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J	Jenhani, AB; Fathalli, A; Ben Naceur, H; Hayouni, D; Aouani, J; Romdhane, MS				Jenhani, Amel Ben Rejeb; Fathalli, Afef; Ben Naceur, Hachem; Hayouni, Dhekra; Aouani, Jaafer; Romdhane, Mohamed Salah			Screening for alien and harmful planktonic species in the Gulf of Gabes (Tunisia, Southeastern Mediterranean Sea)	REGIONAL STUDIES IN MARINE SCIENCE			English	Article						Dinophyceae cysts; Harmful species; Invasive species; Plankton	SHIPS BALLAST WATER; ALGAL BLOOMS; DINOFLAGELLATE CYSTS; RESTING STAGES; MARINE; PHYTOPLANKTON; BIOGEOGRAPHY; SEDIMENTS; BIOINVASIONS; GYMNODIMINE	The Gulf of Gabes, pole of shellfish production in Tunisia, is known by a great maritime traffic. The objective of the present study is to update the planktonic organisms listing and to screen alien and harmful planktonic species in the Gulf. The investigations, conducted in the four commercial ports of the Gulf of Gabes, in 2010, revealed the presence of 138 phytoplankton taxa dominated by the Dinophyceae and Bacillariophyceae and 37 Dinophyceae rest forms from which 17 were not found in their active form. Among the alien phytoplankton species in the Mediterranean, we identified 4 species in water and 6 Dinophyceae cysts taxa in sediments of the Gulf of Gabes. The four encysted forms of potentially toxic dinoflagellates, detected in this work, were wholly non-indigenous species. Eleven known harmful phytoplanktonic species, including 2 native species of Diatoms (Chaetoceros socialis and Pseudo-nitzschia sp.) and 9 Dinophyceae including the non-indigenous species Alexandrium minutum and Karenia selliformis were found during this study. The qualitative analysis of zooplankton in the gulf of Gabes showed the common presence of 21 groups which the most important is copepods. It revealed also the presence of the two Alien species Acartia (Acanthacartia) bifilosa and Paracartia (Acartia) grani. (C) 2019 Elsevier B.V. All rights reserved.	[Jenhani, Amel Ben Rejeb; Hayouni, Dhekra; Romdhane, Mohamed Salah] Inst Natl Agron Tunisie, Unite Rech Ecosyst & Ressources Aquat, 43 Ave Charles Nicolle, Tunis Mahrajene 1082, Tunisia; [Fathalli, Afef] Inst Natl Sci & Technol Mer, Tunis 2060, Tunisia; [Aouani, Jaafer] SOTINFOR, SERAH, Tunis, Tunisia; [Ben Naceur, Hachem] Inst Super Biotechnol Monastir, Lab Rech Bioressources Biol Integrat & Valorisat, Monastir, Tunisia	Universite de Carthage; Institut National des Sciences et Technologies de la Mer; Universite de Monastir	Fathalli, A (通讯作者)，Inst Natl Sci & Technol Mer, Tunis 2060, Tunisia.	fathalli_afef@yahoo.fr	Romdhane, Mohamed Salah/GTB-5864-2022					Abdenadher M, 2012, ESTUAR COAST SHELF S, V106, P102, DOI 10.1016/j.ecss.2012.04.029; [Anonymous], THESIS; [Anonymous], 1984, INTRO PRATIQUE SYSTE; [Anonymous], B I NATN SCI TECH ME; [Anonymous], 2003, THESIS; [Anonymous], 1990, Atlas du phytoplancton marin Chlorarachniophycees, chlorophycees, chrysophycees, cryptophycees, eugle`nophycees, eustigmatophycees, prasinophycees, prymnesiophycees, rhodophycees et tribophycees.; Audemard C, 2004, DIS AQUAT ORGAN, V61, P103, DOI 10.3354/dao061103; Aune T, 2002, TOXICON, V40, P77, DOI 10.1016/S0041-0101(01)00192-1; Belmonte G., 1999, Biologia Marina Mediterranea, V6, P172; Belmonte G, 1995, OLSEN INT S, P53; Belmonte G, 2001, HYDROBIOLOGIA, V453, P171, DOI 10.1023/A:1013192623131; 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; Ben Lamine Y., 2012, B I NATL SCI TECH ME, V39, P114; Berard-Therriault L., 1999, Publ spec can sci halieut aquat, V128, P1; Blackburn S., 2005, Algal Culturing Techniques, P399; Blanco J, 1999, MAR ECOL PROG SER, V176, P153, DOI 10.3354/meps176153; Boudouresque C.F., 2002, Alien Marine Organisms Introduced by Ships in the Mediterranea and Black Seas, V20, P53; BRAVO I, 1990, TOXIC MARINE PHYTOPLANKTON, P449; Chambouvet A, 2008, SCIENCE, V322, P1254, DOI 10.1126/science.1164387; Cleve-Euler A., 1951, DIATOMEEN SCHWEDEN F; Corriero G, 2016, AQUAT CONSERV, V26, P392, DOI 10.1002/aqc.2550; Dale B., 1983, P69; DALE B, 1978, OCEANUS, V21, P41; DGPA, 2007, STAT PECH DIR GEN PE; DGPA, 2006, STAT PECH DIR GEN PE; DGPA, 2005, STAT PECH DIR GEN PE; DGPA, 2008, STAT PECH DIR GEN PE; DGPA, 2009, STAT PECH DIR GEN PE; Drira Z, 2008, SCI MAR, V72, P59; Dukes J., 2003, GLOBAL CLIMATE CHANG, P25; Dussart B. 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Stud. Mar. Sci.	MAR	2019	27								100526	10.1016/j.rsma.2019.100526	http://dx.doi.org/10.1016/j.rsma.2019.100526			10	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	HT6NO					2025-03-11	WOS:000464681100014
