, Katrine; Baranwal, Soma; Andreassen, Karin; Knies, Jochen			Dating and palaeoenvironmental reconstruction of the sediments around the Miocene/Pliocene boundary in Yermak Plateau ODP Hole 911A using marine palynology	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Arctic Ocean; Dinoflagellate cysts; Acritarchs; Biostratigraphy; Palaeoenvironment; Pliocene; Miocene	SEA-ICE COVER; DINOFLAGELLATE CYST STRATIGRAPHY; BASIN NORTHERN BELGIUM; ARCTIC-OCEAN; PLIOCENE-PLEISTOCENE; SURFACE TEMPERATURES; DINOCYST ASSEMBLAGES; ACRITARCH EVENTS; ATLANTIC-OCEAN; UPPER MIOCENE	The late Neogene evolution of the Arctic to Subarctic region is poorly understood due to few available records and poor age control. At the margin of the Arctic Ocean, Yermak Plateau Ocean Drilling Program (ODP) Hole 911A is strategically located for establishing a stratigraphic framework for the Arctic. Here we present dinoflagellate cyst and acritarch data from 24 stratigraphic levels in the lower part (474.26-505.64 metres below the seafloor of ODP Hole 911A The marine palynomorphs indicate a latest Miocene to earliest Pliocene age (between 5.8 and 5.0 Ma) for the base of the hole based on the co-occurrence of the dinoflagellate cyst Barssidinium evangelineae and acritarch Lavradosphaera crista. Our age estimate can possibly be further refined to 5.0-5.33 Ma based on the presence of Achomosphaera andalousiensis suttonensis, which apparently has a range restricted to the Pliocene. An age close to the Miocene/Pliocene boundary agrees with the planktonic foraminifer data. Together with recently available magnetostratigraphic data, the base of the hole is likely to be placed at similar to 5.2 Ma. This new chronostratigraphy is a first step towards a better understanding of the late Neogene palaeoenvironment for the Yermak Plateau and also for the wider Arctic to the Subarctic region. The terrestrial and fresh water palynomorphs were most likely redistributed and/or displaced from the shelf towards deeper parts of the basin during contourite deposition under the influence of the West Spitsbergen Current. The in situ marine dinoflagellate cyst assemblage contains a mixture of cool water and thermophilic taxa, indicating sea-ice free, cool-temperate, and warmer than present conditions at the Yermak Plateau. Rivers were likely the source for the freshwater influence. Warmer than present conditions may have occurred due to northward warm water transport via the West Spitsbergen Current, but also the absence of sea-ice and consequent lower albedo could have played a role. (C) 2014 Elsevier B.V. All rights reserved.	[Grosfjeld, Kari; Fabian, Karl; Baranwal, Soma; Knies, Jochen] Geol Survey Norway, N-7491 Trondheim, Norway; [De Schepper, Stijn] Univ Bergen, Dept Earth Sci, N-5007 Bergen, Norway; [De Schepper, Stijn; Andreassen, Karin] Bjerknes Ctr Climate Res, Uni Res Climate, N-5007 Bergen, Norway; [Husum, Katrine] Univ Tromso, Dept Geol, N-9037 Tromso, Norway; [Husum, Katrine] Norwegian Polar Res Inst, Fram Ctr, N-9296 Tromso, Norway; [Baranwal, Soma; Andreassen, Karin; Knies, Jochen] Univ Tromso, Ctr Arctic Gas Hydrate Environm & Climate, N-9037 Tromso, Norway	Geological Survey of Norway; University of Bergen; Bjerknes Centre for Climate Research; UiT The Arctic University of Tromso; Norwegian Polar Institute; UiT The Arctic University of Tromso	Grosfjeld, K (通讯作者)，Geol Survey Norway, POB 6315 Sluppen, N-7491 Trondheim, Norway.	kari.grosfjeld@ngu.no; stijn.deschepper@uni.no; karl.fabian@ngu.no; katrine.husum@npolar.no; soma.baranwal@ngu.no; karin.andreassen@uit.no; jochen.knies@ngu.no	Husum, Katrine/HGD-4711-2022; Fabian, Karl/AAC-8643-2022; De Schepper, Stijn/A-2836-2011	Husum, Katrine/0000-0003-1380-5900; De Schepper, Stijn/0000-0002-6934-0914; Andreassen, Karin/0000-0002-9407-526X	oil company Det Norske; oil company Statoil ASA; oil company BC Group; Norwegian Research Council through the NFR-Petromaks project "Glaciations in the Barents Sea" (NRC grant) [200672/S60]; Centre of Excellence "CAGE - Arctic Gas hydrate, Environment and Climate" (NRC grant) at the University of Tromso, Norway [223259]; NRC Grant [229819]	oil company Det Norske; oil company Statoil ASA; oil company BC Group; Norwegian Research Council through the NFR-Petromaks project "Glaciations in the Barents Sea" (NRC grant); Centre of Excellence "CAGE - Arctic Gas hydrate, Environment and Climate" (NRC grant) at the University of Tromso, Norway; NRC Grant	This research was funded by the oil companies Det Norske, Statoil ASA and BC Group and the Norwegian Research Council through the NFR-Petromaks project "Glaciations in the Barents Sea" (NRC grant 200672/S60). The study is part of the Centre of Excellence "CAGE - Arctic Gas hydrate, Environment and Climate" (NRC grant 223259) at the University of Tromso, Norway. SDS is funded through NRC Grant 229819. The samples were supplied by the Integrated Ocean Drilling Program (IODP). The staff at the Bremen Core Repository helped with the sampling. Bente Kjosnes and Melanie Mesli at the Geological Survey of Norway processed the samples. Jacques Giraudeau (University of Bordeaux, France) provided additional palynological samples. Stefan Piasecki, Michael Schreck, Stephen Louwye, and Morten Smelror helped with the identification of dinocysts and acritarchs. Andre Rochon and Martin J. Head provided constructive reviews. We sincerely thank all these contributors.	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Paleoclimatol. Paleoecol.	NOV 15	2014	414						382	402		10.1016/j.palaeo.2014.08.028	http://dx.doi.org/10.1016/j.palaeo.2014.08.028			21	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AT8SO					2025-03-11	WOS:000345202500032
J	Tabara, D				Tabara, Daniel			PALYNOLOGY, PALYNOFACIES AND ORGANIC GEOCHEMISTRY ON THE LOWER CRETACEOUS SUCCESSION (AUDIA FORMATION) FROM EASTERN CARPATHIANS, ROMANIA	CARPATHIAN JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCES			English	Article						palynology; palynofacies; organic geochemistry; Lower Cretaceous; Audia Formation	OUTER WESTERN CARPATHIANS; SEQUENCE STRATIGRAPHY; SILESIAN UNIT; BASIN; BIOSTRATIGRAPHY; FACIES	This study focused on the Cretaceous black shale from Audia Formation which cropping out in the Eastern Carpathians. This is multidisciplinary approach to the study of some samples from these formation, supported by organic petrography (palynofacies, Thermal Alteration Index TAT, fluorescence) and organic geochemistry (Total Organic Carbon - TOC). The palynofacies analysis provides evidence that the organic matter is composed of particles belonging to the amorphous organic matter group (in the middle part of the Lower Member) and opaque/translucent phytoclasts which are more numerous in the upper part of Lower Member and the Middle Member of Audia Formation. The palynological assemblage consists of dinoflagellates cysts, some with biostratigaphic importance, and continental palynomorphs such as ferns, Bryophyta and gymnosperms. The TOC data confirm that the samples have a good to very good petroleum potential, and can generate particularly wet gas, condensate or thermogenic gas, and less oil. Type III kerogen is predominant in the samples analyzed, and can be considered thermally mature (in the oil window) based on TAI values and the fluorescence of organic matter.	Alexandru Ioan Cuza Univ, Dept Geol, Iasi 700505, Romania	Alexandru Ioan Cuza University	Tabara, D (通讯作者)，Alexandru Ioan Cuza Univ, Dept Geol, 20A Carol I Blv, Iasi 700505, Romania.	dan.tabara@yahoo.com	Tabara, Daniel/C-6630-2015		project "Geological study, evaluation and possibilities of valorification a gas-bearing clays from Romania (a unconventional source) - second stage"	project "Geological study, evaluation and possibilities of valorification a gas-bearing clays from Romania (a unconventional source) - second stage"	This paper was supported by project "Geological study, evaluation and possibilities of valorification a gas-bearing clays from Romania (a unconventional source) - second stage". Author wish to thank to Prof. dr. Nicolae Anastasiu (University of Bucharest) for having provided the rock samples analyzed during the study.	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J. Earth Environ. Sci.	NOV	2014	9	4					83	91						9	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	AS9SD					2025-03-11	WOS:000344580900008
J	Wang, ZF; Yu, ZM; Song, XX; Cao, XH; Han, XT				Wang Zhifu; Yu Zhiming; Song Xiuxian; Cao Xihua; Han Xiaotian			Effects of modified clay on cysts of <i>Scrippsiella trochoidea</i> for harmful algal bloom control	CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY			English	Article						modified clay; harmful algal bloom (HAB); resting cyst; cyst formation; cyst germination; Scrippsiella trochoidea	TOXIC DINOFLAGELLATE; GONYAULAX-TAMARENSIS; RED-TIDE; DINOPHYCEAE; FLOCCULATION; SEDIMENTS; BAY	We present results on the effect of modified clay on cyst formation of Scrippsiella trochoidea in harmful algal bloom (HAB). Modified clay (in concentration of 0, 0.1, 0.5, and 1.0 g/L) were added to cultures, and observations were made on cysts of S. trochoidea under controlled laboratory conditions. Results indicate that the removal rate of algal cells reached 97.7% at the clay concentration of 1.0 g/L. The cyst formation rate increased from 4.6% to 24.6% when the concentration of clay was increased from 0 to 1.0 g/L. Two cyst metamorphs were observed: spinal calcareous cysts and smooth noncalcareous ones. The proportion of the spinal cysts decreased from 76.9% to 24.1% when clay concentration increased from 0 to 1.0 g/L. In addition, modified clay affected cyst germination. The germination rate decreased with the increases in the clay concentrations. Non-calcareous cysts had a lower germination rate with a longer germination time. We conclude that modified clay could depress algal cell multiplication and promote formation of temporal cysts of S. trochoidea, which may help in controlling HAB outbreaks.	[Wang Zhifu; Yu Zhiming; Song Xiuxian; Cao Xihua; Han Xiaotian] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Wang Zhifu] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Yu, ZM (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	zyu@qdio.ac.cn; songxx@qdio.ac.cn		Yu, Zhiming/0000-0003-0377-1129	National Natural Science Foundation of China [41276115]; Fund for Creative Research Groups by NSFC [41121064]; National Basic Research Program of China (973 Program) [2010CB428706]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Fund for Creative Research Groups by NSFC; National Basic Research Program of China (973 Program)(National Basic Research Program of China)	Supported by the National Natural Science Foundation of China (No. 41276115), the Fund for Creative Research Groups by NSFC (No. 41121064), and the National Basic Research Program of China (973 Program) (No. 2010CB428706)	Anderson DM, 1997, NATURE, V388, P513, DOI 10.1038/41415; ANDERSON DM, 1980, J PHYCOL, V16, P166; 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; Archambault MC, 2004, MAR BIOL, V144, P553, DOI 10.1007/s00227-003-1222-5; Blackburn S., 2005, Algal Culturing Techniques, P399; Cao Xi-hua, 2004, Huanjing Kexue, V25, P148; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Choi Hee Gu, 1998, Journal of the Korean Fisheries Society, V31, P109; Dale B., 1983, P69; DURR G, 1979, ARCH PROTISTENKD, V122, P121; El-Manharawy S, 2003, DESALINATION, V153, P109, DOI 10.1016/S0011-9164(02)01110-4; Elbrächter M, 2003, J PHYCOL, V39, P629, DOI 10.1046/j.1529-8817.2003.39041.x; Fang Qi, 2004, Marine Science Bulletin (Tianjin), V23, P21; Furnas Miles, 2002, P221; Gao Y H, 2007, MARINE SCI B, V26, P54; Guillard R. 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J. Oceanol. Limnol., V13, P62, DOI [10.1007/BF02845350, DOI 10.1007/BF02845350]; Yu Zhi-Ming, 1994, Chinese Journal of Oceanology and Limnology, V12, P193; Zhiming Y, 1998, OCEANOLOGIA LIMNOLOG, V29, P47	45	8	8	6	40	SCIENCE PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING, 100717, PEOPLES R CHINA	0254-4059	1993-5005		CHIN J OCEANOL LIMN	Chin. J. Oceanol. Limnol.	NOV	2014	32	6					1373	1382		10.1007/s00343-015-4008-y	http://dx.doi.org/10.1007/s00343-015-4008-y			10	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	AS9CX					2025-03-11	WOS:000344541900019
J	Wang, ZF; Yu, ZM; Song, XX; Cao, XH; Zhang, Y				Wang, Zhifu; Yu, Zhiming; Song, Xiuxian; Cao, Xihua; Zhang, Yue			Effects of ammonium and nitrate on encystment and growth of <i>Scrippsiella trochoidea</i>	CHINESE SCIENCE BULLETIN			English	Article						Nitrate; Ammonium; Encystment; Scrippsiella trochoidea	PERIDINIUM-CINCTUM; CYST FORMATION; DINOFLAGELLATE; DINOPHYCEAE; TEMPERATURE; IRRADIANCE; SEDIMENTS; DYNAMICS; NITROGEN; WILLEI	To avoid unfavorable environmental conditions, Scrippsiella trochoidea is capable of forming a resting cyst in the process of growth. In the present study, we investigated the effects of nitrate and ammonium on the growth and encystment of S. trochoidea. We incubated S. trochoidea in modified f/2 media without nitrogen and silicate in flasks. The flasks were divided into two groups. Nitrate was added as a nitrogen source in the first group, and ammonium was added in the second group. The concentrations of the nitrogen compounds were 0, 10, 30, 60, and 90 mu mol/L. The results indicate that NO3 (-)-N favors cell growth, and the cultures with a higher concentration of NO3 (-)-N were ineffective at forming cysts. In contrast, NH4 (+)-N promoted cell growth and cyst formation. At similar concentrations as NO3 (-)-N, NH4 (+)-N had a toxic effect on cell growth and increased the cyst formation ratio. Thus, the NH4 (+)-N concentration is an important factor for controlling encystment. We believe that the impact of NH4 (+)-N in inducing cyst formation may be a useful feedback mechanism in ecological systems.	[Wang, Zhifu; Yu, Zhiming; Song, Xiuxian; Cao, Xihua; Zhang, Yue] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Wang, Zhifu; Zhang, Yue] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Yu, ZM (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	zyu@qdio.ac.cn		Zhang, Yue/0000-0002-4427-6127; Yu, Zhiming/0000-0003-0377-1129	Fund for Creative Research Groups by National Natural Science Foundation of China [41121064]; "Strategic Priority Research Program" of the Chinese Academy of Sciences [XDA11020302]; National Natural Science Foundation of China [41276115]; National Basic Research Program of China [2010CB428706]	Fund for Creative Research Groups by National Natural Science Foundation of China; "Strategic Priority Research Program" of the Chinese Academy of Sciences(Chinese Academy of Sciences); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); National Basic Research Program of China(National Basic Research Program of China)	We gratefully acknowledge valuable suggestions of Professor Subbo Rao D. V. This work was supported by the Fund for Creative Research Groups by National Natural Science Foundation of China (41121064), "Strategic Priority Research Program" of the Chinese Academy of Sciences (XDA11020302), the National Natural Science Foundation of China (41276115) and the National Basic Research Program of China (2010CB428706).	ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Blackburn S., 2005, Algal Culturing Techniques, P399; CHAPMAN AD, 1995, J PHYCOL, V31, P355, DOI 10.1111/j.0022-3646.1995.00355.x; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; [邓光 Deng Guang], 2004, [武汉植物学研究, Journal of Wuhan Botanical Research], V22, P129; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Grigorszky I, 2006, HYDROBIOLOGIA, V563, P527, DOI 10.1007/s10750-006-0037-z; Grzebyk D, 1996, J PLANKTON RES, V18, P1837, DOI 10.1093/plankt/18.10.1837; GUILLARD RR, 1973, J PHYCOL, V9, P233; 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; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Jiang Han-Ming, 2004, Acta Hydrobiologica Sinica, V28, P545; Kremp A, 2000, J PLANKTON RES, V22, P2155, DOI 10.1093/plankt/22.11.2155; LHelguen S, 1996, ESTUAR COAST SHELF S, V42, P803, DOI 10.1006/ecss.1996.0051; Lourenço SO, 2002, PHYCOLOGIA, V41, P158, DOI 10.2216/i0031-8884-41-2-158.1; Lundgren V, 2011, AQUAT MICROB ECOL, V63, P231, DOI 10.3354/ame01497; PFIESTER LA, 1976, J PHYCOL, V12, P234; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Qi Yuzao, 1997, Oceanologia et Limnologia Sinica, V28, P588; Rao DVS, 2011, HARMFUL ALGAE, V10, P512, DOI 10.1016/j.hal.2011.04.001; Rintala JM, 2007, MAR BIOL, V152, P57, DOI 10.1007/s00227-007-0652-x; Shikata T, 2008, J OCEANOGR, V64, P355, DOI 10.1007/s10872-008-0028-y; Shumway SE, 2003, HARMFUL ALGAE, V2, P1, DOI 10.1016/S1568-9883(03)00002-7; Stosch H.A. von., 1973, British phycol J, V8, P105; Tang YZ, 2012, HARMFUL ALGAE, V20, P71, DOI 10.1016/j.hal.2012.08.001; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x; Wang ZH, 2007, J PLANKTON RES, V29, P209, DOI 10.1093/plankt/fbm008	28	9	12	4	41	SCIENCE PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA	1001-6538	1861-9541		CHINESE SCI BULL	Chin. Sci. Bull.	NOV	2014	59	33					4491	4497		10.1007/s11434-014-0486-0	http://dx.doi.org/10.1007/s11434-014-0486-0			7	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	AS5PD					2025-03-11	WOS:000344321500015
J	Woods, MA; Vandenbroucke, TRA; Williams, M; Riding, JB; De Schepper, S; Sabbe, K				Woods, Mark A.; Vandenbroucke, Thijs R. A.; Williams, Mark; Riding, James B.; De Schepper, Stijn; Sabbe, Koen			Complex response of dinoflagellate cyst distribution patterns to cooler early Oligocene oceans	EARTH-SCIENCE REVIEWS			English	Article						Dinoflagellate cysts; Eocene; Oligocene; Palaeoclimatology	MIDDLE EOCENE; SOUTHERN-OCEAN; ANTARCTIC GLACIATION; MARINE-SEDIMENTS; ATMOSPHERIC CO2; WESTERN TETHYS; PACIFIC-OCEAN; NORTH-SEA; TRANSITION; BIOSTRATIGRAPHY	Previous studies have made extensive use of dinoflagellate cysts to reconstruct past sea surface temperature (SST). Analysis of associations of dinoflagellate cysts using two new ocean datasets for the mid Eocene (Bartonian) and early Oligocene (Rupelian) reveals clear latitudinally constrained distributions for the Bartonian, but unexpected changes in their Rupelian distribution; a significant number of species with low and mid latitude northern hemisphere occurrences in the Bartonian extend their northward ranges in the Rupelian, including some forms characterised as 'warm water' by previous studies. This suggests either that dinoflagellates are faithfully tracking a complex oceanographic response to Rupelian cooling, or that dinoflagellate sensitivity/adaptability to a range of ecological variables means that at a global scale their distributions are not primarily controlled by sea surface temperature-variability. Previous use of dinoflagellate cysts for palaeoclimate work has relied on rather subjective and inconsistent identification of 'warm' and 'cold' water forms, rather than comprehensive analysis of community associations at the global-scale. It is clear from this study that a better understanding of the (palaeo-)ecology of dinoflagellates and their cysts is required. Rupelian dinoflagellate cyst distribution may reflect changes in a range of environmental variables linked to early Oligocene climate-cooling, for example changes in nutrient fluxes triggered by glacially-induced base-level fall; complex reorganisation of ocean current systems between the Bartonian and Rupelian, or muted changes to Rupelian summer SSTs in the northern hemisphere that have previously been reported. Many extant dinoflagellate species also exhibit relatively broad temperature tolerance. Moreover, they have potentially extensive cryptic diversity, and are able to produce dormant cysts during short-lived environmental deterioration, all of which may act to limit the value of undifferentiated dinoflagellate cyst assemblages for identifying climate signals. (C) 2014 The Authors. Published by Elsevier B.V. All rights reserved.	[Woods, Mark A.; Riding, James B.] British Geol Survey, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England; [Vandenbroucke, Thijs R. A.] Univ Lille 1, CNRS Geosyst, UMR 8217, F-59655 Villeneuve Dascq, France; [Williams, Mark] Univ Leicester, Dept Geol, Leicester LE1 7R11, Leics, England; [De Schepper, Stijn] Univ Bergen, Dept Earth Sci, N-5007 Bergen, Norway; [Sabbe, Koen] Univ Ghent, Dept Biol, B-9000 Ghent, Belgium	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universite de Lille; University of Leicester; University of Bergen; Ghent University	Woods, MA (通讯作者)，British Geol Survey, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England.	maw@bgs.ac.uk; Thijs.Vandenbroucke@univ-lille1.fr; mri@leicester.ac.uk; jbri@bgs.ac.uk; stijn.deschepper@geo.uib.no; Koen.Sabbe@UGent.be	Vandenbroucke, Thijs/B-7974-2009; Williams, Mark/B-7590-2009; De Schepper, Stijn/A-2836-2011	Vandenbroucke, Thijs/0000-0002-8182-3708; Williams, Mark/0000-0002-7987-6069; De Schepper, Stijn/0000-0002-6934-0914	BGS Climate Change Research Programme; French "Agence Nationale de la Recherche" through "SeqStrat-Ice" [ANR-12-BS06-0014]; NERC [bgs05002] Funding Source: UKRI	BGS Climate Change Research Programme; French "Agence Nationale de la Recherche" through "SeqStrat-Ice"(Agence Nationale de la Recherche (ANR)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research was supported by the BGS Climate Change Research Programme directed by Dr Michael A. Ellis. We are grateful to Emily Peckover (University of Leicester) for assisting with data compilation, and to Stewart G. Molyneux and Ian P. Wilkinson (British Geological Survey) for early reviews of this manuscript. MAW and JBR publish with the permission of the Executive Director, British Geological Survey (NERC). TRAV acknowledges financial support from the French "Agence Nationale de la Recherche" through grant ANR-12-BS06-0014 "SeqStrat-Ice".	Alegret L, 2008, PALAEOGEOGR PALAEOCL, V269, P94, DOI 10.1016/j.palaeo.2008.08.006; Anderson JB, 2011, P NATL ACAD SCI USA, V108, P11356, DOI 10.1073/pnas.1014885108; [Anonymous], 1988, Geol. 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Rev.	NOV	2014	138						215	230		10.1016/j.earscirev.2014.02.004	http://dx.doi.org/10.1016/j.earscirev.2014.02.004			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AT6OL		Green Accepted, Green Published			2025-03-11	WOS:000345058600011
J	Daugbjerg, N; Andreasen, T; Happel, E; Pandeirada, MS; Hansen, G; Craveiro, SC; Calado, AJ; Moestrup, O				Daugbjerg, Niels; Andreasen, Toke; Happel, Elisabeth; Pandeirada, Mariana S.; Hansen, Gert; Craveiro, Sandra C.; Calado, Antonio J.; Moestrup, Ojvind			Studies on woloszynskioid dinoflagellates VII. Description of <i>Borghiella andersenii</i> sp nov.: light and electron microscopy and phylogeny based on LSU rDNA	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						asexual reproduction; Borghiella andersenii; cysts; freshwater dinoflagellates; ITS sequences; LSU rDNA; woloszynskioids	LAKE TOVEL; COMB. NOV; GEN.; DINOPHYCEAE; ULTRASTRUCTURE; TOVELLIACEAE; MORPHOLOGY; GENERA	Freshwater woloszynskioid dinoflagellates were collected independently in Scotland and Portugal and found to belong to a previously unknown species of the genus Borghiella, here described as B. andersenii. The new species differs in morphology and nuclear-encoded LSU rDNA and ITS sequences from B. dodgei and B. tenuissima, the two species presently comprising the genus Borghiella. Unusual features of the new species were observed particularly during asexual reproduction, which took place in the motile stage - as in many other dinoflagellates - or in a so-called division cyst, recalling cell division in the family Tovelliaceae. Such diversity in cell division is rarely reported in dinoflagellates. Morphologically Borghiella andersenii differs from B. tenuissima in being only slightly compressed dorsoventrally whereas the latter species is flat. The slight compression is also visible in lateral view. Borghiella andersenii and B. dodgei are more challenging to discriminate but the apical structure complex is only half the length in B. andersenii compared with B. dodgei (3-4 vs 6 mu m). This difference can only be accounted for in the scanning electron microscope. At the light microscopy level the epicone in B. andersenii is rounded whereas it is conical in B. dodgei. Sexual reproduction in Borghiella andersenii was homothallic by formation of planozygotes, followed by apparent resting cysts. Phylogenetic studies on woloszynskioids have recently shown that they comprise a polyphyletic assemblage, which has been divided into the three families Borghiellaceae, Tovelliaceae and Suessiaceae. New species of the three families are now being found rapidly in many parts of the world, proving that the techniques required to investigate these small, morphologically similar dinoflagellates are now in place and proving that such 'gymnodinioids' or 'woloszynskioids' comprise an often overlooked biological entity in both marine and freshwater biotopes. Based on LSU rDNA, B. andersenii is most closely related to B. tenuissima.	[Daugbjerg, Niels; Andreasen, Toke; Happel, Elisabeth; Hansen, Gert; Moestrup, Ojvind] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-2100 Copenhagen O, Denmark; [Pandeirada, Mariana S.; Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; [Pandeirada, Mariana S.; Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, GeoBioSci GeoTechnol & GeoEngn GeoBioTec Res Unit, P-3810193 Aveiro, Portugal	University of Copenhagen; Universidade de Aveiro; Universidade de Aveiro	Daugbjerg, N (通讯作者)，Univ Copenhagen, Dept Biol, Marine Biol Sect, Univ Pk 4, DK-2100 Copenhagen O, Denmark.	n.daugbjerg@bio.ku.dk	Bang-Andreasen, Toke/P-2749-2019; Pandeirada, Mariana/AAF-7448-2019; Hansen, Gert/P-3328-2014; Daugbjerg, Niels/D-3521-2014; Calado, Antonio Jose/D-6263-2015; Pandeirada, Mariana Sofia/E-8803-2015; Calado, Sandra Carla/A-6791-2016	Moestrup, Ojvind/0000-0003-0965-8645; Daugbjerg, Niels/0000-0002-0397-3073; Calado, Antonio Jose/0000-0002-9711-0593; Pandeirada, Mariana Sofia/0000-0001-5061-9029; Calado, Sandra Carla/0000-0002-2738-7626; Bang-Andreasen, Toke/0000-0001-7449-2886	Carlsbergfondet; Villum Kann Rasmussen Fonden; QREN-POPH - Tipologia 4.1 - Formacao Avancada [SFRH/BPD/68537/2010]; European Social Funding; Portuguese Ministry of Education and Science;  [PEst-OE/CTE/UI4035/2014]; Fundação para a Ciência e a Tecnologia [SFRH/BPD/68537/2010, PEst-OE/CTE/UI4035/2014] Funding Source: FCT	Carlsbergfondet(Carlsberg Foundation); Villum Kann Rasmussen Fonden(Villum Fonden); QREN-POPH - Tipologia 4.1 - Formacao Avancada; European Social Funding; Portuguese Ministry of Education and Science(Fundacao para a Ciencia e a Tecnologia (FCT)); ; Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	ND thanks Carlsbergfondet and Villum Kann Rasmussen Fonden for equipment grants. SCC was supported by a grant (SFRH/BPD/68537/2010) financed by QREN-POPH - Tipologia 4.1 - Formacao Avancada and by the European Social Funding and the Portuguese Ministry of Education and Science. GeoBioTec was funded by PEst-OE/CTE/UI4035/2014.	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J. Phycol.	NOV	2014	49	4					436	449		10.1080/09670262.2014.969781	http://dx.doi.org/10.1080/09670262.2014.969781			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AZ1WZ		Bronze			2025-03-11	WOS:000348027000004
J	Ouellet-Bernier, MM; de Vernal, A; Hillaire-Marcel, C; Moros, M				Ouellet-Bernier, Marie-Michele; de Vernal, Anne; Hillaire-Marcel, Claude; Moros, Matthias			Paleoceanographic changes in the Disko Bugt area, West Greenland, during the Holocene	HOLOCENE			English	Article						Baffin Bay; dinocysts; foraminifers; Holocene; sea-surface temperature; West Greenland	SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; BENTHIC FORAMINIFERA; JAKOBSHAVN ISBRAE; BAFFIN-ISLAND; ARCTIC-OCEAN; ICE-SHEET; CLIMATE VARIABILITY; SOUTHERN GREENLAND	Micropaleontological analyses of a sediment core raised in Disko Bugt (West of Greenland) were undertaken in order to document paleoceanographical changes in the eastern Baffin Bay during the Holocene. The modern analogue technique (MAT) applied to dinocyst assemblages provided information on paleo-sea-surface conditions, whereas isotopic analyses of benthic foraminifers aimed at documenting the deep' water mass occupying the site. During the earlier interval recorded (similar to 10 to similar to 7.3cal.kyrBP), important discharge of ice and meltwater from the Greenland Ice Sheet (GIS) margin, notably through the Jakobshavn Isbrae, resulted in harsh conditions with a dense sea-ice cover and low temperatures, productivity, and foraminiferal abundances. Postglacial conditions settled at similar to 7.3cal.kyrBP, with a sharp rise in dinocyst abundance and species diversity, which led to reconstruct increase in summer temperatures. We link this transition to the advection of West Greenland Current waters in the upper part of the water column after the reduction of meltwater inputs from GIS. Optimal temperature conditions reaching up to >10 degrees C were finally achieved in surface waters at similar to 6cal.kyrBP. Slight cooling pulses were then recorded at similar to 4.2-4 and similar to 1.5-1cal.kyrBP, and the final optimum recorded in surface temperature from similar to 1 to 0.8cal.kyrBP is associated with the Medieval Warm Period'. Throughout the postglacial interval, the data suggest an opposition between sea-surface temperatures and salinity, with warmer intervals being characterized by lower salinity waters, probably as a result of the higher freshwater discharge along the ice margin and notably the Jakobshavn Isbrae.	[Ouellet-Bernier, Marie-Michele; de Vernal, Anne; Hillaire-Marcel, Claude] Univ Quebec, Montreal, PQ H3C 3P8, Canada; [Moros, Matthias] Leibniz Inst Balt Sea Res Warnemunde, Rostock, Germany	University of Quebec; University of Quebec Montreal; Leibniz Institut fur Ostseeforschung Warnemunde	Ouellet-Bernier, MM (通讯作者)，Univ Quebec, Ctr Rech Geochim Isotop & Geochronol GEOTOP, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	ouellet.bernier.mm@gmail.com	de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/H-1441-2012; Hillaire-Marcel, Claude/C-9153-2013	Ouellet-Bernier, Marie-Michele/0000-0002-8776-2723; Hillaire-Marcel, Claude/0000-0002-3733-4632	Ministere du Developpement Economique, Innovation et Exportation (MDEIE); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT); Natural Sciences and Engineering Research Council of Canada (NSERC)	Ministere du Developpement Economique, Innovation et Exportation (MDEIE); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	The authors thank the Ministere du Developpement Economique, Innovation et Exportation (MDEIE) and Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT), and the Natural Sciences and Engineering Research Council of Canada (NSERC).	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Geology	AS0OY					2025-03-11	WOS:000343978500015
J	Radmacher, W; Tyszka, J; Mangerud, G; Pearce, MA				Radmacher, W.; Tyszka, J.; Mangerud, G.; Pearce, M. A.			Dinoflagellate cyst biostratigraphy of the Upper Albian to Lower Maastrichtian in the southwestern Barents Sea	MARINE AND PETROLEUM GEOLOGY			English	Article						Dinoflagellate cysts; Barents Sea; Cretaceous; Paleogene; Zonation	WEST GREENLAND; OFFSHORE NORWAY; EVOLUTION; PALYNOLOGY; PALEOGENE; MARGIN; BASIN	The present study of five wells from Upper Albian to Lower Maastrichtian succession in the southwestern Barents Sea yields the first dinoflagellate cyst-based palynological event biostratigraphy for the area. The research focuses on the Upper Cretaceous Kveite and Kviting formations due to the lack of formal palynological documentation, and enables the formation of a biozonation of greater resolution than currently achievable by micropalaeontology. Four new interval zones and one abundance subzone are described, from base upward: Palaeohystrichophora infusorioides and Palaeohystrichophora palaeoinfusa Interval Zone (intra Early Cenomanian intra Late Cenomanian), Dinopterygium alatum Interval Zone (? intra Early Coniacian-Late Santonian), Palaeoglenodinium cretaceum Interval Zone (Early Campanian), and the Chatangiella bondarenkoi Interval Zone (Late Campanian) encompassing the Heterosphaeridium bellii Abundance Subzone (intra-Late Campanian). The zones are well correlated to existing palynological zonations from the Norwegian Greenland Sea, where the previously described Subtilisphaera kalaalliti Interval Zone (intra Late Albian ?intra Early Cenomanian), Heterosphaeridium difficile Interval Zone (Middle Turonian to ?intra Early Coniacian) and Cerodinium diebelii Interval Zone (Early Maastrichtian) are recognised. These data also reveal the presence of three significant unconformities of Late Cenomanian Early Turonian, Middle Campanian and Late Maastrichtian Paleocene age. (C) 2014 Elsevier Ltd. All rights reserved.	[Radmacher, W.; Tyszka, J.] Polish Acad Sci, ING PAN Inst Geol Sci, PL-31002 Krakow, Poland; [Mangerud, G.] Univ Bergen, Dept Earth Sci, NO-5020 Bergen, Norway; [Pearce, M. A.] Evolut Appl Ltd, Liskeard PL14 3JY, Cornwall, England	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; University of Bergen	Radmacher, W (通讯作者)，ING PAN, OBK, Ul Senacka 1, PL-31002 Krakow, Poland.	ndkrol@cyf-kr.edu.pl; ndtyszka@cyf-kr.edu.pl; Gunn.Mangerud@geo.uib.no; martin@evolutionapplied.com	Mangerud, Gunn/ABD-2588-2020; Radmacher, Wiesława/ABH-7042-2020	Radmacher, Wieslawa/0000-0001-7316-3693; Pearce, Martin/0000-0001-7856-1076	EEA Financial Mechanism; Norwegian Financial Mechanism [FSS/2011/V/D3/W/0074/WS/U/0048]; ING PAN internal "MICRO" project	EEA Financial Mechanism; Norwegian Financial Mechanism; ING PAN internal "MICRO" project	The authors would like to thank Norwegian Petroleum Directorate for providing palynological slides and to Statoil ASA for providing samples. WR is grateful to Przemyslaw Gedl for introduction to the field of palynology and to Graham Bell for his continuing tremendous support and introduction to issues involving biostratigraphy at the Norwegian Continental Shelf. We thank Henk Brinkhuis for the access to the Laboratory of Palaeobotany and Palynology in Utrecht (the Netherlands) where some of the samples were been processed. We are grateful to journal reviewers for critical reading and helpful suggestions. This work was supported by technical assistance funds of the EEA Financial Mechanism and the Norwegian Financial Mechanism (Grant no. FSS/2011/V/D3/W/0074/WS/U/0048) within the framework of the Scholarship and Training Fund and partly by the ING PAN internal "MICRO" project.	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Pet. Geol.	NOV	2014	57						109	121		10.1016/j.marpetgeo.2014.04.008	http://dx.doi.org/10.1016/j.marpetgeo.2014.04.008			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AQ1GO					2025-03-11	WOS:000342530100007
J	Rudenko, O; Tarasov, PE; Bauch, HA; Taldenkova, E				Rudenko, Olga; Tarasov, Pavel E.; Bauch, Henning A.; Taldenkova, Ekaterina			A Holocene palynological record from the northeastern Laptev Sea and its implications for palaeoenvironmental research	QUATERNARY INTERNATIONAL			English	Article						Holocene; Palynological record; The Laptev Sea; Palaeoenvironments; Bond events	DINOFLAGELLATE CYST ASSEMBLAGES; LATE-QUATERNARY VEGETATION; OXYGEN-ISOTOPE RECORD; LENA RIVER DELTA; CLIMATE-CHANGE; POLLEN RECORD; ENVIRONMENTAL DYNAMICS; VERKHOYANSK MOUNTAINS; SOUTHERN SIBERIA; LAKE	A 844 cm long core PS51/118-3 (77 degrees 53.54' N; 132 degrees 11.92' E) recovered from the upper slope (122 m water depth) of the Laptev Sea (Russian Arctic) has been studied for pollen, spores and aquatic palynomorphs, including freshwater green algae and cysts of marine dinoflagellates. The age model was established on the basis of radiocarbon dates obtained on marine bivalve mollusk shells. The available dates suggest that the analyzed sediment was accumulated during the last ca. 10.8 cal. ka and reveal two intervals with markedly different sedimentation rates, reflecting the sedimentary regime changes of the Laptev Sea shelf during postglacial sea-level rise. Very high sedimentation rates (ca. 4.7 mm per year) in the lower part of the core (120-866 cm) between ca. 9.2 and 10.8 cal. ka BP reflect lower-than-present sea levels, high erosion activity and much closer position of the palaeo-shoreline with the Lena and Yana river mouths to the core site. Dramatic decrease in sedimentation rates (ca. 0.1 mm per year) during the middle and late Holocene interval reflects high sea-level and decreased amount of suspended material transported to the outer shelf by rivers. Despite the location of the core site at the continental slope and far away from the modern coastline pollen, spores and fresh-water algae constitute a major part of the microfossils throughout the whole record, indicating great impact of the Lena and Yana rivers and possibly prevalent wind regime on the pollen and non-pollen-palynomorph (NPP) assemblages. Although a number of short-term (decadal to multi-century) oscillations deviate from the mean Holocene values, pollen taxa percentages and pollen-based numerical biome reconstructions do not show very clear trends. The latter is likely a result of the mixed environmental signal and complex pollen contribution of several large environmental regions and vegetation zones of Siberia drained by the Lena and Yana rivers. The greater pollen contribution of the forested regions to the PS51/118-3 record reflects higher pollen production of the boreal trees and shrubs over the low-productive Arctic vegetation. The intervals of the relative increase in the tundra biome scores in the PS51/118-3 record reflect decreased arboreal pollen production or/and increased landscape openness within the pollen source area and can be correlated (within the uncertainty of the age models) with the cold episodes observed in the Greenland ice and North Atlantic sediment records. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.	[Rudenko, Olga] Orel State Univ, Fac Earth Sci, Oryol 302026, Russia; [Tarasov, Pavel E.] Free Univ Berlin, Inst Geol Sci, D-12249 Berlin, Germany; [Bauch, Henning A.] Mainz Acad Sci Human & Literature, Kiel, Germany; [Bauch, Henning A.] GEOMAR, Kiel, Germany; [Taldenkova, Ekaterina] Moscow MV Lomonosov State Univ, Fac Geog, Moscow, Russia	Orel State University; Free University of Berlin; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Lomonosov Moscow State University	Tarasov, PE (通讯作者)，Free Univ Berlin, Inst Geol Sci, Malteserstr 74-100, D-12249 Berlin, Germany.	olrudenko2011@yandex.ru; paveltarasov@mail.ru; hbauch@geomar.de; etaldenkova@mail.ru	Tarasov, Pavel/ABG-3993-2020; Rudenko, Olga/R-8750-2016; Taldenkova, Ekaterina/L-7853-2015	Rudenko, Olga/0000-0001-9291-3058; Taldenkova, Ekaterina/0000-0002-0959-4111; /0000-0002-7219-5009	DAAD; OSL fellowship program; German Research Foundation (DFG) [TA 540/5]; Russian Ministry for Education and Science; Russian Foundation for Basic Research [11-05-01091]	DAAD(Deutscher Akademischer Austausch Dienst (DAAD)); OSL fellowship program; German Research Foundation (DFG)(German Research Foundation (DFG)); Russian Ministry for Education and Science(Ministry of Education and Science, Russian Federation); Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	This paper was written during the stay of O. Rudenko as guest scientist at the FU-Berlin financed by DAAD and OSL fellowship program-2013. We thank our colleagues from the Leibniz Laboratory (Kiel) for conducting AMS <SUP>14</SUP>C measurements and all members of the Paleontology Section at FU Berlin for hospitality, creative working atmosphere, and technical support. The assistance of Ya. Ovsepyan (GIN RAS, Moscow) in sub-sampling of the core and N. Petrova in laboratory treatment are greatly acknowledged. We thank Dr. E. Novenko (Institute of Geography RAS, Moscow) for discussion and valuable comments. This research was supported by the German Research Foundation (DFG) via the Heisenberg Program (Grant TA 540/5 to P.E. Tarasov), the Russian Ministry for Education and Science, and the Russian Foundation for Basic Research (Grant 11-05-01091).	Alabyan A.M., 1995, Rep. 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Int.	OCT 20	2014	348						82	92		10.1016/j.quaint.2014.04.032	http://dx.doi.org/10.1016/j.quaint.2014.04.032			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AS4II					2025-03-11	WOS:000344237300007
J	Kretschmann, J; Zinssmeister, C; Gottschling, M				Kretschmann, Juliane; Zinssmeister, Carmen; Gottschling, Marc			Taxonomic clarification of the dinophyte <i>Rhabdosphaera erinaceus</i> KAMPTNER, Scrippsiella erinaceus comb. nov (Thoracosphaeraceae, Peridiniales)	SYSTEMATICS AND BIODIVERSITY			English	Article						calcareous dinoflagellates; coccoid cell; cryptic species; distribution; epitypification; morphology; phylogeny; Rhabdothorax; theca	TROCHOIDEA DINOPHYCEAE; SPECIES BOUNDARIES; RIBOSOMAL-RNA; DINOFLAGELLATE; MORPHOLOGY; CALCIODINELLOIDEAE; DIVERSITY; CYSTS	The Scrippsiella trochoidea species complex (Thoracosphaeraceae, Peridiniales) consists of a cryptic diversity and multiple species, for which established scientific names are not available at present. Previously, the name Scrippsiella trochoidea has been taxonomically clarified, leaving a reliable determination of morphologically similar, but only distantly related species impossible. We isolated and cultivated Scrippsiella erinaceus comb. nov. (strains GeoM*533 and GeoM*534) from material collected near the type locality off Rovinj, Republic of Croatia (Adriatic Sea). We barcoded the species of the Thoracosphaeraceae using rRNA sequences (including 22 new sequences) and investigated the morphology of the strains using light and electron microscopy. The Scrippsiella trochoidea species complex was composed of three primary clades, and the Adriatic strains were reliably assigned to one of them being distinct from the true Scrippsiella trochoidea. We designate an epitype for the basionym Rhabdosphaera erinaceus prepared from the strain GeoM*534. The unambiguous links between a scientific species name, its protologue, genetic characterization and spatial distribution have particular importance for character-poor, unicellular organisms such as the Dinophyceae.	[Kretschmann, Juliane; Zinssmeister, Carmen; Gottschling, Marc] Univ Munich, GeoBioctr, Dept Biol Systemat Bot & Mykol, D-80638 Munich, Germany; [Zinssmeister, Carmen] German Ctr Marine Biodivers Res DZMB, D-26382 Wilhelmshaven, Germany	University of Munich	Gottschling, M (通讯作者)，Univ Munich, GeoBioctr, Dept Biol Systemat Bot & Mykol, Menzinger Str 67, D-80638 Munich, Germany.	gottschling@bio.lmu.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	Financial support was provided by the Deutsche Forschungsgemeinschaft [grants KE 322/36, RI 1738/5 and WI 725/25] and the Munchener Universitatsgesellschaft.	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Biodivers.	OCT 2	2014	12	4					393	404		10.1080/14772000.2014.934406	http://dx.doi.org/10.1080/14772000.2014.934406			12	Biodiversity Conservation; Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Life Sciences & Biomedicine - Other Topics	AR0DC					2025-03-11	WOS:000343235600003
J	Garrett, MJ; Puchulutegui, C; Selwood, AI; Wolny, JL				Garrett, Matthew J.; Puchulutegui, Cecilia; Selwood, Andrew I.; Wolny, Jennifer L.			Identification of the harmful dinoflagellate <i>Vulcanodinium rugosum</i> recovered from a ballast tank of a globally traveled ship in Port Tampa Bay, Florida, USA	HARMFUL ALGAE			English	Article						Vulcanodinium rugosum; Ballast water; Pinnatoxin; Portimine	ALEXANDRIUM DINOPHYCEAE; GYMNODINIUM-CATENATUM; PINNATOXIN G; MARINE; TRANSPORT; COMPLEX; MUSSELS; WATER; DIVERSITY; INFERENCE	The transport of microalgae in the ballast tanks of shipping vessels is of global concern because many algal species can survive in ballast tanks as nonmotile or cyst stages increasing the likelihood of introductions into foreign ports. In 2004 a peridinoid dinoflagellate was collected and isolated from ballast residuals of the merchant vessel Southern Fighter in Port Tampa Bay, Florida, USA. Light and electron microscopy of the motile and nonmotile peridinoid cells indicated the dinoflagellate was Vulcanodinium rugosum. Bayesian and maximum-parsimony (MP) phylogenetic analyses of V. rugosum strain CCFWC516 showed that sequenced regions of its LSU and ITS matched those of V. rugosum strains from Japan but were divergent from those strains from New Zealand and France. LC-MS analyses indicated that strain CCFWC516 did not produce the neurotoxin pinnatoxin, an ability that has been reported for other strains of this species. Analyses did show, however, that strain CCFWC516 did produce portimine, a cyclic imine produced by all other strains of this species. The M/V Southern Fighter visited numerous ports along the coast of Japan and the North Sea before sailing to Florida. The phylogenetic match to Japanese strains, as well as the ship's ballast exchange history, suggests that strain CCFWC516 originated from Japan. In light of the increase in global shipping traffic, increases in vessel size and capacity, and the increased connectivity between the Pacific Ocean and the Caribbean and Gulf of Mexico that will result from the widening of the Panama Canal, the introduction of nonnative, harmful algal species is an area of heightened concern and calls for increased vigilance. (C) 2014 Elsevier B.V. All rights reserved.	[Garrett, Matthew J.; Puchulutegui, Cecilia; Wolny, Jennifer L.] Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, St Petersburg, FL 33701 USA; [Selwood, Andrew I.] Cawthorn Inst, Nelson 7010, New Zealand	Florida Fish & Wildlife Conservation Commission; Cawthron Institute	Wolny, JL (通讯作者)，Maryland Dept Nat Resources, 1919 Lincoln Dr, Annapolis, MD 21401 USA.	jennifer.wolny@maryland.gov	Selwood, Andrew/AAP-7550-2020	Selwood, Andrew/0000-0003-1399-8028; Wolny, Jennifer L./0000-0002-3556-5015	National Fish and Wildlife Foundation from the National Oceanic and Atmospheric Administration (NOAA) [2002-0005-010]; Florida Department of Environmental Protection (FDEP) [CZ616]; NOAA [NA05NOS4191074]; New Zealand Ministry for Business, Innovation and Employment [CAWX1317]	National Fish and Wildlife Foundation from the National Oceanic and Atmospheric Administration (NOAA); Florida Department of Environmental Protection (FDEP); NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); New Zealand Ministry for Business, Innovation and Employment(New Zealand Ministry of Business, Innovation and Employment (MBIE))	The authors would like to thank Bill Richardson for his leadership in the Florida Fish and Wildlife Conservation Commission's Ballast Water Project and Paula Scott for her assistance with the electron microscopy. Support for this project was provided to the Florida Fish and Wildlife Conservation Commission by the National Fish and Wildlife Foundation (Grant #2002-0005-010) under funding to the foundation from the National Oceanic and Atmospheric Administration (NOAA) and the Florida Department of Environmental Protection (FDEP Grant #CZ616). The FDEP grant agreement was funded under the Florida Coastal Zone Management Act of 1972, as amended, NOAA award No. NA05NOS4191074. This study was also supported by funding from the New Zealand Ministry for Business, Innovation and Employment (previously New Zealand Foundation for Research, Science and Technology), contract CAWX1317.	Andersen R. 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J	Hakanen, P; Suikkanen, S; Kremp, A				Hakanen, Paivi; Suikkanen, Sanna; Kremp, Anke			Allelopathic activity of the toxic dinoflagellate <i>Alexandrium ostenfeldii</i>: Intra-population variability and response of co-occurring dinoflagellates	HARMFUL ALGAE			English	Article						Allelopathic interactions; Lytic activity; Alexandrium ostenfeldii; Dinoflagellates; Baltic Sea	HARMFUL ALGAL BLOOMS; TEMPORARY CYST FORMATION; MARINE; PHYTOPLANKTON; DINOPHYCEAE; TAMARENSE; MECHANISM; ALLELOCHEMICALS; OUTCOMPETE; STRATEGY	The paralytic shellfish toxin (PST) producing dinoflagellate Alexandrium ostenfeldii forms dense, recurrent blooms during summer in shallow coastal areas of the Baltic Sea. We studied the intra-population variability of its allelochemical potency and the responses of co-occurring and potentially competing dinoflagellates to the allelochemicals. The lytic activity of 10 northern Baltic A. ostenfeldii strains was evaluated by their EC50 values (i.e. the cell concentration yielding a 50% decline in cryptophyte density), which were found to vary between 236 and 1726 cells ml(-1). When co-occurring dinoflagellates (Kryptoperidinium foliaceum, Levanderina fissa and Heterocapsa triquetra) were exposed to filtrate of A. ostenfeldii, short-term (<1 h) responses of the target species after an initial immobilization were species-specific. Almost all of the K. foliaceum cells formed cysts, L. fissa cells lost their cell shape and lysed, whereas H. triquetra cells shed their thecae. After 24 h, K. foliaceum had returned into vegetative cells and the number of immotile L. fissa and H. triquetra cells had significantly decreased. The results indicate that A. ostenfeldii can disturb the growth of competing dinoflagellates by excreting allelochemicals at bloom concentrations and that co-occurring species may develop efficient means to escape and recover from the allelochemicals, allowing them to coexist with A. ostenfeldii. (C) 2014 Elsevier B.V. All rights reserved.	[Hakanen, Paivi; Suikkanen, Sanna; Kremp, Anke] Finnish Environm Inst, Ctr Marine Res, FI-00560 Helsinki, Finland	Finnish Environment Institute	Suikkanen, S (通讯作者)，Finnish Environm Inst, Erik Palmenin Aukio 1, FI-00560 Helsinki, Finland.	sanna.suikkanen@ymparisto.fi		Suikkanen, Sanna/0000-0002-0768-8149	Academy of Finland [128833]; Finnish Cultural Foundation	Academy of Finland(Research Council of Finland); Finnish Cultural Foundation(Finnish Cultural FoundationFinnish IT center for science)	U. Tillmann and A. Weissbach are thanked for their advice during the experimental design, C. Legrand kindly provided the Rhodomonas sauna culture, and J. Tuimala is thanked for the help with statistical analysis. Financial support for this work was provided by the Academy of Finland (grant 128833 to A.K., S.S.) and Finnish Cultural Foundation for P.H.	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J	Farooqui, A; Pattan, JN; Parthiban, G; Srivastava, J; Ranjana				Farooqui, Anjum; Pattan, J. N.; Parthiban, G.; Srivastava, Jyoti; Ranjana			Palynological record of tropical rain forest vegetation and sea level fluctuations since 140 ka from sediment core, south-eastern Arabian Sea	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Late Quaternary; Palynology; Climate; Sea level; Rain forest; Southeastern-Arabian Sea	LATE QUATERNARY SEDIMENTS; WESTERN-GHATS; INDIAN-OCEAN; DINOFLAGELLATE CYSTS; PLEISTOCENE BOUNDARY; MARINE-SEDIMENTS; ISOTOPIC RECORD; MONSOON REGIME; MODERN POLLEN; OXYGEN	Palyno-chronological study of a 552 cm deep sediment core from the south-eastern Arabian Sea covers a time span of similar to 140 ka. The age estimate is based on oxygen isotopic data of planktic foraminifera. Six zones were identified on the basis of palynology covering partially MIS-6 and MIS-5 to MIS-1 (Marine Isotopic Stages). The interglacial period (MIS-5) shows high rate of sedimentation corresponding to high percentage of terrestrial rain forest pollen. The palynological study reveals highstand and intense rain forest vegetation during MIS 5a which corresponds to the similar earlier records of estuarine ecosystem on land in Kerala. The relative sea level rise and fall since similar to 140 ka have been inferred through quantitative estimate of marine versus terrestrial palynomorphs. The terrigenous non-pollen forms comprised abundant Neogene extinct nanoplanktons (Discoaster spp.) until MIS-3 which was transported from the Varkala Formation (highlands of the Kerala coast). The pollen assemblage is comparable to the present day flora in Kerala except Ongokea gore which is now present in South Africa and therefore, the provenance of pollen recorded in the studied core is Western Ghats of India. High percentage of planktic foraminifera and dinoflagellate cysts throughout the core indicates high productivity that suggests upwelling induced by seasonal reversals in the monsoon winds even during the glacial periods. Botiyococcus remains and poaceous leaf cuticles dominated by the Pooideae group in the marine realm also point towards active winter monsoon. Considerable fragmentation of rain forest took place post 74 ka and during the LGM as the sea retreated to its maximum which resulted into the vast exposure of land favoring the expanse of grassland with pockets of rain forest "plant refugia" on land. Neogene rain forest flora recorded earlier from the Varkala Formation and the present record of its existence since MIS-6 in the region provide an understanding that the monsoon circulation over southern India was similar since the Middle Miocene Climate Optimum and the flora in the South-Western Ghats is a fossil ecosystem and a relic of the Tertiary period. (c) 2014 Elsevier B.V. All rights reserved.	[Farooqui, Anjum; Srivastava, Jyoti; Ranjana] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India; [Pattan, J. N.; Parthiban, G.] CSIR, Natl Inst Oceanog, Panaji 403004, Goa, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO)	Farooqui, A (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	afarooqui_2000@yahoo.com	Srivastava, Jyoti/AAB-1612-2020	Srivastava, Jyoti/0000-0002-5264-7995				AKERS WH, 1965, SCIENCE, V149, P741, DOI 10.1126/science.149.3685.741; Aubry M.P., 1985, HDB CENOZOIC CALCARE; Banakar VK, 2005, MAR GEOL, V219, P99, DOI 10.1016/j.margeo.2005.05.004; 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; Barboni D, 1999, PALAEOGEOGR PALAEOCL, V152, P87, DOI 10.1016/S0031-0182(99)00045-0; Beaufort L, 1996, QUATERN INT, V31, P13, DOI 10.1016/1040-6182(95)00017-D; Bentaleb I, 1997, NATO ASI SER SER I, V49, P475; Bera S.K., 1997, PALEOBOTANIST, V46, P191; Bera S.K., 2000, Jour. 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Paleoclimatol. Paleoecol.	OCT 1	2014	411						95	109		10.1016/j.palaeo.2014.06.020	http://dx.doi.org/10.1016/j.palaeo.2014.06.020			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AP7PM					2025-03-11	WOS:000342269200009
J	Eidvin, T; Ullmann, CV; Dybkjær, K; Rasmussen, ES; Piasecki, S				Eidvin, Tor; Ullmann, Clemens Vinzenz; Dybkjaer, Karen; Rasmussen, Erik Skovbjerg; Piasecki, Stefan			Discrepancy between Sr isotope and biostratigraphic datings of the upper middle and upper Miocene successions (Eastern North Sea Basin, Denmark)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Strontium isotope stratigraphy; Danish Upper Oligocene-Miocene succession	LOOK-UP TABLE; STRONTIUM-ISOTOPE; CAINOZOIC STRATIGRAPHY; CONTINENTAL-SHELF; OLIGOCENE; NEOGENE; AREA; EVOLUTION; UPLIFT; CURVE	One hundred and fifty-six Sr-87/Sr-86 analyses have been performed on 129 samples from 18 outcrops and boreholes in Oligocene-Miocene deposits from Jylland, Denmark. These analyses were mainly conducted on mollusc shells but foraminiferal tests, Bolboforma and one shark tooth were also analysed. The main purpose of the study is to compare the ages of the Danish succession suggested by the biostratigraphic zonation on dinoflagellate cysts (Dybkjmr and Piasecld, 2010) with the ages based on analyses of the Sr-87/Sr-86 composition of marine calcareous fossils in the same succession. Analyses of samples from the Danish Brejning, Vejle Fjord, Klintinghoved, Arnum, Odderup, Hodde, Ornhej and Gram formations gave ages between 25.7 My (late Oligocene) and 10.3 My (late Miocene). The Sr isotope ages from the lower part of the succession, i.e. Brejning to Odderup formations, agree with the age estimates based on biostratigraphy. However, the Sr-87/Sr-86 ratios of fossil carbonates from the middle-upper Miocene, Hodde to Gram succession consistently indicate ages older than those recorded by biostratigraphy. Post-depositional processes as an explanation for this offset are inconsistent with good preservation of shell material and little reworking. A palaeoenvironmental cause for the observed mismatch is therefore indicated. Search for geological events that could explain the older ages obtained by Sr isotope compositions have not led to any conclusions and we had recognised the same problem in earlier reports and communications. We conclude that this is a general and possibly global, middle-late Miocene problem that has to be reconsidered and explained geologically. (c) 2014 The Authors. Published by Elsevier EN.	[Eidvin, Tor] Norwegian Petr Directorate, N-4003 Stavanger, Norway; [Ullmann, Clemens Vinzenz] Univ Copenhagen, Dept Geosci & Nat Resource Management, Sect Geol, IGN, DK-1350 Copenhagen K, Denmark; [Dybkjaer, Karen; Rasmussen, Erik Skovbjerg] Geol Survey Denmark & Greenland GEUS, DK-1350 Copenhagen K, Denmark; [Piasecki, Stefan] Nat Hist Museum Denmark, Geol Museum, DK-1350 Copenhagen K, Denmark	University of Copenhagen; Geological Survey Of Denmark & Greenland	Eidvin, T (通讯作者)，Norwegian Petr Directorate, Prof Olav Hanssens Vei 10,POB 600, N-4003 Stavanger, Norway.	tor.eidvin@npd.no	Ullmann, Clemens/I-3227-2019; Dybkjær, Karen/G-5223-2018	Ullmann, Clemens Vinzenz/0000-0002-5865-7289				[Anonymous], 2004, GEOL SURV DEN GREENL; [Anonymous], 2013, NPD B; Artemieva N., 2002, Bull Czech Geol Surv, V77, P303; Berthelsen A., 1992, CONTINENT REVEALED E, P153; BRAND U, 1991, GEOCHIM COSMOCHIM AC, V55, P505, DOI 10.1016/0016-7037(91)90008-S; Browning JV, 2013, GEOSPHERE, V9, P1434, DOI 10.1130/GES00857.1; Dybkjaer K, 2000, B GEOL SOC DENMARK, V47, P87; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; DYBKJAR K., 2005, P 6 PETR GEOL C LOND, P1347, DOI DOI 10.1144/0061347; Eidvin T, 2001, NORSK GEOL TIDSSKR, V81, P119; Eidvin T, 1998, NORSK GEOL TIDSSKR, V78, P99; Eidvin T, 1998, NORSK GEOL TIDSSKR, V78, P125; Eidvin T, 1999, NORSK GEOL TIDSSKR, V79, P97, DOI 10.1080/002919699433843; Eidvin T., 2013, NGF P, V1, P28; Eidvin T., 2013, NORSK GEOLOGISK FORE, P30; Eidvin T., 2010, NGF ABSTR P 29 NORD, P43; Eidvin T., 2013, NGF ABSTR P, V1, P31; Eidvin T., 2013, NORSK GEOLOGISK FORE, P29; Eidvin T, 2007, NORW J GEOL, V87, P391; Eidvin T, 2007, NORW J GEOL, V87, P75; Frei KM, 2011, APPL GEOCHEM, V26, P325, DOI 10.1016/j.apgeochem.2010.12.006; Gradstein F., 2004, A; HEILMANN-CLAUSEN C, 1985, Bulletin of the Geological Society of Denmark, V33, P287; Hinsch W., 1990, Tertiary Research, V11, P159; HODELL DA, 1994, PALEOCEANOGRAPHY, V9, P405, DOI 10.1029/94PA00292; Howarth RJ, 1997, J GEOL, V105, P441, DOI 10.1086/515938; Japsen P, 2010, PETROL GEOL CONF P, P979, DOI 10.1144/0070979; JAPSEN P, 1993, AAPG BULL, V77, P194; JENSEN LN, 1992, NORSK GEOL TIDSSKR, V72, P275; Jorgensen NO, 1999, HYDROGEOL J, V7, P533, DOI 10.1007/s100400050226; Koch B.E, 1989, GEOLOGY SOBY FASTERH; KOEPNICK RB, 1985, CHEM GEOL, V58, P55, DOI 10.1016/0168-9622(85)90027-2; Kuhlemann J, 2007, GLOBAL PLANET CHANGE, V58, P224, DOI 10.1016/j.gloplacha.2007.03.007; Laursen Gitte Vestergaard, 1999, Contributions to Tertiary and Quaternary Geology, V36, P73; LIBORIUSSEN J, 1987, TECTONOPHYSICS, V137, P21, DOI 10.1016/0040-1951(87)90310-6; Martin EE, 1999, PALEOCEANOGRAPHY, V14, P74, DOI 10.1029/1998PA900008; 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, 2001, J GEOL, V109, P155, DOI 10.1086/319243; MCARTHUR JM, 1994, TERRA NOVA, V6, P331, DOI 10.1111/j.1365-3121.1994.tb00507.x; Miller KG, 2005, SCIENCE, V310, P1293, DOI 10.1126/science.1116412; MILLER KG, 1991, J GEOPHYS RES-SOLID, V96, P6829, DOI 10.1029/90JB02015; Mogensen T.E., 1993, GENERATION ACCUMULAT, V3; MULLER C, 1993, NEWSL STRATIGR, V28, P171; Nielsen LH, 2003, GEOL SURV DEN GREENL, V1, P459; OSLICK JS, 1994, PALEOCEANOGRAPHY, V9, P427, DOI 10.1029/94PA00249; Piasecki S., 2005, GRAM BOOK PALAEONTOS, P29; Rasmussen E.S., 2010, GEOL SURE DEN GREENL, V22; Rasmussen ES, 2009, TECTONOPHYSICS, V465, P84, DOI 10.1016/j.tecto.2008.10.025; Rasmussen ES, 2004, GLOBAL PLANET CHANGE, V41, P15, DOI 10.1016/j.gloplacha.2003.08.004; Rasmussen L.B., 1966, BIOSTRATIGRAPHICAL S, V88; Rasmussen L.B., 1968, MOLLUSCAN FAUNAS B 2, V92; SCHIOLER P., 2007, GEOL SURV DEN GREENL, V12, P77; SPIEGLER D, 1992, MAR MICROPALEONTOL, V20, P45, DOI 10.1016/0377-8398(92)90008-8; Surlyk F, 2007, SEDIMENTOLOGY, V54, P405, DOI 10.1111/j.1365-3091.2006.00842.x; Thybo H, 2001, TECTONOPHYSICS, V334, P155, DOI 10.1016/S0040-1951(01)00055-5; VEJBAEK OV, 1987, TECTONOPHYSICS, V137, P221, DOI 10.1016/0040-1951(87)90321-0; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Ziegler P.A., 1990, GEOL SOC PUBL HOUSE; Ziegler P.A., 1982, GEOLOGICAL ATLAS W C	59	14	15	1	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	OCT 1	2014	411						267	280		10.1016/j.palaeo.2014.07.005	http://dx.doi.org/10.1016/j.palaeo.2014.07.005			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AP7PM		hybrid, Green Published			2025-03-11	WOS:000342269200023
J	Triantaphyllou, MV; Gogou, A; Bouloubassi, I; Dimiza, M; Kouli, K; Rousakis, G; Kotthoff, U; Emeis, KC; Papanikolaou, M; Athanasiou, M; Parinos, C; Ioakim, C; Lykousis, V				Triantaphyllou, M. V.; Gogou, A.; Bouloubassi, I.; Dimiza, M.; Kouli, K.; Rousakis, G.; Kotthoff, U.; Emeis, K. -C.; Papanikolaou, M.; Athanasiou, M.; Parinos, C.; Ioakim, C.; Lykousis, V.			Evidence for a warm and humid Mid-Holocene episode in the Aegean and northern Levantine Seas (Greece, NE Mediterranean)	REGIONAL ENVIRONMENTAL CHANGE			English	Article						Mid-Holocene; NE Mediterranean; Warm; Humid; Climate; Multiproxy	HOLOCENE CLIMATE VARIABILITY; PALEOENVIRONMENTAL EVOLUTION; DINOFLAGELLATE CYSTS; HYDROLOGICAL CHANGES; MONSOON VARIABILITY; SAPROPEL FORMATION; LATE QUATERNARY; ADRIATIC SEA; EASTERN; SEDIMENTS	Marine and terrestrial biological and biogeochemical proxies in three sediment cores from North and SE Aegean and northern Levantine Seas record continuous warm and humid conditions between 5.5 and 4.0 ka BP related to the establishment of relatively stratified conditions in the upper water column. These conditions may have resulted from the concordant albeit weak Mid-Holocene South Asian monsoon forcing, combined with lighter Etesian winds. During this interval, sea surface temperatures fluctuate in the Aegean Sea, although exhibiting a strong positive shift at similar to 4.8 ka BP. The warm and humid climatic conditions triggered upper water column stratification and enhancement of the deep chlorophyll maximum (DCM), leading to dysoxic conditions and the deposition of a sapropel-like layer, but only in the SE Aegean site. In contrast to the shallow water SE Aegean, the deeper North Aegean and the northern Levantine sites, although experiencing stratification in the upper parts of the water column, did not achieve bottom-water dysoxia. Thus, a top-bottom mechanism of stratification-DCM development accompanied by fast transport and burial of organic matter is a likely explanation for the preservation of productivity signal in the shallow sites of the SE Aegean and establishment of sapropelic conditions during the warm and humid Mid-Holocene. The termination of the Mid-Holocene warm and humid phase coincides with the "4.2 ka" climate event. Our data exhibit an N-S time transgressive aridification gradient around the Aegean Sea, most probably associated with the reorganization of the general atmospheric circulation during the Mid-Holocene.	[Triantaphyllou, M. V.; Dimiza, M.; Kouli, K.; Papanikolaou, M.; Athanasiou, M.] Univ Athens, Fac Geol & Geoenvironm, Athens 15784, Greece; [Gogou, A.; Rousakis, G.; Parinos, C.; Lykousis, V.] Hellen Ctr Marine Res, Inst Oceanog, Anavyssos 19013, Greece; [Bouloubassi, I.] Univ Paris 06, Lab Oceanog & Climat Experimentat & Approche Nume, Paris 05, France; [Kotthoff, U.] Univ Hamburg, Geol Palaontol Inst & Museum, D-20146 Hamburg, Germany; [Emeis, K. -C.] Univ Hamburg, Inst Biogeochem & Meereschem, D-20146 Hamburg, Germany; [Ioakim, C.] Inst Geol & Mineral Explorat, Olympic Village 13677, Acharnae Attiki, Greece	National & Kapodistrian University of Athens; Hellenic Centre for Marine Research; Sorbonne Universite; University of Hamburg; University of Hamburg	Triantaphyllou, MV (通讯作者)，Univ Athens, Fac Geol & Geoenvironm, Athens 15784, Greece.	mtriant@geol.uoa.gr	Triantaphyllou, Maria/AAL-7877-2021; Kouli, Katerina/M-8243-2013; Gogou, Alexandra/C-5995-2013; Dimiza, Margarita/A-6857-2015	Triantaphyllou, Maria/0000-0001-7508-7508; Parinos, Constantine/0000-0002-7700-374X; Papanikolaou, Maria/0009-0005-4380-7917; Kouli, Katerina/0000-0003-1656-1091; Gogou, Alexandra/0000-0001-7327-9223; Dimiza, Margarita/0000-0002-9809-1902; Emeis, Kay-Christian/0000-0003-0459-913X	EraNet/Marinera Medecos project; University of Athens/Kapodistrias research grant	EraNet/Marinera Medecos project; University of Athens/Kapodistrias research grant	This work has been made possible thanks to the financial support provided by the EraNet/Marinera Medecos project and University of Athens/Kapodistrias research grant. The authors kindly acknowledge Mira Bar-Matthews for providing delta<SUP>13</SUP>C data from the Soreq cave. Thoughtful discussions with Neil Roberts are greatly appreciated. Critical comments by Phil Meyers and an anonymous reviewer have proved essential in improving the manuscript.	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Envir. Chang.	OCT	2014	14	5			SI		1697	1712		10.1007/s10113-013-0495-6	http://dx.doi.org/10.1007/s10113-013-0495-6			16	Environmental Sciences; Environmental Studies	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Environmental Sciences & Ecology	AQ0EK					2025-03-11	WOS:000342455400003
J	Hssaida, T; Chahidi, S; Benzaggagh, M; Riding, JB; Oumalch, F				Hssaida, Touria; Chahidi, Soumia; Benzaggagh, Mohamed; Riding, James B.; Oumalch, Fatima			Dinoflagellate cyst assemblages of the Upper Jurassic (Oxfordian-Tithonian) from the External Rif Chain (Internal Prerif and Mesorif, Morocco) and regional comparisons	ANNALES DE PALEONTOLOGIE			French	Article						Biostratigraphy; Dinoflagellate cysts; Upper Jurassic; Internal Prerif; Mesorif; External Rif; Morocco	KIMMERIDGIAN PALYNOLOGY; SEQUENCE STRATIGRAPHY; CRETACEOUS BOUNDARY; PARIS BASIN; MIDDLE; AMMONITE; ZONES; PALYNOSTRATIGRAPHY; BIOSTRATIGRAPHY; PENINSULA	A biostratigraphic study of dinoflagellate cysts of the Upper Jurassic series from the eastern External Rif Chain, has been achieved for the first time on four outcrop sections : the DM section (Douar Marticha), the TB section (the Tarhchenna "Sof"), the KSD section (the Ref Mallou "Sof") and the Y section (Douar Lamriene) among which three sections (TB, KSD and Y) are well-dated by ammonites and calpionellids fauna. The DM and TB sections are complementary in terms of stratigraphy and correspond respectively to the upper part of the "Ferrysch" Formation, a thick shaly-silty and sandy sequence assigned to the Callovian-Oxfordian stages and to the El Gouzat limestones Formation (Kimmeridgian - Lower Tithonian age) and to the Tarhchenna many limestones Formation (Upper Tithonian age) from the EL Gouzat area (Mesorif). The KSD and Y sections are also complementary and correspond to the Kimmeridgian-Lower Tithonian Msila limestones Formation and to the overlying many limestones Massif Formation of Upper Tithonian age, outcropping in the Msila region (Internal Prerif). These four sections have shown many dinocysts rich levels, which had allowed characterizing the Middle? and Upper Oxfordian substages in the DM section. In the other sections, the dinoflagellate cyst assemblages are nearly similar to those of the Kimmeridgian-Tithonian of many sections from the Boreal, Sub-boreal and North tethyan realms, particularily from England, Russia and South-East France basin. The results of the present work confirm once again, the important value of dinoflagellate cysts, for age dating of ammonites-lacking Mesozoic sedimentary sequences and for biostratigraphic correlations. (C) 2014 Elsevier Masson SAS. All rights reserved.	[Hssaida, Touria; Chahidi, Soumia] Univ Hassan II Mohammedia, Fac Sci Ben MSik, Casablanca 20800, Morocco; [Benzaggagh, Mohamed] Univ Moulay Ismail, Fac Sci, Zitoune, Meknes, Morocco; [Riding, James B.] British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, Royaume Uni, England; [Oumalch, Fatima] Off Natl Hydrocarbures & Mines ONHYM, Rabat 10000, Morocco	Hassan II University of Casablanca; Moulay Ismail University of Meknes; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Hssaida, T (通讯作者)，Univ Hassan II Mohammedia, Fac Sci Ben MSik, Ave Cdt Driss El Harti,BP 7955, Casablanca 20800, Morocco.	touria.hssaida@gmail.com			NERC [bgs05002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Abou Ela N.M., 1990, EARTH SCI, V4, P95; Al-Saadi Hamad, 2005, Revue de Paleobiologie, V24, P225; [Anonymous], 1983, DINOFLAGELLATE OPPEL, DOI DOI 10.4095/119736; [Anonymous], 1983, GLOUCESTERSHIRE ENGL; Bailey D, 1997, P YORKS GEOL SOC, V51, P235, DOI 10.1144/pygs.51.3.235; Barski Marcin, 2004, Tomy Jurajskie, V2, P61; Barski M, 2012, REV PALAEOBOT PALYNO, V169, P38, DOI 10.1016/j.revpalbo.2011.10.009; BEJU D., 1971, Annales Instituti Geologici Publici Hungarici, V54, P275; Benzaggagh M, 1996, CR ACAD SCI II A, V322, P661; BENZAGGAGH M, 1995, CR ACAD SCI II, V320, P227; Benzaggagh M, 1997, NEWSL STRATIGR, V35, P127; Benzaggagh M., 2000, DOCUMENTS LAB GEOLOG, V152, P1, DOI 10.5169/seals-168192; Benzaggagh M., 1996, CR HEBD ACAD SCI, P681; Benzaggagh M, 2010, PALAEONTOL Z, V84, P301, DOI 10.1007/s12542-009-0045-1; Berger J.P., 1986, ABHANDLUNGEN, V172, P331; Borges MEN, 2011, REV PALAEOBOT PALYNO, V163, P190, DOI 10.1016/j.revpalbo.2010.09.006; Brideaux W.W., 1976, B GEOLOGICAL SURVEY, V259, P3; Conway B.H., 1990, ISR GEOL SURV B, V82, P1; CONWAY BH, 1978, REV PALAEOBOT PALYNO, V26, P337, DOI 10.1016/0034-6667(78)90041-6; Courtinat B., 1989, Documents des Laboratoires de Geologie de la Faculte des Sciences de Lyon, V105, P1; COURTINAT B, 1980, DOCUMENTS LABORATOIR, V78, P1; Dodekova L., 1969, Bulgarska Akademiya na Naukite, Izvestiya na Geologicheskiya Institut, Seriya Paleontologiya, v, V18, p, P13; DODEKOVA L, 1975, BULG ACAD SCI PALAEO, V2, P17; Du Chêne RJ, 2000, BULL CENT RECH ELF E, V22, P273; Dupin F., 1968, Documents du Centre National de Recherches scientifiques, V450, P1; El Beialy S.Y., 2002, Egypt. 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OCT-DEC	2014	100	4					327	342		10.1016/j.annpal.2014.03.001	http://dx.doi.org/10.1016/j.annpal.2014.03.001			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	AX0CF		Green Accepted			2025-03-11	WOS:000346620400004
J	Bosboom, R; Dupont-Nivet, G; Grothe, A; Brinkhuis, H; Villa, G; Mandic, O; Stoica, M; Huang, W; Yang, W; Guo, Z; Krijgsman, W				Bosboom, R.; Dupont-Nivet, G.; Grothe, A.; Brinkhuis, H.; Villa, G.; Mandic, O.; Stoica, M.; Huang, W.; Yang, W.; Guo, Z.; Krijgsman, W.			Linking Tarim Basin sea retreat (west China) and Asian aridification in the late Eocene	BASIN RESEARCH			English	Article							NORTHERN TIBETAN PLATEAU; OLIGOCENE TRANSITION; DINOFLAGELLATE CYST; PALEOGENE EVOLUTION; BIPOLAR GLACIATION; NORTHWESTERN CHINA; CLIMATE-CHANGE; AMERICAN-WEST; SOUTHERN ASIA; XINING BASIN	The Tarim Basin in western China formed the easternmost margin of a shallow epicontinental sea that extended across Eurasia and was well connected to the western Tethys during the Paleogene. Climate modelling studies suggest that the westward retreat of this sea from Central Asia may have been as important as the Tibetan Plateau uplift in forcing aridification and monsoon intensification in the Asian continental interior due to the redistribution of the land-sea thermal contrast. However, testing of this hypothesis is hindered by poor constraints on the timing and precise palaeogeographic dynamics of the retreat. Here, we present an improved integrated bio- and magnetostratigraphic chronological framework of the previously studied marine to continental transition in the southwest Tarim Basin along the Pamir and West Kunlun Shan, allowing us to better constrain its timing, cause and palaeoenvironmental impact. The sea retreat is assigned a latest Lutetian-earliest Bartonian age (ca. 41 Ma; correlation of the last marine sediments to calcareous nannofossil Zone CP14 and correlation of the first continental red beds to the base of magnetochron C18r). Higher up in the continental deposits, a major hiatus includes the Eocene-Oligocene transition (ca. 34 Ma). This suggests the Tarim Basin was hydrologically connected to the Tethyan marine Realm until at least the earliest Oligocene and had not yet been closed by uplift of the Pamir-Kunlun orogenic system. The westward sea retreat at ca. 41 Ma and the disconformity at the Eocene-Oligocene transition are both time-equivalent with reported Asian aridification steps, suggesting that, consistent with climate modelling results, the sea acted as an important moisture source for the Asian continental interior.	[Bosboom, R.; Dupont-Nivet, G.; Huang, W.; Krijgsman, W.] Univ Utrecht, Fac Geosci, Paleomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands; [Dupont-Nivet, G.; Huang, W.; Yang, W.; Guo, Z.] Peking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China; [Dupont-Nivet, G.; Yang, W.] Univ Rennes 1, Geosci Rennes, UMR 6118, Rennes, France; [Grothe, A.; Brinkhuis, H.] Univ Utrecht, Fac Geosci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Brinkhuis, H.] Royal Netherlands Inst Sea Res, Texel, Netherlands; [Villa, G.] Univ Parma, Dipartimento Sci Terra, I-43100 Parma, Italy; [Mandic, O.] Nat Hist Museum Vienna, Geol Palaeontol Dept, Vienna, Austria; [Stoica, M.] Univ Bucharest, Fac Geol & Geophys, Dept Geol & Paleontol, Balcescu, Romania	Utrecht University; Peking University; Universite de Rennes; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Parma; University of Bucharest	Bosboom, R (通讯作者)，Univ Utrecht, Fac Geosci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands.	r.e.bosboom@uu.nl	Stoica, Marius/N-4941-2018; Dupont-Nivet, Guillaume/HII-9066-2022; Brinkhuis, Henk/IUO-8165-2023	Dupont-Nivet, Guillaume/0000-0001-9905-9739; Brinkhuis, Henk/0000-0003-0253-6610	Netherlands Organization for Scientific Research (NWO); Molengraaff Fund (STMF); CaiYanpei programme of EGIDE/Campus France	Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); Molengraaff Fund (STMF); CaiYanpei programme of EGIDE/Campus France	This project was funded by the Netherlands Organization for Scientific Research (NWO) and the Molengraaff Fund (STMF) with grants to Roderic Bosboom and Guillaume Dupont-Nivet. We are grateful to the CaiYanpei programme of EGIDE/Campus France for collaborative support. We thank Cor Langereis, Laurie Bougeois, Gloria Heilbronn, Beibei Zhu and Ziya Yang for their contributions in the field, Tom Mullender and Mark Dekkers for their assistance in the palaeomagnetic laboratory, Giovanna Gianelli for nannofossil sample preparation, Natasja Welters for technical support during palynological sample preparation, Hemmo Abels for providing the composite lithostratigraphic log of the Xining basin and Sander Houben for valuable comments on the manuscript. There is no conflict of interest among the authors.	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OCT	2014	26	5					621	640		10.1111/bre.12054	http://dx.doi.org/10.1111/bre.12054			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AQ6ZF					2025-03-11	WOS:000342961700001
J	Shin, HH; Baek, SH; Li, Z; Han, MS; Oh, SJ; Youn, SH; Kim, YS; Kim, D; Lim, WA				Shin, Hyeon Ho; Baek, Seung Ho; Li, Zhun; Han, Myung-Soo; Oh, Seok Jin; Youn, Seok-Hyun; Kim, Young Sug; Kim, Daekyung; Lim, Weol-Ae			Resting cysts, and effects of temperature and salinity on the growth of vegetative cells of the potentially harmful species <i>Alexandrium insuetum</i> Balech (Dinophyceae)	HARMFUL ALGAE			English	Article						Alexandrium insuetum; Resting cyst; Minutum group; Temperature; Salinity	SETO INLAND SEA; PHYLOGENETIC-RELATIONSHIPS; LABORATORY CONDITIONS; GENUS ALEXANDRIUM; PSEUDO-NITZSCHIA; TOXIN CONTENT; MASAN BAY; DINOFLAGELLATE; TAMARENSE; ENCYSTMENT	The potentially harmful species Alexandrium insuetum established by the incubation of resting cysts isolated from sediment trap samples collected at Jinhae-Masan Bay, Korea was characterized by morphological and phylogenetic analysis. The effects of temperature and salinity on the growth of A. insuetum were also investigated. The resting cysts are characterized by a spherical shape, a small size (20-25 mu m) and the presence of either three or four red accumulation bodies. The similarity of morphological features of the resting cysts to those of other species of the minutum group (consisting of Alexandrium minutum and A. tamutum) indicates that the morphological features of resting cysts might improve the accuracy of the grouping of Alexandrium species. A. insuetum germinated from the resting cysts is morphologically consistent with vegetative cells reported from Korean and Japanese coastal areas, and has an partial large subunit (LSU) rDNA sequence identical to that from Japanese strains. The growth of A. insuetum was observed between salinity 20 and 35, with increasing temperature; however at 25 degrees C, A. insuetum could grow even at the salinity of 15. The highest growth rate (0.60 d(-1)) was observed at 25 degrees C and the salinity of 25, which is higher than the previously reported growth rate of A. tamarense, which is responsible for outbreaks of paralytic shellfish poisoining and blooms in Jinhae-Masan Bay. These results suggest that the proliferation of A. insuetum in Jinhae-Masan Bay is likely to be highest during the summer. (C) 2014 Elsevier B.V. All rights reserved.	[Shin, Hyeon Ho; Li, Zhun] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea; [Baek, Seung Ho] Korea Inst Ocean Sci & Technol, South Sea Inst, Geoje 656830, South Korea; [Li, Zhun; Han, Myung-Soo] Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; [Oh, Seok Jin] Pukyong Natl Univ, Pusan 608737, South Korea; [Youn, Seok-Hyun; Kim, Young Sug; Lim, Weol-Ae] Natl Fisheries Res & Dev Inst, Pusan 619705, South Korea; [Kim, Daekyung] Korea Basic Sci Inst, Cheju 690140, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); Hanyang University; Pukyong National University; Korea Basic Science Institute (KBSI)	Lim, WA (通讯作者)，Natl Fisheries Res & Dev Inst, Pusan 619705, South Korea.	limwa@korea.kr	LI, ZHUN/GLT-3478-2022	Shin, Hyeon Ho/0000-0002-9711-6717; BAEK, SEUNG HO/0000-0002-5402-2518; LI, ZHUN/0000-0001-8961-9966; Baek, Seung Ho/0000-0003-2722-5907; Oh, Seok Jin/0000-0002-2572-5150	National Fisheries Research and Development Institute [RP-2014-ME-019]; KIMST project [PM58160]	National Fisheries Research and Development Institute; KIMST project(Korea Institute of Marine Science & Technology Promotion (KIMST))	This research was supported by a grant from National Fisheries Research and Development Institute (RP-2014-ME-019) and KIMST project (PM58160).	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J	Natsuike, M; Kanamori, M; Baba, K; Moribe, K; Yamaguchi, A; Imai, I				Natsuike, Masafumi; Kanamori, Makoto; Baba, Katsuhisa; Moribe, Kazuomi; Yamaguchi, Atsushi; Imai, Ichiro			Changes in abundances of <i>Alexandrium tamarense</i> resting cysts after the tsunami caused by the Great East Japan Earthquake in Funka Bay, Hokkaido, Japan	HARMFUL ALGAE			English	Article						Alexandrium tamarense; Cyst; Tsunami; The Great East Japan Earthquake; Funka Bay	DINOFLAGELLATE GONYAULAX-TAMARENSIS; MOUNE BAY; SEDIMENTS; KESENNUMA; EXCAVATA; IMPACTS; MIYAGI; LEBOUR; SEA	The 2011 Great East Japan Earthquake and the subsequent huge tsunami greatly affected both human activity and the coastal marine ecosystem along the Pacific coast of Japan. The tsunami also reached Funka Bay in northern Japan and caused serious damage to the scallop cultures there, and this tsunami was believed to have affected the coastal environments in the bay. Therefore, we investigated the changes in the spatial abundance and distribution of the toxic dinofiagellates Alexandrium tamarense cysts before the tsunami (August 2010) and after the tsunami (May 2011, August 2011, May 2012 and August 2012) in the bay. Further, monthly sampling was conducted after the tsunami to identify seasonal changes of Alexandrium catenella/tamarense cysts and vegetative cells. Significant increases were observed in the populations of A. catenella/tamarense cysts, comparing the abundances before the tsunami (in August 2010; 70 +/- 61 cysts g(-1) wet sediment) to those just after it (in May 2011; 108 +/- 84 cysts g(-1) wet sediment), and both A. tamarense bloom (a maximum density was 1.3 x 10(3) cells L-1) and PSP (Paralytic Shellfish Poisoning) toxin contamination of scallops (9.4 mouse unit g(-1) was recorded) occurred in the bay. Seasonal sampling also revealed that the encystment of A. tamarense and the supply of the cysts to bottom sediments did not occur in the bay from September to April. These results strongly suggested that the mixing of the bottom sediments by the tsunami caused the accumulation of the toxic A. tamarense cysts in the surface of bottom sediment through the process of redeposition in Funka Bay. Moreover, this cyst deposition may have contributed to the toxic bloom formation as a seed population in the spring of 2011. (C) 2014 Elsevier B.V. All rights reserved.	[Natsuike, Masafumi; Kanamori, Makoto; Moribe, Kazuomi; Yamaguchi, Atsushi; Imai, Ichiro] Hokkaido Univ, Grad Sch Fisheries Sci, Div Marine Bioresource & Environm Sci, Hakodate, Hokkaido 0418611, Japan; [Natsuike, Masafumi] Moune Inst Forest Sato Sea Studies, Kesennuma, Miyagi 9880582, Japan; [Kanamori, Makoto] Hokkaido Res Org, Fisheries Res Dept, Hakodate Fisheries Res Inst, Hakodate, Hokkaido 0400051, Japan; [Baba, Katsuhisa] Hokkaido Res Org, Fisheries Res Inst, Yoichi, Hokkaido 0468555, Japan	Hokkaido University	Natsuike, M (通讯作者)，Moune Inst Forest Sato Sea Studies, 212 Karakuwa Cho Higashi Moune, Kesennuma, Miyagi 9880582, Japan.	info@mori-umi.org	Yamaguchi, Atsushi/A-8613-2012	Yamaguchi, Atsushi/0000-0002-5646-3608	Ministry of Education, Culture, Sports, Science and Technology program for fostering regional innovation, Japan	Ministry of Education, Culture, Sports, Science and Technology program for fostering regional innovation, Japan	We are grateful to all of the following: Daisuke Achiya of the Yakumo-cho Japan Fisheries cooperative, and the captain and crews 'of the T/S Ushio-Maru for their kind help in the field samplings. We thank Dr. Tomoko Sakami of the Tohoku National Fisheries Research Institute and Dr. Akiyoshi Shinada of the Hokkaido Research Organization, Fisheries Research Institute Central Fisheries Research Institute for their kind support and advice. We thank Professor Tetsuya Takatsu and Kenshi Kuma, Associate Professor Toshikuni Nakatani and Associate Isao Kudo, and the students, Divisions of Marine Bioresource and Environmental Science, Graduate School of Fisheries Sciences, Hokkaido University, for their kind assistance with sampling. We greatly appreciate Dr. Takashi Kamiyama, Tohku National Fisheries Research Institute and Professor Barrie Dale, University of Oslo for giving valuable comments to improve the manuscript. This study was funded by the 'Hakodate Marine Bio Cluster Project' of the Ministry of Education, Culture, Sports, Science and Technology program for fostering regional innovation, Japan.	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J	Richards, K; Bolikhovskaya, NS; Hoogendoorn, RM; Kroonenberg, SB; Leroy, SAG; Athersuch, J				Richards, Keith; Bolikhovskaya, Nataliya S.; Hoogendoorn, Robert M.; Kroonenberg, Salomon B.; Leroy, Suzanne A. G.; Athersuch, John			Reconstructions of deltaic environments from Holocene palynological records in the Volga delta, northern Caspian Sea	HOLOCENE			English	Article						Caspian Sea; dinoflagellate cysts and ostracods; pollen and spores; sea level change; vegetation and climate; Volga delta	NEOGENE PRODUCTIVE SERIES; LEVEL CHANGES; BLACK-SEA; DINOFLAGELLATE CYSTS; ARAL SEA; BASIN; SALINITY; SEDIMENTATION; HISTORY; TRANSGRESSION	New palynological and ostracod data are presented from the Holocene Volga delta, obtained from short cores and surface samples collected in the Damchik region, near Astrakhan, Russian Federation in the northern Caspian Sea. Four phases of delta deposition are recognized and constrained by accelerated mass spectrometry (AMS) radiocarbon ages. Palynological records show that erosive channels, dunes (Baer hills) and inter-dune lakes were present during the period 11,500-8900cal. BP at the time of the Mangyshlak Caspian lowstand. The period 8900-3770cal. BP was characterized regionally by extensive steppe vegetation, with forest present at times with warmer, more humid climates, and with halophytic and xerophytic vegetation present at times of drought. The period 3770-2080cal. BP was a time of active delta deposition, with forest or woodland close to the delta, indicating relatively warm and humid climates and variable Caspian Sea levels. From 2080cal. BP to the present-day, aquatic pollen is frequent in highstand intervals and herbaceous pollen and fungal hyphae frequent in lowstand intervals. Soils and incised valley sediments are associated with the regional Derbent regression and may be time-equivalent with the Medieval Warm Period'. Fungal spores are an indicator of erosional or aeolian processes, whereas fungal hyphae are associated with soil formation. Freshwater algae, ostracods and dinocysts indicate mainly freshwater conditions during the Holocene with minor brackish influences. Dinocysts present include Spiniferites cruciformis, Caspidinium rugosum, Impagidinium caspienense and Pterocysta cruciformis, the latter a new record for the Caspian Sea. The Holocene Volga delta is a partial analogue for the much larger oil and gas bearing Mio-Pliocene palaeo-Volga delta.	[Richards, Keith] KrA Stratig Ltd, Deganwy LL31 9YY, Conwy, Wales; [Richards, Keith] Univ Amsterdam, NL-1012 WX Amsterdam, Netherlands; [Bolikhovskaya, Nataliya S.] Moscow MV Lomonosov State Univ, Moscow, Russia; [Hoogendoorn, Robert M.] Deltares, Delft, Netherlands; [Hoogendoorn, Robert M.; Kroonenberg, Salomon B.] Delft Univ Technol, NL-2600 AA Delft, Netherlands; [Leroy, Suzanne A. G.] Brunel Univ, Uxbridge UB8 3PH, Middx, England	University of Amsterdam; Lomonosov Moscow State University; Deltares; Delft University of Technology; Brunel University	Richards, K (通讯作者)，KrA Stratig Ltd, 116 Albert Dr, Deganwy LL31 9YY, Conwy, Wales.	kr@paly.co.uk	Bolikhovskaya, Nataliya/L-7904-2015; Kroonenberg, Salomon/GQI-4402-2022; Leroy, Suzanne/D-3996-2009	Kroonenberg, Salomon Bernard/0000-0001-7240-8425	IGCP-UNESCO [481]; NWO, Netherlands Science Foundation; RFFI, Russian Science Foundation; BP Exploration (Caspian Sea) Sea Ltd.; BP Exploration (Caspian Sea) Ltd.; Delft University of Technology; KrA Stratigraphic Ltd.; StrataData Ltd.; Deltares	IGCP-UNESCO; NWO, Netherlands Science Foundation(Netherlands Organization for Scientific Research (NWO)); RFFI, Russian Science Foundation(Russian Science Foundation (RSF)); BP Exploration (Caspian Sea) Sea Ltd.; BP Exploration (Caspian Sea) Ltd.; Delft University of Technology; KrA Stratigraphic Ltd.; StrataData Ltd.; Deltares	Funding for the data collection and field work was provided from the following sources: 1 - IGCP-UNESCO 2003-2008 (Project 481 CASPAGE, Dating Caspian Sea Level Change); 2 - NWO, Netherlands Science Foundation and RFFI, Russian Science Foundation 2005-2008 (Programme: 'VHR Seismic Stratigraphy and Paleoecology of the Holocene Volga Delta'); and 3 - BP Exploration (Caspian Sea) Sea Ltd. (Azeri-Chirag-Gunashli) 2005-2008 ('Unravelling the Small-Scale Stratigraphy and Sediment Dynamics of the Modern Volga Delta Using VHR Marine Geophysics'). The palynological work was funded jointly by BP Exploration (Caspian Sea) Ltd., Delft University of Technology and KrA Stratigraphic Ltd. Ostracod analyses were funded by StrataData Ltd. and funding for two additional radiocarbon dates provided by Deltares. Provision for open access publication was made available by the Institute for the Environment, Brunel University.	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J	Leroy, SAG; López-Merino, L; Tudryn, A; Chalié, F; Gasse, F				Leroy, Suzanne A. G.; Lopez-Merino, Lourdes; Tudryn, Alma; Chalie, Francoise; Gasse, Francoise			Late Pleistocene and Holocene palaeoenvironments in and around the middle Caspian basin as reconstructed from a deep-sea core	QUATERNARY SCIENCE REVIEWS			English	Article						Caspian Sea; Pollen; Vegetation history; Dinocysts; Lake level fluctuation; Salinity; Late Pleistocene; Holocene	SOUTHWESTERN BLACK-SEA; SURFACE CONDITIONS; SALINITY CHANGES; LEVEL CHANGES; WEST ASIA; SEDIMENTS; CLIMATE; POLLEN; FLUCTUATIONS; OSCILLATIONS	Late Pleistocene and/or Holocene high-resolution palynological studies are available for the south basin of the Caspian Sea (CS), the world's largest lake. However, the north and middle basins have not been the object of high-resolution palynological reconstructions. This new study presents the pollen, spores and dinoflagellate cysts records obtained from a 10 m-long sediment core recovered in the middle basin, which currently has brackish waters and is surrounded by arid and semi-arid vegetation. An age-depth model built based on six radiocarbon dates on ostracod shells indicates that the sequence spans the period from 14.47 to 2.43 cal. ka BR The present palaeoenvironmental study focuses on the top 666 cm, or from 12.44 to 2.43 cal. ka BR At the vegetation level, the Younger Dryas is characterised by an open landscape dominated by desert vegetation composed by Amaranthaceae with shrubs and salt-tolerant plants. However, although the Early Holocene is also characterised by desert vegetation, it is enriched in various shrubs such as Ephedra and Calligonum, but tree expansion is not important at the Holocene onset. After a major shift at 8.19 cal. ka BP, the Middle Holocene displays now both the character of desert and of steppe, although some trees such as Quercus and Corylus slightly spread. The Late Holocene records steppe vegetation as dominant, with more tree diversity. Regarding the lacustrine signal, the dinocyst assemblage record fluctuates between slightly brackish conditions highlighted by Pyxidinopsis psilata and Spiniferites cruciformis, and more brackish ones similar to the present day with the dominance of Impagidinium caspienense. The Late Pleistocene is characterised by low salinities, related to the Khvalynian highstand. From 11.56 cal. ka BP, slightly more saline waters are reconstructed with an increase of L caspienense for a period of 1000 years, which could be attributed to the Mangyshlak lowstand. From 10.55 cal. ka BP, low salinity conditions return with remains such as Anabaena and Botryococcus abundant until 8.83 cal. ka BP, followed by a slow, progressive decrease of P. psilata and S. cruciformis until 4.11 cal. ka BP, which is the main assemblage change at lacustrine scale. Since then, higher salinities, similar to the present one, are reconstructed. Finally, Lingulodinium machaerophorum starts its development only at 2.75 cal. ka BP, in the Late Holocene. The present research revealed fundamental differences from previously published sea-level curves, in that a 6000 yr-long highstand suggested by low salinities is shown between 10.55 and 4.11 cal. ka BP. Amongst other arguments, using a comparison to a similar palynological regard but in the south basin, a N-S salinity gradient that is the reverse of the present one across the CS, suggests that the Amu Darya was flowing in the CS. Hence the CS levels during the Late Pleistocene and Holocene were influenced by a combination of precipitation over the high European latitudes and the indirect influence of the Indian summer monsoon over the Pamirs. (C) 2014 The Authors. Published by Elsevier Ltd.	[Leroy, Suzanne A. G.; Lopez-Merino, Lourdes] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Tudryn, Alma] Univ Paris 11, Lab GEOPS, UMR8148, F-91405 Orsay, France; [Tudryn, Alma] CNRS, F-91405 Orsay, France; [Chalie, Francoise; Gasse, Francoise] Aix Marseille Univ, CEREGE, UM 34, CNRS UMR 7330, F-13545 Aix En Provence 04, France	Brunel University; Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite	Leroy, SAG (通讯作者)，Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England.	suzanne.leroy@brunel.ac.uk	López-Merino, Lourdes/GLT-0551-2022; Leroy, Suzanne/D-3996-2009	Leroy, Suzanne/0000-0002-2556-2339; Lopez-Merino, Lourdes/0000-0002-6361-5374	European Contract INCO-Copernicus "Understanding the Caspian Sea erratic fluctuations" [IC15-CT96-0112]; Centre National de la Recherche Scientifique within INSU-DYTEC (DYnamique de la Terre et du Climat) Program (France); Brunel IfE MINT;  [1227];  [CLIMSEAS-PIRSES-GA-2009-247512]	European Contract INCO-Copernicus "Understanding the Caspian Sea erratic fluctuations"; Centre National de la Recherche Scientifique within INSU-DYTEC (DYnamique de la Terre et du Climat) Program (France); Brunel IfE MINT; ; 	This study has been conducted within the European Contract INCO-Copernicus "Understanding the Caspian Sea erratic fluctuations" no IC15-CT96-0112. This was funded by the Centre National de la Recherche Scientifique within the framework of the INSU-DYTEC (DYnamique de la Terre et du Climat) Program (France). Thanks are due to the French and Russian colleagues, who organised and participated in the coring and hydrological sea expedition of August 1994. P.-J.. Giannesini kindly provided the carbonate data and he and E. Moreno are the curators of the cores at the Museum National d'Histoire Naturelle de Paris, France. We are especially grateful to P. Tucholka, F. Guichard and K. Arpe who actively contributed to the scientific part of this project. G. Seret (UCL, Belgium) had the first set of palynological residues of core GS18 made available for counting. LLM was funded by the Brunel IfE MINT scheme. The publication is a contribution to the INQUA QuickLakeH project (No. 1227) and to the European project Marie Curie, CLIMSEAS-PIRSES-GA-2009-247512. M. Turner (Brunel University) has kindly checked the English of the manuscript.	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Sci. Rev.	OCT 1	2014	101						91	110		10.1016/j.quascirev.2014.07.011	http://dx.doi.org/10.1016/j.quascirev.2014.07.011			20	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AQ3SS		Green Published, hybrid			2025-03-11	WOS:000342714400007
J	Yanko-Hombach, V; Mudie, PJ; Kadurin, S; Larchenkov, E				Yanko-Hombach, Valentina; Mudie, Petra J.; Kadurin, Sergey; Larchenkov, Evgeny			Holocene marine transgression in the Black Sea: New evidence from the northwestern Black Sea shelf	QUATERNARY INTERNATIONAL			English	Article							LATE PLEISTOCENE; DINOFLAGELLATE CYSTS; MEDITERRANEAN SEA; MARMARA; LEVEL; WATER; POLLEN; ASSEMBLAGES; EVOLUTION; CORRIDOR	For two decades, the timing and rate of Holocene marine transgression and the level of the Black Sea prior to the transgression has been the focus of many geological, palaeoecological and archaeological studies. The potential importance of confirming or rejecting the catastrophic flood hypothesis by refining the chronology of the marine transgression and determining the water level of the early Holocene Black Sea (Neoeuxinian) lake is the aim of many ongoing Black Sea palaeoecological studies. In this report we review previous studies and present new data on the early Holocene marine transgression obtained from multidisciplinary studies of several cores from different parts of the Black Sea. Core 342 from the edge of the Dniester paleovalley on NW shelf is particularly important because it provides wood and leaf material from several peat and muddy peat beds, each up to similar to 10 cm thick, inter-layered in a coastal succession with mud, clay, and shell coquina. AMS ages for wood fragments and sedge leaves in the peat layers provide critical new data for calibrating and "re-tuning" of previously published shell and bulk detrital peat ages. Our multi-disciplinary study of geological material recovered from different shelf areas of the Black Sea refines the chronology of the marine transgression and clarifies conflicting interpretations of the water level and salinity of the Neoeuxinian lake prior to the initial Mediterranean inflow (IMI) and transgression of Mediterranean water in the Holocene, We find that: (1) The level of the Late Neoeuxinan lake prior to the early Holocene Mediterranean transgression stood around -40 m bsl but not -100 m or more as suggested by advocates of catastrophic/rapid/prominent flooding of the Black Sea by Mediterranean water. (2) At all times, the Neoeuxinan lake was brackish with salinity not less that 7 psu. (3) By 8.9 ka BP, the Black Sea shelf was already submerged by the Mediterranean transgression. An increase in salinity took place over 3600 years, with rate of the marine water incursion being estimated in the order of 0.05 cm-1.7 cm a(-1). (4) The combined data set of sedimentological characteristics and microfossil data establish that the Holocene marine transgression was of a gradual, progressive nature in the early Holocene. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.	[Yanko-Hombach, Valentina; Kadurin, Sergey; Larchenkov, Evgeny] Odessa II Mechnikov Natl Univ, Dept Phys & Marine Geol, UA-65082 Odessa, Ukraine; [Yanko-Hombach, Valentina; Kadurin, Sergey; Larchenkov, Evgeny] Odessa II Mechnikov Natl Univ, Interdisciplinary Sci Ctr Geoarchaeol Marine & En, UA-65082 Odessa, Ukraine; [Yanko-Hombach, Valentina] Avalon Inst Appl Sci, Winnipeg, MB R3E 1B4, Canada; [Mudie, Petra J.] Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada	Ministry of Education & Science of Ukraine; Odesa I. I. Mechnikov National University; Ministry of Education & Science of Ukraine; Odesa I. I. Mechnikov National University; Memorial University Newfoundland	Yanko-Hombach, V (通讯作者)，Odessa II Mechnikov Natl Univ, Palaeontol Museum, 2 Dvorianskaia Str, UA-65082 Odessa, Ukraine.	valyan@avalon-institute.org	Sergii, Kadurin/AAF-1938-2021; Yanko-Hombach, Valentina/J-7341-2015	Yanko-Hombach, Valentina/0000-0003-4933-5066; Sergey, Kadurin/0000-0003-0691-1828	Russian-Ukrainian project "The Northwestern Black Sea Region and Global Climate Change: Environmental evolution during the last 20 ka and forecast for the 21st century" - State Fund for Fundamental Research, Ukraine [Phi28/428-2009]; EU [GOCE-CT-2005-511234]; National Science and Engineering Research Council	Russian-Ukrainian project "The Northwestern Black Sea Region and Global Climate Change: Environmental evolution during the last 20 ka and forecast for the 21st century" - State Fund for Fundamental Research, Ukraine; EU(European Union (EU)); National Science and Engineering Research Council(Natural Sciences and Engineering Research Council of Canada (NSERC))	This paper is a contribution to IGCP 521-INQUA 0501 projects as well as to the Russian-Ukrainian project No. Phi 28/428-2009 "The Northwestern Black Sea Region and Global Climate Change: Environmental evolution during the last 20 ka and forecast for the 21st century" sponsored by the State Fund for Fundamental Research, Ukraine, and EU FR6 HERMES Project, contract GOCE-CT-2005-511234. Funding support for Petra Mudie from National Science and Engineering Research Council Discovery Grant is gratefully acknowledged; also the assistance of palynological sample processing mostly by Helen Gillespie at Memorial University of Newfoundland, Canada, with some surface reference samples prepared by Anna Gaponova, PhD student at ONU. We sincerely thank "Prichernomor GRGP" for use of their coring material as well as archive data for our study, and we thank Prof. E.I. Schornikov (A.V. Zhirmunsky Institute of Marine Biology, Far East Division of Russian Academy of Sciences) and Dr. N.I. Dikan' (Institute of Geological Sciences of the National Academy of Sciences of Ukraine) for consulting with us on ostracoda taxonomy and ecological preferences. We also thank T.O. Kondaryuk (Odesa I.I. Mechnikov National University) for preparation of foraminifera and ostracoda shells for imaging in SEM. Prof. J. Teller (University of Manitoba) is sincerely thanked for help and Dr. Revinder Sidhu, Electron Microprobe and SEM Manager, University of Manitoba, for imaging of microfauna in SEM. We also thank R.N Hiscott (Memorial University of Newfoundland) for discussion of our data in an earlier draft.	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Int.	SEP 29	2014	345						100	118		10.1016/j.quaint.2013.07.027	http://dx.doi.org/10.1016/j.quaint.2013.07.027			19	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AR8QB					2025-03-11	WOS:000343838600011
J	Portela, HA; Antonioli, L; Dino, R; Garcia, MJ				Portela, Helena Antunes; Antonioli, Luzia; Dino, Rodolfo; Garcia, Maria Judite			PALYNOFLORAL AND PALEOENVIRONMENTAL CHARACTERIZATION OF THE SANTANA FORMATION (LOWER CRETACEOUS), 4-BO-1-PE WELL, ARARIPE BASIN, NORTHEAST BRAZIL	REVISTA BRASILEIRA DE PALEONTOLOGIA			Portuguese	Article						Araripe Basin; Lower Cretaceous; paleoenvironment; paleopalynology		A paleoenvironmental characterization of the Santana Formation sedimentary rocks (4-BO-1-PE well), Araripe Basin, Late Aptian-Early Albian, was accomplished through qualitative and quantitative analyses of the palynoflora. Palynological and lithological evidence indicate a predominantly continental depositional environment for this section, composed by a fluvial, lacustrine deltaic system in a semi-arid climate. The detection of a single dinoflagellate cyst suggests that small sea ingressions took place during Aptian-Albian times in the region, as also verified in other coeval strata of marginal Brazilian Cretaceous basins. Comparisons with palynofloras from other continents support the hypothesis that this assemblage belongs to the North-Gondwana microfloristic province.	[Portela, Helena Antunes; Antonioli, Luzia; Dino, Rodolfo] Univ Estado Rio De Janeiro, Fac Geol, Dept Estratigrafia & Paleontol, BR-20559013 Rio De Janeiro, RJ, Brazil; [Garcia, Maria Judite] IGc USP, Lab Paleobot & Palinol, BR-05508900 Sao Paulo, Brazil	Universidade do Estado do Rio de Janeiro	Portela, HA (通讯作者)，Univ Estado Rio De Janeiro, Fac Geol, Dept Estratigrafia & Paleontol, Rua Sao Francisco Xavier,524 Bloco A,Sala 2030, BR-20559013 Rio De Janeiro, RJ, Brazil.	helenaportela@gmail.com; luziaa@uerj.br; dino@uerj.br; mj-garcia@uol.com.br	Antonioli, Luzia/AAC-9679-2021; Dino, Rodolfo/AAD-2105-2021					ALVIN K L, 1978, Palaeontology (Oxford), V21, P847; ALVIN K L, 1974, Palaeontology (Oxford), V17, P587; Andrews HN., 1961, Studies in palaeobotany; Antonioli L., 2001, THESIS U FEDERAL RIO; Antonioli L., 2007, PALEONTOLOGIA CENARI, V2, P533; Antonioli L., 1998, BIOESTRATIGRAFIA PAL; Appi, 1990, C BRAS GEOL NAT, V1, P211; Arai M., 1990, 1 S BAC AR BAC INT N, P225; Assine M.L., 2007, B GEOCI NCIAS PETROB, V15, P371; Assine M.L., 1992, Revista Brasileira de Geociencias, V22, P289, DOI [10.25249/0375-7536.1992289300, DOI 10.25249/0375-7536.1992289300]; Batten D.J., 1996, Palynology: principles and applications, P205; BATTEN D.J., 1975, P GEOL ASS, V85, P433; Brenner G.J., 1976, ORIGIN EARLY EVOLUTI, P23; Brito Neves BBA, 1990, S BAC AR BAC INT NOR, P21; Caixeta JM., 1994, B GEOCIENCIAS PETROB, V8, P163; DETTMANN M.E., 1963, P ROY SOC VICTORIA, V77, P1; Dino R., 1999, S CRETACEO, V5, P557; Doyle J.A., 1982, B CENT RECH EXPL, V6, P39; Duarte S.G., 2012, REV INST GEOL, V33, P1, DOI DOI 10.5935/0100-929X.20120006; Gamerro J.C., 1965, AMEGHINIANA, V4, P133; HASHIMOTO A.T., 1987, Revista Brasileira de Geosciencias, V17, P118, DOI DOI 10.25249/0375-7536.1987118122; Herngreen G. F. W., 1981, POLLEN SPORES, V23, P241; Herngreen GFW., 1996, PALYNOLOGY PRINCIPLE, V3, P1157; KRASSILOV VA, 1978, REV PALAEOBOT PALYNO, V26, P113, DOI 10.1016/0034-6667(78)90008-8; Lima M. R., 1971, THESIS U FEDERAL RIO; Lima M.R., 1978, PhD thesis; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; Portela H. A., 2008, THESIS U ESTADO RIO; Regali M.S.P., 1989, REV ESCOLA MINAS, V42, P17; Srivastava S. K., 1978, PALAEOPALYNOLOGY SER, V5; Uesugui N., 1979, Boletim Tecnico da Petrobras, V22, P229; UESUGUI N., 1987, Revista Brasileira de Geociencias, Sao Paulo, V17, P131; UPCHURCH G.R., 1981, Geobotany II, P167, DOI DOI 10.1007/978-1-4899-4989-9_8; Vakhrameev V.A., 1970, PALEONTOL J+, V4, P11; VANKONIJNENBURGVANCITTERT JHA, 1978, REV PALAEOBOT PALYNO, V26, P125, DOI 10.1016/0034-6667(78)90009-X; VIANA M.S.S., 2002, Sitios Geologicos e Paleontologicos do Brasil (SIGEP), P113; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	37	14	15	1	11	SOC BRASILEIRA PALEONTOLOGIA	SAO LEOPOLDO	PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL	1519-7530	2236-1715		REV BRAS PALEONTOLOG	Rev. Bras. Paleontol.	SEP-DEC	2014	17	3					363	372		10.4072/rbp.2014.3.07	http://dx.doi.org/10.4072/rbp.2014.3.07			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	CA2MY		Bronze			2025-03-11	WOS:000348743600007
J	Guédé, KE; Slimani, H; Louwye, S; Asebriy, L; Toufiq, A; Ahmamou, M; El Hassani, IEEA; Digbehi, ZB				Guede, Kore Elysee; Slimani, Hamid; Louwye, Stephen; Asebriy, Lahcen; Toufiq, Abdelkabir; Ahmamou, M'Fedal; El Hassani, Iz-Eddine El Amrani; Digbehi, Zeli Bruno			Organic-walled dinoflagellate cysts from the Upper Cretaceous-lower Paleocene succession in the western External Rif, Morocco: New species and new biostratigraphic results	GEOBIOS			English	Article						Dinalagellate cysts; Taxonomy; Biostratigraphy; Upper Cretaceous; Lower Paleocene; Morocco	TERTIARY BOUNDARY; OULED HADDOU; PALEOGENE BOUNDARY; CALCAREOUS NANNOFOSSIL; SEA; STRATIGRAPHY; FORAMINIFERA; NETHERLANDS; TRANSITION; GEORGIA	Palynological investigation of the Upper Cretaceous-lower Paleocene succession from the Tahar section near Arba Ayacha in northwestern Morocco (westernmost External Rif Chain) reveals the presence of rich, diverse and well-preserved dinoflagellate cyst assemblages. For the first time in the study region, biostratigraphic interpretations based on the dinoflagellate cyst assemblages from the studied interval allow the recognition of the upper Maastrichtian and Danian. Relevant upper Maastrichtian-Danian global dinoflagellate cyst events include: the First Appearance Datum of the upper Maastrichtian species Disphaerogena carposphaeropsis, Glaphyrocysta perforata,and.Manumiella seelandica; the Last Appearance Datum of the Cretaceous taxa Dinogymnium spp., lsabelidinium cooksoniae, and Pterodinium cretaceum; and the First Appearance Datum of the earliest Danian markers Carpatella cornuta, Damassadinium californicum, Membranilarnacia? tenella, and Senoniasphaera inornata. We formally describe the biostratigraphical range and potential of two new dinoflagellate cyst species, namely Nematosphaeropsis silsila Guede and Slimani nov. sp., and Pterodinium ayachensis Cuede and Slimani nov. sp. Both species are found in the westernmost External Rif Chain and are restricted to the upper Maastrichtian. (C) 2014 Published by Elsevier Masson SAS.	[Guede, Kore Elysee; Slimani, Hamid; Asebriy, Lahcen; El Hassani, Iz-Eddine El Amrani] Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, Rabat, Morocco; [Guede, Kore Elysee; Ahmamou, M'Fedal] Univ Mohammed V Agdal, Fac Sci, Lab Geodynam Geoinformat & Geoenvironm, Rabat, 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; [Guede, Kore Elysee; Digbehi, Zeli Bruno] Univ Felix Houphouet Boigny, UFR STRM, Abidjan 22, Cote Ivoire	Mohammed V University in Rabat; Mohammed V University in Rabat; Ghent University; Chouaib Doukkali University of El Jadida; Universite Felix Houphouet-Boigny	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, PB 703, Rabat, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020; Elysee, Guede/ABE-3209-2021; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Slimani, Hamid/0000-0001-6392-1913; Kore Elysee, Guede/0000-0003-1393-5078; EL AMRANI EL HASSANI, Iz-Eddine/0000-0001-6260-2566	"Comite d'Entraide International" (CEI); "Direction de l'Orientation et des Bourses" (DOB) of Cote d'Ivoire; National Center of Scientific and Technical Research (CNRST); University Mohammed V-Agdal [SVT11/09]; National Center of Scientific and Technical Research (research unit URAC 46)	"Comite d'Entraide International" (CEI); "Direction de l'Orientation et des Bourses" (DOB) of Cote d'Ivoire; National Center of Scientific and Technical Research (CNRST); University Mohammed V-Agdal; National Center of Scientific and Technical Research (research unit URAC 46)	The authors thank the Research Unit Palaeontology, Ghent University (Belgium) and the Laboratory of Geology and Remote Sensing, Scientific Institute, University Mohammed V-Agdal (Morocco) for their technical support. KEG thanks the "Comite d'Entraide International" (CEI) and the "Direction de l'Orientation et des Bourses" (DOB) of Cote d'Ivoire for financial support during this study which is part of his Ph.D. thesis. The authors from the Moroccan Scientific Institute acknowledge support from the National Center of Scientific and Technical Research (CNRST; research unit URAC 46) and the University Mohammed V-Agdal (Project SVT11/09). Prof. A. Gautier from the Research Unit Palaeontology of Ghent University kindly helped putting together the final version of the manuscript. Constructive reviews by journal reviewers Drs. Edwige Masure, Fabienne Marret and Vanessa Clare Bowman are greatly appreciated.	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J	El Atfy, H; Brocke, R; Uhl, D; Ghassal, B; Stock, AT; Littke, R				El Atfy, Haytham; Brocke, Rainer; Uhl, Dieter; Ghassal, Bandar; Stock, Alexander T.; Littke, Ralf			Source rock potential and paleoenvironment of the Miocene Rudeis and Kareem formations, Gulf of Suez, Egypt: An integrated palynofacies and organic geochemical approach	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article						Palynofacies; Vitrinite reflectance; TOC; Rock-Eval pyrolysis; Gulf of Suez; Egypt	LUSITANIAN BASIN PORTUGAL; PETROLEUM SOURCE ROCKS; SOUTHERN GULF; RIFT-BASIN; SEQUENCE STRATIGRAPHY; DINOFLAGELLATE CYSTS; AMORPHOUS KEROGENS; SEDIMENTS; GERMANY; HISTORY	A study on source rock characterization and paleoenvironmental interpretation has been carried out on a relatively thick Miocene sedimentary succession from three wells (GH 404-2A, GH 420-1, SA-E6A) in the southern Gulf of Suez, Egypt. The compilation of detailed optical investigations, including palynofacies analysis, spore coloration index (SCI), vitrinite reflectance (VRr) and source rock geochemical data enables a detailed evaluation of organic matter (OM) richness, kerogen type, and thermal maturation level. Despite their high content of calcium carbonate (up to 52%), the studied sediments yielded sufficient palynologic residue for a detailed palynofacies and organic petrographic study. The palynomorph content comprises mainly marine components, essentially dinoflagellate cysts and accessorily microforaminiferal linings, while terrestrial-derived material is relatively rare. Persistent occurrence of amorphous organic matter (ACM) indicates that dysoxic to anoxic conditions prevailed throughout the deposition of the investigated sediments. The main objective of this study is to combine organic geochemical and palynological data in an attempt to assess the source rock potential of the Rudeis and Kareem formations in the Gulf of Suez. These data, in addition, also allow for the reconstruction of the depositional environment. The present investigation employs multimode microscopic methods using transmitted white light along with incident light fluorescence microscopy. For the first time, geochemical and petrographic analyses performed on bulk rock samples and palynological residues demonstrate that both the Rudeis Formation and the Kareem Formation are mainly of kerogen type III or mixed type II/III. Independent thermal maturation specific parameters such as Rock-Eval T-max, VRr and SCI indicate an immature to early mature stage. Palynofacies analyses, combined with organic geochemical data indicate that the Rudeis Formation was deposited under shallow to open marine conditions, whereas the overlying Kareem Formation was formed mainly in an open marine setting. (C) 2014 Elsevier B.V. All rights reserved.	[El Atfy, Haytham; Brocke, Rainer; Uhl, Dieter] Senckenberg Res Inst, D-60325 Frankfurt, Germany; [El Atfy, Haytham; Brocke, Rainer; Uhl, Dieter] Nat Hist Museum, D-60325 Frankfurt, Germany; [El Atfy, Haytham] Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt; [Uhl, Dieter] Univ Tubingen, Senckenberg Ctr Human Evolut & Palaeoenvironm, D-72076 Tubingen, Germany; [Ghassal, Bandar; Stock, Alexander T.; Littke, Ralf] Rhein Westfal TH Aachen, Inst Geol & Geochem Petr & Coal, Energy & Mineral Resources Grp EMR, D-52056 Aachen, Germany	Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Egyptian Knowledge Bank (EKB); Mansoura University; Eberhard Karls University of Tubingen; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); RWTH Aachen University	El Atfy, H (通讯作者)，Senckenberg Res Inst, D-60325 Frankfurt, Germany.	helatfy@senckenberg.de	Atfy, Haytham/AAT-2276-2021; Littke, Ralf/A-6701-2016	Littke, Ralf/0000-0003-0421-8720; Uhl, Dieter/0000-0002-9938-5339; El Atfy, Haytham/0000-0003-1618-7220	German Academic Exchange Service (DAAD) [A/10/92695]; Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F)	German Academic Exchange Service (DAAD)(Deutscher Akademischer Austausch Dienst (DAAD)); Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F)	The German Academic Exchange Service (DAAD) is gratefully acknowledged for supporting this research at the Senckenberg Research Institute, Frankfurt am Main, Germany (grant A/10/92695). Partial financial support from the Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F) is also acknowledged. The authors are also grateful to the Egyptian General Petroleum Corporation (EGPC) and the Gulf of Suez Petroleum Company (GUPCO) for the provision of samples and well logs. Qusay Abeed (LEK, RWTH Aachen University) is highly acknowledged for his aid at running the geochemical analyses in Aachen. This study was conducted as a part of the PhD research project of H. El Atfy.	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J. Coal Geol.	SEP 1	2014	131						326	343		10.1016/j.coal.2014.06.022	http://dx.doi.org/10.1016/j.coal.2014.06.022			18	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Geology	AR8RS					2025-03-11	WOS:000343842800028
J	Richerol, T; Pienitz, R; Rochon, A				Richerol, Thomas; Pienitz, Reinhard; Rochon, Andre			Recent anthropogenic and climatic history of Nunatsiavut fjords (Labrador, Canada)	PALEOCEANOGRAPHY			English	Article						dinocyst; pollen; sediment core; fjord	DINOFLAGELLATE CYST ASSEMBLAGES; SEA-SURFACE CONDITIONS; VEGETATIONAL HISTORY; ENVIRONMENTAL-CHANGE; NORTHERN QUEBEC; LATE QUATERNARY; TUNDRA LAKE; HOLOCENE; TERRESTRIAL; SEDIMENTS	This study aimed at reconstructing past climatic and environmental conditions of a poorly known and documented subarctic region, the Nunatsiavut (northern Labrador). A multiproxy approach was chosen, using fossil dinoflagellate cysts, diatoms and pollen from sediment cores taken into three fjords (Nachvak 59 degrees N, Saglek 58.5 degrees N, and Anaktalak 56.5 degrees N). It allowed estimating terrestrial and marine influences in each fjord and documenting the recent history of human activities of the southern fjords (Saglek and Anaktalak). Fossil pollen and dinoflagellate cyst assemblages allowed depicting the climate history of the region over the last similar to 200-300 years. In contrast to the general warming trend observed in the arctic and subarctic Canada since the beginning of the Industrial Era, the Nunatsiavut has experienced relative climate stability over this period. Fossil pollen data show a shift of the tree limit to the south illustrating the cooling of terrestrial conditions. Our reconstructions suggest that the Labrador region has remained climatically stable over the last similar to 150-300 years, with just a slight cooling trend of the reconstructed sea surface temperatures, only perceptible in Saglek and Anaktalak fjords.	[Richerol, Thomas; Pienitz, Reinhard] Univ Laval, Lab Paleoecol Aquat, Ctr Etudes Nord, Quebec City, PQ, Canada; [Rochon, Andre] Univ Quebec Rimouski UQAR, Inst Sci Mer Rimouski ISMER, Lab Palynol Marine, Rimouski, PQ, Canada	Laval University; University of Quebec; Universite du Quebec a Rimouski	Richerol, T (通讯作者)，Univ Laval, Lab Paleoecol Aquat, Ctr Etudes Nord, Quebec City, PQ, Canada.	thomas_richerol@yahoo.fr	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); Network of Centers of Excellence ArcticNet; Nunatsiavut Government	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Network of Centers of Excellence ArcticNet; Nunatsiavut Government	This work was funded through grants from the Natural Sciences and Engineering Research Council of Canada (NSERC) and the Network of Centers of Excellence ArcticNet (project Nunatsiavut) 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 the sampling. We are also grateful to the two anonymous reviewers from the journal Paleoceanography who took the time to evaluate our manuscript and gave us very helpful comments.	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J	Radmacher, W; Pérez-Rodríguez, I; Arz, JA; Pearce, MA				Radmacher, Wiestawa; Perez-Rodriguez, Irene; Arz, Jose A.; Pearce, Martin A.			Dinoflagellate biostratigraphy at the Campanian-Maastrichtian boundary in Zumaia, northern Spain	CRETACEOUS RESEARCH			English	Review						Campanian-Maastrichtian boundary; Dinoflagellate cysts; Planktonic foraminifera; Zumaia; Northern Spain	CRETACEOUS-TERTIARY BOUNDARY; FRANCE; ZONATION; STRATIGRAPHY; SUCCESSION; EVOLUTION; REGION; MARGIN; CYSTS; BASIN	Dinoflagellate cyst assemblages from a well-exposed uppermost Cretaceous section at Zumaia (northern Spain) provide a basis for comparison with previous biostratigraphic and magnetostratigraphic studies on the problematic location of the Campanian-Maastrichtian boundary in the section. The position of the last occurrence of Corradinisphaeridium horridum and first common occurrence of Alterbidinium acutulum, correspond well with the bioevents defining the Campanian-Maastrichtian boundary in the Global boundary Stratotype Section and Point of Tercis les Bains (130 km to the North). Together with other age-diagnostic dinoflagellate cyst bioevents, we suggest that the boundary should be placed between 239.75 and 224.75 m below the Cretaceous-Palaeogene boundary, about 46 m lower than an interpretation based on the first occurrence of the planktonic foraminifer Pseudoguembelina palpebra and the last occurrence of the nannofossil Broinsonia parca subsp. constricta. A conspicuous acme of the dinoflagellate cyst Thalassiphora cf. delicata is encountered around the lower-upper Maastrichtian boundary (calibrated by foraminiferal, calcareous nannoplankton and magnetic polarity data), which may prove to be a useful correlatable event. (C) 2014 Elsevier Ltd. All rights reserved.	[Radmacher, Wiestawa] INC, PAN, BioGeoLab, PL-31002 Krakow, Poland; [Perez-Rodriguez, Irene; Arz, Jose A.] Univ Zaragoza, Dept Ciencias Tierra Paleontol, Zaragoza 50009, Spain; Univ Zaragoza, Inst Univ Invest Ciencias Ambient Aragon, Zaragoza 50009, Spain; [Pearce, Martin A.] Evolut Appl Ltd, Liskeard PL14 3JY, Cornwall, England	Polish Academy of Sciences; University of Zaragoza; University of Zaragoza	Radmacher, W (通讯作者)，INC, PAN, BioGeoLab, Ul Senacka 1, PL-31002 Krakow, Poland.	ndkrol@cyf-kr.edu.pl; irenepr@unizar.es; josearz@unizar.es; info@evolutionapplied.com	Pérez-Rodríguez, Irene/KEI-3681-2024; Radmacher, Wiesława/ABH-7042-2020; Arz Sola, Jose Antonio/B-5198-2008	Radmacher, Wieslawa/0000-0001-7316-3693; Perez Rodriguez, Irene/0000-0002-4743-0038; Pearce, Martin/0000-0001-7856-1076; Arz Sola, Jose Antonio/0000-0003-0063-8752	ING PAN scholarship for young scientists; Spanish Ministerio de Ciencia e Innovacion project [CGL2011-22912]; European Regional Development Fund	ING PAN scholarship for young scientists; Spanish Ministerio de Ciencia e Innovacion project(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); European Regional Development Fund(European Union (EU))	We would like to thank Dr. Asier Hilario, scientific director of the Basque Coast Geopark, for providing the panoramic photographs for Figs 3 and 4. This research was financed by ING PAN scholarship for young scientists (WR) and by Spanish Ministerio de Ciencia e Innovacion project CGL2011-22912, co-financed by the European Regional Development Fund (IPR and JAA).	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Res.	SEP	2014	51						309	320		10.1016/j.cretres.2014.07.004	http://dx.doi.org/10.1016/j.cretres.2014.07.004			12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	AR1HR		Green Accepted			2025-03-11	WOS:000343336800024
J	Badylak, S; Phlips, EJ; Mathews, AL; Kelley, K				Badylak, Susan; Phlips, Edward J.; Mathews, A. Loren; Kelley, Karen			<i>Akashiwo sanguinea</i> (Dinophyceae) extruding mucous from pores on the cell surface	ALGAE			English	Article						Akashiwo sanguinea; cyst; dinoflagellate; HAB; mucocyst; reproduction; trichocyst	COASTAL LAGOON; PHYTOPLANKTON; BLOOMS; USA; SALINITY; ESTUARY; FLORIDA; CYSTS; FISH; BAY	This is the first recorded observation of Akashiwo sanguinea excreting mucilaginous substances from pores on the cell surface. Observations were from samples collected in the Caloosahatchee Estuary, Florida, USA during a bloom event, with densities of 672 cells mL(-1) of A. sanguinea, including 51 cells surrounded by mucous. Scanning electron microscopy observations revealed that the mucous was secreted from thecal pores on the cell surface. The potential significance of mucous production is discussed.	[Badylak, Susan; Phlips, Edward J.; Mathews, A. Loren] Univ Florida, Sch Forest Resources & Conservat, Gainesville, FL 32653 USA; [Kelley, Karen] Univ Florida, ICBR Elect Microscopy & BioImaging Lab, Gainesville, FL 32611 USA	State University System of Florida; University of Florida; State University System of Florida; University of Florida	Phlips, EJ (通讯作者)，Univ Florida, Sch Forest Resources & Conservat, 7922 NW 71 St, Gainesville, FL 32653 USA.	phlips@ufl.edu	Kelley, Karen/IWM-0030-2023		South Florida Water Management District	South Florida Water Management District	We thank Captain Dan Stephens, Karen Stephens and Joe Mathews for all their help and dedication in the field. The research was funded by the South Florida Water Management District.	ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], MESA39 NOAA ERL; Badylak S, 2004, J PLANKTON RES, V26, P1229, DOI 10.1093/plankt/fbh114; Badylak S, 2007, B MAR SCI, V80, P295; Badylak Susan, 2014, Plankton & Benthos Research, V9, P147; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Dodge J. D., 1973, FINE STRUCTURE ALGAL, P167; Dodge JD., 1987, The Biology of Dinoflagellates, P92; Feyzioglu Ali Muzaffer, 2006, Turkish Journal of Botany, V30, P375; HARPER DE, 1989, CONTRIB MAR SCI, V31, P147; Hirasaka K., 1922, ZOOL MAG, V34, P740; HOMER RA, 1997, LIMNOL OCEANOGR, V42, P1076; Honsell G, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0057291; Hoppenrath M, 2008, J PHYCOL, V44, P451, DOI 10.1111/j.1529-8817.2008.00483.x; KAHRU M., 2004, EOS T AM GEOPHYS UN, V85, P465, DOI DOI 10.1029/2004EO450002; Kim CS, 2000, J EXP MAR BIOL ECOL, V254, P131, DOI 10.1016/S0022-0981(00)00263-X; Kim H. G., 1993, ILLUSTRATIONS PLANKT; Lee Joon-Baek, 2001, Algae, V16, P197; Lu SH, 2004, HYDROBIOLOGIA, V512, P231, DOI 10.1023/B:HYDR.0000020331.75003.18; Matsubara T, 2007, J EXP MAR BIOL ECOL, V342, P226, DOI 10.1016/j.jembe.2006.09.013; Phlips EJ, 2012, ESTUAR COAST, V35, P335, DOI 10.1007/s12237-011-9442-2; Phlips EJ, 2011, HARMFUL ALGAE, V10, P277, DOI 10.1016/j.hal.2010.11.001; Reynolds CS, 2006, ECOL BIODIVERS CONS, P1, DOI 10.2277/ 0521605199; Rines JEB, 2010, CONT SHELF RES, V30, P66, DOI 10.1016/j.csr.2009.11.001; Robichaux Randy J., 1998, NOAA Technical Report NMFS, V0, P19; Schumway S. E., 1990, J WORLD AQUACULT SOC, V21, P65; Smayda Theodore J., 2002, Harmful Algae, V1, P95, DOI 10.1016/S1568-9883(02)00010-0; Steidinger Karen A., 1998, NOAA Technical Report NMFS, V0, P13; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; VOLTOLINA D, 1993, J EXP MAR BIOL ECOL, V168, P217, DOI 10.1016/0022-0981(93)90261-L; ZHOU J, 1993, PHYCOLOGIA, V32, P444, DOI 10.2216/i0031-8884-32-6-444.1	31	8	8	3	31	KOREAN SOC PHYCOLOGY	SEOUL	B1F, TRUST TOWER, 275-7 YANGJAE-DONG, SEOCHO-KU, SEOUL, 137-739, SOUTH KOREA	1226-2617	2093-0860		ALGAE-SEOUL	Algae	SEP	2014	29	3					197	201		10.4490/algae.2014.29.3.197	http://dx.doi.org/10.4490/algae.2014.29.3.197			5	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AQ1FC		Bronze			2025-03-11	WOS:000342526300003
J	Ishikawa, A; Hattori, M; Ishii, KI; Kulis, DM; Anderson, DM; Imai, I				Ishikawa, Akira; Hattori, Mayuko; Ishii, Ken-Ichiro; Kulis, David M.; Anderson, Donald M.; Imai, Ichiro			<i>In situ</i> dynamics of cyst and vegetative cell populations of the toxic dinoflagellate <i>Alexandrium catenella</i> in Ago Bay, central Japan	JOURNAL OF PLANKTON RESEARCH			English	Article						Alexandrium catenella; cyst; in situ germination; bloom formation; population dynamics	RESTING CYSTS; LIFE-CYCLE; GONYAULAX-TAMARENSIS; NORTHEAST JAPAN; ONAGAWA BAY; GYMNODINIUM-CATENATUM; SCRIPPSIELLA-HANGOEI; SEXUAL REPRODUCTION; NUTRITIONAL FACTORS; COASTAL WATERS	Temporal changes in the in situ germination flux of cysts and the abundance of vegetative cells of the toxic dinoflagellate Alexandrium catenella were investigated in Ago Bay, central Japan from July 2003 to December 2004. The in situ germination flux (cells m(-2) day(-1)) was measured using 'plankton emergence trap/chambers (PET chambers)'. Germination of the cysts in the sediments occurred continuously during the study, ranging from 52 to 1753 cells m(-2) day(-1), with no temporal trend. This germination pattern appeared to be promoted by a short mandatory dormancy period for newly formed cysts coupled with a broad temperature window for germination. For the vegetative populations, high abundances (>10(5) cells m(-2)) were recorded in the water column from spring to summer and from autumn to early winter. The size of the vegetative populations did not correlate with the cyst germination flux but rather larger vegetative populations were often observed when the water temperature was around 20 degrees C, indicating that bloom development was mainly regulated by the temperature. Nonetheless, the continuous germination pattern of A. catenella is advantageous enabling the germinated cells to immediately exploit favorable bloom conditions.	[Ishikawa, Akira; Hattori, Mayuko] Mie Univ, Grad Sch Bioresources, Tsu, Mie 5148507, Japan; [Ishii, Ken-Ichiro] Kyoto Univ, Grad Sch Agr, Div Appl Biosci, Sakyo Ku, Kyoto 6068502, Japan; [Kulis, David M.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Imai, Ichiro] Hokkaido Univ, Grad Sch Fisheries Sci, Hakodate, Hokkaido 0418611, Japan	Mie University; Kyoto University; Woods Hole Oceanographic Institution; Hokkaido University	Ishikawa, A (通讯作者)，Mie Univ, Grad Sch Bioresources, 1577 Kurima Machiya Cho, Tsu, Mie 5148507, Japan.	ishikawa@bio.mie-u.ac.jp			Japan Society for the Promotion of Science [18580180]; Woods Hole Center for Oceans and Human Health; National Science Foundation [OCE-1314642]; National Institute of Environmental Health Sciences [1-P01-ES021923-01]; Grants-in-Aid for Scientific Research [18580180, 25450256] Funding Source: KAKEN; Directorate For Geosciences; Division Of Ocean Sciences [1314642] Funding Source: National Science Foundation	Japan Society for the Promotion of Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Woods Hole Center for Oceans and Human Health; National Science Foundation(National Science Foundation (NSF)); 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)); 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)); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This work was supported by a Grant-in-Aid for Scientific Research (C) (18580180) from the Japan Society for the Promotion of Science. Support for D. M. A. and D. M. K. was provided by the Woods Hole Center for Oceans and Human Health, National Science Foundation Grant (OCE-1314642) and National Institute of Environmental Health Sciences Grant (1-P01-ES021923-01).	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Plankton Res.	SEP-OCT	2014	36	5					1333	1343		10.1093/plankt/fbu048	http://dx.doi.org/10.1093/plankt/fbu048			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	AP7CJ	25221373	Green Published, Bronze			2025-03-11	WOS:000342235000014
J	Mafi, A; Ghasemi-Nejad, E; Ashouri, A; Vahidi-Nia, M				Mafi, Abradat; Ghasemi-Nejad, Ebrahim; Ashouri, Alireza; Vahidi-Nia, Mohammad			Dinoflagellate cysts from the Upper Bajocian-Lower Oxfordian of the Dalichai Formation in Binalud Mountains (NE Iran): their biostratigraphical and biogeographical significance	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Dinoflagellate cysts; Late Bajocian-Early Oxfordian; Binalud Mountains; Iran	CRETACEOUS SULAIY FORMATION; DEPOSITIONAL-ENVIRONMENTS; STRATIGRAPHY; MASHHAD; DESERT; EGYPT	The Binalud Mountains of NE Iran represent the easternmost extension of the Alborz Range. After the Mid-Cimmerian orogenic event and rapid subsidence, the deep marine sediments of the Dalichai Formation were deposited. A well-preserved section of the formation was sampled for palynological purposes. The study revealed diverse and nearly well-preserved dinoflagellate cyst assemblages. Thirty-six dinoflagellate cyst species identified lead to identification of four biozones: Cribroperidinium crispum (Late Bajocian), Dichadogonyaulax sellwoodii (Bathonian to Early Callovian), Ctenidodinium continuum (Early to Late Callovian), and Ctenidodinium tenellum (Early Oxfordian) biozones. The close similarities of dinoflagellate cyst assemblages between Binalud Mountains, NE Iran, with those of Alborz Mountains (Northern Iran) during Middle Jurassic confirm the connection between two sedimentary basins during this time in Iran. Meanwhile, this biozonation corresponds largely to that established in Northwest Europe and reveals the marine connection between NE and North of Iran with Northwest Europe and the Northwestern Tethys during the Late Bajocian to Early Oxfordian.	[Mafi, Abradat; Ashouri, Alireza; Vahidi-Nia, Mohammad] Ferdowsi Univ Mashhad, Dept Geol, Fac Sci, Mashhad, Iran; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran	Ferdowsi University Mashhad; University of Tehran	Mafi, A (通讯作者)，Ferdowsi Univ Mashhad, Dept Geol, Fac Sci, Mashhad, Iran.	Abradatmafi@gmail.com	Vahidinia, Mohammad/AAB-7110-2020; Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068; Ashouri, Ali Reza/0000-0002-2913-4913				Aboul Ela NM, 1997, ACTA U CAROLINA GEOL, V41, P45; Aboul Ela NM, 1990, MERC AIN SHAMS U EAR, V4, P95; Al-Ahmed A. A. 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J. Geosci.	SEP	2014	7	9					3683	3692		10.1007/s12517-013-0976-4	http://dx.doi.org/10.1007/s12517-013-0976-4			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AN8RP					2025-03-11	WOS:000340872000023
J	Pozdnyakov, I; Matantseva, O; Negulyaev, Y; Skarlato, S				Pozdnyakov, Ilya; Matantseva, Olga; Negulyaev, Yuri; Skarlato, Sergei			Obtaining Spheroplasts of Armored Dinoflagellates and First Single-Channel Recordings of Their Ion Channels Using Patch-Clamping	MARINE DRUGS			English	Article						dinoflagellates; ion channels; patch-clamp; spheroplasts	MARINE EUKARYOTIC ALGAE; CARBOHYDRATE SOLUTES; QUATERNARY AMMONIUM; OSMOTIC ADJUSTMENT; TERTIARY SULFONIUM; INORGANIC-IONS; CYST FORMATION; MEMBRANE; DIATOMS	Ion channels are tightly involved in various aspects of cell physiology, including cell signaling, proliferation, motility, endo- and exo-cytosis. They may be involved in toxin production and release by marine dinoflagellates, as well as harmful algal bloom proliferation. So far, the patch-clamp technique, which is the most powerful method to study the activity of ion channels, has not been applied to dinoflagellate cells, due to their complex cellulose-containing cell coverings. In this paper, we describe a new approach to overcome this problem, based on the preparation of spheroplasts from armored bloom-forming dinoflagellate Prorocentrum minimum. We treated the cells of P. minimum with a cellulose synthesis inhibitor, 2,6-dichlorobenzonitrile (DCB), and found out that it could also induce ecdysis and arrest cell shape maintenance in these microalgae. Treatment with 100-250 mu M DCB led to an acceptable 10% yield of P. minimum spheroplasts and was independent of the incubation time in the range of 1-5 days. We show that such spheroplasts are suitable for patch-clamping in the cell-attached mode and can form 1-10 GOhm patch contact with a glass micropipette, allowing recording of ion channel activity. The first single-channel recordings of dinoflagellate ion channels are presented.	[Pozdnyakov, Ilya; Matantseva, Olga; Negulyaev, Yuri; Skarlato, Sergei] Russian Acad Sci, Inst Cytol, St Petersburg 194064, Russia; [Negulyaev, Yuri] St Petersburg State Polytech Univ, Dept Med Phys, St Petersburg 195251, Russia	Russian Academy of Sciences; St. Petersburg Scientific Centre of the Russian Academy of Sciences; Institute of Cytology RAS; Peter the Great St. Petersburg Polytechnic University	Pozdnyakov, I (通讯作者)，Russian Acad Sci, Inst Cytol, Tikhoretsky Ave 4, St Petersburg 194064, Russia.	pozdnyakov@cytspb.rssi.ru; matantseva@cytspb.rssi.ru; yurineg@mail.cytspb.rssi.ru; s_skarlato@yahoo.com	Matantseva, Olga/AAE-9918-2021; Skarlato, Sergei/W-4663-2017; Pozdnyakov, Ilya/D-2705-2015; Negulyaev, Yuri/N-6531-2015	Matantseva, Olga/0000-0001-9107-8150; Pozdnyakov, Ilya/0000-0002-0236-3118; Skarlato, Sergei/0000-0001-7579-7227; Negulyaev, Yuri/0000-0002-1773-9798	Russian Foundation for Basic Research [12-04-31952-mol_a, 13-04-00703-a, 13-04-00700-a]; Molecular and Cell Biology Program of the Russian Academy of Sciences	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Molecular and Cell Biology Program of the Russian Academy of Sciences(Russian Academy of Sciences)	The authors thank Tatyana Belevich and Lyudmila Ilyash, Lomonosov Moscow State University, who kindly provided the culture of P. minimum. Hildra Timothy (New York, NY, USA) is gratefully acknowledged for the English language check. This work was supported by the Russian Foundation for Basic Research, Grants No. 12-04-31952-mol_a, 13-04-00703-a, 13-04-00700-a, and The Molecular and Cell Biology Program of the Russian Academy of Sciences (to Yuri Negulyaev).	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Drugs	SEP	2014	12	9					4743	4755		10.3390/md12094743	http://dx.doi.org/10.3390/md12094743			13	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	AQ6EL	25199048	Green Published, Green Submitted, gold			2025-03-11	WOS:000342902500004
J	Barski, M				Barski, Marcin			Shapes of organic walled dinoflagellate cysts in early diagenetic concretions-markers for mechanical compaction	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Compression; Mechanical compaction; Dinosporin; Deflandrea phosphoritica; Pareodinia ceratophora	DEPOSITIONAL-ENVIRONMENTS; PHYSICAL-PROPERTIES; EARLY CEMENTATION; MUDSTONES; DIFFERENTIATION; TEMPERATURE; LIMESTONES; ANCIENT; EXAMPLE; IMPACT	Two species of organic walled dinoflagellate cysts: Pareodinia ceratophora Eisenack 1938 (Jurassic) and Deflandrea phosphoritica Deflandre 1947 (Palaeogene) are proposed as markers for determining the mechanical compaction ratio of fine-grained rocks. The near original shapes of these species are obtained from specimens preserved in siderite and calcareous concretions occurring in mudstone host rocks of various ages. An efficient and simple light microscopy examination method of the dinoflagellate cyst height along the microscope optical axis is presented and quantitatively tested on the available material. The differences of the cyst height measurements between specimens preserved in concretions and specimens preserved in the host rock deposits reflect the compression of dinoflagellate cysts most likely due to mechanical compaction of the rocks studied. The mechanical compaction ratios revealed are about 67% for Jurassic mudstones and about 64% for Palaeogene mudstones. Further marker investigations of samples from different outcrops and strata of different ages are recommended. (C) 2014 Elsevier B.V. All rights reserved.	Univ Warsaw, Inst Geol, Fac Geol, PL-02089 Warsaw, Poland	Polish Geological Institute - National Research Institute; University of Warsaw	Barski, M (通讯作者)，Univ Warsaw, Inst Geol, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	marbar@uw.edu.pl		Barski, Marcin/0000-0002-4102-3538				[Anonymous], 1985, SPOROPOLLENIN DINOFL; APLIN AC, 1995, MAR PETROL GEOL, V12, P955, DOI 10.1016/0264-8172(95)98858-3; Barski M, 2010, GEOL CARPATH, V61, P121, DOI 10.2478/v10096-010-0005-4; BATHURST RGC, 1986, COLO SCHOOL MINES Q, V81, P1; Bjorlykke K, 2010, PETROLEUM GEOSCIENCE: FROM SEDIMENTARY ENVIRONMENTS TO ROCK PHYSICS, P113, DOI 10.1007/978-3-642-02332-3_4; Bogus K, 2012, REV PALAEOBOT PALYNO, V183, P21, DOI 10.1016/j.revpalbo.2012.07.001; Bojanowski M., 2001, MINERAL SOC POL SPEC, V18, P15; DAVAUD E, 1990, GEOLOGY, V18, P816, DOI 10.1130/0091-7613(1990)018<0816:SOESDA>2.3.CO;2; de Leeuw JW, 2006, PLANT ECOL, V182, P209, DOI 10.1007/s11258-005-9027-x; Dybkjær K, 2004, PALAEOGEOGR PALAEOCL, V206, P41, DOI 10.1016/j.palaeo.2003.12.021; Edwards LE, 2003, PALAIOS, V18, P275, DOI 10.1669/0883-1351(2003)018<0275:IDTDFT>2.0.CO;2; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; Fensome R.A., 1993, CLASSIFICATION MODER; Flugel E., 2004, MICROFACIES CARBONAT, DOI [10.1007/978-3-662-08726-8, DOI 10.1007/978-3-662-08726-8]; GAILLARD C, 1987, SEDIMENTOLOGY, V34, P585, DOI 10.1111/j.1365-3091.1987.tb00788.x; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; LASEMI Z, 1990, GEOLOGY, V18, P370, DOI 10.1130/0091-7613(1990)018<0370:NMCFDO>2.3.CO;2; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Majewski W., 2000, ACTA GEOL POL, V50, P431; Marcussen O, 2009, AAPG BULL, V93, P127, DOI 10.1306/08220808044; Matyja B.A., 2006, FIELD TRIP GUIDEBOOK, P154; Mégel J, 2010, AM J PHYS, V78, P738, DOI 10.1119/1.3285975; Mertens KN, 2009, MAR MICROPALEONTOL, V70, P54, DOI 10.1016/j.marmicro.2008.10.004; Mertens KN, 2011, BOREAS, V40, P242, DOI 10.1111/j.1502-3885.2010.00193.x; MEYERS WJ, 1983, J SEDIMENT PETROL, V53, P231; Mondol NH, 2007, MAR PETROL GEOL, V24, P289, DOI 10.1016/j.marpetgeo.2007.03.006; Munnecke Axel, 1996, Palynology, V20, P163; Pross J, 2001, PALAEOGEOGR PALAEOCL, V166, P369, DOI 10.1016/S0031-0182(00)00219-4; Puttiwongrak A, 2013, GEOTECH ENG, V44, P34; Rawsan K.J., 2001, BASIC SHIP THEORY; RICKEN W, 1987, SEDIMENTOLOGY, V34, P571, DOI 10.1111/j.1365-3091.1987.tb00787.x; Ricken W., 1986, LECT NOTES EARTH SCI, V6; Rochon A, 2009, REV PALAEOBOT PALYNO, V155, P52, DOI 10.1016/j.revpalbo.2008.12.017; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; Traverse A., 2007, Paleopalynology, VSecond; Velde B, 1996, MAR GEOL, V133, P193, DOI 10.1016/0025-3227(96)00020-5; Verleye TJ, 2012, MAR MICROPALEONTOL, V86-87, P45, DOI 10.1016/j.marmicro.2012.02.001; Versteegh GJM, 2012, ORG GEOCHEM, V43, P92, DOI 10.1016/j.orggeochem.2011.10.007; Westphal H, 1997, SEDIMENT GEOL, V112, P33, DOI 10.1016/S0037-0738(97)00033-X; Zuschin M, 2003, EARTH-SCI REV, V63, P33, DOI 10.1016/S0012-8252(03)00014-X	40	3	3	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	SEP	2014	208						50	54		10.1016/j.revpalbo.2014.05.002	http://dx.doi.org/10.1016/j.revpalbo.2014.05.002			5	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AL5BZ					2025-03-11	WOS:000339149800004
J	Albinsson, ME; Negri, AP; Blackburn, SI; Bolch, CJS				Albinsson, Maria E.; Negri, Andrew P.; Blackburn, Susan I.; Bolch, Christopher J. S.			Bacterial Community Affects Toxin Production by <i>Gymnodinium</i> <i>catenatum</i>	PLOS ONE			English	Article							PARALYTIC SHELLFISH TOXINS; GENE-CLUSTER; SAXITOXIN BIOSYNTHESIS; LIQUID-CHROMATOGRAPHY; CELL-CYCLE; ALEXANDRIUM; GROWTH; DIVERSITY; PROFILES; TOXICITY	The paralytic shellfish toxin (PST)-producing dinoflagellate Gymnodinium catenatum grows in association with a complex marine bacterial community that is both essential for growth and can alter culture growth dynamics. Using a bacterial community replacement approach, we examined the intracellular PST content, production rate, and profile of G. catenatum cultures grown with bacterial communities of differing complexity and composition. Clonal offspring were established from surface-sterilized resting cysts (produced by sexual crosses of strain GCDE06 and strain GCLV01) and grown with: 1) complex bacterial communities derived from each of the two parent cultures; 2) simplified bacterial communities composed of the G. catenatum-associated bacteria Marinobacter sp. strain DG879 or Alcanivorax sp. strain DG881; 3) a complex bacterial community associated with an untreated, unsterilized sexual cross of the parents. Toxin content (STX-equivalent per cell) of clonal offspring (134-197 fmol STX cell(-1)) was similar to the parent cultures (169-206 fmol STX cell(-1)), however cultures grown with single bacterial types contained less toxin (134-146 fmol STX cell(-1)) than offspring or parent cultures grown with more complex mixed bacterial communities (152-176 fmol STX cell(-1)). Specific toxin production rate (fmol STX day(-1)) was strongly correlated with culture growth rate. Net toxin production rate (fmol STX cell(-1) day(-1)) did not differ among treatments, however, mean net toxin production rate of offspring was 8-fold lower than the parent cultures, suggesting that completion of the sexual lifecycle in laboratory cultures leads to reduced toxin production. The PST profiles of offspring cultures were most similar to parent GCDE06 with the exception of cultures grown with Marinobacter sp. DG879 which produced higher proportions of dcGTX2+3 and GC1+2, and lower proportions of C1+2 and C3+4. Our data demonstrate that the bacterial community can alter intracellular STX production of dinoflagellates. In G. catenatum the mechanism appears likely to be due to bacterial effects on dinoflagellate physiology rather than bacterial biotransformation of PST toxins.	[Albinsson, Maria E.; Bolch, Christopher J. S.] Univ Tasmania, Australian Maritime Coll, Natl Ctr Marine Conservat & Resource Sustainabil, Launceston, Tas 7250, Australia; [Albinsson, Maria E.; Blackburn, Susan I.] Commonwealth Sci & Ind Res Org, Hobart, Tas, Australia; [Negri, Andrew P.] Australian Inst Marine Sci, Townsville, Qld 4810, Australia	University of Tasmania; Australian Maritime College; Commonwealth Scientific & Industrial Research Organisation (CSIRO); Australian Institute of Marine Science	Albinsson, ME (通讯作者)，Univ Tasmania, Australian Maritime Coll, Natl Ctr Marine Conservat & Resource Sustainabil, Launceston, Tas 7250, Australia.	Maria.Albinsson@csiro.au	Blackburn, Susan/M-9955-2013; Bolch, Christopher/J-7619-2014; Negri, Andrew/G-9909-2017	Negri, Andrew/0000-0003-1388-7395	Aquafin CRC Project [4.2(2)]; Australian Postgraduate Scholarship - The Thomas Crawford Memorial Scholarship	Aquafin CRC Project(Australian GovernmentDepartment of Industry, Innovation and ScienceCooperative Research Centres (CRC) Programme); Australian Postgraduate Scholarship - The Thomas Crawford Memorial Scholarship	This research was sponsored by the Aquafin CRC Project 4.2(2). A whole-of-ecosystem assessment of environmental issues for salmonid aquaculture. M. E. Albinsson was supported by an Australian Postgraduate Scholarship - The Thomas Crawford Memorial Scholarship while doing this research. 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	Small, HJ; Meyer, GR; Stentiford, GD; Dunham, JS; Bateman, K; Shields, JD				Small, Hamish J.; Meyer, Gary R.; Stentiford, Grant D.; Dunham, Jason S.; Bateman, Kelly; Shields, Jeffrey D.			<i>Ameson metacarcini</i> sp nov (Microsporidia) infecting the muscles of Dungeness crabs <i>Metacarcinus magister</i> from British Columbia, Canada	DISEASES OF AQUATIC ORGANISMS			English	Article						Ameson; Crab; Crustacea; Parasite; Microspora	LOBSTER PANULIRUS-ARGUS; NOSEMA SP SPRAGUE; ULTRASTRUCTURAL OBSERVATIONS; CANCER-MAGISTER; FINE-STRUCTURE; SEX-RATIO; DINOFLAGELLATE; POPULATIONS; PREVALENCE; DIMORPHISM	The Dungeness crab Metacarcinus magister supports a large and valuable fishery along the west coast of North America. Since 1998, Dungeness crabs exhibiting pink- to orange-colored joints and opaque white musculature have been sporadically observed in low prevalence from the Fraser River delta of British Columbia, Canada. We provide histological, ultrastructural, and molecular evidence that this condition is caused by a new microsporidian parasite. Crabs displaying gross symptoms were confirmed to have heavy infections of ovoid-shaped microsporidian spores (similar to 1.8 x 1.4 mu m in size) within muscle bundles of the skeletal musculature. The parasite apparently infected the outer periphery of each muscle bundle, and then proliferated into the muscle fibres near the centre of each infected bundle. Light infections were observed in heart tissues, and occasionally spores were observed within the fixed phagocytes lining the blood vessels of the hepatopancreas. Transmission electron microscopy (TEM) revealed multiple life stages of a monokaryotic microsporidian parasite within the sarcoplasm of muscle fibres. Molecular analysis of partial small subunit rRNA sequence data from the new species revealed an affinity to Ameson, a genus of Microsporidia infecting marine crustaceans. Based on morphological and molecular data, the new species is distinct from Nadelspora canceri, a related microsporidian that also infects the muscles of this host. At present, little is known about the distribution, seasonality, and transmission of A. metacarcini in M. magister.	[Small, Hamish J.; Shields, Jeffrey D.] Coll William & Mary, Virginia Inst Marine Sci, Dept Environm & Aquat Anim Hlth, Gloucester Point, VA 23062 USA; [Meyer, Gary R.; Dunham, Jason S.] Fisheries & Oceans Canada, Pacific Biol Stn, Dept Fisheries & Oceans, Nanaimo, BC V9T 6N7, Canada; [Stentiford, Grant D.; Bateman, Kelly] European Union Reference Lab Crustacean Dis, Ctr Environm Fisheries & Aquaculture Sci, Weymouth Lab, Weymouth DT4 8UB, Dorset, England	William & Mary; Virginia Institute of Marine Science; Fisheries & Oceans Canada; Centre for Environment Fisheries & Aquaculture Science	Small, HJ (通讯作者)，Coll William & Mary, Virginia Inst Marine Sci, Dept Environm & Aquat Anim Hlth, POB 1346, Gloucester Point, VA 23062 USA.	hamish@vims.edu	Stentiford, Grant/I-5567-2019	Small, Hamish/0009-0007-7450-8447; Stentiford, Grant/0000-0001-6597-5413; Bateman, Kelly/0000-0002-9124-2333; Shields, Jeffrey D./0000-0002-2658-4572	NSF EID Grant [OCE 0723662]; European Commission [C5839]; UK Department for Environment, Food and Rural Affairs [FB002]	NSF EID Grant; European Commission(European Union (EU)European Commission Joint Research Centre); UK Department for Environment, Food and Rural Affairs(Department for Environment, Food & Rural Affairs (DEFRA))	The following people assisted in collecting and sampling Dungeness crabs: fisheries staff Georg Jorgensen, Sarah Davies, and Sandra Bassett, and the Canadian Coast Guard crew of the CCGV 'Neocaligus'. H.J.S. and J.D.S. were supported by NSF EID Grant OCE 0723662. G.D.S. and K.B. were supported by grants from the European Commission (#C5839) and UK Department for Environment, Food and Rural Affairs (#FB002) (both to G.D.S.). This paper is Contribution No. 3364 of the Virginia Institute of Marine Science, College of William & Mary.	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Aquat. Org.	AUG 11	2014	110	3					213	225		10.3354/dao02754	http://dx.doi.org/10.3354/dao02754			13	Fisheries; Veterinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Veterinary Sciences	AQ6LI	25114045	Bronze			2025-03-11	WOS:000342923400006
J	Morquecho, L; Alonso-Rodríguez, R; Martínez-Tecuapacho, GA				Morquecho, Lourdes; Alonso-Rodriguez, Rosalba; Anahi Martinez-Tecuapacho, Gladys			Cyst morphology, germination characteristics, and potential toxicity of <i>Pyrodinium bahamense</i> in the Gulf of California	BOTANICA MARINA			English	Article						cysts; germination; Gulf of California; Mexico; paralytic shellfish toxins; Polysphaeridium zoharyi; Pyrodinium bahamense; saxitoxin	SHELLFISH POISONING TOXINS; DINOFLAGELLATE-CYSTS; VAR. COMPRESSUM; PROTOCERATIUM-RETICULATUM; FLUORESCENCE DETECTION; SURFACE SEDIMENTS; MEXICO; SALINITY; PLATE; BAY	Pyrodinium bahamense is a meroplanktonic dinoflagellate that produces paralytic shellfish toxins that cause human poisoning along tropical and subtropical coasts. Cyst morphology, germination characteristics, and toxicity were investigated using samples from Isla San Jose in the Gulf of California. Morphology was observed through light and scanning electron microscopy. Germination was tested at different temperature (15 degrees C-35 degrees C) and salinity (15-35) conditions in different culture media (natural seawater, GSe, and f/2). To elucidate toxicity of vegetative cells grown from cyst germination, nine strains were subject to toxin analyses through fluorescence high-performance liquid chromatography. Morphological features and size of cysts generally agree with previous descriptions, particularly morphotypes found in the subtropical North Atlantic, where P. bahamense var. bahamense occurs. Cysts exhibit thermophilic and euryhaline characteristics. Highest germination occurred from 20 degrees C to 35 degrees C with the peak between 25 degrees C and 30 degrees C. Excystment occurred at salinities from 20 to 35. Germination occurred in the three culture media, but was highest in the optimal temperature range in the culture medium that included terrestrial soil extract and selenium. Only one strain exhibited toxicity with high saxitoxin concentration (95 pg STX eq cell(-1)).	[Morquecho, Lourdes] Ctr Invest Biol Noroeste CIBN, La Paz 23096, Baja California, Mexico; [Alonso-Rodriguez, Rosalba; Anahi Martinez-Tecuapacho, Gladys] Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Unidad Acad Mazatlan, Mazatlan 82040, Sinaloa, Mexico	CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Universidad Nacional Autonoma de Mexico	Morquecho, L (通讯作者)，Ctr Invest Biol Noroeste CIBN, Calle IPN 195, La Paz 23096, Baja California, Mexico.	lamorquecho@cibnor.mx	Morquecho, Lourdes/JPY-0626-2023; Alonso-Rodriguez, Rosalba/U-9896-2017	Morquecho, Lourdes/0000-0003-2963-8836; Alonso-Rodriguez, Rosalba/0000-0001-7716-3869	CIBNOR [PC3.3, 749-0]; SEMARNAT-CONACYT [2002-C01-0161]; ICMyL-UNAM [326]; IAEA-ARCAL [RLA/7/014]	CIBNOR; SEMARNAT-CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); ICMyL-UNAM; IAEA-ARCAL	Miguel A. Aguilar, Horacio Bervera, Jorge Calvillo, Mario Cota, and Juan J. Ramirez provided technical assistance in the field. Amada Reyes and Ariel Cruz provided technical assistance in taxonomy and eco-physiology of marine microalgae and scanning electron microscopy. Ira Fogel provided editorial support and advice. All are at CIBNOR. German Ramirez of UNAM at Mazatlan provided suggestions for statistical analyses. This study was supported by CIBNOR projects PC3.3 and 749-0, SEMARNAT-CONACYT grant 2002-C01-0161), ICMyL-UNAM grant ICML #326, and IAEA-ARCAL grant RLA/7/014.	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L, 1996, HARMFUL TOXIC ALGAL, P189; WALL D, 1969, J PHYCOL, V5, P140, DOI 10.1111/j.1529-8817.1969.tb02595.x; Wall D., 1974, BLACK SEA GEOLOGY CH, V20, P364	57	17	17	1	23	WALTER DE GRUYTER GMBH	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055	1437-4323		BOT MAR	Bot. Marina	AUG	2014	57	4					303	314		10.1515/bot-2013-0121	http://dx.doi.org/10.1515/bot-2013-0121			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AO5CD					2025-03-11	WOS:000341358300007
J	Mueller, S; Veld, H; Nagy, J; Kürschner, WM				Mueller, Steven; Veld, Harry; Nagy, Jeno; Kurschner, Wolfram M.			Depositional history of the Upper Triassic Kapp Toscana Group on Svalbard, Norway, inferred from palynofacies analysis and organic geochemistry	SEDIMENTARY GEOLOGY			English	Article						Late Triassic; Spitsbergen; Palynofacies; Rock-Eval; Kapp Toscana Group	SEA-LEVEL CHANGES; PLUVIAL-EVENT; TRANSITION; MATTER; MIDDLE; BASIN; PALYNOSTRATIGRAPHY; STRATIGRAPHY; PALYNOLOGY; SECTION	Upper Triassic sediments in the Svalbard Archipelago were deposited in several transgressive-regressive cycles. Understanding their deposition and distribution is of vital importance because of their potential as hydrocarbon reservoir rocks. In this study we integrate palynofacies with organic geochemistry in order to reconstruct the depositional environment of the upper Botneheia Fm up to the lower the Knorringflellet Fm from two sections located in central Spitsbergen, for which distinctive palynofacies zones have been distinguished. These are mainly terrestrially dominated but occasionally contain amorphous organic matter and marine palynomorphs. Rock-Eval pyrolysis reveals overall mature kerogen type III/IV samples. Our results indicate that at least partially restricted marine conditions prevailed during deposition of the Botneheia Fm. The Botneheia Fm is overlain by a regressive cycle from the lower part of the Tschermakfjellet Fm up to the top of the De Geerdalen Fm with terrestrially dominated palynofacies assemblages. The Knorringflellet Fm contains increased marine palynofacies and marine dinoflagellate cysts, which is in accordance with a transgression at the base of this unit. This study integrates for the first time in the Spitsbergen area quantitative palynofacies and sedimentary organic matter characterization, and shows the generally accepted paleo-environmental development for the Svalbard Archipelago. (C) 2014 Elsevier B.V. All rights reserved.	[Mueller, Steven; Nagy, Jeno; Kurschner, Wolfram M.] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; [Veld, Harry] Deltares, NL-3508 AL Utrecht, Netherlands; [Kurschner, Wolfram M.] Univ Oslo, Ctr Earth Evolut & Dynam, N-0316 Oslo, Norway	University of Oslo; Deltares; University of Oslo	Mueller, S (通讯作者)，Univ Oslo, Dept Geosci, POB 1047 Blindern, N-0316 Oslo, Norway.	steven.mueller@geo.uio.no	Kürschner, Wolfram/B-4724-2009	Mueller, Steven/0000-0002-9604-9671; Kurschner, Wolfram Michael/0000-0001-6883-6486	Norwegian Research Council (NFR) [14362]; NORSTRAT	Norwegian Research Council (NFR)(Research Council of Norway); NORSTRAT	WMK and SM acknowledge the financial support by the Norwegian Research Council (NFR) project number (14362), NORSTRAT. We are grateful to G. Mangerud (University of Bergen) on the fruitful discussions and to A Uren (Robertson GeoSpec, A CGG Company) for the helpful comments on the manuscript. Constructive comments by editor J. 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Geol.	AUG 1	2014	310						16	29		10.1016/j.sedgeo.2014.06.003	http://dx.doi.org/10.1016/j.sedgeo.2014.06.003			14	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AN8JQ					2025-03-11	WOS:000340850900002
J	Herzi, F; Jean, N; Hlaili, AS; Mounier, S				Herzi, Faouzi; Jean, Natacha; Hlaili, Asma Sakka; Mounier, Stephane			THREE-DIMENSIONAL (3-D) FLUORESCENCE SPECTROSCOPY ANALYSIS OF THE FLUORESCENT DISSOLVED ORGANIC MATTER RELEASED BY THE MARINE TOXIC DINOFLAGELLATE <i>ALEXANDRIUM CATENELLA</i> EXPOSED TO METAL STRESS BY ZINC OR LEAD	JOURNAL OF PHYCOLOGY			English	Article						3-D fluorescence spectroscopy; A; lexandrium catenella; exudation; fluorescent dissolved organic matter; PARAFAC; trace metals	HARMFUL ALGAL BLOOMS; CUPRIC ION ACTIVITY; COPPER; PHYTOPLANKTON; GROWTH; DIMETHYLSULFONIOPROPIONATE; CHROMATOGRAPHY; TERRESTRIAL; LIGANDS; ESTUARY	We investigated the effects of zinc or lead on growth and on exudation of fluorescent dissolved organic matter (FDOM) by the marine toxic dinoflagellate Alexandrium catenella (Whedon & Kofoid) Balech. The species was exposed to increasing free zinc (1.34x10(-7)M-3.98x10(-6)M) or lead (5.13x10(-9)M-1.82x10(-7)M) concentra-tions. Low metal levels ([Zn2+]=1.34x10(-7)M; [Pb2+]=5.13x10(-9)M) had no effect on cell growth. Toxic effects were observed from higher metal contamination ([Zn2+]=3.98x10(-6)M; [Pb2+]=6.54x10(-8)M), as a conversion of vegetative cells into cysts. Analysis of the released FDOM by three-dimensional (3-D) fluorescence spectroscopy was achieved, using the parallel factor analysis (PARAFAC). The PARAFAC modeling revealed four components associated with two contributions: one related to the biological activity; the other linked to the organic matter decomposition in the culture medium. The C1 component combined a tryptophan peak and characteristics of humic substances, whereas the C2 component was considered as a tryptophan protein fluorophore. The two others C3 and C4 components were associated with marine organic matter production. Relea-sed fluorescent substances were induced by low ([Zn2+]=1.34x10(-7)M; [Pb2+]=5.13x10(-9)M) and moderate([Zn2+]=6.21x10(-7)M; [Pb2+]=2.64x10(-9)M) metal concentrations, suggesting the activation of cellular mechanisms in response to metal stress, to exudate FDOM that could complex metal cations and reduce their toxicity toward A.catenella cells.	[Herzi, Faouzi; Hlaili, Asma Sakka] Univ Carthage, Lab Cytol Vegetale & Phytoplanctonol, Fac Sci Bizerte, Dept Sci Vie, Jarzouna 7021, Bizerte, Tunisia; [Herzi, Faouzi; Jean, Natacha; Mounier, Stephane] Univ Sud Toulon Var, Lab Proc Transferts & Echanges Environm PROTEE EA, Equipe Chim Analyt & Proc Transferts Environm, F-83957 La Garde, France	Universite de Carthage	Herzi, F (通讯作者)，Univ Carthage, Lab Cytol Vegetale & Phytoplanctonol, Fac Sci Bizerte, Dept Sci Vie, Jarzouna 7021, Bizerte, Tunisia.	herzi_faouzi@univ-tln.fr	HLAILI, Asma/AAD-9610-2019; MOUNIER, Stephane Jean Louis/P-9135-2015	MOUNIER, Stephane Jean Louis/0000-0002-9624-0230	ARCUS CERES projet (Region PACA-MAE)	ARCUS CERES projet (Region PACA-MAE)(Region Provence-Alpes-Cote d'Azur)	This work was supported by the ARCUS CERES projet (Region PACA-MAE). We are deeply indebted to Pr. Yves COLLOS and to Drs. Estelle MASSERET and Mohamed LAABIR from the Laboratory ECOSYM UMR 5119 of the Montpellier 2 University, for providing us with the A. catenella strain ACT03 used in this study.	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Phycol.	AUG	2014	50	4					665	674		10.1111/jpy.12181	http://dx.doi.org/10.1111/jpy.12181			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AN3BO	26988450	Green Submitted			2025-03-11	WOS:000340460100006
J	de Souza, KB; Jephson, T; Hasper, TB; Carlsson, P				de Souza, Karine Bresolin; Jephson, Therese; Hasper, Thomas Berg; Carlsson, Per			Species-specific dinoflagellate vertical distribution in temperature-stratified waters	MARINE BIOLOGY			English	Article							HETEROCAPSA-TRIQUETRA; MARINE-PHYTOPLANKTON; DINOPHYSIS-ACUMINATA; MOTILE PHYTOPLANKTON; CYST FORMATION; CELL-DIVISION; BALTIC SEA; RED TIDE; MIGRATION; DIEL	Thermal stratification is increasing in strength as a result of higher surface water temperature. This could influence the vertical distribution of vertically migrating dinoflagellates. We studied the diel vertical distribution of the dinoflagellates Heterocapsa triquetra and Prorocentrum minimum using stratified laboratory columns with two thermoclines of different strength (Delta TA degrees A = 10 or 17 A degrees C), with below cline temperature of 8 A degrees C. Above the thermocline, nutrient depletion simulated the natural summer conditions in the Baltic Sea. Our study shows that H. triquetra and P. minimum can behave differently in terms of their vertical occurrence, both in space and in time when subjected to thermoclines of different strength. Also, both dinoflagellate species showed species-specific distribution patterns. In the Delta TA degrees A = 10 A degrees C treatment, H. triquetra cells performed a diel vertical migration (DVM) behavior just above the thermocline, but not in the Delta TA degrees A = 17 A degrees C. In the Delta TA degrees A = 17 A degrees C, the cells did not migrate and cell densities in the water column decreased over time. Opposing results were observed for P. minimum, where a DVM pattern was found exclusively below the thermocline of Delta TA degrees A = 17 A degrees C, while in the Delta TA degrees A = 10 A degrees C treatment, no clear DVM pattern was observed, and the highest number of cells were found in the cold bottom water. These results indicate that an increase in thermal stratification can influence species-specific dinoflagellate distribution, behavior, and survival.	[de Souza, Karine Bresolin; Hasper, Thomas Berg] Univ Gothenburg, Dept Biol & Environm Sci, S-40530 Gothenburg, Sweden; [Jephson, Therese; Carlsson, Per] Lund Univ, Dept Biol, S-22362 Lund, Sweden	University of Gothenburg; Lund University	Jephson, T (通讯作者)，Lund Univ, Dept Biol, Solvegatan 37, S-22362 Lund, Sweden.	Therese.Jephson@biol.lu.se			Royal Swedish Academy of Sciences; Carl Trygger foundation	Royal Swedish Academy of Sciences; Carl Trygger foundation	We thank Monica Appelgren (University of Gothenburg Marine Culture-GUMACC), University of Gothenburg, Department of Biological and Environmental Sciences, for supplying the dinoflagellate cultures. We also thank the Royal Swedish Academy of Sciences and the Carl Trygger foundation for funding this project.	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Biol.	AUG	2014	161	8					1725	1734		10.1007/s00227-014-2446-2	http://dx.doi.org/10.1007/s00227-014-2446-2			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	AM5LQ					2025-03-11	WOS:000339900700003
J	El-Soughier, MI; Deaf, AS; Mahmoud, MS				El-Soughier, Maher I.; Deaf, Amr S.; Mahmoud, Magdy S.			Palynostratigraphy and palaeoenvironmental significance of the Cretaceous palynomorphs in the Qattara Rim-1X well, North Western Desert, Egypt	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Cretaceous; Palynostratigraphy; Palynofacies; Palaeoecology; North western Egypt	DINOFLAGELLATE CYSTS; PALYNOLOGY; BASIN; STRATIGRAPHY; DEPOSITS; SEDIMENTS; BOREHOLE; NIGERIA; AFRICA; POLLEN	Palynological and palynofacies analyses were carried out on some Cretaceous samples from the Qattara Rim-1X borehole, north Western Desert, Egypt. The recorded palynoflora enabled the recognition of two informal miospore biozones arranged from oldest to youngest as Elaterosporites klaszii-Afropollis jardinus Assemblage Zone (mid Albian) and Elaterocolpites castelainii-Afropollis kahramanensis Assemblage Zone (late Albian-mid Cenomanian). A poorly fossiliferous but however, datable interval (late Cenomanian-Turonian to ?Campanian-Maastrichtian) representing the uppermost part of the studied section was also recorded. The palynofacies and visual thermal maturation analyses indicate a mature terrestrially derived organic matter (kerogen III) dominates the sediments of the Kharita and Bahariya formations and thus these two formations comprise potential mature gas source rocks. The sediments of the Abu Roash Formation are mostly dominated by mature amorphous organic matter (kerogen II) and the formation is regarded as a potential mature oil source rock in the well. The palynomorphs and palynofacies analyses suggest deposition of the clastics of the Kharita and Bahariya formations (middle Albian and upper Albian-middle Cenomanian) in a marginal marine setting under dysoxic-anoxic conditions. By contrast, the mixed clastic-carbonate sediments of the Abu Roash Formation (upper Cenomanian-Turonian) and the carbonates of the Khoman Formation (?Campanian-Maastrichtian) were mainly deposited in an inner shallow marine setting under prevailing suboxic-anoxic conditions as a result of the late Cenomanian and the Campanian marine transgressions. This environmental change from marginal to open (inner shelf) basins reflects the vertical change in the type of the organic matter and its corresponding hydrocarbon-prone types. A regional warm and semi-arid climate but with a local humid condition developed near/at the site of the well is thought to have prevailed.	[El-Soughier, Maher I.] Aswan Univ, Dept Geol, Fac Sci, Aswan 81528, Egypt; [Deaf, Amr S.; Mahmoud, Magdy S.] Assiut Univ, Dept Geol, Fac Sci, Assiut 71516, Egypt	Egyptian Knowledge Bank (EKB); Aswan University; Egyptian Knowledge Bank (EKB); Assiut University	El-Soughier, MI (通讯作者)，Aswan Univ, Dept Geol, Fac Sci, Aswan 81528, Egypt.	miabdelrahim@yahoo.com	Mahmoud, Magdy/ABD-1262-2020; Deaf, Amr/AAF-6269-2020	Deaf, Amr/0000-0002-5073-7911	State Key Laboratory of Palaeobiology and Stratigraphy, Chinese Academy of Sciences, China [65335]	State Key Laboratory of Palaeobiology and Stratigraphy, Chinese Academy of Sciences, China	The first author thanks Prof. Zhiyan Zhou, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, for offering research stay in China and for his support. The present study is supported by the State Key Laboratory of Palaeobiology and Stratigraphy, Chinese Academy of Sciences, China under No. 65335. We are grateful to authorities of Egyptian General Petroleum Corporation for providing samples and borehole log.	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J. Geosci.	AUG	2014	7	8					3051	3068		10.1007/s12517-013-0954-x	http://dx.doi.org/10.1007/s12517-013-0954-x			18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AM4IT					2025-03-11	WOS:000339817900007
J	Fertouna-Bellakhal, M; Dhib, A; Béjaoui, B; Turki, S; Aleya, L				Fertouna-Bellakhal, Mouna; Dhib, Amel; Bejaoui, Bechir; Turki, Souad; Aleya, Lotfi			Driving factors behind the distribution of dinocyst composition and abundance in surface sediments in a western Mediterranean coastal lagoon: Report from a high resolution mapping study	MARINE POLLUTION BULLETIN			English	Article						Dinocysts; Mapping; Enviromental factors; Hydrodynamics; Bizerte Lagoon	DINOFLAGELLATE CYST DISTRIBUTION; NORTHWESTERN INDIAN-OCEAN; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; RESTING STAGES; BALLAST WATER; BUZZARDS BAY; TOKYO-BAY; SEA; SOUTH	Species composition and abundance of dinocysts in relation to environmental factors were studied at 123 stations of surface sediment in Bizerte Lagoon. Forty-eight dinocyst types were identified, mainly dominated by Brigantidinium simplex, Votadinum spinosum, Alexandrium pseudogonyaulax, Alexandrium catenella, and Lingulodinum machaerophorum along with many round brown cysts and spiny round brown cysts. Cysts ranged from 1276 to 20126 cysts g(-1) dry weight sediment. Significant differences in cyst distribution pattern were recorded among the zones, with a higher cyst abundance occurring in the lagoon's inner areas. Redundancy analyses showed two distinct associations of dinocysts according to location and environmental variables. Ballast water discharges are potential introducers of non-indigenous species, especially harmful ones such as A. catenella and Polysphaeridium zoharyi, with currents playing a pivotal role in cyst distribution. Findings concerning harmful cyst species indicate potential seedbeds for initiation of future blooms and outbreaks of potentially toxic species in the lagoon. (C) 2014 Elsevier Ltd. All rights reserved.	[Fertouna-Bellakhal, Mouna] Inst Super Peche & Aquaculture Bizerte, Unite Rech Exploitat Milieux Aquat, Bizerte 7080, Tunisia; [Fertouna-Bellakhal, Mouna; Dhib, Amel; Aleya, Lotfi] Univ Franche Comte, Lab Chronoenvironm, UMR CNRS 6249, F-25030 Besancon, France; [Fertouna-Bellakhal, Mouna; Dhib, Amel; Turki, Souad] INSTM, Ctr Goulette, Salammbo 2025, Tunisia; [Bejaoui, Bechir] INSTM, Salammbo 2025, Tunisia	Universite de Franche-Comte; Institut National des Sciences et Technologies de la Mer; Institut National des Sciences et Technologies de la Mer	Aleya, L (通讯作者)，Univ Franche Comte, Lab Chronoenvironm, UMR CNRS 6249, F-25030 Besancon, France.	lotfi.aleya@univ-fcomte.fr	Béjaoui, Béchir/AGR-1419-2022					Abdenadher M, 2012, ESTUAR COAST SHELF S, V106, P102, DOI 10.1016/j.ecss.2012.04.029; American Public Health Association, 1992, STANDARD METHODS EXA; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; [Anonymous], MANUAL HARMFUL MARIN; [Anonymous], MAR MICROPALEO; 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Pollut. Bull.	JUL 15	2014	84	1-2					347	362		10.1016/j.marpolbul.2014.04.041	http://dx.doi.org/10.1016/j.marpolbul.2014.04.041			16	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	AL0GF	24841716				2025-03-11	WOS:000338804700050
J	Triki, HZ; Daly-Yahia, OK; Malouche, D; Komiha, Y; Deidun, A; Brahim, M; Iaabir, M				Triki, Habiba Zmerli; Daly-Yahia, Ons Kefi; Malouche, Dhafer; Komiha, Yosr; Deidun, Alan; Brahim, Mouldi; Iaabir, Mohamed			Distribution of resting cysts of the potentially toxic dinoflagellate <i>Alexandrium pseudogonyaulax</i> in recently-deposited sediment within Bizerte Lagoon (Mediterranean coast, Tunisia)	MARINE POLLUTION BULLETIN			English	Article						Alexandrium pseudogonyaulax; Harmful algae; Resting cysts; Mapping; Mediterranean Lagoon of Bizerte; Sediment characteristics	SPATIAL-DISTRIBUTION; SURFACE SEDIMENTS; GONYAULAX-EXCAVATA; BENTHIC CYSTS; EUTROPHICATION; BAY; AUTOCORRELATION; DYNAMICS; GULF	This study investigated the spatial distribution of Alexandrium pseudogonyaulax resting cysts in recently-deposited sediment of Bizerte lagoon (South-Western Mediterranean, Tunisia). This lagoon is the subject of many anthropogenic impacts, such as holding important fishing and aquaculture activities. A. pseudogonyaulax has been shown to produce Goniodomin A, which is a biologically-active compound. We showed that this dinoflagellate produces two types of resting cysts, which could be distinguished by the presence or the absence of a paratabulate wall. The average cyst density across the whole lagoon was rather high, reaching 639 cysts g(-1) of dry sediment (DS). Cyst densities varied widely among the sampled stations, with the highest density of 1685 cyst g(-1) DS being recorded at station 51 near a mussel farm. With respect to sediment characteristics, the highest cyst densities were found within silty sediments with high water content values. The distribution of A. pseudongoyaulax cysts in Bizerte lagoon appears to be related to hydrodynamic factors. (C) 2014 Elsevier Ltd. All rights reserved.	[Triki, Habiba Zmerli; Daly-Yahia, Ons Kefi; Komiha, Yosr; Iaabir, Mohamed] Carthage Univ, IRESA, Tunisian Natl Agron Inst INAT, UR Marine Biol FST El Manar 1, Tunis 1082, Tunisia; [Malouche, Dhafer] Ecole Super Stat & Anal Informat, Tunis, Tunisia; [Deidun, Alan] Univ Malta, IOI Malta Operat Ctr, Msida, Malta; [Brahim, Mouldi] INSTM, Tunis, Tunisia; [Iaabir, Mohamed] Univ Montpellier 2, Lab Ecol Syst Marins Cotiers ECOSYM, UMR CNRS IRD IFREMER UM1 UM2 5119, F-34095 Montpellier, France	Universite de Carthage; University of Malta; Institut National des Sciences et Technologies de la Mer; Universite de Montpellier	Triki, HZ (通讯作者)，Carthage Univ, IRESA, Tunisian Natl Agron Inst INAT, UR Marine Biol FST El Manar 1, 43 Ave Charles Nicolle, Tunis 1082, Tunisia.	bibarouma@hotmail.fr	Malouche, Dhafer/HOF-7025-2023	Deidun, Alan/0000-0002-6919-5374; Malouche, Dhafer/0000-0002-0494-7141	JEAI ECO-BIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program - IRD (Institut Francais pour la Recherche et le Developpement), IRD; TOTAL Foundation	JEAI ECO-BIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program - IRD (Institut Francais pour la Recherche et le Developpement), IRD; TOTAL Foundation(Total SA)	This work benefitted from financial supports from the JEAI ECO-BIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program funded by IRD (Institut Francais pour la Recherche et le Developpement), IRD also funded 2 months stay of Dr. Mohamed Laabir in Tunis (INAT). Thanks to TOTAL Foundation for funding LAGUNOTOX project which supported financially the stay of Mrs Triki-Zmerli in Montpellier.	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Pollut. Bull.	JUL 15	2014	84	1-2					172	181		10.1016/j.marpolbul.2014.05.014	http://dx.doi.org/10.1016/j.marpolbul.2014.05.014			10	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	AL0GF	24878303	Green Published			2025-03-11	WOS:000338804700033
J	Willumsen, PS; Dale, B; Jolley, DW; Laursen, GV				Willumsen, Pi Suhr; Dale, Barrie; Jolley, David W.; Laursen, Gitte Vestergaard			Palynostratigraphy and palaeoenvironmental shifts in Oligocene and Miocene strata from offshore Angola, west-central Africa	PALYNOLOGY			English	Article						biostratigraphy; Late Oligocene to earliest Early Miocene; spores-pollen; west-central Africa; taxonomy offshore Angola; dinoflagellate cysts; palaeoecology	DINOFLAGELLATE CYSTS; SEA; GULF; STRATIGRAPHY; FORAMINIFERA; SEDIMENTS; SYSTEM; DELTA; WELL; SUEZ	A palynological investigation of 15 ditch cutting samples from Borehole 8, located off the Angolan coast, west-central Africa, revealed Late Oligocene (Chattian) to latest Middle to earliest Early Miocene (Serravallian/earliest Tortonian?) marine dinoflagellate cysts, freshwater colonial algae and terrestrial palynomorphs. Various early Miocene pollen characterising the Verrutricolporites rotundiporus Zone of Legoux (1978) confirm the location of the Oligocene-Miocene boundary in relation to a new short-ranging early Miocene dinoflagellate cyst taxon Cristadinium headii sp. nov. The Oligocene to Miocene dinoflagellate cyst assemblages reflect three periods, A-C, with high palaeoproductivity, corresponding to periods in the latest Oligocene (late Chattian), Early Miocene (late Aquitanian-early Burdigalian?) and the base of the Middle Miocene (Langhian). Early to middle Miocene acme intervals of Cleistosphaeridium placacanthum and Cribroperidinium tenuitabulatum are considered to reflect two regional oceanographic events due to intense upwelling along the West African coast. A distinct Early Miocene episode of brackish-water outflow from the nearby Angolan mainland is also reflected by the palynological assemblages, perhaps linked to the global Mi-1 event. Changes in relative abundance of grass pollen indicate a gradual change towards a drier and perhaps also warmer Burdigalian-Langhian climate during which the Angolan savanna developed, followed by cooler and perhaps more humid conditions following the Miocene Climatic Optimum.	[Willumsen, Pi Suhr; Dale, Barrie] Univ Oslo, Dept Geol, N-0316 Oslo, Norway; [Jolley, David W.] Kingss Coll, Dept Geol & Petr Geol, Aberdeen AB9 2UE, Scotland; [Laursen, Gitte Vestergaard] Statoil ASA, N-4035 Stavanger, Norway; [Willumsen, Pi Suhr] Aarhus Univ, Dept Geosci, DK-8000 Aarhus C, Denmark	University of Oslo; Equinor; Aarhus University	Willumsen, PS (通讯作者)，Univ Oslo, Dept Geol, PO 1047 Blindern, N-0316 Oslo, Norway.	ps_willumsen@hotmail.com		Jolley, David/0000-0003-0909-2952	Statoil ASA	Statoil ASA	Dr. K. Dybkjaer (GEUS) and M. Jones (Palynological Laboratory Services Scotland) are thanked for their assistance in connection with the palynological processing. Prof. F. Oboh-Ikuenobe (Missouri University of Science and Technology) for constructive advice during the publishing process. The palynological data presented were collected as part of a postdoctoral project carried out at Oslo University, Department of Geology, during 2004 to 2007. The first author acknowledges Statoil ASA, for access to the Angolan cutting material and financial support in the form of a postdoctoral position at the University of Oslo. Dr. Iain Prince (then Statoil, now Shell) is thanked for his support and for initiating this research project. The two reviewers Dr. Dirk Munsterman and Dr. Martin J. Head are thanked for their constructive and careful reviews.	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J	Amenábar, CR; Candel, MS; Guerstein, GR				Amenabar, Cecilia R.; Soledad Candel, Maria; Raquel Guerstein, G.			Small Antarctic Late Cretaceous chorate dinoflagellate cysts: biological and palaeoenvironmental affinities	PALYNOLOGY			English	Article						dinoflagellate cysts; modern analogues; Argentina; Antarctica; Late Cretaceous-Holocene; palaeoenvironment	JAMES-ROSS-ISLAND; TIERRA-DEL-FUEGO; SEYMOUR-ISLAND; VEGA-ISLAND; CAPE LAMB; QUATERNARY; PENINSULA; TAXONOMY; SEA; MICROPLANKTON	Small spiny marine palynomorphs have been the focus of recent palynological studies since their high proportions in Antarctic Late Cretaceous and Cenozoic assemblages were noted. These palynomorphs were assigned to the dinoflagellate cyst Impletosphaeridium clavus and they were believed to have had an affinity with some modern round brown spiny cysts (RBSCs). Our study aims to analyse there together with potential modern analogues by comparing Late Cretaceous and Cenozoic Antarctic specimens with some RBSCs recorded from the Holocene of southern Argentina. We confirm several features in common between these specimens, although differences in processes and the cyst wall are observed. The species could have been produced by dinoflagellates similar to those that generate some RBSCs. Their abundance in the Late Cretaceous may have occurred in response to short term cooling pulses without development of sea-ice cover. Cenozoic records are considered to be reworked, restricting the stratigraphical range of Impletosphaeridium clavus.	[Amenabar, Cecilia R.] Inst Antartico Argentino, RA-290 Buenos Aires, DF, Argentina; [Amenabar, Cecilia R.] Univ Buenos Aires, Inst Estudios Andinos Don Pablo Groeber, Dept Ciencias Geol, Buenos Aires, DF, Argentina; [Amenabar, Cecilia R.; Soledad Candel, Maria; Raquel Guerstein, G.] Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina; [Soledad Candel, Maria; Raquel Guerstein, G.] Univ Nacl Sur, Inst Geol Sur, Dept Geol, RA-670 Bahia Blanca, Buenos Aires, Argentina	Instituto Antartico Argentino; University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Amenábar, CR (通讯作者)，Inst Antartico Argentino, RA-290 Buenos Aires, DF, Argentina.	amenabar@gl.fcen.uba.ar		Guerstein, G. Raquel/0000-0003-1623-1084; AMENABAR, CECILIA R./0000-0003-1280-3903	Agencia Nacional de Promocion Cientifica y Tecnologica [PICTO-2010-0112, PICT Redes 2002-00067, PICT 89/09]; PICT [89/09]; Consejo Nacional de Investigaciones Cientificas y Tecnicas [PIP 02787/02, PIP 112-201101-00566]; Universidad Nacional del Sur [PGI 24/H125]; Fundacion Antorchas [Proyecto A-13672/1-2]	Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); PICT(ANPCyT); Consejo Nacional de Investigaciones Cientificas y Tecnicas(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Universidad Nacional del Sur; Fundacion Antorchas	The authors are grateful to the Instituto Antartico Argentino and Fuerza Aerea Argentina for logistic support during the Argentine Summer Antarctic Expedition 2008, to A. Concheyro, J.M Lirio and A. Mackern for their invaluable assistance in the Antarctic field and to G. Bujalesky for support with fieldwork in the Beagle Channel. We also thank S. Grill and G. Chaves (Universidad Nacional del Sur, Bahia Blanca, Argentina) and G. Holfeltz (Universidad de Buenos Aires, Argentina) for the preparation of palynological samples, and to the Centro de Microscopia Avanzada (CMA) for the SEM image. We are grateful to S. Gonzalez Estebenet and D. Olivera for their help in figure preparation. We thank J. Cornago for her assistance in English grammar. We also thank J. Riding and V. Bowman and three anonymous reviewers for their helpful comments and suggestions that enhanced the manuscript. Financial support was provided by the Agencia Nacional de Promocion Cientifica y Tecnologica PICTO-2010-0112 and PICT Redes 2002-00067 and PICT 89/09), and PICT 89/09, by Consejo Nacional de Investigaciones Cientificas y Tecnicas (PIP 02787/02 and PIP 112-201101-00566), by Universidad Nacional del Sur (PGI 24/H125) and Fundacion Antorchas (Proyecto A-13672/1-2). This paper is contribution number R-128 of the Instituto de Estudios Andinos 'Don Pablo Groeber' (IDEAN - CONICET).	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J	Riding, JB				Riding, James B.			The literature on Triassic, Jurassic and earliest Cretaceous dinoflagellate cysts: supplement 2	PALYNOLOGY			English	Article						Triassic; literature compilation and synthesis; Jurassic; dinoflagellate cysts; earliest Cretaceous	ALGARVE BASIN; PALYNOLOGY	Since the publication of two literature compilations in 2012 and 2013, 89 further contributions on Triassic, Jurassic and earliest Cretaceous (Berriasian) dinoflagellate cysts have been discovered or were issued recently (i.e. between April 2013 and March 2014). These studies are mostly on the Late Jurassic and Early Cretaceous of Europe. They are all listed herein with digital object identifier (doi) numbers where applicable, and a description of each item as a string of keywords. The 15 most significant publications are briefly summarised.	British Geol Survey, Ctr Environm Sci, 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, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk			NERC [bgs05002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		[Anonymous], 1985, SPOROPOLLENIN DINOFL; Antonescu E., 1980, Anuarul Institutului de Geologie si Geofizica, V56, P97; Antonescu E., 1998, Geo-Eco-Marina, V3, P159; Backhouse J, 2002, 226 MIN EN RES I, V226; Beju D., 1971, ANN I GEOLOGICI PUBL, V54, P276; Birkenmajer Krzysztof, 2012, Studia Geologica Polonica, V135, P7; Borges MEN, 2012, REV PALAEOBOT PALYNO, V170, P40, DOI 10.1016/j.revpalbo.2011.10.008; Borges MEN, 2011, REV PALAEOBOT PALYNO, V163, P190, DOI 10.1016/j.revpalbo.2010.09.006; Chen YY, 2013, PALYNOLOGY, V37, P259, DOI 10.1080/01916122.2013.782367; Dorhofer G, 1980, LIFE SCI MISCELLANEO; Feist-Burkhardt S., 1999, SONDIERBOHRUNG BEN A; Feist- Burkhardt S, 2012, PALYNOSTRATIGRAPHI 1, V12- 57; Fensome R.A., 1993, MICROPALEONTOLOGY PR; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Gedl P, 2013, GEOL Q, V57, P485, DOI 10.7306/gq.1106; HABIB D, 1983, INITIAL REP DEEP SEA, V76, P623; HABIB D, 1975, Micropaleontology (New York), V21, P373, DOI 10.2307/1485290; Habib D., 1987, Initial Reports of the Deep Sea Drilling Project, V93, P751; Heilmann-Clausen C., 1987, DANMARKS GEOLOGISKE, V17; Khowaja-Ateequzzaman Garg R, 2006, CATALOGUE DINOFLAGEL; Kramers JW, 1993, 199326 ALB RES COUNC; Li JG, 2013, CRETACEOUS RES, V46, P123, DOI 10.1016/j.cretres.2013.08.012; MacRae RA, 1996, CAN J BOT, V74, P1687, DOI 10.1139/b96-205; Mafi A, 2014, ARAB J GEOSCI, V7, P3683, DOI 10.1007/s12517-013-0976-4; Moldovanu M, 1984, PALYNOLOGY JURASSIC; Monteil E., 1992, Revue de Paleobiologie, V11, P273; Monteil E., 1992, Revue de Paleobiologie, V11, P299; Norris G., 1978, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V156, P1; OGG G, 1994, MAR MICROPALEONTOL, V23, P241, DOI 10.1016/0377-8398(94)90015-9; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; Riding, 2012, AM ASS STRATIGRAPHIC, V46; Riding J.B., 1992, P7; Riding James B., 2002, Palynology, V26, P5, DOI 10.2113/0260005; Riding JB, 2013, PALYNOLOGY, V37, P345, DOI 10.1080/01916122.2013.797256; Riding JB, 2013, REV PALAEOBOT PALYNO, V196, P51, DOI 10.1016/j.revpalbo.2013.01.010; Sarjeant WA., 1974, BIRBAL SAHNI I PALAE, V3, P9; SARJEANT WILLIAM ANTONY S., 1966, GRANA PALYNOL, V6, P503; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; van de Schootbrugge B, 2013, PALAEONTOLOGY, V56, P685, DOI 10.1111/pala.12034; Williams S.K., 2013, B CAN PETROL GEOL, V61, P211, DOI [10.2113/gscpgbull.61.3.211, DOI 10.2113/GSCPGBULL.61.3.211]	40	6	6	0	7	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	JUL 3	2014	38	2					334	347		10.1080/01916122.2014.920122	http://dx.doi.org/10.1080/01916122.2014.920122			14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AR8HL		Green Accepted			2025-03-11	WOS:000343816200011
J	Kreshchenovskaya, MA; Orlova, TY				Kreshchenovskaya, M. A.; Orlova, T. Yu			The ultrastructure of the dinoflagellate <i>Ostreopsis</i> cf. <i>ovata</i> Fukuyo, 1981 (Dinophyceae) from the Sea of Japan	RUSSIAN JOURNAL OF MARINE BIOLOGY			English	Article						dinoflagellates; Ostreopsis; ultrastructure	THE-GREAT BAY; GAMBIERDISCUS; MORPHOLOGY; WATERS	The results of the ultrastructural study of dinoflagellates from the seas of Russia are presented via the example of Ostreopsis cf. ovata for the first time. The basic cell components (nucleus, chloroplasts, mitochondria, amphiesma, Golgi complex, and accumulative bodies) are described. An expanded and updated description of the chloroplasts and accumulative bodies is given. Crystalline aggregates characteristic of hypnozygotic cysts were found in the genus Ostreopsis for the first time. The data are compared with the results of ultrastructural studies on Ostreopsis cf. ovata that inhabits the Adriatic and the Caribbean seas and the coastal waters of Jeju Island (South Korea). New features of the structure of some organelles in Ostreopsis cf. ovata from Russian waters were revealed.	[Kreshchenovskaya, M. A.; Orlova, T. Yu] Russian Acad Sci, Zhirmunsky Inst Marine Biol, Far Eastern Branch, Vladivostok 690041, Russia	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Kreshchenovskaya, MA (通讯作者)，Russian Acad Sci, Zhirmunsky Inst Marine Biol, Far Eastern Branch, Ul Palchevskogo 17, Vladivostok 690041, Russia.	mkreshenovskaya@gmail.com	Orlova, Tatiana/AAU-8448-2020	Orlova, Tatiana/0000-0002-5246-6967	Far Eastern Branch of the Russian Academy of Sciences [12-I-P30-09, 12-III-A-06-093, 12-I-0-02-020, 12-I-P4-02, 12I-P28-03]	Far Eastern Branch of the Russian Academy of Sciences(Russian Academy of Sciences)	This study was performed with financial support from the Far Eastern Branch of the Russian Academy of Sciences (grant nos. 12-I-P30-09, 12-III-A-06-093, 12-I-0-02-020, 12-I-P4-02, and 12I-P28-03). We are sincerely grateful to I.Yu. Dolmatov, M.S. Selina, N.G. Litvinova, and D. V. Fomin (A.V. Zhirmunsky Institute of Marine Biology, Far Eastern Branch, Russian Academy of Sciences) for valuable comments and technical help.	Accoroni S, 2012, CRYPTOGAMIE ALGOL, V33, P191, DOI 10.7872/crya.v33.iss2.2011.191; Baron R, 2007, HARMFUL ALGAE NEWS, P1, DOI 3; Battocchi C, 2010, MAR POLLUT BULL, V60, P1074, DOI 10.1016/j.marpolbul.2010.01.017; BESADA EG, 1982, B MAR SCI, V32, P723; Bibby B.T., 1972, British phycol J, V7, P85; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Durando P., 2007, Eurosurveillance, V12, pE070607, DOI 10.2807/esw.12.23.03212-en; Faimali M, 2012, MAR ENVIRON RES, V76, P97, DOI 10.1016/j.marenvres.2011.09.010; Honsell G, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0057291; Kang NS, 2013, HARMFUL ALGAE, V27, P98, DOI 10.1016/j.hal.2013.05.006; Mangialajo L, 2011, TOXICON, V57, P408, DOI 10.1016/j.toxicon.2010.11.019; Okolodkov Yu.B., 1993, PROTISTY RUKOVODSTVO, V3, P7; Parsons ML, 2012, HARMFUL ALGAE, V14, P107, DOI 10.1016/j.hal.2011.10.017; Penna A, 2012, CRYPTOGAMIE ALGOL, V33, P153, DOI 10.7872/crya.v33.iss2.2011.153; REYNOLDS ES, 1963, J CELL BIOL, V17, P208, DOI 10.1083/jcb.17.1.208; Rhodes L, 2011, TOXICON, V57, P400, DOI 10.1016/j.toxicon.2010.05.010; Sato S., 2011, PLOS ONE, V6, P1; Selina MS, 2011, RUSS J MAR BIOL+, V37, P23, DOI 10.1134/S1063074011010135; Selina MS, 2014, HARMFUL ALGAE, V32, P1, DOI 10.1016/j.hal.2013.11.005; Selina MS, 2010, BOT MAR, V53, P243, DOI 10.1515/BOT.2010.033; Stonik V.A., 2010, USP KHIM, V79, P442; Suzuki T, 2012, HARMFUL ALGAE, V20, P81, DOI 10.1016/j.hal.2012.08.002; WEDEMAYER GJ, 1984, J PROTOZOOL, V31, P444, DOI 10.1111/j.1550-7408.1984.tb02992.x	23	1	1	1	23	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	2014	40	4					273	278		10.1134/S1063074014040051	http://dx.doi.org/10.1134/S1063074014040051			6	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	AO6WK					2025-03-11	WOS:000341493000005
J	Gusev, EA; Anikina, NY; Derevyanko, LG; Klyuvitkina, TS; Polyak, LV; Polyakova, EI; Rekant, PV; Stepanova, AY				Gusev, E. A.; Anikina, N. Yu.; Derevyanko, L. G.; Klyuvitkina, T. S.; Polyak, L. V.; Polyakova, E. I.; Rekant, P. V.; Stepanova, A. Yu.			Environmental evolution of the southern Chukchi Sea in the Holocene	OCEANOLOGY			English	Article							LAPTEV SEA; HYDROGRAPHIC CONDITIONS; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; ARCTIC-OCEAN; LEVEL RISE; MARINE; SHELF; KARA; STRATIGRAPHY	The molluscan shells from three drill and two piston cores obtained in the southern Russian sector of the Chukchi Sea are dated by the AMS C-14 measurement method back to 0.8-3.5 and 9.2-10.5 ka. The period of 9-10 ka was marked by increased sedimentation rates related to the transgression onset. The fossils in the lower Holocene section exhibit the successive upward replacement of brackish-water organisms by their marine counterparts. After the opening of the Bering Strait in the middle Holocene, the sedimentation was under influence of the increased bioproductivity of the waters. The climatic optimum in the Chukotka region corresponds to the early Holocene, while the late Holocene was characterized by the wider development of the ice cover on the shelf.	[Gusev, E. A.; Rekant, P. V.] World Ocean VNIIOkeangeologiya, All Russian Res Inst Geol & Mineral Resources, St Petersburg, Russia; [Anikina, N. Yu.; Derevyanko, L. G.] Cent Geol Prospecting Lab, Syktyvkar, Russia; [Klyuvitkina, T. S.; Polyakova, E. I.] Moscow MV Lomonosov State Univ, Dept Geog, Moscow, Russia; [Polyak, L. V.] Ohio Univ, Athens, OH 45701 USA; [Stepanova, A. Yu.] Russian Acad Sci, Inst Paleontol, Moscow V71, Russia	A.P. Karpinsky Russian Geological Research Institute (VSEGEI); Lomonosov Moscow State University; University System of Ohio; Ohio University; Russian Academy of Sciences	Gusev, EA (通讯作者)，World Ocean VNIIOkeangeologiya, All Russian Res Inst Geol & Mineral Resources, St Petersburg, Russia.	gus-evgeny@yandex.ru	Gusev, Evgeny/C-5156-2012; Klyuvitkina, Tatyana/L-8843-2015; Polyakova, Yelena/L-8889-2015	Gusev, Evgeny/0000-0001-6045-0730				[Anonymous], PALEOCEANOGRAPHY; Astakhov AS, 2013, RUSS GEOL GEOPHYS+, V54, P1056, DOI 10.1016/j.rgg.2013.07.019; Astakhov AS, 2010, RUSS J PAC GEOL, V4, P532, DOI 10.1134/S1819714010060096; Bauch HA, 2001, GLOBAL PLANET CHANGE, V31, P125, DOI 10.1016/S0921-8181(01)00116-3; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Creager J. S., 1965, MAR GEOL, P279; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Grantz A., 1978, 86206 US GEOL SURV; Gusev EA, 2009, GLOBAL PLANET CHANGE, V68, P115, DOI 10.1016/j.gloplacha.2009.03.025; Hill JC, 2007, QUATERNARY RES, V68, P271, DOI 10.1016/j.yqres.2007.04.004; Hill JC, 2010, QUATERNARY RES, V74, P57, DOI 10.1016/j.yqres.2010.03.008; Kalinichenko O. I., 2001, ZB NAUK PR DON NATS, P144; Kaufman DS, 2004, QUATERNARY SCI REV, V23, P529, DOI 10.1016/j.quascirev.2003.09.007; Keigwin LD, 2006, GEOLOGY, V34, P861, DOI 10.1130/G22712.1; Klyuvitkina TS, 2006, OCEANOLOGY+, V46, P859, DOI 10.1134/S0001437006060117; Lein AY, 2007, LITHOL MINER RESOUR+, V42, P221, DOI 10.1134/S0024490207030029; Lev O. M., 1983, GEN PROBLEMS LATE CE, P104; Levitan M. A., 2007, HIST SEDIMENTATION A; Lisitzin AP, 2010, RUSS GEOL GEOPHYS+, V51, P12, DOI 10.1016/j.rgg.2009.12.002; LISITZIN AP, 1994, OKEANOLOGIYA+, V34, P735; Lozhkin AV, 2001, QUATERNARY SCI REV, V20, P217, DOI 10.1016/S0277-3791(00)00121-9; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; Matthiessen Jens, 2005, Palaeontologische Zeitschrift, V79, P3; Matul AG, 2007, OCEANOLOGY+, V47, P80, DOI 10.1134/S0001437007010110; Miller GH, 2010, QUATERNARY SCI REV, V29, P1679, DOI 10.1016/j.quascirev.2010.03.001; Morozova L. N., 1985, GEOLOGY GEOMORPHOLOG, P85; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Pavlidis Yu. A., 1981, CONTINENTAL ISLANDS, P33; Pavlidis Yu.A., 1982, PROBLEMY GEOMORFOLOG, P47; Phillips R. L., 1987, GEOLOGIC STUDIES ALA, P157; Polyakova Ye. I., 1989, GEOLOGY CONTINENTAL, P136; Polyakova Ye. I., 1997, OKEANOLOGIYA, V37, P269; Puminov A. 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L., 2007, GEOLOGY PALEOGEOGRAP; Walker MJC, 2012, J QUATERNARY SCI, V27, P649, DOI 10.1002/jqs.2565; Zykov E., 2011, IZVESTIA HERZEN U J, V141, P131	47	18	20	0	14	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0001-4370	1531-8508		OCEANOLOGY+	Oceanology	JUL	2014	54	4					465	477		10.1134/S0001437014030011	http://dx.doi.org/10.1134/S0001437014030011			13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AN8XL					2025-03-11	WOS:000340889100008
J	White, AE; Watkins-Brandt, KS; McKibben, SM; Wood, AM; Hunter, M; Forster, Z; Du, XN; Peterson, WT				White, Angelicque E.; Watkins-Brandt, Katie S.; McKibben, S. Morgaine; Wood, A. Michelle; Hunter, Matthew; Forster, Zach; Du, Xiuning; Peterson, William T.			Large-scale bloom of <i>Akashiwo sanguinea</i> in the Northern California current system in 2009	HARMFUL ALGAE			English	Article						Akashiwo sanguinea; Cysts; Dinoglagellates; HABS; Harmful algal blooms; Seabird mortality; Surf zone; Upwelling	HARMFUL ALGAL BLOOMS; RED TIDE; PHYTOPLANKTON; OREGON; GROWTH	Significant seabird mortality on the Oregon (OR) and Washington (WA) coast in 2009 has been attributed to a massive bloom of the dinoflagellate Akashiwo sanguinea (K. Hirasaka) G. Hansen & O. Moestrup. Initial, albeit limited, observations suggested this bloom began in WA and reached OR waters through southward transport. Here, we explore a combination of remote sensing products and an exceptional latitudinal dataset of plankton counts collected in the surfzone and offshore in OR and WA coastal waters. Records of satellite ocean color for this period support the new finding that blooms were concurrent in OR and WA waters, with no evidence for latitudinal propagation as had been previously suggested. Plankton analyses further indicate that there was a rapid and synchronized increase of A. sanguinea between late August and mid-September of 2009 along wide swaths of the OR and WA coasts. Bloom onset occurred during a prolonged quiescent and warm period in late August-early September, near the end of the March-October upwelling phase. An upwelling event in October likely contributed to foam production through vertical mixing of A. sanguinea rich waters. Bloom intensity peaked earlier and at higher levels in WA waters as compared to OR with cell concentrations exceeding 1.5 x 10(6) cells L-1 (WA) and similar to 350,000 cells L-1 (OR). In OR samples, A. sanguinea cells comprised upwards of 90% of dinoflagellate cell counts and similar to 30% of total phytoplankton cells. At some locations, A. sanguinea persisted well into November-December of 2009, during which time satellite sea surface temperature records indicated anomalously warm surface waters (up to similar to 5 degrees C greater than climatological means). Taken together, the data reveal a HAB event of a magnitude unprecedented in over a decade of observations. We hypothesize that these blooms originated from either a cryptic cyst bed and/or a pelagic seed bank of viable vegetative cells. (C) 2014 Elsevier B.V. All rights reserved.	[White, Angelicque E.; Watkins-Brandt, Katie S.; McKibben, S. Morgaine] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA; [Wood, A. Michelle] Univ Oregon, Inst Ecol & Evolut, Eugene, OR 97403 USA; [Hunter, Matthew] Oregon Dept Fish & Wildlife, Astoria, OR USA; [Forster, Zach] Washington Dept Fish & Wildlife, Willapa Bay Field Stn, Ocean Park, WA USA; [Du, Xiuning; Peterson, William T.] Oregon State Univ, Hatfield Marine Sci Ctr, Cooperat Inst Marine Resources Studies, Newport, OR 97365 USA; [Du, Xiuning; Peterson, William T.] Oregon State Univ, Hatfield Marine Sci Ctr, NW Fisheries Sci Ctr, Natl Ocean & Atmospher Adm, Newport, OR 97365 USA	Oregon State University; University of Oregon; Washington Department of Fish & Wildlife (WDFW); Oregon State University; Oregon State University; National Oceanic Atmospheric Admin (NOAA) - USA	White, AE (通讯作者)，Oregon State Univ, Coll Earth Ocean & Atmospher Sci, 104 CEOAS Admin, Corvallis, OR 97331 USA.	awhite@coas.oregonstate.edu		Watkins-Brandt, Katie/0000-0002-3868-8491; White, angelicque/0000-0002-0938-7948	NOAA [NA07NOS4780195, NA08NES4400013]	NOAA(National Oceanic Atmospheric Admin (NOAA) - USA)	This study was supported by NOAA grant NA07NOS4780195 (to AW, MW and WP) from the Monitoring and Event Response for Harmful Algal Blooms (MERHAB) program and NA08NES4400013 to the Cooperative Institute for Oceanographic Satellite Studies (CIOSS). We are grateful to Sharnelle Fee, Director of the Wildlife Center of the North Coast and Roy W. Lowe, Project Leader, U.S. Fish and Wildlife Service for sharing data and experiences with seabird rehabilitation during this event along with all of the volunteers who tirelessly collected birds for rehabilitation. We also thank Nick Tufillaro for access to MERIS data and the Olympic Region HAB Partnership for their collegiality and data sharing. 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J	Rao, MR; Verma, P				Rao, M. R.; Verma, Poonam			Palynological Investigation of Neogene (Early Miocene) Sediments of Mangalore Basin, India: Palaeoenvironmental and Palaeoclimatic Implications	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						Palynology; Palaeoecology; Neogene (Early Miocene); Mangalore; Karnataka	POLLEN; EOCENE	A rich palynological assemblage consisting of algal remains (5 genera and 7 species, including dinoflagellate cysts), fungal spores (2 genera and 3 species), pteridophytic spores (5 genera and 8 species), gymnospermous pollen grains (3 genera and 3 species) and angiospermous pollen grains (17 genera and 22 species) has been recorded for the first time from the Miocene sediments exposed along Kullur-Kavur road, near Mangalore along the west coast of Karnataka. Among the important genera are: Achomosphaera, Leptodinium, Staphlosporonites, Hammenisporis, Polypodiaceaesporites, Quilonipollenites, Myricipites, Graminidites, Malvacearumpollis, Palaeomalvaceaepollis and Chenopodipollis. Qualitative and quantitative analyses reveal that the angiosperm pollen grains are dominant over pteridophytic spores and an overall, a warm and humid tropical-sub-tropical coastal climate with heavy precipitation is suggested for the site of deposition. The sediments were deposited in fluctuating conditions ranging from lacustrine to marine environments with fresh water swamps and ponds nearby. The occurrence of Hammenisporis, Polypodiaceaesporites, Quilonipollenites, Myricipites, Graminidites, Malvacearumpollis, Palaeomalvaceaepollis and Chenopodipollis in the present assemblage suggests an early Miocene age. A comparison of the present palynofloral assemblage with those known from the Indian Tertiary sediments shows its close resemblances with the Miocene palynoflora recovered from Quilon and Warkalli beds of Kerala basin.	[Rao, M. R.; Verma, Poonam] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Rao, MR (通讯作者)，Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India.	rao.mr2008@gmail.com						[Anonymous], 1982, Geophytology; [Anonymous], 2004, Journal of Palaeosciences; Baksi S. K., 1971, P SEM PAL IND STRAT, P188; Baksi S.K., 1962, B GEOL MIN METALL SO, V26, P1; BANERJEE D, 1968, REV PALAEOBOT PALYNO, V6, P171, DOI 10.1016/0034-6667(68)90044-4; BANERJEE D., 1964, B GEOL MIN METALL SO, V29, P1; Bharadwaj D C., 1962, The paleobotanist, V9, P68; Bharadwaj D. 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J	Bijl, PK; Sluijs, A; Brinkhuis, H				Bijl, Peter K.; Sluijs, Appy; Brinkhuis, Henk			A magneto- and chemostratigraphically calibrated dinoflagellate cyst zonation of the early Paleogene South Pacific Ocean (vol 124, pg 1, 2013)	EARTH-SCIENCE REVIEWS			English	Correction						Erratum; Dinoflagellate cysts; Stratigraphy; Paleogene; South Pacific Ocean; Magnetostratigraphy	EOCENE; TRANSITION		[Bijl, Peter K.; Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands	Utrecht University	Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Brinkhuis, Henk/IUO-8165-2023; Sluijs, Appy/B-3726-2009	Sluijs, Appy/0000-0003-2382-0215; Brinkhuis, Henk/0000-0003-0253-6610; Bijl, Peter/0000-0002-1710-4012				Bijl PK, 2013, EARTH-SCI REV, V124, P1, DOI 10.1016/j.earscirev.2013.04.010; Bijl PK, 2011, PALEOCEANOGRAPHY, V26, DOI 10.1029/2009PA001905; Bijl PK, 2010, SCIENCE, V330, P819, DOI 10.1126/science.1193654; Bijl PK, 2009, NATURE, V461, P776, DOI 10.1038/nature08399; Crouch EM, 2005, MAR MICROPALEONTOL, V56, P138, DOI 10.1016/j.marmicro.2005.05.002; Kim JH, 2010, GEOCHIM COSMOCHIM AC, V74, P4639, DOI 10.1016/j.gca.2010.05.027; Schellenberg SA, 2004, GEOPH MONOG SERIES, V151, P93; Sexton PF, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001253; Sluijs A, 2011, CLIM PAST, V7, P47, DOI 10.5194/cp-7-47-2011; Vandenberghe N, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P855, DOI 10.1016/B978-0-444-59425-9.00028-7; Westerhold T, 2011, PALEOCEANOGRAPHY, V26, DOI 10.1029/2010PA002092; Wilson G.J., 1988, NZ GEOL SURV B, V57; Zachos JC, 2008, NATURE, V451, P279, DOI 10.1038/nature06588	13	5	5	0	10	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0012-8252	1872-6828		EARTH-SCI REV	Earth-Sci. Rev.	JUL	2014	134						160	163		10.1016/j.earscirev.2014.03.010	http://dx.doi.org/10.1016/j.earscirev.2014.03.010			4	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AJ7CW		Green Published			2025-03-11	WOS:000337855800007
J	Bankole, SI; Schrank, E; Osterloff, PL				Bankole, Samson I.; Schrank, Eckart; Osterloff, Peter L.			Palynostratigraphy, palaeoclimates and palaeodepositional environments of the Miocene aged Agbada Formation in the Niger Delta, Nigeria	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynology; Spores; Pollen; Dinoflagellate cysts; Agbada Formation; Miocene	PALYNOLOGY; BASIN; SUCCESSION; DYNAMICS; EOCENE; FIELD; WELL	A diverse assemblage of palynomorphs dominated by terrestrially derived pollen and spores is reported from three wells penetrating the Miocene Agbada Formation. The pteridophyte and bryophyte spores which form the background assemblages in the three wells are good indicators of humid tropical climates which might have prevailed in the Niger Delta during the Miocene. The abundance and variations of climate-sensitive taxa including mangrove affiliated pollen and spore types Acrostichumsporites, Psilatricolporites crassus, Zonocostites ramonae and Graminidites annulatus representing the savannah vegetation cover indicate a complex interplay between periods of wetter and drier climates. Marine-derived dinoflagellate cysts and foraminiferal test linings are significantly present in the three wells. Taxa indicating freshwater contributions including Botiyococcus spp., Chomotriletes minor, Ovoidites parvus and Pediastrum spp. are also represented numerically across the three wells. The presence of age diagnostic palynomorphs such as Crassoretitriletes vanraadshooveni, Retibrevitricolporites obodoensis, Tuberculodinium vancampoae, Zonocostites ramonae and Tuberculodinium vancampoae recovered in the three sections studied suggest a Miocene age for the investigated Agbada Formation. The proposed age is supported by the ranges of key palynomorphs in contemporaneous basins in Africa, northern South America and other parts of the World. (C) 2014 Elsevier Ltd. All rights reserved.	[Bankole, Samson I.] Univ Lagos, Dept Geosci, Lagos, Nigeria; [Schrank, Eckart] Tech Univ Berlin, Inst Angew Geowissensch, D-52425 Berlin, Germany; [Osterloff, Peter L.] Shell Petr Dev Co, Warri, Delta State, Nigeria	University of Lagos; Technical University of Berlin; Royal Dutch Shell	Bankole, SI (通讯作者)，Univ Lagos, Dept Geosci, Lagos, Nigeria.	sbankole@unilag.edu.ng		Bankole, Samson/0000-0003-4608-9605				Adeniran B. 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J	El Diasty, WS; El Beialy, SY; Ghonaim, AAA; Mostafa, AR; El Atfy, H				El Diasty, W. Sh.; El Beialy, S. Y.; Ghonaim, A. A. Abo; Mostafa, A. R.; El Atfy, H.			Palynology, palynofacies and petroleum potential of the Upper Cretaceous-Eocene Matulla, Brown Limestone and Thebes formations, Belayim oilfields, central Gulf of Suez, Egypt	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynology; Palynofacies; Rock-Eval pyrolysis; Matulla and Brown Limestone formations; Thebes Formation; Gulf of Suez; Egypt	DINOFLAGELLATE CYSTS; NUKHUL FORMATION; OIL-FIELD; MIOCENE; BASIN; RIFT; PALEOENVIRONMENT; SEQUENCE; GEOLOGY; FACIES	Palynological, palynofacies and organic geochemical results of 46 samples retrieved from the Upper Cretaceous - Eocene Matulla, Brown Limestone and Thebes formations, Belayim oilfields, central Gulf of Suez, Egypt are presented. The two latter formations are not dated palynologically as their lithology is not promising for palynological yield. However the Matulla Formation is dated as Turonian-Santonian age, based on the combined evidence of pollen and dinocysts. Palynofacies analysis carried out under both transmitted and fluorescent microscopy indicated that both the Thebes and Brown Limestone formations are deposited under a distal suboxic-anoxic environment. On the other hand, the Turonian-Santonian Matulla Formation supported the existence of a marginal marine deposition under dysoxic-anoxic basin to proximal suboxic-anoxic shelf environments. Rock-Eval pyrolysis and TOC results indicated that most of the studied formations are thermally immature to marginally mature and have a good petroleum potential. They are organically-rich in both oil- and gas-prone kerogen Type-II and deposited under marine reducing conditions favorable for hydrocarbon generation and expulsion. (C) 2014 Elsevier Ltd. All rights reserved.	[El Diasty, W. Sh.; El Beialy, S. Y.; Ghonaim, A. A. Abo; El Atfy, H.] Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt; [Mostafa, A. R.] Univ Alexandria, Fac Sci, Dept Environm Sci, Alexandria, Egypt; [El Atfy, H.] Senckenberg Res Inst, D-60325 Frankfurt, Germany; [El Atfy, H.] Nat Hist Museum, D-60325 Frankfurt, Germany	Egyptian Knowledge Bank (EKB); Mansoura University; Egyptian Knowledge Bank (EKB); Alexandria University; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN)	El Diasty, WS (通讯作者)，Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt.	waleedshukry2006@yahoo.co.uk	Beialy, Salah/AAD-7329-2020; Diasty, Waleed/AAG-7015-2019; Atfy, Haytham/AAT-2276-2021	Shukry El Diasty, Waleed/0000-0002-3144-1189; El Atfy, Haytham/0000-0003-1618-7220				Abdel Mohsen S., 1986, NEUES JB GEOL PAL, V6, P321; Al-Ameri TK, 2011, MAR PETROL GEOL, V28, P880, DOI 10.1016/j.marpetgeo.2010.06.003; Al-Husseini MI, 2012, GEOARABIA, V17, P17; Alsharhan AS, 2003, AAPG BULL, V87, P143; ALSHARHAN AS, 1994, B CAN PETROL GEOL, V42, P312; [Anonymous], 1978, REV MICROPALEONTOLOG; [Anonymous], 1986, B FS; Awad M.Z., 1994, Berliner Geowissenschaftliche Abhandlungen, Reihe A, V161, P163; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Batten D J., 1980, Proceedings of the 4th International Palynological Conference, P589; Batten D.J., 1982, J. 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Afr. Earth Sci.	JUL	2014	95						155	167		10.1016/j.jafrearsci.2014.03.013	http://dx.doi.org/10.1016/j.jafrearsci.2014.03.013			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AJ5ZN					2025-03-11	WOS:000337769600012
J	Leighfield, TA; Muha, N; Ramsdell, JS				Leighfield, Tod A.; Muha, Noah; Ramsdell, John S.			Tissue Distribution of Amino Acid- and Lipid-Brevetoxins after Intravenous Administration to C57BL/6 Mice	CHEMICAL RESEARCH IN TOXICOLOGY			English	Article							FLORIDA RED TIDE; INTRATRACHEAL INSTILLATION; PTYCHODISCUS-BREVIS; GREENSHELL MUSSELS; NEW-ZEALAND; RATS; METABOLITES; ELIMINATION; SHELLFISH; SEMISYNTHESIS	Brevetoxins produced during algal blooms of the dinoflagellate Karenia are metabolized by shellfish into reduction, oxidation, and conjugation products. Brevetoxin metabolites comprising amino acid- and lipid conjugates account for a large proportion of the toxicity associated with the consumption of toxic shellfish. However, the disposition of these brevetoxin metabolites has not been established. Using intravenous exposure to C57BL/6 mice, we investigated the disposition in the body of three radiolabeled brevetoxin metabolites. Amino acid brevetoxin conjugates represented by S-desoxy-BTX-B2 (cysteine-BTX-B) and lipid brevetoxin conjugates represented by N-palmitoyl-S-desoxy-BTX-B2 were compared to dihydro-BTX-B. Tissue concentration profiles were unique to each of the brevetoxin metabolites tested, with dihydro-BTX-B being widely distributed to all tissues, S-desoxy-BTX-B2 concentrated in kidney, and N-palmitoyl-S-desoxy-BTX-B2 having the highest concentrations in spleen, liver, and lung. Elimination patterns were also unique: dihydro-BTX-B had a greater fecal versus urinary elimination, whereas urine was a more important elimination route for S-desoxy-BTX-B2, and N-palmitoyl-S-desoxy-BTX-B2 persisted in tissues and was eliminated equally in both urine and feces. The structures particular to each brevetoxin metabolite resulting from the reduction, amino acid conjugation, or fatty acid addition of BTX-B were likely responsible for these tissue-specific distributions and unique elimination patterns. These observed differences provide further insight into the contribution each brevetoxin metabolite class has to the observed potencies.	[Leighfield, Tod A.; Muha, Noah; Ramsdell, John S.] NOAA Natl Ocean Serv, Ctr Coastal Environm Hlth & Biomol Res, Marine Biotoxins Program, Charleston, SC 29412 USA	National Oceanic Atmospheric Admin (NOAA) - USA	Ramsdell, JS (通讯作者)，NOAA Natl Ocean Serv, Ctr Coastal Environm Hlth & Biomol Res, Marine Biotoxins Program, 219 Ft Johnson Rd, Charleston, SC 29412 USA.	john.ramsdell@noaa.gov		Leighfield, Tod/0000-0002-6780-8800	National Oceanic and Atmospheric Administration	National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA)	This work was supported by the National Oceanic and Atmospheric Administration.	Benson JM, 2005, ENVIRON HEALTH PERSP, V113, P626, DOI 10.1289/ehp.7497; Benson JM, 1999, J TOXICOL ENV HEAL A, V57, P345, DOI 10.1080/009841099157656; Bottein MYD, 2010, TOXICON, V55, P497, DOI 10.1016/j.toxicon.2009.09.022; Brown RP, 1997, TOXICOL IND HEALTH, V13, P407, DOI 10.1177/074823379701300401; CATTET M, 1993, TOXICON, V31, P1483, DOI 10.1016/0041-0101(93)90214-4; Dechraoui MYB, 2007, TOXICON, V50, P825, DOI 10.1016/j.toxicon.2007.06.013; Fleming LE, 2011, HARMFUL ALGAE, V10, P224, DOI 10.1016/j.hal.2010.08.006; Landsberg JH, 2009, HARMFUL ALGAE, V8, P598, DOI 10.1016/j.hal.2008.11.010; Leighfield TA, 2013, CHEM RES TOXICOL, V26, P868, DOI 10.1021/tx4000057; LIN YY, 1981, J AM CHEM SOC, V103, P6773, DOI 10.1021/ja00412a053; Maucher JM, 2007, ENVIRON SCI TECHNOL, V41, P563, DOI 10.1021/es0612605; Morohashi A, 1999, NAT TOXINS, V7, P45, DOI 10.1002/(SICI)1522-7189(199903/04)7:2<45::AID-NT34>3.0.CO;2-H; Murata K, 1998, TETRAHEDRON, V54, P735, DOI 10.1016/S0040-4020(97)10336-2; Plakas SM, 2010, TOXICON, V56, P137, DOI 10.1016/j.toxicon.2009.11.007; POLI MA, 1990, TOXICON, V28, P903, DOI 10.1016/0041-0101(90)90020-8; Poli MA, 2000, TOXICON, V38, P981, DOI 10.1016/S0041-0101(99)00191-9; Radwan FFY, 2006, TOXICOL SCI, V89, P57, DOI 10.1093/toxsci/kfj013; Radwan FFY, 2005, TOXICOL SCI, V85, P839, DOI 10.1093/toxsci/kfi138; 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; TEMPLETON CB, 1989, TOXICON, V27, P1043, DOI 10.1016/0041-0101(89)90155-4; Tibbetts BM, 2006, J TOXICOL ENV HEAL A, V69, P1325, DOI 10.1080/15287390500360091; Wang ZH, 2004, TOXICON, V43, P455, DOI 10.1016/j.toxicon.2004.02.017	23	5	6	1	9	AMER CHEMICAL SOC	WASHINGTON	1155 16TH ST, NW, WASHINGTON, DC 20036 USA	0893-228X	1520-5010		CHEM RES TOXICOL	Chem. Res. Toxicol.	JUL	2014	27	7					1166	1175		10.1021/tx500053f	http://dx.doi.org/10.1021/tx500053f			10	Chemistry, Medicinal; Chemistry, Multidisciplinary; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy; Chemistry; Toxicology	AL9LN	24949875				2025-03-11	WOS:000339462700009
J	Grothe, A; Sangiorgi, F; Mulders, YR; Vasiliev, I; Reichart, GJ; Brinkhuis, H; Stoica, M; Krijgsman, W				Grothe, Arjen; Sangiorgi, Francesca; Mulders, Yannick R.; Vasiliev, Iuliana; Reichart, Gert-Jan; Brinkhuis, Henk; Stoica, Marius; Krijgsman, Wout			Black Sea desiccation during the Messinian Salinity Crisis: Fact or fiction?	GEOLOGY			English	Article							EASTERN PARATETHYS; LATE MIOCENE; TAMAN PENINSULA; NEOGENE; BASINS; POLLEN; EVENT	The late Miocene Messinian Salinity Crisis (MSC) was an extraordinary geologic event in the Mediterranean Basin marked by massive salt accumulation and presumably basin desiccation as a consequence of the reduced water exchange with the Atlantic Ocean. The discovery of a desiccation deposit in the Black Sea, the so-called Pebbly Breccia unit, was used to claim that the Black Sea also became desiccated during the MSC. Erosional features interpreted from seismic profiles of the Black Sea margin, correlated by some to the Pebbly Breccia unit, were used to support this hypothesis. However, the age of the Pebbly Breccia is poorly constrained, and its origin and relevance to the MSC subject to controversy. Here we present new biostratigraphic (dinoflagellate cyst) data from two key sedimentary successions located in a deep and a marginal setting of the Black Sea Basin. These records demonstrate that the Pebbly Breccia predates the Mediterranean water-level drop during the MSC. We argue that the presumed erosional features in the Black Sea Basin are not related to the MSC and likely represent an older Miocene event.	[Grothe, Arjen; Sangiorgi, Francesca; Mulders, Yannick R.; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Vasiliev, Iuliana; Krijgsman, Wout] Univ Utrecht, Paleomagnet Lab Ft Hoofddijk, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Vasiliev, Iuliana; Reichart, Gert-Jan] Univ Utrecht, Fac Geosci, Dept Geochem, NL-3584 CD Utrecht, Netherlands; [Reichart, Gert-Jan; Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, NL-1790 AB Den Burg, Texel, Netherlands; [Stoica, Marius] Univ Bucharest, Fac Geol & Geophys, Dept Geol, Bucharest 010041, Romania	Utrecht University; Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bucharest	Grothe, A (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Brinkhuis, Henk/IUO-8165-2023; Stoica, Marius/N-4941-2018; Reichart, Gert-Jan/N-6308-2018	Sangiorgi, Francesca/0000-0003-4233-6154; Brinkhuis, Henk/0000-0003-0253-6610; Krijgsman, Wout/0000-0002-1472-1074; Stoica, Marius/0000-0003-0126-4270; Vasiliev, Iuliana/0000-0002-1024-6966; Reichart, Gert-Jan/0000-0002-7256-2243	U.S. National Science Foundation; Netherlands Geosciences Foundation (ALW); Netherlands Organisation for Scientific Research (NWO)	U.S. National Science Foundation(National Science Foundation (NSF)); Netherlands Geosciences Foundation (ALW); Netherlands Organisation for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO))	We thank T. Donders for assistance with the pollen determination, J. van Tongeren and N. Welters for their technical support in the laboratory, and the paleomagnetic team of St. Petersburg (A. Iosifidi, V. Popov, and students) for their support during the sampling of Zheleznyi Rog. We are grateful to I. Magyar, B.C. Schreiber, the anonymous reviewers, and the editor (E. Thomas) for their constructive review and comments. This study used samples provided by the Deep Sea Drilling Project, which was sponsored by the U.S. National Science Foundation and participating countries under management of Joint Oceanographic Institutions. This work was financially supported by the Netherlands Geosciences Foundation (ALW) with support from the Netherlands Organisation for Scientific Research (NWO).	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J	Shin, HH; Li, Z; Kim, YO; Jung, SW; Han, MS; Lim, W; Yoon, YH				Shin, Hyeon Ho; Li, Zhun; Kim, Young-Ok; Jung, Seung Won; Han, Myung-Soo; Lim, WolAe; Yoon, Yang Ho			Morphological features and viability of <i>Scrippsiella trochoidea</i> cysts isolated from fecal pellets of the polychaete <i>Capitella</i> sp.	HARMFUL ALGAE			English	Article						Capitella sp.; Fecal pellet; Grazing; Scrippsiella trochoidea cyst	OYSTER CRASSOSTREA-VIRGINICA; DINOFLAGELLATE CYSTS; RESTING CYSTS; DEPOSIT FEEDERS; GAMAK BAY; DINOPHYCEAE; GERMINATION; INGESTION; LACHRYMOSA; HYPOXIA	To investigate the impact of grazing by the polychaete Capitella sp. on the two cyst morphotypes of Scrippsiella trochoidea, the typical morphotype with short calcareous spines (spiny-type cyst) and artificially induced the transparent type without calcareous spines (naked-type cyst), we examined the morphological features and germination capability of the two cyst morphotypes isolated from fecal pellets of the polychaete Capitella sp. produced in a restricted habitat. The morphological destruction was observed in both spiny- and naked type cysts after passage through the gut of Capitella sp., and this seemed to occur rapidly for naked-type cysts. In addition, the germination of both spiny- and naked-type cysts isolated from fecal pellets on day 2 of harvesting was significantly reduced and subsequently completely abolished, in contrast to previous findings from ingestion studies. Our results indicate that continual grazing by Capitella sp. within a restricted habitat can compromise the survival of S. trochoidea cysts. (C) 2014 Elsevier B.V. All rights reserved.	[Shin, Hyeon Ho; Li, Zhun; Jung, Seung Won] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea; [Kim, Young-Ok] Korea Inst Ocean Sci & Technol, South Sea Inst, Geoje 656830, South Korea; [Li, Zhun; Han, Myung-Soo] Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; [Lim, WolAe] NFRDI, Fishery & Ocean Informat Div, Seoul, South Korea; [Yoon, Yang Ho] Chonnam Natl Univ, Fac Marine Technol, Yeosu 550749, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); Hanyang University; Chonnam National University	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea.	shh961121@kiost.ac	KIM, YOUNG JIN/E-9374-2011; Jung, Seung/L-9467-2016; LI, ZHUN/GLT-3478-2022	Yoon, Yang Ho/0000-0001-8529-9512; Shin, Hyeon Ho/0000-0002-9711-6717; LI, ZHUN/0000-0001-8961-9966	Korea Institute of Ocean Science and Technology [PE99191]; Basic Science Research Program through the National Research Foundation of Korea (NRF) - Ministry of Education, Science and Technology [2013005394]	Korea Institute of Ocean Science and Technology; Basic Science Research Program through the National Research Foundation of Korea (NRF) - Ministry of Education, Science and Technology	We thank Dr. Jung Ho Lee for valuable comments on culturing of Capitella sp. This work was supported by a grant from the Korea Institute of Ocean Science and Technology (PE99191), and Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Education, Science and Technology (No. 2013005394).	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J	Guerstein, GR; Estebenet, MSG; Alperín, MI; Casadío, SA; Archangelsky, S				Raquel Guerstein, G.; Gonzalez Estebenet, M. Sol; Alperin, Marta I.; Casadio, Silvio A.; Archangelsky, Sergio			Correlation and paleoenvironments of middle Paleogene marine beds based on dinoflagellate cysts in southwestern Patagonia, Argentina	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Dinoflagellate cyst; Biostratigraphy; Eocene; Austral basin; Argentina	RIO-TURBIO FORMATION; EOCENE SEDIMENTS; SANTA-CRUZ; ENNEADOCYSTA; DEFORMATION; GREENHOUSE; EVOLUTION; DEPOSITS; HISTORY; CARBON	An understanding of paleonvironmental and paleoceanographic evolution of the Southwestern Atlantic Ocean during the Palaeogene is prevented by the lack of precise tools to date and correlate the sedimentary units. Palynological samples collected in the upper portion of the Man Aike Formation, which crops out southern Lago Argentino area, in the southwest of the Austral Basin (50 degrees 21'45"S-72 degrees 14'30"W), contain well preserved marine organic dinoflagellate cysts, which are potentially important biostratigraphic and paleoenvironmental indicators. Herein we describe the composition of the Man Aike Formation's dinoflagellate cyst assemblages and compare them to similar assemblages collected in the same basin in the upper member of the Rio Turbio Formation using Compositional Statistical Analysis. The dinoflagellate cyst assemblages from the upper part of the Man Aike Formation are highly correlated to the assemblages from the upper member of the Rio Turbio Formation from outcropping sections (51 degrees 31'13"S-72 degrees 15'11"W) and with the lower part of sediment cores drilled by Yacimientos Carboniferos Fiscales in the Rio Turbio Formation area. These dinoflagellate cyst assemblages show a very low correlation with the assemblages from the upper part of the Yacimientos Carboniferos Fiscales's cores. The comparison of our results with the high-resolution Southern Pacific Ocean dinoflagellate cyst zonation for the late Palaeocene to late Eocene allow us to date some of the dinoflagellate events recorded in formations of southwestern Patagonia. The assemblages from the Man Aike Formation and the lower part of the upper member of the Rio Turbio Formation relate to the zones SPDZ11 and SPDZ12 and are assigned to the mid-middle Eocene (late Lutetian to early Bartonian). The biostratigraphy proposed herein constrains the age of the Man Aike Formation and equivalent units based on calcareous microfossil data, mollusks affinities and Sr-87/Sr-86 isotopic values to an age ranging between similar to 42 and 39 Ma. The assemblages from the upper part of the upper member of the Rio Turbio Formation relate to the SPDZ13 Zone, which corresponds to the late Eocene (early Priabonian). The dinoflagellate cyst assemblages indicate that they were under the influence of relatively warm, marine open waters in an innershelf environment for the lower part of the sections. In the upper part of the sections, the assemblages suggest shallow marine waters associated with coastal areas and high trophic levels, possibly as a result of freshwater inputs. (C) 2014 Elsevier Ltd. All rights reserved.	[Raquel Guerstein, G.; Gonzalez Estebenet, M. Sol] Univ Nacl Sur, Inst Geol Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Alperin, Marta I.] Univ Natl La Plata, Fac Ciencias Nat & Museo, RA-1900 La Plata, Argentina; [Casadio, Silvio A.] Univ Nacl Rio Negro, Inst Invest Paleobiol & Geol, RA-8332 Roca, Rio Negro, Argentina; [Archangelsky, Sergio] Museo Argentina Ciencias Nat Bernardino Rivadavia, RA-1405 Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); National University of La Plata; Museo La Plata; Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN)	Guerstein, GR (通讯作者)，Univ Nacl Sur, Inst Geol Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	raquel.guerstein@uns.edu.ar		Guerstein, G. Raquel/0000-0003-1623-1084	Agencia Nacional de Promocion Cientifica y Tecnologica [PICT 89/09]; Consejo Nacional de Investigaciones Cientificas y Tecnicas [PIP: 112-201101-00566]; Universidad Nacional del Sur [PGI 24/H125]	Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); Consejo Nacional de Investigaciones Cientificas y Tecnicas(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Universidad Nacional del Sur	The authors thank O. Cardenas (MACN) for the palynological technical assistance and R. Matano (CEOAS, Oregon State University), for his valuable critical reading and linguistic improvement of the manuscript before submission. P.K. Bijl and an anonymous reviewer are thanked for their detailed reviews, whose interesting comments and suggestions led to significant improvements. This research was supported by grants from the Agencia Nacional de Promocion Cientifica y Tecnologica (PICT 89/09), from the Consejo Nacional de Investigaciones Cientificas y Tecnicas (PIP: 112-201101-00566) and Universidad Nacional del Sur (PGI 24/H125).	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South Am. Earth Sci.	JUL	2014	52						166	178		10.1016/j.jsames.2014.02.011	http://dx.doi.org/10.1016/j.jsames.2014.02.011			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AH9LU		Green Published			2025-03-11	WOS:000336464700011
J	Sarkar, S; Mandal, JP				Sarkar, Samir; Mandal, J. P.			First Record of Palynofossils from the Fulra Limestone Formation (Middle Eocene) of Kachchh Basin, Gujarat and their Palaeoenvironmental Implications	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						Palynofossils; Fulra Limestone Formation; Middle Eocene; Kachchh; Gujarat	ALGAE	The present paper deals with the first record of a palynofloral assemblage recovered from the Fulra Limestone Formation exposed at the confluence of Fulra and Panandhro Nalas in the west of Babia hill, Kachchh basin, Gujarat. The recovered palynoflora consists of dinoflagellate cysts, fungal spores and ascostromata, pteridophyte spores, gymnosperm and angiosperm pollen. Some of the important constituents of the palynofloral assemblage are: Lygodiumsporites, Polypodiaceasporites, Polypodiisporites, Margocolporites, Tricolporopilites, Tricolporopollis, Graminidites, Aplanosporites, Phragmothyrites, Spiniferites, Operculodinium and Achomosphaera. Palynological data suggest that the Fulra Limestone Formation was mostly laid down in a shallow marine environment under a warm and humid tropical climate. Abundance of terrestrial palynofossils in some of the samples clearly points towards the relative proximity of the shore. A late middle Eocene age has been assigned for the Fulra Limestone Formation on the basis of recorded palynofossils.	[Sarkar, Samir] 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						[Anonymous], 2003, GONDWANA GEOL MAGZ S; [Anonymous], MONOGR PALAEONTOL SO; Biswas S.K., 1965, Bull. Geol. Min. Met Soc, V15, P1; BISWAS S.K., 1971, Q JOUR GEOL MIN MET, V43, P177; Hardas M.G., 1973, Bulletin ONGC, V10, P47; Humane S.K., 2005, J ENV MICROPAL MICRO, V2, P4; Humane S.K., 2006, PALEOBOTANIST, V55, P45; Humane S.K., 2010, ONGC B, V45, P30; KAR R K, 1981, Geophytology, V11, P103; KAR R K, 1977, Geophytology, V7, P121; Kar R.K., 1978, PALEOBOTANIST, V25, P167; Kar R.K., 1985, Palaeobotanist, V34, P1; Kar R.K., 1976, Palaeobotanists, V23, P1, DOI 10.54991/jop.1974.944; Kar R.K., 1979, GEOPHYTOLOGY, V9, P88; Kundal P, 2006, J GEOL SOC INDIA, V68, P630; Kundal P., 2005, GONDWANA GEOL MAGZ, V20, P119; KUNDAL P, 2002, GONDWANA GEOL MAG, V17, P89; Kundal P., 2007, Micropaleontology: Application in Stratigraphy and Paleoceanography, P145; Mathur Y. K., 1966, Q J GEOLOGICAL MININ, V38, P33; MATHUR YK, 1973, J PALYNOL, V8, P89; Mathur YK, 1969, B GEOLOGICAL MINING, V42, P1; Misra PK, 2006, J GEOL SOC INDIA, V67, P495; MOHAN M, 1970, Micropaleontology (New York), V16, P37, DOI 10.2307/1484845; Pandey J., 1982, PLAEONTOLOGICAL SOC, V1, P95; Raju D. S. N., 1974, PUBLICATION CTR ADV, V10, P136; Samanta B.K., 1985, QUATERNARY J GEOLOGI, V92, P211; Santapau, 1969, J SEN MEMORIAL VOLUM, P109; Saxena RK, 1978, PALEOBOTANIST, V25, P448; Saxena RK, 1980, PALEOBOTANIST, V26, P130; Sen Gupta B. K., 1964, Journal of the Geological Society of India, V5, P138; Singh P., 1986, GEOSCI J, V8, P145; Singh S. K., 2001, Biological Memoirs, V27, P38; Singh SK, 2010, J GEOL SOC INDIA, V75, P749, DOI 10.1007/s12594-010-0059-z; VENKATACHALA B.S., 1968, Palaeobotanist, V17, P157, DOI DOI 10.54991/JOP.1968.792	34	1	1	0	7	SPRINGER INDIA	NEW DELHI	7TH FLOOR, VIJAYA BUILDING, 17, BARAKHAMBA ROAD, NEW DELHI, 110 001, INDIA	0016-7622	0974-6889		J GEOL SOC INDIA	J. Geol. Soc. India	JUN	2014	83	6					641	646		10.1007/s12594-014-0093-3	http://dx.doi.org/10.1007/s12594-014-0093-3			6	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AK0KJ					2025-03-11	WOS:000338101200005
J	Batten, DJ; Zhou, ZY; Li, WB				Batten, David J.; Zhou, Zhi Yan; Li, Wen Ben			Plant remains from Early Cretaceous deposits on the Goban Spur, Bay of Biscay, North Atlantic Ocean, and their palaeoenvironmental significance	PALAEOWORLD			English	Article						Cretaceous; Plant mesofossils; Frenelopsid new species; Miospores; Depositional conditions; Source vegetation	CHEIROLEPIDIACEOUS CONIFER; ENGLISH WEALDEN; FRENELOPSIS; ANATOMY; FLORA; ZONE	Site 549 of the Deep Sea Drilling Project was drilled on the Goban Spur in the Bay of Biscay in 1981. The core recovered from this North Atlantic location included 290 m of Barremian and possibly partly Hauterivian "syn-rift" deposits overlain unconformably by rocks of early Albian age. The number and variety of spores and pollen grains in the palynomorph assemblages and associated palynofacies through these units together with the presence of some pieces of wood, fragments of foliage, and a few megaspores in the lowest part of the Cretaceous succession suggest that the source area vegetation was, at least initially, relatively close to the site of deposition. Ginkgoalean, bennettitalean, and other gymnosperm groups are represented in the plant mesofossil assemblage but most of the fragments of foliage show cheirolepidiaceous characteristics. Five species belonging to this family have been identified and described. Two of these, Frenelopsis atlantica Zhou and Batten and Frenelopsis? alvinii Zhou and Batten, are new and one is unnamed. The composition of the three informally identified suites of spore and pollen assemblages recovered from 49 samples through the Early Cretaceous succession is consistent with age determinations of parts of it determined previously on the basis of dinoflagellate cysts, foraminifera, nannoplankton, and other fossils. (C) 2013 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.	[Batten, David J.] Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England; [Batten, David J.] Aberystwyth Univ, Inst Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales; [Batten, David J.; Zhou, Zhi Yan; Li, Wen Ben] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China	University of Manchester; Aberystwyth University; Chinese Academy of Sciences	Batten, DJ (通讯作者)，Univ Manchester, Sch Earth Atmospher & Environm Sci, Oxford Rd, Manchester M13 9PL, Lancs, England.	david.batten@manchester.ac.uk; zyzhou@nigpas.ac.cn; wenbenli@126.com			MoST of China [2012CB821900]; Chinese Academy of Sciences Visiting Professorship for Senior International Scientists; Chinese Academy of Sciences	MoST of China(Ministry of Science and Technology, China); Chinese Academy of Sciences Visiting Professorship for Senior International Scientists; Chinese Academy of Sciences(Chinese Academy of Sciences)	This collaborative work began while one of us (Zhou) was based at the Department of Botany, Bedford College, University of London during the summer of 1982 and the other two (Batten and Li) were working in Aberdeen University. The project was resurrected by Batten during his stay at the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS) towards the end of 2011 and during the first few months of 2012. Zhou is indebted to Prof. W. G. Chaloner for access to the material and for use of facilities during 1982. Thanks are due to Dr. J. Watson for furnishing the Polish specimens of Frenelopsis hohenneggeri, the late Dr. K. L. Alvin for informative discussions, and Dr. Gong le Shi and Sijia Tang (both NIGPAS), Richard Hartley (SEAES, The University of Manchester) and Antony Smith (Aberystwyth University) for their help in preparing the figures. Zhou's research in London was supported financially by the Chinese Academy of Sciences, and his recent work in Nanjing was financed by MoST of China (2012CB821900). Li's work in Aberdeen was carried out while he was on study leave from NIGPAS during 1983-1985. Batten is grateful for the support of a Chinese Academy of Sciences Visiting Professorship for Senior International Scientists. We thank the anonymous referees for their helpful comments on the manuscript.	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J	Giusberti, L; Bannikov, A; Galazzo, FB; Fornaciari, E; Frieling, J; Luciani, V; Papazzoni, CA; Roghi, G; Schouten, S; Sluijs, A; Bosellini, FR; Zorzin, R				Giusberti, Luca; Bannikov, Alexander; Galazzo, Flavia Boscolo; Fornaciari, Eliana; Frieling, Joost; Luciani, Valeria; Papazzoni, Cesare Andrea; Roghi, Guido; Schouten, Stefan; Sluijs, Appy; Bosellini, Francesca R.; Zorzin, Roberto			A new <i>Fossil-Lagerstatte</i> from the Lower Eocene of Lessini Mountains (northern Italy): A multidisciplinary approach	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Lagerstatte; Foraminifera; Calcareous nannofossils; Dinoflagellates; Meso-bathypelagic ichthyofauna; Early Eocene	SEA-SURFACE TEMPERATURES; BENTHIC FORAMINIFERA; ORGANIC GEOCHEMISTRY; TETRAETHER LIPIDS; MEMBRANE-LIPIDS; PALEOCENE; BIOSTRATIGRAPHY; BOLCA; TEX86; GREENHOUSE	Hemipelagic dark limestones within calciturbiditic deposits at Monte Solane in the western Lessini Mountains of northern Italy yield a fish fauna dominated by stomiiforms. A minor component of the fossil assemblage is represented by a macroalgal non-calcareous flora associated with rarer terrestrial components including few angiosperm leaves and seeds. Micropaleontological (foraminifera, dinoflagellate cysts), sedimentological and geochemical proxies (TEX86) indicate a deposition of the fossil-bearing bed in a hypoxic to possibly anoxic, warm, restricted basin. High-precision dating based on rich foraminiferal and calcareous nannoplankton content allows ascribing the site to the upper part of the Ypresian (Lower Eocene). The site is slightly older than the Ypresian worldwide-famous shallow-water Bolca Konservat-Lagerstatte located in the same region. Convergent paleoenvironmental clues based on both microfossils and ichthyofauna indicate that the sediments were deposited in the upper bathyal zone, probably between 300 and 600 m. Solane is therefore one of the rare and precious Eocene Lagerstdtte to have fossilized in a deep marine setting. The site contains the oldest Cenozoic record of an ichthyofauna dominated by meso-bathypelagic taxa. (C) 2014 Elsevier B.V. All rights reserved.	[Giusberti, Luca; Galazzo, Flavia Boscolo; Fornaciari, Eliana] Univ Padua, Dipartimento Geosci, I-35131 Padua, Italy; [Bannikov, Alexander] Russian Acad Sci, Borisyak Paleontol Inst, Moscow 117997, Russia; [Frieling, Joost; Schouten, Stefan; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Luciani, Valeria] Univ Ferrara, Dipartimento Fis & Sci Terra, I-44100 Ferrara, Italy; [Papazzoni, Cesare Andrea; Bosellini, Francesca R.] Univ Modena & Reggio Emilia, Dipartimento Sci Chim & Geol, I-41121 Modena, Italy; [Roghi, Guido] CNR, Ist Geosci & Georisorse, Padua, Italy; [Schouten, Stefan] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, Texel, Netherlands; [Zorzin, Roberto] Museo Civ Storia Nat Verona, Sez Geol & Paleontol, I-37129 Verona, Italy	University of Padua; Russian Academy of Sciences; Paleontological Institute of the Russian Academy of Sciences; Utrecht University; University of Ferrara; Universita di Modena e Reggio Emilia; Consiglio Nazionale delle Ricerche (CNR); Istituto di Geoscienze e Georisorse (IGG-CNR); Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Giusberti, L (通讯作者)，Univ Padua, Dipartimento Geosci, Via Gradenigo 6, I-35131 Padua, Italy.	luca.giusberti@unipd.it	Boscolo-Galazzo, Flavia/ABB-3830-2021; Giusberti, Luca/AAA-9913-2021; Schouten, Stefan/P-4380-2016; FORNACIARI, ELIANA/ACJ-1340-2022; Papazzoni, Cesare Andrea/D-9024-2013; Francesca, Bosellini/L-7733-2015; Luciani, Valeria/K-8572-2015; Sluijs, Appy/B-3726-2009	GIUSBERTI, LUCA/0000-0002-4401-5410; FORNACIARI, ELIANA/0000-0001-7369-9535; Boscolo-Galazzo, Flavia/0000-0002-5146-5321; Roghi, Guido/0000-0002-7162-0130; Papazzoni, Cesare Andrea/0000-0001-5222-7184; Francesca, Bosellini/0000-0003-2125-0802; Luciani, Valeria/0000-0002-0079-9380; Frieling, Joost/0000-0002-5374-1625; Sluijs, Appy/0000-0003-2382-0215; zorzin, Roberto/0000-0002-8765-3316	MIUR/PRIN COFIN [2010X3PP8J_003]; Padova University [GIUSPRAT10]; European Research Council under the European Community [259627]; Netherlands Organisation for Scientific Research (NWO) [865.06.003]	MIUR/PRIN COFIN(Ministry of Education, Universities and Research (MIUR)Research Projects of National Relevance (PRIN)); Padova University; European Research Council under the European Community(European Research Council (ERC)); Netherlands Organisation for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO))	We thank Lorenzo Franceschin, Carlotta Betto (both Padova) and Natasja Welters (Utrecht) for processing the samples for micropaleontological analyses. Stefano Castelli and Nicola Michelon are acknowledged for technical support. We all acknowledge Mr. Luigi Ambrosi who discovered the site and supported us during fieldwork activity. Funding for this research to LG, EF; FBG; VL, FB, CAP was provided by MIUR/PRIN COFIN 2011/2012 #2010X3PP8J_003. LG, EF and FBG were additionally supported by Padova University funding (Progetto di Ateneo GIUSPRAT10). AS thanks the European Research Council under the European Community's Seventh Framework Program for ERC Starting Grant #259627. SS thanks the Netherlands Organisation for Scientific Research (NWO) for a VICI grant #865.06.003. Conceived and coordinated the "Solane project": LG, GR, and RZ. Sampling and geological interpretation of the site: LG, GR, EF, CAP, and RZ. Macrofossils analyses and interpretation: AB, GR, and FB. Micropaleontological analyses and interpretation of data: EF, FBG, LG, VI, CAP, JF, and AS. Geochemical analyses and interpretation of data: JF, AS, and SS. Wrote the paper: LG, AB, FBG, EF, JF, VI, CAP, GR, SS, and AS. The editor Thierry Correge, two anonymous reviewers and Eustoquio Molina are thanked for constructively reviewing of the manuscript.	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Paleoclimatol. Paleoecol.	JUN 1	2014	403						1	15		10.1016/j.palaeo.2014.03.012	http://dx.doi.org/10.1016/j.palaeo.2014.03.012			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AH9PF		Green Published			2025-03-11	WOS:000336473600001
J	Bechtel, A; Movsumova, U; Pross, J; Gratzer, R; Coric, S; Sachsenhofer, RF				Bechtel, Achim; Movsumova, Ulviyya; Pross, Joerg; Gratzer, Reinhard; Coric, Stjepan; Sachsenhofer, Reinhard F.			The Oligocene Maikop series of Lahich (eastern Azerbaijan): Paleoenvironment and oil-source rock correlation	ORGANIC GEOCHEMISTRY			English	Article						Biomarker; Depositional environment; Eastern Paratethys; Oil-source rock correlation; Eocene; Oligocene	CRUDE OILS; DEPOSITIONAL ENVIRONMENT; MOLECULAR INDICATORS; ORGANIC GEOCHEMISTRY; RESTRICTED UTILITY; POTENTIAL SOURCES; ARYL ISOPRENOIDS; MOLASSE BASIN; SW-GERMANY; CARBON	The Maikop Formation, deposited in eastern Azerbaijan during Oligocene and Early Miocene, represents a prolific source unit for the oils found within the southern Gobustan area and the Kura Depression. Based on biomarker characteristics, the oils are believed to have originated from a clastic source rock deposited in an anoxic to suboxic, transitional marine environment with low to moderate input of terrigenous organic matter. However, due to the thermal immaturity of accessible Maikop rocks, oil-source rock correlation based on biomarker fingerprints is hampered. The results from a sedimentary succession sampled in the Shemakha-Gobustan area near the village of Lahich revealed the presence of marginally mature (Rr = 0.6-0.7%) Maikop rocks. Based on lithology, geo-chemical data and paleontological analyses, the sampled section contains Upper Eocene and Lower Oligocene sediments. Palynological analyses of dinoflagellate cysts indicate an early Rupelian to early Chattian (Oligocene) age for the upper part of the investigated Maikop succession. However, the strati-graphic position of the middle and lower part of the succession remains unclear. Maceral composition, as well as biomarker and stable isotope (C, N) data indicate a major contribution of aquatic organisms and variable inputs from macrophytes and land plants to organic matter deposition during the Oligocene. Microbial communities most probably included heterotrophic bacteria and cyanobacteria, as well as green sulfur bacteria. Higher inputs of terrigenous organic matter occurred during deposition of the lower part of the succession. Increased remineralisation of organic matter in the water column is suggested to result in low TOC and hydrocarbon contents, as well as N-15 enriched total nitrogen of the Eocene to earliest Oligocene sediments. Organic carbon accumulation during the Oligocene occurred in a stratified, episodically euxinic environment. This is indicated by low TOC/S ratios and higher contents of aryl isoprenoids in several samples from the upper units. A moderate to good oil-source rock correlation with oils from the Kura Depression is indicated by sterane and triterpane fingerprints as well as carbon isotopic composition of hydrocarbon fractions. (C) 2014 Elsevier Ltd. All rights reserved.	[Bechtel, Achim; Movsumova, Ulviyya; Gratzer, Reinhard; Sachsenhofer, Reinhard F.] Univ Leoben, Dept Appl Geosci & Geophys, A-8700 Leoben, Austria; [Movsumova, Ulviyya] Azerbaijan Natl Acad Sci, Inst Geol, Baku 370143, Azerbaijan; [Pross, Joerg] Heidelberg Univ, Inst Earth Sci, D-69120 Heidelberg, Germany; [Coric, Stjepan] Geol Survey Austria, Dept Sedimentgeol, A-1030 Vienna, Austria	University of Leoben; Azerbaijan National Academy of Sciences (ANAS); Ruprecht Karls University Heidelberg	Bechtel, A (通讯作者)，Univ Leoben, Dept Appl Geosci & Geophys, Peter Tunner Str 5, A-8700 Leoben, Austria.	Achim.Bechtel@unileoben.ac.at	Sachsenhofer, Reinhard/KFA-6113-2024; Movsumova, Ulviyya/HCH-1905-2022; Bechtel, Achim/A-9885-2011	Sachsenhofer, Reinhard/0000-0002-6616-5583; Movsumova, Ulviyya/0000-0001-8486-2537; Bechtel, Achim/0000-0002-3937-8209	European Research Foundation [237917]; Azerbaijan National Academy of Sciences; British Petroleum	European Research Foundation(European Science Foundation (ESF)); Azerbaijan National Academy of Sciences(Azerbaijan National Academy of Sciences (ANAS)); British Petroleum	The authors thank Sh. A. Babayev, T.N. Kengerli, and Sh. Sh. Bay-ramova from the Azerbaijan National Academy of Sciences for field work and providing sample material. The article benefitted from critical remarks of J. Curiale and an anonymous reviewer. Financial support by the European Research Foundation (Marie-Curie Reintegration Fellowship to AB; Project No. 237917) is gratefully acknowledged. Additional support was provided by the Azerbaijan National Academy of Sciences to UM, and by British Petroleum.	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J	Hallegraeff, G; Coman, F; Davies, C; Hayashi, A; McLeod, D; Slotwinski, A; Whittock, L; Richardson, AJ				Hallegraeff, Gustaaf; Coman, Frank; Davies, Claire; Hayashi, Aiko; McLeod, David; Slotwinski, Anita; Whittock, Lucy; Richardson, Anthony J.			Australian Dust Storm Associated with Extensive <i>Aspergillus sydowii</i> Fungal "Bloom" in Coastal Waters	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article								A massive central Australian dust storm in September 2009 was associated with abundant fungal spores (150,000/m(3)) and hyphae in coastal waters between Brisbane (27 degrees S) and Sydney (34 degrees S). These spores were successfully germinated from formalinpreserved samples, and using molecular sequencing of three different genes (the large subunit rRNA gene [LSU], internal transcribed spacer [ITS], and beta-tubulin gene), they were conclusively identified as Aspergillus sydowii, an organism circumstantially associated with gorgonian coral fan disease in the Caribbean. Surprisingly, no human health or marine ecosystem impacts were associated with this Australian dust storm event. Australian fungal cultures were nontoxic to fish gills and caused a minor reduction in the motility of Alexandrium or Chattonella algal cultures but had their greatest impacts on Symbiodinium dinoflagellate coral symbiont motility, with hyphae being more detrimental than spores. While we have not yet seen any soft coral disease outbreaks on the Australian Great Barrier Reef similar to those observed in the Caribbean and while this particular fungal population was non-or weakly pathogenic, our observations raise the possibility of future marine ecosystem pathogen impacts from similar dust storms harboring more pathogenic strains.	[Hallegraeff, Gustaaf; Hayashi, Aiko; Whittock, Lucy] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia; [Coman, Frank; Davies, Claire; Slotwinski, Anita; Richardson, Anthony J.] CSIRO Marine & Atmospher Res, Ecosci Precinct, Brisbane, Qld, Australia; [Coman, Frank; Davies, Claire; Slotwinski, Anita; Richardson, Anthony J.] Australian Antarctic Div, Dept Sustainabil Environm Water Populat & Communi, Kingston, Tas, Australia; [Richardson, Anthony J.] Univ Queensland, Sch Math & Phys, Ctr Applicat Nat Resource Math, St Lucia, Qld, Australia; [Richardson, Anthony J.] Univ Queensland, Sch Biol Sci, Environm Decis Grp, Brisbane, Qld, Australia	University of Tasmania; Commonwealth Scientific & Industrial Research Organisation (CSIRO); Australian Antarctic Division; University of Queensland; University of Queensland	Hallegraeff, G (通讯作者)，Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia.	hallegraeff@utas.edu.au	Davies, Claire/G-6888-2013; Hallegraeff, Gustaaf/C-8351-2013; Richardson, Anthony/B-3649-2010	Coman, Frank/0000-0001-6743-5154; Hallegraeff, Gustaaf/0000-0001-8464-7343; davies, claire/0000-0002-0424-1835; Hayashi, Aiko/0000-0002-7348-9682; Richardson, Anthony/0000-0002-9289-7366	Integrated Marine Observing System (IMOS); Australian Government through the National Collaborative Research Infrastructure Strategy; Super Science Initiative; Australia Research Council [DP130102725]; NERC [NE/I030062/1] Funding Source: UKRI	Integrated Marine Observing System (IMOS); Australian Government through the National Collaborative Research Infrastructure Strategy(Australian GovernmentDepartment of Industry, Innovation and Science); Super Science Initiative; Australia Research Council(Australian Research Council); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	AusCPR is funded by the Integrated Marine Observing System (IMOS), which is funded by the Australian Government through the National Collaborative Research Infrastructure Strategy and the Super Science Initiative. This work was funded by Australia Research Council grant DP130102725.	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J	Mertens, KN; Takano, Y; Head, MJ; Matsuoka, K				Mertens, Kenneth N.; Takano, Yoshihito; Head, Martin J.; Matsuoka, Kazumi			Living fossils in the Indo-Pacific warm pool: A refuge for thermophilic dinoflagellates during glaciations	GEOLOGY			English	Article							MIDDLE MIOCENE; CLIMATE TRANSITION; OCEAN; CYST; BIODIVERSITY; DIVERSITY; ATLANTIC	How important are refugia for plankton biogeography? Here for the first time we report living cysts of the fossil dinoflagellate Dapsilidinium pastielsii from Southeast Asia: Shioya Bay (Okinawa, Japan), Koror (Palau), Ambon (Indonesia), East Vietnam Sea (Vietnam), and Masinloc (the Philippines). This species, thought to have become extinct in the early Pleistocene, is the last survivor of a major early Cenozoic lineage. Its disappearance from the Atlantic following the early Pleistocene implies cooling, and the discovery of living D. pastielsii in the Indo-Pacific warm pool suggests that this unique environment with stable temperatures served as an important refuge for thermophilic dinoflagellates with a >50 m.y. lineage. This is the first record of a refugium plankton species within the Indo-Pacific warm pool.	[Mertens, Kenneth N.] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Takano, Yoshihito; Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res ECSER, Nagasaki 8528521, Japan; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Ghent University; Nagasaki University; Brock University	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.		Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Mertens, Kenneth/0000-0003-2005-9483	KAKENHI [22-00805]; Natural Sciences and Engineering Research Council of Canada	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(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	Mertens is a Fonds Wetenschappelijk Onderzoek (Belgium) postdoctoral fellow. This study was partly conducted at Nagasaki University and supported by KAKENHI (Grants-in-Aid for Scientific Research) grant 22-00805. Head acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. We thank Lucy Edwards, Jim Riding, and an anonymous reviewer for comments that improved the manuscript.	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J	Bosboom, R; Dupont-Nivet, G; Grothe, A; Brinkhuis, H; Villa, G; Mandic, O; Stoica, M; Kouwenhoven, T; Huang, WT; Yang, W; Guo, ZJ				Bosboom, Roderic; Dupont-Nivet, Guillaume; Grothe, Arjen; Brinkhuis, Henk; Villa, Giuliana; Mandic, Oleg; Stoica, Marius; Kouwenhoven, Tanja; Huang, Wentao; Yang, Wei; Guo, ZhaoJie			Timing, cause and impact of the late Eocene stepwise sea retreat from the Tarim Basin (west China)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Eocene; Asia; Tarim Basin; Paratethys Sea; Biostratigraphy; Palaeogeography	NORTHERN TIBETAN PLATEAU; MIDDLE EOCENE; EARLY OLIGOCENE; TIAN-SHAN; ISOTOPIC CONSTRAINTS; DINOFLAGELLATE CYSTS; PALEOGENE EVOLUTION; RESEARCH BOREHOLE; UPLIFT HISTORY; CLIMATE-CHANGE	A vast shallow epicontinental sea extended across Eurasia and was well-connected to the Western Tethys before it retreated westward and became isolated as the Paratethys Sea. However, the palaeogeography and the timing of this westward retreat are too poorly constrained to determine potential wider environmental impacts, let alone understanding underlying mechanisms of the retreat such as global eustasy and tectonism associated with the Indo-Asia collision. Here, an improved chronostratigraphic and palaeogeographic framework is provided for the onset of the proto-Paratethys Sea retreat at its easternmost extent in the Tarim Basin in western China is provided. Five different third-order sea-level cycles can be recognised from the Cretaceous-Palaeogene sedimentary record in the Tarim Basin, of which the last two stepped successively westwards as the sea retreated after the maximum third incursion. New biostratigraphic data from the fourth and fifth incursions at the western-most margin of the Tarim Basin are compared to our recent integrated bio-magneto-stratigraphic results on the fourth incursion near the palaeodepocentre in the south-western part of the basin. While the fourth incursion extended throughout the basin and retreated at similar to 41 Ma (base Cl8r), the last and fifth incursion is restricted to the westernmost margin and its marine deposits are assigned a latest Bartonian-early Priabonian age from similar to 38.0 to similar to 36.7 Ma (near top Cl 7n.2n to base Cl 6n.2n). Similar to the fourth, the fossil assemblages of the fifth incursion are indicative of shallow marine, near-shore conditions and their widespread distribution across Eurasia suggests that the marine connection to the Western Tethys was maintained. The lack of diachronicity of the fourth incursion between the studied sections across the southwest Tarim Basin suggests that the sea entered and withdrew relatively rapidly, as can be expected in the case of eustatic control on a shallow epicontinental basin. However, the westward palaeogeographic step between the fourth and fifth incursions separated by several millions of years rather suggests the combined long-term effect of tectonism, possibly associated with early uplift of the Pamir-Kunlun Shan thrust belt. The fourth and fifth regressions are time-equivalent with significant aridification steps recorded in the Asian interior, thus supporting climate modelling results showing that the stepwise sea retreat from Central Asia amplified the acidification of the Asian interior. (C) 2014 Elsevier B.V. All rights reserved.	[Bosboom, Roderic; Dupont-Nivet, Guillaume; Huang, Wentao] Univ Utrecht, Fac Geosci, Paleomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands; [Dupont-Nivet, Guillaume; Huang, Wentao; Yang, Wei; Guo, ZhaoJie] Peking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China; [Dupont-Nivet, Guillaume; Huang, Wentao; Yang, Wei] Univ Rennes 1, UMR 6118, F-35042 Rennes, France; [Grothe, Arjen; Brinkhuis, Henk; Kouwenhoven, Tanja] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Villa, Giuliana] Univ Parma, Dipartimento Fis & 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	Utrecht University; Peking University; Universite de Rennes; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Utrecht University; University of Parma; University of Bucharest	Bosboom, R (通讯作者)，Univ Utrecht, Fac Geosci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands.	R.E.Bosboom@uu.nl	Stoica, Marius/N-4941-2018; Brinkhuis, Henk/IUO-8165-2023; Dupont-Nivet, Guillaume/HII-9066-2022	Mandic, Oleg/0000-0003-1955-7514; Stoica, Marius/0000-0003-0126-4270; Dupont-Nivet, Guillaume/0000-0001-9905-9739; Brinkhuis, Henk/0000-0003-0253-6610	Netherlands Organization for Scientific Research (NWO); Egide Cai Yuanpei programme	Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); Egide Cai Yuanpei programme	This project was funded by the Netherlands Organization for Scientific Research (NWO) with grants to Roderic Bosboom and Guillaume Dupont-Nivet and the Molengraaff Fund with a grant to Arjen Grothe. We acknowledge support from the Egide Cai Yuanpei programme. We would like to thank Laurie Bougeois and Gloria Heilbronn for their contributions in the field, Tom Mullender and Mark Dekkers for their assistance in the palaeomagnetic laboratory, Franz Topka (NHM Vienna) for mollusc sample preparation and Natasja Welters for her assistance in the palynological laboratory.	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Paleoclimatol. Paleoecol.	JUN 1	2014	403						101	118		10.1016/j.palaeo.2014.03.035	http://dx.doi.org/10.1016/j.palaeo.2014.03.035			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AH9PF		Green Submitted			2025-03-11	WOS:000336473600009
J	Hennissen, JAI; Head, MJ; De Schepper, S; Groeneveld, J				Hennissen, Jan A. I.; Head, Martin J.; De Schepper, Stijn; Groeneveld, Jeroen			Palynological evidence for a southward shift of the North Atlantic Current at ∼2.6 Ma during the intensification of late Cenozoic Northern Hemisphere glaciation	PALEOCEANOGRAPHY			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; SEA-SURFACE TEMPERATURES; CENTRAL-AMERICAN SEAWAY; LATE PLIOCENE; QUATERNARY SYSTEM/PERIOD; PLEISTOCENE SERIES/EPOCH; PLANKTONIC-FORAMINIFERA; OCEAN CIRCULATION; NORWEGIAN SEA; CHINESE LOESS	The position of the North Atlantic Current (NAC) during the intensification of Northern Hemisphere glaciation (iNHG) has been evaluated using dinoflagellate cyst assemblages and foraminiferal geochemistry from a similar to 260 kyr interval straddling the base of the Quaternary System from two sites: eastern North Atlantic Deep Sea Drilling Project Site 610 in the path of the present NAC and central North Atlantic Integrated Ocean Drilling Program Site U1313 in the subtropical gyre. Stable isotope and foraminiferal Mg/Ca analyses confirm cooling near the marine isotope stage (MIS) G7-G6 transition (2.74Ma). However, a continued dominance of the dinoflagellate cyst Operculodinium centrocarpum sensu Wall and Dale (1966) indicates an active NAC in the eastern North Atlantic for a further 140 kyr. At MIS 104 (similar to 2.60Ma), a profound dinoflagellate cyst assemblage turnover indicates NAC shutdown in the eastern North Atlantic, implying elevated atmospheric pressure over the Arctic and a resulting shift in the westerlies that would have driven the NAC. These findings challenge recent suggestions that there was no significant southward shift of the NAC or the Arctic Front during iNHG, and reveal a fundamental climatic reorganization near the base of the Quaternary.	[Hennissen, Jan A. I.; Head, Martin J.] Univ Toronto, Dept Earth Sci, Toronto, ON, Canada; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [De Schepper, Stijn] Univ Bergen, Dept Earth Sci, Bergen, Norway; [De Schepper, Stijn] Univ Bremen, Dept Geosci, Bremen, Germany; [De Schepper, Stijn] Bjerknes Ctr Climate Res, Bergen, Norway	University of Toronto; Brock University; University of Bergen; University of Bremen; Bjerknes Centre for Climate Research	Hennissen, JAI (通讯作者)，British Geol Survey, Keyworth NG12 5GG, Notts, England.	janh@bgs.ac.uk	Hennissen, Jan/AAT-7729-2020; De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914; Hennissen, Jan/0000-0002-0435-3343	Natural Sciences and Engineering Research Council of Canada; Canadian Consortium for Ocean Drilling; AASP-the Palynological Society; British Geological Survey; Deutsche Forschungsgemeinschaft [SCHE 1665/2-1, SCHE 1665/2-2]; NERC [bgs05002] Funding Source: UKRI	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Canadian Consortium for Ocean Drilling; AASP-the Palynological Society; British Geological Survey; Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This contribution is based on the doctoral research of J.A.I.H. which was supported by a Natural Sciences and Engineering Research Council of Canada Discovery grant to M.J.H. J.A.I.H. also acknowledges support from the Canadian Consortium for Ocean Drilling, AASP-the Palynological Society, and the British Geological Survey, and is grateful to Helmut Willems for his hospitality during an extended visit to his laboratory in Bremen. S. D. S. acknowledges funding from the Deutsche Forschungsgemeinschaft (projects SCHE 1665/2-1 and SCHE 1665/2-2). Samples were kindly provided by the Integrated Ocean Drilling Program. We thank M. Segl (isotopes) and S. Pape (Mg/Ca) for technical support. The reviews of David Naafs and an anonymous colleague are gratefully acknowledged.	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J	De Schepper, S; Head, MJ				De Schepper, Stijn; Head, Martin J.			New late Cenozoic acritarchs: evolution, palaeoecology and correlation potential in high latitude oceans	JOURNAL OF SYSTEMATIC PALAEONTOLOGY			English	Article						Lavradosphaera; Bering Sea; North Atlantic; late Cenozoic; palynology; Cymatiosphaera	DINOFLAGELLATE CYST STRATIGRAPHY; CENTRAL-AMERICAN SEAWAY; PLIOCENE-PLEISTOCENE; ARCTIC-OCEAN; MIOCENE; AGE; ICELAND; PALYNOMORPHS; CIRCULATION; CALIBRATION	Acritarchs have received limited attention in palynological studies of the Cenozoic, although they have much potential both for refining Neogene and Quaternary stratigraphy, especially in mid- and high northern latitudes, and developing palaeoceanographical reconstructions. Here we formally describe and document the stratigraphical and palaeotemperature ranges (from foraminiferal Mg/Ca) of four new acritarch species: Cymatiosphaera? aegirii sp. nov., Cymatiosphaera? fensomei sp. nov., Cymatiosphaera? icenorum sp. nov. and Lavradosphaera canalis sp. nov. In reviewing the stratigraphical distributions of all species of the genus Lavradosphaera De Schepper & Head, 2008, we demonstrate their correlation potential between the North Atlantic and Bering Sea in the Pliocene. Additionally, Lavradosphaera lucifer De Schepper & Head, 2008 and Lavradosphaera canalis sp. nov., while not themselves overlapping stratigraphically, have morphological intermediates that do partially overlap and may represent an evolutionary trend consequent upon climate cooling in the Late Pliocene. Finally, we show that the highest abundances of the acritarchs presented here were living in the eastern North Atlantic, in surface-water temperatures not very different from today. http://zoobank.org/urn:lsid:zoobank.org:pub:7AB934D1-E452-4117-9D38-76C3FCFC00B8	[De Schepper, Stijn] Univ Bremen, Geosci Dept, D-28334 Bremen, Germany; [De Schepper, Stijn] Univ Bergen, Dept Earth Sci, N-5020 Bergen, Norway; [Head, Martin J.] Brock Univ, Dept Earth Sci, Ontario, ON L2S 3A1, Canada	University of Bremen; University of Bergen; Brock University	De Schepper, S (通讯作者)，Univ Bremen, Geosci Dept, POB 330440, D-28334 Bremen, Germany.	smad2@cantab.net	De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914	Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft [SCHE 1665/2-1, SCHE 1665/2-2]; University of Bergen	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); University of Bergen	Samples were kindly provided by the Integrated Ocean Drilling Program. Thanks go to S. Forke (University Bremen), S. Louwye and S. Vancauwenberghe (Ghent University), J. Knies (NGU, Trondheim), J. Giraudeau and the palynology laboratory at the Universite de Bordeaux for facilitating palynological sample preparations; and H. Willems and P. Witte (University of Bremen) for use of the SEM and technical support. Discussions with M. Schreck (AWI, Bremerhaven) who kindly provided information on acritarch ranges from ODP Hole 907A are greatly appreciated. MJH acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. SDS acknowledges funding from the Deutsche Forschungsgemeinschaft (projects SCHE 1665/2-1 and SCHE 1665/2-2) and University of Bergen. We are most grateful to J. Matthiessen and an anonymous reviewer for their constructive reviews of the manuscript.	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Syst. Palaeontol.	MAY 19	2014	12	4					493	519		10.1080/14772019.2013.783883	http://dx.doi.org/10.1080/14772019.2013.783883			27	Evolutionary Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Evolutionary Biology; Paleontology	AE4DA					2025-03-11	WOS:000333929600006
J	Mattingsdal, R; Knies, J; Andreassen, K; Fabian, K; Husum, K; Grosfjeld, K; De Schepper, S				Mattingsdal, Rune; Knies, Jochen; Andreassen, Karin; Fabian, Karl; Husum, Katrine; Grosfjeld, Kari; De Schepper, Stijn			A new 6 Myr stratigraphic framework for the Atlantic-Arctic Gateway	QUATERNARY SCIENCE REVIEWS			English	Article						Stratigraphic framework; Atlantic-Arctic Gateway; Yermak Plateau; Svalbard; High-resolution seismic data; Ocean Drilling Program (ODP); Paleoenvironment; Depositional setting	YERMAK PLATEAU; LATE PLIOCENE; MID-PLIOCENE; DINOFLAGELLATE CYST; LOMONOSOV RIDGE; SEISMIC DATA; ICE-SHEET; NORTHERN; OCEAN; WATER	A comprehensive stratigraphic framework for the Atlantic-Arctic Gateway has been established for the last 6 Myr on the Yermak Plateau, NW Svalbard, based on new paleomagnetic and biostratigraphic sampling and correlation of high-resolution seismic data between Ocean Drilling Program (ODP) Holes 911A, 910C and 912A. The new results indicate a Late Miocene age for the base of both Holes 911A and 910C, providing the first complete late Neogene record for the marginal Arctic Ocean and extending the previously published age model by several million years. During the late Miocene-Pleistocene, the southern Yermak Plateau was dominated by contourite deposition. From the intensification of the Northern Hemisphere glaciation at similar to 2.7 Ma, glacial fans from NW Svalbard prograded onto the southernmost Yermak Plateau. This indicates that the ice sheet on NW Svalbard reached the shelf break at similar to 2.7 Ma, much earlier than on the western Barents Sea-Svalbard margin (similar to 1.5 Ma). Simultaneous with the first shelf break glaciation on the western Barents Sea-Svalbard margin at similar to 1.5 Ma, we observe the first signs of extensive glacial erosion on the Yermak Plateau, indicating a regional glacial intensification at this time for the whole Barents Sea-Svalbard region. Our results agree well with the widening/deepening of the Fram Strait and the opening of the Atlantic Arctic Gateway during the middle Miocene. (C) 2013 Elsevier Ltd. All rights reserved.	[Mattingsdal, Rune; Andreassen, Karin; Husum, Katrine] Univ Tromso, Dept Geol, N-9037 Tromso, Norway; [Knies, Jochen; Fabian, Karl; Grosfjeld, Kari] Geol Survey Norway, N-7491 Trondheim, Norway; [Knies, Jochen; Andreassen, Karin; Fabian, Karl] Univ Tromso, Ctr Arctic Gas Hydrate Environm & Climate, N-9037 Tromso, Norway; [De Schepper, Stijn] Univ Bergen, Dept Earth Sci, N-5007 Bergen, Norway	UiT The Arctic University of Tromso; Geological Survey of Norway; UiT The Arctic University of Tromso; University of Bergen	Mattingsdal, R (通讯作者)，Norwegian Petr Directorate, Verkstedveien 1,POB 787, N-9488 Harstad, Norway.	nme.mattingsdal@npd.no	Fabian, Karl/AAC-8643-2022; Husum, Katrine/HGD-4711-2022; De Schepper, Stijn/A-2836-2011	Andreassen, Karin/0000-0002-9407-526X; De Schepper, Stijn/0000-0002-6934-0914; Husum, Katrine/0000-0003-1380-5900	Norwegian Research Council (NRC) [200672/S60, 223259]; Statoil; Det Norske; BG Norge	Norwegian Research Council (NRC)(Research Council of Norway); Statoil; Det Norske; BG Norge	This work is a contribution to the project "Glaciations in the Barents Sea area" (GlaciBar) funded by the Norwegian Research Council (NRC grant 200672/S60), Statoil, Det Norske and BG Norge. We thank the captain and crew of R/V Jan Mayen (now Helmer Hanssen) and Steinar Iversen for acquisition of the seismic data. We acknowledge the Norwegian Petroleum Directorate for the multichannel seismic data from the Western Svalbard margin. This research also used samples and data provided by the Integrated Ocean Drilling Program (IODP). The staff at the IODP Bremen Core Repository is greatly acknowledged for their support during numerous sampling parties. We thank Thomas Frederichs (University of Bremen) for supporting the paleomagnetic analyses. We appreciate the constructive comments provided by Wolfram Geissler and one anonymous reviewer. The research is part of the Centre of Excellence: Arctic Gas hydrate, Environment and Climate (CAGE) funded by the Norwegian Research Council (grant No. 223259).	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Sci. Rev.	MAY 15	2014	92				SI		170	178		10.1016/j.quascirev.2013.08.022	http://dx.doi.org/10.1016/j.quascirev.2013.08.022			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AI8SX					2025-03-11	WOS:000337198400012
J	Gibb, OT; Hillaire-Marcel, C; de Vernal, A				Gibb, Olivia T.; Hillaire-Marcel, Claude; de Vernal, Anne			Oceanographic regimes in the northwest Labrador Sea since Marine Isotope Stage 3 based on dinocyst and stable isotope proxy records	QUATERNARY SCIENCE REVIEWS			English	Article						Dinoflagellate cysts; Foraminiferal stable isotopes; Labrador Sea; Late Pleistocene; Sea ice; Sea surface conditions	NORTHERNMOST BAFFIN-BAY; SURFACE CONDITIONS; HEINRICH EVENTS; LATE-QUATERNARY; HUDSON STRAIT; HOLOCENE PALEOCEANOGRAPHY; DETRITAL CARBONATE; ICE COVER; NEOGLOBOQUADRINA-PACHYDERMA; CANADIAN ARCHIPELAGO	Sea surface temperature (SST), salinity and density gradients in the upper water column of the northwest Labrador Sea have been reconstructed based on high resolution analysis of a core (HU2008-029-004PC) spanning the last similar to 36 ka, raised off Hudson Strait. The modern analogue technique was applied to dinocyst assemblages and combined with stable isotope data from Neogloboquadrina pachyderma left-coiled (Npl) for this purpose. Three oceanographic regimes were identified, broadly corresponding to the "glacial", "deglacial" and "postglacial" intervals. The site remained under the direct influence of the Laurentide Ice Sheet (LIS) margin until the postglacial and did not record the Bolling-Allerod warming and weakly recorded the Younger Dryas event. The "glacial" regime lasted until similar to 12.2 cal ka BP. It was characterized by generally low concentrations of dinocysts within an assemblage indicative of quasi-perennial sea ice. The "deglacial" regime (ca 12.2-8.3 cal ka BP) was marked by increased biogenic fluxes and more diversified dinocyst assemblages and possibly an enhanced subsurface inflow of North East Atlantic Deep Water. Warm summer (similar to 11 degrees C) but low winter (similar to 0 degrees C) sea surface temperatures, sea ice cover during about 3 months per year, and low summer salinity (similar to 28) suggest strong stratification in the upper water layer in relation to meltwater supply from the LIS. Following the final drainage of glacial Lake Agassiz through Hudson Strait, which is dated here at similar to 8.3 cal ka BP, and the subsequent LIS collapse, increased summer salinity (up to similar to 35) was accompanied by a reduced seasonal gradient of sea surface temperature from winter (similar to 3.8 degrees C) to summer (similar to 8.6 degrees C) suggesting enhanced penetration of North Atlantic Water. Weakened stratification of the surface water layer then allowed for winter convection and Labrador Sea Water formation, which is consistent with increased Npl-delta C-13 values in response to higher ventilation of the subsurface water layer. (C) 2013 Elsevier Ltd. All rights reserved.	[Gibb, Olivia T.; Hillaire-Marcel, Claude; de Vernal, Anne] GEOTOP Res Ctr, Montreal, PQ H3C 3P8, Canada		Gibb, OT (通讯作者)，GEOTOP Res Ctr, CP 8888 Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.	oliviagibb@gmail.com	Hillaire-Marcel, Claude/H-1441-2012; de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/C-9153-2013	Hillaire-Marcel, Claude/0000-0002-3733-4632	Ministere du Developpement Economique, Innovation et Exportation (MDEIE); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT); Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Resources Canada (NRCan); Natural Sciences and Engineering Research Council of Canada (NSERC) [HU2008029]	Ministere du Developpement Economique, Innovation et Exportation (MDEIE); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Resources Canada (NRCan)(Natural Resources CanadaCanadian Forest Service); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	This paper is a contribution to the Past4Future project of the 7th Framework Program of the European Commission. Support from the Ministere du Developpement Economique, Innovation et Exportation (MDEIE) and Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT) is acknowledged. Special thanks to the Canadian Foundation for Climate and Atmospheric Sciences (CFCAS), Natural Resources Canada (NRCan), and the Natural Sciences and Engineering Research Council of Canada (NSERC) for their financial support of the HU2008029 expedition in the Labrador Sea. Special thanks to Owen Brown, Rob Fensome, Peta Mudie, and Graham Williams at NRCan (Bedford Institute of Oceanography) for their in kind support of laboratory equipment, to Pierre Francus (INRS) for the CAT-scan images, and to Maryse Henry and Jean-Francois Helie for their help and expertise in the GEOTOP laboratories. We are also grateful to the reviewers who provided useful and constructive comments on the manuscript.	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Sci. Rev.	MAY 15	2014	92				SI		269	279		10.1016/j.quascirev.2013.12.010	http://dx.doi.org/10.1016/j.quascirev.2013.12.010			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AI8SX					2025-03-11	WOS:000337198400020
J	Arancio, M; Sourisseau, M; Souissi, S				Arancio, Marc; Sourisseau, Marc; Souissi, Sami			Processes leading to the coexistence of a host and its parasitoid in homogeneous environments: The role of an infected dormant stage	ECOLOGICAL MODELLING			English	Article						Individual-based model; Dinoflagellate; Parasitoid; Amoebophrya; Host-parasite interactions; Sources of coexistence	POPULATION-DYNAMICS; DINOFLAGELLATE BLOOMS; CHESAPEAKE BAY; ONAGAWA BAY; DINOPHYCEAE; GROWTH; CYSTS; PHYTOPLANKTON; SCRIPPSIELLA; TEMPERATURE	Theoretical studies have usually been used to explain host-parasitoid persistence in conditions of spatial heterogeneity or in homogeneous environments with specific conditions. In shallow estuaries where spatial heterogeneity is prevented by tides and river input, a common host-parasitoid system (dinoflagellate-Amoebophrya spp.) is able to persist even in the absence of specific conditions described in the literature. Recent observations have revealed that the cyst stage (during which the dinoflagellate host can survive in difficult environmental conditions in a dormant stage) can be infected by the parasitoid. The encystment/excystment process is suspected to be the basis for the long-term persistence of the system. In this work, the coexistence of Amoebophrya spp. and their hosts in homogeneous environments has been tested with an individual-based model of host-parasitoid interactions. Three processes that enable the coexistence were introduced into our model: (1) modifications in infection parameters, (2) a tritrophic food web and (3) a host encystment-excystment process. The persistence of the system was obtained in mixed conditions in all cases; however, the conditions required to obtain persistence with the infection parameter modifications were unrealistic. The tritrophic food web scenario produced short, stable, 10-d-long cycles in which the control of the parasite population in the environment was difficult to observe. The excystment process appears to be responsible for the interannual persistence of the system. Durable cycles with periods of 50 d were produced despite the unstable conditions. Moreover, these cycles did not depend on the proportion of infected cysts as long as a portion of the cysts remained healthy. (c) 2014 Elsevier B.V. All rights reserved.	[Arancio, Marc; Sourisseau, Marc] IFREMER, Ctr Bretagne, Lab Dynam Environm Cotier, F-29280 Plouzane, France; [Arancio, Marc; Souissi, Sami] Univ Lille 1 Sci & Technol, UMR CNRS LOG 8187, Stn Marine, F-62930 Wimereux, France	Universite de Bretagne Occidentale; Ifremer; Universite de Lille; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Arancio, M (通讯作者)，IFREMER, Ctr Bretagne, Lab Dynam Environm Cotier, CS 10070, F-29280 Plouzane, France.	marc.arancio@ifremer.fr	Souissi, Sami/C-5146-2018	sourisseau, marc/0000-0002-0778-0076; Souissi, Sami/0000-0002-6720-0096	PARALEX ANR [2009-PEXT-01201]	PARALEX ANR(Agence Nationale de la Recherche (ANR))	We would like to thank Dr. Wayne Coats for providing and discussing the data set used in this study and Dr. Lourdes Velo-Suarez and Dr. Robin Raine, who helped with corrections. We also thank the anonymous reviewers for their constructive comments. This work was supported by PARALEX ANR project no. 2009-PEXT-01201.	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Model.	MAY 10	2014	279						78	88		10.1016/j.ecolmodel.2014.02.015	http://dx.doi.org/10.1016/j.ecolmodel.2014.02.015			11	Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	AF8TW		Green Published			2025-03-11	WOS:000334989500008
J	Martin, JL; LeGresley, MM; Hanke, AR				Martin, Jennifer L.; LeGresley, Murielle M.; Hanke, Alex R.			Thirty years - <i>Alexandrium fundyense</i> cyst, bloom dynamics and shellfish toxicity in the Bay of Fundy, eastern Canada	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium fundyense; Bay of Fundy; Harmful algal blooms; Cysts	DINOFLAGELLATE GONYAULAX-EXCAVATA; TOXINS; GULF; CIRCULATION; OYSTERS	Sediment and water samples were collected for Alexandrium fundyense spatial and temporal distribution and abundance at more than 120 locations throughout the Bay of Fundy during the summers and winters of 1980-1984. These broad surveys have been repeated at various times through the past 30 years, with more regular sampling since 2004. In addition, A. fundyense abundance has been monitored at several locations within the Bay of Fundy at weekly intervals from April to November and monthly during the remaining months since 1988. Paralytic Shellfish Poisoning (PSP) toxins in shellfish (notably Mya arenaria) have also been monitored at multiple locations in the Bay of Fundy since 1943. The datasets were examined to determine relationships and roles between overwintering resting cysts, bloom initiation, bloom decline, motile cell dispersal and A. fundyense motile populations and resulting shellfish toxicity since 1980. Cysts are widely dispersed throughout the Bay of Fundy in the offshore, inshore and intertidal zones with the largest deposits located in the offshore in silt/clay sediments to the east and north of Grand Manan Island at depths of 60-180 m. Results show that there is a constant stable source of cysts in the Bay of Fundy with highest concentrations of cysts (9780 cysts cm(-3)) observed in 2010 and highest concentrations of A. fundyense motile cells (18 x 10(6) cells L-1) observed in 1980. Interannual changes in abundance in A. fundyense populations, resting cysts and the temporal trends in M. arenaria toxicity are discussed. Results show that there was no relationship between the abundance of overwintering cysts and the magnitude of A. fundyense blooms. The offshore seed beds appear to be relatively constant in cyst density among most years and serve as an important source for the motile cells that lead to initiation of major blooms and resulting shellfish toxicity throughout the Bay of Fundy. Crown Copyright (C) 2013 Published by Elsevier Ltd. All rights reserved.	[Martin, Jennifer L.; LeGresley, Murielle M.; Hanke, Alex R.] Fisheries & Oceans Canada, Biol Stn, St Andrews, NB E5B 2L9, Canada	Fisheries & Oceans Canada	Martin, JL (通讯作者)，Fisheries & Oceans Canada, Biol Stn, 531 Brandy Cove Rd, St Andrews, NB E5B 2L9, Canada.	Jennifer.Martin@dfo-mpo.gc.ca	Martin, Jennifer/G-5217-2011					Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; AOAC, 1990, Official Methods of Analysis, P881; Aretxabaleta AL, 2009, J GEOPHYS RES-OCEANS, V114, DOI 10.1029/2008JC004948; Aretxabaleta AL, 2008, J GEOPHYS RES-OCEANS, V113, DOI 10.1029/2007JC004480; Borkman D, 2009, J SEA RES, V61, P1, DOI 10.1016/j.seares.2008.10.008; Bricelj V. 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Part II-Top. Stud. Oceanogr.	MAY	2014	103						27	39		10.1016/j.dsr2.2013.08.004	http://dx.doi.org/10.1016/j.dsr2.2013.08.004			13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM					2025-03-11	WOS:000338810600003
J	Pilskaln, CH; Anderson, DM; McGillicuddy, DJ; Keafer, BA; Hayashi, K; Norton, K				Pilskaln, C. H.; Anderson, D. M.; McGillicuddy, D. J.; Keafer, B. A.; Hayashi, K.; Norton, K.			Spatial and temporal variability of <i>Alexandrium</i> cyst fluxes in the Gulf of Maine: Relationship to seasonal particle export and resuspension	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Gulf of Maine; Particulate flux; Sediment traps; Alexandrium; Cysts; Resuspension	RED-TIDE DINOFLAGELLATE; APRIL-JUNE 1998; FUNDYENSE BLOOMS; RESTING CYSTS; CASCO BAY; TROPHIC ACCUMULATION; TOXIC DINOFLAGELLATE; GONYAULAX-EXCAVATA; MASSACHUSETTS BAY; COASTAL CURRENT	Quantification of Alexandrium cyst fluxes through the Gulf of Maine water column is central to understanding the linkage between the source and fate of annual Alexandrium blooms in the offshore waters. These blooms often lead to paralytic shellfish poisoning (PSP) and extensive closures of shellfish beds. We report here on time-series sediment trap deployments completed at four offshore locations in the gulf between 2005 and 2010 as components of two ECOHAB-GOM field programs. Data presented documents the substantial spatial and temporal fluctuations in Alexandrium fundyense cyst fluxes in the gulf. Cyst delivery out of the euphotic zone peaked primarily between July and August following annual spring-summer Alexandrium blooms and was greatest in the western gulf. At all sites, cyst flux maxima to the subsurface waters were rarely coincident with seasonal peaks in the total mass export of particulate material indicating that cyst delivery was primarily via individually sinking cysts. Where persistent benthic nepheloid layers (BNLs) exist, significant sediment resuspension input of cysts to the near-bottom water column was evidenced by deep cyst fluxes that were up to several orders of magnitude greater than that measured above the BNL. The largest cyst fluxes in the BNL were observed in the eastern gulf, suggesting greater resuspension energy and BNL cyst inventories in this region. Temporal similarities between peak cyst export out of the upper ocean and peak cyst fluxes in the BNL were observed and document the contribution of seasonal, newly formed cysts to the BNL. The data however also suggest that many Alexandrium cells comprising the massive, short-lived blooms do not transition into cysts. Time-series flow measurements and a simple 1D model demonstrate that the BNL cyst fluxes reflect the combined effects of tidal energy-maintained resuspension, deposition, and input of cysts from the overlying water column. (C) 2012 Elsevier Ltd. All rights reserved.	[Pilskaln, C. H.; Hayashi, K.] Univ Massachusetts Dartmouth, Sch Marine Sci & Technol, New Bedford, MA 02744 USA; [Anderson, D. M.; McGillicuddy, D. J.; Keafer, B. A.; Norton, K.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	University of Massachusetts System; University Massachusetts Dartmouth; Woods Hole Oceanographic Institution	Pilskaln, CH (通讯作者)，Univ Massachusetts Dartmouth, Sch Marine Sci & Technol, New Bedford, MA 02744 USA.	cpilskaln@umassd.edu		McGillicuddy, Dennis/0000-0002-1437-2425	NOAA [NA04NOS4780274 (ECOHAB-GOM/Cyst), NA06NOS4780245 (GOMTOX)]; Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF) [OCE-0430724, OCE-0911031]; National Institute of Environmental Health Sciences (NIEHS) [1-P50-ES012742-01]; Division Of Ocean Sciences; Directorate For Geosciences [1314642] Funding Source: National Science Foundation	NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF)(National Science Foundation (NSF)); 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)); Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We are extremely grateful to the captains and crews of the following vessels who made the 5 years of mooring deployments and recoveries in the Gulf of Maine a success: R/V Oceanus, R/V Connecticut, R/V Argo Maine, and F/V Barbara L. Peters. We thank Mooring Systems, Inc., Ocean Data Technologies, Inc., D. Dooner, J. Brown, C. Faulkner, S. Aubrey, J. Wallinga, J. James, D. Percy, B. White, E. Ward and C. White for assistance with mooring design, fabrication and/or at-sea operations. Special thanks to J. Wood for preparation of Aquadopp current meters and data analysis, to D. Handy for providing WHOI dockside operation assistance, to J. Trowbridge and G. Parker for the Rouse model calculations, and to S. Manganini for helping with just about everything. Primary credit for motivating us to examine deep-water cysts fluxes in the Gulf of Maine goes to the late Maureen Keller, a great friend and colleague. We thank two anonymous reviewers for their comments and suggestions which greatly improved the manuscript. This work was supported by NOAA Grant nos. NA04NOS4780274 (ECOHAB-GOM/Cyst) and NA06NOS4780245 (GOMTOX), as well as by research support provided through the Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF) Grant nos. OCE-0430724, and OCE-0911031; and National Institute of Environmental Health Sciences (NIEHS) Grant no. 1-P50-ES012742-01.	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Part II-Top. Stud. Oceanogr.	MAY	2014	103						40	54		10.1016/j.dsr2.2012.11.001	http://dx.doi.org/10.1016/j.dsr2.2012.11.001			15	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	25431527	Green Accepted			2025-03-11	WOS:000338810600004
J	Pilskaln, CH; Hayashi, K; Keafer, BA; Anderson, DM; McGillicuddy, DJ				Pilskaln, C. H.; Hayashi, K.; Keafer, B. A.; Anderson, D. M.; McGillicuddy, D. J., Jr.			Benthic nepheloid layers in the Gulf of Maine and <i>Alexandrium</i> cyst inventories	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Benthic nepheloid layer; Suspended particulate matter; Gulf of Maine; Alexandrium fundyense; Cysts	BOTTOM BOUNDARY-LAYER; SANTA-CATALINA BASIN; CONTINENTAL-SHELF; GEORGES-BANK; SEDIMENT RESUSPENSION; HYDROGRAPHIC STRUCTURE; FUNDYENSE CYSTS; WILKINSON BASIN; COASTAL CURRENT; NEAR-BOTTOM	Cysts residing in benthic nepheloid layers (BNLs) documented in the Gulf of Maine have been proposed as a possible source of inoculum for annual blooms of a toxic dinoflagellate in the region. Herein we present a spatially extensive data set of the distribution and thickness of benthic nepheloid layers in the Gulf of Maine and the abundance and inventories of suspended Alexandrium fundyense cysts within these near-bottom layers. BNLs are pervasive throughout the gulf and adjacent Bay of Fundy with maximum layer thicknesses of 50-60 m observed. Mean BNL thickness is 30 m in the eastern gulf and Bay of Fundy, and 20 m in the western gulf. Cyst densities in the near-bottom particle resuspension layers varied by three orders of magnitude across the gulf with maxima of 10(5) cysts m(-3). An important interconnection of elevated BNL cyst densities is observed between the Bay of Fundy, the Maine Coastal Current and the south-central region of the gulf. BNL cyst inventories estimated for the eastern and western gulf are each on the order of 10(15) cysts, whereas the BNL inventory in the Bay of Fundy is on the order of 10(16). Although BNL cyst inventories in the eastern and western gulf are 1-2 orders of magnitude smaller than the abundance of cysts in the upper 1 cm of sediment in those regions, BNL and sediment-bound cyst inventories are comparable in the Bay of Fundy. The existence of widespread BNLs containing substantial cyst inventories indicates that these near-bottom layers represent an important source of germinating A. fundyense cysts in the region. (C) 2013 Elsevier Ltd. All rights reserved.	[Pilskaln, C. H.; Hayashi, K.] Univ Massachusetts Dartmouth, Sch Marine Sci & Technol, New Bedford, MA 02744 USA; [Keafer, B. A.; Anderson, D. M.; McGillicuddy, D. J., Jr.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	University of Massachusetts System; University Massachusetts Dartmouth; Woods Hole Oceanographic Institution	Pilskaln, CH (通讯作者)，Univ Massachusetts Dartmouth, Sch Marine Sci & Technol, New Bedford, MA 02744 USA.	cpilskaln@umassd.edu		McGillicuddy, Dennis/0000-0002-1437-2425	NOAA [NA04NOS4780274, NA06NOS4780245]; Woods Hole Center for Oceans and Human Health through National Science Foundation [OCE-0430724, OCE-0911031, OCE-1314642]; National Institute of Environmental Health Sciences [1P50-ES01274201, 1P01ES021923-01]; Division Of Ocean Sciences; Directorate For Geosciences [1314642] Funding Source: National Science Foundation	NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); Woods Hole Center for Oceans and Human Health through 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)); Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We are extremely grateful to Captain D. Ogus and the crew of the R/V Cape Hatteras for making the October 2004 cruise a success (and for tolerating our World Series obsession), and we thank J. Brown, C. Falkner, S. McQuilken, K. Norton and B. Tupper for assistance at sea and/or in the laboratory. R. Signell provided Gulf of Maine bathymetry and V. Kosnyrev assisted in the graphics production. This work was supported by NOAA Grants NA04NOS4780274 (ECOHAB-GOM/Cyst) and NA06NOS4780245 (GOMTOX). Additional support for DMA and DJM was provided by the Woods Hole Center for Oceans and Human Health through National Science Foundation Grants OCE-0430724 and OCE-0911031 and OCE-1314642 and National Institute of Environmental Health Sciences Grants 1P50-ES01274201 and 1P01ES021923-01. This is the Ecology and Oceanography of Harmful Algal Blooms Program contribution number XXXX.	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Part II-Top. Stud. Oceanogr.	MAY	2014	103						55	65		10.1016/j.dsr2.2013.05.021	http://dx.doi.org/10.1016/j.dsr2.2013.05.021			11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	25419055	Green Accepted			2025-03-11	WOS:000338810600005
J	Butman, B; Aretxabaleta, AL; Dickhudt, PJ; Dalyander, PS; Sherwood, CR; Anderson, DM; Keafer, BA; Signell, RP				Butman, Bradford; Aretxabaleta, Alfredo L.; Dickhudt, Patrick J.; Dalyander, P. Soupy; Sherwood, Christopher R.; Anderson, Donald M.; Keafer, Bruce A.; Signell, Richard P.			Investigating the importance of sediment resuspension in <i>Alexandrium fundyense</i> cyst population dynamics in the Gulf of Maine	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Sediment transport; Bottom stress; Sediment resuspension; Harmful algal blooms; Gulf of Maine; Alexandrium fundyense; HAB	PHYSICAL-BIOLOGICAL MODEL; GONYAULAX-TAMARENSIS; WESTERN GULF; DINOFLAGELLATE CYSTS; SETTLING VELOCITY; MASSACHUSETTS BAY; CONTINENTAL-SHELF; TRANSPORT; BLOOMS; GERMINATION	Cysts of Alexandrium fundyense, a dinoflagellate that causes toxic algal blooms in the Gulf of Maine, spend the winter as dormant cells in the upper layer of bottom sediment or the bottom nepheloid layer and germinate in spring to initiate new blooms. Erosion measurements were made on sediment cores collected at seven stations in the Gulf of Maine in the autumn of 2011 to explore if resuspension (by waves and currents) could change the distribution of over-wintering cysts from patterns observed in the previous autumn; or if resuspension could contribute cysts to the water column during spring when cysts are viable. The mass of sediment eroded from the core surface at 0.4 Pa ranged from 0.05 kg m(-2) near Grand Manan Island, to 0.35 kg m(-2) in northern Wilkinson Basin. The depth of sediment eroded ranged from about 0.05 mm at a station with sandy sediment at 70 m water depth on the western Maine shelf, to about 1.2 mm in clayey-silt sediment at 250 m water depth in northern Wilkinson Basin. The sediment erodibility measurements were used in a sediment-transport model forced with modeled waves and currents for the period October 1, 2010 to May 31, 2011 to predict resuspension and bed erosion. The simulated spatial distribution and variation of bottom shear stress was controlled by the strength of the semi-diurnal tidal currents, which decrease from east to west along the Maine coast, and oscillatory wave-induced currents, which are strongest in shallow water. Simulations showed occasional sediment resuspension along the central and western Maine coast associated with storms, steady resuspension on the eastern Maine shelf and in the Bay of Fundy associated with tidal currents, no resuspension in northern Wilkinson Basin, and very small resuspension in western Jordan Basin. The sediment response in the model depended primarily on the profile of sediment erodibility, strength and time history of bottom stress, consolidation time scale, and the current in the water column. Based on analysis of wave data from offshore buoys from 1996 to 2012, the number of wave events inducing a bottom shear stress large enough to resuspend sediment at 80 m ranged from 0 to 2 in spring (April and May) and 0 to 10 in winter (October through March). Wave-induced resuspension is unlikely in water greater than about 100 m deep. The observations and model results suggest that a millimeter or so of sediment and associated cysts may be mobilized in both winter and spring, and that the frequency of resuspension will vary interannually. Depending on cyst concentration in the sediment and the vertical distribution in the water column, these events could result in a concentration in the water column of at least 10(4) cysts m(-3). In some years, resuspension events could episodically introduce cysts into the water column in spring, where germination is likely to be facilitated at the time of bloom formation. An assessment of the quantitative effects of cyst resuspension on bloom dynamics in any particular year requires more detailed investigation. Published by Elsevier Ltd.	[Butman, Bradford; Aretxabaleta, Alfredo L.; Dickhudt, Patrick J.; Dalyander, P. Soupy; Sherwood, Christopher R.; Signell, Richard P.] US Geol Survey, Woods Hole, MA 02543 USA; [Aretxabaleta, Alfredo L.] Integrated Stat, Woods Hole, MA 02543 USA; [Anderson, Donald M.; Keafer, Bruce A.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	United States Department of the Interior; United States Geological Survey; Woods Hole Oceanographic Institution	Butman, B (通讯作者)，US Geol Survey, 384 Woods Hole Rd, Woods Hole, MA 02543 USA.	bbutman@usgs.gov	Dalyander, Soupy/E-9830-2013; Aretxabaleta, Alfredo/H-6566-2019	Signell, Richard/0000-0003-0682-9613; Dalyander, P. Soupy/0000-0001-9583-0872; Aretxabaleta, Alfredo/0000-0002-9914-8018	Woods Hole Center for Oceans and Human Health; National Science Foundation [OCE-0430724, OCE-0911031]; National Institute of Environmental Health Sciences [1-P50-ES012742-01]; ECOHAB Grant program through NOAA [NA06NOS4780245, A09NOS4780193]; MERHAB Grant program through NOAA [NA11NOS4780025]; PCMHAB Grant program through NOAA [NA11NOS4780023]; U.S. Geological Survey	Woods Hole Center for Oceans and Human Health; National Science Foundation(National Science Foundation (NSF)); 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)); ECOHAB Grant program through NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); MERHAB Grant program through NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); PCMHAB Grant program through NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); U.S. Geological Survey(United States Geological Survey)	We thank the officers and crews of RV Endeavor and Oceanus for skillful assistance in sediment sampling operations. Jon Borden, Sandy Baldwin, and Kate McMullen (USGS) assisted in core collection and sample processing at sea, and Kate McMullen did all the sediment texture analysis. Kerry Norton (WHOI) assisted in collection of the Craib cores and counted the UGEMS samples for cyst concentrations. Sean Lucey, NOAA Northeast Fisheries Science Center Ecosystem Assessment Program, provided the SASI bottom trawling estimates. Changsheng Chen (UMASS Dartmouth) ran the FVCOM forecasts that are provided online at the archive http://www.smast.umassd.edu:8080/thredds/archives.html. Three anonymous reviewers and Page Valentine provided very thorough and helpful reviews of the manuscript. D. Shull provided insight and additional runs of a sediment bed model to help clarify the role of mixing. C. Pilskaln provided a helpful review and insight on sediment trap results. D. McGillicuddy provided several careful and constructive reviews. Research support to Donald M. Anderson and Bruce A. Keafer provided through the Woods Hole Center for Oceans and Human Health; National Science Foundation Grants OCE-0430724 and OCE-0911031; and National Institute of Environmental Health Sciences Grant 1-P50-ES012742-01; the ECOHAB Grant program through NOAA Grants NA06NOS4780245 and A09NOS4780193; the MERHAB Grant program through NOAA Grant NA11NOS4780025; and the PCMHAB Grant program through NOAA Grant NA11NOS4780023. This is ECOHAB contribution 746, MERHAB contribution 169, and PCMHAB contribution 8. Research support to all other authors was provided by U.S. Geological Survey.	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Part II-Top. Stud. Oceanogr.	MAY	2014	103						79	95		10.1016/j.dsr2.2013.10.011	http://dx.doi.org/10.1016/j.dsr2.2013.10.011			17	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	25288829	hybrid, Green Accepted, Green Published			2025-03-11	WOS:000338810600007
J	Vahtera, E; Crespo, BG; McGillicuddy, DJ; Olli, K; Anderson, DM				Vahtera, Emil; Crespo, Bibiana G.; McGillicuddy, Dennis J., Jr.; Olli, Kalle; Anderson, Donald M.			<i>Alexandrium fundyense</i> cyst viability and germling survival in light vs. dark at a constant low temperature	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Dinoflagellate; Alexandrium fundyense; Cysts; Excystment; Planomeiocyte; Germling; Dark survival; Gulf of Maine	PHYSICAL-BIOLOGICAL MODEL; RESTING CYSTS; DINOFLAGELLATE CYSTS; GONYAULAX-TAMARENSIS; MAINE; GULF; GERMINATION; DINOPHYCEAE; BLOOM; PHYTOPLANKTON	Both observations and models suggest that large-scale coastal blooms of Alexandrium fundyense in the Gulf of Maine are seeded by deep-bottom cyst accumulation zones ("seed beds") where cysts germinate from the sediment surface or the overlying near-bottom nepheloid layers at water depths exceeding 100 m. The germling cells and their vegetative progeny are assumed to be subject to mortality while in complete darkness, as they swim to illuminated surface waters. To test the validity of this assumption we conducted laboratory investigations of cyst viability and the survival of the germling cells and their vegetative progeny during prolonged exposure to darkness at a temperature of 6 degrees C, simulating the conditions in deep Gulf of Maine waters. We isolated cysts from bottom sediments collected in the Gulf of Maine under low red light and incubated them in 96-well tissue culture-plates in culture medium under a 10:14 h light:dark cycle and under complete darkness. Cyst viability was high, with excystment frequency reaching 90% in the illuminated treatment after 30 days and in the dark treatment after 50 days. Average germination rates were 0.062 and 0.038 d(-1) for light and dark treatments, respectively. The dark treatment showed an approximately 2-week time lag in maximum germination rates compared to the light treatment. Survival of germlings was considerably lower in the dark treatment. In the light treatments, 47% of germinated cysts produced germlings that were able to survive for 7 days and produce vegetative progeny, i.e., there were live cells in the well along with an empty cyst at least once during the experiment. In the dark treatments 12% of the cysts produced germlings that were able to survive for the same length of time. When dark treatments are scaled to take into account non-darkness related mortality, approximately 28% of the cysts produced germlings that were able to survive for at least 7 days. Even though cysts are able to germinate in darkness, the lack of illumination considerably reduces survival rate of germling cells. In addition to viability of cysts in surface sediments and the near-bottom nepheloid layer, survivability of germling cells and their vegetative progeny at aphotic depths is an important consideration in assessing the quantitative role of deep-coastal cyst seed beds in bloom formation. (C) 2013 Elsevier Ltd. All rights reserved.	[Vahtera, Emil; Crespo, Bibiana G.; McGillicuddy, Dennis J., Jr.; Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Olli, Kalle] Univ Tartu, Inst Ecol & Earth Sci, EE-51005 Tartu, Estonia	Woods Hole Oceanographic Institution; University of Tartu; Tartu University Institute of Ecology & Earth Sciences	Vahtera, E (通讯作者)，City Helsinki Environm Ctr, POB 500, FIN-00099 Helsinki, Finland.	emil.vahtera@hel.fi	Olli, Kalle/G-5389-2010	McGillicuddy, Dennis/0000-0002-1437-2425; Nyman, Emil/0009-0006-4201-7750	Academy of Finland [130934]; Xunta de Galicia Angeles Alvarino fellowship; National Oceanic Atmospheric Administration ECOHAB program [NA06NOS4780245, NA09NOS4780193]; National Science Foundation [OCE-0430724, OCE-0911031, OCE-1314642]; National Institute of Environmental Health Sciences through the Woods Hole Center for Oceans and Human Health [1P50-ES01274201, 1P01ES021923-01]; Directorate For Geosciences; Division Of Ocean Sciences [1128041, 1314642] Funding Source: National Science Foundation; Academy of Finland (AKA) [130934] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); Xunta de Galicia Angeles Alvarino fellowship; National Oceanic Atmospheric Administration ECOHAB program(National Oceanic Atmospheric Admin (NOAA) - USA); National Science Foundation(National Science Foundation (NSF)); National Institute of Environmental Health Sciences through the Woods Hole Center for Oceans and Human Health; Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO)); Academy of Finland (AKA)(Research Council of Finland)	E. Vahtera was funded by the Academy of Finland (Grant no. 130934) and B. Gomez-Crespo was supported by a Xunta de Galicia Angeles Alvarino fellowship. Additional funding support was also provided by the National Oceanic Atmospheric Administration ECOHAB program through grants NA06NOS4780245 and NA09NOS4780193, and from National Science Foundation grants OCE-0430724, OCE-0911031, OCE-1314642 and National Institute of Environmental Health Sciences grants 1P50-ES01274201 and 1P01ES021923-01 through the Woods Hole Center for Oceans and Human Health. We are also grateful for technical assistance from Z. Bonin, B. Keafer, K. Smith, and D. Kulis. R. He, and Y. Li are acknowledged for their valuable comments on the manuscript. This is ECOHAB contribution number 734.	Anderson D.M., 1985, P219; Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; Anderson DM, 2014, DEEP-SEA RES PT II, V103, P6, DOI 10.1016/j.dsr2.2013.10.002; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BAUERFEIND E, 1986, MAR BIOL, V93, P323, DOI 10.1007/BF00401099; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CRAIB J. 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Part II-Top. Stud. Oceanogr.	MAY	2014	103						112	119		10.1016/j.dsr2.2013.05.010	http://dx.doi.org/10.1016/j.dsr2.2013.05.010			8	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	25076814	Green Accepted, Green Published, Green Submitted			2025-03-11	WOS:000338810600009
J	McGillicuddy, DJ; Brosnahan, ML; Couture, DA; He, R; Keafer, BA; Manning, JP; Martin, JL; Pilskaln, CH; Townsend, DW; Anderson, DM				McGillicuddy, D. J., Jr.; Brosnahan, M. L.; Couture, D. A.; He, R.; Keafer, B. A.; Manning, J. P.; Martin, J. L.; Pilskaln, C. H.; Townsend, D. W.; Anderson, D. M.			A red tide of <i>Alexandrium fundyense</i> in the Gulf of Maine	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Phytoplankton; Population dynamics; Red tides; Cysts; Paralytic shellfish poisoning; USA; Gulf of Maine	DINOFLAGELLATE GONYAULAX-EXCAVATA; PHYSICAL-BIOLOGICAL MODEL; WESTERN GULF; ALGAL BLOOMS; CELL-CYCLE; TAMARENSE; PHYTOPLANKTON; CYSTS; BIOGEOGRAPHY; HYPOTHESES	In early July 2009, an unusually high concentration of the toxic dinoflagellate Alexandrium fundyense occurred in the western Gulf of Maine, causing surface waters to appear reddish brown to the human eye. The discolored water appeared to be the southern terminus of a large-scale event that caused shellfish toxicity along the entire coast of Maine to the Canadian border. Rapid-response shipboard sampling efforts together with satellite data suggest the water discoloration in the western Gulf of Maine was a highly ephemeral feature of less than two weeks in duration. Flow cytometric analysis of surface samples from the red water indicated the population was undergoing sexual reproduction. Cyst fluxes downstream of the discolored water were the highest ever measured in the Gulf of Maine, and a large deposit of new cysts was observed that fall. Although the mechanisms causing this event remain unknown, its timing coincided with an anomalous period of downwelling-favorable winds that could have played a role in aggregating upward-swimming cells. Regardless of the underlying causes, this event highlights the importance of short-term episodic phenomena on regional population dynamics of A. fundyense. (C) 2013 Elsevier Ltd. All rights reserved.	[McGillicuddy, D. J., Jr.] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA; [Brosnahan, M. L.; Keafer, B. A.; Anderson, D. M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Couture, D. A.] Resource Access Int, Brunswick, ME 04011 USA; [He, R.] N Carolina State Univ, Dept Maine Earth & Atmospher Sci, Raleigh, NC 27695 USA; [Manning, J. P.] NOAA, Northeast Fisheries Sci Ctr, Woods Hole, MA 02543 USA; [Martin, J. L.] Fisheries & Oceans Canada, St Andrews Biol Stn, St Andrews, NB E5B 2L9, Canada; [Pilskaln, C. H.] Univ Massachusetts Dartmouth, Sch Marine Sci, N Dartmouth, MA 02747 USA; [Townsend, D. W.] Univ Maine, Sch Marine Sci, Orono, ME 04469 USA	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; North Carolina State University; National Oceanic Atmospheric Admin (NOAA) - USA; Fisheries & Oceans Canada; University of Massachusetts System; University Massachusetts Dartmouth; University of Maine System; University of Maine Orono	McGillicuddy, DJ (通讯作者)，Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA.	dmcgillicuddy@whoi.edu	Martin, Jennifer/G-5217-2011; He, Ruoying/C-5598-2015	He, Ruoying/0000-0001-6158-2292; McGillicuddy, Dennis/0000-0002-1437-2425; Brosnahan, Michael/0000-0002-2620-7638	National Oceanic Atmospheric Administration (NOAA), National Ocean Service, Center through NOAA [NA17RJ1223]; NOAA [NA06NOS4780245]; Woods Hole Center for Oceans and Human Health through National Science Foundation [OCE-0430724, OCE-0911031, OCE-1314642]; National Institute of Environmental Health Sciences [1P50-ES01274201, 1P01ES021923-01]; Ecology and Oceanography of Harmful Algal Blooms Program [738]; Directorate For Geosciences; Division Of Ocean Sciences [1314642] Funding Source: National Science Foundation	National Oceanic Atmospheric Administration (NOAA), National Ocean Service, Center through NOAA; NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); Woods Hole Center for Oceans and Human Health through 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)); Ecology and Oceanography of Harmful Algal Blooms Program; Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	The R/V Tioga sampling effort was facilitated by event response funding from the National Oceanic Atmospheric Administration (NOAA), National Ocean Service, Center for Sponsored Coastal Ocean Research, through NOAA Cooperative Agreement NA17RJ1223. Additional support for follow-up analysis and synthesis was provided by NOAA grant NA06NOS4780245 for the Gulf of Maine Toxicity (GOMTOX) program and the Woods Hole Center for Oceans and Human Health through National Science Foundation grants OCE-0430724, OCE-0911031, and OCE-1314642, and National Institute of Environmental Health Sciences grants 1P50-ES01274201 and 1P01ES021923-01. This is the Ecology and Oceanography of Harmful Algal Blooms Program contribution number 738.	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J	Brosnahan, ML; Farzan, S; Keafer, BA; Sosik, HM; Olson, RJ; Anderson, DM				Brosnahan, Michael L.; Farzan, Shahla; Keafer, Bruce A.; Sosik, Heidi M.; Olson, Robert J.; Anderson, Donald M.			Complexities of bloom dynamics in the toxic dinoflagellate <i>Alexandrium fundyense</i> revealed through DNA measurements by. imaging flow cytometry coupled with species-specific rRNA probes	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium fundyense; A. tamarense Group I; Algal bloom dynamics; Imaging flow cytometry; Microalgal life cycles	GONYAULAX-TAMARENSIS LEBOUR; CELL-CYCLE; CYST FORMATION; CAPE-COD; DINOPHYCEAE; MAINE; GULF; IDENTIFICATION; BIOGEOGRAPHY; TEMPERATURE	Measurements of the DNA content of different protist populations can shed light on a variety of processes, including cell division, sex, prey ingestion, and parasite invasion. Here, we modified an Imaging FlowCytobot (IFCB), a custom-built flow cytometer that records images of microplankton, to measure the DNA content of large dinoflagellates and other high-DNA content species. The IFCB was also configured to measure fluorescence from Cy3-labeled rRNA probes, aiding the identification of Alexandrium fundyense (syn. A. tamarense Group I), a photosynthetic dinoflagellate that causes paralytic shellfish poisoning (PSP). The modified IFCB was used to analyze samples from the development, peak and termination phases of an inshore A. fundyense bloom (Salt Pond, Eastham, MA, USA), and from a rare A. fimdyense 'red tide' that occurred in the western Gulf of Maine, offshore of Portsmouth, NH (USA). Diploid or G2 phase ('2C') A. fundyense cells were frequently enriched at the near-surface, suggesting an important role for aggregation at the air-sea interface during sexual events. Also, our analysis showed that large proportions of A. fundyense cells in both the Salt Pond and red tide blooms were planozygotes during bloom decline, highlighting the importance of sexual fusion to bloom termination. At Salt Pond, bloom decline also coincided with a dramatic rise in infections by the parasite genus Amoebophrya. The samples that were most heavily infected contained many large cells with higher DNA-associated fluorescence than 2C vegetative cells, but these cells' nuclei were also frequently consumed by Amoebophrya trophonts. Neither large cell size nor increased DNA-associated fluorescence could be replicated by infecting an A. fundyense culture of vegetative cells. Therefore, we attribute these characteristics of the large Salt Pond cells to planozygote maturation rather than Amoebopluya infection, though an interaction between infection and planozygote maturation may also have contributed. The modified IFCB is a valuable tool for exploring the conditions that promote sexual transitions by dinoflagellate blooms but care is needed when interpreting results from samples in which parasitism is prevalent. (C) 2013 Elsevier Ltd. All rights reserved.	[Brosnahan, Michael L.; Keafer, Bruce A.; Sosik, Heidi M.; Olson, Robert J.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Farzan, Shahla] Univ Calif Davis, Dept Entomol, Davis, CA 95616 USA	Woods Hole Oceanographic Institution; University of California System; University of California Davis	Brosnahan, ML (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	mbrosnahan@whoi.edu		Brosnahan, Michael/0000-0002-2620-7638; Sosik, Heidi/0000-0002-4591-2842	NSF [OCE-0430724, OCE-0911031, OCE-0525700, OCE-1130140]; NIEHS through the Woods Hole Center for Oceans and Human Health, National Park Service [1P50-ES01274201, 1P01ES021923, H238015504]; EPA STAR [FP-91688601]; ONR [N00014-08-11044]; NOAA [NANOS4191149, NA09NOS4780210]; NASA [NNX11AF07G]; Gordon and Betty Moore Foundation [934, 2649]; Directorate For Geosciences; Division Of Ocean Sciences [1128041] Funding Source: National Science Foundation; NASA [147316, NNX11AF07G] Funding Source: Federal RePORTER	NSF(National Science Foundation (NSF)); NIEHS through the Woods Hole Center for Oceans and Human Health, National Park Service; EPA STAR(United States Environmental Protection Agency); ONR(United States Department of DefenseUnited States NavyOffice of Naval Research); NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); NASA(National Aeronautics & Space Administration (NASA)); Gordon and Betty Moore Foundation(Gordon and Betty Moore Foundation); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO)); NASA(National Aeronautics & Space Administration (NASA))	We are grateful to B. Crespo, K. Norton, and many other members of the Anderson lab for their contributions to the NMS surveys, to D. Kulis and M. Sengco (US EPA) for their guidance in the rearing of Amoebophrya, to the crews of the R/V Gulf Challenger and the R/V Tioga for their work during the WGOM red tide and event response, to D. McGillicuddy and D. Ralston for helpful discussions, and to two anonymous reviewers for valuable input. This work was supported by NSF grants OCE-0430724 and OCE-0911031 and NIEHS grants 1P50-ES01274201 and 1P01ES021923 to D.M.A. through the Woods Hole Center for Oceans and Human Health, National Park Service Cooperative Agreement H238015504 with D.M.A., by an EPA STAR graduate fellowship (No. FP-91688601) to M.L.B., and by grants from NSF (OCE-0525700 and OCE-1130140), ONR (N00014-08-11044), NOAA (NANOS4191149 and NA09NOS4780210), NASA (NNX11AF07G), and the Gordon and Betty Moore Foundation (934 and 2649) to R.J.O. and H.M.S. This is ECOHAB contribution 733.	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Part II-Top. Stud. Oceanogr.	MAY	2014	103						185	198		10.1016/j.dsr2.2013.05.034	http://dx.doi.org/10.1016/j.dsr2.2013.05.034			14	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	24891769	Green Accepted			2025-03-11	WOS:000338810600014
J	Anderson, DM; Couture, DA; Kleindinst, JL; Keafer, BA; McGillicuddy, DJ; Martin, JL; Richlen, ML; Hickey, JM; Solow, AR				Anderson, Donald M.; Couture, Darcie A.; Kleindinst, Judith L.; Keafer, Bruce A.; McGillicuddy, Dennis J., Jr.; Martin, Jennifer L.; Richlen, Mindy L.; Hickey, J. Michael; Solow, Andrew R.			Understanding interannual, decadal level variability in paralytic shellfish poisoning toxicity in the Gulf of Maine: The HAB Index	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium fundyense; Harmful algal blooms; HABs; PSP; HAB Index	RED-TIDE DINOFLAGELLATE; ALEXANDRIUM-FUNDYENSE POPULATIONS; GONYAULAX-EXCAVATA; WESTERN GULF; RESTING CYSTS; PUGET-SOUND; NEW-ENGLAND; BLOOMS; DYNAMICS; HYPOTHESES	A major goal in harmful algal bloom (HAB) research has been to identify mechanisms underlying interannual variability in bloom magnitude and impact. Here the focus is on variability in Alexandrium fundyense blooms and paralytic shellfish poisoning (PSP) toxicity in Maine, USA, over 34 years (1978-2011). The Maine coastline was divided into two regions - eastern and western Maine, and within those two regions, three measures of PSP toxicity (the percent of stations showing detectable toxicity over the year, the cumulative amount of toxicity per station measured in all shellfish (mussel) samples during that year, and the duration of measurable toxicity) were examined for each year in the time series. These metrics were combined into a simple HAB Index that provides a single measure of annual toxin severity across each region. The three toxin metrics, as well as the HAB Index that integrates them, reveal significant variability in overall toxicity between individual years as well as long-term, decadal patterns or regimes. Based on different conceptual models of the system, we considered three trend formulations to characterize the long-term patterns in the Index - a three-phase (mean-shift) model, a linear two-phase model, and a pulse-decline model. The first represents a "regime shift" or multiple equilibria formulation as might occur with alternating periods of sustained high and low cyst abundance or favorable and unfavorable growth conditions, the second depicts a scenario of more gradual transitions in cyst abundance or growth conditions of vegetative cells, and the third characterizes a "sawtooth" pattern in which upward shifts in toxicity are associated with major cyst recruitment events, followed by a gradual but continuous decline until the next pulse. The fitted models were compared using both residual sum of squares and Akaike's Information Criterion. There were some differences between model fits, but none consistently gave a better fit than the others. This statistical underpinning can guide efforts to identify physical and/or biological mechanisms underlying the patterns revealed by the HAB Index. Although A. fundyense cyst survey data (limited to 9 years) do not span the entire interval of the shellfish toxicity records, this analysis leads us to hypothesize that major changes in the abundance of A. fundyense cysts may be a primary factor contributing to the decadal trends in shellfish toxicity in this region. The HAB Index approach taken here is simple but represents a novel and potentially useful tool for resource managers in many areas of the world subject to toxic HABs. (C) 2013 Elsevier Ltd. All rights reserved.	[Anderson, Donald M.; Kleindinst, Judith L.; Keafer, Bruce A.; McGillicuddy, Dennis J., Jr.; Richlen, Mindy L.; Solow, Andrew R.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Couture, Darcie A.] Maine Dept Marine Resources, West Boothbay Harbor, ME 04605 USA; [Martin, Jennifer L.] Fisheries & Oceans Canada, Biol Stn, St Andrews, NB E5B 2L9, Canada; [Hickey, J. Michael] Massachusetts Div Marine Fisheries, New Bedford, MA USA	Woods Hole Oceanographic Institution; Fisheries & Oceans Canada; Massachusetts Division of Marine Fisheries	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	danderson@whoi.edu; Darcie.Couture@att.net; Jennifer.Martin@dfo-mpo.gc.ca; michael.hickey@state.ma.us	Martin, Jennifer/G-5217-2011	McGillicuddy, Dennis/0000-0002-1437-2425	Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF) [OCE-1128041, OCE-1314642]; National Institute of Environmental Health Sciences (NIEHS) [1-P50-ES021923-01]; ECOHAB Grant program through NOAA [NA06NOS4780245, NA09NOS4780193]; MERHAB Grant program through NOAA [NA11NOS4780025]; PCMHAB Grant program through NOAA [NA11NOS4780023]; state of ME; state of NH; state of MA; Fisheries and Oceans Canada; Division Of Ocean Sciences; Directorate For Geosciences [1314642] Funding Source: National Science Foundation	Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF)(National Science Foundation (NSF)); 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)); ECOHAB Grant program through NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); MERHAB Grant program through NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); PCMHAB Grant program through NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); state of ME; state of NH; state of MA; Fisheries and Oceans Canada; Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	Research support provided through the Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF) Grants OCE-1128041 and OCE-1314642; and National Institute of Environmental Health Sciences (NIEHS) Grant 1-P50-ES021923-01, the ECOHAB Grant program through NOAA Grants NA06NOS4780245 and NA09NOS4780193, the MERHAB Grant program through NOAA Grant NA11NOS4780025, the PCMHAB Grant program through NOAA Grant NA11NOS4780023, and funding through the states of ME, NH, and MA. Funding for J.L Martin was provided by Fisheries and Oceans Canada. This is ECOHAB contribution #735; MERHAB contribution #168; PCMHAB contribution #7.	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Part II-Top. Stud. Oceanogr.	MAY	2014	103						264	276		10.1016/j.dsr2.2013.09.018	http://dx.doi.org/10.1016/j.dsr2.2013.09.018			13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	24948849	Green Accepted, Green Submitted			2025-03-11	WOS:000338810600019
J	Beiranvand, B; Zaghbib-Turki, D; Ghasemi-Nejad, E				Beiranvand, Bijan; Zaghbib-Turki, Dalila; Ghasemi-Nejad, Ebrahim			Integrated biostratigraphy based on planktonic foraminifera and dinoflagellates across the Cretaceous/Paleogene (K/Pg) transition at the Izeh section (SW Iran)	COMPTES RENDUS PALEVOL			English	Article						K/Pg boundary; Biostratigraphy; Planktonic foraminiferal biozonation; Dinocyst events; Izeh section; Zagros Basin; Iran	K-T BOUNDARY; DANIAN STAGE PALEOCENE; KRISHNA-GODAVARI BASIN; TERTIARY BOUNDARY; EL-KEF; CALCAREOUS NANNOFOSSIL; BENTHIC FORAMINIFERA; CHICXULUB IMPACT; CRETACEOUS/TERTIARY BOUNDARY; STRATOTYPE SECTION	The present work is based on semi-quantitative study carried on detailed sampling (samples are spaced by 5, 10 and 15 cm close to the boundary) of an essentially continuous and expanded section crossing the Cretaceous-Paleogene (K/Pg) boundary in Iran. By this work, we attempt to detail biostratigraphy based on planktonic foraminifera biozones and correlate biozones and subzones with dinocyst events. The entire Cretaceous-Paleogene interval contains rich, diversified and well-preserved planktonic foraminifera and dinoflagellate cyst assemblages. Four planktonic foraminiferal biozones have been recognized across the Cretaceous-Paleogene transition (K/Pg): Abathomphalus mayaroensis Biozone including Plummerita hantkeninoides Subzone from the Late Maastrichtian and Guembelitria cretacea (including Hedbergella holmdelensis and Parvularugoglobigerina longiapertura subzones), Parvularugoglobigerina eugubina Biozone and Parasubbotina pseudobulloides Biozone belonging to the Early Danian. These biozones have been correlated with four dinocyst biozones: the Manumiella seelandica Biozone belonging to the Late Maastrichtian and the Alisocysta reticulata, Senoniasphaera inornata and Damassadinium californicum biozones from the Early Danian. At this section, like at the El Kef section (GSSP for the K/Pg) and the auxiliary sections, an Ir anomaly is detected indicating the K/Pg boundary. This geochemical anomaly coincides also with mass extinctions of planktonic foraminifera species. The extinct species are in particular the large, complex tropical and subtropical taxa dwelling in subsurface and lower photic water. The mass extinctions at the Izeh section occurred over a succinct period of time similar to the K/Pg type section at El Kef (Tunisia). These sudden mass extinctions indicate a catastrophic pattern event occurring at the Maastrichtian/Danian boundary. In contrast the organic-walled dinocysts were less affected by the mass extinction and most species crossed the K/Pg boundary without showing mass and sudden extinctions. Nevertheless, they showed changes in their assemblages' structure beyond the K/Pg boundary. Especially, Manumiella seelandica and M. druggii, typical species of Antarctic Maastrichtian dinocysts assemblages, occur in coeval deposits at the Izeh section; they persist through the Lower Danian and, like in Tunisia (e.g., El Kef section, Elles section) show an obvious increase in relative abundance. (C) 2013 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.	[Beiranvand, Bijan] Res Inst Petr Ind, Petr Geol Dept, Explorat & Prod Div, Tehran, Iran; [Zaghbib-Turki, Dalila] Univ Tunis El Manar, Fac Sci Tunis, Tunis 2092, Tunisia; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Geol Sch, Tehran, Iran	Universite de Tunis-El-Manar; Faculte des Sciences de Tunis (FST); University of Tehran	Zaghbib-Turki, D (通讯作者)，Univ Tunis El Manar, Fac Sci Tunis, Campus Univ, Tunis 2092, Tunisia.	dalila.turki@yahoo.fr	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068	Research Institute of Petroleum Industry (RIPI)	Research Institute of Petroleum Industry (RIPI)	This work was supported by the Research Institute of Petroleum Industry (RIPI). The authors thank S.S. Hendi, head of exploration research and development Department of RIPI for sustaining the project and to E.H. Tavakoli and H. Alinaghian for processing the samples. The authors also thank Professor Mark Leckie from the University of Massachusetts Amherst and Associate Professor Edouardo Koutsoukos from the University of Heidelberg and the other anonym reviewers for their acceptance to review our manuscript and for their interesting suggestions and comments that led to improve the earliest version. They are especially grateful to Professor Leckie who also made linguistic corrections.	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R. Palevol	MAY-JUN	2014	13	4					235	258		10.1016/j.crpv.2013.10.003	http://dx.doi.org/10.1016/j.crpv.2013.10.003			24	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	AJ4OJ					2025-03-11	WOS:000337655400001
J	Kim, SY; Lim, DI				Kim, So-Young; Lim, Dhong-il			Signatures of the late Holocene Neoglacial cold event and their marine-terrestrial linkage in the northwestern Pacific margin	PROGRESS IN OCEANOGRAPHY			English	Review							EAST CHINA SEA; HIGHSTAND SYSTEMS TRACTS; LATE QUATERNARY; PALEOENVIRONMENTAL CHANGES; ENVIRONMENTAL-CHANGE; OKINAWA TROUGH; YELLOW SEA; PLANKTONIC-FORAMINIFERA; CONTINENTAL-SHELF; KUROSHIO CURRENT	Marine microfossil assemblages in core sediments from the northern East China Sea (ECS) were investigated to understand late Holocene paleoclimatic changes in the northwestern Pacific margin. We find a pronounced alternation of ocean condition during the late Holocene characterized by an abrupt decrease in dinoflagellate cysts and Kuroshio water species of planktonic foraminifera centered at ca. 4000-2500 C-14 yr BP. Compilation and merger of new and previously published data show that this oceanic event corresponds with terrestrial cooling and dry episodes in the northern China. The synchronicity between marine and terrestrial records is considered to be linked to a weakened Kuroshio influence that is in coupled with intensified winter monsoon, highlighting a significance of oceanic-atmospheric dynamics in determining moisture and heat distribution over both oceanic and terrestrial domains. Superimposed on the late Holocene, the synchronicity between this particular climatic shift in the northwestern Pacific and the Neoglacial cold events in the northern high-latitude regions is tentatively indicative of a global climate signal, possibly associated with dynamics of the North Pacific gyre system and the high latitude North Atlantic thermohaline circulation, and therefore positions of the mean latitude of the Kuroshio extension. (C) 2014 Elsevier Ltd. All rights reserved.	[Kim, So-Young] Korea Polar Res Inst, Arctic Res Ctr, Inchon 406840, South Korea; [Lim, Dhong-il] Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656830, South Korea	Korea Polar Research Institute (KOPRI); Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST)	Lim, DI (通讯作者)，Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656830, South Korea.	oceanlim@kiost.ac	Kim, So-Young/JFS-7698-2023; Lim, Dhongil/ACH-3964-2022	Lim, Dhongil/0000-0002-0832-2907	Korea Institute of Ocean Science and Technology (KIOST) research program [PE99233]; Korea Polar Research Institute research program [PE14062, PP13030]	Korea Institute of Ocean Science and Technology (KIOST) research program; Korea Polar Research Institute research program(Korea Polar Research Institute of Marine Research Placement (KOPRI))	This study was supported by Korea Institute of Ocean Science and Technology (KIOST) research program (Grant no. PE99233), and also partly funded by the Korea Polar Research Institute research program (Grant No. PE14062 and PP13030). We thank "Library of Marine Samples (LIMS)" in KIOST for supplying the core sediments.	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Oceanogr.	MAY	2014	124						54	65		10.1016/j.pocean.2014.03.010	http://dx.doi.org/10.1016/j.pocean.2014.03.010			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AI4ZV					2025-03-11	WOS:000336876100005
J	Pienkowski, AJ; England, JH; Furze, MFA; MacLean, B; Blasco, S				Pienkowski, Anna J.; England, John H.; Furze, Mark F. A.; MacLean, Brian; Blasco, Steve			The late Quaternary environmental evolution of marine Arctic Canada: Barrow Strait to Lancaster Sound	QUATERNARY SCIENCE REVIEWS			English	Article						Deglaciation; Late Wisconsinan; Holocene; Environmental change; Northwest Passage; Sea ice; Palaeoenvironment	QUEEN-ELIZABETH-ISLANDS; LAST GLACIAL MAXIMUM; INNUITIAN ICE-SHEET; WESTERN ROSS-SEA; DELTA-R VALUES; NORTH-AMERICA; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; FRESH-WATER; PALEOENVIRONMENTAL RECONSTRUCTIONS	A marine sediment core from the east-central Canadian Arctic Archipelago (Core 86027-154; 74 degrees 22.0'N 89 degrees 51.26'W; 329 m water depth), studied by a multiproxy approach [lithostratigraphy, biogeochemistry, micropalaeontology (dinoflagellate cysts, other non-pollen palynomorphs, benthic and planktonic foraminifera, ostracods)], and encompassing 14 AMS C-14 dates, provides valuable insights into regional deglacial to Holocene palaeoenvironments. Six palaeoenvironmental zones are recognized, based on prominent changes in the litho- and biostratigraphy. The waterlain diamicton of Zone I records immediate deglaciation, being derived from lift-off and calving of previously grounded glacial ice. Though deglacial timing is complicated by the sparsity of dating materials and the Portlandia Effect, age-depth model extrapolation places deglaciation at 11.54 cal ka BP. Zone II (11.5-11.0 cal ka BP) represents a distinct progression from initially ice-proximal to increasingly ice-distal conditions, interrupted by an interval of pervasive sea-ice (11.4-11.2 cal ka BP). Noteworthy biological activity commences in Zone III (11.0-9.7 cal ka BP) with a prominent signal of planktonic foraminifera (Neogloboquadrina pachyderma). This likely signifies penetration of deeper, Atlantic-derived water through the central Canadian Arctic Archipelago upon deglaciation, facilitated by the greater, glacioisostatically-induced water depths (+80 m), and implies separation of Laurentide and Innuitian ice sheets by similar to 11.0 cal ka BP. Zone IV (9.7-7.2 cal ka BP) records ameliorated, biologically favourable conditions with reduced seasonal sea-ice accompanied by high microfossil species diversity and the presence of subpolar taxa. Zone V (7.2-6.5 cal ka BP) signals the exclusion of Atlantic-derived water, concomitant with increasing sea-ice, simultaneously representing the termination of the dynamic deglacial to early Holocene environments (zones I-IV). Conditions similar to modern typified by uniform sediment characteristics, present-day microfossil assemblage structures, and sparse benthic foraminifera were established by 5.6 cal ka BP (Zone VI).(C) 2013 Elsevier Ltd. All rights reserved.	[Pienkowski, Anna J.] Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales; [England, John H.] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada; [Furze, Mark F. A.] MacEwan Univ, Dept Phys Sci, Edmonton, AB T5J 2P2, Canada; [MacLean, Brian; Blasco, Steve] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada	Bangor University; University of Alberta; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Pienkowski, AJ (通讯作者)，Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales.	a.pienkowski@bangor.ac.uk	Pieńkowski, Anna/AAL-1312-2020; Pienkowski, Anna/J-9339-2013	Pienkowski, Anna/0000-0002-3606-7130; Furze, Mark/0000-0003-4636-6182	NSERC Northern Chair Program	NSERC Northern Chair Program(Natural Sciences and Engineering Research Council of Canada (NSERC))	The NSERC Northern Chair Program awarded to J. England funded this research. Initial foraminiferal data from core 86027-154 were originally generated by the late Gus Vilks during the 1980's and 1990's. We wish to acknowledge Gus' contribution to the foraminiferal dataset used in this study, as well as his major contribution to the field of Arctic foraminiferal studies. We thank Kate Jarret, Bill Leblanc, and Owen Brown at the Geological Survey of Canada Atlantic for help with core sampling, and organic carbon and grain size analyses. Charlie Schweger and Harvey Friebe (University of Alberta; Department of Anthropology) kindly provided the use of their laboratory for palynological processing. We are particularly grateful to Roy Coulthard (University of Alberta) for providing guidance on calibration of post-bomb radiocarbon dates, as well as for the fruitful discussions surrounding appropriate AR values for marine mammals. We thank two anonymous reviewers for their constructive comments which improved this manuscript. David J.A. Evans and Colin Murray-Wallace are thanked for editorial handling of this manuscript.	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Sci. Rev.	MAY 1	2014	91						184	203		10.1016/j.quascirev.2013.09.025	http://dx.doi.org/10.1016/j.quascirev.2013.09.025			20	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AI4EZ					2025-03-11	WOS:000336819800013
J	Satta, CT; Anglès, S; Garcés, E; Sechi, N; Pulina, S; Padedda, BM; Stacca, D; Lugliè, A				Satta, Cecilia T.; Angles, Silvia; Garces, Esther; Sechi, Nicola; Pulina, Silvia; Padedda, Bachisio Mario; Stacca, Daniela; Luglie, Antonella			Dinoflagellate Cyst Assemblages in Surface Sediments from Three Shallow Mediterranean Lagoons (Sardinia, North Western Mediterranean Sea)	ESTUARIES AND COASTS			English	Article						Resting cysts; Eutrophication; Mediterranean Sea; Harmful algae; Alexandrium species	SP-NOV DINOPHYCEAE; MARINE-SEDIMENTS; SCRIPPSIELLA DINOPHYCEAE; ENVIRONMENTAL-FACTORS; SPATIAL-DISTRIBUTION; COASTAL WATERS; CABRAS LAGOON; RESTING CYST; ALEXANDRIUM; GULF	The present study identified and quantified dinoflagellate cysts in surface sediments from three Mediterranean lagoons. Sediment samples were recovered from 11 stations in May 2009 at Cabras Lagoon, eight stations in May 2010 at Corru S'Ittiri Lagoon, and five stations in May 2011 at Santa Giusta Lagoon. Fifty-three dinoflagellate cyst morphotypes were identified. Sixteen species are first reports for the lagoons, and two for the Mediterranean Sea. Moreover, a new Scrippsiella species was discovered in Cabras. Seven harmful algal species were identified, primarily belonging to the potentially toxic genus Alexandrium. Total cyst abundance, number of morphotypes, and assemblages varied among lagoons, and each lagoon showed a distinct morphotype composition. A degree of heterogeneity was also detected within lagoon. Cabras and Santa Giusta cyst assemblages were characterised by morphotypes belonging to the autotrophic genus Scrippsiella, whereas Corru S'Ittiri assemblages showed dominance of heterotrophic morphotypes, including Protoperidinium cf tricingulatum. Differentiation among lagoons was also evident according to environmental conditions. Salinity proved to be a fundamental variable in determining total cyst abundance, morphotype number, and composition. This study was among the first to examine dinoflagellate cyst composition in coastal lagoons, especially from the Mediterranean region, and contributed data that increased our knowledge of cyst-producing dinoflagellates in these environments.	[Satta, Cecilia T.; Sechi, Nicola; Pulina, Silvia; Padedda, Bachisio Mario; Stacca, Daniela; Luglie, Antonella] Univ Sassari, Dipartimento Sci Nat & Territorio, I-07100 Sassari, Italy; [Angles, Silvia; Garces, Esther] CSIC, Inst Ciencias Mar, E-08003 Barcelona, Spain; [Angles, Silvia] Texas A&M Univ, Dept Oceanog, College Stn, TX 77843 USA	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); Texas A&M University System; Texas A&M University College Station	Satta, CT (通讯作者)，Univ Sassari, Dipartimento Sci Nat & Territorio, Via Piandanna 4, I-07100 Sassari, Italy.	ctsatta@uniss.it	Satta, Cecilia Teodora/AAF-6417-2020; Garces, Esther/C-5701-2011; PULINA, Silvia/Q-2684-2017; Angles, Silvia/B-9469-2011; Luglie, Antonella/M-4321-2015	SATTA, Cecilia Teodora/0000-0003-0130-9432; Garces, Esther/0000-0002-2712-501X; Padedda, Bachisio Mario/0000-0002-0988-5613; PULINA, Silvia/0000-0002-4861-4170; Angles, Silvia/0000-0003-0529-7504; Luglie, Antonella/0000-0001-6382-4208	Autonomous Region of Sardinia; Zoumgest project; Spanish Ministry of Economy and Competitiveness; Sassari University Aquatic Ecology group	Autonomous Region of Sardinia(Regione Sardegna); Zoumgest project; Spanish Ministry of Economy and Competitiveness(Spanish Government); Sassari University Aquatic Ecology group	The Autonomous Region of Sardinia provided the principle financial support for the Cabras and Santa Giusta monitoring activities, and the Zoumgest project provided the financial support required for the Corru S'Ittiri Lagoon. The Autonomous Region of Sardinia funded Research Project - Master and Back financed C. T. Satta work. A Postdoctoral Grant from the Spanish Ministry of Economy and Competitiveness partially funded S. Angles work. The authors thank Dr. B. Manca for all laboratory analyses and the Sassari University Aquatic Ecology group for their support.	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J	Anderson, DM; Keafer, BA; Kleindinst, JL; McGillicuddy, DJ; Martin, JL; Norton, K; Pilskaln, CH; Smith, JL; Sherwood, CR; Butman, B				Anderson, Donald M.; Keafer, Bruce A.; Kleindinst, Judith L.; McGillicuddy, Dennis J., Jr.; Martin, Jennifer L.; Norton, Kerry; Pilskaln, Cynthia H.; Smith, Juliette L.; Sherwood, Christopher R.; Butman, Bradford			<i>Alexandrium fundyense</i> cysts in the Gulf of Maine: Long-term time series of abundance and distribution, and linkages to past and future blooms	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium fundyense; Cysts; Resuspension; Gulf of Maine; Harmful algal bloom; HAB; Red tide; Paralytic shellfish poisoning	DINOFLAGELLATE CYSTS; TOXIC DINOFLAGELLATE; RESTING CYSTS; RED TIDE; WESTERN GULF; POPULATION-DYNAMICS; SHELLFISH TOXICITY; COASTAL CURRENT; EASTERN GULF; GERMINATION	Here we document Alexandrium fundyense cyst abundance and distribution patterns over nine years (1997 and 2004-2011) in the coastal waters of the Gulf of Maine (GOM) and identify linkages between those patterns and several metrics of the severity or magnitude of blooms occurring before and after each autumn cyst survey. We also explore the relative utility of two measures of cyst abundance and demonstrate that GOM cyst counts can be normalized to sediment volume, revealing meaningful patterns equivalent to those determined with dry weight normalization. Cyst concentrations were highly variable spatially. Two distinct seedbeds (defined here as accumulation zones with > 300 cysts cm(-3)) are evident, one in the Bay of Fundy (BOF) and one in mid-coast Maine. Overall, seedbed locations remained relatively constant through time, but their area varied 3-4 fold, and total cyst abundance more than 10 fold among years. A major expansion of the mid-coast Maine seedbed occurred in 2009 following an unusually intense A. fundyense bloom with visible red-water conditions, but that feature disappeared by late 2010. The regional system thus has only two seedbeds with the bathymetry, sediment characteristics, currents, biology, and environmental conditions necessary to persist for decades or longer. Strong positive correlations were confirmed between the abundance of cysts in both the 0-1 and the 0-3 cm layers of sediments in autumn and geographic measures of the extent of the bloom that occurred the next year (i.e., cysts --> blooms), such as the length of coastline closed due to shellfish toxicity or the southernmost latitude of shellfish closures. In general, these metrics of bloom geographic extent did not correlate with the number of cysts in sediments following the blooms (blooms --> cysts). There are, however, significant positive correlations between 0-3 cm cyst abundances and metrics of the preceding bloom that are indicative of bloom intensity or vegetative cell abundance (e.g., cumulative shellfish toxicity, duration of detectable toxicity in shellfish, and bloom termination date). These data suggest that it may be possible to use cyst abundance to empirically forecast the geographic extent of the forthcoming bloom and, conversely, to use other metrics from bloom and toxicity events to forecast the size of the subsequent cyst population as the inoculum for the next year's bloom. This is an important step towards understanding the excystment/encystment cycle in A. fundyense bloom dynamics while also augmenting our predictive capability for this HAB-forming species in the GOM. (C) 2013 Elsevier Ltd. All rights reserved.	[Anderson, Donald M.; Keafer, Bruce A.; Kleindinst, Judith L.; McGillicuddy, Dennis J., Jr.; Norton, Kerry; Smith, Juliette L.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Martin, Jennifer L.] Fisheries & Oceans Canada, Biol Stn, St Andrews, NB E5B 2L9, Canada; [Pilskaln, Cynthia H.] Univ Massachusetts Dartmouth, Sch Marine Sci & Technol, New Bedford, MA 02744 USA; [Sherwood, Christopher R.; Butman, Bradford] US Geol Survey, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution; Fisheries & Oceans Canada; University of Massachusetts System; University Massachusetts Dartmouth; United States Department of the Interior; United States Geological Survey	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	danderson@whoi.edu	Martin, Jennifer/G-5217-2011	McGillicuddy, Dennis/0000-0002-1437-2425; Smith, Juliette/0000-0002-9788-3772	ECOHAB Grant program through NOAA [NA06NOS4780245, NA09NOS4780193]; ECOHAB Grant program through Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF) [OCE-0430724, OCE-0911031, OCE-1314642]; National Institute of Environmental Health Sciences (NIEHS) [1-P50-ES012742-01, 1-P01-ES021923-01]; state of Mane; state of New Hampshire; state of Massachusetts; Fisheries and Oceans Canada; Division Of Ocean Sciences; Directorate For Geosciences [1314642] Funding Source: National Science Foundation	ECOHAB Grant program through NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); ECOHAB Grant program through Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF)(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO)); 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)); state of Mane; state of New Hampshire; state of Massachusetts; Fisheries and Oceans Canada; Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We thank the captains and crews of the R/V Oceanus, Endeavor, Cape Hatteras and Gulf Challenger for their assistance during cyst surveys. We also are grateful to the numerous dedicated people that assisted in the collection of samples, including guest investigators and students that came from various institutions around the world. Of those, a number of students from the Northeastern University Cooperative program were very helpful over many years of the study. Maura Thomas (UMaine), Scott McCue (WHOI), and personnel from USGS (S. Baldwin, K. McMullen, J. Borden, and A. Green) contributed greatly to the success of various cruises. Olga Kosnyrev assisted in preparation of cyst abundance maps, and the cyst abundance computations were made by Valery Kosnyrev. We also thank P. Valentine (USGS) and two anonymous reviewers for their helpful comments. Research support provided by the ECOHAB Grant program through NOAA Grants NA06NOS4780245 and NA09NOS4780193, and through the Woods Hole Center for Oceans and Human Health, National Science Foundation (NSF) Grants OCE-0430724, OCE-0911031, and OCE-1314642; and National Institute of Environmental Health Sciences (NIEHS) Grants 1-P50-ES012742-01 and 1-P01-ES021923-01, and funding through the states of Mane, New Hampshire, and Massachusetts. We are also grateful for event response funding provided for many of the cruises. Funding for J.L. Martin was provided by Fisheries and Oceans Canada. This is ECOHAB contribution no. 761 and PCMHAB contribution no. 10.	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Part II-Top. Stud. Oceanogr.	MAY	2014	103						6	26		10.1016/j.dsr2.2013.10.002	http://dx.doi.org/10.1016/j.dsr2.2013.10.002			21	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	25018592	Green Accepted			2025-03-11	WOS:000338810600002
J	Shull, DH; Kremp, A; Mayer, LM				Shull, David H.; Kremp, Anke; Mayer, Lawrence M.			Bioturbation, germination and deposition of <i>Alexandrium fundyense</i> cysts in the Gulf of Maine	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Bioturbation; Cyst; Germination; Model; Toxic dinoflagellates; Gulf of Maine; Alexandrium fundyense	DINOFLAGELLATE CYSTS; VARIABILITY; SEDIMENTS; DYNAMICS; PATTERNS; BLOOM; DINOPHYCEAE; ABUNDANCE; TOXICITY; MODEL	Like many other dinoflagellate species, Alexandrium fundyense possesses a benthic resting cyst which enables long-term persistence and annual blooms of this species in the Gulf of Maine. The size and extent of these harmful algal blooms are associated with high cyst concentrations in the top 1 cm of sediment. Despite the importance of this resting stage in the life history of A. fundyense, little work has been done on bioturbation of cysts in the deep-water cyst beds of the western Gulf of Maine. Our work intensively examined one site within a major regional "seedbed" from February 2003 until August 2005, a time span that included an extraordinarily large bloom of A. fundyense in 2005. Over the course of 2 years we collected samples for benthic infauna and cyst profiles down to a depth of 30 cm. We also measured sediment porosity, organic carbon, Pb-210, and porewater dissolved oxygen. On several dates we measured depth profiles of cyst autofluorescence. Profiles of cysts revealed large subsurface maxima peaking between 10 and 15 cm depth with cyst concentrations declining strongly toward the sediment surface. On one sampling date (August 2004) we observed a cyst concentration peak at the sediment surface. Using these data we constructed a mechanistic model of cyst bioturbation, mortality, germination, and deposition. Modeled bioturbation was calibrated using Pb-210 and modeled cyst profiles were compared to measured profiles. Model runs with constant and interannually-varying rates of cyst deposition produced similar time-averaged cyst profiles. Results indicate that the deeper portions of cyst profiles are determined primarily by bioturbation, germination and cyst mortality and less so by interannual variation in cyst depositional history. This is due to the relatively low sedimentation rate at the study site compared to the rate of bioturbation, and the fact that the number of cysts deposited each year tends to be a small fraction of the total inventory. Seasonal and interannual variation in cyst deposition strongly influenced concentrations of cysts in the top few millimeters of the sediment, however. When cyst deposition rates are low, bioturbation and germination are sufficient to rapidly deplete cysts in this surface layer, leaving relatively few cysts within the sediment depth range that allows germination. But, bioturbation is not rapid enough to homogenize surface sediments within one year. As a result, cyst deposition results in a concentration peak at the sediment surface that persists to fuel germination the following year. Because of this phenomenon, the model predicted that years with high rates of germination follow years with large levels of cyst deposition. Over longer time scales, bioturbation transports cysts from the sediment surface to depth, which, along with germination, creates a persistent subsurface maximum in cyst concentration. Bioturbation also serves to maintain persistence of A. fundyense by transporting older cysts from these deeper layers to the sediment surface where they can germinate. Since high concentrations of cysts near the sediment surface indicate large numbers of cysts deposited during the previous year, if enhanced germination leads to large blooms of A. fundyense, these blooms are predicted to occur in years following large cyst deposition events. (C) 2013 Elsevier Ltd. All rights reserved.	[Shull, David H.] Western Washington Univ, Dept Environm Sci, Bellingham, WA 98225 USA; [Kremp, Anke] Finnish Environm Inst SYKE, Ctr Marine Res, Helsinki 00251, Finland; [Mayer, Lawrence M.] Univ Maine, Darling Marine Ctr, Walpole, ME 04573 USA	Western Washington University; Finnish Environment Institute; University of Maine System; University of Maine Orono	Shull, DH (通讯作者)，Western Washington Univ, Dept Environm Sci, Bellingham, WA 98225 USA.	david.shull@wwu.edu	Shull, David/IUP-8150-2023		NOAA [NA96OP0099]; Academy of Finland; Office of Naval Research	NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); Academy of Finland(Research Council of Finland); Office of Naval Research(United States Department of DefenseUnited States NavyOffice of Naval Research)	This study was supported by grants from NOAA NA96OP0099 (D.H.S.), the Academy of Finland (A.K.), and the Office of Naval Research (L.M.M.). We thank Pete Jumars, Eric Weissburger, and Linda Schick for assistance with sample collection and processing. Daniel Dietrich, Danielle Woolen, and Monte Richardson assisted with the sorting, identification, and biomass measurements of benthic infauna. We also thank Don Anderson and Judy Kleindinst for their comments and support, and Brad Butman, Dennis McGillicuddy and an anonymous reviewer for providing recommendations that improved the manuscript.	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Part II-Top. Stud. Oceanogr.	MAY	2014	103						66	78		10.1016/j.dsr2.2013.09.027	http://dx.doi.org/10.1016/j.dsr2.2013.09.027			13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM					2025-03-11	WOS:000338810600006