J	Lambert, C; Vidal, M; Penaud, A; Le Roy, P; Goubert, E; Pailler, Y; Stephan, P; Ehrhold, A				Lambert, Clement; Vidal, Muriel; Penaud, Aurelie; Le Roy, Pascal; Goubert, Evelyne; Pailler, Yvan; Stephan, Pierre; Ehrhold, Axel			Palaeoenvironmental reconstructions during the Meso- to Neolithic transition (9.2-5.3 cal. ka BP) in Northwestern France: Palynological evidences	HOLOCENE			English	Article						benthic foraminifera; climate variability; dinoflagellate cysts; human impacts; palaeoenvironments reconstructions; pollen grains	WESTERN BRITTANY FRANCE; NORTH-ATLANTIC OCEAN; SEA-LEVEL CHANGES; CLIMATE VARIABILITY; ATMOSPHERIC CIRCULATION; MESOLITHIC AGRICULTURE; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; SOUTHERN BRITTANY; HOLOCENE CLIMATE	Sedimentological, palynological, and micropalaeontological studies carried out throughout the first half of the Holocene, during the Mesolithic/Neolithic transition in the Bay of Brest (i.e. 9200-9000 and 6600-5300 cal. BP) and in the Bay of Douarnenez (i.e. 9200-8400 cal. BP), allowed characterizing coastal environmental changes under the increasing influence of the relative sea-level rise. The gradual flooding of the two studied sites implied a transition from river valleys to oceanic bays as revealed by the gradual retreat of salt marsh environments, as detected through palynological analysis. In addition, these high-resolution studies highlight the regional imprint of the North Atlantic millennial climate variability in north-western coastal environments. Two cold climate events are indeed suggested to have been locally marked by a moisture increase, mainly detected by increases in Lingulodinium machaerophorum, Corylus, and Alnus percentages at 8550 cal. BP in the Bay of Douarnenez and at 6250 cal. BP in the Bay of Brest. Moreover, regarding the Neolithic transition timing in the Bay of Douarnenez, large pollen grains of Poaceae (i.e. Cerealia-type pollen grains) have been detected at around 8600 cal. BP, that is, 1500 years before the general accepted cereal cropping appearance in Western France. These results, consistent with other palynological studies conducted in the French Atlantic coast, could underline a Mesolithic proto-agriculture' in Brittany.	[Lambert, Clement; Vidal, Muriel; Penaud, Aurelie; Le Roy, Pascal] UBO, CNRS, UMR 6538, Lab Geosci Ocean,IUEM, Rue Dumont Urville, F-29280 Plouzane, France; [Goubert, Evelyne] Univ Bretagne Sud, UBO, CNRS, Lab Geosci Ocean,IUEM,UMR 6538, Lorient, France; [Pailler, Yvan] INRAP, UMR 8215, Lab Trajectoires, Grand Ouest, France; [Stephan, Pierre] UBO, CNRS, UMR 6554, LETG Brest GEOMER,IUEM, Plouzane, France; [Ehrhold, Axel] IFREMER, Ctr Brest, Geosci Marines, Issy Les Moulineaux, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Ifremer	Lambert, C (通讯作者)，UBO, CNRS, UMR 6538, Lab Geosci Ocean,IUEM, Rue Dumont Urville, F-29280 Plouzane, France.	clement.lambert24@gmail.com	Lambert, Clément/ABF-5691-2020; ehrhold, axel/KHY-3754-2024; Penaud, Aurelie/F-2485-2011; Vidal, Muriel/B-7856-2014	Stephan, Pierre/0000-0001-7975-2149; Penaud, Aurelie/0000-0003-3578-4549; PAILLER, Yvan/0000-0002-4782-1389; Vidal, Muriel/0000-0003-3699-2083; Lambert, Clement/0000-0002-7746-8504; Ehrhold, Axel/0000-0001-7207-0831	French CNRS; UBO-BQR project: 'PARADE: Signature PAleoenvironnementale des sequences holocenes en RADE de Brest'; 'Laboratoire d'Excellence' LabexMER [ANR-10-LABX-19]; French government under the program 'Investissements d'Avenir'	French CNRS(Centre National de la Recherche Scientifique (CNRS)); UBO-BQR project: 'PARADE: Signature PAleoenvironnementale des sequences holocenes en RADE de Brest'; 'Laboratoire d'Excellence' LabexMER; French government under the program 'Investissements d'Avenir'(Agence Nationale de la Recherche (ANR))	This study was supported by the French CNRS and is a contribution to the 2015-2016 INSU project EC2CO-LEFE: 'CAMOMI: Convergences/Approches croisees des signaux MOleculaires et MIcropaleontologiques pour decrypter les forcages anthropiques et climatiques en milieu cotier (Rade de Brest)' and the UBO-BQR project: 'PARADE: Signature PAleoenvironnementale des sequences holocenes en RADE de Brest'. 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J	Mahmoud, MS; Deaf, AS; Tamam, MA; Khalaf, MM				Mahmoud, Magdy S.; Deaf, Amr S.; Tamam, Mohamed A.; Khalaf, Miran M.			Revised (miospores-based) stratigraphy of the Lower Cretaceous succession of the Minqar-IX well, Shushan Basin, north Western Desert, Egypt: Biozonation and correlation approach	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynostratigraphy; Miospores; Cretaceous; Shushan basin; Western desert; Egypt	SEDIMENTARY ORGANIC-MATTER; TUNIS 1X BOREHOLE; ANGIOSPERM POLLEN; SHOUSHAN BASIN; DAKHLA OASIS; PALYNOLOGY; PALYNOFACIES; SEQUENCE; RECONSTRUCTION; PALYNOMORPHS	Shushan Basin is recently considered one of the important petroliferous basins in the north Western Desert of Egypt, where it contains multiple clastic reservoirs. National and international exploration companies are carrying out extensive correlations within the basin to detect the almost similar clastic reservoirs Alam El Bueib and Kharita formations. Stratigraphy of the Lower Cretaceous of Minqar-IX well in Shushan was previously established based on dinoflagellate cysts recovered from a few and widely spaced samples, where elastic units could not be differentiated. However, the current collection of a large number of closely spaced samples enabled the identification of five informal Lower Cretaceous spore-pollen palynozones (PZ) with high resolution. These zones are used to recognize unidentified elastic rock units and to provide an intrabasinal biostratigraphic correlation of the formations. Three palynozones (PZ 1-PZ 3) identify Alam El-Bueib Formation (?Berriasian-early Aptian). PZ 4 identifies Alamein Formation (late Aptian). PZ 5 corresponds to Kharita Formation (middle Albian). Results reflect the miospores as a powerful stratigraphic tool for dating the largely non-marine sequences, where diverse dinoflagellate cysts are almost lacking and/or facies-controlled. The use of biostratigraphic correlation of strata successions with monotone lithologies was helpful in identifying problematic formations, tracing their lateral facies change, and in detecting an unrecognized hiatus in the studied well.	[Mahmoud, Magdy S.; Deaf, Amr S.] Assiut Univ, Geol Dept, Fac Sci, Assiut 71516, Egypt; [Tamam, Mohamed A.; Khalaf, Miran M.] Sohag Univ, Geol Dept, Fac Sci, Sohag, Egypt	Egyptian Knowledge Bank (EKB); Assiut University; Egyptian Knowledge Bank (EKB); Sohag University	Mahmoud, MS (通讯作者)，Assiut Univ, Geol Dept, Fac Sci, Assiut 71516, Egypt.	magdysm@yahoo.com	Mahmoud, Magdy/ABD-1262-2020; Khalaf, Miran/JWO-5876-2024; Deaf, Amr/AAF-6269-2020	Khalaf, Miran/0000-0002-9561-6873; Deaf, Amr/0000-0002-5073-7911				Andrawis S.F., 1990, GEOLOGY EGYPT, P639; [Anonymous], 1974, B TEC PETROBRAS; [Anonymous], 1992, Western Desert, oil and gas fields (A comprehensive overview), P431; Aram R. 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Afr. Earth Sci.	MAR	2019	151						18	35		10.1016/j.jafrearsci.2018.11.019	http://dx.doi.org/10.1016/j.jafrearsci.2018.11.019			18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	HM9YR					2025-03-11	WOS:000459841400003
J	Keeler, DM; Grandal, MK; McCall, JR				Keeler, Devon M.; Grandal, Meghan K.; McCall, Jennifer R.			Brevenal, a Marine Natural Product, is Anti-Inflammatory and an Immunomodulator of Macrophage and Lung Epithelial Cells	MARINE DRUGS			English	Article						brevenal; marine natural product; immunomodulator; anti-inflammatory; cystic fibrosis; COPD; asthma; cytokine; chemokine; macrophage activation; macrophage phenotype; mucociliary clearance	DINOFLAGELLATE KARENIA-BREVIS; CHANGING EPIDEMIOLOGY; BREVETOXINS; MECHANISMS; TOXIN; MODEL	Chronic respiratory diseases, including chronic obstructive pulmonary disease (COPD), cystic fibrosis, and asthma, are some of the leading causes of illness and fatalities worldwide. The search for novel treatments led to the exploration of marine natural products as drug candidates to combat the debilitating effects of mucus accumulation and chronic inflammation. Previous research showed that an alga-derived compound, brevenal, could attenuate the effects of inflammatory agents, but the mechanisms by which it exerted its effects remained unclear. We investigated the effects of brevenal on lipopolysaccharide (LPS) induced cytokine/chemokine production from murine macrophages and human lung epithelial cells. It was found that brevenal reduces proinflammatory mediator secretion while preserving anti-inflammatory secretion from these cells. Furthermore, we found that brevenal does not alter cell surface Toll-like receptor 4 (TLR4) expression, thereby maintaining the cells' ability to respond to bacterial infection. However, brevenal does alter macrophage activation states, as demonstrated by reduced expression of both M1 and M2 phenotype markers, indicating this putative anti-inflammatory drug shifts innate immune cells to a less active state. Such a mechanism of action would be ideal for reducing inflammation in the lung, especially with patients suffering from chronic respiratory diseases, where inflammation can be lethal.	[Keeler, Devon M.; Grandal, Meghan K.; McCall, Jennifer R.] UNCW Ctr Marine Sci, 5600 Marvin K Moss Lane, Wilmington, NC 28409 USA	University of North Carolina; University of North Carolina Wilmington	McCall, JR (通讯作者)，UNCW Ctr Marine Sci, 5600 Marvin K Moss Lane, Wilmington, NC 28409 USA.	dmk9506@uncw.edu; grandal@musc.edu; mccalljr@uncw.edu	McCall, Jennifer/AFU-2750-2022		Cahill Program Award from the University of North Carolina Wilmington	Cahill Program Award from the University of North Carolina Wilmington	This research was funded in part by a Cahill Program Award from the University of North Carolina Wilmington.	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Drugs	MAR	2019	17	3							184	10.3390/md17030184	http://dx.doi.org/10.3390/md17030184			14	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	HW0UW	30897777	Green Published, Green Submitted, gold			2025-03-11	WOS:000466398200048
J	Deckers, J; Louwye, S				Deckers, Jef; Louwye, Stephen			A reinterpretation of the ages and depositional environments of the lower and middle Miocene stratigraphic records in a key area along the southern margin of the North Sea Basin	GEOLOGICAL MAGAZINE			English	Article						depositional environment; Genk Sand Member; Miocene; North Sea Basin	LOWER RHINE BASIN; BELGIUM; PALEOGEOGRAPHY; TERTIARY; SEQUENCE; BORDER; ORIGIN	The stratigraphic reinterpretation of the palynologically analysed Miocene succession of the Wijshagen borehole along the southern margin of the North Sea Basin allowed an age assessment - late Burdigalian to early Serravalian - for the Genk Sand Member of the Bolderberg Formation. The depositional environment varied during Burdigalian to Serravalian times from continental (peat formation) to open marine (glauconitic sands), respectively from south to north in the Roer Valley Rift System. The study area of the Wijshagen borehole is located in the central part of the Roer Valley Rift System between these extreme environments. During the Burdigalian, the glauconitic fine clayey sands of the