J	McGillicuddy, DJ; Townsend, DW; Keafer, BA; Thomas, MA; Anderson, DM				McGillicuddy, D. J., Jr.; Townsend, D. W.; Keafer, B. A.; Thomas, M. A.; Anderson, D. M.			Georges Bank: A leaky incubator of <i>Alexandrium fundyense</i> blooms	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Phytoplankton; Population dynamics; Red tides; Paralytic shellfish poisoning; USA; Gulf of Maine; Georges Bank	SCALLOPS PLACOPECTEN-MAGELLANICUS; NORTHEASTERN UNITED-STATES; PARALYTIC SHELLFISH POISON; INTERANNUAL VARIABILITY; MAINE; GULF; DYNAMICS; POPULATIONS; TOXICITY; MODEL	A series of oceanographic surveys on Georges Bank document variability of populations of the toxic dinoflagellate Alexandrium fundyense on time scales ranging from synoptic to seasonal to interannual. Blooms of A. fundyense on Georges Bank can reach concentrations on the order of 104 cells l(-1), and are generally bank-wide in extent. Georges Bank populations of A. fundyense appear to be quasi-independent of those in the adjacent coastal Gulf of Maine, insofar as they occupy a hydrographic niche that is colder and saltier than their coastal counterparts. In contrast to coastal populations that rely on abundant resting cysts for bloom initiation, very few cysts are present in the sediments on Georges Bank. Bloom dynamics must therefore be largely controlled by the balance between growth and mortality processes, which are at present largely unknown for this population. Based on correlations between cell abundance and nutrient distributions, ammonium appears to be an important source of nitrogen for A. fundyense blooms on Georges Bank. (C) 2012 Elsevier Ltd. All rights reserved.	[McGillicuddy, D. J., Jr.] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA; [Townsend, D. W.; Thomas, M. A.] Univ Maine, Sch Marine Sci, Orono, ME 04469 USA; [Keafer, B. A.; Anderson, D. M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution; University of Maine System; University of Maine Orono; Woods Hole Oceanographic Institution	McGillicuddy, DJ (通讯作者)，Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA.	dmcgillicuddy@whoi.edu		McGillicuddy, Dennis/0000-0002-1437-2425	National Oceanic Atmospheric Administration [NA06NOS4780245]; Woods Hole Center for Oceans and Human Health through National Science Foundation [OCE-0430724, OCE-0911031]; National Institute of Environmental Health Sciences [1P50-ES01274201]; Ecology and Oceanography of Harmful Algal Blooms Program [730]; Division Of Ocean Sciences; Directorate For Geosciences [1314642] Funding Source: National Science Foundation	National Oceanic Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); Woods Hole Center for Oceans and Human Health through 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)); Ecology and Oceanography of Harmful Algal Blooms Program; Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We are very grateful for the outstanding efforts of the officers, crews, and shore support of R/V Oceanus, R/V Endeavor, and R/V Tioga, as well as the hard work of all those who participated in the seagoing science teams. Additional observations in 2008 were contributed by the Massachusetts Water Resources Authority and the Center for Coastal Studies. Olga Kosnyrev, Valery Kosnyrev, and Keston Smith assisted in data analysis and figure preparation. Jim Manning provided the drifter track illustrating the advective connection between the western Gulf of Maine and Georges Bank (Fig. 8). Discussion with Julianne Nassif was beneficial in recounting the prior history of toxicity and plankton sampling on Georges Bank. Hydrographic data presented in Appendix B were collected by the National Oceanic Atmospheric Administration's Northeast Fisheries Science Center as part of an ongoing mission to monitor and assess the Northeast Continental Shelf ecosystem. We appreciate financial support of the National Oceanic Atmospheric Administration (Grant NA06NOS4780245 for the Gulf of Maine Toxicity (GOMTOX) program) and the Woods Hole Center for Oceans and Human Health through National Science Foundation Grants OCE-0430724 and OCE-0911031 and National Institute of Environmental Health Sciences Grant 1P50-ES01274201. This is the Ecology and Oceanography of Harmful Algal Blooms Program contribution number 730.	Anderson D, 2005, DEEP-SEA RES PT II, V52, P2365, DOI 10.1016/j.dsr2.2005.08.001; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2467, DOI 10.1016/j.dsr2.2005.06.015; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 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, 2014, DEEP-SEA RES PT II, V103, P6, DOI 10.1016/j.dsr2.2013.10.002; [Anonymous], GEORGES BANK; [Anonymous], G BANK; Backus R., 1987, GEORGES BANK, P593; Beardsley R.C., 1997, Proceedings of the Gulf of Maine ecosystem dynamics scientific symposium and workshop, P39; Bigelow H.B., 1927, FISH B-NOAA, V40, P511; BOURNE N, 1965, J FISH RES BOARD CAN, V22, P1137, DOI 10.1139/f65-102; Brink KH, 2009, PROG OCEANOGR, V82, P191, DOI 10.1016/j.pocean.2009.07.004; Brink KH, 2003, J GEOPHYS RES-OCEANS, V108, DOI 10.1029/2001JC001019; BUTMAN B, 1987, J PHYS OCEANOGR, V17, P367, DOI 10.1175/1520-0485(1987)017<0367:LTOOTS>2.0.CO;2; Deeds JR, 2014, DEEP-SEA RES PT II, V103, P329, DOI 10.1016/j.dsr2.2013.04.013; DeGrasse S, 2014, DEEP-SEA RES PT II, V103, P288, DOI 10.1016/j.dsr2.2013.01.036; Etheridge SM, 2005, DEEP-SEA RES PT II, V52, P2491, DOI 10.1016/j.dsr2.2005.06.026; Flagg CN., 1987, Georges Bank, P108; Franks PJS, 2001, DEEP-SEA RES PT II, V48, P457, DOI 10.1016/S0967-0645(00)00125-9; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; Hattenrath TK, 2010, HARMFUL ALGAE, V9, P402, DOI 10.1016/j.hal.2010.02.003; Home E.P.W., 1989, SCI MAR, V53, P145; Hu S, 2008, J MARINE SYST, V74, P528, DOI 10.1016/j.jmarsys.2008.04.007; JAMIESON GS, 1983, CAN J FISH AQUAT SCI, V40, P313, DOI 10.1139/f83-046; Ji RB, 2008, J MARINE SYST, V73, P31, DOI 10.1016/j.jmarsys.2007.08.002; Keafer BA, 2005, DEEP-SEA RES PT II, V52, P2674, DOI 10.1016/j.dsr2.2005.06.016; Leong SCY, 2004, TOXICON, V43, P407, DOI 10.1016/j.toxicon.2004.01.015; Levasseur Maurice, 1995, P463; LODER JW, 1980, J PHYS OCEANOGR, V10, P1399, DOI 10.1175/1520-0485(1980)010<1399:TROTCO>2.0.CO;2; Lynch DR, 1996, CONT SHELF RES, V16, P875, DOI 10.1016/0278-4343(95)00028-3; McGillicuddy DJ, 2011, LIMNOL OCEANOGR, V56, P2411, DOI 10.4319/lo.2011.56.6.2411; McGillicuddy DJ, 2005, DEEP-SEA RES PT II, V52, P2698, DOI 10.1016/j.dsr2.2005.06.021; McGillicuddy DJ, 2005, DEEP-SEA RES PT II, V52, P2843, DOI 10.1016/j.dsr2.2005.06.020; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; Nassif J., 1993, 223894064 DEP HLTH H; O'Reilly J.E., 1987, GEORGES BANK, P220; Petitpas CM, 2014, DEEP-SEA RES PT II, V103, P350, DOI 10.1016/j.dsr2.2013.04.012; Pilskaln CH, 2014, DEEP-SEA RES PT II, V103, P55, DOI 10.1016/j.dsr2.2013.05.021; Poulton NJ, 2005, DEEP-SEA RES PT II, V52, P2501, DOI 10.1016/j.dsr2.2005.06.029; Prakash A., 1967, J FISH RES BOARD CAN, V24; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; Smith PC, 2001, DEEP-SEA RES PT II, V48, P37, DOI 10.1016/S0967-0645(00)00081-3; Smith PC, 2012, AM FISH S S, V79, P185; Steele JH, 2007, PROG OCEANOGR, V74, P423, DOI 10.1016/j.pocean.2007.05.003; Townsend DW, 2002, MAR ECOL PROG SER, V228, P57, DOI 10.3354/meps228057; Townsend DW, 2001, CONT SHELF RES, V21, P347, DOI 10.1016/S0278-4343(00)00093-5; Turner JT, 2010, HARMFUL ALGAE, V9, P578, DOI 10.1016/j.hal.2010.04.008; Twichell DC, 1987, GEORGES BANK, P31; WHITE AW, 1993, DEV MAR BIO, V3, P435; Wiebe P.H., 2006, DEEP SEA RES 2, V53, P378	52	23	26	2	22	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.	MAY	2014	103						163	173		10.1016/j.dsr2.2012.11.002	http://dx.doi.org/10.1016/j.dsr2.2012.11.002			11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AL0IM	24976691	Green Accepted, Green Submitted			2025-03-11	WOS:000338810600012
J	Flaim, G; Obertegger, U; Anesi, A; Guella, G				Flaim, Giovanna; Obertegger, Ulrike; Anesi, Andrea; Guella, Graziano			Temperature-induced changes in lipid biomarkers and mycosporine-like amino acids in the psychrophilic dinoflagellate <i>Peridinium aciculiferum</i>	FRESHWATER BIOLOGY			English	Article						temperature stress; life stages; lipidomics; mycosporine-like amino acids; psychrophiles	FATTY-ACID; DIGALACTOSYLDIACYLGLYCEROL COMPOSITION; STEROL COMPOSITION; ENVIRONMENTAL-CONDITIONS; BIOCHEMICAL-COMPOSITION; ULTRAVIOLET SUNSCREENS; ANTIOXIDANT ACTIVITY; OXIDATIVE STRESS; GROWTH-RATES; POLAR LIPIDS	Life at low temperature imposes many constraints linked to sustaining cellular functions. The cold-adapted freshwater dinoflagellate Peridinium aciculiferum has overcome these barriers, often causing blooms in winter but forming resting cysts in spring. Little is known of the biochemical changes that accompany this temperature-induced transformation from vegetative cells to resting cysts. We investigated how the profiles of lipids and mycosporine-like amino acids (MAAs) vary with temperature in vegetative cells and resting cysts of P.aciculiferum. The freshwater dinoflagellate was grown at four temperatures (2.7-7.7 degrees C), simulating the seasonal changes from winter to spring that also induce the transition from cells to cysts. Biochemical profiles were established by liquid chromatography/mass spectrometry with the simultaneous detection of polar and non-polar compounds. Data were analysed by non-metric multidimensional scaling and ANOVA. Over 100 species of galactolipids, betaine lipids, phospholipids and triacylglycerols (TAGs) were found, and many were strong biomarkers for specific temperatures and life stage. Variations in galactolipids, betaine lipids and phospholipids were unidirectional, as shown by an overall decrease in the unsaturation index with temperature. In contrast, changes in TAGs were specific to life stages: short-chain TAGs (cumulative acyl length of 44-52 carbon atoms) decreased in cysts with respect to vegetative cells, while long-chain TAGs (54-62) showed the opposite pattern. The concentration of MAAs decreased with increasing temperature. Final cell yield, a measure of population fitness, also decreased with increasing temperature, confirming the psychrophilic status of P.aciculiferum. We report the first detailed biochemical profiles of vegetative cells and resting cysts for a dinoflagellate and show how small-scale temperature variations alter the biochemical make-up within and between life stages, thus contributing to our understanding of seasonal succession of species.	[Flaim, Giovanna; Obertegger, Ulrike] FEM Res & Innovat Ctr, I-38010 San Michele All Adige, TN, Italy; [Anesi, Andrea; Guella, Graziano] Univ Trento, Povo, TN, Italy; [Guella, Graziano] CNR, Ist Biofis Trento, Povo, TN, Italy	Fondazione Edmund Mach; University of Trento; Consiglio Nazionale delle Ricerche (CNR); Istituto di Biofisica (IBF-CNR)	Flaim, G (通讯作者)，FEM Res & Innovat Ctr, Via Mach 2, I-38010 San Michele All Adige, TN, Italy.	giovanna.flaim@fmach.it	Flaim, Giovanna/AAD-5013-2020; Anesi, Andrea/ACJ-6729-2022; 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; Anesi, Andrea/0000-0002-9334-2610	FEM-CRI; Department of Physics-UNITN	FEM-CRI; Department of Physics-UNITN	This study was carried out within the research activity funded by FEM-CRI and the Department of Physics-UNITN. For excellent technical assistance, the authors thank Adriano Sterni (University of Trento) - LC/MS measurements - and Lorena Ress (FEM-CRI) - algal cultures and sample preparation.	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Biol.	MAY	2014	59	5					985	997		10.1111/fwb.12321	http://dx.doi.org/10.1111/fwb.12321			13	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	AE1AV					2025-03-11	WOS:000333698500008
J	Ivanova, E; Schornikov, E; Marret, F; Murdmaa, I; Zenina, M; Aliev, R; Bradley, L; Chepalyga, A; Wright, L; Kremenetsky, V; Kravtsov, V				Ivanova, Elena; Schornikov, Eugene; Marret, Fabienne; Murdmaa, Ivar; Zenina, Maria; Aliev, Ramiz; Bradley, Lee; Chepalyga, Andrey; Wright, Lisa; Kremenetsky, Vyacheslav; Kravtsov, Victor			Environmental changes on the inner northeastern Black Sea shelf, off the town of Gelendzhik, over the last 140 years	QUATERNARY INTERNATIONAL			English	Article							DINOFLAGELLATE CYSTS; SURFACE CONDITIONS; HOLOCENE; MARMARA; INDICATORS; SALINITY; VARIABILITY; CORES; SCALE; WATER	A comprehensive multi-proxy study of mini-core Ash-2009-08 from the inner shelf of the northeastern Black Sea, allowed us to define recent environmental changes in the area, on a sub-decadal resolution. The age model of the core based on radionuclide (Pb-210 and Cs-137) measurements suggests an average sedimentation rate of 2 mm/y and, consequently, a sedimentary record spanning the last similar to 140 years. Overall, four fossil groups studied from the core indicate subtle environmental changes. The dinocyst assemblages show stable surface water conditions with a possible cooling in the 1930s-1950s and a slight decline in salinity from the 1960s, which corresponds to an increase in precipitation and the fresh water balance of the Black Sea, known from the published instrumental data. A gradually increasing abundance of the heterotroph species suggests a nutrient increase from the 1920s. Ostracods and molluscs demonstrate rather stable bottom-water salinity and biotopes over the last similar to 75 years. Changes in abundance of ostracods and benthic foraminifers, as well as changes in the mollusc diversity, most likely reflect variations in trophic conditions with the higher food supply to the sea floor in the 1940s-1960s and from the late 1990s. Enhanced bottom-water energy is inferred from the mollusc enrichment and a relatively high content of the fine sand grain-size fraction in the 1990s. In the pollen assemblages, trees mainly represented by Pinus strongly prevail over herbs throughout the record. However, the trees to herbs ratio demonstrates a slight decline from the 1920s, most likely resulting from human impact on the vegetation of the nearby land. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.	[Ivanova, Elena; Murdmaa, Ivar; Zenina, Maria; Kremenetsky, Vyacheslav] RAS, Shirshov Inst Oceanol, Moscow 117997, Russia; [Schornikov, Eugene; Zenina, Maria] RAS, AV Zhirmunsky Inst Marine Biol, Far East Div, Vladivostok 690041, Russia; [Marret, Fabienne; Bradley, Lee; Wright, Lisa] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Aliev, Ramiz] Moscow MV Lomonosov State Univ, Skobeltsyn Inst Nucl Phys, Moscow 119992, Russia; [Chepalyga, Andrey] RAS, Inst Geog, Moscow 119017, Russia; [Kravtsov, Victor] RAS, PP Shirshov Inst Oceanol, Atlantic Branch, Kaliningrad, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology; Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences; University of Liverpool; Lomonosov Moscow State University; Institute of Geography, Russian Academy of Sciences; Russian Academy of Sciences; Russian Academy of Sciences; Shirshov Institute of Oceanology	Ivanova, E (通讯作者)，RAS, Shirshov Inst Oceanol, 36 Nakhimovsky Prosp, Moscow 117997, Russia.	e_v_ivanova@ocean.ru; eschornikov@yandex.ru; f.marret@liv.ac.uk; murdmaa@mail.ru; maria_zenina@mail.ru; ramiz.aliev@gmail.com; L.R.Bradley@liv.ac.uk; tchepalyga@mail.ru; lswrght88@gmail.com; sk@ocean.ru; kravtsov@atlas.baltnet.ru	Tchepalyga, Andrey/AAF-9790-2021; Ivanova, Elena/B-3775-2016; Kravtsov, Victor/AAH-8661-2020; Bradley, Lee/AAA-6818-2019; Murdmaa, Ivar/T-3538-2017; Aliev, Ramiz/U-1959-2019; Kremenetskiy, Viacheslav/F-5196-2017	Aliev, Ramiz/0000-0002-4150-928X; Bradley, Lee/0000-0003-0833-9351; Marret-Davies, Fabienne/0000-0003-4244-0437; Tchepalyga, Andrey/0000-0001-8654-1614; Kremenetskiy, Viacheslav/0000-0003-3313-5908	European project Marie Curie [CLIMSEAS-PIRSES-GA-2009-247512]; Russian Foundation for Basic Research [12-05-00617-a]	European project Marie Curie(European Union (EU)Marie Curie Actions); Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	This manuscript is a contribution to the European project Marie Curie, CLIMSEAS-PIRSES-GA-2009-247512: "Climate Change and Inland Seas: Phenomena, Feedback and Uncertainties. The Physical Science Basis". The study is partly supported by the Russian Foundation for Basic Research grant 12-05-00617-a. The technical assistance of Oksana Ivanova, Sultim Lupsandorgiev, and Dmitrii Borisov for collection of microfossils, sample processing and drawing of the map, respectively, is gratefully acknowledged. We thank Dr. Ron Martin and another anonymous reviewer for the constructive comments that allowed us to improve the manuscript.	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Int.	APR 10	2014	328						338	348		10.1016/j.quaint.2013.09.044	http://dx.doi.org/10.1016/j.quaint.2013.09.044			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AE6JB					2025-03-11	WOS:000334096100025
J	Goodman, A; McCall, JR; Jacocks, HM; Thompson, A; Baden, D; Abraham, WM; Bourdelais, A				Goodman, Allan; McCall, Jennifer R.; Jacocks, Henry M.; Thompson, Alysha; Baden, Daniel; Abraham, William M.; Bourdelais, Andrea			Structure Activity Relationship of Brevenal Hydrazide Derivatives	MARINE DRUGS			English	Article						brevenal; brevetoxin; derivatives; structure activity relationship; cystic fibrosis; drug development	SODIUM-CHANNELS; KARENIA-BREVIS; BREVETOXINS	Brevenal is a ladder frame polyether produced by the dinoflagellate Karenia brevis. This organism is also responsible for the production of the neurotoxic compounds known as brevetoxins. Ingestion or inhalation of the brevetoxins leads to adverse effects such as gastrointestinal maladies and bronchoconstriction. Brevenal shows antagonistic behavior to the brevetoxins and shows beneficial attributes when administered alone. For example, in an asthmatic sheep model, brevenal has been shown to increase tracheal mucosal velocity, an attribute which has led to its development as a potential treatment for Cystic Fibrosis. The mechanism of action of brevenal is poorly understood and the exact binding site has not been elucidated. In an attempt to further understand the mechanism of action of brevenal and potentially develop a second generation drug candidate, a series of brevenal derivatives were prepared through modification of the aldehyde moiety. These derivatives include aliphatic, aromatic and heteroaromatic hydrazide derivatives. The brevenal derivatives were tested using in vitro synaptosome binding assays to determine the ability of the compounds to displace brevetoxin and brevenal from their native receptors. A sheep inhalation model was used to determine if instillation of the brevenal derivatives resulted in bronchoconstriction. Only small modifications were tolerated, with larger moieties leading to loss of affinity for the brevenal receptor and bronchoconstriction in the sheep model.	[Goodman, Allan; McCall, Jennifer R.; Jacocks, Henry M.; Thompson, Alysha; Baden, Daniel; Bourdelais, Andrea] Univ N Carolina, Ctr Marine Sci, Wilmington, NC 28409 USA; [Abraham, William M.] Mt Sinai Med Ctr, Dept Res, Miami Beach, FL 33140 USA	University of North Carolina; University of North Carolina Wilmington; Mount Sinai Medical Center	Bourdelais, A (通讯作者)，Univ N Carolina, Ctr Marine Sci, 5600 Marvin K Moss Lane, Wilmington, NC 28409 USA.	goodmana@uncw.edu; mccalljr@uncw.edu; hjacocks@ec.rr.com; amthomp2@ncsu.edu; baden@uncw.edu; william.abraham@msmc.com; bourdelaisa@uncw.edu	McCall, Jennifer/AFU-2750-2022		NIH [P01 ES 10594];  [NIH-1R21NS067503]	NIH(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USA); 	Funding for this research was provided by NIH-1R21NS067503 and NIH P01 ES 10594. Thanks go to Susan Niven and Tanya Hogue for isolating the brevenal used to prepare the analogs and to Emily Probst in the Mass Spectroscopy Facility in the Chemistry Department at UNCW for running the HRMS samples.	Abraham W. M., 2011, TOXICOLOGIST, V120, P476; Abraham WM, 2005, AM J RESP CRIT CARE, V171, P26, DOI 10.1164/rccm.200406-735OC; BADEN DG, 1989, FASEB J, V3, P1807, DOI 10.1096/fasebj.3.7.2565840; Bourdelais AJ, 2005, J NAT PROD, V68, P2, DOI 10.1021/np049797o; Bourdelais AJ, 2004, CELL MOL NEUROBIOL, V24, P553, DOI 10.1023/B:CEMN.0000023629.81595.09; Gold EP, 2013, HARMFUL ALGAE, V26, P12, DOI 10.1016/j.hal.2013.03.001; Mattei C, 2008, PLOS ONE, V3, DOI 10.1371/journal.pone.0003448; McCall JR, 2012, HARMFUL ALGAE, V19, P85, DOI 10.1016/j.hal.2012.06.003; Nguyen-Huu TD, 2010, TOXICON, V56, P792, DOI 10.1016/j.toxicon.2009.08.002; Purkerson SL, 1999, NEUROTOXICOLOGY, V20, P909; Whitney Philip L., 1996, Natural Toxins, V4, P261	11	2	2	1	18	MDPI AG	BASEL	POSTFACH, CH-4005 BASEL, SWITZERLAND	1660-3397			MAR DRUGS	Mar. Drugs	APR	2014	12	4					1839	1858		10.3390/md12041839	http://dx.doi.org/10.3390/md12041839			20	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	AG9SI	24686558	gold, Green Published			2025-03-11	WOS:000335759500008
J	Horikx, M; Heimhofer, U; Dinis, J; Huck, S				Horikx, Maurits; Heimhofer, Ulrich; Dinis, Jorge; Huck, Stefan			Integrated stratigraphy of shallow marine Albian strata from the southern Lusitanian Basin of Portugal	NEWSLETTERS ON STRATIGRAPHY			English	Article						Lusitanian Basin; Albian; carbon isotopes; strontium-isotope stratigraphy; intrabasinal correlation; dinoflagellate cyst biostratigraphy	STRONTIUM-ISOTOPE STRATIGRAPHY; OCEANIC ANOXIC EVENT; LOW-MG CALCITE; LOOK-UP TABLE; SE FRANCE; CENOMANIAN BOUNDARY; COASTAL DEPOSITS; BLACK SHALES; CARBON; WESTERN	Stratigraphic age assignment of Cretaceous shoal-water deposits is notoriously difficult and often hampered by the lack of typical index fossils and the prevalence of sedimentary gaps. Here, we present new bio-and chemostratigraphic data for three sections located in the Lusitanian Basin, Portugal, composed of Albian strata. Sections are correlated and dated using dinoflagellate cyst biostratigraphy, strontium-isotope stratigraphy based on oyster and rudist shells and carbon-isotope stratigraphy. The measured Sr-isotope values from pristine shells are in line with global open marine Sr-87/Sr-86 values from the Albian. Correlation of the Portuguese C-isotope curve with hemipelagic Albian reference records and the presence of typical Albian dinoflagellate cysts further constrain the age of the different sections. The proximal-marine and thick (similar to 190 m) Sao Juliao section serves hereby as reference curve. Correlation with the independently well-dated and more distal Guincho section in the Lusitanian Basin slightly revise the age of the Sao Juliao and Magoito sections compared to previously published results. Furthermore, our findings demonstrate the time-transgressive nature of marine deposition in the southern Lusitanian Basin. The onset of marine conditions in the Agua Doce Member and the deposition of rudist bearing carbonates of the Ponta da Gale Member are diachronous and started significantly earlier in the southernmost part of the basin compared to the north. In summary, the combined geochemical and biostratigraphic results provide an enhanced time control and slightly revise the age of the sections in comparison to previously published studies while providing lithological descriptions, Sr-isotope derived ages and carbon-isotope records. Furthermore, the carbon-isotope record of Sao Juliao can be correlated with Italian (Umbria-Marche Basin) and French (Vocontian Trough) sections and highlights the applicability of shallow marine deposits as chemostratigraphic archives.	[Horikx, Maurits; Heimhofer, Ulrich; Huck, Stefan] Leibniz Univ Hannover, Inst Geol, D-30167 Hannover, Germany; [Dinis, Jorge] Univ Coimbra, IMAR, Inst Marine Res, Dept Earth Sci, P-3000272 Coimbra, Portugal	Leibniz University Hannover; Universidade de Coimbra	Horikx, M (通讯作者)，Leibniz Univ Hannover, Inst Geol, Callinstr 30, D-30167 Hannover, Germany.	horikx@geowi.uni-hannover.de; heimhofer@geowi.uni-hannover.de; jodinis@dct.uc.pt; huck@geowi.uni-hannover.de	Huck, Stefan/AAY-8484-2020	Huck, Stefan/0000-0002-1761-5699	Deutsche Forschungsgemeinschaft (DFG) [HE4467/6-1]	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	We thank Dieter Buhl and Christiane Wenske for laboratory assistance, Rolf Neuser for CL-microscopy assistance and Hans-Ulrich Metzger for providing the oyster and rudist thin-sections. Peter Skelton is thanked for rudist identification, Peter Hochuli for help with the dinoflagellate identification and Jean Cors for field assistance. 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Stratigr.	APR	2014	47	1					85	106		10.1127/0078-0421/2014/0041	http://dx.doi.org/10.1127/0078-0421/2014/0041			22	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AH9EB					2025-03-11	WOS:000336443000004
J	Omaña, L; Torres, JR; Donce, RL; Alencáster, G; Caballero, IL				Omana, Lourdes; Ramon Torres, Jose; Lopez Donce, Ruben; Alencaster, Gloria; Lopez Caballero, Iriliana			A pithonellid bloom in the Cenomanian-Turonian boundary interval from Cerritos in the western Valles-San Luis Potosi platform, Mexico: Paleoenvironmental significance	REVISTA MEXICANA DE CIENCIAS GEOLOGICAS			English	Article						pithonellids; Cenomanian-Turonian boundary Valles-San Luis Potosi platform; Mexico	CRETACEOUS PLANKTONIC-FORAMINIFERA; MIDCRETACEOUS CARBONATE PLATFORM; SOUTH-CENTRAL PYRENEES; SEA-LEVEL; CALCAREOUS DINOFLAGELLATE; ANOXIC EVENT; HIGH-RESOLUTION; BIO-EVENTS; BASIN; STRATIGRAPHY	A calcisphere (Pithonellid) acme is recorded from Cerritos, western Valles-San Luis Potosi platform, Mexico. The abundance of these microfossils appears to constitute a global event in the Cenomanian-Turonian boundary Their large quantity is interpreted as an indicator of changes in primary productivity during transgressive episodes. The pithonellids Bonetocardiella conoidea (Bonet, 1956), Pithonella sphaerica (Kaufmann, 1865), and P ovalis (Kaufmann, 1865) are associated with the r and r-k strategists planktic foraminifera Muricohedbergella delrioensis (Carsey, 1926), M. planispira (Tappan, 1940), Heterohelix moremani (Cushman, 1938), Heterohelix reussi (Cushman, 1938), Macroglobigerinelloides caseyi (Bolli, Loeblich and Tappan, 1957), Whiteinella archaeocretacea Pessagno, W cf. W aprica (Loeblich and Tappan, 1961), W brittonensis (Loeblich and Tappan, 1961), W baltica (Douglas and Rankin, 1969) and W paradubia (Sigal, 1952), which are also considered to be indicators of high nutrient content in unstable paleoenvironments. The abundance of pithonellids occurred at the base of the Whiteinella archaeocretacea Partial Range zone. This great temporal abundance in the material could be related to the environmental changes caused by the drowning of the Valles-San Luis Potosi platform, as nutrient supply increased in the latest Cenomanian, which is linked to a sea-level transgression that occurred on a global scale. In this interval, the occurrence of benthic foraminifera Gavelinella spp., Lingulogavelinella sp., Dorothia sp. and roveacrinids is also recorded. This sequence overlies an extinction level of the platform benthic foraminifera dated as late Cenomanian. The calcispheres Bonetocardiella conoidea (Bonet, 1956), Pithonella sphaerica (Kaufmann, 1865) and P. ovalis (Kaufmann, 1865) show a pithonelloid wall type as well as an inner space (pericoel) of the cyst, in-filled with sparry cements.	[Omana, Lourdes; Alencaster, Gloria] Univ Nacl Autonoma Mexico, Inst Geol, Dept Paleontol, Mexico City 04510, DF, Mexico; [Ramon Torres, Jose; Lopez Donce, Ruben] Univ Autonoma San Luis Potosi, Inst Geol, San Luis Potosi, Mexico; [Lopez Caballero, Iriliana] Univ Nacl Autonoma Mexico, Inst Geol, Posgrad Ciencias Tierra, Mexico City 04510, DF, Mexico	Universidad Nacional Autonoma de Mexico; Universidad Autonoma de San Luis Potosi; Universidad Nacional Autonoma de Mexico	Omaña, L (通讯作者)，Univ Nacl Autonoma Mexico, Inst Geol, Dept Paleontol, Ciudad Univ, Mexico City 04510, DF, Mexico.	lomanya@geologia.unam.mx	López-Caballero, Iriliana/AAS-1098-2021; Lopez-Doncel, Ruben Alfonso/K-7262-2018	Omana, Lourdes/0000-0003-1619-1115; Lopez-Doncel, Ruben Alfonso/0000-0002-7596-8505	DGAPA-PAPIIT [IN119208]	DGAPA-PAPIIT(Programa de Apoyo a Proyectos de Investigacion e Innovacion Tecnologica (PAPIIT))	This work was supported by DGAPA-PAPIIT IN119208 Project grants. We are greatly indebted to Dr. Rafael Barboza Gudino, Director of the Instituto de Geologia de la Universidad Autonoma de San Luis Potosi, for logistical field assistance. We are very grateful to Dr. Malcolm B. Hart (Plymouth University, UK) for the valuable comments and suggestions that much improved the manuscript and to an anonymous reviewer for the useful remarks. We are thankful to Dr. Jens Wendler (Smithsonian Institution, United States of America) for the useful corrections. The authors gratefully acknowledge the editorial corrections contributed by Dr. Thierry Calmus (UNAM, Mexico), which were very helpful. We thank Joaquin Aparicio for preparing numerous thin sections and Jose Carlos Jimenez for helping in the preparation of the figures. Dr. Juan Carlos Garcia y Barragan and Ing. Jesus Silva Corona are acknowledged for the valuable review.	ADAMS T. 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F., 2005, Palaeontologische Zeitschrift, V79, P61; Zugel P., 1994, COURIER FORSCHUNGSIN, V176, P1159	146	21	23	0	5	CENTRO GEOCIENCIAS UNAM	QUERETARO	CENTRO GEOCIENCIAS, UNAM, CAMPUS JURIQUILLA, QUERETARO, QRO 76230, MEXICO	1026-8774			REV MEX CIENC GEOL	Rev. Mex. Cienc. Geol.	APR	2014	31	1					28	44						17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AH0JT					2025-03-11	WOS:000335805900003
J	Accoroni, S; Romagnoli, T; Pichierri, S; Totti, C				Accoroni, Stefano; Romagnoli, Tiziana; Pichierri, Salvatore; Totti, Cecilia			New insights on the life cycle stages of the toxic benthic dinoflagellate <i>Ostreopsis</i> cf. <i>ovata</i>	HARMFUL ALGAE			English	Article						Ostreopsis; Harmful algae; Cysts; Life cycle; Gamete fusion; Benthic dinoflagellates	ALEXANDRIUM-TAYLORI DINOPHYCEAE; GYMNODINIUM-CATENATUM; GONYAULAX-TAMARENSIS; SEXUAL REPRODUCTION; LC-MS; GROWTH; SEA; TEMPERATURE; HARMFUL; HISTORY	New observations on the life cycle stages of Ostreopsis cf. ovata are reported in the field and in cultures samples from the northern Adriatic Sea (Mediterranean Sea). Cultures of O. cf. ovata were performed using both replete and N-free growth media and analyzed for 5 months. Ostreopsis cells displayed a high morphological variability. Some cells were characterized by the presence of orange accumulation bodies, which represented a signal of stress conditions. Two mechanisms of gamete mating seem to occur. In the first (already reported) vegetative cells conjugated through the epitheca without plasmogamy; in this regard we observed a new 'process' on the top of the epitheca which might represent a structure involved in this mating mechanism. In the second, small cells acting as gametes were aligned laterally with the two cingula perpendicular to each other. Meiosis possibly occurred as suggested by tetrad formation, originating four vegetative cells. At least two types of cyst were formed, a non-dormant (pellicle) cyst germinating within 2 days and a resting cyst which is able to germinate after a 5-month dormancy only at temperatures over 25 degrees C. (C) 2014 Elsevier B.V. All rights reserved.	[Accoroni, Stefano; Romagnoli, Tiziana; Pichierri, Salvatore; Totti, Cecilia] Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, I-60131 Ancona, Italy	Marche Polytechnic University	Totti, C (通讯作者)，Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, Via Brecce Bianche, I-60131 Ancona, Italy.	c.totti@univpm.it	TOTTI, Cecilia Maria/A-9178-2016; Accoroni, Stefano/F-5818-2014	TOTTI, Cecilia Maria/0000-0002-1532-6009; Romagnoli, Tiziana/0009-0009-5181-987X; Accoroni, Stefano/0000-0002-1134-7849				Accoroni S, 2012, HARMFUL ALGAE, V19, P15, DOI 10.1016/j.hal.2012.05.003; Accoroni S, 2012, CRYPTOGAMIE ALGOL, V33, P191, DOI 10.7872/crya.v33.iss2.2011.191; Accoroni S, 2011, MAR POLLUT BULL, V62, P2512, DOI 10.1016/j.marpolbul.2011.08.003; Agrawal SC, 2009, FOLIA MICROBIOL, V54, P273, DOI 10.1007/s12223-009-0047-0; Aligizaki K, 2006, HARMFUL ALGAE, V5, P717, DOI 10.1016/j.hal.2006.02.005; 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; Barone Rossella, 2006, Naturalista Siciliano, V30, P401; Battocchi C, 2010, MAR POLLUT BULL, V60, P1074, DOI 10.1016/j.marpolbul.2010.01.017; Beam C. 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A., 1973, BRIT PHYCOL J, V8, P105, DOI DOI 10.1080/00071617300650141; Wang ZT, 2009, EUKARYOT CELL, V8, P1856, DOI 10.1128/EC.00272-09	69	33	36	1	55	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	APR	2014	34						7	16		10.1016/j.hal.2014.02.003	http://dx.doi.org/10.1016/j.hal.2014.02.003			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	AG2VX					2025-03-11	WOS:000335276300002
J	Sliwinska, KK; Dybkjaer, K; Schoon, PL; Beyer, C; King, C; Schouten, S; Nielsen, OB				Sliwinska, Kasia K.; Dybkjaer, Karen; Schoon, Petra L.; Beyer, Claus; King, Chris; Schouten, Stefan; Nielsen, Ole Bjorslev			Paleoclimatic and paleoenvironmental records of the Oligocene-Miocene transition, central Jylland, Denmark	MARINE GEOLOGY			English	Article						GDGT proxies; dinocysts; foraminifera; magnetostratigraphy; Oligocene/Miocene boundary; Mi-1 cooling event; delta C-13	TERRESTRIAL ORGANIC-MATTER; GLOBAL SEA-LEVEL; DINOFLAGELLATE CYSTS; UPPERMOST OLIGOCENE; STRATIGRAPHY; CLIMATE; SUCCESSION; EVOLUTION; ASSEMBLAGES; CALIBRATION	A multidisciplinary study of the Oligocene/Miocene (O/M) transition was carried in two boreholes (Harre-1 and Horn-1) from the Danish land area in order to improve the understanding of the paleodimatological and environmental changes across the Mi-1, the earliest Miocene cooling event. Dinoflagellate cyst (dinocyst) biostratigraphy, supported by re-evaluation of the foraminiferid biostratigraphy, a new set of magnetic data and stable carbon isotope (delta C-13) records were applied to improve the age model for the studied succession; as well as the positioning of the O/M boundary. These data further enabled a correlation of the two investigated profiles with the well-established stratigraphical framework for the Danish area. The BIT index (an organic proxy indicating the relative input of soil-derived organic matter), dinocyst assemblages and palynofacies have been applied for establishing the paleoenvironmental changes across the Oligocene/Miocene (O/M) boundary. Our data indicate a shallowing upward trend in the latest Oligocene, resulting in the establishment of a very restricted marine setting in the earliest Miocene. Our study confirms that the O/M boundary is located at a sequence boundary (the local sequence boundary B - SB B) and corresponds to an increase in terrestrial organic matter input. A mean air temperature record based on the MBT'/CBT proxy reveals an similar to 2 degrees C drop in temperature at the O/M and the sequence boundary. Our findings confirm previous suggestions that this sequence boundary is a result of the glacio-eustatic sea level fall related with the Mi-1 cooling event The unconformity at the sequence boundary probably correlates with the coldest part of Mi-1, and thus no deposits from this period have been preserved. This suggests that the temperature drop might have been greater than 2 degrees C. (C) 2014 Elsevier B.V. All rights reserved.	[Sliwinska, Kasia K.; Nielsen, Ole Bjorslev] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Dybkjaer, Karen] GEUS Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark; [Schoon, Petra L.; Schouten, Stefan] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, Texel, Netherlands; [Beyer, Claus] CB Magneto, DK-8670 Lasby, Denmark	Aarhus University; Geological Survey Of Denmark & Greenland; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Sliwinska, KK (通讯作者)，GEUS Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	kksl@geus.dk	Schouten, Stefan/P-4380-2016; Nielsen, Ole/O-1060-2013; Dybkjær, Karen/G-5223-2018; Sliwinska, Kasia K./G-9097-2018	Sliwinska, Kasia K./0000-0001-5488-8832	Danish Council for Independent Research/Natural Sciences (FNU) [272-08-0256]; Fur Museum (Denmark); NINO through a VICI grant	Danish Council for Independent Research/Natural Sciences (FNU)(Det Frie Forskningsrad (DFF)Danish Natural Science Research Council); Fur Museum (Denmark); NINO through a VICI grant	The presented study has been performed as a part of liwinska's PhD project carried out at Aarhus University under main supervision of Claus Heilmann-Clausen. The organic geochemical and magnetostratigraphical studies were financed from grant no. 272-08-0256 received from the Danish Council for Independent Research/Natural Sciences (FNU). Kid acknowledges financial support from Fur Museum (Denmark). SS acknowledges financial support from NINO through a VICI grant. Anchelique Mets, Ellen Hopmans and jolt Ossebaar (NIOZ) are thanked for their support in the laboratory work. Stefan Solberg (GEUS) is thanked for preparing some of the figures. Ian C. Harding (University of Southampton) and Henrik Nohr Hansen (GEUS) are acknowledged for their valuable comments and suggestions on the early stage of the manuscript. Erik Skovbjerg Rasmussen (GEUS) is thanked for his critical reading of the sedimentological part of the manuscript. Timme Donders and two anonymous reviewers are appreciated for their thorough review of the manuscript.	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Geol.	APR 1	2014	350						1	15		10.1016/j.margeo.2013.12.014	http://dx.doi.org/10.1016/j.margeo.2013.12.014			15	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	AG0IB					2025-03-11	WOS:000335098100001
J	Do Couto, D; Popescu, SM; Suc, JP; Melinte-Dobrinescu, MC; Barhoun, N; Gorini, C; Jolivet, L; Poort, J; Jouannic, G; Auxietre, JL				Do Couto, Damien; Popescu, Speranta-Maria; Suc, Jean-Pierre; Melinte-Dobrinescu, Mihaela Carmen; Barhoun, Nadia; Gorini, Christian; Jolivet, Laurent; Poort, Jeffrey; Jouannic, Gwenael; Auxietre, Jean-Luc			Lago Mare and the Messinian Salinity Crisis: Evidence from the Alboran Sea (S. Spain)	MARINE AND PETROLEUM GEOLOGY			English	Article						Dinoflagellate cysts; Calcareous nannoplankton; Lago Mare; Alboran Sea; Messinian Salinity Crisis; Post-crisis reflooding	NEOGENE TECTONIC EVOLUTION; LATE MIOCENE; NIJAR BASIN; MEDITERRANEAN SEA; DEPOSITIONAL-ENVIRONMENTS; NORTHERN APENNINES; SORBAS BASIN; DACIC BASIN; AGE; SEDIMENTATION	This paper provides a new environmental, sedimentological and stratigraphic context of the Lago Mare deposits from the North Alboran region and clarifies their chronologic location with respect to the Messinian Salinity Crisis. We present new micropalaeontological data (dinoflagellate cysts, calcareous nannoplankton, planktonic foraminifers), correlated with field observations and offshore seismic interpretations. We show that the Lago Mare event known in three onshore localities (Rio Mendelin near Malaga, Zorreras near Sorbas, Gafares near Nijar) follows the marine reflooding of the Mediterranean Basin which ended the Messinian Salinity Crisis. Chronologically, these Lago Mare deposits last from the latest Messinian to the early Zanclean. In fact, the first influx of Paratethyan organisms is revealed by the dinoflagellate cyst record from near Malaga within a Gilbert-type fan delta overlying the Messinian Erosional Surface. Invading molluscs and/or ostracods may have persisted in lagoonal coastal areas more or less affected by discontinuous marine influxes (Sorbas and Nijar). The Malaga area is convenient for a palaeogeographic and sedimentary reconstruction which shows the prevalent forcing of sea-level changes during the time-interval 5.600-5.332 Ma at the difference of the usually solicited prevalent tectonics. The studied Lago Mare event is the third episode resulting in such a palaeobiological assemblage in the Mediterranean region and corresponds to the final two-way water exchange at high sea level between the Mediterranean and the former Paratethys. It documents the onset of the modern marine circulation in the Mediterranean after the reflooding ending the Messinian Salinity Crisis. (C) 2014 Elsevier Ltd. All rights reserved.	[Do Couto, Damien; Suc, Jean-Pierre; Gorini, Christian; Poort, Jeffrey] Univ Paris 06, ISTEP, UMR 7193, F-75005 Paris, France; [Do Couto, Damien; Suc, Jean-Pierre; Gorini, Christian; Poort, Jeffrey] CNRS, ISTEP, UMR 7193, F-75005 Paris, France; [Do Couto, Damien; Auxietre, Jean-Luc] TOTAL, F-92400 Paris, France; [Popescu, Speranta-Maria] GeoBioStratData Consulting, F-69140 Rillieux La Pape, France; [Melinte-Dobrinescu, Mihaela Carmen] Natl Inst Marine Geol & Geoecol, Bucharest 70318, Romania; [Barhoun, Nadia] Univ Hassan II Mohammedia, Fac Sci Ben MSik, Casablanca, Morocco; [Jolivet, Laurent] Univ Orleans, ISTO, UMR 7327, F-45071 Orleans, France; [Jolivet, Laurent] CNRS, INSU, ISTO, UMR 7327, F-45071 Orleans, France; [Jolivet, Laurent] Bur Rech Geol & Minieres, ISTO, UMR 7327, F-45060 Orleans, France; [Jouannic, Gwenael] Cerema, DTer Est, Lab Reg Ponts & Chaussees Nancy, F-54510 Tomblaine, 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 - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite; Total SA; National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Hassan II University of Casablanca; Bureau de Recherches Geologiques et Minieres (BRGM); Centre National de la Recherche Scientifique (CNRS); Universite de Orleans; CNRS - National Institute for Earth Sciences & Astronomy (INSU); Bureau de Recherches Geologiques et Minieres (BRGM); Centre National de la Recherche Scientifique (CNRS); Universite de Orleans; CNRS - National Institute for Earth Sciences & Astronomy (INSU); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Bureau de Recherches Geologiques et Minieres (BRGM); Universite de Orleans	Do Couto, D (通讯作者)，Univ Paris 06, ISTEP, 4 Pl Jussieu,Case 129, F-75252 Paris 05, France.	docoutodamien@gmail.com; speranta.popescu@gmail.com; jeanpierre.suc@gmail.com; melinte@geoecomar.ro; nbarhoun@yahoo.fr; christian.gorini@gmail.com; laurent.jolivet@univ-orleans.fr; gwenael.jouannic@cerema.ir; jean-luc.auxietre@total.com	Jolivet, Laurent/D-5598-2009; Mihaela, mihaela/AAF-5894-2021; Jouannic, Gwenael/ABG-7687-2020; DO COUTO, Damien/W-9543-2018	Jouannic, Gwenael/0000-0003-3399-389X; DO COUTO, Damien/0000-0003-0589-208X; Poort, Jeffrey/0000-0001-5964-9697; Popescu, Speranta- Maria/0000-0001-5345-395X; Melinte-Dobrinescu, Mihaela Carmen/0000-0003-4716-6844	CIFRE PhD grant [584/2010]; CNRS/INSU "Actions Marges" Program	CIFRE PhD grant; CNRS/INSU "Actions Marges" Program	Field trips and micropalaeontological analyses have been supported by the CIFRE PhD grant No 584/2010 (TOTAL/UPMC/ANRT) and by the CNRS/INSU "Actions Marges" Program. 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Pet. Geol.	APR	2014	52						57	76		10.1016/j.marpetgeo.2014.01.018	http://dx.doi.org/10.1016/j.marpetgeo.2014.01.018			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AE6GT		Green Submitted			2025-03-11	WOS:000334089300005
J	Mafi, A; Ghasemi-Nejad, E; Ashouri, A; Vahidi-Nia, M				Mafi, Abradat; Ghasemi-Nejad, Ebrahim; Ashouri, Alireza; Vahidi-Nia, Mohammad			A note on the discovery of the suturocavate dinoflagellate cyst (<i>Limbodinium absidatum</i>) in the Middle East (Binalud Mountains, NE Iran)	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Limbodinium absidatum; Suturocavate dinocyst; Dalichai Formation; Iran; Middle East		Limbodinium absidatum is a suturocavate dinocyst that is being reported here from the Binalud Mountains, NE Iran, which is also the first record of this rare species from the Middle East. A few specimens of L. absidatum are recorded from samples taken from the Dalichai Formation at a section measured at Ghoroneh. The stratigraphic range of this species (Late Callovian-Early Oxfordian) is very important for Jurassic palynologists. Morphological characteristics of this Sexiform species are described in detail to support the identification. (C) 2014 Published by Elsevier Ltd.	[Mafi, Abradat; Ashouri, Alireza; Vahidi-Nia, Mohammad] Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Mashhad, Iran; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran	Ferdowsi University Mashhad; University of Tehran	Mafi, A (通讯作者)，Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Mashhad, Iran.	Abradatmafi@gmail.com	Ghasemi-Nejad, Ebrahim/AAF-6087-2020; Vahidinia, Mohammad/AAB-7110-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068; Ashouri, Ali Reza/0000-0002-2913-4913				[Anonymous], 1894, SYSTEMATISCHE PHYLOG, DOI DOI 10.3931/E-RARA-72554-XVI,[1]-400; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; Fritsch F.E., 1929, NEW PHYTOL, V28, P165, DOI [10.1111/J.1469-8137.1929.TB06754.X, DOI 10.1111/J.1469-8137.1929.TB06754.X]; Ghasemi-Nejad E, 2012, J ASIAN EARTH SCI, V43, P1, DOI 10.1016/j.jseaes.2011.08.006; Pascher A., 1914, Berlin Ber D bot Ges, V32; RIDING J B, 1987, Palynology, V11, P55; RIDING J B, 1984, Palynology, V8, P195; Riding JB, 2011, REV PALAEOBOT PALYNO, V163, P227, DOI 10.1016/j.revpalbo.2010.10.009; RILEY L A, 1982, Palynology, V6, P193; SARJEANT WAS, 1974, S STRAT PAL B SAHN I, P9; Seyed-Emami K., 1998, GEOLOGIE, V38, P97; Seyed-Emami K, 2011, NEUES JAHRB GEOL P-A, V261, P373, DOI 10.1127/0077-7749/2011/0181; Taheri J, 2009, GEOL SOC SPEC PUBL, V312, P205, DOI 10.1144/SP312.10; Traverse A., 2007, Palaeopalynology, V2nd; Wilmsen M, 2009, TERRA NOVA, V21, P211, DOI 10.1111/j.1365-3121.2009.00876.x; Woollam R., 1983, 832 I GEOL SCI	17	0	0	0	5	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1464-343X	1879-1956		J AFR EARTH SCI	J. Afr. Earth Sci.	APR	2014	92						21	24		10.1016/j.jafrearsci.2013.12.012	http://dx.doi.org/10.1016/j.jafrearsci.2013.12.012			4	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AE5DX					2025-03-11	WOS:000334009100003
J	Al-Ameri, TK; Al-Ekabi, AH; Al-Jawad, SN				Al-Ameri, Thamer Khazal; Al-Ekabi, Afrah Hasan; Al-Jawad, Sameer Noori			Palynomorph stratigraphy, palynofacies and organic geochemistry assessments for hydrocarbon generation of Ratawi Formation, Iraq	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Palynomorphs; Palynofacies; Kerogen geochemistry; Maturation; Hydrocarbon generation; Modelling; Lower Cretaceous; Iraq	PETROLEUM SYSTEM; SOUTHERN IRAQ; OIL-FIELDS; RESERVOIR; KINETICS; ZUBAIR	Seventy-two core and cutting samples of the Ratawi Formation from selected wells of central and southern Iraq in Mesopotamian Foredeep Basin are analysed for their sedimentary organic matters. Dinoflagellates, spores and pollen are extracted by palynological techniques from these rocks. Accordingly, Hauterivian and late Valanginian ages are suggested for their span of depositional time. These palynomorphs with other organic matter constituents, such as foraminifer's linings, bacteria and fungi, are used to delineate three palynofacies types that explain organic matter accumulation sites and their ability to generate hydrocarbons. Palaeoenvironments of these sites were mainly suboxic to anoxic with deposition of inshore and neritic marine environments especially for palynofacies type 2. Total organic matters of up to 1.75 total organic carbon (TOC) wt.% and early mature stage of up to 3.7 TAI based on the brown colour of the spore species Cyathidites australis and Gleichenidites senonicus with mottled interconnected amorphous organic matter are used for hydrocarbon generation assessment from this formation. On the other hand, these rock samples are processed with Rock-Eval pyrolysis. Outcomes and data calculations of these analyses are plotted on diagrams of kerogen types and hydrocarbon potential. Theses organic matter have reached the mature stage of up to T (max) = 438 A degrees C, hydrogen index of up to 600 mg hydrocarbons for each gram of TOC wt.% and mainly low TOC (0.50-1.55). Accordingly, this formation could generate fair quantities of hydrocarbons in Baghdad oil field and Basrah oil fields. Organic matters of this formation in the fields of Euphrates subzone extends from Hilla to Nasiriyah cities have not reached mature stage and hence not generated hydrocarbons from the Ratawi Formation. Software 1D PetroMod basin modelling of the Ratawi Formation has confirmed this approach of hydrocarbon generation with 100 % transformations of the intended organic matters to generate hydrocarbons to oil are performed in especially oil fields of East Baghdad, West Qurna and Majnoon while oil fields Ratawi and Subba had performed 80-95 % transformation to oil and hence end oil generation had charged partly the Tertiary traps that formed during the Alpine Orogeny. Oil fields of Nasiriyah and Kifle had performed least transformation ratio of about 10-20 % transformation to oil, and hence, most of the present oil in this field is migrated from eastern side of the Mesopotamian Foredeep Basin that hold higher maturation level.	[Al-Ameri, Thamer Khazal; Al-Ekabi, Afrah Hasan] Univ Baghdad, Coll Sci, Dept Geol, Baghdad, Iraq; [Al-Jawad, Sameer Noori] Minist Oil, Reservoirs & Oil Field Dev Inst, Baghdad, Iraq	University of Baghdad	Al-Ekabi, AH (通讯作者)，Univ Baghdad, Coll Sci, Dept Geol, Baghdad, Iraq.	d.afrah@yahoo.com	Saleh, Afrah/Y-8531-2019; AlJawad, Noori/AAF-7521-2020					Al-Ameri T.K., 2011, Hydrocarbon generation odeling of the Basrah oil fields; Al-Ameri TK, 2009, GEOARABIA, V14, P91; Al-Ameri TK, 2011, ARAB J GEOSCI, V4, P1239, DOI 10.1007/s12517-010-0160-z; Al-Ameri TK, 2011, ARAB J GEOSCI, V4, P915, DOI 10.1007/s12517-009-0115-4; Al-Ameri TK, 1996, IRAQI J SCI, V37, P1393; Al-Ameri TK, 1983, PALAEO, V3 3, P103; Al-Obaidi RY, 2013, ARAB J GEOSCI, V6, P3303, DOI 10.1007/s12517-012-0613-7; [Anonymous], PETROLEUM FORMATION; Aqrawi A., 2010, The Petroleum Geology of Iraq; Auchi WMT, 1990, THESIS U SALAHUDDIN; 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; Bujack JP, 1977, OIL GAS J, V75, P193; Davey JR, 1982, DENMARKS GEOLOGIC B, V6; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; Dettmann M.E, 1986, ASS AUSTR PALAEONTOL, V3, P79; Downie C., 1971, Geoscience Man, V3, P29; Durand B., 1980, Kerogen Insoluble Organic Matter From Sedimentary Rocks, P35; HARLAND R, 1973, Palaeontology (Oxford), V16, P665; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Hunt J.M., 1996, PETROLEUM GEOLOGY GE; Ibrahim Mohamed, 1996, Bulletin Centre de Recherches Exploration-Production Elf-Aquitaine Memoire, V16, P611; Lewan MD, 2002, ORG GEOCHEM, V33, P1457, DOI 10.1016/S0146-6380(02)00182-1; Milliod MA, 1974, AM ASS STRATIGRAPHIC, V4; Owen R.M.S., 1958, Habitat of Oil: AAPG, P1252; Peter K.E., 2005, BIOMARKER GUIDE, V2; Pitman J.K., 2004, GeoArabia, V9, P41, DOI [10.2113/geoarabia090441, DOI 10.2113/GEOARABIA090441]; POTONIE R., 1954, GEOL JAHRB, V69, P111; SCOTT RW, 1977, CRETACEOUS CARBONATE, V89, P169; Sharland P.R., 2001, GEOARABIA SPECIAL PU, DOI DOI 10.2113/GEOARABIA0901199; SWEENEY JJ, 1990, AAPG BULL, V74, P1559; THOMPSON CL, 1986, INT J COAL GEOL, V6, P229, DOI 10.1016/0166-5162(86)90003-0; Thusu B, 1995, J MICROPALAEONTOL, V4, P113; Tschudy RobertH., 1969, Aspects of Palynology; Tyson RV, 1995, SEDIMENTARY ORGANIC, VXviii, P615; Uwins PJ, 1988, EARLY MIDCRETACEOUS, P215; Van Bellen R. C., 1959, C GEOL INT COMM STRA, VIII; William GL, 1998, AASP CONTRIBUTION SE, V34; [No title captured]	40	1	1	0	12	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	APR	2014	7	4					1433	1455		10.1007/s12517-013-0913-6	http://dx.doi.org/10.1007/s12517-013-0913-6			23	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AD8OD					2025-03-11	WOS:000333524600012
J	Kamiyama, T; Yamauchi, H; Nagai, S; Yamaguchi, M				Kamiyama, Takashi; Yamauchi, Hiroyuki; Nagai, Satoshi; Yamaguchi, Mineo			Differences in abundance and distribution of <i>Alexandrium</i> cysts in Sendai Bay, northern Japan, before and after the tsunami caused by the Great East Japan Earthquake	JOURNAL OF OCEANOGRAPHY			English	Article						Great East Japan Earthquake; Tsunami; Alexandrium; Cysts; PSP; Sendai Bay	SETO-INLAND SEA; SPP. RESTING CYSTS; TOXIC DINOFLAGELLATE; VERTICAL-DISTRIBUTION; SURFACE SEDIMENTS; HIROSHIMA BAY; BENTHIC CYSTS; A.-CATENELLA; TAMARENSE; DINOPHYCEAE	The tsunami caused by the Great East Japan Earthquake on 11 March 2011 greatly influenced the coastal benthic environment on the northern Pacific coast of Japan. We used the direct count method to investigate changes in the abundance and distribution of Alexandrium (Alexandrium tamarense and Alexandrium catenella) cysts before and after the tsunami in Sendai Bay. Densities of Alexandrium cysts in sediments collected in summer 2011 ranged from 0 to 8,190 cysts cm(-3). In the western part of the bay, the density increased greatly after the tsunami, the highest density being approximately 10 times the density recorded in 2005. Molecular identification of single cysts with multiplex polymerase chain reaction (PCR) showed that Alexandrium tamarense dominated the cyst population in the southwestern part of the bay in 2011. Furthermore, accumulation of cysts on the surface sediment after disturbance of the sediment was confirmed by a laboratory experiment. The main factor causing the drastic changes in abundance and distribution of Alexandrium cysts after the earthquake was considered to be vertical and horizontal redistribution of the cysts in sediments after the tsunami.	[Kamiyama, Takashi] Tohoku Natl Fisheries Res Inst, Fisheries Res Agcy, Shiogama, Miyagi 9850001, Japan; [Yamauchi, Hiroyuki] Miyagi Prefectural Govt, Aoba Ku, Sendai, Miyagi 9808570, Japan; [Nagai, Satoshi] Natl Res Inst Fisheries Sci, Kanazawa Ku, Yokohama, Kanagawa 2368648, Japan; [Yamaguchi, Mineo] Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA)	Kamiyama, T (通讯作者)，Tohoku Natl Fisheries Res Inst, Fisheries Res Agcy, 3-27-5 Shinhama, Shiogama, Miyagi 9850001, Japan.	kamiyama@affrc.go.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063	Fisheries Research Agency; Miyagi Prefecture in Japan	Fisheries Research Agency; Miyagi Prefecture in Japan	The authors thank the researchers of Tohoku National Fisheries Research Institute, Fisheries Research Agency (Drs. Yutaka Kurita, Youji Narimatsu, Shin-ichi Itoh, Yuji Okazaki, Shigeho Kakei, Ryo Inagawa, and Toshikazu Yano), and the captain and crew of R/V Wakataka-Maru of the Fisheries Research Agency, for their cooperation with the sediment sampling. We also thank the captain and crew of the R/V Kaiyo for their cooperation during the field survey. Financial support from the Fisheries Research Agency and Miyagi Prefecture in Japan is greatly appreciated.	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Oceanogr.	APR	2014	70	2					185	195		10.1007/s10872-014-0221-0	http://dx.doi.org/10.1007/s10872-014-0221-0			11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AD0KW					2025-03-11	WOS:000332923900006
J	Bogus, K; Mertens, KN; Lauwaert, J; Harding, IC; Vrielinck, H; Zonneveld, KAF; Versteegh, GJM				Bogus, Kara; Mertens, Kenneth Neil; Lauwaert, Johan; Harding, Ian C.; Vrielinck, Henk; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.			Differences in the chemical composition of organic-walled dinoflagellate resting cysts from phototrophic and heterotrophic dinoflagellates	JOURNAL OF PHYCOLOGY			English	Article						phototrophic; heterotrophic; nutritional strategy; dinosporin; dinoflagellate cyst; infrared spectroscopy; macromolecule	SURFACE SEDIMENTS; THECA RELATIONSHIP; UPWELLING SYSTEM; FEEDING-BEHAVIOR; GROWTH-RATES; CELL-WALL; TEMPERATURE; SALINITY; CHITIN; MACROMOLECULES	Dinoflagellates constitute a large proportion of the planktonic biomass from marine to freshwater environments. Some species produce a preservable organic-walled resting cyst (dinocyst) during the sexual phase of their life cycle that is an important link between the organisms, the environment in which their parent motile theca grew, and the sedimentary record. Despite their abundance and widespread usage as proxy indicators for environmental conditions, there is a lack of knowledge regarding the dinocyst wall chemical composition. It is likely that numerous factors, including phylogeny and life strategy, determine the cyst wall chemistry. However, the extent to which this composition varies based on inherent (phylogenetic) or variable (ecological) factors has not been studied. To address this, we used micro-Fourier transform infrared spectroscopy to analyze nine cyst species produced by either phototrophic or heterotrophic dinoflagellates from the extant orders Gonyaulacales, Gymnodiniales, and Peridiniales. Based on the presence of characteristic functional groups, two significantly different cyst wall compositions are observed that correspond to the dinoflagellate's nutritional strategy. The dinocyst wall compositions analyzed appeared carbohydrate-based, but the cyst wall produced by phototrophic dinoflagellates suggested a cellulose-like glucan, while heterotrophic forms produced a nitrogen-rich glycan. This constitutes the first empirical evidence nutritional strategy is related to different dinocyst wall chemistries. Our results indicated phylogeny was less important for predicting composition than the nutritional strategy of the dinoflagellate, suggesting potential for cyst wall chemistry to infer past nutritional strategies of extinct taxa preserved in the sedimentary record.	[Bogus, Kara] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Bogus, Kara; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.] MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Lauwaert, Johan; Vrielinck, Henk] Univ Ghent, Dept Solid State Sci, B-9000 Ghent, Belgium; [Harding, Ian C.] Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England	University of Bremen; University of Bremen; Ghent University; Ghent University; NERC National Oceanography Centre; University of Southampton	Bogus, K (通讯作者)，Texas A&M Univ, Int Ocean Discovery Program, 1000 Discovery Dr, College Stn, TX 77845 USA.	bogus@iodp.tamu.edu	Lauwaert, Johan/KIK-2307-2024; Vrielinck, Henk/M-8367-2016; Harding, Ian/K-3320-2012; Mertens, Kenneth/AAO-9566-2020; Versteegh, Gerard J.M./H-2119-2011; Mertens, Kenneth/C-3386-2015	Versteegh, Gerard J.M./0000-0002-9320-3776; Vrielinck, Henk/0000-0003-4861-9630; Harding, Ian/0000-0003-4281-0581; Bogus, Kara/0000-0003-4690-0576; Mertens, Kenneth/0000-0003-2005-9483	DFG (Deutsche Forschungsgemeinschaft) as part of the European Graduate College "Proxies in Earth's History" (EUROPROX); DFG (Deutsche Forschungsgemeinschaft) as part of MARUM; DFG [VE-486/2, VE-486/3]	DFG (Deutsche Forschungsgemeinschaft) as part of the European Graduate College "Proxies in Earth's History" (EUROPROX)(German Research Foundation (DFG)); DFG (Deutsche Forschungsgemeinschaft) as part of MARUM(German Research Foundation (DFG)); DFG(German Research Foundation (DFG))	We appreciate the technical assistance of Ross Williams (NOCS, Southampton) regarding the FTIR (OMNIC) analysis. We would like to thank Francine McCarthy for the reuse of the palynological sample from Honey Harbour. We also thank two anonymous reviewers whose comments improved the manuscript. Financial support for K. B. was provided by the DFG (Deutsche Forschungsgemeinschaft) as part of the European Graduate College "Proxies in Earth's History" (EUROPROX) and the MARUM, and by the DFG to G.J.M.V. in the framework of a Heisenberg grant (VE-486/2 and/3). K.N.M is a postdoctoral fellow of FWO (Fonds Wetenschappelijk Onderzoek) Belgium.	Allard B, 1998, ORG GEOCHEM, V28, P543, DOI 10.1016/S0146-6380(98)00012-6; Allard B, 1997, ORG GEOCHEM, V26, P691, DOI 10.1016/S0146-6380(97)00037-5; Almendros G, 1997, J ANAL APPL PYROL, V40-1, P599, DOI 10.1016/S0165-2370(97)00034-X; [Anonymous], 1993, CLASSIFICATION FOSSI; ARNOSTI C, 1995, GEOCHIM COSMOCHIM AC, V59, P4247, DOI 10.1016/0016-7037(95)00247-W; Aspinall G. 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Phycol.	APR	2014	50	2					254	266		10.1111/jpy.12170	http://dx.doi.org/10.1111/jpy.12170			13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AE0AE	26988183	Green Published			2025-03-11	WOS:000333625100003
J	Quaijtaal, W; Donders, TH; Persico, D; Louwye, S				Quaijtaal, Willemijn; Donders, Timme H.; Persico, Davide; Louwye, Stephen			Characterising the middle Miocene Mi-events in the Eastern North Atlantic realm: A first high-resolution marine palynological record from the Porcupine Basin	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Miocene; Atlantic Ocean; Porcupine Basin; Organic-walled dinoflagellate cysts; Palaeoecology	WALLED DINOFLAGELLATE CYSTS; SEA-LEVEL; ISOTOPE STRATIGRAPHY; NEW-JERSEY; PLIOCENE; CLIMATE; ANTARCTICA; GLACIATION; BIOSTRATIGRAPHY; SEDIMENTATION	The warm climate of the Miocene peaked during the middle Miocene Climatic Optimum (MMCO; 17-14.5 Ma). After the MMCO, global climate went through several short-lived cooling events: the Mi-events (Miocene isotope events). One of the more severe Mi-events is Mi-3, associated with East Antarctic Ice Sheet growth, species turnover in terrestrial and marine realms, Northern Hemisphere and mid-latitude aridification and Antarctic sea-surface temperature cooling. CO2 reconstructions, as well as the aforementioned observations, suggest that a drawdown of CO2 and/or changes in ocean circulation led to the changes surrounding Mi-3. A combination of eccentricity and obliquity amplitude modulation minima, favourable conditions for ice growth, has also been suggested as a possible triggering mechanism. However, an exact cause cannot be pinpointed yet. High-resolution records necessary to investigate the exact order of events surrounding Mi-3 and the possible role of orbital forcing, a very likely trigger, are sparse. Integrated Ocean Drilling Program (IODP) Leg 307 recovered such a high resolution record from the middle Miocene at the Porcupine Basin (offshore south-western Ireland). Well-preserved palynomorphs, mainly organic-walled dinoflagellate cysts, acritarchs and some pollen were extracted from Site U1318, and relative and absolute abundance changes were determined. Using dinocysts and calcareous nannoplankton the age model for the record was improved. Based on the palynology, the Mi-3a, Mi-3b and Mi-4 events were successfully identified and concomitant palaeoenvironmental change was observed. These events, although different in magnitude, can be associated with a decrease in sea-surface temperature, as well as with a likely fall in sea-level. Furthermore, possible palaeoenvironmental preferences of 5 dinocyst taxa were determined, based on observations from the record and multivariate statistics. (C) 2014 Elsevier B.V. All rights reserved.	[Quaijtaal, Willemijn; Louwye, Stephen] Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Donders, Timme H.] Univ Utrecht, Fac Geosci, Dept Phys Geog, NL-3584 CD Utrecht, Netherlands; [Persico, Davide] Univ Parma, Dipartimento Fis Sci Terra M Melloni, I-43124 Parma, Italy	Ghent University; Utrecht University; University of Parma	Quaijtaal, W (通讯作者)，Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, Krijgslaan 28-S8, B-9000 Ghent, Belgium.	willemijn.quaijtaal@ugent.be	Quaijtaal, Willemijn/HNB-5108-2023; Donders, Timme/J-5044-2012; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Persico, Davide/0000-0001-5194-9724; Donders, Timme/0000-0003-4698-3463; Quaijtaal, Willemijn/0000-0001-6016-0194	Research Foundation-Flandres (FWO)	Research Foundation-Flandres (FWO)	We would like to thank Sabine Van Cauwenberghe for technical assistance. Alex Wulbers and Walter Hale are acknowledged for their help during sampling at the Bremen Core Repository. Christian Zeeden and Hemmo Abels are kindly thanked for the useful discussions on the timing of the Mi-events and the age model. David van Rooij is acknowledged for his help regarding sedimentological issues. The comments and suggestions of two anonymous reviewers are appreciated. This research was funded by the Research Foundation-Flandres (FWO).	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Paleoclimatol. Paleoecol.	APR 1	2014	399						140	159		10.1016/j.palaeo.2014.02.017	http://dx.doi.org/10.1016/j.palaeo.2014.02.017			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AF8PP					2025-03-11	WOS:000334978400012
J	Jansson, IM; Mertens, KN; Head, MJ; de Vernal, A; Londeix, L; Marret, F; Matthiessen, J; Sangiorgi, F				Jansson, Ida-Maria; Mertens, Kenneth Neil; Head, Martin J.; de Vernal, Anne; Londeix, Laurent; Marret, Fabienne; Matthiessen, Jens; Sangiorgi, Francesca			Statistically assessing the correlation between salinity and morphology in cysts produced by the dinoflagellate <i>Protoceratium reticulatum</i> from surface sediments of the North Atlantic Ocean, Mediterranean-Marmara-Black Sea region, and Baltic-Kattegat-Skagerrak estuarine system	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						North Atlantic; Model development; Hierarchical partitioning; Collinearity; Operculodinium centrocarpum	PROCESS LENGTH VARIATION; GYMNODINIUM CATENATUM; DISTRIBUTION PATTERNS; CONSERVATION BIOLOGY; HOLOCENE; MODEL; EUTROPHICATION; COMMUNITIES; ASSEMBLAGES; VARIABILITY	Recent studies have correlated dinoflagellate resting cyst morphology to salinity and density variations in the water column, suggesting that morphology can be used for paleoceanographic reconstructions. However, the univariate statistics used by these studies are appropriate only where morphology is related to a single variable. Density is a function of salinity and temperature, so more advanced statistical methods are needed to understand which parameters affect morphology. In this study based on surface (coretop) sediments, a set of environmental variables (sea-surface salinity, temperature, nitrate, and phosphate) was simultaneously correlated to morphological variations seen in resting cysts produced by the dinoflagellate Protoceratium reticulatum (= Operculodinium centrocarpum sensu Wall and Dale). Approximately 3200 measurements were obtained from the North Atlantic Ocean and used to generate a working model based on the Akaike information criterion. Hierarchical partitioning was then applied to establish the independent and joint effects for each predictor variable. Results from these analyses showed that while salinity constitutes the dominant variable affecting process length in the cysts of P. reticulatum in the North Atlantic, it is not the sole explanatory variable and that multicollinearity exists. Temperature and nutrients also showed a significant relationship to the morphology, requiring multiple regression to construct a representative model. The applicability of the North Atlantic working model was finally evaluated by comparing the results to data from the Mediterranean, Marmara, and Black seas, and Baltic-Kattegat-Skagerrak estuarine system. This comparison showed regional differences in morphological-environmental correlation. While salinity constitutes the most important explanatory factor in both the North Atlantic and Baltic-Skagerrak system, this is not so for the Mediterranean-Black Sea region where temperature is the dominant variable. It is concluded that a predictive salinity model based on P. reticulatum cyst morphology has at best a regional application. (C) 2014 Elsevier B.V. All rights reserved.	[Jansson, Ida-Maria; Head, Martin J.] Univ Toronto, Dept Earth Sci, Ctr Earth Sci, Toronto, ON M5S 3B1, Canada; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [de Vernal, Anne] Univ Quebec, GEMOP, Montreal, PQ H3C 3P8, Canada; [Londeix, Laurent] Univ Bordeaux, CNRS, UMR 5805, Dept Geol & Oceanog, F-33405 Talence, France; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Matthiessen, Jens; Sangiorgi, Francesca] Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands	University of Toronto; Ghent University; Brock University; University of Quebec; University of Quebec Montreal; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; University of Liverpool	Jansson, IM (通讯作者)，Univ Toronto, Dept Earth Sci, Ctr Earth Sci, 22 Russell St, Toronto, ON M5S 3B1, Canada.	jansson@es.utoronto.ca	de Vernal, Anne/D-5602-2013; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Marret-Davies, Fabienne/0000-0003-4244-0437; Sangiorgi, Francesca/0000-0003-4233-6154; Matthiessen, Jens/0000-0002-6952-2494; Mertens, Kenneth/0000-0003-2005-9483	University of Toronto; Ontario Graduate Scholarship; NSERC	University of Toronto(University of Toronto); Ontario Graduate Scholarship(Ontario Graduate Scholarship); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	This research was supported by a University of Toronto studentship and scholarship and Ontario Graduate Scholarship to I.-M.J., and an NSERC Discovery Grant to M.J.H. K.N.M. is a postdoctoral fellow of FWO Belgium. Marie-Josee Fortin (University of Toronto) is warmly thanked for her generous advice on numerical ecology. We are grateful to Rehab Elshanawany, Kari Grosfjeld, Rex Harland, Ulrich Kotthoff, Peta Mudie, Speranta Popescu, Vera Pospelova, and Sofia Ribeiro, for the loan of microscope slides. Sample material from the Malangen fjord was provided by the National Lacustrine Core Repository (LacCore). Elisabeth Levac provided samples from Nova Scotia, and Simon Troelstra provided information on Greenland cores and samples from the Mediterranean. Michal Kucera and an anonymous reviewer provided very helpful comments on the manuscript.	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Paleoclimatol. Paleoecol.	APR 1	2014	399						202	213		10.1016/j.palaeo.2014.01.012	http://dx.doi.org/10.1016/j.palaeo.2014.01.012			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	AF8PP					2025-03-11	WOS:000334978400016
J	Liu, TT; Gu, HF; Mertens, KN; Lan, DZ				Liu, Tingting; Gu, Haifeng; Mertens, Kenneth Neil; Lan, Dongzhao			New dinoflagellate species <i>Protoperidinium haizhouense</i> sp. nov. (Peridiniales, Dinophyceae), its cyst-theca relationship and phylogenetic position within the <i>Monovela</i> group	PHYCOLOGICAL RESEARCH			English	Article						Protoperidinium tricingulatum; Protoperidinium americanum; Protoperidinium parthenopes; transitional plate; large subunit ribosomal DNA; cysts; Protoperidinium; archeopyle	MOLECULAR PHYLOGENY; FEEDING-BEHAVIOR; GENUS; ULTRASTRUCTURE; DIPLOPSALIS; ISLANDINIUM; QUATERNARY; DNA	The number of cingular plates has been used to differentiate Protoperidinium from Peridinium and related genera. Protoperidinium is characterized by the presence of three cingular plates plus a transitional plate (3C+t). However, many Protoperidinium species have been described that exhibit different cingular plate tabulations. How these species should be classified within the genus remains unclear. To address this question, the phylogenetic relationship of four Protoperidinium species, with three or four cingular plates and lacking a transitional plate, were examined in relationship to other Protoperidinium species. These four species were germinated from cysts deposited in surface sediments collected from the East China Sea, the Bohai Sea and the Yellow Sea. Three of the isolated species, P. tricingulatum, P. americanum and P. parthenopes, were described previously. The fourth is here described as P. haizhouense sp. nov. with the plate formula Po, X, 4 ', 3a, 7 '', 3C, 6S, 5 ''', 2 ''''. Differences in the cyst stages of these four species, which can be taxonomically informative, were compared. Partial large subunit ribosomal DNA sequences were obtained by single-cell polymerase chain reaction. Maximum-likelihood and Bayesian inference showed that these four species, P. fukuyoi and Islandinium minutum form a monophyletic clade with maximal support. The genus as a whole, however, appeared polyphyletic. Our results suggest that the presence/absence of a transitional plate is significant in the phylogeny of Protoperidinium.	[Liu, Tingting; Gu, Haifeng; Lan, Dongzhao] SOA, Inst Oceanog 3, Xiamen, Peoples R China; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Third Institute of Oceanography, Ministry of Natural Resources; Ghent University	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen, Peoples R China.	haifenggu@yahoo.com	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022	Mertens, Kenneth/0000-0003-2005-9483; Gu, Haifeng/0000-0002-2350-9171	National Science Foundation of China [41376170]	National Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank the associate editor Dr Mona Hoppenrath for constructive suggestions. This project was supported by the National Science Foundation of China (41376170). Kenneth Neil Mertens is a postdoctoral fellow of FWO Belgium.	Abe T. 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Res.	APR	2014	62	2					109	124		10.1111/pre.12041	http://dx.doi.org/10.1111/pre.12041			16	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	AE6QN		Green Published			2025-03-11	WOS:000334118700005
J	Inaba, N; Watanabe, T; Sakami, T; Nishi, H; Tahara, Y; Imai, I				Inaba, Nobuharu; Watanabe, Tsuyoshi; Sakami, Tomoko; Nishi, Hiromi; Tahara, Yoshio; Imai, Ichiro			Temporal and spatial distribution of algicidal and growth-inhibiting bacteria in the coastal sea of southwest Japan	JOURNAL OF PLANKTON RESEARCH			English	Article						algicidal bacteria; growth-inhibiting bacteria; particle-associated bacteria; free-living bacteria; harmful algal blooms	SETO INLAND SEA; RED TIDE; HIROSHIMA BAY; ALEXANDRIUM DINOPHYCEAE; TOXIC DINOFLAGELLATE; GLIDING BACTERIUM; CYST FORMATION; CYTOPHAGA SP; RAPHIDOPHYCEAE; PHYTOPLANKTON	Algicidal and growth-inhibiting bacteria (GIB) are promising tools for mitigating the negative impacts of harmful algal blooms in coastal environments; however, there is a paucity of quantitative data describing their ecological effects. Here, we investigate their temporal and spatial distribution in the southwest Yatsushiro Sea during the summer of 2011, by co-culturing bacterial isolates with an axenic culture of a fish-killing raphidophyte Chattonella antiqua. This novel co-culturing method excludes other biological influences, such as promotion of algal growth by some bacteria. The highest density (1.6 x 10(4) cells mL(-1)) of algicidal bacteria (AB) was detected at the surface of the nearshore station on 3 August 2011 when the maximum chlorophyll a concentration was observed, associated with the high abundance of two centric diatoms, low abundance of dinoflagellates and the absence of C. antiqua. On 10 August, total bacterial abundance increased at 10 m, suggesting that the bacteria used decaying organic matter derived from dead microalgae sinking to the bottom to promote their growth. Most of AB (87.5%) were found to be particle associated, suggesting these bacteria attached to the dead phytoplankton particles after killing them. Two types of GIB impaired co-cultured C. antiqua by inducing unusual cell deformations, including round and elongated cell morphologies. Partial 16S rRNA sequencing showed that algicidal and GIB were mainly comprised of "gamma- and a-proteobacteria". This study provides a new perspective on the dynamics of AB, suggesting that they play a significant role in regulating microalgal composition, physiology and abundance in coastal marine environments.	[Inaba, Nobuharu; Imai, Ichiro] Hokkaido Univ, Plankton Lab, Grad Sch Fisheries Sci, Hakodate, Hokkaido 0418611, Japan; [Watanabe, Tsuyoshi; Sakami, Tomoko] Fisheries Res Agcy, Tohoku Natl Fisheries Res Inst, Shiogama, Miyagi 9850001, Japan; [Nishi, Hiromi; Tahara, Yoshio] Kagoshima Prefectural Fisheries Technol & Dev Ctr, Ibusuki, Kagoshima 8910315, Japan	Hokkaido University; Japan Fisheries Research & Education Agency (FRA)	Inaba, N (通讯作者)，Hokkaido Univ, Plankton Lab, Grad Sch Fisheries Sci, 3-1-1 Minato Cho, Hakodate, Hokkaido 0418611, Japan.	n_inaba84@fish.hokudai.ac.jp; imai1ro@fish.hokudai.ac.jp		Inaba, Nobuharu/0000-0002-5115-0063	Ministry of Agriculture, Forestry and Fisheries of Japan	Ministry of Agriculture, Forestry and Fisheries of Japan(Ministry of Agriculture Forestry & Fisheries - Japan)	This study was supported by a Grant-in-Aid (Marine Metagenomics for Monitoring the Coastal Microbiota) from the Ministry of Agriculture, Forestry and Fisheries of Japan.	Adachi M, 2003, APPL ENVIRON MICROB, V69, P6560, DOI 10.1128/AEM.69.11.6560-6568.2003; Adachi M, 2002, AQUAT MICROB ECOL, V26, P223, DOI 10.3354/ame026223; Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; Agustí S, 1998, LIMNOL OCEANOGR, V43, P1836; [Anonymous], 2001, ASIA PACIFIC EC PROG; CHEN LCM, 1969, J PHYCOL, V5, P211, DOI 10.1111/j.1529-8817.1969.tb02605.x; CRAWFORD DW, 1993, DEV MAR BIO, V3, P389; DELONG EF, 1992, P NATL ACAD SCI USA, V89, P5685, DOI 10.1073/pnas.89.12.5685; Doucette G.J., 1998, NATO ASI Series Series G Ecological Sciences, V41, P619; Ferrier M, 2002, J APPL MICROBIOL, V92, P706, DOI 10.1046/j.1365-2672.2002.01576.x; Hammer BK, 2003, MOL MICROBIOL, V50, P101, DOI 10.1046/j.1365-2958.2003.03688.x; IMAI I, 1991, NIPPON SUISAN GAKK, V57, P1409, DOI 10.2331/suisan.57.1409; Imai I, 1996, FISHERIES SCI, V62, P834, DOI 10.2331/fishsci.62.834; IMAI I, 1993, MAR BIOL, V116, P527, DOI 10.1007/BF00355470; Imai I, 2001, MAR BIOL, V138, P1043, DOI 10.1007/s002270000513; Imai I., 1987, Bull. 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Ecol., V2, P1; Imai I, 2009, P 5 WORLD FISH C; Imai Ichiro, 2006, Plankton & Benthos Research, V1, P71; Imai I, 2002, FISHERIES SCI, V68, P493, DOI 10.2331/fishsci.68.sup1_493; Imai Ichiro, 2013, Bulletin of Fisheries Sciences Hokkaido University, V63, P7; Imai I, 2012, HARMFUL ALGAE, V14, P46, DOI 10.1016/j.hal.2011.10.014; Imai Ichiro, 1998, Phycological Research, V46, P139, DOI 10.1111/j.1440-1835.1998.tb00106.x; JENSEN LM, 1983, MAR ECOL PROG SER, V11, P39; Kim MC, 1998, MAR ECOL PROG SER, V170, P25, DOI 10.3354/meps170025; Liu JQ, 2008, HARMFUL ALGAE, V7, P1, DOI 10.1016/j.hal.2007.04.009; Mayali X, 2004, J EUKARYOT MICROBIOL, V51, P139, DOI 10.1111/j.1550-7408.2004.tb00538.x; Mayali X., 2007, BACTERIAL INFLUENCE, P154; Mayali X, 2008, J PHYCOL, V44, P923, DOI 10.1111/j.1529-8817.2008.00549.x; Nagai S, 1998, PHYCOLOGIA, V37, P363, DOI 10.2216/i0031-8884-37-5-363.1; Nakashima T, 2006, APPL MICROBIOL BIOT, V73, P684, DOI 10.1007/s00253-006-0507-2; NYGAARD K, 1993, LIMNOL OCEANOGR, V38, P273, DOI 10.4319/lo.1993.38.2.0273; Park JH, 2010, AQUAT MICROB ECOL, V60, P151, DOI 10.3354/ame01416; PORTER KG, 1980, LIMNOL OCEANOGR, V25, P943, DOI 10.4319/lo.1980.25.5.0943; Skerratt JH, 2002, MAR ECOL PROG SER, V244, P1, DOI 10.3354/meps244001; Stackebrandt E., 1991, NUCL ACID TECHNIQUES; WOLTER K, 1982, MAR ECOL PROG SER, V7, P287, DOI 10.3354/meps007287; Yoshinaga I, 1997, FISHERIES SCI, V63, P94, DOI 10.2331/fishsci.63.94	37	14	15	2	40	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	MAR-APR	2014	36	2					388	397		10.1093/plankt/fbt119	http://dx.doi.org/10.1093/plankt/fbt119			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	AH9UP		Bronze			2025-03-11	WOS:000336489800008
J	Ismael, A; El-Masry, G; Khadr, A				Ismael, A.; El-Masry, G.; Khadr, A.			Dinoflagellate [cyst] [S1] as signals for eutrophication in the eastern harbour of Alexandria-Egypt	INDIAN JOURNAL OF GEO-MARINE SCIENCES			English	Article						Dinoflagellate cysts; Eutrophication; Eastern Harbour; Egypt	TOKYO-BAY; NORWEGIAN FJORD; COASTAL WATERS; YOKOHAMA-PORT; SEDIMENTS; JAPAN; ASSEMBLAGES; INDICATORS; POLLUTION	Present study provides information about the cyst assemblages as an indication of eutrophication in the harbour. Two sediment core samples were collected from the Eastern Harbour during 2008. Fifteen genera with 26 species were identified from the two cores with total cyst abundance ranging from 138 to 1296 cysts [g-1] [s2] dry wt. Protoperidinium spp. cysts contributed a maximum of 43% to the total cysts, followed by Alexandrium spp. 21% and Diplopsalis cysts with 13%. During this study, six cyst genera with thirteen heterotrophic dinoflagellate species were identified with cyst concentration ranging from 12 to 820 cyst [g-1] [s3] dry wt. Total heterotrophic cyst showed a significant positive correlation with diatoms, sedimentary TP and TN, indicating that increase in diatoms and nutrient concentrations are the main cause of heterotrophic dinoflagellate.	[Ismael, A.; El-Masry, G.; Khadr, A.] Univ Alexandria, Fac Sci, Dept Oceanog, Alexandria 21511, Egypt	Egyptian Knowledge Bank (EKB); Alexandria University	Ismael, A (通讯作者)，Univ Alexandria, Fac Sci, Dept Oceanog, Alexandria 21511, Egypt.	amany_3@yahoo.com	; Ismael, Amany/N-8517-2017	El-Masry, Esraa/0000-0003-3555-986X; Ismael, Amany/0000-0002-3693-3422				ASPILA KI, 1976, ANALYST, V101, P187, DOI 10.1039/an9760100187; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dale B, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; El-Wakeel S, 1957, ICES J Mar Sci, V22, P180, DOI [10.1093/icesjms/22.2.180, DOI 10.1093/ICESJMS/22.2.180]; Fensome R.A., 1993, Micropaleontology Press Special Paper; Folk R. L., 1957, Jour. Sed. Petrol., V27, P3, DOI [10.1306/74d70646-2b21-11d7-8648000102c1865, 10.1306/74D70646-2B21-11D7-8648000102C1865D]; HASSAN AK, 1972, THESIS ALEXANDRIA U; Head M.J., 1996, Palynology: Principles and Applications, P1197; Ismael A. A., 1993, THESIS ALEXANDRIA U; Ismael A. A., 2001, P 9 C HARMF ALG BLOO, V24, P179; Ismael AA, 2003, OCEANOLOGIA, V45, P721; Jacobson DM, 1996, J PHYCOL, V32, P279, DOI 10.1111/j.0022-3646.1996.00279.x; Krumbein WC., 1938, GEOL FOREN STOCK FOR, DOI [10.1080/11035893909452786, DOI 10.1080/11035893909452786]; LABIB W, 1994, P 4 C ENV PROT MUST, P181; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; 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; Matsuoka K., 1987, NATURAL SCI, V28, P35, DOI org/10.1016/0377-8398(94)00016-G; MATSUOKA K, 1985, NAT SCI B, V25, P1; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Mudroch A., 1997, PHYSICOCHEMICAL ANAL; Pospelova V, 2002, J PHYCOL, V38, P593, DOI 10.1046/j.1529-8817.2002.t01-1-01206.x; Pospelova V, 1998, NORGES TEKNISK NATUR, V1, P122; Pospelova V, 2010, MAR MICROPALEONTOL, V76, P37, DOI 10.1016/j.marmicro.2010.04.003; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406	32	5	7	1	5	NATL INST SCIENCE COMMUNICATION-NISCAIR	NEW DELHI	DR K S KRISHNAN MARG, PUSA CAMPUS, NEW DELHI 110 012, INDIA	0379-5136	0975-1033		INDIAN J GEO-MAR SCI	Indian J. Geo-Mar. Sci.	MAR	2014	43	3					365	371						7	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AH0JL					2025-03-11	WOS:000335805100007
J	Wyatt, T; Zingone, A				Wyatt, Timothy; Zingone, Adriana			Population dynamics of red tide dinoflagellates	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Red tides; Harmful algal blooms; Growth; Reproduction	RESTING CYSTS; LIFE-HISTORY; BLOOMS; PATTERNS; PLANKTON; DISTRIBUTIONS; REPRODUCTION; DINOPHYCEAE; MIXOTROPHY; EVOLUTION	Sea-surface discolorations due to high concentrations of phytoplankton are called red tides. Their ecological significance is a long standing puzzle, and they are sometimes considered pathological. Here we propose that many red tides, particularly but not exclusively those composed of certain autotrophic dinoflagellates, are presexual/sexual swarms, essential links in their complex life cycles. This view provides a rationale for the appearance of these organisms in thin surface layers, and helps explain their ephemeral nature. We suggest that further understanding of this phenomenon, and of phytoplankton ecology in general, would benefit from attention to the 'net reproductive value' (r) over the whole life cycle as well as to the division rate (mu) of the vegetative phase. It is argued that r is strategically adapted to seasonal cycles and long term environmental variability, while mu reflects tactical needs (timing) and constraints (grazers, parasites) on vegetative growth. (C) 2013 Elsevier Ltd. All rights reserved.	[Wyatt, Timothy] Inst Invest Marinas Punta Betin, Vigo 36208, Spain; [Zingone, Adriana] Stn Zool Anton Dohrn, I-80121 Naples, Italy	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Stazione Zoologica Anton Dohrn	Wyatt, T (通讯作者)，Inst Invest Marinas Vigo, CE Duardo Cabello 6, E-36208 Vigo, Spain.	twyatt@iim.csic.es	Zingone, Adriana/E-4518-2010	Zingone, Adriana/0000-0001-5946-6532				ALLEN WINFRED EMORY, 1941, AMER MIDLAND NAT, V26, P603, DOI 10.2307/2420738; [Anonymous], COLD SPRING HARB SYM; [Anonymous], LIFEHAB LIFE HIST MI; [Anonymous], ICHA P OCT IN PRESS; Bakun A., 1996, Ocean Process and Marine Population Dynamics, P323; Balch W.M., 1986, Lecture Notes on Coastal and Estuarine Studies, V17, P193; Beaumont HJE, 2009, NATURE, V462, P90, DOI 10.1038/nature08504; BJORNSEN PK, 1991, MAR ECOL PROG SER, V73, P263, DOI 10.3354/meps073263; Burkholder JM, 2008, HARMFUL ALGAE, V8, P77, DOI 10.1016/j.hal.2008.08.010; COHEN D, 1966, J THEOR BIOL, V12, P119, DOI 10.1016/0022-5193(66)90188-3; Crawford DW, 1997, ESTUAR COAST SHELF S, V45, P799, DOI 10.1006/ecss.1997.0242; d'Ovidio F, 2010, P NATL ACAD SCI USA, V107, P18366, DOI 10.1073/pnas.1004620107; Demura M, 2012, PHYCOL RES, V60, P316, DOI 10.1111/j.1440-1835.2012.00662.x; Dickson Robert R., 1995, P70; DROOP MR, 1973, J PHYCOL, V9, P264; Eilertsen HC, 2000, S AFR J MARINE SCI, V22, P323, DOI 10.2989/025776100784125717; Estrada M, 2010, DEEP-SEA RES PT II, V57, P308, DOI 10.1016/j.dsr2.2009.09.007; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Fisher R., 2005, TEACHING CHILDREN TH, V2nd; Franks PJS, 2008, J MARINE SYST, V69, P254, DOI 10.1016/j.jmarsys.2006.03.027; Franks PJS, 2002, J OCEANOGR, V58, P379, DOI 10.1023/A:1015874028196; Genovesi-Giunti B, 2006, VIE MILIEU, V56, P327; Hamilton WD, 1998, ETHOL ECOL EVOL, V10, P1, DOI 10.1080/08927014.1998.9522867; HAMILTON WD, 1964, J THEOR BIOL, V7, P1, DOI 10.1016/0022-5193(64)90039-6; Hense I, 2010, J MARINE SYST, V83, P108, DOI 10.1016/j.jmarsys.2010.02.014; Imai I, 2012, HARMFUL ALGAE, V14, P46, DOI 10.1016/j.hal.2011.10.014; JENKINSON IR, 1992, J PLANKTON RES, V14, P1697, DOI 10.1093/plankt/14.12.1697; Kaitala V, 2001, P ROY SOC B-BIOL SCI, V268, P1769, DOI 10.1098/rspb.2001.1718; KELLER MD, 1989, ACS SYM SER, V393, P167; KIEFER DA, 1975, FISH B-NOAA, V73, P675; Leung TLF, 2012, OIKOS, V121, P641, DOI 10.1111/j.1600-0706.2011.19873.x; LEWIS WM, 1977, ECOLOGY, V58, P850, DOI 10.2307/1936220; Mac Arthur R. 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Part II-Top. Stud. Oceanogr.	MAR	2014	101				SI		231	236		10.1016/j.dsr2.2013.09.021	http://dx.doi.org/10.1016/j.dsr2.2013.09.021			6	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	AE6XQ		Green Submitted			2025-03-11	WOS:000334141700019
J	Czarnecki, JM; Dashtgard, SE; Pospelova, V; Mathewes, RW; MacEachern, JA				Czarnecki, Joanna M.; Dashtgard, Shahin E.; Pospelova, Vera; Mathewes, Rolf W.; MacEachern, James A.			Palynology and geochemistry of channel-margin sediments across the tidal-fluvial transition, lower Fraser River, Canada: Implications for the rock record	MARINE AND PETROLEUM GEOLOGY			English	Article						Dinoflagellate cyst; Pollen; Carbon isotopes; Estuary; Delta; Marginal-marine; McMurray Formation	DINOFLAGELLATE CYST ASSEMBLAGES; RECENT MARINE-SEDIMENTS; ATHABASCA OIL SANDS; NEW-SOUTH-WALES; SURFACE SEDIMENTS; BRITISH-COLUMBIA; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; THECA RELATIONSHIP; ORGANIC-CARBON	In the tidally influenced Fraser River, Canada, palynological and carbon isotope (delta C-13(org)) signatures of channel-margin sediments are compared to environmental parameters (e.g., grain size, water salinity) to establish how the signatures vary across the tidal-fluvial transition. Palynological assemblages in the Fraser River are dominated by tree pollen, which constitutes between 85% and 95% of all assemblages. Dinocyst abundances do not exceed 2% of the total palynological assemblage, and the number and diversity of dinocysts gradually decreases landward. The calculated landward limit for dinocysts is at approximately 83 river km, which is relatively close to the upstream limit of the tidal backwater (at similar to 100 km). delta C-13(org) values show minimal variability across the tidal fluvial transition, and the average value is approximately -26 parts per thousand. The delta C-13(org) signature of river sediments indicates a dominance of terrestrially sourced organic matter regardless of brackish-water and tidal influence on sediment deposition. Six palynological and geochemical trends are identified as relevant to the rock record. 1) In deltaic environments, palynological and geochemical characteristics are less useful than sedimentological and ichnological characteristics for establishing depositional conditions. 2) In marginal-marine settings, low abundances and low species diversities of dinocysts, coupled with a "terrestrial" geochemical signature (delta C-13(org) < -25 parts per thousand.) do not necessarily indicate deposition in a terrestrial environment. 3) Dinocyst abundances above 1% of the total palynomorph population can indicate a significant marine influence on sediment deposition. 4) Mud beds, preferably bioturbated, should be preferentially sampled in order to maximize palynomorph recovery. 5) Marine palynomorphs can occur, albeit in very low concentrations, to the landward limit of the tidal-backwater zone. 6) Palynological and geochemical data should be compared across the paleo-depositional environment in order to establish general trends and remove local variations caused by biases such as grain size. (C) 2013 Elsevier Ltd. All rights reserved.	[Czarnecki, Joanna M.; Dashtgard, Shahin E.; MacEachern, James A.] Simon Fraser Univ, Appl Res Ichnol & Sedimentol ARISE Grp, Dept Earth Sci, Burnaby, BC V5A 1S6, Canada; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada; [Mathewes, Rolf W.] Simon Fraser Univ, Dept Biol Sci, Burnaby, BC V5A 1S6, Canada	Simon Fraser University; University of Victoria; Simon Fraser University	Czarnecki, JM (通讯作者)，Simon Fraser Univ, Appl Res Ichnol & Sedimentol ARISE Grp, Dept Earth Sci, Burnaby, BC V5A 1S6, Canada.	jczarnec@sfu.ca	Dashtgard, Shahin/L-2101-2019	Pospelova, Vera/0000-0003-4049-8133; MacEachern, James/0000-0003-2425-5908; MATHEWES, ROLF/0000-0001-7637-199X	Nexen Energy Inc.; Suncor Energy; Statoil Ltd.; Natural Sciences and Engineering Research Council (NSERC) of Canada	Nexen Energy Inc.; Suncor Energy; Statoil Ltd.; Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	We kindly thank Nexen Energy Inc., Suncor Energy, Statoil Ltd., and the Natural Sciences and Engineering Research Council (NSERC) of Canada for their financial support. Special thanks to Dr. Jeremy Venditti for providing river kilometer data for most sample sites, and to Korhan Ayranci and Andrew La Croix for their invaluable contributions to this study. Lastly, thanks to James Dunlop, Stacy Johnson, Adam Montgomery, Emily Helmer, and Andrea Price for their assistance in the field and laboratory.	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Pet. Geol.	MAR	2014	51						152	166		10.1016/j.marpetgeo.2013.12.008	http://dx.doi.org/10.1016/j.marpetgeo.2013.12.008			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AC8UR					2025-03-11	WOS:000332811100013
J	Chen, L; Xu, GW; Da, XJ; Ji, CJ; Yi, HS				Chen, Lan; Xu, Guiwen; Da, Xuejuan; Ji, Changjun; Yi, Haisheng			Biomarkers of Middle to Late Jurassic marine sediments from a canonical section: New records from the Yanshiping area, northern Tibet	MARINE AND PETROLEUM GEOLOGY			English	Article						Middle to Late Jurassic; Biomarkers; Palaeoenvironment; Yanshiping Group; Tibet	DINOFLAGELLATE CYSTS; QIANGTANG BASIN; NORMAL-ALKANES; SOURCE ROCKS; INDICATORS; DISTRIBUTIONS; HYDROCARBONS; MATURATION; EVOLUTION; PRISTANE	The Yanshiping section, which includes the Quemo Co, Buqu, Xiali, Suowa and Xueshan Formations (Yanshiping Group) exposes organic-rich Middle to Late Jurassic deposits in the Qiangtang Basin of northern Tibet. The biostratigraphic data, from bivalves, brachiopods as well as dinoflagellate cysts, define a Bajocian to Tithonian age. This study focuses on the biomarkers present in these mudstones and limestones to determine the sources, thermal maturity and depositional environment of the organic matter. Most samples show a clear dominance of short-chain (C-15-C-20) n-alkanes with a maximum at C-19 or C-19 with a secondary maximum at C-23 except for the sample BP01(22)S1 where the predominant range is C-22 to C-26 with a maximum at C-24, significant CPI and odd-to-even predominance. The hopanoids and steroids suggest that the sources of organic matter were dominated by phytoplankton, especially algae, as the primary source. Furthermore, the Pr/Ph, Pr/nC(17) and Ph/nC(18), with relatively low values plus high abundance of 17 alpha(H)-hopanes, support deposition in dysoxic to reducing, relatively shallow-water depositional settings, and the presence of gammacerane indicates normal marine salinity and/or water-column stratification. All samples are fairly mature with respect to petroleum generation, a conclusion supported by maturity parameters such as C-31 22S/(22S + 22R) hopanes and C-29 alpha alpha alpha 20S/(20S + 20R) steranes. (C) 2014 Elsevier Ltd. All rights reserved.	[Chen, Lan; Xu, Guiwen; Da, Xuejuan] Chongqing Univ Sci & Technol, Coll Petr Engn, Chongqing 401331, Peoples R China; [Chen, Lan] Univ Oxford, Dept Earth Sci, Oxford OX1 3AN, England; [Ji, Changjun; Yi, Haisheng] Chengdu Univ Technol, Inst Sedimentary Geol, Chengdu 610059, Peoples R China; [Yi, Haisheng] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Peoples R China	Chongqing University of Science & Technology; University of Oxford; Chengdu University of Technology; Chengdu University of Technology	Chen, L (通讯作者)，Chongqing Univ Sci & Technol, Coll Petr Engn, Chongqing 401331, Peoples R China.	cllc-10@163.com			National Natural Science Foundation of China [41102066]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We would like to specially thank the research teams for fieldwork. This work was financially supported by the National Natural Science Foundation of China (Grant NO. 41102066). Hugh Jenkyns helped correct the English text.	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J	Al-Ameri, TK; Najaf, AA; Al-Khafaji, AS; Zumberge, J; Pitman, J				Al-Ameri, Thamer K.; Najaf, Ahmed A.; Al-Khafaji, Amer S.; Zumberge, John; Pitman, Janet			Hydrocarbon potential of the Sargelu Formation, North Iraq	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						North Iraq; Oil biomarkers; Middle Jurassic Sargelu Formation; Source rocks; Cretaceous-Tertiary reservoired oil	GENERATION; KINETICS; KEROGENS	Microscopic and chemical analysis of 85 rock samples from exploratory wells and outcrops in northern Iraq indicate that limestone, black shale and marl within the Middle Jurassic Sargelu Formation contain abundant oil-prone organic matter. For example, one 7-m (23-ft.)-thick section averages 442 mgHC/g S2 and 439 degrees C Tmax (Rock-Eval pyrolysis analyses) and 16 wt.% TOC. The organic matter, comprised principally of brazinophyte algae, dinoflagellate cysts, spores, pollen, foraminiferal test linings and phytoclasts, was deposited in a distal, suboxic to anoxic basin and can be correlated with kerogens classified as type A and type B or, alternatively, as type II. The level of thermal maturity is within the oil window with TAI=3(-) to 3(+), based on microspore colour of light yellowish brown to brown. Accordingly, good hydrocarbon generation potential is predicted for this formation. Terpane and sterane biomarker distributions, as well as stable isotope values, were determined for oils and potential source rock extracts to determine valid oil-to-source rock correlations. Two subfamily carbonate oil types-one of Middle Jurassic age (Sargelu) carbonate rock and the other of Upper Jurassic/Cretaceous age-as well as a different oil family related to Triassic marls, were identified based on multivariate statistical analysis (HCA and 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 R-28 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. One-dimension petroleum system models of key wells were developed using IES PetroMod Software to evaluate burial-thermal history, source-rock maturity and the timing and extent of petroleum generation; interpreted well logs served as input to the models. The oil-generation potential of sulphur-rich Sargelu source rocks was simulated using closed system type II-S kerogen kinetics. Model results indicate that throughout northern Iraq, generation and expulsion of oil from the Sargelu began and ended in the late Miocene. At present, Jurassic source rocks might have generated and expelled between 70 % and 100 % of their total oil.	[Al-Ameri, Thamer K.] Univ Baghdad, Coll Sci, Dept Geol, Jadiriyah, Iraq; [Najaf, Ahmed A.] Univ Al Nahrain, Coll Sci, Dept Chem, Baghdad, Iraq; [Al-Khafaji, Amer S.] Univ Babylon, Coll Sci Woman, Dept Chem, Hilla, Iraq; [Zumberge, John] GeoMark Res Ltd, Houston, TX 77095 USA; [Pitman, Janet] US Geol Survey, Denver, CO 80225 USA; [Najaf, Ahmed A.] Univ Al Nahrain, Baghdad, Iraq	University of Baghdad; Al-Nahrain University; University of Babylon; United States Department of the Interior; United States Geological Survey; Al-Nahrain University	Najaf, AA (通讯作者)，Univ Al Nahrain, Baghdad, Iraq.	drahmedaskar@yahoo.com	Najaf, Ahmed/AAJ-5602-2021; /B-9812-2016	Al Ahmed, Ahmed/0000-0003-2526-1015; /0000-0001-8489-394X				Al-Ahmed A. A. 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J. Geosci.	MAR	2014	7	3					987	1000		10.1007/s12517-013-0875-8	http://dx.doi.org/10.1007/s12517-013-0875-8			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AC4JS					2025-03-11	WOS:000332487800012
J	Aydin, H; Uzar, S				Aydin, Hilal; Uzar, Serdar			Distribution and abundance of modern dinoflagellate cysts from Marmara, Aegean and Eastern Seas of Turkey	JOURNAL OF ENVIRONMENTAL BIOLOGY			English	Article						Dinoflagellate cysts; Izmir Bay; Marmara Sea; Surface sediment; Toxic species	SURFACE SEDIMENTS; IZMIR BAY; RESTING CYSTS; ASSEMBLAGES; COAST; EUTROPHICATION; ALEXANDRIUM	Twenty-one surface sediment samples were collected from coastal areas of Turkey to determine horizontal distribution and abundance of the cysts. A total of 40 dinoflagellate cyst types were identified and recorded in the range of 34 and 31532 cyst g(-1) d.wt. in the sediments. The concentration of Lingulodinium machaerophorum, Polykrikos kofoidil, Quinquecuspis concreta, Dubridinium caperatum and Spiniferites bulloideus cysts dominated over other species. Although cysts of potentially toxic species of Alexandrium affine type and A. catenelleamarense complex were found only in Izmir Bay. A. minutum type, Lingulodinium machaerophorum and Operculodinium centrocarpum were observed in the surface sediments of Marmara Sea and Fethiye Bay. The present study provides a database on the distribution and composition of dinoflagellate cysts in the Eastern Mediterranean sea coastal waters of Turkey where modern dinoflagellate cysts have been little studied.	[Aydin, Hilal; Uzar, Serdar] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Manisa, Turkey	Celal Bayar University	Aydin, H (通讯作者)，Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Manisa, Turkey.	hilalaydin66@gmail.com	UZAR, SERDAR/G-9956-2014	UZAR, SERDAR/0000-0002-9477-7413	Scientific Investigation Project to Coordinate of Celal Bayar University [FEF2008-004]	Scientific Investigation Project to Coordinate of Celal Bayar University(Celal Bayar University)	We wish to thank Hulya Caner (Istanbul University) who helped in collection of sediment samples from Marmara sea. The author thanks to Scientific Investigation Project to Coordinate of Celal Bayar University (Project No. FEF2008-004) for financial support. This study contains a part of Master dissertation prepared by Serdar Uzar in Celal Bayar University.	Aydin H, 2011, MAR MICROPALEONTOL, V80, P44, DOI 10.1016/j.marmicro.2011.03.004; Balkis Neslihan, 2004, Journal of the Black Sea Mediterranean Environment, V10, P123; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Buyukisik B., 1994, EGE U FACULTY SCI J, V16, P1161; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; Estrada M, 2010, DEEP-SEA RES PT II, V57, P308, DOI 10.1016/j.dsr2.2009.09.007; Feyzioglu Ali Muzaffer, 2006, Turkish Journal of Botany, V30, P375; Gencay H.A., 2004, EGE U J FISHERIES AQ, V21, P107; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Joyce LB, 2005, HARMFUL ALGAE, V4, P309, DOI 10.1016/j.hal.2004.08.001; Kim Hyeung-Sin, 1998, Bulletin of Plankton Society of Japan, V45, P133; Kim SY, 2009, ESTUAR COAST, V32, P1225, DOI 10.1007/s12237-009-9212-6; Koray Tufan, 2001, Su Urunleri Dergisi, V18, P1; Kucuksezgin F, 2006, ENVIRON INT, V32, P41, DOI 10.1016/j.envint.2005.04.007; 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, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Matsuoka K., 2004, ATLAS MODERN DINOFLA; Mudie PJ, 2004, REV PALAEOBOT PALYNO, V128, P143, DOI 10.1016/S0034-6667(03)00117-9; 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; Ribeiro S, 2008, MAR MICROPALEONTOL, V68, P156, DOI 10.1016/j.marmicro.2008.01.013; Rubino F, 2010, DEEP-SEA RES PT II, V57, P243, DOI 10.1016/j.dsr2.2009.09.011; Sabanci F.C., 2005, EUJ FISH AQUAT SCI, V22, P273; Sangiorgi F, 2005, ESTUAR COAST SHELF S, V64, P395, DOI 10.1016/j.ecss.2005.03.005; Sangiorgi F, 2004, ESTUAR COAST SHELF S, V60, P69, DOI 10.1016/j.ecss.2003.12.001; Sayin E, 2003, CONT SHELF RES, V23, P957, DOI 10.1016/S0278-4343(03)00083-9; 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; Tüfekci V, 2010, TURK J BIOL, V34, P199, DOI 10.3906/biy-0812-1; Uzar S, 2010, SCI RES ESSAYS, V5, P285; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	35	13	14	1	7	TRIVENI ENTERPRISES	LUCKNOW	C/O KIRAN DALELA, 1/206 VIKAS NAGAR, KURSI RD, LUCKNOW 226 022, INDIA	0254-8704			J ENVIRON BIOL	J.Environ.Biol.	MAR	2014	35	2					413	419						7	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	AC4OG	24665771				2025-03-11	WOS:000332500000018
J	Crouch, EM; Willumsen, PS; Kulhanek, DK; Gibbs, SJ				Crouch, Erica M.; Willumsen, Pi Suhr; Kulhanek, Denise K.; Gibbs, Samantha J.			A revised Paleocene (Teurian) dinoflagellate cyst zonation from eastern New Zealand	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cyst; Paleocene; Teurian; New Zealand; zonation; systematics	MID-WAIPARA RIVER; CRETACEOUS/TERTIARY BOUNDARY; SOUTHWEST PACIFIC; PALEOCEANOGRAPHIC SIGNIFICANCE; ENVIRONMENTAL-CHANGE; NORTH CANTERBURY; CLARENCE VALLEY; SOUTHERN-OCEAN; CARBON-CYCLE; SEA-LEVEL	Organic-walled dinoflagellate cyst (dinocyst) assemblages are documented from Paleocene (New Zealand Teurian Stage) sediments in five sections from eastern New Zealand: Tawanui, Angora Road and Toi Flat-1 core in the East Coast Basin, mid-Waipara River in the Canterbury Basin, and ODP Site 1121 on the eastern margin of Campbell Plateau. Based on dinocyst results from these sections, along with published earliest Paleocene records from the East Coast, Canterbury and Great South Basins, a revised Paleocene (Teurian) dinocyst zonation is proposed. The zones are labelled as NZDP - New Zealand Dinocyst Paleocene - and are all interval zones. The eight zones, NZDP1 to NZDP8, encompass the entire Paleocene, from the Cretaceous-Paleogene boundary at 66.04 Ma to the Paleocene-Eocene boundary at 55.96 Ma. Correlation of the NZDP zones with the International and New Zealand Time Scales is provided, and is primarily based on correlation with calcareous nannofossil biostratigraphy. Three new dinocyst species are described: Leptodinium? pustulatum sp. nov., Cerodinium angulatum sp. nov., and Vozzhennikovia towanuiensis sp. nov. (C) 2013 Elsevier B.V. All rights reserved.	[Crouch, Erica M.; Kulhanek, Denise K.] GNS Sci, Dept Paleontol, Lower Hutt 5040, New Zealand; [Willumsen, Pi Suhr] MUSERUM, Nat Hist Div, DK-7800 Skive, Denmark; [Willumsen, Pi Suhr] Aarhus Univ, Dept Geosci, DK-8000 Aarhus C, Denmark; [Kulhanek, Denise K.] Texas A&M Univ, Integrated Ocean Drilling Program, College Stn, TX 77845 USA; [Gibbs, Samantha J.] Univ Southampton, Sch Ocean & Earth Sci, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England	GNS Science - New Zealand; Aarhus University; Texas A&M University System; Texas A&M University College Station; NERC National Oceanography Centre; University of Southampton	Crouch, EM (通讯作者)，GNS Sci, Dept Paleontol, POB 30368, Lower Hutt 5040, New Zealand.	e.crouch@gns.cri.nz	Crouch, Erica/C-2820-2013	Kulhanek, Denise/0000-0002-2156-6383	GNS Science research programmes Global Change; Tithe; Petroleum Basin Research; MUSERUM, Skive, Denmark	GNS Science research programmes Global Change; Tithe; Petroleum Basin Research; MUSERUM, Skive, Denmark	We thank Brad Field, Chris Hollis, Hugh Morgans, Ian Raine, Percy Strong, and Michael Tayler for sample collection. Sonja Fry, Randall McDonnell and Roger Tremain are thanked for sample preparation and palynology and nannofossil processing. Assistance with dinocyst systematics from Henk Brinkhuis, Poul Schioler and Graeme Wilson was greatly appreciated. Peter Bijl is thanked for access to ODP Site 1172 dinocyst data and on-going discussions. Discussions and comments by Chris Hollis and Poul Schioler greatly improved the manuscript. EMC and DKK acknowledge support from GNS Science research programmes Global Change with Tithe, and Petroleum Basin Research. PSW acknowledges financial support by MUSERUM, Skive, Denmark. We thank Peter Bijl and Michael Hannah for constructive reviews.	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J	Roje-Busatto, R; Ujevic, I				Roje-Busatto, Romana; Ujevic, Ivana			PSP toxins profile in ascidian <i>Microcosmus vulgaris</i> (Heller, 1877) after human poisoning in Croatia (Adriatic Sea)	TOXICON			English	Article						Paralytic Shellfish Poisoning; Ascidian; Microcosmus; Adriatic Sea; Human intoxication; HPLC-FLD	HARMFUL ALGAL BLOOMS; PARALYTIC SHELLFISH TOXINS; ALEXANDRIUM-TAMARENSE; GYMNODINIUM-CATENATUM; LIQUID-CHROMATOGRAPHY; CULTURE STRAINS; RESTING CYSTS; DINOFLAGELLATE; MUSSELS; DINOPHYCEAE	Toxins known to cause Paralytic Shellfish Poisoning (PSP) syndrome in humans that can have serious economic consequences for aquaculture were determined in ascidians of the genus Microcosms. Significant concentrations of toxins were confirmed in all tested samples collected from the western coast of Istria Peninsula (Adriatic Sea, Croatia) when six people were poisoned following the consumption of fresh ascidians. Several species of bivalves that were under continuous monitoring had not accumulated PSP toxins although they were exposed to the same environmental conditions over the survey period. In the present study, HPLC-FLD with pre-column oxidation of PSP toxins has been carried out to provide evidence for the first human intoxication due to consumption of PSP toxic ascidians (Microcosmus vulgaris, Heller, 1877) harvested from the Adriatic Sea. Qualitative analysis established the presence of six PSP toxins: saxitoxin (SIX), decarbamoylsaxitoxin (dcSTX), gonyautoxins 2 and 3 (GTX2,3), decarbamoylgonyautoxins 2 and 3 (dcGTX2,3), gonyautoxin 5 (GTX5) and N-sulfocarbamoylgonyautoxins 1 and 2 (C1,2), while quantitative analysis suggested SIX and GTX2,3 as dominant toxin types and the ones that contribute the most to the overall toxicity of these samples with concentrations near the regulatory limit. (C) 2014 Elsevier Ltd. All rights reserved.	[Roje-Busatto, Romana; Ujevic, Ivana] Inst Oceanog & Fisheries, Split 21000, Croatia	Croatian Institute of Oceanography & Fisheries (IZOR)	Ujevic, I (通讯作者)，Inst Oceanog & Fisheries, Setaliste I Mestrovica 63,POB 500, Split 21000, Croatia.	rroje@izor.hr; ujevic@izor.hr	; Roje-Busatto, Romana/GQB-0704-2022	Ujevic, Ivana/0000-0001-6686-1418; Roje-Busatto, Romana/0000-0002-9270-6646	Erasmus Mundus Master of Science in Marine Biodiversity and Conservation; Croatian Ministry of Science, Education and Sports of the Republic of Croatia [001-0010501-0848]	Erasmus Mundus Master of Science in Marine Biodiversity and Conservation; Croatian Ministry of Science, Education and Sports of the Republic of Croatia(Ministry of Science, Education and Sports, Republic of Croatia)	Erasmus Mundus Master of Science in Marine Biodiversity and Conservation scholarship and the Croatian Ministry of Science, Education and Sports of the Republic of Croatia (through the grant 001-0010501-0848) supported this study.	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J	Onishi, Y; Mohri, Y; Tuji, A; Ohgi, K; Yamaguchi, A; Imai, I				Onishi, Yuka; Mohri, Yuka; Tuji, Akihiro; Ohgi, Kohei; Yamaguchi, Atsushi; Imai, Ichiro			The seagrass <i>Zostera marina</i> harbors growth-inhibiting bacteria against the toxic dinoflagellate <i>Alexandrium tamarense</i>	FISHERIES SCIENCE			English	Article						Toxic blooms; Alexandrium tamarense; Algicidal bacteria; Seagrass; Zostera marina; Mitigation; Prevention	HETEROSIGMA-AKASHIWO RAPHIDOPHYCEAE; SETO INLAND SEA; RED TIDE; ALGICIDAL BACTERIA; HIROSHIMA BAY; POPULATION-STRUCTURE; GLIDING BACTERIUM; CYST FORMATION; CYTOPHAGA SP; BLOOMS	Seagrasses are known to have allelopathic activity to reduce growth of phytoplankton. We found growth-inhibiting bacteria (strains E8 and E9) from Zostera marina possessing strong activity against the toxic dinoflagellate Alexandrium tamarense. Strain E9 markedly inhibited growth of A. tamarense even with initial inoculum size as small as 2.9 cells ml(-1). This bacterium also had growth-inhibiting effects on the red-tide raphidophytes Chattonella antiqua and Heterosigma akashiwo, the dinoflagellate Heterocapsa circularisquama, and the diatom Chaetoceros mitra. Small subunit (SSU) ribosomal DNA (rDNA) sequencing analysis demonstrated that the most probable affiliation of these strains was Flavobacteriaceae, and proved that another inhibitory bacterial strain (E8) was the same species as strain E9. Two other bacterial strains (E4-2 and E10), showing different colony color and isolated from the same seagrass sample, revealed no growth-inhibiting activity. Interestingly, strain E4-2 showed the same sequences as E8 and E9 (100 %), and strain E10 matched E8 and E9 with 99.80 % similarity. Growth-inhibiting bacteria against the toxic dinoflagellate Alexandrium tamarense associated with seagrass, such as Flavobacterium spp. E8 and E9, are able to repress shellfish poisoning besides the allelopathic activity of seagrass itself.	[Onishi, Yuka; Ohgi, Kohei; Yamaguchi, Atsushi; Imai, Ichiro] Hokkaido Univ, Plankton Lab, Grad Sch Fisheries Sci, Hakodate, Hokkaido 0418611, Japan; [Mohri, Yuka; Tuji, Akihiro] Natl Museum Nat & Sci, Dept Bot, Tsukuba, Ibaraki 3050005, Japan	Hokkaido University; National Museum of Nature and Science	Imai, I (通讯作者)，Hokkaido Univ, Plankton Lab, Grad Sch Fisheries Sci, 3-1-1 Minato Cho, Hakodate, Hokkaido 0418611, Japan.	imai1ro@fish.hokudai.ac.jp	Tuji, Akihiro/K-7400-2019; Yamaguchi, Atsushi/A-8613-2012	Yamaguchi, Atsushi/0000-0002-5646-3608	Hakodate Green Innovation of UMI (Universal Marine Industry)	Hakodate Green Innovation of UMI (Universal Marine Industry)	We are grateful to Dr. Hiroyuki Munehara of Usujiri Marine Station, Field Science Center for Northern Biosphere, Hokkaido University, for his kind arrangement of seagrass sampling. We thank Mr. Kiyoshi Nomura for his technical assistance for sampling at Usujiri Port. This study was supported in part by the project of Hakodate Green Innovation of UMI (Universal Marine Industry).	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Sci.	MAR	2014	80	2					353	362		10.1007/s12562-013-0688-4	http://dx.doi.org/10.1007/s12562-013-0688-4			10	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	AD9VU					2025-03-11	WOS:000333613500027
J	Miettinen, A; Head, MJ; Knudsen, KL				Miettinen, Arto; Head, Martin J.; Knudsen, Karen Luise			Eemian sea-level highstand in the eastern Baltic Sea linked to long-duration White Sea connection	QUATERNARY SCIENCE REVIEWS			English	Article						Eemian interglacial; Sea level; Diatoms; Dinoflagellate cysts; Foraminifera; Baltic Sea; White sea	LAST INTERGLACIAL PERIOD; NORTH-ATLANTIC; SOUTH DENMARK; HYDROGRAPHIC CONDITIONS; DINOFLAGELLATE CYSTS; PYROPHACUS-STEINII; MOLLUSK FAUNAS; RISTINGE KLINT; POHJA-UHTJU; ICE-SHEET	Revised diatom and new dinoflagellate cyst and benthic foraminiferal data from the eastern Baltic Sea have refined our understanding of Eemian (Last Interglacial; 131-119.5 ka) sea-level change on the Russian Karelia, a former seaway linking the Baltic to the White Sea. Results from Peski, eastern Baltic show the initiation of marine conditions just before 131 ka in the latest Saalian, after the opening of a connection to the North Sea. Following the onset of the Eemian marine highstand and the opening of the White Sea connection at around 130.25 ka, near-fully marine conditions persisted in the eastern Baltic area for ca 6 kyr, until ca 124 ka. For most of the Eemian, a strong thermal stratification in the eastern Baltic resulted from an Arctic and possible North Atlantic water component from the White Sea merging with warmer waters from the North Sea. From ca 124 ka, decreasing salinity indicates the end of the marine highstand and a simultaneous closure of the Baltic Sea-White Sea connection, i.e. a duration of ca 6 kyr for this seaway. The main influence of White Sea inflow appears to be restricted to the eastern Baltic area, although a large submerged area in the Russian Karelia associated with temperate Atlantic waters could have assisted in creating a more oceanic climate for Central Europe. (C) 2013 Elsevier Ltd. All rights reserved.	[Miettinen, Arto] Univ Helsinki, Dept Geosci & Geog, FI-00014 Helsinki, Finland; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Knudsen, Karen Luise] Aarhus Univ, Dept Geosci, DK-8000 Aarhus C, Denmark	University of Helsinki; Brock University; Aarhus University	Miettinen, A (通讯作者)，Univ Helsinki, Dept Geosci & Geog, POB 64, FI-00014 Helsinki, Finland.	arto.miettinen@helsinki.fl	Knudsen, Karen/A-4849-2012; Miettinen, Arto/AAG-2835-2019; Miettinen, Arto/E-2458-2013	Miettinen, Arto/0000-0003-4537-2556	European Commission's Environment and Climate Programme project Palaeoenvironment and Palaeoclimatic Evolution of the Baltic Sea during the Last Interglacial (Eemian, Mikulino) BALTEEM [ENV4-CT98-0809]; Natural Sciences and Engineering Research Council of Canada Discovery Grant	European Commission's Environment and Climate Programme project Palaeoenvironment and Palaeoclimatic Evolution of the Baltic Sea during the Last Interglacial (Eemian, Mikulino) BALTEEM; Natural Sciences and Engineering Research Council of Canada Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC))	The initial phase of this research was financed by the European Commission's Environment and Climate Programme project Palaeoenvironment and Palaeoclimatic Evolution of the Baltic Sea during the Last Interglacial (Eemian, Mikulino) BALTEEM (ENV4-CT98-0809) under the leadership of P.L. Gibbard (University of Cambridge, U.K.). M.J.H. acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. We thank two anonymous reviewers for their constructive comments.	Andersen C, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2002PA000873; Andersen S.T. R., 1966, Palaeobotanist, V15, P117; Anderson P, 2006, QUATERNARY SCI REV, V25, P1383, DOI 10.1016/j.quascirev.2006.01.033; [Anonymous], 1975, Danm. Geol. Undersog. 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Sci. Rev.	FEB 15	2014	86						158	174		10.1016/j.quascirev.2013.12.009	http://dx.doi.org/10.1016/j.quascirev.2013.12.009			17	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	AB7SN					2025-03-11	WOS:000331991100012
J	Adriaens, R; Vandenberghe, N; Elsen, J				Adriaens, R.; Vandenberghe, N.; Elsen, J.			NATURAL CLAY-SIZED GLAUCONITE IN THE NEOGENE DEPOSITS OF THE CAMPINE BASIN (BELGIUM)	CLAYS AND CLAY MINERALS			English	Article						Belgium; Clay-sized Glauconite; Neogene; Transport	NORTH-SEA BASIN; DINOFLAGELLATE CYSTS; SOUTHERN BORDER; MIOCENE; SHALLOW; MIDDLE; ILLITE; STRATIGRAPHY; SEDIMENTS; EXAMPLES	Natural clay-sized glauconite has the same mineralogical composition as sand-sized glauconite pellets but occurs in <2 pm clay fractions. This particular glauconite habit has been described previously from soil environments resulting from pelletal weathering but is rarely reported in higher-energy sedimentary environments. In the present study, clay-sized glauconite was identified as a common constituent in transgressive Neogene glauconite pellet-rich deposits of the southern North Sea in Belgium. X-ray diffraction results revealed that the characteristics of the clay-sized glauconite are very similar to the associated glauconite pellets in sand deposits. Both glauconite types consisted of two glauconite-smectite R1 phases with generally small percentages of expandable layers (<30%) with d(060) values ranging between 1.513 angstrom and 1.519 angstrom. Clay-sized glauconite was not neoformed but formed by the disintegration of sand-sized glauconite pellets which were abraded or broken up during short-distance transport within the sedimentary basin or over the hinterland. Even in an environment where authigenic glauconite pellets occur, minimal transport over transgressive surfaces is sufficient to produce clay-sized glauconite. Furthermore, clay-sized glauconite can be eroded from marine deposits and subsequently resedimented in estuarine deposits. Clay-sized glauconite is, therefore, a proxy for the transport intensity of pelletal glauconite in energetic depositional environments and, moreover, indicates reworking in such deposits which lack pelletal glauconite.	[Adriaens, R.; Vandenberghe, N.; Elsen, J.] Univ Leuven, Dept Earth & Environm Sci, B-3000 Leuven, Belgium	KU Leuven	Adriaens, R (通讯作者)，Univ Leuven, Dept Earth & Environm Sci, Celestijnenlaan 200E, B-3000 Leuven, Belgium.	rieko.adriaens@ees.kuleuven.be	elsen, jan/AAB-9873-2021	elsen, jan/0000-0002-4370-3852				Adriaens R., 2009, THESIS U LEUVEN LEUV; AMOROSI A, 1995, J SEDIMENT RES B, V65, P419; Amorosi A, 1997, SEDIMENT GEOL, V109, P135, DOI 10.1016/S0037-0738(96)00042-5; [Anonymous], 1985, DEV SEDIMENTOLOGY; [Anonymous], 1989, CLAY SEDIMENTOLOGY, DOI 10.1007/978-3-642-85916-8; [Anonymous], 1998, X-Ray diffraction and the identification and analysis of clay minerals, DOI DOI 10.1016/S0012-8252(97)00020-2; [Anonymous], 1994, B SOC BELGE GEOLOGIE; [Anonymous], 1988, Rev. 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FEB-APR	2014	62	1-2					35	52		10.1346/CCMN.2014.0620104	http://dx.doi.org/10.1346/CCMN.2014.0620104			18	Chemistry, Physical; Geosciences, Multidisciplinary; Mineralogy; Soil Science	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Geology; Mineralogy; Agriculture	AM4WZ					2025-03-11	WOS:000339858200004
J	Radmacher, W; Tyszka, J; Mangerud, G				Radmacher, Wieslawa; Tyszka, Jaroslaw; Mangerud, Gunn			Distribution and biostratigraphical significance of <i>Heterosphaeridium bellii</i> sp nov and other Late Cretaceous dinoflagellate cysts from the southwestern Barents Sea	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						palynology; dinoflagellate cyst; Barents Sea; Campanian	AGGLUTINATED FORAMINIFERA; PALEOCENE; PALYNOLOGY; SUCCESSION; EVOLUTION; BASIN	A palynological study of the Upper Cretaceous Kveite Formation and Lower Palaeogene Torsk Formation in two exploration wells from the southwestern Barents Sea is presented. The investigation has revealed an interval characterised by the acme of a new dinoflagellate cyst species Heterosphaeridium bellii sp. nov. Its calibration to a comparable Heterosphaeridium event in ammonite-dated strata from the Western Interior Basin of North America supports the Late Campanian age. An emendation of Heterosphaeridium heteracanthum is provided in order to emphasize the differences between both Heterosphaeridium species. The Turonian to Coniacian age is based on the last common occurrence (LCO) of Heterosphaeridium difficile and the last occurrence (LO) of Stephodinium coronatum. The Early Campanian is established based on the last occurrence of Callaiosphaeridium asymmetricum, Chatangiella bondarenkoi and Palaeoglenodinium cretaceum. The Late Campanian to Early Maastrichtian age is suggested by the last common occurrence of the new species H. bellii, the last occurrence of Odontochitina operculata and common occurrence of Spongodinium delitiense. The last occurrence of Raetiaedinium truncigerum occurs within this interval coinciding with the last super abundant occurrence (LSAO) of H. bellii sp. nov. The palynological events are put alongside geophysical logs to check the validity of the correlation. The study documents several hiatuses, indicating that Upper Cenomanian, Santonian, Middle Campanian, Upper Maastrichtian and lowermost Palaeocene strata are missing in well 7120/7-3, whereas strata of Upper Cenomanian to Santonian and Upper Maastrichtian to lowermost Palaeocene age seem to be missing in well 7119/9-1. The interval represented by the acme of the new gonyaulacacean species H. bellii is considered here to be a useful Late Campanian biostratigraphic marker horizon. (C) 2013 Elsevier B.V. All rights reserved.	[Radmacher, Wieslawa; Tyszka, Jaroslaw] Polish Acad Sci, ING PAN, Inst Geol Sci, Krakow Res Ctr,BioGeoLab, PL-31002 Krakow, Poland; [Radmacher, Wieslawa; Mangerud, Gunn] Univ Bergen, Dept Earth Sci, NO-5020 Bergen, Norway	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; University of Bergen	Radmacher, W (通讯作者)，OBK, ING PAN, Ul Senacka 1, PL-31002 Krakow, Poland.	ndkrol@cyf-kr.edu.pl; ndtyszka@cyf-kr.edu.pl; Gunn.Mangerud@geo.uib.no	Radmacher, Wiesława/ABH-7042-2020; Mangerud, Gunn/ABD-2588-2020	Radmacher, Wieslawa/0000-0001-7316-3693	EEA Financial Mechanism; Norwegian Financial Mechanism; ING PAN internal "MIKRO" project	EEA Financial Mechanism; Norwegian Financial Mechanism; ING PAN internal "MIKRO" project	The authors would like to thank the Norwegian Petroleum Directorate for the loan of palynological slides and Statoil for providing samples. We are grateful for the help of Henk Brinkhuis, Jan van Tongeren and Natasja Welters from the Laboratory of Palaeobotany and Palynology in Utrecht, where some of the samples were processed. We are also grateful to the following people for their help in various stages of the project: Graham Bell, Martin Pearce, Mike Kaminski, Przemyslaw Gedl, Eiichi Setoyama and Stijn de Schepper. WR was co-financed by technical assistance funds of the EEA Financial Mechanism and the Norwegian Financial Mechanism within the framework of the Scholarship and Training Fund. JT was supported by the ING PAN internal "MIKRO" project. The authors acknowledge the reviewers for their detailed and helpful comments on the manuscript.	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Palaeobot. Palynology	FEB	2014	201						29	40		10.1016/j.revpalbo.2013.10.003	http://dx.doi.org/10.1016/j.revpalbo.2013.10.003			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AB3HS					2025-03-11	WOS:000331682500003
J	Ali, MO				Ali, Maysoon Omar			Palynological evidences on paleoclimate and paleoenvironmental changes during Holocene of Al-Hussaynia District, Central Iraq	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Palynology; Paleoclimate; Paleoenvironmental; Hussaynia; Iraq		This paper is concerned with the study of paleoclimate and paleoenvironmental changes of Hussaynia township which is located in Karbala at the center of the Mesopotamian plain during Holocene. Ten soil samples were examined to determine their content of pollens, spores, and marine organisms (dinoflagellates). These palynomorphs include: Graminidites, Palmaepollenites, <Emphasis Type="ItalicUnderline">Chenopodiaceae, Composita, <Emphasis Type="ItalicUnderline">Cyperaceae, Sphaginum sporites, Pinus pollenites, Convovolus, Artimesia, Laevigatosporites, Quercus, dinoflagellates, and fungi. The study revealed climatic and environmental changes in the area during Holocene and four climatic zones were determined in the studied sequence and correlated with other areas in and outside of Iraq. The climate was pluvial with intervening dry periods in the 10000 years bp. The study indicated as well, some marine effects on the studied area on the commencement of Holocene due to the global transgression. This is based on the presence of marine organisms, dinoflagellate.	Univ Baghdad, Coll Sci, Dept Earth Sci, Baghdad, Iraq	University of Baghdad	Ali, MO (通讯作者)，Univ Baghdad, Coll Sci, Dept Earth Sci, Baghdad, Iraq.	m.geo_99@yahoo.com						Abboud IA, 1999, THESIS U BAGHDAD; Al-Ameri TK, 2007, AR SEA INT C SCI TEC; Al-Dulaimy AS, 1999, THESIS U BAGHDAD; Al-Tawash BS, 1996, THESIS U BAGHDAD; Ali MO, 2005, THESIS U BAGHDAD; Aqrawi AAM, 1993, THESIS U LONDON; Bars MS, 1977, GEOL SURV CANADA, V73, P25; Benni TJ, 2001, THESIS U BAGHDAD; Buday T, 1987, REGIONAL GEOLOGY IRA, V2; El-Muslimany AP, 1994, LATE QUATERNARY CHRO, P1; El-Muslimany AP, 1990, REV PALAEOBOT PALYNO, V64, P343; El-Muslimany AP, 1986, VEGETATION, V68, P55; El-Muslimany AP, 1987, VEGETATION, V72, P131; Euphrates Center for Irrigation Studies and Designations, 1995, LOW LEV GROUND WAT K, P10; HARRISON SP, 1993, QUATERNARY SCI REV, V12, P233, DOI 10.1016/0277-3791(93)90079-2; Jassim RZ, 2007, GEOSURV BAGHDAD, V3, P1; Jassim S.Z., 2006, GEOLOGY IRAQ DOLIN S; McClure H. A., 1984, Doctoral dissertation; van Zeist W., 1977, PALAEOHISTORIA, V19, P19, DOI [10.1191/0959683605hl846rp, DOI 10.1191/0959683605HL846RP]; YAN ZW, 1994, PALAEOGEOGR PALAEOCL, V110, P217, DOI 10.1016/0031-0182(94)90085-X	20	3	3	1	3	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	FEB	2014	7	2					589	595		10.1007/s12517-012-0801-5	http://dx.doi.org/10.1007/s12517-012-0801-5			7	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AA3HF					2025-03-11	WOS:000330982800014
J	Lundholm, N; Nielsen, LR; Ribeiro, S; Ellegaard, M				Lundholm, Nina; Nielsen, Lene Rostgaard; Ribeiro, Sofia; Ellegaard, Marianne			Microsatellite markers for the palaeo-temperature indicator <i>Pentapharsodinium dalei</i> (Dinophyceae)	JOURNAL OF APPLIED PHYCOLOGY			English	Article						Dinoflagellate; Global change; Microsatellites; Multiplex PCR; Pentapharsodinium dalei; Population genetics; Sediment; Temperature	LOCI; SOFTWARE; RECORD	Pentapharsodinium dalei is a widely distributed cold-water dinoflagellate, which is used in palaeoecology as an indicator of relatively warmer conditions in polar and sub-polar regions. This species has been proposed to be one of the first indicators of global warming at high latitudes. We developed the first microsatellite markers for P. dalei to facilitate the study of spatial and temporal population genetic changes. Single cysts were isolated from surface sediments in Koljo Fjord, Sweden. After cyst germination, single vegetative cells were isolated for establishing monoclonal cultures. Six dinucleotide polymorphic microsatellite markers were developed as multiplex polymerase chain reactions and were genotyped in 32 strains. The number of alleles per locus varied between 4 and 12, and the estimated gene diversity varied from 0.588 to 0.891. The haploid state of the vegetative cells was confirmed. The six selected microsatellites will be useful to explore population dynamics in P. dalei from contemporary planktonic and revived benthic samples to enable, for example, detailed studies into the evolutionary consequences of anthropogenic and climate-driven habitat changes.	[Lundholm, Nina] Univ Copenhagen, Nat Hist Museum Denmark, DK-1307 Copenhagen K, Denmark; [Nielsen, Lene Rostgaard] Univ Copenhagen, Dept Geosci & Nat Resource Management, DK-1958 Frederiksberg C, Denmark; [Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Marine Geol & Glaciol Dept, DK-1350 Copenhagen K, Denmark; [Ellegaard, Marianne] Univ Copenhagen, Dept Biol, DK-1353 Copenhagen K, Denmark	University of Copenhagen; University of Copenhagen; Geological Survey Of Denmark & Greenland; 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; Lundholm, Nina/AAY-6249-2020; Ellegaard, Marianne/H-6748-2014; Lundholm, Nina/A-4856-2013; Ribeiro, Sofia/G-9213-2018; Nielsen, Lene/E-6769-2015	Ellegaard, Marianne/0000-0002-6032-3376; Lundholm, Nina/0000-0002-2035-1997; Ribeiro, Sofia/0000-0003-0672-9161; Nielsen, Lene/0000-0002-7214-8691	Danish Research Council [2111-04-0011]; Carlsberg Foundation, Denmark [2011_01_0337]	Danish Research Council(Det Frie Forskningsrad (DFF)); Carlsberg Foundation, Denmark(Carlsberg Foundation)	This study was part of the Danish Research Council project 2111-04-0011. SR holds a postdoctoral grant from the Carlsberg Foundation, Denmark (no. 2011_01_0337).	ARMOUR JAL, 1994, HUM MOL GENET, V3, P599, DOI 10.1093/hmg/3.4.599; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Doyle J. 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Appl. Phycol.	FEB	2014	26	1					417	420		10.1007/s10811-013-0123-3	http://dx.doi.org/10.1007/s10811-013-0123-3			4	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	AA3CF					2025-03-11	WOS:000330969800046
J	Hakimi, MH; Abdullah, WH; Shalaby, MR; Alramisy, GA				Hakimi, Mohammed Hail; Abdullah, Wan Hasiah; Shalaby, Mohamed Ragab; Alramisy, Gamal A.			Geochemistry and organic petrology study of Kimmeridgian organic-rich shales in the Marib-Shabowah Basin, Yemen: Origin and implication for depositional environments and oil-generation potential	MARINE AND PETROLEUM GEOLOGY			English	Article						Kimmeridgian; Organic rich-shales; Amorphous; Oil-generative potential; Marib-Shabowah Basin; Yemen	CARBON-ISOTOPE COMPOSITION; CRUDE OILS; MASILA BASIN; SOURCE ROCKS; SHALLOW-MARINE; EASTERN YEMEN; MATTER; INDICATORS; PYROLYSIS; AUSTRALIA	Kimmeridgian organic-rich shales of the Madbi Formation from the Marib-Shabowah Basin in western Yemen were analysed to evaluate the type of organic matter, origin and depositional environments as well as their oil-generation potential. Results of the current study establishes the organic geochemical characteristics of the Kimmeridgian organic-rich shales and identifies the kerogen type based on their organic petrographic characteristics as observed under reflected white light and blue light excitation. Kerogen microscopy shows that the Kimmeridgian organic-rich shales contain a large amount of organic matter, consisting predominantly of yellow fluorescing alginite and amorphous organic matter with marine-microfossils (e.g., dinoflagellate cysts and micro-foraminiferal linings). Terrigenous organic matters (e.g., vitrinite, spores and pollen) are also present in low quantities. The high contributions of marine organic matter with minor terrigenous organic matter are also confirmed by carbon isotopic values. The organic richness of the Kimmeridgian shales is mainly due to good preservation under suboxic to relatively anoxic conditions, as indicated by the percent of numerous pyritized fragments associated with the organic matter. The biomarker parameters obtained from mass spectrometer data on m/z 191 and m/z 217 also indicate that these organic-rich shales contain mixed organic matter that were deposited in a marine environment and preserved under suboxic to relatively anoxic conditions. The Kimmeridgian organic-rich shales thus have high oil and low gas-generation potential due to oil window maturities and the nature of the organic matter, with high content of hydrogen-rich Type II and mixed Type II-III kerogens with minor contributions of Type III kerogen. (C) 2013 Elsevier Ltd. All rights reserved.	[Hakimi, Mohammed Hail; Alramisy, Gamal A.] Taiz Univ, Fac Sci Appl, Dept Geol, Taizi 6803, Taiz, Yemen; [Abdullah, Wan Hasiah] Univ Malaya, Dept Geol, Kuala Lumpur 50603, Malaysia; [Shalaby, Mohamed Ragab] Univ Brunei Darussalam, Fac Sci, Petr Geoscience Dept, Bandar Seri Begawan, Brunei	Taiz University; Universiti Malaya; University Brunei Darussalam	Hakimi, MH (通讯作者)，Taiz Univ, Fac Sci Appl, Dept Geol, Taizi 6803, Taiz, Yemen.	ibnalhakimi@yahoo.com	Alramisy, Gamal/MGA-8477-2025; Shalaby, Mohamed/B-5662-2017; Hakimi, Mohammed/ABG-3908-2021; Abdullah, Wan Hasiah/C-1007-2010	Abdullah, Wan Hasiah/0000-0002-6748-1019; Alramisy, Gamal/0009-0000-5359-0989; Shalaby, Mohamed/0000-0003-0556-2726; Hakimi, Mohammed/0000-0002-3320-9690				Abdullah WH, 1999, MAR PETROL GEOL, V16, P467, DOI 10.1016/S0264-8172(98)00086-5; Alaug AS, 2011, IRAN J EARTH SCI, V3, P134; Alaug A.S., 2002, PhD Thesis; Baker D.R., 1972, J. Geol. 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FEB	2014	50						185	201		10.1016/j.marpetgeo.2013.09.012	http://dx.doi.org/10.1016/j.marpetgeo.2013.09.012			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	304LF					2025-03-11	WOS:000330747700011
J	Knies, J; Mattingsdal, R; Fabian, K; Grosfjeld, K; Baranwal, S; Husum, K; De Schepper, S; Vogt, C; Andersen, N; Matthiessen, J; Andreassen, K; Jokat, W; Nam, SI; Gaina, C				Knies, Jochen; Mattingsdal, Rune; Fabian, Karl; Grosfjeld, Kari; Baranwal, Soma; Husum, Katrine; De Schepper, Stijn; Vogt, Christoph; Andersen, Nils; Matthiessen, Jens; Andreassen, Karin; Jokat, Wilfried; Nam, Seung-Il; Gaina, Carmen			Effect of early Pliocene uplift on late Pliocene cooling in the Arctic-Atlantic gateway	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Arctic Ocean; gateway; Pliocene; uplift; Northern Hemisphere glaciation	NORTHERN NORTH-ATLANTIC; LATE CENOZOIC UPLIFT; BARENTS SEA; ICE-SHEET; THERMOHALINE CIRCULATION; SURFACE TEMPERATURES; DINOFLAGELLATE CYST; CONTINENTAL-MARGIN; WESTERN SVALBARD; GLACIAL EROSION	Despite the undisputed role of the Arctic Ocean in the modern and Pliocene climate system, the Arctic has only recently attracted public awareness that ongoing, fundamental change in the Arctic cryosphere could be a response to global warming. Clarification of the Arctic's role in global climate during the Pliocene is, however, largely hampered by equivocal stratigraphic constraints. From a well-dated Pliocene sequence from the Yermak Plateau, off NW Spitsbergen, we present sedimentological and geochemical data indicating that 4 million years ago terrigenous sediment supply and sources changed abruptly in response to a regional tectonic uplift event. We argue that this event together with contemporary uplift and tilting along the northwestern European continental margin preconditioned the landmasses for glacial ice build-up during intensification of the Northern Hemisphere Glaciation (INHG). Our data further suggest that the final deepening/widening of the Arctic-Atlantic gateway, the Fram Strait, between 6.5 and 5 Ma gradually caused increased deep-water mass exchange which, in turn, likely contributed to the intensification of the North Atlantic thermohaline circulation. Coupled to the North Atlantic warm pool as a regional moisture source, declining atmospheric CO2 levels and other feedback mechanisms during the Pliocene, the regional tectonic activities in the high northern latitudes caused decreased summer ablation and thus allowed the initial build-up of glacial ice both in Scandinavia, and the sub-aerially exposed Svalbard/Barents Sea, culminating in the first large-scale coastline-shelf edge glaciations at similar to 2.75 Ma ago. (C) 2013 Elsevier B.V. All rights reserved.	[Knies, Jochen; Fabian, Karl; Grosfjeld, Kari; Baranwal, Soma] Geol Survey Norway, NO-7491 Trondheim, Norway; [Knies, Jochen; Fabian, Karl; Baranwal, Soma; Andreassen, Karin] Univ Tromso, Ctr Arctic Gas Hydrate Environm & Climate, NO-9037 Tromso, Norway; [Mattingsdal, Rune; Husum, Katrine; Andreassen, Karin] Univ Tromso, NO-9037 Tromso, Norway; [De Schepper, Stijn] Univ Bergen, NO-5020 Bergen, Norway; [Vogt, Christoph] Univ Bremen, Crystallog ZEKAM, DE-28359 Bremen, Germany; [Andersen, Nils] Univ Kiel, Leibniz Lab Radiometr Dating & Stable Isotope Res, DE-24118 Kiel, Germany; [Matthiessen, Jens; Jokat, Wilfried] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, DE-27568 Bremerhaven, Germany; [Nam, Seung-Il] Korea Polar Res Inst, Inchon 406840, South Korea; [Gaina, Carmen] Univ Oslo, Ctr Earth Evolut & Dynam, NO-0316 Oslo, Norway	Geological Survey of Norway; UiT The Arctic University of Tromso; UiT The Arctic University of Tromso; University of Bergen; University of Bremen; University of Kiel; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Korea Polar Research Institute (KOPRI); Korea Institute of Ocean Science & Technology (KIOST); University of Oslo	Knies, J (通讯作者)，Geol Survey Norway, NO-7491 Trondheim, Norway.		Gaina, Carmen/I-5213-2015; Fabian, Karl/AAC-8643-2022; Husum, Katrine/HGD-4711-2022; De Schepper, Stijn/A-2836-2011	Jokat, Wilfried/0000-0002-7793-5854; Husum, Katrine/0000-0003-1380-5900; Matthiessen, Jens/0000-0002-6952-2494; Andreassen, Karin/0000-0002-9407-526X; Gaina, Carmen/0000-0001-5533-8103; De Schepper, Stijn/0000-0002-6934-0914	Statoil ASA; Det Norske Oljeselskap; BG Group; Norwegian Research Council, NFR-Petromaks project "Glaciations in the Barents Sea" (NRC) [200672/S60]; DFG [Fi-442/13-1, Fi-442/13-2, Fi-442/14-1, SCHE1665/2-1, SCHE1665/2-2]; Norwegian Research Council for the Centre of Excellence: Earth Evolution and Dynamics (CEED) [223272]; K-Polar Program of KOPRI [PP13030]; Norwegian Research Council [223259]	Statoil ASA; Det Norske Oljeselskap; BG Group(Royal Dutch Shell); Norwegian Research Council, NFR-Petromaks project "Glaciations in the Barents Sea" (NRC); DFG(German Research Foundation (DFG)); Norwegian Research Council for the Centre of Excellence: Earth Evolution and Dynamics (CEED); K-Polar Program of KOPRI(Korea Polar Research Institute of Marine Research Placement (KOPRI)); Norwegian Research Council(Research Council of Norway)	This study was funded by Statoil ASA, Det Norske Oljeselskap, and BG Group as well as the Norwegian Research Council, NFR-Petromaks project "Glaciations in the Barents Sea" (NRC grant 200672/S60). This research used samples and data provided by the Integrated Ocean Drilling Program (IODP). We sincerely thank the staff at the IODP core repository in Bremen, Germany, for all their help during various sampling parties, and the NGU laboratory staff for the analyses of the samples. We acknowledge Leif Rise and Monica Winsborrow for their helpful comments on an earlier version of the manuscript. CV and SDS were funded by DFG research funds (Fi-442/13-1,2 and 14-1; SCHE1665/2-1 and 2-2). CG acknowledges funding from the Norwegian Research Council for the Centre of Excellence: Earth Evolution and Dynamics (CEED) (grant No. 223272). SIN was supported by K-Polar Program (PP13030) of KOPRI. This research is part of the Centre of Excellence: Arctic Gas hydrate, Environment and Climate (CAGE) funded by the Norwegian Research Council (grant No. 223259).	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Sci. Lett.	FEB 1	2014	387						132	144		10.1016/j.epsl.2013.11.007	http://dx.doi.org/10.1016/j.epsl.2013.11.007			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	AA5RI					2025-03-11	WOS:000331156900016
J	Moestrup, O; Hansen, G; Daugbjerg, N; Lundholm, N; Overton, J; Vestergård, M; Steenfeldt, SJ; Calado, AJ; Hansen, PJ				Moestrup, Ojvind; Hansen, Gert; Daugbjerg, Niels; Lundholm, Nina; Overton, Julia; Vestergard, Martin; Steenfeldt, Svend Jorgen; Calado, Antonio Jose; Hansen, Per Juel			The dinoflagellates <i>Pfiesteria shumwayae</i> and <i>Luciella masanensis</i> cause fish kills in recirculation fish farms in Denmark	HARMFUL ALGAE			English	Article						Fish kills; Luciella; Pfiesteria; Pikeperch; RAS fish farms	SUBUNIT RIBOSOMAL DNA; PARTIAL LSU RDNA; SP-NOV; HETEROTROPHIC DINOFLAGELLATE; TOXIC DINOFLAGELLATE; GEN. NOV; PISCICIDA DINOPHYCEAE; STOECKERIA-ALGICIDA; MICROPREDATION; PHYLOGENY	Fish kills in two geographically separate fish farms in northern Denmark in 2012, one using marine, the other brackish water 'Recirculation Aquaculture Systems' (RAS), were found to be caused by Pfiesteria shumwayae and Luciella masanensis, two species of dinoflagellates belonging to the family Pfiesteriaceae. There were no other harmful algae present in either of the aquaculture plants. Serious fish kills in the US have been attributed to Pfiesteria during the past 20 years, but this type of mortality has not been documented elsewhere. L. masanensis, described recently from Korea and USA, has not been previously reported to be the source of fish kills. In the marine farm, the affected fish was rainbow trout, in the brackish water farm pikeperch. Light microscopy is presently insufficient to discriminate between the approx. 20 species of the family Pfiesteriaceae described. Identification of the two algal species was therefore based on molecular sequencing of nuclear-encoded LSU rDNA, confirmed by scanning electron microscopy and, eventually, also by examination of the very thin amphiesmal plates of the flagellates by calcofluor-stained cells in a fluorescence microscope. Although the two fish farms differed in light and salinity conditions, both farms used re-circulating water in closed circuit systems. The dinoflagellates were examined in detail and shown to feed on organic material such as live, damaged nematodes, as described for the single pfiesteriacean flagellate known from freshwater, Tyrannodinium edax. Algal cells were observed to attach to their prey by an attachment filament and subsequently used a peduncle to suck up the food. Fish farms utilizing water recirculation technology are gaining popularity due to their reduced effect on the environment. The two cases from Denmark are apparently the first RAS farms in which serious fish kills have been reported. In the marine farm (Luciella) fish mortality increased dramatically despite treatment of the water with peracetic acid and chloramine-T. The plant was temporarily closed down pending investigation into the cause of mortality and subsequently to determine a method of management to control the dinoflagellate and avoid future fish kills. In the brackish water farm (Pfiesteria), water was treated with chloramine-T, which caused the dinoflagellates to disappear temporarily from the water column, apparently forming temporary cysts. The treatment was repeated after a few days to a week, when the temporary cysts appeared to germinate and the dinoflagellates reappeared in the water column. (C) 2013 Elsevier B.V. All rights reserved.	[Moestrup, Ojvind; Hansen, Gert; Daugbjerg, Niels] Univ Copenhagen, Marine Biol Sect, Dept Biol, DK-21000 Copenhagen O, Denmark; [Lundholm, Nina] Univ Copenhagen, Nat Hist Museum Denmark, DK-1307 Copenhagen K, Denmark; [Overton, Julia; Vestergard, Martin] Aquapri Innovat, DK-6040 Egtved, Denmark; [Steenfeldt, Svend Jorgen] Danish Tech Univ, DK-9850 Hirtshals, Denmark; [Calado, Antonio Jose] Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; [Calado, Antonio Jose] Univ Aveiro, GeoBioTec Res Unit, P-3810193 Aveiro, Portugal; [Hansen, Per Juel] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-3000 Helsingor, Denmark	University of Copenhagen; University of Copenhagen; Technical University of Denmark; Universidade de Aveiro; Universidade de Aveiro; University of Copenhagen	Daugbjerg, N (通讯作者)，Univ Copenhagen, Marine Biol Sect, Dept Biol, Univ Pk 4, DK-21000 Copenhagen O, Denmark.	moestrup@bio.ku.dk; n.daugbjerg@bio.ku.dk	Lundholm, Nina/AAY-6249-2020; Daugbjerg, Niels/D-3521-2014; Lundholm, Nina/A-4856-2013; Hansen, Gert/P-3328-2014; Calado, Antonio Jose/D-6263-2015; Hansen, Per Juel/E-9969-2011	Moestrup, Ojvind/0000-0003-0965-8645; Daugbjerg, Niels/0000-0002-0397-3073; Lundholm, Nina/0000-0002-2035-1997; Hansen, Gert/0000-0002-5751-8316; Calado, Antonio Jose/0000-0002-9711-0593; Hansen, Per Juel/0000-0003-0228-9621	Danish Strategic Research Council; Villum Kann Rasmussen Foundation; Carlsberg Foundation	Danish Strategic Research Council(Danske Strategiske Forskningsrad (DSF)); Villum Kann Rasmussen Foundation(Villum Fonden); Carlsberg Foundation(Carlsberg Foundation)	This study was supported by the Danish Strategic Research Council (project Harmful algae and fish kills, HABFISH). ND thanks the Villum Kann Rasmussen Foundation and the Carlsberg Foundation for equipment grants. We thank Leif Bolding for the photo showing the fish farm in Ejsing, and Charlotte Hansen for help with the sequencing. Finally, we would like to express our gratitude to the reviewers of the article for suggestions which improved the manuscript. 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J	López-Rosales, L; Gallardo-Rodríguez, JJ; Sánchez-Mirón, A; Contreras-Gómez, A; García-Camacho, F				Lopez-Rosales, L.; Gallardo-Rodriguez, J. J.; Sanchez-Miron, A.; Contreras-Gomez, A.; Garcia-Camacho, F.			Evaluation of the grazer-prey interaction as a biotechnological strategy to increase toxin production by dinoflagellate cultures in photobioreactors	JOURNAL OF APPLIED PHYCOLOGY			English	Article						Dinoflagellate; Protoceratium reticulatum; Artemia salina; Grazers; Yessotoxins; Photobioreactor	PROROCENTRUM-LIMA; ARTEMIA; ALEXANDRIUM; MICROALGA; COPEPODS; RATES	In this paper, we extend an existing approach to biotechnologically assess grazer-prey interactions between the crustacean Artemia salina (grazer) and the toxic dinoflagellate Protoceratium reticulatum (prey). The applied strategy is presented as a bioprocessing tool for enhancing the production of toxins and bioactive compounds in dinoflagellate cultures. Interactions were based on direct and indirect contact between the grazer and the prey, as well as on the use of different extracts from A. salina cysts and supernatants from cultures in which A. salina had been grown. Several treatments were found to stimulate the growth and yessotoxin production of P. reticulatum mainly due to the action of dissolved excreted substances and/or metabolites released and/or extracted from A. salina. One of the best results was obtained with a culture medium formulation containing 10 % (v/v) supernatant from a culture of A. salina nauplii. This treatment was scaled up to a 15-L photobioreactor. The average maximum specific growth rate (mu (max)) of P. reticulatum in this photobioreactor, operated in batch mode, increased by 27 %, whereas the maximum cell concentration (C (max)) decreased by 20 % relative to the corresponding control culture. An average increase in yessotoxin production of 50 % with respect to the control culture was observed.	[Lopez-Rosales, L.; Gallardo-Rodriguez, J. J.; Sanchez-Miron, A.; Contreras-Gomez, A.; Garcia-Camacho, F.] Univ Almeria, Chem Engn Area, Almeria 04120, Spain	Universidad de Almeria	García-Camacho, F (通讯作者)，Univ Almeria, Chem Engn Area, Almeria 04120, Spain.	fgarcia@ual.es	Rodríguez, Juan/R-9009-2019; Mirón, Asterio/K-8809-2014; Lopez Rosales, Lorenzo/K-8830-2014; GARCIA-CAMACHO, FRANCISCO/L-7793-2014	Gallardo Rodriguez, Juan Jose/0000-0003-2953-7699; Lopez Rosales, Lorenzo/0000-0001-5881-6086; Sanchez Miron, Asterio/0000-0001-5119-8035; GARCIA-CAMACHO, FRANCISCO/0000-0001-6168-3632	Spanish Ministry of Science and Innovation [CTQ2008-06754-C04-02/PPQ]; Spanish Ministry of Education and Science [SAF2011-28883-C03-02]; European Regional Development Fund Program	Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); Spanish Ministry of Education and Science(Spanish Government); European Regional Development Fund Program	This research was funded by the Spanish Ministry of Science and Innovation (CTQ2008-06754-C04-02/PPQ), the Spanish Ministry of Education and Science (SAF2011-28883-C03-02) and the European Regional Development Fund Program.	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Appl. Phycol.	FEB	2014	26	1					257	263		10.1007/s10811-013-0092-6	http://dx.doi.org/10.1007/s10811-013-0092-6			7	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	AA3CF					2025-03-11	WOS:000330969800029
J	Dia, A; Guillou, L; Mauger, S; Bigeard, E; Marie, D; Valero, M; Destombe, C				Dia, A.; Guillou, L.; Mauger, S.; Bigeard, E.; Marie, D.; Valero, M.; Destombe, C.			Spatiotemporal changes in the genetic diversity of harmful algal blooms caused by the toxic dinoflagellate <i>Alexandrium minutum</i>	MOLECULAR ECOLOGY			English	Article						bloom dynamics; clonality; linkage disequilibrium; population genetics; resting cyst; sexual reproduction	MICROSATELLITE MARKERS; CLONAL DIVERSITY; LIFE-HISTORY; SPRING BLOOM; POPULATION; DINOPHYCEAE; SEX; DIFFERENTIATION; BIOGEOGRAPHY; TEMPERATURE	Organisms with sexual and asexual reproductive systems benefit from both types of reproduction. Sexual recombination generates new combinations of alleles, whereas clonality favours the spread of the fittest genotype through the entire population. Therefore, the rate of sexual vs. clonal reproduction has a major influence on the demography and genetic structure of natural populations. We addressed the effect of reproductive system on populations of the dinoflagellate Alexandrium minutum. More specifically, we monitored the spatiotemporal genetic diversity during and between bloom events in two estuaries separated by 150km for two consecutive years. An analysis of population genetic patterns using microsatellite markers revealed surprisingly high genotypic and genetic diversity. Moreover, there was significant spatial and temporal genetic differentiation during and between bloom events. Our results demonstrate that (i) interannual genetic differentiation can be very high, (ii) estuaries are partially isolated during bloom events and (iii) genetic diversity can change rapidly during a bloom event. This rapid genetic change may reflect selective effects that are nevertheless not strong enough to reduce allelic diversity. Thus, sexual reproduction and/or migration may regularly erase any genetic structure produced within estuaries during a bloom event.	[Dia, A.; Guillou, L.; Mauger, S.; Bigeard, E.; Marie, D.; Valero, M.; Destombe, C.] Univ Paris 06, Univ Sorbonne, UMR 7144, Stn Biol Roscoff, F-29688 Roscoff, France; [Dia, A.; Guillou, L.; Mauger, S.; Bigeard, E.; Marie, D.; Valero, M.; Destombe, C.] CNRS, UMR 7144, Stn Biol Roscoff, F-29688 Roscoff, France	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Sorbonne Universite; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE)	Dia, A (通讯作者)，Univ Paris 06, Univ Sorbonne, UMR 7144, Stn Biol Roscoff, Pl Georges Teissier,CS 90074, F-29688 Roscoff, France.	adia@sb-roscoff.fr; destombe@sb-roscoff.fr	Valero, Myriam/M-6052-2019; Valero, Myriam/C-7550-2011	Valero, Myriam/0000-0002-9000-1423; Bigeard, Estelle/0000-0003-2256-8986; Mauger, Stephane/0000-0002-8779-1516; Destombe, Christophe/0000-0001-5656-9659; Guillou, Laure/0000-0003-1032-7958	ANR; Brittany Regional Council [ARE10087: POPALEX]; CNRS program EC2CO; French ANR project PARALEX [ANR-2009-PEXT-01201]; French ANR project CLONIX [ANR11-BSV7-00704]; European Project MaCuMBa [FP7-KBBE-2012-6-311975]; EC2CO project PALMITO	ANR(Agence Nationale de la Recherche (ANR)); Brittany Regional Council(Region Bretagne); CNRS program EC2CO; French ANR project PARALEX(Agence Nationale de la Recherche (ANR)); French ANR project CLONIX(Agence Nationale de la Recherche (ANR)); European Project MaCuMBa; EC2CO project PALMITO	We are very grateful to Yannis Michalakis, Denis Roze and Carolyn Engel for constructive comments on an earlier draft and three anonymous reviewers who helped improve this manuscript. We thank Laurent Leveque for the map design. We warmly thank the IFREMER laboratory in Dinard (France) and especially Claude Lebec and Claire Rollet. Thanks to the Roscoff Culture Collection (RCC), Service Mer et Observation (Marine Operations Department) at the Roscoff Biological Station and all the partners in the Paralex project for their help with sampling. Sequences and microsatellite genotypes were generated by Morgan Perennou and Gwenn Tanguy at the Roscoff Biological Station (Ouest-Genopole). This project was carried out in partial fulfilment of Aliou Dia's PhD degree, supported by funds from the ANR and a PhD fellowship from the Brittany Regional Council (ARE10087: POPALEX). This work was financially supported by the Brittany Regional Council, the CNRS program EC2CO, the French ANR projects PARALEX ('The sixth extinction' ANR-2009-PEXT-01201) and CLONIX ('Programme Blanc' ANR11-BSV7-00704), the European Project MaCuMBa (FP7-KBBE-2012-6-311975) and the EC2CO project PALMITO.	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Ecol.	FEB	2014	23	3					549	560		10.1111/mec.12617	http://dx.doi.org/10.1111/mec.12617			12	Biochemistry & Molecular Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Environmental Sciences & Ecology; Evolutionary Biology	293NW	24330231	Green Submitted			2025-03-11	WOS:000329980000006
J	Roy, S; Letourneau, L; Morse, D				Roy, Sougata; Letourneau, Louis; Morse, David			Cold-Induced Cysts of the Photosynthetic Dinoflagellate <i>Lingulodinium polyedrum</i> Have an Arrested Circadian Bioluminescence Rhythm and Lower Levels of Protein Phosphorylation	PLANT PHYSIOLOGY			English	Article							TRANSFER RNA-SYNTHETASE; AU-RICH ELEMENTS; MESSENGER-RNAS; PROTEOMIC ANALYSIS; GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE; RESPONSIVE TRANSCRIPTOME; SELECTIVE DEGRADATION; RAPID DEGRADATION; ESCHERICHIA-COLI	Dinoflagellates are microscopic, eukaryotic, and primarily marine plankton. Temporary cyst formation is a well-known physiological response of dinoflagellate cells to environmental stresses. However, the molecular underpinnings of cold-induced cyst physiology have never been described. Cultures of the photosynthetic dinoflagellate Lingulodinium polyedrum readily form temporary cysts when placed at low (8 degrees C +/- 1 degrees C) temperature and excyst to form normal motile cells following a return to normal temperature (18 degrees C +/- 1 degrees C). The normal circadian bioluminescence rhythm and the expected changes in Luciferin Binding Protein abundance were arrested in L. polyedrum cysts. Furthermore, after excystment, the bioluminescence rhythm initiates at a time corresponding to zeitgeber 12, independent of the time when the cells encysted. Phosphoprotein staining after two-dimensional polyacrylamide gel electrophoresis, as well as column-based phosphoprotein enrichment followed by liquid chromatography tandem mass spectrometry, showed cyst proteins are hypophosphorylated when compared with those from motile cells, with the most marked decreases found for predicted Casein Kinase2 target sites. In contrast to the phosphoproteome, the cyst proteome is not markedly different from motile cells, as assessed by two-dimensional polyacrylamide gel electrophoresis. In addition to changes in the phosphoproteome, RNA sequencing revealed that cysts show a significant decrease in the levels of 132 RNAs. Of the 42 RNAs that were identified by sequence analysis, 21 correspond to plastid-encoded gene products and 11 to nuclear-encoded cell wall/plasma membrane components. Our data are consistent with a model in which the highly reduced metabolism in cysts is achieved primarily by alterations in the phosphoproteome. The stalling of the circadian rhythm suggests temporary cysts may provide an interesting model to address the circadian system of dinoflagellates.	[Roy, Sougata; Morse, David] Univ Montreal, Inst Rech Biol Vegetale, Dept Sci Biol, Montreal, PQ H1X 2B2, Canada; [Letourneau, Louis] McGill Univ, Ctr Innovat Genome Quebec, Montreal, PQ H3A 1A4, Canada	Universite de Montreal	Morse, D (通讯作者)，Univ Montreal, Inst Rech Biol Vegetale, Dept Sci Biol, 4101 Sherbrooke Est, Montreal, PQ H1X 2B2, Canada.	david.morse@umontreal.ca		Morse, David/0000-0003-4131-4367; Roy, Sougata/0000-0001-9718-873X; Roy, Sougata/0000-0003-0168-5737	National Science and Engineering Research Council of Canada [171382-03]	National Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work was supported by the National Science and Engineering Research Council of Canada (grant no. 171382-03 to D.M.).	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FEB	2014	164	2					966	977		10.1104/pp.113.229856	http://dx.doi.org/10.1104/pp.113.229856			12	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	AA5JN	24335505	Bronze, Green Published			2025-03-11	WOS:000331132300036
J	Sancay, RH				Sancay, Recep Hayrettin			The occurrence of <i>Mediaverrunites</i> in the Upper Miocene of the Black Sea, Turkey	PALYNOLOGY			English	Article						Turkey; Black Sea; Upper Miocene; Neogene; Mediaverrunites	PETROLEUM GEOLOGY; EVOLUTION	Fossil fungal spores, endemic Paratethyan dinoflagellate cysts, organic-walled algal cysts, spores and pollen are very common in the onshore and offshore Neogene sediments of the Black Sea, Turkey. Amongst these assemblages, the fungal spore form-genus Mediaverrunites Nandi and Sinha 2007, emend. nov., described from Neogene strata from tropical to temperate paleoclimates, commonly occurs in Upper Miocene sediments. The presence of stratigraphically important dinoflagellate cyst and pollen taxa confirms the stratigraphic importance of this genus in the Upper Miocene of the Black Sea. Two new fungal spore species, Mediaverrunites batii sp. nov. and Mediaverrunites pontidiensis sp. nov., are described from Upper Miocene sediments of the Black Sea.	Turkish Petr Corp Res Ctr, TR-06100 Cankaya, Turkey	Ministry of Energy & Natural Resources - Turkey	Sancay, RH (通讯作者)，Turkish Petr Corp Res Ctr, Sogutozu Mah 2180,Cad 86, TR-06100 Cankaya, Turkey.	hsancay@tpao.gov.tr						[Anonymous], 1996, Palynology: principles and applications; Banerjee S., 1992, J MYCOPATHOLOGICAL R, V30, P81; Bat Z, 2009, 3470 TURK PETR CORP; Bozkurt E, 2001, GEODIN ACTA, V14, P3, DOI 10.1016/S0985-3111(01)01066-X; Elsik W.C., 1996, PALYNOLOGY, V1, P293; Elsik WC, 2009, PALYNOLOGY, V33, P99, DOI 10.1080/01916122.2009.9989687; Gorur N, 1997, AAPG MEMOIR, V68, P241; GORUR N, 1988, TECTONOPHYSICS, V147, P247, DOI 10.1016/0040-1951(88)90189-8; JARZEN D M, 1986, Palynology, V10, P35; Jones RW, 1997, AAPG MEMOIR, V68, P39; Menlikli C, 2008, LEADING EDGE, V28, P1066; MULLER JAN, 1959, MICROPALEONTOLOGY, V5, P1, DOI 10.2307/1484153; Nandi B, 2007, PALYNOLOGY, V31, P95, DOI 10.2113/gspalynol.31.1.95; Nikishin AM, 2003, SEDIMENT GEOL, V156, P149, DOI 10.1016/S0037-0738(02)00286-5; Okay AI, 1999, GEOL SOC SPEC PUBL, V156, P475, DOI 10.1144/GSL.SP.1999.156.01.22; Popescu SM, 2009, PALYNOLOGY, V33, P105, DOI 10.1080/01916122.2009.9989688; Robinson AG, 1996, MAR PETROL GEOL, V13, P195, DOI 10.1016/0264-8172(95)00042-9; Sancay RH, 2011, 3662 TURK PETR CORP; Shikhlinsky AS, 2012, 5320 TURK PETR CORP; Shikhlinsky AS, 2010, 5233 TURK PETR CORP; Shikhlinsky AS, 2010, 5215 TURK PETR CORP; Shillington DJ, 2008, EARTH PLANET SC LETT, V265, P360, DOI 10.1016/j.epsl.2007.10.033; Traverse A., 1978, Initial Reports of the Deep Sea Drilling Project, V42B, P993; Tunoglu Cemal, 2002, Turkiye Jeoloji Bulteni, V45, P99; Tunolu C, 1991, GEOLOGICAL B TURKEY, V34, P37; Tuysuz O, 2004, TURKIYE STRATIGR KOM, V1, P92; Vasiliev I, 2011, PALAEOGEOGR PALAEOCL, V310, P163, DOI 10.1016/j.palaeo.2011.06.022; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Yilmaz Y, 1997, AAPG MEMOIR, V68, P183	29	6	6	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	JAN 2	2014	38	1					28	37		10.1080/01916122.2013.806962	http://dx.doi.org/10.1080/01916122.2013.806962			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AF6LX					2025-03-11	WOS:000334827700002
J	Verhoeven, K; Louwye, S; Paez-Reyes, M; Mertens, KN; Vercauteren, D				Verhoeven, Koen; Louwye, Stephen; Paez-Reyes, Manuel; Mertens, Kenneth Neil; Vercauteren, Dries			New acritarchs from the late Cenozoic of the southern North Sea Basin and the North Atlantic realm	PALYNOLOGY			English	Article						biostratigraphy; taxonomy; Atlantic Ocean; acritarchs; North Sea Basin; Cenozoic	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; MIDDLE MIOCENE; PLIOCENE-PLEISTOCENE; HOLOCENE SEDIMENTS; DIEST FORMATION; TJORNES; BELGIUM; STRATIGRAPHY; PALEOECOLOGY; PALYNOMORPHS	Biostratigraphical investigations of Miocene deposits from the southern North Sea Basin, the Oligocene and Miocene of the Bahamas, and the lower Pliocene of northern Iceland revealed the presence of new acritarch species. Halodinium eirikssonii n. sp. is recovered from the lower Pliocene Serripes Zone of the Tjornes beds in northern Iceland, where its range is well constrained through magnetostratigraphy and biostratigraphy using dinoflagellate cysts. Leiosphaeridia spongiosa n. sp. is recovered from lower to upper Miocene deposits of the southern North Sea Basin and from upper Oligocene and Miocene deposits of the Bahamas. Palaeostomocystis orbiculata n. sp. appears to be restricted to the middle Miocene of the North Sea Basin.	[Verhoeven, Koen; Louwye, Stephen; Mertens, Kenneth Neil] Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Paez-Reyes, Manuel] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Vercauteren, Dries] Univ Ghent, Lab Gen Biochem & Phys Pharm, B-9000 Ghent, Belgium	Ghent University; Brock University; Ghent University	Louwye, S (通讯作者)，Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	stephen.louwye@ugent.be	Verhoeven, Koen/IZP-9609-2023; 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	Fund for Scientific Research, Flanders; NSERC	Fund for Scientific Research, Flanders(FWO); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	Ms. Sabine Van Cauwenberghe is kindly thanked for the palynological preparation of the samples. M. Bosselaers and Dr. O. Lambert provided the samples from the Posthofbrug outcrop. The research was carried out by the first author within the framework of an assistantship at the Palaeontology Research Unit of Ghent University. The palynological analysis of the Posthofbrug sediments was carried out within the framework of a research project funded by the Fund for Scientific Research, Flanders. M. P-R. conducted the research during his graduate studies at Brock University, supported by a NSERC Discovery Grant to M.J. Head K.N.M. is a postdoctoral fellow of the Fund for Scientific Research, Flanders. K. V. studied the palynology of the Tjornes section during an assistantship at Ghent University. K. Dybkjaer and S. De Schepper are kindly thanked for their meticulous review of the manuscript and their constructive and stimulating comments.	Bardarson GG, 1925, K DAN VIDENSK SELSK, VIV, P118; Betzler C, 2000, INT J EARTH SCI, V89, P140, DOI 10.1007/s005310050322; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; CRONIN TM, 1991, J PALEONTOL, V65, P767, DOI 10.1017/S002233600003777X; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; De Schepper S, 2008, STRATIGRAPHY, V5, P137; De Schepper S, 2009, PALYNOLOGY, V33, P179; De Schepper S, 2009, GEOL MAG, V146, P92, DOI 10.1017/S0016756808005438; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Drugg W.S., 1967, Tulane Studies in Geology, V5, P181; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; Einarsson T., 1967, The Bering Land Bridge, P312; Eisenack A., 1958, Palaeontographica, V110A, P1; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P298, DOI 10.1073/pnas.49.3.298; Fensome R. 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J	Price, AM; Pospelova, V				Price, Andrea Michelle; Pospelova, Vera			<i>Spiniferites multisphaerus</i>, a new dinoflagellate cyst from the Late Quaternary of the Guaymas Basin, Gulf of California, Mexico	PALYNOLOGY			English	Article						dinoflagellate cysts; eastern Pacific; Late Quaternary; taxonomy; Gonyaulax; Gulf of California; Spiniferites	SPATIAL-DISTRIBUTION; BALTIC SEA; MORPHOLOGY; PACIFIC; THECA; NOV; USA; MASSACHUSETTS; DINOPHYCEAE; ASSEMBLAGES	A new organic-walled dinoflagellate cyst species, Spiniferites multisphaerus sp. nov., is described from Late Quaternary sediments of Guaymas Basin, Gulf of California (Mexico). This species is characterized by a pronounced apical protuberance and bubble-like elements that comprise the central body wall, sutural septae and processes. The central body wall is similar to 1.0-2.1 mu m thick and appears pseudoreticulate in transmitted light microscopy. Processes are generally stubby and have blunt or furcated tips. Tabulation is expressed by low to moderate sutural septae, and is typical of the genus. Spiniferites multisphaerus sp. nov. has been found in low abundances throughout the Late Quaternary in Guaymas Basin with maximum abundances of 6% or 1670 cysts g(-1), and is rare in the Holocene, including modern sediments.	[Price, Andrea Michelle; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada	University of Victoria	Price, AM (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ H3A 0B9, Canada.			Price, Andrea/0000-0002-5359-053X; Pospelova, Vera/0000-0003-4049-8133	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))	This work was supported by the Natural Science and Engineering Research Council of Canada (NSERC).	[Anonymous], 1971, POLLEN SPORES; Beaulieu L.J., 2002, Mapping the Assets of Your Community: A key Component for Building Local Capacity, P1; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DOBELL P E R, 1981, Palynology, V5, P99; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Gomez Fernando, 2005, Acta Botanica Croatica, V64, P129; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; HARLAND R, 1980, Grana, V19, P211; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2007, GEOL MAG, V144, P987, DOI 10.1017/S0016756807003780; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Lewis J, 1999, GRANA, V38, P113, DOI 10.1080/00173139908559220; Mantell GA, 1850, PICTORIAL ATLAS FOSS, P191; Marret F, 2001, CAN J EARTH SCI, V38, P373, DOI 10.1139/e00-092; Matsuoka K, 2013, MICROPALEAEONTOLOGIC, P325; MATSUOKA K, 1983, Palaeontographica Abteilung B Palaeophytologie, V187, P89; McClean DM, 1971, J PALEONTOL, V45, P729; McClymont EL, 2012, PALEOCEANOGRAPHY, V27, DOI 10.1029/2011PA002226; Mertens KN, 2012, MAR MICROPALEONTOL, V96-97, P48, DOI 10.1016/j.marmicro.2012.08.002; Mertens KN, 2012, REV PALAEOBOT PALYNO, V184, P74, DOI 10.1016/j.revpalbo.2012.06.012; Mertens KN, 2009, REV PALAEOBOT PALYNO, V157, P238, DOI 10.1016/j.revpalbo.2009.05.004; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; Pichevin L, 2012, PALEOCEANOGRAPHY, V27, DOI 10.1029/2011PA002237; Pospelova V, 2005, MAR ECOL PROG SER, V292, P23, DOI 10.3354/meps292023; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Pospelova V, 2010, MAR MICROPALEONTOL, V75, P17, DOI 10.1016/j.marmicro.2010.02.003; Price AM, 2013, PALEOCEANOGRAPHY, V28, DOI 10.1002/palo.20019; Reid P.C., 1974, Nova Hedwigia, V25, P579; Rochon A, 2009, REV PALAEOBOT PALYNO, V155, P52, DOI 10.1016/j.revpalbo.2008.12.017; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Rossignol M., 1964, Revue de Micropaleontologie, V7, P83; SARJEANT W A S, 1970, Grana, V10, P74; SUN X-K, 1992, Acta Micropalaeontologica Sinica, V9, P45; THUNELL R, 1993, QUATERNARY SCI REV, V12, P451, DOI 10.1016/S0277-3791(05)80009-5; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WALL D., 1967, PALAEONTOLOGY, V10, P95; ZHAO YY, 1994, GEOBIOS-LYON, V27, P261, DOI 10.1016/S0016-6995(94)80172-X; Zonneveld KAF, 2009, J SEA RES, V62, P189, DOI 10.1016/j.seares.2009.02.003	43	15	15	0	6	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	JAN 2	2014	38	1					101	116		10.1080/01916122.2013.864341	http://dx.doi.org/10.1080/01916122.2013.864341			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AF6LX					2025-03-11	WOS:000334827700007
J	Dolby, G				Dolby, Graham			<i>Lopsidinium</i> gen. nov., a dinoflagellate cyst from the Early Cretaceous (Early and Middle Albian) of northern Alberta, Canada	PALYNOLOGY			English	Article						dinoflagellate cysts; palaeoecology; Early Cretaceous (Albian); Alberta, Canada; taxonomy		Two species of a distinctive new genus of dinoflagellate cyst are described from the Early Cretaceous of northern Alberta, Canada. The genotype, Lopsidinium subrisum, comes from the Lower Albian Clearwater Formation, in wells drilled to extract the enormous heavy oil and bitumen resources of the Athabasca and Cold Lake Oil Sands areas, northeastern Alberta. The second species, Lopsidinium paxense, occurs in the Middle Albian, upper Loon River Formation exposed in the banks of the Peace River, northwestern Alberta. Lopsidinium subrisum occurs in assemblages of dinoflagellate cysts associated with brackish water and it is likely that L. paxense is derived from similar environments.	G Dolby & Associates Ltd, Calgary, AB T3E 6H6, Canada		Dolby, G (通讯作者)，G Dolby & Associates Ltd, 6719 Leaside Dr SW, Calgary, AB T3E 6H6, Canada.	gdolby@shaw.ca						[Anonymous], 1993, GRONL GEOL UNDERS B; BRIDEAUX W., 1971, PALAEONTOGRAPHICA B, V135, P53; Burden E.T., 1982, PhD thesis, P422; Burden E. T., 1984, MESOZOIC MIDDLE N AM, V9, P249; Demchuk TD, 2007, HEAVY OIL BITUMEN FO, P5; Dolby G, 2012, AAPG BULL, V64, P251; HARDING IC, 1990, PALAEONTOLOGY, V33, P35; Hathway B., 2013, Bulletin of Canadian Petroleum Geology, v, V61, P331, DOI DOI 10.2113/GSCPGBULL.61.4.331; Hayes B.J.R., 1994, GEOLOGICAL ATLAS W C, P317; Hein F., 2006, 200606 ESR ALB EN UT, P67; Hein F. J., 2012, AAPG BULL, V64, P207; Hein FJ, 2006, 200603 ALB EN UT BOA, P17; KRAMERS J.W., 1974, MEMOIR CANADIAN SOC, P68; Morgan R, 1975, J P ROYAL SOC NEW S, V8, P157; NORRIS G., 1967, PALAEONTOGRAPHICA B, V120, P72; NORRIS G, 1975, GEOL ASSOC CAN SPEC, V13, P333; PLAYFORD G, 1971, Palaeontology (Oxford), V14, P533; Pocock S., 1962, PALAEONTOGRAPHICA, V111, P1; Pocock SAJ., 1976, GEOSCIENCE MAN, V15, P101, DOI DOI 10.2307/3687262; Singh C, 1964, RES COUNCIL ALBERTA, V15, P239; Singh C, 1975, GEOL ASSOC CANADA SP, V13, P365; SINGH C, 1971, RES COUNCIL ALBERTA, V28, P301; Stelck CR, 2007, CAN J EARTH SCI, V44, P1627, DOI 10.1139/E07-033; Vagvolgyi A, 1969, B CAN PETROL GEOL, V17, P155; Wightman D.M., 1995, ALBERTA ENERGY EXTER, V10; Wightman DM, 1988, 4 UNITAR UNDP C HEAV, P50	26	2	2	0	1	TAYLOR & FRANCIS INC	PHILADELPHIA	520 CHESTNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	JAN 2	2014	38	1					171	178		10.1080/01916122.2014.880078	http://dx.doi.org/10.1080/01916122.2014.880078			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AF6LX					2025-03-11	WOS:000334827700013
J	Riding, JB; Dettmann, ME				Riding, James B.; Dettmann, Mary E.			The first Australian palynologist: Isabel Clifton Cookson (1893-1973) and her scientific work	ALCHERINGA			English	Review						Australia; botany; history; Isabel C; Cookson; palaeobotany; palynology	UPPER JURASSIC STRATA; BAYU-UNDAN FIELD; NORTH-WEST SHELF; SEQUENCE STRATIGRAPHY; POLLEN GRAINS; DINOFLAGELLATE; MIDDLE; BARAGWANATHIA; PALEOENVIRONMENTS; VICTORIA	Isabel Clifton Cookson (1893-1973) of Melbourne, Australia, was one of that country's first professional woman scientists. She is remembered as one of the most eminent palaeontologists of the twentieth century and had a distinguished research career of 58years, authoring or co-authoring 93 scientific publications. Isabel worked with great distinction on modern and fossil plants, and pioneered palynology in Australia. She was a consumate taxonomist and described, or jointly described, a prodigious total of 110 genera, 557 species and 32 subspecific taxa of palynomorphs and plants. Cookson was a trained biologist and initially worked as a botanist during the 1920s. At the same time she became interested in fossil plants and then, Mesozoic-Cenozoic terrestrial (1940s-1950s) and aquatic (1950s-1970s) palynomorphs. Cookson's research into the late Silurian-Early Devonian plants of Australia and Europe, particularly the Baragwanathia flora, between the 1920s and the 1940s was highly influential in the field of early plant evolution. The fossil plant genus Cooksonia was named for Isabel in 1937 by her principal mentor in palaeobotany, Professor William H. Lang. From the 1940s Cookson focussed on Cenozoic floras and, with her students, elucidated floral affinities by comparative analyses of micromorphology, anatomy and in situ pollen/spores between fossil and extant taxa. This led to an interest in pre-Quaternary and Quaternary terrestrial pollen and spores; hence Isabel was the first palynologist in Australia. Her work on Paleogene and Neogene pollen and spores during the 1940s and 1950s provided incontrovertible evidence of the former widespread distribution of many important elements of Southern Hemisphere floras. During the early 1950s, while approaching her 60th year, Isabel turned her attention to marine palynomorphs. She worked with great distinction with Georges Deflandre and Alfred Eisenack, and also as a sole author, on acritarchs, dinoflagellate cysts and prasinophytes from the Jurassic to Quaternary of Australia and Papua New Guinea. She also co-authored papers on aquatic palynomorphs with Lucy M. Cranwell, Norman F. Hughes and Svein B. Manum. Isabel Cookson laid out the taxonomic basis for the study of Australasian Mesozoic and Cenozoic marine palynofloras by establishing, or jointly establishing, 76 genera and 386 species of marine microplankton. Her studies throughout her career, although especially in marine palynology, concentrated largely on taxonomy. However, she was one of the first palynologists to demonstrate the utility of dinoflagellate cysts for relative age dating and correlation in geological exploration. ?????????????????? (Isabel Clifton Cookson, 1893-1973), ??????????????, ????????????????????58???????, ???????93????????????????????????????????, ?????????????????????????????, ????????110??? 557???32?????????????????????????, ???20??20?????????????, ??????????????, ?-??????? (1940 - 1950) ????? (1950 - 1970) ???????20??20???40??????????????? - ??????, ???Baragwanathia???, ?????????????????????????Cooksonia???????????, ?? H ??????1937????????20??40????, ????????????, ????????, ??????????????????????????????/?????????????????????????????????????????????????????????????20??40???50??????????????????????????????????????????????1950????, ??60??????????????????????Deflandre??????Eisenack?? , ???????, ????????????????????????, ?????????????????? M ??????? F ?????? B Manum??, ????????????????? ??????????????????76???386??, ???????????????????????????????????????, ???????????, ?????????????????, ???????????????????????????????????	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J	Deaf, AS; Harding, IC; Marshall, JEA				Deaf, Amr S.; Harding, Ian C.; Marshall, John E. A.			Cretaceous (Albian-?early Santonian) palynology and stratigraphy of the Abu Tunis 1x borehole, northern Western Desert, Egypt	PALYNOLOGY			English	Article						biostratigraphy; Egypt; northern Western Desert; zonation; Cretaceous	DINOFLAGELLATE CYSTS; SOUTHERN ALPS; POLLEN; SPORES; BASIN; PALYNOSTRATIGRAPHY; SEDIMENTS; HISTORY; AFRICA; EVENTS	A palynological analysis has been conducted on the Cretaceous sediments of the Abu Tunis 1x borehole, in the northern Western Desert, Egypt. The palynomorphs recovered have been analysed both qualitatively and quantitatively, and permit a refinement of the original stratigraphy with the identification of four time-rock units. These have been divided into four informal sporomorph units and one dinoflagellate cyst palynozone. These biozones are, from oldest to youngest: the Afropollis jardinus-Tricolporopollenites-Elaterosporites klaszii Assemblage Zone (early-mid Albian), the Elaterosporites verrucatus-Sofrepites legouxae-Cretacaeiporites Assemblage Zone (late Albian-early Cenomanian), the Sofrepites legouxae Partial Range Zone (early-?mid Cenomanian), the Proteacidites cf. africaensis Total Range Zone (mid-late Cenomanian) and the Canningia senonica Total Range Zone (early? Santonian). A barren interzone has been identified immediately below the youngest palynozone, and this may be related to the unfavourable lithology (i.e., limestone and dolostone). The absolute abundances of spores and pollen represent the first quantitative description of an Egyptian Albian-Cenomanian palynofloral, a flora that is characteristic of the Albian-Cenomanian Elaterate Phytogeographical Province. The early Santonian palynoflora is exclusively marine phytoplankton; terrestrial palynomorphs representative of the Senonian Palmae Province are completely absent. The quantitative and semi-quantitative distributions of Afropollis jardinus are compared with similar semi-quantitative distributions of this species from other wells in the northern Western Desert of Egypt, and this permitted the identification of a mid Albian-early Cenomanian Afropollis jardinus 'acme' as an important local biostratigraphical event in the mid Cretaceous.	[Deaf, Amr S.; Harding, Ian C.; Marshall, John E. A.] Univ Southampton, Southampton NOCS, Natl Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England; [Deaf, Amr S.] Assiut Univ, Dept Geol, Fac Sci, Assiut 71516, Egypt	Egyptian Knowledge Bank (EKB); Assiut University	Deaf, AS (通讯作者)，Univ Southampton, Southampton NOCS, Natl Oceanog Ctr, Sch Ocean & Earth Sci, European Way, Southampton SO14 3ZH, Hants, England.	amr.daif@science.au.edu.eg	Deaf, Amr/AAF-6269-2020; Harding, Ian/K-3320-2012; Marshall, John/M-9154-2018	Marshall, John/0000-0002-9242-3646; Deaf, Amr/0000-0002-5073-7911; Harding, Ian/0000-0003-4281-0581	Egyptian Government	Egyptian Government	A.S. Deaf thanks the Egyptian Government for generously funding him a PhD scholarship at University of Southampton, UK. The authors wish to thank the Egyptian General Petroleum Corporation for providing well logs and samples of the Abu Tunis 1x borehole. 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Pal, V29, P61; Lawver LA, 2004, PLATES 2009 ATLAS PL; Mahmoud M.S., 2002, Revista Espanola de Micropaleontologia, V34, P129; Mahmoud MS, 2007, RIV ITAL PALEONTOL S, V113, P203, DOI 10.13130/2039-4942/5871; Meshref WM., 1990, GEOLOGY EGYPT, P113; Morgan R., 1978, INIT REPS DSDP, V40, P915; Muller J, 1966, BLUMEA, V4, P231; Norton P, 1967, INTERNAL REPORT; OMRAN AM, 1990, REV PALAEOBOT PALYNO, V66, P293, DOI 10.1016/0034-6667(90)90044-J; Penny JHJ, 1986, SPEC PAP PALAEONTOL, V35, P119; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; Regali M., 1974, B TEC PETROBRAS, V17, P177; Regali M., 1989, LATE JURASSIC EARLY; Roncaglia L, 1997, REV PALAEOBOT PALYNO, V97, P177, DOI 10.1016/S0034-6667(96)00070-X; Said R., 1990, GEOLOGY EGYPT, P439; Said R., 1962, GEOLOGY EGYPT, P28; SALARDCHEBOLDAEFF M, 1990, J AFR EARTH SCI, V11, P1, DOI 10.1016/0899-5362(90)90072-M; Schrank E, 1998, J AFR EARTH SCI, V26, P167, DOI 10.1016/S0899-5362(98)00004-9; SCHRANK E, 1992, CRETACEOUS RES, V13, P351, DOI 10.1016/0195-6671(92)90040-W; Schrank E., 1995, BERLINER GEOWISSENSC, V177, P1; Schrank E., 2001, Proceedings of the IX International Palynological Congress, Huston, Texas, U.S.A., P201; Stover LE, 1963, J MICROPALAEONTOL, V9, P85; Sultan I.Z., 1986, Bulletin of the Faculty of Science, Alexandria University, Egypt, V26, P80; Tea-Yassi J, 1999, J AFR EARTH SCI, V29, P783, DOI 10.1016/S0899-5362(99)00129-3; Thusu B, 1985, J MICROPALAEONTOL, V10, P131; Thusu B., 1988, SUBSURFACE PALYNOSTR, P171; Torricelli S, 2003, RIV ITAL PALEONTOL S, V109, P499, DOI 10.13130/2039-4942/5519; Torricelli S, 2006, RIV ITAL PALEONTOL S, V112, P95; Uwins F.J.R., 1988, SUBSURFACEPALYNOSTRA, P215; WEPCO, 1968, FIN REP COMP LOG AB	70	37	38	0	11	TAYLOR & FRANCIS INC	PHILADELPHIA	520 CHESTNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	JAN 2	2014	38	1					51	77		10.1080/01916122.2013.828662	http://dx.doi.org/10.1080/01916122.2013.828662			27	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	AF6LX					2025-03-11	WOS:000334827700004
C	Patrick, MEJF; Hart, MB; Forber, DA		Rocha, R; Pais, J; Kullberg, JC; Finney, S		Patrick, Meriel E. J. Fitz; Hart, Malcolm B.; Forber, David A.			Dinocyst Stratigraphy and Palaeoenvironmental Interpretation of the Cretaceous-Palaeogene Boundary at Stevns Klint, Denmark	STRATI 2013	Springer Geology		English	Proceedings Paper	1st International Congress on Stratigraphy (STRATI)	JUL 01-07, 2013	Lisbon, PORTUGAL	IUGS, Int Commiss Stratig, New Univ Lisbon, Fac Sci & Technol, Res Ctr Geol Sci & Engn, New Univ Lisbon, Fac Sci & Techno, Dept Earth Sci, GALP Energia SGPS S A, Partex Oil & Gas, Inst Francais Portugal, Centro Investigacao Ciencia & Engn Geologica, New Univ Lisbon		Dinocyst stratigraphy; Cretaceous-Palaeogene boundary; Stevns Klint; Denmark	TERTIARY BOUNDARY; STABLE-ISOTOPE; FORAMINIFERS; SUCCESSION	There has been some doubt cast upon the results of dinoflagellate cyst studies previously undertaken at Stevns Klint, Denmark, one of the classic outcrops of the Cretaceous-Palaeogene (K-Pg) boundary. A re-examination of both the uppermost Maastrichtian chalks and an expanded section of the Fish Clay (Fiskeler Member) has identified some differences between our findings and the earlier work. The white coccolith chalk of the uppermost Maastrichtian (Sigerslev Member) is placed in the Palynodinium grallator Zone. The last occurrence of P. grallator lies within the Hojerup Member, which represents a shallower-water marine succession that is characterized by a series of dune-like structures. This confirms a latest Maastrichtian age for the P. grallator Zone. Within the Fiskeler Member, a number of new taxa appear, including Carpatella cornuta, Xenicodinium reticulatum, and Fibrocysta spp. The highest samples in the Fiskeler Member indicate a progressive transition towards more proximal environments, with no dinoflagellate cysts recorded, having been replaced in the samples by pollen grains.	[Patrick, Meriel E. J. Fitz; Hart, Malcolm B.; Forber, David A.] Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England	University of Plymouth	Patrick, MEJF (通讯作者)，Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England.	mefitzpatrick@plymouth.ac.uk	Hart, Malcolm/KMD-8444-2024					[Anonymous], B SOC GEOLOGIQUE FRA; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Damholt T., 2012, STEVNS KLINT INCLUSI, P160; FIRTH J V, 1987, Palynology, V11, P199; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; Hansen J. M., 1979, CRETACEOUS TERTIARY, P136; 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; Hultberg S.U., 1986, Journal of Micropalaeontology, V5, P37; Hultberg S. U., 1987, J MICROPALAEONTOL, V6, P35; HULTBERG SU, 1985, THESIS U STOCKHOLM; Molina E, 2006, EPISODES, V29, P263, DOI 10.18814/epiiugs/2006/v29i4/004; Morgenroth P., 1968, Geologisches Jahrbuch, V86, P533; Prauss ML, 2009, PALAEOGEOGR PALAEOCL, V283, P195, DOI 10.1016/j.palaeo.2009.09.024; Rasmussen JA, 2005, B GEOL SOC DENMARK, V52, P113; SCHMITZ B, 1992, PALAEOGEOGR PALAEOCL, V96, P233, DOI 10.1016/0031-0182(92)90104-D; Surlyk F, 2006, B GEOL SOC DENMARK, V54, P1; VERSTEEGH GJM, 1994, MAR MICROPALEONTOL, V23, P147, DOI 10.1016/0377-8398(94)90005-1; Walliser O.H., 1986, LECTURE NOTES EARTH, V8, P381	19	0	0	0	3	SPRINGER INT PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2197-9545		978-3-319-04364-7; 978-3-319-04363-0	SPR GEOL			2014							33	36		10.1007/978-3-319-04364-7_7	http://dx.doi.org/10.1007/978-3-319-04364-7_7			4	Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geology	BD2OZ					2025-03-11	WOS:000359019400007
C	Crouch, EM; Willumsen, PS; Kulhanek, D; Gibbs, S		Rocha, R; Pais, J; Kullberg, JC; Finney, S		Crouch, Erica M.; Willumsen, Pi Suhr; Kulhanek, Denise; Gibbs, Samantha			A Revised Palaeocene (Teurian) Dinoflagellate Cyst Zonation from Eastern New Zealand	STRATI 2013	Springer Geology		English	Proceedings Paper	1st International Congress on Stratigraphy (STRATI)	JUL 01-07, 2013	Lisbon, PORTUGAL	IUGS, Int Commiss Stratig, New Univ Lisbon, Fac Sci & Technol, Res Ctr Geol Sci & Engn, New Univ Lisbon, Fac Sci & Techno, Dept Earth Sci, GALP Energia SGPS S A, Partex Oil & Gas, Inst Francais Portugal, Centro Investigacao Ciencia & Engn Geologica, New Univ Lisbon		Dinoflagellate cyst; Palaeocene; Teurian; New Zealand; Zonation	CRETACEOUS-PALEOGENE; TRANSITION; EOCENE; PALEOECOLOGY; PACIFIC	Organic-walled dinoflagellate cyst (dinocyst) assemblages are documented from Palaeocene (New Zealand Teurian Stage) sediments in five sections from eastern New Zealand: Tawanui, Angora Road, and Toi Flat-1 core in the East Coast Basin, the mid-Waipara River in the Canterbury Basin, and ODP Site 1121 on the eastern margin of Campbell Plateau. Based on dinocyst results from these sections, along with published earliest Palaeocene records from the East Coast, Canterbury, and Great South basins, a revised Palaeocene dinocyst zonation is proposed. The interval zones are labelled as New Zealand Dinocyst Palaeocene (NZDP), and the eight zones, NZDP1-NZDP8, encompass the entire Palaeocene extending from 66.04 to 55.96 Ma. Correlation of the NZDP zones with the International and New Zealand time scales is provided, and is based primarily on correlation with calcareous nannofossil biostratigraphy.	[Crouch, Erica M.; Kulhanek, Denise] GNS Sci, Dept Palaeontol, Lower Hutt 5040, New Zealand; [Willumsen, Pi Suhr] Fur Museum, Museum Salling, DK-7884 Fur, Denmark; [Kulhanek, Denise] Texas A&M Univ, Integrated Ocean Drilling Program, College Stn, TX 77845 USA; [Gibbs, Samantha] Univ Southampton, Natl Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England	GNS Science - New Zealand; Texas A&M University System; Texas A&M University College Station; NERC National Oceanography Centre; University of Southampton	Crouch, EM (通讯作者)，GNS Sci, Dept Palaeontol, POB 30368, Lower Hutt 5040, New Zealand.	e.crouch@gns.cri.nz; ps_willumsen@hotmail.com; kulhanek@iodp.tamu.edu; Samantha.Gibbs@noc.soton.ac.uk	Crouch, Erica/C-2820-2013	Kulhanek, Denise/0000-0002-2156-6383				Ballance P.F., 1993, SEDIMENTARY BASINS W, V2, P93; Bijl P. K., 2011, LPP CONTRIBUTION SER, V34, P213; Crouch E.M., 2001, Ultrecht Univaersity, Laboratory of Palaeobotany and Palynology contributions series, V14, P216; Crouch EM, 2005, MAR MICROPALEONTOL, V56, P138, DOI 10.1016/j.marmicro.2005.05.002; Crouch EM, 2014, REV PALAEOBOT PALYNO, V202, P47, DOI 10.1016/j.revpalbo.2013.12.004; Ferrow E, 2011, GEOCHIM COSMOCHIM AC, V75, P657, DOI 10.1016/j.gca.2010.10.016; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P1; Heilmann-Clausen C., 1985, DGU, VA7, P1, DOI DOI 10.34194/SERIEA.V7.7026; Hollis CJ, 2009, GEOLOGY, V37, P99, DOI 10.1130/G25200A.1; Hornibrook N.d. B., 1989, MANUAL NZ PERMIAN PL; Morgans H.E.G., 2004, I GEOLOGICAL NUCL SC, V22; MUDGE DC, 1994, MAR PETROL GEOL, V11, P166, DOI 10.1016/0264-8172(94)90093-0; Partridge A. D., 2004, LATE CRETACEOUS CENO; Schioler P, 2010, MAR PETROL GEOL, V27, P351, DOI 10.1016/j.marpetgeo.2009.09.006; Willumsen P. S., 2003, THESIS VICTORIA U WE, P387; Willumsen PS, 2012, PALYNOLOGY, V36, P48, DOI 10.1080/01916122.2011.642260; Willumsen PS, 2011, ALCHERINGA, V35, P199, DOI 10.1080/03115518.2010.494484; Willumsen PS, 2010, ALCHERINGA, V34, P523, DOI 10.1080/03115518.2010.519258; Willumsen PS, 2006, CRETACEOUS RES, V27, P954, DOI 10.1016/j.cretres.2006.06.002; Willumsen PS, 2004, J MICROPALAEONTOL, V23, P119, DOI 10.1144/jm.23.2.119; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; Wilson G.J., 1988, NZ GEOLOGICAL SURVEY, V57; Wilson G.J., 1987, NZ Geol. Surv. Rec, V20, P8	23	0	0	0	0	SPRINGER INT PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2197-9545		978-3-319-04364-7; 978-3-319-04363-0	SPR GEOL			2014							75	78		10.1007/978-3-319-04364-7_15	http://dx.doi.org/10.1007/978-3-319-04364-7_15			4	Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geology	BD2OZ					2025-03-11	WOS:000359019400015
C	Iakovleva, AI; Quesnel, F; Dupuis, C; Storme, JY; Breillat, N; Magioncalda, R; Iacumin, P; Fléhoc, C; Roche, E; Smith, T; Baele, JM; Yans, J; De Coninck, J		Rocha, R; Pais, J; Kullberg, JC; Finney, S		Iakovleva, Alina I.; Quesnel, Florence; Dupuis, Christian; Storme, Jean-Yves; Breillat, Noemie; Magioncalda, Roberto; Iacumin, Paola; Flehoc, Christine; Roche, Emile; Smith, Thierry; Baele, Jean-Marc; Yans, Johan; De Coninck, Jan			New Integrated High-Resolution Dinoflagellate Cyst Stratigraphy and Litho-and Chemostratigraphy from the Paris and Dieppe-Hampshire Basins for the "Sparnacian''	STRATI 2013	Springer Geology		English	Proceedings Paper	1st International Congress on Stratigraphy (STRATI)	JUL 01-07, 2013	Lisbon, PORTUGAL	IUGS, Int Commiss Stratig, New Univ Lisbon, Fac Sci & Technol, Res Ctr Geol Sci & Engn, New Univ Lisbon, Fac Sci & Techno, Dept Earth Sci, GALP Energia SGPS S A, Partex Oil & Gas, Inst Francais Portugal, Centro Investigacao Ciencia & Engn Geologica, New Univ Lisbon		PETM; "Sparnacian''; Paris and dieppe-hampshire basins; Dinoflagellate cysts; CIE		The Paris Basin represents an historical cradle of Palaeogene stratigraphy, where during the nineteenth century the Palaeocene Series and the "Sparnacian Stage'' were established. As highlighted by Aubry et al. (2005), whereas the chronostratigraphic connotation of the "Sparnacian Stage'' has been controversial since its definition, modern studies of the late Palaeocene-early Eocene interval have revealed that the so-called "Sparnacian'' deposits encompass a remarkable and short (similar to 170 kyr) episode of the Cenozoic, the Palaeocene-Eocene Thermal Maximum (PETM, similar to 55.8-55.6 Ma). Dinoflagellate assemblages from the "Sparnacian'' of the Dieppe-Hampshire and Paris basins do not contain the key species Apectodinium augustum, whereas it is present in the northern Belgian Basin Tienen Formation and is coeval there with the CIE and the Apectodinium acme interval. However, our calibration of the Apectodinium acme to the CIE in the Dieppe-Hampshire and Paris basins suggests its attribution to the A. augustum zone. The absence of species A. augustum in the Anglo-Paris Basin may be explained by its restriction to more offshore conditions.	[Iakovleva, Alina I.] Russian Acad Sci, Inst Geol, Moscow 119017, Russia; [Quesnel, Florence; Breillat, Noemie] BRGM French Geol Survey, DGR GAT, F-45060 Orleans 2, France; [Dupuis, Christian; Baele, Jean-Marc] Univ Mons, Dept Geol & Appl Geol, B-7000 Mons, Belgium; [Storme, Jean-Yves; Yans, Johan] FUNDP, Dept Geol, B-5000 Namur, Belgium; [Breillat, Noemie] Univ Bourgogne, Biogeosci, F-21000 Dijon, France; [Magioncalda, Roberto] Geonumeric, F-95100 Argenteuil, France; [Iacumin, Paola] Univ Parma, Dipartimento Sci Terra, I-43100 Parma, Italy; [Flehoc, Christine] BRGM French Geol Survey, LAB ISO, F-45060 Orleans 2, France; [Roche, Emile] Univ Liege, Dept Palaeobotany, B-7000 Liege, Belgium; [Smith, Thierry] Royal Belgian Inst Nat Sci, Dept Palaeontol, B-1000 Brussels, Belgium; [De Coninck, Jan] Univ Ghent, Dept Geol & Soil Sci & Paleontol, B-9000 Ghent, Belgium	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Bureau de Recherches Geologiques et Minieres (BRGM); University of Mons; University of Namur; Universite de Bourgogne; University of Parma; Bureau de Recherches Geologiques et Minieres (BRGM); University of Liege; Royal Belgian Institute of Natural Sciences; Ghent University	Iakovleva, AI (通讯作者)，Russian Acad Sci, Inst Geol, Pyzhevsky Per 7, Moscow 119017, Russia.	alina.iakovleva@gmail.com; f.quesnel@brgm.fr; christian.dupuis@umons.ac.be; jean-yves.storme@fundp.ac.be; noemie.breillat@brgm.fr; rmagioncalda@geonumeric.com; paola.iacumin@unipr.it; c.flehoc@brgm.fr; rocheemile@yahoo.fr; Thierry.Smith@naturalsciences.be; jean-marc.baele@umons.ac.be; johan.yans@fundp.ac.be; de_coninck_jan@hotmail.com	Iacumin, Paola/AAV-8855-2021; IAKOVLEVA, ALINA/ABH-9243-2020; QUESNEL, Florence/AAR-9253-2021; , christine flehoc/JXM-9922-2024	QUESNEL, florence/0000-0002-4081-1911; Smith, Thierry/0000-0002-1795-2564; , christine flehoc/0009-0002-3839-6031; Baele, Jean-Marc/0000-0002-8709-6249				[Anonymous], SPECIAL PUBLICATIONS; [Anonymous], 1999, B SOC BELG GEOL; [Anonymous], 1880, B SOC GEOLOGIQUE NOR; AUBRY M., 2005, STRATIGRAPHY, V2, P65; Chateauneuf J. J., 1978, MEMOIRE BRGM, V4, P59; Chateauneuf J. J., 1968, MEMOIRE BRGM, V59, P16; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; De Coninck J., 1975, PROFESSIONAL PAPER S, V2, P165; GRUAS-CAVAGNETTO C., 1974, PALEOBIOLOGIE CONTIN, V5, P3; Schimper W. P., 1874, TRAITE PALEONTOL, V1, P738; Steurbaut E., 2003, Geological Society of America Special Paper, V369, P291; Steurbaut E, 2000, GFF, V122, P154, DOI 10.1080/11035890001221154	13	5	5	0	9	SPRINGER INT PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2197-9545		978-3-319-04364-7; 978-3-319-04363-0	SPR GEOL			2014							107	111		10.1007/978-3-319-04364-7_22	http://dx.doi.org/10.1007/978-3-319-04364-7_22			5	Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geology	BD2OZ					2025-03-11	WOS:000359019400022
C	Castro, L; Borges, M; Pereira, Z; Fernandes, P; Pais, J		Rocha, R; Pais, J; Kullberg, JC; Finney, S		Castro, Ligia; Borges, Marisa; Pereira, Zelia; Fernandes, Paulo; Pais, Joao			Miocene Dinoflagellate Cyst Assemblages: Preliminary Correlation Between the Lower Tagus and Algarve Basins (Portugal)	STRATI 2013	Springer Geology		English	Proceedings Paper	1st International Congress on Stratigraphy (STRATI)	JUL 01-07, 2013	Lisbon, PORTUGAL	IUGS, Int Commiss Stratig, New Univ Lisbon, Fac Sci & Technol, Res Ctr Geol Sci & Engn, New Univ Lisbon, Fac Sci & Techno, Dept Earth Sci, GALP Energia SGPS S A, Partex Oil & Gas, Inst Francais Portugal, Centro Investigacao Ciencia & Engn Geologica, New Univ Lisbon		Dinoflagellate cysts; Lower Tagus Basin; Algarve Basin; Miocene; Portugal		Biostratigraphic studies of several sections and a borehole (Belverde) of the Lower Tagus Basin, based on Miocene dinoflagellate cyst assemblages, have allowed a detailed stratigraphic investigation to be conducted. Assemblages are very diverse and abundant and can be used as important biostratigraphic guides. Recently, a palynostratigraphic study based on dinoflagellate cysts was conducted in two offshore wells, Ruivo-1 and Corvina, located in the Algarve Basin (southern Portugal). The recovered dinoflagellate assemblages are less abundant and diverse than those obtained in the Lower Tagus Basin. New inferences are made regarding the correlation between the dinoflagellate cysts known from the Lower Tagus Basin with the assemblages recently recovered from the Algarve Basin. Species of selected dinoflagellate cyst assemblages recovered are similar in both basins. Continuing progress with these new palynological studies and biostratigraphic data will help to refine knowledge of and correlations between Portuguese Miocene deposits.	[Castro, Ligia; Pais, Joao] Univ Nova Lisboa, Fac Ciencias & Tecnol, CICEGe, Dept Ciencias Terra, P-2829516 Caparica, Portugal; [Borges, Marisa] PetroStrat Ltd, Tan Y Graig, Conwy LL32 8FA, Wales; [Pereira, Zelia] LNEG, Unidade Geol Hidrogeol & Geol Costeira, P-4465965 Sao Mamede de Infesta, Portugal; [Fernandes, Paulo] Univ Algarve, CIMA, P-8005139 Faro, Portugal	Universidade Nova de Lisboa; Laboratorio Nacional de Energia e Geologia IP (LNEG); Universidade do Algarve	Castro, L (通讯作者)，Univ Nova Lisboa, Fac Ciencias & Tecnol, CICEGe, Dept Ciencias Terra, Campus Caparica, P-2829516 Caparica, Portugal.	lscastro@fct.unl.pt	Pais, João/H-5054-2011; Castro, Ligia/AAA-6409-2020; Fernandes, Paulo/J-6577-2014; Pereira, Zelia/B-2740-2017	Castro, Ligia/0000-0002-4584-4501; Fernandes, Paulo/0000-0003-4888-0230; Pais, Joao/0000-0002-4567-7483; Pereira, Zelia/0000-0003-3056-6219				Antunes M.T., 1999, Bol. Soc. Geol. Espana, V12, P3; Borges M., 2011, 44 AASP M SOUTH; Borges M. E. N., 2012, THESIS U ALGARVE 1, P265; Castro L, 2006, THESIS U NOVA LISBOA, P380; Castro L., 2008, C TERRA CONFLITOS OR, P159; Challenger Portugal Inc, 1976, GEOL COMPL REP CORN; Chevron Overseas Petroleum Inc, 1975, EVAL REP RUIV 1; Fernandes P., 2010, 2 CENTR N ATL CONJ M, V3, P111; Fernandes P., 2013, MARINE PETROLE UNPUB, V27, P455; Pais J, 2012, SPRINGERBR EARTH SCI, P1, DOI 10.1007/978-3-642-22401-0; Pais J., 2003, CIENCIAS TERRA UNL, V13; Sousa L., 2004, Pollen, Madrid, V14, P415	12	0	0	0	5	SPRINGER INT PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2197-9545		978-3-319-04364-7; 978-3-319-04363-0	SPR GEOL			2014							1061	1065		10.1007/978-3-319-04364-7_202	http://dx.doi.org/10.1007/978-3-319-04364-7_202			5	Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geology	BD2OZ					2025-03-11	WOS:000359019400202
C	Li, JG		Rocha, R; Pais, J; Kullberg, JC; Finney, S		Li, Jianguo			Upper Jurassic and Lower Cretaceous Palynological Successions in the Qinghai-Xizang Plateau, China	STRATI 2013	Springer Geology		English	Proceedings Paper	1st International Congress on Stratigraphy (STRATI)	JUL 01-07, 2013	Lisbon, PORTUGAL	IUGS, Int Commiss Stratig, New Univ Lisbon, Fac Sci & Technol, Res Ctr Geol Sci & Engn, New Univ Lisbon, Fac Sci & Techno, Dept Earth Sci, GALP Energia SGPS S A, Partex Oil & Gas, Inst Francais Portugal, Centro Investigacao Ciencia & Engn Geologica, New Univ Lisbon		Palynostratigraphy; J-K boundary; Qinghai-Xizang plateau; Tethys	STRATIGRAPHIC PALYNOLOGY; EROMANGA BASIN; QUEENSLAND; AUSTRALIA; STRATA	Two Upper Jurassic-Lower Cretaceous palynological successions from the Qinghai-Xizang Plateau, China, are briefly introduced in this paper. The northern succession, from the Tanggula Mountains area, consists of three assemblage zones whereas the southern comprises two zones. Both of them are from marine sequences with diverse dinoflagellate cysts occurring in association. The positions of the J-K boundary are discussed and evaluated through comparison with the dinocyst stratigraphy. It shows that the first occurrences of Aequitriradites spinulosus and Cicatricosisporites sp. may be the best markers for the boundary from a miospore perspective. The peak occurrence of Dicheiropollis in the equatorial Tethys region might be significant for this boundary.	Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing, Jiangsu, Peoples R China	Chinese Academy of Sciences	Li, JG (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing, Jiangsu, Peoples R China.	jgli@nigpas.ac.cn						Backhouse J., 1988, Geological Survey of Western Australia Bulletin, V135, P1; Dettmann M. E., 1963, P ROYAL SOC VICTORIA, V77; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Li Jianguo, 2004, Cretaceous Research, V25, P531, DOI 10.1016/j.cretres.2004.04.005; Li JG, 2011, REV PALAEOBOT PALYNO, V166, P38, DOI 10.1016/j.revpalbo.2011.04.007; Li JG, 2011, ISL ARC, V20, P35, DOI 10.1111/j.1440-1738.2010.00715.x; Sajjadi F, 2002, PALAEONTOGR ABT B, V261, P1; Sajjadi F, 2002, PALAEONTOGR ABT B, V261, P99; Song Z., 2000, FOSSIL SPORES POLLEN, V2	9	0	1	0	2	SPRINGER INT PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2197-9545		978-3-319-04364-7; 978-3-319-04363-0	SPR GEOL			2014							1197	1202		10.1007/978-3-319-04364-7_229	http://dx.doi.org/10.1007/978-3-319-04364-7_229			6	Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geology	BD2OZ					2025-03-11	WOS:000359019400229
J	Andreychouk, V; Worobiec, E; Gedl, P; Worobiec, G				Andreychouk, Viacheslav; Worobiec, Elzbieta; Gedl, Przemyslaw; Worobiec, Grzegorz			ORIGIN OF THE PALAEOKARST IN MIOCENE EVAPORITES ON THE SW PERIPHERY OF THE EASTERN EUROPEAN PLATFORM IN THE LIGHT OF PALYNOLOGICAL STUDIES - A CASE STUDY OF THE ZOLOUSHKA CAVE, BUKOVINA, WESTERN UKRAINE	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						palaeokarst; palynology; sporomorphs; dinoflagellate cysts; caves; Western Ukraine; Eastern European Platform; Badenian	DINOFLAGELLATE CYSTS; CARPATHIAN FOREDEEP; CENTRAL PARATETHYS; POLLEN RECORDS; PALEOENVIRONMENT; PALEOCLIMATE; VEGETATION; SITE	The Zoloushka Cave belongs to a group of the largest gypsum caves in Western Ukraine (Bukovina region), developed in the middle Miocene (upper Badenian) evaporite series (Tyras Formation) on the SW periphery of the East European Platform. It is developed in the lower part of the evaporite series composed of gypsum, which is covered by a carbonate layer (Ratyn Limestone). The uneven upper surface of the gypsum at the contact with the limestone, the frequent occurrence of palaeokarst forms, and the presence of karstified fissures filled with allochthonous material indicate a sedimentation break between the gypsum and the overlying limestone. To support this thesis and to add new data on the age and palaeoenvironmental conditions of palaeokarst formation in the Bukovina region, palynological studies were carried out on material from the Zoloushka Cave. Palynofacies, sporomorphs and dinoflagellate cysts were studied. In total, over 70 sporomorph taxa and over 25 dinoflagellate cyst taxa have been identified in four samples collected from the filling of the palaeokarstic forms in the cave. The results of the analysis of sporomorphs and dinoflagellate cysts point to the formation of the palaeokarst during the sedimentation break that took place at the end of the late Badenian evaporitic cycle in the Western Ukraine region. The subsequent marine transgression led to the filling of the karst forms in gypsum with chemogenic carbonate material, precipitated from marine water (draperies) and with fine-grained, clastic material (pockets and fissures).	[Andreychouk, Viacheslav] Pope John Paul II State Sch Higher Educ Biala Pod, PL-21500 Biala Podlaska, Poland; [Worobiec, Elzbieta; Worobiec, Grzegorz] Polish Acad Sci, Wladyslaw Szafer Inst Bot, PL-31512 Krakow, Poland; [Gedl, Przemyslaw] Polish Acad Sci, Res Ctr Krakow, Inst Geol Sci, PL-31002 Krakow, Poland	Pope John Paul II State School of Higher Education in Biala Podlaska; Polish Academy of Sciences; W. Szafer Institute of Botany of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Andreychouk, V (通讯作者)，Pope John Paul II State Sch Higher Educ Biala Pod, Sidorska 95-97, PL-21500 Biala Podlaska, Poland.	geo@wnoz.us.edu.pl; e.worobiec@botany.pl; ndgedl@cyf-kr.edu.pl; g.worobiec@botany.pl	Andreychouk, Viacheslav/AGP-4083-2022	Worobiec, Elzbieta/0000-0001-5997-9602; Worobiec, Grzegorz/0000-0002-2916-9905	W. Szafer Institute of Botany, Polish Academy of Sciences	W. Szafer Institute of Botany, Polish Academy of Sciences	The study was partly supported by the W. Szafer Institute of Botany, Polish Academy of Sciences, through Statutory Funds for E. and G. Worobiec. The authors thank Nela Dolakova (UGV Masaryk University, Brno, Czech Republic) and Pavel Bosak (Institute of Geology AS CR, Prague, Czech Republic) for their critical reading of the manuscript and valuable comments. We also would like to express our gratitude to Frank Simpson (University of Windsor, Ontario, Canada) for his detailed linguistic revision and remarks.	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Volume 2 Gymnosperms; Stuchlik L., 2014, ATLAS POLLEN SPORES, V4; Syabryaj S, 2007, PALAEOGEOGR PALAEOCL, V253, P153, DOI 10.1016/j.palaeo.2007.03.038; Syabryaj Svetlana, 2004, Acta Palaeobotanica, V44, P55; Syabryay Svetlana V., 1994, Acta Palaeobotanica, V34, P165; Szulc J, 2012, ANN SOC GEOL POL, V82, P371; TAKAHASHI K., 1982, B FAC LIBERAL ARTS N, V23, P23; Tomescu AMF, 2000, REV PALAEOBOT PALYNO, V109, P219, DOI 10.1016/S0034-6667(99)00056-1; Walsh P, 1996, GEOL MAG, V133, P713, DOI 10.1017/S0016756800024560; Wazynska H., 1998, PRACE PANSTWOWEGO I, P35; Worobiec E, 2013, ANN SOC GEOL POL, V83, P51; Worobiec E, 2011, J PALEOLIMNOL, V45, P311, DOI 10.1007/s10933-011-9499-8; Worobiec E, 2010, REV PALAEOBOT PALYNO, V163, P1, DOI 10.1016/j.revpalbo.2010.06.007; Zevenboom D., 1995, PhD Thesis Diss	59	3	3	0	7	POLISH GEOLOGICAL SOC	KRAKOW	UL. OLEANDRY 2A, KRAKOW, POLAND	0208-9068			ANN SOC GEOL POL	Ann. Soc. Geol. 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J	M'Hamdi, A; Slimani, H; Ben Ismail-Lattrache, K; Ben Ali, W				M'Hamdi, Amel; Slimani, Hamid; Ben Ismail-Lattrache, Kmar; Ben Ali, Walid			DINOFLAGELLATE CYSTS, PALYNOFACIES AND ORGANIC GEOCHEMISTRY OF THE CRETACEOUS-PALAEOGENE (K-Pg) BOUNDARY TRANSITION AT THE ELLES SECTION, NORTHEASTERN TUNISIA	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						Cretaceous-Palaeogene (K-Pg) boundary; dinoflagellate cysts; palynofacies; organic matter; Elles section; Tunisia	SEA-LEVEL FLUCTUATIONS; TERTIARY BOUNDARY; OULED HADDOU; CRETACEOUS/PALAEOGENE BOUNDARY; PLANKTIC FORAMINIFERA; MASS EXTINCTION; WOODSIDE CREEK; RIF; BIOSTRATIGRAPHY	A palynofacies study carried out across the Cretaceous-Palaeogene (K-Pg) boundary in the El Haria Formation at Elles, northeastern Tunisia, revealed the presence of organic matter dominated by marine palynomorphs, mainly dinoflagellate cyst assemblages. Continental palynomorphs (sporomorphs) and amorphous organic matter (AOM) are also present in all samples. The total organic carbon (TOC) content is generally less than 0.7 wt.%. The Rock-Eval S1 parameters vary from 0.01 to 0.3 mgHC/g rock. The Rock-Eval S2 parameters vary from 0.15 to 0.57 mgHC/g rock. The hydrogen index (HI) and oxygen index (OI) values range from 61 to 214 mgHC/g TOC and 149 to 638 mgHC/g TOC, respectively. The Tmax values range from 420 to 440 degrees C. The TOC, Rock-Eval pyrolysis and palynofacies analyses indicate that the El Haria Formation is characterized by immature organic matter type II and III and a low thermal alteration index(TAI). Also, the authors present in this paper the biostratigraphic, palaeoenvironmentl and palaeobiogeographic frame work for the dinoflagellate cyst assemblages below and above the Cretaceous-Palaeogene boundary in the Elles section.	[M'Hamdi, Amel; Ben Ismail-Lattrache, Kmar; Ben Ali, Walid] Univ Tunis El Manar, Fac Sci Tunis, Dept Geol, El Manar 2092 2, Tunisia; [Slimani, Hamid] Univ Mohammed V Agdal, Dept Earth Sci, Lab Geol & Remote Sensing, URAC 46,Sci Inst, Rabat 10106, Morocco	Universite de Tunis-El-Manar; Faculte des Sciences de Tunis (FST); Mohammed V University in Rabat	M'Hamdi, A (通讯作者)，Univ Tunis El Manar, Fac Sci Tunis, Dept Geol, UR 11 ES 15 Campus Univ, El Manar 2092 2, Tunisia.	mhamdiamel25@yahoo.fr	Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913	Joint Committee Morocco-Tunisia [88/MT/08]; National Center of Scientific and Technical Research (CNRST) (Research Unit URAC 46); University Mohammed V-Agdal [SVT11/09]	Joint Committee Morocco-Tunisia; National Center of Scientific and Technical Research (CNRST) (Research Unit URAC 46); University Mohammed V-Agdal	The authors thank the Research Unit: Environments Sedimentary, Petroleum Systems and Characterization (UR 11 ES 15) of the Faculty of Sciences of Tunis, University of Tunis El Manar (Tunisia) and the Laboratory Geology and Remote Sensing Scientific Institute, University Mohammed V-Agdal-Rabat (Morocco) for the preparation of the palynological samples. They thank the Joint Committee Morocco-Tunisia (Project 88/MT/08) for the financial support of internships and missions in Morocco and Tunisia. The second author acknowledges support from the National Center of Scientific and Technical Research (CNRST) (Research Unit URAC 46) and the University Mohammed V-Agdal (Project SVT11/09).	Adatte T, 2002, PALAEOGEOGR PALAEOCL, V178, P165, DOI 10.1016/S0031-0182(01)00395-9; Batten D.J., 1983, PETROLEUM GEOCHEMIST, P275; Batten D.J., 1982, J. Micropal., V1, P107; BATTEN DJ, 1996, PALYNOLOGY PRINCIPLE, P1022; Bergen P.F., 1990, INT S ORG PETR MED R, V45, P23; BERTRAND P, 1994, ORG GEOCHEM, V22, P511, DOI 10.1016/0146-6380(94)90123-6; 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; Burollet P.F., 1956, Ann. Mines. 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J	Gedl, P				Gedl, Przemyslaw			Eocene dinoflagellate cysts from the Sotokija Graben (Roztocze, SE Poland): biostratigraphy and palaeoenvironment	GEOLOGICAL QUARTERLY			English	Article						dinoflagellate cysts; biostratigraphy; Eocene; epicontinental basin; Roztocze; SE Poland	OLIGOCENE TRANSITION; MAGURA NAPPE; STRATIGRAPHY; TERTIARY; DEPOSITS; MIOCENE; FOLUSZ; AREA	The Sofokija Graben is a tectonic structure in Roztocze, in southeastern Poland, unique by its infill of Eocene marine strata. The more than 40 m thick sandy succession is the only well-dated palaeontological evidence of the Eocene marine transgression of an epicontinental sea in this part of Poland: the surrounding area is devoid of coeval marine strata, which were since eroded away. The Solokija Graben succession is hence crucial for the palaeogeographic reconstruction of southeastern Poland during the Eocene as well as for the tectonic history of this region. To obtain precise age determination, the 33 m thick succession of loamy sands that fill the Solokija Graben at Leliszka and the 4 m thick succession at Laszczowka were sampled via borehole cores for dinoflagellate cysts. Samples from Laszczowka are barren, whereas those from Leliszka contain rich and taxonomically diverse assemblages. Their biostratigraphical interpretation supports previous results suggesting a Bartonian age for most of the Sofokija Graben succession; the postulated Priabonian age of its non-calcareous part was documented in its uppermost part only. The palynological record also allows reconstruction of the sedimentary setting of the Leliszka succession. The basal part of the Bartonian was deposited in a shallow but extensive marine basin characterized by normal salinity and relatively high-energy hydrodynamic conditions. Subsequently, marine basin underwent gradual shallowing with a temporary halt in sedimentation. During the Late Bartonian the basin became brackish. A short-duration Early Priabonian marine basin was characterized by shallow-marine conditions; it became brackish during its final stage. Comparison with neighbouring Eocene deposits of the epicontinental and Carpathian basins shows that the marine basin at Roztocze was presumably connected with both during the Bartonian, and separated from the Carpathian basin during the Early Priabonian. Factors controlling the seaway pattern of the Roztocze Basin included eustasy and tectonic movements, the former dominating during the Bartonian, and co-occurring with uplift of the Meta-Carpathian Swell during the Early Priabonian.	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						Agelopoulos J., 1964, Neues Jahrbuch fuer Geologie und Palaeontologie Monatshefte, V11, P673; Agelopoulos J., 1967, THESIS KARLS U TUBIN; Alberti G., 1961, Palaeontographica, V116, P1; Andreyeva-Grigorovich A, 2011, ATLAS PALEOGENE DINO; [Anonymous], 1996, Palynology: principles and applications; AUBRY MP, 1986, PALAEOGEOGR PALAEOCL, V55, P267, DOI 10.1016/0031-0182(86)90154-9; Batten D., 1996, Palynology: principles and applications, P1011; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Birkenmajer K., 1989, Annales Societatis Geologorum Poloniae, V59, P145; 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; BUJAK J P, 1979, Micropaleontology (New York), V25, P308, DOI 10.2307/1485305; Bujak J.P., 1994, Journal of Micropalaeontology, V13, P119; BUJAK J. 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Q.		2014	58	4					707	728		10.7306/gq.1167	http://dx.doi.org/10.7306/gq.1167			22	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AZ2YL		Bronze			2025-03-11	WOS:000348095100005
J	Estebenet, MSG; Guerstein, GR; Alperin, MI				Gonzalez Estebenet, M. Sol; Guerstein, G. Raquel; Alperin, Marta I.			DINOFLAGELLATE CYST DISTRIBUTION DURING THE MIDDLE EOCENE IN THE DRAKE PASSAGE AREA: PALEOCEANOGRAPHIC IMPLICATIONS	AMEGHINIANA			English	Article						Dinoflagellate cysts; Middle Eocene; Drake Passage; Early opening	SCOTIA SEA; SOUTHERN-OCEAN; PALEOGENE; ENNEADOCYSTA; ANTARCTICA; PATAGONIA; FLOW	The middle-late Eocene (45-36 Ma) dinoflagellate cyst distribution in high latitudes of the Southern Hemisphere has been explained by a surface ocean circulation pattern characterized by extensive subpolar gyres around Antarctica. Based on global paleoclimate models it has been proposed that these surface ocean gyres might favored the development of an Antarctic-endemic dinoflagellate cyst assemblage, which was consistently abundant until the end of the Eocene. During the late Eocene the deepening of the Tasman Gateway and the Drake Passage would have generated a circumpolar water flow responsible for the disruption of the local gyre system and the subsequent extinction of the endemic assemblage. Some authors have recently suggested that during the middle Eocene shallow water flows had already developed through incipient openings of the Tasman Gateway and the Drake Passage. In this review we have compared the middle Eocene dinoflagellate cysts assemblages dominated by the Antarctic-endemic species from localities of the Drake Passage area and performed a multivariate analysis to evaluate this hypothesis. Our results point out a clear differentiation between localities to the north and south of what now is the Drake Passage. While localities from the Antarctic Peninsula and Scotia Sea would had been affected by Antarctic surface waters, the Austral Basin would had been flooded by Antarctic waters together with Pacific waterflows developed through an incipient Drake Passage during the middle Eocene.	[Gonzalez Estebenet, M. Sol; Guerstein, G. Raquel] Univ Nacl Sur, Inst Geol Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Alperin, Marta I.] Natl Univ La Plata, Fac Ciencias Nat & Museo, RA-1900 La Plata, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); National University of La Plata; Museo La Plata	Estebenet, MSG (通讯作者)，Univ Nacl Sur, Inst Geol Sur, Dept Geol, San Juan 670,B8000ICN, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	sol.gonzalezestebenet@uns.edu.ar; raquel.guerstein@uns.edu.ar; marta.alperin@gmail.com		Guerstein, G. Raquel/0000-0003-1623-1084	Agencia Nacional de Promocion Cientifica y Tecnologica [PICT 89/09]; Consejo Nacional de Investigaciones Cientificas y Tecnicas [PIP: 112-201101-00566]; Universidad Nacional del Sur [PGI 24/H125]	Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); Consejo Nacional de Investigaciones Cientificas y Tecnicas(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Universidad Nacional del Sur	The authors thank V. Bowman and P. Bijl for their constructive reviews and valuable suggestions that greatly improved this manuscript. The samples from the Austral Basin studied by MSGE and GRG were processed by O. Cardenas. The present work was funded by projects granted by Agencia Nacional de Promocion Cientifica y Tecnologica (PICT 89/09), Consejo Nacional de Investigaciones Cientificas y Tecnicas (PIP: 112-201101-00566) and Universidad Nacional del Sur (PGI 24/H125).	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J	Peryt, D; Gedl, P; Peryt, TM				Peryt, Danuta; Gedl, Przemyslaw; Peryt, Tadeusz Marek			Foraminiferal and palynological records of the Late Badenian (Middle Miocene) transgression in Podolia (Shchyrets near Lviv, western Ukraine)	GEOLOGICAL QUARTERLY			English	Article						Paratethys; Carpathian Foredeep; Upper Badenian; foraminifers; dinoflagellate cysts; palaeoenvironment	CENTRAL PARATETHYS; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; CARPATHIAN FOREDEEP; SALINITY CRISIS; STABLE-ISOTOPE; OXYGEN INDEX; SEDIMENTS; DEPOSITS; PATTERNS	The Upper Badenian many shales overlying gypsum and the Ratyn Limestone at Shchyrets, Ukraine, contain moderately to well-preserved benthic (calcareous only) and planktonic foraminifers, and palynofacies dominated by bisaccate pollen grains, presumably transported by wind. Both foraminiferal and dinoflagellate cyst assemblages indicate an open marine environment with normal-marine salinity and cool waters. The palaeodepth was ca. 50 m except for the uppermost part of the section studied, where a distinctive deepening is indicated by the dominance of Uvigerina in benthic foraminiferal assemblages and a high P/B ratio. The water was thermally stratified and the differences between the bottom water and the water column show an upwards-increasing trend. Bulimina and Globocassidulina are the most common and dominant component of benthic foraminiferal assemblages, except for the uppermost part where Uvigerina dominates the assemblage. The composition of benthic foraminifer assemblages and delta C-13 values of foraminifers indicate nutrient-rich waters and mesotrophic to eutrotrophic environments in surface waters, and low oxygenation at the sea floor in the Ukrainian Carpathian Foredeep Basin during the Late Badenian.	[Peryt, Danuta] Polish Acad Sci, Inst Paleobiol, PL-00818 Warsaw, Poland; [Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland; [Peryt, Tadeusz Marek] Polish Geol Inst, Natl Res Inst, PL-00975 Warsaw, Poland	Polish Academy of Sciences; Institute of Paleobiology of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Geological Institute - National Research Institute	Peryt, D (通讯作者)，Polish Acad Sci, Inst Paleobiol, Twarda 51-55, PL-00818 Warsaw, Poland.	d.peryt@twarda.pan.pl	Peryt, Tadeusz/F-9289-2019; Peryt, Danuta/F-9988-2019		Committee on Scientific Research [6 P04D 009 11]; Ministry of Science and Higher Education [Ukraina/193/2006]	Committee on Scientific Research; Ministry of Science and Higher Education	The fieldwork and analyses were funded by research grant No. 6 P04D 009 11 (Committee on Scientific Research) to T.M. Peryt and special grant No. Ukraina/193/2006 (Ministry of Science and Higher Education) to M. Kotarba. We thank A.V. Poberezhskyy for his help in the field. The comments and suggestions given by the journal reviewers, N. Hudackova and A. Poberezhskyy, are appreciated.	AndreyevaGrigorovich AS, 1997, GEOL CARPATH, V48, P123; [Anonymous], 1982, Utrecht Micropaleontological Bulletins; Báldi K, 2006, INT J EARTH SCI, V95, P119, DOI 10.1007/s00531-005-0019-9; Bernhard JM, 1999, MODERN FORAMINIFERA, P201; BERNHARD JM, 1986, J FORAMIN RES, V16, P207, DOI 10.2113/gsjfr.16.3.207; Bilonizhka P., 2012, B PANSTWOWEGO I GEOL, V449, P137; Bobrinskaya O.G., 1998, ABH SENCKENB NAT, V549, P34; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; Brugman W. 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J	Rolland, DC; Vincent, WF				Rolland, Delphine C.; Vincent, Warwick F.			Characterization of phytoplankton seed banks in the sediments of a drinking water reservoir	LAKE AND RESERVOIR MANAGEMENT			English	Article						Blooms; cyanobacteria; inocula; pigments; resting stages; sediments	MICROCYSTIS-AERUGINOSA; CYANOBACTERIAL TOXINS; POPULATION-DYNAMICS; ALGAL RECRUITMENT; LAKE-SEDIMENTS; BLOOMS; VARIABILITY; MANAGEMENT; PIGMENTS; COLUMN	The presence, abundance, and composition of algal and cyanobacterial populations in lake sediments were evaluated in Lake St. Charles (Quebec City, Canada), an urban drinking water reservoir. This water body has recently experienced cyanobacterial blooms, and we tested the hypothesis that a seed population of noxious taxa that could potentially re-inoculate the water column was present in the lake sediments. Cores were obtained from 8 sites spanning a range of depth and sediment conditions in both basins of the lake; sampling was from May to October over 2 years. Three techniques were applied: observation of the surficial sediments by epifluorescence microscopy; pigment analysis by high-performance liquid chromatography (HPLC); and laboratory enrichment culture of sediment samples under different light, temperature, and nutrient conditions. These analyses revealed the presence of diverse phytoplankton pigments and fluorescent cells in the sediments, with a predominance of diatoms along with dinoflagellates, chrysophytes, chlorophytes, euglenophytes, and cryptophytes. Growth of benthic filamentous cyanobacteria was induced from the sediments during the incubations, but bloom-forming genera that occurred in the lake such as Anabaena and Microcystis were not detected in any of the sediments, either before or after incubation. These observations imply that the episodic blooms of cyanobacteria in Lake St. Charles were not derived from an abundant seed population distributed throughout the surficial sediments of the lake. Alternative inoculum sources may include localized populations in sediments at sites that were not sampled in the present study, cyanobacteria that may enter via the inflows, or holoplanktonic populations that persist in the water column at low cell concentrations.	[Rolland, Delphine C.] Univ Laval, Dept Biol, Quebec City, PQ G1V 0A6, Canada; Univ Laval, CEN, Quebec City, PQ G1V 0A6, Canada	Laval University; Laval University	Rolland, DC (通讯作者)，Univ Laval, Dept Biol, Quebec City, PQ G1V 0A6, Canada.	delphine.rolland.1@ulaval.ca	Vincent, Warwick/AAH-6152-2019	Vincent, Warwick/0000-0001-9055-1938	Natural Sciences and Engineering Research Council (NSERC); Canada Research Chair program	Natural Sciences and Engineering Research Council (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Canada Research Chair program(Canada Research Chairs)	This research was supported by the Natural Sciences and Engineering Research Council (NSERC) and the Canada Research Chair program.	ALLEN MM, 1968, J GEN MICROBIOL, V51, P203, DOI 10.1099/00221287-51-2-203; [Anonymous], 1958, Mitt. Int. Ver. Theor. Angew. 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Manag.		2014	30	4					371	380		10.1080/10402381.2014.950438	http://dx.doi.org/10.1080/10402381.2014.950438			10	Limnology; Marine & Freshwater Biology; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Water Resources	AS3GZ					2025-03-11	WOS:000344167000005
J	Yans, J; Marandat, B; Masure, E; Serra-Kiel, J; Schnyder, J; Storme, JY; Marivaux, L; Adnet, S; Vianey-Liaud, M; Tabuce, R				Yans, Johan; Marandat, Bernard; Masure, Edwige; Serra-Kiel, Josep; Schnyder, Johann; Storme, Jean-Yves; Marivaux, Laurent; Adnet, Sylvain; Vianey-Liaud, Monique; Tabuce, Rodolphe			Refined bio- (benthic foraminifera, dinoflagellate cysts) and chemostratigraphy (δ<SUP>13</SUP>C<sub>org</sub>) of the earliest Eocene at Albas-Le Clot (Corbieres, France): implications for mammalian biochronology in Southern Europe	NEWSLETTERS ON STRATIGRAPHY			English	Article						Mammals; carbon isotopes; Le Clot; Corbieres; "Sparnacian"; PETM	CARBON-ISOTOPE STRATIGRAPHY; THERMAL MAXIMUM; CENTRAL PYRENEES; ORGANIC-MATTER; LATE PALEOCENE; STABLE CARBON; BIOSTRATIGRAPHY; BOUNDARY; MARINE; SECTION	Utilizing bio- and chemostratigraphy, we propose an integrated dating of the upper part of the continental "Sparnacien des Corbieres" and the overlying marine "lower-middle Ilerdian" succession of Albas-Le Clot (Corbieres, France), in order to refine the position and age of the Le Clot mammalian locality. Our data show that this locality, which has yielded a mammal fauna early Ypresian in age (close to MP7, Mammal Paleogene level), is located above the end of the carbon isotope excursion (CIE) the base of which defines the Paleocene-Eocene boundary. The Le Clot mammalian locality is therefore younger than the Paleocene-Eocene Thermal Maximum (PETM), and also younger than the Dormaal MP7 reference fauna in Belgium, which is correlated with the onset of the CIE (nannoplankton Zone NP9b). Moreover, we demonstrate that the Le Clot mammalian locality is older than the Eocene Thermal Maximum 2 (ETM2) event, located in the lower part of NP11 Zone. Associated with the ages of benthic foraminifera and dinocysts observed in the succession, our delta C-13(org) chemostratigraphy suggests that the Le Clot locality is correlated to the upper NP10-lower NP11 Zones. The refined location of the CIE in the Albas-Le Clot section is discussed because two carbon isotope excursions are potentially recorded in the upper "Sparnacien des Corbieres", here recognized as mainly Thanetian in age.	[Yans, Johan; Storme, Jean-Yves] Univ Namur, Dept Geol, NaGRIDD, B-5000 Namur, Belgium; [Marandat, Bernard; Marivaux, Laurent; Adnet, Sylvain; Vianey-Liaud, Monique; Tabuce, Rodolphe] Univ Montpellier 2, Lab Paleontol, Inst Sci Evolut Montpellier, UMR5554,UM2,CNRS,IRD, F-34095 Montpellier 05, France; [Masure, Edwige] UPMC, CNRS UPMC MNFIN, Ctr Rech Paleobiodiversite & Paleoenvironm CR2P, UMR 7207, F-75252 Paris 05, France; [Serra-Kiel, Josep] Univ Barcelona, Dept Stratig Paleontol & Marine Geosci, Fac Geol, E-08028 Barcelona, Spain; [Schnyder, Johann] Univ Paris 06, Sorbonne Univ, UMR ISTeP 7193, F-75005 Paris, France; [Schnyder, Johann] CNRS, UMR 7193, ISTeP, F-75005 Paris, France; [Storme, Jean-Yves] Univ Liege, Dept Geol, B-4000 Liege, Belgium	University of Namur; Universite de Montpellier; Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; University of Barcelona; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Liege	Yans, J (通讯作者)，Univ Namur, Dept Geol, 61 Rue Bruxelles, B-5000 Namur, Belgium.	johan.yans@unamur.be; bernard.marandat@univ-montp2.fr; edwige.masure@upmc.fr; josepserra@ub.edu; johann.schnyder@upmc.fr; jystorme@ulg.ac.be; laurent.marivaux@univ-montp2.fr; sylvain.adnet@univ-montp2.fr; monique.vianey-liaud@univ-montp2.fr; rodolphe.tabuce@univ-montp2.fr	Schnyder, Johann/IQV-5253-2023	MARIVAUX, Laurent/0000-0002-2882-0874; Tabuce, Rodolphe/0000-0002-4713-3981	Belgian Science Policy Office [BR/121/A3/PALEURAFRICA]; Spanish Ministry of Science and Innovation [CGL2011-27869]; project EVOLTHERM of the Institut des Sciences de l'Evolution of Montpellier	Belgian Science Policy Office(Belgian Federal Science Policy Office); Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); project EVOLTHERM of the Institut des Sciences de l'Evolution of Montpellier	Thanks are due to Etienne Steurbaut for search of nannoplankton in samples of the Albas-Le Clot section, Gaetan Rochez for sampling and analytical procedure, and Prof. M. Joachimski (University of Erlangen) for performing the isotopic analyses. J.Y. was partly funded by the project BR/121/A3/PALEURAFRICA of the Belgian Science Policy Office, J.S.K. by the project CGL2011-27869 of the Spanish Ministry of Science and Innovation, and B.M., L.M., S.A., M. V.-L., R.T. by the project EVOLTHERM of the Institut des Sciences de l'Evolution of Montpellier.	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Stratigr.		2014	47	3					331	353		10.1127/nos/2014/0050	http://dx.doi.org/10.1127/nos/2014/0050			23	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AQ8JU					2025-03-11	WOS:000343072600005
J	Onda, DFL; Lluisma, AO; Azanza, RV				Onda, Deo Florence L.; Lluisma, Arturo O.; Azanza, Rhodora V.			Development, morphological characteristics and viability of temporary cysts of <i>Pyrodinium bahamense</i> var. <i>compressum</i> (Dinophyceae) <i>in vitro</i>	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						confocal laser scanning microscopy; intracellular bacteria; pellicle formation; Pyrodinium bahamense var. compressum; temperature/nutrient stress; temporary cyst	RED-TIDE DINOFLAGELLATE; GONYAULAX-TAMARENSIS; LIFE-CYCLE; CHLOROPHYLL; TEMPERATURE; ENCYSTMENT; GROWTH; BLOOM; BAY; EXCYSTMENT	Pellicle or temporary cysts of Pyrodinium bahamense var. compressum (B hm) Steidinger, Tester & F. J. R. Taylor and their role in bloom dynamics have not yet been adequately characterized and understood. We investigated the role of temperature- and nutrient-mediated stress as factors that could induce pellicle formation in batch cultures. Cellular features and their implications for temporary cyst viability were examined using confocal laser scanning microscopy (CLSM). Our data suggest that temperature change is one of the key factors influencing pellicle formation, preserving viability at low temperature (i.e. 13 degrees C). Hypnocysts (resting cysts) were not observed. During pellicle formation, motile cells generally undergo ecdysis, extrusion of cytoplasmic materials and bacteria, compaction of the nucleus and non-motility. The outermost covering of the temporary cysts shows red autofluorescence and it contains lower concentrations of chlorophyll (chl) a and no detectable chl c. The nuclear region is surrounded by transitional red bodies and other unidentified cellular structures. Temporary cysts can immediately revert back to the motile state upon exposure to optimum conditions. This is accompanied by the expansion of the nuclear region, regeneration of the chloroplasts and enlargement of the cell. Developmental changes during reversal of temporary cysts to motile forms were also observed to cause breaks in the cell covering that could serve as sites for bacterial entry. Though observed in vitro, such behaviour may also be occurring in nature especially as a response to drastic short-lived environmental changes. This is the first detailed report on the characteristics of temporary cysts of P. bahamense var. compressum.	[Onda, Deo Florence L.; Lluisma, Arturo O.; Azanza, Rhodora V.] Univ Philippines, Coll Sci, Inst Marine Sci, Quezon City 1101, Philippines	University of the Philippines System; University of the Philippines Diliman	Azanza, RV (通讯作者)，Univ Philippines, Coll Sci, Inst Marine Sci, Velasquez St, Quezon City 1101, Philippines.	rhodaazanza@yahoo.com	Azanza, Rhodora/HGU-5811-2022		Department of Science and Technology (DOST) through the Philippine Council for Aquatic and Marine Research and Development (PCAARRD); UNESCO IOC-SCOR	Department of Science and Technology (DOST) through the Philippine Council for Aquatic and Marine Research and Development (PCAARRD)(Department of Science & Technology (DOST), Philippines); UNESCO IOC-SCOR	This study is part of the research programme 'Ecology and Oceanography of Harmful Algal Blooms in the Philippines (PhilHABs), Project 1: Biodiversity/Genetic Diversity of selected HAB-forming species in the Philippines and their associated bacterial communities', funded and supported by the Department of Science and Technology (DOST) through the Philippine Council for Aquatic and Marine Research and Development (PCAMRD now PCAARRD) and a national project of the UNESCO IOC-SCOR programme entitled 'Global Ecology and Oceanography of Harmful Algal Blooms' (GEOHAB). We would also like to thank the Marine Toxinology Laboratory of the MSI headed by Dr Lourdes J. Cruz for the use of the sonicator and the spectrophotometer, Emelita Eugenio for her help in maintaining the algal cultures, and Garry Benico, Johanna Munar and Powell Marquez for some technical assistance. Also, we are grateful to the comments of some anonymous reviewers and to Dr Mary Anne Gonzales-Santos for her insights into Pyrodinium biology and ecology.	Aminot A., 2001, ICES Tech. Mar. Environ. Sci, V30, P1, DOI DOI 10.25607/OBP-278; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Azanza MPV, 2006, MICROB ECOL, V52, P756, DOI 10.1007/s00248-006-9128-7; Azanza R.V., 1997, SCI DILIMAN, V9, P1; Azanza R.V., 1997, 8 INT C HARMF ALG VI; AZANZACORRALES R, 1993, DEV MAR BIO, V3, P725; Binder J. 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J. Phycol.		2014	49	3					265	275		10.1080/09670262.2014.915062	http://dx.doi.org/10.1080/09670262.2014.915062			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AO0JU		Bronze			2025-03-11	WOS:000340995700001
J	Aydin, H; Yürür, EE; Uzar, S				Aydin, Hilal; Yurur, Emine Erdem; Uzar, Serdar			DINOFLAGELLATE CYST ASSEMBLAGES IN SURFACE SEDIMENTS FROM HOMA LAGOON (IZMIR BAY, EASTERN AEGEAN SEA, THE MEDITERRANEAN)	FRESENIUS ENVIRONMENTAL BULLETIN			English	Article						Dinoflagellate cyst; Homa Lagoon; Sediment; Aegean Sea	CLAM TAPES-DECUSSATUS; SPATIAL-DISTRIBUTION; ALEXANDRIUM-CATENELLA; ENVIRONMENTAL-FACTORS; MARINE-SEDIMENTS; RESTING CYSTS; DINOPHYCEAE; ATLANTIC; MASSACHUSETTS; POPULATIONS	The occurrence and abundance of dinoflagellate cysts was investigated for the first time in Homa Lagoon, one of the most important lagoons of Aegean Coast of Turkey. Twelve cyst morphotypes were identified and cyst abundance was ranged between 15 and 71 cyst g(-1) dry weight sediment in the study area. Dinoflagellate cyst assemblages were mainly dominated by cyst of Alexandrium minutum, Spiniferites delicatus, Spiniferites bulloideus. Sediment types were mainly clay and silty sand. Dinoflagellate cysts were particularly distributed in the clay and silty sediment.	[Aydin, Hilal; Yurur, Emine Erdem; Uzar, Serdar] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, Manisa, Turkey	Celal Bayar University	Aydin, H (通讯作者)，Celal Bayar Univ, Fac Sci & Arts, Dept Biol, Muradiye Campus, Manisa, Turkey.	hilalaydin66@gmail.com	UZAR, SERDAR/G-9956-2014	UZAR, SERDAR/0000-0002-9477-7413				Angles S., 2011, 9 INT C FOSS MOD DIN, P9; Anglès S, 2010, DEEP-SEA RES PT II, V57, P210, DOI 10.1016/j.dsr2.2009.09.002; [Anonymous], 2009, EGE U URUNLERI DERGI; [Anonymous], 1996, HARMFUL TOXIC ALGAL; [Anonymous], 2007, SAFETY PRECAUTIONS M, P1; Atilgan I, 2001, EU J FISH AQUAT SCI, V18, P225; Aydin H, 2011, MAR MICROPALEONTOL, V80, P44, DOI 10.1016/j.marmicro.2011.03.004; Bayhan B, 2008, J ANIM VET ADV, V7, P1146; Biebow N., 1993, 5 INT C MOD FOSS DIN, P20; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; Borel C.M., 2006, ARGENTINIA GEOACTA, V31, P23; BRADFORD MR, 1975, CAN J BOT, V53, P3064, DOI 10.1139/b75-335; Can E., 2009, TRANSITIONAL WATER B, V3, P10; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Genovesi B, 2007, HARMFUL ALGAE, V6, P837, DOI 10.1016/j.hal.2007.04.007; Genovesi B, 2011, J PLANKTON RES, V33, P405, DOI 10.1093/plankt/fbq127; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Grill S., 1995, POLEN, V7, P40; Horner RA, 2011, HARMFUL ALGAE, V11, P96, DOI 10.1016/j.hal.2011.08.004; Irwin A, 2003, HARMFUL ALGAE, V2, P61, DOI 10.1016/S1568-9883(02)00084-7; Joyce LB, 2005, HARMFUL ALGAE, V4, P309, DOI 10.1016/j.hal.2004.08.001; Kjerfve Bjorn, 1994, V60, P1; Kremp A, 2000, J PLANKTON RES, V22, P2155, DOI 10.1093/plankt/22.11.2155; 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., 2000, TECHNICAL GUIDE MODE; Matsuoka K., 2004, ATLAS MODERN DINOFLA; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Mudie PJ, 2004, REV PALAEOBOT PALYNO, V128, P143, DOI 10.1016/S0034-6667(03)00117-9; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Onen M., 1991, S 10 YEAR ED IZM; Pospelova V, 2005, MAR ECOL PROG SER, V292, P23, DOI 10.3354/meps292023; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Pulat I., 2003, EGE U J FISHERIES AQ, V20, P399; Ribeiro S, 2008, MAR MICROPALEONTOL, V68, P156, DOI 10.1016/j.marmicro.2008.01.013; Rochon A., 1999, American Association of Stratigraphic Palynologists Contributions Series, V35, P1, DOI DOI 10.1016/0377-8398(94)00016-G; Sabanci FÇ, 2012, TURK J FISH AQUAT SC, V12, P841, DOI 10.4194/1303-2712-v12_4_12; Sabanci FC, 2011, FRESEN ENVIRON BULL, V20, P346; Sabanci FÇ, 2010, TURK J BOT, V34, P531, DOI 10.3906/bot-0912-285; Satta CT, 2014, ESTUAR COAST, V37, P646, DOI 10.1007/s12237-013-9705-1; Satta CT, 2010, DEEP-SEA RES PT II, V57, P256, DOI 10.1016/j.dsr2.2009.09.013; Serdar S, 2007, AQUACULT ENG, V37, P89, DOI 10.1016/j.aquaeng.2007.02.004; Serdar S, 2009, AQUACULTURE, V293, P81, DOI 10.1016/j.aquaculture.2009.03.052; Shannon CE., 1949, MATH THEORY COMMUNIC, P1; Strickland J.D.H., 1972, B FISH RES BOARD CAN, V157, P310, DOI DOI 10.1002/IROH.19700550118; Uluturhan E, 2011, MAR POLLUT BULL, V62, P1989, DOI 10.1016/j.marpolbul.2011.06.019; Unsal S., 2000, EGE U J FISHERIES AQ, V17, P85; Uzar S, 2010, SCI RES ESSAYS, V5, P285; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; Yazici M, 2007, SU URUN DERG, V24, P267; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	59	9	9	30	71	PARLAR SCIENTIFIC PUBLICATIONS (P S P)	FREISING	ANGERSTR. 12, 85354 FREISING, GERMANY	1018-4619	1610-2304		FRESEN ENVIRON BULL	Fresenius Environ. Bull.		2014	23	8					1795	1801						7	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	AN3TV					2025-03-11	WOS:000340512500009
S	Wilkinson, IP; Poirier, C; Head, MJ; Sayer, CD; Tibby, J		Waters, CN; Zalasiewicz, JA; Williams, M; Ellis, M; Snelling, AM		Wilkinson, I. P.; Poirier, C.; Head, M. J.; Sayer, C. D.; Tibby, J.			Microbiotic signatures of the Anthropocene in marginal marine and freshwater palaeoenvironments	STRATIGRAPHICAL BASIS FOR THE ANTHROPOCENE	Geological Society Special Publication		English	Article; Book Chapter							DINOFLAGELLATE GYMNODINIUM-CATENATUM; CYPRIDEIS-TOROSA CRUSTACEA; KATTEGAT-SKAGERRAK REGION; CANDIDATE REFERENCE LAKES; MURRAY-DARLING BASIN; ESTUARY SOUTHERN BAY; LATE-HOLOCENE; LAND-USE; ENVIRONMENTAL-CHANGES; FORAMINIFERAL RECORD	The term 'Anthropocene' has been proposed to indicate a geological interval characterized by global anthropogenic environmental change. This paper attempts to recognize a method by which the Anthropocene can be defined micropalaeontologically. In order to do this, microfloras and microfaunas (diatoms, macrophytes, dinoflagellate cysts, foraminifera and ostracods) from nearshore waters through to paralic and freshwater aquatic milieux are considered, and biotic variability with an anthropogenic causation identified. Microbiotic change can be related to anthropogenically induced extinctions, pollution-related mutation, environmentally influenced assemblage variability, geochemistry of carapaces/tests, floral change related to lacustrine acidification, faunal and floral correlation to industrial and agricultural signatures and introduction of exotic species via shipping. The influence of humanity on a local scale can be recognized in assemblages as far back as 5000 years BP. However, widespread anthropogenic change took place in Europe and America, particularly in the nineteenth and twentieth centuries, although in Asia (e.g. Japan) it cannot be observed prior to the twentieth century. Profound and global biotic change began in the mid-twentieth century and, if the Anthropocene is to be defined in this way, then the period 1940-1945 might encompass the biotic base of the interval.	[Wilkinson, I. P.] British Geol Survey, Nottingham NG12 5GG, England; [Wilkinson, I. P.] Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England; [Poirier, C.] Univ La Rochelle, CNRS, Littoral Environm Soc, F-17000 La Rochelle, France; [Head, M. J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Sayer, C. D.] UCL, Dept Geog, Environm Change Res Ctr, London WC1E 6BT, England; [Tibby, J.] Univ Adelaide, Dept Geog Environm & Populat, Adelaide, SA 5005, Australia	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Leicester; Centre National de la Recherche Scientifique (CNRS); La Rochelle Universite; Brock University; University of London; University College London; University of Adelaide	Wilkinson, IP (通讯作者)，British Geol Survey, Nottingham NG12 5GG, England.	ipw@bgs.ac.uk	; Poirier, Clement/B-9652-2015	Tibby, John/0000-0002-5897-2932; Poirier, Clement/0000-0002-8311-8463	NERC [bgs05002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		ABE K, 1983, Journal of the Faculty of Science University of Tokyo Section II Geology Mineralogy Geography Geophysics, V20, P443; Adl SM, 2012, J EUKARYOT MICROBIOL, V59, P429, DOI 10.1111/j.1550-7408.2012.00644.x; ALADIN NV, 1993, OSTRACODA IN THE EARTH AND LIFE SCIENCES, P387; Allen PE, 2011, HYDROBIOLOGIA, V668, P203, DOI 10.1007/s10750-011-0711-7; Almeida IM, 2009, J COASTAL RES, P574; Alve E., 1991, Holocene, V1, P243, DOI 10.1177/095968369100100306; Alve E, 2000, T GEOBIOL, V15, P323; Alve E., 1996, Nor. 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J	Fani, F; Nuccio, C; Lazzara, L; Massi, L; Battocchi, C; Penna, A				Fani, F.; Nuccio, C.; Lazzara, L.; Massi, L.; Battocchi, C.; Penna, A.			<i>Fibrocapsa japonica</i> (Raphidophyceae) occurrence and ecological features within the phytoplankton assemblage of a cyclonic eddy, offshore the Eastern Alboran Sea	MEDITERRANEAN MARINE SCIENCE			English	Article						Fibrocapsa japonica; Harmful Algal Bloom (HAB); Western Mediterranean Sea; cyclonic eddy; 5.8S-ITS rDNA	SHORT-TERM VARIABILITY; COASTAL SEDIMENTS; MEDITERRANEAN-SEA; RESTING CYSTS; GROWTH; STRAINS; HARMFUL; FRONT; DINOFLAGELLATE; CHLOROPHYLLS	The Raphidophycean Fibrocapsa japonica Toriumi & Takano was detected for the first time offshore in the Eastern Alboran Sea (Western Mediterranean) in October 2006. Its distribution appeared very localised and atypical, as it was abundant in the open waters of a cyclonic eddy. Microscope counts of the natural phytoplankton assemblages revealed that F. japonica was dominant in the microplankton, together with Dinophyceae, within and below the cyclonic nutrient-rich dome (25 - 30 m). Bacillariophyceae were the primary microplanktonic fraction in only a few samples on the edges of the eddy. Moderately high abundances of F. japonica (maximum of 60 cells ml(-1)), with preliminary cysts and many cells aggregated in mucous nets, indicated a senescent phase. Despite the Atlantic origin of the cyclonic water masses, the molecular identification and the water temperature of 15 degrees C, which could have favoured pre-cyst formation, would suggest a Mediterranean source for F. japonica cells. Finally, we hypothesise that F. japonica, which is generally a coastal species, could have a coastal origin. In fact, F. japonica was mainly detected at a depth of 40-60 m at the coastal sites and at 25-30 m at the cyclonic dome. F. japonica generally being a coastal species, it can be hypothesised that it was entrapped by the cyclonic eddy, which typically detaches from the coastal waters, and thus carried offshore to the cyclonic waters.	[Fani, F.; Nuccio, C.; Lazzara, L.; Massi, L.] Univ Florence, Dipartimento Biol, I-50121 Florence, Italy; [Battocchi, C.; Penna, A.] Univ Urbino, Dipartimento Sci Biomol, Sez Biol Ambientale, I-61121 Pesaro, Italy	University of Florence; University of Urbino	Fani, F (通讯作者)，Univ Florence, Dipartimento Biol, Via PA Micheli 1, I-50121 Florence, Italy.	fabiola.fani@unifi.it	; Lazzara, Luigi/C-6838-2012	Nuccio, Caterina/0000-0002-4750-9782; Lazzara, Luigi/0000-0002-1351-9683	ordinary Scientific Research funds of the Universita di Firenze	ordinary Scientific Research funds of the Universita di Firenze	This work was financed by ordinary Scientific Research funds of the Universita di Firenze (ex 60% MIUR) and was part of F. Fani's PhD Thesis. We thank Alberto Ribotti (CNR - IAMC), Mireno Borghini (CNR - ISMAR) and the crew of the R/V 'Urania' for their support during the oceanographic cruise. The authors want to also thank Gian Pietro Gasparini for his helpful suggestions on the hydrological analysis and Karin de Boer for confirming the F. japonica pre-cyst identification. The authors wish to acknowledge the anonymous reviewers whose suggestions improved the manuscript.	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J	Shumilovskikh, LS; Fleitmann, D; Nowaczyk, NR; Behling, H; Marret, F; Wegwerth, A; Arz, HW				Shumilovskikh, L. S.; Fleitmann, D.; Nowaczyk, N. R.; Behling, H.; Marret, F.; Wegwerth, A.; Arz, H. W.			Orbital- and millennial-scale environmental changes between 64 and 20 ka BP recorded in Black Sea sediments	CLIMATE OF THE PAST			English	Article							LAST GLACIAL PERIOD; LASCHAMP GEOMAGNETIC EXCURSION; DINOFLAGELLATE CYST RECORD; OXYGEN-ISOTOPE RECORDS; CHAINE DES PUYS; NORTH-ATLANTIC; MEDITERRANEAN REGION; HYDROLOGICAL CHANGES; SURFACE CONDITIONS; HOLOCENE CLIMATE	High-resolution pollen and dinoflagellate cyst records from sediment core M72/5-25-GC1 were used to reconstruct vegetation dynamics in northern Anatolia and surface conditions of the Black Sea between 64 and 20 ka BP. During this period, the dominance of Artemisia in the pollen record indicates a steppe landscape and arid climate conditions. However, the concomitant presence of temperate arboreal pollen suggests the existence of glacial refugia in northern Anatolia. Long-term glacial vegetation dynamics reveal two major arid phases similar to 64-55 and 40-32 ka BP, and two major humid phases similar to 54-45 and 28-20 ka BP, correlating with higher and lower summer insolation, respectively. Dansgaard-Oeschger (D-O) cycles are clearly indicated by the 25-GC1 pollen record. Greenland interstadials are characterized by a marked increase in temperate tree pollen, indicating a spread of forests due to warm/wet conditions in northern Anatolia, whereas Greenland stadials reveal cold and arid conditions as indicated by spread of xerophytic biomes. There is evidence for a phase lag of similar to 500 to 1500 yr between initial warming and forest expansion, possibly due to successive changes in atmospheric circulation in the North Atlantic sector. The dominance of Pyxidinopsis psilata and Spiniferites cruciformis in the dinocyst record indicates brackish Black Sea conditions during the entire glacial period. The decrease of marine indicators (marine dinocysts, acritarchs) at similar to 54 ka BP and increase of freshwater algae (Pediastrum, Botryococcus) from 32 to 25 ka BP reveals freshening of the Black Sea surface water. This freshening is possibly related to humid phases in the region, to connection between Caspian Sea and Black Sea, to seasonal freshening by floating ice, and/or to closer position of river mouths due to low sea level. In the southern Black Sea, Greenland interstadials are clearly indicated by high dinocyst concentrations and calcium carbonate content, as a result of an increase in primary productivity. Heinrich events show a similar impact on the environment in the northern Anatolia/Black Sea region as Greenland stadials.	[Shumilovskikh, L. S.; Behling, H.] Univ Gottingen, Dept Palynol & Climate Dynam, D-37073 Gottingen, Germany; [Fleitmann, D.] Univ Reading, Dept Archaeol, Sch Archaeol Geog & Environm Sci, Reading, Berks, England; [Fleitmann, D.] Inst Geol Sci, Bern, Switzerland; [Fleitmann, D.] Univ Bern, Oeschger Ctr Climate Change Res, Bern, Switzerland; [Nowaczyk, N. R.] Helmholtz Ctr Potsdam GFZ German Res Ctr Geosci, Potsdam, Germany; [Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 3BX, Merseyside, England; [Wegwerth, A.; Arz, H. W.] Leibniz Inst Balt Sea Res Warnemunde, Rostock, Germany	University of Gottingen; University of Reading; University of Bern; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; University of Liverpool; Leibniz Institut fur Ostseeforschung Warnemunde	Shumilovskikh, LS (通讯作者)，Univ Gottingen, Dept Palynol & Climate Dynam, D-37073 Gottingen, Germany.	shumilovskikh@yahoo.com	Fleitmann, Domnik/HSF-0516-2023; Arz, Helge/A-6659-2013; Shumilovskikh, Lyudmila/P-2493-2015	Fleitmann, Dominik/0000-0001-5977-8835; Wegwerth, Antje/0000-0002-5104-9408; Shumilovskikh, Lyudmila/0000-0002-7429-3163; Arz, Helge Wolfgang/0000-0002-1997-1718; Marret-Davies, Fabienne/0000-0003-4244-0437	PAGES; Deutsche Forschungsgemeinschaft (DFG) [SPP 1266, BE 2116/20-1, BE 2116/20-2, AR 367/9-1, FL 710/1-1]; Swiss National Science Foundation [PP002-110554/1]	PAGES; Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); Swiss National Science Foundation(Swiss National Science Foundation (SNSF))	We thank the guest editor of Climate of the Past R. Saraswat, reviewers M. F. Sanchez Goni and U. Muller for critical reading and improving the manuscript. Special thanks go to the captain and crew of R/V Meteor for their support and contribution to the overall success of the M72/5 Black Sea research cruise in 2007. The first author thanks PAGES for organization of Young Scientist Meeting in 2013 and financial support. This work is financially supported by the Deutsche Forschungsgemeinschaft (DFG) within the SPP 1266 "INTERDYNAMIC" (BE 2116/20-1, 2, AR 367/9-1, FL 710/1-1) and the Swiss National Science Foundation (grant PP002-110554/1 to D. Fleitmann).	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J	Blanco, EP; Lewis, J				Blanco, Eva Perez; Lewis, Jane			A comparative study of Alexandrium tamarense cyst distribution in Belfast Lough	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Alexandrium tamarense; anthropogenic activity; Belfast Lough; cyst concentration; cyst distribution; sediment disturbance	DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; RESTING CYSTS; PUGET-SOUND; EUTROPHICATION; GERMINATION; INDICATORS; CATENELLA; GULF; BAY	Alexandrium tamarense is a cyst-forming dinoflagellate that can cause toxicity in shellfish. Belfast Lough, in northeast Ireland, has experienced toxicity events due to the presence of A. tamarense, which are monitored because of shellfish farms in the Lough. Since 1992 anthropogenic influences on the Lough have changed with the introduction of a 'fast cat' ferry service and an increase in mussel farming. In 2002 Belfast Lough was surveyed for A. tamarense cyst distribution in the sediments and the results are compared to a previous cyst survey carried out in the Lough in 1992. Cyst numbers were generally lower in 2002 than in 1992 (t-test, P < 0.01). The highest concentration found in 2002 was 1058 cysts g(-1) dry sediment compared with 3330 in 1992. Although sediment disturbance increased in the period between the surveys and plays a role in cyst distribution, A. tamarense cysts are still present in the seabed of the Lough. These cysts remain an important repository of inoculating cells for A. tamarense blooms that have not been removed by the recent anthropogenic activity in the Lough and therefore the requirement for monitoring remains. Comparisons between cyst counts per volume of wet sediment and per weight of dry sediment were carried out, and although the first is needed for ecological studies allowing a deeper analysis, it is also recommended that cyst counts per dry weight of sediment are always reported for wider comparative purposes.	[Blanco, Eva Perez; Lewis, Jane] Univ Westminster, Fac Sci & Technol, London W1W 6UW, England	University of Westminster	Blanco, EP (通讯作者)，Linnaeus Univ, Ctr Ecol & Evolut Microbial Model Syst EEMiS, SE-39182 Kalmar, Sweden.	evaperezi@gmail.com			Centre for the Environment, Fisheries and Aquaculture Science (CEFAS)	Centre for the Environment, Fisheries and Aquaculture Science (CEFAS)	The authors would like to thank Dr Tim Tylor for providing his data from 1992 for comparison purposes, and to Drs April McKinney, Matt Service and Heather Moore for their help in sample collection and the data and information provided, as well as Drs Adam Mellor, M. E. Charlesworth and all the crew who helped during sample collection from the Aquatic Sciences Research Division (ASRD) of the Department of Agriculture in Northern Ireland. This work was funded by the Centre for the Environment, Fisheries and Aquaculture Science (CEFAS).	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Phycol.		2014	49	2					255	263		10.1080/09670262.2014.912761	http://dx.doi.org/10.1080/09670262.2014.912761			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AJ2ZH					2025-03-11	WOS:000337533700005
J	Vandenberghe, N; Harris, WB; Wampler, JM; Houthuys, R; Louwye, S; Adriaens, R; Vos, K; Lanckacker, T; Matthijs, J; Deckers, J; Verhaegen, J; Laga, P; Westerhoff, W; Munsterman, D				Vandenberghe, Noel; Harris, W. Burleigh; Wampler, J. M.; Houthuys, Rik; Louwye, Stephen; Adriaens, Rieko; Vos, Koen; Lanckacker, Timothy; Matthijs, Johan; Deckers, Jef; Verhaegen, Jasper; Laga, Piet; Westerhoff, Wim; Munsterman, Dirk			The implications of K-Ar glauconite dating of the Diest Formation on the paleogeography of the Upper Miocene in Belgium	GEOLOGICA BELGICA			English	Article						Glauconite reworking; Tortonian; Campine; Hageland; paleogeography	NORTH-SEA BASIN; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SOUTHERN BORDER; STRATIGRAPHY; MIDDLE; NEOGENE; SANDS	The glauconite-rich Diest Formation in central and north Belgium contains sands in the Campine subsurface and the hilly Hageland area that can be distinguished from each other. The Hageland Diest Sands member contains no stratigraphically relevant fossils while in the Campine subsurface dinoflagellate cysts are common and show a stratigraphic range covering the entire Tortonian stage. K-Ar dates were determined for glauconite from 13 selected samples spread over both areas. A glauconite date corresponding to the earliest Tortonian indicates newly formed glauconite was incorporated into a greensand at the base of the Diest Formation in the central Campine area. All other dates point at reworked glauconite and can be organized in two groups, one reflecting a Burdigalian age and another reflecting a Langhian age. These data and the thickness and glauconite content of the Diest Formation imply massive reworking of older Miocene deposits. The paleogeographic implications of these data lead to the tentative recognition of two Tortonian sedimentary sequences. An older one corresponding to dinoflagellate biochron DN8 comprises the Deurne Member, part of the Dessel Member, the Hageland Diest member, the eastern Campine Diest member and some basal sands of the Diest Formation in the central Campine. A younger sequence corresponding to dinoilagellate biochrons DN9 and 10 was strongly influenced by the prograding proto-Rhine delta front in the Roer Valley Graben to the northeast. The subsiding Campine basin was filled from east to west during this second cycle.	[Vandenberghe, Noel; Adriaens, Rieko; Vos, Koen; Verhaegen, Jasper] Katholieke Univ Leuven, Dept Earth & Environm Sci, Louvain, Belgium; [Harris, W. Burleigh] North Carolina Geol Survey, Raleigh, NC 27699 USA; [Wampler, J. M.] Georgia State Univ, Dept Geosci, Atlanta, GA 30303 USA; [Houthuys, Rik] Geoconsultant, Halle, Belgium; [Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Lanckacker, Timothy; Matthijs, Johan; Deckers, Jef] Vlaamse Instelling Technol Onderzoek, Flemish Inst Technol Res, B-2400 Mol, Belgium; [Laga, Piet] Belgian Geol Survey, Brussels, Belgium; [Westerhoff, Wim; Munsterman, Dirk] Geol Survey Netherlands TNO, Utrecht, Netherlands	KU Leuven; University System of Georgia; Georgia State University; Ghent University; VITO; Netherlands Organization Applied Science Research	Vandenberghe, N (通讯作者)，Katholieke Univ Leuven, Dept Earth & Environm Sci, Louvain, Belgium.	Noel.Vandenberghe@ees.kuleuven.be; harrisw@uncw.edu; rik.houthtuys@telenet.be; Stephen.Louwye@UGent.be; jef.deckers@vito.be; Piet.laga@skynet.be; wim.westerhoff@tno.nl; dirk.munsterman@tno.nl	Verhaegen, Jasper/S-5729-2019; Vos, Kilian/AAW-3454-2020; Louwye, Stephen/D-3856-2012	Verhaegen, Jasper/0000-0002-9629-2655; Louwye, Stephen/0000-0003-4814-4313				Amorosi A, 2007, DEEP-SEA RES PT II, V54, P1364, DOI 10.1016/j.dsr2.2007.04.006; [Anonymous], 2010, Bulletin de la Societe Geologique du Nord; [Anonymous], BASIN RES; Bastin A., 1966, INGENIEURSBLAD, V35, P547; Dalrymple G.B., 1969, POTASSIUM ARGON DATI; Dalrymple RW, 2007, EARTH-SCI REV, V81, P135, DOI 10.1016/j.earscirev.2006.10.002; De Batist M, 1998, GEOL MIJNBOUW, V77, P17, DOI 10.1023/A:1003446611678; de Heinzelin J., 1963, MEMOIRES SOCIETE BEI, P247; De Man E, 2010, EPISODES, V33, P3; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; Delvaux E., 1884, ANN SOC GEOL BELG, V12, P74; Demyttenaere R., 1989, Letteren en Schone Kunsten van Belgi, V51, P51; Demyttenaere R., 1988, THESIS; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Geets S., 1991, NATUURWETENSCHAPPELI, V73, P3; Gliese J., 1978, GEOL MIJNBOUW, V57, P517; Gulinck M., 1964, ARCH BELGIAN GEOLOGI; Gulinck M., 1962, MEMOIRES SOC BELGE G, V6, P30; Gulinck M., 1973, ARCH BELGIAN GEOLOGI; Gullentops F, 1957, B SOC BELG GEOL, V66, P81; Gullentops F., 1988, I A S 9 EUR REG M EX, p[226, 255]; Gullentops F., 1963, 6 C INT SED BELG PAY, P7; Gullentops F., 1999, AARDKUNDIGE MEDEDELI, V9, P191; Hardenbol J., 1998, SPECIAL PUBLICATION, V60; Harris W.B., 1975, THESIS; HARRIS WB, 1974, GEOL SOC AM BULL, V85, P1475, DOI 10.1130/0016-7606(1974)85<1475:RSOCLG>2.0.CO;2; Hilgen FJ, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P923, DOI 10.1016/B978-0-444-59425-9.00029-9; Hooyberghs HJF, 2005, NEUES JAHRB GEOL P-A, V237, P5, DOI 10.1127/njgpa/237/2005/5; Houbolt J. 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Jahrb.; Wong T.H.E., 2007, Geology of the Netherlands, Netherlands, P151; Zaitlin B.A., 1994, STRATIGRAPHIC ORG IN, V51, P45, DOI [DOI 10.2110/PEC.94.12.0045, 10.2110/pec.94.12.0045]	74	36	36	0	7	GEOLOGICA BELGICA	BRUSSELS	JENNER STREET 13, BRUSSELS, BELGIUM	1374-8505	2034-1954		GEOL BELG	Geol. Belg.		2014	17	2					161	174						14	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AJ3GV					2025-03-11	WOS:000337555400005
J	Sinnyovsky, D; Pavlishina, P				Sinnyovsky, Dimitar; Pavlishina, Polina			NANNOPLANKTON AND PALYNOLOGICAL EVIDENCE FOR THE ALBIAN-CENOMANIAN BOUNDARY IN NORTHWEST BULGARIA	COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES			English	Article						Albian-Cenomanian boundary; calcareous nannofossils; dinoflagelate cysts		Albian-Cenomanian grey-green marl succession crops out at several restricted outcrops north of Rabisha mound in Northwest Bulgaria. The continuous sequence near Tolovitsa karst spring is characterised by calcareous nannofossils and dinoflagellate cysts. It is subdivided in two nannofossil zones: Eiffellithus turriseiffelii and Lithraphidites acutum. The former is subdivided in two subzones: Prediscosphaera columnata and Prediscosphaera cretacea. The boundary between them is used to define the Albian-Cenomanian boundary. Thus, the present study demonstrates the higher stratigraphic potential of this event for the Albian-Cenomanian boundary, and provides a new reliable datum for its identification. Dinoflagellate cyst assemblages indicate the Litosphaeridium siphoniphorum dinocyst zone. The concurrent presence of L. siphoniphorum, E. spinosa, X. alatum, P. infusorioides, P. cingulatum and O. costata allows correlation to its lower part and confirms again a latest Albian - earliest Cenomanian age for the studied interval. High amounts of granular amorphous organic matter (AOM), together with sharp increase in dinocyst abundance in the lowermost part of the section could be considered to indicate the well-documented global latest Albian ocean anoxic event (OAE 1d).	[Sinnyovsky, Dimitar] Univ Min & Geol St Ivan Rilski, Geol & Geoinformat Dept, Sofia 1700, Bulgaria; [Pavlishina, Polina] Sofia Univ St Kliment Ohridski, Dept Geol Palaeontol & Fossil Fuels, Sofia 1504, Bulgaria	University of Mining & Geology - Bulgaria; University of Sofia	Sinnyovsky, D (通讯作者)，Univ Min & Geol St Ivan Rilski, Geol & Geoinformat Dept, Sofia 1700, Bulgaria.	sinsky@mgu.bg	Pavlishina, Polina/AAL-5710-2021	Pavlishina, Polina/0000-0002-1172-9142	Bulgarian Science Fund [DDVU 02/72]	Bulgarian Science Fund(National Science Fund of Bulgaria)	This investigation is a contribution to the Project DDVU 02/72 of the Bulgarian Science Fund.	Bown P.R., 1998, P86; Burnett J.A., 1998, P132; Foucher J.-C., 1998, SEPM SPECIAL PUBLICA, V60; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; Granet G., 2012, GEOSCIENCE; JOLKICHEV N., 1988, REV BULGARIAN GEOLOG, V49, P24; Kennedy WJ, 2004, EPISODES, V27, P21, DOI 10.18814/epiiugs/2004/v27i1/003; Leckie RM, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2001PA000623; Leereveld H., 1995, LPP CONTRIBUTION SER, V2; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; SINNYOVSKY D. S., 2013, UPPER CRETACEOUS NAN; 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]; TZANKOV TZ, 1972, GEOLOGIE, V21, P24; TZANKOV V., 1960, CONTR GEOL BULGARIA, V1, P204; WILLIAMS G. L., 2004, OCEAN DRILLING PROGR, V189, P1	16	1	1	0	2	PUBL HOUSE BULGARIAN ACAD SCI	SOFIA	ACADEMICIAN G BONCEV ST, 1113 SOFIA, BULGARIA	1310-1331			CR ACAD BULG SCI	C. R. Acad. Bulg. Sci.		2014	67	4					551	556						8	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	AI1UL					2025-03-11	WOS:000336640500013
J	Guler, MV; Borel, CM; Brinkhuis, H; Navarro, E; Astini, R				Veronica Guler, M.; Marcela Borel, C.; Brinkhuis, Henk; Navarro, Edgardo; Astini, Ricardo			BRACKISH TO FRESHWATER DINOFLAGELLATE CYST ASSEMBLAGES FROM THE LA COLONIA FORMATION (PALEOCENE?), NORTHEASTERN PATAGONIA, ARGENTINA	AMEGHINIANA			English	Article						Dinocysts; Green algae; Paleosalinity; Paleocene? Patagonia	BUENOS-AIRES; HOLOCENE; PALYNOMORPHS; BOTRYOCOCCUS; ACRITARCHS; DEPOSITS; NORTH; ALGAE	A palynological analysis of the section of La Colonia Formation exposed at Estancia San Miguel yielded conspicuous assemblages of organic-walled dinoflagellate cysts (dinocysts) and green algae. The monotypic palaeoperidinioid dinocyst assemblage of ? Ginginodinium sp. in the basal beds of this section indicates low-salinity water conditions in a restricted shallow marine paleoenvironment. The green-algae-dominated assemblages together with specimens of ? Morkallacysta spp., Dinocysts type P and ? Vesperopsis sp. recorded in the middle and upper part of the San Miguel section indicate brackish to freshwater and freshwater depositional conditions, respectively. The changes in the composition of the palynological assemblages, in agreement with the analysis of the sedimentary facies, reflect a salinity-drop in the water bodies and a progressive upward-shallowing trend. The occurrence of specimens of the neritic open marine Cribroperidinium spp., Apteodinium sp., Circulodinium sp. and Areoligera sp. cf. A. circumsenonensis Fensome et al. is here considered as reflecting contemporaneous transported material from the adjacent shelf. The marine part of the La Colonia Formation is associated to Late Cretaceous and Paleocene ages. Nevertheless, palynomorphs together with a stratigraphical criterion suggest an age non older than Paleocene for the deposits of the unit at the San Miguel section.	[Veronica Guler, M.; Marcela Borel, C.; Navarro, Edgardo] Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Brinkhuis, Henk] Univ Utrecht, Lab Palaeobot & Palynol, Dept Earth Sci, Fac Geosci, NL-3584 CD Utrecht, Netherlands; [Astini, Ricardo] UNC, CONICET, CICTERRA, Lab Anal Cuencas, Cordoba, Argentina; [Veronica Guler, M.; Marcela Borel, C.] Consejo Nacl Invest Cient & Tecn, INGEOSUR, RA-1033 Buenos Aires, DF, Argentina; [Navarro, Edgardo] Comis Invest Cient Prov Buenos Aires CIC, Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Utrecht University; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of Cordoba; Cicterra; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Comision de Investigaciones Cientificas	Guler, MV (通讯作者)，Univ Nacl Sur, Dept Geol, San Juan 670,B8000ICN, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	vguler@criba.edu.ar; maborel@criba.edu.ar; h.brinkhuis@uu.nl; enavarro@criba.edu.ar; raastini@gtwing.efn.uncor.edu	Brinkhuis, Henk/IUO-8165-2023	Borel, C. Marcela/0000-0001-5772-4534; Brinkhuis, Henk/0000-0003-0253-6610	 [PIP-CONICET 02047]		We are grateful to O.Cardenas for the palynological processing of part of the samples from the San Miguel section. We also thank M. Pramparo and an anonymous reviewer for their helpful comments and suggestions. This contribution was partially financed by grant PIP-CONICET 02047.	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J	Beiranvand, B; Ghasemi-Nejad, E; Kamali, MR; Ahmadi, A				Beiranvand, Bijan; Ghasemi-Nejad, Ebrahim; Kamali, Mohammad Reza; Ahmadi, Akram			Sequence stratigraphy of the Late Cretaceous-Paleocene Gurpi Formation in southwest Iran	GEOARABIA			English	Article							SEA-LEVEL CHANGE; TERTIARY BOUNDARY; CALCAREOUS NANNOFOSSIL; DINOFLAGELLATE CYSTS; FORAMINIFERAL BIOSTRATIGRAPHY; SERGIPE BASIN; PRODUCTIVITY; NORTH; ENVIRONMENTS; CIRCULATION	Facies associations, microplanktonic diversity, palynofacies variations, geochemical data, and natural gamma-ray logs were analyzed from the Danial and Gurpi sections of the Campanian-Selandian Gurpi Formation in the Zagros Mountains, southwest Iran. The biostratigraphic data indicate that deposition across the Cretaceous/Paleogene boundary was continuous in the Danial Section. In contrast, a minor stratigraphic break seems to be present in the Gurpi Section, where several planktonic foraminiferal subzones are not identified. Nine depositional sequences were interpreted and correlated between the two sections. They are apparently of great lateral extent because they closely correlate to the global sea-level cycles. The Maastrichtian maximum flooding surface MFS K180 (68 Ma) of the Arabian Plate was also identified. Detailed palynofacies analysis, integrated with standard tropical/subtropical planktonic foraminifera, indicate warm Neo-Tethyan upper-bathyal to middle-shelf depositional environments for the Gurpi Formation.	[Beiranvand, Bijan] NIOC, RIPI, Tehran, Iran; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Dept Geol, Tehran 14174, Iran; [Kamali, Mohammad Reza] Res Inst Petr Ind, Ctr Explorat & Prod, Tehran, Iran; [Ahmadi, Akram] RIPI, Tehran, Iran	National Iranian Oil Company (NIOC); University of Tehran	Beiranvand, B (通讯作者)，NIOC, RIPI, Tehran, Iran.	biranvandb@ripi.ir; eghasemi@khayam.ut.ac.ir; kamalimr@ripi.ir; ahmadi812000@yahoo.com	Ghasemi-Nejad, Ebrahim/AAF-6087-2020		Research Institute of Petroleum Industry (RIPI) of Iran	Research Institute of Petroleum Industry (RIPI) of Iran	This study was supported by the Research Institute of Petroleum Industry (RIPI) of Iran. We thank Mr. S.S. Hendi, Head of Exploration and Production Research Center for supporting the work and Mrs. E.H. Tavakoli and H. Alinaghian for processing the samples. The authors thank Roger Davies, Mike Bidgood and Moujahed Al-Husseini for their careful review and many constructive remarks that greatly improved the quality of this paper. Kathy Breining is thanked for proofreading the text and GeoArabia's Production Co-manager, Arnold Egdane, for designing the paper for press.	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J	Milzer, G; Giraudeau, J; Schmidt, S; Eynaud, F; Faust, J				Milzer, G.; Giraudeau, J.; Schmidt, S.; Eynaud, F.; Faust, J.			Qualitative and quantitative reconstructions of surface water characteristics and recent hydrographical changes in the Trondheimsfjord, central Norway	CLIMATE OF THE PAST			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; PLANKTONIC-FORAMINIFERA; HIGH-LATITUDES; SEA; SEDIMENTS; INDICATORS; PRODUCTIVITY; TEMPERATURE; PRESERVATION	In the present study we investigated dinocyst assemblages in the Trondheimsfjord over the last 25 to 50 yr from three well-dated multi-cores (Pb-210 and Cs-137) retrieved along the fjord axis. The downcore distribution of the dinocysts is discussed in view of changes in key hydrographic parameters of the surface waters (sea-surface temperatures (SSTs), sea-surface salinities (SSSs), and river discharges) monitored in the fjord. We examine the impact of the North Atlantic Oscillation pattern and of waste water supply from the local industry and agriculture on the fjord ecological state and thus dinocyst species diversity. Our results show that dinocyst production and diversity in the fjord is not evidently affected by human-induced eutrophication. Instead the assemblages appear to be mainly controlled by the NAO-related changes in nutrient availability and the physicochemical characteristics of the surface mixed layer. Still, discharges of major rivers have been modulated since 1985 by the implementation of hydropower plants, which certainly influences the amounts of nutrients supplied to the fjord. The impact, however, is variable according to the local geographical setting, and barely differentiated from natural changes in river run off. We ultimately test the use of the modern analogue technique (MAT) for the reconstruction of winter and summer SSTs and SSSs and annual primary productivity (PP) in this particular fjord setting. The reconstructed data are compared with time series of summer and winter SSTs and SSSs measured at 10m water depth, as well as with mean annual PPs along the Norwegian coast and in Scandinavian fjords. The reconstructions are generally in good agreement with the instrumental measurements and observations from other fjords. Major deviations can be attributed to peculiarities in the assemblages linked to the particular fjord setting and the related hydrological structure.	[Milzer, G.; Giraudeau, J.; Schmidt, S.; Eynaud, F.] Univ Bordeaux 1, CNRS, UMR5805, F-33405 Talence, France; [Faust, J.] Geol Survey Norway NGU, Trondheim, Norway	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Geological Survey of Norway	Milzer, G (通讯作者)，Univ Bordeaux 1, CNRS, UMR5805, Ave Fac, F-33405 Talence, France.	gcmilzer@gmx.de	Giraudeau, Jacques/AAF-5764-2019; Schmidt, Sabine/G-1193-2013	Eynaud, Frederique/0000-0003-1283-7425; Faust, Johan C./0000-0001-8177-7097; Schmidt, Sabine/0000-0002-5985-9747; Giraudeau, Jacques/0000-0002-5069-4667	European Community [238111]	European Community	This work is a contribution to the CASE initial training network funded by the European Community's 7th Framework Programme FP7 2007/2013, Marie-Curie Actions, under grant agreement no. 238111 (http://caseitn.epoc.ubordeaux1.fr/index.php/home.html). Temperature and salinity data sets from the fjord mooring hydrological stations are provided by the Trondheim Biological Station of the Norwegian University of Science and Technology. We gratefully acknowledge Bendik Eithun Halgunset from Sor-Trondelag Fylkeskommune, Viggo Finset from TronderEnergi Kraft AS, as well as Arne Jorgen Kjosnes and Eva Klausen from the Norwegian Water Resources and Energy Directorate for their cooperation, helpful suggestions and data access. Anne de Vernal (GEOTOP, UQAM) is gratefully acknowledged for her support, helpful suggestions and reference data. Ultimately, we would like to thank R. Telford (UIB, Norway) for critical comments and helpful discussions concerning statistical data treatment and transfer functions.	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Past.		2014	10	1					305	323		10.5194/cp-10-305-2014	http://dx.doi.org/10.5194/cp-10-305-2014			19	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	AE2XV		Green Submitted, gold			2025-03-11	WOS:000333837600021
J	Concheyro, A; Caramés, A; Amenábar, CR; Lescano, M				Concheyro, Andrea; Carames, Andrea; Amenabar, Cecilia R.; Lescano, Marina			Nannofossils, foraminifera and microforaminiferal linings in the Cenozoic diamictites of Cape Lamb, Vega Island, Antarctica	POLISH POLAR RESEARCH			English	Article						Antarctica; James Ross Basin; Cenozoic diamictites; calcareous nannofossils; Foraminifera; microforaminiferal linings	JAMES-ROSS-ISLAND; MARAMBIO SEYMOUR ISLAND; CALCAREOUS NANNOFOSSILS; BENTHIC FORAMINIFERS; BASIN; SEA; ATLANTIC; DEPOSITS	Micropaleontological and palynological samples from three Cenozoic diamictites at Cape Lamb, Vega Island, James Ross Basin were analysed. Fossiliferous samples yielded reworked and autochthonous assemblages of Mesozoic calcareous nannofossils, impoverished Cretaceous foraminifera together with Neogene species, as well as Late Cretaceous dinoflagellate cysts, pollen, spores and abundant Cenozoic microforaminiferal linings. The recovered nannoflora indicates Early Cretaceous (Hauterivian-Albian) and Late Cretaceous (Santonian-Early Campanian) ages, suggesting an intensive reworking of marine sediments. The presence of the Early Cretaceous species Nannoconus circularis Deres et Acheriteguy in the diamictite represents its first record for the James Ross Basin. The scarce foraminiferal fauna includes Pullenia jarvisi Cushman, which indicates reworking from lower Maastrichtian-lower Paleocene sediments, and also the Neogene autochthonous Trochammina sp. aff. T. intermedia. The inner-organic layer observed inside this specimen appears to be identical to microforaminiferal linings recovered from the same sample. Palynomorphs found in the studied samples suggest erosion from the underlying Snow Hill Island and the Lopez de Bertodano Formation beds (upper Campanian-upper Maastrichtian). These recovered assemblages indicate either different periods of deposition or reworking from diverse sources during Cenozoic glaciation, originating in James Ross Island and the Antarctic Peninsula with the influence of local sediment sources.	[Concheyro, Andrea; Carames, Andrea; Amenabar, Cecilia R.; Lescano, Marina] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Consejo Nacl Invest Cient & Tecn, IDEAN Inst Estudios Andinos Don Pablo Groeber, RA-1428 Buenos Aires, DF, Argentina; [Concheyro, Andrea; Amenabar, Cecilia R.] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, RA-1428 Buenos Aires, DF, Argentina; [Concheyro, Andrea; Amenabar, Cecilia R.] Inst Antartico Argentino, Buenos Aires, DF, Argentina	University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; Instituto Antartico Argentino	Concheyro, A (通讯作者)，Univ Buenos Aires, Fac Ciencias Exactas & Nat, Consejo Nacl Invest Cient & Tecn, IDEAN Inst Estudios Andinos Don Pablo Groeber, Pabellon 2 Ciudad Univ, RA-1428 Buenos Aires, DF, Argentina.	andrea@glfcen.uba.ar; carames@gl.fcen.uba.ar; amenabar@gl.fcen.uba.ar; lescano@gl.fcen.uba.ar		AMENABAR, CECILIA R./0000-0003-1280-3903	 [PICTO-2010-0112]		The authors are most grateful to J.M. Lirio for providing the samples, the Instituto Antartico Argentino for the logistic support during the Argentine Summer Antarctic Expedition 2007, P. Alvarez and S. Adamonis for sample preparations and picking, respectively, M.J. Clark for her assistance in English grammar, and the Centro de Microscopia Avanzada, Universidad de Buenos Aires, Argentina, for taking the SEM photographs. This paper is the contribution number R-119 of the Instituto de Estudios Andinos "Don Pablo Groeber" (IDEAN-CONICET). This work was supported by grant PICTO-2010-0112. We would like to thank Dr Brian T. Huber (Smithsonian Institution), Prof. Patrick G. Quilty (University of Tasmania) and two anonymous reviewers for their constructive remarks, which improved the paper.	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J	Jiang, T; Xu, YX; Li, Y; Jiang, TJ; Wu, F; Zhang, F				Jiang, Tao; Xu, Yixiao; Li, Yang; Jiang, Tianjiu; Wu, Feng; Zhang, Fan			Seasonal dynamics of <i>Alexandrium tamarense</i> and occurrence of paralytic shellfish poisoning toxins in bivalves in Nanji Islands, East China Sea	MARINE AND FRESHWATER RESEARCH			English	Article						HABs, marine biotoxins.	ENVIRONMENTAL-FACTORS; CRASSOSTREA-GIGAS; RESTING CYSTS; PSP TOXINS; DINOFLAGELLATE; RIVER; DINOPHYCEAE; ESTUARY; JAPAN; ACCUMULATION	A monitoring program for seasonal dynamics of A. tamarense and paralytic shellfish poisoning toxins (PSTs) in bivalves was carried out from April 2006 to March 2007 in Nanji Islands, East China Sea. Low abundances of A. tamarense (fewer than 4.0 x 10(2) cells L-1) were first observed on 15 April 2006. During middle May, blooms of A. tamarense were documented, with the mean density of 3.8 x 10(3) cells L-1 and 0.75 x 10(3) cells L-1, corresponding to surface and bottom water columns, respectively. Environmental conditions of temperature range 18-20 degrees C and salinity range 29.5-31 coincided with a high abundance of A. tamarense in the region, and the bloom collapse was likely to be a response to P limitation. Toxin concentrations in cultured Patinopecten yessoensis, Mytilus galloprovincialis and wild Mytilus coruscus during A. tamarense blooms ranged from 68.9 to 96.3 mu g STXeq per 100 g flesh. Toxin profiles were similar among bivalve shellfish samples, dominated by C1 and C2 in 51.4-64.6 mol% of toxins, with an average of 60.6 mol%, followed by GTX5, GTX1-GTX4, dcGTX2 and dcGTX3. However, from January to March 2007, lower toxin concentrations, 18.9-40.8 mu g STXeq per 100 g were found only in the wild Oyster sp., comprising GTX4, GTX5 and GTX1.	[Jiang, Tao; Jiang, Tianjiu; Wu, Feng; Zhang, Fan] Jinan Univ, Res Ctr Harmful Algae & Marine Biol, Guangzhou 510632, Guangdong, Peoples R China; [Xu, Yixiao] Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210093, Jiangsu, Peoples R China; [Li, Yang] S China Normal Univ, Coll Life Sci, Guangzhou 510630, Guangdong, Peoples R China	Jinan University; Nanjing University; South China Normal University	Jiang, TJ (通讯作者)，Jinan Univ, Res Ctr Harmful Algae & Marine Biol, Guangzhou 510632, Guangdong, Peoples R China.	tjiangtj@jnu.edu.cn	Jiang, Tao/AAQ-6588-2020		National Basic Research Program of China [2010CB428702]; National Marine Public Welfare Research Project of China [201305010]; National Natural Science Foundation of China [41106090]; Natural Science Foundation of Guangdong Province [S2011040003113]; Special Fund for Basic Scientific Research of Central Universities [21612401]; Wenzhou Science and Technology Plan Program [S2006A007]	National Basic Research Program of China(National Basic Research Program of China); National Marine Public Welfare Research Project of China; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Natural Science Foundation of Guangdong Province(National Natural Science Foundation of Guangdong Province); Special Fund for Basic Scientific Research of Central Universities; Wenzhou Science and Technology Plan Program	The authors thank Mr SP You and his colleagues for sample collection and nutrient measurements, and also Dr Richlen, Woods Hole Oceanographic Institution, for nice review and language help before submission. This research was supported by the National Basic Research Program of China (2010CB428702), the National Marine Public Welfare Research Project of China (201305010), the National Natural Science Foundation of China (41106090), and Natural Science Foundation of Guangdong Province (S2011040003113), the Special Fund for Basic Scientific Research of Central Universities (21612401), and the Wenzhou Science and Technology Plan Program (S2006A007).	Anderson DM, 1996, TOXICON, V34, P579, DOI 10.1016/0041-0101(95)00158-1; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; [Anonymous], MAR BIOT; BRAVO I, 1998, HARMFUL ALGAE, P356; Bricelj V. 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Freshw. Res.		2014	65	4					350	358		10.1071/MF13001	http://dx.doi.org/10.1071/MF13001			9	Fisheries; Limnology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology; Oceanography	AD3XW					2025-03-11	WOS:000333180800007
J	Kurokawa, T; Okamura, Y				Kurokawa, Tatsuki; Okamura, Yasushi			Mapping of sites facing aqueous environment of voltage-gated proton channel at resting state: A study with PEGylation protection	BIOCHIMICA ET BIOPHYSICA ACTA-BIOMEMBRANES			English	Article						Ion channel; Proton; Voltage; Membrane potential; Gating; pH	2 PORES; HV1; DOMAIN; DINOFLAGELLATE; COOPERATIVITY; MECHANISM; SENSOR; KV1.3	Hvi (also named, voltage-sensor only protein, VSOP) lacks an authentic pore domain, and its voltage sensor domain plays both roles in voltage sensing and proton permeation. The activities of a proton channel are intrinsic to protomers of Hvl, while Hvl is dimeric in biological membranes; cooperative gating is exerted by interaction between two protomers. As the signature pattern conserved among voltage-gated channels and voltage-sensing phosphatase, Hvl has multiple arginines intervened by two hydrophobic residues on the fourth transmembrane segment, 54. S4 moves upward relative to other helices upon depolarization, causing conformational change possibly leading to the formation of a proton-selective conduction pathway. However, detailed mechanisms of proton-selectivity and gating of fivl are unknown. Here we took an approach of PEGylation protection assay to define residues facing the aqueous environment of mouse Hvl (mHv1). Accessibilities of two maleimide molecules, N-ethylmaleimide (NEM) and 4-acetamido-4'-malehnidylstilbene-2,2'-disulfonic acid (AMS), were examined on cysteine introduced into individual sites. Only the first arginine on S4 (R1: R201) was inaccessible by NEM and AMS in mHvl. This is consistent with previous results of electrophysiology on the resting state channel, suggesting that the accessibility profile represents the resting state of mHvl. 0108, critical for proton selectivity, was accessible by AMS and NEM, suggesting that 0108 faces the vestibule. F146, a site critical for bloddng by a guanidiniumreagent, was accessible by NEM, suggesting that F146 also faces the inner vestibule. These findings suggest an inner vestibule lined by several residues on S2 including F146, D108 on S1, and the C-terminal half of S4. (C) 2013 Elsevier B.V. All rights reserved.	[Kurokawa, Tatsuki; Okamura, Yasushi] Osaka Univ, Grad Sch Med, Dept Physiol, Lab Integrat Physiol, Suita, Osaka 5650871, Japan; [Okamura, Yasushi] Osaka Univ, Grad Sch Frontier Biosci, Suita, Osaka 5650871, Japan	Osaka University; Osaka University	Okamura, Y (通讯作者)，Osaka Univ, Grad Sch Med, Dept Physiol, Lab Integrat Physiol, Yamada Oka 2-2, Suita, Osaka 5650871, Japan.	yokamura@phys2.med.osaka-u.ac.jp	Okamura, Yasushi/KIE-2106-2024		Ministry of Education, Culture, Sports, Science, and Technology (MEXT) [21229003, 21770171]; Grants-in-Aid for Scientific Research [21229003, 21770171] Funding Source: KAKEN	Ministry of Education, Culture, Sports, Science, and Technology (MEXT)(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 all members of the laboratory for helpful discussion. This work was supported by the Ministry of Education, Culture, Sports, Science, and Technology (MEXT) [grant numbers 21229003 and 21770171 (to Y.O. and T.K.)].	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Biophys. Acta-Biomembr.	JAN	2014	1838	1	B				382	387		10.1016/j.bbamem.2013.10.001	http://dx.doi.org/10.1016/j.bbamem.2013.10.001			6	Biochemistry & Molecular Biology; Biophysics	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Biophysics	AA0UX	24140009	Bronze			2025-03-11	WOS:000330814000031
J	Murray, SA; Hoppenrath, M; Orr, RJS; Bolch, C; John, U; Diwan, R; Yauwenas, R; Harwood, T; de Salas, M; Neilan, B; Hallegraeff, G				Murray, Shauna A.; Hoppenrath, Mona; Orr, Russell J. S.; Bolch, Christopher; John, Uwe; Diwan, Rutuja; Yauwenas, Rouna; Harwood, Tim; de Salas, Miguel; Neilan, Brett; Hallegraeff, Gustaaf			<i>Alexandrium</i> <i>diversaporum</i> sp. nov., a new non-saxitoxin producing species: Phylogeny, morphology and <i>sxtA</i> genes	HARMFUL ALGAE			English	Article						Alexandrium diversaporum; Phylogenetics; PSP; PST; Saxitoxin; sxtA; Systematics	PARALYTIC SHELLFISH TOXINS; DINOFLAGELLATE GENUS ALEXANDRIUM; HARMFUL ALGAL BLOOMS; GYMNODINIUM-CATENATUM; MINUTUM DINOPHYCEAE; COASTAL WATERS; DIVERSITY; CATENELLA; COMPLEX; BIOGEOGRAPHY	Species of the PST producing planktonic marine dinoflagellate genus Alexandrium have been intensively scrutinised, and it is therefore surprising that new taxa can still be found. Here we report a new species, Alexandrium diversaporum nov. sp., isolated from spherical cysts found at two sites in Tasmania, Australia. This species differs in its morphology from all previously reported Alexandrium species, possessing a unique combination of morphological features: the presence of 2 size classes of thecal pores on the cell surface, a medium cell size, the size and shape of the 6 '', 1', 2'''' and Sp plates, the lack of a ventral pore, a lack of anterior and posterior connecting pores, and a lack of chain formation. We determined the relationship of the two strains to other species of Alexandrium based on an alignment of concatenated SSU-ITS1, 5.8S, ITS2 and partial LSU ribosomal RNA sequences, and found A. diversaporum to be a sister group to Alexandrium leei with high support. A. leei shares several morphological features, including the relative size and shapes of the 6 '', 1', 2'''' and Sp plates and the fact that some strains of A. leei have two size classes of thecal pores. We examined A. diversaporum strains for saxitoxin production and found them to be non-toxic. The species lacked sequences for the domain A4 of sxtA, as has been previously found for non-saxitoxin producing species of Alexandrium. (C) 2013 Elsevier B.V. All rights reserved.	[Murray, Shauna A.; Diwan, Rutuja; Yauwenas, Rouna] Sydney Inst Marine Sci, Mosman, NSW, Australia; [Murray, Shauna A.; Neilan, Brett] Univ New S Wales, Sch Biotechnol & Biomol Sci, Sydney, NSW 2052, Australia; [Hoppenrath, Mona] German Ctr Marine Biodivers Res DZMB, Senckenberg Res Inst, D-26382 Wilhelmshaven, Germany; [Orr, Russell J. S.] Univ Oslo, Dept Biosci, Microbial Evolut Res Grp, N-0316 Oslo, Norway; [Bolch, Christopher] Univ Tasmania, Australian Maritime Coll, Natl Ctr Marine Conservat & Resource Sustainabil, Launceston, Tas 7250, Australia; [John, Uwe] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Institut, Sect Ecol Chem, Bremerhaven, Germany; [Harwood, Tim] Cawthron Inst, Nelson 7042, New Zealand; [de Salas, Miguel] Univ Tasmania, Tasmanian Herbarium, Hobart, Tas 7001, Australia; [Hallegraeff, Gustaaf] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas 7001, Australia	Sydney Institute of Marine Science; University of New South Wales Sydney; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); University of Oslo; University of Tasmania; Australian Maritime College; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Cawthron Institute; University of Tasmania; University of Tasmania	Murray, SA (通讯作者)，Univ Technol Sydney, Plant Funct Biol & Climate Change Cluster, Sydney, NSW 2007, Australia.	s.murray@unsw.edu.au	Murray, Shauna/JAN-6668-2023; Bolch, Christopher/J-7619-2014; Neilan, Brett/AGW-6984-2022; Harwood, Tim/H-3636-2012; Hallegraeff, Gustaaf/C-8351-2013; Neilan, Brett/I-5767-2012; John, Uwe/S-3009-2016; Murray, Shauna A/K-5781-2015	Hallegraeff, Gustaaf/0000-0001-8464-7343; Neilan, Brett/0000-0001-6113-772X; John, Uwe/0000-0002-1297-4086; Murray, Shauna A/0000-0001-7096-1307	Australian Research Council [DP120103199]	Australian Research Council(Australian Research Council)	This study was funded by the Australian Research Council Grants DP120103199 to SM and UJ. 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J	Cosgrove, S; Rathaille, AN; Raine, R				Cosgrove, Sarah; Rathaille, Aoife Ni; Raine, Robin			The influence of bloom intensity on the encystment rate and persistence of <i>Alexandrium minutum</i> in Cork Harbor, Ireland	HARMFUL ALGAE			English	Article						Alexandrium; Bloom dynamics; Cyst stocks; Encystment rate; Ireland	WHOLE-CELL HYBRIDIZATION; RESTING CYSTS; GENUS ALEXANDRIUM; POPULATION-DYNAMICS; COASTAL WATERS; DINOFLAGELLATE; DINOPHYCEAE; TAMARENSE; GERMINATION; GULF	Toxic Alexandrium minutum blooms recur annually in Cork Harbor, Ireland where they initiate in an inlet known as the North Channel. The dynamics of these blooms have been studied since 2003, and a high degree of inter-annual variability in the cell densities has been observed. Two intense blooms, with maximum cell densities >500,000 cells L-1, were observed in the summers of 2004 and 2011. Annual cyst surveys during winter found that cyst densities decreased after the 2004 bloom, and by 2010 an average of ca. 40 cysts g dry wt sediment(-1) was recorded. The intensity of blooms was found to be independent of the cyst density measured the previous winter. The cyst input to the sediment during both intense and low density blooms was measured directly through the deployment of sediment traps in the North Channel. The data allowed an estimate of the proportion of the A. minutum vegetative cells that underwent successful encystment, which averaged at 2.5% across a range of cell densities spanning three orders of magnitude. Maturation times of fresh cysts were determined at 5, 10 and 15 degrees C. The maturation time at 15 degrees C was found to be approximately 5 months, a value which increased by two months for a 5 degrees decrease in temperature. A cyst dynamics model was constructed based on the field data to simulate the temporal variation of A. minutum cysts in the oxic layer of sediment. It revealed that a degree of resuspension is required to prevent cyst stocks from becoming exhausted in the thin oxic layer at the surface of the sediment. The model also demonstrated that the cysts supplied by periodic intense blooms, which occur with a frequency of every 7-8 years, are not in themselves enough to allow the population to persist over long time scales (decades). The cyst input from interim blooms of lower density is however enough to ensure the annual inoculation of the water column with A. minutum cells. (C) 2013 Elsevier B.V. All rights reserved.	[Cosgrove, Sarah; Rathaille, Aoife Ni; Raine, Robin] Natl Univ Ireland, Ryan Inst, Galway, Ireland; [Raine, Robin] Natl Univ Ireland, Sch Nat Sci, Galway, Ireland	Ollscoil na Gaillimhe-University of Galway; Ollscoil na Gaillimhe-University of Galway	Cosgrove, S (通讯作者)，Natl Univ Ireland, Martin Ryan Bldg,Univ Rd, Galway, Ireland.	s.cosgrove2@nuigalway.ie			EC 6th Framework Program (SEED project) [GOCE-CT-2005-003375]; INTERREG IIIB (NWE: FINAL) programs; Irish IRCSET Enterprise Partnership Scheme with the Environmental Protection Agency; Irish Marine Institute under the National Development Plan	EC 6th Framework Program (SEED project); INTERREG IIIB (NWE: FINAL) programs; Irish IRCSET Enterprise Partnership Scheme with the Environmental Protection Agency(Environmental Protection Agency Ireland (EPA)); Irish Marine Institute under the National Development Plan	This work was funded through grants obtained from the EC 6th Framework Program (SEED project: GOCE-CT-2005-003375) and INTERREG IIIB (NWE: FINAL) programs. Postgraduate fellowships were awarded to S.C. from the Irish IRCSET Enterprise Partnership Scheme with the Environmental Protection Agency, and A. Ni R. as an RTDI Scholarship by the Irish Marine Institute under the National Development Plan (2000-2006). The authors would like to acknowledge the contributions of Gary McCoy, Nicolas Touzet, Isobel Evans, Paul O'Connor, Barbara O'Sullivan, Cathy Richards, Diarmaid Collins and Shane Thompstone for their assistance with fieldwork and sample processing. The assistance of Brian Byrne, Donal Geary, and David and Tristan Hugh-Jones throughout the program is also gratefully acknowledged.[SS]	Anderson D.M., 1980, J PHYCOL, V16; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 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 Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; Andrieux-Loyer F, 2008, BIOGEOCHEMISTRY, V88, P213, DOI 10.1007/s10533-008-9199-2; Anglès S, 2012, HARMFUL ALGAE, V16, P1, DOI 10.1016/j.hal.2011.12.006; Band-Schmidt CJ, 2003, BOT MAR, V46, P44, DOI 10.1515/BOT.2003.007; BINDER BJ, 1987, J PHYCOL, V23, P99; Blanco EP, 2009, HARMFUL ALGAE, V8, P518, DOI 10.1016/j.hal.2008.10.008; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Calbet A, 2003, MAR ECOL PROG SER, V259, P303, DOI 10.3354/meps259303; Cembella Allan D., 1998, NATO ASI Series Series G Ecological Sciences, V41, P381; Chambouvet A, 2008, SCIENCE, V322, P1254, DOI 10.1126/science.1164387; Chapelle A, 2010, J MARINE SYST, V83, P181, DOI 10.1016/j.jmarsys.2010.05.012; Cosgrove S., 2010, P 14 INT C HARMF ALG; Estrada M, 2010, DEEP-SEA RES PT II, V57, P308, DOI 10.1016/j.dsr2.2009.09.007; Figueroa RI, 2007, J PHYCOL, V43, P1039, DOI 10.1111/j.1529-8817.2007.00393.x; FRANCO JM, 1994, J APPL PHYCOL, V6, P275, DOI 10.1007/BF02181938; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Giacobbe MG, 2007, HYDROBIOLOGIA, V580, P125, DOI 10.1007/s10750-006-0459-7; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; He R., 2008, J GEOPHYS RES OCEANS, V113; Lewis J., 1998, J MAR BIOL ASSOC UK, V68, P701; Lewis J., 2002, RES ENCLOSED SEAS SE, V12, P113; Lilly EL, 2005, HARMFUL ALGAE, V4, P1004, DOI 10.1016/j.hal.2005.02.001; Lyons S., 2006, 2005SS43M1 EPA, P42; Matrai P, 2005, DEEP-SEA RES PT II, V52, P2560, DOI 10.1016/j.dsr2.2005.06.013; McDermott G., 2010, MICROSCOPIC MOL METH, P21; Miller PE, 1998, J PHYCOL, V34, P371, DOI 10.1046/j.1529-8817.1998.340371.x; Ni Rathaille A., 2008, P 12 INT C HARMF ALG, P223; Ni Rathaille A., 2009, P 6 INT C MOLL SHELL, P49; Ni Rathaille A., 2007, THESIS NATL U IRELAN; Parker N.S., 2000, 9 INT C HARMF ALG TA; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Probert I., 1999, THESIS U WESTMINSTER, P117; Rathaille AN, 2011, HARMFUL ALGAE, V10, P629, DOI 10.1016/j.hal.2011.04.015; Silke J., 1998, THESIS TRINITY COLL, P140; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1132, DOI 10.4319/lo.1997.42.5_part_2.1132; Sorokin YI, 1996, J SEA RES, V35, P251, DOI 10.1016/S1385-1101(96)90752-2; Stoeker D.K., 2012, BIOL ECOLOGY TINTINN; Touzet N, 2011, MAR ECOL PROG SER, V425, P21, DOI 10.3354/meps08983; Touzet N, 2008, AQUAT MICROB ECOL, V51, P285, DOI 10.3354/ame01189; Touzet N, 2007, PHYCOLOGIA, V46, P168, DOI 10.2216/06-11.1; Vila M, 2005, HARMFUL ALGAE, V4, P673, DOI 10.1016/j.hal.2004.07.006; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; Wyatt T., 2002, RES ENCLOSED SEAS SE, V12, P113	51	14	16	1	25	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	JAN	2014	31						114	124		10.1016/j.hal.2013.10.015	http://dx.doi.org/10.1016/j.hal.2013.10.015			11	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	300XO	28040100				2025-03-11	WOS:000330497500013
J	Vasícek, Z; Rabrenovic, D; Skupien, P; Radulovic, VJ; Radulovic, BV; Mojsic, I				Vasicek, Zdenek; Rabrenovic, Dragoman; Skupien, Petr; Radulovic, Vladan J.; Radulovic, Barbara V.; Mojsic, Ivana			Ammonites (Phylloceratina, Lytoceratina and Ancyloceratina) and organic-walled dinoflagellate cysts from the Late Barremian in Boljetin, eastern Serbia	CRETACEOUS RESEARCH			English	Article						Ammonites; Organic-walled dinoflagellates; Palaeoenvironment; Late Barremian; Danubic Unit; Eastern Serbia	OUTER WESTERN CARPATHIANS; LOWER CRETACEOUS AMMONITE; SILESIAN UNIT; FAUNAS; BASIN	Late Barremian ammonite fauna from the epipelagic marlstone and marly limestone interbeds of Boljetin Hill (Boljetinsko Brdo) of Danubic Unit (eastern Serbia) is described. The ammonite fauna includes representatives of three suborders (Phylloceratina, Lytoceratina and Ancyloceratina), specifically Hypophylloceras danubiense n. sp., Lepeniceras lepense Rabrenovic, Holcophylloceras avrami n. sp., Phyllopachyceras baborense (Coquand), Phyllopachyceras petkovici n. sp., Phyllopachyceras eichwaldi eichwaldi (Karakash), Phyllopachyceras ectocostatum Drushchits, Protetragonites crebrisulcatus (Uhlig), Macroscaphites perforatus Avram, Acantholytoceras cf. subcirculare (Avram), Dissimilites cf. trinodosus (d'Orbigny) and Argvethites? sp. The taxonomic composition and Percent abundance of the identified ammonites indicate that their taxa are predominantly confined to the Tethyan realm. Ammonites with smooth and slightly sculptured shells predominate among the studied fauna. The ammonite-bearing succession from Boljetin represents the lower part of the Upper Barremian, ranging in ammonite zonation from the Toxancyloceras vandenheckei Zone to the lower part of the Imerites giraudi Zone. The associated organic-walled dinoflagellate cysts confirm the Late Barremian age of the ammonite-bearing levels. (C) 2013 Elsevier Ltd. All rights reserved.	[Vasicek, Zdenek] Acad Sci Czech Republ, Inst Geon, CZ-70800 Ostrava, Czech Republic; [Rabrenovic, Dragoman; Mojsic, Ivana] Univ Belgrade, Dept Hist & Dynam Geol, Fac Min & Geol, Belgrade 11000, Serbia; [Skupien, Petr] VSB Tech Univ Ostrava, Inst Geol Engn, CZ-70833 Ostrava, Czech Republic; [Radulovic, Vladan J.; Radulovic, Barbara V.] Univ Belgrade, Dept Palaeontol, Fac Min & Geol, Belgrade 11000, Serbia	Czech Academy of Sciences; Institute of Geonics of the Czech Academy of Sciences; University of Belgrade; Technical University of Ostrava; University of Belgrade	Radulovic, VJ (通讯作者)，Univ Belgrade, Dept Palaeontol, Fac Min & Geol, Kamenicka 6, Belgrade 11000, Serbia.	vrad@eunet.rs	Vasicek, Zdenek/I-2303-2014; Skupien, Petr/G-8767-2019	Rabrenovic, Dragoman/0000-0001-8367-4411; Skupien, Petr/0000-0001-9158-466X; Radulovic, Barbara/0000-0003-3362-0217				AnCelkovic⠃ M., 1974, ZBORNIK RADOVA, V16, P57; Anderson F.M., 1938, GEOLOGY, V2, P1; Andjelkovic M., 1980, U BELGRADE MONOGRAPH, V20, P1; [Anonymous], 1869, PALAEONTOLOGY; ARKELL W.J., 1957, Treatise on invertebrate paleontology. 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J	Atwood, AR; Volkman, JK; Sachs, JP				Atwood, Alyssa R.; Volkman, John K.; Sachs, Julian P.			Characterization of unusual sterols and long chain diols, triols, keto-ols and <i>n</i>-alkenols in El Junco Lake, Galapagos	ORGANIC GEOCHEMISTRY			English	Article							MARINE DIATOMS BACILLARIOPHYTA; ALKYL DIOLS; DINOFLAGELLATE STEROLS; CARIBBEAN GORGONIANS; HISTORICAL ECOLOGY; BIOMARKER EVIDENCE; TROPICAL PACIFIC; 4-METHYL STEROLS; LIPID BIOMARKERS; CUTICULAR WAXES	A variety of lipid biomarkers were identified in sediments from El Junco Lake, Galapagos and their sources investigated for potential use in paleoclimate applications. A series of unusual sterols was also found, including 4 alpha-methylgorgostanol, reported in only four species of dinoflagellates to date. We also tentatively assigned 22,23-methylene-4 alpha-methyl-24-ethylcholest-5-en-3 beta-ol, the mass spectrum of which matched a sterol found in resting cysts of the dinoflagellate Peridinium umbonatum. In addition, we identified the novel sterol 4 alpha,22,23,24-tetramethyl-5 alpha-cholest-22E-en-3 beta-ol. Based on the unique sterol distribution, we hypothesize that a dinoflagellate from the genus Peridinium was the primary source of dinosterol and the novel sterols throughout the sediment record. The source specificity and abundance throughout the 3.7 m of recovered sediment make dinosterol an excellent target for hydrogen isotope analysis for use as a paleohydrological proxy in future studies. The abundant C-30 and C-32 1,omega 20-diols and keto-ols, C-29 9,10-diol and C-29 1,omega 9, omega 10-triol likely derive from the ferns Azolla microphylla and Cyathea weatherbyana, while sources of the C-30 1,omega 16-diol and keto-ol, C-32 1,omega 18-diol and keto-ol, and the C-30-C-32 n-alken-1-ols are likely limited to aquatic microalgae. Due to their source specificity, these diol, triol, keto-ol, and n-alkenol biomarkers present further tools for studying past environmental and climatic change. (C) 2013 Elsevier Ltd. All rights reserved.	[Atwood, Alyssa R.; Sachs, Julian P.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA; [Volkman, John K.] CSIRO Marine & Atmospher Res, Hobart, Tas 7001, Australia	University of Washington; University of Washington Seattle; Commonwealth Scientific & Industrial Research Organisation (CSIRO)	Atwood, AR (通讯作者)，Univ Washington, Sch Oceanog, Seattle, WA 98195 USA.	aatwood@uw.edu	Volkman, John/A-6592-2008		U.S. National Science Foundation [EAR-0823503, ESH-0639640]; U.S. National Oceanic and Atmospheric Administration [NA08OAR4310685]; National Science Foundation Graduate Research Fellowship Program; Department of Energy Global Change Education Program; Directorate For Geosciences; Division Of Earth Sciences [0823503] Funding Source: National Science Foundation	U.S. National Science Foundation(National Science Foundation (NSF)); U.S. National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); National Science Foundation Graduate Research Fellowship Program(National Science Foundation (NSF)); Department of Energy Global Change Education Program; Directorate For Geosciences; Division Of Earth Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This study was based upon work supported by the U.S. National Science Foundation under Grants EAR-0823503 and ESH-0639640and the U.S. National Oceanic and Atmospheric Administration under Grant No. NA08OAR4310685 to J.S. A.A. was supported by the National Science Foundation Graduate Research Fellowship Program and the Department of Energy Global Change Education Program. The authors would like to thank R. Smittenberg and K. Ricke for preparation and GC-MS analysis of vegetation samples - initial analyses of the vegetation samples can be found in Ricke (2004). We would also like to thank Z. Zhang for sample preparation and O. Kawka and J. Gregersen for support in the lab. We acknowledge P. Colinvaux for bringing El Junco Lake to our attention and the following for assistance in the field and logistical support: P. Colinvaux, J. Overpeck, M. Steinitz-Kannan, J. Conroy, R. Smittenberg, the Galapagos National Park and the Charles Darwin Research Station. Finally, we thank S. Wakeham and I. Bull for useful discussions, as well as S. Rampen and M. Amo for thoughtful reviews.	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Geochem.	JAN	2014	66						80	89		10.1016/j.orggeochem.2013.11.004	http://dx.doi.org/10.1016/j.orggeochem.2013.11.004			10	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	281VQ					2025-03-11	WOS:000329129500008
J	Hanif, M; Hart, MB; Grimes, ST; Leng, MJ				Hanif, Muhammad; Hart, Malcolm B.; Grimes, Stephen T.; Leng, Melanie J.			Integrated stratigraphy and palaeoenvironment of the P/E boundary interval, Rakhi Nala section, Indus Basin (Pakistan)	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Paleocene; Eocene; Indus Basin; Foraminifera; Dinoflagellates; Isotopes	EOCENE THERMAL MAXIMUM; BENTHIC FORAMINIFERAL EXTINCTION; PARTICULATE ORGANIC-MATTER; CARBON-ISOTOPE RATIOS; DINOFLAGELLATE CYSTS; PALEOCENE; SEDIMENTS; ESTUARY; OCEAN; PALEOPRODUCTIVITY	Marine sedimentary section across the Paleocene/Eocene (P/E) boundary interval is preserved in the Dungan Formation (Lower Indus Basin), Pakistan. Four dinoflagellate zones in the P/E interval of the Rakhi Nala section (Lower Indus Basin) are identified and correlated. The quantitative analysis of the dinoflagellate cyst assemblages together with geochemical data are used to reconstruct the palaeoenvironment across the P/E interval. The dinocyst assemblages allow the local correlation of the Dungan Formation (part) of the Sulaiman Range with the Patala Formation (part) of the Upper Indus Basin and global correlation of the Zone Pak-DV with the Apectodinium acme Zone of the Northern and Southern hemispheres. The onset of the carbon isotopic excursion (CIE) associated with Paleocene Eocene Thermal Maximum (PETM) is used globally to identify the P/E boundary. The CIE for the total organic carbon (fine fraction) delta C-13(FF) is of a magnitude of -1.7aEuro degrees is recorded for the first time in the Indus Basin. The Apectodinium acme precedes and straddles the onset of the CIE in the Indus Basin. This Apectodinium acme is also accompanied by a planktonic and benthonic foraminifera "barren zone." The CIE in the Indus Basin, coupled with the changes in the dinocyst distribution and the benthonic and planktonic foraminifera assemblages, provides evidence of the changes associated with the PETM in this little-known part of the world. The benthonic foraminiferal assemblage indicates bathyal environment of deposition at the time of P/E boundary interval; the presence of dominantly open marine dinoflagellates and high planktonic foraminiferal ratio suggest that the water column at this site was well connected with the rest of the Tethys.	[Hanif, Muhammad; Hart, Malcolm B.; Grimes, Stephen T.] Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England; [Hanif, Muhammad] Univ Peshawar, Natl Ctr Excellence Geol, Peshawar 25120, Pakistan; [Leng, Melanie J.] British Geol Survey, NERC Isotope Geosci Lab, Nottingham NG12 5GG, England	University of Plymouth; University of Peshawar; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Hanif, M (通讯作者)，Univ Peshawar, Natl Ctr Excellence Geol, Peshawar 25120, Pakistan.	hanif.nceg@gmail.com	Hart, Malcolm/KMD-8444-2024; Hanif, Muhammad/H-7320-2013	Grimes, Stephen/0000-0002-7881-1861; Leng, Melanie/0000-0003-1115-5166; Hanif, Muhammad/0000-0002-1133-5661	National Centre of Excellence in Geology University of Peshawar, Pakistan; Higher Education Commission of Pakistan; NERC [nigl010001] Funding Source: UKRI	National Centre of Excellence in Geology University of Peshawar, Pakistan; Higher Education Commission of Pakistan(Higher Education Commission of Pakistan); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	Authors gratefully acknowledge funding of this work by the National Centre of Excellence in Geology University of Peshawar, Pakistan, and Higher Education Commission of Pakistan. 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J	Furze, MFA; Scourse, JD; Pienkowski, AJ; Marret, F; Hobbs, WO; Carter, RA; Long, BT				Furze, Mark F. A.; Scourse, James D.; Pienkowski, Anna J.; Marret, Fabienne; Hobbs, William O.; Carter, Rosemary A.; Long, Brian T.			Deglacial to postglacial palaeoenvironments of the Celtic Sea: lacustrine conditions versus a continuous marine sequence	BOREAS			English	Review							LAST GLACIAL MAXIMUM; GLACIMARINE SEDIMENTARY ENVIRONMENTS; IRISH ICE-SHEET; BRITISH-ISLES; DINOFLAGELLATE CYSTS; LEVEL CHANGE; HIGH-RESOLUTION; SEASONAL STRATIFICATION; SEISMIC STRATIGRAPHY; ISOSTATIC-ADJUSTMENT	Recent work on the last glaciation of the British Isles has led to an improved understanding of the nature and timing of the retreat of the British-Irish Ice Sheet (BIIS) from its southern maximum (Isles of Scilly), northwards into the Celtic and Irish seas. However, the nature of the deglacial environments across the Celtic Sea shelf, the extent of subaerial exposure and the existence (or otherwise) of a contiguous terrestrial linkage between Britain and Ireland following ice retreat remains ambiguous. Multiproxy research, based on analysis of 12 BGS vibrocores from the Celtic Deep Basin (CDB), seeks to address these issues. CDB cores exhibit a shell-rich upward fining sequence of Holocene marine sand above an erosional contact cut in laminated muds with infrequent lonestones. Molluscs, in situ Foraminifera and marine diatoms are absent from the basal muds, but rare damaged freshwater diatoms and foraminiferal linings occur. Dinoflagellate cysts and other non-pollen palynomorphs evidence diverse, environmentally incompatible floras with temperate, boreal and Arctic glaciomarine taxa co-occurring. Such multiproxy records can be interpreted as representing a retreating ice margin, with reworking of marine sediments into a lacustrine basin. Equally, the same record may be interpreted as recording similar conditions within a semi-enclosed marine embayment dominated by meltwater export and deposition of reworked microfossils. As assemblages from these cores contrast markedly with proven glaciomarine sequences from outside the CDB, a glaciolacustrine interpretation is favoured for the laminated sequence, truncated by a Late Weichselian transgressive sequence fining upwards into fully marine conditions. Reworked rare intertidal molluscs from immediately above the regional unconformity provide a minimum date c.13.9cal. ka BP for commencement of widespread marine erosion. Although suggestive of glaciolacustrine conditions, the exact nature and timing of laminated sediment deposition within the CDB, and the implications this has on (pen)insularity of Ireland following deglaciation, remain elusive.	[Furze, Mark F. A.] MacEwan Univ, Dept Phys Sci, Earth & Planetary Sci Div, Edmonton, AB T5J 4S2, Canada; [Scourse, James D.; Pienkowski, Anna J.; Carter, Rosemary A.; Long, Brian T.] Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Hobbs, William O.] Sci Museum Minnesota, St Croix Watershed Res Stn, St Croix, MN 55047 USA	Bangor University; University of Liverpool	Furze, MFA (通讯作者)，MacEwan Univ, Dept Phys Sci, Earth & Planetary Sci Div, Edmonton, AB T5J 4S2, Canada.	furzem@macewan.ca	Pieńkowski, Anna/AAL-1312-2020; Pienkowski, Anna/J-9339-2013; Hobbs, William/P-1110-2016	Marret-Davies, Fabienne/0000-0003-4244-0437; Furze, Mark/0000-0003-4636-6182; Pienkowski, Anna/0000-0002-3606-7130; Hobbs, William/0000-0001-7321-0779	NERC [GT04/97/289/ES]; NSERC [746/0898, 814/0999]; RSACAF grant; MacEwan University; NERC [NRCF010001, NE/J007579/1] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); RSACAF grant; MacEwan University; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	Mark F. A. Furze gratefully acknowledges the receipt of a NERC PhD research studentship grant (GT04/97/289/ES) and two NSERC-funded radiocarbon allocations (746/0898; 814/0999) in support of this research. Also gratefully acknowledged is the award of an RSACAF grant and a Professional Development Conference Attendance grant from MacEwan University to Mark F. A. Furze. Staff at the NERC Radiocarbon Facility in East Kilbride, Scotland, in particular Charlotte Bryant, Brian Miller and Margaret Currie must be thanked for their valued discussions regarding radiocarbon-dating issues. Thanks must also be extended to the British Geological Survey for making core materials central to this study available, in particular Helen Glaves, Graham Tulloch and the late Robin Wingfield. Douglas Peacock, Vera Pospelova, Kenneth Mertens, John England and David Evans are also highly deserving of thanks for fruitful discussions essential to the development of this paper. Nancy McKeown at MacEwan University is thanked for her help with displaying bathymetric data. Anna J. Pienkowski wishes to thank Charlie Schweger and Harvey Friebe at the University of Alberta for the generous use of their Environmental Archaeology Laboratory in the preparation and processing of dinoflagellate cysts and other non-pollen palynomorphs. Collectively, the authors wish to thank two anonymous reviews for their constructive comments that greatly improved this manuscript, as well as Jan A. Piotrowski for his editorial handling of this paper. This is a contribution to the Climate Change Consortium of Wales (C3W).	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J	Sluijs, A; van Roij, L; Harrington, GJ; Schouten, S; Sessa, JA; Levay, LJ; Reichart, GJ; Slomp, CP				Sluijs, A.; van Roij, L.; Harrington, G. J.; Schouten, S.; Sessa, J. A.; LeVay, L. J.; Reichart, G-J; Slomp, C. P.			Warming, euxinia and sea level rise during the Paleocene-Eocene Thermal Maximum on the Gulf Coastal Plain: implications for ocean oxygenation and nutrient cycling	CLIMATE OF THE PAST			English	Article							ISOPRENOID TETRAETHER LIPIDS; EARLY WASATCHIAN MAMMALS; PHOTIC ZONE EUXINIA; NORTH-AMERICA; ORGANIC-MATTER; CARBON-DIOXIDE; SURFACE TEMPERATURE; MARINE ECOSYSTEMS; LATEST PALEOCENE; MEMBRANE-LIPIDS	The Paleocene-Eocene Thermal Maximum (PETM, similar to 56 Ma) was a similar to 200 kyr episode of global warming, associated with massive injections of C-13-depleted carbon into the ocean-atmosphere system. Although climate change during the PETM is relatively well constrained, effects on marine oxygen concentrations and nutrient cycling remain largely unclear. We identify the PETM in a sediment core from the US margin of the Gulf of Mexico. Biomarker-based paleotemperature proxies (methylation of branched tetraether-cyclization of branched tetraether (MBT-CBT) and TEX86) indicate that continental air and sea surface temperatures warmed from 27-29 to similar to 35 degrees C, although variations in the relative abundances of terrestrial and marine biomarkers may have influenced these estimates. Vegetation changes, as recorded from pollen assemblages, support this warming. The PETM is bracketed by two unconformities. It overlies Paleocene silt- and mudstones and is rich in angular (thus in situ produced; autochthonous) glauconite grains, which indicate sedimentary condensation. A drop in the relative abundance of terrestrial organic matter and changes in the dinoflagellate cyst assemblages suggest that rising sea level shifted the deposition of terrigenous material landward. This is consistent with previous findings of eustatic sea level rise during the PETM. Regionally, the attribution of the glauconite-rich unit to the PETM implicates the dating of a primate fossil, argued to represent the oldest North American specimen on record. The biomarker isorenieratene within the PETM indicates that euxinic photic zone conditions developed, likely seasonally, along the Gulf Coastal Plain. A global data compilation indicates that O-2 concentrations dropped in all ocean basins in response to warming, hydrological change, and carbon cycle feedbacks. This culminated in (seasonal) anoxia along many continental margins, analogous to modern trends. Seafloor deoxygenation and widespread (seasonal) anoxia likely caused phosphorus regeneration from suboxic and anoxic sediments. We argue that this fueled shelf eutrophication, as widely recorded from microfossil studies, increasing organic carbon burial along many continental margins as a negative feedback to carbon input and global warming. If properly quantified with future work, the PETM offers the opportunity to assess the biogeochemical effects of enhanced phosphorus regeneration, as well as the timescales on which this feedback operates in view of modern and future ocean deoxygenation.	[Sluijs, A.; van Roij, L.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Harrington, G. J.] Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England; [Schouten, S.; Reichart, G-J] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands; [Schouten, S.; Reichart, G-J; Slomp, C. P.] Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Sessa, J. A.] Amer Museum Nat Hist, Devis Paleontol, New York, NY 10024 USA; [Sessa, J. A.; LeVay, L. J.] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA; [LeVay, L. J.] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA; [LeVay, L. J.] Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77845 USA	Utrecht University; University of Birmingham; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University; American Museum of Natural History (AMNH); Pennsylvania Commonwealth System of Higher Education (PCSHE); Pennsylvania State University; Pennsylvania State University - University Park; Texas A&M University System; Texas A&M University College Station; Texas A&M University System; Texas A&M University College Station	Sluijs, A (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	a.sluijs@uu.nl	Slomp, Caroline/A-9406-2012; Schouten, Stefan/P-4380-2016; Sluijs, Appy/B-3726-2009; Reichart, Gert-Jan/N-6308-2018	Sessa, Jocelyn A./0000-0003-1509-5519; Slomp, Caroline/0000-0002-7272-0109; Sluijs, Appy/0000-0003-2382-0215; Reichart, Gert-Jan/0000-0002-7256-2243	Netherlands Organization for Scientific Research (Veni) [863.07.001]; European Research Council under the European Community [259627, 278364]; Netherlands Organization for Scientific Research (Vici)	Netherlands Organization for Scientific Research (Veni)(Netherlands Organization for Scientific Research (NWO)); European Research Council under the European Community(European Research Council (ERC)); Netherlands Organization for Scientific Research (Vici)(Netherlands Organization for Scientific Research (NWO))	Funding for this research was provided by the Netherlands Organization for Scientific Research (Veni grant 863.07.001 to A. Sluijs and a Vici grant to S. Schouten) and the European Research Council under the European Community's Seventh Framework Programme (Starting Grant no. 259627 to A. Sluijs and Consolidator Grant no. 278364 to C. P. Slomp). Paul Markwick provided his paleogeographic reconstruction. We thank E. Thomas, M. Huber, M. Schaller, A. Riboulleau, and R. Fluegeman for discussions and reviews on the Climate of the Past Discussions forum, which considerably improved this manuscript. We thank several colleagues, including G. R. Dickens for comments on an earlier version of this paper; C. Beard (Carnegie Museum of Natural History, Pittsburgh) for discussions regarding the stratigraphy at the Red Hot Truck Stop; and D. Dockery (Office of Geology at the Mississippi Department of Environmental Quality) for discussions, access to sediment cores, and assistance with sampling. We thank P. de Boer (Utrecht University) for confirming our thin section observations, and A. van Dijk, J. van Tongeren, N. Welters (Utrecht University), E. Hopmans, A. Mets, and J. Ossebaar (Royal NIOZ) for technical support.	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Past.		2014	10	4					1421	1439		10.5194/cp-10-1421-2014	http://dx.doi.org/10.5194/cp-10-1421-2014			19	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	AM5KF		Green Submitted, gold, Green Published			2025-03-11	WOS:000339896100010
J	Hessler, I; Harrison, SP; Kucera, M; Waelbroeck, C; Chen, MT; Anderson, C; de Vernal, A; Fréchette, B; Cloke-Hayes, A; Leduc, G; Londeix, L				Hessler, I.; Harrison, S. P.; Kucera, M.; Waelbroeck, C.; Chen, M. -T.; Anderson, C.; de Vernal, A.; Frechette, B.; Cloke-Hayes, A.; Leduc, G.; Londeix, L.			Implication of methodological uncertainties for mid-Holocene sea surface temperature reconstructions	CLIMATE OF THE PAST			English	Article							LAST GLACIAL MAXIMUM; SOUTH CHINA SEA; PLANKTONIC-FORAMINIFERA; NORTH-ATLANTIC; MG/CA PALEOTHERMOMETRY; INTERGLACIAL CHANGES; CLEANING PROCEDURES; MODEL ENSEMBLES; LATE QUATERNARY; OCEAN	We present and examine a multi-sensor global compilation of mid-Holocene (MH) sea surface temperatures (SST), based on Mg = Ca and alkenone palaeothermometry and reconstructions obtained using planktonic foraminifera and organic-walled dinoflagellate cyst census counts. We assess the uncertainties originating from using different methodologies and evaluate the potential of MH SST reconstructions as a benchmark for climate-model simulations. The comparison between different analytical approaches (time frame, baseline climate) shows the choice of time window for the MH has a negligible effect on the reconstructed SST pattern, but the choice of baseline climate affects both the magnitude and spatial pattern of the reconstructed SSTs. Comparison of the SST reconstructions made using different sensors shows significant discrepancies at a regional scale, with uncertainties often exceeding the reconstructed SST anomaly. Apparent patterns in SST may largely be a reflection of the use of different sensors in different regions. Overall, the uncertainties associated with the SST reconstructions are generally larger than the MH anomalies. Thus, the SST data currently available cannot serve as a target for bench-marking model simulations. Further evaluations of potential subsurface and/or seasonal artifacts that may contribute to obscure the MH SST reconstructions are urgently needed to provide reliable benchmarks for model evaluations.	[Hessler, I.; Harrison, S. P.] Macquarie Univ, Dept Biol Sci, N Ryde, NSW, Australia; [Hessler, I.; Kucera, M.] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Harrison, S. P.] Univ Reading, Ctr Climate Change, Reading, Berks, England; [Harrison, S. P.] Univ Reading, SAGES, Reading, Berks, England; [Waelbroeck, C.] Lab CNRS CEA UVSQ, Lab Sci Climat & Environm LSCE IPSL, Gif Sur Yvette, France; [Chen, M. -T.] Natl Taiwan Ocean Univ, Inst Appl Geosci, Keelung, Taiwan; [Anderson, C.] Uni Res, Uni Climate, Bergen, Norway; [Anderson, C.] Bjerknes Ctr Climate Res, Bergen, Norway; [de Vernal, A.; Frechette, B.] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Cloke-Hayes, A.] Univ Limerick, Mary Immaculate Coll, Limerick, Ireland; [Leduc, G.] Univ Kiel, Kiel, Germany; [Leduc, G.] CEREGE, UMR7330, Aix En Provence, France; [Londeix, L.] Univ Bordeaux, UMR EPOC CNRS, Talence, France	Macquarie University; University of Bremen; University of Reading; University of Reading; Universite Paris Saclay; CEA; National Taiwan Ocean University; Bjerknes Centre for Climate Research; University of Quebec; University of Quebec Montreal; University of Limerick; Mary Immaculate College - University Limerick; University of Kiel; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux	Hessler, I (通讯作者)，Macquarie Univ, Dept Biol Sci, N Ryde, NSW, Australia.	ines.hessler@mq.edu.au	Chen, Min-Te/ABF-2935-2020; Harrison, Sandy/ADX-4692-2022; Leduc, Guillaume/A-8930-2008; de Vernal, Anne/D-5602-2013; Chen, Min-Te/AAD-5990-2021; Kucera, Michal/B-9277-2009	Harrison, Sandy/0000-0001-5687-1903; waelbroeck, claire/0000-0002-7256-5727; Hessler, Ines/0000-0002-7471-8854; Chen, Min-Te/0000-0002-7552-1615; Frechette, Bianca/0000-0002-4986-5772; Kucera, Michal/0000-0002-7817-9018; Andersson Dahl, Carin/0000-0002-7113-6066	Australian Research Council [DP1201100343]; PAGES; Division Of Earth Sciences; Directorate For Geosciences [1440015] Funding Source: National Science Foundation	Australian Research Council(Australian Research Council); PAGES; Division Of Earth Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This research was supported by the Australian Research Council, grant no. DP1201100343. We thank Daniel Ariztegui, Lucilla Capotondi, Basil Davis, Valentino Di Donato, Maria Geraga, Zhimin Jian, Yoshimi Kubota, Baohua Li, Gema Martinez Mendez, Tarek Melki, Andrea Piva, Imene Rouis, Liang-Jian Shiau, Yurika Ujiie, and Rong Xiang for contributing data to this compilation. We also would like to thank Richard Telford and an anonymous referee for reviewing our manuscript and Brad Rosenheim for his short comment, with all comments contributing to the improvement of the manuscript. This paper was initiated during the COMPARE (Comparing Ocean Models with paleo-Archives) workshop held in Bremen, Germany 2012, which was supported by Past Global Changes (PAGES). Therefore, special thanks goes to PAGES for their support and providing the means to establish the network necessary to conduct this study.	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Past.		2014	10	6					2237	2252		10.5194/cp-10-2237-2014	http://dx.doi.org/10.5194/cp-10-2237-2014			16	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	AY4SY		Green Submitted, Green Accepted, gold			2025-03-11	WOS:000347569500016
J	Pandeirada, MS; Craveiro, SC; Daugbjerg, N; Moestrup, O; Calado, AJ				Pandeirada, Mariana S.; Craveiro, Sandra C.; Daugbjerg, Niels; Moestrup, Ojvind; Calado, Antonio J.			Studies on woloszynskioid dinoflagellates VI: description of <i>Tovellia aveirensis</i> sp nov (Dinophyceae), a new species of Tovelliaceae with spiny cysts	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						cyst; dinoflagellates; LSU rDNA; phylogeny; taxonomy; Tovelliaceae; Tovellia aveirensis; ultrastructure	LAKE TOVEL; ELECTRON-MICROSCOPY; RDNA SEQUENCES; GEN. NOV.; LSU; ULTRASTRUCTURE; PHYLOGENY; EVOLUTION; GENERA; LIGHT	A new species of Tovellia, T. aveirensis, is described on the basis of light (LM) and scanning electron microscopy (SEM) of motile cells and resting cysts, complemented with transmission electron microscopy (TEM) of flagellate cells and phylogenetic analysis of partial sequences of the large subunit ribosomal rRNA gene. Both vegetative cells and several stages of a life cycle involving sexual reproduction and the production of resting cysts were examined in cultures established from a tank in the University of Aveiro campus. Vegetative cells were round and little compressed dorsoventrally; planozygotes were longer and had a proportionally larger epicone. Chloroplast lobes were shown by TEM to radiate from a central, branched pyrenoid, although this was difficult to ascertain in LM. The amphiesma of flagellate cells had mainly 5 or 6-sided vesicles with thin plates, arranged in 5-7 latitudinal series on the epicone, 3-5 on the hypocone. The cingulum had 2 rows of plates, the posterior row extending into the hypocone and crossed by a series of small projecting knobs along the lower edge of the cingulum. A line of narrow amphiesmal plates extended over the cell apex, from near the cingulum on the ventral side to the middle of the dorsal side of the epicone. Eight or 9 narrow amphiesmal plates lined each side of this apical line of plates (ALP). Resting cysts differed from any described before in having numerous long, tapering spines with branched tips distributed over most of the surface. Most mature cysts showed an equatorial constriction. Neither cysts nor motile cells were seen to accumulate red cytoplasmic bodies in any stage of the cultures. The phylogenetic analysis placed, with high statistical support, the new species within the genus Tovellia; it formed a clade, with moderate support, with T. sanguinea, a species notable for its reddening cells.	[Pandeirada, Mariana S.; Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; [Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, GeoBioTec Res Unit, P-3810193 Aveiro, Portugal; [Daugbjerg, Niels; Moestrup, Ojvind] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-2100 Copenhagen O, Denmark	Universidade de Aveiro; Universidade de Aveiro; University of Copenhagen	Calado, AJ (通讯作者)，Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal.	acalado@ua.pt	Pandeirada, Mariana/AAF-7448-2019; Calado, Antonio Jose/D-6263-2015; Pandeirada, Mariana Sofia/E-8803-2015; Calado, Sandra Carla/A-6791-2016; Daugbjerg, Niels/D-3521-2014	Calado, Antonio Jose/0000-0002-9711-0593; Pandeirada, Mariana Sofia/0000-0001-5061-9029; Calado, Sandra Carla/0000-0002-2738-7626; Daugbjerg, Niels/0000-0002-0397-3073	QREN-POPH - Tipologia 4.1 - Formacao Avancada; European Social Funding (FSE); Portuguese Ministry of Education and Science (MEC); GeoBioTec [PEst-OE/CTE/UI4035/2014];  [SFRH/BPD/68537/2010]; Fundação para a Ciência e a Tecnologia [SFRH/BPD/68537/2010] Funding Source: FCT	QREN-POPH - Tipologia 4.1 - Formacao Avancada; European Social Funding (FSE)(European Social Fund (ESF)); Portuguese Ministry of Education and Science (MEC); GeoBioTec; ; Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	We thank Newton Gomes and the staff at the Laboratory of Molecular Studies for Marine Environments (LEMAM), Univ. Aveiro, Portugal, for access to their facilities; Marina Cunha and Ascensao Ravara for help and advice during the molecular work; Jose Alberto Duarte, Univ. Oporto, for access and assistance with the TEM. Sandra C. Craveiro was supported by grant SFRH/BPD/68537/2010 financed by the programme 'QREN-POPH - Tipologia 4.1 - Formacao Avancada' and by the European Social Funding (FSE) and the Portuguese Ministry of Education and Science (MEC). GeoBioTec was funded by PEst-OE/CTE/UI4035/2014.	Calado AJ, 2006, J PHYCOL, V42, P434, DOI 10.1111/j.1529-8817.2006.00195.x; Calado AJ, 2011, PHYCOLOGIA, V50, P641, DOI 10.2216/11-21.1; CHRISTEN H. 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J. Phycol.		2014	49	2					230	243		10.1080/09670262.2014.910610	http://dx.doi.org/10.1080/09670262.2014.910610			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	AJ2ZH		Bronze			2025-03-11	WOS:000337533700003
J	Burson, A; Matthijs, HCP; de Bruijne, W; Talens, R; Hoogenboom, R; Gerssen, A; Visser, PM; Stomp, M; Steur, K; van Scheppingen, Y; Huisman, J				Burson, Amanda; Matthijs, Hans C. P.; de Bruijne, Wilco; Talens, Renee; Hoogenboom, Ron; Gerssen, Arjen; Visser, Petra M.; Stomp, Maayke; Steur, Kees; van Scheppingen, Yvonne; Huisman, Jef			Termination of a toxic <i>Alexandrium</i> bloom with hydrogen peroxide	HARMFUL ALGAE			English	Article						Alexandrium ostenfeldii; Coastal management; Harmful algal blooms; Hydrogen peroxide; Saxitoxin; Spirolides	HARMFUL ALGAL BLOOMS; OSTENFELDII DINOPHYCEAE; WATER TEMPERATURE; OXIDATIVE STRESS; EUTROPHICATION; CYANOBACTERIA; PHYTOPLANKTON; COASTAL; GROWTH; LIGHT	The dinoflagellate Alexandrium ostenfeldii is a well-known harmful algal species that can potentially cause paralytic shellfish poisoning (PSP). Usually A. ostenfeldii occurs in low background concentrations only, but in August of 2012 an exceptionally dense bloom of more than 1 million cells L-1 occurred in the brackish Ouwerkerkse Kreek in The Netherlands. The A. ostenfeldii bloom produced both saxitoxins and spirolides, and is held responsible for the death of a dog with a high saxitoxin stomach content. The Ouwerkerkse Kreek routinely discharges its water into the adjacent Oosterschelde estuary, and an immediate reduction of the bloom was required to avoid contamination of extensive shellfish grounds. Previously, treatment of infected waters with hydrogen peroxide (H2O2) successfully suppressed cyanobacterial blooms in lakes. Therefore, we adapted this treatment to eradicate the Alexandrium bloom using a three-step approach. First, we investigated the required H2O2 dosage in laboratory experiments with A. ostenfeldii. Second, we tested the method in a small, isolated canal adjacent to the Ouwerkerkse Kreek. Finally, we brought 50 mg L-1 of H2O2 into the entire creek system with a special device, called a water harrow, for optimal dispersal of the added H2O2. Concentrations of both vegetative cells and pellicle cysts declined by 99.8% within 48 h, and PSP toxin concentrations in the water were reduced below local regulatory levels of 15 mu g L-1. Zooplankton were strongly affected by the H2O2 treatment, but impacts on macroinvertebrates and fish were minimal. A key advantage of this method is that the added H2O2 decays to water and oxygen within a few days, which enables rapid recovery of the system after the treatment. This is the first successful field application of H2O2 to suppress a marine harmful algal bloom, although Alexandrium spp. reoccurred at lower concentrations in the following year. The results show that H2O2 treatment provides an effective emergency management option to mitigate toxic Alexandrium blooms, especially when immediate action is required. (C) 2013 Elsevier B.V. All rights reserved.	[Burson, Amanda; Matthijs, Hans C. P.; Visser, Petra M.; Stomp, Maayke; Huisman, Jef] Univ Amsterdam, Dept Aquat Microbiol, Inst Biodivers & Ecosyst Dynam, NL-1090 GE Amsterdam, Netherlands; [de Bruijne, Wilco; Talens, Renee] Arcadis Netherlands BV, NL-7321 CT Apeldoorn, Netherlands; [Hoogenboom, Ron; Gerssen, Arjen] RIKILT Wageningen UR, NL-6708 WB Wageningen, Netherlands; [Steur, Kees; van Scheppingen, Yvonne] Waterschap Scheldestromen, NL-4330 ZW Middelburg, Netherlands	University of Amsterdam; Arcadis; Wageningen University & Research	Huisman, J (通讯作者)，Univ Amsterdam, Dept Aquat Microbiol, Inst Biodivers & Ecosyst Dynam, POB 94248, NL-1090 GE Amsterdam, Netherlands.	j.huisman@uva.nl	Stomp, Maayke/J-1484-2012; Hoogenboom, Ron/AAB-3062-2021; Huisman, Jef/A-1089-2013	Burson, Amanda/0000-0003-0729-3793; Gerssen, Arjen/0000-0003-4271-1516; Huisman, Jef/0000-0001-9598-3211; Visser, Petra/0000-0003-3294-1908; Hoogenboom, Ron/0000-0002-8913-5328	Waterschap Scheldestromen; ZKO-program North Sea; Netherlands Organisation of Scientific Research (NWO)	Waterschap Scheldestromen; ZKO-program North Sea; Netherlands Organisation of Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO))	We are most grateful to all staff of Waterschap Scheldestromen for their great help during the project. We thank Jaap van Steenwijk and Bert van Munster for their advice facilitating this innovative approach, the support staff of ARCADIS for their technical innovations and hard work during the execution of the H<INF>2</INF>O<INF>2</INF> treatment, the expertise center Koeman and Bijkerk B.V. for plankton analyses, Pieter Slot and Bas van Beusekom of the University of Amsterdam for their assistance in the field and laboratory, and the anonymous reviewer for his/her helpful comments on the manuscript. 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J	Heikkilä, M; Pospelova, V; Hochheim, KP; Kuzyk, ZZA; Stern, GA; Barber, DG; Macdonald, RW				Heikkila, Maija; Pospelova, Vera; Hochheim, Klaus P.; Kuzyk, Zou Zou A.; Stern, Gary A.; Barber, David G.; Macdonald, Robie W.			Surface sediment dinoflagellate cysts from the Hudson Bay system and their relation to freshwater and nutrient cycling	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Hudson Bay; Sediment; Sea-ice; Biogenic silica; Nitrogen; Lignin	ORGANIC-WALLED MICROFOSSILS; PROCESS LENGTH VARIATION; NORTHERN NORTH-ATLANTIC; SEA-ICE; ARCTIC-OCEAN; MARINE-SEDIMENTS; CLIMATE-CHANGE; PROTOCERATIUM-RETICULATUM; PHYTOPLANKTON GROWTH; SCRIPPSIELLA-HANGOEI	Surface sediment samples from the Hudson Bay system were analysed in order to examine the role of key regulators of arctic marine productivity light and nutrients as affected by freshwater stratification and sea-ice cover on the spatial distribution and production of dinoflagellate cysts. Total cyst fluxes vary from 0.2 x 10(6) to 30.6 x 106 cysts m(-2) a(-1), with the highest values observed in eastern Hudson Bay. A total of 24 cyst taxa, representing 11 genera of five orders, were identified and distribution maps of the most common taxa have been produced. This is the first record of Echinidinium aculeatum, Echinidinium karaense, cf. Echinidinium delicatum, Islandinium brevispinosum, Selenopemphix quanta, cysts of Protoperidinium americanum, cysts of cf. Biecheleria sp. and Polarella glacialis in the Hudson Bay system. Dinoflagellate cyst assemblages show distinct spatial patterns revealing three compositional domains: eastern Hudson Bay, western-central Hudson Bay and Hudson Strait. The eastern domain is characterised by a dominance of autotrophic cysts of Pentapharsodinium dalei whereas the western-central domain is characterised by autotrophic Operculodinium centrocarpum with some contribution by heterotrophic Polykrikos sp. var. arctic morphotype and Polykrikos spp. Sites from Hudson Strait are distinguished by an overwhelming prevalence of heterotrophic Protoperidiniaceae cysts, mainly Islandinium minutum, and have the highest values of sedimentary biogenic silica, used as a proxy for diatom productivity. Sediment geochemical tracers are used as proxies for freshwater inputs (lignin and its biomarkers) and nitrate availability (nitrogen isotopes), and sea-ice concentrations derived from passive microwave data as a proxy for light availability. Sea-ice regulated length of the dark season has a negligible influence on the proportion and production of heterotrophic (dark-adapted) versus autotrophic (light-dependent) dinoflagellate cysts, perhaps due to the location of our study area on the southern fringe of the Arctic. Instead, cyst populations in Hudson Bay are primarily regulated by vertical stratification and nitrate availability, while in Hudson Strait the pivotal mechanism constitutes food availability. (C) 2013 Elsevier B.V. All rights reserved.	[Heikkila, Maija; Hochheim, Klaus P.; Kuzyk, Zou Zou A.; Stern, Gary A.; Barber, David G.; Macdonald, Robie W.] Univ Manitoba, Ctr Earth Observat Sci, Winnipeg, MB R3T 2N2, Canada; [Heikkila, Maija; Stern, Gary A.] Fisheries & Oceans Canada, Inst Freshwater, Dept Fisheries & Oceans, Winnipeg, MB R3T 2N6, Canada; [Heikkila, Maija] Univ Helsinki, Dept Environm Sci, ECRU, FI-00014 Helsinki, Finland; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada; [Macdonald, Robie W.] Inst Ocean Sci, Dept Fisheries & Oceans, Sidney, BC V8L 4B2, Canada	University of Manitoba; Fisheries & Oceans Canada; University of Helsinki; University of Victoria; Fisheries & Oceans Canada	Heikkilä, M (通讯作者)，Univ Helsinki, Dept Environm Sci, ECRU, Viikinkaari 1,POB 65, FI-00014 Helsinki, Finland.	maija.heikkila@helsinki.fi	Macdonald, Robie/A-7896-2012; Heikkila, Maija/N-7659-2013	Stern, Gary/0000-0003-2160-0841; Macdonald, Robie/0000-0002-1141-8520; Barber, David/0000-0001-9466-3291; Heikkila, Maija/0000-0003-3885-8670; Pospelova, Vera/0000-0003-4049-8133	ArcticNet, a Canadian Network of Centres of Excellence, Fisheries and Oceans Canada; Academy of Finland [252512]; Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation (CFI); Canada Research Chairs (CRC); Canada Excellence Research Chairs (CERC); University of Manitoba; Academy of Finland (AKA) [252512] Funding Source: Academy of Finland (AKA)	ArcticNet, a Canadian Network of Centres of Excellence, Fisheries and Oceans Canada; Academy of Finland(Research Council of Finland); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Canada Foundation for Innovation (CFI)(Canada Foundation for Innovation); Canada Research Chairs (CRC)(Canada Research Chairs); Canada Excellence Research Chairs (CERC); University of Manitoba; Academy of Finland (AKA)(Research Council of Finland)	This paper is dedicated to our friend and colleague, Dr. Klaus Hochheim, who tragically lost his life while doing sea ice research in the Canadian Arctic, September of 2013. We are grateful to the officers and crew of CCGS Amundsen for the support during the cruise, M. O'Brien for the assistance with coring, and Z. Sandwith and A. Price for the help with sample preparation. Funding and support were received from ArcticNet, a Canadian Network of Centres of Excellence, Fisheries and Oceans Canada (G.S. & R.M.), the Academy of Finland (grant 252512 to M.H.), Natural Sciences and Engineering Research Council of Canada (V.P.), Canada Foundation for Innovation (CFI), Canada Research Chairs (CRC), Canada Excellence Research Chairs (CERC) Program and University of Manitoba (G.S.). Journal editors Richard Jordan and Frans Jorissen, as well as Jens MatthieBen and an anonymous reviewer offered comments that significantly improved the manuscript.	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Micropaleontol.	JAN	2014	106						79	109		10.1016/j.marmicro.2013.12.002	http://dx.doi.org/10.1016/j.marmicro.2013.12.002			31	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	AC4MU					2025-03-11	WOS:000332496200007
J	Watts, PC; Lundholm, N; Ribeiro, S; Ellegaard, M				Watts, Phillip C.; Lundholm, Nina; Ribeiro, Sofia; Ellegaard, Marianne			A century-long genetic record reveals that protist effective population sizes are comparable to those of macroscopic species	BIOLOGY LETTERS			English	Article						dinoflagellate; drift; effective population size; palaeogenetics	PATTERNS; EVOLUTION	Effective population size (N-e) determines the rate of genetic drift and the relative influence of selection over random genetic changes. While free-living protist populations characteristically consist of huge numbers of cells (N), the absence of any estimates of contemporary N-e raises the question whether protist effective population sizes are comparably large. Using microsatellite genotype data of strains derived from revived cysts of the marine dinoflagellate Pentapharsodinium dalei from sections of a sediment record that spanned some 100 years, we present the first estimates of contemporary N-e for a local population in a free-living protist. The estimates of N-e are relatively small, of the order of a few 100 individuals, and thus are similar in magnitude to values of N-e reported for multicellular animals: the implications are that N-e of P. dalei is of many orders of magnitude lower than the number of cells present (N-e/N similar to 10(-12)) and that stochastic genetic processes may be more prevalent in protist populations than previously anticipated.	[Watts, Phillip C.] Univ Liverpool, Inst Integrat Biol, Liverpool L69 7ZB, Merseyside, England; [Watts, Phillip C.] Univ Jyvaskyla, Dept Biol & Environm Sci, FIN-40014 Jyvaskyla, Finland; [Lundholm, Nina] Nat Hist Museum Denmark, DK-1307 Copenhagen, Denmark; [Ribeiro, Sofia] Geol Survey Denmark & Greenland, Dept Marine Geol & Glaciol, DK-1350 Copenhagen, Denmark; [Ellegaard, Marianne] Univ Copenhagen, Dept Biol, DK-1353 Copenhagen, Denmark	University of Liverpool; University of Jyvaskyla; Geological Survey Of Denmark & Greenland; University of Copenhagen	Watts, PC (通讯作者)，Univ Liverpool, Inst Integrat Biol, Biosci Bldg, Liverpool L69 7ZB, Merseyside, England.	phill@liv.ac.uk	Watts, Phill/G-7257-2011; Ribeiro, Sofia/AAZ-2782-2021; Lundholm, Nina/AAY-6249-2020; Lundholm, Nina/A-4856-2013; Ribeiro, Sofia/G-9213-2018; Ellegaard, Marianne/H-6748-2014	Lundholm, Nina/0000-0002-2035-1997; Ribeiro, Sofia/0000-0003-0672-9161; Watts, Phillip/0000-0001-7755-187X; Ellegaard, Marianne/0000-0002-6032-3376	PRODIVERSA, a NordForsk; Danish Research Council [2111-04-0011]; Carlsberg Foundation [2011_01_0337]	PRODIVERSA, a NordForsk; Danish Research Council(Det Frie Forskningsrad (DFF)); Carlsberg Foundation(Carlsberg Foundation)	The authors are part of PRODIVERSA, a NordForsk-funded network on protist population genetics. Laboratory work was financially supported by the Danish Research Council (2111-04-0011) and fieldwork by Goteborg University Marine Research Centre. S. R. holds a postdoctoral fellowship from the Carlsberg Foundation (2011_01_0337).	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Lett.	DEC 23	2013	9	6							20130849	10.1098/rsbl.2013.0849	http://dx.doi.org/10.1098/rsbl.2013.0849			4	Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Environmental Sciences & Ecology; Evolutionary Biology	297YG	24284562	Bronze, Green Published			2025-03-11	WOS:000330290400045
J	Harland, R; Asteman, IP; Nordberg, K				Harland, Rex; Asteman, Irina Polovodova; Nordberg, Kjell			A two-millennium dinoflagellate cyst record from Gullmar Fjord, a Swedish Skagerrak sill fjord	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Holocene; Subatlantic; Dinoflagellate cysts; Palaeoclimates; Skagerrak; Sweden	NORTH-ATLANTIC OSCILLATION; SURFACE OCEAN CONDITIONS; LATE-HOLOCENE; WEST-COAST; TEMPERATURE VARIABILITY; GYMNODINIUM CATENATUM; RECENT SEDIMENTS; WARM PERIOD; SEA; RECONSTRUCTION	Gullmar Fjord, a sill fjord on the Skagerrak coast of western Sweden, contains a valuable sedimentary archive for the last 2500 years. This archive encompasses a temporal record from the Roman Warm Period, the Dark Ages, the Medieval Warm Period, the Little Ice Age and into the modern warm period. A high resolution dinoflagellate cyst analysis has been completed on this archive using material from two cores taken from the deepest part of the fjord, Alsback Deep. The recovered dinoflagellate cysts have provided a quantitative temporal record that has been used to construct a dinoflagellate cyst spectrum and has been subjected to both Q-mode cluster analysis and CABFAC factor analysis with varimax rotation. In addition the heterotrophic ratio and both the thermophilic and cryophilic ratios have been calculated to assist with the interpretation of the results. Well preserved and diverse dinoflagellate cyst assemblages have been recovered throughout the sedimentary sequence and have been used to explore surface water conditions within the fjord over this time interval. Although a clear link is observed between the cyst assemblages and the climate phases of the Subatlantic, established from previous stable isotope work, there was little change in the cyst populations and indeed they reflect the known modem cyst floras. However a major change was seen in the incoming of Gymnodinium nolleri during the Dark Age and its reduction to a relict species towards the end of the Little Ice Age. Comparisons to other published work confirm the regional nature of this dinoflagellate cyst event but its ecological preferences remain enigmatic. A second major change was also recognised around the late 1960s/early 1970s and was associated with differences in nutrient availability from either a diminution in upwelling, as the NAO changed from a negative phase to a positive, or from marine pollution or a combination of both. Otherwise the dinoflagellate cyst assemblages can be grouped, using the factor analysis, into F1 Protoperidinium spp. indet (round, brown cysts); F2 G. nolleri and F3 Lingulodinium polyedrum and Protoceratium reticulatum. The cluster analysis shows a similar subdivision into units closely associated with the recognised climate phases of the Subatlantic. Possible climate environments have been explored, but because of the relatively minor variations in the assemblages and the lack of autecological information, only relatively small scale changes were recognised except for the clear, but complex nature of the recent warm period. (C) 2013 Elsevier B.V. All rights reserved.	[Harland, Rex; Asteman, Irina Polovodova; Nordberg, Kjell] Univ Gothenburg, Dept Earth Sci, SE-40530 Gothenburg, Sweden	University of Gothenburg	Harland, R (通讯作者)，50 Long Acre, Nottingham NG13 8AH, England.	rex.harland@ntlworld.com		Nordberg, Kjell/0000-0003-0085-4607; Polovodova Asteman, Irina/0000-0001-7300-5548	Lamm Foundation; Swedish Research Council (VR) [621-2007-4369, G-AA/GU 09874-307, G-AA/GU 09874-309]; Futura Foundation; Carl Trygger Foundation; Wahlsrom Foundation; Goteborg University Research Centre	Lamm Foundation; Swedish Research Council (VR)(Swedish Research Council); Futura Foundation; Carl Trygger Foundation; Wahlsrom Foundation; Goteborg University Research Centre	The authors thank the crews of the RV Slanic, RV Arne Tiselius and RV Skagerak for their help in collecting the cores. Samples from GA113-2Ab were processed in the laboratories of the Palynology Research Facility, University of Sheffield and Mr Steve Ellin and Ahwad B. Ibrahim are thanked for their technical expertise. Samples from Core 9004 were processed by Mr David Bodman at MB Stratigraphy, Sheffield and we also thank him for his care and expertise. We would also like to thank Ardo Robijn (University of Gothenburg), who ran the samples from core G113-119A for C<INF>org</INF> and C/N ratio. The research has been supported through a postdoctoral fellowship to IPA, the Lamm Foundation and the Swedish Research Council (VR) (grants 621-2007-4369, G-AA/GU 09874-307 and G-AA/GU 09874-309 to KN together with grants from the Futura Foundation, the Carl Trygger Foundation, the Wahlsrom Foundation and Goteborg University Research Centre (GMF). We are pleased to acknowledge the helpful comments and constructive criticisms from two anonymous reviewers.	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Paleoclimatol. Paleoecol.	DEC 15	2013	392						247	260		10.1016/j.palaeo.2013.09.006	http://dx.doi.org/10.1016/j.palaeo.2013.09.006			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	300UB					2025-03-11	WOS:000330488400017
J	Hellyer, SD; Selwood, AI; Rhodes, L; Kerr, DS				Hellyer, Shane D.; Selwood, Andrew I.; Rhodes, Lesley; Kerr, D. Steven			Neuromuscular blocking activity of pinnatoxins E, F and G	TOXICON			English	Article						Pinnatoxin; Neuromuscular block; Harmful algal toxins; Electrophysiology	BIVALVE PINNA-MURICATA; ACETYLCHOLINE-RECEPTORS; HIGH-AFFINITY; DINOFLAGELLATE; DIAPHRAGM; DINOPHYCEAE; SPIROLIDE; TOXICITY; RAT	Pinnatoxins are produced by dinoflagellates and belong to the cyclic imine family of toxins. They are fast-acting and highly toxic when administered in vivo in rodent bioassays, causing death by respiratory depression within minutes. Studies have revealed that some cyclic imine toxins cause their toxicity by antagonizing both muscle type and heteromeric and homomeric neuronal nicotinic acetylcholine receptors (nAChRs). Pinnatoxins E, F and G all display potent toxicity in in vivo bioassays, with symptoms of toxicity similar to other cyclic imine toxins. However, very little work has been done on the mechanism of action of these pinnatoxin isomers. Thus the aim of the current study was to investigate the rank order of potency and mechanism of action of pinnatoxins E, F and G. The effects of pinnatoxin E, F and G on in vitro rat hemidiaphragm preparations were investigated using twitch tension and electrophysiological techniques to determine the effects of these toxins on cholinergic transmission at the neuromuscular junction. Pinnatoxins E, F and G all produced concentration-dependent reductions in the nerve evoked twitch response of the rat hemidiaphragm, with IC50 values ranging from 11 to 53 nM and a rank order of potency of F > G > E. Only complete washout of pinnatoxin E was evident, with pinnatoxins F and G displaying slow and incomplete washout profiles. Pinnatoxins F and G also reduced the amplitudes of spontaneous miniature endplate potentials and evoked endplate potentials at the neuromuscular junction, without affecting miniature endplate potential frequency or the resting membrane potential of the muscle fibres. These results show that pinnatoxins E, F and G are all potent neuromuscular blocking agents and cause toxicity by acting as antagonists at muscle type nicotinic acetylcholine receptors. (C) 2013 Elsevier Ltd. All rights reserved.	[Hellyer, Shane D.; Kerr, D. Steven] Univ Otago, Sch Med Sci, Dept Pharmacol & Toxicol, Dunedin, New Zealand; [Selwood, Andrew I.; Rhodes, Lesley] Cawthron Inst, Nelson, New Zealand	University of Otago; Cawthron Institute	Kerr, DS (通讯作者)，Univ Otago, Sch Med Sci, Dept Pharmacol & Toxicol, Dunedin, New Zealand.	Shane.hellyer@studentotago.ac.nz; Andy.Selwood@cawthron.org.nz; Lesley.Rhodes@cawthron.org.nz; steve.kerr@otago.ac.nz	Hellyer, Shane/JNS-1761-2023; Selwood, Andrew/AAP-7550-2020	Selwood, Andrew/0000-0003-1399-8028; Hellyer, Shane Dennis/0000-0003-0688-6060				Araoz R, 2011, J AM CHEM SOC, V133, P10499, DOI 10.1021/ja201254c; BARSTAD JAB, 1962, EXPERIENTIA, V18, P579, DOI 10.1007/BF02172193; Bourne Y, 2010, P NATL ACAD SCI USA, V107, P6076, DOI 10.1073/pnas.0912372107; CHANG CC, 1975, J PHYSIOL-LONDON, V250, P161, DOI 10.1113/jphysiol.1975.sp011047; Chou T, 1996, TETRAHEDRON LETT, V37, P4023, DOI 10.1016/0040-4039(96)00752-6; Espiña B, 2011, TOXICOLOGY, V287, P69, DOI 10.1016/j.tox.2011.06.003; GIBB AJ, 1986, BRIT J PHARMACOL, V89, P619, DOI 10.1111/j.1476-5381.1986.tb11164.x; Hauser TA, 2012, NEUROPHARMACOLOGY, V62, P2239, DOI 10.1016/j.neuropharm.2012.01.009; Hellyer SD, 2011, TOXICON, V58, P693, DOI 10.1016/j.toxicon.2011.09.006; Hess P, 2013, TOXICON, V75, P16, DOI 10.1016/j.toxicon.2013.05.001; Kharrat R, 2008, J NEUROCHEM, V107, P952, DOI 10.1111/j.1471-4159.2008.05677.x; Knight D, 2003, J PHYSIOL-LONDON, V546, P789, DOI 10.1113/jphysiol.2002.030924; Molgo J., 2007, Phycotoxins: chemistry and biochemistry, P319; Munday R, 2012, TOXICON, V60, P995, DOI 10.1016/j.toxicon.2012.07.002; Munday Rex, 2008, P581; Nézan E, 2011, CRYPTOGAMIE ALGOL, V32, P3, DOI 10.7872/crya.v32.iss1.2011.003; 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; Satta CT, 2013, HARMFUL ALGAE, V24, P65, DOI 10.1016/j.hal.2013.01.007; Selwood AI, 2010, J AGR FOOD CHEM, V58, P6532, DOI 10.1021/jf100267a; Smith KF, 2011, HARMFUL ALGAE, V10, P702, DOI 10.1016/j.hal.2011.05.006; Takada N, 2001, TETRAHEDRON LETT, V42, P3491, DOI 10.1016/S0040-4039(01)00480-4; TSAI MC, 1987, ARCH INT PHARMACOD T, V285, P316; UEMURA D, 1995, J AM CHEM SOC, V117, P1155, DOI 10.1021/ja00108a043; VANDERKLOOT W, 1994, PHYSIOL REV, V74, P899, DOI 10.1152/physrev.1994.74.4.899; Wandscheer CB, 2010, CHEM RES TOXICOL, V23, P1753, DOI 10.1021/tx100210a; Zeng N, 2012, NEW ZEAL J MAR FRESH, V46, P511, DOI 10.1080/00288330.2012.719911; Zheng S.Z., 1990, Chin. J. Mar. Drugs, V33, P33	28	16	16	3	15	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0041-0101			TOXICON	Toxicon	DEC 15	2013	76						214	220		10.1016/j.toxicon.2013.10.009	http://dx.doi.org/10.1016/j.toxicon.2013.10.009			7	Pharmacology & Pharmacy; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy; Toxicology	275EH	24139849				2025-03-11	WOS:000328658600026