Houthalen Sand Member were deposited in the study area. From the late Burdigalian onwards, the glauconite content decreased and lignite content increased as a result of high influx of clastic material in the Roer Valley Rift System, and marked the start of the deposition of the Genk Sand Member. The Genk Sand Member shows an overall coarsening-upwards trend, which is consistent with the gradual infill of the available accommodation space in the Roer Valley Rift System by northwest-prograding clastic delta sequences. Dinoflagellate cyst analyses indicate that the Genk Sand Member was largely deposited in a marginal marine environment with only short pulses of continental input. These pulses of continental input increase in a southerly or landward direction where they led to the development of thick lignite seams.	[Deckers, Jef] VITO, Flemish Inst Technol Res, Boeretang 200, B-2400 Mol, Belgium; [Louwye, Stephen] Univ Ghent, Dept Geol, Res Unit Palaeontol, Ghent, Belgium	VITO; Ghent University	Deckers, J (通讯作者)，VITO, Flemish Inst Technol Res, Boeretang 200, B-2400 Mol, Belgium.	jef.deckers@vito.be	; Louwye, Stephen/D-3856-2012	Deckers, Jef/0000-0002-5373-8733; Louwye, Stephen/0000-0003-4814-4313	Land and Soil Protection, Subsoil, and Natural Resources Division of the Flemish Government	Land and Soil Protection, Subsoil, and Natural Resources Division of the Flemish Government	We gratefully acknowledge financial support from the Land and Soil Protection, Subsoil, and Natural Resources Division of the Flemish Government. We would like to thank K. van Baelen for her work on the figures. We would also like to thank Dr T. Utescher and an anonymous reviewer for detailed and helpful comments.	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MAR	2019	156	3					525	532		10.1017/S0016756817000991	http://dx.doi.org/10.1017/S0016756817000991			8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	HL4AW					2025-03-11	WOS:000458658500007
J	Thoha, H; Muawanah; Intan, MDB; Rachman, A; Sianturi, OR; Sidabutar, T; Iwataki, M; Takahashi, K; Avarre, JC; Masseret, E				Thoha, Hikmah; Muawanah; Intan, Mariana D. Bayu; Rachman, Arief; Sianturi, Oksto Ridho; Sidabutar, Tumpak; Iwataki, Mitsunori; Takahashi, Kazuya; Avarre, Jean-Christophe; Masseret, Estelle			Resting Cyst Distribution and Molecular Identification of the Harmful Dinoflagellate <i>Margalefidinium polykrikoides</i> (Gymnodiniales, Dinophyceae) in Lampung Bay, Sumatra, Indonesia	FRONTIERS IN MICROBIOLOGY			English	Article						Margalefidinium polykrikoides; dinoflagellate; harmful algal blooms; resting and hyaline cysts; Indonesia	KOREAN COASTAL WATERS; COCHLODINIUM-POLYKRIKOIDES; ALEXANDRIUM-CATENELLA; PHYLOGENETIC-RELATIONSHIPS; UNARMORED DINOFLAGELLATE; COMPLEX DINOPHYCEAE; SP-NOV; SEDIMENTS; BLOOMS; MORPHOLOGY	Margalefidinium polykrikoides, an unarmored dinoflagellate, was suspected to be the causative agent of the harmful algal blooms - associated with massive fish mortalities - that have occurred continually in Lampung Bay, Indonesia, since the first bloom event in October 2012. In this study, after examination of the morphology of putative M. polykrikoides-like cysts sampled in bottom sediments, cyst bed distribution of this harmful species was explored in the inner bay. Sediment samples showed that resting cysts, including several morphotypes previously reported as M. polykrikoides, were most abundant on the northern coast of Lampung Bay, ranging from 20.6 to 645.6 cysts g(-1) dry sediment. Molecular phylogeny inferred from LSU rDNA revealed that the so-called Mediterranean ribotype was detected in the sediment while M. polykrikoides motile cells, four-cell chain forming in bloom conditions, belonged to the American-Malaysian ribotype. Moreover, hyaline cysts, exclusively in the form of four-cell chains, were also recorded. Overall, these results unequivocally show that the species M. polykrikoides is abundantly present, in the form of vegetative cells, hyaline and resting cysts in an Indonesian area.	[Thoha, Hikmah; Intan, Mariana D. Bayu; Rachman, Arief; Sianturi, Oksto Ridho; Sidabutar, Tumpak; Masseret, Estelle] Indonesian Inst Sci, Res Ctr Oceanog, Jakarta, Indonesia; [Muawanah] Directorate Gen Aquaculture, Main Ctr Marine Aquaculture Lampung, Lampung, Indonesia; [Iwataki, Mitsunori; Takahashi, Kazuya] Univ Tokyo, Asian Nat Environm Sci Ctr, Tokyo, Japan; [Avarre, Jean-Christophe] Univ Montpellier, ISEM, IRD, CNRS,EPHE, Montpellier, France; [Masseret, Estelle] Univ Montpellier, IRD, CNRS, Ifnamer,MARBEC, Montpellier, France	National Research & Innovation Agency of Indonesia (BRIN); Indonesian Institute of Sciences (LIPI); University of Tokyo; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Institut de Recherche pour le Developpement (IRD); Ifremer; Centre National de la Recherche Scientifique (CNRS); Universite de Montpellier	Avarre, JC (通讯作者)，Univ Montpellier, ISEM, IRD, CNRS,EPHE, Montpellier, France.	