J	De Schepper, S; Groeneveld, J; Naafs, BDA; Van Renterghem, C; Hennissen, J; Head, MJ; Louwye, S; Fabian, K				De Schepper, Stijn; Groeneveld, Jeroen; Naafs, B. David A.; Van Renterghem, Cederic; Hennissen, Jan; Head, Martin J.; Louwye, Stephen; Fabian, Karl			Northern Hemisphere Glaciation during the Globally Warm Early Late Pliocene	PLOS ONE			English	Article							SEA-LEVEL; OVERTURNING CIRCULATION; DINOFLAGELLATE CYSTS; ATLANTIC-OCEAN; PLEISTOCENE; RECONSTRUCTION; PRODUCTIVITY; STRATIGRAPHY; CALIBRATION; DELTA-O-18	The early Late Pliocene (3.6 to similar to 3.0 million years ago) is the last extended interval in Earth's history when atmospheric CO2 concentrations were comparable to today's and global climate was warmer. Yet a severe global glaciation during marine isotope stage (MIS) M2 interrupted this phase of global warmth similar to 3.30 million years ago, and is seen as a premature attempt of the climate system to establish an ice-age world. Here we propose a conceptual model for the glaciation and deglaciation of MIS M2 based on geochemical and palynological records from five marine sediment cores along a Caribbean to eastern North Atlantic transect. Our records show that increased Pacific-to-Atlantic flow via the Central American Seaway weakened the North Atlantic Current and attendant northward heat transport prior to MIS M2. The consequent cooling of the northern high latitude oceans permitted expansion of the continental ice sheets during MIS M2, despite near-modern atmospheric CO2 concentrations. Sea level drop during this glaciation halted the inflow of Pacific water to the Atlantic via the Central American Seaway, allowing the build-up of a Caribbean Warm Pool. Once this warm pool was large enough, the Gulf Stream-North Atlantic Current system was reinvigorated, leading to significant northward heat transport that terminated the glaciation. Before and after MIS M2, heat transport via the North Atlantic Current was crucial in maintaining warm climates comparable to those predicted for the end of this century.	[De Schepper, Stijn] Univ Bergen, Dept Earth Sci, Bergen, Norway; [De Schepper, Stijn] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Groeneveld, Jeroen] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Naafs, B. David A.] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany; [Van Renterghem, Cederic; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Hennissen, Jan; Head, Martin J.] Univ Toronto, Dept Earth Sci, Toronto, ON, Canada; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Fabian, Karl] Norwegian Geol Survey, Trondheim, Norway	University of Bergen; University of Bremen; University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Ghent University; University of Toronto; Brock University; Geological Survey of Norway	De Schepper, S (通讯作者)，Univ Bergen, Dept Earth Sci, Bergen, Norway.	smad2@cantab.net	Hennissen, Jan/AAT-7729-2020; Fabian, Karl/AAC-8643-2022; De Schepper, Stijn/A-2836-2011; Louwye, Stephen/D-3856-2012; Naafs, Bernhard/F-5257-2012	Hennissen, Jan/0000-0002-0435-3343; De Schepper, Stijn/0000-0002-6934-0914; Louwye, Stephen/0000-0003-4814-4313; Naafs, Bernhard/0000-0001-5125-6928	Deutsche Forschungsgemeinschaft [SCHE 1665/2-1, SCHE 1665/2-2, NA973/1-1]; University of Bergen; MARUM Student Summer Fellowship; NSERC Canada Discovery Grant; NERC [bgs05002] Funding Source: UKRI	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); University of Bergen; MARUM Student Summer Fellowship; NSERC Canada Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research was supported by Deutsche Forschungsgemeinschaft grants SCHE 1665/2-1 and SCHE 1665/2-2 (SDS) and NA973/1-1 (BDAN), the University of Bergen (SDS), a MARUM Student Summer Fellowship (CVR), and a NSERC Canada Discovery Grant (MJH). 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	Prabowo, DA; Hiraishi, O; Suda, S				Prabowo, Danang Ambar; Hiraishi, Ooshi; Suda, Shoichiro			DIVERSITY OF <i>Crypthecodinium</i> spp. (DINOPHYCEAE) FROM OKINAWA PREFECTURE, JAPAN	JOURNAL OF MARINE SCIENCE AND TECHNOLOGY-TAIWAN			English	Article						Crypthechodinium chonii; taxonomy; phylogeny; diversity; heterotrophic dinoflagellates	CELL-CYCLE; DINOFLAGELLATE; PHYLOGENY; TAXONOMY; HISTORY; COMPLEX; MEMBERS; ACID	The genus Crypthecodinium (Dinophyceae) currently consists of only one species: C. cohnii, a heterotrophic marine dinoflagellate widely known able to produce prolific amount of DHA. However, previous studies revealed that there are morphological and genetic differences among Crypthedodinium cohnii-like strains, indicating the potential of undiscovered diversity of this dinoflagellate. Attempts of isolating heterotrophic marine dinoflagellate strains were made from submerged mangrove leaves and seaweed. A total of nine strains were established, cultured and maintained using seawater-based GTY medium for taxonomic identification and phylogenetic analyses based on SSU, ITS 1, 5.8S, ITS2 and LSU rDNA. Morphological observation revealed all strains shared similar morphology, e.g.: motile cells were delicately thin armored with single or double flagella surrounding the cingulum and protruding along the sulcus posteriorly, while non-motile cell stage (cyst) may retain more than two daughter cells inside the transparent and thick cell wall. Both cell stages varied in sizes and shapes even within the same clonal culture. Numerous lipid granules can be observed in the cytoplasm. Two types of cingulum encirclement were observed: partially or completely surrounding the cell body. All strains indicated close relatedness (>95% sequence similarity) with previously reported Cryphtecodinium cohnii strains, except for C. cohnii CAAE-CL2 (87.2-87.4% similarity) in SSU and C. cohnii CCMP316 (79.9-80.4% similarity) in ITS. Moreover, molecular phylogenetic tree grouped the Okinawan isolates into two genetically distinct clades with high similarity (>98%) among members of each clade in SSU and LSU but only shared 80.5% similarity in ITS rDNA. The results of this study showed evidences of undiscovered diversity in the heterotrophic dinoflagellates currently regarded as Crypthecodinium.	[Prabowo, Danang Ambar] Univ Ryukyus, Fac Sci, Grad Sch Engn & Sci, Okinawa, Japan; [Hiraishi, Ooshi; Suda, Shoichiro] Univ Ryukyus, Fac Sci, Dept Chem Biol & Marine Sci, Okinawa, Japan	University of the Ryukyus; University of the Ryukyus	Suda, S (通讯作者)，Univ Ryukyus, Fac Sci, Dept Chem Biol & Marine Sci, Okinawa, Japan.	sudas@sci.u-ryukyu.ac.jp	Suda, Shoichiro/ABA-9738-2020; Prabowo, Danang/AAC-8440-2021; Ambar Prabowo, Danang/K-1612-2016	Ambar Prabowo, Danang/0000-0001-8200-1266	Okinawa Intellectual Cluster Program; International Research Hub Project for Climate Change and Coral Reef/Island Dynamics of the University of the Ryukyus, Japan	Okinawa Intellectual Cluster Program; International Research Hub Project for Climate Change and Coral Reef/Island Dynamics of the University of the Ryukyus, Japan	This work was partially supported by Okinawa Intellectual Cluster Program and International Research Hub Project for Climate Change and Coral Reef/Island Dynamics of the University of the Ryukyus, Japan.	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Mar. Sci. Technol.-Taiwan	DEC	2013	21			S			181	191		10.6119/JMST-013-1220-8	http://dx.doi.org/10.6119/JMST-013-1220-8			11	Engineering, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Oceanography	AE5FX					2025-03-11	WOS:000334014300023
J	Tang, YZ; Harke, MJ; Gobler, CJ				Tang, Ying Zhong; Harke, Matthew J.; Gobler, Christopher J.			MORPHOLOGY, PHYLOGENY, DYNAMICS, AND ICHTHYOTOXICITY OF <i>PHEOPOLYKRIKOS HARTMANNII</i> (DINOPHYCEAE) ISOLATES AND BLOOMS FROM NEW YORK, USA	JOURNAL OF PHYCOLOGY			English	Article						harmful algal blooms (HABs); ichthyotoxicity; Pheopolykrikos hartmannii; sheepshead minnows	HARMFUL ALGAL BLOOMS; POLYKRIKOS-KOFOIDII; LONG-ISLAND; DINOFLAGELLATE; CYSTS; EUTROPHICATION; GYMNODINIALES; SCHWARTZII; INFERENCE; MRBAYES	We report on morphological observations, phylogenetic analyses, bloom dynamics, and ichthyotoxicity of the common but poorly characterized dinoflagellate Pheopolykrikos hartmannii (Zimmermann) Matsuoka et Fukuyo. From 2008 to 2010 in the Forge River Estuary, NY, USA, P.hartmannii bloomed during summer and early fall, achieving densities exceeding 8,000 cellsmL(-1) and often dominating microphytoplankton communities. Large subunit (LSU) and small subunit (SSU) rDNA sequences demonstrated that NY isolates of P.hartmannii sequences were 99%-100% identical to P.hartmannii isolates from eastern US and Korea. In both the LSU and SSU rDNA phylogenies, the clades containing P.hartmannii sequences were distinct sister clades to those composed of Polykrikos schwartzii and P.kofoidii. In the LSU rDNA phylogeny, however, the clade composed of P.hartmannii and a sequence of the photosynthetic Polykrikos lebourae was well separated from the clade composed of 10 entries of Polykrikos schwartzii and P.kofoidii. In addition, a gap of similar to 180 bases was observed when the LSU rDNA sequences of P.hartmannii were aligned with P.schwartzii and P.kofoidii but was not observed in the alignment between P.hartmannii and P.lebourae. Using scanning electron microscopy, several morphological features previously not reported for P.hartmannii were observed: a ventral groove located in the sulcus, a deep arc-like apical concavity within the area of apical groove, scale-like vesicles, and a shallow, completely enclosed, loop-like apical groove. Resting cysts with arrow-like surface spines were produced heterothallically by crossing clonal isolates and germinated single gymnoid cells. Finally, filtered and unfiltered bloom water from the Forge River and clonal cultures of P.hartmannii exhibited acute ichthyotoxicity to juvenile sheepshead minnows (Cyprinodon variegates) and aeration did not mitigate this effect, suggesting P.hartmannii is an ichthyotoxic, harmful alga.	[Tang, Ying Zhong; Harke, Matthew J.; Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA; [Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Shandong, Peoples R China	State University of New York (SUNY) System; Stony Brook University; Chinese Academy of Sciences; Institute of Oceanology, CAS	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; New Renaissance Foundation	Suffolk County; New Renaissance Foundation	This project was funded by Suffolk County and from the New Renaissance Foundation. This is contribution 1420 from the School of Marine and Atmospheric Sciences, Stony Brook University.	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Phycol.	DEC	2013	49	6					1084	1094		10.1111/jpy.12114	http://dx.doi.org/10.1111/jpy.12114			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	270UD	27007629				2025-03-11	WOS:000328343400007
J	Hernández-Becerril, DU; Rodríguez-Palacio, MC; Lozano-Ramírez, C				Hernandez-Becerril, David U.; Rodriguez-Palacio, Monica C.; Lozano-Ramirez, Cruz			Morphology and life stages of the potentially pinnatoxin-producing thecate dinoflagellate <i>Vulcanodinium rugosum</i> from the tropical Mexican Pacific	BOTANICA MARINA			English	Article						dinoflagellates; Mexican Pacific; new record; phytoplankton; Vulcanodinium rugosum	BENTHIC DINOFLAGELLATE; NOV. DINOPHYCEAE; GEN. NOV.; COASTS; AUSTRALIA; WATERS; OCEAN	During a phytoplankton survey, non-motile (cyst-like) cells were isolated and cultured from the tropical Mexican Pacific, which belong to the thecate dinoflagellate Vulcanodinium rugosum Nezan et Chomerat, recently described from the Mediterranean and recently identified as a source of pinnatoxins in Australia, New Zealand, and Japan. Motile cells and putative cysts were studied by light microscopy and scanning electron microscopy. The most characteristic features of the species agree with a previous description: (i) large and conspicuous apical pore, which extrudes mucilaginous material; (ii) polygonal and striated theca; (iii) ventral, sigmoid canal running from the apical pore to the anterior margin of the cingulum; (iv) three connected anterior intercalary plates; and (v) production of spherical cyst-like cells. The species is photosynthetic, containing many small greenish-brown chloroplasts. The tabulation of the species is Po, X, 4', 3a, 7 '', 6c, 5s?, 5''', 2''''. Organic cyst-like cells were nearly spherical to subspherical, solitary, or aggregations linked by mucilaginous material; they are considered to be a stage in the life cycle of the species. Vulcanodinium rugosum is a new record in the study area. The ecology and the geographical distribution of the species are also discussed.	[Hernandez-Becerril, David U.] Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Mexico City 04510, DF, Mexico; [Rodriguez-Palacio, Monica C.; Lozano-Ramirez, Cruz] Univ Autonoma Metropolitana Iztapalapa, Dept Hidrobiol, Lab Ficol Aplicada, Mexico City 09340, DF, Mexico	Universidad Nacional Autonoma de Mexico; Universidad Autonoma Metropolitana - Mexico	Hernández-Becerril, DU (通讯作者)，Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Apartado Postal 70-305, Mexico City 04510, DF, Mexico.	dhernand@cmarl.unam.mx	RODRIGUEZ PALACIO, MONICA CRISTINA/G-8190-2019	Rodriguez Palacio, Monica Cristina/0000-0001-5643-958X				[Anonymous], 2003, PLANCTOLOG A MEXICAN; [Anonymous], 2006, ACTA BOT MEX, DOI DOI 10.21829/ABM74.2006.1008; Esqueda-Lara K, 2005, CAH BIOL MAR, V46, P335; Esqueda-Lara K, 2013, J MAR BIOL ASSOC UK, V93, P1187, DOI 10.1017/S0025315412001750; Faust MA, 1998, PHYCOLOGIA, V37, P47, DOI 10.2216/i0031-8884-37-1-47.1; Faust MA, 1996, J PHYCOL, V32, P669, DOI 10.1111/j.0022-3646.1996.00669.x; Gottschling M, 2012, PROTIST, V163, P15, DOI 10.1016/j.protis.2011.06.003; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Hernandez-Becerril D.U., 2012, OCEANOGR, V47, P553; Hernández-Becerril DU, 2008, J MAR BIOL ASSOC UK, V88, P1, DOI 10.1017/S0025315408000143; Hernández-Becerril DU, 2007, J ENVIRON SCI HEAL A, V42, P1349, DOI 10.1080/10934520701480219; Hernández-Becerril DU, 2010, CRYPTOGAMIE ALGOL, V31, P245; Hernández-Becerril DU, 2004, BOT MAR, V47, P417, DOI 10.1515/BOT.2004.051; Hernández-Becerril DU, 2004, PHYCOLOGIA, V43, P341, DOI 10.2216/i0031-8884-43-4-341.1; HORIGUCHI T, 1983, BOT MAG TOKYO, V96, P351, DOI 10.1007/BF02488179; Jeong Hae Jin, 2012, Ocean Science Journal, V47, P1, DOI 10.1007/s12601-012-0001-y; Nézan E, 2011, CRYPTOGAMIE ALGOL, V32, P3, DOI 10.7872/crya.v32.iss1.2011.003; 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, 2011, PHYCOLOGIA, V50, P624, DOI 10.2216/11-19.1; Rodriguez-Palacio M.C., 2007, 4 EUR PHYC C OV SPAI, P111; Sekida Satoko, 2001, Phycological Research, V49, P163, DOI 10.1111/j.1440-1835.2001.tb00247.x; Smith KF, 2011, HARMFUL ALGAE, V10, P702, DOI 10.1016/j.hal.2011.05.006; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; Ten-Hage L, 2001, EUR J PHYCOL, V36, P129, DOI 10.1017/S0967026201003146	25	16	16	1	28	WALTER DE GRUYTER GMBH	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055	1437-4323		BOT MAR	Bot. Marina	DEC	2013	56	5-6					535	540		10.1515/bot-2013-0079	http://dx.doi.org/10.1515/bot-2013-0079			6	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	269UM					2025-03-11	WOS:000328267600013
J	Danesh, DC; McCarthy, FMG; Volik, O; Drljepan, M				Danesh, Donya C.; McCarthy, Francine M. G.; Volik, Olena; Drljepan, Matea			Non-pollen palynomorphs as indicators of water quality in Lake Simcoe, Ontario, Canada	PALYNOLOGY			English	Article						non-pollen palynomorphs; water quality; eutrophication; Lake Simcoe; polders	CRAWFORD LAKE; DINOFLAGELLATE CYSTS; SPATIAL VARIABILITY; LAND-USE; PHOSPHORUS; EUTROPHICATION; SEDIMENT; RECORD; LOADS; TRENDS	The distribution of non-pollen palynomorphs (NPP) in a core from Cook's Bay, Lake Simcoe, shows a response to changes in water quality accompanying agriculture, urbanization and industrialization. Low concentrations of nutrients in sediments with little non-arboreal pollen (NAP) record low disturbance prior to European settlement approximate to 1850s. These sediments are rich in desmids such as Cosmarium spp., Euastrum spp., and Staurastrum spp., an assemblage indicative of oligotrophic conditions. A decline in desmids together with an increase in dinoflagellates and thecamoebians up-core is consistent with increased nutrients. Abundant phytoliths in sediments that are relatively rich in Poaceae and other NAP records the draining of the Holland Marshes. A sharp increase in nutrient levels, together with a transition from high nitrite (NO2) to high nitrate (NO3) concentrations, records a sudden increase in biological oxygen demand leading to depletion of dissolved oxygen associated with the creation of polders in the 1920s and 1930s. A second influx of phytoliths immediately preceded the sharp rise in Ambrosia, recording rapid land clearing accompanying the five-fold post-World War II population boom in the Cook's Bay watershed. These Ambrosia-rich sediments are rich in metals and have high total phosphorus and NO3, with abundant Pediastrum spp. and Peridinium spp., notably Peridinium willei and Peridinium volzii, recording eutrophication. The abundance of the ciliate Codonella cratera and the difflugiid thecamoebians Cucurbitella tricuspis and Difflugia protaeiformis in palynological preparations as well as in washed thecamoebian samples from the upper part of the core records low dissolved oxygen associated with continued eutrophication of Cook's Bay.	[Danesh, Donya C.; McCarthy, Francine M. 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J	Chen, YY				Chen, Yow-Yuh			<i>Palaecysta</i> gen. nov., the greatest <i>Systematophora</i> imposter no more: introducing a lineage of latest Jurassic to Early Cretaceous (Tithonian-Hauterivian) dinoflagellate cysts from Madagascar	PALYNOLOGY			English	Article						Amphorula; Amphorulacysta; arcuate; biochronostratigraphy; dinoflagellate; Hauterivian; Kilwacysta; Madagascar; Palaecysta; Systematophora; Tithonian	STRATIGRAPHY; STRATA; MIDDLE	A lineage of dinoflagellate cysts possessing arcuate process clusters from Madagascar is described. The lineage has helped to reveal the true identity of a group of skolochorate dinoflagellate cysts, bearing numerous long processes and process clusters, which have been reported as species of Systematophora. The revelation is that that group does not belong to Systematophora, but affiliates with the Madagascar lineage. A new genus, Palaecysta, is proposed. Seven new species: P. integra (type species), P. crispabaculata, P. foveoreticulata, P. melakyensis, P. morondavaensis, P. pectita, and P. virgae; eight new subspecies: P. integra subsp. digitata, P. integra subsp. mahajangaensis, P. crispabaculata subsp. delicata, P. foveoreticulata subsp. madagascarensis, P. palmula subsp. ankamotraensis, P. pectita subsp. merinai, P. virgae subsp. externa, and P. virgae subsp. lanceolata; and three new combinations: P. complicata (Neale and Sarjeant, 1962), P. palmula (Davey, 1982), and P. silyba (Davey, 1979a) are described. Palaecysta shares some morphological features with Systematophora, including skolochorate cyst, intra- to penitabular paratabulation, and gonyaulacacean, sexiform and apical archeopyle, but differs in having arcuate process clusters and two unlinked isolated paracingular processes in each paracingular paraplate, as oppose to nearly penitabular, annulate process clusters and two linked (by a low basal ridge) paracingular processes in each paracingular paraplate in the latter genus. Palaecysta occurred globally from the Tithonian to the Hauterivian. Its rapid evolution provides useful timelines for biostratigraphy; six assemblage zones are established. The zonation is compared with that from neighbouring regions in Australia and Papua New Guinea. The morphological differences and similarities between Palaecysta and other related genera, Systematophora, Kilwacysta, and Amphorulacysta gen. nov., are discussed. The significance of the arcuate dinoflagellate cysts group and the interrelationship amongst their member genera, reflected in the geological record, are commented upon. The genus Amphorula is emended.	ExxonMobil Explorat Co, Houston, TX 77060 USA	Exxon Mobil Corporation	Chen, YY (通讯作者)，ExxonMobil Explorat Co, 233 Benmar Dr, Houston, TX 77060 USA.	yowyuh.chen@exxonmobil.com						Abbink OA, 2001, P YORKS GEOL SOC, V53, P275, DOI 10.1144/pygs.53.4.275; BEJU D., 1971, Annales Instituti Geologici Publici Hungarici, V54, P275; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; Brenner W., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V122, P511, DOI 10.2973/odp.proc.sr.122.158.1992; BRENNER W., 1988, Tubinger Mikropalaontologische Mitteilungen, V6, P1; BURGER D, 1982, Palynology, V6, P161; Chen Y Y., 1978, THESIS U ARIZONA ARI; Courtinat B, 1980, INVENTAIRE REPARTITI, V78, P123; Davey R.J., 1982, Danmarks Geologiske Undersogelse Serie B, P1; DAVEY R J, 1979, Palaeontology (Oxford), V22, P427; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; Davey R.J., 1987, Memoir of Geological Survey of Papua New Guinea, V13, P1; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; DAVEY RJ, 1969, B BRIT MUSEUM NATU S, V3, P15; Dodekova L., 1969, Izvestiya na Geologicheskaya Institut Sofia (Paleont), V18, P13; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; Durr G., 1988, TUBINGER MIKROPALAON, V5, P159; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; Feist-Burkhardt S, 2012, DUXBURY 1983 DATABAS, V186, P18; GITMEZ G.U., 1970, B BRIT MUS NAT HIST, V18, P231; Grove W. B., 1922, J BOT BRIT FOREIGN, V60, P81; Helby R., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V123, P407, DOI 10.2973/odp.proc.sr.123.121.1992; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Ioannides N.S., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P471; IOANNIDES N S, 1976, Micropaleontology (New York), V22, P443, DOI 10.2307/1485174; JIANG Q, 1992, REV PALAEOBOT PALYNO, V74, P77, DOI 10.1016/0034-6667(92)90139-8; Klement K. W., 1960, Palaeontographica, VA114, P1; KUNZ R, 1990, Palaeontographica Abteilung B Palaeophytologie, V216, P1; Lentin J.K., 1976, Bedford Institute of Oceanography, Report Series, VBI-R-75-16, P237; Mantle DJ, 2009, PALAEONTOGR ABT B, V280, P87, DOI 10.1127/palb/280/2009/87; MONTEIL E, 1990, B CENT RECH EXPL, V14, P597; NeaLE J.W., 1962, GEOL MAG, V99, P439; NOhr-Hansen H., 1986, GEOL SOC DENMARK B, V35, P31; Partridge A D., 2006, JURASSIC EARLY CREAT; Pavlishina Polina, 2004, Spisanie na B"lgarskoto Geologichesko Druzhestvo, V65, P107; Raynaud J.F., 1978, Palinologia, P387; RIDING J B, 1988, Palynology, V12, P65; Riding J B, 2001, MEM ASS AUSTRAL PALA, V24, P111; Riding JB, 2010, REV PALAEOBOT PALYNO, V162, P543, DOI 10.1016/j.revpalbo.2010.07.008; Riding JB., 1999, American Association of Stratigraphic Palynologists Contributions Series., V36, P179; Sarjeant W.A.S., 1980, Acta Palaeontologica Polonica, V25, P279; Schrank E, 2005, PALYNOLOGY, V29, P49, DOI 10.2113/29.1.49; STANCLIFFE RPW, 1990, MICROPALEONTOLOGY, V36, P197, DOI 10.2307/1485506; Stover L.E., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P261; Stover L.E., 1978, Analyses of Pre-Pleistocene Organic-Walled Dinoflagellates, V15; van Helden B.G.T., 1986, Palynology, V10, P181; Volkheimer W, 1993, NEUES JB GEOLOGIE PA, V1993, P246; Volkheimer Wolfgang, 2010, Rev. Mus. Argent. Cienc. Nat., V12, P233; WIGGINS V D, 1969, Micropaleontology (New York), V15, P145, DOI 10.2307/1484918; Williams G.L., 1975, GEOL SURV CAN PAP, V2, P107, DOI DOI 10.4095/102513; WILLIAMS GL, 1980, INITIAL REPORTS DEEP, V50, P467; ZOTTO M, 1987, MICROPALEONTOLOGY, V33, P193, DOI 10.2307/1485637	52	6	6	0	3	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	DEC 1	2013	37	2					259	297		10.1080/01916122.2013.782367	http://dx.doi.org/10.1080/01916122.2013.782367			39	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	265JG					2025-03-11	WOS:000327946600008
J	Clowes, CD				Clowes, Christopher D.			<i>Graptodinium</i>, a new Paleogene dinoflagellate cyst	PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Paleogene (Eocene-Oligocene); New Zealand	SOUTHWEST ATLANTIC-OCEAN; BIOSTRATIGRAPHY; OLIGOCENE; SEA	Graptodinium is a new genus of proximate dinoflagellate cysts with an apical archaeopyle, a cladopyxiacean tabulation and a distinctive intratabular ornamentation. It is represented by Graptodinium inconditum sp. nov. and Graptodinium omnireticulatum sp. nov. These species range from the Middle Eocene to at least the Early Oligocene in New Zealand. Graptodinium ranges geographically from the Arctic to the high southerly latitudes.	Victoria Univ Wellington, Sch Earth Sci, Wellington, New Zealand	Victoria University Wellington	Clowes, CD (通讯作者)，Victoria Univ Wellington, Sch Earth Sci, POB 600, Wellington, New Zealand.	chris@peripatus.gen.nz						[Anonymous], ANAL PREPLEISTOCENE; [Anonymous], AM ASS PETROLEUM GEO; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; AUBRY MP, 1986, PALAEOGEOGR PALAEOCL, V55, P267, DOI 10.1016/0031-0182(86)90154-9; Brinkhuis H, 1992, THESIS U UTRECHT UTR, P169; CHATEAUNEUF JJ, 1980, MEM BRGM, V116, P360; Clowes C D, 1984, NZ GEOL SURV REC, V3, P30; Cooper R. A., 2004, NZ GEOLOGICAL I GEOL, V22, P284; De Coninck J., 1986, MEDEDELINGEN RIJKS G, V40, P49; Edwards. L.E, 1984, P124; Edwards L E., 1977, THESIS U CLAIFORNIA; Fensome R.A., 1993, Micropaleontology Press Special Paper; GOODMAN DK, 1983, INITIAL REP DEEP SEA, V71, P859; Head M J, 1989, OCEAN DRILLING PROGR, V105, P515; Lentin, 1990, AM ASS STRATIGRAPHIC, V23, P221; Schioler P, 2005, J MICROPALAEONTOL, V24, P1, DOI 10.1144/jm.24.1.1; Stover Lewis E., 1994, Bulletin de la Societe Belge de Geologie, V102, P5; Vozzhennikova T.F., 1967, FOSSIL PERIDINEAE JU; Wilson G J, 1982, PAL, V56, P1; Wilson G J, 1982, PAL, V60, P1; Wilson G.J., 1985, NZ GEOLOGICAL SURVEY, V8, P93; Wilson G J, 1996, 9639 I GEOL NUCL SCI, P182; WISE SW, 1983, INITIAL REP DEEP SEA, V71, P481	24	1	1	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	DEC 1	2013	37	2					316	324		10.1080/01916122.2013.775007	http://dx.doi.org/10.1080/01916122.2013.775007			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	265JG					2025-03-11	WOS:000327946600010
J	Dehbozorgi, A; Sajjadi, F; Hashemi, H				Dehbozorgi Afsaneh; Sajjadi Freshteh; Hashemi Hossein			Middle Jurassic palynomorphs of the Dalichai Formation, central Alborz Ranges, northeastern Iran: Paleoecological inferences	SCIENCE CHINA-EARTH SCIENCES			English	Article						palynomorphs; Middle Jurassic; paleoecology; Alborz Ranges; Dalichai Formation	IN-SITU; AREA; PALYNOLOGY; BASIN; FLORA	Palynological data are used to draw paleoecological inferences for the Dalichai Formation, northeast of Semnan, northeastern Iran. All samples examined yield well-preserved, diverse palynofloras consisting predominantly of miospores; dinoflagellate cysts, foraminiferal test linings, and fungal spores occur as minor constituents. Fifty-four species of spores (37 genera), 18 species of pollen (9 genera), and 16 species of dinoflagellate cysts (13 genera) are recognized. Co-occurrence of such miospore species with known vertical ranges as Klukisporites variegatus, Sellaspora asperata, Murospora florida, and Concavissimisporites verrucosus suggests a Middle Jurassic (Bajocian-Callovian) age for the host strata, thus corroborating the available paleozoological evidence. Such spore species as Klukisporites, Cyathidites, and Dictyophyllidites known to have been produced by Pterophyta dominate the palynofloras. Thus the contemporaneous coastal vegetation was characterized by predominance of Pterophyta whereas representatives of Ginkgophyta, Pteridospermophyta, Lycophyta, Coniferophyta, and Bryophyta were rarely represented. This reconstruction implies that a moist, warm climate prevailed in northeastern Iran during the Middle Jurassic (Bajocian-Callovian). This is confirmed by occurrence of fungal spores accompanied by such warm water dinoflagellate cysts as Mendicodinium groenlandicum, Pareodinia ceratophora, and Gonyaulacysta jurassica. Abundance of Amorphous Organic Matter (AOM) signifies a shallow, low-energy, dysoxic-anoxic depositional site for the host strata. Furthermore, the ratio of AOM to marine palynomorphs as well as abundance of blade-shaped to eqiudimensional opaque palynomacerals could indicate low sedimentation rate in a shallow, low-oxygenated marine environment. Additionally, occurrence of chorate dinoflagellate cysts (e.g., Adnatosphaeridium caulleryi) and acritarchs bearing relatively long processes (e.g., Micrhystridium) possibly suggests deepening upward in the study section.	[Dehbozorgi Afsaneh; Sajjadi Freshteh] Univ Tehran, Coll Sci, Fac Sci, Tehran 141556455, Iran; [Hashemi Hossein] Kharazmi Univ, Fac Sci, Dept Geol, Tehran 15614, Iran; [Hashemi Hossein] Kharazmi Univ, Res Sch Appl Sci, Tehran 15614, Iran	University of Tehran; Kharazmi University; Kharazmi University	Dehbozorgi, A (通讯作者)，Univ Tehran, Coll Sci, Fac Sci, Enghelab Ave, Tehran 141556455, Iran.	dehbozorgi58@yahoo.com						Abbink O.A., 1998, Contributions Series, V8, P192; Alavi-Naeini M., 1972, 23 GEOL SURV IR, P293; ALVIN K L, 1978, Palaeontology (Oxford), V21, P847; Backhouse J., 1988, LATE JURASSIC EARLY, V135, P233; BALME BE, 1995, REV PALAEOBOT PALYNO, V87, P85; Barrón E, 2006, REV PALAEOBOT PALYNO, V138, P187, DOI 10.1016/j.revpalbo.2006.01.002; Couper R.A., 1960, NZ GEOL SURV PALEONT, V32, P87; DETTMANN M.E., 1963, P ROY SOC VICTORIA, V77, P1; DETTMANN ME, 1992, ALCHERINGA, V16, P269, DOI 10.1080/03115519208619111; Diéguez C, 2010, REV PALAEOBOT PALYNO, V162, P325, DOI 10.1016/j.revpalbo.2010.06.004; DiMichele WA, 2002, REV PALAEOBOT PALYNO, V119, P143, DOI 10.1016/S0034-6667(01)00134-8; Fakhr M S, 1975, THESIS U PIERRE M CU, V2, P421; Filatoff J., 1975, Palaeontographica Abteilung B Palaeophytologie, V154, P1; Filatoff J., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P89; Ghasemi-Nejad E, 1999, SCHWEIZ PALAONTOL AB, V119, P69; Ghasemi-Nejad E, 2012, J ASIAN EARTH SCI, V43, P1, DOI 10.1016/j.jseaes.2011.08.006; Jansson IM, 2008, REV PALAEOBOT PALYNO, V150, P5, DOI 10.1016/j.revpalbo.2008.01.002; Jasper K, 2010, REV PALAEOBOT PALYNO, V162, P123, DOI 10.1016/j.revpalbo.2010.06.009; Lindström S, 2006, PALAEOGEOGR PALAEOCL, V241, P339, DOI 10.1016/j.palaeo.2006.04.006; Madler K.A., 1964, Fortschritte in der Geologie von Rheinland und Westfalen, V12, P169; Nabavi M.H, 1977, Neues Jb Geol Paleont Abh, V153, P70; NANDI B, 1990, REV PALAEOBOT PALYNO, V65, P119, DOI 10.1016/0034-6667(90)90063-O; Peppers RA, 1997, REV PALAEOBOT PALYNO, V98, P223, DOI 10.1016/S0034-6667(97)00013-4; Pflug H., 1953, PALAEONTOGRAPHICA, V95, P60; Pocock S. 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J., 1970, Palaeontographica Abteilung B, V130, P73; Riding James B., 1999, Palynology, V23, P15; Roghi G, 2004, REV PALAEOBOT PALYNO, V132, P1, DOI 10.1016/j.revpalbo.2004.03.001; Sajjadi F, 2002, PALAEONTOGR ABT B, V261, P99; Schairer G., 1991, Mitteilungen der Bayerischen Staatssammlung fuer Palaeontologie und Historische Geologie, V31, P47; Schweitzer Hans-Joachim, 1998, Palaeontographica Abteilung B Palaeophytologie, V248, P1; Schweitzer Hans-Joachim, 1997, Palaeontographica Abteilung B Palaeophytologie, V243, P103; Schweitzer Hans-Joachim, 1996, Palaeontographica Abteilung B Palaeophytologie, V238, P77; Schweitzer Hans-Joachim, 1995, Palaeontographica Abteilung B Palaeophytologie, V237, P1; Schweitzer HJ, 2003, PALAEONTOGR ABT B, V264, P1; Seyed-Emami K, 2008, ACTA PALAEONTOL POL, V53, P237, DOI 10.4202/app.2008.0206; Taylor TN, 2009, PALEOBOTANY: THE BIOLOGY AND EVOLUTION OF FOSSIL PLANTS, 2ND EDITION, P1; Traverse A., 2007, Paleopalynology, VSecond; Tryon A.F., 1982, Ferns and Allied Plants with Special Reference to Tropical America, P857; Vaez-Javadi F, 2006, ALCHERINGA, V30, P63, DOI 10.1080/03115510608619345; Vakhrameev V.A., 1991, Jurassic and Cretaceous floras and climates of the Earth, P318; van der Ham RWJM, 2003, REV PALAEOBOT PALYNO, V127, P77, DOI 10.1016/S0034-6667(03)00095-2; van Konijnenburg-van Cittert JHA, 2008, P GEOLOGIST ASSOC, V119, P59, DOI 10.1016/S0016-7878(08)80258-1; Wheeler J.W., 1990, Modern Geology, V14, P267; Wikström N, 2001, MOL PHYLOGENET EVOL, V19, P177, DOI 10.1006/mpev.2001.0936; Wu XG, 2006, REV PALAEOBOT PALYNO, V138, P209, DOI 10.1016/j.revpalbo.2006.01.009; Zhou ZY, 2006, GEOL J, V41, P363, DOI 10.1002/gj.1049; Zhou ZY., 2009, PALAEOWORLD, V18, P1, DOI [DOI 10.1016/j.palwor.2009.01.001, 10.1016/j.palwor.2009.01.001]	47	20	20	0	7	SCIENCE PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA	1674-7313	1869-1897		SCI CHINA EARTH SCI	Sci. China-Earth Sci.	DEC	2013	56	12					2107	2115		10.1007/s11430-013-4697-z	http://dx.doi.org/10.1007/s11430-013-4697-z			9	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	267CN					2025-03-11	WOS:000328074400011
J	Goudeau, MLS; Grauel, AL; Bernasconi, SM; de Lange, GJ				Goudeau, Marie-Louise S.; Grauel, Anna-Lena; Bernasconi, Stefano M.; de Lange, Gert J.			Provenance of surface sediments along the southeastern Adriatic coast off Italy: An overview	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						geochemistry; organic matter; grain size; multi-proxy; West Adriatic current (WAC); Adriatic mud belt	WATER CORAL PROVINCE; ORGANIC-MATTER; IONIAN SEA; MEMBRANE-LIPIDS; GULF; SHELF; INDICATORS; PROXIES; MARINE; ORIGIN	Multi-proxy studies are necessary to understand sediment composition and related provenance on continental shelfs. Here it is shown that the spatial distribution of geochemical composition and grain size for surface sediments along the southeastern Italian coast is related to provenance and mechanisms influencing sediment pathways. A northern Adriatic/Italian provenance can be distinguished from a southern Apennine river source. This is done independent of grain size using the element ratios Ce/Ni and Zr/Cr. Furthermore, the origin of organic matter is determined using bulk carbon isotopes and the C/N ratio. Integrating these results with those from complementary studies on delta O-18 and delta C-13 of Globigerinoides ruber (white), the BIT index, stable isotopes of plant waxes and dinoflagellate cyst distribution from the same set of samples reveals that: Sediments from the northwestern Adriatic are transported as far southward as the Gallipoli shelf (eastern Gulf of Taranto) by the Western Adriatic Current (WAC) Along the WAC, there is a consistent southward decrease in Po river/northern Apennines provenance and a concomitant decrease in terrestrial (soil) organic matter (OM), whereas the percentage of marine OM increases. The provenance for Gallipoli shelf sediments is for similar to 80% attributed to Po River/northern Apennines sources and for similar to 20% to southern Italian sources. OM in the eastern Gulf of Taranto contains more marine OM than other areas within the WAC, whereas OM and sediments from the western part of the Gulf of Taranto have a more local, riverine provenance. (C) 2013 Elsevier Ltd. All rights reserved.	[Goudeau, Marie-Louise S.; de Lange, Gert J.] Geosci Utrecht Univ, Inst Earth Sci Geochem, NL-3584 CD Utrecht, Netherlands; [Grauel, Anna-Lena; Bernasconi, Stefano M.] ETH, Inst Geol, CH-8092 Zurich, Switzerland	Swiss Federal Institutes of Technology Domain; ETH Zurich	Goudeau, MLS (通讯作者)，Geosci Utrecht Univ, Inst Earth Sci Geochem, NL-3584 CD Utrecht, Netherlands.	m.s.goudeau@uu.nl	; Bernasconi, Stefano/E-5394-2010; De Lange, Gert/B-9639-2014	Goudeau, Marie-Louise Sophie/0000-0001-7350-3424; Bernasconi, Stefano/0000-0001-7672-8856; De Lange, Gert/0000-0002-9420-3022	Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO); Swiss National Science Foundation (SNF) as part of the MOCCHA-project [20MA21-115934]; European Science Foundation (ESF) Eurocores Programme EuroMARC; Swiss National Science Foundation (SNF) [20MA21-115934] Funding Source: Swiss National Science Foundation (SNF)	Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO)(Netherlands Organization for Scientific Research (NWO)); Swiss National Science Foundation (SNF) as part of the MOCCHA-project(Swiss National Science Foundation (SNSF)); European Science Foundation (ESF) Eurocores Programme EuroMARC; Swiss National Science Foundation (SNF)(Swiss National Science Foundation (SNSF))	This work was supported by the Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO) and the Swiss National Science Foundation (SNF Project 20MA21-115934) as part of the MOCCHA-project funded by the European Science Foundation (ESF) Eurocores Programme EuroMARC.	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Coast. Shelf Sci.	DEC 1	2013	134						45	56		10.1016/j.ecss.2013.09.009	http://dx.doi.org/10.1016/j.ecss.2013.09.009			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	261PO					2025-03-11	WOS:000327677300005
J	Slimani, H; Toufiq, A				Slimani, Hamid; Toufiq, Abdelkabir			A Cretaceous-Palaeogene boundary geological site, revealed by planktic foraminifera and dinoflagellate cysts, at Ouled Haddou, eastern external Rif Chain, Morocco	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Cretaceous-Palaeogene boundary; Planktic foraminifera; Dinoflagellate cysts; Biostratigraphy; Ouled Haddou geosite; Morocco	TERTIARY BOUNDARY; EL-KEF; CALCAREOUS NANNOFOSSIL; WOODSIDE CREEK; BIOSTRATIGRAPHY; EXTINCTION; SECTION; IMPACT; STRATIGRAPHY; TRANSITION	Planktic foraminifera and organic-walled dinoflagellate cyst investigations in the Ouled Haddou outcrop (eastern external Rif Belt) in northern Morocco, revealed a continuous sedimentation and a complete record of the Cretaceous-Palaeogene (K-Pg) transition. Both planktic foraminifera and dinoflagellate cyst assemblages observed in the studied Maastrichtian-Danian boundary interval are diverse and well-preserved and contain numerous chronostratigraphically significant bio-events that have allowed a high resolution biostratigraphic analysis, based on the first and last occurrences of index species and also on the massive disappearance and abundance changes of different taxa. Planktic foraminifera allow correlation of the studied interval with the uppermost Maastrichtian Abathomphalus mayaroensis Zone and the lower Danian Guembelitria cretacea, Parvularugoglobigerina eugubina, Parasubbotina pseudobulloides and Subbotina triloculinoides zones. A mass extinction of planktic foraminifera is observed at the end of the Abathomphalus mayaroensis Zone. This mass extinction is followed by three renewal steps of planktic foraminifera in the basal Danian. The Cretaceous-Palaeogene boundary is placed just above the mass extinction of Globotruncanids and Heterohelicids and below the first appearences of earliest Danian markers genera Globoconusa, and Parvularugoglobigerina. According to dinoflagellate cysts, the recognition of the latest Maastrichtian and earliest Danian is based on global bio-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 and Senoniasphaera inornata. The dinoflagellate Damassadinium californicum Zone characterizing the Danian in the Northern Hemisphere is recognized in this section. The Cretaceous-Palaeogene boundary is placed, at the same position determined by Planktic foraminifera, immediately above the acme of Manumiella seelandica and the last appearance of few Cretaceous taxa such as Dinogymnium spp. and Alisogymnium euclaense, and directly below the first occurrences of Carpatella cornuta, Damassadinium californicum and Senoniasphaera inornata. However, in contrast to calcareous planktic foraminifera, dinoflagellate cysts did not undergo a mass extinction at the K-Pg boundary, but shows important changes in the relative abundances of different species or groups of morphologically related species. Both planktic foraminifera and dinoflagellate cyst assemblages suggest deposition in subtropical to warm temperate province, but in an austere sea environments under a regressive regime during the uppermost Maastrichtian and open sea environments under a transgressive regime during the lower Danian. Dinoflagellate cysts indicate relatively stable warm conditions during the upper Maastrichtian, followed successively by cooler conditions in the uppermost Maastrichtian and at the K-Pg boundary, a gradual warming alternated by 3 rapid successive cooling pulses in the lower most Danian, and then a gradual returning to relatively warm conditions. The Ouled Haddou section needs to be preserved as a geoheritage site, because it is the sole Moroccan section with a good quality and an easy access, and hosts a complete registration of the Cretaceous-Palaeogene boundary transition. (C) 2013 Elsevier Ltd. All rights reserved.	[Slimani, Hamid] Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, URAC 46, Rabat 10106, Morocco; [Toufiq, Abdelkabir] Univ Chouaib Doukkali, Fac Sci, Lab Geosci & Environm Tech, El Jadida 24000, Morocco	Mohammed V University in Rabat; 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.	h_slimani@yahoo.com; toufiq_a@yahoo.fr	Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913	University Mohammed V-Agdal, Morocco [SVT 11/09]; National Center of Scientific Research (CNRST), Morocco [URAC46]	University Mohammed V-Agdal, Morocco(Mohammed First University of Oujda); National Center of Scientific Research (CNRST), Morocco	The authors thank Dr. Stephen Louwye and Mrs. Sabine Van Cauwenberghe (Palaeontology Research Unit, University of Gent, Belgium) for the palynological preparation of the studied samples and the University Mohammed V-Agdal (Project SVT 11/09) and the National Center of Scientific Research (CNRST) (URAC46), Morocco for financial support. 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Afr. Earth Sci.	DEC	2013	88						38	52		10.1016/j.jafrearsci.2013.08.008	http://dx.doi.org/10.1016/j.jafrearsci.2013.08.008			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	252JR					2025-03-11	WOS:000327001500003
J	Bowman, VC; Francis, JE; Riding, JB				Bowman, Vanessa C.; Francis, Jane E.; Riding, James B.			Late Cretaceous winter sea ice in Antarctica?	GEOLOGY			English	Article							ISOTOPE STRATIGRAPHY; EXTINCTION PATTERNS; CARBON; BOUNDARY; QUATERNARY; BELEMNITE; EVOLUTION; STRONTIUM; PROFILES; CLIMATES	The Late Cretaceous is considered to have been a time of greenhouse climates, although evidence from Maastrichtian sediments for rapid and significant sea-level changes suggests that ice sheets were growing and decaying on Antarctica at that time. There is no direct geological evidence for glaciation, but we present palynomorph records from Seymour Island, Antarctica, that may suggest Maastrichtian sea ice. The dinoflagellate cyst Impletosphaeridium clavus is dominant. We propose that its profusion may signify the accumulation of resting cysts from dinoflagellate blooms related to winter sea ice decay. Prior to the Cretaceous-Paleogene transition, I. clavus decreased dramatically in abundance; we link this with climate warming. Terrestrial conditions inferred from pollen and spore data are consistent with our climate interpretations based on I. clavus together with delta O-18 values from macrofossils. These data and our interpretation support the presence of ephemeral ice sheets on Antarctica during the latest Cretaceous, highlighting the extreme sensitivity of this region to global climate change.	[Bowman, Vanessa C.; Francis, Jane E.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England; [Riding, James B.] British Geol Survey, Keyworth NG12 5GG, Notts, England	University of Leeds; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Bowman, VC (通讯作者)，British Antarctic Survey, Madingley Rd, Cambridge CB3 0ET, England.	Vanessa.Bowman@bas.ac.uk		Bowman, Vanessa/0000-0002-4887-3949	Natural Environment Research Council (NERC) [NE/C506399/1, NE/100582X/1]; TransAntarctic Association; NERC [NE/I005803/1, bgs05002, NE/I00582X/2, bas0100026, NE/I00582X/1] Funding Source: UKRI	Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); TransAntarctic Association; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We thank J.A. Crame, A.M. Haywood, S.J. Hunter, and J. Witts for discussions, and the British Antarctic Survey and crew of HMS Endurance for logistics during Antarctic field work. C. Day, B. Maltman, and M. Priestman provided field support. We thank the Natural Environment Research Council (NERC) for grants NE/C506399/1 (Antarctic Funding Initiative) and NE/100582X/1. Bowman also received TransAntarctic Association funding and an Antarctic Science Bursary. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC).	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J	Browning, JV; Miller, KG; Sugarman, PJ; Barron, J; McCarthy, FMG; Kulhanek, DK; Katz, ME; Feigenson, MD				Browning, James V.; Miller, Kenneth G.; Sugarman, Peter J.; Barron, John; McCarthy, Francine M. G.; Kulhanek, Denise K.; Katz, Miriam E.; Feigenson, Mark D.			Chronology of Eocene-Miocene sequences on the New Jersey shallow shelf: Implications for regional, interregional, and global correlations	GEOSPHERE			English	Article							SEA-LEVEL CHANGE; COASTAL-PLAIN; ISOTOPE STRATIGRAPHY; CONTINENTAL-SHELF; STRONTIUM-ISOTOPE; STABLE-ISOTOPE; PASSIVE MARGIN; MIDDLE MIOCENE; NORTH-ATLANTIC; RECORDS	Integrated Ocean Drilling Program Expedition 313 continuously cored and logged latest Eocene to early-middle Miocene sequences at three sites (M27, M28, and M29) on the inner-middle continental shelf offshore New Jersey, providing an opportunity to evaluate the ages, global correlations, and significance of sequence boundaries. We provide a chronology for these sequences using integrated strontium isotopic stratigraphy and biostratigraphy (primarily calcareous nannoplankton, diatoms, and dinocysts [dinoflagellate cysts]). Despite challenges posed by shallow-water sediments, age resolution is typically +/- 0.5 m.y. and in many sequences is as good as +/- 0.25 m.y. Three Oligocene sequences were sampled at Site M27 on sequence bottom-sets. Fifteen early to early-middle Miocene sequences were dated at Sites M27, M28, and M29 across clinothems in topsets, foresets (where the sequences are thickest), and bottomsets. A few sequences have coarse (similar to 1 m.y.) or little age constraint due to barren zones; we constrain the age estimates of these less well dated sequences by applying the principle of superposition, i.e., sediments above sequence boundaries in any site are younger than the sediments below the sequence boundaries at other sites. Our age control provides constraints on the timing of deposition in the clinothem; sequences on the topsets are generally the youngest in the clinothem, whereas the bottomsets generally are the oldest. The greatest amount of time is represented on foresets, although we have no evidence for a correlative conformity. Our chronology provides a baseline for regional and interregional correlations and sea-level reconstructions: (1) we correlate a major increase in sedimentation rate precisely with the timing of the middle Miocene climate changes associated with the development of a permanent East Antarctic Ice Sheet; and (2) the timing of sequence boundaries matches the deep-sea oxygen isotopic record, implicating glacioeustasy as a major driver for forming sequence boundaries.	[Browning, James V.; Miller, Kenneth G.; Sugarman, Peter J.; Feigenson, Mark D.] Rutgers State Univ, Dept Earth & Planetary Sci, Piscataway, NJ 08854 USA; [Barron, John] US Geol Survey, Menlo Pk, CA 94025 USA; [McCarthy, Francine M. G.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Kulhanek, Denise K.] GNS Sci, Dept Paleontol, Lower Hutt 5040, New Zealand; [Katz, Miriam E.] Rensselaer Polytech Inst, Troy, NY 12180 USA	Rutgers University System; Rutgers University New Brunswick; United States Department of the Interior; United States Geological Survey; Brock University; GNS Science - New Zealand; Rensselaer Polytechnic Institute	Browning, JV (通讯作者)，Rutgers State Univ, Dept Earth & Planetary Sci, Piscataway, NJ 08854 USA.		Miller, Kenneth/LZE-2268-2025	Browning, James/0000-0002-0664-6342; Barron, John/0000-0002-9309-1145; Kulhanek, Denise/0000-0002-2156-6383				Andrews G.W., 1988, 1481 US GEOL SURV; [Anonymous], PLANKTON STRATIGRAPH; Austin J.A., 1998, P OCEAN DRILLING P A, V174A, DOI [10.2973/odp.proc.ir.174a.1998., DOI 10.2973/0DP.PR0C.IR.174A.1998]; BARRETT PJ, 1987, GEOLOGY, V15, P634, DOI 10.1130/0091-7613(1987)15<634:MROGAS>2.0.CO;2; Barron JA, 2003, DIATOM RES, V18, P203; Barron JA, 2013, GEOSPHERE, V9, P1286, DOI 10.1130/GES00864.1; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Billups K, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2000PA000568; Boulila S, 2011, EARTH-SCI REV, V109, P94, DOI 10.1016/j.earscirev.2011.09.003; Bown P.R., 1998, P16; Bown Paul R., 1998, CALCAREOUS NANNOFOSS, V1, P315, DOI [10.1007/978-94-011-4902-0, DOI 10.1007/978-94-011-4902-0]; Broecker W.S., 1982, TRACERS SEA; BURKE WH, 1982, GEOLOGY, V10, P516, DOI 10.1130/0091-7613(1982)10<516:VOSSTP>2.0.CO;2; Christie-Blick N., 1990, NATL RES COUNCIL STU, P116; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Dybkjær K, 2008, GEOL SURV DEN GREENL, P29; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; Embry A., 2009, Practical Sequence Stratigraphy; Gradstein F., 2004, A Geological Time Scale; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P1; Greenlee S.M., 1988, SEA LEVEL CHANGESAN, P329, DOI DOI 10.2110/PEC.88.01.0329; GREENLEE SM, 1992, GEOL SOC AM BULL, V104, P1403, DOI 10.1130/0016-7606(1992)104<1403:ISSOND>2.3.CO;2; HART SR, 1974, GEOCHIM COSMOCHIM AC, V38, P1799, DOI 10.1016/0016-7037(74)90163-X; HATHAWAY JC, 1979, SCIENCE, V206, P515, DOI 10.1126/science.206.4418.515; HODELL DA, 1990, CHEM GEOL, V80, P291, DOI 10.1016/0168-9622(90)90011-Z; Holbourn A, 2007, EARTH PLANET SC LETT, V261, P534, DOI 10.1016/j.epsl.2007.07.026; Karakaya S., 2012, THESIS RUTGERS U NEW; Katz ME, 2013, GEOSPHERE, V9, P1488, DOI 10.1130/GES00872.1; KENNETT JP, 1986, INITIAL REP DEEP SEA, V90, P1383, DOI 10.2973/dsdp.proc.90.1986; Kominz MA, 2008, BASIN RES, V20, P211, DOI 10.1111/j.1365-2117.2008.00354.x; Lear CH, 2010, PALEOCEANOGRAPHY, V25, DOI 10.1029/2009PA001880; Martini E., 1971, Proceeding of the 2nd International Conference of Planktonic Microfossils in Roma, P739, DOI DOI 10.1002/IROH.19720570511; McArthur JM, 2001, J GEOL, V109, P155, DOI 10.1086/319243; McCarthy FMG, 2013, GEOSPHERE, V9, P1457, DOI 10.1130/GES00853.1; Miller K.G., 2003, Proceedings of the Ocean Drilling Program, Initial reports, V174AX, P1; Miller KG, 2013, GEOSPHERE, V9, P1236, DOI 10.1130/GES00884.1; Miller KG, 2013, GEOSPHERE, V9, P1257, DOI 10.1130/GES00858.1; Miller KG, 2013, GEOSPHERE, V9, P74, DOI 10.1130/GES00795.1; Miller Kenneth G., 1997, Proceedings of the Ocean Drilling Program Scientific Results, V150X, P169; Miller KG, 1991, PALEOCEANOGRAPHY, V6, P33, DOI 10.1029/90PA01941; Miller KG, 1998, REV GEOPHYS, V36, P569, DOI 10.1029/98RG01624; Miller KG, 1996, SCIENCE, V271, P1092, DOI 10.1126/science.271.5252.1092; Miller KG, 2005, SCIENCE, V310, P1293, DOI 10.1126/science.1116412; MILLER KG, 1991, J GEOPHYS RES-SOLID, V96, P6829, DOI 10.1029/90JB02015; MILLER KG, 1985, GEOLOGY, V13, P257, DOI 10.1130/0091-7613(1985)13<257:OBMAIS>2.0.CO;2; Monteverde D.H., 2008, THESIS RUTGERS U NEW; Monteverde DH, 2008, BASIN RES, V20, P249, DOI 10.1111/j.1365-2117.2008.00351.x; Mountain G., 2010, P INTEGRATED OCEAN D, DOI [10.2204/iodp.proc.313.102.2010, DOI 10.2204/I0DP.PR0C.313.102.2010]; Mountain G., 2010, P INTEGRATED OCEAN D, DOI [10.2204/iodp.proc.313.103.2010, DOI 10.2204/I0DP.PR0C.313.103.2010]; Mountain G., 2010, P INTEGRATED OCEAN D, DOI [10.2204/iodp.proc.313.105.2010, DOI 10.2204/I0DP.PR0C.313.105.2010]; Mountain G., 2010, P INTEGRATED OCEAN D, DOI [10.2204/iodp.proc.313.104.2010, DOI 10.2204/I0DP.PR0C.313.104.2010]; Mountain G., 2012, AM GEOPH UN FALL M; Mountain G. 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J	McCarthy, FMG; Katz, ME; Kotthoff, U; Browning, JV; Miller, KG; Zanatta, R; Williams, RH; Drljepan, M; Hesselbo, SP; Bjerrum, CJ; Mountain, GS				McCarthy, Francine M. G.; Katz, Miriam E.; Kotthoff, Ulrich; Browning, James V.; Miller, Kenneth G.; Zanatta, Ryan; Williams, Ross H.; Drljepan, Matea; Hesselbo, Stephen P.; Bjerrum, Christian J.; Mountain, Gregory S.			Sea-level control of New Jersey margin architecture: Palynological evidence from Integrated Ocean Drilling Program Expedition 313	GEOSPHERE			English	Article							WALLED DINOFLAGELLATE CYSTS; POLLEN TRANSPORT; ORGANIC-MATTER; LATE PLIOCENE; PRESERVATION; ATLANTIC; MIOCENE; STRATIGRAPHY; SEDIMENTS; RECORD	Integrated Ocean Drilling Program Expedition 313 recovered Miocene sequences at Holes M0027A and M0029A on the New Jersey shallow shelf that contain a characteristic acid-resistant organic component. The palynofacies within each sequence reflects variations in terrigenous versus authigenic flux through the Miocene that are associated with sea-level change. Very high ratios of terrigenous versus marine palynomorphs and of oxidation- resistant versus susceptible dinocysts are associated with seismic sequence boundaries, consistent with their interpretation as sequence-bounding unconformities generated at times of low sea level. Comparison of palynological distance from shoreline estimates with paleodepth estimates derived from foraminiferal data allows relative sea level to be reconstructed at both sites. Ages assigned using dinocyst bio-stratigraphy are consistent with other chronostratigraphic indicators allowing sequence boundaries to be correlated with Miocene oxygen isotope (Mi) events. Paleoclimatic evidence from the pollen record supports the global climate changes seen in the oxygen isotope data. Although chronological control is relatively crude, Milankovitch- scale periodicity is suggested for parasequences visible in thick sequences deposited in relatively deep water where substantial accommodation existed, such as during the early Langhian at Site 29 (Middle Miocene Climatic Optimum). Palynological analysis thus supports the long-held hypothesis that glacioeustasy is a dominant process controlling the architecture of continental margins.	[McCarthy, Francine M. G.; Zanatta, Ryan; Drljepan, Matea] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Katz, Miriam E.; Williams, Ross H.] Rensselaer Polytech Inst, Dept Earth & Environm Sci, Troy, NY 12180 USA; [Kotthoff, Ulrich] Univ Hamburg, Inst Geol, D-20146 Hamburg, Germany; [Browning, James V.; Miller, Kenneth G.; Mountain, Gregory S.] Rutgers State Univ, Dept Earth & Planetary Sci, Piscataway, NJ 08854 USA; [Hesselbo, Stephen P.] Univ Exeter, Coll Engn Math & Phys Sci, Camborne Sch Mines, Penryn TR10 9EZ, Cornwall, England; [Bjerrum, Christian J.] NordCEE, DK-1350 Copenhagen K, Denmark; [Bjerrum, Christian J.] Dept Geosci & Nat Resource Management, DK-1350 Copenhagen K, Denmark	Brock University; Rensselaer Polytechnic Institute; University of Hamburg; Rutgers University System; Rutgers University New Brunswick; University of Exeter	McCarthy, FMG (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.		Miller, Kenneth/LZE-2268-2025; Bjerrum, Christian Jannik/A-4247-2015	Bjerrum, Christian Jannik/0000-0002-7804-1633; Hesselbo, Stephen/0000-0001-6178-5401; Williams, Ross/0000-0002-8843-5257	Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant; NSERC Undergraduate Student Research Awards; U.S. Science Support Program and National Science Foundation awards; German Science Foundation (DFG) [KO 3944/3-1]; NERC [NE/E007511/1, NE/F001428/1] Funding Source: UKRI	Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); NSERC Undergraduate Student Research Awards(Natural Sciences and Engineering Research Council of Canada (NSERC)); U.S. Science Support Program and National Science Foundation awards; German Science Foundation (DFG)(German Research Foundation (DFG)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We acknowledge the input of the entire Integrated Ocean Drilling Program (IODP) Expedition 313 Scientific Party and the IODP staff in Bremen, and current and former students and colleagues in the Palynology Lab at Brock University: E. Fischer, S. Tiffin, J. Hopkins, K. Gostlin, M. Mahdavi, M. Head, and K. Sihra. Mike Lozon provided invaluable assistance with drafting. This research used samples and/or data provided by the IODP and the International Continental Scientific Drilling Program (ICDP). Funding for this research was provided by a Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant to McCarthy, NSERC Undergraduate Student Research Awards to Zanatta and Drljepan, U.S. Science Support Program and National Science Foundation awards (Browning, Katz, Miller, and Mountain), and by the German Science Foundation (DFG project KO 3944/3-1 to Kotthoff). We thank two anonymous reviewers and editor Carol Frost for their helpful comments on an earlier draft of our paper, and especially guest editor Jean-Noel Proust, who meticulously edited the revised draft of this paper.	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J	Persson, A; Smith, BC; Morton, S; Shuler, A; Wikfors, GH				Persson, Agneta; Smith, Barry C.; Morton, Steve; Shuler, Andrew; Wikfors, Gary H.			Sexual life stages and temperature dependent morphological changes allow cryptic occurrence of the Florida red tide dinoflagellate <i>Karenia brevis</i>	HARMFUL ALGAE			English	Article						Behavior; Bloom; Cryptic; Cyst; Dinoflagellate; Gamete; Karenia brevis; Mating; Morphology; Zygote	GYMNODINIUM-BREVE; CELL-CYCLE; MOLECULAR-DETECTION; DINOPHYCEAE; CYSTS; GULF; TAKAYAMA; BLOOMS; MICROCERATIUM; ASTERODINIUM	Karenia brevis, the Florida red tide dinoflagellate, has been studied extensively, but very little attention has been paid to its sexual life cycle. We found that the life cycle of K. brevis is heterothallic, most probably not resting cyst-producing, but with life stages of different morphology. The isogamous gametes were slightly smaller than vegetative cells and not as broad and flat. The late zygote was yellow-brown in appearance with a thicker wall and more rounded shape lacking carina. Pellicle cysts of these zygotes closely resembled the few earlier descriptions of "possible cysts" of the species. In addition, temperature-dependent, morphological changes and pellicle-cyst formation were observed. Cells placed in the cold (15 degrees C) formed spherical, thin-walled pellicle cysts that germinated into cells that were round in cross-section and longer than wide - so morphologically different from vegetative cells that they would not be correctly identified if encountered in field samples. Cells grown at 25 degrees C were wider and flatter than cells grown at 20 degrees C. Cells warmed from cold conditions became flat and wide within hours, returning to the typical shape. Also the morphological differences between sexual life stages were large enough to allow misidentification and cryptic occurrence of K. brevis. The cell shape of K. brevis was not fixed, but could vary from very wide and flat to elongate with rounded cross-section in the same culture of clonal cells and in the same cells within a short time (hours). In addition to the culture studies, sediment samples from a Karenia "hot spot" area were concentrated, and the dinoflagellate cyst fraction was investigated for resting cysts. Cysts were not found, and Karenia cells did not germinate from slurry cultures of the concentrated cyst fraction. (C) 2013 Elsevier B.V. All rights reserved.	[Persson, Agneta] Univ Gothenburg, Dept Biol & Environm Sci, SE-40530 Gothenburg, Sweden; [Smith, Barry C.; Wikfors, Gary H.] Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, Milford, CT USA; [Morton, Steve; Shuler, Andrew] NOAA NOS Ctr Coastal Environm Hlth & Biomol Res, Charleston, SC USA	University of Gothenburg; National Oceanic Atmospheric Admin (NOAA) - USA; National Oceanic Atmospheric Admin (NOAA) - USA	Persson, A (通讯作者)，Smedjebacksvagen 13, SE-77190 Ludvika, Sweden.	agnetapersson77@gmail.com		Persson, Agneta/0000-0003-0202-6514	Magnus Bergvall Foundation	Magnus Bergvall Foundation	We are very grateful to Dr. Aswani Volety at Florida Gulf Coast University, Fort Meyers, Florida, for providing us with sediment samples, to Jennifer Alix for assistance in Milford and to an anonymous reviewer for valuable comments on the manuscript. The research was partly funded by a travel grant from the Magnus Bergvall Foundation to Dr. Agneta Persson.[SS]	Anderson D, 2005, DEEP-SEA RES PT II, V52, P2365, DOI 10.1016/j.dsr2.2005.08.001; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Brand LE, 2007, HARMFUL ALGAE, V6, P232, DOI 10.1016/j.hal.2006.08.005; Brand LE, 2012, HARMFUL ALGAE, V14, P156, DOI 10.1016/j.hal.2011.10.020; Bricelj VM, 2012, HARMFUL ALGAE, V16, P27, DOI 10.1016/j.hal.2012.01.001; BRICHEUX G, 1992, PROTOPLASMA, V168, P159, DOI 10.1007/BF01666262; Bronk DA., 2004, HARMFUL ALGAE 2002 F, P80; BROWN DL, 1988, CELL MOTIL CYTOSKEL, V9, P361, DOI 10.1002/cm.970090408; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Cremer H, 2007, CARIBB J SCI, V43, P23; Dale B., 1983, P69; DAVIS CC, 1948, BOT GAZ, V109, P358, DOI 10.1086/335488; De Salas MF, 2005, NEW ZEAL J MAR FRESH, V39, P135, DOI 10.1080/00288330.2005.9517296; de Salas MF, 2003, J PHYCOL, V39, P1233, DOI 10.1111/j.0022-3646.2003.03-019.x; 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Tomlinson MC, 2004, REMOTE SENS ENVIRON, V91, P293, DOI 10.1016/j.rse.2004.02.014; Van Dolah FM, 1999, J PHYCOL, V35, P1404, DOI 10.1046/j.1529-8817.1999.3561404.x; Van Dolah FM, 2008, CONT SHELF RES, V28, P11, DOI 10.1016/j.csr.2007.01.030; Van Dolah FM, 2009, HARMFUL ALGAE, V8, P562, DOI 10.1016/j.hal.2008.11.004; Vargo GA, 2009, HARMFUL ALGAE, V8, P573, DOI 10.1016/j.hal.2008.11.002; Vásquez-Bedoya LF, 2008, MAR MICROPALEONTOL, V68, P49, DOI 10.1016/j.marmicro.2008.03.002; WALKER LM, 1982, T AM MICROSC SOC, V101, P287, DOI 10.2307/3225818; Walsh JJ, 2001, J GEOPHYS RES-OCEANS, V106, P11597, DOI 10.1029/1999JC000123; Watkins SM, 2008, MAR DRUGS, V6, P431, DOI 10.3390/md20080021; WILSON WB, 1967, CONTRIB MAR SCI, V12, P120; Zingone A, 2006, HARMFUL ALGAE, V5, P321, DOI 10.1016/j.hal.2005.09.002	70	22	23	1	35	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	DEC	2013	30						1	9		10.1016/j.hal.2013.08.004	http://dx.doi.org/10.1016/j.hal.2013.08.004			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	267LH					2025-03-11	WOS:000328098700001
J	Srivastava, J; Farooqui, A; Hussain, SM				Srivastava, Jyoti; Farooqui, Anjum; Hussain, Shaik M.			Climate-induced Late-Holocene ecological changes in Pichavaram estuary, India	MARINE ECOLOGY-AN EVOLUTIONARY PERSPECTIVE			English	Article						Climate; Late Holocene; Pichavaram; salinity; thecamoebians	ARCELLACEANS THECAMOEBIANS; NOVA-SCOTIA; SMALL LAKES; SEA-LEVEL	Variation in sedimentology as well as freshwater and marine palynomorphs has been studied in ecological perspective in two 2.5- and 5-m deep sediment cores deposited since 3440 and 3630cal BP, respectively in the central part of Pichavaram mangrove wetland, Cauvery River delta. The palynological and sedimentological results of the sediments reveal a monsoonal circulation and a climatic shift from warm and humid with strengthened monsoon (3630-3190cal BP) to dry and arid (similar to 2750-760cal BP). Since the last millennium (similar to 760cal BP), Pichavaram estuary has been influenced by a similar cyclicity but with a less wet and humid climate due to weakened monsoon conditions. These ecological changes in turn affect the relative sea level rise and fall which is reflected by the variability/extinction of freshwater and marine palynomorphs. The estuary remained an active water channel between similar to 3630 and 2750cal BP, responding to the strengthened monsoon, during which the freshwater algal remains with thecamoebians and marine dinoflagellate cysts and foraminiferal linings both dominated with a ratio of 1.5 for marine/freshwater forms. After this period, since similar to 2750cal BP there has been a dominance of marine forms with a ratio of 4.5 for marine/freshwater forms, indicating fluvio-marine sediment deposition and suggesting the recent landward intrusion of seawater during weakened monsoon conditions. Freshwater thecamoebians are vulnerable to the salinity >3 in the aqueous soil solution of estuarine sediment, and therefore serve as an excellent proxy for monitoring salinity gradient along with short-term high resolution palaeoecological fluctuations induced by climate and relative sea-level changes in an estuarine ecosystem.	[Srivastava, Jyoti; Farooqui, Anjum] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India; [Hussain, Shaik M.] Univ Madras, Madras, Tamil Nadu, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); University of Madras	Srivastava, J (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	caprice2628@yahoo.com	Srivastava, Jyoti/AAB-1612-2020	Srivastava, Jyoti/0000-0002-5264-7995	Department of Science and Technology, New Delhi [SR/S4/ES-264/2007]	Department of Science and Technology, New Delhi(Department of Science & Technology (India))	The authors are grateful to Director BSIP for granting permission and providing necessary facilities to accomplish this work. J.S. thanks the Department of Science and Technology, New Delhi for providing financial support as Junior Research Fellowship in a DST sponsored Project No. SR/S4/ES-264/2007.	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H., 2004, COLOR NOTATION ILLUS, P74; Ogden CG., 1980, ATLAS FRESHWATER TES, P222; Overpeck J, 1996, CLIM DYNAM, V12, P213, DOI 10.1007/BF00211619; PATTERSON RT, 1985, J FORAMIN RES, V15, P114, DOI 10.2113/gsjfr.15.2.114; Patterson RT, 2002, PALAEOGEOGR PALAEOCL, V180, P225, DOI 10.1016/S0031-0182(01)00430-8; Ramanathan AL, 1997, INDIAN J MAR SCI, V26, P319; Roe HM, 2006, J FORAMIN RES, V36, P116, DOI 10.2113/36.2.116; Round F.E., 1965, BIOL OFTHE ALGAE, P269; SELVARAJ K., 2008, CLIMATE OF THE PAST, V4, P929, DOI DOI 10.5194/CPD-4-929-2008; SINGH G, 1974, PHILOS T ROY SOC B, V267, P467, DOI 10.1098/rstb.1974.0006; Sparks D., 1995, Environmental soil chemistry, P267; USDA, 1992, 42 USDA; Vishnu-Mittre Sharma C., 1975, PALEOBOTANIST, V22, P118	30	7	9	0	16	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0173-9565	1439-0485		MAR ECOL-EVOL PERSP	Mar. Ecol.-Evol. Persp.	DEC	2013	34	4					474	483		10.1111/maec.12048	http://dx.doi.org/10.1111/maec.12048			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	255PB					2025-03-11	WOS:000327251200009
J	Riding, JB				Riding, James B.			The literature on Triassic, Jurassic and earliest Cretaceous dinoflagellate cysts: supplement 1	PALYNOLOGY			English	Article						dinoflagellate cysts; Triassic; Jurassic; earliest Cretaceous; literature compilation	RAYNAUD 1978 LENTIN; OFFSHORE; SEQUENCE; AGE	Since the publication of a major literature compilation issued in mid 2012, 94 further contributions on Triassic, Jurassic and earliest Cretaceous (Berriasian) dinoflagellate cysts have been discovered, or were issued recently (i.e. during late 2012 and early 2013). These studies are mostly on the Late Jurassic and Early Cretaceous of Europe, and are listed herein with a description of each item as a string of keywords.	British Geol Survey, Ctr Environm Sci, 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, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk			NERC [bgs05002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Arkadiev V. V., 2012, BERRIASIAN STAGE MOU; Barski M, 2012, GEOL Q, V56, P391, DOI 10.7306/gq.1030; Chen Y-Y, 2013, PALYNOLOGY IN PRESS; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; Jell P A, 1987, MEM ASS AUSTR PALAEO, V4, P341; Mantle DJ, 2012, REV PALAEOBOT PALYNO, V180, P41, DOI 10.1016/j.revpalbo.2012.03.005; Munsterman DK, 2012, NETH J GEOSCI, V91, P555; Riding, 2012, AM ASS STRATIGRAPHIC, V46; Riding JB, 2013, REV PALAEOBOT PALYNO, V196, P51, DOI 10.1016/j.revpalbo.2013.01.010; Riding JB, 2013, PALAEOGEOGR PALAEOCL, V374, P16, DOI 10.1016/j.palaeo.2012.10.019; Riding JB, 2012, REV PALAEOBOT PALYNO, V176, P68, DOI 10.1016/j.revpalbo.2012.02.008; RILEY LA, 1984, INITIAL REP DEEP SEA, V77, P675; Schnyder J, 2012, GEOBIOS-LYON, V45, P485, DOI 10.1016/j.geobios.2012.01.003; Srivastava SK, 2011, PALAEONTOGR ABT B, V285, P113, DOI 10.1127/palb/285/2011/113; van de Schootbrugge B, 2013, PALAEONTOLOGY, V56, P685, DOI 10.1111/pala.12034; Weston JF, 2012, CAN J EARTH SCI, V49, P1417, DOI 10.1139/e2012-070	16	7	7	1	3	TAYLOR & FRANCIS INC	PHILADELPHIA	325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	DEC 1	2013	37	2					345	354		10.1080/01916122.2013.797256	http://dx.doi.org/10.1080/01916122.2013.797256			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	265JG		Green Accepted			2025-03-11	WOS:000327946600012
J	Vajda, V; Lyson, TR; Bercovici, A; Doman, JH; Pearson, DA				Vajda, Vivi; Lyson, Tyler R.; Bercovici, Antoine; Doman, Jessamy H.; Pearson, Dean A.			A snapshot into the terrestrial ecosystem of an exceptionally well-preserved dinosaur (Hadrosauridae) from the Upper Cretaceous of North Dakota, USA	CRETACEOUS RESEARCH			English	Article						Hell Creek; Maastrichtian; Paleoclimate; Palynology; Hadrosaur; Dinosaur; Swamp	HELL CREEK FORMATION; HORSESHOE CANYON FORMATION; TERTIARY BOUNDARY; SOUTHERN ALBERTA; SOFT-TISSUE; SEED FERNS; RECORD; PALYNOSTRATIGRAPHY; STRATIGRAPHY; EVENT	A palynological investigation of sedimentary rocks enclosing an exceptionally well-preserved fossil dinosaur (Hadrosauridae) discovered in the upper part of the Hell Creek Formation in south western North Dakota was conducted in order to document the immediate paleoenvironment of this dinosaur. The specimen, an Edmontosaurus annectens is remarkable in having exceptional three-dimensional preservation of soft tissue around the skeleton, indicating rapid burial. A well-preserved palynological assemblage dominated by fern and bryophyte spores, with lesser gymnosperm and angiosperm pollen was recovered. Sparse fresh-water algae and marine dinoflagellate cysts were also recorded. The palynofacies is dominated by wood fragments, including charcoal, with little amorphous organic matter. The presence of some typical pollen taxa of the Wodehouseia spinata Assemblage Zone including Striatellipollis striatellus, Tricolpites microreticulatus, Leptopecopites pocockii as well as a diverse suite of Aquilapollenites, is fully consistent with a Late Cretaceous (late Maastrichtian) age. The palynoflora indicates a local vegetation composed of a canopy of conifers dominated by Pinaceae and a minor sub-canopy of Taxodium and cycads, as well as an understory of hydrophilous ferns, mosses and herbaceous angiosperms, indicative of a warm and humid climate - an environment where this specific hadrosaur roamed over 66 million years ago. (C) 2013 Elsevier Ltd. All rights reserved.	[Vajda, Vivi; Bercovici, Antoine] Lund Univ, Dept Geol, SE-22362 Lund, Sweden; [Lyson, Tyler R.] Natl Museum Nat Hist, Smithsonian Inst, Dept Vertebrate Zool, Washington, DC 20013 USA; [Lyson, Tyler R.] Marmarth Res Fdn, Marmarth, ND 58643 USA; [Doman, Jessamy H.] Yale Univ, Dept Anthropol, New Haven, CT 06511 USA; [Pearson, Dean A.] Pioneer Trails Reg Museum, Dept Paleontol, Bowman, ND 58623 USA	Lund University; Smithsonian Institution; Smithsonian National Museum of Natural History; Yale University	Vajda, V (通讯作者)，Lund Univ, Dept Geol, Solvegatan 12, SE-22362 Lund, Sweden.	vivi.vajda@geol.lu.se	Vajda, Vivi/N-7693-2018	Vajda, Vivi/0000-0003-2987-5559; Doman, Jessamy/0000-0002-5040-3348	Knut and Alice Wallenberg Foundation; Swedish Research Council; Smithsonian Institution Peter Buck Postdoctoral Fellowship; Swedish Research Council (VR) [2011-7176]	Knut and Alice Wallenberg Foundation(Knut & Alice Wallenberg Foundation); Swedish Research Council(Swedish Research Council); Smithsonian Institution Peter Buck Postdoctoral Fellowship; Swedish Research Council (VR)(Swedish Research Council)	We thank landowners M. and J. Sonsalla for donating the material to the Marmarth Research Foundation. This material is based on work supported by the Royal Swedish Academy of Sciences Research Fellow funded through the Knut and Alice Wallenberg Foundation (to V.Vajda), the Swedish Research Council through Linnaeus grant (LUCCI) to V. Vajda and A. Bercovici. T.R. Lyson was supported by a Smithsonian Institution Peter Buck Postdoctoral Fellowship. A. Bercovici is supported through the Swedish Research Council (VR) postdoctoral fellowship grant 2011-7176. Two anonymous reviewers are thanked for constructive criticism that greatlyimproved this paper. Russ Harms, Global Geolab Ltd. is thanked for palynological processing.	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J	dos Santos, AD; Helenes, J; Carvalho, MD				dos Santos, Alessandra da Silva; Helenes, Javier; Carvalho, Marcelo de Araujo			Palynofacies evidence of dysoxia and upwelling in the Turonian of the Sergipe Basin, Brazil	CRETACEOUS RESEARCH			English	Review						Sergipe Basin; Turonian; Palynofacies; Dinocysts assemblages; Dysoxia; Upwelling; Brazil	DINOFLAGELLATE CYST ASSEMBLAGES; SEA-LEVEL CHANGES; PALEOENVIRONMENTAL ANALYSIS; SEQUENCE STRATIGRAPHY; PRIMARY PRODUCTIVITY; VOCONTIAN BASIN; ANOXIC EVENTS; SEDIMENTS; OXYGEN	This paper presents the integrated results of palynofacies and geochemical analyses in Turonian carbonate strata from the Sergipe Basin, Brazil. Forty-three outcrop samples were analyzed from sections of the Cotinguiba Formation in the Votorantim and Rita Cacete quarries. Our results allow for the characterization of the organic matter and interpretation of the environments of deposition. Together with the existing geochemical data, the results allow for recognition of oxic and dysoxic intervals and inferences pertaining to local oceanographic conditions to explain these environmental changes. The palynofacies groups are dominated by marine palynomorphs and amorphous organic matter (AOM), with minor amounts of terrigenous palynomorphs and phytoclasts. The total organic carbon (TOC) and delta C-13 ratio are directly correlated with the dominant palynofacies elements, particularly AOM. The upper section in Rita Cacete quarry has the most complete data set, and the TOC, delta C-13 and marine-derived AOM in this section tend to decrease upsection and serve to differentiate the oxic and dysoxic intervals. The sections also contain abundant, low-diversity dinoflagellate assemblages composed primarily of Trichodinium boltenhagenii, Cribroperidinium? muderongense, Canningia reticulata and Xenascus plotei. The palynofacies and dinoflagellate assemblages indicate deposition in shallow marine to outer neritic environments. The dysoxic events are recognized by an increase in TOC and delta C-13, high amounts of AOM, an abundance of the low-diversity dinoflagellate assemblages and the lowest amounts of terrestrial components. The changes in marine productivity seem to be related to periods of low-intensity upwelling, which likely decreased the levels of dissolved oxygen in the basin. (C) 2013 Elsevier Ltd. All rights reserved.	[dos Santos, Alessandra da Silva] Univ Vale Rio dos Sinos, Inst Tecnol Micropaleontol ITT FOS SIL, BR-93022000 Sao Leopoldo, RS, Brazil; [dos Santos, Alessandra da Silva] Univ Fed Rio de Janeiro, Programa Posgrad, Inst Geociencias, Ilha Fundao, BR-21949900 Rio De Janeiro, Brazil; [Helenes, Javier] CICESE, Dept Geol, Mexicali 22860, Baja California, Mexico; [Carvalho, Marcelo de Araujo] Museu Nacl, Lab Paleoecol Vegetal, Dept Geol & Paleontol, BR-22040040 Rio De Janeiro, Brazil	Universidade do Vale do Rio dos Sinos (Unisinos); Universidade Federal do Rio de Janeiro; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	dos Santos, AD (通讯作者)，Univ Vale Rio dos Sinos, Inst Tecnol Micropaleontol ITT FOS SIL, BR-93022000 Sao Leopoldo, RS, Brazil.	alessandrass@unisinos.br	Carvalho, Marcelo/G-8463-2015; Helenes, Javier/J-5033-2016	Helenes, Javier/0000-0002-0135-1879	Federal University of Rio de Janeiro; CAPES [Processo 1762-21-2]	Federal University of Rio de Janeiro; CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	We are grateful to Cecilia Lana for allowing us to use the samples studied here, to the Federal University of Rio de Janeiro and to CAPES for financial support during the doctoral program at UFRJ and the stay at CICESE with the Doctoral Sandwich program (No. Processo 1762-21-2); to ITT FOSSIL/UNISINOS, Sao Leopoldo, Brazil, and to the Geology Department at CICESE, Baja California, Mexico, for allowing the use of their facilities to study the material; and finally to Dr. Juan Flores at CICESE for our discussions of this work. This article is part of a doctoral thesis prepared at the Federal University of Rio de Janeiro (Brazil). Thanks are also owed to Prof. David Batten (University of Manchester, UK) and an anonymous reviewer, and editor-in-chief Eduardo Koutsoukos, who notably improved the original content of the paper.	AbdelKireem MR, 1996, J AFR EARTH SCI, V22, P93, DOI 10.1016/0899-5362(95)00125-5; Al-Ameri TK, 1999, CRETACEOUS RES, V20, P359, DOI 10.1006/cres.1999.0157; Andrade E.J., 2005, THESIS RUPRECHT KARL; [Anonymous], AAPG MEMOIR; ARTHUR MA, 1979, AAPG BULL, V63, P870; Barroso-Barcenilla F, 2011, P GEOLOGIST ASSOC, V122, P67, DOI 10.1016/j.pgeola.2010.11.002; Batten D., 1996, Palynology: principles and applications, P1011; Bengtson P., 1983, Fossil and Strata, V12, P1; Campos Neto O.P. 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Res.	NOV	2013	46						151	165		10.1016/j.cretres.2013.09.005	http://dx.doi.org/10.1016/j.cretres.2013.09.005			15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	287PE					2025-03-11	WOS:000329553900014
J	de Vernal, A; Hillaire-Marcel, C; Rochon, A; Fréchette, B; Henry, M; Solignac, S; Bonnet, S				de Vernal, Anne; Hillaire-Marcel, Claude; Rochon, Andre; Frechette, Bianca; Henry, Maryse; Solignac, Sandrine; Bonnet, Sophie			Dinocyst-based reconstructions of sea ice cover concentration during the Holocene in the Arctic Ocean, the northern North Atlantic Ocean and its adjacent seas	QUATERNARY SCIENCE REVIEWS			English	Article						Sea ice; Dinocysts; Arctic Ocean; Atlantic Ocean; Holocene	LAST GLACIAL MAXIMUM; DINOFLAGELLATE CYST ASSEMBLAGES; SURFACE CONDITIONS; HIGH-LATITUDES; ATMOSPHERIC CIRCULATION; CLIMATE-CHANGE; BEAUFORT SEA; BAFFIN-BAY; QUANTITATIVE RECONSTRUCTION; PALYNOLOGICAL EVIDENCE	Sea ice cover extent expressed in terms of mean annual concentration was reconstructed from the application of the modern analogue technique to dinocyst assemblages. The use of an updated database, which includes 1492 sites and 66 taxa, yields sea ice concentration estimates with an accuracy of +/- 1.1/10. Holocene reconstructions of sea ice cover were made from dinocyst counts in 35 cores of the northern North Atlantic and Arctic seas. In the Canadian Arctic, the results show high sea ice concentration (>7/10) with little variations throughout the interval. In contrast, in Arctic areas such as the Chukchi Sea and the Barents Sea, the reconstructions show large amplitude variations of sea ice cover suggesting millennial type oscillations with a pacing almost opposite in western vs. eastern Arctic. Other records show tenuous changes with some regionalism either in trends or sea ice cover variability. During the mid-Holocene, and notably at 6 +/- 0.5 ka, minimum sea ice concentration is recorded in the eastern Fram Strait, northern Baffin Bay and Labrador Sea. However, this minimum cannot be extrapolated at the scale of the Arctic and circum-Arctic. The comparison of recent observations and reconstructions suggests larger variations in the Arctic sea ice cover during the last decades than throughout the Holocene. (C) 2013 Elsevier Ltd. All rights reserved.	[de Vernal, Anne; Hillaire-Marcel, Claude; Frechette, Bianca; Henry, Maryse; Solignac, Sandrine; Bonnet, Sophie] Univ Quebec, Ctr Rech Geochim & Geodynam Geotop, Montreal, PQ H3C 3P8, Canada; [Rochon, Andre] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada	University of Quebec; University of Quebec Montreal; University of Quebec	de Vernal, A (通讯作者)，Univ Quebec, Ctr Rech Geochim & Geodynam Geotop, POB 8888, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	Hillaire-Marcel, Claude/H-1441-2012; de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/C-9153-2013	Frechette, Bianca/0000-0002-4986-5772; de Vernal, Anne/0000-0001-5656-724X; Hillaire-Marcel, Claude/0000-0002-3733-4632; Solignac, Sandrine/0000-0003-3373-6922	European Union [243908]; Ministere du Developpement economique, de l'innovation et de l'exportation (MDEIE) du Quebec; Fonds de Recherche du Quebec Nature et Technologies (FRQNT); Natural Sciences and Engineering Research Council of Canada (NSERC)	European Union(European Union (EU)); Ministere du Developpement economique, de l'innovation et de l'exportation (MDEIE) du Quebec; 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 project "Past4Future. Climate change - Learning from the past climate" of the European Union's Seventh Framework programme (FP7/2007-2013) under grant agreement no 243908. The Geotop participation to Past4Future has been supported by the Ministere du Developpement economique, de l'innovation et de l'exportation (MDEIE) du Quebec. Additional financial support was provided by the Fonds de Recherche du Quebec Nature et Technologies (FRQNT) and the Natural Sciences and Engineering Research Council of Canada (NSERC) are acknowledged. The manuscript is a contribution of the Sea Ice Proxy (SIP) working group endorsed by PAGES, which provided support for the first workshop at the origin of the present special issue on sea ice in the paleoclimate system. Thanks are due to the anonymous reviewers of the journal, who made constructive and useful comments.	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J	Shumilovskikh, LS; Arz, HW; Wegwerth, A; Fleitmann, D; Marret, F; Nowaczyk, N; Tarasov, P; Behling, H				Shumilovskikh, Lyudmila S.; Arz, Helge W.; Wegwerth, Antje; Fleitmann, Dominik; Marret, Fabienne; Nowaczyk, Norbert; Tarasov, Pavel; Behling, Hermann			Vegetation and environmental changes in Northern Anatolia between 134 and 119 ka recorded in Black Sea sediments	QUATERNARY RESEARCH			English	Article						Pollen; Dinoflagellate cysts; Fagus; Vegetation history; Paleoclimate; Black Sea; Penultimate glacial; MIS 5e; Eemian	LAST CLIMATIC CYCLE; LONG POLLEN RECORD; ATLANTIC; BEECH; FAGUS; RECONSTRUCTION; SURFACE; EUROPE; DIFFERENTIATION; GRADIENT	This multiproxy study on SE Black Sea sediments provides the first detailed reconstruction of vegetation and environmental history of Northern Anatolia between 134 and 119 ka. Here, the glacial-interglacial transition is characterized by several short-lived alternating cold and warm events preceding a meltwater pulse (similar to 130.4-131.7 ka). The latter is reconstructed as a cold arid period correlated to Heinrich event 11. The initial warming is evidenced at similar to 130.4 ka by increased primary productivity in the Black Sea, disappearance of ice-rafted detritus, and spreading of oaks in Anatolia. A Younger Dryas-type event is not identifiable. The Eemian vegetation succession corresponds to the main climatic phases in Europe: i) the Quercus-Juniperus phase (128.7-126.4 ka) indicates a dry continental climate; ii) the Ostrya-Corylus-Quercus-Carpinus phase (126.4-122.9 ka) suggests warm summers, mild winters, and high year-round precipitation; iii) the Fagus-Caipinus phase (122.9-119.5 ka) indicates cooling and high precipitation; and iv) increasing Pinus at similar to 121 ka marks the onset of cooler/drier conditions. Generally, pollen reconstructions suggest altitudinal/latitudinal migrations of vegetation belts in Northern Anatolia during the Eemian caused by increased transport of moisture. The evidence for the wide distribution of Fagus around the Black Sea contrasts with the European records and is likely related to climatic and genetic factors. (C) 2013 University of Washington. Published by Elsevier Inc All rights reserved.	[Shumilovskikh, Lyudmila S.; Behling, Hermann] Univ Gottingen, Dept Palynol & Climate Dynam, D-37073 Gottingen, Germany; [Arz, Helge W.; Wegwerth, Antje] Leibniz Inst Balt Sea Res Warnemunde, D-18119 Rostock, Germany; [Fleitmann, Dominik] Univ Reading, Sch Archaeol Geog & Environm Sci, Dept Archaeol, Reading RG6 6AB, Berks, England; [Fleitmann, Dominik] Univ Bern, Inst Geol Sci, CH-3012 Bern, Switzerland; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Nowaczyk, Norbert] Helmholtz Ctr Potsdam GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany; [Tarasov, Pavel] Free Univ Berlin, Palaeontol Sect, Inst Geol Sci, D-12249 Berlin, Germany; [Fleitmann, Dominik] Univ Bern, Oeschger Ctr Climate Change Res, CH-3012 Bern, Switzerland	University of Gottingen; Leibniz Institut fur Ostseeforschung Warnemunde; University of Reading; University of Bern; University of Liverpool; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; Free University of Berlin; University of Bern	Shumilovskikh, LS (通讯作者)，Univ Gottingen, Albrecht von Haller Inst Plant Sci, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany.	shumilovskikh@yahoo.com	Fleitmann, Domnik/HSF-0516-2023; Shumilovskikh, Lyudmila/P-2493-2015; Tarasov, Pavel/ABG-3993-2020; Arz, Helge/A-6659-2013	/0000-0002-7219-5009; Wegwerth, Antje/0000-0002-5104-9408; Marret-Davies, Fabienne/0000-0003-4244-0437; Fleitmann, Dominik/0000-0001-5977-8835; Arz, Helge Wolfgang/0000-0002-1997-1718	Deutsche Forschungsgemeinschaft (DFG) [BE 2116/20-1, SPP 1266]	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	We warmly thank Mariana Filipova and Eliso Kvavadze for providing publications, Associate Editor Peter Langdon, anonymous reviewers for critical reading and improving the manuscript, and Laura Sutcliffe for polishing the English. Financial support was provided by the Deutsche Forschungsgemeinschaft (DFG) (BE 2116/20-1) within the SPP 1266 "INTERDYNAMIC".	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Res.	NOV	2013	80	3					349	360		10.1016/j.yqres.2013.07.005	http://dx.doi.org/10.1016/j.yqres.2013.07.005			12	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	256BU					2025-03-11	WOS:000327285500001
J	Verleye, TJ; Martinez, P; Robinson, RS; Louwye, S				Verleye, Thomas J.; Martinez, Philippe; Robinson, Rebecca S.; Louwye, Stephen			Changes in the source of nutrients associated with oceanographic dynamics offshore southern Chile (41°S) over the last 25,000 years	QUATERNARY RESEARCH			English	Article						delta N-15; Microfossils; Oceanography; Southeast Pacific; Late Quaternary	PACIFIC HYDROGRAPHIC SECTION; PHYTOPLANKTON GROWTH; CLIMATE VARIABILITY; UPWELLING REGION; GLACIAL MAXIMUM; LATE QUATERNARY; ICE-SHEET; OCEAN; IRON; NITROGEN	In order to obtain a better knowledge of past oceanographic variability offshore southern Chile, this study reappraises the changes in the sources of nutrients over the last 25 ka based on a detailed comparison of previously published nitrogen isotope and microfossil records (dinoflagellate cysts, coccoliths and diatoms) from ODP Site 1233 (41 degrees S). Our findings support the main conclusions of Martinez et al. (2006) in the sense that both the Subantarctic Surface Water and the Gunther Undercurrent are potential sources for the recorded late Quaternary sedimentary delta N-15 signatures at Site 1233, with variable contributions of both sources during different time periods. This study indicates that Subantarctic Surface Water forms the main source for nutrients during the last glacial maximum (25-18.6 cal ka BP), the first part of the deglaciation (18.6-15.7 cal ka BP) and the Holocene (9.8 cal ka BP until present). An increased contribution of Equatorial Subsurface Water as a source of nutrients to the photic zone offshore southern Chile is observed between 14.4 and 9.8 cal ka BP, which is indicative for upwelling conditions at least after 13.2 cal ka BP as indicated by the microfossil data. (C) 2013 University of Washington. Published by Elsevier Inc. All rights reserved.	[Verleye, Thomas J.; Louwye, Stephen] Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Verleye, Thomas J.] Flanders Marine Inst VLIZ, B-8200 Oostende, Belgium; [Martinez, Philippe] Univ Bordeaux 1, UMR EPOC 5805, F-33405 Talence, France; [Robinson, Rebecca S.] Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA	Ghent University; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Rhode Island	Verleye, TJ (通讯作者)，Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, Krijgslaan 281 S8-WE13, B-9000 Ghent, Belgium.	thomas.verleye@vliz.be	; Louwye, Stephen/D-3856-2012	Robinson, Rebecca/0000-0002-8072-1603; Martinez, Philippe/0000-0002-9825-2032; Louwye, Stephen/0000-0003-4814-4313	Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT); NSF	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)); NSF(National Science Foundation (NSF))	Financial support to the first author was provided by the Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT). This research used samples provided by the Ocean Drilling Program (ODP). The ODP is sponsored by NSF and participating countries under management of Joint Oceanographic Institutions (JOI), Inc. The reviewers are kindly acknowledged for their constructive comments and suggestions which considerably improved the manuscript.	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Res.	NOV	2013	80	3					495	501		10.1016/j.yqres.2013.07.002	http://dx.doi.org/10.1016/j.yqres.2013.07.002			7	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	256BU		Green Published			2025-03-11	WOS:000327285500014
J	Wendler, JE; Wendler, I; Huber, BT				Wendler, Jens E.; Wendler, Ines; Huber, Brian T.			REVISION AND EVALUATION OF THE SYSTEMATIC AFFINITY OF THE CALCITARCH GENUS <i>PITHONELLA</i> BASED ON EXQUISITELY PRESERVED TURONIAN MATERIAL FROM TANZANIA	JOURNAL OF PALEONTOLOGY			English	Article							CALCAREOUS DINOFLAGELLATE CYSTS; THORACOSPHAERA-HEIMII DINOPHYCEAE; STABLE OXYGEN; LITHOSTRATIGRAPHY; CHEMOSTRATIGRAPHY; BIOSTRATIGRAPHY; RECONSTRUCTION; PALEOECOLOGY; STRATIGRAPHY; TEMPERATURE	Extraordinarily well-preserved pithonellid microfossils (calcitarchs, "calcispheres") from the Turonian (upper Cretaceous) of Tanzania reveal previously unknown morphological traits, crystallographic patterns, and chemical signatures, providing new insight to this enigmatic group of microfossils. Using combined transmitted-reflected light microscopy, scanning electron microscope imagery, electron microprobe elemental analysis and stable isotope geochemistry, the present study reveals four new aspects of the genus Pithonella, notably, the following. An affinity with cyst-forming organisms, potentially the dinoflagellates, is indicated by the presence of a hatch opening and corresponding operculum. The pristine outer wall architecture consists of thin, smooth shingle-shaped plates with regular rows of slit-shaped pores and an apical sub-angular or circular pore. This primary surface pattern is significantly different from previous descriptions of an outer wall consisting a "parquet-shaped" prismatic crystal rows; this latter surface pattern is formed by secondary overgrowth. The crystallographic pattern of the inner wall is crypto-crystalline. Unaltered pithonellids reveal a calcite chemistry characterized by comparably high Mg-contents, relatively enriched stable carbon isotope values, and stable oxygen values indicating a surface water habitat. Based on these previously unseen traits, the diagnosis of the genus Pithonella is emended. A new species, Pithonella diconica, is described from the lower-middle Turonian sediments of Tanzania.	[Wendler, Jens E.; Wendler, Ines; Huber, Brian T.] NMNH, Smithsonian Inst, Dept Paleobiol, Washington, DC 20013 USA; [Wendler, Jens E.; Wendler, Ines] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	Smithsonian Institution; Smithsonian National Museum of Natural History; University of Bremen	Wendler, JE (通讯作者)，NMNH, Smithsonian Inst, Dept Paleobiol, POB 37012, Washington, DC 20013 USA.	wendler@uni-bremen.de			German Science Foundation [WE 4587/1-1]; National Science Foundation [NSF EAR 0641956]; Smithsonian Institution	German Science Foundation(German Research Foundation (DFG)); National Science Foundation(National Science Foundation (NSF)); Smithsonian Institution(Smithsonian Institution)	This research was funded by the German Science Foundation (grant WE 4587/1-1), National Science Foundation (NSF EAR 0641956) and the Smithsonian Institution's Charles Walcott Fund and Scholarly Studies Program. We thank the Tanzania Petroleum Development Corporation, and particularly Dr. J. Singano, for logistical support and the Tanzania Commission for Science and Technology for permission to drill. J. Wingerath, S. Whittaker, A. Logan, T. Rose (Smithsonian Institution) are acknowledged for technical assistance. KG. MacLeod (University of Missouri) performed stable isotope measurements. M. Kirsch provided culture material and gave perspectives and comparisons with recent dinoflagellates. We acknowledge inspiring discussions with H. Keupp, G. Versteegh, and H. Willems. We thank S. Meier, M. Streng and M. Head for insightful reviews and fruitful communication that strongly improved the manuscript.	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Paleontol.	NOV	2013	87	6					1077	1106		10.1666/12-121	http://dx.doi.org/10.1666/12-121			30	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	257BT					2025-03-11	WOS:000327359000010
J	Mousing, EA; Andersen, TJ; Ellegaard, M				Mousing, Erik Askov; Andersen, Thorbjorn Joest; Ellegaard, Marianne			Changes in the Abundance and Species Composition of Phytoplankton in the Last 150 Years in the Southern Black Sea	ESTUARIES AND COASTS			English	Article						Black Sea; Paleoecology; Eutrophication; Diatoms; Dinoflagellate cysts	COASTAL WATERS; CHLOROPHYLL-A; EUTROPHICATION; SIZE; TEMPERATURE; OXIDATION; NUTRIENT; SURFACE	Changes in total abundance and in species composition of phytoplankton in the last 150 years in the southern Black Sea were investigated through a paleoecological study of two sediment cores. The results show changes in the species composition and a marked increase in total abundance of siliceous protists after around 1960. In core 22 (42A degrees 13.534' N/36A degrees 29.555' E), the dominating species before 1960 were Cyclotella choctawhatcheeana and Thalassiosira oestrupii. In core 25 (42A degrees 6.212' N/36A degrees 37.460' E), the dominating species before 1960 were T. oestrupii, Cyclotella meneghiniana, C. choctawhatcheeana, and Pseudosolenia cf. calcar-avis. Core 22 was located in closer proximity to the rim current than core 25, and the differences in total abundance between the cores could be related to differences in local nutrient loading prior to 1960. After around 1960, both cores changed to a community dominated by C. choctawhatcheeana. The changes in total abundance and species composition after around 1960 could be related to the increased nutrient loading from the Danube River into the rim current after the late 1960s. The results also showed changes in both total abundance and in species composition of dinoflagellate cysts. The dominating dinoflagellate cysts recorded were Lingulodinium polyedrum, Polykrikos schwartzii, and Spiniferites spp.	[Mousing, Erik Askov] Univ Copenhagen, Dept Biol, Ctr Macroecol Evolut & Climate, DK-2100 Copenhagen, Denmark; [Ellegaard, Marianne] Univ Copenhagen, Marine Biol Sect, Dept Biol, DK-1353 Copenhagen, Denmark; [Andersen, Thorbjorn Joest] Univ Copenhagen, Dept Geog & Geol, DK-1350 Copenhagen, Denmark	University of Copenhagen; University of Copenhagen; University of Copenhagen	Mousing, EA (通讯作者)，Univ Copenhagen, Dept Biol, Ctr Macroecol Evolut & Climate, Univ Pk 15, DK-2100 Copenhagen, Denmark.	eamousing@bio.ku.dk	Andersen, Thorbjorn Joest/N-7560-2014; Mousing, Erik Askov/C-4371-2015; Ellegaard, Marianne/H-6748-2014	Andersen, Thorbjorn Joest/0000-0001-5032-9945; Mousing, Erik Askov/0000-0003-1663-2507; Ellegaard, Marianne/0000-0002-6032-3376				[Anonymous], 1988, SUSSWASSERFLORA MITT; [Anonymous], 2013, R LANG ENV STAT COMP; [Anonymous], 1991, Bacillariophyceae 4. 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J	Li, JG; Peng, JG; Batten, DJ				Li, Jianguo; Peng, Jungang; Batten, David J.			Palynostratigraphy of a Jurassic-Cretaceous transitional succession in the Himalayan Tethys, southern Xizang (Tibet), China	CRETACEOUS RESEARCH			English	Article						Stratigraphy; Jurassic/Cretaceous boundary; Spores; Pollen; Dinoflagellate cysts; Xizang; Tibet	BOUNDARY; AUSTRALIA; STRATA; BASIN	A palynological analysis of a Late Jurassic-Early Cretaceous succession in the Himalayan Tethys, Gyangze County, southern Xizang (Tibet) provides, for the first time, evidence of changing palynofloras through the Jurassic/Cretaceous (J/K) boundary. Species that are stratigraphically important and potential markers for delineating the boundary include both miospores and dinoflagellate cysts. The presence of the spores Ciybelosporites sp. cf. stylosus, Foraminisporis wonthaggiensis, Jiaohepollis verus and Toroisporis welzowense and the cysts Cassiculosphaeridia delicata and Rhynchodiniopsis serrata imply that the J/K boundary is between samples 06-21-1 and 06-21-3. The occurrence of Aequitriradites spinulosus and Cicatricosisporites spp. a little below this level and of ?Dictyotosporites sp. cf. speciosus slightly above it is also significant. These results show that it is possible to locate the J/K boundary in the Himalayan Tethys near top of the Weimei Formation and the lower part of the Gyabula Formation in southern Xizang. This succession also contains various marine invertebrate fossils, including ammonites, bivalves and belemnites, and thus has considerable potential for erecting an integrated biostratigraphy around the J/K boundary in the eastern Tethyan realm. Palynofloristic correlation implies a more northerly location for the fossil locality at Gyangze than that of northwest Australia during the latest Jurassic and earliest Cretaceous, which can be further constrained to around 43 degrees S. (C) 2013 Elsevier Ltd. All rights reserved.	[Li, Jianguo; Peng, Jungang; Batten, David J.] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China; [Batten, David J.] Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England	Chinese Academy of Sciences; University of Manchester	Li, JG (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China.	jgli@nigpas.ac.cn			Chinese Academy of Sciences [XDB03010103]; National Basic Research Program of China [2012CB822004]; National Natural Science Foundation of China [41172011]; Chinese Academy of Sciences	Chinese Academy of Sciences(Chinese Academy of Sciences); National Basic Research Program of China(National Basic Research Program of China); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Chinese Academy of Sciences(Chinese Academy of Sciences)	This is a contribution to the Berriasian/J-K Boundary Working Group of the Cretaceous Subcommittee under the leadership of Dr William A.P. Wimbledon who we thank for constructive discussion during the preparation of the manuscript. We thank Dr Eckart Schrank (Institut fur Angewandte Geowissenschaften, Technische Universitat Berlin) for his helpful review of the manuscript. We are indebted to Miss Feng Limei (NIGPCAS) for technical help in processing the samples. The research is sponsored by the "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences (Grant No. XDB03010103), the National Basic Research Program of China (2012CB822004) and the National Natural Science Foundation of China (Project No. 41172011). DJB was supported by a Chinese Academy of Sciences Visiting Professorship for Senior International Scientists.	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Res.	NOV	2013	46						123	135		10.1016/j.cretres.2013.08.012	http://dx.doi.org/10.1016/j.cretres.2013.08.012			13	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	287PE					2025-03-11	WOS:000329553900012
J	Mertens, KN; Yamaguchi, A; Takano, Y; Pospelova, V; Head, MJ; Radi, T; Pienkowski, AJ; de Vernal, A; Kawami, H; Matsuoka, K				Mertens, Kenneth N.; Yamaguchi, Aika; Takano, Yoshihito; Pospelova, Vera; Head, Martin J.; Radi, Taoufik; Pienkowski, Anna J.; de Vernal, Anne; Kawami, Hisae; Matsuoka, Kazumi			A New Heterotrophic Dinoflagellate from the North-eastern Pacific, <i>Protoperidinium fukuyoi</i>: Cyst-Theca Relationship, Phylogeny, Distribution and Ecology	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						LSU rDNA; round spiny brown cyst; Saanich Inlet; San Pedro Harbor; single-cell PCR; SSU rDNA; Strait of Georgia	SP-NOV DINOPHYCEAE; MINUTUM DINOPHYCEAE; SURFACE SEDIMENTS; SEA; PERIDINIALES; SALINITY; ULTRASTRUCTURE; PRODUCTIVITY; ISLANDINIUM; TEMPERATURE	The cyst-theca relationship of Protoperidinium fukuyoi n. sp. (Dinoflagellata, Protoperidiniaceae) is established by incubating resting cysts from estuarine sediments off southern Vancouver Island, British Columbia, Canada, and San Pedro Harbor, California, USA. The cysts have a brown-coloured wall, and are characterized by a saphopylic archeopyle comprising three apical plates, the apical pore plate and canal plate; and acuminate processes typically arranged in linear clusters. We elucidate the phylogenetic relationship of P. fukuyoi through large and small subunit (LSU and SSU) rDNA sequences, and also report the SSU of the cyst-defined species Islandinium minutum (Harland & Reid) Head etal. 2001. Molecular phylogenetic analysis by SSU rDNA shows that both species are closely related to Protoperidinium americanum (Gran & Braarud 1935) Balech 1974. Large subunit rDNA phylogeny also supports a close relationship between P. fukuyoi and P. americanum. Three subgroups in total are further characterized within the Monovela group. The cyst of P. fukuyoi shows a wide geographical range along the coastal tropical to temperate areas of the North-east Pacific, its distribution reflecting optimal summer sea-surface temperatures of similar to 14-18 degrees C and salinities of 22-34psu.	[Mertens, Kenneth N.] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Yamaguchi, Aika] Okinawa Inst Sci & Technol, Kunigami, Okinawa 9040412, Japan; [Yamaguchi, Aika] Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 6578501, Japan; [Takano, Yoshihito; Kawami, Hisae; Matsuoka, Kazumi] Inst East China Sea Res ECSER, Nagasaki 8528521, Japan; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB A405, Victoria, BC V8W 2Y2, Canada; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Radi, Taoufik; de Vernal, Anne] Univ Quebec & Montreal, Geotop, Montreal, PQ H3C 3P8, Canada; [Pienkowski, Anna J.] Bangor Univ, Sch Ocean Sci, Coll Nat Sci, Menai Bridge LL59 5AB, Anglesey, Wales	Ghent University; Okinawa Institute of Science & Technology Graduate University; Kobe University; University of Victoria; Brock University; University of Quebec; University of Quebec Montreal; Bangor University	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 s8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be	Mertens, Kenneth/AAO-9566-2020; Pieńkowski, Anna/AAL-1312-2020; Mertens, Kenneth/C-3386-2015; Pienkowski, Anna/J-9339-2013; de Vernal, Anne/D-5602-2013	Pospelova, Vera/0000-0003-4049-8133; Mertens, Kenneth/0000-0003-2005-9483; Pienkowski, Anna/0000-0002-3606-7130; de Vernal, Anne/0000-0001-5656-724X	Kakenhi [22-00805]; NSERC [224236]; Ship Time grants; Marie Curie Career Integration Grant	Kakenhi(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Ship Time grants; Marie Curie Career Integration Grant(Marie Curie Actions)	K.N.M. is a postdoctoral fellow of FWO Belgium and this research was partly conducted at Nagasaki University and supported by a Kakenhi grant 22-00805. This research was also partly supported by NSERC Discovery (224236) and Ship Time grants to V. P., an NSERC Discovery Grant to M.J.H., as well as a Marie Curie Career Integration Grant awarded to A.J.P. Carrie Wolfe, Adam Willingham, and Dennis Dunn from the Southern California Marine Institute, are thanked for help with sampling in San Pedro Harbor. Captain Brown and the crew of the marine sciences vessel John Strickland provided valuable assistance during the CM3 sediment core sampling cruise. Andrea Price kindly provided a sample from Brentwood Bay. The VENUS (Victoria Experimental Network Under the Sea) team is thanked for their assistance in collecting of Saanich Inlet and Strait of Georgia surface sediments. Surface sediment samples from the coastal northeastern Pacific were provided by the Scripps Institution of Oceanography (SIO), Oregon State University (OSU), Woods Hole Oceanographic Institution and the U.S. Geological Survey. We are grateful to Robbie Bennett and Bob Murphy (Geological Survey of Canada - Atlantic), and Mark Furze (Grant MacEwan University), as well as the crew of the Canadian Coastguard Vessel Amundsen, for help with sampling in Arctic Canada. V. P. is grateful to Brent Gowen (Electron Microscopy Laboratory, Biology Department, University of Victoria) for assistance with the SEM work. Associate editor Bob Anderson and two anonymous reviewers offered comments that significantly improved the manuscript.	Abe T. H., 1936, Science Reports of the Tohoku University (4), V10, P639; Abe T. H., 1981, PUBLICATIONS SETO MA, V6, P1; ABE TOHRU HIDEMITI, 1927, SCI REPT TOHOKU IMP UNIV 4TH SER BIOL, V2, P383; [Anonymous], 1914, BER DTSCH BOT GES, DOI DOI 10.1111/J.1438-8677.1914.TB07573.X; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Balech E., 1988, Publ. Espec. Inst. Esp. Oceanogr., V1, P1; Bergh R. 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J	Craveiro, SC; Pandeirada, MS; Daugbjerg, N; Moestrup, O; Calado, AJ				Craveiro, Sandra C.; Pandeirada, Mariana S.; Daugbjerg, Niels; Moestrup, Ojvind; Calado, Antonio J.			Ultrastructure and phylogeny of <i>Theleodinium calcisporum</i> gen. et sp nov., a freshwater dinoflagellate that produces calcareous cysts	PHYCOLOGIA			English	Article						Calcareous cyst; Dinophyceae; ITS; LSU rDNA; Microtubular basket; Phylogeny; SSU rDNA; Theleodinium gen. nov.; Ultrastructure	RDNA-BASED PHYLOGENY; MARINE DINOFLAGELLATE; FLAGELLAR APPARATUS; SCRIPPSIELLA-TROCHOIDEA; LIFE-CYCLE; HETEROTROPHIC DINOFLAGELLATE; SEQUENCE DATA; DINOPHYCEAE; THORACOSPHAERACEAE; PERIDINIUM	A freshwater photosynthetic dinoflagellate isolated from a shallow lake near Aveiro, Portugal, was examined by light microscopy, scanning electron microscopy (SEM) and serial-section transmission electron microscopy (TEM), and characterized genetically. Cells were small, spherical to slightly elongated, and had a projecting, nearly cylindrical, apical pore. The chloroplasts were yellowish-brown, arranged near the surface of the cell, and had up to four pyrenoids surrounded by starch sheaths. The cells had a peridinioid plate pattern with Kofoidian plate formula pp, cp, x, 3' (seldom 4'), 2a, 7 '', 6c, 5s (6s?), 5 ''', 2 ''''. A small extruded peduncle was observed by SEM in cells with intact membranes. A microtubular basket, made of about 46 microtubules disposed in four rows, was seen in the ventral area in connection with the cytoplasmic extension that made the peduncle. The flagellar apparatus was typical of a peridinioid with two roots associated with each of the basal bodies and a layered connective linking the proximal ends of roots 1 and 4. In dense cultures, this organism produced a round resting cyst with a thick wall covered by irregular calcified elements. Energy dispersive X-ray analysis (EDS) analysis of the cysts showed calcium as the most abundant element. A total of 3048 nucleotides of the nuclear ribosomal operon were sequenced and used in a phylogenetic analysis that placed this organism as a sister group to a clade of Scrippsiella species and the parasitic Duboscquodinium collinii. Theleodinium calcisporum gen. et sp. nov. is described for the first freshwater dinoflagellate reported to produce calcareous cysts.	[Craveiro, Sandra C.; Pandeirada, Mariana S.; Calado, Antonio J.] Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; [Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, GeoBioTec Res Unit, P-3810193 Aveiro, Portugal; [Daugbjerg, Niels; Moestrup, Ojvind] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-2100 Copenhagen O, Denmark	Universidade de Aveiro; Universidade de Aveiro; University of Copenhagen	Craveiro, SC (通讯作者)，Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal.	scraveiro@ua.pt	Pandeirada, Mariana/AAF-7448-2019; Calado, Sandra Carla/A-6791-2016; Calado, Antonio Jose/D-6263-2015; Pandeirada, Mariana Sofia/E-8803-2015; Daugbjerg, Niels/D-3521-2014	Calado, Sandra Carla/0000-0002-2738-7626; Moestrup, Ojvind/0000-0003-0965-8645; Calado, Antonio Jose/0000-0002-9711-0593; Pandeirada, Mariana Sofia/0000-0001-5061-9029; Daugbjerg, Niels/0000-0002-0397-3073	program "QREN - POPH - Tipologia 4.1 - Formacao Avancada" [SFRH/BPD/68537/2010]; European Social Funding (FSE); Portuguese Ministry of Education and Science (MEC); Fundação para a Ciência e a Tecnologia [SFRH/BPD/68537/2010] Funding Source: FCT	program "QREN - POPH - Tipologia 4.1 - Formacao Avancada"; European Social Funding (FSE)(European Social Fund (ESF)); Portuguese Ministry of Education and Science (MEC); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	SCC was supported by a grant (SFRH/BPD/68537/2010) from the financing program "QREN - POPH - Tipologia 4.1 - Formacao Avancada'' and by the European Social Funding (FSE) and the Portuguese Ministry of Education and Science (MEC).	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J	de Vernal, A; Gersonde, R; Goosse, H; Seidenkrantz, MS; Wolff, EW				de Vernal, Anne; Gersonde, Rainer; Goosse, Hugues; Seidenkrantz, Marit-Solveig; Wolff, Eric W.			Sea ice in the paleoclimate system: the challenge of reconstructing sea ice from proxies - an introduction	QUATERNARY SCIENCE REVIEWS			English	Editorial Material						Sea-ice; Arctic; Antarctic; Diatoms; Dinocysts; Biomarkers; Ostracods; Foraminifers; Ice cores; Polar oceans; Proxies	NORTHERN NORTH-ATLANTIC; DINOFLAGELLATE CYST DISTRIBUTION; LAST GLACIAL MAXIMUM; ARCTIC-OCEAN; MARINE ENVIRONMENTS; SURFACE CONDITIONS; SOUTHERN-OCEAN; VARIABILITY; HISTORY; ASSEMBLAGES	Sea ice is an important component of the Earth system with complex dynamics imperfectly documented from direct observations, which are primarily limited to the last 40 years. Whereas large amplitude variations of sea ice have been recorded, especially in the Arctic, with a strikingly fast decrease in recent years partly attributed to the impact of anthropogenic climate changes, little is known about the natural variability of the sea ice cover at multi-decadal to multi-millennial time scales. Hence, there is a need to establish longer sea ice time series to document the full range of sea ice variations under natural forcings. To do this, several approaches based on biogenic or geochemical proxies have been developed from marine, ice core and coastal records. The status of the sea ice proxies has been discussed by the Sea Ice Proxy (SIP) working group endorsed by PAGES during a first workshop held at GEOTOP in Montreal. The present volume contains a set of papers addressing various sea ice proxies and their application to large scale sea ice reconstruction. Here we summarize the contents of the volume, including a table of various proxies available in marine sediments and ice cores, with their possibilities and limitations. (C) 2013 Elsevier Ltd. All rights reserved.	[de Vernal, Anne] Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada; [Gersonde, Rainer] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Bremerhaven, Germany; [Goosse, Hugues] Univ Catholic Louvain la Neuve, ELIC, TECLIM, Louvain, Belgium; [Seidenkrantz, Marit-Solveig] Aarhus Univ, Ctr Past Climate Studies, Dept Geosci, DK-8000 Aarhus C, Denmark; [Seidenkrantz, Marit-Solveig] Aarhus Univ, Arctic Climate Ctr, DK-8000 Aarhus C, Denmark; [Wolff, Eric W.] Univ Cambridge, Dept Earth Sci, Cambridge CB2 1TN, England; [Wolff, Eric W.] British Antarctic Survey, Cambridge CB3 0ET, England	University of Quebec; University of Quebec Montreal; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Aarhus University; Aarhus University; University of Cambridge; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey	de Vernal, A (通讯作者)，Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	de Vernal, Anne/D-5602-2013; 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Sci. Rev.	NOV 1	2013	79				SI		1	8		10.1016/j.quascirev.2013.08.009	http://dx.doi.org/10.1016/j.quascirev.2013.08.009			8	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	264VU		Green Published			2025-03-11	WOS:000327909900001
J	de Vernal, A; Rochon, A; Fréchette, B; Henry, M; Radi, T; Solignac, S				de Vernal, Anne; Rochon, Andre; Frechette, Bianca; Henry, Maryse; Radi, Taoufik; Solignac, Sandrine			Reconstructing past sea ice cover of the Northern Hemisphere from dinocyst assemblages: status of the approach	QUATERNARY SCIENCE REVIEWS			English	Article						Sea ice cover; Arctic; Subarctic; Palynology; Dinoflagellates; Organic-walled microfossils; Climate; Modern analogue technique	DINOFLAGELLATE CYST ASSEMBLAGES; LAST GLACIAL MAXIMUM; SURFACE CONDITIONS; BEAUFORT SEA; ARCTIC-OCEAN; QUANTITATIVE RECONSTRUCTION; ATMOSPHERIC CIRCULATION; HYDROGRAPHIC CONDITIONS; MARINE ENVIRONMENTS; SOUTHERN-OCEAN	Dinocysts occur in a wide range of environmental conditions, including polar areas. We review here their use for the reconstruction of paleo sea ice cover in such environments. In the Arctic Ocean and subarctic seas characterized by dense sea ice cover, Islandinium minutum, Islandinium? cezare, Echinidinium karaense, Polykrikos sp. var. Arctic, Spiniferites elongatus-frigidus and Impagidinium pallidum are common and often occur with more cosmopolitan taxa such as Operculodinium centrocarpum sensu Wall 81 Dale, cyst of Pentapharsodinium dalei and Brigantedinium spp. Canonical correspondence analyses conducted on dinocyst assemblages illustrate relationships with sea surface parameters such as salinity, temperature, and sea ice cover. The application of the modern analogue technique permits quantitative reconstruction of past sea ice cover, which is expressed in terms of seasonal extent of sea ice cover (months per year with more than 50% of sea ice concentration) or mean annual sea ice concentration (in tenths). The accuracy of reconstructions or root mean square error of prediction (RMSEP) is +/- 1.1 over 10, which corresponds to perennial sea ice. Such an error is close to the interannual variability (standard deviation) of observed sea ice cover. Mismatch between the time interval of instrumental data used as reference (1953-2000) and the time interval represented by dinocyst populations in surface sediment samples, which may cover decades if not centuries, is another source of error. Despite uncertainties, dinocyst assemblages are useful for making quantitative reconstruction of seasonal sea ice cover. (C) 2013 Elsevier Ltd. All rights reserved.	[de Vernal, Anne; Rochon, Andre; Frechette, Bianca; Henry, Maryse; Radi, Taoufik; Solignac, Sandrine] Univ Quebec, Ctr Rech Geochim & Geodynam Geotop, Montreal, PQ H3C 3P8, Canada; [Rochon, Andre] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada	University of Quebec; University of Quebec Montreal; University of Quebec	de Vernal, A (通讯作者)，Univ Quebec, Ctr Rech Geochim & Geodynam Geotop, POB 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	; de Vernal, Anne/D-5602-2013	Solignac, Sandrine/0000-0003-3373-6922; Frechette, Bianca/0000-0002-4986-5772; de Vernal, Anne/0000-0001-5656-724X	European Union [243908]; Ministere du Developpement Economique de l'innovation et de l'exportation (MDEIE) du Quebec; Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT); Natural Sciences and Engineering Research Council of Canada (NSERC)	European Union(European Union (EU)); Ministere du Developpement Economique de l'innovation et de l'exportation (MDEIE) du Quebec; 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 project "Past4Future. Climate change - Learning from the past climate" of the European Union's Seventh Framework programme (FP7/2007-2013) under grant agreement no 243908. The Geotop participation to Past4Future has been supported by the Ministere du Developpement Economique de l'innovation et de l'exportation (MDEIE) du Quebec. 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) is acknowledged. The manuscript is a contribution of the Sea Ice Proxy (SIP) working group endorsed by PAGES, which provided support for the first workshop at the origin of the present special issue on sea ice in the paleoclimate system. Thanks are due to the anonymous reviewers of the Journal, who made constructive and useful comments.	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Sci. Rev.	NOV 1	2013	79				SI		122	134		10.1016/j.quascirev.2013.06.022	http://dx.doi.org/10.1016/j.quascirev.2013.06.022			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	264VU					2025-03-11	WOS:000327909900011
J	Maranda, L; Cox, AM; Campbell, RG; Smith, DC				Maranda, Lucie; Cox, Annie M.; Campbell, Robert G.; Smith, David C.			Chlorine dioxide as a treatment for ballast water to control invasive species: Shipboard testing	MARINE POLLUTION BULLETIN			English	Article						Ballast water; Chlorine dioxide; ClO2; Invasive species; Shipping; Biocide	EURYTEMORA-AFFINIS COPEPODA; VIBRIO-CHOLERAE O1; DINOFLAGELLATE CYSTS; NATURAL-POPULATIONS; DIAPAUSE EGGS; SHIPS; ZOOPLANKTON; SEDIMENTS; EFFICACY; TIME	The efficacy of chlorine dioxide (ClO2) in eliminating organisms present in estuarine ballast water of a containership was determined under actual operating conditions by comparing the survival of planktonic communities present in waters of treated and control ballast tanks. Sampling was via ballast-tank hatches. The treatment (5 mg L-1 ClO2 without pre-filtration) delivered by a prototype ClO2-generating system was generally effective against planktonic assemblages, although bacterial communities rebounded after a few days. Regardless of temperature, ClO2 was very effective against phytoplankton; the effect was immediate, without resurgence. Some zooplankters in the >= 50-mu m fraction may survive the biocide, especially those able to find refuge within a protective coating (e.g., cysts, resting eggs, and shells) or in sediment. In order to boost efficacy, a pre-filtration step is recommended (now installed as standard equipment) to lower the intake of the >= 50-mu m fraction and lessen the challenge posed by this size class. (C) 2013 Elsevier Ltd. All rights reserved.	[Maranda, Lucie; Cox, Annie M.; Campbell, Robert G.; Smith, David C.] Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA	University of Rhode Island	Maranda, L (通讯作者)，Univ Rhode Isl, Grad Sch Oceanog, South Ferry Rd, Narragansett, RI 02882 USA.	lmaranda@mail.uri.edu	Smith, David/A-8309-2013	Smith, David/0000-0003-0627-5788	U.S. National Oceanic and Atmospheric Administration [RA06OAR4170136]; URI Maritime grant; URI Undergraduate/Graduate Research Grant	U.S. National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); URI Maritime grant; URI Undergraduate/Graduate Research Grant	Funding was primarily provided by U.S. National Oceanic and Atmospheric Administration (RA06OAR4170136) for the conduct of the research. Additional support came from Ecochlor, Inc. for maintenance of the ClO<INF>2</INF> distribution system, and from Atlantic Container Line for providing space and lodging to the scientific and technical team. We thank the crew of the Atlantic Compass and numerous students who helped with sampling. J.S. Krumholtz analyzed dissolved organic carbon samples, and R.J. Bell, J.S. Collie and D. A. Bengtson provided inputs with statistical analyses. A.M. Cox received funds from the URI Maritime grant and a URI Undergraduate/Graduate Research Grant. None of the authors had or have a financial relationship with the manufacturer. Comments from anonymous reviewers improved the final version of the manuscript.	Anderson M. 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Pollut. Bull.	OCT 15	2013	75	1-2					76	89		10.1016/j.marpolbul.2013.08.002	http://dx.doi.org/10.1016/j.marpolbul.2013.08.002			14	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	249HL	23987094				2025-03-11	WOS:000326768200022
J	Masure, E; Dejax, J; De Ploëg, G				Masure, Edwige; Dejax, Jean; De Ploeg, Gael			Blowin' in the wind ... 100 Ma old multi-staged dinoflagellate with sexual fusion trapped in amber: Marine-freshwater transition	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Amber; Dinoflagellates; Palaeobiology; Taphonomy; Cretaceous; Phylogeny	ARCHINGEAY CHARENTE-MARITIME; SP-NOV; MIDCRETACEOUS AMBER; CYST FORMATION; DINOPHYCEAE; REPRODUCTION; DIVERSITY; SEDIMENTS; MICROORGANISMS; PALEOECOLOGY	Here we report the unexpected discovery of multi-staged dinoflagellates with organic cellular contents from a paralic habitat trapped in 100 million year (100 Ma) old amber. Amber formed from resin, a fluid medium, that trapped, then remarkably embedded and preserved soft parts of organisms usually destroyed by fossilization processes. We assume that the marine-costal dinoflagellates reached the sticky resin carried away by the wind, inside spray droplets. We answer to a fundamental question dealing with the Peridiniaceae: the paratabulation of Cretaceous cysts reflects the tabulation of Cretaceous thecae. We provide the first life cycle of the fossil record with evidence of cellulosic thecae, sexual fusion and zygote. We highlight an ancestral behaviour for the sexual phase: naked gametes complete fusion outside of gametic thecae, a process known in rare extant Peridinium species. The new taxon, Succiniperidinium inopinatum gen. et sp. nov., belongs to the Peridiniaceae and shares characters with extant marine-brackish Scrippsiella and two freshwater Peridinium clades identified by morphological characters (tabulation, cingular plates, ecdysis, plasmogamy) and molecular phylogenies. Understanding the processes of marine-freshwater transition in microbial lineages is a central goal in evolutionary ecology. Marine dinoflagellates passed through the osmotic barrier and the studies of marine-costal Cretaceous species help to understand the adaptation and the diversification of these species. We discuss the migration according to biological, paleontological and molecular phylogenies data and suggest that the freshwater colonization was the result of Cretaceous species adapted to costal habitats; their lineage isolated in ponds following the Cenozoic global sea-level fall passed through the osmotic barrier. A Scrippsiella-like group (i.e. Subtilisphaera terrula, Palaeoperidinium cretaceum and Succiniperidinium inopinatum gen. et sp. nov.) is suggested as intermediate species in the Peridinium freshwater colonization line. (C) 2013 Elsevier B.V. All rights reserved.	[Masure, Edwige] Univ Paris 06, CNRS, MNHN, CR2P UMR7207, F-75252 Paris 05, France; [Dejax, Jean] Univ Paris 06, CNRS, MNHN, CR2P UMR7207, F-75231 Paris 05, France	Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); Museum National d'Histoire Naturelle (MNHN)	Masure, E (通讯作者)，Univ Paris 06, CNRS, MNHN, CR2P UMR7207, F-75252 Paris 05, France.	edwige.masure@upmc.fr						[Anonymous], CONTRIBUTIONS SERIES; [Anonymous], 1974, OPTICS; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Aké-Castillo JA, 2011, ACTA BOT MEX, V94, P125; Arnaud H., 1877, MEMOIRES SOC GEOLOGI, V2; Bachofen-Echt A., 1949, Der Bernstein und Seine Einschlusse; Balech E., 1963, ZOOLOGIA, V20, P111; Balech E., 1974, NAT HIDROBIOLOGIA, V4, P1; BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; BATTEN D J, 1989, Cretaceous Research, V10, P271, DOI 10.1016/0195-6671(89)90023-2; Batten D.J., 1985, MONATSHEFTE, V7, P427; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; Biecheler B., 1952, B BIOL FRANCE BELG S; Bolch CJS, 1999, J PHYCOL, V35, P356, DOI 10.1046/j.1529-8817.1999.3520356.x; Boltovskoy A., 1979, Limnobios, V1, P325; Boltovskoy A., 1973, Revista Esp Micropaleont, V5, P81; Bourrelly P, 1970, EUGLENIENS PERIDINIE; Brewster David., 1816, PHILOS T ROYAL SOC, P156, DOI [10.1098/rstl.1816.0011, DOI 10.1098/RSTL.1816.0011]; BUJAK JP, 1979, MAR MICROPALEONTOL, V4, P1, DOI 10.1016/0377-8398(79)90002-1; CARTY S, 1989, T AM MICROSC SOC, V108, P64, DOI 10.2307/3226208; Chomerat N, 2008, PHYCOLOGIA, V47, P392, DOI 10.2216/PH07-82.1; Coker E.G., 1931, TREATISE PHOTOELASTI; Coleman CO, 2004, ORG DIVERS EVOL, V4, P119, DOI 10.1016/j.ode.2004.01.003; Conwentz H., 1890, MONOGRAPHIE BALTISCH; Coquand H., 1856, Bulletin de la Societe geologique de France, V14, P55; COX ER, 1976, J PHYCOL, V12, P21; Crie L., 1890, ANN SOC SCI NATURELL, V26, P321; d'Archiac EJAD, 1837, Memoires de la Societe geologique de France, V2, P157; Da P. 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Paleoclimatol. Paleoecol.	OCT 15	2013	388						128	144		10.1016/j.palaeo.2013.08.008	http://dx.doi.org/10.1016/j.palaeo.2013.08.008			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	249JP					2025-03-11	WOS:000326773800012
J	Ahn, S; Peterson, TD; Righter, J; Miles, DM; Tratnyek, PG				Ahn, Samyoung; Peterson, Tawnya D.; Righter, Jason; Miles, Danielle M.; Tratnyek, Paul G.			Disinfection of Ballast Water with Iron Activated Persulfate	ENVIRONMENTAL SCIENCE & TECHNOLOGY			English	Article							TOXIC DINOFLAGELLATE CYSTS; WASTE-WATER; OXIDATION; SHIPS; TRANSPORT; MECHANISM; KINETICS; TRICHLOROETHYLENE; BACILLARIOPHYCEAE; MICROORGANISMS	The treatment of ballast water carried onboard ships is critical to reduce the spread of nonindigenous aquatic organisms that potentially include noxious and harmful taxa. We tested the efficacy of persulfate (peroxydisulfate, S2O82-, PS) activated with zerovalent iron (Fe-0) as a chemical biocide against two taxa of marine phytoplankton grown in bench-scale, batch cultures: the diatom, Pseudonitzshia delicatissima and the green alga, Dunaliella tertiolecta. After testing a range of PS concentrations (0-4 mM activated PS) and exposure times (1-7 days), we determined that a dosage of 4 mM of activated PS was required to inactivate cells from both species, as indicated by reduced or halted growth and a reduction in photosynthetic performance. Longer exposure times were required to fully inactivate D. tertiolecta (7 days) compared to P. delicatissima (5 days). Under these conditions, no recovery was observed upon placing cells from the exposed cultures into fresh media lacking biocide. The results demonstrate that activated PS is an effective chemical biocide against species of marine phytoplankton. The lack of harmful byproducts produced during application makes PS an attractive alternative to other biocides currently in use for ballast water treatments and merits further testing at a larger scale.	[Ahn, Samyoung; Peterson, Tawnya D.; Righter, Jason; Miles, Danielle M.; Tratnyek, Paul G.] Oregon Hlth & Sci Univ, Inst Environm Hlth, Div Environm & Biomol Syst, Portland, OR 97239 USA; [Ahn, Samyoung] Sunchon Natl Univ, Dept Environm Educ, Sunchon 540950, Jeonnam, South Korea	Oregon Health & Science University; Sunchon National University	Peterson, TD (通讯作者)，Oregon Hlth & Sci Univ, Inst Environm Hlth, Div Environm & Biomol Syst, 3181 SW Sam Jackson Pk Rd, Portland, OR 97239 USA.	petersont@ebs.ogi.edu	Tratnyek, Paul/C-8729-2013	Tratnyek, Paul/0000-0001-8818-6417	Sunchon National University; National Science Foundation [OCE-0424602]	Sunchon National University; National Science Foundation(National Science Foundation (NSF))	S.A. gratefully acknowledges funding from the Sunchon National University for the sabbatical year. This work was supported in part through National Science Foundation grant OCE-0424602. The authors thank Philip Block (FMC Corp.) for his helpful input on this manuscript.	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Sci. Technol.	OCT 15	2013	47	20					11717	11725		10.1021/es402508k	http://dx.doi.org/10.1021/es402508k			9	Engineering, Environmental; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology	240UQ	24024829				2025-03-11	WOS:000326123600045
J	Skupien, P; Smarzová, A; Mechová, L				Skupien, Petr; Smarzova, Alexandra; Mechova, Lucie			Palaeoenvironmental change in the Early Cretaceous Silesian Basin of the Western Carpathians (NE Czech Republic) inferred from palynological data	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Outer Western Carpathians; Early Cretaceous; Paleoenvironment; Palynology; dinoflagellate cyst	SEA-LEVEL CHANGES; DINOFLAGELLATE CYSTS; VOCONTIAN BASIN; PALYNOFACIES; UNIT; BIOSTRATIGRAPHY	A Berriasian-lowermost Cenomanian composite stratigraphic section of the Silesian Basin of the Outer Western Carpathians was studied palynologically with an emphasis on quantitative palynomorphs and dinoflagellate cyst distribution. The quantitative composition of the dinoflagellate cyst assemblages reflects a palaeoenvironmental change from inner neritic to outer neritic or oceanic conditions. This change is considered to reflect a relative rise in sea level (according to the 2nd order eustatic curve) and/or tectonic subsidence in the basin. In the lower part (Berriasian to Hauterivian), dinoflagellate cysts characterising a shallow-water environment with variable salinity dominate. The quantitative composition of the dinoflagellate cysts of the latest Hauterivian to early Aptian is characteristic of a deeper shelf environment. In the latest Aptian to Albian, there is already sedimentation in a basinal sedimentary environment (oceanic dinoflagellate cysts are present here as an autochthonous element), with the redeposition of material supplied from littoral to deeper shelf areas. For the composition of palynomorph assemblages, sporomorphs play a more important role in the period from the late Valanginian to the early Aptian. This role is proved by an increased supply of terrestrial material, and it corresponds to a higher amount of black daystones and sandstones. (C) 2013 Elsevier B.V. All rights reserved.	[Skupien, Petr; Smarzova, Alexandra; Mechova, Lucie] 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 the anonymous reviewers and M.H. Stephenson for reading the manuscript, which was significantly improved by their critical remarks. Dr. Terry Needle is acknowledged for his assistance with the improvement of English.	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Palaeobot. Palynology	OCT 15	2013	197						143	151		10.1016/j.revpalbo.2013.06.002	http://dx.doi.org/10.1016/j.revpalbo.2013.06.002			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	217KV					2025-03-11	WOS:000324359300009
J	Leroy, SAG; Tudryn, A; Chalié, F; López-Merino, L; Gasse, F				Leroy, Suzanne A. G.; Tudryn, Alina; Chalie, Francoise; Lopez-Merino, Lourdes; Gasse, Francoise			From the Allerod to the mid-Holocene: palynological evidence from the south basin of the Caspian Sea	QUATERNARY SCIENCE REVIEWS			English	Article						Caspian Sea; Pollen; Dinocysts; Vegetation; Sea level fluctuations; Palaeohydrography; Younger Dryas; Holocene	BLACK-SEA; LEVEL CHANGES; ARAL SEA; DINOFLAGELLATE CYSTS; HOLOCENE VEGETATION; SURFACE CONDITIONS; POLLEN RECORD; LONG-TERM; HISTORY; PLEISTOCENE	Pollen and dinoflagellate cysts have been analysed in a core from the south basin of the Caspian Sea, providing a picture of respectively past vegetation and water salinity for the Late Pleistocene to middle Holocene. A relatively sharp lithological change at 0.86 m depth reflects a shift from detrital silts to carbonates-rich fine silts. From this depth upwards, a Holocene chronology is built based on ten radiocarbon dates on ostracod shells and bulk carbonates. From the vegetation point of view, the Late Pleistocene deserts and steppes were partially replaced in the most sheltered areas by an open woodland with Pinus, Juniperus-Hippophae-Elaeagnus and even Alnus-Quercus-Pterocarya and Fraxinus, related to the Allerod palynozone. This was interrupted by the Younger Dryas palynozone when Artemisia reaches a maximum in a first instance followed by a very dry phase with only a slight return of Pinus and Quercus and the rare presence of Ulmus-Zelkova. From 11.5 to 8.4 cal. ka BP, an open landscape dominated by shrubs such as Ephedra and progressively increasing Quercus appeared. The final spread of diverse evergreen and deciduous trees is delayed and occurs after 8.4 cal. ka BP. It is suggested that this delay is caused by an arid climate in the Early Holocene linked to high insolation and perhaps to a lake effect. The dinocyst assemblages fluctuate between slightly brackish (Pyxidinopsis psilata and Spiniferites cruciformis, 7 psu and lower) and more brackish (Impagidinium caspienense, similar to 13 psu). In the Lateglacial (Khvalynian highstand), the assemblages remained dominated by relative low salinity taxa. A late and brief increase of salinity occurred prior to 11.2 cal. ka BP associated with the Mangyshlak lowstand. It is suggested that it was caused by a brief drop in meltwater flow from both the north and the southeast (Uzboy) and a likely evaporation increase. This lowstand occurs quasi at the same time as the end of a longer lowstand in the Black Sea. The freshest waters are then inferred as having occurred between 8.4 and <= 4.4 cal. ka BP, linked to a connection with the Amu Darya and the melting glaciers on the Pamir Mountains. The Caspian Sea is a sensitive environment, easily perturbed by global climatic changes, such as the Allenod and Holocene warming, and the Lateglacial and Younger Dryas cooling, as well as by regional changes in its hydrography, such as shifts in the Eurasian meltwater and the Volga and Amu Darya inflows. (C) 2013 Published by Elsevier Ltd.	[Leroy, Suzanne A. G.; Lopez-Merino, Lourdes] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Tudryn, Alina] Univ Paris Sud, Lab IDES, UMR8148, F-91405 Orsay, France; [Tudryn, Alina] CNRS, F-91405 Orsay, France; [Chalie, Francoise; Gasse, Francoise] Aix Marseille Univ, CNRS, CEREGE, IRD,UM 34,UMR 7330,UMR 161, F-13545 Aix En Provence 04, France	Brunel University; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Leroy, SAG (通讯作者)，Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England.	suzanne.leroy@brunel.ac.uk	López-Merino, Lourdes/GLT-0551-2022; Leroy, Suzanne/D-3996-2009	Lopez-Merino, Lourdes/0000-0002-6361-5374	European Contract INCO-Copernicus "Understanding the Caspian Sea erratic fluctuations" [IC15-CT96-0112]; Centre National de la Recherche Scientifique within the framework of the INSU-DYTEC (DYnamique de la Terre et du Climat) Program (France); INQUA QuickLakeH project [1227]; European project Marie Curie [CLIMSEAS-PIRSES-GA-2009-247512]; Brunel IfE MINT Scheme	European Contract INCO-Copernicus "Understanding the Caspian Sea erratic fluctuations"; Centre National de la Recherche Scientifique within the framework of the INSU-DYTEC (DYnamique de la Terre et du Climat) Program (France); INQUA QuickLakeH project; European project Marie Curie(European Union (EU)); Brunel IfE MINT Scheme	This study has been conducted within the European Contract INCO-Copernicus "Understanding the Caspian Sea erratic fluctuations" no IC15-CT96-0112. This was funded by the Centre National de la Recherche Scientifique within the framework of the INSU-DYTEC (DYnamique de la Terre et du Climat) Program (France). Thanks are due to the French and Russian colleagues, who organized and participated in the coring and hydrological sea expedition of August 1994. P.-J. Giannesini kindly provided the carbonate data and he and E. Moreno are the curators of the cores at the Museum National d'Histoire Naturelle de Paris, France. We are especially grateful to P. Tucholka and F. Guichard who actively contributed to the scientific part of this project. The publication is a contribution to the INQUA QuickLakeH project (No. 1227) and to the European project Marie Curie, CLIMSEAS-PIRSES-GA-2009-247512. Mr M. Turner (Brunel University) has kindly revised the English of the manuscript. LLM is funded by the Brunel IfE MINT Scheme.	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Sci. Rev.	OCT 15	2013	78						77	97		10.1016/j.quascirev.2013.07.032	http://dx.doi.org/10.1016/j.quascirev.2013.07.032			21	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	264VK		hybrid, Green Published			2025-03-11	WOS:000327908900006
J	di Pasquo, M; Martin, JE				di Pasquo, Mercedes; Martin, James E.			Palynoassemblages associated with a theropod dinosaur from the Snow Hill Island Formation (lower Maastrichtian) at the Naze, James Ross Island, Antarctica	CRETACEOUS RESEARCH			English	Review						Palynostratigraphy; Paleoenvironment; Snow Hill Island Formation; Early Maastrichtian; James Ross Island; Antarctica	LATE CRETACEOUS STRATIGRAPHY; DINOFLAGELLATE CYST; SEYMOUR-ISLAND; MARAMBIO GROUP; SEDIMENTARY CYCLES; CAPE LAMB; BASIN; PALYNOLOGY; BIOSTRATIGRAPHY; AREA	The Cape Lamb Member of the Snow Hill Island Formation at The Naze on the northern margin of James Ross Island, east of the Antarctic Peninsula, yielded a theropod dinosaur recovered near the middle of a 90 m thick section that begins at sea level, ends below a basalt sill, and is composed of interbedded green-gray massive and laminated fine-grained sandstones and mudstones. Sixteen palynoassemblages were recovered from this section, which yielded moderately diverse assemblages with a total of 100 relatively well-preserved species. The principal terrestrial groups (32%) are represented by lycophytes (8 species), pteridophytes (15 species), gymnosperms (13 species), angiosperms (21 species) and freshwater chlorococcaleans (3 species). Marine palynomorphs (68%) belong to dinoflagellates (61 species), chlorococcaleans (6 species), and one acritarch. The vertical distribution of selected species allows the distinction of two informal assemblages, the lower Odontochitina ponfera assemblage from the base to its disappearance in the lower part of the section, and the remaining section characterized by the Batiacasphaera grandis assemblage. The global stratigraphic ranges of selected palynomorphs suggest an early Maastrichtian age for this section and the entombed dinosaur that is also supported by the presence of the ammonoid Kitchinites darwinii. These assemblages share many species with latest Campanian-early Maastrichtian palynofloras from Vega and Humps Islands, New Zealand, and elsewhere in the Southern Ocean, establishing a good correlation among them. The dominance or frequent presence of dinoflagellates throughout the section supports the general interpretation of a shelf marine depocenter. The consistent presence of terrestrial palynomorphs suggests contributions from littoral/inland environments. (C) 2013 Elsevier Ltd. All rights reserved.	[di Pasquo, Mercedes] CICyTTP CONICET, Lab Palinoestratig & Paleobot, Consejo Invest Cient & Tecnol CONICET, Entre Rios, Argentina; [Martin, James E.] JE Martin Geosci Consultat, Sturgis, SD 57785 USA; [Martin, James E.] Univ SW Louisiana, Sch Geosci, Lafayette, LA 70504 USA	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Louisiana Lafayette	di Pasquo, M (通讯作者)，CICyTTP CONICET, Lab Palinoestratig & Paleobot, Consejo Invest Cient & Tecnol CONICET, Dr Matteri & Espana S-N,Diamante CP E3105BWA, Entre Rios, Argentina.	medipa@cicyttp.org.ar; JEMartinGeoscientific@gmail.com		di Pasquo, Mercedes/0000-0003-3068-0089	NSF [0087972, 0003844]; ANPCyT [Pict 07-36166]; Office of Polar Programs (OPP); Directorate For Geosciences [0087972, 0003844] Funding Source: National Science Foundation	NSF(National Science Foundation (NSF)); ANPCyT(ANPCyT); Office of Polar Programs (OPP); Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	The authors would like to sincerely thank the Instituto Antarctico Argentino and the National Science Foundation, Office of Polar Programs, who were responsible for the support of the expeditions (NSF grants awarded to J.E. Martin (OPP#0087972) and J.A. Case (OPP#0003844)). This research would not have been possible without the collaboration from Dr. Judd A. Case, Eastern Washington University. Dr. J. Foster Sawyer (SD School of Mines and Technology), collaborated in measuring and sampling the section in Antarctica. M. Di Pasquo acknowledges the Fulbright Scholarship Program and CONICET of Argentina for providing her the opportunity for cooperation with colleagues from USA and for continuing collaboration. Support from home institutions is greatly appreciated (e.g. ANPCyT Pict 07-36166). Captain Mike Terminal and crew of the Lawrence M. Gould research vessel are thanked for their congeniality and for transportation to James Ross Island. Mr. John Evans and his staff in Raytheon Polar made every effort to make our sojourn possible, safe, and comfortable. We thank all our field companions, Dr. Marcelo Reguero, Dr. J. Foster Sawyer, Dr. Allen J. Kihm, Dr. Jennifer Hargrave, Dr. Robert Meredith, Ms. Amanda Person, Dr. Wayne Thompson, Ms. Melissa Rider, Dr. Kristin van Konynenburg, Mr. Joe Pettit, Mr. Dan Martin, and Ms. Lucy Bledsoe, whose dedication to science and congeniality during extremely difficult field conditions are the cornerstone of this research. Dr. Wayne Thompson aided further in the sketch of the outcrop for which we are thankful. The authors thank to the anonimous reviewers and the Editor E.A.M. Koutsoukos for their suggestions that allowed us to improve our manuscript.	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Res.	OCT	2013	45						135	154		10.1016/j.cretres.2013.07.008	http://dx.doi.org/10.1016/j.cretres.2013.07.008			20	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	273GO		Green Published			2025-03-11	WOS:000328523500012
J	Gu, HF; Luo, ZH; Zeng, N; Lan, BB; Lan, DZ				Gu, Haifeng; Luo, Zhaohe; Zeng, Ni; Lan, Binbin; Lan, Dongzhao			First record of <i>Pentapharsodinium</i> (Peridiniales, Dinophyceae) in the China Sea, with description of <i>Pentapharsodinium dalei</i> var. aciculiferum	PHYCOLOGICAL RESEARCH			English	Article						calcareous dinoflagellates; Ensiculifera; Pentapharsodinium; Pentapharsodinium dalei; South China Sea	DINOFLAGELLATE CYSTS; PHYLOGENY; SEDIMENTS; MODEL	The dinophyte genus Pentapharsodinium shares an identical plate formula with that of Ensiculifera, but lacks a spine on the first cingulum plate and a median sulcal plate (Sm). Herein we established eight strains by incubating single cysts of Pentapharsodiniumdalei from the Chukchi Sea, Yellow Sea, and South China Sea. The six strains from the Chukchi Sea and Yellow Sea fit the description of P.dalei, and they share identical internal transcribed spacer region (ITS1, ITS2 and 5.8S rDNA) sequences. The two other strains (G96 and PDFC01) from the South China Sea are morphologically similar to P.dalei, but they possess a spine on the anterior sulcal plate and an additional Sm plate. These two strains were described as P.dalei var. aciculiferum. They share identical ITS sequences and differ from P.dalei strains PDCH01 (Yellow Sea) and SZN19 (Norway origin) at 20 and 26 positions (96.40% and 95.32% similarity) respectively. Maximum-likelihood and Bayesian inference resolved a well supported clade consisting of P.dalei and P.dalei var. aciculiferum. Our results reveal that cysts of P.dalei might comprise several morphologically, genetically, and ecologically different varieties.	[Gu, Haifeng; Luo, Zhaohe; Zeng, Ni; Lan, Binbin; Lan, Dongzhao] State Ocean Adm, Inst Oceanog 3, Xiamen, Peoples R China; [Luo, Zhaohe; Zeng, Ni] Jinan Univ, Coll Life Sci & Technol, Guangzhou, Guangdong, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources; Jinan University	Gu, HF (通讯作者)，State Ocean Adm, Inst Oceanog 3, Xiamen, 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 Scientific-Basic Special Fund [2009FY210400]; National Natural Science Foundation of China [30900081]	National Scientific-Basic Special Fund; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank Dr Mona Hoppenrath and three anonymous reviewers for constructive suggestions. This project was supported by the National Scientific-Basic Special Fund (Grant no. 2009FY210400) and National Natural Science Foundation of China (30900081).	Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Balech E., 1967, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nat (Hidrologia), V2, P77; Balech E, 1988, Publ. Espec. Inst. EspanOl. De. Oceanogr., Via; Coleman AW, 2009, MOL PHYLOGENET EVOL, V50, P197, DOI 10.1016/j.ympev.2008.10.008; Cox E. R., 1971, CONTRIBUTIONS PHYCOL, P121; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; Darty K, 2009, BIOINFORMATICS, V25, P1974, DOI 10.1093/bioinformatics/btp250; Edgar RC, 2004, NUCLEIC ACIDS RES, V32, P1792, DOI 10.1093/nar/gkh340; Elbrächter M, 2008, TAXON, V57, P1289, DOI 10.1002/tax.574019; Farr E. 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Res.	OCT	2013	61	4					256	267		10.1111/pre.12024	http://dx.doi.org/10.1111/pre.12024			12	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	271ME					2025-03-11	WOS:000328395200001
J	Prebble, JG; Crouch, EM; Carter, L; Cortese, G; Nodder, SD				Prebble, J. G.; Crouch, E. M.; Carter, L.; Cortese, G.; Nodder, S. D.			Dinoflagellate cysts from two sediment traps east of New Zealand	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate; Cyst; Modern; Sediment trap; Flux; Palaeoceanographic proxies	SUBTROPICAL CONVERGENCE REGION; SEA-SURFACE CONDITIONS; SUB-ANTARCTIC WATERS; PACIFIC-OCEAN; SOUTHLAND CURRENT; AUSTRAL WINTER; FRONT REGION; CHATHAM RISE; PHYTOPLANKTON; VARIABILITY	Two discontinuous sediment trap records of organic-walled dinoflagellate cyst ( dinocyst) flux, each sampling > 300 days within the years 2005-2009, were derived from two time-incremental traps deployed at 1500 m water depth east of New Zealand. The traps sampled flux from beneath two distinct surface water masses on either side of the Subtropical Front: (i) warm, seasonally macronutrient-depleted Subtropical and (ii) cold, micronutrient-limited Subantarctic waters. Nineteen dinocyst taxa or taxonomic groups were identified from the trap samples. Trap assemblages at both sites were dominated by cysts of Protoperidiniaceae, notably Brigantedinium spp., which comprised almost similar to 98% of the dinocyst flux. The seasonality of the dinocyst flux differed between the traps, with a pronounced spring flux in the Subtropical trap, while seasonal variation in the Subantarctic trap was relatively muted. In Subtropical waters, moderate correlation was observed between Protoperidiniaceae cyst flux and chlorophyll a concentrations in surface waters in the 3-4 weeks prior to sampling. In Subantarctic waters, there was a weak correlation between Protoperidiniaceae cyst flux and reduced intensity of storm-induced turbulence during the preceding 2-3 weeks. There was a large discrepancy between dinocyst assemblages in the traps and those observed in nearby sea-floor sediments. Protoperidiniaceae dinocysts, particularly Echinidinium and Brigantedinium, were highly under-represented in the sea-floor assemblages. These forms are more susceptible to degradation in oxygenated sediments than other dinocysts, but inter-annual variability in cyst flux, or short-term variation not covered by sampling discontinuities in the current study could also have contributed to this discrepancy. The major differences in the seasonality of dinocyst fluxes between the two water masses examined in this initial study, suggest that mean-annual rather than seasonal climatologies are more appropriate for dinocyst-based quantitative palaeoenvironmental reconstructions in the New Zealand region. (C) 2013 Elsevier B.V. All rights reserved.	[Prebble, J. G.; Carter, L.] Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand; [Prebble, J. G.; Crouch, E. M.; Cortese, G.] GNS Sci, Lower Hutt 5040, New Zealand; [Nodder, S. D.] Natl Inst Water & Atmospher Res NIWA, Wellington, New Zealand	Victoria University Wellington; GNS Science - New Zealand; National Institute of Water & Atmospheric Research (NIWA) - New Zealand	Prebble, JG (通讯作者)，GNS Sci, POB 30368, Lower Hutt 5040, New Zealand.	j.prebble@gns.cri.nz	Crouch, Erica/C-2820-2013; Cortese, Giuseppe/C-8281-2011	Cortese, Giuseppe/0000-0003-1780-3371; Prebble, Joseph/0000-0002-7268-4187	TEC Bright Futures Scholarship by the New Zealand Government; GNS Science through its Global Change through Time (GCT) Programme; FRST; Ministry of Business, Innovation and Employment, NIWA's CAPEX [CO1X0702, CO1X0501]	TEC Bright Futures Scholarship by the New Zealand Government; GNS Science through its Global Change through Time (GCT) Programme; FRST(New Zealand Foundation for Research, Science and Technology); Ministry of Business, Innovation and Employment, NIWA's CAPEX	We thank the officers and crew of the RV Tangaroa for more than twenty 3- to 6-monthly deployment voyages over the last decade of this trap experiment, including the current mooring team (Malcolm Greig, Bill Main, Peter Gerring, Craig Stewart, Brett Grant, Fiona Elliot). Lisa Northcote at NIWA and Sonja Fry at GNS Science split and processed the trap and sediment samples, respectively. Paulo Calil, NIWA, provided modelled wind data, Lisa Northcote shared unpublished data on foraminifera flux. We also acknowledge the MODIS mission scientists and associated NASA and NOAA personnel for production of the satellite environmental data used in this study. JP was supported by a TEC Bright Futures Scholarship provided by the New Zealand Government. EC and GC acknowledge support from GNS Science through its Global Change through Time (GCT) Programme, LC was supported by the FRST funded Antarctica New Zealand Interglacial Climate Extremes (ANZICE) programme, and SN acknowledges funding support from the New Zealand Foundation of Science, Research & Technology (now Ministry of Business, Innovation and Employment) in the programmes CO1X0702 and CO1X0501, NIWA's CAPEX fund. 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Micropaleontol.	OCT	2013	104						25	37		10.1016/j.marmicro.2013.08.003	http://dx.doi.org/10.1016/j.marmicro.2013.08.003			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	260DY					2025-03-11	WOS:000327576400003
J	Herzi, F; Jean, N; Zhao, HY; Mounier, S; Mabrouk, HH; Hlaili, AS				Herzi, Faouzi; Jean, Natacha; Zhao, Huiyu; Mounier, Stephane; Mabrouk, Hassine Hadj; Hlaili, Asma Sakka			Copper and cadmium effects on growth and extracellular exudation of the marine toxic dinoflagellate <i>Alexandrium catenella</i>: 3D-fluorescence spectroscopy approach	CHEMOSPHERE			English	Article						Metals; DOC; 3D-fluorescence spectroscopy; PARAFAC; Alexandrium catenella; Toxic dinoflagellate	DISSOLVED ORGANIC-MATTER; RED-TIDE; FLUORESCENCE SPECTROSCOPY; EXCITATION; TERRESTRIAL; HARMFUL; MATRIX; DIMETHYLSULFONIOPROPIONATE; PHYTOPLANKTON; ACCUMULATION	In this study, metal contamination experiments were conducted to investigate the effects of copper and cadmium on the growth of the marine toxic dinoflagellate Alexandrium catenella and on the production of dissolved organic matter (Dissolved Organic Carbon: DOC; Fluorescent Dissolved Organic Matter: FDOM). This species was exposed to increasing concentrations of Cu2+ (9.93 x 10(-10)-1.00 x 10(-7) M) or Cd2+ (1.30 x 10(-8)-4.38 x 10(-7) M), to simulate polluted environments. The drastic effects were observed at pCu(2+) = 7.96 (Cu2+: 1.08 x 10(-8) M) and pCd(2+) = 7.28 (Cd2+: 5.19 x 10(-8) M), where cyst formation occurred. Lower levels of Cu2+ (pCu(2+) > 9.00) and Cd2+ (pCd(2+) > 7.28) had no effect on growth. However, when levels of Cu2+ and Cd2+ were beyond 10(-7) M, the growth was totally inhibited. The DOC released per cell (DOC/Cell) was different depending on the exposure time and the metal contamination, with higher DOC/Cell values in response to Cu2+ and Cd2+, comparatively to the control. Samples were also analyzed by 3D-fluorescence spectroscopy, using the Parallel Factor Analysis (PARAFAC) algorithm to characterize the FDOM. The PARAFAC analytical treatment revealed four components (C1, C2, C3 and C4) that could be associated with two contributions: one, related to the biological activity; the other, linked to the decomposition of organic matter. The C1 component combined a tryptophan peak and a characteristic humic substances response, and the C2 component was considered as a tryptophan protein fluorophore. The C3 and C4 components were associated to marine organic matter production. (C) 2013 Elsevier Ltd. All rights reserved.	[Herzi, Faouzi; Mabrouk, Hassine Hadj; Hlaili, Asma Sakka] Univ Carthage, Fac Sci Bizerte, LCVP, Jarzouna 7021, Bizerte, Tunisia; [Herzi, Faouzi; Jean, Natacha; Zhao, Huiyu; Mounier, Stephane] Univ Toulon & Var, PROTEE, EA 3819, F-83957 La Garde, France	Universite de Carthage; Universite de Toulon	Mounier, S (通讯作者)，Univ Carthage, Fac Sci Bizerte, LCVP, Jarzouna 7021, Bizerte, Tunisia.	faouzi-herzi@univ-tln.fr; jean@univ-tln.fr; huiyu.zhao@univ-tln.fr; mounier@univ-tln.fr; asma_sak-ka@yahoo.fr	HLAILI, Asma/AAD-9610-2019; Zhao, Huiyu/LYO-7907-2024; MOUNIER, Stephane Jean Louis/P-9135-2015	MOUNIER, Stephane Jean Louis/0000-0002-9624-0230	Conseil General du Var (CG); Toulon Provence Mediterranee (TPM); ARCUS CERES project (Region PACA-MAE)	Conseil General du Var (CG)(Region Provence-Alpes-Cote d'Azur); Toulon Provence Mediterranee (TPM); ARCUS CERES project (Region PACA-MAE)(Region Provence-Alpes-Cote d'Azur)	This research was supported by the Conseil General du Var (CG), Toulon Provence Mediterranee (TPM) and ARCUS CERES project (Region PACA-MAE). We are deeply indebted to Yves COLLOS and Estelle MASSERET from the Laboratory ECOSYM UMR 5119 of the Montpellier 2 University, for providing us with the A. catenella strain ACT03 used in the study.	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J	Balestra, B; Bertini, A; de Vernal, A; Monechi, S; Reale, V				Balestra, Barbara; Bertini, Adele; de Vernal, Anne; Monechi, Simonetta; Reale, Viviana			Late Quaternary sea surface conditions in the Laurentian Fan: Evidence from coccolith and dinocyst assemblages	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Laurentian Fan; Coccolith; Dinocyst; St. Lawrence River; Late Quaternary; Holocene	NORTHERN NORTH-ATLANTIC; NORWEGIAN-GREENLAND SEA; SUB-ARCTIC FRONT; NORDIC SEAS; OCEANOGRAPHIC CHANGES; DINOFLAGELLATE CYSTS; LAST DEGLACIATION; HOLOCENE CLIMATE; MEAN CIRCULATION; LABRADOR SEA	The analyses of coccoliths and dinocysts from the IMAGES core MD95-2033, collected on the Laurentian Fan (44 degrees 39.87N, 55 degrees 37.21W; water depth = 1412 m) in the northwest North Atlantic provide a new dataset to assess the magnitude of climatic changes during the Holocene with a millennial time resolution. Coccolith and dinocyst data were combined to reconstruct changes in past sea surface conditions. In addition, the dinocyst assemblages were used to reconstruct the sea-surface temperature (SST) and salinity (SSS) based on the modern analog technique. The distribution of the coccolith and dinocyst assemblages, suggests a succession of climatic events during the late Quaternary and early Holocene, linked to change in the influence of the Labrador Current and/or the St. Lawrence River discharge. The dinocyst assemblages recorded a thermal optimum during the mid-Holocene. In the late Holocene, coccolith concentrations show two peaks at 2.3 and 1.1 ky, which coincide with the presence of species with different ecological properties, likely due to the localized influence of the Slope Water Jet (SWJ) current. The presence of this current has played a role in the development of the coccolith and dinocyst assemblages and SST fluctuations, especially in the last 2 ky. Overall, the interaction between the St. Lawrence River, the SWJ, the LC, and the NAC has all controlled the SSS, SSTs, and the development of the coccolith and dinocyst assemblages, confirming a significant regionalism of the entire area. (C) 2013 Published by Elsevier B.V.	[Balestra, Barbara] CUNY Queens Coll, Sch Earth & Environm Sci, Flushing, NY 11367 USA; [Balestra, Barbara] Univ Calif Santa Cruz, Inst Marine Sci, Santa Cruz, CA 95064 USA; [Bertini, Adele; Monechi, Simonetta; Reale, Viviana] Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy; [Bertini, Adele] CNR, Inst Geosci & Earth Resources, Sect Florence, I-50121 Florence, Italy; [de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	City University of New York (CUNY) System; Queens College NY (CUNY); University of California System; University of California Santa Cruz; University of Florence; Consiglio Nazionale delle Ricerche (CNR); Istituto di Geoscienze e Georisorse (IGG-CNR); University of Quebec; University of Quebec Montreal	Balestra, B (通讯作者)，Univ Calif Santa Cruz, Inst Marine Sci, 1156 High St, Santa Cruz, CA 95064 USA.	balestrabb@gmail.com	monechi, simonetta/AAN-6148-2020; Bertini, Adele/KFQ-7894-2024; de Vernal, Anne/D-5602-2013	Balestra, Barbara/0000-0001-7064-3173; BERTINI, Adele/0000-0002-9332-6725; de Vernal, Anne/0000-0001-5656-724X	CONISMA; PSCUNY 42 grant; Advanced Fellowship NATO-CNR grant	CONISMA; PSCUNY 42 grant; Advanced Fellowship NATO-CNR grant	This research has been supported by a CONISMA and a PSCUNY 42 grant to Barbara Balestra and an Advanced Fellowship NATO-CNR grant to Adele Bertini. Two anonymous reviewers are also thanked for their constructive comments.	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Paleoclimatol. Paleoecol.	OCT 1	2013	387						200	210		10.1016/j.palaeo.2013.07.002	http://dx.doi.org/10.1016/j.palaeo.2013.07.002			11	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	233WA					2025-03-11	WOS:000325599000016
J	Leroy, SAG; Lahijani, HAK; Reyss, JL; Chalié, F; Haghani, S; Shah-Hosseini, M; Shahkarami, S; Tudryn, A; Arpe, K; Habibi, P; Nasrollahzadeh, HS; Makhlough, A				Leroy, S. A. G.; Lahijani, H. A. K.; Reyss, J. -L.; Chalie, F.; Haghani, S.; Shah-Hosseini, M.; Shahkarami, S.; Tudryn, A.; Arpe, K.; Habibi, P.; Nasrollahzadeh, H. S.; Makhlough, A.			A two-step expansion of the dinocyst <i>Lingulodinium machaerophorum</i> in the Caspian Sea: the role of changing environment	QUATERNARY SCIENCE REVIEWS			English	Article						Caspian Sea; Dinocysts; Past sea surface temperature; Last centuries; Last millennia	BLACK-SEA; SURFACE CONDITIONS; SALINITY CHANGES; LEVEL CHANGES; DEEP-WATER; PHYTOPLANKTON; SEDIMENTS; AGE; VARIABILITY; CIRCULATION	Dinoflagellate cyst assemblages were analysed in four short sediment cores collected in the south Basin of the Caspian Sea for assessing environmental changes over the last few millennia. Two of these cores were dated by radionuclides. The sedimentation rate of one of them was very high, in the order of 20 mm per year. The interpretation of the four sequences is supported by a collection of 27 lagoonal or marine surface sediment samples. A sharp increase in the concentration of the dinocyst occurs after 1967, especially owing to Lingulodinium machaerophorum. Considering nine other cores covering parts or the whole of Holocene, it became clear that this species started to develop in the Caspian Sea only during the last three millennia. By analysing instrumental data and collating existing reconstructions of sea level changes over the last decades, we show that the main forcing for the recent increase of L machaerophorum percentages and concentration is global climate change, especially sea surface temperature increase. Sea level fluctuations likely only have a minor impact. We argue that the recent increase in L machaerophorum indicates that the Caspian Sea clearly is in the Anthropocene. (C) 2013 The Authors. Published by Elsevier Ltd. All rights reserved.	[Leroy, S. A. G.; Haghani, S.; Arpe, K.] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Lahijani, H. A. K.; Haghani, S.; Shah-Hosseini, M.; Shahkarami, S.; Habibi, P.] Iranian Natl Inst Oceanog, Tehran 1411813389, Iran; [Reyss, J. -L.] CEA, CNRS, Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France; [Chalie, F.; Shah-Hosseini, M.] Aix Marseille Univ, CEREGE, CNRS UMR 7330, UM34, F-13545 Aix En Provence 04, France; [Haghani, S.; Shahkarami, S.] Univ Tehran, Sch Geol, Tehran, Iran; [Tudryn, A.] Univ Paris 11, Lab CNRS UPS UMR 8148, IDES, Dept Sci Terre, F-91405 Orsay, France; [Arpe, K.] Max Planck Inst Meteorol, D-20146 Hamburg, Germany; [Nasrollahzadeh, H. S.; Makhlough, A.] Caspian Sea Ecol Res Ctr, Dept Ecol, Sari 961, Iran	Brunel University; Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); CEA; Aix-Marseille Universite; University of Tehran; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay; Max Planck Society	Leroy, SAG (通讯作者)，Brunel Univ, Inst Environm, Kingston Lane, Uxbridge UB8 3PH, Middx, England.	suzanne.leroy@brunel.ac.uk	Leroy, Suzanne/D-3996-2009; Alizadeh Ketek Lahijani, Hamid/GRF-3549-2022; Nasrollahzadeh Saravi, Dr Hassan/K-9476-2017; Makhlough, Asieh/P-8083-2017	Nasrollahzadeh Saravi, Dr Hassan/0000-0003-1362-1036; Alizadeh Ketek Lahijani, Hamid/0000-0001-6136-3655; Makhlough, Asieh/0000-0002-6798-2673				Adrian R, 2009, LIMNOL OCEANOGR, V54, P2283, DOI 10.4319/lo.2009.54.6_part_2.2283; AMINI A., 2012, Journal of Basic and Applied scientific Research, V2, P289; [Anonymous], 1890, GEOGRAPHISCHE ABHAND; Appleby P.G., 2000, LIMNOLOGY, V59, P1, DOI DOI 10.4081/JLIMNOL.2000.S1.1; Arpe K, 2000, GEOPHYS RES LETT, V27, P2693, DOI 10.1029/1999GL002374; Arpe K, 2012, HYDROL EARTH SYST SC, V16, P19, DOI 10.5194/hess-16-19-2012; Arpe K, 2007, QUATERN INT, V173, P144, DOI 10.1016/j.quaint.2007.03.008; Bagheri Siamak, 2011, American Journal of Applied Sciences, V8, P1328, DOI 10.3844/ajassp.2011.1328.1336; Bagheri S, 2012, EKOLOJI, V21, P32, DOI 10.5053/ekoloji.2012.834; Beni AN, 2013, GEOMORPHOLOGY, V187, P11, DOI 10.1016/j.geomorph.2012.11.026; Bennett K., 2007, PSIMPOLL PSCOMB PROG; Birshtein Y A, 1968, ATLAS INVERTEBRATES; Boomer I, 2005, PALAEOGEOGR PALAEOCL, V225, P173, DOI 10.1016/j.palaeo.2004.10.023; Boomer I., 2003, PALEONTOL SOC PAPERS, V9, P153, DOI [180.10.1017/S1089332600002199, DOI 10.1017/S1089332600002199]; Bradley LR, 2012, J QUATERNARY SCI, V27, P835, DOI 10.1002/jqs.2580; Carroll J., 2003, SEDIMENTARY PROCESSE; Cazenave A, 1997, GEOPHYS RES LETT, V24, P881, DOI 10.1029/97GL00809; Crétaux JF, 2006, CR GEOSCI, V338, P1098, DOI 10.1016/j.crte.2006.08.002; Crutzen PJ, 2002, NATURE, V415, P23, DOI 10.1038/415023a; DEAN WE, 1974, J SEDIMENT PETROL, V44, P242; Dee DP, 2011, Q J ROY METEOR SOC, V137, P553, DOI 10.1002/qj.828; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Develi EE., 2008, RES LETT ECOLOGY, DOI [10.1155/2008/185642, DOI 10.1155/2008/185642]; Dumont HJ, 1998, LIMNOL OCEANOGR, V43, P44, DOI 10.4319/lo.1998.43.1.0044; Einsele G, 1997, GEOL RUNDSCH, V86, P288, DOI 10.1007/s005310050141; Ghaffari P, 2010, OCEAN SCI, V6, P877, DOI 10.5194/os-6-877-2010; Ginzburg AI, 2005, HANDB ENVIRON CHEM, V5, P59, DOI 10.1007/698_5_004; Golitsyn G. 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Sci. Rev.	OCT 1	2013	77						31	45		10.1016/j.quascirev.2013.06.026	http://dx.doi.org/10.1016/j.quascirev.2013.06.026			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	229BA		Green Published, hybrid			2025-03-11	WOS:000325235600004
J	Prasad, V; Singh, IB; Bajpai, S; Garg, R; Thakur, B; Singh, A; Saravanan, N; Kapur, VV				Prasad, Vandana; Singh, Indra Bir; Bajpai, Sunil; Garg, Rahul; Thakur, Biswajeet; Singh, Abha; Saravanan, Nachiappan; Kapur, Vivesh Vir			Palynofacies and sedimentology-based high-resolution sequence stratigraphy of the lignite-bearing muddy coastal deposits (early Eocene) in the Vastan Lignite Mine, Gulf of Cambay, India	FACIES			English	Article						Lignite; Sequence stratigraphy; Sedimentology; Palynofacies; Early Eocene thermal maxima; Vastan Lignite Mine; Gulf of Cambay (Khambhat); Western India	PALEOCENE-EARLIEST EOCENE; DINOFLAGELLATE CYSTS; CHENIER-PLAIN; CONTINENTAL-MARGIN; SURAT DISTRICT; GUJARAT; BASIN; CLIMATE; FACIES; MODEL	Geological records of early Paleogene warming are rare in low latitudinal regions. The Indian subcontinent preserves records of this global event on western and eastern margins. We attempt to decipher paleoenvironmental setup and facies architecture of the paleo-equatorial early Eocene succession at the Vastan Lignite Mine, Gulf of Cambay, western India. The Vastan lignite succession was deposited in a low-energy coastal marsh-bay complex receiving only fine-grained muddy sediments from the weathered Deccan Traps. The lower part of the Vastan lignite deposit, designated as "Vastan Succession A", comprises four depositional facies representing distinct environments (open bay, restricted bay, creek and channel, and coastal marsh) and one diagenetic facies. Palynofacies analysis, backed by precise sedimentological framework, records changes in terrestrial supply and fluctuating marine characters of bay and marshes. Eleven Palyno-Units are identified in distinct lithofacies sequences stacked in shallowing-upward cycles representing five parasequences that constitute a Transgressive Systems Tract (TST) deposit. Each parasequence starts with a transgressive sheet deposit, followed by shallowing-upward bay fill-marsh deposits. In the vertical succession, each parasequence acquires increasing marine character, culminating in a maximum flooding surface (shell carbonate) that represents large-scale coastal onlap during early Ypresian time. The TST is followed by a Highstand Systems Tract deposit, which shows an erosional surface at the top of the upper lignite indicating Lowstand Systems Tract and a sequence boundary at similar to 52 Ma. The Vastan Succession A represents TST (3rd-order cycle) deposits with parasequences and hemicycles representing 4th- and 5th-order cycles. The study demonstrates sea level rise along the Indian western coastal margin in response to early Eocene warming between similar to 55 and similar to 52 Ma with maximum transgression at 53.7 Ma.	[Prasad, Vandana; Garg, Rahul; Thakur, Biswajeet; Singh, Abha] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India; [Singh, Indra Bir; Garg, Rahul] Univ Lucknow, Dept Geol, Lucknow 226007, Uttar Pradesh, India; [Bajpai, Sunil; Saravanan, Nachiappan; Kapur, Vivesh Vir] Indian Inst Technol Roorkee, Dept Earth Sci, Roorkee 247667, Uttar Pradesh, India; [Saravanan, Nachiappan] Shell Technol Ltd, Bangalore, Karnataka, India; [Kapur, Vivesh Vir] Dadswood, Harlow Town CM 20 JG, Essex, England	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Lucknow University; Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Roorkee	Singh, IB (通讯作者)，Univ Lucknow, Dept Geol, Lucknow 226007, Uttar Pradesh, India.	ibsinghuniv@gmail.com	Singh, Abha/O-3631-2019; Kapur, Vivesh/AAO-4885-2021; PRASAD, VANDANA/KUF-4093-2024; Bajpai, Sunil/E-8416-2010		INSA; Department of Science and Technology (DST)	INSA; Department of Science and Technology (DST)(Department of Science & Technology (India))	IBS is thankful to INSA for the award of an INSA Senior Scientist Position. Financial support to SB from the Department of Science and Technology (DST) is thankfully acknowledged. The authors are grateful to Director BSIP for providing the laboratory facility. Thanks are expressed to Prof. A. K. Jaitly for his help in the identification of the molluscan fauna.	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J	Al-Ameri, TK; Al-Jubouri, NM; Isa, MJ; Al-Azzawi, RE				Al-Ameri, Thamer Khazaal; Al-Jubouri, Nagham Mohammed; Isa, Murtadha J.; Al-Azzawi, Rami Eidan			Hydrocarbons generation potential of the Jurassic-Lower Cretaceous Formation, Ajeel field, Iraq	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Source rocks; Palynomorphs; Hydrocarbon generation; Middle Iraq	PETROLEUM SYSTEM; SOUTHERN IRAQ; RESERVOIR; KEROGENS	Organic geochemical analysis and palynological studies of the organic matters of subsurface Jurassic and Lower Cretaceous Formations for two wells in Ajeel oil field, north Iraq showed evidences for hydrocarbon generation potential especially for the most prolific source rocks Chia Gara and Sargelu Formations. These analyses include age assessment of Upper Jurassic (Tithonian) to Lower Cretaceous (Berriasian) age and Middle Jurassic (Bathonian-Tithonian) age for Chia Gara and Sargelu Formations, respectively, based on assemblages of mainly dinoflagellate cyst constituents. Rock-Eval pyrolysis have indicated high total organic carbon (TOC) content of up to 18.5 wt%, kerogen type II with hydrogen index of up to 415 mg HC/g TOC, petroleum potential of 0.70-55.56 kg hydrocarbon from each ton of rocks and mature organic matter of maximum temperature reached (T-max) range between 430 and 440 A degrees C for Chia Gara Formation, while Sargelu Formation are of TOC up to 16 wt% TOC, Kerogen type II with hydrogen index of 386 mg HC/g TOC, petroleum potential of 1.0-50.90 kg hydrocarbon from each ton of rocks, and mature organic matter of T-max range between 430 and 450 A degrees C. Qualitative studies are done in this study by textural microscopy used in assessing amorphous organic matter for palynofacies type belonging to kerogen type A which contain brazinophyte algae, Tasmanites, and foraminifera test linings, as well as the dinoflagellate cysts and spores, deposited in dysoxic-anoxic environment for Chia Gara Formation and similar organic constituents deposited in distal suboxic-anoxic environment for Sargelu Formation. The palynomorphs are of dark orange and light brown, on the spore species Cyathidites australis, that indicate mature organic matters with thermal alteration index of 2.7-3.0 for the Chia Gara Formation and 2.9-3.1 for the Sargelu Formation by Staplin's scale. These characters have rated the succession as a source rock for very high efficiency for generation and expulsion of oil with ordinate gas that charged mainly oil fields of Baghdad, Dyala (BUyenaquba), and Salahuddin (Tikrit) Governorates. Oil charge the Cretaceous-Tertiary total petroleum system (TPS) are mainly from Chia Gara Formation, because most oil from Sargelu Formation was prevented passing to this TPS by the regional seal Gotnia Formation. This case study of mainly Chia Gara oil source is confirmed by gas chromatography-mass spectrometry analysis for oil from reservoirs lying stratigraphically above the Chia Gara Formation in Ajeel and Hamrine oil fields, while oil toward the north with no Gotnia seal could be of mainly Sargelu Formation source.	[Al-Ameri, Thamer Khazaal; Al-Jubouri, Nagham Mohammed; Isa, Murtadha J.; Al-Azzawi, Rami Eidan] Univ Baghdad, Dept Geol, Coll Sci, Jadiriyah, Iraq	University of Baghdad	Al-Ameri, TK (通讯作者)，Univ Baghdad, Dept Geol, Coll Sci, Jadiriyah, Iraq.	thamer_alameri@yahoo.com	Idan, Rami/V-6290-2017	Idan, Rami/0000-0003-2882-8937				Al-Ameri, 2011, J PET GEOL, V34, P1; Al-Ameri TK, 2009, GEOARABIA, V14, P91; Al-Ameri TK, 2011, ARAB J GEOSCI, V4, P915, DOI 10.1007/s12517-009-0115-4; Al-Ameri TK, 1999, CRETACEOUS RES, V20, P359, DOI 10.1006/cres.1999.0157; Al-Ameri TK, 2006, P AAPG C HOUST TEX; Alsharhan AS., 1997, Sedimentary Basins and Petroleum Geology of the Middle East, DOI DOI 10.1016/B978-044482465-3/50003-6; [Anonymous], PETROLEUM FORMATION; Aqrawi AAM, 2010, PETROLEUM GEOLOGY IR, P440; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Bellen R.C., 1959, Lexique Stratigraphique International: Asie, Iraq., V3, P333; Durand B, 1980, KEROGEN INSOLUBLE OR, P450; HELBY R, 1987, STUDIES AUSTR MESOZO, V4, P1; Hunt JM., 1996, PETROLEUM GEOCHEMIST; Ibrahim M, 1996, GEOL AFRIQUE ATLANTI, P611; MILIOUD ME, 1975, AM ASS STRATIGRAPHIC, V4, P65; RAHMAN M, 1995, J PETROL GEOL, V18, P91, DOI 10.1111/j.1747-5457.1995.tb00743.x; Riding JB, 1987, PALYNOLOGY, V7, P197; Sharland P.R., 2001, GEO ARABIA SPECIAL P, V2; 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; Thusu B, 1995, J MICROPALAEONTOL, V4, P113; Tyson RV, 1995, SEDIMENTARY ORGANIC, VXviii, P615	23	4	4	0	11	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511			ARAB J GEOSCI	Arab. J. Geosci.	OCT	2013	6	10					3725	3735		10.1007/s12517-012-0636-0	http://dx.doi.org/10.1007/s12517-012-0636-0			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	216XP					2025-03-11	WOS:000324320400011
J	Tahoun, SS; Mohamed, O				Tahoun, Sameh S.; Mohamed, Omar			Palynology and genetic sequence stratigraphy of the reservoir rocks (Cenomanian, Bahariya Formation) in the Salam Oil Field, north Western Desert, Egypt	CRETACEOUS RESEARCH			English	Article						Genetic sequences; Palynofacies; Cenomanian; Bahariya Formation; north Western Desert	SEDIMENTARY ORGANIC-MATTER; WELL; PALYNOFACIES; PALYNOMORPHS; ENVIRONMENT; BOREHOLE	Twenty-eight samples from the Bahariya Formation of the Salam-17 Well in the north Western Desert were palynologically investigated. These samples are of Cenomanian age. Fair diversity and fair to moderately preserved palynomorph assemblage has been recovered. Among them, the dinoflagellate cysts showed very poor diversity and abundance. Four miospore zones have been informally identified in the lower Cenomanian. Various palynofacies criteria, adopted from previous publications (e.g. relative particle abundance data, brown to black wood ratio, equi-dimensional to lath-shaped black wood ratio, average size of phytoclasts and spores/pollen ratio) are applied as alternative indicators to monitor the proximal distal trends instead of the marine palynomorphs-based parameters. The method can be applied in the Egyptian Western Desert to overcome the rarity and absence of dinoflagellate cysts in the recovered organic residues. The palynofacies study of the section demonstrates a predominantly regressive phase, characterized by deltaic, distributary or tidal channels, interrupted by short-lived marine incursions. The palynofacies trends within the studied succession indicate six genetic sequences informally described as Genetic Stratigraphic Sequences A through F. (C) 2013 Elsevier Ltd. All rights reserved.	[Tahoun, Sameh S.] Cairo Univ, Fac Sci, Dept Geol, Giza 12613, Egypt; [Mohamed, Omar] Menia Univ, Dept Geol, Fac Sci, El Minia, Egypt	Egyptian Knowledge Bank (EKB); Cairo University; Egyptian Knowledge Bank (EKB); Minia University	Mohamed, O (通讯作者)，Menia Univ, Dept Geol, Fac Sci, El Minia, Egypt.	omar.mohamed@mu.edu.eg		Mohamed, Omar/0000-0002-2817-1683; Tahoun, Sameh S./0000-0002-0425-8848				Abd El Shafy E., 1991, B FS ZAGAZIG U, V13, P306; Aboul Ela N.M., 1992, NEUES JB GEOLOGIE PA, V10, P595; [Anonymous], 2007, Paleopalynology; [Anonymous], P 13 PETR C EG GEN P; Bassiouni M.E., 1992, B FACULTY SCI ALEXAN, V32, P466; BOULTER MC, 1986, SEDIMENTOLOGY, V33, P871, DOI 10.1111/j.1365-3091.1986.tb00988.x; BUSTIN RM, 1988, AAPG BULL, V72, P277; El Beialy S.Y., 1990, NEWSL STRATIGR, V29, P71; El Beialy S.Y., 1994, Sciences Geologiques Bulletin, V47, P51; El Beialy S, 2011, J AFR EARTH SCI, V59, P215, DOI 10.1016/j.jafrearsci.2010.10.007; El Beialy Salah Y., 1994, Qatar University Science Journal, V14, P184; El Beialy SY, 2010, MAR PETROL GEOL, V27, P370, DOI 10.1016/j.marpetgeo.2009.10.006; El Beialy Salah Y. 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Res.	OCT	2013	45						342	351		10.1016/j.cretres.2013.06.004	http://dx.doi.org/10.1016/j.cretres.2013.06.004			10	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	273GO					2025-03-11	WOS:000328523500024
J	Edvardsen, B; Dittami, SM; Groben, R; Brubak, S; Escalera, L; Rodríguez, F; Reguera, B; Chen, JX; Medlin, LK				Edvardsen, Bente; Dittami, Simon M.; Groben, Rene; Brubak, Sissel; Escalera, Laura; Rodriguez, Francisco; Reguera, Beatriz; Chen, Jixin; Medlin, Linda K.			Molecular probes and microarrays for the detection of toxic algae in the genera <i>Dinophysis</i> and <i>Phalacroma</i> (Dinophyta)	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Dot blot hybridization; Dinophysis; Harmful algal blooms; HABs; Microarray; Molecular probes; Phalacroma; Phylochips; Toxic algae	DIARRHETIC SHELLFISH TOXINS; RIBOSOMAL-RNA PROBES; MORPHOLOGICAL VARIABILITY; ALEXANDRIUM-TAMARENSE; SPECIES DINOPHYCEAE; NATURAL-POPULATIONS; GENETIC DIVERSITY; DINOFLAGELLATE; CELL; IDENTIFICATION	Dinophysis and Phalacroma species containing diarrheic shellfish toxins and pectenotoxins occur in coastal temperate waters all year round and prevent the harvesting of mussels during several months each year in regions in Europe, Chile, Japan, and New Zealand. Toxicity varies among morphologically similar species, and a precise identification is needed for early warning systems. Molecular techniques using ribosomal DNA sequences offer a means to identify and detect precisely the potentially toxic species. We designed molecular probes targeting the 18S rDNA at the family and genus levels for Dinophysis and Phalacroma and at the species level for Dinophysis acuminata, Dinophysis acuta, and Dinophysis norvegica, the most commonly occurring, potentially toxic species of these genera in Western European waters. Dot blot hybridizations with polymerase chain reaction (PCR)-amplified rDNA from 17 microalgae were used to demonstrate probe specificity. The probes were modified along with other published fluorescence in situ hybridization and PCR probes and tested for a microarray platform within the MIDTAL project (http://www.midtal.com). The microarray was applied to field samples from Norway and Spain and compared to microscopic cell counts. These probes may be useful for early warning systems and monitoring and can also be used in population dynamic studies to distinguish species and life cycle stages, such as cysts, and their distribution in time and space.	[Edvardsen, Bente; Dittami, Simon M.; Brubak, Sissel] Univ Oslo, Dept Biol, N-0316 Oslo, Norway; [Groben, Rene] VOR Marine Res Ctr Breioafjorour, IS-355 Olafsvik, Iceland; [Escalera, Laura; Rodriguez, Francisco; Reguera, Beatriz] Inst Espanol Oceanog, Ctr Oceanog Vigo, Vigo 36390, Spain; [Chen, Jixin; Medlin, Linda K.] Marine Biol Assoc UK, Plymouth PL1 2PB, Devon, England	University of Oslo; Spanish Institute of Oceanography; Marine Biological Association United Kingdom	Edvardsen, B (通讯作者)，Univ Oslo, Dept Biol, POB 1066, N-0316 Oslo, Norway.	bente.edvardsen@bio.uio.no	medlin, linda/G-4820-2010; Groben, René/P-1436-2019; Escalera, Laura/S-2836-2018; Reguera, Beatriz/AAG-8273-2020; Dittami, Simon/E-8354-2011; Rodriguez, Francisco/A-5934-2019; Groben, Rene/A-8457-2012	medlin, linda k/0000-0001-6014-8339; Dittami, Simon/0000-0001-7987-7523; Reguera, Beatriz/0000-0003-4582-9798; Rodriguez, Francisco/0000-0002-6918-4771; Escalera, Laura/0000-0003-0938-4250; Edvardsen, Bente/0000-0002-6806-4807; Groben, Rene/0000-0003-3034-2629	EU's 7th Framework Program [FP7-ENV-2007-1-MIDTAL-201724]; Norwegian Research Council [140286/120, 196702/S40]; Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany	EU's 7th Framework Program(European Union (EU)); Norwegian Research Council(Research Council of Norway); Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany	MIDTAL is a project under the EU's 7th Framework Program (FP7-ENV-2007-1-MIDTAL-201724) and provided funding for all but RG during this work. The Norwegian Research Council provided funding to BE through the project MOLHAS (140286/120) and TOXALGAE (196702/S40). RG was funded in part by the Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany. Vladyslava Hostyeva and Wenche Eikrem are thanked for the cell counts at the Oslofjorden station OF2. Two anonymous reviewers are thanked for the valuable comments to an earlier version that improved the manuscript considerably.	Anderson Donald M., 1995, P3; [Anonymous], 1958, Mitt. Int. Ver. Theor. Angew. 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Sci. Pollut. Res.	OCT	2013	20	10					6733	6750		10.1007/s11356-012-1403-1	http://dx.doi.org/10.1007/s11356-012-1403-1			18	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	223OJ	23263760	Green Submitted, hybrid, Green Published			2025-03-11	WOS:000324815100006
J	Potvin, É; Rochon, A; Lovejoy, C				Potvin, Eric; Rochon, Andre; Lovejoy, Connie			CYST-THECA RELATIONSHIP OF THE ARCTIC DINOFLAGELLATE CYST <i>ISLANDINIUM MINUTUM</i> (DINOPHYCEAE) AND PHYLOGENETIC POSITION BASED ON SSU rDNA AND LSU rDNA	JOURNAL OF PHYCOLOGY			English	Article						Amphidiniopsis dragescoi; Archaeperidinium; Baffin Bay; Echinidinium; Herdmania litoralis; Islandinium minutum; Protoperidiniaceae; Protoperidinium minutum; round brown spiny cyst; single-cell PCR	SP-NOV DINOPHYCEAE; SUBUNIT RIBOSOMAL-RNA; SAND-DWELLING DINOFLAGELLATE; SURFACE SEDIMENTS; HYDROGRAPHIC CONDITIONS; PACIFIC-OCEAN; SPATIAL-DISTRIBUTION; POLARELLA-GLACIALIS; MOLECULAR PHYLOGENY; BEAUFORT SEA	Round brown spiny cysts constitute a morphological group common in high latitude dinoflagellate cyst assemblages. The dinoflagellate cyst Islandinium minutum (Harland et Reid) Head, Harland et Matthiessen is the main paleoecological indicator of seasonal sea-ice cover in the Arctic. Despite the importance of this cyst in paleoceanographical studies, its biological affinity has so far been unknown. The biological affinity of the species I.minutum and its phylogenetic position based on the small subunit ribosomal RNA gene (SSU rDNA) and the large subunit ribosomal RNA gene (LSU rDNA) were established from cyst incubation experiments in controlled conditions, optical and scanning electron microscopy, and single-cell PCR. The thecal motile cell obtained was undescribed. Although the motile cell was similar to Archaeperidinium minutum (Kofoid) Jorgensen, the motile cell of I.minutum lacked a transitional plate in the cingular series, which is present in Archaeperidinium spp. Islandinium minutum and Archaeperidinium spp. were paraphyletic in all phylogenetic analyses. Furthermore, Protoperidinium tricingulatum, which also lacks a transitional plate, was closely related to I.minutum and transfered to the genus Islandinium. Based on available data, it is clear that Islandinium is distinct from Archaeperidinium. Therefore, we considered Islandinium Head, Harland et Matthiessen as a non-fossil genus and emend its description, as well as the species I.minutum. This is the first description of a cyst-theca relationship and the first study that reports molecular data based on SSU rDNA and LSU rDNA on a species assigned to the genus Islandinium.	[Potvin, Eric] Seoul Natl Univ, Sch Earth & Environm Sci, Coll Nat Sci, Seoul 151747, South Korea; [Rochon, Andre] Univ Quebec, Inst Sci Mer Rimouski, Rimouski, PQ G5L 3A1, Canada; [Lovejoy, Connie] Univ Laval, Dept Biol, Quebec City, PQ G1V 0A6, Canada	Seoul National University (SNU); University of Quebec; Laval University	Potvin, É (通讯作者)，Seoul Natl Univ, Sch Earth & Environm Sci, Coll Nat Sci, Seoul 151747, South Korea.	ericpotvin@snu.ac.kr	Lovejoy, Connie/A-3756-2008	Lovejoy, Connie/0000-0001-8027-2281	Fonds de Recherche du Quebec - Nature et Technologies; Natural Sciences and Engineering Research Council of Canada; Northern Scientific Training Program from the Department of Indian Affairs and Northern Development; ArcticNet	Fonds de Recherche du Quebec - Nature et Technologies(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Northern Scientific Training Program from the Department of Indian Affairs and Northern Development; ArcticNet	We thank Dr Martin J. Head, Dr John Dodge and Dr Yuri B. Okolodkov for providing relevant comments and literature as well as the anonymous reviewers for valuable suggestions. We thank the scientists, crew, and officers from the CCGS Amundsen for there help during sampling. This article was funded by the MSc scholarship from the Fonds de Recherche du Quebec - Nature et Technologies awarded to Eric Potvin, the Natural Sciences and Engineering Research Council of Canada Discovery Grants awarded to Andre Rochon and Connie Lovejoy, the Northern Scientific Training Program from the Department of Indian Affairs and Northern Development and ArcticNet.	Abe T. H., 1981, PUBLICATIONS SETO MA, V6, P1; Abe T. 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J	Riding, JB; Michoux, D				Riding, James B.; Michoux, Daniel			Further observations on the Jurassic dinoflagellate cyst <i>Gonyaulacysta dentata</i> (Raynaud 1978) Lentin & Vozzhennikova 1990 emended Riding 2012	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Gonyaulacysta dentate; Dinoflagellate cysts; Palaeobiology; Biostratigraphy; Middle-Late Jurassic; Northern hemisphere	MIDDLE	Gonyaulacysta dentata is a large and morphologically distinctive dinoflagellate cyst. It is confined to the Late Callovian to earliest Oxfordian (Peltoceras athleta to Quenstedtoceras mariae zones) interval of the Boreal Realm and the Subboreal Province in the northern hemisphere, and has therefore been interpreted as a cold water species. The holotype of G. dentate is from the Staffin Shale Formation of Staffin Bay, Isle of Skye, northwest Scotland and has been lost. Consequently another well-preserved specimen from the Staffin Shale Formation of the Isle of Skye is proposed as a neotype. The ventral and apical areas of G. dentata are characterised by discontinuous, low, smooth sutural ridges. However, the 5"/6", 4'/6" and 4'/1' sutures on the ventral side of the epicyst are frequently indicated by relatively high denticulate crests. The 2" '/1p suture and the cingular sutures may also be developed on the ventral face. Conversely, the dorsal and lateral sutural crests, except in the apical area, are prominent and denticulate. G. dentata is present in East Greenland. Two specimens were recorded, as Gonyaulacysta eisenackii subsp. oligodentata, from the Late Callovian of Jameson Land. These are probably from the Olympen Formation, and not the Upper Vardekloft Formation as was originally stated. This occurrence is entirely consistent with the Boreal distribution of G. dentata. The range of G. dentata, the Callovian-Oxfordian transition, was characterised by significantly lowered palaeotemperatures. Several other dinoflagellate cyst species are also believed to be cold water taxa, and migrated south from the Boreal Realm into Europe at this time. (C) 2013 Natural Environment Research Council. Published by Elsevier B.V. All rights reserved.	[Riding, James B.] British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England; [Michoux, Daniel] CSTJF, F-64018 Pau, France	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Total SA; Centre Scientifique et Technique Jean Feger (CSTJF)	Riding, JB (通讯作者)，British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk			RCUK Individual Merit project; NERC [bgs05002] Funding Source: UKRI	RCUK Individual Merit project; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	Henry W. Holbrook and Keith J. Henderson (BGS) expertly drafted Figs. 1 and 2 respectively. Caroline F. Adkin kindly assisted with Plate I. Sev Kender (BGS) kindly reviewed an early draft of the manuscript. The extremely helpful input of Daniel J. Mantle (Morgan Goodall Palaeo Pty. Ltd., Australia) and an anonymous referee is acknowledged. This study was completed under the RCUK Individual Merit project entitled "Global Jurassic dinoflagellate cyst palaeobiology and its applications" awarded to James B. Riding, who publishes with the approval of the Executive Director, British Geological Survey (NERC).	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J	Carvalho, MD; Ramos, RRC; Crud, MB; Witovisk, L; Kellner, AWA; Silva, HD; Grillo, ON; Riff, D; Romano, PSR				Carvalho, Marcelo de A.; Cabral Ramos, Renato R.; Crud, Monika Beatriz; Witovisk, Luciana; Kellner, Alexander W. A.; Silva, Helder de P.; Grillo, Orlando N.; Riff, Douglas; Romano, Pedro S. R.			Palynofacies as indicators of paleoenvironmental changes in a Cretaceous succession from the Larsen Basin, James Ross Island, Antarctica	SEDIMENTARY GEOLOGY			English	Article						Paleoenvironmental reconstruction; Organic matter sedimentation; Palynofacies association; Cretaceous; James Ross Island; Antarctica	SEDIMENTARY ORGANIC-MATTER; BACK-ARC BASIN; DINOFLAGELLATE CYSTS; SEQUENCE STRATIGRAPHY; SERGIPE BASIN; GUSTAV-GROUP; SEA; CARBONATES; EVOLUTION; MARGIN	In order to reconstruct the paleoenvironment of one of the most extensive marine Cretaceous successions in the Southern Hemisphere, palynofacies analyses were conducted on 83 samples from the Whisky Bay (Albian-Turonian), Hidden Lake (Coniacian) and Santa Marta (Santonian-Campanian) formations in the Larsen Basin, James Ross Island, Antarctica. Categories of particulate organic matter were counted and investigated by cluster analysis. The trends and parameters of palynofacies constituents were used to reconstruction paleoenvironments based on the existing sedimentological interpretation. The stratigraphic distribution of the four identified palynofacies associations (A-D) reflects a continuous terrestrial influx throughout the succession. From base to top, a conspicuous increase in woody elements, especially non-opaque particles, is observed. This increase in continental elements occurs despite the presence of marine elements. This finding corroborates the sedimentological interpretation of a deeper water paleoenvironment during deposition of the Whisky Bay Formation and initiation of a shallowing-upward trend in the Hidden Lake Formation, culminating with shallow marine shelf environment of the Santa Marta Formation. (c) 2013 Published by Elsevier B.V.	[Carvalho, Marcelo de A.; Cabral Ramos, Renato R.; Crud, Monika Beatriz; Witovisk, Luciana; Kellner, Alexander W. A.; Silva, Helder de P.; Grillo, Orlando N.] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Museu Nacl, BR-20940040 Rio De Janeiro, Brazil; [Riff, Douglas] Univ Fed Uberlandia, Inst Biol, BR-38400902 Uberlandia, MG, Brazil; [Romano, Pedro S. R.] Univ Fed Vicosa, Dept Biol Anim, Museu Zool Joao Moojen, BR-36570000 Vicosa, MG, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal de Uberlandia; Universidade Federal de Vicosa	Carvalho, MD (通讯作者)，Quinta da Boa Vista S-N, BR-20940040 Rio De Janeiro, RJ, Brazil.	mcarvalho@mn.ufrj.br	Kellner, Alexander/ABE-9591-2020; Carvalho, Marcelo/G-8463-2015; Grillo, Orlando/Q-4162-2019; Riff, Douglas/B-5183-2012; Romano, Pedro/C-5093-2011	Riff, Douglas/0000-0003-0805-2828; Romano, Pedro/0000-0002-6819-2729	Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq]) [557347/2005-0, 302064/2010-9]; Research Support Foundation of Rio de Janeiro State (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Rio de Janeiro [FAPERJ]) [E-26/103.028/2008]; Research Center of Petrobras (Centro de Pesquisa Miguez, Petroleo Brasileiro [CENPES-PETROBRAS]) [CENPES 10292]	Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq])(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Research Support Foundation of Rio de Janeiro State (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Rio de Janeiro [FAPERJ])(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Research Center of Petrobras (Centro de Pesquisa Miguez, Petroleo Brasileiro [CENPES-PETROBRAS])	This project was primarily funded by the Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq] grant nos. 557347/2005-0 and 302064/2010-9 to M. Carvalho), the Research Support Foundation of Rio de Janeiro State (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Rio de Janeiro [FAPERJ] grant no. E-26/103.028/2008 to M. Carvalho) and the Research Center of Petrobras (Centro de Pesquisa Miguez, Petroleo Brasileiro [CENPES-PETROBRAS] grant no. CENPES 10292 to M. Carvalho). We wish to thank the Brazilian Navy for logistical and technical support during the expedition to Antarctica.	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Geol.	SEP 15	2013	295						53	66		10.1016/j.sedgeo.2013.08.002	http://dx.doi.org/10.1016/j.sedgeo.2013.08.002			14	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	234SV					2025-03-11	WOS:000325665500004
J	Heinrich, S; Zonneveld, KAF				Heinrich, S.; Zonneveld, K. A. F.			Influence of the Amazon River development and constriction of the Central American Seaway on Middle/Late Miocene oceanic conditions at the Ceara Rise	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Calcareous dinoflagellate cysts; Middle-Late Miocene; Ceara Rise; Amazon River; Central American Seaway; Ocean circulation	CALCAREOUS DINOFLAGELLATE CYSTS; DEEP-WATER CIRCULATION; MARIA INES RAMOS; WERNER E. PILLER; SURFACE SEDIMENTS; ATLANTIC-OCEAN; SOLIMOES FORMATION; MARTIN GROSS; SOUTH; ENVIRONMENTS	Sediment samples from ODP 154 Site 926A (Ceara Rise, western equatorial Atlantic Ocean) spanning the Neogene from 12.8 to 9.2 Ma were investigated on their calcareous dinoflagellate contents to better understand the oceanographic changes in relation to the closure of the Central American Seaway and the development of the Amazon River. Intervals with increased cyst accumulation rates and dissolution sensitive species occur from 12.4 Ma onward. They correspond to periods of enhanced North Atlantic Deep Water production indicating the presence of this water mass at the research site during these intervals. This suggests that pulses of North Atlantic Deep waters sporadically flew into the South Atlantic related to uplift phases of the Panama Sill. At about 11.2 Ma the first appearance of Leonella granifera indicates river influence at the sample site. This first indication of river influence in the western equatorial Atlantic can be linked to the developing Amazon River. The cyst association changes at about 11.2 Ma from almost monospecific to highly diverse and the permanent presence and increased abundance of L granifera suggest that river waters were able to reach the study site by now, probably as a result of the southward flowing North Brazil Current. After 10.5 Ma the cyst association indicates a decrease in Amazon influence at Site 926A. This change can be correlated to a reducing inflow of Pacific waters through the Central American Seaway leading to a reverse of the North Brazil Current to its modern northwards flow pattern. (C) 2013 Elsevier B.V. All rights reserved.	[Heinrich, S.; Zonneveld, K. A. F.] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; [Zonneveld, K. A. F.] Univ Bremen, MARUM, Ctr Marine Environm Sci, D-28359 Bremen, Germany	University of Bremen; University of Bremen	Zonneveld, KAF (通讯作者)，Univ Bremen, Dept Geosci, POB 330 440, D-28334 Bremen, Germany.	zonnev@uni-bremen.de		Heinrich, Sonja/0000-0001-7536-0017	DFG	DFG(German Research Foundation (DFG))	We thank Inga Preiss-Daimler for making the carbonate mass accumulation rates available. Thanks are also given to the members of the working group of Historical Geology and Palaeontology and Division of Marine Palynology for their general assistance and helpful discussions. We thank two anonymous reviewers for their helpful comments and Gerard Versteegh for correcting the English. This research was carried out within the framework of the International Graduate College: Proxies in Earth History (EUROPROX) and the DFG funded research centre MARUM.	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Paleoclimatol. Paleoecol.	SEP 15	2013	386						599	606		10.1016/j.palaeo.2013.06.026	http://dx.doi.org/10.1016/j.palaeo.2013.06.026			8	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	223YQ					2025-03-11	WOS:000324848800046
J	Gu, HF; Kirsch, M; Zinssmeister, C; Soehner, S; Meier, KJS; Liu, TT; Gottschling, M				Gu, Haifeng; Kirsch, Monika; Zinssmeister, Carmen; Soehner, Sylvia; Meier, K. J. Sebastian; Liu, Tingting; Gottschling, Marc			Waking the Dead: Morphological and Molecular Characterization of Extant †<i>Posoniella tricarinelloides</i> (Thoracosphaeraceae, Dinophyceae)	PROTIST			English	Article						Calcareous dinoflagellates; cyst; distribution; molecular systematics; theca; ultrastructure	SP-NOV DINOPHYCEAE; CALCAREOUS DINOFLAGELLATE CYSTS; SCRIPPSIELLA-TROCHOIDEA; PHYLOGENETIC POSITION; SURFACE SEDIMENTS; RIBOSOMAL-RNA; LIFE-CYCLE; COMB-NOV; PERIDINIALES; CALCIODINELLOIDEAE	The Thoracosphaeraceae are dinophytes that produce calcareous shells during their life history, whose optical crystallography has been the basis for the division into subfamilies. To evaluate the validity of the classification (mainly applied by palaeontologists), living material of phylogenetic key species is necessary albeit frequently difficult to access for contemporary morphological and molecular analyses. We isolated and established five living strains of the rare fossil-taxon dagger Posoniella tricarinelloides from different sediment samples collected in the South China Sea, Yellow Sea and in the Mediterranean Sea (west coast off Italy). Here, we provide detailed descriptions of its morphology and conducted phylogenetic analyses based on hundreds of accessions and thousands of informative sites on concatenated rRNA datasets. Within the monophyletic Peridiniales, dagger P. tricarinelloides was reliably nested in the Thoracosphaeraceae and exhibited two distinct morphological types of coccoid cells. The two morphologies of coccoid cells would have been assigned to different taxa at the subfamily level if found separately in fossil samples. Our results thus challenge previous classification concepts within the dinophytes and underline the importance of comparative morphological and molecular studies to better understand the complex biology of unicellular organisms such as dagger P. tricarinelloides. (c) 2013 Elsevier GmbH. All rights reserved.	[Gu, Haifeng; Liu, Tingting] State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Kirsch, Monika] Univ Bremen, Fachbereich Geowissensch, Fachrichtung Hist Geol Palaontol, D-28359 Bremen, Germany; [Zinssmeister, Carmen; Soehner, Sylvia; Gottschling, Marc] Univ Munich, Dept Biol Systemat Bot & Mykol, GeoBioctr, D-80638 Munich, Germany; [Zinssmeister, Carmen; Soehner, Sylvia] Free Univ Berlin, Fachbereich Geol Wissensch, Fachrichtung Palaontol, D-12249 Berlin, Germany; [Meier, K. J. Sebastian] Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany	Third Institute of Oceanography, Ministry of Natural Resources; University of Bremen; University of Munich; Free University of Berlin; University of Kiel	Gottschling, M (通讯作者)，Univ Munich, Dept Biol Systemat Bot & Mykol, GeoBioctr, Menzinger Str 67, D-80638 Munich, Germany.	gottschling@biologie.uni-muenchen.de	Gottschling, Marc/K-2186-2014; Gu, Haifeng/ADN-4528-2022; Meier, K. J. Sebastian/H-7914-2014	Gu, Haifeng/0000-0002-2350-9171; 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))	The work was supported by the Deutsche Forschungsgemeinschaft (grant numbers KE 322/36, RI 1738/5 and WI 725/25). We thank three anonymous reviewers and the Monitoring Editor editor Mona Hoppenrath (Wilhelmshaven) for valuable comments on a previous version of the manuscript.	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F., 2005, Palaeontologische Zeitschrift, V79, P61	90	31	33	1	32	ELSEVIER GMBH	MUNICH	HACKERBRUCKE 6, 80335 MUNICH, GERMANY	1434-4610			PROTIST	Protist	SEP	2013	164	5					583	597		10.1016/j.protis.2013.06.001	http://dx.doi.org/10.1016/j.protis.2013.06.001			15	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	227GA	23850812				2025-03-11	WOS:000325098000001
J	Shin, HH; Lim, D; Park, SY; Heo, S; Kim, SY				Shin, Hyeon Ho; Lim, Dhongil; Park, Soung-Yun; Heo, Seung; Kim, So-Young			Distribution of dinoflagellate cysts in Yellow Sea sediments	ACTA OCEANOLOGICA SINICA			English	Article						Yellow Sea; dumping site; dinoflagellate cyst; Alexandrium catenella/tamarense type; Operculodinium centrocarpum	CHANGJIANG DILUTED WATER; EAST CHINA SEAS; SURFACE SEDIMENTS; PROTOCERATIUM-RETICULATUM; SPATIAL-DISTRIBUTION; WARM CURRENT; TOKYO-BAY; EUTROPHICATION; TEMPERATURE; SALINITY	To investigate the distribution, abundance, and species composition of dinoflagellate cysts in the Yellow Sea, surface sediment samples were collected at 37 sites, including the Korean dump site. Twenty-one dinoflagellate cyst taxa were identified, with the assemblages dominated mainly by Spiniferites bulloideus, Operculodinium centrocarpum, and cyst of Alexandrium catenella/tamarense type. A high frequency of O. centrocarpum in the Yellow Sea was observed for the first time, and it is likely that this can be attributed to the dynamics of the Yellow Sea Cold Water Mass and the Changjiang (Yangtze) River runoff. Total cyst concentrations ranged from 23 to 48 442 cysts/g dry weight, and high cyst concentrations were recorded adjacent to the dumping site. This result suggests that anthropogenic activities such as ocean dumping stimulate the growth of dinoflagellates in the Yellow Sea, which in turn leads to high levels of dinoflagellate cyst production.	[Shin, Hyeon Ho; Lim, Dhongil] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea; [Park, Soung-Yun; Heo, Seung] Natl Fisheries Res & Dev Inst, West Sea Fisheries Res Inst, Inchon 400420, South Korea; [Kim, So-Young] Korea Polar Res Inst, Div Polar Climate Res, Inchon 406840, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); Korea Polar Research Institute (KOPRI)	Kim, SY (通讯作者)，Korea Polar Res Inst, Div Polar Climate Res, Songdomiraero 26, Inchon 406840, South Korea.	kimsy@kopri.re.kr	Lim, Dhongil/ACH-3964-2022; Kim, So-Young/JFS-7698-2023	Lim, Dhongil/0000-0002-0832-2907; Shin, Hyeon Ho/0000-0002-9711-6717	Korea Ocean Research and Development Institute [PE99165]; Korea-China Cooperative Project on the Yellow Sea Cold Water Mass	Korea Ocean Research and Development Institute; Korea-China Cooperative Project on the Yellow Sea Cold Water Mass	Part of the Korea-China Cooperative Project on the Yellow Sea Cold Water Mass; a grant from the Korea Ocean Research and Development Institute (PE99165); the samples were partly supplied from NFRDI (RP-2012-ME-051).	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Sin.	SEP	2013	32	9					91	98		10.1007/s13131-013-0356-7	http://dx.doi.org/10.1007/s13131-013-0356-7			8	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	221CY					2025-03-11	WOS:000324636300011
J	Warns, A; Hense, I; Kremp, A				Warns, Alexandra; Hense, Inga; Kremp, Anke			Encystment of a cold-water dinoflagellate - From in vitro to in silico	JOURNAL OF MARINE SYSTEMS			English	Article						Life cycle; Cyst formation; Seed population; Growth; Dinoflagellates	NORTHERN BALTIC SEA; SCRIPPSIELLA-HANGOEI; CYST FORMATION; RESTING CYSTS; POPULATION-DYNAMICS; SPRING-BLOOM; LIFE-CYCLE; CULTURE; GROWTH; DINOPHYCEAE	Blooms of dinoflagellates are frequently observed in coastal regions. The dynamics of these blooms are strongly affected by life cycle transitions. For example, many species form resting cysts at the end of the growth period that act as a seed population. Despite considerable efforts, one major process of the dinoflagellate life cycle - the encystment - is not fully understood. In this study, we reanalyse a published laboratory data set for the cold-water dinoflagellate Biecheleria baltica and develop a numerical model to study cyst formation. We find significant differences between cell counts and biomass, leading to different conclusions about the encystment process. To accurately reproduce the laboratory data, two mechanisms have to be taken into account in the model: a time lag in cyst formation and a reduction in the growth rate of vegetative cells as soon as cysts are formed. Using this model we are able to identify and formalise the functional dependence among growth, cyst formation, and environmental factors. Our model can serve as a prerequisite for dinoflagellate life cycle models to study the dynamics of bloom formations. (c) 2012 Elsevier B.V. All rights reserved.	[Warns, Alexandra; Hense, Inga] Univ Hamburg, Inst Hydrobiol & Fisheries Sci, D-22767 Hamburg, Germany; [Kremp, Anke] Finnish Environm Inst SYKE, Ctr Marine Res, Helsinki 00251, Finland	University of Hamburg; Finnish Environment Institute	Warns, A (通讯作者)，Univ Hamburg, Inst Hydrobiol & Fisheries Sci, KlimaCampus, D-22767 Hamburg, Germany.	alexandra.warns@zmaw.de	Kremp, Anke/I-8139-2013		Cluster of Excellence "CliSAP", University of Hamburg [EXC177]; German Science Foundation (DFG)	Cluster of Excellence "CliSAP", University of Hamburg; German Science Foundation (DFG)(German Research Foundation (DFG))	This study has been supported through the Cluster of Excellence "CliSAP" (EXC177), University of Hamburg, funded through the German Science Foundation (DFG). We thank M. Pahlow for his helpful comments on the paper. The suggestions of two anonymous reviewers are acknowledged.	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J	Paez-Reyes, M; Head, MJ				Paez-Reyes, Manuel; Head, Martin J.			THE CENOZOIC GONYAULACACEAN DINOFLAGELLATE GENERA <i>OPERCULODINIUM</i> WALL, 1967 AND <i>PROTOCERATIUM</i> BERGH, 1881 AND THEIR PHYLOGENETIC RELATIONSHIPS	JOURNAL OF PALEONTOLOGY			English	Article							HARMFUL ALGAL BLOOMS; PLEISTOCENE SERIES/EPOCH; QUATERNARY SYSTEM/PERIOD; RECENT SEDIMENTS; NORTH-SEA; CYSTS; RETICULATUM; DINOPHYCEAE; MORPHOLOGY; SALINITY	To clarify the systematic positions of the important gonyaulacacean genera Operculodinium Wall, 1967 emend. Matsuoka et al., 1997 and Protoceratium Bergh, 1881, we present in detail the tabulation of the Oligocene- Pleistocene, thermophilic, cyst-defined species Operculodinium bahamense Head in Head and Westphal, 1999 emend., and the extant, cosmopolitan, theca-defined species Protoceratium reticulatum (Claparede and Lachmann, 1859) Butschli, 1885. Both species have a sexiform hyposomal tabulation, and L-type (Protoceratium reticulatum) or modified L-type (Operculodinium bahamense) ventral organization. Protoceratium reticulatum has dextral torsion of the hypotheca, requiring assignation of the genus to the subfamily Cribroperidinioideae Fensome et al., 1993, whereas Operculodinium bahamense has neutral torsion requiring assignation to the subfamily Leptodinioideae Fensome et al., 1993. The stratigraphic range of this subfamily is now extended upwards to the lower Pleistocene. Paradoxically, Protoceratium reticulatum produces a cyst whose morphology is circumscribed by the cyst-defined genus Operculodinium, either implying polyphyletic origins for this genus or that combinations of ventral organization and torsion used to subdivide the family Gonyaulacaceae cannot always be applied rigidly. In detail, Operculodinium bahamense is shown to have an unusual ventral tabulation in which the first apical plate contacts the apical pore complex but not the sulcus. The new term "episert" is proposed to describe this plate relationship, which appears to have evolved independently in several lineages of the suborder Gonyaulacineae.	[Paez-Reyes, Manuel; Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Paez-Reyes, Manuel] Smithsonian Trop Res Inst, Balboa, Ancon, Panama	Brock University; Smithsonian Institution; Smithsonian Tropical Research Institute	Paez-Reyes, M (通讯作者)，Brock Univ, Dept Earth Sci, 500 Glenridge Ave, St Catharines, ON L2S 3A1, Canada.	manuel.paez@gmail.com; mjhead@broku.ca			Natural Sciences and Engineering Research Council of Canada; Brock University; Smithsonian Tropical Research Institute	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Brock University; Smithsonian Tropical Research Institute(Smithsonian InstitutionSmithsonian Tropical Research Institute)	We thank M. Hoppenrath (DZMB, Forschungsinstitut Senckenberg) for making available published and unpublished microphotographs of Protoceratium reticulatum, and K. Mertens (Ghent University) for bringing our attention to some of the older literature. K. Matsuoka (Nagasaki University) and K. Mertens provided helpful comments on the episert condition in extant species. The Integrated Ocean Drilling Program provided the samples for this research. MJH acknowledges support from a Discovery Grant of the Natural Sciences and Engineering Research Council of Canada. MP-R is grateful to Brock University and the Smithsonian Tropical Research Institute for financial support at various stages of this research. Mr. Jorge Ceballos (Smithsonian Tropical Research institute) helped with SEM photography. Helpful reviews of the manuscript by L. E. Edwards and J. Lucas-Clark are greatly appreciated, especially insightful comments from L. E. Edwards regarding the episert condition.	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J	Bijl, PK; Sluijs, A; Brinkhuis, H				Bijl, Peter K.; Sluijs, Appy; Brinkhuis, Henk			A magneto- and chemostratigraphically calibrated dinoflagellate cyst zonation of the early Palaeogene South Pacific Ocean	EARTH-SCIENCE REVIEWS			English	Article						Southern Ocean; Palaeogene; Organic-walled dinoflagellate cysts (dinocysts); Stratigraphy; Zonation	MIDDLE EOCENE; CONTINENTAL-MARGIN; NEW-ZEALAND; SEA-LEVEL; PALEOCENE; OLIGOCENE; CLIMATE; GENERA; TEMPERATURES; ASSEMBLAGES	Investigation of the early Palaeogene palaeoecological and palaeoclimatological evolution of the Polar Regions is hindered by the absence of calcite microfossils in sedimentary archives, which are conventionally the main dating tool. To overcome this problem, we have generated large datasets of organic dinoflagellate cyst (dinocyst) assemblages from Southern Ocean shelf sediments over the past decade, and we here calibrate these to the Geomagnetic Polarity Time Scale (GPTS) using magnetostratigraphy and stable isotope stratigraphy. This now for the first time allows a high-resolution Southern Pacific Ocean dinocyst zonation for the late Palaeocene to late Eocene (58-36 million years ago; Ma). We compile published dinocyst chronologies from Ocean Drilling Program COOP) Hole 11710 on the South Tasman Rise, Hole 1172A/D on the East Tasman Plateau and Integrated Ocean Drilling Program (IODP) Hole U1356A on the Wilkes Land margin. Correlation to dinocyst zonations from New Zealand lead to revisions of the magnetostratigraphic age model at Holes 1171D and 1172A/D. Stable carbon and oxygen isotope records reveal the stratigraphic location of the Palaeocene-Eocene Thermal Maximum (similar to 56 Ma) and the Middle Eocene Climatic Optimum (similar to 40 Ma), respectively. The resulting zonation consists of thirteen dinocyst zones, calibrated to the Geomagnetic Polarity Time Scale (GPTS) of Vandenberghe et al. (2012), which can likely be applied to the entire Southern Ocean. Finally, we apply the revised stratigraphy to all published TEX86 data, a biomarker-based proxy for sea surface temperature (SST), from ODP Site 1172 to assess long-term climate evolution. This shows that Southwest Pacific SST trends mimic the global compilation of benthic foraminiferal oxygen isotopes even better than previously appreciated. (C) 2013 Elsevier B.V. All rights reserved.	[Bijl, Peter K.; Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Dept Earth Sci, Fac Geosci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands	Utrecht University	Bijl, PK (通讯作者)，Univ Utrecht, Dept Earth Sci, Fac Geosci, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	p.k.bijl@uu.nl	Brinkhuis, Henk/IUO-8165-2023; Sluijs, Appy/B-3726-2009	Brinkhuis, Henk/0000-0003-0253-6610; Bijl, Peter/0000-0002-1710-4012; Sluijs, Appy/0000-0003-2382-0215	NSF; Utrecht University; LPP Foundation; Netherlands Organization for Scientific Research [863.07.001]; European Research Council under the European Community [259627]	NSF(National Science Foundation (NSF)); Utrecht University; LPP Foundation; Netherlands Organization for Scientific Research(Netherlands Organization for Scientific Research (NWO)); European Research Council under the European Community(European Research Council (ERC))	This research used samples and data provided by the Ocean Drilling Program (ODP) and the Integrated Ocean Drilling Program (IODP), both sponsored by NSF and participating countries under management of Joint Oceanographic Institutions Inc. We thank Erica Crouch, Jorg Pross and Alexander J.P. Houben for useful discussions, Frits Hilgen for providing the GTS time scale, and Natasja Welters and Jan van Tongeren for laboratory assistance and scanning-electron-microscope photography, respectively. We thank Utrecht University, the LPP Foundation (P.K.B.) and the Netherlands Organization for Scientific Research (Veni grant 863.07.001 to A.S.) for financial support. A.S. also acknowledges the European Research Council under the European Community's Seventh Framework Program for ERC Starting Grant 259627.	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Rev.	SEP	2013	124						1	31		10.1016/j.earscirev.2013.04.010	http://dx.doi.org/10.1016/j.earscirev.2013.04.010			31	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	217IA		Green Published			2025-03-11	WOS:000324352000001
J	Jauzein, C; Erdner, DL				Jauzein, Cecile; Erdner, Deana L.			Stress-related Responses in <i>Alexandrium tamarense</i> Cells Exposed to Environmental Changes	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Apoptosis; caspase-like enzymes; cell cycle; dinoflagellate; metacaspases; physico-chemical challenge; reactive oxygen species; temporary cyst	UNICELLULAR CHLOROPHYTE; TOXIC DINOFLAGELLATE; LEISHMANIA-MAJOR; KARENIA-BREVIS; DEATH; CASPASES; METACASPASES; APOPTOSIS; CYCLE; ADAPTATION	Organisms tend to be sensitive to drastic changes in environmental conditions. For unicellular microorganisms, variations in physico-chemical conditions are particularly challenging and may result in acclimation, entrance into quiescence, or death through necrotic or autocatalytic pathways. This study focuses on the thecate dinoflagellate Alexandrium tamarense. Cellular responses to oxidative, thermal, and nutrient stress were characterized using stress indicators, such as pigment content, efficiency of photosystem II or production of reactive oxygen species (ROS), as well as hallmarks of apoptosis including activity of caspase-like enzymes and expression of a metacaspase gene homolog. The formation of temporary cysts, a survival strategy of short-term quiescence, was also monitored. Cellular responses appeared to depend on multifactorial influences where type and intensity of stimulus as well as position in cell cycle may act in combination. Sequences of events observed implicate ROS production as a key determinant of stress-related pathways, playing potential roles in intracellular signaling, formation of temporary cysts, or cellular damage. Variations observed in caspase-like activities and metacaspase gene expression did not appear to be associated with programmed cell death pathways; our results suggest a wider range of functions for these proteases in phytoplankton cells, including roles in survival pathways and cell cycle progression.	[Jauzein, Cecile; Erdner, Deana L.] Univ Texas, Inst Marine Sci, Port Aransas, TX 78373 USA	University of Texas System	Erdner, DL (通讯作者)，Univ Texas, Inst Marine Sci, 750 Channel View Dr, Port Aransas, TX 78373 USA.	derdner@utexas.edu	; Erdner, Deana/C-4981-2008	Jauzein, Cecile/0000-0001-6291-6821; Erdner, Deana/0000-0002-1736-8835	National Oceanic and Atmospheric Administration Center for Sponsored Coastal Ocean Research [NA09NOS4780166]	National Oceanic and Atmospheric Administration Center for Sponsored Coastal Ocean Research(National Oceanic Atmospheric Admin (NOAA) - USA)	This article is a result of research funded by the National Oceanic and Atmospheric Administration Center for Sponsored Coastal Ocean Research under award no. NA09NOS4780166 to the University of Texas Marine Science Institute. The authors are grateful to Dr. Yun hee Park for nutrient and pigment analyses. We also acknowledge Dr. Ludovic "Chou" Donaghy for his constructive comments. This is ECOHAB contribution no. 752.	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Eukaryot. Microbiol.	SEP	2013	60	5					526	538		10.1111/jeu.12065	http://dx.doi.org/10.1111/jeu.12065			13	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	213XT	23865757				2025-03-11	WOS:000324094600009
J	Gómez, F; Artigas, LF				Gomez, Fernando; Artigas, Luis Felipe			The formation of the twin resting cysts in the dinoflagellate <i>Dissodinium pseudolunula</i>, a parasite of copepod eggs	JOURNAL OF PLANKTON RESEARCH			English	Article						Dinophyceae; life cycle; overwintering cyst; parasitism; resting spores	DINOPHYTA	The dinoflagellate Dissodinium pseudolunula is the most common and widespread ecto-parasite of copepod eggs in neritic waters. When the host is absent, the species survives with a distinctive pair of twin resting cysts described as Pyrocystis margalefii. Based on live samples, the formation of the twin resting cysts is illustrated here for the first time. The gymnodinioid infective cells did not form overwintering cysts under unfavourable conditions. These are formed inside the secondary lunate sporangium.	[Gomez, Fernando; Artigas, Luis Felipe] ULCO, MREN, CNRS, UMR 8187,LOG, F-62930 Wimereux, France; [Gomez, Fernando] Univ Sao Paulo, Lab Plankton Syst, Oceanog Inst, BR-05508120 Sao Paulo, Brazil	Universite du Littoral-Cote-d'Opale; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universidade de Sao Paulo	Gómez, F (通讯作者)，ULCO, MREN, CNRS, UMR 8187,LOG, 32 Av Foch, F-62930 Wimereux, France.	fernando.gomez@fitoplancton.com	Artigas, Luis/L-1264-2016; Gomez, Fernando/B-2495-2009	Gomez, Fernando/0000-0002-5886-3488; Artigas, Luis Felipe/0000-0003-0512-5315	UL1 post-doctoral grant; CNRS convention of research on phytoplankton; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [BJT 370646/2013-14]	UL1 post-doctoral grant; CNRS convention of research on phytoplankton; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	F.G. was supported by a UL1 post-doctoral grant and a CNRS convention of research on phytoplankton. F. G. is currently supported by the Brazilian contract BJT 370646/2013-14 of Conselho Nacional de Desenvolvimento Cientifico e Tecnologico.	[Anonymous], 1989, ADV MAR BIOL, DOI DOI 10.1016/S0065-2881(08)60189-3; Cachon J., 1987, Botanical Monographs (Oxford), V21, P571; Coats DW, 2010, J EUKARYOT MICROBIOL, V57, P468, DOI 10.1111/j.1550-7408.2010.00504.x; Coats DW, 1999, J EUKARYOT MICROBIOL, V46, P402, DOI 10.1111/j.1550-7408.1999.tb04620.x; DREBES G, 1984, HELGOLANDER MEERESUN, V37, P603; DREBES G, 1981, BRIT PHYCOL J, V16, P207, DOI 10.1080/00071618100650211; DREBES G, 1978, BRIT PHYCOL J, V13, P319, DOI 10.1080/00071617800650381; Gómez F, 2011, ACTA PROTOZOOL, V50, P255, DOI 10.4467/16890027AP.11.024.0024; Gómez F, 2009, EUR J PROTISTOL, V45, P260, DOI 10.1016/j.ejop.2009.05.004; JOHN AWG, 1983, BRIT PHYCOL J, V18, P61, DOI 10.1080/00071618300650071; Mauchline J, 1998, ADV MAR BIOL, V33, P1; Pouchet G., 1885, J ANAT PHYSIOL, V21, P28	12	6	6	1	25	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	SEP-OCT	2013	35	5					1167	1171		10.1093/plankt/fbt066	http://dx.doi.org/10.1093/plankt/fbt066			5	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	212FC		Green Published, Bronze			2025-03-11	WOS:000323966900019
J	Al-Obaidi, RY; Al-Ameri, TK; Al-Khafaji, AJ				Al-Obaidi, Ryadh Younis; Al-Ameri, Thamer Khazal; Al-Khafaji, Amer Jassim			Palynofacies, palaeoenvironment, and source rocks evaluation of Ratawi Formation, Southern Iraq	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Palynofacies; Palaeoenvironment; Petroleum potential; Ratawi formation; South Iraq	PROGRAMMED PYROLYSIS; OIL; GENERATION; MARINE; BASINS	Palynological analysis were done on 12 rock samples for Ratawi Formation from Rumailah well 131 and eight samples for the same formation from Zubair well 47, South Iraq, to extract sedimentary organic matters. Microscopic examination led to diagnose large numbers of spores, pollen, dinoflagellates (proximat, cavate, and chorate), foraminifera, melanogen, hylogen, and amorphogen. Three palynological facies were determined on the bases of percentages of sedimentary organic matter and palynomorphs from two sections. Analysis of these palynofacies clarified Ratawi Formation as deposited from environments ranging from delta and lagoon (suboxic-dysoxic) to shelf facies (anoxic near the shore-suboxic) with the presence of some layers deposited from semideep open marine environment (bathyal). Organic geochemical analysis of total organic carbon and Rock Eval pyrolysis were done to determine quantity, quality, and degree of maturation of the kerogen. Poor to medium proportion of total organic carbon of kerogen types II and III within a catagenesis stage are recorded in these rocks, and hence, poor hydrocarbon generation could be suggested for these strata.	[Al-Obaidi, Ryadh Younis] Univ Baghdad, Coll Sci Women, Dept Phys, Baghdad, Iraq; [Al-Ameri, Thamer Khazal] Univ Baghdad, Coll Sci, Dept Geol, Baghdad, Iraq; [Al-Khafaji, Amer Jassim] Univ Baghdad, Coll Sci Women, Dept Chem, Baghdad, Iraq	University of Baghdad; University of Baghdad; University of Baghdad	Al-Obaidi, RY (通讯作者)，Univ Baghdad, Coll Sci Women, Dept Phys, Baghdad, Iraq.	ryadhyounis99@yahoo.com	/B-9812-2016	/0000-0001-8489-394X				Al-Ameri TK, 2009, GEOARABIA, V14, P91; Al-Jibori NMM, 1994, THESIS U BAGHDAD; [Anonymous], 1977, QUESTIONS PHYTOSTRAT; Auchi WM, 1990, THESIS U SALAHDDIN; Bujack JP, 1977, OIL GAS J, V75, P193; CLAYPOOL GE, 1976, AAPG BULL, V60, P608; CLEMENTZ DM, 1979, AAPG BULL, V63, P2227; CLEMENTZ DM, 1979, OFFSHORE TECHNOL C, V1, P465; Downie C., 1971, Geoscience Man, V3, P29; ESPITALIE J, 1980, AAPG BULL, V64, P59; HARLAND R, 1973, Palaeontology (Oxford), V16, P665; Horsfield B., 1985, Advances in Petroleum Geochemistry, V1, P247; Jude EO, 2011, J PET COAL, V53, P35; Leythaeuser D, 1983, ADV ORG GEOCHEM, P136; PETERS KE, 1986, AAPG BULL, V70, P318; PETERS KE, 1983, AAPG BULL, V67, P2137; PITMAN JK, 1987, AAPG BULL, V71, P76; SAVRDA CE, 1984, AAPG BULL, V68, P1179; SCOTT RW, 1977, CRETACEOUS CARBONATE, V89, P169; STEIN R, 1986, MAR GEOL, V72, P199, DOI 10.1016/0025-3227(86)90119-2; THOMPSON CL, 1986, INT J COAL GEOL, V6, P229, DOI 10.1016/0166-5162(86)90003-0; TISSOT BP, 1987, AAPG BULL, V71, P1445; Tyson RV, 1993, APPL MICROPALAEONTOL, P91; Tyson RV, 1995, SEDIMENTARY ORGANIC, VXviii, P615; Uwins PJ, 1988, EARLY MIDCRETACEOUS, P215; VIDAL G, 1988, Palynology, V12, P215; WATERHOUSE HK, 1995, GEOLOGICAL SOC LONDO, V85, P75	27	3	4	0	6	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511			ARAB J GEOSCI	Arab. J. Geosci.	SEP	2013	6	9					3303	3312		10.1007/s12517-012-0613-7	http://dx.doi.org/10.1007/s12517-012-0613-7			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	202NW					2025-03-11	WOS:000323225400013
J	Jasim, SY				Jasim, Sahar Y.			The potential of hydrocarbons generation in the Chia Gara Formation at Amadia area, north of Iraq	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Source rocks; Palynomorphs; Hydrocarbon generation; North Iraq	SOUTHERN IRAQ; KEROGENS	Sixteen rock samples of outcrop of Chia Gara Formations from the type locality area, south of Amadia, North Iraq showed evidences for hydrocarbon generation potential by palynological studies. These analyses include age assessment of Upper Jurassic (Tithonian) to Lower Cretaceous (Berriasian) age based on assemblages of mainly dinoflagellate cyst constituents. Qualitative studies are done in this study by textural microscopy used in assessing amorphous organic matter for palynofacies type belong to kerogen type A of Thompson and Dembiki (Int J Coal Geol 6: 229-249, 1986) which contain brazinophyte algae, Tasmanites, and foraminifera test linings, as well as the dinoflagellate cysts and spores, deposited in dysoxic-anoxic environment. The palynomorphs are of dark orange and light brown, on the spore species Cyathidites australis, that indicate mature organic matters with thermal alteration index of 2.7-3.0 by Staplin's scale. These characters and total organic carbon of 0.5-8.5 wt% have rated the succession as a source rock for high efficiency for generation and expulsion of oil with ordinate gas that charged mainly oil fields of Tawqi. Some oil is released from the Chia Gara Formation to charge the Cretaceous-Tertiary total petroleum system.	Univ Baghdad, Coll Sci, Dept Geol, Baghdad, Iraq	University of Baghdad	Jasim, SY (通讯作者)，Univ Baghdad, Coll Sci, Dept Geol, Baghdad, Iraq.	umyounis@yahoo.com	Y.Jasim, Sahar/R-5992-2019					Al-Ameri TK, 2009, GEOARABIA, V14, P91; Al-Ameri TK, 1999, CRETACEOUS RES, V20, P359, DOI 10.1006/cres.1999.0157; Al-Ameri TK, 1992, IRAQ J SCI, V36, P672; Al-Ameri TK, 2001, ARAB J GEOSCI SPRING, V4, P915; [Anonymous], DANMARKS GEOLOGISK B; Aqrawi AAM, 2010, PETROLEUM GEOLOGY IR, P440; BARS MS, 1973, GEOLOGICAL SURVEY CA, P25; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Bordenave ML., 1993, APPL PETROLEUM GEOCH, P524; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; HELBY R, 1987, STUDIES AUSTR MESOZO, V4, P1; Hunt JM, 1997, PETROLEUM GEOCHEMIST, P743; MILLIOUD ME, 1975, AM ASS STRATIGRAPHIC, V4, P65; Pollastro R.M., 1999, 97470B US GEOL SURV, DOI 10.3133/ofr97470B; RAHMAN M, 1995, J PETROL GEOL, V18, P91, DOI 10.1111/j.1747-5457.1995.tb00743.x; 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; Thusu B, 1985, J MICROPALAEONTOL, V10, P131; Thusu B, 1995, J MICROPALAEONTOL, V4, P113; Tissot B. P., 1984, 2nd ed. Berlin: Springer; Tyson R.V., 1993, Applied Micropalaeontology, P153, DOI [10.1007/978-94-017-0763-35, DOI 10.1007/978-94-017-0763-35]; Tyson RV., 1995, SEDIMENTARY ORGANIC, P615, DOI [DOI 10.1007/978-94-011-0739-6, 10.1007/978-94-011-0739-6]; Van Bellen R.C., 1959, INT GEOL CONG COMSTR, VIII, P333	24	4	4	0	3	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511			ARAB J GEOSCI	Arab. J. Geosci.	SEP	2013	6	9					3313	3318		10.1007/s12517-012-0619-1	http://dx.doi.org/10.1007/s12517-012-0619-1			6	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	202NW					2025-03-11	WOS:000323225400014
J	Mathews, RP; Tripathi, SM; Banerjee, S; Dutta, S				Mathews, Runcie P.; Tripathi, Suryakant M.; Banerjee, Santanu; Dutta, Suryendu			Palynology, palaeoecology and palaeodepositional environment of Eocene lignites and associated sediments from Matanomadh mine, Kutch Basin, western India	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						Palynomorphs; Eocene lignites; Matanomadh; Kutch Basin; Gujarat	PHYLOGENY	Extensive Cenozoic lignite-bearing sediments in the western part of Kutch, western India provide a unique opportunity to study the floral diversity at a crucial time of early Eocene Climatic Optimum (EECO). Rock samples representing a lignite-bearing sequence from the open cast mine at Matanomadh, Gujarat, western India were collected to study the palynofloral composition and to interpret the palaeoclimate and environment of deposition. The sequence mainly composed of lignites, shales and calcareous mudstones yielded rich assemblage consists of pteridophytic spores (7 genera, 10 species), angiosperm pollens (20 genera, 26 species), fungal remains (14 genera, 16 species) and dinoflagellate cysts. The palynofloral assemblage is marked with dominance of angiospermic pollen, particularly those having affinity with the family Arecaceae. Occurrence of fungal remains in high abundance is also noticed. Based on palynomorph contents, the studied sequence is divisible into two palynozones. It is inferred that lower part of the sequences was deposited in a near-shore environment with intermittent marine incursions whereas the depositional regime of upper part was shallow marine. The climate is found to be tropical-subtropical, humid with heavy precipitation during the deposition of Matanomadh lignite-bearing sequence.	[Mathews, Runcie P.; Banerjee, Santanu; Dutta, Suryendu] Indian Inst Technol, Dept Earth Sci, Bombay 400076, Maharashtra, India; [Tripathi, Suryakant M.] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Bombay; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Mathews, RP (通讯作者)，Indian Inst Technol, Dept Earth Sci, Bombay 400076, Maharashtra, India.	runciepaul@iitb.ac.in	Banerjee, Santanu/H-4617-2018; Dutta, Suryakanti/JXM-1340-2024	Banerjee, Santanu/0000-0002-9548-7047; Dutta, Suryendu/0000-0003-2969-116X	Department of Science and Technology [SR/FTP/ES-19/2008]; Council for Scientific and Industrial Research (CSIR)	Department of Science and Technology(Department of Science & Technology (India)); Council for Scientific and Industrial Research (CSIR)(Council of Scientific & Industrial Research (CSIR) - India)	S.D. acknowledges Department of Science and Technology for the financial support (SR/FTP/ES-19/2008). R.P.M. is thankful to Council for Scientific and Industrial Research (CSIR) for fellowship. The authors are grateful to Dr. N.C. Mehrotra, Director, BSIP, Lucknow for providing necessary infrastructure for the studies.	Ashton P. S., 1982, Flora Malesiana, I, Spermatophyta, V9, P237; ASHTON PS, 1987, J BIOGEOGR, V14, P249, DOI 10.2307/2844895; Biswas S.K., 1992, Journal of the Palaeontological Society of India, V37, P1; Clementz M, 2011, GEOLOGY, V39, P15, DOI 10.1130/G31585.1; Conti E, 2002, EVOLUTION, V56, P1931; Dayanandan S, 1999, AM J BOT, V86, P1182, DOI 10.2307/2656982; Ducousso M, 2004, MOL ECOL, V13, P231, DOI 10.1046/j.1365-294X.2003.02032.x; Dutta S, 2011, REV PALAEOBOT PALYNO, V166, P63, DOI 10.1016/j.revpalbo.2011.05.002; Dutta S, 2011, INT J COAL GEOL, V85, P91, DOI 10.1016/j.coal.2010.10.003; Frederiksen Norman O., 1994, Palynology, V18, P91; KAPOOR P.N., 1996, CONTR 15 IND C MICR, P647; Kar R. 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K., 1980, PALEOBOTANIST, V26, P279; Saxena RK, 1978, PALEOBOTANIST, V25, P448; Saxena RK., 1979, PALAEOBOTANIST, V26, P130; Schrank E., 1984, BERLINER GEOWISSEN A, V50, P189; Tripathi S.K.M., 1994, PALEOBOTANIST, V421, P61; Tripathi SKM., 1997, PALAEOBOTANIST, V46, P168; Tripathi SKM., 2003, PALEOBOTANIST, V52, P87; VENKATACHALA B S, 1968, Pollen et Spores, V10, P335; VENKATACHALA B.S., 1968, Palaeobotanist, V17, P157, DOI DOI 10.54991/JOP.1968.792; Venkatachala BS., 1969, PALEOBOTANIST, V18, P75	44	20	22	0	10	SPRINGER INDIA	NEW DELHI	7TH FLOOR, VIJAYA BUILDING, 17, BARAKHAMBA ROAD, NEW DELHI, 110 001, INDIA	0016-7622	0974-6889		J GEOL SOC INDIA	J. Geol. Soc. India	SEP	2013	82	3					236	248		10.1007/s12594-013-0146-z	http://dx.doi.org/10.1007/s12594-013-0146-z			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	217WY					2025-03-11	WOS:000324394800004
J	Wesselingh, FP; Peters, WJM; Munsterman, DK				Wesselingh, F. P.; Peters, W. J. M.; Munsterman, D. K.			A brachiopod-dominated sea-floor assemblage from the Late Pliocene of the eastern Netherlands	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						Calyptraea; Glottidia; dinoflagellate cysts; North Sea Basin; Oosterhout Formation; palaeoecology	DINOFLAGELLATE CYST STRATIGRAPHY; PALEOECOLOGY; SEQUENCE	A sea-floor assemblage from hardened sandstone boulders in which lingulid brachiopods predominate is recorded from the Oosterhout Formation near Balgoy (province of Gelderland, the Netherlands). Dinoflagellate cysts indicate a late Early-Late Pliocene (late Zanclean-Piacenzian) age of these boulders; the entire assemblage is indicative of clear marine waters near storm wave base along the southeastern margin of the North Sea Basin at the time. A possible commensal relationship between the lingulid brachiopods and the gastropod Calyptraea chinensis is implied.	[Wesselingh, F. P.] Naturalis Biodivers Ctr, NL-2300 RA Leiden, Netherlands; [Munsterman, D. K.] TNO Earth Environm & Life Sci EELS, NL-3508 TA Utrecht, Netherlands	Naturalis Biodiversity Center	Wesselingh, FP (通讯作者)，Naturalis Biodivers Ctr, POB 9517, NL-2300 RA Leiden, Netherlands.	frank.wesselingh@naturalis.nl	Wesselingh, Frank/C-1367-2018	Wesselingh, Frank/0000-0003-3655-0701				Bosch J., 2006, CAINOZOIC RES, V4, P109; De Schepper S., 2006, THESIS U CAMBRIDGE; De Schepper S, 2009, PALYNOLOGY, V33, P179; De Schepper S, 2009, GEOL MAG, V146, P92, DOI 10.1017/S0016756808005438; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Gremare A, 1998, ESTUAR COAST SHELF S, V47, P447, DOI 10.1006/ecss.1998.0379; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Kuhlmann G., 2004, THESIS U UTRECHT; Kuhlmann G, 2006, PALAEOGEOGR PALAEOCL, V239, P426, DOI 10.1016/j.palaeo.2006.02.004; Louwye S, 2004, GEOL MAG, V141, P353, DOI 10.1017/S0016756804009136; Louwye S, 2010, GEOL BELG, V13, P269; Marquet R., 2006, CAINOZOIC RES, V5, P13; Overeem I, 2001, BASIN RES, V13, P293, DOI 10.1046/j.1365-2117.2001.00151.x; Peters N., 2013, REUZENHAAI CHALICOTH; Peters Werner J.M., 2009, Afzettingen Werkgroep voor Tertiaire en Kwartaire Geologie, V30, P12; SAVAZZI E, 1991, PALAEOGEOGR PALAEOCL, V85, P101, DOI 10.1016/0031-0182(91)90027-O; Wijnker E, 2008, NETH J GEOSCI, V87, P165, DOI 10.1017/S0016774600023209; Williams A, 2000, PALAEONTOLOGY, V43, P999, DOI 10.1111/1475-4983.00159	18	4	5	0	2	CAMBRIDGE UNIV PRESS	CAMBRIDGE	EDINBURGH BLDG, SHAFTESBURY RD, CB2 8RU CAMBRIDGE, ENGLAND	0016-7746	1573-9708		NETH J GEOSCI	Neth. J. Geosci.	SEP	2013	92	2-3					171	176		10.1017/S0016774600000111	http://dx.doi.org/10.1017/S0016774600000111			6	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	AT1BW		Green Submitted, Bronze			2025-03-11	WOS:000344669100011
J	Nikitenko, BL; Shurygin, BN; Knyazev, VG; Meledina, SV; Dzyuba, OS; Lebedeva, NK; Peshchevitskaya, EB; Glinskikh, LA; Goryacheva, AA; Khafaeva, SN				Nikitenko, B. L.; Shurygin, B. N.; Knyazev, V. G.; Meledina, S. V.; Dzyuba, O. S.; Lebedeva, N. K.; Peshchevitskaya, E. B.; Glinskikh, L. A.; Goryacheva, A. A.; Khafaeva, S. N.			Jurassic and Cretaceous stratigraphy of the Anabar area (Arctic Siberia, Laptev Sea coast) and the Boreal zonal standard	RUSSIAN GEOLOGY AND GEOPHYSICS			English	Article						Jurassic; Cretaceous; stratigraphy; Boreal zonal standard; ammonites; belemnites; bivalves; foraminifers; ostracods; dinoflagellate cysts; spores and pollen; Siberia; Anabar area	OXFORDIAN/KIMMERIDGIAN BOUNDARY; NORDVIK PENINSULA; BIOSTRATIGRAPHY; AMMONITE; PALEOBIOGEOGRAPHY; FORAMINIFERA; SUCCESSION; ZONATION	Recent integrated studies of Mesozoic reference sections of the Anabar area (northern Middle Siberia, Laptev Sea coast) and the reinterpretation of all the previous data on a modern stratigraphic basis permit considerable improvement of the bio- and lithostratigraphic division and facies zoning of Jurassic and Cretaceous sediments in the region. Analysis of abundant paleontological data allows the development or considerable improvement of zonal scales for ammonites, belemnites, bivalves, foraminifers, ostracods, dinocysts, and terrestrial palynomorphs from several Jurassic and Cretaceous intervals. All the zonal scales have been calibrated against one another and against regional ammonite scale. Reference levels of different scales useful for interregional correlation have been defined and substantiated based on the analysis of lateral distribution of fossils in different regions of the Northern Hemisphere. It provides the possibilities to propose and consider parallel zonal scales within the Boreal zonal standard for the Jurassic and Cretaceous periods. A combination of these scales forms an integrated biostratigraphic basis for a detailed division of Boreal-type sediments regardless of the place of their formation and for the comparison with the international stratigraphic standard as far as a possible use of a set of reference levels for correlation. (C) 2013, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.	[Nikitenko, B. L.; Shurygin, B. N.; Meledina, S. V.; Dzyuba, O. S.; Lebedeva, N. K.; Peshchevitskaya, E. B.; Glinskikh, L. A.; Goryacheva, A. A.; Khafaeva, S. N.] Russian Acad Sci, Siberian Branch, AA Trofimuk Inst Petr Geol & Geophys, Novosibirsk 630090, Russia; [Knyazev, V. G.] Russian Acad Sci, Siberian Branch, Yakutsk Sci Ctr, Diamond & Precious Met Geol Inst, Yakutsk 677891, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Diamond & Precious Metal Geology Institute Siberian Branch of Russian Academy of Sciences; Russian Academy of Sciences	Nikitenko, BL (通讯作者)，Russian Acad Sci, Siberian Branch, AA Trofimuk Inst Petr Geol & Geophys, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia.	NikitenkoBL@ipgg.sbras.ru	Glinskikh, Larisa/Y-8646-2018; Nikitenko, Boris/S-9028-2017; Khafaeva, Svetlana/AAU-3482-2020; Knyazev, Valery/J-3970-2018; Anna, Goryacheva/T-5116-2017; Shurygin, Boris/I-8387-2018; Dzyuba, Oksana/I-8639-2018; Natalia, Lebedeva/T-6040-2017	Glinskikh, Larisa/0000-0001-8241-188X; Anna, Goryacheva/0000-0002-9012-7376; Shurygin, Boris/0000-0001-5512-7509; Dzyuba, Oksana/0000-0003-1523-8153; Pestchevitskaya, Ekaterina/0000-0001-8174-0737; Natalia, Lebedeva/0000-0002-7192-8303	Presidium of the Russian Academy of Sciences [23, 28]; Russian Foundation for Basic Research [12-05-00453]	Presidium of the Russian Academy of Sciences(Russian Academy of Sciences); Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	The study was supported by the Presidium of the Russian Academy of Sciences (programs no. 23, 28) and the Russian Foundation for Basic Research (project no. 12-05-00453).	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KOPTYUGA, 3, NOVOSIBIRSK, 630090, RUSSIA	1068-7971	1878-030X		RUSS GEOL GEOPHYS+	Russ. Geol. Geophys.	AUG	2013	54	8			SI		808	837		10.1016/j.rgg.2013.07.005	http://dx.doi.org/10.1016/j.rgg.2013.07.005			30	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	221MQ					2025-03-11	WOS:000324663400005
J	Laanaia, N; Vaquer, A; Fiandrino, A; Genovesi, B; Pastoureaud, A; Cecchi, P; Collos, Y				Laanaia, Nabil; Vaquer, Andre; Fiandrino, Annie; Genovesi, Benjamin; Pastoureaud, Annie; Cecchi, Philippe; Collos, Yves			Wind and temperature controls on <i>Alexandrium</i> blooms (2000-2007) in Thau lagoon (Western Mediterranean)	HARMFUL ALGAE			English	Article						Alexandrium catenella/tamarense; Wind stress; SST; Thau lagoon; Mediterranean	SMALL-SCALE TURBULENCE; SOUTHERN FRANCE; RESTING CYSTS; SEA WATER; DINOFLAGELLATE; HARMFUL; DINOPHYCEAE; CATENELLA; GROWTH; DYNAMICS	Since 1998, blooms of Alexandrium catenella/tamarense in the lagoon of Thau developed regularly each autumn, reaching a maximum of several millions cells per liter in 2004. By contrast, spring blooms occurred only twice (in 2000 and 2007). During these periods, sea surface temperatures (SST) and the wind patterns appear to impact the bloom occurrences much more than the apparent limiting resources such as inorganic nutrients. The analysis of SST and wind from April to June and September to November (from 2000 to 2007) indicates first that there has to be an initial wind stress in order to resuspend the cysts buried in the sediment. Blooms then occur after a period of weak winds (<4 m s(-1)) and of stable SST close to 20 degrees C (+/- 2 degrees C). Those conditions appear to be most favorable for germination of Alexandrium cysts and its ensuing vegetative growth. This period of stability (a few days to a few weeks) allows the development of the inoculum from the cyst's germination, its cohesion because of reduced hydrodynamics, and development of vegetative cells that are sensitive to agitation. Strong winds during 1-2 day periods can interrupt the bloom dynamics by dispersing (advection due to southeasterly winds) and/or eliminating (turbulence due to northwesterly winds) the vegetative cells. In the spring, under the same conditions of optimal SST, strong wind episodes dominate and those, as well as biological factors very likely lead to a lower occurrence of blooms relative to the fall situation. (C) 2013 Elsevier B.V. All rights reserved.	[Laanaia, Nabil; Fiandrino, Annie; Pastoureaud, Annie] IFREMER, Lab LER LR, F-34203 Sete, France; [Vaquer, Andre; Genovesi, Benjamin; Collos, Yves] Univ Montpellier 2, UMR 5119, CNRS IRD UM2, F-34095 Montpellier 5, France; [Cecchi, Philippe] IRD G EAU, Ouagadougou 01, Burkina Faso	Ifremer; Universite de Montpellier	Collos, Y (通讯作者)，Univ Montpellier 2, Case 093, F-34095 Montpellier 5, France.	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J	Bujtor, L; Janssen, NMM; Verreussel, RMCH				Bujtor, Laszlo; Janssen, Nico M. M.; Verreussel, Roel M. C. H.			Early Cretaceous (Valanginian and Hauterivian) belemnites and organic-walled dinoflagellate cysts from a marine hydrothermal vent site and adjacent facies of the Mecsek Mts., Hungary	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article						Valanginian; Hauterivian; belemnites; organic-walled dinoflagellate cysts; Mecsek Mountains; stratigraphy; hydrothermal vent; Hungary	NEOCOMIAN BELEMNITES; MOUNTAINS; BASIN	The first record of belemnites from fossil hydrothermal vent sites in the Mecsek Mountains of Hungary emphasizes the occurrences of belemnites in Mesozoic chemosynthetic-microbial based ecosystems reported only from cold seep carbonates to date. From the outer shelf-upper bathyal (<300 m) hydrothermal vent site latest Valanginian - Early Hauterivian taxa Adiakritobelus (?), Hibolithes, Duvalia, and Pseudobelus (belemnites) and organic-walled dinoflagellate cysts (a.o. Spiniferites dentatus) are reported. The laterally extending hemipelagic facies yielded latest Berriasian and earliest Valanginian taxa, like: Duvalia, Pseudobelus, and Berriasibelus. The reported belemnite assemblage from this vent site and its coeval beds dated the time span of the iron-ore formation and venting more precisely, between the Early Valanginian and earliest Hauterivian. The belemnite and dinoflagellate cyst assemblages are typical of the Mediterranean Province of the Tethyan Realm.	[Bujtor, Laszlo] Univ Pecs, Fac Nat Sci, Dept Geol, H-7624 Pecs, Hungary; [Verreussel, Roel M. C. H.] TNO Geol Survey Netherlands, NL-3508 TA Utrecht, Netherlands	University of Pecs; Netherlands Organization Applied Science Research	Bujtor, L (通讯作者)，Univ Pecs, Fac Nat Sci, Dept Geol, 6 Ifjusag Utja, H-7624 Pecs, Hungary.	bujtor.laszlo.geology@gmail.com; Hibolithes@hotmail.com; roel.verreussel@tno.nl	Bujtor, László/GWV-4474-2022	Bujtor, Laszlo/0000-0001-9699-7711	Hungarian Academy of Sciences	Hungarian Academy of Sciences(Hungarian Academy of Sciences)	Special thanks are due to Mr. TAMAS FEHER for his field support in collecting fossils in the Mecsek Mts. The authors thanks to Dr. ISTVAN FOZY (Hungarian Natural History Museum, Budapest) for providing belemnite rostra originated from GGIH collection in his possession. We are thankful to WOLFGANG RIEGRAF for his remarks and improvements on an early version of this paper. LB enjoyed the financial support of the Bolyai Janos Research Grant of the Hungarian Academy of Sciences during this research. Photos were taken by WILLEM BONT (Amsterdam, NL). Critical reviews by DZYUBA OKSANA (Novosibirsk, Russia) and JORG MUTTERLOSE (Bochum, Germany) significantly improved the quality of this work, and their remarks and suggestions were highly appreciated.	Agirrezabala LM, 2009, SEDIMENTOLOGY, V56, P969, DOI 10.1111/j.1365-3091.2008.01013.x; Alsen P, 2009, PALAEOGEOGR PALAEOCL, V280, P168, DOI 10.1016/j.palaeo.2009.06.011; Bilik I., 1983, P 17 ASS EUR SEISM C, P569; Bilik I., 1974, ACTA GEOL ACAD SCI H, V18, P315; Bujtor L., 2007, Cent. Eur. 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Ges, V155, P70; Jáger V, 2012, EARTH-SCI REV, V114, P250, DOI 10.1016/j.earscirev.2012.06.003; Janssen N.M.M., 2003, Scripta Geologica (Leiden), V126, P121; Janssen Nico M. M., 2004, Fragmenta Palaeontologica Hungarica, V22, P27; Janssen Nico M. M., 2009, Carnets de Geologie, P1; Kelly SRA, 2000, GEOL SOC SPEC PUBL, V177, P227, DOI 10.1144/GSL.SP.2000.177.01.13; KELLY SRA, 1995, J SEDIMENT RES A, V65, P274; Kolosvary G., 1959, Acta Biologica Szegediensis N S, V5, P125; Kolosvary G., 1954, Magy. All Foldt Int. 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Kozl, V3, P11; Vad?sz E., 1912, MAGYAR KIRALYI FOLDT, V20, P189; Vadasz E., 1935, GEOLOGISCHE BESCHREI; Voight JR, 2000, J ZOOL, V252, P335, DOI 10.1017/S0952836900000078; Wein Gy, 1961, MAGYAR ALLAMI FOLDTA, V49, P759; WEIN Gy, 1965, MECSEK HEGYSEG ESZAK, P35; Wolff T, 2005, CAH BIOL MAR, V46, P97	58	7	7	0	6	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	AUG	2013	269	2					135	148		10.1127/0077-7749/2013/0341	http://dx.doi.org/10.1127/0077-7749/2013/0341			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	186TF					2025-03-11	WOS:000322067600003
J	Pienkowski, AJ; Marret, F; Scourse, JD; Thomas, DN				Pienkowski, Anna J.; Marret, Fabienne; Scourse, James D.; Thomas, David N.			Organic-walled microfossils from the north-west Weddell Sea, Antarctica: records from surface sediments after the collapse of the Larsen-A and Prince Gustav Channel ice shelves	ANTARCTIC SCIENCE			English	Article						Antarctic Peninsula; cysts; dinoflagellates; Islandinium minutum; non-pollen palynomorphs; Southern Ocean	DINOFLAGELLATE CYSTS; SOUTHWESTERN ATLANTIC; SPECIES COMPOSITION; FALKLAND TROUGH; LATE QUATERNARY; MARINE; PALYNOMORPHS; RECONSTRUCTION; ASSEMBLAGES; ABUNDANCE	Surface sediments from six box cores along the north-eastern Antarctic Peninsula document the dinoflagellate cyst (=dinocyst) and other non-pollen palynomorph (NPP) content soon after overlying ice shelves collapsed. Prince Gustav Channel (PGC) and Larsen-A (LA) areas exhibited markedly different dinocyst abundances, concentrations being low in LA (0-20 cysts g(-1)) and high in PGC (2600-9100 cysts g(-1), average: c. 3800 cysts g(-1)). Since similar water masses impact both areas, differences may be due to low biological productivity, limited sediment accumulation, and/or restricted fine-grain deposition at Larsen-A. Islandinium minutum (Harland & Reid in Harland et al.) Head et al. dominated dinocyst assemblages, occurring as both excysted and encysted forms (lesser abundance). Other taxa (Echinidinium cf. transparantum Zonneveld, Impagidinium pallidum Bujak, Bitectatodinium tepikiense Wilson, Operculodinium centrocarpum Wall & Dale, Brigantedinium spp., Selenopemphix antarctica Marret & de Vernal, Polykrikos? sp. A, and Polykrikos schwartzii Butschli) were rare. Such assemblage composition is unusual compared to previously published Southern Ocean data, but may be specific to ice shelf and/or recently ice-free environments. Alternatively, it may be attributable to excessive production facilitated by environmental factors and/or abundant food, or similar cyst morphologies produced by different dinoflagellates. Accompanying NPPs included zooplankton remains, acritarchs, and freshwater algae. Tintinnid loricae were most abundant (max. 800 g(-1)), followed by foraminiferal linings (max. 320 g(-1)), and the acritarch Palaeostomocystis fritilla (Bujak) Roncaglia (max. 150 g(-1)). Collectively, NPPs were more abundant in PGC compared to LA samples.	[Pienkowski, Anna J.; Scourse, James D.; Thomas, David N.] Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Thomas, David N.] Finnish Environm Inst, Ctr Marine Res, Helsinki, Finland; [Thomas, David N.] Aarhus Univ, Arctic Res Ctr, Aarhus, Denmark	Bangor University; University of Liverpool; Finnish Environment Institute; Aarhus University	Pienkowski, AJ (通讯作者)，Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales.	a.pienkowski@bangor.ac.uk	Pieńkowski, Anna/AAL-1312-2020; Thomas, David/B-1448-2010; Pienkowski, Anna/J-9339-2013	Thomas, David/0000-0001-8832-5907; Pienkowski, Anna/0000-0002-3606-7130; Marret-Davies, Fabienne/0000-0003-4244-0437				Armand LeanneK., 2010, Sea Ice, P469, DOI [10.1002/9781444317145.ch13, DOI 10.1002/9781444317145.CH13]; BOLTOVSKOY D, 1990, J PLANKTON RES, V12, P403, DOI 10.1093/plankt/12.2.403; BUCK KR, 1992, ANTARCT SCI, V4, P3, DOI 10.1017/S0954102092000038; Buffen A, 2007, MAR MICROPALEONTOL, V62, P7, DOI 10.1016/j.marmicro.2006.07.002; Caron D.A., 2010, Sea ice, P327; Cearreta A, 2000, HOLOCENE, V10, P155, DOI 10.1191/095968300669405262; Crouch EM, 2010, MAR GEOL, V270, P235, DOI 10.1016/j.margeo.2009.11.004; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; Ellegaard M, 1998, J PLANKTON RES, V20, P1743, DOI 10.1093/plankt/20.9.1743; Esper O, 2007, MAR MICROPALEONTOL, V65, P185, DOI 10.1016/j.marmicro.2007.07.002; Hannah MJ, 2006, PALAEOGEOGR PALAEOCL, V231, P120, DOI 10.1016/j.palaeo.2005.07.029; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; Harland R, 1999, REV PALAEOBOT PALYNO, V107, P265, DOI 10.1016/S0034-6667(99)00023-8; Harland R, 1998, PALAEONTOLOGY, V41, P1093; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Kjæret AH, 2000, SARSIA, V85, P453, DOI 10.1080/00364827.2000.10414594; Kopczynska EE, 2007, POLAR BIOL, V31, P77, DOI 10.1007/s00300-007-0335-6; Kunz-Pirrung Martina, 1998, Berichte zur Polarforschung, V281, P1; Lemke P, 2007, AR4 CLIMATE CHANGE 2007: THE PHYSICAL SCIENCE BASIS, P337; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Marret F, 2001, J QUATERNARY SCI, V16, P739, DOI 10.1002/jqs.648; Matsuoka K, 2009, REV PALAEOBOT PALYNO, V154, P79, DOI 10.1016/j.revpalbo.2008.12.013; MCKENZIE CH, 1991, POLAR BIOL, V11, P139; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; Murray JW, 2004, MAR MICROPALEONTOL, V53, P67, DOI 10.1016/j.marmicro.2004.04.001; Nicholls KW, 2004, GEOPHYS RES LETT, V31, DOI 10.1029/2004GL019924; Pienkowski AJ, 2012, BOREAS, V41, P141, DOI 10.1111/j.1502-3885.2011.00227.x; Pienkowski AJ, 2011, J QUATERNARY SCI, V26, P839, DOI 10.1002/jqs.1503; Pienkowski AJ, 2009, POLAR BIOL, V32, P1331, DOI 10.1007/s00300-009-0630-5; PUDSEY C.J., 2002, RRS JC ROSS JR71 CRU; Pudsey CJ, 2001, GEOLOGY, V29, P787, DOI 10.1130/0091-7613(2001)029<0787:FSOASI>2.0.CO;2; Riedel A, 2003, CANADIAN DATA REPORT, V159, P1; Roberts D, 2007, POLAR BIOL, V30, P143, DOI 10.1007/s00300-006-0169-7; Roncaglia L, 2004, GRANA, V43, P81, DOI 10.1080/00173130410018966; ROTT H., 1996, SCIENCE, V296, P2020; Sherr EB, 2007, MAR ECOL PROG SER, V352, P187, DOI 10.3354/meps07161; STOECKER D.K., 1991, ANTARCT J US, V26, P143; STORKEY C.A., 2006, THESIS VICTORIA U WE; Thompson GA, 2005, AQUAT MICROB ECOL, V40, P85, DOI 10.3354/ame040085; Thomson PG, 2004, J PHYCOL, V40, P867, DOI 10.1111/j.1529-8817.2004.03169.x; Umani SF, 2005, J MARINE SYST, V55, P31, DOI 10.1016/j.jmarsys.2004.05.030; Warny S, 2009, GEOLOGY, V37, P955, DOI 10.1130/G30139A.1	43	8	8	0	21	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0954-1020	1365-2079		ANTARCT SCI	Antarct. Sci.	AUG	2013	25	4					565	574		10.1017/S0954102012001186	http://dx.doi.org/10.1017/S0954102012001186			10	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	182QY					2025-03-11	WOS:000321760000009
J	Costas, E; Gonzalez, R; López-Rodas, V; Huertas, IE				Costas, Eduardo; Gonzalez, Raquel; Lopez-Rodas, Victoria; Huertas, I. Emma			Mutation of microalgae from antifouling sensitivity to antifouling resistance allows phytoplankton dispersal through ships' biofouling	BIOLOGICAL INVASIONS			English	Article						Biofouling; Mutation; Resistance; Dispersal; Introduced species; Microalgae	BALLAST WATER; DICTYOSPHAERIUM-CHLORELLOIDES; MICROCYSTIS-AERUGINOSA; DINOFLAGELLATE CYSTS; RAPID ADAPTATION; CHLOROPHYCEAE; TRANSPORT; ENVIRONMENTS; CONTAMINANTS; ORGANISMS	Marine ecosystems are affected by introduced species including microalgae. We propose that biofouling on ships' hulls is a potentially important mechanism for microalgae dispersal worldwide. Biofouling samples, for phytoplankton composition analysis, were collected in Spanish Mediterranean ports from the hulls of ships that had completed oceanic journeys from other Mediterranean ports, and long journeys from the Atlantic and Indian Oceans. Samples representing the local population of phytoplankton either in the water column or attached to the biofouling of locally-based ship-hulls were used as controls. A broad variety of microalgae species (including toxic dinoflagellates), which were not present in the local phytoplankton populations were found on the biofouling film of the ships that had been on distant journeys. In spite of the presence of the antifouling paints containing toxic compounds, microalgae were able to rapidly adapt to these non-favourable conditions. Consequently, our study shows that ships' biofouling seems to be a powerful vector for microalgae dispersal at a global scale due to the capacity of microalgae to attach to the biofouling film and to cope by adaptation mechanisms with antifouling compounds.	[Costas, Eduardo; Gonzalez, Raquel; Lopez-Rodas, Victoria] Univ Complutense, Fac Vet, E-28040 Madrid, Spain; [Huertas, I. Emma] Inst Ciencias Marinas Andalucia CSIC, Cadiz 11519, Spain	Complutense University of Madrid; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Ciencias Marinas de Andalucia (ICMAN)	López-Rodas, V (通讯作者)，Univ Complutense, Fac Vet, E-28040 Madrid, Spain.	vlrodas@vet.ucm.es	HUERTAS, EMMA/ABH-9719-2020	HUERTAS, I. EMMA/0000-0003-1033-7937	Spanish Ministry of Sciences and Innovation [CTM 2008-05680 C02-02, CGL 2008-00652/BOS]; Spanish Ministry of Education and Science, through FPU program	Spanish Ministry of Sciences and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); Spanish Ministry of Education and Science, through FPU program(German Research Foundation (DFG))	This work has been financially supported by the Spanish Ministry of Sciences and Innovation through the grants CTM 2008-05680 C02-02 and CGL 2008-00652/BOS. Authors thank the financial support given by the Spanish Ministry of Education and Science, through FPU program. Special Thanks are given Lara de Miguel Fernandez by technical support and J. A. Gonzalez Fuster by his enriching advices. Authors are also very grateful with to the assistance provided by the anonymous reviewers.	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Invasions	AUG	2013	15	8					1739	1750		10.1007/s10530-012-0405-8	http://dx.doi.org/10.1007/s10530-012-0405-8			12	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	175WM					2025-03-11	WOS:000321264300009
J	Shin, HH; Jung, SW; Jang, MC; Kim, YO				Shin, Hyeon Ho; Jung, Seung Won; Jang, Min-Chul; Kim, Young-Ok			Effect of pH on the morphology and viability of <i>Scrippsiella trochoidea</i> cysts in the hypoxic zone of a eutrophied area	HARMFUL ALGAE			English	Article						Scrippsiella trochoidea cyst; Morphological change; pH; Acidic sediment; Hypoxic zone; Eutrophied area	DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; HYDROGRAPHIC CONDITIONS; COASTAL WATERS; ARABIAN SEA; TOKYO-BAY; OCEAN; PRODUCTIVITY; DINOPHYCEAE; ASSEMBLAGES	To investigate the cause of morphological change of Scrippsiella trochoidea cysts and its ecological significance in the hypoxic zone of a eutrophied area, the effect of pH on the morphology and viability of S. trochoidea cysts was studied. In the acidification experiment, the dissolution of calcareous spines of S. trochoidea cysts was observed at less than pH 7.39, indicating that the morphological change of S. trochoidea cysts is caused by the low pH levels in acidic sediments of hypoxic zone. After being exposed to intense acidic environments, cysts of S. trochoidea without calcareous spines were able to germinate; however, they seem to be easily linked to degradation in the sediments. These results suggest that the survival of S. trochoidea cysts is being threatened by environmental conditions in the hypoxic zone of eutrophied area. (C) 2013 Elsevier B.V. All rights reserved.	[Shin, Hyeon Ho; Jung, Seung Won; Jang, Min-Chul; Kim, Young-Ok] Korea Inst Ocean Sci & Technol, South Sea Inst, Geoje 656830, South Korea	Korea Institute of Ocean Science & Technology (KIOST)	Kim, YO (通讯作者)，Korea Inst Ocean Sci & Technol, South Sea Inst, Geoje 656830, South Korea.	yokim@kiost.ac	Jung, Seung/L-9467-2016; KIM, YOUNG JIN/E-9374-2011	Shin, Hyeon Ho/0000-0002-9711-6717	Korea Institute of Ocean Science and Technology [PE99151, PM57090]	Korea Institute of Ocean Science and Technology	We thank Ms. Eun Sun Lee for her kind help with the cyst analysis and also wish to express our gratitude to Dr. D. M. Anderson for his critical comments, which helped to improve the manuscript. This work was supported by a grant from the Korea Institute of Ocean Science and Technology (PE99151 and PM57090).	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J	Gu, HF; Liu, TT; Vale, P; Luo, ZH				Gu, Haifeng; Liu, Tingting; Vale, Paulo; Luo, Zhaohe			Morphology, phylogeny and toxin profiles of <i>Gymnodinium inusitatum</i> sp nov., <i>Gymnodinium catenatum</i> and <i>Gymnodinium microreticulatum</i> (Dinophyceae) from the Yellow Sea, China	HARMFUL ALGAE			English	Article						Gymnodinium; Microreticulate cysts; PSP toxin; Ultrastructure	BLOOM-FORMING DINOFLAGELLATE; LSU RDNA SEQUENCES; COASTAL WATERS; COMB. NOV; ALEXANDRIUM DINOPHYCEAE; ELECTRON-MICROSCOPY; MOLECULAR EVIDENCE; MEDITERRANEAN SEA; GEN. NOV.; CYSTS	Four Gymnodinium species have previously been reported to produce microreticulate cysts. Worldwide, Gymnodinium catenatum strains are conservative in terms of larger subunit (LSU) rDNA and internal transcribed spacer region (ITS) sequences, but only limited information on the molecular sequences of other species is available. In the present study, we explored the diversity of Gymnodinium by incubating microreticulate cysts collected from the Yellow Sea off China. A total of 18 strains of Gymnodinium, from three species, were established. Two of these were identified as Gymnodinium catenatum and Gymnodinium microreticulatum, and the third was described as a new species, Gymnodinium inusitatum. Motile cells of G. inusitatum are similar to those of Gymnodinium trapeziforme, but they only share 82.52% similarity in LSU sequences. Cysts of G. inusitatum are polygonal in shape, with its microreticulate wall composed of approximately 14 concave sections. G. microreticulatum strains differ from each other at 69 positions (88.00% similarity) in terms of ITS sequences, whereas all G. catenatum strains share identical ITS sequences and belonged to the global populations. Phylogenetic analyses, based on LSU sequences, revealed that Gymnodinium species that produce microreticulate cysts are monophyletic. Nevertheless, the genus as a whole appears to be polyphyletic. Paralytic shellfish toxins (PSTs) were found in all G. catenatum strains tested (dominated by 11-hydroxysulfate benzoate analogs and N-sulfocarmaboyl analogs) but not in any of the G. microreticulatum and G. inusitatum strains. Our results support the premise that cyst morphology is taxonomically informative and is a potential feature for subdividing the genus Gymnodinium. (C) 2013 Elsevier B.V. All rights reserved.	[Gu, Haifeng; Liu, Tingting; Luo, Zhaohe] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Vale, Paulo] IPMA, Dept Mar & Recursos Marinhos, P-1449006 Lisbon, Portugal	Third Institute of Oceanography, Ministry of Natural Resources; Instituto Portugues do Mar e da Atmosfera	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com; pvale@ipma.pt	Luo, Zhaohe/ITT-7163-2023; Gu, Haifeng/ADN-4528-2022; Vale, Paulo/K-5415-2012	Gu, Haifeng/0000-0002-2350-9171; Vale, Paulo/0000-0002-2524-4453; Luo, Zhaohe/0000-0001-8662-2414	National Scientific-Basic Special Fund [2009FY210400]; Natural Science Foundation of Fujian, China [2012J01135]	National Scientific-Basic Special Fund; Natural Science Foundation of Fujian, China(Natural Science Foundation of Fujian Province)	This project was supported by the National Scientific-Basic Special Fund (Grant No. 2009FY210400) and Natural Science Foundation of Fujian, China (2012J01135).	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J	El Atfy, H; Brocke, R; Uhl, D				El Atfy, Haytham; Brocke, Rainer; Uhl, Dieter			A fungal proliferation near the probable Oligocene/Miocene boundary, Nukhul Formation, Gulf of Suez, Egypt	JOURNAL OF MICROPALAEONTOLOGY			English	Article						fungal palynomorphs; fungal proliferation; Oligocene/Miocene boundary; Nukhul Formation; Gulf of Suez; Egypt	SEQUENCE STRATIGRAPHY; DINOFLAGELLATE CYSTS; RIFT-BASIN; MIOCENE; SPORES; RECORD; BIOSTRATIGRAPHY; SEDIMENTOLOGY; DISTRICT; REMAINS	Moderately to well-preserved palynomorph assemblages were recorded from thirty samples of the Nukhul Formation (GH 404-2A Well), southern Gulf of Suez, Egypt. The taxa are dominated by highly diverse fungi, freshwater algae (e.g. Botryococcus, Pediastrum) beside a sparse record of spores and pollen. Marine palynomorphs, such as dinoflagellate cysts (dinocysts), are very rare. The stratigraphy and age of the Nukhul Formation is highly debated due to lack of diagnostic fossils (e.g. foraminifera, nannoplankton). It has been referred mostly to the Early Miocene; however, some recent publications interpret it as being of latest Oligocene-Early Miocene age. A prominent fungal proliferation composed of diverse and moderately well-preserved fungal spores, fungal fragments, fructifications and hyphae is recorded. This fungi-rich interval occurs mainly from 11370 to 11430 ft in the GH 404-2A Well. Such an observation has not been noted previously within the Nukhul Formation or its stratigraphic equivalents in Egypt. This putative 'eco-event' is probably associated with the well-known eustatic sea-level fall in the latest Chattian to early Aquitanian or at the Oligocene/Miocene boundary (OMB). It also seems possible that it may represent a more local event related to the rifting of the Gulf of Suez during this period. The high diversity of fossil fungi is interpreted herein as an indication of an episodic prevalence of humid climate at the end of a regressive phase, as also indicated by a lithological change near the top of the Shoab Ali Member of the Nukhul Formation. In addition, the co-occurrence of freshwater algae, mainly Botryococcus and Pediastrum, together with some aquatic fungal genera, such as Involutisporonites, Paragrantisporites, Quilonia, Striadiporites and Reduviasporonites, suggests the temporary existence of shallow, pond- or lake-like aquatic habitats, possibly related to tectonic activity.	[El Atfy, Haytham; Brocke, Rainer; Uhl, Dieter] Senckenberg Res Inst, D-60325 Frankfurt, Germany; [El Atfy, Haytham; Brocke, Rainer; Uhl, Dieter] Nat Hist Museum, D-60325 Frankfurt, Germany; [El Atfy, Haytham] Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt; [Uhl, Dieter] Univ Tubingen, Senckenberg Ctr Human Evolut & Palaeoenvironm, D-72076 Tubingen, Germany	Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Egyptian Knowledge Bank (EKB); Mansoura University; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Eberhard Karls University of Tubingen	El Atfy, H (通讯作者)，Senckenberg Res Inst, D-60325 Frankfurt, Germany.	helatfy@senckenberg.de	Atfy, Haytham/AAT-2276-2021		German Academic Exchange Service (DAAD), Senckenberg Research Institute, Frankfurt am Main, Germany [A/10/92695]; Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F)	German Academic Exchange Service (DAAD), Senckenberg Research Institute, Frankfurt am Main, Germany; Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F)	The German Academic Exchange Service (DAAD) is gratefully acknowledged for supporting the first author in his research at the Senckenberg Research Institute, Frankfurt am Main, Germany (grant A/10/92695). Part financial support from the Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F) is also acknowledged. We thank Prof. Dr. Dr. h.c. Volker Mosbrugger for his continuous support. The authors are grateful to the Egyptian General Petroleum Corporation (EGPC) and the Gulf of Suez Petroleum Company (GUPCO) for the provision of samples and well logs. The authors are grateful to the Handling Editor and an anonymous reviewer for their constructive comments. This study was conducted as a part of the PhD research project of H. El Atfy.	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Micropalaentol.	JUL	2013	32		2				183	195		10.1144/jmpaleo2013-004	http://dx.doi.org/10.1144/jmpaleo2013-004			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	199HM		hybrid			2025-03-11	WOS:000322985300005
J	Drits, AV; Nikishina, AB; Sergeeva, VM; Solov'ev, KA				Drits, A. V.; Nikishina, A. B.; Sergeeva, V. M.; Solov'ev, K. A.			Feeding, respiration, and excretion of the Black Sea <i>Noctiluca scintillans</i> MacCartney in summer	OCEANOLOGY			English	Article							ALEXANDRIUM-TAYLORI DINOPHYCEAE; DINOFLAGELLATE; POPULATION; DYNAMICS; PLANKTON	Studies were conducted at the end of June 2011 in the coastal region of the northeastern part of the Black Sea. The bulk of the Noctiluca scintillans population was observed in the thermocline and reached a density of 40000 ind./m(3). Analysis of digestive vacuoles content showed that Noctiluca could consume cells of Neoceratium tripos and N. furca, which had been considered inedible for Black Sea zooplankton, as well as temporary cysts of dinoflagellates, presumably of the toxic genus Alexandrium. The Noctiluca population consumed in total 10-30% of the abundance of temporary cysts, 2-29% of primary production, and 2-9% of potential Calanus euxinus egg production. For the first time, the excretion rates of ammonium nitrogen and mineral phosphorus were measured for N. scintillans. Our calculations showed that in summer, excretion by Noctiluca contributed from 4 to 18% and from 15 to 53% of phytoplankton total nitrogen and phosphorus requirements, respectively. The specific growth rate of Noctiluca (0.17-0.35) in summer, estimated from data on the daily food intake and respiration rate, was close to the values obtained in spring.	[Drits, A. V.; Nikishina, A. B.; Sergeeva, V. M.; Solov'ev, K. A.] Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology	Drits, AV (通讯作者)，Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia.	adrits@mail.ru	Soloviev, Kirill/AAU-7217-2021; Amelina, Anastasia/G-2717-2014; Drits, Alexander/G-1171-2014; Sergeeva, Valentina/F-9823-2014	Amelina, Anastasia/0000-0001-7320-0597; Drits, Alexander/0000-0002-9210-2607; Sergeeva, Valentina/0000-0001-6576-6267				Arashkevich E. G., 2002, COMPLEX STUDIES N E, P257; Bordovskii O.K., 1992, Modern Methods of Hydrochemical Research of the Ocean; Conover R.J., 1978, RAPP PV REUN CONS IN, P66; Frangópulos M, 2011, HARMFUL ALGAE, V10, P304, DOI 10.1016/j.hal.2010.11.002; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Gömez F, 2004, HYDROBIOLOGIA, V517, P43, DOI 10.1023/B:HYDR.0000027336.05452.07; HARGRAVE BT, 1970, J FISH RES BOARD CAN, V27, P1395, DOI 10.1139/f70-165; Hernández-León S, 2008, J PLANKTON RES, V30, P577, DOI 10.1093/plankt/fbn021; Konovalova N. V., 2006, FUNDAM PRIKL PROBL M, P100; MACKAS D, 1976, J EXP MAR BIOL ECOL, V25, P77, DOI 10.1016/0022-0981(76)90077-0; MARSHALL SM, 1955, J MAR BIOL ASSOC UK, V34, P495, DOI 10.1017/S0025315400008778; Menden-Deuer S, 2000, LIMNOL OCEANOGR, V45, P569, DOI 10.4319/lo.2000.45.3.0569; Montani S, 1998, J MAR BIOTECHNOL, V6, P224; Nikishina AB, 2011, OCEANOLOGY+, V51, P1029, DOI 10.1134/S0001437011060129; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Pasternak A.F., 1983, P139; Redfield A. C., 1963, SEA, VPP, P26; Shushkina E. A., 1980, EKOSISTEMY PELAGIALI, P223; Sorokin Y.I., 1982, Black Sea: Nature, Resources, DOI DOI 10.1175/2009JPO4052.1; Teen L. P., 2005, HARMFUL ALGAE, V4, P391; Vinogradov M.E., 1991, VARIABILITY BLACK SE, P224; WALKER LM, 1979, J PHYCOL, V15, P312; Zaika V.E., 2005, Morskyi Ekolohichnyi Zhurnal, V4, P42; ZAIKA VE, 1972, SPECIFIC PRODUCTION; Zaitsev Yu. P., 1987, CURRENT STATE ECOSYS, P216	26	14	15	1	21	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0001-4370			OCEANOLOGY+	Oceanology	JUL	2013	53	4					442	450		10.1134/S0001437013040036	http://dx.doi.org/10.1134/S0001437013040036			9	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	208HV					2025-03-11	WOS:000323669600006
J	Ganini, D; Hollnagel, HC; Colepicolo, P; Barros, MP				Ganini, D.; Hollnagel, H. C.; Colepicolo, P.; Barros, M. P.			Hydrogen peroxide and nitric oxide trigger redox-related cyst formation in cultures of the dinoflagellate <i>Lingulodinium polyedrum</i>	HARMFUL ALGAE			English	Article						Carotenoid; Gonyaulax; Harmful algal blooms; Oxidative stress; Peridinin; Photosynthesis	NITRATE REDUCTASE-ACTIVITY; SUPEROXIDE-DISMUTASE; GONYAULAX-POLYEDRA; ALEXANDRIUM-MINUTUM; LIPID-PEROXIDATION; PRODUCTION PATHWAY; CHLOROPHYLL-A; ENCYSTMENT; PERIDININ; OXYGEN	The dinoflagellate Lingulodinium polyedrum is a toxin producer that shows the ability of turning to resting cysts as a survival strategy when exposed to environmental unfavorable conditions, such as nitrogen and phosphorus depletion, abrupt changes in temperature or light, and chemical or mechanical stress. Algal adaptation to all these conditions involves hydrogen peroxide (H2O2) and nitric oxide (NO center dot) as key redox signals for housekeeping cellular processes. Thus, we aim here to shed light on the role of H2O2 and NO center dot (from aqueous decomposition of sodium nitroprusside, SNP)- as prooxidant agents and putative redox signals for encystment of the dinoflagellate L. polyedrum. Harsh oxidative stress imposed by 500 mu M H2O2 treatment forced L. polyedrum cells to rapidly encyst, in less than 30 min, whereas slower cyst formation was observed upon lower H2O2 doses. L. polyedrum encystment was marked by a significant increase in the antioxidant carotenoid peridinin, although other photosynthetic pigments (chlorophyll a and beta-carotene) and light-harvesting complexes (peridinin complex protein, PCP) were all diminished in cyst forms. Although SOD activity (a frontline antioxidant enzyme) was severely inhibited by increasing doses of H2O2, a theoretical compensatory effect was provided by the dose-dependent increase of ascorbate peroxidase activity (APX), which resulted in significant lower levels of lipid peroxidation during cyst formation. Although SNP data cannot be fully compared to those found with H2O2 treatments, changes in APX activity and in biomarkers of lipid and protein oxidation matched the dose-responses found in H2O2 experiments, revealing similar biochemical and morphological responses against increasing oxidative conditions during cyst formation. Our data significantly contribute to a better understanding of the relationship between encystment, photosynthesis, and antioxidant responses triggered by H2O2 and NO center dot in L. polyedrum, a harmful diarrhetic shellfish poisoning toxin (DSPs) producer. (C) 2013 Elsevier B.V. All rights reserved.	[Ganini, D.; Barros, M. P.] Univ Cruzeiro Sul, CBS, Postgrad Program Hlth Sci Environm Chem, BR-08060070 Sao Paulo, Brazil; [Ganini, D.] NIEHS, Free Radical Metab Grp, Lab Toxicol & Pharmacol, NIH, Res Triangle Pk, NC 27709 USA; [Hollnagel, H. C.] Fac Mario Schenberg, Postgrad Program Environm Management, Cotia, SP, Brazil; [Colepicolo, P.] Univ Sao Paulo IQ USP, Dept Biochem, Inst Quim, Sao Paulo, Brazil	Universidade Cruzeiro do Sul; National Institutes of Health (NIH) - USA; NIH National Institute of Environmental Health Sciences (NIEHS)	Barros, MP (通讯作者)，Univ Cruzeiro Sul, CBS, Av Ussiel Cirilo 225, BR-08060070 Sao Paulo, Brazil.	marcelo.barros@cruzeirodosul.edu.br	Colepicolo, Pio/C-1349-2013; Paes de Barros, Marcelo/K-1410-2013; Fapesp, Biota/F-8655-2017	Paes de Barros, Marcelo/0000-0003-3565-8331; Fapesp, Biota/0000-0002-9887-8449	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP); Programa de Suporte a Pos-graduacao de Instituicoes de Ensino Particulares; da Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (PROSUP/CAPES, Brazil); Projeto Redoxoma, and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (Bolsa Produtividade em Pesquisa, Nivel 2 [307474/2012-7]; CNPq, Brazil	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Programa de Suporte a Pos-graduacao de Instituicoes de Ensino Particulares; da Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (PROSUP/CAPES, Brazil); Projeto Redoxoma, and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (Bolsa Produtividade em Pesquisa, Nivel 2; CNPq, Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are indebted to Dr. Chrislaine O. Soares and B.Sc. Aline B. Glavina for technical support in dinoflagellate cultures, and to Prof. David Morse, at Institut de Recherche en Biologie Vegetale, Departement de Sciences Biologiques, Universite de Montreal, Montreal, Canada, for providing specific rabbit antibodies against dinoflagellate Rubisco and PCP proteins. 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J	Luo, ZH; Yang, WD; Xu, B; Gu, HF				Luo Zhaohe; Yang Weidong; Xu Bin; Gu Haifeng			First record of <i>Biecheleria cincta</i> (Dinophyceae) from Chinese coasts, with morphological and molecular characterization of the strains	CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY			English	Article						Biecheleria; cyst; internal transcribed spacer region (ITS); type E eyespot; ultrastructure; Woloszynskia cincta	SP-NOV; ALEXANDRIUM DINOPHYCEAE; WOLOSZYNSKIA-CINCTA; RIBOSOMAL DNA; LAKE TOVEL; COMB. NOV; GEN. NOV.; DINOFLAGELLATE; ULTRASTRUCTURE; BACILLARIOPHYCEAE	The presence of Biecheleria cincta (= Woloszynskia cincta) in the Chinese coasts is reported for the first time. In scanning electron microscope, three to five series of vesicles and an elongated apical vesicle (EAV) were visible in the epicone, and both the hypocone and the cingulum had three series of vesicles each. Thin sections revealed that B. cincta possesses stalked pyrenoids and an unusual eyespot consisting of a stack of cisternae with brick-like materials (type E), thus supporting its transfer from Woloszynskia to Biecheleria. Spiny cysts formed spontaneously in culture, with an encystment rate of around 20%. Both large subunit ribosomal DNA (LSU rDNA) and internal transcribed spacer region (ITS) sequences in 12 strains from the Chinese coasts were determined. Phylogenetic analyses based on LSU rDNA and ITS sequences using Bayesian inference and maximum likelihood revealed two distinct ribotypes (referred to as ribotype A and B) in B. cincta. ITS region pairwise distances within B. cincta ranged from 0.024 to 0.072, suggesting the existence of a complex of cryptic species.	[Luo Zhaohe; Yang Weidong] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China; [Xu Bin] Chinese Acad Sci, Inst Urban Environm, Xiamen 361021, Peoples R China; [Luo Zhaohe; Gu Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China	Jinan University; Chinese Academy of Sciences; Institute of Urban Environment, CAS; Third Institute of Oceanography, Ministry of Natural Resources	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com	luo, Zhuanxi/B-8441-2009; Gu, Haifeng/ADN-4528-2022	Luo, Zhaohe/0000-0001-8662-2414; Gu, Haifeng/0000-0002-2350-9171	National Scientific-Basic Special Fund [2009FY210400]	National Scientific-Basic Special Fund	Supported by the National Scientific-Basic Special Fund (No. 2009FY210400)	Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Balzano S, 2012, BIOGEOSCIENCES, V9, P4553, DOI 10.5194/bg-9-4553-2012; Biecheler B., 1952, Bull. Biol. Fr. 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J	Pienkowski, AJ; England, JH; Furze, MFA; Blasco, S; Mudie, PJ; MacLean, B				Pienkowski, Anna J.; England, John H.; Furze, Mark F. A.; Blasco, Steve; Mudie, Peta J.; MacLean, Brian			11,000 yrs of environmental change in the Northwest Passage: A multiproxy core record from central Parry Channel, Canadian High Arctic	MARINE GEOLOGY			English	Article						Holocene; environmental change; deglaciation; Canadian Arctic Archipelago; microfossils; palynology	WALLED DINOFLAGELLATE CYSTS; HOLOCENE PALAEOCEANOGRAPHIC CHANGES; LAST GLACIAL MAXIMUM; SEA-ICE VARIATIONS; WESTERN ROSS-SEA; BENTHIC FORAMINIFERA; BARROW STRAIT; PALEOENVIRONMENTAL RECONSTRUCTIONS; NUTRIENT DISTRIBUTIONS; ARCHIPELAGO EVIDENCE	Piston core 97022-004PC (74 degrees 48.0'N 97 degrees 05.9'W; 267 m water depth) represents a rare paleoenvironmental archive from the understudied west-central Canadian Arctic Archipelago. Lithological, biogeochemical, and microfossil (dinoflagellate cysts, non-pollen palynomorphs, benthic and planktonic foraminifera) characteristics, in combination with a chronostratigraphy based on seventeen radiocarbon dates, show seven prominent paleoenvironmental episodes since the end of the last regional glaciation. The basal diamict (Zone I) records decoupling of previously grounded glacial ice, followed by ice-proximal conditions (Zone Ha) commencing at similar to 10.8 cal ka BP (age-depth model extrapolation). After an interval of pervasive sea-ice (Zone Ilb), ice-distal conditions are established (Zone IIc). Although sparse microfossils are present in glaciomarine sediments (Zone II), noticeable biological activity with heightened abundances and diversities across all groups begins in the postglacial Zone III (10.3-10.0 cal ka BP) when planktonic foraminifera (Neogloboquadrina pachyderma) appear. As planktonics are excluded from the study area today (due to shallow inter-channel sills), this likely signals the inflow of relatively warm and saline Atlantic-derived Arctic Intermediate Water below 250 m, presumably facilitated by glacio-isostatically enhanced deglacial water depths. The subsequent Zone IV (10.0-7.0 cal ka BP), characterized by heightened biological productivity in both plankton and benthos and reduced seasonal sea-ice cover, may correspond to a previously proposed Holocene Thermal Maximum. This apparent amelioration ends by the mid Holocene (Zone V; 7.0-5.7 cal ka BP) when Arctic Intermediate Water is excluded from the study area and water depths approach modern values. High-Arctic conditions with seasonal sea-ice cover, a circulation dominated by Arctic Ocean Surface Water, and microfossil assemblages similar to modern are found from similar to 5.7 cal ka BP onwards (Zones VI-VII). As only minor environmental fluctuations are apparent during the late Holocene, shorter-term climatic episodes (e.g. Little Ice Age) are not recognized in this record. Crown Copyright (C) 2013 Published by Elsevier B.V. All rights reserved.	[Pienkowski, Anna J.] Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales; [England, John H.] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada; [Furze, Mark F. A.] MacEwan Univ, Dept Phys Sci, Earth & Planetary Sci Div, Edmonton, AB T5J 4S2, Canada; [Blasco, Steve; Mudie, Peta J.; MacLean, Brian] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada	Bangor University; University of Alberta; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Pienkowski, AJ (通讯作者)，Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales.	a.pienkowski@bangor.ac.uk	Pieńkowski, Anna/AAL-1312-2020; Pienkowski, Anna/J-9339-2013	Furze, Mark/0000-0003-4636-6182; Pienkowski, Anna/0000-0002-3606-7130	NSERC Northern Chair Program; MacEwan University Faculty Research, Scholarly Activity and Creative Achievements Fund	NSERC Northern Chair Program(Natural Sciences and Engineering Research Council of Canada (NSERC)); MacEwan University Faculty Research, Scholarly Activity and Creative Achievements Fund	Funding from the NSERC Northern Chair Program awarded to England enabled this research. A MacEwan University Faculty Research, Scholarly Activity and Creative Achievements Fund awarded to Furze, Pienkowski, England, Blasco, and MacLean ("Deglacial Environments of the Western Canadian High Arctic") is gratefully acknowledged. We thank Charlie Schweger and Harvey Friebe (University of Alberta) for enabling access to their palynology laboratory. We are particularly grateful to Kate Jarrett for core subsampling, and to Owen Brown (both GSC-Atlantic) for conducting grain size analyses. Maureen Soon at the Pacific Centre for Isotopic and Geochemical Research (University of British Columbia) is thanked for BioSil measurements and help with data interpretation, We thank Vera Pospelova, Andre Rochon, and one anonymous reviewer whose comments improved the manuscript. Geert de Lange is thanked for editorial handling of this manuscript.	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Geol.	JUL 1	2013	341						68	85		10.1016/j.margeo.2013.04.008	http://dx.doi.org/10.1016/j.margeo.2013.04.008			18	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	183HY					2025-03-11	WOS:000321806500006
J	Marret, F; Kim, SY; Scourse, J				Marret, Fabienne; Kim, So-Young; Scourse, James			A 30,000 yr record of land-ocean interaction in the eastern Gulf of Guinea	QUATERNARY RESEARCH			English	Article						Dinoflagellate cysts; Pollen; East equatorial Atlantic; Salinity; River discharge; Late Pleistocene-Holocene	RECENT MARINE-SEDIMENTS; WEST EQUATORIAL AFRICA; DINOFLAGELLATE-CYST; ENVIRONMENTAL-CHANGE; SURFACE SEDIMENTS; TROPICAL AFRICA; LATE QUATERNARY; ATLANTIC; VEGETATION; TERRESTRIAL	A 30,000 yr dinocyst and pollen record from the eastern equatorial Atlantic (off Cameroon) has been investigated in order to identify land-ocean linkages during the last deglacial transition. A strong correlation between the abundance of Brigantedinium spp. and the Ca/Fe ratio during the last glacial period suggests enhanced marine productivity in association with cool seawater temperatures and nutrient input linked to coastal upwelling and/or a proximal river mouth. Dry conditions are recorded on the adjacent continent with a significant representation of open vegetation indicators and the Afromontane taxon Podocarpus. After 17 cal ka BP these indicators register a sharp decline as a result of a climatic transition from the dry/cooler conditions of the last glacial period to the wetter/warmer conditions of the deglaciation. Simultaneously, dinocysts show a significant shift from dominant heterotrophs to an increasing abundance of auto-trophs, reflecting warmer conditions. Significant changes are observed during the Younger Dryas, with a return to drier conditions and higher salinities. The start of the Holocene is marked by very low-salinity conditions, reflecting optimal monsoonal conditions over west equatorial Africa. The end of the African Humid Period is observed between 6 and 5 cal ka BP, followed by significant fluctuations in both terrestrial and oceanic proxies. Crown Copyright (C) 2013 Published by Elsevier Inc. on behalf of University of Washington. All rights reserved.	[Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Scourse, James] Univ Wales, Sch Ocean Sci, Bangor, Gwynedd, Wales	University of Liverpool; Bangor University	Marret, F (通讯作者)，Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England.	f.marret@liv.ac.uk	Kim, So-Young/JFS-7698-2023	Marret-Davies, Fabienne/0000-0003-4244-0437	KORDI research program [PE98562]	KORDI research program	We thank Mr. Brian Long for his technical assistance in the palynological preparation of the samples. We also thank Ralph Schneider for access to core GeoB4905-4. This study was supported by a KORDI research program (grant no. PE98562) and is a contribution to the Climate Change Consortium of Wales (C3W). We are thankful to Lydie Dupont and an anonymous reviewer for their constructive comments.	Adegbie A. 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Res.	JUL	2013	80	1					1	8		10.1016/j.yqres.2013.04.003	http://dx.doi.org/10.1016/j.yqres.2013.04.003			8	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	178VU					2025-03-11	WOS:000321476300001
J	Bouimetarhan, I; Groeneveld, J; Dupont, L; Zonneveld, K				Bouimetarhan, Ilham; Groeneveld, Jeroen; Dupont, Lydie; Zonneveld, Karin			Low- to high-productivity pattern within Heinrich Stadial 1: Inferences from dinoflagellate cyst records off Senegal	GLOBAL AND PLANETARY CHANGE			English	Article						Heinrich Stadial 1; Senegal; Marine productivity; Dinoflagellate cysts; Upwelling; Two-phase pattern; NE trade winds	SEA-SURFACE TEMPERATURE; NORTHWEST AFRICA; MARINE-SEDIMENTS; NW AFRICA; TROPICAL ATLANTIC; PLANKTONIC-FORAMINIFERA; ESTUARINE SEDIMENTS; GLOBAL DISTRIBUTION; CANARY-ISLANDS; LEVEL RISE	In order to investigate a possible connection between tropical northeast (NE) Atlantic primacy productivity, Atlantic meridional overturning circulation (AMOC), and drought in the Sahel region during Heinrich Stadial 1 (HS1), we used dinoflagellate cyst (dinocyst) assemblages, Mg/Ca based reconstructed temperatures, stable carbon isotopes (delta C-13) and geochemical parameters of a marine sediment core (GeoB 9508-5) from the continental slope offshore Senegal. Our results show a two-phase productivity pattern within HS1 that progressed from an interval of low marine productivity between similar to 19 and 16 kyr BP to a phase with an abrupt and large productivity increase from similar to 16 to 15 kyr BP. The second phase is characterized by distinct heavy planktonic delta C-13 values and high concentrations of heterotrophic dinocysts in addition to a significant cooling signal based on the reconstructions of past sea surface temperatures (SSTs). We conclude that productivity variations within HS1 can be attributed to a substantial shift of West African atmospheric processes. Taken together our results indicate a significant intensification of the North East (NE) trade winds over West Africa leading to more intense upwelling during the last millennium of HS1 between similar to 16 and 15 kyr BP, thus leaving a strong imprint on the dinocyst assemblages and sea surface conditions. Therefore, the two-phase productivity pattern indicates a complex hydrographic setting suggesting that HS1 cannot be regarded as uniform as previously thought (C) 2013 Elsevier B.V. All rights reserved.	[Bouimetarhan, Ilham; Groeneveld, Jeroen; Dupont, Lydie; Zonneveld, Karin] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany; [Bouimetarhan, Ilham; Groeneveld, Jeroen; Dupont, Lydie; Zonneveld, Karin] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; [Groeneveld, Jeroen] Alfred Wegener Inst Polar & Marine Res, 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, MARUM Ctr Marine Environm Sci, POB 330, D-28334 Bremen, Germany.	bouimetarhan@uni-bremen.de	Bouimetarhan, Ilham/D-2388-2011	Dupont, Lydie/0000-0001-9531-6793; Bouimetarhan, Ilham/0000-0003-3369-3811	Deutsche Forschungsgemeinschaft as part of the DFG-Research Center/Excellence cluster "The Ocean in the Earth System"	Deutsche Forschungsgemeinschaft as part of the DFG-Research Center/Excellence cluster "The Ocean in the Earth System"(German Research Foundation (DFG))	This work was funded by the Deutsche Forschungsgemeinschaft as part of the DFG-Research Center/Excellence cluster "The Ocean in the Earth System". We thank the captain, the crew and participants of R/V Meteor cruise M65/1 for recovering the studied material. Thanks to Matthias Zabel for providing the Ti/Ca ratios. Thanks to Kara Bogus for thoughtful discussions and constructive comments and to Mirja Hoins for assistance with palynological processing. The Mg/Ca and delta<SUP>13</SUP>C data were generated within Project OC3 of the DFG-Research Center/Cluster of Excellence, The Ocean in the Earth System. Data have been submitted to the Publishing Network for Geoscientific & Environmental Data (PANGAEA, www.pangaea.de).	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Planet. Change	JUL	2013	106						64	76		10.1016/j.gloplacha.2013.03.007	http://dx.doi.org/10.1016/j.gloplacha.2013.03.007			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	165NO					2025-03-11	WOS:000320490800007
J	Natsuike, M; Nagai, S; Matsuno, K; Saito, R; Tsukazaki, C; Yamaguchi, A; Imai, I				Natsuike, Masafumi; Nagai, Satoshi; Matsuno, Kohei; Saito, Rui; Tsukazaki, Chiko; Yamaguchi, Atsushi; Imai, Ichiro			Abundance and distribution of toxic <i>Alexarzdrium tamarense</i> resting cysts in the sediments of the Chukchi Sea and the eastern Bering Sea	HARMFUL ALGAE			English	Article						Abundance and distribution; Alexandrium tamarense; Arctic and subarctic; Bering Sea; Chukchi Sea; Cyst	SETO-INLAND-SEA; DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; HARMFUL ALGAL BLOOMS; RED-TIDE; HIROSHIMA-BAY; VERTICAL-DISTRIBUTION; GONYAULAX-EXCAVATA; MARINE-SEDIMENTS; CLIMATE-CHANGE; BENTHIC CYSTS	Abundance and distribution of the toxic dinoflagellate Alexandrium tamarense species complex resting cyst were investigated in the eastern Bering Sea and the Chukchi Sea for the first time. Sediment samples (top 0-3 cm depth) were collected from the continental shelf of the eastern Bering Sea (17 stations) and the Chukchi Sea (13 stations) together with a long core sample (top 0-21 cm depth) from one station in the Chukchi Sea during 2009-2012. The cysts were enumerated using the primuline staining method. Species identification of the cysts was carried out with multiplex PCR assay and the plate morphology of vegetative cells germinated from cysts in the both areas. Alexandrium cysts were widely detected in the both areas, ranging from not detected (<1 cysts cm(-3)) to 835 cysts cm(-3) wet sediment in the eastern Bering Sea and from not detected (<1 cysts cm(-3)) to 10,600 cysts cm(-3) in the Chukchi Sea, and all isolated cysts were genetically and morphologically identified as the North American clade A. tamarense. Their cysts were mainly distributed in the shallow continental shelf where the water depth was less than 100 m in both areas. The cysts were detected from the deep layer (18-21 cm depth of sediment core) of the long core sample. The present study confirmed the abundant existence of A. tamarense with wide range of distribution in these areas. This fact suggests that A. tamarense vegetative cells have appeared in the water column in the both areas. Furthermore, these abundant cyst depositions indicate that this species originally distributed in the Arctic and subarctic regions and well adapted to the environments in the marginal ice zone. (C) 2013 The Authors. Published by Elsevier B.V. All rights reserved.	[Natsuike, Masafumi; Tsukazaki, Chiko; Yamaguchi, Atsushi; Imai, Ichiro] Hokkaido Univ, Grad Sch Fisheries Sci, Plankton Lab Marine Biol, Hakodate, Hokkaido 0418611, Japan; [Nagai, Satoshi] Natl Res Inst Fisheries Sci, Kanazawa Ku, Yokohama, Kanagawa 2368648, Japan; [Matsuno, Kohei] Natl Inst Polar Res, Arctic Environm Res Ctr, Tachikawa, Tokyo 1908518, Japan; [Saito, Rui] Univ Tokyo, Atmosphere & Ocean Res Inst, Div Fisheries & Environm Oceanog, Kashiwa, Chiba 2778564, Japan	Hokkaido University; Japan Fisheries Research & Education Agency (FRA); Research Organization of Information & Systems (ROIS); National Institute of Polar Research (NIPR) - Japan; University of Tokyo	Natsuike, M (通讯作者)，Hokkaido Univ, Grad Sch Fisheries Sci, Plankton Lab Marine Biol, 3-1-1 Minatomachi, Hakodate, Hokkaido 0418611, Japan.	natsu138@fish.hokudai.ac.jp; imai1ro@fish.hokudai.ac.jp	Nagai, Satoshi/HOA-8686-2023; Matsuno, Kohei/AAJ-6510-2021; Yamaguchi, Atsushi/A-8613-2012	Matsuno, Kohei/0000-0001-9793-7622; Yamaguchi, Atsushi/0000-0002-5646-3608; Nagai, Satoshi/0000-0001-7510-0063				Anderson D.M., 1985, P219; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; [Anonymous], HARMFUL ALGAE; Arrigo KR, 2008, GEOPHYS RES LETT, V35, DOI 10.1029/2008GL035028; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Brodeur RD, 1999, FISH OCEANOGR, V8, P296, DOI 10.1046/j.1365-2419.1999.00115.x; COACHMAN LK, 1986, CONT SHELF RES, V5, P23, DOI 10.1016/0278-4343(86)90011-7; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; Dale B., 1983, P69; DALE B, 1978, OCEANUS, V21, P41; Fauchot J, 2005, J PHYCOL, V41, P263, DOI 10.1111/j.1529-8817.2005.03092.x; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1985, B MAR SCI, V37, P529; Genovesi B., 2008, Harmful Algae News, V37, P1; Grebmeier JM, 2012, ANNU REV MAR SCI, V4, P63, DOI 10.1146/annurev-marine-120710-100926; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hallegraeff GM, 2010, J PHYCOL, V46, P220, DOI 10.1111/j.1529-8817.2010.00815.x; Horner R., 1984, The Alaskan Beaufort Sea, P295; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Ishikawa Akira, 2007, Bulletin of the Japanese Society of Fisheries Oceanography, V71, P183; Itakura S, 2002, FISHERIES SCI, V68, P77, DOI 10.1046/j.1444-2906.2002.00392.x; Kamiyama T, 1996, J PLANKTON RES, V18, P1253, DOI 10.1093/plankt/18.7.1253; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; Lewitus AJ, 2012, HARMFUL ALGAE, V19, P133, DOI 10.1016/j.hal.2012.06.009; Lilly EL, 2007, J PHYCOL, V43, P1329, DOI 10.1111/j.1529-8817.2007.00420.x; Markus T, 2009, J GEOPHYS RES-OCEANS, V114, DOI 10.1029/2009JC005436; Matsuno K, 2011, POLAR BIOL, V34, P1349, DOI 10.1007/s00300-011-0988-z; McKay JL, 2008, CAN J EARTH SCI, V45, P1377, DOI 10.1139/E08-046; Mendez S.M., 1996, HARMFUL TOXIC ALGAL, P113; Miyazono A, 2012, HARMFUL ALGAE, V16, P81, DOI 10.1016/j.hal.2012.02.001; Miyazono Akira, 2007, Bulletin of Plankton Society of Japan, V54, P85; Mizushima K, 2004, PHYCOL RES, V52, P408, DOI 10.1111/j.1440-183.2004.00358.x; Nagai S, 2011, J PHYCOL, V47, P703, DOI 10.1111/j.1529-8817.2011.00976.x; Okolodkov YB, 1996, J EXP MAR BIOL ECOL, V202, P19, DOI 10.1016/0022-0981(96)00028-7; Orlova TY, 2007, PHYCOLOGIA, V46, P534, DOI 10.2216/06-17.1; Orlova TY, 2004, BOT MAR, V47, P184, DOI 10.1515/BOT.2004.019; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Schumacher J.D., 1998, The Sea, V11, P789; Selina M.S., 2006, RUSS J MAR BIOL, V32, P321; Shimada Hiroshi, 2005, Plankton Biology and Ecology, V52, P76; Shimada K, 2006, GEOPHYS RES LETT, V33, DOI 10.1029/2005GL025624; SMITH SD, 1990, J GEOPHYS RES-OCEANS, V95, P9461, DOI 10.1029/JC095iC06p09461; Sorokin YI, 1996, J SEA RES, V35, P251, DOI 10.1016/S1385-1101(96)90752-2; Stabeno P. 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J	Gu, HF; Zeng, N; Liu, TT; Yang, WD; Müller, A; Krock, B				Gu, Haifeng; Zeng, Ni; Liu, Tingting; Yang, Weidong; Mueller, Annegret; Krock, Bernd			Morphology, toxicity, and phylogeny of <i>Alexandrium</i> (Dinophyceae) species along the coast of China	HARMFUL ALGAE			English	Article						Alexandrium andersonii; Alexandrium leei; Alexandrium tamarense; Atama complex; China Sea; Cryptic species; Cysts; PSP toxin	TAMARENSE LEBOUR BALECH; SP-NOV DINOPHYCEAE; DINOFLAGELLATE GENUS ALEXANDRIUM; SETO INLAND SEA; TOXIN PROFILE; OSTENFELDII DINOPHYCEAE; LABORATORY CONDITIONS; MINUTUM DINOPHYCEAE; MOLECULAR PHYLOGENY; RESTING CYST	The toxigenic genus Alexandrium includes similar to 30 species, but information about its biogeography at a regional scale is limited. In this study, we explored the diversity of Alexandrium along the coast of China by incubating resting cysts collected from 7 sites. A total of 231 strains of Alexandrium belonging to 7 morphospecies were found. Among them, Alexandrium andersonii, Alexandrium fraterculum, Alexandrium leei, Alexandrium pseudogonyaulax, and Alexandrium tamutum were recorded from the China Sea for the first time. Partial large subunit (LSU) and/or internal transcribed spacer region (ITS1, ITS2, and 5.8S rDNA) sequences revealed two ribotypes of Alexandrium andersonii, Alexandrium leei, and Alexandrium tamarense: Atama complex Group I and IV. Atama complex Group I was exclusively distributed in the Yellow Sea and the Bohai Sea, whereas Group IV was restricted to the East China Sea and South China Sea. Atama complex Group I produced mainly N-sulfocarbamoyl toxins (C1/C2, 61-79% of total toxins) and gonyautoxins (GTX1/4, 17-37%). Alexandrium ostenfeldii strain ASBH01 produced NEO and STX exclusively (65% and 35%, respectively). Our results support the premise that Atama complex Group I is endemic to the Asian Pacific and includes cold water species, whereas Atama complex Group IV tends to inhabit warmer waters. (C) 2013 Elsevier B.V. All rights reserved.	[Gu, Haifeng; Zeng, Ni; Liu, Tingting] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Zeng, Ni; Yang, Weidong] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China; [Mueller, Annegret; Krock, Bernd] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany	Third Institute of Oceanography, Ministry of Natural Resources; Jinan University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com; bernd.krock@awi.de	Krock, Bernd/ABB-7541-2020; Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171	National Scientific-Basic Special Fund [2009FY210400]; National Natural Science Foundation of China [40476053, 41176088]	National Scientific-Basic Special Fund; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This project was supported by the National Scientific-Basic Special Fund (Grant No. 2009FY210400) and National Natural Science Foundation of China (Grant Nos. 40476053 and 41176088). 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J	Van de Waal, DB; John, U; Ziveri, P; Reichart, GJ; Hoins, M; Sluijs, A; Rost, B				Van de Waal, Dedmer B.; John, Uwe; Ziveri, Patrizia; Reichart, Gert-Jan; Hoins, Mirja; Sluijs, Appy; Rost, Bjoern			Ocean Acidification Reduces Growth and Calcification in a Marine Dinoflagellate	PLOS ONE			English	Article							THORACOSPHAERA-HEIMII DINOPHYCEAE; CARBON-ISOTOPE FRACTIONATION; LIFE-CYCLE; CONCENTRATING MECHANISMS; CO2; SEAWATER; WATER; LIGHT; ACID; PHYTOPLANKTON	Ocean acidification is considered a major threat to marine ecosystems and may particularly affect calcifying organisms such as corals, foraminifera and coccolithophores. Here we investigate the impact of elevated pCO(2) and lowered pH on growth and calcification in the common calcareous dinoflagellate Thoracosphaera heimii. We observe a substantial reduction in growth rate, calcification and cyst stability of T. heimii under elevated pCO(2). Furthermore, transcriptomic analyses reveal CO2 sensitive regulation of many genes, particularly those being associated to inorganic carbon acquisition and calcification. Stable carbon isotope fractionation for organic carbon production increased with increasing pCO(2) whereas it decreased for calcification, which suggests interdependence between both processes. We also found a strong effect of pCO(2) on the stable oxygen isotopic composition of calcite, in line with earlier observations concerning another T. heimii strain. The observed changes in stable oxygen and carbon isotope composition of T. heimii cysts may provide an ideal tool for reconstructing past seawater carbonate chemistry, and ultimately past pCO(2). Although the function of calcification in T. heimii remains unresolved, this trait likely plays an important role in the ecological and evolutionary success of this species. Acting on calcification as well as growth, ocean acidification may therefore impose a great threat for T. heimii.	[Van de Waal, Dedmer B.; John, Uwe; Hoins, Mirja; Rost, Bjoern] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany; [Van de Waal, Dedmer B.] Netherlands Inst Ecol NIOO KNAW, Dept Aquat Ecol, Wageningen, Netherlands; [Ziveri, Patrizia] Univ Autonoma Barcelona, Inst Environm Sci & Technol ICTA, E-08193 Barcelona, Spain; [Ziveri, Patrizia] Vrije Univ Amsterdam, Dept Earth Sci, Amsterdam, Netherlands; [Reichart, Gert-Jan; Hoins, Mirja; Sluijs, Appy] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands; [Reichart, Gert-Jan] Royal Netherlands Inst Sea Res NIOZ, Dept Geol, Den Hoorn, Texel, Netherlands	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Royal Netherlands Academy of Arts & Sciences; Netherlands Institute of Ecology (NIOO-KNAW); Autonomous University of Barcelona; Vrije Universiteit Amsterdam; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Van de Waal, DB (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany.	d.vandewaal@nioo.knaw.nl	Rost, Bjoern/B-4447-2015; Van de Waal, Dedmer/B-8002-2012; Reichart, Gert-Jan/N-6308-2018; Sluijs, Appy/B-3726-2009; Ziveri, Patrizia/I-3856-2015; KNAW, NIOO-KNAW/A-4320-2012; John, Uwe/S-3009-2016	Reichart, Gert-Jan/0000-0002-7256-2243; Sluijs, Appy/0000-0003-2382-0215; Van de Waal, Dedmer/0000-0001-8803-1247; Ziveri, Patrizia/0000-0002-5576-0301; KNAW, NIOO-KNAW/0000-0002-3835-159X; Rost, Bjorn/0000-0001-5452-5505; John, Uwe/0000-0002-1297-4086	BIOACID; German Ministry of Education and Research; European Community's Seventh Framework Programme/ERC [205150, 259627]; EC [211384, 265103]; European Research Council (ERC) [205150] Funding Source: European Research Council (ERC)	BIOACID; German Ministry of Education and Research(Federal Ministry of Education & Research (BMBF)); European Community's Seventh Framework Programme/ERC; EC(European Union (EU)European Commission Joint Research Centre); European Research Council (ERC)	The work was funded by BIOACID, financed by the German Ministry of Education and Research. Furthermore, this work was supported by the European Community's Seventh Framework Programme/ERC grant agreements #205150 and #259627, and contributes to the EC FP7 projects EPOCA, grant agreement #211384, and MedSeA, grant agreement #265103. 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	Bijl, PK; Bendle, JAP; Bohaty, SM; Pross, J; Schouten, S; Tauxe, L; Stickley, CE; Mckay, RM; Röhl, U; Olney, M; Sluijs, A; Escutia, C; Brinkhuis, H; Klaus, A; Fehr, A; Williams, T; Carr, SA; Dunbar, RB; Gonzàlez, JJ; Hayden, TG; Iwai, M; Jimenez-Espejo, FJ; Katsuki, K; Kong, GS; Nakai, M; Passchier, S; Pekar, SF; Riesselman, C; Sakai, T; Shrivastava, PK; Sugisaki, S; Tuo, S; van De Flierdt, T; Welsh, K; Yamane, M				Bijl, Peter K.; Bendle, James A. P.; Bohaty, Steven M.; Pross, Joerg; Schouten, Stefan; Tauxe, Lisa; Stickley, Catherine E.; McKay, Robert M.; Roehl, Ursula; Olney, Matthew; Sluijs, Appy; Escutia, Carlota; Brinkhuis, Henk; Klaus, Adam; Fehr, Annick; Williams, Trevor; Carr, Stephanie A.; Dunbar, Robert B.; Gonzalez, Jhon J.; Hayden, Travis G.; Iwai, Masao; Jimenez-Espejo, Francisco J.; Katsuki, Kota; Kong, Gee Soo; Nakai, Mutsumi; Passchier, Sandra; Pekar, Stephen F.; Riesselman, Christina; Sakai, Toyosaburo; Shrivastava, Prakash K.; Sugisaki, Saiko; Tuo, Shouting; van de Flierdt, Tina; Welsh, Kevin; Yamane, Masako		Expedition 318 Scientists	Eocene cooling linked to early flow across the Tasmanian Gateway	PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA			English	Article						climate cooling; dinoflagellate cysts; organic palaeothermometry; paleoceanography	CONTINENTAL-MARGIN; TETRAETHER LIPIDS; MEMBRANE-LIPIDS; SOUTH-PACIFIC; CLIMATE; OCEAN; GREENHOUSE; EVOLUTION; ASSEMBLAGES; ICEHOUSE	The warmest global temperatures of the past 85 million years occurred during a prolonged greenhouse episode known as the Early Eocene Climatic Optimum (52-50 Ma). The Early Eocene Climatic Optimum terminated with a long-term cooling trend that culminated in continental-scale glaciation of Antarctica from 34 Ma onward. Whereas early studies attributed the Eocene transition from greenhouse to icehouse climates to the tectonic opening of Southern Ocean gateways, more recent investigations invoked a dominant role of declining atmospheric greenhouse gas concentrations (e.g., CO2). However, the scarcity of field data has prevented empirical evaluation of these hypotheses. We present marine microfossil and organic geochemical records spanning the early-to-middle Eocene transition from the Wilkes Land Margin, East Antarctica. Dinoflagellate biogeography and sea surface temperature paleothermometry reveal that the earliest throughflow of a westbound Antarctic Counter Current began similar to 49-50 Ma through a southern opening of the Tasmanian Gateway. This early opening occurs in conjunction with the simultaneous onset of regional surface water and continental cooling (2-4 degrees C), evidenced by biomarker- and pollen-based paleothermometry. We interpret that the westbound flowing current flow across the Tasmanian Gateway resulted in cooling of Antarctic surface waters and coasts, which was conveyed to global intermediate waters through invigorated deep convection in southern high latitudes. Although atmospheric CO2 forcing alone would provide a more uniform middle Eocene cooling, the opening of the Tasmanian Gateway better explains Southern Ocean surface water and global deep ocean cooling in the apparent absence of (sub-) equatorial cooling.	[Bijl, Peter K.; Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Dept Earth Sci, Fac Geosci, NL-3584 CD Utrecht, Netherlands; [Bendle, James A. P.] Univ Glasgow, Glasgow G12 8QQ, Lanark, Scotland; [Bohaty, Steven M.] Univ Southampton, Southampton SO14 3ZH, Hants, England; [Pross, Joerg] Goethe Univ Frankfurt, Inst Geosci, Paleoenvironm Dynam Grp, D-60438 Frankfurt, Germany; [Pross, Joerg] Biodivers & Climate Res Ctr, D-60325 Frankfurt, Germany; [Schouten, Stefan; Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands; [Tauxe, Lisa] Univ Calif San Diego, Scripps Inst Oceanog, Geosci Res Div, La Jolla, CA 92093 USA; [Stickley, Catherine E.] Univ Troms, Dept Geol, N-9037 Tromso, Norway; [McKay, Robert M.] Victoria Univ Wellington, Antarctic Res Ctr, Wellington 6140, New Zealand; [Roehl, Ursula] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Olney, Matthew] Univ S Florida, Dept Geol, Tampa, FL 33620 USA; [Escutia, Carlota] Univ Granada, Consejo Super Invest Cient Spain, Inst Andaluz Ciencias Tierra, Granada 18002, Spain; [Klaus, Adam] Texas A&M Univ, US Implementing Org, Integrated Ocean Drilling Program, College Stn, TX 77845 USA; [Fehr, Annick] Rhein Westfal TH Aachen, Inst Appl Geophys & Geothermal Energy, D-52074 Aachen, Germany; [Williams, Trevor] Columbia Univ, Lamont Doherty Geol Observ, Borehole Res Grp, Palisades, NY 10964 USA; [Carr, Stephanie A.] Colorado Sch Mines, Dept Chem & Geochem, Golden, CO 80401 USA; [Dunbar, Robert B.; Pekar, Stephen F.] Stanford Univ, Dept Environm Earth Syst Sci, Stanford, CA 94305 USA; [Gonzalez, Jhon J.; Jimenez-Espejo, Francisco J.] Univ Granada, Inst Andaluz Ciencias Tierra, CSIC, Granada, Spain; [Hayden, Travis G.] Western Michigan Univ, Dept Geol, Kalamazoo, MI 49008 USA; [Iwai, Masao] Kochi Univ, Dept Nat Sci, Kochi, Japan; [Jimenez-Espejo, Francisco J.] Japan Agcy Marine Earth Sci & Technol, Inst Res Earth Evolut, 2-15 Natsushimacho, Yokosuka, Kanagawa 2370061, Japan; [Katsuki, Kota] Kochi Univ, Marine Ctr Adv Core Res, Kochi, Japan; [Kong, Gee Soo] Korea Inst Geosci & Mineral Resource, Petr & Marine Res Div, Daejeon 305350, South Korea; [Nakai, Mutsumi] Daito Bunka Univ, Dept Educ, Itabashi Ku, 1-9-1 Takashima Daira, Tokyo 1758571, Japan; [Passchier, Sandra] Montclair State Univ, Earth & Environm Studies, Montclair, NJ 07043 USA; [Pekar, Stephen F.] CUNY Queens Coll, Sch Earth & Environm Studies, Flushing, NY 11367 USA; [Pekar, Stephen F.] US Geol Survey, Eastern Geol & Palaeoclimate Sci Ctr, Reston, VA 20192 USA; [Sakai, Toyosaburo] Utsunomiya Univ, Dept Geol, Utsunomiya, Tochigi 3218505, Japan; [Shrivastava, Prakash K.] NIT, NH5P, Geol Survey India, Antarctica Div, Faridabad, Haryana, India; [Sugisaki, Saiko] Grad Univ Adv Studies, Dept Polar Sci, Tachikawa, Tokyo 1908518, Japan; [Sugisaki, Saiko] Japan Agcy Marine Earth Sci & Technol, 2-15 Natsushimacho, Yokosuka, Kanagawa 2370061, Japan; [Sugisaki, Saiko] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; [Tuo, Shouting] Tongji Univ, Sch Ocean & Earth Sci, Shanghai 200092, Peoples R China; [van de Flierdt, Tina] Univ London Imperial Coll Sci Technol & Med, Dept Earth Sci & Engn, London SW7 2AZ, England; [Welsh, Kevin] Univ Queensland, Sch Earth Sci, Brisbane, Qld 4072, Australia; [Yamane, Masako] Univ Tokyo, Earth & Planetary Sci, Tokyo 1130033, Japan	Utrecht University; University of Glasgow; University of Southampton; Goethe University Frankfurt; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of California System; University of California San Diego; Scripps Institution of Oceanography; UiT The Arctic University of Tromso; Victoria University Wellington; University of Bremen; State University System of Florida; University of South Florida; University of Granada; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT); Texas A&M University System; Texas A&M University College Station; RWTH Aachen University; Columbia University; Colorado School of Mines; Stanford University; University of Granada; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT); Western Michigan University; Kochi University; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); Kochi University; Korea Institute of Geoscience & Mineral Resources (KIGAM); Montclair State University; City University of New York (CUNY) System; Queens College NY (CUNY); United States Department of the Interior; United States Geological Survey; Utsunomiya University; Geological Survey India; Graduate University for Advanced Studies - Japan; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); University of California System; University of California San Diego; Scripps Institution of Oceanography; Tongji University; Imperial College London; University of Queensland; University of Tokyo	Bijl, PK (通讯作者)，Univ Utrecht, Dept Earth Sci, Fac Geosci, NL-3584 CD Utrecht, Netherlands.	p.k.bijl@uu.nl	Passchier, Sandra/AAQ-2243-2021; Brinkhuis, Henk/IUO-8165-2023; Jimenez-Espejo, Francisco/F-4486-2016; Williams, Trevor/L-7670-2014; Riesselman, Christina/H-5037-2012; McKay, Robert/N-2449-2015; Schouten, Stefan/P-4380-2016; Flores, Jose-Abel/D-4218-2009; Escutia, Carlota/B-8614-2015; Sluijs, Appy/B-3726-2009; Rohl, Ursula/G-5986-2011; Welsh, Kevin/A-9808-2012; Passchier, Sandra/B-1993-2008	Flores, Jose-Abel/0000-0003-1909-293X; Brinkhuis, Henk/0000-0003-0253-6610; Escutia, Carlota/0000-0002-4932-8619; van de Flierdt, Tina/0000-0001-7176-9755; Bendle, James/0000-0002-6826-8658; Sluijs, Appy/0000-0003-2382-0215; Bijl, Peter/0000-0002-1710-4012; Yamane, Masako/0000-0002-5063-0719; Rohl, Ursula/0000-0001-9469-7053; McKay, Robert/0000-0002-5602-6985; Welsh, Kevin/0000-0002-4834-4190; Dunbar, Robert/0000-0002-9728-5609; Passchier, Sandra/0000-0001-7204-7025	Netherlands Organization for Scientific Research [86610110]; LPP Foundation; Natural Environmental Research Council (NERC); IODP-Unite Kingdom for Standard Research Grant [NE/I00646X/1]; Cruise Participation Grant [NE/H014616/1]; NERC [NE/H020098/1, NE/J019801/1]; German Research Foundation [PR 651/10, RO 1113/6]; Biodiversity and Climate Research Center (BIK-F) within the Hessian Initiative for Scientific and Economic Excellence (LOEWE); National Science Foundation [OCE 1058858]; European Research Council [259627]; NERC [NE/H014616/1, NE/I006257/1, NE/I00646X/1, NE/I00646X/2, NE/H020098/1, NE/H025162/1, NE/J019801/1] Funding Source: UKRI; Directorate For Geosciences; Division Of Ocean Sciences [1058858] Funding Source: National Science Foundation; Directorate For Geosciences; Division Of Ocean Sciences [1129101] Funding Source: National Science Foundation	Netherlands Organization for Scientific Research(Netherlands Organization for Scientific Research (NWO)); LPP Foundation; Natural Environmental Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); IODP-Unite Kingdom for Standard Research Grant; Cruise Participation Grant; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); German Research Foundation(German Research Foundation (DFG)); Biodiversity and Climate Research Center (BIK-F) within the Hessian Initiative for Scientific and Economic Excellence (LOEWE); National Science Foundation(National Science Foundation (NSF)); European Research Council(European Research Council (ERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Directorate For Geosciences; Division Of Ocean Sciences(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))	The authors thank Peter J. Hill and Neville F. Exon for discussions. This research used samples from the Ocean Drilling Program (ODP) and the Integrated Ocean Drilling Program (IODP). P.K.B. and H.B. thank the Netherlands Organization for Scientific Research [Grant 86610110 (to H.B.)] and the LPP Foundation for funding, and N.L.D. Welters for sample processing. J.A.P.B. acknowledges the Natural Environmental Research Council (NERC) and IODP-Unite Kingdom for Standard Research Grant NE/I00646X/1 and Cruise Participation Grant NE/H014616/1. S.M.B. acknowledges NERC for Cruise Participation Grant NE/H020098/1 and postcruise research support (Grant NE/J019801/1). J.P. and U.R. acknowledge support through German Research Foundation Grants PR 651/10 and RO 1113/6. J.P. was supported by the Biodiversity and Climate Research Center (BIK-F) within the Hessian Initiative for Scientific and Economic Excellence (LOEWE). L.T. acknowledges support from National Science Foundation Grant OCE 1058858. 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JUN 11	2013	110	24					9645	9650		10.1073/pnas.1220872110	http://dx.doi.org/10.1073/pnas.1220872110			6	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	171LM	23720311	Green Published, Green Submitted			2025-03-11	WOS:000320930100026
J	Wendler, I; Huber, BT; MacLeod, KG; Wendler, JE				Wendler, Ines; Huber, Brian T.; MacLeod, Kenneth G.; Wendler, Jens E.			Stable oxygen and carbon isotope systematics of exquisitely preserved Turonian foraminifera from Tanzania - Understanding isotopic signatures in fossils	MARINE MICROPALEONTOLOGY			English	Article						foraminifera; Turonian stable isotopes; isotopic covariance; vital effect; Tanzania	STAINED BENTHIC FORAMINIFERA; LIVING PLANKTONIC-FORAMINIFERA; CRETACEOUS-TERTIARY BOUNDARY; SEA-SURFACE TEMPERATURES; JURASSIC PREBETIC ZONE; DEEP-SEA; MICROHABITAT PREFERENCES; VOCONTIAN BASIN; THORACOSPHAERA-HEIMII; GLOBIGERINA-BULLOIDES	The interpretation of delta O-18 and delta C-13 analyses of extinct foraminifera is hampered by insufficient knowledge on the contribution of environmental versus biological factors on the measured values. We present single-species stable isotope data for 18 benthic and 11 planktic foraminiferal species and one calcareous dinoflagellate cyst species from a Turonian equatorial record measured on samples collected in SE Tanzania. All microfossils analyzed were excellently preserved and results are compared to isotopic measurements from bulk sediment of the same material. Remarkably low intra-specific variability (standard deviations <0.2 parts per thousand) across the studied interval and consistently large benthic/planktic offsets in delta O-18 (similar to 2.8 parts per thousand.) and delta C-13 (similar to 1.5 parts per thousand) indicate absence of major long-term environmental fluctuations and presence of a well stratified water column. Stratigraphic isotopic trends show small shifts that are parallel in all studied benthic species (with the exception of the delta C-13 record of Lenticulina species), but within-sample inter-specific offsets reflect a combination of habitat differences and species-specific isotopic disequilibrium fractionation. Among planktic taxa closely related taxa tend to have similar isotopic values. Biserial taxa have the lowest delta O-18 values (similar to-4.7 parts per thousand) but also have relatively low delta C-13 values (similar to 1.6 parts per thousand) indicating that, for the assumption of a surface water habitat, additional metabolic effects need to be involved, which supports the concept of their opportunistic lifestyle. Among trochospiral planktics the keeled taxa with compressed chambers have slightly higher delta O-18 (similar to-4.2 parts per thousand) and lower delta C-13 (similar to 2.3 parts per thousand) values than taxa with globular chambers (similar to-4.4 parts per thousand and similar to 2.4 parts per thousand, respectively), suggesting differences in habitat or in peak seasonal abundance. Benthic taxa are subdivided into three isotopically distinct groups with differences reflecting mineralogy, life strategy and habitat; Group I: aragonitic taxa (Epistomina, Colomia africana), Group II: calcitic trochospiral taxa with isotopic values seemingly close to equilibrium (Berthelina berthelini, Oridorsalis umbonatus, Lingulogavelinella globosa, Lingulogavelinella convexa) and Group III: calcitic taxa with low delta O-18 values and large scatter in delta C-13 values (Lenticulina). Four other benthic species show values between Groups II and III. The wealth and consistency of data, especially for benthic taxa, permit refined conclusions. The five studied species of Epistomina have a similar isotopic signature and are inferred to form their aragonitic shells with close to equilibrium values. Small isotopic offsets are seen among species that differ in orientation of the septal foramen, but no offsets are seen that seem to co-vary with test shape or ornamentation. The conical species C africana has delta O-18 values similar to 0.2 parts per thousand lower and delta C-13 values degrees 0.7 parts per thousand lower than species of Epistomina. The latter offset probably reflects an infaunal habitat for C. africana. Epistomina and Group II species are recommended for paleoenviromental studies. Mono-specific Lenticulina delta O-18 values may be used if increased by correction factors of 0.4 parts per thousand to 0.9 parts per thousand, but this taxon's low and variable delta C-13 values are interpreted to reflect incorporation of respiratory CO2, possibly combined with fast growth rates related to opportunism, rather than equilibrium with benthic dissolved inorganic carbon. The observed stability of inter-specific isotopic offsets suggests disequilibrium isotopic effects are relatively consistent for many taxa in this section, and correction factors are proposed that may help to generate more robust Upper Cretaceous foraminiferal isotopic records. However, delta O-18/delta C-13 covariance in some benthic inter-specific comparisons suggests offsets might vary with changes in temperature, food supply or other factors so the appropriateness of the correction factors should be confirmed before being applied at different sites. Similarities between the observed single-species isotopic patterns from this and other studies are used to present a summarizing scheme of influences on the stable isotopic composition in foraminiferal tests. By applying the new insights from our study to data from other Cretaceous studies we demonstrate that the selection of species for isotopic analysis and understanding these signals are critical to the outcome of paleoceanographic interpretations. (C) 2013 Elsevier B.V. All rights reserved.	[Wendler, Ines; Huber, Brian T.; Wendler, Jens E.] Smithsonian Museum Nat Hist, Dept Paleobiol, Washington, DC 20013 USA; [Wendler, Ines; Wendler, Jens E.] Univ Bremen, Dept Geol Sci, D-28334 Bremen, Germany; [MacLeod, Kenneth G.] Univ Missouri, Dept Geol Sci, Columbia, MO 65211 USA	Smithsonian Institution; Smithsonian National Museum of Natural History; University of Bremen; University of Missouri System; University of Missouri Columbia	Wendler, I (通讯作者)，Univ Bremen, Dept Geol Sci, POB 330 440, D-28334 Bremen, Germany.	flatter@uni-bremen.de	MacLeod, Kenneth/C-4042-2017	MacLeod, Kenneth/0000-0002-6016-0837	National Science Foundation [NSF EAR 0641956]; Smithsonian Institution Scholarly Studies Program; German Science Foundation (DFG) [WE 4587/1-1]	National Science Foundation(National Science Foundation (NSF)); Smithsonian Institution Scholarly Studies Program; German Science Foundation (DFG)(German Research Foundation (DFG))	Logistical and field support from the Tanzania Petroleum Development Corporation was critical to the success of the Tanzania Drilling Program; we are particularly grateful for the generous assistance of TPDC staff including Joyce Singano, Michael Kereme, Ephrem Mchana, Amina Mweneinda, Emma Msaki, and Frank Mayagilo. For assistance with sample preparation and foraminifer picking we thank Shannon Haynes, Carlos Rodriguez-Russo, Sarah Ehlinger, Joshua Johnson, John Vincent, Erin Jacobs and Loren Petruny. Comments and suggestions by L Alegret, O. Friedrich, an anonymous third reviewer and by F. Jorissen are highly acknowledged. This study was funded by the National Science Foundation (NSF EAR 0641956), the Smithsonian Institution Scholarly Studies Program and the German Science Foundation (DFG, WE 4587/1-1).	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Micropaleontol.	JUN	2013	102						1	33		10.1016/j.marmicro.2013.04.003	http://dx.doi.org/10.1016/j.marmicro.2013.04.003			33	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	211NB					2025-03-11	WOS:000323913800001
J	Limoges, A; Londeix, L; de Vernal, A				Limoges, Audrey; Londeix, Laurent; de Vernal, Anne			Organic-walled dinoflagellate cyst distribution in the Gulf of Mexico	MARINE MICROPALEONTOLOGY			English	Article						Gulf of Mexico; Dinoflagellates; Cysts; Harmful algal bloom; Melitasphaeridium choanophorum	SEA-SURFACE CONDITIONS; NORTHERN NORTH-ATLANTIC; HARMFUL ALGAL BLOOMS; PYRODINIUM-BAHAMENSE; MARINE-SEDIMENTS; HIGH-LATITUDES; LABRADOR SEA; LOOP CURRENT; WESTERN; SALINITY	In order to document the distribution of organic-walled dinoflagellate cysts (dinocysts) and their relationship with sea-surface parameters (temperature, salinity, primary productivity), palynological analyses were performed on 44 surface sediment samples from the Gulf of Mexico (17 degrees N to 29 degrees N). Samples display low to moderate concentrations with values ranging from 78 to 3576 dinocysts.g(-1) dry weight sediment. Assemblages are dominated by either Brigantedinium spp. or Polysphaeridium zoharyi along with the phototrophic taxa Spiniferites spp. and Operculodinium spp. Redundancy analyses (RDA) identified the distance to the coast and/or water depth and annual temperature as being the most important factors that control cyst distribution in the Gulf of Mexico. The first two axes explain respectively 44.7% and 20% of the total variance. The inshore to offshore trend in cyst distribution emphasized by the RDA involves changes in associations of species with the presence of Impagidinium spp. in more oceanic assemblages and higher representation of P. zohaiyi nearshore. This latter species, produced by the potentially toxic dinoflagellate Pyrodinium bahamense, reaches very high abundances notably on the west Florida shelf and in the Mexican lagoons. Additionally, Melitasphaeridium choanophorum, which was considered to have gone extinct by the end of the Pleistocene, appears as a modern component of marine sediment from the north and southwestern Gulf. Our results thus demonstrate a biostratigraphical range extending to the present at least in the study area. This palynological investigation highlights the importance of the Gulf of Mexico as potential refuge for late Cenozoic species thought to be extinct (C) 2013 Elsevier B.V. All rights reserved.	[Limoges, Audrey; de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Londeix, Laurent] Univ Bordeaux 1, UMR EPOC 5805, F-33405 Talence, France	University of Quebec; University of Quebec Montreal; Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux; CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Limoges, A (通讯作者)，Univ Quebec, Geotop, CP 8888,Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.	limoges.audrey@gmail.com	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Limoges, Audrey/0000-0002-4587-3417	Fonds de Recherche Nature et Technologies of Quebec	Fonds de Recherche Nature et Technologies of Quebec	This study was possible through the financial support of Fonds de Recherche Nature et Technologies of Quebec. We thank Ana-Carolina Ruiz-Fernandez, Rosalba Alonso-Rodriguez and Marie-Yasmine Bottein for the organization of the sampling campaign in the Mexican lagoons and along the Florida coast We are grateful to Captain Dean and Charles for their help and assistance at sea along the Florida coast and Maria Luisa Machain Castillo for providing sediments from the southwestern Gulf of Mexico. Special thanks go to Maryse Henry, Taoufik Radi, Nicolas Van Nieuwenhove and Andre Rochon for their help with the dinocyst identifications. We also gratefully acknowledge Stijn De Schepper and Sophie Warny for their helpful and constructive review comments.	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J	Mohamed, O; Wagreich, M				Mohamed, Omar; Wagreich, Michael			Organic-walled dinoflagellate cyst biostratigraphy of the Well Hoflein 6 in the Cretaceous-Paleogene Rhenodanubian Flysch Zone (Vienna Basin, Austria)	GEOLOGICA CARPATHICA			English	Article						Cretaceous; Paleogene; Vienna Basin; Rhenodanubian Flysch Zone; biostratigraphy; organic-walled dinoflagellate cysts	OUTER WESTERN CARPATHIANS; EOCENE THERMAL MAXIMUM; PALAEOCENE/EOCENE BOUNDARY; TERTIARY BOUNDARY; PALEOCENE; MARINE; PATTERNS; ISOTOPE; GERMANY; RECORDS	Palynological analysis of the Rhenodanubian Flysch Zone section recovered from Well Hoflein 6 north of Vienna allows the successful application of non-calcareous dinoflagellate biostratigraphy to the deep-water sediments of the Greifenstein Nappe. All 62 cuttings samples contained organic-walled dinoflagellate cysts (dinocysts) and some of them allow age-assessment. The results corroborated the presence of two thrust slices. The upper thrust unit A comprises a Campanian to Lower Eocene succession including, from old to young, the Rothenbach Subgroup, Perneck Formation, Altlengbach Formation and Greifenstein Formation. The lower thrust unit B contains in addition a pre-Campanian base, probably the Wolfpassing Formation of Early to mid-Cretaceous age.	[Mohamed, Omar] Menia Univ, Fac Sci, Dept Geol, El Minia, Egypt; [Mohamed, Omar; Wagreich, Michael] Univ Vienna, Ctr Earth Sci, Dept Geodynam & Sedimentol, A-1090 Vienna, Austria	Egyptian Knowledge Bank (EKB); Minia University; University of Vienna	Mohamed, O (通讯作者)，Menia Univ, Fac Sci, Dept Geol, El Minia, Egypt.	omar.mohamed@mu.edu.eg	Wagreich, Michael/D-2279-2013	Mohamed, Omar/0000-0002-2817-1683; Wagreich, Michael/0000-0002-8828-0857				Auffret J.-P., 1975, Bulletin de la Societe Geologique de France, V17, P641; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; Caro Y., 1973, Revista Esp Micropaleont, V5, P329; Chateauneuf J.J., 1980, Memorie du Bureau de Recherches Geologiques et Minieres, V116, P1; Corradini D., 1973, B SOC PALEONTOL ITAL, V11, P119; Costa L.I., 1992, P99; Costa L.I., 1981, GEOL BAVARIA, V82, P315; de Coninck J., 1983, Tertiary Research, V5, P83; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Edwards L.E., 1989, 1489C US GEOL SURV, P1; Egger H, 1995, N JB GEOL PALAONT AB, V196, P69; Egger H, 2008, CRETACEOUS RES, V29, P405, DOI 10.1016/j.cretres.2007.03.002; Egger Hans, 1993, Zitteliana, V20, P59; El-Beialy S.Y., 1990, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V180, P117; Faupl P., 1996, GEOLOGISCHE BUNDESAN, V33, P1; Fensome R.A., 1993, CLASSIFICATION FOSSI; Fensome R.A., 2008, AM ASS STRATIGRAPHIC, V1; Ferrow E, 2011, GEOCHIM COSMOCHIM AC, V75, P657, DOI 10.1016/j.gca.2010.10.016; Gedl Przemyslaw, 2007, Studia Geologica Polonica, V127, P101; Gorka H., 1963, Acta Palaeontologica Polonica, V8, P1; Grun W., 1972, Jahrbuch der Geologischen Bundesanstalt Wien, V115, P103; Hamilton W., 2000, MITTEILUNGEN OSTERRE, V92, P235; Heilmann-Clausen C., 1989, Geol. 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Carpath.	JUN	2013	64	3					209	+		10.2478/geoca-2013-0015	http://dx.doi.org/10.2478/geoca-2013-0015			34	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	214XU		gold			2025-03-11	WOS:000324172900004
J	Leighfield, TA; Muha, N; Miles, CO; Ramsdell, JS				Leighfield, Tod A.; Muha, Noah; Miles, Christopher O.; Ramsdell, John S.			Semisynthesis of Radio labeled Amino Acid and Lipid Brevetoxin Metabolites and Their Blood Elimination Kinetics in C57BL/6 Mice	CHEMICAL RESEARCH IN TOXICOLOGY			English	Article							TISSUE DISTRIBUTION; GREENSHELL MUSSELS; PERNA-CANALICULUS; PBTX-3; OYSTER; EXCRETION; BINDING; PLASMA; ESTERS	Brevetoxin B (BTX-B), produced by dinoflagellates of the species Karenia, is a highly reactive molecule, due in part to an alpha,beta-unsaturated aldehyde group at the terminal side chain, leading to the production of metabolites in shellfish by reduction, oxidation, and conjugation. We have investigated in mice the blood elimination of three common bioactive brevetoxin metabolites found in shellfish, which have been semisynthesized from BTX-B in radioactive forms. BTX-B was reduced at C42 to yield [H-3] dihydro-BTX-B. [H-3] S-desoxy-BTX-B2 (cysteine brevetoxin B) was semisynthesized from BTX-B by the conjugation of cysteine at the C50 olefinic group then [H-3] radiolabeled by C42 aldehyde reduction. [HC] N-Palmitoyl-S-desoxy-BTX-B2 was prepared using S-desoxy-BTX-B2 as the starting material with addition of the [C-14] radiolabeled fatty acid via cysteine amide linkage. The elimination of intravenously administered [H-3] S-desoxy-BTX-B2, [C-14] N-palmitoyl-S-desoxy-BTX-B2, or [H-3] dihydroBTX-B was measured in blood collected from C57BL/6 mice over a 48 h period. Each brevetwdn metabolite tested exhibited biexponential elimination kinetics and fit a two-compartment model of elimination that was applied to generate toxicokinetic parameters. The rate of transfer between the central compartment (i.e., blood) and the peripheral compartment (e.g., tissue) for each brevetoxin differed substantially, with dihydro-BTX-B exchanging rapidly with the peripheral compartment, S-desoxy-BTX-B2 eliminating rapidly from the central compartment, and N-palmitoyl-S-desoxy-BTX-B2 eliminating slowly from the central compartment. Toxicokinetic parameters were analyzed in the context of the unique structure of each brevetoxin metabolite resulting from a reduction, amino acid conjugation, or fatty acid addition to BTX-B.	[Leighfield, Tod A.; Muha, Noah; Ramsdell, John S.] NOAA, Natl Ocean Serv, Marine Biotoxins Program, Ctr Coastal Environm Hlth & Biomol Res, Charleston, SC 29412 USA; [Miles, Christopher O.] Norwegian Vet Inst, N-0106 Oslo, Norway	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; Norwegian Veterinary Institute	Ramsdell, JS (通讯作者)，NOAA, Natl Ocean Serv, Marine Biotoxins Program, 219 Ft Johnson Rd, Charleston, SC 29412 USA.	john.ramsdell@noaa.gov		Leighfield, Tod/0000-0002-6780-8800	National Oceanic and Atmospheric Administration; Marie Curie International Incoming Fellowship within the seventh European Community Framework Programme [221117]	National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); Marie Curie International Incoming Fellowship within the seventh European Community Framework Programme(European Union (EU))	This work was supported by the National Oceanic and Atmospheric Administration and a Marie Curie International Incoming Fellowship within the seventh European Community Framework Programme (FP7/2007-2013) under grant agreement No. 221117 (to C.O.M.).	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Res. Toxicol.	JUN	2013	26	6					868	877		10.1021/tx4000057	http://dx.doi.org/10.1021/tx4000057			10	Chemistry, Medicinal; Chemistry, Multidisciplinary; Toxicology	Science Citation Index Expanded (SCI-EXPANDED); Index Chemicus (IC)	Pharmacology & Pharmacy; Chemistry; Toxicology	168EU	23642029				2025-03-11	WOS:000320689300004
J	Soliman, A; Feist-Burkhardt, S; Harzhauser, M; Kern, AK; Piller, WE				Soliman, Ali; Feist-Burkhardt, Susanne; Harzhauser, Mathias; Kern, Andrea K.; Piller, Werner E.			<i>Mendicodinium mataschenensis</i>: a new endemic dinoflagellate cyst from the Late Miocene (Tortonian) of Lake Pannon (Austria)	PALYNOLOGY			English	Article						dinoflagellate cysts; Mendicodinium; Lake Pannon; Mataschen; Austria; Late Miocene	BIOSTRATIGRAPHY; INDICATORS; MARMARA; MARGIN; MIDDLE; BASIN	The organic-walled dinoflagellate cyst Mendicodinium mataschenensis is introduced here as a new species. The taxon derives from lower Tortonian clays from the Mataschen clay pit in Styria, Austria. These deposits formed in Lake Pannon, which was characterized throughout the Late Miocene by its highly endemic and rapidly evolving biota. As most species of Mendicodinium are known from restricted marine and brackish paleoenvironments, its occurrence in Lake Pannon may be considered further evidence for the brackish water conditions prevailing in this lake.	[Soliman, Ali; Piller, Werner E.] Graz Univ, Inst Earth Sci, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Geol Department, Fac Sci, Tanta 31527, Egypt; [Feist-Burkhardt, Susanne] SFB Geol Consulting & Serv, D-64372 Ober Ramstadt, Germany; [Harzhauser, Mathias; Kern, Andrea K.] Nat Hist Museum Vienna, Geol Paleontol Dept, A-1010 Vienna, Austria	University of Graz; Egyptian Knowledge Bank (EKB); Tanta University	Soliman, A (通讯作者)，Graz Univ, Inst Earth Sci, Heinrichstr 26, A-8010 Graz, Austria.	ali.soliman@uni-graz.at	Soliman, Ali/R-1583-2018; Feist-Burkhardt, Susanne/B-1522-2009; Kern, Andrea K./V-5078-2017	Piller, Werner E./0000-0003-2808-4720; Kern, Andrea K./0000-0002-9343-0696; Harzhauser, Mathias/0000-0002-4471-6655; Feist-Burkhardt, Susanne/0000-0001-6019-6242; Soliman, Ali/0000-0001-7366-4607	FWF [P21414-B16]; Austrian Science Fund (FWF) [P21414] Funding Source: Austrian Science Fund (FWF)	FWF(Austrian Science Fund (FWF)); Austrian Science Fund (FWF)(Austrian Science Fund (FWF))	This study was supported by the FWF-project P21414-B16. We are grateful to Martin Gross (Joanneum Museum, Graz) for samples and valuable discussions. We would also like to thank J.B. Riding, S. Louwye and an anonymous reviewer for their constructive comments and suggestions.	[Anonymous], 1914, BER DTSCH BOT GES, DOI DOI 10.1111/J.1438-8677.1914.TB07573.X; [Anonymous], 1885, HG BRONNS KLASSEN OR; 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]; BUTLER N, 1995, J MICROPALAEONTOL, V14, P25, DOI 10.1144/jm.14.1.25; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; Davey R.J., 1979, American Association of Stratigraphic Palynologists Contributions Series, V5B, P48; Donders TH, 2009, EARTH PLANET SC LETT, V281, P215, DOI 10.1016/j.epsl.2009.02.034; Draxler I, 1994, JUBILAUMSSCHRIFT 20, P19; Ensom PC, 2009, CRETACEOUS RES, V30, P699, DOI 10.1016/j.cretres.2008.12.005; Feist-Burkhardt S, 1996, 9 INT PAL C 23 28 JU, P42; Fensome R. 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J	Lindström, S				Lindstrom, Sofie			A review of the enigmatic microalga <i>Tetranguladinium</i> Yu etal. 1983 ex Chen etal. 1988; palaeoecology, stratigraphy and palaeogeographical distribution	PALYNOLOGY			English	Article						Zygnemataceae; zygospores; Tetranguladinium; palaeoecology; Scandinavia	YELLOW SEA BASIN; AQUATIC PALYNOMORPHS; TECTONIC EVOLUTION; RABEKKE FORMATION; TENDAGURU BEDS; STRATA; BOUNDARY; ZYGNEMATACEAE; BORNHOLM; ALGAE	The probable zygnematacean zygospore Tetranguladinium is recorded in Mesozoic strata from southern Scandinavia for the first time. Tetranguladinium, which exhibits morphological similarities to the extant filamentous green alga Mougeotia, occurs in Jurassic-Cretaceous (J/K) boundary (latest Tithonian-Early Berriasian) assemblages from the Vomb Trough, southern Sweden and on the Danish island of Bornholm. The J/K boundary strata of southern Scandinavia were deposited in marginal marine settings, varying from freshwater marshes, lakes and flood plains, to lagoons, shoreface, and shallow marine to fully marine environments. The assemblages containing Tetranguladinium are diverse, consisting of spores and pollen, the colonial green alga Botryococcus, various other zygnematacean zygospores e.g. Ovoidites, Schizosporis and Tetraporina, and rare marine dinoflagellate cysts. A review of published fossil occurrences of Tetranguladinium reveals that its stratigraphical range extends at least from the Late Guadalupian (Mid Permian) to the Holocene. It has been recorded from Africa (Tanzania), Asia (China, Korea), Australia, northwest Europe (Denmark, Great Britain, Sweden), North America (Canada, USA), and South America (Argentina). Depositional and palaeoclimatological data for the known localities of Tetranguladinium confirm a preference for freshwater settings in a humid warm temperate to subtropical-tropical climate, often with a pronounced dry season. The palaeogeographical positions of all the known Tetranguladinium localities indicate that it is has stayed restricted within narrow belts between 30-40 south and 30-60 north of the palaeoequator since the Late Jurassic.	[Lindstrom, Sofie] Geol Survey Denmark & Greenland GEUS, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Lindström, S (通讯作者)，Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	sli@geus.dk	Lindström, Sofie/G-5481-2018	Lindstrom, Malin Sofie/0000-0001-8278-1055	Swedish Geological Survey (SGU); Crafoord Foundation	Swedish Geological Survey (SGU); Crafoord Foundation	The Fararp-1 core drilling was financed by grants to the author from the Swedish Geological Survey (SGU) and the Crafoord Foundation. Dr Y. Tsukii, Hosei University, Japan, is gratefully acknowledged for allowing the author permission to reprint the photographs of Mougeotia. The author is grateful for helpful comments from Pierre Zippi and an anonymous reviewer.	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J	Candel, MS; Borromei, AM; Martínez, MA; Bujalesky, G				Soledad Candel, Maria; Maria Borromei, Ana; Martinez, Marcelo A.; Bujalesky, Gustavo			Palynofacies analysis of surface sediments from the Beagle Channel and its application as modern analogues for Holocene records of Tierra del Fuego, Argentina	PALYNOLOGY			English	Article						palynofacies; surface sediments; modern analogues; Beagle Channel; Argentina	WALLED DINOFLAGELLATE CYSTS; SOUTHERNMOST SOUTH-AMERICA; LATE QUATERNARY; ARCTIC-OCEAN; MARINE; INDICATORS; PRESERVATION; REGION; PALYNOLOGY; EVOLUTION	Palynofacies analysis of surface sediments from the Beagle Channel, Tierra del Fuego, Argentina, was carried out to establish modern analogues for comparison with other Holocene marine records in southern Isla Grande de Tierra del Fuego. Our results show the dominance of highly degraded translucent phytoclasts, associated with amorphous organic matter (AOM) and palynomorphs, while opaque phytoclasts are poorly represented. The organic constituents indicate the proximity of the continental source area to marine environments, with distances and/or times of relatively short transport. The predominance of translucent phytoclasts associated with pyrite suggests reducing conditions, probably associated with marginal-marine environments. Among the terrestrial palynomorph group, the predominance of Nothofagus pollen reveals the presence of forests along the channel. The high terrestrial organic matter input to the depositional area are consistent with a marginal-marine environment. The aquatic palynomorphs, mainly dinoflagellate cyst's show assemblages characterised by low species diversity and low concentration values. The dominance of Peridiniales over Gonyaulacales suggests inner neritic environments. Comparison with two fossil sections of Mid-Late Holocene age (Albufera Lanushuaia and Rio Ovando) shows similar distribution of the total palynological matter.	[Soledad Candel, Maria; Maria Borromei, Ana; Martinez, Marcelo A.] Univ Nacl Sur, INGEOSUR CONICET, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Bujalesky, Gustavo] CADIC CONICET, Ushuaia, Tierra Del Fueg, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); 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, INGEOSUR CONICET, Dept Geol, San Juan 670,B8000ICN, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	scandel@uns.edu.ar		Martinez, Marcelo/0000-0003-0538-4739	CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas) [PIP 02787/02, PIP 06/06 6200, PIP 09/011 0533]; Agencia de Promocion Cientifica y Tecnologica [PICT Redes 2002-00067]; Fundacion Antorchas [A-13672/1-2]	CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Agencia de Promocion Cientifica y Tecnologica(ANPCyT); Fundacion Antorchas	The authors are grateful to Mirta Quattrocchio (INGEOSUR-CONICET, Universidad Nacional del Sur) for the critical reading on an earlier version of the manuscript. We wish to thank two anonymous reviewers for their constructive comments that helped to improve the final version of the manuscript. We are also grateful to Anne de Vernal and Taoufik Radi from the Centre de recherche en geochimie et geodynamique (GEOTOP-UQAM, Universite du Quebec a Montreal) for their help in the systematic identifications of dinoflagellate cysts. This study was supported by CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas; PIP 02787/02) and the Agencia de Promocion Cientifica y Tecnologica (PICT Redes 2002-00067) grants to Mirta Quattrocchio and Ana Maria Borromei, respectively. CONICET (PIP 06/06 6200, PIP 09/011 0533) and Fundacion Antorchas (Proyecto A-13672/1-2) provided to Gustavo Bujalesky the financial support for field-work in the Beagle Channel.	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J	Wang, ZH; Fu, YH; Kang, W; Liang, JF; Gu, YG; Jiang, XL				Wang, Zhao-Hui; Fu, Yong-Hu; Kang, Wei; Liang, Ju-Fang; Gu, Yang-Guang; Jiang, Xiao-Liang			Germination of phytoplankton resting cells from surface sediments in two areas of the Southern Chinese coastal waters	MARINE ECOLOGY-AN EVOLUTIONARY PERSPECTIVE			English	Article						Cysts; germination; phytoplankton; resting stages; sediments; Southern China	HARMFUL ALGAL BLOOMS; DINOFLAGELLATE CYSTS; DAYA BAY; DINOPHYCEAE; SCRIPPSIELLA; TEMPERATURE; SALINITY	To understand the role of phytoplankton resting cells in the outbreak of algal blooms, particularly harmful algal blooms, surface sediments were collected monthly from April 2007 to March 2008 from two bays near the international ports in the Southern Chinese coastal waters. Sieved sediments were incubated for 20 and 40days, and germinated vegetative cells were observed. Altogether, 97 taxa were recorded, of which 50 were diatoms and 35 dinoflagellates. Vegetative cells of cyanobacteria, chlorophytes, dictyophytes, euglenophytes, haptophytes, and raphidophytes were also observed. Centric diatoms such as Chaetoceros, Melosira, Skeletonema, and Thalassiosira dominated. Scrippsiella, Gymnodinium, and Alexandrium were common dinoflagellate taxa. Diatom spores germinated in samples from all seasons but were abundant in the autumn and winter samples. Low numbers of dinoflagellate cells germinated in the winter samples. The nanophytoplankton taxa, Gymnodinium corii and Chrysochromulina sp., which have not been recorded in the previous phytoplankton surveys, were abundant, suggesting either their new appearance in the water column or perhaps that they were overlooked in routine phytoplankton monitoring due to their small sizes. Vegetative cells of harmful or potentially harmful taxa were germinated, and some of them such as Amphidinium, Gambierdiscus, Ostreopsis, and Coolia have not previously been reported in the study area. Based on the results of the incubation of sediments from the two bays near the international ports, it is suggested that international shipping increases the risk of the introduction of new phytoplankton species and thus promotes the incidence of harmful algal blooms.	[Wang, Zhao-Hui; Fu, Yong-Hu; Kang, Wei; Liang, Ju-Fang; Gu, Yang-Guang; Jiang, Xiao-Liang] Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Guangdong, Peoples R China; [Wang, Zhao-Hui] Guangdong Higher Educ Inst, Key Lab Aquat Eutrophicat & Control Harmful Algal, Guangzhou, Guangdong, Peoples R China	Jinan University; Chinese Academy of Sciences	Wang, ZH (通讯作者)，Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Guangdong, Peoples R China.	twzh@jnu.edu.cn	Kang, Wei/JUV-4778-2023; Gu, Yang-Guang/C-8275-2009	Gu, Yang-Guang/0000-0003-2314-0463; Chi, Hai/0000-0003-3072-511X	National Key Technology R & D Program of China [2012BAC07B05]; National Natural Foundation of China [41076093]	National Key Technology R & D Program of China(National Key Technology R&D Program); National Natural Foundation of China(National Natural Science Foundation of China (NSFC))	The authors gratefully acknowledge Dr. Larry B. Liddle of Long Island University, USA, for reviewing the manuscript. 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Ecol.-Evol. Persp.	JUN	2013	34	2					218	232		10.1111/maec.12009	http://dx.doi.org/10.1111/maec.12009			15	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	150VV					2025-03-11	WOS:000319420400007
J	Bowman, VC; Riding, JB; Francis, JE; Crame, JA; Hannah, MJ				Bowman, Vanessa C.; Riding, James B.; Francis, Jane E.; Crame, J. Alistair; Hannah, Michael J.			The taxonomy and palaeobiogeography of small chorate dinoflagellate cysts from the Late Cretaceous to Quaternary of Antarctica	PALYNOLOGY			English	Article						dinoflagellate cysts; acritarchs; taxonomy; palaeobiogeography; Cretaceous-Quaternary; Antarctica	JAMES-ROSS-ISLAND; SEYMOUR-ISLAND; COCKBURN ISLAND; MARAMBIO GROUP; HUMPS-ISLAND; GUSTAV-GROUP; VEGA-ISLAND; CAPE LAMB; STRATIGRAPHY; PENINSULA	Small chorate dinoflagellate cysts are common in Upper Cretaceous to Quaternary sedimentary successions around the Antarctic margin. Taxonomic confusion surrounding dinoflagellate cysts and acritarchs of similar morphology throughout the southern high palaeolatitudes has hitherto limited investigation of their palaeoecological significance. This study aims to solve the taxonomic problems, and to allow a new assessment of dinoflagellate cyst acmes. A detailed morphological study of new material from the Lopez de Bertodano Formation of Seymour Island, Antarctic Peninsula, is presented. These dinoflagellate cysts are identified as Impletosphaeridium clavus Wrenn & Hart 1988 emend. nov. Their gross morphology and their vast abundances in the James Ross Basin are strongly suggestive of dinoflagellate blooms. This scenario implies similarities to modern dinoflagellate cysts from the polar regions.	[Bowman, Vanessa C.; Francis, Jane E.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England; [Riding, James B.] British Geol Survey, Environm Sci Ctr, Keyworth NG12 5GG, Notts, England; [Crame, J. Alistair] British Antarctic Survey, Cambridge CB3 0ET, England; [Hannah, Michael J.] Victoria Univ Wellington, Sch Geog Environm & Earth Sci, Wellington 6012, New Zealand	University of Leeds; 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; Victoria University Wellington	Bowman, VC (通讯作者)，Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England.	v.c.bowman@leeds.ac.uk	; Hannah, Michael/H-1083-2015	Bowman, Vanessa/0000-0002-4887-3949; Hannah, Michael/0000-0002-2275-0086	Natural Environment Research Council (NERC) Antarctic Funding Initiative (AFI) project [NE/C506399/1]; NERC project [NE/100582X/1]; TransAntarctic Association; Antarctic Science Bursary; NERC [NE/I00582X/1, bgs05002, NE/I005803/1, NE/I00582X/2, bas0100026] Funding Source: UKRI	Natural Environment Research Council (NERC) Antarctic Funding Initiative (AFI) project(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC project(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); TransAntarctic Association; Antarctic Science Bursary; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research was funded by a Natural Environment Research Council (NERC) Antarctic Funding Initiative (AFI) project (Grant NE/C506399/1) entitled "Terminal Cretaceous climate change and biotic response in Antarctica' and a subsequent related NERC project entitled "Impact of global disturbances on the evolution of life in the polar regions during the Cenozoic' (Grant NE/100582X/1). The fieldwork was supported logistically by the British Antarctic Survey. Vanessa C. Bowman thanks the TransAntarctic Association and the Antarctic Science Bursary for additional financial support and Eric Condliffe (formerly of the Leeds Electron Microscopy and Spectroscopy Centre, University of Leeds) for technical assistance. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). The authors wish to thank Rex Harland, Kenneth N. Mertens, Meriel Fitzpatrick and Sophie Warny for constructive reviews that significantly improved the manuscript.	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J	Slimani, H; Louwye, S				Slimani, Hamid; Louwye, Stephen			New organic-walled dinoflagellate cyst species from the Upper Cretaceous-Lower Palaeocene Chalk Group in the Meer and Turnhout boreholes, Campine Basin, northern Belgium	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Campanian-Danian; biostratigraphy; Campine Basin; northern Belgium	BIOSTRATIGRAPHY; NETHERLANDS	The Campanian to Danian Chalk Group from the Meer and Turnhout boreholes in the Campine Basin, northern Belgium, contains four new species and a subspecies of organic-walled dinoflagellate cyst previously left in open nomenclature. These species were recorded within rich, diverse and well-preserved assemblages and are formally described here. A re-assessment of their stratigraphic ranges is presented. Apteodinium crassus sp. nov. is characterized by a very thick and finely spongeous wall, with or without a cingulum. Cribroperidinium wilsonii subsp. trabeculosum subsp. nov. is distinguished by its slender processes that are distally uniformly connected by thin trabeculae. Elytrocysta elongata sp. nov. differs from other Elytrocysta species by its small size and the elongate cylindrical shape. Spinidinium delicatum sp. nov. is a small Spinidinium species and has very delicate sutural crests that are very finely serrate to finely denticulate. Spumadinium irregulare sp. nov. is an intermediate to large holocavate dinoflagellate cyst with the endophragm and periphragm irregularly connected by thin columellae or pillars of different length. (C) 2013 Elsevier B.V. All rights reserved.	[Slimani, Hamid] Univ Mohammed V Agdal, Lab Geol & Remote Sensing, URAC 46, Inst Sci, 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, Lab Geol & Remote Sensing, URAC 46, Inst Sci, 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))	Mrs. S. Vancauwenberghe (Research Unit Palaeontology, Ghent University, Belgium) is kindly thanked for the palynological preparation of the samples. The financial support by the University Mohammed V-Agdal (project SVT 11/09) and the "Centre National de la Recherche Scientifique et Technique" (CNRST) (URAC46), Morocco is respectfully acknowledged. Dr. Mike Stephenson (Editor) and two anonymous journal reviewers are thanked for their careful reviews.	[Anonymous], 1978, ANALYSES PREPLEISTOC; Brinkhuis H, 2000, REV PALAEOBOT PALYNO, V110, P93, DOI 10.1016/S0034-6667(99)00062-7; DRUGG W.S., 1967, PALAEONTOGRAPHICA B, V120, P1; Felder P.J., 2001, Memoirs of the Geological Survey of Belgium, V47, P1; Felder P.J., 1981, PUBLICATIES NATUURHI, V31, P1; Felder P.J, 1985, GEOLOGICAL SURVEY BE, V214, P1; Felder P.J., 1994, GEOLOGICAL SURVEY BE, V275, P1; Felder W. M., 1975, Toelichting bij geologische overzichtskaarten van Nederland, P63; Felder W.M, 2000, GEOLOGIE NEDERLAND 5, P1; Fensome R. 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Palaeobot. Palynology	MAY 15	2013	192						10	21		10.1016/j.revpalbo.2012.12.001	http://dx.doi.org/10.1016/j.revpalbo.2012.12.001			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	165OG					2025-03-11	WOS:000320492600002