jean-christophe.avarre@ird.fr	Intan, Mariana/AAA-2212-2020; Sidabutar, Tumpak/GPP-3873-2022; Rachman, Arief/GWM-8363-2022; Avarre, Jean-Christophe/E-4170-2019; Takahashi, Kazuya/LCD-6164-2024; Iwataki, Mitsunori/H-9640-2019	Avarre, Jean-Christophe/0000-0001-6899-7052; Sianturi, Oksto Ridho/0000-0002-8805-6767; Intan, Mariana DB/0000-0002-7391-5979; Takahashi, Kazuya/0000-0003-1349-1120; Iwataki, Mitsunori/0000-0002-5844-2800; Rachman, Arief/0000-0001-8603-0611	Research Center for Oceanography-LIPI; Main Center for Marine Aquaculture of Lampung-Balai Besar Perikanan Budidaya Laut Lampung (Indonesia); Institut de Recherche pour le Developpement (IRD); University of Montpellier (France); JSPS KAKENHI [25304029]; Core-to-Core Program (B. Asia-Africa Science Platforms) of JSPS (Japan); Grants-in-Aid for Scientific Research [25304029] Funding Source: KAKEN	Research Center for Oceanography-LIPI; Main Center for Marine Aquaculture of Lampung-Balai Besar Perikanan Budidaya Laut Lampung (Indonesia); Institut de Recherche pour le Developpement (IRD); University of Montpellier (France); JSPS KAKENHI(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); Core-to-Core Program (B. Asia-Africa Science Platforms) of JSPS (Japan); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	This work was supported by the Research Center for Oceanography-LIPI, the Main Center for Marine Aquaculture of Lampung-Balai Besar Perikanan Budidaya Laut Lampung (Indonesia), the Institut de Recherche pour le Developpement (IRD) who also funded Estelle Masseret's research stay at the RCO-LIPI in Jakarta, the University of Montpellier (France) and the Grants-in-Aid for Scientific Research, JSPS KAKENHI 25304029, and the Core-to-Core Program (B. Asia-Africa Science Platforms) of JSPS (Japan).	Aditya V., 2013, Mar. Res. 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J	Mazzega, E; Beran, A; Cabrini, M; de Marco, A				Mazzega, Elisa; Beran, Alfred; Cabrini, Marina; de Marco, Ario			<i>In vitro</i> isolation of nanobodies for selective <i>Alexandrium minutum</i> recognition: A model for convenient development of dedicated immunoreagents to study and diagnostic toxic unicellular algae	HARMFUL ALGAE			English	Article						Dinoflagellate detection; Harmful algal bloom; Panning strategy; Fluobodies; Nanobodies	TAMARENSE SPECIES COMPLEX; SINGLE-DOMAIN ANTIBODIES; BLOOMS; DINOFLAGELLATE; MICROALGAE; SURFACE; ASSAY; GENE	At the present, the identification of planktonic species in coastal water is still a time intensive process performed by highly trained personnel that relies either on qPCR or on light microscopy observation and in vitro culturing. Furthermore, the increasing danger represented by Harmful Algal Blooms (HABs) inside phytoplankton community and the recent implementation of the legislation on ballast water management to prevent the introduction of HABs and NIS (Non Indigenous Species) urge the development of faster and reliable diagnostic methods. Immuno-based approaches could fulfil this need provided that the costs for antibody selection and production will be reduced. In this work it is demonstrated for the first time the feasibility to recover nanobodies (VHHs) selective for native surface epitopes of Alexandrium minutum by direct whole cell bio-panning using a pre-immune phage display library. The recombinant nature of VHHs enabled their rapid engineering into eGFP fluorescent reagents (fluobodies) that were produced recombinantly in bacteria and are directly suitable for fluorescence microscopy and flow cytometry. Immune-detection identified also cysts and anti-Alexandrium fluobodies showed no cross-reactivity with indigenous not-toxic phytoplankton microalgae belonging to different geni. The fluobodies were able to bind selectively to the target cells in both fixed and fresh samples with minimal processing.	[Mazzega, Elisa; de Marco, Ario] Univ Nova Gorica, Lab Environm & Life Sci, Nova Gorica, Slovenia; [Beran, Alfred; Cabrini, Marina] Ist Nazl Oceanog & Geofis Sperimentale OGS, Trieste, Italy	University of Nova Gorica; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale	de Marco, A (通讯作者)，Univ Nova Gorica, LELS, Vipavska Cesta 13, S-5000 Nova Gorica, Slovenia.	ario.demarco@ung.si	de Marco, Ario/A-2760-2014	de Marco, Ario/0000-0001-7729-819X; Beran, Alfred/0000-0003-3723-4161	ARRS program [P4-0107];  [1degrees str/0005]	ARRS program(Slovenian Research Agency - Slovenia); 	AdM and EM were supported by the ARRS program P4-0107. The microalgae strains were isolated in the frame of IPA Adriatic Cross-Border Cooperation Programme -strategic project Ballast Water Management System for Adriatic Sea Protection (BALMAS) (Project Code 1 degrees str/0005). 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J	Zhao, Y; Yu, RC; Kong, FZ; Wei, CJ; Liu, Z; Geng, HX; Dai, L; Zhou, ZX; Zhang, QC; Zhou, MJ				Zhao, Yue; Yu, Ren-Cheng; Kong, Fan-Zhou; Wei, Chuan-Jie; Liu, Ze; Geng, Hui-Xia; Dai, Li; Zhou, Zheng-Xi; Zhang, Qing-Chun; Zhou, Ming-Jiang			Distribution Patterns of Picosized and Nanosized Phytoplankton Assemblages in the East China Sea and the Yellow Sea: Implications on the Impacts of Kuroshio Intrusion	JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS			English	Article							AUREOCOCCUS-ANOPHAGEFFERENS HARGRAVES; COMMUNITY STRUCTURE; PICOPLANKTON DISTRIBUTION; HETEROTROPHIC BACTERIA; MARINE SYNECHOCOCCUS; WATER MASSES; PROCHLOROCOCCUS ECOTYPES; DINOFLAGELLATE CYSTS; SUBSURFACE WATER; PICOPHYTOPLANKTON	Kuroshio, the strongest west boundary current of the Pacific Ocean, has significant impacts on the oceanographic conditions and ecological processes of the Pacific-Asian marginal seas through exchange of water, heat, and materials. In two cruises organized in the East China Sea (ECS) and the Yellow Sea in the spring 2014, observations of picosized and nanosized phytoplankton assemblages using flow cytometry reflected potential impacts of Kuroshio intrusion on phytoplankton communities, particularly in the ECS. The distribution pattern of Prochlorococcus in the ECS clearly depicts the intrusion route of Nearshore Kuroshio Branch Current from the main stream of Kuroshio northeast to Taiwan Island to the coastal waters adjacent to the Changjiang River estuary, an important red tide zone in the coastal waters of China. High abundance of photosynthetic nanoeukaryotes in the coastal waters adjacent to the Changjiang River estuary reflects the occurrence of diatom and dinoflagellate blooms during the investigation. The presence of Prochlorococcus in the coastal waters adjacent to the Changjiang River estuary offers a strong evidence that waters and materials associated with Nearshore Kuroshio Branch Current could be transported into the red tide zone adjacent to the Changjiang River estuary and will affect dynamics of harmful algal blooms in this region. Plain Language Summary Kuroshio is the strongest west Pacific boundary current. The oceanographic and ecological processes of Pacific Asian marginal seas are strongly affected by Kuroshio and its branches. During spring 2014, two cruises were conducted in the East China Sea and the Yellow Sea to find out how Kuroshio intrusion influence the environment and phytoplankton there. Four phytoplankton assemblages with different distribution patterns were detected by flow-cytometry. The assemblage with larger cell size (nanoeukaryotes) preferred to live in the coastal waters and reflected harmful algal blooms in the sea area adjacent to Changjiang River estuary. The abundance of the smallest photosynthetic organism Prochlorococcus was the highest where Kuroshio main stream flows by. The distribution pattern of Prochlorococcus in the East China Sea well depicted the route of a branch stretched from Kuroshio to the coastal waters adjacent to Changjiang River estuary (Nearshore Kuroshio Branch Current), and Prochlorococcus could be an indicator to reflect the influence Kuroshio intrusion has on phytoplankton. The results provide important aspect that open ocean could affect coastal ecological problems related to phytoplankton, such as harmful algal blooms.	[Zhao, Yue; Yu, Ren-Cheng; Kong, Fan-Zhou; Geng, Hui-Xia; Dai, Li; Zhou, Zheng-Xi; Zhang, Qing-Chun; Zhou, Ming-Jiang] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Zhao, Yue; Yu, Ren-Cheng; Dai, Li] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China; [Yu, Ren-Cheng; Kong, Fan-Zhou; Zhang, Qing-Chun] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Yu, Ren-Cheng; Kong, Fan-Zhou; Wei, Chuan-Jie; Liu, Ze; Geng, Hui-Xia; Zhou, Zheng-Xi; Zhang, Qing-Chun] Ctr Ocean Mega Sci, Qingdao, Peoples R China; [Wei, Chuan-Jie] Chinese Acad Sci, Inst Oceanol, Engn & Technol Dept, Qingdao, Peoples R China; [Wei, Chuan-Jie; Liu, Ze] Qingdao Natl Lab Marine Sci & Technol, Lab Ocean Dynam & Climate, Qingdao, Peoples R China; [Liu, Ze] Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Institute of Oceanology, CAS	Yu, RC (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China.; Yu, RC (通讯作者)，Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China.; Yu, RC (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China.; Yu, RC (通讯作者)，Ctr Ocean Mega Sci, Qingdao, Peoples R China.	rcyu@qdio.ac.cn	lidong, dai/AGO-6525-2022; Zhou, Zhengxi/U-4968-2019; Yu, Rencheng/J-4450-2017; Geng, Hui-Xia/X-5380-2018	Yu, Rencheng/0000-0001-6430-9224; Zhou, Zhengxi/0000-0001-7482-4297; Geng, Hui-Xia/0000-0002-6398-7864; Dai, Lidong/0000-0002-9081-765X; Chuanjie, Wei/0000-0002-1430-4887	National key R&D Program of China [2017YFC1404304]; Qingdao National Laboratory for Marine Science and Technology [2016ASKJ02]; Shandong province; National Natural Science Foundation of China (NSFC) [U1606404]; Strategic Priority Research Program of Chinese Academy of Sciences (CAS) [XDA11020304]	National key R&D Program of China; Qingdao National Laboratory for Marine Science and Technology; Shandong province; National Natural Science Foundation of China (NSFC)(National Natural Science Foundation of China (NSFC)); Strategic Priority Research Program of Chinese Academy of Sciences (CAS)	The data of hydrographic parameters were downloaded from Marine Science Data Center of Institute of Oceanology, Chinese Academy of Sciences with permission (http://msdc.qdio.ac.cn/).Data of chlorophyll a concentration and phytoplankton assemblages were collected through cruises and can be found in the supporting information Table S1. This study was supported by The National key R&D Program of China (grant 2017YFC1404304), the Program of the Qingdao National Laboratory for Marine Science and Technology (grant 2016ASKJ02), the project jointly supported by Shandong province and the National Natural Science Foundation of China (NSFC; grant U1606404), and the Strategic Priority Research Program of Chinese Academy of Sciences (CAS; grant XDA11020304).	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Res.-Oceans	FEB	2019	124	2					1262	1276		10.1029/2018JC014681	http://dx.doi.org/10.1029/2018JC014681			15	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	HP7GR					2025-03-11	WOS:000461856400026