J	Sarai, C; Yamaguchi, A; Kawami, H; Matsuoka, K				Sarai, Chihiro; Yamaguchi, Aika; Kawami, Hisae; Matsuoka, Kazumi			Two new species formally attributed to <i>Protoperidinium oblongum</i> (Aurivillius) Park et Dodge (Peridiniales, Dinophyceae): Evidence from cyst incubation experiments	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Votadinium calvum; Protoperidinium quadrioblongum; Protoperidinium paraoblongum; dinoflagellate; cyst-motile form relationship; molecular phylogeny	DINOFLAGELLATE RESTING CYSTS; MOLECULAR PHYLOGENY; THECA RELATIONSHIP; RECENT SEDIMENTS; SP-NOV; GENUS	Cyst-theca relationships of the common armored dinoflagellate Protoperidinium oblongum were re-investigated by incubation experiments and molecular phylogenetic analysis. Living cysts provided for incubation experiments were collected from several places in Japan, including Omura Bay, West Japan and Lake Saroma in Hokkaido, North Japan. One hundred and four cysts were incubated and 18 motile cells were germinated from these cysts. To clarify their morphological characteristics both cysts and germinated thecate cells were observed, especially the archeopyle type, the number and shape of anterior intercalary plates, and the shape and development of apical and antapical horns. In order to provide molecular phylogenetic analysis, germinated cells from incubated cysts were examined for their LSU rDNA sequences. Results reveal that three morphologically different cysts produced three morphologically different thecate cells, which were previously known as Protoperidinium oblongum var. latidorsale, Protoperidinium oblongum var. inaequale, and Protoperidinium oblongum var. symmetricum. The molecular phylogenetic analysis demonstrated that the Oceania group in the genus Protoperidinium includes these three varieties as well as Protoperidinium divergens, Protoperidinium claudicans, and Protoperidinium steigingerae. This group is separated from Protoperidinium sensu strict, and the three plankton forms are phylogenetically separate and independent species. Based on these facts, two new species, Protoperidinium quadrioblongum Sarai, Kawami et Matsuoka, the new name for Protoperidinium oblongum var. symmetricum and Protoperidinium paraoblongum Sarai, Kawami et Matsuoka for Protoperidinium oblongum var. inaequale are described. (C) 2013 Elsevier B.V. All rights reserved.	[Sarai, Chihiro] Nagasaki Univ, Fac Fisheries, Nagasaki 8528521, Japan; [Yamaguchi, Aika] Okinawa Inst Sci & Technol, Microbiol & Biochem Secondary Metabolites Unit, Kunigami, Okinawa 9040412, Japan; [Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, Nagasaki 8512213, Japan	Nagasaki University; Okinawa Institute of Science & Technology Graduate University; Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst East China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.	kazu-mtk@nagasaki-u.ac.jp			 [21340153]		The authors much appreciate Dr. Y. Takano and Ms Y. Ikeda who kindly helped in molecular phylogenetic analysis and cyst incubation experiments. We also thank deeply Dr. Rex Harland and another reviewer for their constructive suggestions, comments and linguistic corrections. This work was partly supported by Grant-in-Aid (Re: 21340153) for Science of Japan Society for the Promotion of Science.	Abe T. 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Palaeobot. Palynology	MAY 15	2013	192						103	118		10.1016/j.revpalbo.2012.12.007	http://dx.doi.org/10.1016/j.revpalbo.2012.12.007			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	165OG					2025-03-11	WOS:000320492600008
J	Prebble, JG; Crouch, EM; Carter, L; Cortese, G; Bostock, H; Neil, H				Prebble, J. G.; Crouch, E. M.; Carter, L.; Cortese, G.; Bostock, H.; Neil, H.			An expanded modern dinoflagellate cyst dataset for the Southwest Pacific and Southern Hemisphere with environmental associations	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cyst; modern; sea surface temperature; Southwest Pacific; Southern Hemisphere	SEA-SURFACE CONDITIONS; EAST AUSTRALIAN CURRENT; NEW-ZEALAND; SUBTROPICAL FRONT; HYDROGRAPHIC CONDITIONS; PHYTOPLANKTON ASSEMBLAGES; PLANKTONIC-FORAMINIFERA; PHYSICAL OCEANOGRAPHY; PRIMARY PRODUCTIVITY; SOUTHLAND CURRENT	Organic-walled dinoflagellate cyst (dinocyst) assemblages were examined in 120 sea floor sediment samples from the Southwest (SW) Pacific to highlight dinocyst distribution in the region. From these 120 samples, census counts of 40 samples were added to previously published census data from the Southern Hemisphere to form a modern dataset of 311 samples (SH-311). Cluster analysis (k-means clustering) of a 98-sample sub-set from the SW Pacific (NZ-98) reveals four distinct assemblages which coincide with modern Subantarctic surface water, the Subtropical Front and two clusters from Subtropical surface water. A similar clustering of the SH-311 dataset reveals an additional three assemblages, two associated with Polar waters colder than those sampled in the SW Pacific, and one that may be endemic to the South Atlantic Ocean. Multivariate ordination (canonical correspondence analysis and redundancy analysis) indicates that the dinocyst assemblages change most along a sea surface temperature (SST) gradient, in both the regional SW Pacific and Southern Hemisphere datasets. SST accounts for 38% to 56% of the species-environmental relationship after removal of covarying variables, and contributes 2-3 times the explainable inertia than the other environmental variables tested. Both modern datasets (SH-311 and NZ-98) are suitable as a training set for quantitative palaeotemperature transfer functions applied to Late Quaternary records, with the caveat that the modern assemblage also displays sensitivity to productivity, shoreline proximity, bottom water oxygen, and water mass; variation that may be exploited in certain situations. (c) 2013 Elsevier B.V. All rights reserved.	[Prebble, J. G.; Crouch, E. M.; Cortese, G.] GNS Sci, Lower Hutt 5040, New Zealand; [Prebble, J. G.; Carter, L.] Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand; [Bostock, H.; Neil, H.] Natl Inst Water & Atmospher Res NIWA, Wellington, New Zealand	GNS Science - New Zealand; Victoria University Wellington; National Institute of Water & Atmospheric Research (NIWA) - New Zealand	Prebble, JG (通讯作者)，GNS Sci, POB 30368, Lower Hutt 5040, New Zealand.	j.prebble@gns.cri.nz	Cortese, Giuseppe/C-8281-2011; Crouch, Erica/C-2820-2013; Bostock, Helen/A-6834-2013	Bostock, Helen/0000-0002-8903-8958; Prebble, Joseph/0000-0002-7268-4187; Cortese, Giuseppe/0000-0003-1780-3371	New Zealand government "Bright Futures" scholarship; GNS Science through its Global Change through Time (GCT) programme; FRST	New Zealand government "Bright Futures" scholarship; GNS Science through its Global Change through Time (GCT) programme; FRST(New Zealand Foundation for Research, Science and Technology)	Samples were processed by Sonja Fry and Roger Tremain at the GNS Science Palynology Laboratory. George Scott and Marcus Vandergoes, GNS Science, are thanked for discussion on variation in natural environments, and Karin Zonneveld for sharing data and providing comment on an early version of the manuscript. JP was supported by a New Zealand government "Bright Futures" scholarship, EC and GC acknowledge support from GNS Science through its Global Change through Time (GCT) programme, LC was supported by the FRST funded Antarctica New Zealand Interglacial Climate Extremes (ANZICE) programme. Reviews by R.W. Jordan (Editor) and A. McMinn have improved this manuscript.	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Micropaleontol.	MAY	2013	101						33	48		10.1016/j.marmicro.2013.04.004	http://dx.doi.org/10.1016/j.marmicro.2013.04.004			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	179QP					2025-03-11	WOS:000321536700004
J	Schreck, M; Meheust, M; Stein, R; Matthiessen, J				Schreck, M.; Meheust, M.; Stein, R.; Matthiessen, J.			Response of marine palynomorphs to Neogene climate cooling in the Iceland Sea (ODP Hole 907A)	MARINE MICROPALEONTOLOGY			English	Article						Iceland Sea; Neogene; dinoflagellate cysts; acritarchs; alkenone; paleoenvironment	DINOFLAGELLATE CYST STRATIGRAPHY; NORTHERN NORTH-ATLANTIC; DEEP-WATER CIRCULATION; ICE-RAFTING HISTORY; MIDDLE-MIOCENE; NORDIC SEAS; PLIOCENE-PLEISTOCENE; ARCTIC AMPLIFICATION; SURFACE CONDITIONS; COCCOLITH RECORDS	The present study on ODP Leg 151 Hole 907A combines a detailed analysis of marine palynomorphs (dinoflagellate cysts, prasinophytes, and acritarchs) and a low-resolution alkenone-based sea-surface temperature (SST) record for the interval between 14.5 and 25 Ma, and allows to investigate the relationship between palynomorph assemblages and the paleoenvironmental evolution of the Iceland Sea. A high marine productivity is indicated in the Middle Miocene, and palynomorphs and SSTs both mirror the subsequent long-term Neogene climate deterioration. The diverse Middle Miocene palynomorph assemblages clearly diminish towards the impoverished assemblages of the Late Pliocene; parallel with a somewhat gradual decrease of SSTs being as high as 20 degrees C at similar to 13.5 Ma to around 8 degrees C at similar to 3 Ma. Superimposed, palynomorph assemblages not only reflect Middle to Late Miocene climate variability partly coinciding with the short-lived global Miocene isotope events (Mi-events), but also the initiation of a proto-thermohaline circulation across the Middle Miocene Climate Transition, which led to increased meridionality in the Nordic Seas. Last occurrences of species cluster during three events in the Late Miocene to Early Pliocene and are ascribed to the progressive strengthening and freshening of the proto-East Greenland Current towards modem conditions. A significant high latitude cooling between 6.5 and 6 Ma is depicted by the supraregional "Decahedrella event" coeval with lowest Miocene productivity and a SST decline. In the Early Pliocene, a transient warming is accompanied by surface water stratification and increased productivity that likely reflects a high latitude response to the global biogenic bloom. The succeeding crash in palynomorph accumulation, and a subsequent interval virtually barren of marine palynomorphs may be attributed to enhanced bottom water oxygenation and substantial sea ice cover, and indicates that conditions seriously affecting marine productivity in the Iceland Sea were already established well before the marked expansion of the Greenland Ice Sheet at 3.3 Ma. (c) 2013 Elsevier B.V. All rights reserved.	[Schreck, M.; Meheust, M.; Stein, R.; Matthiessen, J.] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Schreck, M (通讯作者)，Korea Polar Res Inst, Get Pearl Tower,12 Gaetbeol Ro, Inchon, South Korea.	Michael.Schreck@kopri.re.kr		Matthiessen, Jens/0000-0002-6952-2494; Stein, Ruediger/0000-0002-4453-9564	German Research Foundation [DFG MA 3913/2]	German Research Foundation(German Research Foundation (DFG))	This research uses samples and data provided by the Ocean Drilling Program (ODP), and Walter Hale and Alex Willbers are thanked for technical support while sampling at the IODP Core Repository Bremen. J.M. and M.S. acknowledge support by the German Research Foundation (DFG MA 3913/2). We are very grateful to the Editor-in-Chief and two anonymous reviewers for constructive comments. Data supplement is available online at http://doi.pangaea.de/10.1594/PANGAEA.807163.	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Micropaleontol.	MAY	2013	101						49	67		10.1016/j.marmicro.2013.03.003	http://dx.doi.org/10.1016/j.marmicro.2013.03.003			19	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	179QP					2025-03-11	WOS:000321536700005
J	Hessler, I; Young, M; Holzwarth, U; Mohtadi, M; Lückge, A; Behling, H				Hessler, Ines; Young, Martin; Holzwarth, Ulrike; Mohtadi, Mahyar; Lueckge, Andreas; Behling, Hermann			Imprint of eastern Indian Ocean surface oceanography on modern organic-walled dinoflagellate cyst assemblages	MARINE MICROPALEONTOLOGY			English	Article						Organic-walled dinoflagellate cysts; Eastern Indian Ocean; Marine surface sediments; Sea surface conditions	MIXED-LAYER; SEA; SEDIMENTS; PRESERVATION; TEMPERATURE; EQUATORIAL; DYNAMICS; SHELF; JAVA; VARIABILITY	Assemblages of organic-walled dinoflagellate cysts (dinocysts) from 116 marine surface samples have been analysed to assess the relationship between the spatial distribution of dinocysts and modern local environmental conditions [e.g. sea surface temperature (SST), sea surface salinity (SSS), productivity] in the eastern Indian Ocean. Results from the percentage analysis and statistical methods such as multivariate ordination analysis and end-member modelling, indicate the existence of three distinct environmental and oceanographic regions in the study area. Region I is located in western and eastern Indonesia and controlled by high SSTs and a low nutrient content of the surface waters. The Indonesian Throughflow (ITF) region (Region 2) is dominated by heterotrophic dinocyst species reflecting the region's high productivity. Region 3 is encompassing the area offshore north-west and west Australia which is characterised by the water masses of the Leeuwin Current, a saline and nutrient depleted southward current featuring energetic eddies. (c) 2013 Elsevier B.V. All rights reserved.	[Hessler, Ines; Behling, Hermann] Univ Gottingen, Albrecht von Haller Inst, Dept Palynol & Climate Dynam, D-37073 Gottingen, Germany; [Young, Martin] CSIRO Earth Sci & Resource Engn, N Ryde, NSW 2113, Australia; [Hessler, Ines; Holzwarth, Ulrike; Mohtadi, Mahyar] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28358 Bremen, Germany; [Lueckge, Andreas] Bundesanstalt Geowissensch & Rohstoffe, D-30655 Hannover, Germany	University of Gottingen; Commonwealth Scientific & Industrial Research Organisation (CSIRO); University of Bremen	Hessler, I (通讯作者)，Macquarie Univ, Dept Biol Sci, N Ryde, NSW 2109, Australia.	ihessler@marum.de; Martin.Young@csiro.au; uholzwarth@marum.de; mohtadi@uni-bremen.de; Andreas.lueckge@bgr.de; Hermann.Behling@bio.uni-goettingen.de	Mohtadi, Mahyar/N-2106-2014	Mohtadi, Mahyar/0000-0003-3306-0969; Hessler, Ines/0000-0002-7471-8854	Deutsche Forschungsgemeinschaft [BE 2116/10-1]; Deutsche Forschungsgemeinschaft as part of the Bremen International Graduate School for Marine Sciences "Global Change in the Marine Realm"	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); Deutsche Forschungsgemeinschaft as part of the Bremen International Graduate School for Marine Sciences "Global Change in the Marine Realm"	This study was funded by the Deutsche Forschungsgemeinschaft (BE 2116/10-1) and by the Deutsche Forschungsgemeinschaft as part of the Bremen International Graduate School for Marine Sciences "Global Change in the Marine Realm". 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J	Shumilovskikh, LS; Marret, F; Fleitmann, D; Arz, HW; Nowaczyk, N; Behling, H				Shumilovskikh, Lyudmila S.; Marret, Fabienne; Fleitmann, Dominik; Arz, Helge W.; Nowaczyk, Norbert; Behling, Hermann			Eemian and Holocene sea-surface conditions in the southern Black Sea: Organic-walled dinoflagellate cyst record from core 22-GC3	MARINE MICROPALEONTOLOGY			English	Article						Mediterranean-Black Sea reconnection; sea-surface temperature; sea-surface salinity; nutrients; sea-level change; last interglacial	CLIMATE RECONSTRUCTION; HYDROLOGICAL CHANGES; CHLOROPHYLL-A; RED-SEA; SALINITY; MARMARA; TEMPERATURE; LEVEL; DYNAMICS; ASSEMBLAGES	In order to compare the sea-surface conditions in the Black Sea during the Holocene and Eemian, sapropelic parts of marine core 22-GC3 (42 degrees 13.53'N/36 degrees 29.55'E, 838 m water depth) were studied for organic-walled dinoflagellate cyst content. The record shows a change from freshwater/brackish assemblages (Pyxidinopsis psilata, Spiniferites cruciformis, and Caspidinium rugosum) to more marine assemblages (Lingulodinium machaerophorum and Spiniferites ramosus complex) during each interglacial, due to the inflow of saline Mediterranean water. The lacustrine-marine transitions in 22-GC3 occurred at similar to 8.3 cal kyr BP during the early Holocene and similar to 128 kyr BP during the early Eemian, slightly later compared to the onset of interglacial conditions on the adjacent land. Dinoflagellate cyst assemblages reveal higher sea-surface salinity (similar to 28-30) (e.g. Spiniferites pachydermus, Bitectatodinium tepikiense, and Spiniferites mirabilis) around similar to 126.5-121 kyr BP in comparison to the Holocene (similar to 15-20) as well as relatively high sea-surface temperature (e.g. Tuberculodinium vancampoae, S. pachydermus, and S. mirabilis) especially at similar to 127.6-125.3 kyr BP. Establishment of high sea-surface salinity during the Eemian correlates very well with reconstructed relatively high global sea-level and is explained as a combined effect of increased Mediterranean supply and high temperatures at the beginning of the last interglacial. The observed changes in the dinocyst record highlight the importance of nutrients for the composition of the Eemian and Holocene dinocyst assemblages. (C) 2013 Elsevier B.V. All rights reserved.	[Shumilovskikh, Lyudmila S.; Behling, Hermann] Univ Gottingen, Dept Palynol & Climate Dynam, D-37073 Gottingen, Germany; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Fleitmann, Dominik] Inst Geol Sci, CH-3012 Bern, Switzerland; [Fleitmann, Dominik] Univ Bern, Oeschger Ctr Climate Change Res, CH-3012 Bern, Switzerland; [Arz, Helge W.] Leibniz Inst Balt Sea Res, D-18119 Rostock, Germany; [Nowaczyk, Norbert] Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany	University of Gottingen; University of Liverpool; University of Bern; Leibniz Institut fur Ostseeforschung Warnemunde; 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, Untere Karspule 2, D-37073 Gottingen, Germany.	shumilovskikh@yahoo.com	Shumilovskikh, Lyudmila/P-2493-2015; Arz, Helge/A-6659-2013; Fleitmann, Domnik/HSF-0516-2023	Fleitmann, Dominik/0000-0001-5977-8835; Marret-Davies, Fabienne/0000-0003-4244-0437; Arz, Helge Wolfgang/0000-0002-1997-1718	German Research Foundation [BE 2116/20-1, AR 367/9-1, FL 710/1-1]; GFZ-Potsdam; Gary Comer Science and Education Foundation; Swiss National Science Foundation [PP002-110554/1];  [SPP 1266 INTERDYNAMIK]	German Research Foundation(German Research Foundation (DFG)); GFZ-Potsdam; Gary Comer Science and Education Foundation; Swiss National Science Foundation(Swiss National Science Foundation (SNSF)); 	We thank Birgit Plessen, Helmholtz Centre Potsdam-German Research Centre for Geosciences (GFZ-Potsdam), for performing the stable isotope measurements on ostracods. We also thank Antje Wegwerth, Robert Kopp and Frank Schlutz for helpful discussions and comments on the manuscript and Laura Sutcliffe for polishing the English:We gratefully acknowledge the Editor of "Marine Micropaleontology" Frans Jorissen as well as to Kenneth N. Mertens and Stephen Louwye for critical reading and improving the manuscript. Finally, we thank the captain and crew of RV METEOR for their support during the M72/5 Black Sea cruise in 2007. The work was funded by the German Research Foundation (BE 2116/20-1, AR 367/9-1, and FL 710/1-1) through the SPP 1266 INTERDYNAMIK, the GFZ-Potsdam and the Gary Comer Science and Education Foundation. Work on speleothems from Turkey was supported by the Swiss National Science Foundation (grant PP002-110554/1 to D.F.).	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J	Mikulás, R; Boorová, D; Holcová, K				Mikulas, R.; Boorova, D.; Holcova, K.			Problematic microscopic trace (?) fossils, Oligocene, Slovakia	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Pannonian Basin; Oligocene; microfossils; meiofauna; burrows	CALCAREOUS DINOFLAGELLATE CYSTS; SURFACE-WATER; QUATERNARY EASTERN; DISSOLVED-OXYGEN; ATLANTIC; SOUTH; NANNOFOSSILS; DISSOLUTION; DIVERSITY; DYNAMICS	Meioscopic to microscopic capsules found in reddish, probably marine or brackish shales (Oligocene, Pannonian Basin; South Slovakia) are interpreted as possible trace fossils. They may represent burrows of meioscopic in-fauna. Ferruginous walls of the capsules appeared very probably as late as during diagenesis; however, the (possibly organic) matrix had to exist before the diagenetic processes. Other discussed explanations (inorganic "ironstones"; coprolites) are not plausible.	[Mikulas, R.] Acad Sci Czech Republ, Inst Geol, CR-16502 Prague, Czech Republic; [Boorova, D.] Slovak Geol Survey, Bratislava, Slovakia; [Holcova, K.] Charles Univ Prague, Inst Geol & Palaeontol, Prague 12843, Czech Republic	Czech Academy of Sciences; Institute of Geology of the Czech Academy of Sciences; Charles University Prague	Mikulás, R (通讯作者)，Acad Sci Czech Republ, Inst Geol, Rozvojova 269, CR-16502 Prague, Czech Republic.	mikulas@gli.cas.cz; daniela.boorova@geology.sk; holcova@natur.cuni.cz	Mikulas, Radek/F-4136-2010; Holcova, Katarina/I-6992-2017	Mikulas, Radek/0000-0002-9827-2367; Holcova, Katarina/0000-0002-8371-3510	 [MSM0021620855];  [AVOZ 30130516]	; 	This research was supported by grants nos. MSM0021620855 and AVOZ 30130516. We would like to acknowledge the helpful discussion about problematic microfossils by Dr. Milan Havril and Dr. Michal Potfaj (State Geological Institute of Dionyz Stur, Bratislava).	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Geol. Correl.	MAY	2013	21	3					300	311		10.1134/S0869593813030052	http://dx.doi.org/10.1134/S0869593813030052			12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	163WY					2025-03-11	WOS:000320370000006
J	Chen, L; Zonneveld, KAF; Versteegh, GJM				Chen, Liang; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.			Paleoclimate of the Southern Adriatic Sea region during the 'Medieval Climate Anomaly' reflected by organic walled dinoflagellate cysts	HOLOCENE			English	Article						climate; dinoflagellate cysts; Italy; Medieval period; river discharge; temperature	NORTH-ATLANTIC OSCILLATION; RADIOCARBON AGE CALIBRATION; SELECTIVE PRESERVATION; TEMPERATURE VARIATIONS; MEDITERRANEAN REGION; ISOTOPE RECORD; WESTERN-EUROPE; SAHARAN DUST; VOLCANIC ASH; WARM PERIOD	To obtain insight into the character and forcing of southern Italian climate change during the 'Medieval Climate Anomaly' (c. AD 900-1200), marine sediments deposited between ad 990 and 1200 from the Gulf of Taranto have been analyzed for their dinoflagellate cyst content with a 3.5 yr resolution. The reconstructed sea surface temperature (SST) appears to be lower than today. We observe a clear 11.4 yr cyclicity in the reconstructed SST series. Furthermore, there is a good matching between SST and global C-14 anomalies. This suggests that solar activity might have had an important influence on the local climate during Medieval time. Short-term fluctuations in accumulation rates of aerobic degradation resistant species that react sensitively on the trophic state of the upper waters and/or are characteristic for river plume waters indicate that the trophic state of the upper waters is closely linked to river discharge, which in turn is strongly related to precipitation in Italy. We reconstruct low river discharge/precipitations in the Adriatic area synchronous to widespread drought events in other nearby subtropical regions. We attribute this to NAO and ENSO related large-scale ocean-atmosphere circulation shifts during the Medieval period. Furthermore, we suggest that eruptions of southern Italian volcanoes might have influenced the local upper water nutrient conditions as well.	[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-28334 Bremen, Germany	University of Bremen; University of Bremen	Chen, L (通讯作者)，Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany.	lichen@uni-bremen.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776	DFG as part of the ESF/EuroMarc project MOCCHA (Multidisciplinary study of continental/ocean climate dynamics using high-resolution records from the eastern Mediterranean)	DFG as part of the ESF/EuroMarc project MOCCHA (Multidisciplinary study of continental/ocean climate dynamics using high-resolution records from the eastern Mediterranean)	The study is funded by the DFG as part of the ESF/EuroMarc project MOCCHA (Multidisciplinary study of continental/ocean climate dynamics using high-resolution records from the eastern Mediterranean).	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J	Setoyama, E; Radmacher, W; Kaminski, MA; Tyszka, J				Setoyama, Eiichi; Radmacher, Wieslawa; Kaminski, Michael A.; Tyszka, Jaroslaw			Foraminiferal and palynological biostratigraphy and biofacies from a Santonian-Campanian submarine fan system in the Voring Basin (offshore Norway)	MARINE AND PETROLEUM GEOLOGY			English	Article						Foraminifera; Dinoflagellate cysts; Palynology; Biostratigraphy; Palaeoenvironment; Upper Cretaceous; Campanian; Norwegian Sea	SEA BENTHIC FORAMINIFERA; NORWEGIAN SEA; TAXONOMIC COMPOSITION; CONTINENTAL-MARGIN; OXYGEN; ASSEMBLAGES; SEDIMENTARY; ENVIRONMENT; SANDSTONES; DEPOSITION	Foraminiferal assemblages from a Santonian-Campanian submarine fan system in the northwestern Wiring Basin, offshore Norway were investigated with the primary objectives to document the stratigraphic ranges of foraminiferal taxa calibrated with dinoflagellate cysts, and to interpret foraminiferal biofacies of different fan sub-environments previously proposed based on the analysis of ichnofossils. The assemblages are composed of deep-water agglutinated foraminifera (DWAF) without carbonate-cemented taxa. DWAF taxa of high biostratigraphic value are absent, but the complete agglutinated nature of the assemblages and the presence of Gerochammina stanislawi and Rectogerochammina eugubina are similar to those of the lower Campanian Fenestrella bellii Zone of the Norwegian Sea. More reliable dating was provided by palynology, and the age of the interval is estimated to be Santonian to Campanian. The inner to middle fan assemblages contain small numbers of specimens, and consequently the species diversity and relative abundance of morphogroups are inconsistent. Deep infaunal forms may be more common in this sub-environment, but because the abundance is low, this observation should be treated carefully. In contrast, the abundance and diversity of the assemblages of the overbank, fringe and basin plain sub-environments are fairly high. Their morphogroup composition is also similar and comparable to each other when the assemblage size is large. The assemblage from the interval with suggested hydrothermal activity is similar to those from outside the channel sub-environment. The presence of bottom water currents, possibly in the form of a western boundary current, in the basin is suggested based on the abundant occurrence of tubular forms in the overbank, fringe, and basin plain sub-environments. (C) 2013 Elsevier Ltd. All rights reserved.	[Setoyama, Eiichi; Kaminski, Michael A.] King Fahd Univ Petr & Minerals, Res Grp Reservoir Characterizat, Dept Earth Sci, Dhahran 31261, Saudi Arabia; [Setoyama, Eiichi; Radmacher, Wieslawa; Tyszka, Jaroslaw] Polish Acad Sci, Inst Geol Sci, ING PAN, Cracow Res Ctr,BioGeoLab, PL-31002 Krakow, Poland; [Kaminski, Michael A.] UCL, Dept Earth Sci, London WC1E 6BT, England	King Fahd University of Petroleum & Minerals; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; University of London; University College London	Setoyama, E (通讯作者)，Polish Acad Sci, Inst Geol Sci, ING PAN, Cracow Res Ctr,BioGeoLab, Ul Senacka 1, PL-31002 Krakow, Poland.	setoyama@kfupm.edu.sa; kaminski@kfupm.edu.sa	Setoyama, Eiichi/N-9406-2019; Kaminski, Michael/K-3334-2012; Radmacher, Wiesława/ABH-7042-2020	Kaminski, Michael A/0000-0002-7344-5874; Radmacher, Wieslawa/0000-0001-7316-3693; Setoyama, Eiichi/0000-0001-9972-7055	Total s.a.; Geological Society of America; Research Council of Norway; ING PAN internal project "MIKRO"; 7th European Framework Programme, ATLAB [285989]	Total s.a.(Total SA); Geological Society of America; Research Council of Norway(Research Council of Norway); ING PAN internal project "MIKRO"; 7th European Framework Programme, ATLAB(European Union (EU))	The authors thank Felix Gradstein for providing faunal slides and the NPD for palynological slides. We are grateful to the associate editor Finn Surlyk and two anonymous reviewers for critical reviews and constructive comments which improved the quality of the manuscript. Thanks are due to David Graham Bell, Gunn Mangerud, Martin Anthony Pearce and others for their help and essential discussions on palynology. ES was supported by grant to MAK from Total s.a. and from the W. Storrs Cole Memorial Research Award of the Geological Society of America. WR is supported by the Research Council of Norway. ES, WR and JT acknowledge the support from the ING PAN internal project "MIKRO". The ING PAN is supported by the 7th European Framework Programme, ATLAB Project no 285989.	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Pet. Geol.	MAY	2013	43						396	408		10.1016/j.marpetgeo.2012.12.007	http://dx.doi.org/10.1016/j.marpetgeo.2012.12.007			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	142XR					2025-03-11	WOS:000318831400027
J	Genovesi, B; Mouillot, D; Laugier, T; Fiandrino, A; Laabir, M; Vaquer, A; Grzebyk, D				Genovesi, Benjamin; Mouillot, David; Laugier, Thierry; Fiandrino, Annie; Laabir, Mohamed; Vaquer, Andre; Grzebyk, Daniel			Influences of sedimentation and hydrodynamics on the spatial distribution of <i>Alexandrium catenella/tamarense</i> resting cysts in a shellfish farming lagoon impacted by toxic blooms	HARMFUL ALGAE			English	Article						Alexandrium; Thau Lagoon (Mediterranean Sea); Resting cyst; Mapping; Sediment; Hydrodynamics; Spatial correlation	THAU LAGOON; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; COMPLEX DINOPHYCEAE; SEASONAL DYNAMICS; NOLTII HORNEM.; ZOSTERA-NOLTII; CATENELLA; SEAGRASS; POPULATIONS	Since resting cysts are a potential seeding source for blooms, the presence of these cysts in sediments is a marker of an established population for a number of harmful algal species. The spatial patterns of cyst density in relation to sediment characteristics and hydrodynamics are still largely misunderstood. This study investigated the spatial distribution of resting cysts belonging to the Alexandrium tamarense species complex (Dinophyceae) in sediments of a Mediterranean coastal lagoon (Thau Lagoon, France). This lagoon, hosting shellfish farming, is regularly impacted by toxic Alexandrium catenella blooms. The average cyst density across the whole lagoon was rather low, <20 cysts g(-1) of dry sediment (DS). However, densities varied widely among sampled stations, with the highest density (similar to 440 cysts g(-1) DS) recorded in a shallow cove named Crique-de-l'Angle, which is the only area where dense blooms of A. catenella and A. tamarense have been recorded in the years preceding this survey. An analysis using spatial autoregressive models demonstrated that cyst densities were highly spatially autocorrelated (indicating that close stations tended to have more similar cyst densities) with accumulation sites. With respect to sediment characteristics (5 granulometric fractions <2 mm and biochemical components), the highest densities were found in silty sediments containing high proportions of water and organic matter. Nevertheless, the linkage between cyst density and sediment structure was not always verified; this reflected the influence of hydrodynamics on the sedimentation of cysts and sediment particles, and on the dispersal of cysts away from the bloom area by wind-induced currents, suggesting that hydrodynamics was responsible for the spatially autocorrelated distribution of cyst densities. (c) 2013 Elsevier B.V. All rights reserved.	[Genovesi, Benjamin; Mouillot, David; Laabir, Mohamed; Vaquer, Andre; Grzebyk, Daniel] Univ Montpellier 2, UMR 5119, Lab Ecol Syst Marins Cotiers ECOSYM, IFREMER,CNRS,IRD,UM2,UM1, F-34095 Montpellier, France; [Laugier, Thierry] IFREMER, Unite Rech Lagons Ecosyst & Aquaculture Durable, F-98846 Noumea, Nouvelle Caledo, France; [Fiandrino, Annie] IFREMER, LER LR, F-34203 Sete, France	Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); Ifremer; Ifremer; Ifremer	Grzebyk, D (通讯作者)，Univ Montpellier 2, UMR 5119, Lab Ecol Syst Marins Cotiers ECOSYM, IFREMER,CNRS,IRD,UM2,UM1, Pl Eugene Bataillon, F-34095 Montpellier, France.	daniel.grzebyk@univ-montp2.fr	Mouillot, David/HCH-5670-2022; Grzebyk, Daniel/A-9286-2009	Grzebyk, Daniel/0000-0002-1130-7724; Laugier, Thierry/0000-0003-0409-4510	Region Languedoc-Roussillon; Programme National d'Environnement Cotier (PNEC-France)	Region Languedoc-Roussillon(Region OccitanieRegion Ile-de-France); Programme National d'Environnement Cotier (PNEC-France)	This study has been conducted with support from the Region Languedoc-Roussillon through a Ph.D. fellowship granted to B.G., and with financial support from the Programme National d'Environnement Cotier (PNEC-France). The authors thank P. Cecchi and Y. Collos for their helpful discussions and comments on an early version of the manuscript. The authors also thank IFREMER LER/LR for assistance and logistical support, in particular, J. Oheix, P. Le Gall and F. 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J	Garcés, E; Alacid, E; Reñé, A; Petrou, K; Simó, R				Garces, Esther; Alacid, Elisabet; Rene, Albert; Petrou, Katherina; Simo, Rafel			Host-released dimethylsulphide activates the dinoflagellate parasitoid <i>Parvilucifera sinerae</i>	ISME JOURNAL			English	Article						Alexandrium; dimethylsulphide; dinoflagellates; infochemistry; parasitoid; Parvilucifera	HARMFUL ALGAL BLOOMS; DIMETHYLSULFONIOPROPIONATE; ALEXANDRIUM; PLANKTON; SULFIDE; DMSP	Parasitoids are a major top-down cause of mortality of coastal harmful algae, but the mechanisms and strategies they have evolved to efficiently infect ephemeral blooms are largely unknown. Here, we show that the generalist dinoflagellate parasitoid Parvilucifera sinerae (Perkinsozoa, Alveolata) is activated from dormancy, not only by Alexandrium minutum cells but also by culture filtrates. We unequivocally identified the algal metabolite dimethylsulphide (DMS) as the density-dependent cue of the presence of potential host. This allows the parasitoid to alternate between a sporangium-hosted dormant stage and a chemically-activated, free-living virulent stage. DMS-rich exudates of resistant dinoflagellates also induced parasitoid activation, which we interpret as an example of coevolutionary arms race between parasitoid and host. These results further expand the involvement of dimethylated sulphur compounds in marine chemical ecology, where they have been described as foraging cues and chemoattractants for mammals, turtles, birds, fish, invertebrates and plankton microbes. The ISME Journal (2013) 7, 1065-1068; doi:10.1038/ismej.2012.173; published online 24 January 2013	[Garces, Esther; Alacid, Elisabet; Rene, Albert; Simo, Rafel] CSIC, Inst Ciencies Mar, E-08003 Barcelona, Catalonia, Spain; [Petrou, Katherina] Univ Technol Sydney, Plant Funct Biol & Climate Change Cluster, Sydney, NSW 2007, Australia	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); University of Technology Sydney	Garcés, E (通讯作者)，CSIC, Inst Ciencies Mar, Passeig Maritim Barceloneta 37-49, E-08003 Barcelona, Catalonia, Spain.	esther@icm.csic.es; rsimo@icm.csic.es	Rene, Albert/D-4560-2012; Alacid, Elisabet/AAB-6468-2021; Garces, Esther/C-5701-2011	Rene, Albert/0000-0002-0488-3539; Alacid, Elisabet/0000-0003-0777-1855; Simo, Rafel/0000-0003-3276-7663; Garces, Esther/0000-0002-2712-501X; Petrou, Katherina/0000-0002-2703-0694	Spanish Ministry of Science and Innovation; Australian Endeavour Foundation (Australian Government)	Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); Australian Endeavour Foundation (Australian Government)(Australian GovernmentDepartment of Industry, Innovation and Science)	Support was provided by the (former) Spanish Ministry of Science and Innovation through projects PARAL (to E. G.) and SUMMER (to R. S.). K. P. acknowledges a grant from Australian Endeavour Foundation (Australian Government). We thank Beatriz Garriz for the drawing of the infection cycle.	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L., 2008, P173; Zingone A, 2000, OCEAN COAST MANAGE, V43, P725, DOI 10.1016/S0964-5691(00)00056-9	21	39	39	1	42	NATURE PUBLISHING GROUP	LONDON	MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND	1751-7362			ISME J	ISME J.	MAY	2013	7	5					1065	1068		10.1038/ismej.2012.173	http://dx.doi.org/10.1038/ismej.2012.173			4	Ecology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Microbiology	131AS	23344241	Bronze, Green Published			2025-03-11	WOS:000317963300015
J	Candel, MS; Borromei, AM				Soledad Candel, Maria; Maria Borromei, Ana			TAXONOMIC AND PALEOECOLOGICAL CHARACTERIZATION OF HOLOCENE INGRESSION IN THE BEAGLE CHANNEL (TIERRA DEL FUEGO), BASED ON DINOCYSTASSEMBLAGES AND OTHERAQUATIC PALYNOMORPHS	REVISTA BRASILEIRA DE PALEONTOLOGIA			Portuguese	Article						aquatic palynomorphs; Holocene marine sediments; Beagle Channel	WALLED DINOFLAGELLATE CYSTS; SEA-SURFACE CONDITIONS; BAHIA-BLANCA ESTUARY; BUENOS-AIRES; LATE QUATERNARY; HYDROGRAPHIC CONDITIONS; MARINE-SEDIMENTS; NORTH-ATLANTIC; HIGH-LATITUDES; ASSEMBLAGES	On the southern coast of Tierra del Fuego, Argentina, the Holocene marine ingression took place around 8,000 C-14 years BP, and it is represented by several discontinuous marine terraces along the north coast of the Beagle Channel. During the beginning of the marine incursion, the aquatic assemblages developed in Bahia Lapataia and Rio Varela localities, were characterized by a scarce participation of marine components, especially of dinoflagellate cysts. After 6,000 C-14 years BP, in Rio Ovando and Albufera Lanushuaia localities, an increase in the number of aquatic species was observed with a major participation of Peridiniales dinocysts in the associations, suggesting the establishment of marginal marine environments with low to moderate salinities and high nutrient content in the water. The analysis of the dinofiagellate cysts and other aquatic palynomorphs assemblages recorded in the marine sediments from northern coast of the Beagle Channel, indicate that the environmental conditions during the middle-late Holocene correspond to fjord (estuarine) environments close to ice fields affected by glacier meltwater discharge with anomalously low salinities. These aquatic assemblages identified have a similar composition to those observed in modem sediments of the Beagle Channel.	[Soledad Candel, Maria; Maria Borromei, Ana] Univ Nacl Sur, INGEOSUR CONICET, 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)	Candel, MS (通讯作者)，Univ Nacl Sur, INGEOSUR CONICET, Dept Geol, San Juan,670,B8000ICN, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	scandel@uns.edu.ar; borromei@criba.edu.ar						Albero M.C., 1988, QUATERNARY S AM ANTA, V5, P59; [Anonymous], NEOGENE QUATERNARY D; [Anonymous], 1986, INT S SEA LEV CHANG; Batten D.J., 1996, Palynology: principles and applications, P205; Borel CM, 2007, AMEGHINIANA, V44, P359; Borel CM, 2006, AMEGHINIANA, V43, P399; Borel CM, 2003, AMEGHINIANA, V40, P531; Borromei A.M., 2001, Revista Espanola de Micropaleontologia, V33, P61; Borromei AM, 2007, AMEGHINIANA, V44, P161; Brocke Rainer, 1996, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V200, P53; BUJALESKY G, 2004, B GEOFISICA TEORICA, V45, P235; Candel M.S., 2013, PALYNOLOGY, V37, P62, DOI [10.1080/01916122.2012.718994., DOI 10.1080/01916122.2012.718994]; Candel M.S., 2010, THESIS U NACL SUR; Coronato A., 1999, C ARGENTINO GEOMORFO, V1, P27; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; de Vernal A., 1989, P OCEAN DRILLING PRO, V105, P387, DOI DOI 10.2973/0DP.PR0C.SR.105.133.1989; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42, P909; Gómez EA, 2005, J S AM EARTH SCI, V20, P139, DOI 10.1016/j.jsames.2005.06.01; Gordillo S, 1999, SCI MAR, V63, P15, DOI 10.3989/scimar.1999.63s115; GORDILLO S, 1993, QUATERNARY SCI REV, V12, P889, DOI 10.1016/0277-3791(93)90027-J; Gordillo S, 2005, SCI MAR, V69, P337, DOI 10.3989/scimar.2005.69s2337; GORDILLO S, 1992, PALAEOGEOGR PALAEOCL, V99, P41, DOI 10.1016/0031-0182(92)90006-Q; GORDILLO S, 1993, 12 C GEOL ARG 2 C EX, P34; Gordillo S., 1992, THESIS U NACL CORDOB; GORIN GE, 1991, PALAEOGEOGR PALAEOCL, V85, P303, DOI 10.1016/0031-0182(91)90164-M; Grill S., 2002, Revista Espanola de Micropaleontologia, V34, P145; Grill S.C., 1995, POLEN, V7, P41; Grill Silvia, 1996, Ameghiniana, V33, P435; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; GUYOHLSON D, 1992, PHYCOLOGIA, V31, P523, DOI 10.2216/i0031-8884-31-6-523.1; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Harland R, 1998, PALAEONTOLOGY, V41, P1093; HEAD MJ, 1993, J PALEONTOL, V67, P1; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; HEUSSER L E, 1984, Palynology, V8, P225; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; Limoges A, 2010, MAR MICROPALEONTOL, V76, P104, DOI 10.1016/j.marmicro.2010.06.003; Marcela Borel C., 2006, Revista del Museo Argentino de Ciencias Naturales Nueva Serie, V8, P119; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Marret F, 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; Martínez MA, 2008, AMEGHINIANA, V45, P719; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; Matsuoka K., 1987, NATURAL SCI, V28, P35, DOI org/10.1016/0377-8398(94)00016-G; Matsuoka K, 2009, REV PALAEOBOT PALYNO, V154, P79, DOI 10.1016/j.revpalbo.2008.12.013; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; McMinn A, 1995, MICROPALEONTOLOGY, V41, P383, DOI 10.2307/1485813; McMinn A, 1997, MAR MICROPALEONTOL, V29, P407, DOI 10.1016/S0377-8398(96)00012-6; Medeanic S, 2006, REV PALAEOBOT PALYNO, V141, P83, DOI 10.1016/j.revpalbo.2006.03.012; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; PALS JP, 1980, REV PALAEOBOT PALYNO, V30, P371, DOI 10.1016/0034-6667(80)90020-2; Prauss M., 1989, Neues Jahrbuch fuer Geologie und Palaeontologie Monatshefte, V1989, P671; Prauss M, 2001, PALAEOGEOGR PALAEOCL, V174, P221, DOI 10.1016/S0031-0182(01)00295-4; Prauss M., 1996, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V200, P107; Rabassa J, 2000, QUATERN INT, V68, P217, DOI 10.1016/S1040-6182(00)00046-X; Rabassa J., 1990, 11 C GEOL ARG SAN JU, V1, P290; Rabassa J., 2004, REUNION GEOMORFOLOGI, V2, P333; RABASSA J, 1992, SVERIGES GEOLOGISKA, V81, P249; Rabassa J, 2011, BIOL J LINN SOC, V103, P316, DOI 10.1111/j.1095-8312.2011.01681.x; Rabassa Jorge, 2009, Rev. 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Bras. Paleontol.	MAY-AUG	2013	16	2					245	262		10.4072/rbp.2013.2.07	http://dx.doi.org/10.4072/rbp.2013.2.07			18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	AC1OP		Bronze, Green Published			2025-03-11	WOS:000332266200007
J	Filipova-Marinova, M; Pavlov, D; Coolen, M; Giosan, L				Filipova-Marinova, Mariana; Pavlov, Danail; Coolen, Marco; Giosan, Liviu			First high-resolution marinopalynological stratigraphy of Late Quaternary sediments from the central part of the Bulgarian Black Sea area	QUATERNARY INTERNATIONAL			English	Article							MARMARA SEA; DINOFLAGELLATE CYSTS; HOLOCENE CLIMATE; LATE-PLEISTOCENE; POLLEN; HISTORY; RECORDS; WATER; VARIABILITY; OUTFLOW	Spores, pollen and dinoflagellate cysts of Late Pleistocene and Holocene sediments were analyzed from Giant Gravity Core 18 from the Black Sea continental slope, recovered from a water depth of 971 m. The investigated length of the core is 203.5 cm. It includes 3 lithological units: light grey clay, sapropels and coccolith-bearing ooze. The core was sampled at 5-10 cm intervals. Sampling of the interval 141.5 -126 cm was carried out at every cm. AMS radiocarbon dating of bulk organic carbon was performed on 18 selected sediment layers. This chronological data allowed the first high-resolution pollen stratigraphy of Late Quaternary sediments from the western Black Sea area to be presented. The percentage spore-pollen diagram is divided into 6 local pollen assemblage zones. The trends in the vegetation dynamics and climate changes and the early history of migration of the majority of the arboreal taxa that nowadays occur in the Eastern Balkan Range were traced out. The palynological record suggests that open oak forests were spread in the Eastern Balkan Range at the beginning of the Holocene and shows early migration of the major temperate arboreal species such as Quercus, Ulmus, Tilia and Carpinus betulus. This vegetation palaeosuccession continues with the spreading of mixed oak forests from 8950 until 2620 cal. BP (8650 +/- 40 until 3120 +/- 35 C-14 BP) followed by destructive changes due to human impact and climate deterioration. A cooling of Holocene climate that is well known in the North Atlantic region as the "8200 yrs cold event" is identified for the first time in marine records from the Bulgarian Black Sea area. The assemblages of dinoflagellate cysts and acritarchs were investigated to provide a reconstruction of surface seawater salinity and surface seawater temperature changes. Two main dinoflagellate cyst assemblages, one dominated by fresh- to brackish water species such as Spiniferites cruaformis and Pyxidinopsis psilata and a subsequent one, that is characterized by euryhaline marine Mediterranean species such as Lingulodinium machaerophorum, Spiniferites belerius, Spiniferites bentorii, Operculodinium centroccupum and acritarchs Cymatiosphaera globulosa testified a change in SSS from low salinity (<7 parts per thousand) to present day conditions after 7990 cal. BP. Substantial freshening of Black Sea surface waters at 2570 cal. BP is established and connected with the transition from a relatively dry and warm to relatively cold and wet climate. (C) 2012 Elsevier Ltd and INQUA. All rights reserved.	[Filipova-Marinova, Mariana] Museum Nat Hist Varna, Varna 9000, Bulgaria; [Filipova-Marinova, Mariana; Pavlov, Danail] Soc Innovat Ecologists Bulgaria, Varna 9010, Bulgaria; [Coolen, Marco; Giosan, Liviu] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution	Filipova-Marinova, M (通讯作者)，Museum Nat Hist Varna, 41 Maria Louisa Blvd, Varna 9000, Bulgaria.	marianafilipova@yahoo.com; danailpavlov@gmail.com; mcoolen@whoi.edu; lgiosan@whoi.edu	Giosan, Liviu/F-1809-2010; Pavlov, Danail/N-7815-2013; Coolen, Marco/B-8263-2015	Coolen, Marco/0000-0002-0417-920X; Pavlov, Danail/0000-0001-7382-2054; Filipova-Marinova, Mariana/0000-0002-0786-9476	US National Science Foundation [OCE 0602423]; WHOI; Andrew W. Mellon Foundation Endowed Fund for Innovative Research	US National Science Foundation(National Science Foundation (NSF)); WHOI; Andrew W. Mellon Foundation Endowed Fund for Innovative Research	We would like to thank R/V Akademik crew and IO-BAS researchers for their extensive organizational and participatory help with the cruise. 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. Constructive comments from the editor Daniel Veres, Professor Donatella Magri and the anonymous reviewer, are greatly acknowledged.	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APR 19	2013	293						170	183		10.1016/j.quaint.2012.05.002	http://dx.doi.org/10.1016/j.quaint.2012.05.002			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	129AH					2025-03-11	WOS:000317810300016
J	Houben, AJP; Bijl, PK; Pross, J; Bohaty, SM; Passchier, S; Stickley, CE; Röhl, U; Sugisaki, S; Tauxe, L; van de Flierdt, T; Olney, M; Sangiorgi, F; Sluijs, A; Escutia, C; Brinkhuis, H; Brinkhuis, H; Dotti, CE; Klaus, A; Fehr, A; Williams, T; Bendle, JA; Bijl, PK; Bohaty, SM; Carr, SA; Dunbar, RB; Flores, JA; Gonzàlez, JJ; Hayden, TG; Iwai, M; Jimenez-Espejo, FJ; Katsuki, K; Kong, GS; Mckay, RM; Nakai, M; Olney, MP; Passchier, S; Pekar, SF; Pross, J; Riesselman, C; Röhl, U; Sakai, T; Salzmann, U; Shrivastava, PK; Stickley, CE; Sugisaki, S; Tauxe, L; Tuo, S; van de Flierdt, T; Welsh, K; Yamane, M				Houben, Alexander J. P.; Bijl, Peter K.; Pross, Joerg; Bohaty, Steven M.; Passchier, Sandra; Stickley, Catherine E.; Roehl, Ursula; Sugisaki, Saiko; Tauxe, Lisa; van de Flierdt, Tina; Olney, Matthew; Sangiorgi, Francesca; Sluijs, Appy; Escutia, Carlota; Brinkhuis, Henk; Brinkhuis, Henk; Dotti, Carlota Escutia; Klaus, Adam; Fehr, Annick; Williams, Trevor; Bendle, James A. P.; Bijl, Peter K.; Bohaty, Steven M.; Carr, Stephanie A.; Dunbar, Robert B.; Flores, Jose-Abel; Gonzalez, Jhon J.; Hayden, Travis G.; Iwai, Masao; Jimenez-Espejo, Francisco J.; Katsuki, Kota; Kong, Gee Soo; McKay, Robert M.; Nakai, Mutsumi; Olney, Matthew P.; Passchier, Sandra; Pekar, Stephen F.; Pross, Jorg; Riesselman, Christina; Rohl, Ursula; Sakai, Toyosaburo; Salzmann, Ulrich; Shrivastava, Prakash K.; Stickley, Catherine E.; Sugisaki, Saiko; Tauxe, Lisa; Tuo, Shouting; van de Flierdt, Tina; Welsh, Kevin; Yamane, Masako		Expedition 318 Scientists	Reorganization of Southern Ocean Plankton Ecosystem at the Onset of Antarctic Glaciation	SCIENCE			English	Article							ICE-SHEET EXPANSION; SEA-ICE; SEDIMENTOLOGICAL EVIDENCE; DINOFLAGELLATE CYSTS; INDICATORS; ICEHOUSE	The circum-Antarctic Southern Ocean is an important region for global marine food webs and carbon cycling because of sea-ice formation and its unique plankton ecosystem. However, the mechanisms underlying the installation of this distinct ecosystem and the geological timing of its development remain unknown. Here, we show, on the basis of fossil marine dinoflagellate cyst records, that a major restructuring of the Southern Ocean plankton ecosystem occurred abruptly and concomitant with the first major Antarctic glaciation in the earliest Oligocene (similar to 33.6 million years ago). This turnover marks a regime shift in zooplankton-phytoplankton interactions and community structure, which indicates the appearance of eutrophic and seasonally productive environments on the Antarctic margin. We conclude that earliest Oligocene cooling, ice-sheet expansion, and subsequent sea-ice formation were important drivers of biotic evolution in the Southern Ocean.	[Houben, Alexander J. P.; Bijl, Peter K.; Sangiorgi, Francesca; Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, LPP, NL-3584 CD Utrecht, Netherlands; [Pross, Joerg] Goethe Univ Frankfurt, Inst Geosci, Paleoenvironm Dynam Grp, D-60438 Frankfurt, Germany; [Pross, Joerg] Biodivers & Climate Res Ctr, D-60325 Frankfurt, Germany; [Bohaty, Steven M.] Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England; [Passchier, Sandra] Montclair State Univ, Dept Earth & Environm Studies, Montclair, NJ 07043 USA; [Stickley, Catherine E.] Univ Tromso, Dept Geol, N-9037 Tromso, Norway; [Roehl, Ursula] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Sugisaki, Saiko; Tauxe, Lisa] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; [van de Flierdt, Tina] Univ London Imperial Coll Sci Technol & Med, Dept Earth Sci & Engn, London SW7 2AZ, England; [Olney, Matthew] Univ S Florida, Dept Geol, Tampa, FL 33620 USA; [Escutia, Carlota] Inst Andaluz Ciencias Terra, Armilla 18100, Granada, Spain; [Brinkhuis, Henk; Bijl, Peter K.] Univ Utrecht, Lab Palaeobot & Palynol, Fac Geosci, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Dotti, Carlota Escutia; Gonzalez, Jhon J.; Jimenez-Espejo, Francisco J.] Univ Granada, CSIC, Inst Andaluz Ciencias Tierra, Granada 18002, Spain; [Klaus, Adam] Texas A&M Univ, Integrated Ocean Drilling Program, US Implementing Org, College Stn, TX 77845 USA; [Fehr, Annick] Univ Aachen, Inst Appl Geophys & Geothermal Energy, D-52074 Aachen, Germany; [Williams, Trevor] Columbia Univ, Lamont Doherty Earth Observ, Borehole Res Grp, Palisades, NY 10964 USA; [Bendle, James A. P.] Univ Glasgow, Geog & Earth Sci, Glasgow G12 8QQ, Lanark, Scotland; [Bohaty, Steven M.] Univ Southampton, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England; [Carr, Stephanie A.] Colorado Sch Mines, Dept Chem & Geochem, Golden, CO 80401 USA; [Dunbar, Robert B.; Riesselman, Christina] Stanford Univ, Dept Environm Earth Syst Sci, Stanford, CA 94305 USA; [Flores, Jose-Abel] Univ Salamanca, Fac Ciencias, Dept Geol, Geosci Grp, Salamanca 37008, Spain; [Hayden, Travis G.] Western Michigan Univ, Dept Geol, Kalamazoo, MI 49008 USA; [Iwai, Masao] Kochi Univ, Dept Nat Sci, Kochi 7808520, Japan; [Jimenez-Espejo, Francisco J.] Japan Agcy Marine Earth Sci & Technol, Inst Res Earth Evolut, Yokosuka, Kanagawa 2370061, Japan; [Katsuki, Kota] Kochi Univ, Marine Ctr Adv Core Res, Kochi 7838502, Japan; [Kong, Gee Soo] Korea Inst Geosci & Mineral Resources, Petrol & Marine Res Div, Daejeon 305350, South Korea; [McKay, Robert M.] Victoria Univ Wellington, Antarct Res Ctr, Wellington 6140, New Zealand; [Nakai, Mutsumi] Daito Bunka Univ, Educ Dept, Tokyo 1758571, Japan; [Nakai, Mutsumi] Univ S Florida, Dept Geol, Tampa, FL 33620 USA; [Passchier, Sandra] Montclair State Univ, Earth & Environm Studies, Montclair, NJ 07043 USA; [Pekar, Stephen F.] CUNY Queens Coll, Sch Earth & Environm Sci, Flushing, NY 11367 USA; [Pross, Jorg] Goethe Univ Frankfurt, Inst Geosci, Paleoenvironm Dynam Grp, D-60438 Frankfurt, Germany; [Riesselman, Christina] US Geol Survey, Eastern Geol & Paleoclimate Sci Ctr, Reston, VA 20192 USA; [Rohl, Ursula] Univ Bremen, Ctr Marine Environm Sci, MARUM, D-28359 Bremen, Germany; [Sakai, Toyosaburo] Utsunomiya Univ, Dept Geol, Utsunomiya, Tochigi 3218505, Japan; [Salzmann, Ulrich] Northumbria Univ, Sch Built & Nat Environm, Earth & Environm, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England; [Shrivastava, Prakash K.] NIT, NH5P, Geol Survey India, Antarct Div, Faridabad 121001, Haryana, India; [Stickley, Catherine E.] Univ Tromso, Dept Geol, N-9037 Tromso, Norway; [Sugisaki, Saiko] Japan Agcy Marine Earth Sci & Technol, Yokosuka, Kanagawa 2370061, Japan; [Sugisaki, Saiko; Tauxe, Lisa] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; [Tuo, Shouting] Tongji Univ, Sch Ocean & Earth Sci, Shanghai 200092, Peoples R China; [van de Flierdt, Tina] Imperial Coll London, Dept Earth Sci & Engn, London SW7 2AZ, England; [Welsh, Kevin] Univ Queensland, Sch Earth Sci, Brisbane, Qld 4072, Australia; [Yamane, Masako] Univ Tokyo, Earth & Planetary Sci, Tokyo 1130033, Japan	Utrecht University; Goethe University Frankfurt; University of Southampton; NERC National Oceanography Centre; Montclair State University; UiT The Arctic University of Tromso; University of Bremen; University of California System; University of California San Diego; Scripps Institution of Oceanography; Imperial College London; State University System of Florida; University of South Florida; Utrecht University; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT); University of Granada; Texas A&M University System; Texas A&M University College Station; RWTH Aachen University; Columbia University; University of Glasgow; NERC National Oceanography Centre; University of Southampton; Colorado School of Mines; Stanford University; University of Salamanca; Western Michigan University; Kochi University; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); Kochi University; Korea Institute of Geoscience & Mineral Resources (KIGAM); Victoria University Wellington; State University System of Florida; University of South Florida; Montclair State University; City University of New York (CUNY) System; Queens College NY (CUNY); Goethe University Frankfurt; United States Department of the Interior; United States Geological Survey; University of Bremen; Utsunomiya University; Northumbria University; Geological Survey India; UiT The Arctic University of Tromso; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); University of California System; University of California San Diego; Scripps Institution of Oceanography; Tongji University; Imperial College London; University of Queensland; University of Tokyo	Houben, AJP (通讯作者)，Netherlands Org Appl Sci Res TNO, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands.	Alexander.Houben@TNO.nl	Passchier, Sandra/GYU-2381-2022; Williams, Trevor/L-7670-2014; Brinkhuis, Henk/IUO-8165-2023; McKay, Robert/N-2449-2015; Riesselman, Christina/H-5037-2012; Brinkhuis, Henk/B-4223-2009; Passchier, Sandra/AAQ-2243-2021; Flores, José-Abel/D-4218-2009; Escutia, Carlota/B-8614-2015; Sluijs, Appy/B-3726-2009; Salzmann, Ulrich/H-9929-2017; Rohl, Ursula/G-5986-2011; Welsh, Kevin/A-9808-2012; Passchier, Sandra/B-1993-2008; JIMENEZ-ESPEJO, Francisco J./F-4486-2016	McKay, Robert/0000-0002-5602-6985; Sangiorgi, Francesca/0000-0003-4233-6154; Brinkhuis, Henk/0000-0003-0253-6610; Yamane, Masako/0000-0002-5063-0719; Bendle, James/0000-0002-6826-8658; Escutia, Carlota/0000-0002-4932-8619; Sluijs, Appy/0000-0003-2382-0215; Salzmann, Ulrich/0000-0001-5598-5327; van de Flierdt, Tina/0000-0001-7176-9755; Rohl, Ursula/0000-0001-9469-7053; Houben, Alexander/0000-0002-9497-1048; Riesselman, Christina/0000-0002-2436-4306; Welsh, Kevin/0000-0002-4834-4190; Bijl, Peter/0000-0002-1710-4012; Dunbar, Robert/0000-0002-9728-5609; Passchier, Sandra/0000-0001-7204-7025; JIMENEZ-ESPEJO, Francisco J./0000-0002-0335-8580	NSF [ANT-1245283, OCE 1058858, OCE 1054497]; Statoil; Netherlands Organisation for Scientific Research (NWO) [86610110]; LPP Foundation; German Research Foundation [PR 651/10, RO 1113/6]; Biodiversity and Climate Research Center within the Hessian Initiative for Scientific and Economic Excellence (LOEWE); Post-Expedition Activity award; Natural Environmental Research Council (UK) [NE/H025162/1, NE/H020098/1, NE/J019801/1]; European Commission [IRG 230828]; UK IODP [NE/I006257/1]; European Research Council [259627]; Spanish Ministry for Science and Innovation [CTM2011-2079]; NERC [NE/J019801/1, NE/I006257/1, NE/I00646X/1, NE/H020098/1, NE/H014616/1, NE/I00646X/2, NE/H025162/1] Funding Source: UKRI; Directorate For Geosciences; Division Of Ocean Sciences [1058858] Funding Source: National Science Foundation; Office of Polar Programs (OPP); Directorate For Geosciences [1245283] Funding Source: National Science Foundation	NSF(National Science Foundation (NSF)); Statoil; Netherlands Organisation for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); LPP Foundation; German Research Foundation(German Research Foundation (DFG)); Biodiversity and Climate Research Center within the Hessian Initiative for Scientific and Economic Excellence (LOEWE); Post-Expedition Activity award; Natural Environmental Research Council (UK)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); European Commission(European Union (EU)European Commission Joint Research Centre); UK IODP; European Research Council(European Research Council (ERC)); Spanish Ministry for Science and Innovation(Spanish Government); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO)); Office of Polar Programs (OPP); Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This research used samples from the ODP and the IODP. The ODP was sponsored by the NSF and participating countries under management of Joint Oceanographic Institutions (JOI) Incorporated. A.J.P.H. and H.B. thank Statoil for funding. P.K.B., F.S., and H.B. thank the Netherlands Organisation for Scientific Research (NWO) (grant 86610110) and the LPP Foundation for funding. J.P. and U.R. acknowledge support through the German Research Foundation (grants PR 651/10 and RO 1113/6). J.P. thanks the Biodiversity and Climate Research Center within the Hessian Initiative for Scientific and Economic Excellence (LOEWE) for support. S.P. acknowledges financial support from a Post-Expedition Activity award administered by the U.S. Science Support Program and research support from NSF award ANT-1245283. T.v.d.F. acknowledges the Natural Environmental Research Council (UK) for a cruise participation grant (NE/H025162/1) and the European Commission for a Marie Curie Reintegration grant (IRG 230828). S.M.B. and T.v.d.F. further acknowledge UK IODP funding (grant NE/I006257/1). S.M.B. acknowledges the Natural Environmental Research Council (UK) for a cruise participation grant (NE/H020098/1) and postcruise research support (NE/J019801/1). L.T. acknowledges support from NSF grants OCE 1058858 and OCE 1054497. A.S. thanks the European Research Council for ERC Starting Grant 259627. C.E. thanks the Spanish Ministry for Science and Innovation (grant CTM2011-2079). The reported data are available in the supplementary materials.	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J	Verhoeven, K; Louwye, S				Verhoeven, Koen; Louwye, Stephen			Palaeoenvironmental reconstruction and biostratigraphy with marine palynomorphs of the Plio-Pleistocene in Tjornes, Northern Iceland	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Pliocene; Pleistocene; Dinoflagellate cysts; Tjornes; Breidavik Group; Iceland; Ecology; Oceanic currents	DINOFLAGELLATE CYST STRATIGRAPHY; UPPER MIOCENE; LATE PLIOCENE; PALEOECOLOGY; BELGIUM; SEDIMENTS; TECTATODINIUM; ASSEMBLAGES; SEQUENCE; SHELF	Deposits from the Tjornes Peninsula in northern Iceland enable the assessment of past ocean currents and the influence of the nearby island. Most palaeoecological studies with dinoflagellate cysts from the northern and central Atlantic focus on oceanic or shelf settings and deal with outer neritic and oceanic species. Dinoflagellate cyst studies of marginal marine settings are scarce and represent only short time intervals. The Tjornes section however accommodates 1200 m of sediments that are mainly shallow marine. The sediments are attributed to the Lower Pliocene Tjornes beds and the overlying Upper Pliocene to Pleistocene Breidavik Group. The dinoflagellate cysts and other marine palynomorphs from 68 samples from the Tjornes beds and 20 samples from the Breidavik Group are studied. The deposits are divided into five dinoflagellate cyst assemblage zones (DAZ) and one barren interzone (BIZ). The changes in the assemblages proved to be independent of the changes in bathymetry of the sedimentary environment. Heterotrophic dinoflagellate cysts dominate in DAZ1. An abrupt impoverishment in species diversity is observed in DAZ2 when autotrophic species dominate the assemblage. Slightly preceding the entrance of Pacific molluscs in the area in unit 14 of the Serripes Zone, heterotrophic species (unit 12/13) re-enter the area in DAZ3. The marked decrease and return of the heterotrophic species does not relate to conditions of preservation, but may result from the loss of nutrients. The upper part of DAZ1 and the base of DAZ3 reflect major changes in the palaeoceanography and span a period during which the polar front may have moved temporarily from the area. The first event situated at the top of DAZ1 occurred in litholog unit 4 halfway the Tapes Zone between circa 5 and 4.8 Ma. The second event at the top of litholog unit 12 around 4.5 Ma has been linked to the shoaling of the Central American Seaway. Heterotrophic dinoflagellates disappear almost completely from the area during the deposition of the Pleistocene Breidavik Group (DAZ4-5). A transition from a heterotrophic dominated assemblage to an autotrophic dominated assemblage is observed in the Horgi Formation (DAZ4a). An assemblage dominated by autotrophic cold water species, comparable to the present-day assemblage of the area north of Iceland, occurs from unit 10 in the Pleistocene Svarthamar Member on (DAZ5). This study underscores that the distribution of temperature sensitive dinoflagellate cysts is influenced by the availability of nutrients and changes in ocean currents. (C) 2013 Elsevier B.V. All rights reserved.	[Verhoeven, Koen; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Ghent University	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	Stephen.Louwye@UGent.be	Verhoeven, Koen/IZP-9609-2023; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				ALBERTSSON K J, 1978, Natturufraedingurinn, V48, P1; [Anonymous], THESIS; [Anonymous], TITLE ERROR; Bardarson G. 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Paleoclimatol. Paleoecol.	APR 15	2013	376						224	243		10.1016/j.palaeo.2013.03.002	http://dx.doi.org/10.1016/j.palaeo.2013.03.002			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	136RR					2025-03-11	WOS:000318381600018
J	Zonneveld, KAF; Marret, F; Versteegh, GJM; Bogus, K; Bonnet, S; Bouimetarhan, I; Crouch, E; de Vernal, A; Elshanawany, R; Edwards, L; Esper, O; Forke, S; Grosfjeld, K; Henry, M; Holzwarth, U; Kielt, JF; Kim, SY; Ladouceur, S; Ledu, D; Chen, L; Limoges, A; Londeix, L; Lu, SH; Mahmoud, MS; Marino, G; Matsouka, K; Matthiessen, J; Mildenhal, DC; Mudie, P; Neil, HL; Pospelova, V; Qi, YZ; Radi, T; Richerol, T; Rochon, A; Sangiorgi, F; Solignac, S; Turon, JL; Verleye, T; Wang, Y; Wang, ZH; Young, M				Zonneveld, Karin A. F.; Marret, Fabienne; Versteegh, Gerard J. M.; Bogus, Kara; Bonnet, Sophie; Bouimetarhan, Ilham; Crouch, Erica; de Vernal, Anne; Elshanawany, Rehab; Edwards, Lucy; Esper, Oliver; Forke, Sven; Grosfjeld, Kari; Henry, Maryse; Holzwarth, Ulrike; Kielt, Jean-Francois; Kim, So-Young; Ladouceur, Stephanie; Ledu, David; Chen, Liang; Limoges, Audrey; Londeix, Laurent; Lu, S. -H.; Mahmoud, Magdy S.; Marino, Gianluca; Matsouka, Kazumi; Matthiessen, Jens; Mildenhal, D. C.; Mudie, Peta; Neil, H. L.; Pospelova, Vera; Qi, Yuzao; Radi, Taoufik; Richerol, Thomas; Rochon, Andre; Sangiorgi, Francesca; Solignac, Sandrine; Turon, Jean-Louis; Verleye, Thomas; Wang, Yan; Wang, Zhaohui; Young, Marty			Atlas of modern dinoflagellate cyst distribution based on 2405 data points	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Ecology; Geographic distribution; Modern environment	RECENT MARINE-SEDIMENTS; SEA-SURFACE CONDITIONS; ALEXANDRIUM-MINUTUM DINOPHYCEAE; UPPER QUATERNARY SEDIMENTS; SP-NOV DINOPHYCEAE; RESTING CYSTS; GYMNODINIUM-CATENATUM; ENVIRONMENTAL-FACTORS; LATE PLEISTOCENE; BLOOM DYNAMICS	Dinoflagellate cysts are useful for reconstructing upper water conditions. For adequate reconstructions detailed information is required about the relationship between modern day environmental conditions and the geographic distribution of cysts in sediments. This Atlas summarises the modem global distribution of 71 organic-walled dinoflagellate cyst species. The synthesis is based on the integration of literature sources together with data of 2405 globally distributed surface sediment samples that have been prepared with a comparable methodology and taxonomy. The distribution patterns of individual cyst species are being compared with environmental factors that are known to influence dinoflagellate growth, gamete production, encystment, excystment and preservation of their-organic-walled cysts: surface water temperature, salinity, nitrate, phosphate, chlorophyll-a concentrations and bottom water oxygen concentrations. Graphs are provided for every species depicting the relationship between seasonal and annual variations of these parameters and the relative abundance of the species. Results have been compared with previously published records; an overview of the ecological significance as well as information about the seasonal production of each individual species is presented. The relationship between the cyst distribution and variation in the aforementioned environmental parameters was analysed by performing a canonical correspondence analysis. All tested variables showed a positive relationship on the 99% confidence level. Sea-surface temperature represents the parameter corresponding to the largest amount of variance within the dataset (40%) followed by nitrate, salinity, phosphate and bottom-water oxygen concentration, which correspond to 34%, 33%, 25% and 24% of the variance, respectively. Characterisations of selected environments as well as a discussion about how these factors could have influenced the final cyst yield in sediments are included. (C) 2012 Elsevier B.V. All rights reserved.	[Zonneveld, Karin A. F.; Bogus, Kara; Bouimetarhan, Ilham; Elshanawany, Rehab; Forke, Sven; Holzwarth, Ulrike; Chen, Liang] Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Zonneveld, Karin A. F.; Versteegh, Gerard J. M.; Bogus, Kara; Bouimetarhan, Ilham; Esper, Oliver; Holzwarth, Ulrike] Univ Bremen, MARUM, D-28359 Bremen, Germany; [Bonnet, Sophie; de Vernal, Anne; Henry, Maryse; Kielt, Jean-Francois; Ladouceur, Stephanie; Ledu, David; Limoges, Audrey; Lu, S. -H.; Radi, Taoufik] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Crouch, Erica; Mildenhal, D. C.] GNS Sci, Paleontol & Environm Change Sect, Lower Hutt, New Zealand; [Edwards, Lucy] US Geol Survey, Reston, VA 22092 USA; [Esper, Oliver; Matthiessen, Jens] AWI Bremerhaven, D-27515 Bremerhaven, Germany; [Grosfjeld, Kari] Geol Survey Norway, N-7491 Trondheim, Norway; [Kim, So-Young] Korea Polar Res Inst, Div Polar Climate Res, Inchon 406840, South Korea; [Londeix, Laurent; Turon, Jean-Louis] Univ Bordeaux 1, UMR CNRS EPOC 5805, F-33405 Talence, France; [Mahmoud, Magdy S.] Assiut Univ, Dept Geol, Fac Sci, Assiut 71516, Egypt; [Marino, Gianluca; Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, Fac Geol, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Matsouka, Kazumi] Nagasaki Univ, Inst East China Res, Nagasaki 8528521, Japan; [Neil, H. L.] Natl Inst Water & Atmospher Res Ltd NIWA, Wellington 6021, New Zealand; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, Victoria, BC V8W 2Y2, Canada; [Richerol, Thomas; Rochon, Andre] UQAR ISMER, Rimouski, PQ G5L 3A1, Canada; [Verleye, Thomas] Univ Ghent, Res Unit Palaeontol, Dept Geol & Soil Sci, B-9000 Ghent, Belgium; [Young, Marty] CSIRO Earth Sci & Resource Engn, N Ryde, NSW 2113, Australia; [Solignac, Sandrine] Univ Aarhus, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Marino, Gianluca] Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals, Bellaterra 08193, Spain; [Qi, Yuzao; Wang, Yan; Wang, Zhaohui] Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Guangdong, Peoples R China; [Elshanawany, Rehab] Univ Alexandria, Fac Sci, Moharam Bey 21511, Egypt; [Mudie, Peta] Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada	University of Bremen; University of Liverpool; University of Bremen; University of Quebec; University of Quebec Montreal; GNS Science - New Zealand; United States Department of the Interior; United States Geological Survey; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Geological Survey of Norway; Korea Institute of Ocean Science & Technology (KIOST); Korea Polar Research Institute (KOPRI); Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux; Egyptian Knowledge Bank (EKB); Assiut University; Utrecht University; Nagasaki University; National Institute of Water & Atmospheric Research (NIWA) - New Zealand; University of Victoria; University of Quebec; Universite du Quebec a Rimouski; Ghent University; Commonwealth Scientific & Industrial Research Organisation (CSIRO); Aarhus University; Autonomous University of Barcelona; Chinese Academy of Sciences; Jinan University; Egyptian Knowledge Bank (EKB); Alexandria University; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Zonneveld, KAF (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.	zonnev@uni-bremen.de; F.Marret@liverpool.ac.uk; versteegh@uni-bremen.de; ka_bo@uni-bremen.de; devernal.anne@uqam.ca; bouimetarhan@uni-bremen.de; E.Crouch@gns.cri.nz; devernal.anne@uqam.ca; rehab_shanawany@yahoo.com; leedward@usgs.gov; Oliver.Esper@awi.de; sven.forke@zmt-bremen.de; Kari.Grosfjeld@NGU.no; devernal.anne@uqam.ca; holzwarth@uni-bremen.de; devernal.anne@uqam.ca; kimsy@kordi.re.kr; devernal.anne@uqam.ca; devernal.anne@uqam.ca; lichen@uni-bremen.de; devernal.anne@uqam.ca; l.londeix@epoc.u-bordeaux1.fr; devernal.anne@uqam.ca; magdysm@yahoo.com; Gianluca.Marino@uab.cat; kazu-mtk@nagasaki-u.ac.jp; jmatthiessen@awi-bremerhaven.de; E.Crouch@gns.cri.nz; Peta.Mudie@NRCan-RNCan.gc.ca; E.Crouch@gns.cri.nz; vpospe@uvic.ca; tywd@jnu.edu.cn; radi.taoufik@uqam.ca; andre_rochon@uqar.qc.ca; andre_rochon@uqar.qc.ca; f.sangiorgi@uu.nl; devernal.anne@uqam.ca; jl.turon@epoc.u-bordeaux1.fr; Thomas.Verleye@ugent.be; tywd@jnu.edu.cn; tywd@jnu.edu.cn; Martin.Young@csiro.au	Bouimetarhan, Ilham/D-2388-2011; Marino, Gianluca/AAN-3969-2020; RICHEROL, Thomas/G-4598-2017; Mahmoud, Magdy/ABD-1262-2020; Ledu, David/X-4166-2019; Kim, So-Young/JFS-7698-2023; Wang, Zhaohui/C-9795-2016; Crouch, Erica/C-2820-2013; de Vernal, Anne/D-5602-2013; Versteegh, Gerard J.M./H-2119-2011	Pospelova, Vera/0000-0003-4049-8133; Bogus, Kara/0000-0003-4690-0576; Marret-Davies, Fabienne/0000-0003-4244-0437; de Vernal, Anne/0000-0001-5656-724X; Bouimetarhan, Ilham/0000-0003-3369-3811; Versteegh, Gerard J.M./0000-0002-9320-3776; Sangiorgi, Francesca/0000-0003-4233-6154; Marino, Gianluca/0000-0001-9795-5337; Limoges, Audrey/0000-0002-4587-3417; Matthiessen, Jens/0000-0002-6952-2494; RICHEROL, Thomas/0000-0001-5295-0022; Ledu, David/0000-0001-5313-7068; Esper, Oliver/0000-0002-4342-3471; Solignac, Sandrine/0000-0003-3373-6922	German Science Foundation (DFG) [SPP 1158]; NWO (Dutch science foundation)	German Science Foundation (DFG)(German Research Foundation (DFG)); NWO (Dutch science foundation)(Netherlands Organization for Scientific Research (NWO))	We thank the German Science Foundation (DFG) for providing the financial support for the Centre of Excellence MARUM, the international graduate college EUROPROX and the SPP 1158 project "PROPAC' in which frame a major part of the scientific activities leading to this Atlas have been carried out. We furthermore thank the DFG for the financial support of the Heisenberg stipendium "Biogeomolecules" of G. Versteegh.Simon Troelstra (Vrije Universiteit amsterdam) is thanked for providing samples of the western Mediterranean Sea that have been collected with the financial support of NWO (Dutch science foundation).	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Palaeobot. Palynology	APR 15	2013	191				SI		1	197		10.1016/j.revpalbo.2012.08.003	http://dx.doi.org/10.1016/j.revpalbo.2012.08.003			197	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	172BV		Green Published			2025-03-11	WOS:000320975800001
J	Ribeiro, S; Berge, T; Lundholm, N; Ellegaard, M				Ribeiro, Sofia; Berge, Terje; Lundholm, Nina; Ellegaard, Marianne			Hundred Years of Environmental Change and Phytoplankton Ecophysiological Variability Archived in Coastal Sediments	PLOS ONE			English	Article							DINOFLAGELLATE CYSTS; KOLJO-FJORD; GENETIC DIFFERENTIATION; MARINE-PHYTOPLANKTON; EMILIANIA-HUXLEYI; GROWTH; PH; PATTERNS; DIATOM; CALCIFICATION	Marine protist species have been used for several decades as environmental indicators under the assumption that their ecological requirements have remained more or less stable through time. However, a growing body of evidence suggests that marine protists, including several phytoplankton species, are in fact highly diverse and may quickly respond to changes in the environment. Predicting how future climate will impact phytoplankton populations is important, but this task has been challenged by a lack of time-series of ecophysiological parameters at time-scales relevant for climate studies (i.e. at least decadal). Here, we report on ecophysiological variability in a marine dinoflagellate over a 100-year period of well-documented environmental change, by using the sedimentary archive of living cysts from a Scandinavian fjord (Koljo Fjord, Sweden). During the past century, Koljo Fjord has experienced important changes in salinity linked to the North Atlantic Oscillation (NAO). We revived resting cysts of Pentapharsodinium dalei preserved in the fjord sediments and determined growth rates for 18 strains obtained from 3 sediment core layers at salinity 15 and 30, which represent extreme sea-surface conditions during periods of predominantly negative and positive NAO phases, respectively. Upper pH tolerance limits for growth were also tested. In general, P. dalei grew at a higher rate in salinity 30 than 15 for all layers, but there were significant differences among strains. When accounting for inter-strain variability, cyst age had no effect on growth performance or upper pH tolerance limits for this species, indicating a stable growth response over the 100-year period in spite of environmental fluctuations. Our findings give some support for the use of morphospecies in environmental studies, particularly at decadal to century scales. Furthermore, the high intra-specific variability found down to sediment layers dated as ca. 50 years-old indicates that cyst-beds of P. dalei are repositories of ecophysiological diversity.	[Ribeiro, Sofia; Ellegaard, Marianne] Univ Copenhagen, Fac Sci, Dept Biol, Copenhagen, Denmark; [Berge, Terje] Univ Copenhagen, Marine Biol Sect, Dept Biol, Helsingor, Denmark; [Lundholm, Nina] Univ Copenhagen, Nat Hist Museum Denmark, Copenhagen, Denmark	University of Copenhagen; University of Copenhagen; University of Copenhagen	Ribeiro, S (通讯作者)，Geol Survey Denmark & Greenland, Dept Marine Geol & Glaciol, Copenhagen, Denmark.	sri@geus.dk	Ribeiro, Sofia/AAZ-2782-2021; Lundholm, Nina/AAY-6249-2020; Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/G-9213-2018; Lundholm, Nina/A-4856-2013	Ellegaard, Marianne/0000-0002-6032-3376; Ribeiro, Sofia/0000-0003-0672-9161; Lundholm, Nina/0000-0002-2035-1997; Berge, Terje/0009-0003-3916-8927	Danish Research Council project [2111-04-0011]; Gotheburg Marine Research Centre in Sweden; Carlsberg Foundation, Denmark [2001_01_0337]	Danish Research Council project; Gotheburg Marine Research Centre in Sweden; Carlsberg Foundation, Denmark(Carlsberg Foundation)	This study was funded by the Danish Research Council project 2111-04-0011. The authors would like to thank Dr. Anna Godhe and Dr. Karolina Harnstrom, Gothenburg University and the Gotheburg Marine Research Centre in Sweden (grant to AG) for organising and sponsoring the fieldwork in Koljo Fjord. The funders had no role in the design of this study, data collection and analysis, decision to publish, or preparation of the manuscript. The first author holds a postdoctoral fellowship from the Carlsberg Foundation, Denmark (2001_01_0337).	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J	Gracia, S; Roy, S; Starr, M				Gracia, Stephanie; Roy, Suzanne; Starr, Michel			Spatial distribution and viability of <i>Alexandrium tamarense</i> resting cysts in surface sediments from the St. Lawrence Estuary, Eastern Canada	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						St. Lawrence Estuary (Eastern Canada); Alexandrium tamarense; dinoflagellate cysts; algal blooms; red tides	TOXIC DINOFLAGELLATE; GONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; ENVIRONMENTAL-FACTORS; FUNDYENSE BLOOM; WESTERN GULF; GROWTH-RATE; DINOPHYCEAE; GERMINATION; DYNAMICS	The dinoflagellate Alexandrium tamarense Group 1 (as defined by Lilly et al., 2007) is responsible for recurrent outbreaks of paralytic shellfish poisoning (PSP) in the St. Lawrence Estuary (SLE), Eastern Canada. In August 2008, a major bloom of A. tamarense developed in the SLE and caused major mortality of fish, seabirds and marine mammals notably in the vicinity of a marine park. Eleven months later, surface (0-5 cm) and deeper (5-10 cm) sediments were sampled to determine resting cysts concentrations, locate prospective cyst seedbeds and examine if these had changed following this major bloom. This information is thought to be important to understand inter-annual patterns in algal toxicity, cyst abundance being a good predictor of subsequent bloom magnitude in some regions. Surface cyst distribution was heterogeneous and it confirmed the location of the cyst seedbed previously reported on the north shore near the Manicouagan/aux-Outardes Rivers (>500 cysts cm(-3)). A zone of cyst accumulation was also observed on the south shore of the SLE (maximum of 1200 cysts cm(-3)), with higher concentrations relative to previous cyst mapping in the 1980s. A mismatch was observed between the zones with high surface cyst concentrations and those where the highest PSP toxins were detected (used as a proxy for vegetative cells in the water column). Cyst concentrations were negatively correlated with PSP levels from the same sites, suggesting that cysts were formed and deposited away from the major sites of toxicity. Deposition likely took place near the end of the bloom, once it had reached the eastern boundary of the SLE. PSP toxicity was worse near the peak of the bloom, which occurred westward of this region. This highlights the dynamic behaviour of local blooms, influenced by the estuarine and mesoscale circulation. Interestingly, the major bloom of August 2008 was not followed by particularly large cyst deposition or by any major bloom in 2009 in this region. Cyst viability was also examined, using Sytox Green, and found to be highest (nearly 100%) in the sites where cyst concentrations were maximum. Our results call for further investigation of the cyst mapping hypothesis in the St. Lawrence, where the local circulation seems to have an overriding influence on cyst deposition patterns. (C) 2013 Elsevier Ltd. All rights reserved.	[Gracia, Stephanie; Roy, Suzanne] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada; [Starr, Michel] Fisheries & Oceans Canada, Maurice Lamontagne Inst, Mont Joli, PQ G5H 3Z4, Canada	University of Quebec; Fisheries & Oceans Canada	Roy, S (通讯作者)，Univ Quebec, ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	suzanne_roy@uqar.ca			Department of Fisheries and Oceans; Institut des Sciences de la Mer (ISMER - Universite du Quebec a Rimouski, Quebec, Canada); Quebec-Ocean; S. Roy's NSERC discovery grant	Department of Fisheries and Oceans; Institut des Sciences de la Mer (ISMER - Universite du Quebec a Rimouski, Quebec, Canada); Quebec-Ocean; S. Roy's NSERC discovery grant	The authors wish to thank the captain and crew of the CCGS Frederick G. Creed; E. Alou, O. Casas-Monroy, B. Cayouette, G. Desmeules, D. Lavallee, S. Leblanc, M. Parenteau, P. Rioux, M. Simard, L St-Amand, for field and laboratory assistance; P. Archambault, A. Caron, F. Lesmerises, R. Lesmerises for help with the statistical analyses. This work was part of an M.Sc. thesis (SG) and it was supported by funds from the Department of Fisheries and Oceans and from the Institut des Sciences de la Mer (ISMER - Universite du Quebec a Rimouski, Quebec, Canada) and Quebec-Ocean, as well as S. Roy's NSERC discovery grant.	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Coast. Shelf Sci.	APR 10	2013	121						20	32		10.1016/j.ecss.2013.01.019	http://dx.doi.org/10.1016/j.ecss.2013.01.019			13	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	128ZB					2025-03-11	WOS:000317807100003
J	Bringué, M; Pospelova, V; Pak, D				Bringue, Manuel; Pospelova, Vera; Pak, Dorothy			Seasonal production of organic-walled dinoflagellate.cysts in an upwelling system: A sediment trap study from the Santa Barbara Basin, California	MARINE MICROPALEONTOLOGY			English	Article						Northeastern Pacific; Primary productivity; Sea surface temperatures; Lingulodinium machaerophorum; Harmful Algal Blooms	HARMFUL ALGAL BLOOMS; GULF-OF-CALIFORNIA; CYST PRODUCTION; EL-NINO; SOUTHERN-CALIFORNIA; SURFACE SEDIMENTS; VANCOUVER-ISLAND; LINGULODINIUM-POLYEDRUM; CHARACTERISTIC PATTERNS; HYDROGRAPHIC CONDITIONS	Seasonal variations in dinoflagellate cyst fluxes and assemblage composition were investigated for the first time on the west coast of the United States of America. We analyzed the palynological content of an -two year-long (May 1995 to March 1997) fortnightly sediment trap time series from the Santa Barbara Basin (SBB, off Southern California), a region characterized by seasonal upwelling and high levels of primary productivity. A total of 47 dinoflagellate cyst taxa were identified in the trap samples, with assemblages dominated by cysts produced by heterotrophic taxa. Multivariate analyses support that dinoflagellate cyst fluxes and assemblages are reliable indicators of primary productivity, and reflect sea surface temperature (SST) variations associated with upwelling in the SBB. In particular, Brigantedinium spp. are associated with active upwelling intervals (fluxes up to 127,430 cysts m(-2) day(-1) and up to 86.6% of the assemblage), when SST is lower, stratification is weaker and diatom production is maximal. Conversely, Lingulodinium machaerophorum indicates relaxed upwelling conditions (up to 9640 cysts m(-2) day(-1) and 29.9% of the assemblage) characterized by higher SST, stronger stratification and reduced primary productivity. Selenopemphix undulata is associated with colder SST in the region, whereas cyst type A abundances increase with higher SST. Thecae of potentially toxic dinoflagellates are also documented, such as Lingulodinium polyedrum and Prorocentrum micans, which are mainly recorded under conditions of higher SST and strong stratification, and Dinophysis spp. with higher fluxes between June and September of both 1995 and 1996. (C) 2013 Elsevier B.V. All rights reserved.	[Bringue, Manuel; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada; [Pak, Dorothy] Univ Calif Santa Barbara, Inst Marine Sci, Santa Barbara, CA 93106 USA	University of Victoria; University of California System; University of California Santa Barbara	Bringué, M (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada.	mbringue@uvic.ca	Bringue, Manuel/KIH-8224-2024	Bringue, Manuel/0000-0003-4460-8344; Pospelova, Vera/0000-0003-4049-8133	Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) B2 fellowship; Natural Sciences and Engineering Research Council of Canada (NSERC) [224236]; National Science Foundation [OCE-952984]; NOAA [NA77RJ0453]	Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) B2 fellowship; Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); National Science Foundation(National Science Foundation (NSF)); NOAA(National Oceanic Atmospheric Admin (NOAA) - USA)	M. Bringue was supported by the Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) B2 fellowship. The research was funded by a Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery grant (224236) to Dr.V. Pospelova. The Santa Barbara Mooring Project was funded by the National Science Foundation grant OCE-952984 and the NOAA grant NA77RJ0453 to Drs. A. Alldredge and M. Brzezinski. We thank C. Gottschalk, S. Anderson and C. Wyatt-Evans for the technical support with the mooring. We are deeply grateful to Drs. A. Alldredge and U. Passow (University of California, Santa Barbara), and R. Shipe (University of California, Los Angeles) for sharing the environmental and geochemical data collected during the UCSB Santa Barbara Mooring Project. We also thank Dr. David Field (Monterey Bay Aquarium Research Institute) for providing a dated sediment sample from the SBB. Finally, the authors thank Dr. R. Jordan and two anonymous reviewers for their constructive and thoughtful comments.	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Micropaleontol.	APR	2013	100						34	51		10.1016/j.marmicro.2013.03.007	http://dx.doi.org/10.1016/j.marmicro.2013.03.007			18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	179QO					2025-03-11	WOS:000321536600005
J	Schukat, A; Teuber, L; Hagen, W; Wasmund, N; Auel, H				Schukat, Anna; Teuber, Lena; Hagen, Wilhelm; Wasmund, Norbert; Auel, Holger			Energetics and carbon budgets of dominant calanoid copepods in the northern Benguela upwelling system	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						Community consumption; Grazing pressure; Ingestion; Respiration	OXYGEN MINIMUM LAYER; COMMUNITY STRUCTURE; RESPIRATORY CARBON; PELAGIC COPEPODS; LIFE STRATEGIES; METABOLIC-RATES; GRAZING IMPACT; MESOZOOPLANKTON; PHYTOPLANKTON; ZOOPLANKTON	Respiration rates of 16 calanoid copepod species from the northern Benguela upwelling system were measured on board RRS Discovery in September/October 2010 to determine their energy requirements and assess their significance in the carbon cycle. Individual respiration rates were standardised to a mean copepod body mass and a temperature regime typical of the northern Benguela Current. These adjusted respiration rates revealed two different activity levels (active and resting) in copepodids C5 of Calanoides carinatus and females of Rhincalanus nasutus, which reduced their metabolism during dormancy by 82% and 62%, respectively. An allometric function (I-max) and an energy budget approach were performed to calculate ingestion rates. I-max generally overestimated the ingestion rates derived from the energy budget approach by >75%. We suggest that the energy budget approach is the more reliable approximation with a total calanoid copepod (mainly females) consumption of 78 mg C M-2 d(-1) in neritic regions and 21 mg C m(-2) d(-1) in oceanic regions. The two primarily herbivorous copepods C. carinatus (neritic) and Nannocalanus minor (oceanic) contributed 83% and 5%, respectively, to total consumption by calanoid copepods. Locally, C. carinatus can remove up to 90% of the diatom biomass daily. In contrast, the maximum daily removal of dinoflagellate biomass by N. minor was 9%. These estimates imply that C. carinatus is an important primary consumers in the neritic province of the northern Benguela system, while N. minor has little grazing impact on phytoplankton populations further offshore. Data on energy requirements and total consumption rates of dominant calanoid copepods of this study are essential for the development of realistic carbon budgets and food-web models for the northern Benguela upwelling system. (c) 2013 Elsevier B.V. All rights reserved.	[Schukat, Anna; Teuber, Lena; Hagen, Wilhelm; Auel, Holger] Univ Bremen, BreMarE Bremen Marine Ecol, D-28334 Bremen, Germany; [Wasmund, Norbert] Leibniz Inst Baltic Sea Res, D-18119 Warnemunde, Germany	University of Bremen; Leibniz Institut fur Ostseeforschung Warnemunde	Schukat, A (通讯作者)，Univ Bremen, BreMarE Bremen Marine Ecol, POB 330440, D-28334 Bremen, Germany.	schukat@uni-bremen.de		Hagen, Wilhelm/0000-0002-7462-9931; Schukat, Anna/0000-0003-2703-1029; Ronn, Lena/0009-0009-9789-5763	German Federal Ministry of Education and Research (BMBF)	German Federal Ministry of Education and Research (BMBF)(Federal Ministry of Education & Research (BMBF))	We thank the captains and crews of RRS Discovery and FRS Africana for their skilful support during the cruises. Special thanks to Anja Hansen for assistance in the collection and identification of phytoplankton. We are grateful to Francois Seguin and Dr. Rainer Kiko for their support during respiration experiments. 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Mar. Biol. Ecol.	APR	2013	442						1	9		10.1016/j.jembe.2013.01.024	http://dx.doi.org/10.1016/j.jembe.2013.01.024			9	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	164QW					2025-03-11	WOS:000320425600001
J	Casas-Monroy, O; Roy, S; Rochon, A				Casas-Monroy, Oscar; Roy, Suzanne; Rochon, Andre			Dinoflagellate cysts in ballast sediments: differences between Canada's east coast, west coast and the Great Lakes	AQUATIC CONSERVATION-MARINE AND FRESHWATER ECOSYSTEMS			English	Article						ballast sediment introductions; dinoflagellate cysts; non-indigenous species; Canadian coastal regions; ballast water exchange	EEMIAN HYDROGRAPHIC CONDITIONS; BIOLOGICAL INVASIONS; TANK SEDIMENTS; RESTING CYSTS; BALTIC SEA; NORTH-SEA; WATER; SHIPS; TRANSPORT; COCHLODINIUM	The abundances and diversity of dinoflagellate cysts (including non-indigenous or harmful species) in ballast sediments were examined for the east and west coasts and the Great Lakes, to assess the potential invasion risk for these organisms and to determine similarity across regions. In total, 147 ships were sampled, distributed among three categories: (1) transoceanic, with mandatory ballast water exchange (BWE); (2) coastal with BWE; and (3) coastal without BWE. Factors that could account for variability in results were examined including ship routes, BWE, ballast water age and sediment volume in ballast tanks. The pattern of potential invasion risk differs according to the region examined. The east coast had greater concentrations of viable cysts per tank, particularly for coastal ships (with a maximum close to 2x106 cysts per tank in coastal exchanged ships compared with 1x105 for the west coast). When considering viable cysts g-1 dry sediment, maximum concentrations were found in unexchanged coastal ships from the east coast (28 cysts g-1 compared with 5 for the west coast), but these ships contained less sediment, decreasing the overall abundance of cysts per tank. These results are in the lower range of values reported for Scotland or Australia, which reached a maximum of 2.3x104 cysts cm3 of sediment. Ballast water exchange had a different influence according to the region: on the east coast, the invasion risk was reduced by BWE while it had no significant effect in the other two regions. Ballast water age and sediment volume were also different among regions, but they were not clearly related with cyst concentrations in ballast tanks. Future management of ballast sediment should take into consideration these regional differences in order to reduce the introduction of dinoflagellate NIS that threaten the conservation of coastal habitats through reduction of native diversity.Copyright (c) 2012 John Wiley & Sons, Ltd.	[Casas-Monroy, Oscar; Roy, Suzanne; Rochon, Andre] Univ Quebec, Inst Sci Mer Rimouski, Rimouski, PQ G5L 3A1, Canada	University of Quebec	Casas-Monroy, O (通讯作者)，Univ Quebec, Inst Sci Mer Rimouski, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	oscargabriel.casas-monroy@uqar.qc.ca			Canadian Aquatic Invasive Species Network (CAISN); Natural Sciences and Engineering Research Council of Canada (NSERC); Fisheries and Oceans Canada (DFO); Institut des Sciences de la Mer de Rimouski (ISMER, Universite du Quebec a Rimouski); Quebec-Ocean	Canadian Aquatic Invasive Species Network (CAISN); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fisheries and Oceans Canada (DFO); Institut des Sciences de la Mer de Rimouski (ISMER, Universite du Quebec a Rimouski); Quebec-Ocean	This research was made possible by the financial support from the Canadian Aquatic Invasive Species Network (CAISN), the Natural Sciences and Engineering Research Council of Canada (NSERC), Fisheries and Oceans Canada (DFO) and the Institut des Sciences de la Mer de Rimouski (ISMER, Universite du Quebec a Rimouski) and Quebec-Ocean. We thank all CAISN sampling teams on the west and east coasts and the Great Lakes. Special thanks to Transport Canada, shipping agents in ports and shipping companies sampled. Finally, we also thank Jean-Guy Nistad for help with the production of maps.	ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson M.J., 2008, PRIMER E PLYMOUTH; [Anonymous], 2004, INT CONVENTION CONTR; [Anonymous], 1983, Chin. J. Oceanol. 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Conserv.-Mar. Freshw. Ecosyst.	APR	2013	23	2					254	276		10.1002/aqc.2310	http://dx.doi.org/10.1002/aqc.2310			23	Environmental Sciences; Marine & Freshwater Biology; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Water Resources	127EE					2025-03-11	WOS:000317678300010
J	Rao, MR; Sahni, A; Rana, RS; Verma, P				Rao, M. R.; Sahni, Ashok; Rana, R. S.; Verma, Poonam			Palynostratigraphy and depositional environment of Vastan Lignite Mine (Early Eocene), Gujarat, western India	JOURNAL OF EARTH SYSTEM SCIENCE			English	Article						Palynostratigraphy; palaeoecology and depositional environment; Early Eocene; Vastan Lignite Mine; Gujarat	DINOFLAGELLATE CYSTS; SURAT DISTRICT; SEDIMENTS; MAMMALIA; PALYNOLOGY; TERTIARY; DIVERSE; BASIN; AMBER; AGE	Early Eocene sedimentary successions of south Asia, are marked by the development of extensive fossil-bearing, lignite-rich sediments prior to the collision of India with Asia and provide data on contemporary equatorial faunal and vegetational assemblages. One such productive locality in western India is the Vastan Lignite Mine representing approximately a 54-52 Ma sequence dated by the presence of benthic zone marker species, Nummulites burdigalensis burdigalensis. The present study on Vastan Lignite Mine succession is based on the spore-pollen and dinoflagellate cyst assemblages and documents contemporary vegetational changes. 86 genera and 105 species belonging to algal remains (including dinoflagellate cysts), fungal remains, pteridophytic spores and angiospermous pollen grains have been recorded. On the basis of first appearance, acme and decline of palynotaxa, three cenozones have been recognized and broadly reflect changing palaeodepositional environments. These are in ascending stratigraphic order (i) Proxapertites Spp. Cenozone, (ii) Operculodinium centrocarpum Cenozone and (iii) Spinizonocolpites Spp. Cenozone. The basal sequence is lagoonal, palm-dominated and overlain by more open marine conditions with dinoflagellate cysts and at the top, mangrove elements are dominant. The succession has also provided a unique record of fish, lizards, snakes, and mammals.	[Rao, M. 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S.] HNB Garhwal Univ, Dept Geol, Srinagar 246175, Uttarakhand, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Lucknow University; Hemwati Nandan Bahuguna Garhwal University	Rao, MR (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	rao.mr2008@gmail.com						Alimohammadian H, 2005, CURR SCI INDIA, V89, P1328; [Anonymous], 1967, A Palynologic Study on the Upper Los Cuervos and Mirador Formations (Lower and Middle Eocene); [Anonymous], 1962, Bulletin of the Geological Mining and Metallurgical Society of India, V25, P1; [Anonymous], PALAEOBOTANIST; Bajpai S, 2004, CURR SCI INDIA, V87, P433; Bajpai Sunil, 2006, Journal of the Palaeontological Society of India, V51, P101; Bajpai Sunil, 2007, Journal of the Palaeontological Society of India, V52, P231; Bajpai Sunil, 2005, Journal of the Palaeontological Society of India, V50, P43; Bajpai Sunil, 2005, Journal of the Palaeontological Society of India, V50, P147; Bhandari A., 1991, P C INT EXPL RES ACH, P169; Bhandari Anil, 2005, Journal of the Palaeontological Society of India, V50, P141; BUJAK J P, 1980, Special Papers in Palaeontology, P1; Chandra P., 1969, Bull. 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J	Tillmann, U; Hoppenrath, M				Tillmann, Urban; Hoppenrath, Mona			Life Cycle of the Pseudocolonial Dinoflagellate Polykrikos kofoidii (Gymnodiniales, Dinoflagellata)	JOURNAL OF PHYCOLOGY			English	Article						cysts hatching; dinoflagellate; gamete; life cycle; nuclear cyclosis; Polykrikos kofoidii	SEXUAL REPRODUCTION; CATENATUM DINOPHYCEAE; CULTURE; MEIOSIS; MORPHOLOGY; NOCTILUCA; NOV; ENCYSTMENT; PHYLOGENY; EHRENBERG	The athecate, pseudocolonial polykrikoid dinoflag-ellates show a greater morphological complexity than many other dinoflagellate cells and contain not only elaborate extrusomes but sulci, cinguli, flagellar pairs, and nuclei in multiple copies. Among polykrikoids, Polykrikos kofoidii is a common species that plays an important role as a grazer of toxic planktonic algae but whose life cycle is poorly known. In this study, the main life cycle stages of P. kofoidii were examined and documented for the first time. The formation of gametes, 2-zooid-1-nucleus stages very different from vegetative cells, was observed and the process of gamete fusion, isogamy, was recorded. Karyogamy followed shortly after completed plasmogamy. A complex reorganization of furrows (cinguli and sulci) and flagella followed zygote formation, resulting in a 4-zooid zygote with one nucleus. The fate of zygotes under different nutritional conditions was also investigated; well-fed zygotes were able to reenter the vegetative cycle via meiotic divisions as indicated by nuclear cyclosis. However, nuclear cyclosis was preceded by a presumably mitotic division of the primary zygote nucleus which by definition would imply that P. kofoidii has a diplohaplontic life cycle. Nuclear cyclosis in germlings hatched from spiny resting cysts indicate that these cysts are of zygote origin (hypnozygotes). Hypnozygote formation, cyst hatching, the morphology of the germling (a 1-zooid cell), and its development into a normal pseudocolony are documented here for the first time. There is evidence that P. kofoidii has a system of complex heterothallism.	[Tillmann, Urban] Alfred Wegener Inst, D-27570 Bremerhaven, Germany; [Hoppenrath, Mona] Deutsch Zentrum Marine Biodiversitatsforsch, D-26382 Wilhelmshaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Tillmann, U (通讯作者)，Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany.	urban.tillmann@awi.de						ALLEN JR, 1975, CELL, V6, P161, DOI 10.1016/0092-8674(75)90006-9; [Anonymous], 1998, HARMFUL ALGAE XUNTA; Archetti M, 2004, J EVOLUTION BIOL, V17, P1098, DOI 10.1111/j.1420-9101.2004.00726.x; Beam C. A., 1980, BIOCH PHYSL PROTOZOA, V3, P171; BHAUD Y, 1988, J CELL SCI, V89, P197; Biecheler B., 1952, Bull. Biol. Fr. 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Phycol.	APR	2013	49	2					298	317		10.1111/jpy.12037	http://dx.doi.org/10.1111/jpy.12037			20	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	122DQ	27008517				2025-03-11	WOS:000317297200010
J	Caulle, C; Penaud, A; Eynaud, F; Zaragosi, S; Roche, DM; Michel, E; Boulay, S; Richter, T				Caulle, Clemence; Penaud, Aurelie; Eynaud, Frederique; Zaragosi, Sebastien; Roche, Didier M.; Michel, Elizabeth; Boulay, Sebastien; Richter, Thomas			Sea-surface hydrographical conditions off South Faeroes and within the North-Eastern North Atlantic through MIS 2: the response of dinocysts	JOURNAL OF QUATERNARY SCIENCE			English	Article						dinoflagellate cysts; European ice sheets; Faeroe Margin; Last Glacial Maximum; sea-surface parameters	GLACIAL MAXIMUM LGM; B ICE SHELF; NORWEGIAN SEA; NORDIC SEAS; ANTARCTIC PENINSULA; SHETLAND CHANNEL; SEDIMENT DRIFTS; LATE QUATERNARY; RAPID CHANGES; CLIMATE	The last glacial period, showing the progressive development of large boreal ice sheets, was punctuated by large climatic excursions. These excursions were triggered mainly by atmosphereoceanice coupled dynamics and are thus exemplary case studies of natural climate variability. To characterize the sea-surface palaeohydrographical changes accompanying these oscillations along the European margin, we have integrated new palynological data (dinocysts) acquired on core MD99-2281 (60 degrees N, Faeroe Margin) during Marine Isotope Stage 2 in a latitudinal transect including published cores MD95-2002 (47 degrees N, Celtic Margin) and MD95-2010 (66 degrees N, Voring Plateau). This transect is superimposed on the modern North Atlantic Drift pathway, but also at the outskirts of glacial European ice sheets, thus ideally located to track sea-ice extent and ice-sheet instabilities through time. The results show a coherent and sensitive response of sea-surface environments to the complex chain of abrupt events that punctuated the end of the last glacial period. The Last Glacial Maximum was marked by large seasonal contrasts of temperatures, whereas Heinrich events (HE) were characterized by a sharp cooling and sea-ice development. A tripartite structure is identified within HE1, with indices of melting at 19k cal a BP, followed by a temperate phase synchronous of a relative stability of ice sheets, and a terminal phase (17.515k cal a BP) characteristic of the conventional Laurentian' HE1. Copyright (c) 2013 John Wiley & Sons, Ltd.	[Caulle, Clemence; Penaud, Aurelie] IUEM UBO, UMR Domaines Ocean 6538, Plouzane, France; [Caulle, Clemence; Eynaud, Frederique; Zaragosi, Sebastien] Univ Bordeaux 1, UMR EPOC Environm & Paleoenvironm Ocean 5805, F-33405 Talence, France; [Roche, Didier M.; Michel, Elizabeth; Boulay, Sebastien] CEA CNRS INSU UVSQ, LSCE, UMR 8212, Gif S Syvette, France; [Roche, Didier M.] Vrije Univ Amsterdam, Amsterdam, Netherlands; [Richter, Thomas] NIOZ Royal Netherlands Inst Sea Res AB, Den Burg, Texel, Netherlands	Universite de Bretagne Occidentale; 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; Vrije Universiteit Amsterdam; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Eynaud, F (通讯作者)，Univ Bordeaux 1, UMR EPOC Environm & Paleoenvironm Ocean 5805, F-33405 Talence, France.	f.eynaud@epoc.u-bordeaux1.fr	ZARAGOSI, Sébastien/JXL-2488-2024; Roche, Didier M./C-9875-2010; Penaud, Aurelie/F-2485-2011	Roche, Didier M./0000-0001-6272-9428; Penaud, Aurelie/0000-0003-3578-4549; Eynaud, Frederique/0000-0003-1283-7425; Zaragosi, Sebastien/0000-0002-1456-8129	ARTEMIS 14C AMS French project	ARTEMIS 14C AMS French project	We are grateful to IPEV, the captain and crew of the Marion Dufresne and the scientific team of the GINNA cruise. We thank Mr Y. Balut for his assistance at sea. J. St Paul, O. Ther, M-H. Castera, I. Billy and M. Georget provided invaluable technical assistance, and we thank D. Urrego for reviewing the language. We acknowledge financial support by the ARTEMIS <SUP>14</SUP>C AMS French project. Part of the analyses conducted on MD99-2281 was supported by the French INSU (Institut National des Sciences de l'Univers) programme 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'. We also thank the European Union's Seventh Framework programme "Past4Future. Climate change-Learning from the past climate." The authors declare no conflict of interest. This is U.M.R./EPOC 5805 (Universite Bordeaux I-C.N.R.S.) contribution.	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1998, WORLD OCEAN ATLAS	98	9	9	0	20	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0267-8179	1099-1417		J QUATERNARY SCI	J. Quat. Sci.	APR	2013	28	3					217	228		10.1002/jqs.2601	http://dx.doi.org/10.1002/jqs.2601			12	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	133DR					2025-03-11	WOS:000318118100001
J	Satta, CT; Anglès, S; Lugliè, A; Guillén, J; Sechi, N; Camp, J; Garcés, E				Satta, Cecilia T.; Angles, Silvia; Luglie, Antonella; Guillen, Jorge; Sechi, Nicola; Camp, Jordi; Garces, Esther			Studies on dinoflagellate cyst assemblages in two estuarine Mediterranean bays: A useful tool for the discovery and mapping of harmful algal species	HARMFUL ALGAE			English	Article						Alexandrium species; Biodiversity; Dinoflagellates; Estuaries; HABs; Mediterranean Sea; Resting cysts	SP-NOV DINOPHYCEAE; RECENT MARINE-SEDIMENTS; RESTING CYSTS; ALEXANDRIUM DINOPHYCEAE; GONYAULAX-EXCAVATA; SURFACE SEDIMENTS; BAHIA CONCEPCION; LIFE-CYCLE; GULF; COAST	The composition and assemblages of living dinoflagellate cysts from two estuarine bays (Alfacs and Fangar bays) in the northwestern Mediterranean Sea were investigated, focusing on the presence and distribution of harmful species. Sediment cores were taken from 10 stations in Alfacs Bay and from 6 stations in Fangar Bay. Sediment samples from the surface (the top 1 cm) and the subsurface profile (from 2 to 5 cm depth) in selected stations, were analyzed. Sixty-two morphotypes were recovered, some of which are new reports for the northwestern Mediterranean area. Few morphotypes dominated in terms of abundance and relative percentage (e.g. the Scrippsiella trochoidea complex was the dominant and most widely distributed morphotype in each bay, reaching maxima of 163 cysts cm(-3) wet sediment (ws) and 102 cysts cm(-3) ws in Alfacs and Fangar bays, respectively). The assemblage in Alfacs Bay was also characterized by the presence of Biecheleria cincta (maximum 116 cysts cm(-3) ws), whereas the occurrence of Pentapharsodinium tyrrhenicum (maximum 37 cysts cm(-3) ws) was greater in Fangar Bay. Twelve morphotypes belonging to potentially toxic or noxious species were detected, with the genus Alexandrium dominating. Among the harmful species, Gymnodinium litoralis and Vulcanodinium rugosum are reported for the first time from the study areas. Furthermore, cysts of the high biomass bloom-forming species Kryptoperidinium foliaceum are reported for the first time in the Mediterranean Sea. All the harmful species, with the exception of Alexandrium minutum, showed greatest abundances in subsurface samples. Profile analysis led to the description of a new cyst morphotype belonging to the Alexandrium genus (presumably A. insuetum). Our results provide information on the presence of harmful species in the studied bays, confirming the usefulness of cyst analysis in assessment of the potential risk of harmful blooms in aquaculture areas. (C) 2013 Elsevier B.V. All rights reserved.	[Satta, Cecilia T.; Luglie, Antonella; Sechi, Nicola] Univ Sassari, Dipartimento Sci Nat & Terr, I-07100 Sassari, Italy; [Angles, Silvia; Guillen, Jorge; Camp, Jordi; Garces, Esther] CSIC, Inst Ciencies Mar, E-08003 Barcelona, Spain; [Angles, Silvia] Texas A&M Univ, Dept Oceanog, College Stn, TX 77843 USA	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); Texas A&M University System; Texas A&M University College Station	Satta, CT (通讯作者)，Univ Sassari, Dipartimento Sci Nat & Terr, Via Piandanna 4, I-07100 Sassari, Italy.	ctsatta@uniss.it	Satta, Cecilia Teodora/AAF-6417-2020; Guillen, Jorge/E-6564-2010; Luglie, Antonella/M-4321-2015; Angles, Silvia/B-9469-2011; Garces, Esther/C-5701-2011	Guillen, Jorge/0000-0001-7162-8135; Luglie, Antonella/0000-0001-6382-4208; Angles, Silvia/0000-0003-0529-7504; SATTA, Cecilia Teodora/0000-0003-0130-9432; Garces, Esther/0000-0002-2712-501X; Camp, Jordi/0000-0002-5202-9783	Agencia Catalana de l'Aigua (Department de Medi Ambient, Generalitat de Catalunya); CSIC through the contract 'Pia de vigilancia de fitoplancton nociu i toxic a la Costa Catalana'; Autonomous Region of Sardinia; Spanish Ministry of Economy and Competitiveness	Agencia Catalana de l'Aigua (Department de Medi Ambient, Generalitat de Catalunya); CSIC through the contract 'Pia de vigilancia de fitoplancton nociu i toxic a la Costa Catalana'; Autonomous Region of Sardinia(Regione Sardegna); Spanish Ministry of Economy and Competitiveness(Spanish Government)	Financial support was provided by the Agencia Catalana de l'Aigua (Department de Medi Ambient, Generalitat de Catalunya) and the CSIC through the contract 'Pia de vigilancia de fitoplancton nociu i toxic a la Costa Catalana'. The work of Cecilia T. Satta was supported by the Autonomous Region of Sardinia financed Research Project "Master and Back". The work of S. Angles was partially supported by a Postdoctoral Grant from the Spanish Ministry of Economy and Competitiveness.[SS]	Alves-De-Souza C, 2008, BOT MAR, V51, P399, DOI 10.1515/BOT.2008.052; Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anglès S, 2012, HARMFUL ALGAE, V16, P1, DOI 10.1016/j.hal.2011.12.006; Anglès S, 2010, DEEP-SEA RES PT II, V57, P210, DOI 10.1016/j.dsr2.2009.09.002; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P572, DOI 10.2216/07-02.1; Balzano S, 2012, BIOGEOSCIENCES, V9, P4553, DOI 10.5194/bg-9-4553-2012; BLANCO J, 1989, Scientia Marina, V53, P785; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; 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; CAMP J, 1987, Investigacion Pesquera (Barcelona), V51, P351; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; Dale B., 1983, P69; Elshanawany R, 2010, PALYNOLOGY, V34, P233, DOI 10.1080/01916121003711665; Fessard V., 2012, CONV ET PROGR 206 SO; Figueroa RI, 2008, HARMFUL ALGAE, V7, P653, DOI 10.1016/j.hal.2008.02.005; Figueroa RI, 2009, PROTIST, V160, P285, DOI 10.1016/j.protis.2008.12.003; FUKUYO Y, 1985, B MAR SCI, V37, P529; Garces E., 2012, LIFE MEDITERRANEAN S, P519; Giannakourou A, 2005, CONT SHELF RES, V25, P2585, DOI 10.1016/j.csr.2005.08.003; [Glibert P. 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J	Prikryl, T; Skupien, P				Prikryl, Tomas; Skupien, Petr			Some new Eocene elasmobranch reports from the Outer Western Carpathians (Moravia, Czech Republic)	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article						Elasmobranchii; Leidybatis jugosus; Centrophorus; Eocene; Western Carpathian	DINOFLAGELLATE CYSTS; OLIGOCENE; BIOSTRATIGRAPHY; DENTICLES; CARTILAGE; SKELETON; MIOCENE; RAJIDAE; FOSSIL; UNIT	The Eocene deposits from the Stare Mesto locality (Frydlant Formation, Subsilesian Unit) provided fossil fish remains, which can be assigned to two elasmobranch taxa: the eagle ray Leidybatis jugosus and the shark Centrophorus sp. The specimens are represented by associated dental plates and isolated teeth. This is the first record of L. jugosus in the Czech portion of the Western Carpathians and is thus the second record for the entire Carpathian area. Presence of the taxon confirms the Eocene age of the deposits. The common occurrence with genus Centrophorus suggests sedimentation in deeper conditions (> 200 m). Other material (obtained by microvertebrate preparation technique), isolated dermal denticles and calcified cartilage prisms, are described using open nomenclature (Myliobatoidei indet. and ? Myliobatiformes indet., respectively).	[Prikryl, Tomas] Acad Sci Czech Republ, Inst Geol, Vvi, CZ-16500 Prague 6, 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; Technical University of Ostrava	Prikryl, T (通讯作者)，Acad Sci Czech Republ, Inst Geol, Vvi, Rozvojova 269, CZ-16500 Prague 6, Czech Republic.	prikryl@gli.cas.cz; petr.skupien@vsb.cz	Prikryl, Tomas/F-7962-2010; Skupien, Petr/G-8767-2019	Skupien, Petr/0000-0001-9158-466X; Prikryl, Tomas/0000-0002-7939-3622	Institute of Geology AS CR, v.v.i. [AVOZ30130516, RVO67985831];  [MSM 61989100 19]	Institute of Geology AS CR, v.v.i.(Czech Academy of Sciences); 	We are very grateful to both reviewers, Dr. HENRI CAPPETTA (Universite Montpellier, France) and Dr. ALBERTO LUIS cione (Museo de La Plata, Argentina), for their constructive remarks, which greatly improved the quality of the manuscript and linguistic corrections. We are grateful to Prof. ROSTISLAV BRZOBOHATY (Masaryk University in Brno, Czech Republic) and Dr. MALGORZATA BIENKOWSKA-WASILUK (Instytut Paleobiologii PAN, Warszawa, Poland) for their suggestions. Dr. GUNTER SCHWEIGERT is acknowledged for his help during editorial process. The work of T.P. was supported by the institutional projects AVOZ30130516 and RVO67985831 from the Institute of Geology AS CR, v.v.i. The research of P.S. was supported by the project MSM 61989100 19.	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S., 1888, ANN MAGAZINE NATUR 6, V1, P36	73	0	0	0	8	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	APR	2013	268	1					113	123		10.1127/0077-7749/2013/0322	http://dx.doi.org/10.1127/0077-7749/2013/0322			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	113JA					2025-03-11	WOS:000316661600006
J	Guler, MV; Lazo, DG; Pazos, PJ; Borel, CM; Ottone, EG; Tyson, RV; Cesaretti, N; Aguirre-Urreta, MB				Guler, M. V.; Lazo, D. G.; Pazos, P. J.; Borel, C. M.; Ottone, E. G.; Tyson, R. V.; Cesaretti, N.; Aguirre-Urreta, M. B.			Palynofacies analysis and palynology of the Agua de la Mula Member (Agrio Formation) in a sequence stratigraphy framework, Lower Cretaceous, Neuquen Basin, Argentina	CRETACEOUS RESEARCH			English	Article						Palynofacies; Palynology; Agrio Formation; Lower Cretaceous; Neuquen Basin; Argentina	DINOFLAGELLATE CYST STRATIGRAPHY; SEA-LEVEL CHANGES; GYMNOSPERM POLLEN; PILMATUE MEMBER; LOWSTAND WEDGE; ULTRASTRUCTURE; PATAGONIA; GRAINS; RAMP	Variations in the sedimentary organic matter were documented throughout the Agua de la Mula Member (late Hauterivian) of the Agrio Formation, at a combined section in the type area of the Agrio Formation; the base at Agrio del Medio and the middle to top at Bajada del Agrio. A main organic-rich interval was identified in the basal Agua de la Mula Member, dominated by marine-derived Amorphous Organic Matter (AOM), coinciding with the highest Total Organic Carbon (TOC) content, between 1.4 and 3.8 wt.%, suggesting dysoxic conditions. The rest of the Member is predominantly characterized by terrestrially-derived organic matter, mainly phytoclasts, with low TOC values, around 1% or lower, indicating predominantly oxic depositional settings. By integrating stacking pattern and shell beds analysis, four depositional sequences SQ1-SQ4 were recognized. The organic-rich, finely laminated bituminous black shales of the Spitidiscus riccardii zone constitute a mayor and rapid inundation defining a Transgressive System tract (TST), related to a third order asymmetrical mesosequence dominated by a thick High System Tract (HST). It represents the most widespread and important flooding episode within the Neuquen Basin during the late Hauterivian. Inside sequences of higher frequency (SQ1, SQ2, SQ3, SQ4) of probably fourth order were recognized and analysed including several ammonids zones (Spitidiscus riccardii, Crioceratites schlagintweiti, C diamantensis and Paraspiticeras groeberi). With the exception of the oxygen-controlled, basinal and outer ramp settings indicated for the TST1, which is equivalent to the TST of a lower order sequence, and the lower TST2, respectively, the prevalence of well oxygenated, inner to middle ramp depositional environments, is suggested for the rest of the sedimentary succession and emphasized in HST of SQ2, SQ3 and SQ4. Thus, a shallowing-upward trend with improved oxygenation is recorded through the Agua de la Mula Member, reflected by decreasing TOC, AOM content and preservation state of the organic matter. Based on the whole rock fluorescence analysis of the two selected organic-rich intervals from the Spitidiscus riccardii and the lowermost Crioceratites diamantensis zones, the presence of hydrocarbons suggests a very early in situ generation. (c) 2012 Elsevier Ltd. All rights reserved.	[Guler, M. V.; Borel, C. M.; Cesaretti, N.] Univ Nacl Sur, Dept Geol, Inst Geol Sur, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Lazo, D. G.; Pazos, P. J.; Ottone, E. G.; Aguirre-Urreta, M. B.] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Inst Estudios Andinos Don Pablo Graeber, RA-1428 Buenos Aires, DF, Argentina; [Tyson, R. V.] Getech, Leeds LS8 2LJ, W Yorkshire, England; [Guler, M. V.; Lazo, D. G.; Pazos, P. J.; Borel, C. M.; Ottone, E. G.; Aguirre-Urreta, M. B.] Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); University of Buenos Aires; University of Leeds; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Guler, MV (通讯作者)，Univ Nacl Sur, INGEOSUR, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	vguler@criba.edu.ar	Pazos, Pablo/D-5973-2014; Lazo, Dario/AAT-9498-2021	Borel, C. Marcela/0000-0001-5772-4534; Pazos, Pablo/0000-0003-3728-6906; Lazo, Dario G./0000-0002-8270-1577	ANPCyP PICT [189]; UBACyT [x001]	ANPCyP PICT; UBACyT	Cecilia Cataldo and Diana Fernandez (Universidad de Buenos Aires) are specially thanked for their help during fieldwork. To Marcelo Martinez (Laboratorio de Palinologia, Universidad Nacional del Sur) for his assistance in the fluorescence observations. The authors would also like to thank two anonymous referees and E. Koutsoukos for their constructive revision of the manuscript. This work was partially financed by ANPCyP PICT 189 and UBACyT x001 projects to M.B. Aguirre-Urreta (UBA). This is a contribution R-35 of the Instituto de Estudios Andinos Don Pablo Groeber (IDEAN).	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Res.	APR	2013	41						65	81		10.1016/j.cretres.2012.10.006	http://dx.doi.org/10.1016/j.cretres.2012.10.006			17	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	112HG		Green Published			2025-03-11	WOS:000316582700006
J	McMinn, A; Martin, A				McMinn, A.; Martin, A.			Dark survival in a warming world	PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES			English	Review						dark survival; Antarctic; winter; microalgae; phytoplankton	SEA-ICE ALGAE; MCMURDO SOUND; WEDDELL SEA; MARINE-PHYTOPLANKTON; ANTARCTIC LAKE; LIGHT; DIATOMS; WINTER; PHOTOSYNTHESIS; TEMPERATURE	Most algae regularly experience periods of darkness ranging from a few hours to a few days. During this time, they are unable to photosynthesize, and so must consume stored energy products. However, some organisms such as polar algae and some microalgal cysts and spores are exposed to darkness for months to years, and these must use alternative strategies to survive. Some taxa, such as dinoflagellates, form cysts and become dormant. Others use physiological methods or adopt mixotrophy. The longest documented survival of more than a century was for dinoflagellates buried in sediments in a Norwegian fjord. Seasonal changes in daylight hours are naturally unaffected by climate change. This means that polar microalgae will in the future need to survive the same period of seasonal darkness but at higher temperatures, and this will require a greater drawdown of stored energy. Recent experimental work has shown that both Arctic and Antarctic phytoplankton are able to survive increases of up to 6 degrees C in the dark.	[McMinn, A.; Martin, A.] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia	University of Tasmania	McMinn, A (通讯作者)，Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia.	andrew.mcminn@utas.edu.au	Martin, Andrew/F-5688-2013; McMinn, Andrew/A-9910-2008	Martin, Andrew/0000-0001-8260-5529				Agustí S, 2004, AQUAT MICROB ECOL, V35, P197; [Anonymous], 2011, LIGHT PHOTOSYNTHESIS, DOI DOI 10.1017/CBO9781139168212; Backhaus JO, 2003, MAR ECOL PROG SER, V251, P1, DOI 10.3354/meps251001; Balzer I, 1996, BIOL RHYTHM RES, V27, P386, DOI 10.1076/brhm.27.3.386.12961; BINDER BJ, 1987, J PHYCOL, V23, P99; Britt AB, 1996, ANNU REV PLANT PHYS, V47, P75, DOI 10.1146/annurev.arplant.47.1.75; BUNT JS, 1972, LIMNOL OCEANOGR, V17, P458, DOI 10.4319/lo.1972.17.3.0458; CULLEN JJ, 1982, CAN J FISH AQUAT SCI, V39, P791, DOI 10.1139/f82-108; DAYTON PK, 1986, POLAR BIOL, V6, P207, DOI 10.1007/BF00443397; DOUCETTE GJ, 1983, MAR BIOL, V78, P1, DOI 10.1007/BF00392964; DURBAN E, 1974, J BACTERIOL, V118, P129, DOI 10.1128/JB.118.1.129-138.1974; 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R. Soc. B-Biol. Sci.	MAR 22	2013	280	1755							20122909	10.1098/rspb.2012.2909	http://dx.doi.org/10.1098/rspb.2012.2909			7	Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Environmental Sciences & Ecology; Evolutionary Biology	081YC	23345578	Bronze, Green Published			2025-03-11	WOS:000314357600013
J	Mohamed, O; Piller, WE; Egger, H				Mohamed, Omar; Piller, Werner E.; Egger, Hans			Dinoflagellate cysts and palynofacies across the Cretaceous/Palaeogene boundary at the Neritic Waidach Section (Eastern Alps, Austria)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Helvetic thrust unit; Cretaceous-Palaeogene boundary; geochemistry; calcareous nannoplankton; dinoflagellate cysts; palynofacies	CRETACEOUS-TERTIARY BOUNDARY; CALCAREOUS NANNOFOSSIL; NEW-ZEALAND; SEA-LEVEL; EL-KEF; STRATIGRAPHY; IMPACT; BIOSTRATIGRAPHY; EUROPE	In this study, dinoflagellate cyst and calcareous nannoplankton biostratigraphy allowed the recognition of the Cretaceous/Palaeogene boundary (K/Pg boundary) at the neritic Waidach section, north of Salzburg, Austria (Helvetic nappe system). The microfossil assemblages indicate calcareous nannoplankton Zone CC26 of latest Cretaceous age and part of the lowermost Palaeocene Zone NP1. However, the stratigraphic record across the K/Pg boundary is incomplete due to a minor fault The studied samples have yielded well preserved and high diversity dinoflagellate cyst assemblages with a total of 163 dinoflagellate cyst species and subspecies belonging to 62 genera. The composition of the dinoflagellate cyst assemblages changes drastically from Areoligera-dominated assemblages in the upper Maastrichtian to Hystrichosphaeridium-dominated assemblages in the lower Danian. This composition shows two Manumiella spikes in the upper Maastrichtian and an acme of Spongodinium delitiense in the lower Danian which are interpreted to reflect slight coolings of oceanic surface waters. The earliest Danian markers Carpatella cornuta, Senoniasphaera inornata and Damassadinium californicum have their first occurrences immediately above the K/Pg boundary. The peridinioid/gonyaulacoid (P/G) ratio of most samples suggests high paleoproductivity. Two palynofacies assemblages were distinguished indicating shelf to basin transitions and dysoxic to anoxic conditions. (c) 2012 Elsevier B.V. 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; werner.piller@uni-graz.at; hans.egger@geologie.ac.at		Piller, Werner E./0000-0003-2808-4720; Mohamed, Omar/0000-0002-2817-1683	Ministry of High Education of Egypt	Ministry of High Education of Egypt(Ministry of Higher Education & Scientific Research (MHESR))	We are indebted to Pi Willumsen (Lund University, Sweden) for constructive comments and review of an early version of this manuscript. Thanks go to the staff of the geochemical laboratory of the Institute of Earth Sciences at Graz University. Helpful reviews by Vivi Vajda (Lund University, Sweden) and others are gratefully acknowledged. Omar Mohamed thanks the Ministry of High Education of Egypt for funding this study which is part of his Ph.D. thesis.	Askin R.A., 1988, Geology and Paleontology of Seymour Island Antarctic Peninsula, V169, P155, DOI [10.1130/MEM169-p155, DOI 10.1130/MEM169-P155, 10.1130/mem169-p155]; Below Raimond, 1997, Palaeontographica Abteilung B Palaeophytologie, V242, P1; Benson D.G. 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Palaeobot. Palynology	MAR 15	2013	190						85	103		10.1016/j.revpalbo.2012.11.002	http://dx.doi.org/10.1016/j.revpalbo.2012.11.002			19	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	118LQ					2025-03-11	WOS:000317027400008
J	Riding, JB; Leng, MJ; Kender, S; Hesselbo, SP; Feist-Burkhardt, S				Riding, James B.; Leng, Melanie J.; Kender, Sev; Hesselbo, Stephen P.; Feist-Burkhardt, Susanne			Isotopic and palynological evidence for a new Early Jurassic environmental perturbation	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Environmental change; Palynomorphs; Stable isotopes; Early Jurassic (Late Sinemurian); Central England	EOCENE THERMAL MAXIMUM; OCEANIC ANOXIC EVENT; SEA-LEVEL FALL; SEQUENCE STRATIGRAPHY; DINOFLAGELLATE CYSTS; MASSIVE DISSOCIATION; METHANE RELEASE; GAS HYDRATE; FOSSIL WOOD; LIAS GROUP	The Early Jurassic Epoch was a predominantly greenhouse phase of Earth history, but a comprehensive understanding of its climate dynamics is hampered by a lack of high resolution multi-proxy environmental records. Here we report a geologically brief (approximately several hundred thousand years) negative carbon isotope excursion (CIE) of 2-3 parts per thousand in both marine and terrestrial materials, recognised for the first time for the Late Sinemurian Substage (Early Jurassic, similar to 194 Ma) of eastern England. The Late Sinemurian carbon isotope excursion, which is termed the S-CIE herein, is accompanied by peaks in the abundance of the pollen grain Classopollis classoides and the dinoflagellate cyst Liasidium variabile. Classopollis classoides was thermophilic and is a reliable proxy for hot/warm climatic conditions. Liasidium variabile is interpreted as thermophilic and eutrophic using multivariate statistics, its fluorescence properties being similar to living heterotrophic dinoflagellate cysts, and its association with C. classoides. Moreover, the morphological and ecological similarities of L. variabile to the Cenozoic genus Apectodinium are noteworthy. The co-occurrence of the acmes of C. classoides and L variabile with a negative CIE is interpreted here as having wide geographical significance due to the marine and terrestrial carbon isotope signals being precisely in phase within an open marine setting. This is consistent with an oceanic-atmospheric injection of isotopically-light carbon, coupled with global warming and increased marginal marine nutrient supply, possibly the result of increased precipitation due to an enhanced hydrological cycle or a seasonally-stratified water column. A probable sea level rise of at least regional extent has been identified at the L variabile event in other records, which supports this putative phase of global warming. All these features are common to the Paleocene/Eocene thermal maximum (PETM, similar to 56 Ma), and there are also similarities with the Early Toarcian oceanic anoxic event (T-OAE, similar to 182 Ma). (C) 2012 Natural Environment Research Council. Published by Elsevier B.V. All rights reserved.	[Riding, James B.; Kender, Sev] British Geol Survey, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England; [Leng, Melanie J.] Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England; [Leng, Melanie J.] British Geol Survey, NERC Isotope Geosci Lab, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England; [Hesselbo, Stephen P.] Univ Oxford, Dept Earth Sci, Oxford OX1 3AN, 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; University of Leicester; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Oxford	Riding, JB (通讯作者)，British Geol Survey, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk	Feist-Burkhardt, Susanne/B-1522-2009; Kender, Sev/B-9409-2016	Feist-Burkhardt, Susanne/0000-0001-6019-6242; Leng, Melanie/0000-0003-1115-5166; Kender, Sev/0000-0003-4216-3214; Hesselbo, Stephen/0000-0001-6178-5401	NERC [nigl010001, bgs05002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Abbink O.A., 1998, CONTRIBUTIONS SERIES, V8; ALVIN KL, 1982, REV PALAEOBOT PALYNO, V37, P71, DOI 10.1016/0034-6667(82)90038-0; [Anonymous], 1998, Mesozoic and Cenozoic Sequence Stratigraphy of European Basins; [Anonymous], 2004, Taxon; [Anonymous], 1999, WARM CLIMATES EARTH, DOI DOI 10.1017/CBO9780511564512.011; BATTEN D.J., 1975, P GEOL ASS, V85, P433; Batten DJ., 1984, 3 S MES TERR EC, P7; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; Berridge N.G., 1999, MEMOIR BRIT GEOLOGIC, V127, P1; Bodin S, 2010, PALAEOGEOGR PALAEOCL, V297, P377, DOI 10.1016/j.palaeo.2010.08.018; Bradshaw M.J., 1992, Atlas of Palaeogeography and Lithofacies: Geological Society Memoir #13, P107, DOI [DOI 10.1144/GSL.MEM.1992.013.01.12, 10.1144/GSL.MEM.1992.013.01.12]; Brandon A., 1990, P. 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MAR 15	2013	374						16	27		10.1016/j.palaeo.2012.10.019	http://dx.doi.org/10.1016/j.palaeo.2012.10.019			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	122MR		Green Accepted, Green Published, hybrid			2025-03-11	WOS:000317322700002
J	Gu, HF; Luo, ZH; Liu, TT; Lan, DZ				Gu, Haifeng; Luo, Zhaohe; Liu, Tingting; Lan, Dongzhao			Morphology and phylogeny of <i>Scrippsiella enormis</i> sp nov and S. cf. <i>spinifera</i> (Peridiniales, Dinophyceae) from the China Sea	PHYCOLOGIA			English	Article						Calcareous dinoflagellates; Cysts; ITS rRNA; Scrippsiella enormis; Scrippsiella spinifera	MARINE DINOFLAGELLATE; MEDITERRANEAN SEA; RECENT SEDIMENTS; SEQUENCE DATA; MIXED MODELS; CYSTS; THORACOSPHAERACEAE; TROCHOIDEA; CALCIODINELLOIDEAE; CALIFORNIA	The genus Scrippsiella contains approximately 20 species that are widespread in coastal and oceanic areas. Classification of Scrippsiella traditionally relied on cyst morphology because the plate pattern was rather conserved. A new species, S. enormis sp. nov. was obtained by incubating a noncalcified cyst from sediments collected in the East China Sea. The vegetative cells consisted of a conical-convex epitheca and a round hypotheca with the plate formula of po, x, 4', 3a, 7', 6c (5c+t), 5s, 5'''', 2''''. It differed from other Scrippsiella species by possessing an asymmetrical 1' and generating noncalcareous, spherical cysts with paratabulation. Phylogenetic analyses based on internal transcribed spacer (ITS) and 5.8S rDNA sequences revealed that S. enormis was nested within the Calciodinellum clade. In addition, two strains of S. cf. spinifera (strains SSFC02, SSFC03) were obtained by incubating calcareous cysts from sediments collected in the South China Sea. They shared identical ITS sequence and formed a sister clade of the S. trochoidea species complex, suggesting little phylogenetic significance of antapical spines in Scrippsiella.	[Gu, Haifeng; Luo, Zhaohe; Liu, Tingting; Lan, Dongzhao] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com	Luo, Zhaohe/ITT-7163-2023; Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171; Luo, Zhaohe/0000-0001-8662-2414	National Scientific-Basic Special Fund [2009FY210400]; National Natural Science Foundation of China [0900081, 41101060]	National Scientific-Basic Special Fund; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We are greatly indebted to Masanobu Kawachi (National Institute for Environmental Studies, Japan) for help with identification of strain NIES-684. We thank Marc Gottschling, Ken-ichiro Ishida, and two anonymous reviewers for constructive suggestions. This project was supported by the National Scientific-Basic Special Fund (Grant No. 2009FY210400) and National Natural Science Foundation of China (Grant No. 0900081, 41101060).	Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P572, DOI 10.2216/07-02.1; BALECH E, 1959, BIOL BULL-US, V116, P195, DOI 10.2307/1539204; BALECH E., 1963, U NACL PLATA FACULTA, V20, P111; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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J	Taldenkova, E; Bauch, HA; Stepanova, A; Ovsepyan, Y; Pogodina, I; Klyuvitkina, T; Nikolaev, S				Taldenkova, Ekaterina; Bauch, Henning A.; Stepanova, Anna; Ovsepyan, Yaroslav; Pogodina, Irina; Klyuvitkina, Tatiana; Nikolaev, Sergei			Reprint of: Benthic and planktic community changes at the North Siberian margin in response to Atlantic water mass variability since last deglacial times	MARINE MICROPALEONTOLOGY			English	Article						Atlantic-derived water; Laptev Sea; Planktic and benthic foraminifers; Ostracods; Deglaciation; Holocene	SEA CONTINENTAL-MARGIN; SW BARENTS SEA; LAPTEV SEA; ARCTIC-OCEAN; HOLOCENE PALEOCEANOGRAPHY; DINOFLAGELLATE CYSTS; HIGH-RESOLUTION; ICE-SHEET; CLIMATE VARIABILITY; SVALBARD MARGIN	The eastward penetration of Atlantic-derived water (ADW) into the Eurasian Basin of the Arctic Ocean was investigated at the western Laptev Sea continental margin for the time since c. 17.6 ka. Using a high-resolution investigation of the lithology, geochemistry, planktic and benthic foraminifers, and ostracods on a sediment core from 270 m water depth major steps in the environmental evolution of the region are recognized. In general, ADW was continuously present in the study area. Between 17.6 and 15.4 ka ADW manifested itself through open-water polynyas and associated upwelling events. Comparison between the Laptev Sea and northern Svalbard shelf using Cassidulina neoteretis allows assuming an unmodified subsurface inflow of ADW within its northern branch between 15.4 and 13.2, which was strongest after 14.7-ka and in line with the overall climate amelioration. A local freshwater event at 13 ka followed by shelf flooding and the establishment of a freshened shelf water mass resulted in an off-shelf displacement of ADW from the studied site as suggested by the disappearance of C neoteretis between 12 and 7 ka. As evidenced by an abundance peak in Nonion labradoricum, the sea-ice marginal zone was located at the site around 12-11 ka but then shifted northward during the early Holocene warming. Enhanced ADW inflow since 7 ka correlated with climate cooling and southward retreat of the seasonal drift-ice margin. The inflow of ADW during mid-late Holocene differed from deglacial times because of the combined influence of northern and eastern ADW branches. (C) 2013 Published by Elsevier B.V.	[Taldenkova, Ekaterina; Ovsepyan, Yaroslav; Klyuvitkina, Tatiana; Nikolaev, Sergei] Lomonosov Moscow State Univ, Fac Geog, Moscow 119991, Russia; [Bauch, Henning A.] GEOMAR, Mainz Acad Sci Humanities & Literature, D-24148 Kiel, Germany; [Stepanova, Anna] Paleontol Inst RAS, Moscow 117997, Russia; [Pogodina, Irina] Murmansk Marine Biol Inst, Murmansk 183010, Russia	Lomonosov Moscow State University; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Russian Academy of Sciences; Russian Academy of Sciences; Murmansk Marine Biological Institute	Taldenkova, E (通讯作者)，Lomonosov Moscow State Univ, Fac Geog, Leninskie Gory 1, Moscow 119991, Russia.	etaldenkova@mail.ru; hbauch@geomar.de; a.yu.stepanova@gmail.com; yaovsepyan@yandex.ru; t.klyuvitkina@mail.ru; cdnik@rambler.ru	Nikolaev, Sergei/L-8882-2015; Ovsepyan, Yaroslav/D-4667-2014; Klyuvitkina, Tatyana/L-8843-2015; Taldenkova, Ekaterina/L-7853-2015	Taldenkova, Ekaterina/0000-0002-0959-4111; Ovsepyan, Yaroslav/0000-0003-1172-4357	BMBF; Russian Ministry for Education and Science (OSL fellowship projects); Russian Foundation for Basic Research [08-05-00849, 11-05-01091]; INTAS [03-51-6682]	BMBF(Federal Ministry of Education & Research (BMBF)); Russian Ministry for Education and Science (OSL fellowship projects); Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); INTAS(INTAS)	We thank the team from the Leibniz Laboratory (Kiel) for conducting AMS<SUP>14</SUP>C measurements and T. Mueller-Lupp for providing geochemical data. We acknowledge the assistance of collaborators of the Otto Schmidt Laboratory for Polar and Marine Sciences (OSL) in sample processing. We thank M. Slubowska-Woldengen with her co-authors for providing us with their original data. This research was supported by the BMBF and Russian Ministry for Education and Science (OSL fellowship projects), the Russian Foundation for Basic Research (projects 08-05-00849 and 11-05-01091), and INTAS (project 03-51-6682).	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Micropaleontol.	MAR	2013	99						29	44		10.1016/j.marmicro.2013.03.010	http://dx.doi.org/10.1016/j.marmicro.2013.03.010			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	164NR					2025-03-11	WOS:000320417300005
J	Miller, CS; Leroy, SAG; Izon, G; Lahijani, HAK; Marret, F; Cundy, AB; Teasdale, PA				Miller, Ch. S.; Leroy, S. A. G.; Izon, G.; Lahijani, H. A. K.; Marret, F.; Cundy, A. B.; Teasdale, P. A.			Palynology: A tool to identify abrupt events? An example from Chabahar Bay, southern Iran	MARINE GEOLOGY			English	Article						palynology; palaeoevent; Sea of Oman; flood; storm; tsunami	NORTHWESTERN INDIAN-OCEAN; GRAIN-SIZE DISTRIBUTION; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; MARINE-SEDIMENTS; STORM DEPOSITS; TSUNAMI; PAKISTAN; COASTS; NORTH	Tsunami, storm and flood events are destructive agents that have the potential to cause much damage and cost lives. The coastal regions around the north-western Arabian Sea are prone to these natural disasters with recent events including the storm and flood of AD 1842, the Makran tsunami of 1945, and Cyclone Gonu in 2007. Despite their severity, the paucity of reliable historical records does not allow us to answer pertinent questions concerning their frequency, intensity and impact. Palaeo-event analysis from the geological record allows us to extend, and test, the historical record. Here we have dated and examined a 92 cm long sediment core from the tectonically active, cyclone and storm prone Chabahar Bay area (southern Iran). Our appraisal directly tests conventional proxies for identifying abrupt events (e.g. grain-size, geochemical data), which we supplement with a novel palynological (pollen and dinocyst) approach. Both sedimentological and palynological approaches suggest a large event which was dated at <AD 1808 +/- 41, whereas geochemical approaches remain inconclusive. The increase of continentally derived pollen (Pinaceae, Salix, Betula and Typha-Sparganium), increases in Brigantedinium sp. and S. ramosus as well as decreases in Lingulodinium machaerophorum suggest enhanced fluvial delivery in association with a flood. This investigation provides evidence of a major flash-flood affecting the Chabahar Bay region at <AD 1808 +/- 41 which we infer is the geological expression of the storm and associated flash flood of AD 1842. Moreover, our study demonstrates the utility of palynology in identifying and understanding the causes of abrupt events to complement more widely applied techniques. (C) 2013 Elsevier B.V. All rights reserved.	[Miller, Ch. S.; Leroy, S. A. G.] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Izon, G.] Univ St Andrews, Dept Earth Sci, St Andrews KY16 9AL, Fife, Scotland; [Izon, G.] Univ Leeds, Sch Earth & Environm, Leeds LS2 1JT, W Yorkshire, England; [Lahijani, H. A. K.] INIO, Tehran 1411813389, Iran; [Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Cundy, A. B.; Teasdale, P. A.] Univ Brighton, Sch Environm & Technol, Brighton BN2 4GJ, E Sussex, England	Brunel University; University of St Andrews; University of Leeds; University of Liverpool; University of Brighton	Miller, CS (通讯作者)，Open Univ, Dept Environm Earth & Ecosyst, CEPSAR, Milton Keynes MK7 6AA, Bucks, England.	c.s.miller@open.ac.uk; Suzanne.Leroy@brunel.ac.uk; G.J.Izon@leeds.ac.uk; lahijani@inio.ac.ir; F.Marret@liv.ac.uk; A.Cundy@brighton.ac.uk; P.A.Teasdale@brighton.ac.uk	Leroy, Suzanne/D-3996-2009; Cundy, Andy/AAE-3234-2020; Alizadeh Ketek Lahijani, Hamid/GRF-3549-2022; Izon, Gareth/AAQ-4033-2020	Izon, Gareth/0000-0003-2742-4922; Cundy, Andy/0000-0003-4368-2569; Alizadeh Ketek Lahijani, Hamid/0000-0001-6136-3655; Marret-Davies, Fabienne/0000-0003-4244-0437	Brunel University	Brunel University	CSM would like to thank L Miller, G. Miller and Brunel University for financial support. Gratitude is extended to S. Kershaw and C. Baeteman for useful and pertinent suggestions provided as part of CSM's viva examination. Finally we are grateful to R. Fensome and H. Brinkhuis for discussion regarding species identification.	Al-Qurashi A. M., 2010, INDIAN OCEAN TROPI S; Ambraseys N.N., 1982, HIST PERSIAN EARTHQU; [Anonymous], QUATERNARY GEOLOGY; [Anonymous], GEOSCIENCE TEXTS; Appleby P. 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Geol.	MAR 1	2013	337						195	201		10.1016/j.margeo.2013.03.004	http://dx.doi.org/10.1016/j.margeo.2013.03.004			7	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	159ZI		hybrid, Green Published, Green Submitted, Green Accepted			2025-03-11	WOS:000320085400015
J	Jiménez-Moreno, G; Pérez-Asensio, JN; Larrasoaña, JC; Aguirre, J; Civis, J; Rivas-Carballo, MR; Valle-Hernández, MF; González-Delgado, JA				Jimenez-Moreno, Gonzalo; Noel Perez-Asensio, Jose; Cruz Larrasoana, Juan; Aguirre, Julio; Civis, Jorge; Rosario Rivas-Carballo, Maria; Valle-Hernandez, Maria F.; Angel Gonzalez-Delgado, Jose			Vegetation, sea-level, and climate changes during the Messinian salinity crisis	GEOLOGICAL SOCIETY OF AMERICA BULLETIN			English	Article							GUADALQUIVIR FORELAND BASIN; STABLE-ISOTOPE STRATIGRAPHY; HIGH-RESOLUTION CHRONOLOGY; NORTH-BETIC STRAIT; SORBAS BASIN; LATE MIOCENE; TEMPERATE CARBONATES; MEDITERRANEAN BASIN; TRIPOLI FORMATION; MARINE-SEDIMENTS	The Messinian salinity crisis (late Miocene) is one of the most fascinating paleoceanographic events in the recent geological history of the Mediterranean Sea, defining a time when it partly or nearly completely dried out. However, the relative roles of tectonic processes and sea-level changes, as triggers for restriction and isolation of the Mediterranean Sea from the open ocean, are still under debate. In this study, we present a detailed pollen, dinoflagellate cyst (dinocyst), and magnetic susceptibility analysis of a sequence of late Neogene (between ca. 7.3 and 5.2 Ma) marine sediments from the Montemayor-1 core (lower Guadalquivir Basin, southwestern Spain), which provides a continuous record of paleoenvironmental variations in the Atlantic side of the Betic corridors during the late Miocene. Our results show that significant paired vegetation and sea-level changes occurred during the Messinian, likely triggered by orbital-scale climate change. Important cooling events and corresponding glacio-eustatic sea-level drops are observed in this study at ca. 5.95 and 5.75 Ma, coinciding with the timing and duration of oxygen isotopic events TG32 and TG22-20 recorded in marine sediments worldwide. It is generally accepted that the onset of the Messinian salinity crisis began at ca. 5.96 +/- 0.02 Ma. Therefore, this study suggests that the restriction of the Mediterranean could have been triggered, at least in part, by a strong glacio-eustatic sea-level drop linked to a climate cooling event occurring at the time of initiation of the Messinian salinity crisis.	[Jimenez-Moreno, Gonzalo; Noel Perez-Asensio, Jose; Aguirre, Julio] Univ Granada, Dept Estratig & Paleontol, Granada 18002, Spain; [Cruz Larrasoana, Juan] Inst Geol & Minero Espana, Unidad Zaragoza, Zaragoza 50006, Spain; [Civis, Jorge; Rosario Rivas-Carballo, Maria; Valle-Hernandez, Maria F.; Angel Gonzalez-Delgado, Jose] Univ Salamanca, Dept Geol, E-37008 Salamanca, Spain	University of Granada; University of Salamanca	Jiménez-Moreno, G (通讯作者)，Univ Granada, Dept Estratig & Paleontol, Fuente Nueva S-N, Granada 18002, Spain.	gonzaloj@ugr.es	Pérez-Asensio, José N./J-2971-2014; Larrasoana, Juan/O-1350-2013; Jimenez-Moreno, Gonzalo/K-6753-2017	Jimenez-Moreno, Gonzalo/0000-0001-7185-8686; Perez-Asensio, Jose N./0000-0002-1393-7412; Larrasoana, Juan Cruz/0000-0003-4568-631X; Gonzalez-Delgado, Jose Angel/0000-0002-2591-7013; Rivas Carballo, M.R./0000-0001-5267-7767	Spanish Ministry of Science and Education [CGL-2007-60774/BTE, CGL-2010-20857/BTE]; Junta de Andalucia (Spain) [RNM-190]; Spanish Ministry of Education [AP2007-00345]	Spanish Ministry of Science and Education(Spanish Government); Junta de Andalucia (Spain)(Junta de Andalucia); Spanish Ministry of Education(Spanish Government)	The authors' research was funded by research grants CGL-2007-60774/BTE and CGL-2010-20857/BTE from the Spanish Ministry of Science and Education, and the Research Group RNM-190 of the Junta de Andalucia (Spain). Perez-Asensio was funded by a research scholarship provided by the Spanish Ministry of Education (F.P.U. scholarship, ref. AP2007-00345). We also would like to thank three anonymous reviewers and the editor for very constructive comments on a previous version of the manuscript.	AGUIRRE J, 1995, PALAEOGEOGR PALAEOCL, V117, P139, DOI 10.1016/0031-0182(94)00123-P; Aguirre J, 2004, SEDIMENT GEOL, V168, P71, DOI 10.1016/j.sedgeo.2004.03.004; Aguirre J., 2007, 13 JORN SOC ESP PAL, P53; Aguirre J, 1995, REV SOC GEOL ESP, V8, P161; Aguirre Rodriguez J., 1992, Revista Espanola de Paleontologia, P3; Agustí J, 2006, PALAEOGEOGR PALAEOCL, V238, P5, DOI 10.1016/j.palaeo.2006.03.013; AHARON P, 1993, GEOLOGY, V21, P771, DOI 10.1130/0091-7613(1993)021<0771:SLEITS>2.3.CO;2; Baceta J.I., 1999, Rev. Soc. Geol. 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Soc. Am. Bull.	MAR-APR	2013	125	3-4					432	444		10.1130/B30663.1	http://dx.doi.org/10.1130/B30663.1			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	130IJ					2025-03-11	WOS:000317907000010
J	Bechtel, A; Movsumova, U; Strobl, SAI; Sachsenhofer, RF; Soliman, A; Gratzer, R; Püttmann, W				Bechtel, Achim; Movsumova, Ulviyya; Strobl, Susanne A. I.; Sachsenhofer, Reinhard F.; Soliman, Ali; Gratzer, Reinhard; Puettmann, Wilhelm			Organofacies and paleoenvironment of the Oligocene Maikop series of Angeharan (eastern Azerbaijan)	ORGANIC GEOCHEMISTRY			English	Article							DINOFLAGELLATE CYST BIOSTRATIGRAPHY; ORGANIC-MATTER; SOURCE ROCKS; DEPOSITIONAL ENVIRONMENT; ISOPRENOID THIOPHENES; ISOTOPIC COMPOSITIONS; BIOLOGICAL MARKERS; MULHOUSE BASIN; FORELAND BASIN; MOLASSE BASIN	The Maikop Formation, deposited in eastern Azerbaijan during Oligocene and Early Miocene times, contains prolific source rocks with primarily Type II organic matter. Paleontological analyses of dinoflagellate cysts revealed a Lower to Upper Oligocene age for the investigated succession near Angeharan. A major contribution of aquatic organisms (diatoms, green algae, dinoflagellates, chrysophyte algae) and minor inputs from macrophytes and land plants to organic matter accumulation is indicated by n-alkane distribution patterns, composition of steroids and delta C-13 of hydrocarbon biomarkers. Microbial communities included heterotrophic bacteria, cyanobacteria, chemoautotrophic bacteria, as well as green sulfur bacteria. Higher inputs of terrigenous organic matter occurred during deposition of the Upper Oligocene units of the Maikop Formation from Angeharan mountains. The terpenoid hydrocarbon composition argues for angiosperm dominated vegetation in the Shamakhy-Gobustan area. High primary bioproductivity resulted in a stratified water column and the accumulation of organic matter rich sediments in the Lower Oligocene units of the Maikop Formation. Organic carbon accumulation during this period occurred in a permanently (salinity-) stratified, mesohaline environment with free H2S in the water column. This is indicated by low pristane/phytane ratios of all sediments (varying from 0.37-0.69), lower methylated-(trimethyltridecyl) chromans ratio in the lower units and their higher contents of aryl isoprenoids and highly branched isoprenoid thiophenes. Subsequently, the depositional environment changed to normal marine conditions with oxygen deficient bottom water. The retreat of the chemocline towards the sediment-water interface and enhanced oxic respiration of OM during deposition of the Upper Oligocene Maikop sediments is proposed. Parallel depth trends in delta C-13 of total OM, n-alkanes, isoprenoids and steranes argue for changes in the regional carbon cycle, associated with the changing environmental conditions. Increased remineralisation of OM in a more oxygenated water column is suggested to result in low TOC and hydrocarbon contents, as well as N-15 enriched total nitrogen of the Upper Oligocene units. (C) 2013 Elsevier Ltd. All rights reserved.	[Bechtel, Achim; Strobl, Susanne A. I.; Sachsenhofer, Reinhard F.; Gratzer, Reinhard] Univ Leoben, Dept Appl Geosci & Geophys, A-8700 Leoben, Austria; [Movsumova, Ulviyya] Azerbaijan Natl Acad Sci, Inst Geol, Baku 370143, Azerbaijan; [Soliman, Ali] Karl Franzens Univ Graz, Inst Earth Sci, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Puettmann, Wilhelm] Goethe Univ Frankfurt, Dept Environm Analyt Chem, Inst Atmospher & Environm Sci, D-60438 Frankfurt, Germany	University of Leoben; Azerbaijan National Academy of Sciences (ANAS); University of Graz; Egyptian Knowledge Bank (EKB); Tanta University; Goethe University Frankfurt	Bechtel, A (通讯作者)，Univ Leoben, Dept Appl Geosci & Geophys, Peter Tunner Str 5, A-8700 Leoben, Austria.	Achim.Bechtel@mu-leoben.at	Movsumova, Ulviyya/HCH-1905-2022; Bechtel, Achim/A-9885-2011; Soliman, Ali/R-1583-2018; Sachsenhofer, Reinhard/KFA-6113-2024	Sachsenhofer, Reinhard/0000-0002-6616-5583; Movsumova, Ulviyya/0000-0001-8486-2537; Bechtel, Achim/0000-0002-3937-8209; Soliman, Ali/0000-0001-7366-4607	European Research Foundation [237917]; Azerbaijan National Academy of Sciences; British Petroleum	European Research Foundation(European Science Foundation (ESF)); Azerbaijan National Academy of Sciences(Azerbaijan National Academy of Sciences (ANAS)); British Petroleum	Financial support by the European Research Foundation (Marie-Curie Re-integration Fellowship to A. B.; Project No. 237917) is gratefully acknowledged. Additional support was provided by the Azerbaijan National Academy of Sciences to U. M., and by British Petroleum. This article benefited from critical remarks of C. C. Walters and an anonymous reviewer.	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J	Gale, AS; Surlyk, F; Anderskouv, K				Gale, A. S.; Surlyk, F.; Anderskouv, K.			Channelling versus inversion: origin of condensed Upper Cretaceous chalks, eastern Isle of Wight, UK	JOURNAL OF THE GEOLOGICAL SOCIETY			English	Article							DINOFLAGELLATE CYST BIOSTRATIGRAPHY; PHOSPHATIC CHALKS; STEVNS-KLINT; MAASTRICHTIAN CHALK; SEISMIC EXPRESSION; BOTTOM CURRENTS; CARBON ISOTOPES; DENMARK; GEOCHEMISTRY; STRATIGRAPHY	Evidence from regional stratigraphical patterns in Santonian-Campanian chalk is used to infer the presence of a very broad channel system (5 km across) with a depth of at least 50 m, running NNW-SSE across the eastern Isle of Wight; only the western part of the channel wall and fill is exposed. Within this channel were smaller erosional structures (<10 m deep) that truncate originally horizontal bedding, are floored by hardgrounds, and locally have a basal fill of granular phosphorite. The entire channel system was progressively infilled by chalk, as demonstrated by the expanded succession of the lower Campanian Culver Chalk Formation. The beds of the channel fill are cut by small step faults, resulting from gravitational collapse. Complete burial had taken place by the base of the upper Campanian Portsdown Chalk Formation, which is of even thickness across the region. The structures are interpreted with reference to high-resolution seismic profiles through chalk channel systems described from the German sector of the North Sea, and the Santonian-Campanian of the eastern Paris Basin, and were formed by persistent bottom currents. Previous interpretations of the condensed Santonian-Campanian chalks in the eastern Isle of Wight, involving penecontemporaneous tectonic inversion of the underlying basement structure, are rejected.	[Gale, A. S.] Univ Portsmouth, Sch Earth & Environm Sci, Portsmouth PO1 3QL, Hants, England; [Surlyk, F.; Anderskouv, K.] Univ Copenhagen, Dept Geog & Geol, DK-1350 Copenhagen K, Denmark	University of Portsmouth; University of Copenhagen	Gale, AS (通讯作者)，Univ Portsmouth, Sch Earth & Environm Sci, Burnaby Bldg,Burnaby Rd, Portsmouth PO1 3QL, Hants, England.	Andy.Gale@port.ac.uk		Anderskouv, Kresten/0000-0002-6853-9737	Danish Natural Science Research Council; VILLUM Foundation	Danish Natural Science Research Council(Danish Natural Science Research Council); VILLUM Foundation(Villum Fonden)	The Danish Natural Science Research Council supported work by K. A. and F. S. The Velux Visting Professor Programme of the VILLUM Foundation is gratefully thanked for funding a 4 month visit to the University of Copenhagen of A. S. G. We thank the referees, D. Bosence and I. Jarvis, for most useful reviews of the paper.	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J	Gu, HF; Zeng, N; Xie, ZX; Wang, DZ; Wang, WG; Yang, WD				Gu, Haifeng; Zeng, Ni; Xie, Zhangxian; Wang, Dazhi; Wang, Weiguo; Yang, Weidong			Morphology, phylogeny, and toxicity of Atama complex (Dinophyceae) from the Chukchi Sea	POLAR BIOLOGY			English	Article						Alexandrium tamarense; Atama complex; Chukchi Sea; Morphology; Phylogeny; PSP toxin	DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; NORTH-AMERICAN; RIBOSOMAL DNA; CATENELLA DINOPHYCEAE; GENUS ALEXANDRIUM; LEBOUR BALECH; TOXIN; VARIABILITY; DYNAMICS; STRAINS	The "Atama complex", which consists of Alexandrium tamarense, A. fundyense, and A. catenella, is one of the most important groups within the dinoflagellate genus Alexandrium. Information of the biogeography of the Atama complex is limited in the Arctic Ocean. In the present study, we established 55 strains of the Atama complex by incubating ellipsoidal cysts collected from the Chukchi Sea. The vegetative cells are characterized by a prominent ventral pore, thereby fitting the description of A. tamarense morphotype. Large subunit (LSU) and/or internal transcribed spacer (ITS) region sequences of these strains were examined. Both sequences showed intragenomic polymorphism. The 708 bp of the LSU sequences from the strains differed from each other at 0-44 sites (0.0-6.2 %), and the ITS region sequences differed from one another at 0-28 sites (0.0-5.4 %). Phylogenetic analysis revealed that the Chukchi Sea strains were nested within Atama complex (Group I). Assessment of paralytic shellfish poisoning toxin production by four Chukchi Sea strains using high-performance liquid chromatography showed that total toxin per cell ranged from 9 to 41 fmol cell(-1). The toxin profile of the four strains from the Chukchi Sea is conserved, with the major toxins being N-sulfocarbamoyl toxin (C2), saxitoxin, and gonyautoxin-4. Our results support that dispersal of the Atama complex (Group I) from the Bering Sea to the Chukchi Sea might have occurred.	[Gu, Haifeng; Zeng, Ni; Wang, Weiguo] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Xie, Zhangxian; Wang, Dazhi] Xiamen Univ, Environm Sci Res Ctr, State Key Lab Marine Environm Sci, Xiamen 361005, Peoples R China; [Yang, Weidong] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources; Xiamen University; Jinan University	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com; dzwang@xmu.edu.cn	Wang, Da-Zhi/G-3412-2010; Wang, Shuo/AAX-7481-2021; Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171	China Program for International Polar Year; Special Research Foundation for Public Welfare Marine Program [201105022-2]; National Natural Science Foundation of China [40476053]	China Program for International Polar Year; Special Research Foundation for Public Welfare Marine Program; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank Dieter Piepenburg and three anonymous reviewers for constructive suggestions to improve the manuscript. This work was supported by the China Program for International Polar Year 2007-2011, the Special Research Foundation for Public Welfare Marine Program (201105022-2), and the National Natural Science Foundation of China (40476053).	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J	Warns, A; Hense, I; Kremp, A				Warns, Alexandra; Hense, Inga; Kremp, Anke			Modelling the life cycle of dinoflagellates: a case study with <i>Biecheleria baltica</i>	JOURNAL OF PLANKTON RESEARCH			English	Article						life cycle; encystment; excystment; seed pool; spring bloom; dinoflagellate	HARMFUL ALGAL BLOOMS; SCRIPPSIELLA-HANGOEI DINOPHYCEAE; POPULATION-DYNAMICS; RESTING STAGES; SPRING-BLOOM; CYST FORMATION; GYMNODINIUM-CATENATUM; GONYAULAX-TAMARENSIS; SEASONAL SUCCESSION; SEA	The cold-water dinoflagellate Biecheleria baltica has increasingly dominated the phytoplankton spring bloom in the Baltic Sea during the past years. Life cycle transitions between bloom forming cells and resting cysts are assumed to regulate the bloom dynamics of this species. We investigate the seasonal cycle and succession of Biecheleria balticas life cycle stages using a numerical model with four different stages, vegetative cells, gametes, resting cysts and germinating cells. The transitions among the stages are functions of environmental conditions and endogenous factors. Coupled to a water column model, the model is able to represent the seasonal cycle of Biecheleria baltica with two blooms in spring. The first bloom can be explained by germination of resting cysts in winter, the second by growth of vegetative cells. Sensitivity experiments indicate that temperature is an important factor regulating the composition of Biecheleria baltica life cycle stages; increased or decreased temperature leads to fewer growing cells and more resting cysts during spring. Our newly developed life cycle model can be used to study in more detail cyst formation, cyst distribution and consequences for biogeochemical cycling in the past and future.	[Warns, Alexandra; Hense, Inga] Univ Hamburg, Inst Hydrobiol & Fisheries Sci, D-22767 Hamburg, Germany; [Kremp, Anke] Finnish Environm Inst, Helsinki 00251, Finland	University of Hamburg; Finnish Environment Institute	Warns, A (通讯作者)，Univ Hamburg, Inst Hydrobiol & Fisheries Sci, Klimacampus, D-22767 Hamburg, Germany.	alexandra.warns@zmaw.de	Kremp, Anke/I-8139-2013		Cluster of Excellence "CliSAP" [EXC177]; University of Hamburg through the German Science Foundation (DFG)	Cluster of Excellence "CliSAP"; University of Hamburg through the German Science Foundation (DFG)(German Research Foundation (DFG))	This work has been supported by the Cluster of Excellence "CliSAP" (EXC177), University of Hamburg, funded through the German Science Foundation (DFG).	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Plankton Res.	MAR-APR	2013	35	2					379	392		10.1093/plankt/fbs095	http://dx.doi.org/10.1093/plankt/fbs095			14	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	106FY		Bronze			2025-03-11	WOS:000316129700012
J	Kern, AK; Harzhauser, M; Soliman, A; Piller, WE; Mandic, O				Kern, Andrea K.; Harzhauser, Mathias; Soliman, Ali; Piller, Werner E.; Mandic, Oleg			High-resolution analysis of upper Miocene lake deposits: Evidence for the influence of Gleissberg-band solar forcing	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						High-resolution analysis; Solar cycles; Palynomorphs; Lake Pannon; Miocene	WALLED DINOFLAGELLATE CYSTS; TREE-RING DATA; QUANTITATIVE-ANALYSIS; CLIMATE VARIABILITY; POLLEN DISTRIBUTION; SURFACE SEDIMENTS; ATMOSPHERIC C-14; CENTRAL-EUROPE; VEGETATION; SEA	A high-resolution multi-proxy analysis was conducted on a 1.5-m-long core of Tortonian age (similar to 10.5 Ma; Late Miocene) from Austria (Europe). The lake sediments were studied with a 1-cm resolution to detect all small-scale variations based on palynomorphs (pollen and dinoflagellate cysts), ostracod abundance, geochemistry (carbon and sulfur) and geophysics (magnetic susceptibility and natural gamma radiation). Based on an already established age model for a longer interval of the same core, this sequence can be limited to approx two millennia of Late Miocene time with a resolution of similar to 13.7 years per sample. The previous study documented the presence of solar forcing, which was verified within various proxies on this 1.5-m core by a combination of REDFIT spectra and Gaussian filters. Significant repetitive signals ranged in two discrete intervals corresponding roughly to 55-82 and 110-123 years, fitting well within the lower and upper Gleissberg cycle ranges. Based on these results, the environmental changes along the 2000-year late Miocene sequence are discussed. No major ecological turnovers are expected in this very short interval. Nonetheless, even within this brief time span, dinoflagellates document rapid changes between oligotrophic and eutrophic conditions, which are frequently coupled with lake stratification and dysoxic bottom waters. These phases prevented ostracods and molluscs from settling and promoted the activity of sulfur bacteria. The pollen record indicates rather stable wetland vegetation with a forested hinterland. Shifts in the pollen spectra can be mainly attributed to variations in transport mechanisms. These are represented by a few phases of fluvial input but mainly by changes in wind intensity and probably also wind direction. Such influence is most likely caused by solar cycles, leading to a change in source area for the input into the lake. Furthermore, these solar-induced variations seem to be modulated by longer solar cycles. The filtered data display comparable patterns and modulations, which seem to be forced by the 1000-year and 1500-year cycles. The 1000-year cycle modulated especially the lake surface proxies, whereas the 1500-year cycle is mainly reflected in hinterland proxies, indicating strong influence on transport mechanisms. (c) 2012 Elsevier B.V. All rights reserved.	[Kern, Andrea K.; Harzhauser, Mathias; Mandic, Oleg] Nat Hist Museum Vienna, Geol Paleontol Dept, A-1010 Vienna, Austria; [Kern, Andrea K.] State Museum Nat Hist Stuttgart, Paleontol Dept, D-70191 Stuttgart, Germany; [Soliman, Ali; Piller, Werner E.] Graz Univ, Inst Earth Sci, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Dept Geol, Fac Sci, Tanta 31527, Egypt	University of Graz; Egyptian Knowledge Bank (EKB); Tanta University	Kern, AK (通讯作者)，State Museum Nat Hist Stuttgart, Paleontol Dept, Rosenstein 1, D-70191 Stuttgart, Germany.	andrea.kern@nhm-wien.ac.at	Soliman, Ali/R-1583-2018; Kern, Andrea K./V-5078-2017	Soliman, Ali/0000-0001-7366-4607; Harzhauser, Mathias/0000-0002-4471-6655; Kern, Andrea K./0000-0002-9343-0696; Mandic, Oleg/0000-0003-1955-7514; Piller, Werner E./0000-0003-2808-4720	FWF grant [P21414-B16]; Austrian Science Fund (FWF) [P21414] Funding Source: Austrian Science Fund (FWF)	FWF grant(Austrian Science Fund (FWF)); Austrian Science Fund (FWF)(Austrian Science Fund (FWF))	This study was supported by the FWF grant P21414-B16. We thank Dipl.-Ing. Hermann Sammer and the Wienerberger AG for providing access to the clay pit Hennersdorf and for their friendly support during field work. Furthermore, we want to thank Anton Englert, Anton Furst, Franz Topka, Andy Leggat and Lisa Schmidinger for core preparation, sample processing and counting of the ostracods. We thank Martin Gross for background information concerning geophysics and geochemistry. This paper contributes to the NECLIME network.	[Anonymous], 1650A US GEOL SURV; Averyanov Leonid V., 2009, Taiwania, V54, P191; Babinszki E, 2007, PALAEOGEOGR PALAEOCL, V252, P626, DOI 10.1016/j.palaeo.2007.06.001; Bard E, 2006, EARTH PLANET SC LETT, V248, P1, DOI 10.1016/j.epsl.2006.06.016; Beer J, 2000, QUATERNARY SCI REV, V19, P403, DOI 10.1016/S0277-3791(99)00072-4; BEER J, 1990, NATURE, V347, P164, DOI 10.1038/347164a0; BERNER RA, 1984, GEOCHIM COSMOCHIM AC, V48, P605, DOI 10.1016/0016-7037(84)90089-9; Blum P., 1997, Proc. 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Paleoclimatol. Paleoecol.	JAN 15	2013	370						167	183		10.1016/j.palaeo.2012.12.005	http://dx.doi.org/10.1016/j.palaeo.2012.12.005			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	101GB	23407808	Green Published, hybrid			2025-03-11	WOS:000315762100014
J	Van Nieuwenhove, N; Bauch, HA; Andruleit, H				Van Nieuwenhove, Nicolas; Bauch, Henning A.; Andruleit, Harald			Multiproxy fossil comparison reveals contrasting surface ocean conditions in the western Iceland Sea for the last two interglacials	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Holocene; Last Interglacial; Planktic microfossils; East Greenland Current; Irminger Current; Nordic seas	NORWEGIAN-GREENLAND SEA; NORDIC SEAS; NORTH-ATLANTIC; DINOFLAGELLATE CYSTS; HIGH-RESOLUTION; ICE-SHEET; HOLOCENE PALEOCEANOGRAPHY; DINOCYST ASSEMBLAGES; PALEO-OCEANOGRAPHY; WATER CONDITIONS	Dinoflagellate cyst (dinocyst), coccolith and planktic foraminiferal assemblages from a core in the western Iceland Sea were used to reconstruct and compare the surface ocean developments of the Holocene and the Last Interglacial (Marine Isotopic Stage or MIS 5e). While increasing subpolar planktic foraminifers from similar to 10 ka indicate subsurface warming peaking around 7.5 ka, the dinocyst data suggest that the uppermost ocean remained dominated by cold waters until similar to 6.5 ka. A reduced advection of cold polar waters through the East Greenland/East Icelandic Current thereafter entailed warmest and most saline Holocene conditions between 6.5 and 5 ka, in turn followed by a general cooling trend. By contrast both planktic foraminifers and dinocysts show an increased presence of Atlantic (-type) waters from similar to 122 ka onward resulting in a MIS 5e thermal optimum around 120.5 ka. Nonetheless, occasional freshwater input from melting drift ice created stratified but also seasonally variable conditions during this first half of MIS 5e. This stratification signature disappeared at similar to 120 ka when a marked repositioning of the oceanographic fronts occurred. Slightly colder conditions are indicated by both phyto- and zooplankton from there on until the end of MIS 5e around similar to 117 ka. A late MIS 5e cooling at the Iceland Plateau is opposite to a late MIS 5e optimum observed in the eastern Nordic seas. This regional difference is likely explained by various feedback mechanisms following the major reorganisation of the oceanic fronts at similar to 120 ka. The Holocene and MIS 5e interglacial variability is not reflected in the (quasi-monospecific) coccolith assemblages and illustrates the low sensitivity of living coccolithophore communities to subtle temperature changes in the low-temperature regions of the Nordic seas. Overall, quite different surface water properties appear to have characterised both interglacial intervals, with a higher share of warm, Atlantic elements in the planktic communities during MIS 5e. This suggests a higher contribution of Atlantic waters in the southwestern Nordic seas probably due to a more northward expansion of the Irminger Current under weakened polar East Greenland/East Icelandic currents. Such a reduced influence of polar waters in the southwestern Nordic seas may thus explain other evidence for relatively warm conditions in MIS 5e all around southern Greenland. (c) 2012 Elsevier B.V. All rights reserved.	[Van Nieuwenhove, Nicolas; Bauch, Henning A.] GEOMAR Helmholtz Ctr Ocean Res Kiel, D-24148 Kiel, Germany; [Van Nieuwenhove, Nicolas] Univ Quebec, Geotop, Montreal, PQ H2X 3Y7, Canada; [Bauch, Henning A.] Mainz Acad Sci Humanities & Literature, D-55131 Mainz, Germany; [Andruleit, Harald] Bundesanstalt Geowissensch & Rohstoffe, D-30655 Hannover, Germany	Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; University of Quebec; University of Quebec Montreal	Van Nieuwenhove, N (通讯作者)，GEOMAR Helmholtz Ctr Ocean Res Kiel, Wischhofstr 1-3, D-24148 Kiel, Germany.	nvannieuwenhove.geotop@gmail.com	Van Nieuwenhove, Nicolas/IAQ-1532-2023	Van Nieuwenhove, Nicolas/0000-0001-6369-2751	Deutsche Forschungsgemeinschaft [NI1248/12]; European Union's Seventh Framework programme (FP7) [243908]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); European Union's Seventh Framework programme (FP7)(European Union (EU))	We thank the teams from the Leibniz Laboratory for Radiometric Dating and Stable Isotope Research (Kiel University) and the Stable Isotope Laboratory at GEOMAR (Kiel) for their support in the isotope analyses. 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Paleoclimatol. Paleoecol.	JAN 15	2013	370						247	259		10.1016/j.palaeo.2012.12.018	http://dx.doi.org/10.1016/j.palaeo.2012.12.018			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	101GB					2025-03-11	WOS:000315762100020
J	Brown, L; Bresnan, E; Summerbell, K; O'Neill, FG				Brown, Lyndsay; Bresnan, Eileen; Summerbell, Keith; O'Neill, Finbarr Gerard			The influence of demersal trawl fishing gears on the resuspension of dinoflagellate cysts	MARINE POLLUTION BULLETIN			English	Article						Sediment; Resuspension; Dinoflagellate cyst; Towed fishing gear	ALEXANDRIUM-TAMARENSE DINOPHYCEAE; RECENT MARINE-SEDIMENTS; SWEDISH WEST-COAST; RESTING CYSTS; BALTIC SEA; ENVIRONMENTAL-FACTORS; SCRIPPSIELLA-HANGOEI; SCOTTISH WATERS; SHORT-TERM; GERMINATION	To investigate the influence of towed demersal fishing gears on dinoflagellate cyst resuspension, towing trials with four gear components were carried out at three sites of differing sediment type in the Moray Firth, Scotland. Samples of sediment plumes were collected using plankton nets mounted on a towed sledge. Diversity of resuspended dinoflagellate cysts was similar at all sites and included Protoperidinium and Gonyaulax spp., Proroceratium reticulatum and unidentified 'round brown' cysts. Cyst concentrations per gram of resuspended sediment varied by gear component and sediment particle size distribution. Gear components with lower hydrodynamic drag generated wakes with smaller shear stresses, mobilising fewer larger sand particles, giving larger concentrations of cysts. Muddy sediments contained higher cyst concentrations which declined with increasing grain size. This study has shown that fishing gear and sediment type can influence the redistribution of dinoflagellate cysts and highlights the importance this may have in relation to dinoflagellate blooms. Crown Copyright (C) 2012 Published by Elsevier Ltd. All rights reserved.	[Brown, Lyndsay; Bresnan, Eileen; Summerbell, Keith; O'Neill, Finbarr Gerard] Marine Lab Aberdeen, Marine Scotland Sci, Aberdeen AB11 9DB, Scotland	Marine Scotland Science (MSS)	Brown, L (通讯作者)，Marine Lab Aberdeen, Marine Scotland Sci, POB 101,375 Victoria Rd, Aberdeen AB11 9DB, Scotland.	Lyndsay.Brown@scotland.gsi.gov.uk; Eileen.Bresnan@scotland.gsi.gov.uk; Keith.Summerbell@scotland.gsi.gov.uk; b.oneill@marlab.ac.uk	O'Neill, Barrry/AAL-8602-2021	O'Neill, Finbarr/0000-0002-2797-4548				Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; ANDERSON DM, 2003, MANUAL HARMFUL MARIN, P165; Blanco EP, 2009, HARMFUL ALGAE, V8, P518, DOI 10.1016/j.hal.2008.10.008; Boyd SE, 2005, ICES J MAR SCI, V62, P145, DOI 10.1016/j.icesjms.2004.11.014; Bresnan E, 2009, J SEA RES, V61, P17, DOI 10.1016/j.seares.2008.05.007; Brown L, 2010, EUR J PHYCOL, V45, P375, DOI 10.1080/09670262.2010.495164; CANNON JA, 1993, DEV MAR BIO, V3, P103; Cembella, 2003, MANUAL HARMFUL MARIN, P511; Collins C, 2009, J PHYCOL, V45, P692, DOI 10.1111/j.1529-8817.2009.00678.x; Dale B, 2002, QUATERNARY ENVIRONMENTAL MICROPALAEONTOLOGY, P207; Dale B., 1983, P69; de Madron XD, 2005, CONT SHELF RES, V25, P2387, DOI 10.1016/j.csr.2005.08.002; Desprez M, 2000, ICES J MAR SCI, V57, P1428, DOI 10.1006/jmsc.2000.0926; Dolmer P, 2002, J SHELLFISH RES, V21, P529; Dolmer P, 2001, HYDROBIOLOGIA, V465, P115, DOI 10.1023/A:1014549026157; Edvardsen B, 2006, ECOL STU AN, V189, P67, DOI 10.1007/978-3-540-32210-8_6; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Genovesi B, 2009, J PLANKTON RES, V31, P1209, DOI 10.1093/plankt/fbp066; Giannakourou A, 2005, CONT SHELF RES, V25, P2585, DOI 10.1016/j.csr.2005.08.003; Gilkinson KD, 2005, ICES J MAR SCI, V62, P925, DOI 10.1016/j.icesjms.2005.03.009; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; Hall SJ, 1999, EFFECTS FISHING MARI, P274; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Jennings S, 1998, ADV MAR BIOL, V34, P201, DOI 10.1016/S0065-2881(08)60212-6; Joyce LB, 2004, BOT MAR, V47, P173, DOI 10.1515/BOT.2004.018; Kaiser MJ, 2002, FISH FISH, V3, P114, DOI 10.1046/j.1467-2979.2002.00079.x; Kirn SL, 2005, DEEP-SEA RES PT II, V52, P2543, DOI 10.1016/j.dsr2.2005.06.009; Kremp A, 2000, J PLANKTON RES, V22, P2155, DOI 10.1093/plankt/22.11.2155; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; Lewis Jane, 1995, P175; Lokkeborg S., 2005, T472 UN FAO; Matrai P, 2005, DEEP-SEA RES PT II, V52, P2560, DOI 10.1016/j.dsr2.2005.06.013; Matsuoka K., 2000, Technical guide for modern dinoflagellate cyst study, P1; Matsuzaki K, 2003, MATER SCI FORUM, V426-4, P563, DOI 10.4028/www.scientific.net/MSF.426-432.563; McQuoid MR, 2002, J PHYCOL, V38, P881, DOI 10.1046/j.1529-8817.2002.01169.x; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; O'Neill FG, 2011, MAR POLLUT BULL, V62, P1088, DOI 10.1016/j.marpolbul.2011.01.038; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Round FE, 1990, The Diatoms: Biology and Morphology of the Genera, DOI DOI 10.1017/S0025315400059245; Sardá R, 2000, ICES J MAR SCI, V57, P1446, DOI 10.1006/jmsc.2000.0922; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x	46	10	12	2	28	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0025-326X	1879-3363		MAR POLLUT BULL	Mar. Pollut. Bull.	JAN 15	2013	66	1-2					17	24		10.1016/j.marpolbul.2012.11.017	http://dx.doi.org/10.1016/j.marpolbul.2012.11.017			8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	098IT	23231914				2025-03-11	WOS:000315543500015
J	D'Silva, MS; Anil, AC; Sawant, SS				D'Silva, Maria Shamina; Anil, Arga Chandrashekar; Sawant, Subhash Shivram			Dinoflagellate cyst assemblages in recent sediments of Visakhapatnam harbour, east coast of India: Influence of environmental characteristics	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cyst; Sediment; Environmental characteristics; Harmful species; Protoceratium reticulatum; Visakhapatnam harbour	RECENT MARINE-SEDIMENTS; PROTOCERATIUM-RETICULATUM; SURFACE SEDIMENTS; TOKYO-BAY; SPATIAL-DISTRIBUTION; WATER-QUALITY; YOKOHAMA-PORT; WEST-COAST; POLLUTION; EUTROPHICATION	The distribution and abundance of dinoflagellate cysts in recent sediments from Visakhapatnam harbour, east coast of India was investigated and compared with sediment characteristics and physico-chemical variables of the overlying water column. The cyst abundance varied from 11 to 1218 cysts g(-1) dry sediment. Changes in the cyst assemblages from phototrophic to heterotrophic forms were observed from inner to outer harbour stations, and related to changes in environmental characteristics. Enhanced cyst production of potentially harmful dinoflagellate Protoceratium reticulatum was recorded in the inner harbour stations with higher nutrient concentrations. Protoperidinium cysts were the most diversified group, and were dominant in the outer harbour stations having improved water conditions and circulation. This study points out the potential use of dinoflagellate cyst populations in providing information on environmental conditions. (C) 2012 Elsevier Ltd. All rights reserved.	[D'Silva, Maria Shamina; Anil, Arga Chandrashekar; Sawant, Subhash Shivram] Natl Inst Oceanog, CSIR, Panaji 403004, Goa, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO)	Anil, AC (通讯作者)，Natl Inst Oceanog, CSIR, Panaji 403004, Goa, India.	acanil@nio.org			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)	The authors are grateful to the Director of CSIR-National Institute of Oceanography, Goa for his support and encouragement. This work was carried out as part of Ballast Water Management Programme, India, funded by Directorate General of Shipping, Government of India. We thank Mr. K. Venkat, Mr. Prakash Babu and Mr. V. Khedekar for their help at various stages of research work. We also thank our members of the project team for their help and suggestions. M.S.D. acknowledges the Council of Scientific and Industrial Research (CSIR) for the award of Senior Research Fellowship (SRF). This is an NIO contribution (No. 5276).	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JAN 15	2013	66	1-2					59	72		10.1016/j.marpolbul.2012.11.012	http://dx.doi.org/10.1016/j.marpolbul.2012.11.012			14	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	098IT	23228518				2025-03-11	WOS:000315543500020