J	Harland, R; Asteman, IP; Nordberg, K				Harland, Rex; Asteman, Irina Polovodova; Nordberg, Kjell			Dinoflagellate cysts from the 'Anthropocene' of Gullmar Fjord, west coast of Sweden and their potential for monitoring climate change	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article							KOLJO-FJORD; BENTHIC FORAMINIFERA; OXYGEN DEPLETION; RECENT SEDIMENTS; REGIME SHIFT; MAJOR CHANGE; SILL FJORD; RECORD; PHYTOPLANKTON; PRESERVATION	A small set of samples from Gullmar Fjord, on the west coast of Sweden, together with published data, has allowed the investigation of the 'Anthropocene' within the fjord. The dinoflagellate cyst record and its statistical analysis fails to show any marked changes within the assemblages either across the proposed boundary or indeed within the youngest sediments at the top of the sequence. However there are some small scale differences in the youngest assemblages that are of interest. In particular these include quantitative shifts in the numbers of some of the species especially Pentapharsodinium dalei, which may be indicative of somewhat cooler environments linked to the winter North Atlantic Oscillation (NAO) and extra availability of nutrients from Ekman pumping. These small scale shifts in the assemblages point to clear dynamism within the phytoplankton populations reacting to both anthropogenic and natural environmental change; evidence of the complexity of the system. The proven utility of dinoflagellate cysts in charting climate change throughout both the Pleistocene and Holocene within Gullmar Fjord, and elsewhere along the west coast of Sweden is in marked contrast to the little change at the 'Anthropocene' boundary. Nonetheless the geographical position of the fjords along the Skagerrak are ideal to monitor environmental change within the North Sea basin and perhaps further afield in the eastern North Atlantic Ocean; especially since further climate change threatens regime change within the marine environment affecting tourism, industry and mariculture along the coast. (C) 2018 Elsevier B.V. All rights reserved.	[Harland, Rex] 50 Long Acre, Nottingham NG13 8AH, England; [Asteman, Irina Polovodova; Nordberg, Kjell] Univ Gothenburg, Dept Marine Sci, POB 461, SE-40530 Gothenburg, Sweden; [Asteman, Irina Polovodova] Marin Mattekn MMT Sweden AB, Sven Kallfelts Gata 11, S-42671 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				Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; Arndt DS, 2017, B AM METEOROL SOC, V98, pS1, DOI 10.1175/2017BAMSStateoftheClimate.1; Arneborg L, 2004, CONT SHELF RES, V24, P443, DOI 10.1016/j.csr.2003.12.005; Asteman IP, 2018, CLIM PAST, V14, P1097, DOI 10.5194/cp-14-1097-2018; Barton AD, 2016, P NATL ACAD SCI USA, V113, P2964, DOI 10.1073/pnas.1519080113; Beaugrand G, 2002, SCIENCE, V296, P1692, DOI 10.1126/science.1071329; Björk G, 2003, CONT SHELF RES, V23, P1143, DOI 10.1016/S0278-4343(03)00081-5; 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Palaeobot. Palynology	FEB	2019	261						31	40		10.1016/j.revpalbo.2018.11.009	http://dx.doi.org/10.1016/j.revpalbo.2018.11.009			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	HO1ZW					2025-03-11	WOS:000460712200004
J	Guédé, KÉ; Slimani, H; Yao, NJP; Chekar, M; Koffi, NJC; M'Hamdi, A; Mouah, R; Digbehi, BZ				Guede, Kore Elysee; Slimani, Hamid; Yao, Ngoran Jean-Paul; Chekar, Mouna; Koffi, N'zi Jean-Claude; M'Hamdi, Amel; Mouah, Raymond; Digbehi, Bruno Zeli			Late Cretaceous to Early Eocene dinoflagellate cysts from the "12 freres" borehole, Fresco, southwestern Cote d'Ivoire: Biostratigraphy and paleobiogeographic implication	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Cretaceous; Paleogene; Dinoflagellate cysts; Palynostratigraphy; Fresco; Cote d'Ivoire	WESTERN EXTERNAL RIF; TERTIARY BOUNDARY; CALCAREOUS NANNOPLANKTON; PALEOGENE BOUNDARY; NORTHERN APENNINES; BASIN; STRATIGRAPHY; PALYNOMORPHS; ASSEMBLAGES; TRANSITION	The Upper Cretaceous to lower Eocene sediments from the "12 Freres" borehole in Fresco, southwestern Cote d'Ivoire are here subject of a palynological study: systematic, palynostratigraphy and paleogeography. Eight thousand eight hundred and ten palynomorphs, including 68 species of dinoflagellate cysts (dinocysts), 14 species of spores and pollen grains and Chlorophyceae were identified. The biostratigraphy based on dinocyst marker events and compared with various reference sections from the Northern Hemisphere allowed us to refine to the stage level the Maastrichtian, Paleocene and Eocene deposits of the section. The dinocyst events, recorded from the base to the top of the studied section, include the last occurrences of Odontochitina operculata, Andalusiella ivoirensis, Cerodiniwn granulostriatum, Dinogymnium spp., Andalusiella spp., Cerodinium diebelii, highest relative abundances of Adnatosphaeridiwn vittatum, Kallosphaeridiwn yorubaense and highest relative abundances of Apectodinum spp. According to Lentin and Williams (1980), the observed dinocyst assemblages suggest a tropical to subtropical province for the studied deposits.	