J	Lacasse, O; Rochon, A; Roy, S				Lacasse, Olivia; Rochon, Andre; Roy, Suzanne			High cyst concentrations of the potentially toxic dinoflagellate <i>Alexandrium tamarense species complex in</i> Bedford Basin, Halifax, Nova Scotia, Canada	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cysts; Alexandrium tamarense species complex; Nova Scotia, Canada; Harmful algae; Ballast water; Ballast sediment; Invasive species	SHIPS BALLAST WATER; GONYAULAX-EXCAVATA; GENUS ALEXANDRIUM; TRANSPORT; SEDIMENTS; BIOGEOGRAPHY; DINOPHYCEAE; MINUTUM; DIATOMS; NORWAY	We report a large cyst bed of the potentially toxic and bloom-forming dinoflagellate Alexandrium tamarense species complex in bottom sediments from the port of Halifax, Nova Scotia, Canada. The average cyst concentrations of that species ranged from 4033 +/- 2647 to 220872 +/- 148 086 cysts g(-1) of dry sediments and the highest concentrations were found near ship terminals in Bedford Basin. Although this species is endemic to this region, our work strongly suggests that some of the cysts of A. tamarense species complex found in the port of Halifax were introduced through discharged ballast water and sediments. (C) 2012 Elsevier Ltd. All rights reserved.	[Lacasse, Olivia; Rochon, Andre; Roy, Suzanne] Univ Quebec, Inst Sci Mer, Rimouski, PQ G5L 3A1, Canada	University of Quebec	Rochon, A (通讯作者)，Univ Quebec, Inst Sci Mer, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	andre_rochon@uqar.ca			Natural Science and Engineering Research Council of Canada (NSERC) through the Canadian Aquatic Invasive Species Network (CAISN)	Natural Science and Engineering Research Council of Canada (NSERC) through the Canadian Aquatic Invasive Species Network (CAISN)	Financial support for this study came from the Natural Science and Engineering Research Council of Canada (NSERC) through the Canadian Aquatic Invasive Species Network (CAISN). We thank Dr H. MacIsaac, leader of the CAISN program, and Dr. Chris McKindsey, leader of the sampling team of this project. This study is also a contribution to the research programs of ISMER and Quebec-Ocean.	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Pollut. Bull.	JAN 15	2013	66	1-2					230	233		10.1016/j.marpolbul.2012.10.016	http://dx.doi.org/10.1016/j.marpolbul.2012.10.016			4	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	098IT	23154137				2025-03-11	WOS:000315543500040
J	Zinssmeister, C; Keupp, H; Tischendorf, G; Kaulbars, F; Gottschling, M				Zinssmeister, Carmen; Keupp, Helmut; Tischendorf, Gilbert; Kaulbars, Freya; Gottschling, Marc			Ultrastructure of Calcareous Dinophytes (<i>Thoracosphaeraceae</i>, <i>Peridiniales</i>) with a Focus on Vacuolar Crystal-Like Particles	PLOS ONE			English	Article							FRESH-WATER DINOFLAGELLATE; RDNA-BASED PHYLOGENY; FLAGELLAR APPARATUS; MARINE DINOFLAGELLATE; CYST FORMATION; FINE-STRUCTURE; SCRIPPSIELLA; GEN.; BIOMINERALIZATION; NOV	Biomineralization in calcareous dinophytes (Thoracosphaeracaea, Peridiniales) takes place in coccoid cells and is presently poorly understood. Vacuolar crystal-like particles as well as collection sites within the prospective calcareous shell may play a crucial role during this process at the ultrastructural level. Using transmission electron microscopy, we investigated the ultrastructure of coccoid cells at an early developmental stage in fourteen calcareous dinophyte strains (corresponding to at least ten species of Calciodinellum, Calcigonellum, Leonella, Pernambugia, Scrippsiella, and Thoracosphaera). The shell of the coccoid cells consisted either of one (Leonella, Thoracosphaera) or two matrices (Scrippsiella and its relatives) of unknown element composition, whereas calcite is deposited in the only or the outer layer, respectively. We observed crystal-like particles in cytoplasmic vacuoles in cells of nine of the strains investigated and assume that they are widespread among calcareous dinophytes. However, similar structures are also found outside the Thoracosphaeraceae, and we postulate an evolutionarily old physiological pathway (possibly involved in detoxification) that later was specialized for calcification. We aim to contribute to a deeper knowledge of the biomineralization process in calcareous dinophytes.	[Zinssmeister, Carmen; Gottschling, Marc] Univ Munich, Dept Biol Syst Bot & Mykol, Munich, Germany; [Zinssmeister, Carmen; Keupp, Helmut] Free Univ Berlin, Fachrichtung Palaontol, Fachbereich Geol Wissensch, Berlin, Germany; [Tischendorf, Gilbert; Kaulbars, Freya] Free Univ Berlin, Fachbereich Biol, Inst Biol Mikrobiol, Berlin, Germany	University of Munich; Free University of Berlin; Free University of Berlin	Gottschling, M (通讯作者)，Univ Munich, Dept Biol Syst Bot & Mykol, Munich, Germany.	gottschling@bio.lmu.de	Gottschling, Marc/K-2186-2014		Deutsche Forschungsgemeinschaft [KE 322/30, KE 322/36, WI 725/18, WI 725/25]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	Financial support was provided by the Deutsche Forschungsgemeinschaft (grants KE 322/30, KE 322/36, WI 725/18 and WI 725/25), and the Munchener Universitatsgesellschaft for equipment support. 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	King, C; Iakovleva, A; Steurbaut, E; Heilmann-Clausen, C; Ward, D				King, Chris; Iakovleva, Alina; Steurbaut, Etienne; Heilmann-Clausen, Claus; Ward, David			The Aktulagay section, west Kazakhstan: a key site for northern mid-latitude Early Eocene stratigraphy	STRATIGRAPHY			English	Article							HOLOPLANKTONIC MOLLUSCA GASTROPODA; PALEOCENE; BIOSTRATIGRAPHY; TETHYS; OCEAN; BASIN; PART; NANNOPLANKTON; SYSTEMATICS; TRANSITION	A section at Aktulagay (west Kazakhstan), in the Peri-Tethys realm, exposes mid-neritic to upper bathyal Ypresian marls, clays and silts. These range from Zone NP10 to early Zone NP14, with abundant and diverse microfossil assemblages. Multidisciplinary analysis has identified dinoflagellate cyst, calcareous nannofossil, planktonic and benthic foraminiferid and pteropod zones and events. Calibration of a key interval in the evolution of the shark Otodus has been possible for the first time. Episodic low-oxygen facies, including sapropelic clays widely distributed in Peri-Tethys, are represented here and can be placed within a detailed biostratigraphic framework. The current lithostratigraphic terminology is modified, with the introduction of the Aktulagay Formation. Paleoenvironmental aspects are discussed; five depositional sequences are tentatively identified. This section can be correlated in detail with the succession in the North Sea Basin, with implications for paleogeographic reconstructions. High-resolution biostratigraphic calibration between disparate fossil groups makes this a key reference section for northern mid-latitude Ypresian biostratigraphy.	[Iakovleva, Alina] Russian Acad Sci, Inst Geol, Moscow 119017, Russia; [Steurbaut, Etienne] Royal Belgian Inst Nat Sci, B-1000 Brussels, Belgium; [Steurbaut, Etienne] Katholieke Univ Leuven, Louvain, Belgium; [Heilmann-Clausen, Claus] Aarhus Univ, Dept Geosci, DK-8000 Aarhus C, Denmark; [Ward, David] Nat Hist Museum, Dept Earth Sci, London SW7 5BD, England	Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Royal Belgian Institute of Natural Sciences; KU Leuven; Aarhus University; Natural History Museum London	King, C (通讯作者)，16A Pk Rd, Bridport DT6 5DA, England.	chrking@globalnet.co.uk; alina.iakovleva@gmail.com; etienne.steurbaut@naturalsciences.be; claus.heilmann@geo.au.dk; david@fossil.ws	Heilmann-Clausen, Claus/A-4848-2012; IAKOVLEVA, ALINA/ABH-9243-2020		Danish Natural Science Research Council [21-04-0298]	Danish Natural Science Research Council(Danish Natural Science Research Council)	Fieldwork was carried out with the authorisation of the Institute of Geology, Aqtobe (Kazakhstan), which also provided logistical support. Much help in the field and in logistics was provided by Tigran Akopov (formerly Institute of Geology, Aqtobe), Tatiana Malyshkina (Institute of Geology, Ekaterinburg, Russia) and Jason Ali (University of Hong Kong, China). Jason Ali funded a third expedition, providing the opportunity to acquire additional critical data. Our driver Viktor Savin (Navoiy, Uzbekistan) transported CK, DJW and colleagues without complaint over remote and inhospitable terrain with rudimentary maps. Arie Janssen (Netherlands Centre for Biodiversity, Palaeontology Department, Leiden) identified and provided comments on the pteropods. Kirsten Rosendal (Aarhus University, Denmark) is thanked for processing the palynological samples. A post-doctoral post for Alina Iakovleva at the Department of Geoscience, Aarhus University (Denmark) was financially supported by the Danish Natural Science Research Council (grant no. 21-04-0298). 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S	Firth, JV; Eldrett, JS; Harding, IC; Coxall, HK; Wade, BS		Jovane, L; HerreroBervera, E; Hinnov, LA; Housen, B		Firth, J. V.; Eldrett, J. S.; Harding, I. C.; Coxall, H. K.; Wade, B. S.			Integrated biomagnetochronology for the Palaeogene of ODP Hole 647A: implications for correlating palaeoceanographic events from high to low latitudes	MAGNETIC METHODS AND THE TIMING OF GEOLOGICAL PROCESSES	Geological Society Special Publication		English	Article; Book Chapter							DRILLING-PROJECT SITE-558; CENOZOIC ARCTIC-OCEAN; MIDDLE EOCENE; NORTH-ATLANTIC; NANNOFOSSIL BIOCHRONOLOGY; CALCAREOUS NANNOFOSSILS; CALCITE COMPENSATION; BIPOLAR GLACIATION; OLIGOCENE; SEA	Lower Eocene to Oligocene microfossil-rich hemipelagic sediments in ODP Hole 647A, southern Labrador Sea, provide a strategic section for resolving the early history of high North Atlantic climates and ocean circulation, and for correlating with carbonate-poor lower Cenozoic sediments in the Arctic and Nordic seas. Our new, integrated palaeomagneto-and multigroup biostratigraphy (63 dinoflagellate cyst, calcareous nannofossil, planktonic foraminifer and diatom datums) significantly improves Site 647 chronostratigraphy and provides a framework for future studies. This new age model, coupled with provisional delta O-18 analyses, provides greater confidence in the location of significant ocean-climate events at this site, including the Eocene-Oligocene transition and the Middle Eocene Climatic Optimum. Early Eocene hyperthermals may also be present near the base of the section. Palaeomagnetic age control is significantly improved in the Eocene, but not in the Oligocene. Revised estimates of sedimentation and biogenic flux indicate changes in supply and preservation that may be climatically controlled. A Lower to Middle Eocene hiatus is more precisely constrained, with a c. 4 million year duration. Age and depth errors quantify the age uncertainties throughout the section. Our revised age model will play an important role in stratigraphic correlation between very high latitude and lower latitude sites.	[Firth, J. V.] Integrated Ocean Drilling Program, College Stn, TX 77845 USA; [Eldrett, J. S.] Shell Explorat & Prod Inc, Houston, TX 77001 USA; [Harding, I. C.] Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England; [Coxall, H. K.] Cardiff Univ, Sch Earth & Ocean Sci, Cardiff CF10 3YE, S Glam, Wales; [Wade, B. 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C., 2004, P OC DRILL PROGR SCI, V208; Zachos JC, 1996, PALEOCEANOGRAPHY, V11, P251, DOI 10.1029/96PA00571	103	12	14	0	2	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		978-1-86239-354-7	GEOL SOC SPEC PUBL	Geol. Soc. Spec. Publ.		2013	373						29	78		10.1144/SP373.9	http://dx.doi.org/10.1144/SP373.9			50	Geochemistry & Geophysics; Geology	Book Citation Index– Science (BKCI-S)	Geochemistry & Geophysics; Geology	BB3MA					2025-03-11	WOS:000342848300003
B	Head, MJ; Harland, R		Lewis, JM; Marret, F; Bradley, LR		Head, M. J.; Harland, R.			A History of the International Conferences on Modern and Fossil Dinoflagellates, 1978-2011	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							ESTUARINE; CYSTS	The international conferences on modern and fossil dinoflagellates, held every 3-5 years, are an essential forum for all researchers of dinoflagellates. They bring together all aspects of this important group of protists, whether living or preserved as fossils. Dinoflagellates are an important component of the plankton, both as autotrophs and heterotrophs, but also include representatives that inhabit the cells of other organisms (including other dinoflagellates) as endosymbionts or parasites. The conferences were initiated in 1978 as a Penrose Conference of the Geological Society of America and have continued ever since. The latest conference, Dino 9, continues the tradition of bringing phycologists working as biologists, geneticists, ecologists and public health scientists together with palynologists working within the disciplines of earth science, geography and biology. The paramount impact of this series of conferences is the interdisciplinary cross-fertilization of ideas between these two otherwise disparate groups, and the spreading of their acquired specialist knowledge from one to the other. This series of conferences is set to extend into the future and to continue its important role of integrating and furthering the study of dinoflagellates and their cysts.	[Head, M. J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Harland, R.] Univ Gothenburg, Dept Earth Sci, S-40530 Gothenburg, Sweden	Brock University; University of Gothenburg	Head, MJ (通讯作者)，Brock Univ, Dept Earth Sci, 500 Glenridge Ave, St Catharines, ON L2S 3A1, Canada.	mjhead@brocku.ca						Anderson DM, 2013, MICROPALEAEONTOLOGIC, P141; [Anonymous], 2004, Personal interview; BUJAK J.P., 1980, DINOFLAGELLATE CYSTS, V24, P36; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; Burkholder JM, 2012, HARMFUL ALGAE, V14, P196, DOI 10.1016/j.hal.2011.10.022; DALE B, 1978, Palynology, V2, P187; De Schepper S, 2009, PALEOCEANOGRAPHY, V24, DOI 10.1029/2008PA001725; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Dodge J.D., 1985, ATLAS DINOFLAGELLATE; DODGE J. D., 1986, BRIT MICROPALAEONTOL, V28, P20; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; EATON G L, 1980, Palaeontology (Oxford), V23, P667; Evitt W. 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J., 1989, CANADIAN ASS PALYNOL, V12, p[15, 16]; NUNEZ-BETELU K., 1998, AM ASS STRATIGRAPHIC, V31, P5; Place AR, 2012, HARMFUL ALGAE, V14, P179, DOI 10.1016/j.hal.2011.10.021; POWELL A. J., 1986, BRIT MICROPALAEON TO, V28, P20; RADI T., 2009, REV MICROPALEONTOL, V52, P265; SANGIORGI F., 2008, STUIFMAIL PALAEOBOTA, V28, P34; SARJEANT W. A. S., 1998, NORGES TEKNISK NATUR, V1998-2, P1; SARJEANT W. A. S., 1982, AASP NEWSL, V15, P5; Smelror M, 1999, GRANA, V38, P65; SMELROR M., 1998, NORGES TEKNISKNATURV, V1998-1, P1; STEIDINGER K., 2008, 8 INT C MOD FOSS DIN, P56; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WOOD G., 1998, AM ASSOCIATION STRAT, V31, P4; WRENN J. H., 1989, AM ASS STRATIGRAPHIC, V23, P20; ZONNEVELD C. A. F., 1994, REV PALAEOBOT PALYNO, V84, p[i, 1]	61	1	1	0	3	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							1	21						21	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500001
B	Riding, JB		Lewis, JM; Marret, F; Bradley, LR		Riding, J. B.			Dino 9: Lifetime Achievement Award 2011	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Biographical-Item; Book Chapter								The Dino 9 Lifetime Achievement Award was bestowed upon Dr Robert A. Fensome of the Geological Survey of Canada in recognition of his outstanding research record in the field of dinoflagellate cysts. This is specifically his work on the classification, biostratigraphy, evolution, phylogeny and taxonomy of dinofllagellate cysts, his work on the geology of Canada, public outreach and as an organizer of conferences.	British Geol Survey, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Keyworth NG12 5GG, Notts, England.								0	0	0	0	0	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							25	30						6	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500003
B	Harland, R; Nordberg, K; Robijn, A		Lewis, JM; Marret, F; Bradley, LR		Harland, R.; Nordberg, K.; Robijn, A.			Latest Holocene dinoflagellate cyst records from the west coast of Sweden and their impact on the interpretation of environmental change	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							GULLMAR FJORD; KOLJO-FJORD; SURFACE SEDIMENTS; PRESERVATION	The fjords along the west coast of Sweden have attracted attention for a number of unfortunate reasons, including the development of enhanced primary production and the presence of oxygen deficiency in bottom waters with its consequential benthic mortality. These difficulties have impacted local fisheries, mariculture and leisure activities along the coast. In the early 1990s a research programme, using the fjord sediments as an archive, was initiated to understand the various environmental processes at play. Included were studies on the foraminifera to access bottom water environments, and dinoflagellate cyst analysis for the interpretation of surface water conditions. In addition the sedimentary history within several of the fjords was constructed using Pb-210 dating and a constant rate of supply model together with heavy metal analysis. Several fjords were analysed for their dinoflagellate cyst record including Koljofjord, Gullmarsfjord and Havstensfjord. This contribution adds to the published information with the inclusion of Sannasfjord and Dyneldlen. All the dinoflagellate cyst records are consistent with modern cyst floras of the area, and include Lingulodinium polyedrum, Protoceratium reticulatum, Spiniferites bentorii and Pentapharsodinium dalei. It is however apparent that the temporal cyst record from Gullmarsfjord differs from the other fjords and is reacting differently to environmental change. Ultra-high-resolution dinoflagellate cyst analysis has a particular impact on the interpretation of environmental change within the marine realm.	[Harland, R.; Nordberg, K.; Robijn, A.] 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						APLER A., 2007, STUDY HEAVY METAL PO, VB479, P1; Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; 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, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; 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; Gustafsson M, 2002, HOLOCENE, V12, P325, DOI 10.1191/0959683602hl547rp; 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, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; Harland R, 2010, GEOL SOC SPEC PUBL, V344, P75, DOI 10.1144/SP344.7; 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; ROBIJN A., 2010, USING HEAVY ME UNPUB, P1; ROSENBERG R, 1990, MAR POLLUT BULL, V21, P335, DOI 10.1016/0025-326X(90)90794-9; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zonneveld KAF, 2007, MAR GEOL, V237, P109, DOI 10.1016/j.margeo.2006.10.023	21	3	3	0	2	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							43	54						12	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500005
B	Bonnet, S; De Vernal, A; Henry, M		Lewis, JM; Marret, F; Bradley, LR		Bonnet, S.; De Vernal, A.; Henry, M.			Dinoflagellate cyst assemblage distributions as tracers of Pacific v. Atlantic water masses in the Northern Hemisphere	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							SEA-SURFACE CONDITIONS; HYDROGRAPHIC CONDITIONS; SOUTHERN-OCEAN; HIGH-LATITUDES; BARENTS SEA; SEDIMENTS; PRODUCTIVITY; RECONSTRUCTION; COAST; QUATERNARY	The distribution of dinoflagellate cyst assemblages is currently used to reconstruct sea-surface conditions. Assemblages provide information about sea-surface temperature and salinity, sea-ice cover and productivity. However, the endemic or regional character of several species, in addition to morphological variability, questions the ecological affinities of taxa and assemblages from one region to another. So far, the North Pacific Ocean represents one of the least-documented areas relative to the North Atlantic and Arctic oceans. In this paper, we incorporate results from recent studies realized in this region and we discuss some species (Impagidinium japoni cum, Impagidinium velorum, a new Pyxidinopsis reticulata morphotype, Dalella chathamensis and some Echinidinium species) that seem to be endemic to the Pacific Ocean. Likewise, the taxon that we identify as Selenopemphix nephroides in the North Atlantic Ocean presents a few morphological dissimilarities in the North Pacific. Do we have to consider it as another morphotype or species? Do we need to take into account its variability? In order to answer these questions and avoid inconsistencies in reference databases and consequently in palaeoceanographical interpretations, it is of primary importance to standardize the identification of ambiguous species and to carry out more taxonomic/phylogenetic studies on dinoflagellate-dinocyst relationships.	[Bonnet, S.; De Vernal, A.; Henry, M.] Univ Quebec, Ctr Rech Geochim Isotop & Geochronol Geotop, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Bonnet, S (通讯作者)，Univ Quebec, Ctr Rech Geochim Isotop & Geochronol Geotop, Montreal, PQ H3C 3P8, Canada.	sbrasta1@gmail.com	de Vernal, Anne/D-5602-2013					Bonnet S, 2012, MAR MICROPALEONTOL, V84-85, P87, DOI 10.1016/j.marmicro.2011.11.006; Bonnet S, 2010, MAR MICROPALEONTOL, V74, P59, DOI 10.1016/j.marmicro.2009.12.001; Crouch EM, 2010, MAR GEOL, V270, P235, DOI 10.1016/j.margeo.2009.11.004; 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; Esper O, 2002, MAR MICROPALEONTOL, V46, P177, DOI 10.1016/S0377-8398(02)00041-5; Esper O, 2007, MAR MICROPALEONTOL, V65, P185, DOI 10.1016/j.marmicro.2007.07.002; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Grosfjeld K, 2009, NORW J GEOL, V89, P121; Guiot J, 2011, QUATERNARY SCI REV, V30, P1965, DOI 10.1016/j.quascirev.2011.04.022; HARLAND R, 1986, Palynology, V10, P25; HARLAND R, 1988, NEW PHYTOL, V108, P111, DOI 10.1111/j.1469-8137.1988.tb00210.x; Krepakevich A, 2010, CONT SHELF RES, V30, P1924, DOI 10.1016/j.csr.2010.09.002; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; Limoges A, 2010, MAR MICROPALEONTOL, V76, P104, DOI 10.1016/j.marmicro.2010.06.003; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matsuoka K, 2009, REV PALAEOBOT PALYNO, V154, P79, DOI 10.1016/j.revpalbo.2008.12.013; McMinn Andrew, 1994, Palynology, V18, P41; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; Novichkova EA, 2007, OCEANOLOGY+, V47, P660, DOI 10.1134/S0001437007050086; Pospelova V, 2008, MAR MICROPALEONTOL, V68, P21, DOI 10.1016/j.marmicro.2008.01.008; 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, 2008, MAR MICROPALEONTOL, V68, P84, DOI 10.1016/j.marmicro.2008.01.012; Radi T, 2007, MAR MICROPALEONTOL, V62, P269, DOI 10.1016/j.marmicro.2006.09.002; Radi T, 2013, MAR MICROPALEONTOL, V98, P41, DOI 10.1016/j.marmicro.2012.11.001; Richerol T, 2008, J MARINE SYST, V74, P825, DOI 10.1016/j.jmarsys.2007.11.003; Rochon A., 1999, Surface Sediments From the North Atlantic Ocean and Adjacent Seas in Relation to Sea-Surface Parameters, V35; Schlitzer R., 2010, OCEAN DATA VIEW VERS; Solignac S, 2009, NORW J GEOL, V89, P109; Vásquez-Bedoya LF, 2008, MAR MICROPALEONTOL, V68, P49, DOI 10.1016/j.marmicro.2008.03.002; Verleye TJ, 2011, MAR MICROPALEONTOL, V78, P65, DOI 10.1016/j.marmicro.2010.10.001; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650	34	2	2	0	6	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							55	63						9	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500006
B	De Vernal, A; Rochon, A; Radi, T; Henry, M		Lewis, JM; Marret, F; Bradley, LR		De Vernal, A.; Rochon, A.; Radi, T.; Henry, M.			Dinocysts as proxies of sea-ice cover in Arctic and subarctic environments	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							WALLED DINOFLAGELLATE CYSTS; SURFACE CONDITIONS; NORTH-ATLANTIC; HIGH-LATITUDES; TRACERS; PALEOCEANOGRAPHY; PRODUCTIVITY; HOLOCENE; MIDDLE	Dinoflagellate cysts occur in a wide range of environmental conditions, including polar areas. In Arctic and subarctic seas characterized by dense sea-ice cover (>6 months/year), Is landinium minutum, Islandinium? cezare, Echinidinium karaense, Polykrikos sp. var. arctic, Spiniferites elongatus-frigidus and Impaginium pallidum are common. They can occur with more cosmopolitan taxa such as Operculodinium centrocarpum sensu Wall & Dale, Pentapharsodinium dalei and Brigantedinium spp. Canonical correspondence analyses of assemblages illustrate relationships with sea-surface parameters such as salinity, temperature and sea-ice cover. The application of the modern analogue technique to dinocyst assemblages permits reconstruction of past seasonal extent of sea-ice cover (months/year with more than 50% of concentration) with an accuracy of about +/- 1.25 months/year.	[De Vernal, A.; Rochon, A.; Radi, T.; Henry, M.] Univ Quebec, Ctr Rech Geochim Isotop & Geochronol Geotop, Montreal, PQ H3C 3P8, Canada; [Rochon, A.] Univ Quebec, ISMER UQAR, Rimouski, PQ G5L 3A1, Canada	University of Quebec; University of Quebec Montreal; University of Quebec; Universite du Quebec a Rimouski	De Vernal, A (通讯作者)，Univ Quebec, Ctr Rech Geochim Isotop & Geochronol Geotop, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	de Vernal, Anne/D-5602-2013					[Anonymous], J GEOPHYSICAL RES, V116; Bonnet S, 2010, MAR MICROPALEONTOL, V74, P59, DOI 10.1016/j.marmicro.2009.12.001; 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, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A, 2008, GEOPHYS MONOGR SER, V180, P27, DOI 10.1029/180GM04; de Vernal A, 2007, DEV MARINE GEOL, V1, P371, DOI 10.1016/S1572-5480(07)01014-7; Dyck S, 2010, QUATERNARY SCI REV, V29, P3457, DOI 10.1016/j.quascirev.2010.05.008; Goossse H., 2007, Climate of the Past Discussions, V3, P999; Gosselin M, 1997, DEEP-SEA RES PT II, V44, P1623, DOI 10.1016/S0967-0645(97)00054-4; 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; Holland MM, 2003, CLIM DYNAM, V21, P221, DOI 10.1007/s00382-003-0332-6; Ledu D, 2010, QUATERNARY SCI REV, V29, P3468, DOI 10.1016/j.quascirev.2010.06.018; Meir W.N., 2011, SNOW WATER ICE PERMA, P1; Niemi A, 2011, POLAR BIOL, V34, P1803, DOI 10.1007/s00300-011-1059-1; Notz D, 2012, GEOPHYS RES LETT, V39, DOI 10.1029/2012GL051094; Okolodkov YB, 1998, SARSIA, V83, P267, DOI 10.1080/00364827.1998.10413687; Poulin Michel, 2011, Marine Biodiversity, V41, P13, DOI 10.1007/s12526-010-0058-8; Radi T, 2008, MAR MICROPALEONTOL, V68, P84, DOI 10.1016/j.marmicro.2008.01.012; Rampal P, 2011, J GEOPHYS RES-OCEANS, V116, DOI 10.1029/2011JC007110; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; ter Braak C.J., 2002, CANOCO WINDOWS VERSI; Zonneveld KAF, 2008, MAR MICROPALEONTOL, V68, P179, DOI 10.1016/j.marmicro.2008.01.015	25	0	0	0	2	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							65	69						5	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500007
B	Rochon, A; Harland, R; De Vernal, A		Lewis, JM; Marret, F; Bradley, LR		Rochon, A.; Harland, R.; De Vernal, A.			Dinoflagellates and their cysts: key foci for future research	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							SEA-SURFACE CONDITIONS; THECA RELATIONSHIP; DINOPHYCEAE; RECONSTRUCTION; ASSEMBLAGES; LATITUDES; SEDIMENTS; NOV	The study of dinoflagellates and their cysts has been ongoing for the last c. 250 years following the pioneering work of the early, passionate researchers who first described them with rudimentary microscopes. The quality of modern microscopes and other laboratory equipment, coupled with enhanced computer capabilities, has extended the frontiers of research beyond what was thought possible even half a century ago. New research topics have emerged in accordance with today's scientific and socio-economic priorities. Here we describe six of these research areas that have the most potential to advance our knowledge of dinoflagellate ecology and systematics.	[Rochon, A.] ISMER UQAR, Rimouski, PQ G5L 3A1, Canada; [Rochon, A.] Geotop, Rimouski, PQ G5L 3A1, Canada; [Harland, R.] Univ Gothenburg, Dept Earth Sci, S-40530 Gothenburg, Sweden; [De Vernal, A.] Univ Quebec Montreal, Montreal, PQ H3C 3P8, Canada; [De Vernal, A.] Geotop, Montreal, PQ H3C 3P8, Canada	University of Quebec; Universite du Quebec a Rimouski; University of Gothenburg; University of Quebec; University of Quebec Montreal	Rochon, A (通讯作者)，ISMER UQAR, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	andre_rochon@uqar.ca	de Vernal, Anne/D-5602-2013					[Anonymous], 1999, Phylogenetic systematics; [Anonymous], 1974, FOSSIL LIVING DINOFL; BAKER M., 1753, EMPLOYMENT MICROSCOP; Dale B, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; Durantou L, 2012, BIOGEOSCIENCES, V9, P5391, DOI 10.5194/bg-9-5391-2012; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; Evitt W. R., 1961, Micropaleontology, V7, P385, DOI 10.2307/1484378; Fahnenstiel G, 2009, INT VER THEOR ANGEW, V30, P1035; Fofonoff Paul W., 2003, P152; Fuentes-Grünewald C, 2012, J IND MICROBIOL BIOT, V39, P207, DOI 10.1007/s10295-011-1016-6; Fuentes-Grünewald C, 2009, J IND MICROBIOL BIOT, V36, P1215, DOI 10.1007/s10295-009-0602-3; GenBank, 2012, GENB OVERV; Gomez F., 2012, CICIMAR Oceanides, V27, P65; Hallegraeff G.M., 2003, Monographs on Oceanographic Methodology, V11, P25; Head M.J., 1996, Palynology: Principles and Applications, P1197; Lewis J, 2001, EUR J PHYCOL, V36, P137, DOI 10.1017/S0967026201003171; McMINN A., 1997, MARINE ECOLOGY PROGR, V161, P165; Mertens KN, 2012, MAR MICROPALEONTOL, V96-97, P48, DOI 10.1016/j.marmicro.2012.08.002; Monroy O. C., 2011, AQUAT INVASIONS, V6, P231; Muller O. F., 1786, ANIMALCULA INFUSORIA; MULLER O. F., 1773, PRIMA HAVNIAE LIPSIA, V1, P32; POTVIN E., 2010, THESIS; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Radi T, 2013, MAR MICROPALEONTOL, V98, P41, DOI 10.1016/j.marmicro.2012.11.001; Ribeiro S, 2010, PHYCOLOGIA, V49, P48, DOI 10.2216/09-11.1; ROCHON A., 2011, 9 INT CONFER ENCE MO; Rochon A, 2009, REV PALAEOBOT PALYNO, V155, P52, DOI 10.1016/j.revpalbo.2008.12.017; Roy S, 2012, CAN J FISH AQUAT SCI, V69, P627, DOI [10.1139/F2012-008, 10.1139/f2012-008]; Sournia Alain, 1995, P103; SUAREZ-DIAZ E., 2008, STUD HIST PHILOS M P, V39, P451; United Nations Department of Economic and Social Affairs Population Division, 2011, ESAPWP UN NAT; WALL D, 1967, Review of Palaeobotany and Palynology, V2, P349, DOI 10.1016/0034-6667(67)90165-0; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Wall D., 1965, Grana Palynologica, V6, P297; WALL D., 1967, PHYCOLOGIA, V6, P83; WETZEL O., 1933, PALAEONTOGR ABT A, V78, P47; Wetzel O., 1933, PALAEONTOGR ABT A, V77, P147; Zonneveld KAF, 2012, MAR POLLUT BULL, V64, P114, DOI 10.1016/j.marpolbul.2011.10.012	40	4	4	0	1	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							89	95						7	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500008
B	Masure, E; Aumar, AM; Vrielynck, B		Lewis, JM; Marret, F; Bradley, LR		Masure, E.; Aumar, A. -M.; Vrielynck, B.			Worldwide palaeogeography of Aptian and Late Albian dinoflagellate cysts: Implications for sea-surface temperature gradients and palaeoclimate	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							EQUAMARGE-II CRUISE; NORTH-ATLANTIC; CENOMANIAN BOUNDARY; CRETACEOUS CLIMATE; SOUTH-ATLANTIC; HIGH-LATITUDES; STRATIGRAPHY; OCEAN; SEDIMENTS; BASIN	Worldwide distribution of dinoflagellate cysts from the Aptian and Late Albian periods has been reported on palaeogeographical maps. A total of 32 and 38 species, derived from 36 and 70 studies located in the Northern Hemisphere and 14 and 17 studies in the Southern Hemisphere respectively, have been encountered in the literature. Based on their geographical range, we have defined Aptian cosmopolitan, restricted cosmopolitan, Boreal, Austral, Tethyan and restricted to the Northern Hemisphere taxa, with Late Albian Tethyan, Boreal and Austral taxa. The assemblage distribution has enabled the definition of sea-surface temperature (SST) gradients from 70 degrees N to 70 degrees S and latitudinal climatic belts and the establishment of preliminary biomes. Warmer conditions were found in southern latitudes compared to northern latitudes, as indicated by the worldwide distribution of Tethyan subtropical species. The asymmetric configuration of SST gradients is the same for both the Aptian and Late Albian periods. An estimation of the temperature requirements of extinct planktonic dinoflagellates is obtained by combining estimated temperatures from 8180 from fish teeth, belemnites, oysters and TEX86 ratios related to latitude with the latitudinal distribution of their cysts. Aptian and Albian Tethyan currents with tropical-like temperatures close to 22 degrees C and 24 degrees C, respectively, reached 60-70 degrees S.	[Masure, E.] Univ Paris 06, Ctr Rech Biodiversite & Paleoenvironm, CNRS, MNHN,CR2P,UMR7207, F-75252 Paris 05, France; [Vrielynck, B.] Univ Paris 06, Inst Sci Terre Paris, ISTEP, CNRS,UMR7193, F-75252 Paris 05, France	Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS)	Masure, E (通讯作者)，Univ Paris 06, Ctr Rech Biodiversite & Paleoenvironm, CNRS, MNHN,CR2P,UMR7207, 4 Pl Jussieu, F-75252 Paris 05, France.	edwige.masure@upmc.fr						Ainsworth N.R., 1985, Marine and Petroleum Geology, V2, P341, DOI 10.1016/0264-8172(85)90029-7; Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], MEMOIRS; [Anonymous], 1993, CLASSIFICATION FOSSI; Antonescu E., 1985, Dari de Seama ale Sedintelor Institutul de Geologie si Geofizica (Bucharest), V69, P77; Arai M, 2000, CRETACEOUS RES, V21, P351, DOI 10.1006/cres.2000.0211; ARHUS N, 1991, CRETACEOUS RES, V12, P209; Backhouse J, 2006, PALYNOLOGY, V30, P43, DOI 10.2113/gspalynol.30.1.43; Bak Krzysztof, 1995, Grzybowski Foundation Special Publication, V3, P13; BALTES N, 1967, Review of Palaeobotany and Palynology, V5, P183, DOI 10.1016/0034-6667(67)90222-9; BATTEN D. 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F., 1974, INITIAL REPORTS DEEP, P272; Zippi Pierre A., 1998, Micropaleontology (New York), V44, P1, DOI 10.2307/1485998	200	8	8	0	2	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							97	125						29	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500009
B	Bradley, LR; Marret, F		Lewis, JM; Marret, F; Bradley, LR		Bradley, L. R.; Marret, F.			Studying Holocene environmental change in the Marmara Sea, Black Sea, Caspian Sea and Aral Sea using dinoflagellate cysts	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							ASSEMBLAGES; WATER	Organic-walled dinoflagellate cysts are generally abundant and well preserved in the sediments of the Marmara Sea, Black Sea, Caspian Sea and Aral Sea making them an attractive proxy to study changes in sea-surface conditions. The number of studies involving dinoflagellate cysts from sediments of these seas has proliferated over the past decade and this paper aims to present an introduction to research in this region. The environments, both at present and during the Holocene, are unique in character and represent a number of challenges to researchers. Many of the dinoflagellate cysts recorded in the region are endemic, exhibit large morphological variation and have ecological niches that are poorly constrained. Those that are relatively well known are usually cosmopolitan, euryhaline species such as Lingulodinium machaerophorum, making precise environmental reconstruction difficult. Yet despite these challenges, dinoflagellate cysts have played an important role in understanding Holocene sea-surface conditions, notably salinities, of these seas.	[Bradley, L. R.; Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England	University of Liverpool	Marret, F (通讯作者)，Univ Liverpool, Sch Environm Sci, Roxby Bldg, Liverpool L69 7ZT, Merseyside, England.	f.marret@liv.ac.uk	Bradley, Lee/AAA-6818-2019	Bradley, Lee/0000-0003-0833-9351				[Anonymous], ANN SOFIA U ST KLIME; [Anonymous], 2006, Advances in Phycological Studies Festschrift in Honour of Prof. Dobrina Temniskova-Topalova; Atanassova J, 2005, HOLOCENE, V15, P576, DOI 10.1191/0959683605hl832rp; BALTES N, 1971, REV PALAEOBOT PALYNO, V11, P125, DOI 10.1016/0034-6667(71)90023-6; Bradley LR, 2012, J QUATERNARY SCI, V27, P835, DOI 10.1002/jqs.2580; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Eaton GL, 1996, REV PALAEOBOT PALYNO, V91, P151, DOI 10.1016/0034-6667(95)00073-9; FILIPOVA-MARINOVA M., 2012, QUATERN INT, V293, P170; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Leroy SAG, 2007, QUATERNARY SCI REV, V26, P3359, DOI 10.1016/j.quascirev.2007.09.012; Leroy SAG, 2006, QUATERN INT, V150, P52, DOI 10.1016/j.quaint.2006.01.007; Leroy SAG, 2010, REV PALAEOBOT PALYNO, V160, P181, DOI 10.1016/j.revpalbo.2010.02.011; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Londeix L, 2009, REV PALAEOBOT PALYNO, V158, P52, DOI 10.1016/j.revpalbo.2009.07.004; 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; Mertens KN, 2012, QUATERNARY SCI REV, V39, P45, DOI 10.1016/j.quascirev.2012.01.026; Mudie PJ, 2007, QUATERN INT, V167, P73, DOI 10.1016/j.quaint.2006.11.009; 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, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; Rochon Andre, 2002, Palynology, V26, P95, DOI 10.2113/0260095; Ryan WBF, 1997, MAR GEOL, V138, P119, DOI 10.1016/S0025-3227(97)00007-8; Shumilovskikh LS, 2012, PALAEOGEOGR PALAEOCL, V337, P177, DOI 10.1016/j.palaeo.2012.04.015; Sorrel P, 2006, PALAEOGEOGR PALAEOCL, V234, P304, DOI 10.1016/j.palaeo.2005.10.012; Verleye TJ, 2009, PALYNOLOGY, V33, P77; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; Wall D., 1973, Geoscience Man, V7, P95; Wall D., 1974, BLACK SEA GEOLOGY CH, V20, P364, DOI [10.1306/m20377c3, DOI 10.1306/M20377C3]	29	6	6	0	4	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							127	131						5	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500010
B	McCarthy, FMG; Krueger, AM		Lewis, JM; Marret, F; Bradley, LR		McCarthy, F. M. G.; Krueger, A. M.			Freshwater dinoflagellates in palaeolimnological studies: <i>Peridinium</i> cysts as proxies of cultural eutrophication in the SE Great Lakes region of Ontario, Canada	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							CRAWFORD LAKE; ACIDIFICATION; SEDIMENT; RECORD	Recent studies illustrate the potential of dinoflagellates as palaeolimnological proxies using a combined phycological and palynological approach, relating the stratigraphic and biogeographic distribution of cysts attributed to several species of Peridinium to environmental conditions in lakes with documented anthropogenic impact. Cultural eutrophication associated with both indigenous and Euro-Canadian settlement at various sites in the Great Lakes region of Ontario is expressed by a sharp increase in dinocyst abundance and a decline in Peridinium wisconsinense Eddy relative to species better adapted to eutrophic conditions. Total concentrations exceeded 46 000 cysts/mL in varved sediments deposited when Crawford Lake was impacted by Iroquois agriculture in the 13-15th century, even higher than the peak concentrations of nearly 36 x 10(3) cysts/mL associated with Euro-Canadian logging and agriculture. Most of these cysts were attributed to Peridinium inconspicuum Lemmermann and Peridinium volzii Lemmermann, whose cysts have not previously been reported in other palynological studies from this region. The lack of reports of these cysts elsewhere may reflect exceptional preservation of cysts and thecae in Crawford Lake, or the failure of palynologists to notice these relatively small, nondescript cysts and recognize their affinity.	[McCarthy, F. M. G.; Krueger, A. M.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Brock University	McCarthy, FMG (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	fmccarthy@brocku.ca						[Anonymous], 9 ONT MIN CULT RECR; BOYKO M., 1973, THESIS U TORONTO ONT; Boyko-Diakonow M., 1979, Moraines and varves, P303; BURDEN ET, 1986, CAN J EARTH SCI, V23, P43, DOI 10.1139/e86-005; Canion AK, 2005, J FRESHWATER ECOL, V20, P617, DOI 10.1080/02705060.2005.9664783; CARTY S, 1993, OHIO J SCI, V93, P140; Carty S., 2002, FRESHWATER ALGAE N A; Chittenden R., 1990, The Origin of Wye Marsh; Chu G, 2008, J PALEOLIMNOL, V39, P319, DOI 10.1007/s10933-007-9106-1; 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; DANESH D., 2011, THESIS BROCK U ST CA; Ekdahl EJ, 2004, GEOLOGY, V32, P745, DOI 10.1130/G20496.1; Ekdahl EJ, 2007, J PALEOLIMNOL, V37, P233, DOI 10.1007/s10933-006-9016-7; Evitt W.R., 1968, STANFORD U PUBL   GS, V10, P1; Hall RI, 1996, CAN J FISH AQUAT SCI, V53, P1, DOI 10.1139/cjfas-53-1-1; Hansen G, 2007, J LIMNOL, V66, P107, DOI 10.4081/jlimnol.2007.107; Kim E, 2004, MICROB ECOL, V48, P521, DOI 10.1007/s00248-004-0219-z; KRUEGER A. M., 2011, LEAD EDG C; McAndrews J H, 1989, QUATERNARY GEOLOGY C, V1, P528; McCarthy FMG, 2011, REV PALAEOBOT PALYNO, V166, P46, DOI 10.1016/j.revpalbo.2011.04.008; MEYER R L, 1969, Arkansas Academy of Science Proceedings, V23, P145; NICHOLLS KH, 1992, CAN J FISH AQUAT SCI, V49, P40, DOI 10.1139/f92-299; NORRIS G, 1970, REV PALAEOBOT PALYNO, V10, P131, DOI 10.1016/0034-6667(70)90016-3; Popovski J., 1990, SUSSWASSERFLORA MITT, V6, P243; Prescott G.W., 1962, ALGAE W GREAT LAKES; Shen Y., 1990, Modern Biomonitoring Techniques Using Fresh Water Microbiota; Tardio M, 2006, J PALEOLIMNOL, V36, P315, DOI 10.1007/s10933-006-9001-1; Turton CL, 2006, REV PALAEOBOT PALYNO, V141, P1, DOI 10.1016/j.revpalbo.2006.03.017; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Zippi P.A., 1991, RAC Project no. 464G)	31	10	11	0	1	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							133	139						7	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500011
B	Ellegaard, M; Ribeiro, S; Lundholm, N; Andersen, TJ; Berge, T; Ekelund, F; Härnström, K; Godhe, A		Lewis, JM; Marret, F; Bradley, LR		Ellegaard, M.; Ribeiro, S.; Lundholm, N.; Andersen, T. J.; Berge, T.; Ekelund, F.; Harnstrom, K.; Godhe, A.			Using the sediment archive of living dinoflagellate cysts and other protist resting stages to study temporal population dynamics	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							MARINE; GERMINATION; VIABILITY; COUNTS; FJORD; SOIL	This overview of methodology and applications of sediment archives of living dinoflagellates and other protists examines their potential to study ecology and evolution of unicellular eukaryotes through time. Sediment cores from Koljo Fjord on the west coast of Sweden and from Manager Fjord in Northern Denmark, both enclosed embayments with recurring anoxic bottom water, provide a virtually undisturbed sediment record. Cultures of dinoflagellates (and other protists) were established by individually isolating specimens from dated sediment layers. Twelve sediment cores were used from which over 500 dinoflagellate strains from 20 different taxa, as well as numerous strains of diatoms, haptophytes, prasinophytes and heterotrophic protists, were established. Model dinoflagellate species included Pentapharsodinium dalei and Scrippsiella trochoidea. The culture strains were used to test for intraspecific variation through time in morphology, genotypes and physiology. In this paper we discuss the potential for using the sediment archive for temporal population studies, including applications relevant to palaeoecological studies.	[Ellegaard, M.; Ribeiro, S.; Lundholm, N.; Berge, T.; Ekelund, F.] Univ Copenhagen, Dept Biol, DK-1353 Copenhagen K, Denmark; [Ribeiro, S.] Geol Survey Denmark & Greenland GEUS, Marine Geol & Glaciol Dept, DK-1350 Copenhagen K, Denmark; [Lundholm, N.] Nat Hist Museum Denmark, Lab Mol Systemat, DK-1307 Copenhagen K, Denmark; [Andersen, T. J.] Univ Copenhagen, Dept Geosci & Nat Resource Management, DK-1350 Copenhagen K, Denmark; [Harnstrom, K.; Godhe, A.] Univ Gothenburg, Dept Biol & Environm Sci, SE-40530 Gothenburg, Sweden	University of Copenhagen; Geological Survey Of Denmark & Greenland; University of Copenhagen; University of Gothenburg	Ellegaard, M (通讯作者)，Univ Copenhagen, Dept Biol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	me@bio.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Lundholm, Nina/AAY-6249-2020; Ekelund, Flemming/M-1731-2014; Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/G-9213-2018; Lundholm, Nina/A-4856-2013; Andersen, Thorbjorn Joest/N-7560-2014	Ellegaard, Marianne/0000-0002-6032-3376; Ribeiro, Sofia/0000-0003-0672-9161; Lundholm, Nina/0000-0002-2035-1997; Andersen, Thorbjorn Joest/0000-0001-5032-9945				ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; Björk G, 2000, ESTUARIES, V23, P367, DOI 10.2307/1353329; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; CARON DA, 1989, MICROB ECOL, V18, P89, DOI 10.1007/BF02030118; Dale B., 1979, P443; Fallesen G, 2000, J MARINE SYST, V25, P313, DOI 10.1016/S0924-7963(00)00024-5; Härnström K, 2011, P NATL ACAD SCI USA, V108, P4252, DOI 10.1073/pnas.1013528108; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Koch TA, 2005, PROTIST, V156, P97, DOI 10.1016/j.protis.2004.12.001; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; Lundholm N, 2011, PHYCOLOGIA, V50, P629, DOI 10.2216/11-16.1; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; Mizushima K, 2004, PHYCOL RES, V52, P408, DOI 10.1111/j.1440-183.2004.00358.x; OLSEN RA, 1987, MICROB ECOL, V13, P59, DOI 10.1007/BF02014963; Ribeiro S, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0061184; Ribeiro S, 2011, NAT COMMUN, V2, DOI 10.1038/ncomms1314; RONN R, 1995, PEDOBIOLOGIA, V39, P10	17	14	18	0	11	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							149	153						5	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500013
B	Marret, F; Garcés, E		Lewis, JM; Marret, F; Bradley, LR		Marret, F.; Garces, E.			Future research foci for the ecology and palaeoecology of dinoflagellates and their cysts	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							LIFE-CYCLE; BLOOM; DINOPHYCEAE; SEDIMENTS; REPRODUCTION; ENCYSTMENT; PATTERNS; NORTH	The study of the ecology and palaeoecology of dinoflagellates and their cysts has made momentous progress since they were first discovered and described. With the help of field studies, their ecological affinities have been established; in parallel, laboratory studies have facilitated progress on the understanding of their life cycle and enabled the theca to be related to their cyst. More recently, molecular analysis has helped to discriminate species with similar morphologies. Such advances have also highlighted new fields of exciting research and led to a better understanding of the ecological significance of this major phytoplanIcton group: cryptic species, multiple stages in the life cycle, initial conditions for bloom formation and morphological variability under environmental forcing. These topics, among others, are discussed in this note.	[Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Garces, E.] CSIC, Inst Ciencies Mar, Dept Biol Marina & Oceanog, E-08003 Barcelona, Catalunya, Spain	University of Liverpool; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Marret, F (通讯作者)，Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England.	f.marret@liv.ac.uk	Garces, Esther/C-5701-2011	Garces, Esther/0000-0002-2712-501X				Anderson DM, 2013, MICROPALEAEONTOLOGIC, P141; Anglès S, 2012, HARMFUL ALGAE, V16, P1, DOI 10.1016/j.hal.2011.12.006; Anglès S, 2010, DEEP-SEA RES PT II, V57, P210, DOI 10.1016/j.dsr2.2009.09.002; Barton AD, 2010, SCIENCE, V327, P1509, DOI 10.1126/science.1184961; Bradley LR, 2013, MICROPALEAEONTOLOGIC, P127; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Brosnahan ML, 2010, DEEP-SEA RES PT II, V57, P175, DOI 10.1016/j.dsr2.2009.09.005; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; De Schepper S, 2013, MICROPALEAEONTOLOGIC, P31; De Vernal A, 2013, MICROPALEAEONTOLOGIC, P359; DODGE JD, 1991, NEW PHYTOL, V118, P593, DOI 10.1111/j.1469-8137.1991.tb01000.x; Elbrächter M, 2003, J PHYCOL, V39, P629, DOI 10.1046/j.1529-8817.2003.39041.x; Estrada M, 2010, DEEP-SEA RES PT II, V57, P308, DOI 10.1016/j.dsr2.2009.09.007; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Figueroa RI, 2008, HARMFUL ALGAE, V7, P653, DOI 10.1016/j.hal.2008.02.005; Figueroa RI, 2007, J PHYCOL, V43, P1039, DOI 10.1111/j.1529-8817.2007.00393.x; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; HALLEGRAEFF C. M., 2003, MANUAL HARMFUL MARIN; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Hinder SL, 2012, NAT CLIM CHANGE, V2, P271, DOI [10.1038/NCLIMATE1388, 10.1038/nclimate1388]; Holzwarth U, 2010, REV PALAEOBOT PALYNO, V159, P35, DOI 10.1016/j.revpalbo.2009.10.005; HOPPENRATH M., 2013, BIOL GEOLOGICAL PERS, V244; Huisman J, 2010, SCIENCE, V329, DOI 10.1126/science.1189880; 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; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matsuoka K, 2013, MICROPALEAEONTOLOGIC, P325; McCauley LAR, 2009, J PHYCOL, V45, P454, DOI 10.1111/j.1529-8817.2009.00650.x; Mertens KN, 2009, BOREAS, V38, P647, DOI 10.1111/j.1502-3885.2009.00095.x; Okolodkov YB, 2005, HARMFUL ALGAE, V4, P351, DOI 10.1016/j.hal.2004.06.016; Rochon A, 2013, MICROPALEAEONTOLOGIC, P89; TILLMAN U., 2013, BIOL GEOLOGICAL PERS, P242; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS D.B., 1971, MICROPALAEONTOLOGY O; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	39	3	3	0	1	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							189	195						7	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500015
B	Kremp, A		Lewis, JM; Marret, F; Bradley, LR		Kremp, A.			Diversity of dinoflagellate life cycles: facets and implications of complex strategies	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							GYMNODINIUM-CATENATUM DINOPHYCEAE; ALEXANDRIUM-MINUTUM; CYST FORMATION; SCRIPPSIELLA-HANGOEI; REPRODUCTIVE SUCCESS; SEXUAL REPRODUCTION; MATING-TYPE; ENCYSTMENT; BLOOM; PHYTOPLANKTON	The life cycle research of the past years has revealed an unexpectedly high diversity of reproduction and survival strategies. Dinoflagellate life cycles often seem to be plastic, i.e. different pathways and mechanisms may be complementary in one and the same species. The diversity of life cycle stages, strategies and regulation mechanisms will have implications for the understanding of ecological processes and functions. Versatility in reproduction and survival strategies will affect genetic diversity patterns and standing genetic variation which are important factors in adaptation to changing conditions and stability against environmental disturbance. Complex regulation mechanisms and multiple cues for life cycle transformations can lead to differences in the magnitude of cyst formation and sedimentation and thereby determine the fate of primary production. Life cycles are an important life history trait of dinofiagellates which, in their versatility and complexity, contribute to the functional diversity that structures and determines the functioning of aquatic systems.	Finnish Environm Inst, Ctr Marine Res, Helsinki, Finland	Finnish Environment Institute	Kremp, A (通讯作者)，Finnish Environm Inst, Ctr Marine Res, Helsinki, Finland.	anke.kremp@ymparisto.fi						Alpermann TJ, 2009, MOL ECOL, V18, P2122, DOI 10.1111/j.1365-294X.2009.04165.x; ANDERSON D. 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B	Ellegaard, M; Figueroa, RL; Versteegh, GJM		Lewis, JM; Marret, F; Bradley, LR		Ellegaard, M.; Figueroa, R. L.; Versteegh, G. J. M.			Dinoflagellate life cycles, strategy and diversity: key foci for future research	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							SEXUAL REPRODUCTION; CYST FORMATION; GEOCHEMICAL SIGNIFICANCE; STEROL COMPOSITION; MOLECULAR EVIDENCE; SURFACE SEDIMENTS; ORGANIC-MATTER; DINOPHYCEAE; SCRIPPSIELLA; PRESERVATION	Within dinoflagellate research the fields of geology and biology come together in studies of the resting stage, the cyst. Studies of this stage and life-cycle transitions can tie together the geological fossil record of dinoflagellates and the ecology of living dinoflagellates. This review focuses on possible new research areas within ploidy shifts in dinoflagellate life cycles, the role of the cyst in benthic-pelagic coupling, the cyst as the link between the past and present, the role of cysts in long-term survival and preservation of cysts and cyst-wall chemistry.	[Ellegaard, M.] Univ Copenhagen, Dept Biol, DK-1353 Copenhagen K, Denmark; [Figueroa, R. L.] Lund Univ, Dept Biol, SE-22362 Lund, Sweden; [Versteegh, G. J. 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B	Matsuoka, K; Kawami, H		Lewis, JM; Marret, F; Bradley, LR		Matsuoka, Kazumi; Kawami, Hisae			Phylogenetic subdivision of the genus <i>Protoperidinium</i> (Peridiniales, Dinophyceae) with emphasis on the <i>Monovela</i> Group	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							HETEROTROPHIC DINOFLAGELLATE GENUS; CYST-THECA RELATIONSHIP; MOLECULAR PHYLOGENY; ULTRASTRUCTURE; SSU	The genus Protoperidinium is the most diverse of the thecate dinofiagellates in both coastal and offshore environments. This genus consists of c. 300 species (Hoppenrath et al. 2009), all of which are completely heterotrophic. Although several different classification schemes in the genus Protoperidinium Berg (formerly the genus Peridinium Ehrenberg) have been proposed by different scientists (e.g. Jorgensen 1912; Lebour 1925; Abe 1981), the genus has been treated as a well-established taxonomic unit even after the revision of the genus Peridinium by Balech (1974). Since the plate formula and the shape of each plate developed in Protoperidinium species are stable, the combination of plate topology and shape have been regarded as key features for subdivision within the genus and identification of species.	[Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, Nagasaki 8528521, Japan	Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst East China Sea Res, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan.	kazu-mtk@nagasaki-u.ac.jp						Abe T. H., 1981, PUBLICATIONS SETO MA, V6, P1; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; 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; GRIBBLE K. E., 2006, J PHYCOL, V42, P1081; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Hoppenrath M., 2009, KL SENCKENBERG-REIHE, V49, P264; Hoppenrath M, 2012, PHYCOLOGIA, V51, P157, DOI 10.2216/11-35.1; JOrgensen E, 1912, SVENSKA HYDROGRAFISK, V4, P1; Kawami H, 2009, PALYNOLOGY, V33, P11, DOI 10.1080/01916122.2009.9989680; Kawami H, 2009, PHYCOL RES, V57, P259, DOI 10.1111/j.1440-1835.2009.00545.x; LEBOUR M. V., 1925, DINOFIAGELLATES NO S; Lewis J., 1987, Journal of Micropalaeontology, V6, P113; Matsuoka K, 2006, PHYCOLOGIA, V45, P632, DOI 10.2216/05-42.1; Matsuoka K, 2009, REV PALAEOBOT PALYNO, V154, P79, DOI 10.1016/j.revpalbo.2008.12.013; Mertens KN, 2012, MAR MICROPALEONTOL, V96-97, P48, DOI 10.1016/j.marmicro.2012.08.002; Ribeiro S, 2010, PHYCOLOGIA, V49, P48, DOI 10.2216/09-11.1; Saldarriaga JF, 2001, J MOL EVOL, V53, P204, DOI 10.1007/s002390010210; Sarai C, 2013, REV PALAEOBOT PALYNO, V192, P103, DOI 10.1016/j.revpalbo.2012.12.007; Takano Y, 2004, PHYCOL RES, V52, P107, DOI 10.1111/j.1440-183.2004.00332.x; Taylor F.J.R., 1976, BIBLIOTHECA BOT, V132, P1; Yamaguchi A, 2005, PHYCOL RES, V53, P30; Yamaguchi A, 2006, PHYCOL RES, V54, P317, DOI 10.1111/j.1440-1835.2006.00438.x; Yamaguchi A, 2011, EUR J PHYCOL, V46, P98, DOI 10.1080/09670262.2011.564517	24	13	13	0	2	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							275	283						9	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500023
B	Arai, M; Viviers, MC		Lewis, JM; Marret, F; Bradley, LR		Arai, M.; Viviers, M. C.			Dinoflagellate cyst superdominance assemblages from the Upper Cretaceous of the Santos Basin, offshore SE Brazil, and their palaeoecological significance	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter								Several distinct dinoflagellate cyst (dinocyst) 'superdominance' assemblages, characterized by the overwhelming dominance of a single taxon, are present in the Upper Cretaceous succession of the Santos Basin, offshore SE Brazil. Three of these assemblages are conspicuous in the central part of the basin: the Chatangiella/Isabelidinium assemblage (middle Santonian), Nelsoniella assemblage (lower Campanian), and Cerodinium assemblage (upper Campanian). The Chatangiellal Isabelidinium superdominance event is preceded by a minor Odontochitina superdominance and accompanied by an abundance of copepod eggs. This interval characterized by Odontochitina is sparse in terrestrial palynomorphs, suggesting that it represents a phase with only minor terrigenous input. By contrast, the strata containing the Chatangiellal Isabelidinium assemblage are rich in terrestrial palynomorphs. The Nelsoniella-rich strata occur at the top of an interval dominated by terrestrial palynomorphs. This suggests that the Nelsoniella superdominance event occurred at the end of a phase featuring high terrigenous input. The Cerodinium superdominance event sometimes accompanied by a Dinogymnium superdominance is succeeded by a superdominance of Pediastrum (freshwater algae). These facts support the hypothesis that superdominance events of peridinioid dinocysts tend to occur in eutrophic water caused by a significant nutrient supply due to terrigenous input. An understanding of the bioevent succession, probably related to recurrent microplankton blooms, is important because of the palaeoecological information it provides. In this case study, dinocyst superdominance events tend to occur during regressive sea-level events. This fact is demonstrated by correlation with the palaeobathymetric curve based on the distribution of benthic foraminiferal biofacies. Moreover, the dinocyst superdominance horizons may provide an additional tool for local stratigraphic correlation.	[Arai, M.; Viviers, M. C.] Petrobras CENPES PDGEO BPA, Dept Biostratig & Paleoecol, BR-21941915 Rio De Janeiro, RJ, Brazil		Arai, M (通讯作者)，Petrobras CENPES PDGEO BPA, Dept Biostratig & Paleoecol, BR-21941915 Rio De Janeiro, RJ, Brazil.	mitsuru.arai@gmail.com						ARAI M., 2010, B MUSEU PARAENSE EMI, V5, P175; Arai M., 1990, 1 S BAC AR BAC INT N, P225; ARAI M., 2004, POLEN, V14, P120; ARAI M., 2007, PALEONTOLOGIA CENARI, V2, P595; AZEVEDO R.L.M., 1987, REV BRASIL GEOCIENC, V17, P147; Correia G.A., 2005, B GEOSCIENCES PETROB, V13, P123; LANA C. C., 2011, PALEONTOLOGIA CENCIR, V3, P211; Milani E.J., 2007, Boletim de Geociencias da Petrobras, V15; Moreira J.L. P., 2007, Boletim de Geociencias da Petrobras, V15, P531; Mudie PJ, 2002, PALAEOGEOGR PALAEOCL, V180, P159, DOI 10.1016/S0031-0182(01)00427-8; NOE-NYGAARD N, 1987, Palaios, V2, P263, DOI 10.2307/3514676; PEDRAO E., 2000, P 10 BRAZ M PAL PAL, P81; TANGEN K., 1980, BLYTTIA, V38, P145; TAYLOR FJR, 1987, BOTANICAL MONOGRAPHS, V21; Uesugui N., 1979, Boletim Tecnico da Petrobras, V22, P229; Viviers M.C., 1988, Revista Brasileira de Geociencias, V18, P291	16	9	9	0	3	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							285	292						8	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500024
B	Schreck, M; Matthiessen, J		Lewis, JM; Marret, F; Bradley, LR		Schreck, M.; Matthiessen, J.			<i>Batiacasphaera micropapillata</i>: Palaeobiogeographic distribution and palaeoecological implications of a critical Neogene species complex	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							DINOFLAGELLATE CYST BIOSTRATIGRAPHY; NORTH-SEA BASIN; MIDDLE MIOCENE; DINOCYST STRATIGRAPHY; PLIOCENE-PLEISTOCENE; ACRITARCH EVENTS; BELGIUM; PACIFIC; ICELAND; PALEOENVIRONMENTS	The extinct dinoflagellate cyst complex Batiacasphaeramicropapillata (B. micropapillata, B. minute) has been frequently reported from Neogene sediments of the North Atlantic region, but little is known about its palaeoecology. To utilize it for future palaeoenvironmental interpretations, distribution maps for Middle Miocene-Pliocene time slices have been generated by using new data from Ocean Drilling Program (ODP) Hole 907A (Iceland Sea) and Integrated ODP (IODP) Hole M0002A (Central Arctic Ocean) and recent publications. This species complex is adapted to outer-neritic to oceanic environments, judging by its abundance at many deep-water sites in comparison to marginal marine settings and the co-occurrence of well-known oceanic species. The centre of distribution is the high-latitude North Atlantic, but it tolerates a range of sea-surface temperatures from 7-10 degrees C to >20 degrees C. The relatively low concentration in the Arctic Ocean represents an occurrence close to its ecological limit, and suggests that it may occur in regions with pronounced seasonal gradients in temperature, sea-ice and light. Increased nutrient availability may be a another important ecological factor under optimum living conditions. A distinct Late Miocene decline in the Iceland Sea and Arctic Ocean and a near-synchronous Pliocene disappearance in the North Atlantic suggest a response to Late Cenozoic cooling.	[Schreck, M.; Matthiessen, J.] Helmholtz Ctr Marine & Polar Res, Alfred Wegener Inst, D-27568 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Schreck, M (通讯作者)，Korea Polar Res Inst, 26 Songdomirae Ro, Inchon 406840, South Korea.	Michael.Schreck@kopri.re.kr						Brenner WW, 2001, NEUES JAHRB GEOL P-A, V219, P229, DOI 10.1127/njgpa/219/2001/229; 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]; BROWN S., 1985, INITIAL REPORTS DSDP, V80, P643; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Butzin M, 2011, PALEOCEANOGRAPHY, V26, DOI 10.1029/2009PA001901; COSTA L. 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A., 1986, AASP CONTRIBUTIONS S, V17; Pudsey C.J., 2001, Proceedings of the Ocean Drilling Program, Scientific Results, V178, P1; QUATTROCCHIO M., 1986, PAPERS 1 S NEOGENE D, V17; Rasmussen ES, 2008, EPISODES, V31, P66, DOI 10.18814/epiiugs/2008/v31i1/010; Rusbult J., 1992, N JB GEOL PALAONT MH, V3, P150; Santarelli A, 1998, MAR MICROPALEONTOL, V33, P273, DOI 10.1016/S0377-8398(97)00042-X; Schreck M, 2013, MAR MICROPALEONTOL, V101, P49, DOI 10.1016/j.marmicro.2013.03.003; Schreck M, 2012, REV PALAEOBOT PALYNO, V187, P66, DOI 10.1016/j.revpalbo.2012.08.006; St John K, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2007PA001483; Stabell B., 1996, P OCEAN DRILLING PRO, V151, P483, DOI DOI 10.2973/ODP.PROC.SR.151.137.1996; STOCKMARR J, 1971, Pollen et Spores, V13, P615; STOVER L. E., 1977, AASP CONTRIBUTIONS S, V5A, P66; TAYLOR FJ.R., 1987, BIOL DINOFLAGELLATES, P1; Thiede J., 2011, Polarforschung, V80, P141; Udeze CU, 2005, PALAEOGEOGR PALAEOCL, V219, P199, DOI 10.1016/j.palaeo.2004.12.026; Verhoeven K, 2011, PALAEOGEOGR PALAEOCL, V309, P33, DOI 10.1016/j.palaeo.2011.04.001; VERSTEEGH GJM, 1994, MAR MICROPALEONTOL, V23, P147, DOI 10.1016/0377-8398(94)90005-1; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7; Warny SA, 2002, MICROPALEONTOLOGY, V48, P257, DOI 10.2113/48.3.257; Weller P, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2007PA001472; Williams Graham L., 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P99; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; Zachos JC, 2008, NATURE, V451, P279, DOI 10.1038/nature06588; Zegarra M, 2011, MAR MICROPALEONTOL, V81, P107, DOI 10.1016/j.marmicro.2011.09.005; Zevenboom D., 1995, PhD Thesis Diss	93	9	10	0	1	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							301	314						14	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500026
B	Matsuoka, K; Head, MJ		Lewis, JM; Marret, F; Bradley, LR		Matsuoka, K.; Head, M. J.			Clarifying cyst-motile stage relationships in dinollagellates	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							SP-NOV DINOPHYCEAE; HETEROTROPHIC DINOFLAGELLATE GENUS; THECA RELATIONSHIP; GYMNODINIUM-CATENATUM; MOLECULAR PHYLOGENY; RECENT SEDIMENTS; MICRORETICULATE CYST; FOSSIL RECORD; RESTING CYST; COMB-NOV	Elucidating the relationships between the resting cysts of dinoflagellates (studied mostly by palaeontologists) and their corresponding motile stages (studied mostly by biologists) allows a wealth of biological and palaeontological information to be combined. It enables the presence of living cysts in modern sediments to predict the seasonal appearance of motile stages in the water column, and of fossil cysts in the geological record to test molecular phylogenetic relationships, calibrate molecular clocks and facilitate palaeoenvironmental reconstructions. The morphology of the living cysts, in conjunction with motile-stage morphology and ultrastructure and molecular studies, can also be useful for constructing phylogenetic relationships. Dinoflagellate resting cysts were first recorded in plankton surveys in the 1870s and 1880s, although their significance as such was not then recognized. Much later, in the 1940s and 1950s, they were encountered in cultures of motile cells and in the 1960s were shown to be hypnozygotic cysts. From the 1960s there was a rapid increase in the knowledge of cyst-motile stage equivalencies based on cyst incubation experiments, but the limitations of this method including taxonomic uncertainties for both motile stages and cysts required new approaches. The advent of molecular characterization of dinoflagellates in the 1980s and 1990s, and the desire to analyse individual cells, led the way in the 2000s to the single-cell (cyst) polymerase chain reaction (PCR) technique. The historical development of cyst-theca relationship studies is examined, the successes and limitations of the various methods are illustrated with examples, and the impact of single-cell PCR is assessed in detail.	[Matsuoka, K.] Nagasaki Univ, Inst East China Sea Res, Nagasaki 8528521, Japan; [Head, M. J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Nagasaki University; Brock University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst East China Sea Res, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan.	kazu-mtk@nagasaki-u.ac.jp						AKSELMAN R, 1987, Boletim do Instituto Oceanografico, V35, P17; ANDERSON DM, 1988, J PHYCOL, V24, P255; [Anonymous], 1995, Marine ecological processes; [Anonymous], 1981, Studies on the family Peridiniidae. An unfinished monograph of the armored Dinoflagellata; [Anonymous], 1878, Der Organismus der Infusionsthiere nach eigenen Forschungen in systematischer Reihenfolge bearbeitet. III. Abteilung, Die Naturgeschichte de Flagellaten oder geisselinfusorien. 1. Halfte; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P644, DOI 10.2216/07-05.1; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Balech E., 1988, Publ. Espec. Inst. Esp. 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B	Bolch, C; Percy, L		Lewis, JM; Marret, F; Bradley, LR		Bolch, C.; Percy, L.			DINO 9 Workshop Report: Linking dinoflagellate life-cycle stages using single-cell isolation and molecular typing	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							PCR; DINOPHYCEAE; PROTISTS; PROTOPERIDINIUM; IDENTIFICATION; AMPLIFICATION; CYSTS; DNA	This workshop aimed to expose the participants to simple techniques for manipulation of single cells and cysts, with current and emerging DNA technologies to identify the genetic and taxonomic affinities of cyst/cell morphotypes and link different life-cycle stages of dinoflagellates. The workshop was attended by over 45 participants (from 23 countries), ranging from research (Masters and PhD) students through to senior researchers. The workshop kicked off with two short presentations from the workshop leaders. Dr Bolch described and demonstrated the practice of manual mouth pipetting (including a short video) using both stereo- and compound microscopes. Simple techniques to improve success rate of manual manipulations were covered as were ways of minimizing saltwater/media carry over with transfer of single cells to PCR tubes. Dr Percy presented a range of alternative manipulation methods (including video presentations) that avoid mouth pipetting, a practice that is increasingly banned in laboratories where work with human or infectious agents may be carried out in the same areas as lower-risk activities. Following the presentations, all participants practised the demonstrated methods with live dinoflagellate cells using simple mouth pipettes and other devices supplied by the presenters, using a range of equipment made available by the University of Liverpool laboratory and academic staff. Most participants experienced successful manipulation and transfer of single cells during the hour of practice. All participants considered the workshop valuable and that the very simple manipulations could be usefully implemented in their own laboratories for specific research questions and projects. A number of participants also decided to keep their piece of silicon tubing to manufacture a similar device on return to their lab. Toward the end of the workshop, a short presentation from Dr Bolch focused on how some current and emerging technologies (laser-microdissection, flow cytometry, pico-litre droplet manipulation) can be combined with molecular methods (multiple displacement amplification) to achieve both highly selective and automated high-throughput manipulation for molecular and genomic scale analysis of single bacteria through to phytoplankton protistan cells. The workshop presenters thank Dr David Montagnes and lab staff at the University of Liverpool for enthusiastic assistance and efforts to round up suitable equipment to run the workshop. Thanks also go to Dr Joe Taylor (University of Westminster) for his on-the-ground organization and logistics to ensure that the workshop would be a success. The workshop technical notes are reproduced below for a wider audience.	[Bolch, C.] Univ Tasmania, Australian Maritime Coll, Natl Ctr Marine Conservat & Resource Sustainabil, Launceston, Tas 7250, Australia; [Percy, L.] Univ Westminster, Sch Life Sci, London W1W 6UW, England	University of Tasmania; Australian Maritime College; University of Westminster	Bolch, C (通讯作者)，Univ Tasmania, Australian Maritime Coll, Natl Ctr Marine Conservat & Resource Sustainabil, Locked Bag 1370, Launceston, Tas 7250, Australia.	cjsbolch@amc.edu.au	Bolch, Christopher/J-7619-2014					Auinger BM, 2008, APPL ENVIRON MICROB, V74, P2505, DOI 10.1128/AEM.01803-07; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Bolch CJS, 2001, PHYCOLOGIA, V40, P162, DOI 10.2216/i0031-8884-40-2-162.1; Godhe Anna, 2002, Harmful Algae, V1, P375, DOI 10.1016/S1568-9883(02)00049-5; Gribble KE, 2007, PHYCOLOGIA, V46, P315, DOI 10.2216/06-68.1; Handy SM, 2009, J PHYCOL, V45, P1163, DOI 10.1111/j.1529-8817.2009.00738.x; Hart MC, 2007, HARMFUL ALGAE, V6, P271, DOI 10.1016/j.hal.2006.10.001; Heywood JL, 2011, ISME J, V5, P674, DOI 10.1038/ismej.2010.155; Lynn DH, 2009, J EUKARYOT MICROBIOL, V56, P406, DOI 10.1111/j.1550-7408.2009.00439.x; Marín I, 2001, BIOTECHNIQUES, V30, P88, DOI 10.2144/01301st05; Ribeiro S, 2010, PHYCOLOGIA, V49, P48, DOI 10.2216/09-11.1; STERN R. F., 2010, PLOS ONE, V5, P11, DOI [10.1371/journal.pone.0013991, DOI 10.1371/J0URNAL.P0NE.0013991]; Zhang K, 2006, NAT BIOTECHNOL, V24, P680, DOI 10.1038/nbt1214	13	0	0	0	4	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-368-4	MICROPALEAEONTOLOGIC			2013							351	358						8	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500028
B	Hart, MB; Bailey, HW		Bowden, AJ; Gregory, FJ; Henderson, AS		Hart, Malcolm B.; Bailey, Haydon W.			Key figures from the history of research on the Foraminifera of the Chalk Group in the UK	LANDMARKS IN FORAMINIFERAL MICROPALAEONTOLOGY: HISTORY AND DEVELOPMENT	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							CALCAREOUS DINOFLAGELLATE CYST; BENTHIC FORAMINIFERA; BOUNDARY SUCCESSION; STEVNS KLINT; CALCIFICATION; EUROPE; CARBON; BIOSTRATIGRAPHY; ACIDIFICATION; EASTBOURNE	The chalk facies dominates Upper Cretaceous strata in the Anglo-Paris Basin, northern Germany, Poland, southern Sweden, Denmark and the North Sea Basin. The very name of the Cretaceous is derived from `creta', the Latin word for chalk. It is unsurprising, therefore, that some of the earliest uses of micropalaeontology in France and the United Kingdom was to determine the biostratigraphy of the chalk: by Alcide d'Orbigny in France and by staff of the (British) Geological Survey in the UK. This approach was extended, in the 1940s, to the analysis of on-shore, and then offshore, hydrocarbon exploration wells. The continuing interest in the foraminifera of the chalk can be linked to the site investigation for the Channel Tunnel, construction of the Thames Barrier and the development of chalk oilfields in the North Sea Basin. Supporting these interests is a body of research aimed at the understanding of both the overall biostratigraphy of the chalk and some of the key bio-events of the Late Cretaceous: most notably the Cenomanian/Turonian boundary event (OAE 11) and the end-Cretaceous mass extinction.	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SEPM Concepts in Sedimentology and Paleontology No. 6, P79, DOI DOI 10.2110/CSP.98.06.0079; Wilkinson IP, 2011, P GEOLOGIST ASSOC, V122, P862, DOI 10.1016/j.pgeola.2011.09.001; Williams-Mitchell E., 1948, Proceedings of the Geological Association, V59, P91; WILLIAMS-MITCHELL E., 1956, P GEOLOGISTS ASS LON, V67, P221; Wray DS, 1999, GEOL MAG, V136, P361, DOI 10.1017/S0016756899002836; Ziegler P.A., 1982, GEOLOGICAL ATLAS W C	173	3	3	0	3	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			978-1-86239-371-4	MICROPALEAEONTOLOGIC			2013							85	102						18	Geology; Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FL					2025-03-11	WOS:000332424200009
J	Narale, DD; Patil, JS; Anil, AC				Narale, Dhiraj Dhondiram; Patil, Jagadish S.; Anil, Arga Chandrashekar			Dinoflagellate cyst distribution in recent sediments along the south-east coast of India	OCEANOLOGIA			English	Article						Dinoflagellate cysts; Heterotrophic; Phototrophic; South-east coast of India; Coastal sediments	RECENT MARINE-SEDIMENTS; SURFACE SEDIMENTS; BAY; PHYTOPLANKTON; SEA; WATERS; EUTROPHICATION; PRESERVATION; ASSEMBLAGES; INDICATORS	The spatial variation in the dinoflagellate cyst assemblage from the south-east coast of India is presented along with a comparison of the cyst abundance from other regions of the world. Samples from 8 stations revealed the presence of 24 species from the genera Protoperidinium, Zygabikodinium, Gonyaulax, Lingulodinium and Gyrodinium. Cyst abundance was comparatively high at northern stations and was well correlated with the fine-grained (silt-clay dominated) sediments. In contrast, low cyst abundance was recorded in sandy sediments at southern stations. Fourteen cyst-forming dinoflagellate species previously unrecorded in planktonic samples were detected in the sediments. The cyst abundance recorded here is low (29-331 cysts g(-1). dry sediment) as compared to sub-tropical and temperate regions, but it is on a par with tropical regions, including the west coast of India. Comparison of the cyst assemblage along the Indian coast revealed a smaller number of potentially harmful and red-tide-forming dinoflagellate species on the south-east coast (6 species) than on the west coast (10 species). Calcareous cysts of the genus Scrippsiella reported from the west coast and Visakhapatnam harbour (south-east coast) were not observed in this study although their planktonic cells have been reported.	[Narale, Dhiraj Dhondiram; Patil, Jagadish S.; Anil, Arga Chandrashekar] 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			Ministry of Earth Sciences (MoES) under the Indian XBT programme; Ballast Water Management programme; Directorate General of Shipping, India	Ministry of Earth Sciences (MoES) under the Indian XBT programme; Ballast Water Management programme; Directorate General of Shipping, India	The financial support for this work was received from the Ministry of Earth Sciences (MoES) under the Indian XBT programme and the Ballast Water Management programme, funded by the Directorate General of Shipping, India.	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J	Egger, H; Mohamed, O; Rögl, F				Egger, Hans; Mohamed, Omar; Roegl, Fred			PLANKTON STRATIGRAPHY OF THE SANTONIAN AT MORZG, SALZBURG (GOSAU GROUP, NORTHERN CALCAREOUS ALPS, AUSTRIA)	AUSTRIAN JOURNAL OF EARTH SCIENCES			English	Article						calcareous nannoplankton; planktonic foraminifera; dinoflagellate cysts; Upper Cretaceous; Eastern Alps; Gosau Group	FORAMINIFERAL BIOEVENTS; INOCERAMID BIVALVES; BOUNDARY STRATOTYPE; CARBON ISOTOPES; BIOSTRATIGRAPHY; NANNOFOSSILS; AMMONITES; PLATEAU; SECTION; TEXAS	Montfort hill, lying in Morzg, within the southern outskirts of Salzburg, consists of Upper Cretaceous deposits of the Gosau Group. Alluvial fan deposits of the Kreuzgraben Formation (?Turonian) and Coniacian neritic limestone (Glanegg beds of the Paratexanites serratomarginatus ammonite zone) are overlain by bathyal marlstone ("Morzg beds"). Diverse planktonic assemblages (foraminifera, calcareous nannoplankton and dinoflagellate cysts) indicate that they lie in the upper part of the Dicarinella asymetrica planktonic foraminifera zone and the Lucianorhabdus cayeuxii calcareous nannoplankton zone (CC16 resp. UC12) of the middle to upper Santonian. As in the near-by Untersberg region (Eitelgraben section), the succession at Morzg is punctuated by a stratigraphic gap comprising the lower Santonian and probably parts of the middle Santonian.	[Egger, Hans] Geol Survey Austria, A-1030 Vienna, Austria; [Mohamed, Omar] Menia Univ, Fac Sci, Dept Geol, El Minia, Egypt; [Roegl, Fred] Museum Nat Hist, A-1014 Vienna, Austria	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						[Anonymous], 1935, MITTEILUNNGEN GEOLOG; [Anonymous], 1967, PALAEONTOGRAPHICA AM; [Anonymous], MITTEILUNGEN GEOLOGI; [Anonymous], 1981, CUSHMAN FDN FORAMINI; Belford D. J., 1960, Bulletin Aust Bur Min Res geol geophys, V57, P1; Blair SA, 2009, CRETACEOUS RES, V30, P367, DOI 10.1016/j.cretres.2008.07.016; Burnett J.A., 1998, P132; Caron M., 1985, P17; Egger H., 1990, JB GEOLOGISCHE BUNDE, V133, P424; Fensome R. A., 2008, AM ASS STRATIGRAPHIC, V1; Fensome RA., 1993, MICROPALEONTOLOGY, V7; Fugger E., 1885, NATURWISSENSCHAFTLIC; Gale AS, 2008, CRETACEOUS RES, V29, P131, DOI 10.1016/j.cretres.2007.04.006; Gale AS, 2007, ACTA GEOL POL, V57, P113; Georgescu MD, 2010, J MICROPALAEONTOL, V29, P149, DOI 10.1144/0262-821X10-004; Georgescu MD, 1996, MICROPALEONTOLOGY, V42, P305, DOI 10.2307/1485955; Hradecka L., 2003, BEITRAGE GEOLOGIE SA, V2, P149; Huber BT, 2011, J FORAMIN RES, V41, P53, DOI 10.2113/gsjfr.41.1.53; KENNEDY W J, 1981, Annals of the South African Museum, V86, P115; Kirsch K.-H., 1991, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V22, P1; KRASHENINNIKOV VA, 1983, INITIAL REP DEEP SEA, V71, P789, DOI 10.2973/dsdp.proc.71.129.1983; LAMOLDA M.A, 2013, 5 C CRET ESP, P32; Lamolda MA, 2007, CRETACEOUS RES, V28, P18, DOI 10.1016/j.cretres.2006.05.020; LOEBLICH A.R., 1987, Foraminiferal genera and their classification, V2, P1; McIntyre D. J, 1975, GEOSCIENCE MAN, V11, P61; NEDERBRAGT AJ, 1991, MICROPALEONTOLOGY, V37, P329, DOI 10.2307/1485910; Oberhauser R., 1963, Jahrbuch der Geologischen Bundesanstalt Wien, V106, P1; Oberhauser R., 1968, Jahrbuch der Geologischen Bundesanstalt Wien, V111, P115; Oberhauser R., 1963, EXK ACHT EUR MIKR K, P81; Perch-Nielsen K., 1985, P329; Petrizzo M. R., 2013, GEOPH RES ABSTR, V15; Petrizzo MR, 2011, CRETACEOUS RES, V32, P387, DOI 10.1016/j.cretres.2011.01.010; Petrizzo MR, 2000, CRETACEOUS RES, V21, P479, DOI 10.1006/cres.2000.0218; Petrizzo MR, 2003, J FORAMIN RES, V33, P330, DOI 10.2113/0330330; Prey S., 1969, GEOLOGISCHE KARTE UM; Prince IM, 1999, REV PALAEOBOT PALYNO, V105, P143, DOI 10.1016/S0034-6667(98)00077-3; Reuss A.E., 1854, DENKSCHRAKAD WISS, V7, P1; Robaszynski F., 1979, CAH MICROPALEONT, V1, P1; WAGREICH M, 1995, TECTONOPHYSICS, V242, P63, DOI 10.1016/0040-1951(94)00151-X; WAGREICH M, 1994, PALAEOGEOGR PALAEOCL, V110, P235, DOI 10.1016/0031-0182(94)90086-8; Wagreich M., 2009, SOC SEDIMENTARY GEOL, V91, P69; Wagreich M., 2003, OSTERREICHISCHE AKAD, V16, P141; Weidich KF, 1984, ABHANDLUNGEN BAYERIS, V162, P1; Williams G.L., 1985, P847; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; YUN H-S, 1981, Palaeontographica Abteilung B Palaeophytologie, V177, P1	46	8	8	0	4	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.		2013	106	2					89	114						26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	282RB					2025-03-11	WOS:000329189000008
C	Rozanov, AY; Hoover, RB		Hoover, RB; Levin, GV; Rozanov, AY; Wickramasinghe, NC		Rozanov, Alexei Yu; Hoover, Richard B.			Acritarchs in carbonaceous meteorites and terrestrial rocks	INSTRUMENTS, METHODS, AND MISSIONS FOR ASTROBIOLOGY XVI	Proceedings of SPIE		English	Proceedings Paper	Conference on Instruments, Methods, and Missions for Astrobiology XVI	AUG 27, 2013	San Diego, CA	SPIE		acritarchs; palynomorphs; organic-walled microfossils; meteorites; Murray; Orgueil; Murchison	ORGUEIL METEORITE; ORGANIZED ELEMENTS; CHONDRITES; HYSTRICHOSPHERES; PHYTOPLANKTON; MICROFOSSILS; PROPOSALS; SEARCH; LIFE	Acritarchs are a group of organic-walled, acid-resistant microfossils of uncertain or unknown origin. Some are thought to represent the cysts or resting stages of unicellular protists (possibly dinoflagellates), chrysophytes (green algae) or other planktonic eukaryotic algae. Acritarchs are found throughout the geologic column extending back as far at 3.2 Ga. The presence of large sphaeromorphs in the Archaean provides evidence that the eukaryotic lineage extends much farther back in time than previously thought possible. Acritarchs are abundant in the Paleoproterozoic shales (1.9-1.6 Ga) of the former Soviet Union and they have been extensively used for the investigation of Proterozoic and Paleozoic biostratigraphy and paleoenvironmental parameters. Scanning Electron Microscope studies have revealed the fossilized remains of organic-walled microfossils of unknown origin and exhibiting characteristics of acritarchs in a variety of carbonaceous meteorites. In many cases, these remains are black or brown in color and have Carbon/Oxygen ratios suggesting they have been diagenetically converted into kerogen. It is not feasible that the fossilized remains of organic-walled microfossils such as acritarchs represent biological contaminant that invaded and became embedded in the rock matrix of carbonaceous meteorites within the short time periods of their residence on Earth. Consequently, these groups of microfossils are considered to provide an additional line for the existence of indigenous extraterrestrial microbial remains in meteorites. This paper presents a brief review of acritarchs in terrestrial rocks and provides images of a number of similar morphotypes of uncertain origin found in freshly fractured samples of carbonaceous meteorites.	[Rozanov, Alexei Yu] RAS, Astrobiol Inst, Joint Inst Nucl Res, Dubna, Russia	Joint Institute for Nuclear Research - Russia; Russian Academy of Sciences	Rozanov, AY (通讯作者)，RAS, Astrobiol Inst, Joint Inst Nucl Res, Dubna, Russia.	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J	El Atfy, H; Brocke, R; Uhl, D				El Atfy, Haytham; Brocke, Rainer; Uhl, Dieter			Age and paleoenvironment of the Nukhul Formation, Gulf of Suez, Egypt: Insights from palynology, palynofacies and organic geochemistry	GEOARABIA			English	Article							MIDDLE MIOCENE; SEQUENCE STRATIGRAPHY; SOURCE-ROCK; RIFT-BASIN; RED-SEA; DINOFLAGELLATE CYSTS; SEDIMENTS; VEGETATION; NEOGENE; BIOSTRATIGRAPHY	Palynological results of a detailed study carried out on 56 samples retrieved from two selected wells (GH 404-2A and SA-E6A) of the Hilal and Shoab Ali fields within the southern part of the Gulf of Suez, Egypt, are presented. This study is mainly focused on the poorly dated Nukhul Formation, for which very little information from palynology is available despite its importance from a petroleum viewpoint. The assemblages discovered in our study are moderately preserved and reveal a sparse but significant record of spores and pollen and dinoflagellates together with highly diverse fungi and algal taxa, e.g. Botryococcus and Pediastrum. A latest Oligocene Early Miocene (Chattian-Aquitanian) age has been suggested for the Nukhul Formation, based on compiling palynostratigraphic and ecologic data obtained from palynomorphs that have previously been assumed to be representatives for this period on a regional scale. In addition, the Oligocene/Miocene Boundary (OMB) could be lithostratigraphically defined within the studied formation, most likely at the boundary between the lower Shoab Ali Member and upper Ghara Member. A fungal/algal 'event' within the interval from 11,370-11,430 ft in the GH 404-2A Well may be associated with a strong regressive phase. Such a regression was previously observed in the Nile Delta and other locations around the Red Sea province, and may be assigned to the global Mi-1 glaciation event at the OMB. However, not only glacial-driven eustacy but also tectonic activity related to the Gulf of Suez rifting may have contributed in forming such an event. Palynofacies investigations were carried out under both transmitted and fluorescence microscopy and the results were partly supplemented by existing organic geochemical analyses (GH 404-2A Well) involving Rock-Eval pyrolysis and total organic carbon (TOC) measurements. The analysis was used to interpret the depositional regime, paleoenvironment and thermal maturation history of the studied succession. These results support the temporary existence of shallow, pond- or lake-like aquatic habitats during deposition of the lower Shoab Ali Member that evolved into a shallow-marine environment with the onset of the deposition of upper Ghara Member of the Nukhul Formation.	[El Atfy, Haytham] Mansoura Univ, Dept Geol, Mansoura, Egypt; [El Atfy, Haytham] Goethe Univ Frankfurt, Frankfurt, Germany; [Brocke, Rainer] Senckenberg Res Inst, Sect Palynol & Microvertebrates Paleozo, Frankfurt, Germany; [Brocke, Rainer; Uhl, Dieter] Nat Hist Museum, Frankfurt, Germany; [Uhl, Dieter] Senckenberg Res Inst, Sect Paleoclimate & Paleoenvironm Res, Frankfurt, Germany; [Uhl, Dieter] Univ Tubingen, Tubingen, Germany	Egyptian Knowledge Bank (EKB); Mansoura University; Goethe University Frankfurt; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Eberhard Karls University of Tubingen		haytham.elatfy@senckenberg.de; rainer.brocke@senckenberg.de; dieter.uhl@senckenberg.de	Atfy, Haytham/AAT-2276-2021		German Academic Exchange Service (DAAD) [A/10/92695]; Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F)	German Academic Exchange Service (DAAD)(Deutscher Akademischer Austausch Dienst (DAAD)); Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F)	The authors are grateful to the Egyptian General Petroleum Corporation (EGPC) and the Gulf of Suez Petroleum Company (GUPCO, in particular Raouf Rateb and Abu-Bakr Ahmed) for the provision of samples and well logs. The first author was supported by a grant (A/10/92695), from the German Academic Exchange Service (DAAD). Partial financial support from the Biodiversitat und Klimaforschungszentrum Frankfurt (BiK-F) is also acknowledged. Prof. Dr. Dr. h.c. Volker Mosbrugger should also be mentioned for his continuous support. We would like to thank two anonymous reviewers whose careful and perceptive comments greatly improved the paper. Thanks are also extended to GeoArabia's Assistant Editor Kathy Breining for proofreading of the manuscript and the design of the paper for press by GeoArabia's Production Co-manager, Arnold Egdane. This study was conducted as a part of the PhD dissertation research project of H. El Atfy.	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J	Milzer, G; Giraudeau, J; Faust, J; Knies, J; Eynaud, F; Rühlemann, C				Milzer, G.; Giraudeau, J.; Faust, J.; Knies, J.; Eynaud, F.; Ruehlemann, C.			Spatial distribution of benthic foraminiferal stable isotopes and dinocyst assemblages in surface sediments of the Trondheimsfjord, central Norway	BIOGEOSCIENCES			English	Article							WALLED DINOFLAGELLATE CYSTS; NORTHERN NORTH-ATLANTIC; CARBON ISOTOPES; PLANKTONIC-FORAMINIFERA; WESTERN NORWAY; SEA; OXYGEN; FJORD; INDICATORS; WATER	Instrumental records from the Norwegian Sea and the Trondheimsfjord show evidence that changes of bottom water temperature and salinity in the fjord are linked to the salinity and temperature variability of the North Atlantic Current (NAC). Changes in primary productivity and salinity in the surface and intermediate water masses in the Trondheimsfjord as well as the fjord sedimentary budget are mainly driven by changes in riverine input. In this study we use 59 surface sediment samples that are evenly distributed in the fjord to examine whether dinocyst assemblages and stable isotope ratios of benthic foraminifera reflect the present-day hydrology and can be used as palaeoceanographic proxies. In general, modern benthic delta O-18 and delta C-13 values decrease from the fjord entrance towards the fjord head with lowest values close to river inlets. This is essentially explained by gradients in the amounts of fresh water and terrigenous organic matter delivered from the hinterland. The distribution of benthic delta C-13 ratios across the fjord is controlled by the origin (terrigenous vs. marine) of organic matter, local topography-induced variability in organic matter flux at the water-sediment interface, and organic matter degradation. The dinocyst assemblages display the variations in hydrography with respect to the prevailing currents, the topography, and the freshwater and nutrient supply from rivers. The strength and depth of the pycnocline in the fjord strongly vary seasonally and thereby affect water mass characteristics as well as nutrient availability, temporally creating local conditions that explain the observed species distribution. Our results prove that dinocyst assemblages and benthic foraminiferal isotopes reliably mirror the complex fjord hydrology and can be used as proxies of Holocene climatic variability.	[Milzer, G.; Giraudeau, J.; Eynaud, F.] Univ Bordeaux, CNRS, EPOC, UMR5805, Talence, France; [Faust, J.; Knies, J.] Geol Survey Norway NGU, Trondheim, Norway; [Ruehlemann, C.] Fed Inst Geosci & Nat Resources BGR, Hannover, Germany	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Geological Survey of Norway	Milzer, G (通讯作者)，Univ Bordeaux, CNRS, EPOC, UMR5805, Talence, France.	g.milzer@epoc.u-bordeaux1.fr	Giraudeau, Jacques/AAF-5764-2019	Giraudeau, Jacques/0000-0002-5069-4667; Faust, Johan C./0000-0001-8177-7097; Eynaud, Frederique/0000-0003-1283-7425	European Community [238111]	European Community	This work is a contribution to the CASE Initial Training Network funded by the European Community's 7th Framework Programme FP7 2007/2013, Marie Curie Actions, under Grant Agreement No. 238111. (http://caseitn.epoc.u-bordeaux1.fr/). The Trondheim Biological Station of the Norwegian University of Science and Technology provided temperature and salinity data sets from the fjord mooring hydrological stations. Anne de Vernal (GEOTOP, UQAM) and Christophe Fontanier (BIAF, Universite Angers) are gratefully acknowledged for their support and helpful suggestions during the preparation of this manuscript.	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C	Zhou, JF; Xu, LP; Feng, DL; Hu, AB; Xie, TF		Xu, QJ; Ju, YH; Ge, HH		Zhou Junfeng; Xu Leping; Feng Daolun; Hu Anbang; Xie Tingfei			Study on Inactivation of Microalgae in Ship Ballast Water by Pulsed Electric Field and Heat Treatment	PROGRESS IN ENVIRONMENTAL SCIENCE AND ENGINEERING, PTS 1-4	Advanced Materials Research		English	Proceedings Paper	2nd International Conference on Energy, Environment and Sustainable Development (EESD 2012)	OCT 12-14, 2012	Jilin, PEOPLES R CHINA	NE Dianli Univ, Shanghai Univ Elect Power		Ballast Water Treatment (BWT); Pulsed Electric Field (PEF); Thermal Pretreatment; Inactivation Mechanism	DINOFLAGELLATE CYSTS; TRANSPORT	Invasive aquatic species discharged through ship ballast water is one of the most serious problems posed nowadays in the marine environment. Inactivation effect on microalgae by combined PEF and engine waste heat pretreatment was studied. Effect factors such as pulsed voltage, electrode gap, pulse width and preheating temperature were explored, and its mechanism of inactivate the microalgae was analyzed. The results show that at the same experimental parameters, the inlet temperature of PEF treatment stage keeps at 24 degrees C, the inactivation percentage is difficult to achieve 90% unless the electric field strength rises to 22 kV/cm. Once the PEF treatment sample is preheated to 48 degrees C, the inactivation percentage will be up to 99% as the electric field strenth is just 10 kV/cm.	[Zhou Junfeng; Hu Anbang; Xie Tingfei] Shanghai Maritime Univ Shanghai, Merchant Marine Coll, Shanghai 201306, Peoples R China; [Xu Leping; Feng Daolun] Shanghai Maritime Univ Shanghai, Coll Ocean Environm & Engn, Shanghai 201306, Peoples R China	Shanghai Maritime University; Shanghai Maritime University	Zhou, JF (通讯作者)，Shanghai Maritime Univ Shanghai, Merchant Marine Coll, Shanghai 201306, Peoples R China.	jfzhou@shmtu.edu.cn; lpxu@shmtu.edu.cn; dlfeng@shmtu.edu.cn						Bax N, 2003, MAR POLICY, V27, P313, DOI 10.1016/S0308-597X(03)00041-1; 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; Hua J, 2007, OCEAN ENG, V34, P1901, DOI 10.1016/j.oceaneng.2006.09.007; Lebovka NI, 2004, J FOOD ENG, V65, P211, DOI 10.1016/j.jfoodeng.2004.01.017; McCollin T, 2007, HARMFUL ALGAE, V6, P531, DOI 10.1016/j.hal.2006.04.015; National Research Council (NRC), 1996, STEMM TID CONTR INTR; Rigby GR, 1999, MAR ECOL PROG SER, V191, P289, DOI 10.3354/meps191289; Rose P., 2005, Water and Wastewater International, V20, P27; Ruiz GM, 2000, ANNU REV ECOL SYST, V31, P481, DOI 10.1146/annurev.ecolsys.31.1.481; Su PH, 2012, ADV MATER RES-SWITZ, V356-360, P1539, DOI 10.4028/www.scientific.net/AMR.356-360.1539; Tang ZJ, 2006, MAR ENVIRON RES, V61, P410, DOI 10.1016/j.marenvres.2005.06.003; Waite TD, 2003, MAR ECOL PROG SER, V258, P51, DOI 10.3354/meps258051	13	2	2	0	16	TRANS TECH PUBLICATIONS LTD	DURNTEN-ZURICH	KREUZSTRASSE 10, 8635 DURNTEN-ZURICH, SWITZERLAND	1022-6680		978-3-03785-550-8	ADV MATER RES-SWITZ			2013	610-613		1-4				3163	+		10.4028/www.scientific.net/AMR.610-613.3163	http://dx.doi.org/10.4028/www.scientific.net/AMR.610-613.3163			2	Energy & Fuels; Engineering, Environmental; Materials Science, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Energy & Fuels; Engineering; Materials Science	BFG64					2025-03-11	WOS:000319792101242
J	Filipova-Marinova, M; Pavlov, D; Vergiev, S; Slavchev, V; Giosan, L				Filipova-Marinova, Mariana; Pavlov, Danail; Vergiev, Stoyan; Slavchev, Vladimir; Giosan, Liviu			PALAEOECOLOGY AND GEOARCHAEOLOGY OF VARNA LAKE, NORTHEASTERN BULGARIA	COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES			English	Article						pollen; dinocysts; non-pollen palynomorphs; AMS dating	VEGETATION; POLLEN	Palaeoenvironmental data from the high-resolution spore-pollen analysis of laminated sediments from newly-taken Core 3 - Varna Lake were combined with analyses of dinoflagellate cysts, acritarchs and other non-pollen palynomorphs (NPP), including fossil algal and fungal remains. The location of the core is close to submerged prehistorical sites and permits the palaeoenvironmental correlations of obtained results with available archaeological and geothronological data. The established Age Model shows that the accumulation of lake sediments started after 7870 cal. BP and is connected with a rise of the Black Sea level. One-hundred-ninety-cm-long molluskan shell hash layer of Mytilus galloprovincialis covers the interval from 7776 to 6183 cal. BP. The mixed oak and hornbeam forests dominated the vegetation cover during the Atlantic, Sub-boreal and Subatlantic chronozones of the Holocene. An important change in the forest composition occurred at ca 5598 cal. BP, when Carpinus betulus increased its spreading due to climatic changes. The high-resolution reconstruction of palaeovegetation also reveals the extent of anthropogenic influence in Varna Lake area. Two periods of significant presence of pollen from cultivated cereals, weeds and ruderals were identified. According to the available AMS-radiocarbon data, these periods are attributed to the Late Eneolithic and Early Bronze Age. The anthropogenic impact on the natural vegetation has been identified by deforestation and agricultural practice. The Transitional period without human activities between these two periods lasted ca 319 years and coincided with a rise of the Black Sea level, reflected by the increase of euryhaline marine dinoflagelate cysts and acritarchs.	[Filipova-Marinova, Mariana; Vergiev, Stoyan] Museum Nat Hist Varna, Varna 9000, Bulgaria; [Pavlov, Danail] Soc Innovat Ecologists Bulgaria, Varna 9010, Bulgaria; [Slavchev, Vladimir] Archaeol Museum Varna, Varna 9000, Bulgaria; [Giosan, Liviu] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution	Filipova-Marinova, M (通讯作者)，Museum Nat Hist Varna, 41 Maria Louisa Blvd, Varna 9000, Bulgaria.	marianafilipova@yahoo.com	Pavlov, Danail/N-7815-2013; Giosan, Liviu/F-1809-2010; Vergiev, Stoyan/E-2588-2012; Slavchev, Vladimir/G-4695-2013	Pavlov, Danail/0000-0001-7382-2054; Vergiev, Stoyan/0000-0003-4921-669X; Slavchev, Vladimir/0000-0002-6369-4527; Filipova-Marinova, Mariana/0000-0002-0786-9476	Bulgarian National Science Fund; Romanian National Authority for Scientific Research	Bulgarian National Science Fund(National Science Fund of Bulgaria); Romanian National Authority for Scientific Research	The financial support of the bilateral project "Comparative PaleoEcology and GeoArchaeology of Varna Lake (Bulgaria) and Mamaia Lake (Romania) - E.G.A.L." funded by the Bulgarian National Science Fund and the Romanian National Authority for Scientific Research is greatly acknowledged.	[Anonymous], 1995, POLLEN SPORES EUROPE; [Anonymous], 2011, TILIA 17; Bozilova E, 1998, VEG HIST ARCHAEOBOT, V7, P141, DOI 10.1007/BF01374002; Bozilova E., 1994, VEG HIST ARCHAEOBOT, V3, P143, DOI [10.1007/BF00202022, DOI 10.1007/BF00202022]; Chepalyga A, 2002, Dynamics of Terrestrial Landscape Components and Inner Marine Basins of Northern Eurasia during the Last 130.000, P170; DRAGANOV V, 1998, J H GAUL MEMORIAM, P203; Faegri K., 1989, J BIOGEOGR, V4th; Filipova M.V.F.M., 1985, ECOL MEDITERR, V11, P148, DOI DOI 10.3406/ECMED.1985.1084; Filipova-Marinova M., 2006, THESIS MUSEUM NATURA; FilipovaMarinova M., 2011, SUBMERGED PREHISTORY, P230; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Marinova E, 2006, REV PALAEOBOT PALYNO, V141, P165, DOI 10.1016/j.revpalbo.2006.03.011; Orcel A., 1991, THRACIA PONTICA, V4, P145; Reille M., 1992, POLLEN SPORES DEUROP; STUIVER M, 1993, RADIOCARBON, V35, P35, DOI 10.1017/S0033822200013801; Todorova H., 1986, Eneolithic in Bulgaria: Vth millennia BC; Todorova H., 2002, DURANKULAK, P17; VAJSOV I, 2002, DURANKULAK, V2, P159; van Geel B., 2001, TRACKING ENV CHANGE, P99, DOI DOI 10.1007/0-306-47668-1_6; Van Geel B., 1998, A Study of Non-pollen Objects in Pollen Slides (the types as described by Dr Bas Van Geel and colleagues)	20	12	12	0	4	PUBL HOUSE BULGARIAN ACAD SCI	SOFIA	ACADEMICIAN G BONCEV ST, 1113 SOFIA, BULGARIA	1310-1331			CR ACAD BULG SCI	C. R. Acad. Bulg. Sci.		2013	66	3					377	392						16	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	134FO					2025-03-11	WOS:000318196000009
J	Price, AM; Mertens, KN; Pospelova, V; Pedersen, TF; Ganeshram, RS				Price, Andrea M.; Mertens, Kenneth N.; Pospelova, Vera; Pedersen, Thomas F.; Ganeshram, Raja S.			Late Quaternary climatic and oceanographic changes in the Northeast Pacific as recorded by dinoflagellate cysts from Guaymas Basin, Gulf of California (Mexico)	PALEOCEANOGRAPHY			English	Article							SANTA-BARBARA BASIN; SURFACE SEDIMENTS; TOKYO-BAY; SEA; PRODUCTIVITY; VARIABILITY; INDICATORS; OCEAN; PRESERVATION; ASSEMBLAGES	A high-resolution record of organic-walled dinoflagellate cyst production in Guaymas Basin, Gulf of California (Mexico) reveals a complex paleoceanographic history over the last similar to 40 ka. Guaymas Basin is an excellent location to perform high resolution studies of changes in late Quaternary climate and paleo-productivity because it is characterized by high primary productivity, high sedimentation rates, and low oxygen bottom waters. These factors contribute to the deposition and preservation of laminated sediments throughout large portions of the core MD02-2515. In this study, we document dinoflagellate cyst production at a centennial to millennial scale throughout the late Quaternary. Based on the cyst assemblages, three dinoflagellate cyst zones were established and roughly correspond to Marine Isotope Stages (MISs) 1 to 3. MISs 1 and 3 are dominated by cysts of heterotrophic dinoflagellates, whereas MIS 2 is characterized by enhanced variability and a greater proportion of cysts produced by autotrophic taxa. The most dominant dinoflagellate cyst taxa found throughout the core were Brigantedinium spp. and Operculodinium centrocarpum. Dansgaard-Oeschger event 8 is observed in the dinoflagellate cyst record where it is characterized by an increase in warm taxa, such as Spiniferites pachydermus. Other intervals of interest are the Younger Dryas where warmer conditions are recorded and the Holocene which is characterized by the consistent presence of tropical species Stelladinium reidii, Tuberculodinidum vancampoae, Bitectatodinium spongium, and an increase in Quinquecuspis concreta. Changes in cyst assemblages, concentrations, and species diversity, along with geochemical data reflect major orbital to millennial-scale climatic and oceanographic changes. Citation: Price, A. M., K. N. Mertens, V. Pospelova, T. F. Pedersen, and R. S. Ganeshram (2013), Late Quaternary climatic and oceanographic changes in the Northeast Pacific as recorded by dinoflagellate cysts from Guaymas Basin, Gulf of California (Mexico), Paleoceanography, 28, 200-212, doi:10.1002/palo.20019.	[Price, Andrea M.; Pospelova, Vera; Pedersen, Thomas F.] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada; [Mertens, Kenneth N.] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Ganeshram, Raja S.] Univ Edinburgh, Grant Inst, Sch Geosci, Edinburgh, Midlothian, Scotland	University of Victoria; Ghent University; University of Edinburgh	Price, AM (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, OEASB, PO A405,Box 1700 STN CSC, Victoria, BC V8W 2Y2, Canada.	pricea@uvic.ca	Ganeshram, Raja S/JPX-5314-2023; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Mertens, Kenneth/0000-0003-2005-9483; Pospelova, Vera/0000-0003-4049-8133; Price, Andrea/0000-0002-5359-053X	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))	Funding was provided by the Natural Science and Engineering Research Council of Canada (NSERC). We would like to thank Ruth Dwyer for sampling the core (University of Edinburgh), Ellen Roosen for providing the surface sediment sample analysed in this study (Woods Hole Oceanographic Institute), Laetitia Pichevin (University of Edinburgh) and Erin McClymont (Durham University) for sharing previously published data, and Alice Chang for interesting discussions regarding geochemistry data from the core (University of British Columbia). Victoria Gray, Kirsten Kennedy, and Alanna Krepakevich are thanked for their laboratory assistance and Manuel Bringue for assistance with Figure 1 (University of Victoria). K.N.M. is a postdoctoral fellow of FWO (Belgium), who conducted this research at the University of Victoria (British Columbia, Canada). We are grateful to the Editor and anonymous reviewers for constructive feedback and insightful suggestions which greatly improved this manuscript.	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J	Asteman, IP; Nordberg, K; Filipsson, HL				Asteman, I. Polovodova; Nordberg, K.; Filipsson, H. L.			The Little Ice Age: evidence from a sediment record in Gullmar Fjord, Swedish west coast	BIOGEOSCIENCES			English	Article							NORTH-ATLANTIC OSCILLATION; MEDIEVAL WARM PERIOD; DEEP-WATER RENEWAL; BENTHIC FORAMINIFERA; OXYGEN CONCENTRATIONS; ENVIRONMENTAL-FACTORS; DINOFLAGELLATE CYSTS; CLIMATE VARIABILITY; STABLE-ISOTOPE; ORGANIC-CARBON	We discuss the climatic and environmental changes during the last millennium in NE Europe based on a ca. 8-m long high-resolved and well-dated marine sediment record from the deepest basin of Gullmar Fjord (SW Sweden). According to the Pb-210- and C-14-datings, the record includes the period of the late Holocene characterised by anomalously cold summers and well-known as the Little Ice Age (LIA). Using benthic foraminiferal stratigraphy, lithology, bulk sediment geochemistry and stable carbon isotopes we reconstruct various phases of the cold period, identify its timing in the study area and discuss the land-sea interactions occurring during that time. The onset of the LIA is indicated by an increase in cold-water foraminiferal species Adercotryma glomerata at similar to 1350 AD The first phase of the LIA was characterised by a stormy climate and higher productivity, which is indicated by a foraminiferal unit of Nonionella iridea and Cassidulina laevigata. Maximum abundances of N. iridea probably mirror a short and abrupt warming event at similar to 1600 AD. It is likely that due to land use changes in the second part of the LIA there was an increased input of terrestrial organic matter to the fjord, which is indicated by lighter delta C-13 values and an increase of detritivorous and omnivorous species such as Textularia earlandi and Eggerelloides scaber. The climate deterioration during the climax of the LIA (1675-1704 AD), as suggested by the increase of agglutinated species, presence of Hyalinea balthica, and a decline of N. iridea may have driven the decline in primary productivity during this time period.	[Asteman, I. Polovodova; Nordberg, K.] Univ Gothenburg, Dept Earth Sci, S-40530 Gothenburg, Sweden; [Filipsson, H. L.] Lund Univ, Dept Geol, S-22362 Lund, Sweden	University of Gothenburg; Lund University	Asteman, IP (通讯作者)，Univ Gothenburg, Dept Earth Sci, POB 460, S-40530 Gothenburg, Sweden.	irina.polovodova@gvc.gu.se	; Filipsson, Helena/F-7419-2011	Polovodova Asteman, Irina/0000-0001-7300-5548; Nordberg, Kjell/0000-0003-0085-4607; Filipsson, Helena/0000-0001-7200-8608	University of Gothenburg; Lamm Foundation; Swedish Research Council (VR) [621-2007-4369, 621-2005-4265, 621-2011-5090]	University of Gothenburg; Lamm Foundation; Swedish Research Council (VR)(Swedish Research Council)	The authors thank the crews of R/V Svanic, R/V Skagerak, and personally Lennart Bornmalm and Ardo Robijn (University of Gothenburg) for help with sampling. Ardo Robijn also helped with picking of C. laevigata for isotope analysis; Monika Segl (University of Bremen, Germany) ran the stable isotope measurements; Asli Oflaz and Sofia Andersson did some foraminiferal analysis, and Tim Gallagher (University of Michigan, USA) scrutinized the English of the text. The manuscript has benefitted from the valuable comments and suggestions by Elisabeth Alve (University of Oslo, Norway) and Christian Hass (Alfred Wegener Institute, Germany). The research has been supported by University of Gothenburg (a postdoctoral fellowship to IPA), the Lamm Foundation and the Swedish Research Council (VR) (grants 621-2007-4369 to KN and 621-2005-4265 & 621-2011-5090 to HLF). The full datasets discussed in this manuscript will be available online through the PANGAEA database.	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J	Orlova, TY; Morozova, TV				Orlova, T. Yu; Morozova, T. V.			Dinoflagellate cysts in recent marine sediments of the western coast of the Bering Sea	RUSSIAN JOURNAL OF MARINE BIOLOGY			English	Article						cysts; dinoflagellates; Bering Sea; Alexandrium	RESTING CYSTS; GONYAULAX-EXCAVATA; NEW-ZEALAND; RESUSPENSION EVENTS; THECA RELATIONSHIPS; NORTH-ATLANTIC; EAST-COAST; DINOPHYCEAE; ASSEMBLAGES; JAPAN	The quantitative and qualitative composition of live dinoflagellate cysts was studied in the upper two-centimeter layer of recent marine sediments that were collected at 19 stations in the coastal waters of the western Bering Sea. A total of 28 types of identified cysts belonged to the following 11 genera: Alexandrium, Diplopsalis, Ensiculifera, Gonyaulax, Gyrodinium, Pentapharsodinium, Polykrikos, Preperidinium, Protocera- tium, Protoperidinium, and Scrippsiella. The morphology of dinoflagellate cysts from recent sediments of Russian seas, such as the shape, the size, and also the structure of the phragma, including the processes and the archeopyle, was described comprehensively for the first time. Cysts of the species Gonyaulax spinifera, Pentapharsodinium dalei, Protoceratium reticulatum, Protoperidinium americanum, P. conicoides, P. subinerme, Scrippsiella crystallina, and S. trochoidea were the most widespread. Those of the potentially toxic species Alexandrium tamarense were also widely distributed and prevailed in the studied area. Their concentration varied from 0 to 25 860 cells/cm(3); the maximum concentration was recorded in Pavel Bay, Koryak Okrug, and Kamchatka.	[Orlova, T. Yu; Morozova, T. V.] Russian Acad Sci, Zhirmunsky Inst Marine Biol, Far East Branch, 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, Zhirmunsky Inst Marine Biol, Far East Branch, Vladivostok 690059, Russia.	tatiana_morozova@mail.ru	Morozova, Tatiana/G-4468-2018; Orlova, Tatiana/AAU-8448-2020	Orlova, Tatiana/0000-0002-5246-6967	Russian Foundation for Basic Research [10-04-01438a, 09-04-98570-r_vostok_a]; Far Eastern Branch of the Russian Academy of Sciences [11-III-V-06-115, 09-I-P23-12, 12-I-P30-09, 12-I-P4-02, 12-I-P28-03, 12-III-A-06-093]; World Ocean Federal Program [16.420.12.0012]; Targeted Complex Program of the Far Eastern Branch of the Russian Academy of Sciences Biological Safety of Far Eastern Seas of the Russian Federation	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Far Eastern Branch of the Russian Academy of Sciences(Russian Academy of Sciences); World Ocean Federal Program; Targeted Complex Program of the Far Eastern Branch of the Russian Academy of Sciences Biological Safety of Far Eastern Seas of the Russian Federation	This study was partially supported by the Russian Foundation for Basic Research (project no. 10-04-01438a), the Far Eastern Branch of the Russian Academy of Sciences and the Russian Foundation for Basic Research (project no. 09-04-98570-r_vostok_a), the Far Eastern Branch of the Russian Academy of Sciences (project nos. 11-III-V-06-115, 09-I-P23-12, 12-I-P30-09, 12-I-P4-02, 12-I-P28-03, and 12-III-A-06-093), the World Ocean Federal Program (contract no. 16.420.12.0012), and the Targeted Complex Program of the Far Eastern Branch of the Russian Academy of Sciences Biological Safety of Far Eastern Seas of the Russian Federation.	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J. Mar. Biol.	JAN	2013	39	1					15	29		10.1134/S1063074013010069	http://dx.doi.org/10.1134/S1063074013010069			15	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	114RX					2025-03-11	WOS:000316761200002
J	Lane, CS; Clark, JJ; Knudsen, A; McFarlin, J				Lane, Chad S.; Clark, Jeffrey J.; Knudsen, Andrew; McFarlin, Jamie			Late-Holocene paleoenvironmental history of bioluminescent Laguna Grande, Puerto Rico	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Stable isotopes; Pollen; Charcoal; Dinoflagellate; Particle size	RADIOCARBON AGE CALIBRATION; HURRICANE ACTIVITY; TROPICAL CYCLONES; ORGANIC-MATTER; ST-CROIX; RECORD; SEDIMENTS; RECONSTRUCTION; ATLANTIC; COAST	Coastal lagoons are valuable natural resources and ecotourism hotspots that are at great risk due to human development and global climate change. In order to protect these resources it is important that we fully understand the paleoenvironmental history of these unique ecosystems and their sensitivity to environmental change. Here we present a multi-proxy (pollen, charcoal, grain-size, dinoflagellate cyst, stable isotope geochemistry, and foraminifera) 3600 cal yr B.P. record of paleoenvironmental change for Laguna Grande, Puerto Rico, which is a particularly unique coastal lagoon as it contains high abundances of the bioluminescent dinoflagellate Pyrodinium bahamense. Sedimentary evidence indicates that the Laguna Grande basin began accumulating sediment similar to 3600 cal yr B.P. coincident with regional sea level rise, but the modern lagoon itself is geologically quite young and did not become fully enclosed until similar to 575 cal yr B.P. due to longshore depositional processes and mangrove swamp development. Foraminifera assemblages suggest a potential breach of a protective barrier similar to 1550 cal yr B.P. perhaps as a result of a tropical storm or tsunami and is coincident with an increase in fire activity. Only two high-energy depositional units (tempestites) could be identified in the lagoon sediments over the last 575 cal yr B.P. indicating minimal impact by tropical storms or tsunamis on the lagoon since isolation from the open ocean. Fossil dinoflagellate cyst concentrations and influxes do not approach modern levels until similar to 200 cal yr B.P. and are currently at the highest levels in the history of the lagoon, indicating the lagoon may have become bioluminescent only recently, perhaps as a result of anthropogenic nutrient additions. Sedimentation rates support this hypothesis indicating a recent tripling of sedimentation rates when compared to millennial-scale sedimentation rates. This study highlights. the utility of paleolimnological data in the management and preservation of at-risk coastal lagoon ecosystems. (C) 2012 Elsevier B.V. All rights reserved.	[Lane, Chad S.] Univ N Carolina, Dept Geog & Geol, Wilmington, NC 28403 USA; [Clark, Jeffrey J.; Knudsen, Andrew; McFarlin, Jamie] Lawrence Univ, Dept Geol, Appleton, WI 54911 USA	University of North Carolina; University of North Carolina Wilmington; Lawrence University	Lane, CS (通讯作者)，Univ N Carolina, Dept Geog & Geol, Wilmington, NC 28403 USA.	lanec@uncw.edu		McFarlin, Jamie/0000-0002-8185-8185; Lane, Chad/0000-0001-8934-5379	LU Department of Geology; UNCW College of Arts and Sciences	LU Department of Geology; UNCW College of Arts and Sciences	We thank the LU Department of Geology and UNCW College of Arts and Sciences for funding this research. Logistical support and site access were kindly provided by administrators of the Las Cabezas de San Juan Nature Preserve. And last, but certainly not least, we thank and applaud the efforts of the Lawrence University Geology 427 and 550 students who assisted in the recovery of this sediment core and with proxy analyses.	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Paleoclimatol. Paleoecol.	JAN 1	2013	369						99	113		10.1016/j.palaeo.2012.10.007	http://dx.doi.org/10.1016/j.palaeo.2012.10.007			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	092MR					2025-03-11	WOS:000315127200009
J	Liu, DY; Shen, XH; Di, BP; Shi, YJ; Keesing, JK; Wang, YJ; Wang, YQ				Liu, Dongyan; Shen, Xuhong; Di, Baoping; Shi, Yajun; Keesing, John K.; Wang, Yujue; Wang, Yueqi			Palaeoecological analysis of phytoplankton regime shifts in response to coastal eutrophication	MARINE ECOLOGY PROGRESS SERIES			English	Article						Palaeoecology; Eutrophication; Diatom; Dinoflagellate; Biomarkers	HARMFUL ALGAL BLOOMS; ECOSYSTEM STRUCTURE; CHESAPEAKE BAY; SISHILI BAY; YELLOW SEA; EAST CHINA; LAND-USE; DIATOM; NUTRIENTS; STEROLS	We used a multiple-proxy palaeoecological method to reconstruct a 100 yr time series showing coastal eutrophic processes and phytoplankton responses. Total organic carbon, total nitrogen, diatom frustules, dinoflagellate cysts, brassicasterol and dinosterol were extracted from chronologic sediment cores in Sishili Bay, a polluted area in China. The cores showed that eutrophication occurred during about 1975 to 1985, which corresponds to increased human activity associated with China's economic development since 1978. During eutrophication, the biomass of diatoms and dinoflagellates increased, and dominant species shifted abruptly. The small, heavily silicified diatoms Cyclotella stylorum and Paralia sulcata gradually took the place of the large dominant diatom Coscinodiscus radiatus, while dinoflagellates displayed a progressive in crease since 1975. Compared to changes in temperature and rainfall during 1950 to 2010, increased fertilizer use, marine aquaculture and sewage discharge showed a better match to the increasing trend in biomass, species shift and nutrient concentration. Altered nutrient supply ratios caused by increased nitrogen inputs play an important role in the shifts in diatom and dinoflagellate assemblages.	[Liu, Dongyan; Shen, Xuhong; Di, Baoping; Shi, Yajun; Keesing, John K.; Wang, Yujue; Wang, Yueqi] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Key Lab Coastal Zone Environm Proc, Shandong Prov Key Lab Coastal Zone Environm Proc, Yantai 264003, Shandong, Peoples R China; [Shen, Xuhong; Wang, Yueqi] Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China; [Keesing, John K.] CSIRO Wealth Oceans Natl Res Flagship, Wembley, WA 6913, Australia	Chinese Academy of Sciences; Yantai Institute of Coastal Zone Research, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Commonwealth Scientific & Industrial Research Organisation (CSIRO)	Liu, DY (通讯作者)，Chinese Acad Sci, Yantai Inst Coastal Zone Res, Key Lab Coastal Zone Environm Proc, Shandong Prov Key Lab Coastal Zone Environm Proc, Yantai 264003, Shandong, Peoples R China.	dyliu@yic.ac.cn	Shi, Yajun/GPS-8969-2022; Keesing, John/B-1955-2009	Keesing, John/0000-0002-0876-2144; Shen, Xuhong/0000-0002-7886-1586	Chinese Academy of Sciences Innovative Programme [KZCX2-YW-Q07-04]; Natural Science Foundation of China [40976097]	Chinese Academy of Sciences Innovative Programme; Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank Y. Chen at YIC-CAS and Q. Sun at China East Normal University for assistance during sample analysis. The study was funded by the Chinese Academy of Sciences Innovative Programme (No. KZCX2-YW-Q07-04) and the Natural Science Foundation of China (No. 40976097).	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Ser.		2013	475						1	14		10.3354/meps10234	http://dx.doi.org/10.3354/meps10234			14	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	089UH		Bronze			2025-03-11	WOS:000314935000001
J	Persson, A; Smith, BC; Wikfors, GH; Alix, JH				Persson, Agneta; Smith, Barry C.; Wikfors, Gary H.; Alix, Jennifer H.			Differences in swimming pattern between life cycle stages of the toxic dinoflagellate <i>Alexandrium fundyense</i>	HARMFUL ALGAE			English	Article						Alexandrium fundyense; Behavior; Bloom; Dinoflagellate; Gamete; Mating; Motion; Swimming; Zygote	MARINE DINOFLAGELLATE; DINOPHYCEAE; ENCYSTMENT; MOTILITY; SPEED	Different life stages of Alexandrium fundyense have different swimming behavior; gametes often are said to "swarm" or "dance" before mating. This behavior was studied, and quantitative measures of these motility patterns in two-dimensions were generated using motion-analysis software applied to video records of individual-cell movements. Behavior, swimming patterns, and growth were studied in two strains of A. fundyense and compared in encystment medium and growth medium. Vegetative cells swam straight, rotating around the apical axis until they hit something and then swam straight in a different direction. Gamete swimming behavior was slower and characterized by frequent direction changes and circular motion. Gametes contacted other cells frequently (>5 cell contacts min(-1) cell(-1)). Zygotes swam slowly when newly formed and later became nearly immobile; these cells continued to contact other cells and also surfaces. The results are in accordance with field observations of long swimming distances for vegetative cells, accumulation in thin layers of gametes, and sinking of developing resting cysts attached to marine snow for zygotes. (C) 2012 Elsevier B.V. All rights reserved.	[Persson, Agneta] Univ Gothenburg, Dept Biol & Environm Sci, SE-40530 Gothenburg, Sweden; [Smith, Barry C.; Wikfors, Gary H.; Alix, Jennifer H.] NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT USA	University of Gothenburg; National Oceanic Atmospheric Admin (NOAA) - USA	Persson, A (通讯作者)，Smedjebacksvagen 13, SE-77190 Ludvika, Sweden.	agnetapersson77@gmail.com		Persson, Agneta/0000-0003-0202-6514	Oscar and Lili Lamm Foundation for Scientific Research; Magnus Bergvall Foundation; Wilhelm and Martina Lundgren Scientific Foundation	Oscar and Lili Lamm Foundation for Scientific Research; Magnus Bergvall Foundation; Wilhelm and Martina Lundgren Scientific Foundation	The research was funded by the Oscar and Lili Lamm Foundation for Scientific Research, the Magnus Bergvall Foundation, and the Wilhelm and Martina Lundgren Scientific Foundation. The authors also wish to thank Paul A. Blaszka for translating video clips and Hayley Skelton Flores for measuring advice. We are grateful to the anonymous reviewers for valuable comments on the earlier version of the manuscript. Mention of trade names does not imply endorsement. 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B	De Schepper, S		Lewis, JM; Marret, F; Bradley, LR		De Schepper, Stijn			Combining dinoflagellate cyst studies with geochemical proxies: application to palaeoceanography, palaeoecology and biostratigraphy	BIOLOGICAL AND GEOLOGICAL PERSPECTIVES OF DINOFLAGELLATES	Micropaleaeontological Society Special Publications		English	Article; Book Chapter							SEA-SURFACE TEMPERATURE; NORTHERN-HEMISPHERE GLACIATIONS; MID-PLIOCENE; PLANKTONIC-FORAMINIFERA; ATLANTIC OCEAN; CLIMATE; ICE; MG/CA; ASSEMBLAGES; GREENHOUSE	This paper highlights the potential of combining (organic) geochemical proxies with dinoflagellate cyst studies. Firstly, such a multiproxy approach is a powerful tool for palaeoceanography and for providing insights into the natural variability of the climate system in the past. Geochemical proxies have the advantage of providing absolute estimates for environmental variables, but the importance of assemblage studies is especially highlighted here because fossil assemblages are excellent indicators of large-scale changes in surface water masses such as shifts of ocean currents. Secondly, the geochemical proxies can also be exploited to determine the environmental preferences of individual species. Until now, only the temperature preference of extant and extinct dinoflagellate cyst species in fossil assemblages has been investigated by comparing them directly to geochemical proxy. Finally, an integrated geochemical and palynological approach is useful for biostratigraphy because it can improve the existing biozonations, provide chronostratigraphic calibration and/or aid in identifying stage boundaries.	Univ Bergen, Dept Earth Sci, N-5020 Bergen, Norway	University of Bergen	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				Anand P, 2003, PALEOCEANOGRAPHY, V18, DOI 10.1029/2002PA000846; [Anonymous], 9 INT C MOD FOSS DIN; [Anonymous], AASP CONTRIBUTION A; [Anonymous], PALEOCEANOGRAPHY; [Anonymous], CLIM CHANG 2007; [Anonymous], 61 NOAA ATL NESDIS; [Anonymous], GEOCHEMISTRY GEOPHYS; Bartoli G, 2011, PALEOCEANOGRAPHY, V26, DOI 10.1029/2010PA002055; Beerling DJ, 2011, NAT GEOSCI, V4, P418, DOI 10.1038/ngeo1186; Belt ST, 2007, ORG GEOCHEM, V38, P16, DOI 10.1016/j.orggeochem.2006.09.013; Bonnet S, 2012, MAR MICROPALEONTOL, V84-85, P87, DOI 10.1016/j.marmicro.2011.11.006; Bonnet S, 2010, MAR MICROPALEONTOL, V74, P59, DOI 10.1016/j.marmicro.2009.12.001; BRASSELL SC, 1986, NATURE, V320, P129, DOI 10.1038/320129a0; Brinkhuis H, 2006, NATURE, V441, P606, DOI 10.1038/nature04692; 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Microbiology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Microbiology; Paleontology	BA1FO					2025-03-11	WOS:000332424500004
J	Willumsen, PS; Filipsson, HL; Reinholdsson, M; Lenz, C				Willumsen, Pi Suhr; Filipsson, Helena L.; Reinholdsson, Maja; Lenz, Conny			Surface salinity and nutrient variations during the Littorina Stage in the Faro Deep, Baltic Sea	BOREAS			English	Article							EEMIAN HYDROGRAPHIC CONDITIONS; DINOFLAGELLATE CYST RECORD; HOLOCENE HISTORY; KOLJO FJORD; WEST-COAST; SEDIMENTS; CLIMATE; EUROPE; SWEDEN	Willumsen, P. S., Filipsson, H. L., Reinholdsson, M. & Lenz, C. 2013 (January): Surface salinity and nutrient variations during the Littorina Stage in the Faro Deep, Baltic Sea. Boreas, Vol. 42, pp. 210-223. 10.1111/j.15023885.2012.00286.x. ISSN 0300-9483. Early to late Holocene sediments from core F80, Faro Deep, Baltic Sea, are investigated for their palynomorph composition and dinoflagellate cyst record to map variations in sea-surface-water salinity and palaeoproductivity during the past 6000 years. The F80 palynomorph assemblages are subdivided into four Assemblage Zones (AZs) named A to D. The transition from the stratigraphically oldest AZ A to B reflects a marked increase in palaeoproductivity and a gradual increase in surface-water salinity over the similar to 1500 years between the Initial Littorina (former Mastogloia Sea Stage) and Littorina Sea Stage. A period with maximum sea-surface salinity is recorded within the overlying AZ C from 7200 to 5200 cal. a BP, where the process length of Operculodinium centrocarpum indicates that average salinities were probably the highest (similar to 15-17 versus 7.5 psu today) since the last glaciation. The change from AZ C to D correlates with a shift from laminated to non-laminated sediments, and the dinoflagellate cyst assemblages suggest that the surface-and the deep-water environment altered from c. 5250 cal. a BP, with less productivity in the surface water and more oxygenated conditions in the deep water. Here we demonstrate that past regional changes in surface salinity, primary productivity and deep-water oxygenation status in the Baltic Sea can be traced by mapping overall palynomorph composition, dinoflagellate cyst assemblages and variations in the process length of O. centrocarpum in relation to periods of laminated/non-laminated sedimentation and proportion of organic-matter in the sediments. An understanding of past productivity changes is particularly important to better understand present-day environmental changes within the Baltic Sea region.	[Willumsen, Pi Suhr; Filipsson, Helena L.; Reinholdsson, Maja; Lenz, Conny] 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; helena.filipsson@geol.lu.se; Maja.Reinholdsson@geol.lu.se; Conny.Lenz@geol.lu.se	Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608	Linnaeus environment: Lund University Centre for studies of the Carbon Cycle and Climate Interactions (LUCCI) [156309]; Swedish Research Council (VR) [621-2005-4265]; Crafoord Foundation; FORMAS	Linnaeus environment: Lund University Centre for studies of the Carbon Cycle and Climate Interactions (LUCCI); Swedish Research Council (VR)(Swedish Research Council); Crafoord Foundation; FORMAS(Swedish Research Council Formas)	The authors thank the crew of the RV 'Aranda' for their assistance in collecting the core. The study was financed by the Linnaeus environment: Lund University Centre for studies of the Carbon Cycle and Climate Interactions (LUCCI) (RI3 grant no. 156309 to PSW), the Swedish Research Council (VR grant no. 621-2005-4265; HLF), the Crafoord Foundation (HLF, PSW) and the FORMAS-funded strong research environment Managing Multiple Stressors in the Baltic Sea (HLF). The authors are grateful to Professor D. Conley and Professor R. Harland for their fruitful comments on an earlier version of the manuscript. Professor M. Ellegaard (Copenhagen University) is thanked for her assistance during SEM studies of the palynomorph assemblages. Thanks to the reviewers Professor M. J. Head and Dr K. N. Mertens for their constructive advice that considerably improved this paper.	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J	Gedl, P				Gedl, Przemyslaw			Dinoflagellate cysts from the Szlachtowa Formation (Jurassic) and adjacent deposits (Jurassic Cretaceous) of the Grajcarek Unit at Szczawnica-Zabaniszcze (Pieniny Klippen Belt, Carpathians, Poland)	GEOLOGICAL QUARTERLY			English	Article						Szlachtowa Formation; "black flysch"; biostratigraphy; Jurassic; Cretaceous; Pieniny Klippen Belt	BLACK FLYSCH; OUTER CARPATHIANS; BAJOCIAN; FRANCE; AGE	The Jurassic Cretaceous fine-clastic dark deposits of the Grajcarek Unit (Pieniny Klippen Belt, Carpathians, Poland) show lithological similarities, which may lead to erroneous age correlations. Their well-exposed outcrop at Szczawnica-Zabaniszcze allows detailed sampling for their precise age determination. For this purpose, dinoflagellate cysts have been studied from a set of samples collected from the Szlachtowa, Opaleniec, Pieniny Limestone, Kapusnica and Wronine formations exposed at that site (additional sample from the Pieniny Limestone Formation was studied). The Szlachtowa Formation, a very characteristic lithostratigraphic unit, which consists of black shale and sandstones extremely rich in mica flakes, occasionally referred to literature as the so-called "black flysch", yielded rich and well-preserved assemblages. Their age is Middle Jurassic, spanning the Aalenian to Lower Bajocian. The exposures of the Szlachtowa Formation at Szczawnica-Zabaniszcze are located close to the outcrops of the Opaleniec Formation. The calcareous spotted shale from this lithostratigraphic unit yielded rich dinoflagellate cyst assemblage characteristic for Late Bathonian (Early Callovian?). The Opaleniec Formation tectonically contacts with very similar non-calcareous spotted shale of the Wronine Formation. Its age, based on infrequent dinoflagellate cysts is Aptian - Albian. Similar, Lower Aptian age was concluded for the Kapuenica Formation. Late Barremian - earliest Aptian dinoflagellate cysts have been found in the underlying topmost part of the Pieniny Limestone Formation.	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						Andrusov D., 1938, ROZPRAVY STA TNIHO U, V9, P1; ANDRUSOV D, 1929, VESTNIK STATNIHO GEO, V5, P327; [Anonymous], 2012, MINER SLOV; Barski M, 2012, GEOL Q, V56, P391, DOI 10.7306/gq.1030; BIRKENMAJER K, 1977, Acta Geologica Polonica, V27, P387; Birkenmajer K., 1968, Acta Geologica Polonica, V18, P325; Birkenmajer K., 1963, Bulletin de l'Academie Polonaise des Sciences Ser Sci Geol Geogr, V11, P127; Birkenmajer K., 1986, STUDIA GEOLOGICA POL, V88, P7; BIRKENMAJER K, 1979, WYDAWNICTWA GEOL; BIRKENMAJER K, 1970, STUDIA GEOLOGICA POL, V61, P7; Birkenmajer K., 1996, STUD GEOL POL, V109, P7; Birkenmajer K., 1977, Stud. Geol. 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Pol. Tow. Geol, V4, P221; Skupien Petr, 2003, Bulletin of Geosciences, V78, P67; STOVER LE, 1996, AM ASS STRATIGRAPHIC, V2, P641; Torricelli S, 2000, REV PALAEOBOT PALYNO, V108, P213, DOI 10.1016/S0034-6667(99)00041-X; Uhlig V., 1890, Jahrb. Geol. Reichanst, V40, P559; Wille W., 1979, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V158, P221	53	10	10	0	4	POLISH GEOLOGICAL INST	WARSAW	RAKOWIECKA 4, BLDG A, ROOM 434, PL-00-975 WARSAW, POLAND	1641-7291	2082-5099		GEOL Q	Geol. Q.		2013	57	3					485	502		10.7306/gq.1106	http://dx.doi.org/10.7306/gq.1106			18	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	227NM		Bronze			2025-03-11	WOS:000325120600009
C	Jenhani, AB; Fathalli, A; Romdhane, MS		Ozhan, E		Jenhani, Amel Ben Rejeb; Fathalli, Afef; Romdhane, Mohamed Salah			Dinoflagellate Cysts in the Gulf of Gabes (Tunisia)	GLOBAL CONGRESS ON ICM: LESSONS LEARNED TO ADDRESS NEW CHALLENGES, VOLS. 1 AND 2			English	Proceedings Paper	Global Congress on Integrated Coastal Management (ICM) - Lessons Learned to Address New Challenges	OCT 30-NOV 03, 2013	Marmaris, TURKEY	Mediterranean Coastal Fdn, Int EMECS Ctr, Mugla Sitki Kocman Univ, Republ Turkey Promot Fund, Asia Pacific Network Global Change Res, Springer Sci Business Media, PEGASO FP7 Project, MARLISCO FP7 Project			RESTING STAGES; EUTROPHICATION; PHYTOPLANKTON; BAY; PLANKTON; RECORDS; SUMMER	In marine areas, several planktonic species produce resting stages as part of their life cycle. In confined basins, usually characterised by low hydrodynamic conditions and high productivity, cysts produced in the water column sink to the sediments where they may remain viable for many years, constituting a reservoir of potential biodiversity. Dinoflagellate species are capable of forming dormant cysts. The analysis of these resting forms leads to a better consideration of rare species in the water column and to improve knowledge of planktonic biodiversity. In this context, a study was conducted, through two field campaigns in 2010, touching the four commercial ports situated in the Gulf of Gabes namely the ports of Sfax, Skhira Gabes and Zarzis. Thus, the search for Dinophyceae rest forms was resulted in the identification of 37 cysts taxa that can be added to the list of plankton species, and from which 17 were not found in their active form. Furthermore, the surface sediments of the Sfax, Skhira, Gabes and Zarzis harbour areas were characterized, respectively, by the presence of 16, 18, 18 and 13 cysts taxa, belonging to the orders, Gymnodiniales, Prorocentrales, Gonyaulacales and Peridiniales. The two latters represented the most dominant groups. Among the non-indigenous species in the Mediterranean sea we identified in this work, 6 encysted forms including those of the five potentially toxic species Gymnodinium catenatum, Karenia selliformis, Alexandrium minutum and Protoceratium reticulatum. The two encysted forms of Gymnodinium cf impudicum and Ensiculifera cf carinata were reported for the first time in Gulf of Gabes. The highest density cyst was mainly observed in the Zarzis port area (660 cysts g(-1) DW sediment). It was generated by the alien species Scrippsiella trochoida.	[Jenhani, Amel Ben Rejeb; Fathalli, Afef; Romdhane, Mohamed Salah] Univ Carthage, URA, INAT, Tunis 1082, Tunisia	Universite de Carthage	Jenhani, AB (通讯作者)，Univ Carthage, URA, INAT, Tunis 1082, Tunisia.	jenhani.amel@gmail.com; fathalli_afef@yaho.fr; ramadhanms@gmail.com	Romdhane, Mohamed Salah/GTB-5864-2022					Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; [Anonymous], 1993, SPEC PUBL NUMBER; [Anonymous], ANN STAT; Ben Amor O., 2006, P 8 C INT LIMN EXPR, P44; Ben Ismail S, 2012, DEEP-SEA RES PT I, V63, P65, DOI 10.1016/j.dsr.2011.12.009; 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; Drira Z, 2008, SCI MAR, V72, P59; Glibert Patricia M., 2005, Oceanography, V18, P198; Gomez Fernando, 2003, Acta Botanica Croatica, V62, P65; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hattour A., 1995, RAPP COMM INT MER ME, V34, P33; Head MJ., 1996, PALYNOLOGY, V3, P197; Hesse KJ, 1995, OLSEN INT S, P11; Marchand M., 2009, PROGRAMME DESECO IFR; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Matsuoka K, 2000, WESTPAC HAB WESTPAC; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; Mezghani-Chaari S, 2011, ENVIRON MONIT ASSESS, V180, P477, DOI 10.1007/s10661-010-1800-1; Moscatello S, 2004, SCI MAR, V68, P85, DOI 10.3989/scimar.2004.68s185; Mudie PJ, 2002, PALAEOGEOGR PALAEOCL, V180, P159, DOI 10.1016/S0031-0182(01)00427-8; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Rekik A, 2012, MAR POLLUT BULL, V64, P336, DOI 10.1016/j.marpolbul.2011.11.005; Rubino F, 2009, J MARINE SYST, V78, P536, DOI 10.1016/j.jmarsys.2008.12.023; Rubino F, 2000, MAR ECOL-P S Z N I, V21, P263, DOI 10.1046/j.1439-0485.2000.00725.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; Shin HH, 2010, MAR MICROPALEONTOL, V77, P15, DOI 10.1016/j.marmicro.2010.07.001; Shin HH, 2010, MAR POLLUT BULL, V60, P1243, DOI 10.1016/j.marpolbul.2010.03.019; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Yahia-Kéfi OD, 2005, MEDITERR MAR SCI, V6, P17, DOI 10.12681/mms.190	34	0	0	0	5	MEDITERRANEAN COASTAL FOUNDATION-MEDCOAST FOUNDATION	AKYAKA	CATALCAM CAD NO 52, AKYAKA, MUGLA 48650, TURKEY			978-605-88990-9-4				2013							737	747						11	Ecology; Marine & Freshwater Biology; Water Resources	Conference Proceedings Citation Index - Science (CPCI-S)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Water Resources	BI2UA					2025-03-11	WOS:000410345100072
J	Thakur, OP; Sarkar, S; Dogra, NN				Thakur, O. P.; Sarkar, Samir; Dogra, N. N.			A Late Maastrichtian palynofloral assemblage from Nahan area of Himachal Pradesh, India: palaeoenvironmental and age implications	HIMALAYAN GEOLOGY			English	Article						Palynoflora; Late Maastrichtian; Nahan; Lesser Himalaya; India		The paper deals with a fairly rich palynofloral assemblage from the basal part of the Kakara-Subathu succession exposed near Nahan, Sirmaur District, Himachal Pradesh, India. The assemblage consists of 30 genera and 33 species of dinoflagellate cysts, bryophytic and pteridophytic spores, gymnospermous and angiospermous pollen, and fungal spores and ascostromata. Dominant palynotaxa recorded in the palynoflora are: Dinogymnium, Fusiformacysta, Fibrocysta, Polysphaeridium, Schizosporis, Rouseisporites, Osmundacidites, Cicatricosisporites, Monocolpites, Araucariacites, Palmidites and Protocolletotrichum. Recorded palynotaxa suggest a Late Maastrichtian age for this assemblage. The present investigation has also provided palynological confirmation of the presence of Late Cretaceous sediments in the Lesser Himalaya of Himachal Pradesh. It also supports the earlier view on the probable occurrence of a Late Cretaceous transgressive event along the Lesser Himalayan rift zone. The abundance of fungal spores and ascostromata in the assemblage indicates the prevalence of a tropical humid climate during the deposition of these sediments.	[Thakur, O. P.; Dogra, N. N.] Kurukshetra Univ, Dept Geol, Kurukshetra 136119, Haryana, India; [Sarkar, Samir] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Kurukshetra University; 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		Thakur, Om Prakash/0000-0001-9034-5261; Dogra, N.N./0000-0002-5907-4763				Auden J. B., 1937, Records Geological Survey of India, V71, P407; Bak K., 1998, STUDIA GEOLOGICA POL, V13, P7; BATRA RS, 1989, J GEOL SOC INDIA, V33, P503; Bhatia S.B., 2005, J PALAEONTOLOGICAL S, V2, P105; BHATIA SB, 1980, STRATIGRAPHY CORRELA, P79; BRENNER W, 1994, REV PALAEOBOT PALYNO, V80, P209, DOI 10.1016/0034-6667(94)90002-7; DETTMANN M.E., 1963, P ROY SOC VICTORIA, V77, P1; Eren M, 1999, INT J EARTH SCI, V88, P593, DOI 10.1007/s005310050287; Evitt W.R., 1967, STANFORD U PUBLICATI, V10, P36; Frederiksen N., 1983, Contributions Series, V12, P32; Gupta A., 1986, BRYOPHYTORUM BIBLIOT, V29, P1; Jafar S.A., 1988, Palaeobotanist (Lucknow), V37, P115; JAFAR SA, 1992, CURR SCI INDIA, V62, P409; Juyal KP, 2009, CURR SCI INDIA, V96, P1308; Juyal K.P., 1990, J HIMALAYAN GEOLOGY, V1, P209; Kapoor R., 1997, B INDIAN GEOLOGICAL, V30, P31; Khanna A.K., 1979, Himalayan Geology, V8, P209; Kumar Kishor, 1996, P493; Martin-Closas C., 2003, Geologica Acta, V1, P315; Mathur N.S., 1998, WORKSH HIM FOR BAS S, P44; Mathur N.S., 1978, RECENT RES GEOLOGY, V5, P96; Mathur N.S., 1977, Bulletin Indian Geologists Association, V10, P21; Mathur NS, 2000, WIHG MONOGRAPH SERIE, V1; SARKAR S, 1991, REV PALAEOBOT PALYNO, V67, P1, DOI 10.1016/0034-6667(91)90013-S; Sarkar S., 1988, GEOL MIJNBOUW, V55, P179; Sarkar Samir, 2000, Journal of the Palaeontological Society of India, V45, P137; Sarkar Samir, 2000, Himalayan Geology, V21, P167; SINGH P, 1980, CURR SCI INDIA, V49, P255; Srikantia S.V., 1967, B GEOLOGICAL SOC IND, V1, P114; SRIKANTIA SV, 1970, J GEOL SOC INDIA, V11, P185; Valdiya K.S., 1980, GEOLOGY KUMAON LESSE; Wang CS, 2005, CRETACEOUS RES, V26, P21, DOI 10.1016/j.cretres.2004.11.010	32	1	1	0	0	WADIA INST HIMALAYAN GEOLOGY	DEHRA DUN	33 GENERAL MAHADEO SINGH RD, DEHRA DUN, 248 001, INDIA	0971-8966			HIMAL GEOL	Himal. Geol.		2013	34	2					148	157						10	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	V40CZ					2025-03-11	WOS:000209458000006
J	Radi, T; Bonnet, S; Cormier, MA; de Vernal, A; Durantou, L; Faubert, É; Head, MJ; Henry, M; Pospelova, V; Rochon, A; Van Nieuwenhove, N				Radi, Taoufik; Bonnet, Sophie; Cormier, Marc-Andre; de Vernal, Anne; Durantou, Lise; Faubert, Etienne; Head, Martin J.; Henry, Maryse; Pospelova, Vera; Rochon, Andre; Van Nieuwenhove, Nicolas			Operational taxonomy and (paleo-)autecology of round, brown, spiny dinoflagellate cysts from the Quaternary of high northern latitudes	MARINE MICROPALEONTOLOGY			English	Article						round brown spiny cysts; Echinidinium; Islandinium; determination key; taxonomy; paleoecology	SEA-SURFACE CONDITIONS; EEMIAN HYDROGRAPHIC CONDITIONS; ORGANIC-WALLED MICROFOSSILS; SPATIAL-DISTRIBUTION; MARINE ENVIRONMENTS; ESTUARINE SEDIMENTS; BRITISH-COLUMBIA; BALTIC SEA; PRODUCTIVITY; ASSEMBLAGES	Round brown spiny dinoflagellate cysts from high latitudes of the Northern Hemisphere have been examined in order to define criteria for their determination during routine counts. The round brown spiny cysts belong to several taxa including the paleontological genera Echinidinium and Islandinium and the biological genera Oblea, Polykrikos, and Protoperidinium. Here, we present a synthesis of descriptions with remarks on the morphology, taxonomy, nomenclature and ecology of cysts from the observations of samples collected in high latitude environments. These observations have led us to establish a practical identification key based on the most distinct morphological features that characterize all specimens. These features exclude the archeopyle, which is rarely observed. Two new cyst types are described from Holocene and Pleistocene sediments of the North Pacific and North Atlantic oceans, respectively. The identification key permits the following to be distinguished: "Echinidinium aculeatum", Echinidinium delicatum, Echinidinium granulatum, Echinidinium karaense, Echinidinium sleipnerensis, Echinidinium "transparantum"/zonneveldiae, Islandinium brevispinosum, Islandinium? cezare, and Islandinium minutum, the cysts of Oblea acanthocysta and Polykrikos hartmannii (al. Pheopolykrikos hartmannii), and the new cyst types Echinidinium? sp. A and Echinidinium? sp. B. (C) 2012 Elsevier B.V. All rights reserved.	[Radi, Taoufik] McGill Univ, Montreal, PQ H3A 2A7, Canada; [Radi, Taoufik; Bonnet, Sophie; Cormier, Marc-Andre; de Vernal, Anne; Henry, Maryse; Van Nieuwenhove, Nicolas] Univ Quebec, GEOTOP UQAM McGill, Montreal, PQ H3C 3P8, Canada; [Durantou, Lise; Faubert, Etienne; Rochon, Andre] Univ Quebec, GEOTOP ISMER UQAR, Rimouski, PQ G5L 3A1, Canada; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8P5C2, Canada; [Van Nieuwenhove, Nicolas] Helmholtz Ctr Ocean Res Kiel, GEOMAR, D-24148 Kiel, Germany	University of Quebec; University of Quebec Montreal; University of Quebec; Brock University; University of Victoria; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Radi, T (通讯作者)，McGill Univ, 3450 Univ St, Montreal, PQ H3A 2A7, Canada.	radi.taoufik@courrier.uqam.ca	Van Nieuwenhove, Nicolas/IAQ-1532-2023; de Vernal, Anne/D-5602-2013	Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Pospelova, Vera/0000-0003-4049-8133; Cormier, Marc-Andre, Francis/0000-0001-7645-1375; de Vernal, Anne/0000-0001-5656-724X	Natural Sciences and Engineering Research Council of Canada (NSERC); Fonds de la Recherche sur la Nature et les technologies of Quebec (FQRNT)	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds de la Recherche sur la Nature et les technologies of Quebec (FQRNT)	We thank the Integrated Ocean Drilling Program (IODP), the international Innovative North Pacific Experiment project (INOPEX), and the MALINA project for providing us with sedimentary samples. NV is grateful to J. Matthiessen (AWI) for help in identifying the cyst Echnidinium sp. A. Financial support from the Natural Sciences and Engineering Research Council of Canada (NSERC) and from the Fonds de la Recherche sur la Nature et les technologies of Quebec (FQRNT) is acknowledged. We are most grateful to K. Matsuoka for supplying photographs of Polykrikos hartmannii, and to the reviewers for their constructive criticism.	Abe T. 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Micropaleontol.	JAN	2013	98						41	57		10.1016/j.marmicro.2012.11.001	http://dx.doi.org/10.1016/j.marmicro.2012.11.001			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	091QG					2025-03-11	WOS:000315064300004
J	Akgün, F; Akkiraz, MS; Üçbas, SD; Bozcu, M; Yesilyurt, SK; Bozcu, A				Akgun, Funda; Akkiraz, Mehmet Serkan; Ucbas, Sariye Duygu; Bozcu, Mustafa; Yesilyurt, Sevinc Kapan; Bozcu, Ayse			Oligocene vegetation and climate characteristics in north-west Turkey: data from the south-western part of the Thrace Basin	TURKISH JOURNAL OF EARTH SCIENCES			English	Article						Oligocene; mangrove; palaeoecology; Thrace basin; north-west Turkey	EARLY-MIDDLE MIOCENE; PALEOENVIRONMENTAL SIGNIFICANCE; LARGER FORAMINIFERA; SHALLOW-MARINE; EOCENE; EVOLUTION; PALEOECOLOGY; STRATIGRAPHY; PARATETHYS; TERTIARY	In this paper we present the first palynomorph and mollusc assemblages from the sediments in three different sections. From east to west, these are the Sevketiye (northern Biga Peninsula), the Tayfur (Gelibolu Peninsula) and the Kuzu harbour (Gokceada) (parts of the Danismen Formation) sections in the south and south-western side of the Thrace Basin (north-west Turkey), with the aim of obtaining information about the composition and structure of vegetation and climate during the Oligocene. The stratigraphic interval extends from late Rupelian to Chattian. The Danismen Formation in the Sevketiye section yielded a palynomorph association with abundant coastal palms (Arecaceae; Lepidocaryoidae), and mangrove pollen (Pelliciera). A similar assemblage from the Kuzu harbour section was also obtained, with minor contributions of mangrove elements Nypa and Acrostichum aureum, Arecaceae type palm, undifferentiated dinoflagellate cysts and microforaminiferal linings. These palynomorph assemblages, combined with the mollusc data, indicate that low-lying coastal environments prevailed. In contrast, the palynomorphs from the Tayfur section represent a non-marine environment lacking mangrove elements, palm trees, dinoflagellate cysts and microforaminiferal linings. The diversity of angiosperm taxa in the Tayfur palynoflora, which form the bulk of the assemblage, indicates terrestrial vegetation. Quantitative palaeoclimate analyses are based on the Coexistence Approach method, and yield over 22 degrees C at the coast as indicated by mangrove elements and palms in the Sevketiye and Kuzu harbour palynofloras. For the Tayfur palynoflora, mean annual temperature ranged between 16.5 and 21.3 degrees C. This indicates a climate cooling, corresponding to the transition from Rupelian to Chattian, and resulted in the pollen changes from mangrove bearing coastal deposits to more inland vegetation.	[Akgun, Funda] Dokuz Eylul Univ, Dept Geol Engn, Izmir, Turkey; [Akkiraz, Mehmet Serkan; Ucbas, Sariye Duygu] Dumlupinar Univ, Dept Geol Engn, Kutahya, Turkey; [Bozcu, Mustafa; Yesilyurt, Sevinc Kapan; Bozcu, Ayse] Canakkale Onsekiz Mart Univ, Dept Geol Engn, Canakkale, Turkey	Dokuz Eylul University; Dumlupinar University; Canakkale Onsekiz Mart University	Akgün, F (通讯作者)，Dokuz Eylul Univ, Dept Geol Engn, Izmir, Turkey.	funda.akgun@deu.edu.tr	akkiraz, mehmet/ADP-2366-2022; Akgün, Funda/AAC-2859-2020; Yeşilyurt, Sevinç/HPH-2713-2023; Durak, Sariye/JJE-8836-2023; YESILYURT, Sevinc/L-5778-2015	YESILYURT, Sevinc/0000-0002-0062-0491; Akgun, Funda/0000-0002-6028-6704; Durak, Sariye Duygu/0000-0003-4209-2081	Scientific and Technological Research Council of Turkey (TUBITAK) [106Y104]	Scientific and Technological Research Council of Turkey (TUBITAK)(Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK))	This study was supported by a research grant from the Scientific and Technological Research Council of Turkey (TUBITAK Grant Code 106Y104). The assistance provided by Riza Gorkem Ozkay, who took part in field work, is acknowledged. The authors would like thank Dr. Torsten Utescher and anonymous referee for their helpful comments and their constructive criticisms of the manuscript.	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Geol. Meded, V30, P183; WESTGATE JW, 1990, PALAEOGEOGR PALAEOCL, V78, P163, DOI 10.1016/0031-0182(90)90210-X; YARCI C, 2000, ERCIYES U FEN BILIML, V16, P1	82	21	23	0	38	Tubitak Scientific & Technological Research Council Turkey	ANKARA	ATATURK BULVARI NO 221, KAVAKLIDERE, TR-06100 ANKARA, TURKIYE	1300-0985			TURK J EARTH SCI	Turk. J. Earth Sci.		2013	22	2					277	303		10.3906/yer-1201-3	http://dx.doi.org/10.3906/yer-1201-3			27	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	129EO		Bronze			2025-03-11	WOS:000317821900008
J	Benvenuti, A; Kombrink, H; ten Veen, JH; Munsterman, DK; Bardi, F; Benvenuti, M				Benvenuti, A.; Kombrink, H.; ten Veen, J. H.; Munsterman, D. K.; Bardi, F.; Benvenuti, M.			Late Cenozoic shelf delta development and Mass Transport Deposits in the Dutch offshore area - results of 3D seismic interpretation	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						Mass transport deposits; Eridanos delta; sequence stratigraphy; Pilo-Pleistocene	NORTH-SEA BASIN; SUBMARINE LANDSLIDES; DINOFLAGELLATE CYST; STRATIGRAPHY; PALEOENVIRONMENT; TECTONICS; MOVEMENTS; EVOLUTION; OLIGOCENE; SEDIMENTS	In this study, seismic stratigraphic criteria have been used to characterise the evolution of the Southern North Sea (SNS) shelf-delta system that progressively filled the Southern North Sea basin during Plio-Pleistocene times. Based on the prograding and down-stepping architecture of the shelf-delta sequence it is inferred that deposition occurred during a time of high sediment supply and overall sea-level lowering. During this time the delta slopes failed several times, creating at least 30 internally coherent Mass Transport Deposits (MTDs) mainly grouped in common areas, affecting the same clinoform set and partially sharing the basal shear surface (groups of MTDs). The most important features of the studied MTDs are 1) the dominance of brittle deformation; 2) the small amount of material removal from the headwall domain (lack of completely depleted areas above the basal shear surface); and 3) the lack of an emergent toe domain above the un-failed sediment located basinward, although proper confining geometries for the MTD are not detected. Therefore, the studied MTDs can neither be classified as frontally confined nor as frontally emergent but they are a new intermediate type of submarine landslides which has not been described before. These characteristics suggest that the mass movement ceased relatively soon after initiation of failure. Incisions on top of the MTDs suggest the presence of erosive flows. These flows were probably generated due to a concentration of the drainage in the negative morphology the failure event left behind in the upper sector of the slope. The stronger progradational character of the reflections on top of MTDs confirms a concentration of drainage after the erosional phase too. The interplay between high sediment supply and constant or even decreasing accommodation space (caused by constant or decreasing sea-level) is supposed to be the main precondition for slope instability for most of the MTDs in this study area. Slope failures themselves can also be considered a preconditioning factor by the creation of local very high sedimentation rates (see groups of MTDs). Salt-induced seismicity and storm waves' effect superimposed on high frequency sea level fall are considered the most important triggering factors.	[Benvenuti, A.; Kombrink, H.; ten Veen, J. H.; Munsterman, D. K.] TNO Geol Survey Netherlands, NL-3508 TA Utrecht, Netherlands; [Bardi, F.] DataCo Ltd, England Head Off, Berkhamsted, Herts, England; [Bardi, F.] DataCo Ltd, The Hague, Netherlands; [Benvenuti, A.; Benvenuti, M.] Univ Florence, Dept Earth Sci, I-50121 Florence, Italy	Netherlands Organization Applied Science Research; University of Florence	Benvenuti, A (通讯作者)，Univ Geneva, Dept Geol & Paleontol, Rue Maraichers 13, CH-1205 Geneva, Switzerland.	antonio.benvenuti@unige.ch						[Anonymous], 1993, Selected studies in the U.S. Exclusive economic zone; [Anonymous], 2008, Zeitschrift der Deutschen Gesellschaft fur Geowissenschaften, DOI [DOI 10.1127/1860-1804/2008/0159-0687, 10.1127/1860-1804/2008/0159-0687]; Bijlsma S., 1981, GEOLOGIE MIJNBOUW, P337; Bull S, 2009, MAR PETROL GEOL, V26, P1132, DOI 10.1016/j.marpetgeo.2008.09.011; CAMERON TDJ, 1993, MAR PETROL GEOL, V10, P591, DOI 10.1016/0264-8172(93)90061-V; Canals M, 2004, MAR GEOL, V213, P9, DOI 10.1016/j.margeo.2004.10.001; Cartwright J.A., 1994, GEOLOGY, V10, P591; Catuneanu O, 2009, EARTH-SCI REV, V92, P1, DOI 10.1016/j.earscirev.2008.10.003; Catuneanu O., 2006, PRINCIPLES SEQUENCE; de Jager J, 2003, NETH J GEOSCI, V82, P339, DOI 10.1017/S0016774600020175; De Lugt I.R., 2007, THESIS UTRECHT U UTR; De Schepper S, 2009, PALYNOLOGY, V33, P179; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Eidvin T, 1999, NORSK GEOL TIDSSKR, V79, P97, DOI 10.1080/002919699433843; Ethridge F.G., 2009, Fluvial Sedimentology VII, P211, DOI [DOI 10.1002/9781444304350.CH13, 10.1002/9781444304350.ch13]; Frey-Martínez J, 2006, MAR PETROL GEOL, V23, P585, DOI 10.1016/j.marpetgeo.2006.04.002; Hampton MA, 1996, REV GEOPHYS, V34, P33, DOI 10.1029/95RG03287; Helland-Hansen W., 2008, J SEDIMENT RES, V66, P670; HUNT D, 1992, SEDIMENT GEOL, V81, P1, DOI 10.1016/0037-0738(92)90052-S; Huuse M, 2002, B GEOL SOC DENMARK, V49, P145; 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; Huuse M., 2005, Petroleum Geology of Northwest Europe: Proceedings of the Conference, V6, P1577, DOI DOI 10.1144/0061577; Huvenne VAI, 2002, TERRA NOVA, V14, P33, DOI 10.1046/j.1365-3121.2002.00386.x; Japsen P, 1999, B GEOL SOC DENMARK, V46, P79; Köthe A, 2007, Z DTSCH GES GEOWISS, V158, P287, DOI 10.1127/1860-1804/2007/0158-0287; Kuhlmann G., 2004, THESIS UTRECHT U UTR; Kuhlmann G, 2008, MAR PETROL GEOL, V25, P173, DOI 10.1016/j.marpetgeo.2007.05.009; Kuhlmann G, 2006, PALAEOGEOGR PALAEOCL, V239, P426, DOI 10.1016/j.palaeo.2006.02.004; Laursen GV, 1997, B SOC GEOL FR, V168, P187; Lee HJ, 2009, MAR GEOL, V264, P53, DOI 10.1016/j.margeo.2008.09.009; LEITH W, 1986, J GEOPHYS RES-SOLID, V91, P689, DOI 10.1029/JB091iB01p00689; Leynaud D, 2009, MAR PETROL GEOL, V26, P618, DOI 10.1016/j.marpetgeo.2008.02.008; Locat J, 2002, CAN GEOTECH J, V39, P193, DOI 10.1139/T01-089; Lucente CC, 2003, AM J SCI, V303, P565, DOI 10.2475/ajs.303.7.565; Martinsen O.J., 1994, GEOLOGICAL DEFORMATI, P127, DOI DOI 10.1007/978-94-011-0731-0_5; Martinsen O.J., 1998, Mesozoic and Cenozoic sequence stratigraphy of European Basins, P91; Masson DG, 2006, PHILOS T R SOC A, V364, P2009, DOI 10.1098/rsta.2006.1810; Micallef A, 2007, ADV NAT TECHNOL HAZ, V27, P119, DOI 10.1007/978-1-4020-6512-5_13; Miller KG, 2005, SCIENCE, V310, P1293, DOI 10.1126/science.1116412; Mulder T, 1996, J SEDIMENT RES, V66, P43; Munsterman DK, 2004, NETH J GEOSCI, V83, P267, DOI 10.1017/S0016774600020369; Overeem I, 2001, BASIN RES, V13, P293, DOI 10.1046/j.1365-2117.2001.00151.x; Owen M, 2007, QUATERNARY SCI REV, V26, P958, DOI 10.1016/j.quascirev.2006.12.011; Rasmussen ES, 2009, TECTONOPHYSICS, V465, P84, DOI 10.1016/j.tecto.2008.10.025; Rasmussen ES, 2004, GLOBAL PLANET CHANGE, V41, P15, DOI 10.1016/j.gloplacha.2003.08.004; Schmuck E.A., 1993, SUBMARINE LANDSLIDES, P40; Sorensen JC, 1997, MAR PETROL GEOL, V14, P99, DOI 10.1016/S0264-8172(96)00052-9; Storvoll V, 2005, AAPG BULL, V89, P359, DOI 10.1306/10150404033; ten Veen JH, 2012, NETH J GEOSCI, V91, P447; Ten Veen J.H., 2008, 26 REG M INT ASS SED; vanWees JD, 1996, TECTONOPHYSICS, V266, P343, DOI 10.1016/S0040-1951(96)00197-7; Ziegler P.A., 1990, GEOLOGICAL ATLAS W C	53	11	12	0	15	CAMBRIDGE UNIV PRESS	CAMBRIDGE	EDINBURGH BLDG, SHAFTESBURY RD, CB2 8RU CAMBRIDGE, ENGLAND	0016-7746	1573-9708		NETH J GEOSCI	Neth. J. Geosci.	DEC	2012	91	4					591	608						18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	065NA					2025-03-11	WOS:000313154000010
J	Morquecho, L; Alonso-Rodríguez, R; Arreola-Lizárraga, JA; Reyes-Salinas, A				Morquecho, Lourdes; Alonso-Rodriguez, Rosalba; Arreola-Lizarraga, Jose A.; Reyes-Salinas, Amada			Factors associated with moderate blooms of <i>Pyrodinium bahamense</i> in shallow and restricted subtropical lagoons in the Gulf of California	BOTANICA MARINA			English	Article						bloom dynamics; cysts; ecology; Gulf of California; Mexico; Pyrodinium bahamense; subtropical lagoons	INDIAN RIVER LAGOON; PHYTOPLANKTON COMPOSITION; ORGANIC-MATTER; COASTAL LAGOON; DINOFLAGELLATE; DYNAMICS; BAY; LITTERFALL; SEDIMENTS; FLORIDA	We examined the environmental and biological factors related to blooms of the toxic dinoflagellate Pyrodinium bahamense in three shallow, restricted subtropical lagoons in the Gulf of California during the rainy summer. In the San Jose, Yavaros, and El Colorado lagoons, the vegetative stage peaked at 63, 108, and 151 (x10(3) cells l(-1)), respectively. At San Jose, production of cysts peaked at 9.7x10(3) g(-1) of dry sediment mass as the bloom declined. Large diatoms predominated, with P. bahamense the most common dinoflagellate during the blooms. Abundance of P. bahamense at San Jose was positively correlated with salinity (r=0.50, p=0.0003), seawater temperature (r=0.44, p=0.005), silicates (r=0.45, p=0.003), and ammonium (r=0.32, p=0.005), and negatively correlated with dissolved oxygen (r=-0.34, p<0.0001). No such correlations were found at El Colorado and Yavaros. The environmental window that favors development of blooms is restricted to the summer and is influenced by seawater temperature, salinity, and relative concentrations of ammonium and phosphates that, in turn, depend on rainfall and runoff, which is greater on the eastern side of the Gulf where seawater quality is degraded.	[Morquecho, Lourdes; Reyes-Salinas, Amada] Inst Politecn Nacl 195, Ctr Invest Biol Noroeste CIBNOR, La Paz 23096, Bcs, Mexico; [Alonso-Rodriguez, Rosalba] Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Unidad Acad Mazatlan, Mazatlan 82040, Sinaloa, Mexico; [Arreola-Lizarraga, Jose A.] Ctr Invest Biol Noroeste CIBNOR, Unidad Guaymas, Guaymas 85454, Sonora, Mexico	CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Universidad Nacional Autonoma de Mexico; CIBNOR - Centro de Investigaciones Biologicas del Noroeste	Morquecho, L (通讯作者)，Inst Politecn Nacl 195, Ctr Invest Biol Noroeste CIBNOR, La Paz 23096, Bcs, Mexico.	lamorquecho@cibnor.mx	Morquecho, Lourdes/JPY-0626-2023; Arreola Lizarraga, Jose Alfredo/G-5038-2018; Alonso-Rodriguez, Rosalba/U-9896-2017	Arreola Lizarraga, Jose Alfredo/0000-0002-0936-8886; Alonso-Rodriguez, Rosalba/0000-0001-7716-3869	CIBNOR research project [PC3.3, 180C]; SEMARNAT-CONACYT [2002-C01-0161]	CIBNOR research project; SEMARNAT-CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	Miguel A. Aguilar, Horacio Bervera, Mario Cota, and Juan J. Ramirez provided technical assistance in the field. Iban Murillo, Celina Beltran, and Refugio Lopez provided technical assistance in processing the nutrient samples. Patricia Gonzalez provided information about mangroves of the region. Carlos H. Lechuga provided a multiparameter water quality sonde. German Ramirez provided suggestions and comments to improve figures and statistical analyses. Edgar Alcantara provided meteorological data from Sonora. Ira Fogel provided editorial suggestions. Comision Nacional del Agua (CONAGUA) and Servicio Meteorologico Nacional (SMN) provided weather data. This study was supported by CIBNOR research project nos. PC3.3 and 180C, and by SEMARNAT-CONACYT grant no. 2002-C01-0161.	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Marina	DEC	2012	55	6					611	623		10.1515/bot-2012-0171	http://dx.doi.org/10.1515/bot-2012-0171			13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	047LL		Bronze			2025-03-11	WOS:000311842200006
J	Candel, MS; Radi, T; de Vernal, A; Bujalesky, G				Soledad Candel, M.; Radi, Taoufik; de Vernal, Anne; Bujalesky, Gustavo			Distribution of dinoflagellate cysts and other aquatic palynomorphs in surface sediments from the Beagle Channel, Southern Argentina	MARINE MICROPALEONTOLOGY			English	Article						Dinocyst assemblages; Aquatic palynomorphs; Distribution; Beagle Channel; Argentina; South America	TIERRA-DEL-FUEGO; RECENT MARINE-SEDIMENTS; HYDROGRAPHIC CONDITIONS; NORTHERN-HEMISPHERE; LATE QUATERNARY; HIGH-LATITUDES; INDIAN-OCEAN; SEA; ASSEMBLAGES; PRODUCTIVITY	Palynological analyses of 22 surface sediment samples from the Beagle Channel, Tierra del Fuego, Argentina, were performed in order to investigate the distribution of dinocyst assemblages and other aquatic palynomorphs and to explore their relationships with sea-surface conditions, which are regionally characterized by cold and low salinity conditions (4-9 degrees C and 27-33.5, respectively). Results show relatively low dinocyst concentrations (253 to 5568 cysts/g) and species diversity (19 taxa identified). The assemblages are mostly composed of Protoperidiniaceae and appear typical of a marginal marine environment with surface waters characterized by low to moderate salinity and high nutrient content due to river inputs. The assemblages are thus compatible with the occurrence of freshwater to brackish water taxa Botryococcus braunii, Botryococcus sp., Polyasterias sp., Halodinium sp., and Radiosperma corbiferum. The dinocyst assemblages are dominated by Brigantedinium spp., Echinidinium spp. and Selenopemphix quanta accompanied by cysts of Pentapharsodinium dalei, Islandinium minutum, Votadinium spinosum, Polykrikos kofoidii and Polykrikos schwartzii. The assemblages from the Beagle Channel show similarities with those of high latitude regions of the Northern Hemisphere. However, some taxa, which were exclusively reported from relatively warm environments in the Northern Hemisphere, occur in relatively high percentages in the Beagle Channel (e.g. Echinidinium delicatum and Votadinium spinosum). The absence of Selenopemphix antarctica in the Beagle Channel is consistent with its known ecological affinities, since it characterizes environments marked by seasonal sea-ice cover. (C) 2012 Elsevier B.V. All rights reserved.	[Soledad Candel, M.] Univ Nacl Sur, Dept Geol, INGEOSUR CONICET, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Radi, Taoufik; de Vernal, Anne] Univ Quebec, Ctr Rech Geochim & Geodynam GEOTOP, Montreal, PQ H3C 3P8, Canada; [Radi, Taoufik] McGill Univ, Montreal, PQ H3A 2A7, Canada; [Bujalesky, Gustavo] CADIC CONICET, Ushuaia, Tierra Del Fueg, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Quebec; University of Quebec Montreal; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Candel, MS (通讯作者)，Univ Nacl Sur, Dept Geol, INGEOSUR CONICET, San Juan 670,B8000ICN, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	scandel@uns.edu.ar	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X	CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas) [PIP 02787/02]; Agencia de Promocion Cientifica y Tecnologica [PICT Redes 2002-00067]; CONICET [PIP 06/06 6200, PIP 09/011 0533]; Fundacion Antorchas [A-13672/1-2]	CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Agencia de Promocion Cientifica y Tecnologica(ANPCyT); CONICET(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Fundacion Antorchas	This study was supported by CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas, PIP 02787/02) and the Agencia de Promocion Cientifica y Tecnologica (PICT Redes 2002-00067) grants to Dr. Mirta Quattrocchio and Dr. Ana Maria Borromei, respectively. CONICET (PIP 06/06 6200, PIP 09/011 0533) and Fundacion Antorchas (Proyecto A-13672/1-2) provided Gustavo Bujalesky the financial support for field works in the Beagle Channel. We are grateful to Maryse Henry (GEOTOP) for her help in the laboratory, Gustavo Lovrich (CADIC-CONICET) for his help in providing salinity and temperature data and Daniela Olivera (Departamento de Geologia-UNS) for her help with statistical analysis. Our thanks are also extended to Dr. Richard Jordan and two anonymous reviewers for their constructive comments, suggestions and English revision of the manuscript.	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Micropaleontol.	DEC	2012	96-97						1	12		10.1016/j.marmicro.2012.06.009	http://dx.doi.org/10.1016/j.marmicro.2012.06.009			12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	039RL		Green Published			2025-03-11	WOS:000311264100001
J	Taldenkova, E; Bauch, HA; Stepanova, A; Ovsepyan, Y; Pogodina, I; Klyuvitkina, T; Nikolaev, S				Taldenkova, Ekaterina; Bauch, Henning A.; Stepanova, Anna; Ovsepyan, Yaroslav; Pogodina, Irina; Klyuvitkina, Tatiana; Nikolaev, Sergei			Benthic and planktic community changes at the North Siberian margin in response to Atlantic water mass variability since last deglacial times	MARINE MICROPALEONTOLOGY			English	Article						Atlantic-derived water; Laptev Sea; Planktic and benthic foraminifers; Ostracods; Deglaciation; Holocene	SEA CONTINENTAL-MARGIN; SW BARENTS SEA; LAPTEV SEA; ARCTIC-OCEAN; HOLOCENE PALEOCEANOGRAPHY; DINOFLAGELLATE CYSTS; HIGH-RESOLUTION; ICE-SHEET; CLIMATE VARIABILITY; SVALBARD MARGIN	The eastward penetration of Atlantic-derived water (ADW) into the Eurasian Basin of the Arctic Ocean was investigated at the western Laptev Sea continental margin for the time since c. 17.6 ka. Using a high-resolution investigation of the lithology, geochemistry, planktic and benthic foraminifers, and ostracods on a sediment core from 270 m water depth major steps in the environmental evolution of the region are recognized. In general, ADW was continuously present in the study area. Between 17.6 and 15.4 ka ADW manifested itself through open-water polynyas and associated upwelling events. Comparison between the Laptev Sea and northern Svalbard shelf using Cassidulina neoteretis allows assuming an unmodified subsurface inflow of ADW within its northern branch between 15.4 and 13.2, which was strongest after 14.7-ka and in line with the overall climate amelioration. A local freshwater event at 13 ka followed by shelf flooding and the establishment of a freshened shelf water mass resulted in an off-shelf displacement of ADW from the studied site as suggested by the disappearance of C neoteretis between 12 and 7 ka. As evidenced by an abundance peak in Nonion labradoricum, the sea-ice marginal zone was located at the site around 12-11 ka but then shifted northward during the early Holocene warming. Enhanced ADW inflow since 7 ka correlated with climate cooling and southward retreat of the seasonal drift-ice margin. The inflow of ADW during mid-late Holocene differed from deglacial times because of the combined influence of northern and eastern ADW branches. (C) 2012 Elsevier By. All rights reserved.	[Taldenkova, Ekaterina; Klyuvitkina, Tatiana; Nikolaev, Sergei] Moscow MV Lomonosov State Univ, Fac Geog, Moscow 119991, Russia; [Bauch, Henning A.] GEOMAR, Mainz Acad Sci Humanities & Literature, D-24148 Kiel, Germany; [Stepanova, Anna] RAS, Inst Paleontol, Moscow 117997, Russia; [Ovsepyan, Yaroslav] Moscow MV Lomonosov State Univ, Geol Fac, Moscow 119991, Russia; [Pogodina, Irina] Murmansk Marine Biol Inst, Murmansk 183010, Russia	Lomonosov Moscow State University; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Russian Academy of Sciences; Lomonosov Moscow State University; Russian Academy of Sciences; Murmansk Marine Biological Institute	Taldenkova, E (通讯作者)，Moscow MV Lomonosov State Univ, Fac Geog, Leninskie Gory 1, Moscow 119991, Russia.	etaldenkova@mail.ru; hbauch@geomar.de; a.yu.stepanova@gmail.com; yaovsepyan@yandex.ru; t.klyuvitkina@mail.ru; cdnik@rambler.ru	Klyuvitkina, Tatyana/L-8843-2015; Nikolaev, Sergei/L-8882-2015; Ovsepyan, Yaroslav/D-4667-2014; Taldenkova, Ekaterina/L-7853-2015	Taldenkova, Ekaterina/0000-0002-0959-4111; Ovsepyan, Yaroslav/0000-0003-1172-4357	BMBF; Russian Ministry for Education and Science (OSL fellowship projects); Russian Foundation for Basic Research [08-05-00849, 11-05-01091]; INTAS [03-51-6682]	BMBF(Federal Ministry of Education & Research (BMBF)); Russian Ministry for Education and Science (OSL fellowship projects); Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); INTAS(INTAS)	We thank the team from the Leibniz Laboratory (Kiel) for conducting AMS<SUP>14</SUP>C measurements and T. Mueller-Lupp for providing geochemical data. We acknowledge the assistance of collaborators of the Otto Schmidt Laboratory for Polar and Marine Sciences (OSL) in sample processing. We thank M. Slubowska-Woldengen with her co-authors for providing us with their original data. This research was supported by the BMBF and Russian Ministry for Education and Science (OSL fellowship projects), the Russian Foundation for Basic Research (projects 08-05-00849 and 11-05-01091), and INTAS (project 03-51-6682).	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Micropaleontol.	DEC	2012	96-97						13	28		10.1016/j.marmicro.2012.06.007	http://dx.doi.org/10.1016/j.marmicro.2012.06.007			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	039RL					2025-03-11	WOS:000311264100002
J	Mertens, KN; Yamaguchi, A; Kawami, H; Ribeiro, S; Leander, BS; Price, AM; Pospelova, V; Ellegaard, M; Matsuoka, K				Mertens, Kenneth Neil; Yamaguchi, Aika; Kawami, Hisae; Ribeiro, Sofia; Leander, Brian S.; Price, Andrea Michelle; Pospelova, Vera; Ellegaard, Marianne; Matsuoka, Kazumi			<i>Archaeperidinium saanichi</i> sp nov.: A new species based on morphological variation of cyst and theca within the <i>Archaeperidinium minutum</i> Jorgensen 1912 species complex	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate; Saanich Inlet; LSU rDNA; Single-cell PCR; Spiny brown cyst; SSU rDNA	HETEROTROPHIC DINOFLAGELLATE GENUS; SAND-DWELLING DINOFLAGELLATE; PROTOPERIDINIUM DINOPHYCEAE; PACIFIC-OCEAN; SEQUENCE DATA; COMB-NOV; PHYLOGENY; ULTRASTRUCTURE; PERIDINIALES; SEDIMENTS	In this paper we describe a new species. Archaeperidinium saanichi sp. nov. within the Archaeperidinium minutum Jorgensen 1912 species complex. We examined the morphological variation of the cyst and motile stage by incubation experiments from sediment samples collected in coastal British Columbia (Canada), and compared it to closely related species. The theca of A. saanichi is differentiated from related species by overall size, the asymmetry of the intercalary plates and the right-sulcal plate (S.d.) not touching the cingulum. We provide a key to differentiate all closely related species. A. saanichi can be readily distinguished from A. minutum by a distinctively large cyst with a broad 2a type archeopyle and regularly spaced processes with relatively broad bases and aculeate process tips. Molecular phylogenetic analyses of large and small subunit (LSU and SSU) rDNA sequences demonstrated a close affinity of this species to A. minutum; however, the relatively high level of sequence conservation in dinoflagellate rDNA sequences made these particular markers inadequate for distinguishing one species from the other. Sediment-trap data suggest that A. saanichi has a preference for cooler temperatures and lowered salinities. (C) 2012 Elsevier B.V. All rights reserved.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Yamaguchi, Aika; Leander, Brian S.] Univ British Columbia, Dept Bot, Vancouver, BC V6T 1Z4, Canada; [Yamaguchi, Aika; Leander, Brian S.] Univ British Columbia, Dept Zool, Vancouver, BC V6T 1Z4, Canada; [Kawami, Hisae; Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res ECSER, Nagasaki 8528521, Japan; [Ribeiro, Sofia; Ellegaard, Marianne] Univ Copenhagen, Fac Sci, Dept Biol, DK-1353 Copenhagen K, Denmark; [Price, Andrea Michelle; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada	Ghent University; University of British Columbia; University of British Columbia; Nagasaki University; University of Copenhagen; 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	Mertens, Kenneth/AAO-9566-2020; Ribeiro, Sofia/AAZ-2782-2021; Mertens, Kenneth/C-3386-2015; Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/G-9213-2018	Mertens, Kenneth/0000-0003-2005-9483; Ellegaard, Marianne/0000-0002-6032-3376; Price, Andrea/0000-0002-5359-053X; Ribeiro, Sofia/0000-0003-0672-9161; Pospelova, Vera/0000-0003-4049-8133	Kakenhi [22-00805]; Assembling the Tree of Life grant (NSF) [EF-0629624]; National Science and Engineering Research Council of Canada [NSERC 283091-09]; Canadian Institute for Advanced Research, Programs in Evolutionary Biology and Integrated Microbial Biodiversity; NSERC [224236]	Kakenhi(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); Assembling the Tree of Life grant (NSF); National Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Canadian Institute for Advanced Research, Programs in Evolutionary Biology and Integrated Microbial Biodiversity; NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	Kenneth Neil Mertens is a postdoctoral fellow of FWO Belgium and this research was partly conducted at Nagasaki University and was supported by a Kakenhi grant 22-00805. Aika Yamaguchi was supported by a postdoctoral research salary from the Assembling the Tree of Life grant (NSF #EF-0629624) and operating funds to B.S.L. from the National Science and Engineering Research Council of Canada (NSERC 283091-09) and the Canadian Institute for Advanced Research, Programs in Evolutionary Biology and Integrated Microbial Biodiversity. This research was partly supported by NSERC's Discovery (224236) and Ship Time grants to Vera Pospelova. Andre Catrijsse (VLIZ, Belgium) is thanked for providing us with surface sediment samples from the North Sea which unfortunately did not contain any spiny brown cysts. One Effingham Inlet sediment trap sample was kindly provided by Dr. R. Timothy Patterson (Carleton University, Canada). The VENUS (Victoria Experimental Network Under the Sea) team is thanked for their assistance with collection of Saanich Inlet sediment trap material, and surface sediments from Site A in Patricia Bay. 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