[Guede, Kore Elysee] Univ Man, UFR Geol & Min Sci, BPV 20, Man, Cote Ivoire; [Slimani, Hamid; Chekar, Mouna] Mohammed V Univ Rabat, Lab Geobiodivers & Nat Patrimony GEOBIO, Sci Inst, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco; [Guede, Kore Elysee; Yao, Ngoran Jean-Paul; Koffi, N'zi Jean-Claude; Mouah, Raymond; Digbehi, Bruno Zeli] Univ Felix Houphouet Boigny, UFR STRM, 22 PB 582, Abidjan 22, Cote Ivoire; [M'Hamdi, Amel] Univ Tunis El Manar, Fac Sci, Dept Geol, Res Unit UR 11 ES 15, Univ Campus 2092, El Manar Ii, Tunisia	Universite de Man; Mohammed V University in Rabat; Universite Felix Houphouet-Boigny; Universite de Tunis-El-Manar; Faculte des Sciences de Tunis (FST)	Guédé, KÉ (通讯作者)，Univ Man, UFR Geol & Min Sci, BPV 20, Man, Cote Ivoire.	elyseegk@hotmail.com	Elysee, Guede/ABE-3209-2021; Slimani, Hamid/AAL-4055-2020	Kore Elysee, Guede/0000-0003-1393-5078; Slimani, Hamid/0000-0001-6392-1913	UNESCO through ANESI; Mohammed V University [SVT 11/09]; National Center of Scientific Research, Morocco [URAC46]	UNESCO through ANESI; Mohammed V University(Mohammed V University in Rabat); National Center of Scientific Research, Morocco	The first author thanks PETROCI for providing him samples of the "12 freres" borehole and UNESCO through ANESI for financial support during this study. All the authors thank the Laboratory of Geo-Biodiversity and Natural Patrimony, (GEOBIO), Scientific Institute, Research Center of Geophysics, Natural Patrimony and Green Chemistry (GEOPAC), Mohammed V University of Rabat, Scientific Institute, where the study was carried out as part of two projects: SVT 11/09 (Mohammed V University) and URAC46 (National Center of Scientific Research, Morocco).	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J	Zhao, XQ; Dupont, L; Schefuss, E; Granger, R; Wefer, G				Zhao, Xueqin; Dupont, Lydie; Schefuss, Enno; Granger, Robyn; Wefer, Gerold			Late-Holocene oceanic variability in the southern Benguela region driven by interplay of upwelling, fluvial discharge, and Agulhas leakage	HOLOCENE			English	Article						Agulhas leakage; fluvial discharge; late-Holocene; organic-walled dinoflagellate cysts; paleoceanography; southern Benguela upwelling	WALLED DINOFLAGELLATE CYSTS; DECADAL VARIABILITY; PALYNOLOGICAL EVIDENCE; PRIMARY PRODUCTIVITY; QUATERNARY CLIMATE; SURFACE SEDIMENTS; MARINE-SEDIMENTS; ATLANTIC OCEANS; LATE PLIOCENE; DEEP-SEA	The southern Benguela upwelling system near the St. Helena Bay has been proposed to be affected by various factors, while few investigations about the late-Holocene oceanic conditions has been carried out in this area. To determine the oceanic variability and its forcing mechanisms in the southern Benguela region during the late-Holocene, we examined organic-walled dinoflagellate cyst (dinocyst) records from two marine sediment cores located in the southernmost and central Benguela upwelling system. We compare our results with other proxies including alkenone-derived SSTs, grain size, and coccolithophore assemblages from the same samples. The results indicate a distinctive behavior between the southernmost Benguela system and the central Benguela area. We infer that the oceanic conditions in these two regions are primarily governed by an interplay of wind-induced upwelling, fluvial discharge, and advection of cold sub-Antarctic waters, which is consistent with the current understanding of the paleoclimate conditions in this area. However, the findings also suggest that the southernmost Benguela system also receives additional effects of warm and saline waters via the Agulhas leakage, which has a clear influence on the oceanic conditions in this area.	[Zhao, Xueqin; Dupont, Lydie; Schefuss, Enno; Wefer, Gerold] Univ Bremen, Ctr Marine Environm Sci MARUM, Leobener Str 8, D-28359 Bremen, Germany; [Granger, Robyn] Univ Cape Town, Dept Oceanog, Rondebosch, South Africa	University of Bremen; University of Cape Town	Zhao, XQ (通讯作者)，Univ Bremen, Ctr Marine Environm Sci MARUM, Leobener Str 8, D-28359 Bremen, Germany.	snowybolter@gmail.com	Wefer, Gerold/S-2291-2016; Schefuss, Enno/A-7101-2015	Wefer, Gerold/0000-0002-6803-2020; Zhao, Xueqin/0000-0003-3354-3768; Schefuss, Enno/0000-0002-5960-930X	German Federal Ministry of Education and Research (BMBF) [03G0840A]	German Federal Ministry of Education and Research (BMBF)(Federal Ministry of Education & Research (BMBF))	This work was supported by the German Federal Ministry of Education and Research (BMBF) (Grant/Award Number: '03G0840A'). The investigations were conducted within the collaborative project 'Regional Archives for Integrated Investigations' (RAiN), which is embedded in the international research programme SPACES (Science Partnership for the Assessment of Complex Earth System Processes).	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J	Dybkjær, K; Rasmussen, ES; Sliwinska, KK; Esbensen, KH; Mathiesen, A				Dybkjaer, Karen; Rasmussen, Erik S.; Sliwinska, Kasia K.; Esbensen, Kim H.; Mathiesen, Anders			A palynofacies study of past fluvio-deltaic and shelf environments, the OligOcene-Miocene succession, North Sea Basin: A reference data set for similar Cenozoic systems	MARINE AND PETROLEUM GEOLOGY			English	Article						Palynofacies; Depositional environments; Fluvio-deltaic; Miocene; North Sea Basin	IODP EXPEDITION 313; SEQUENCE STRATIGRAPHY; UPPERMOST OLIGOCENE; CLIMATE DEVELOPMENT; BILLUND DELTA; LATE EOCENE; JYLLAND; CLASSIFICATION; DINOFLAGELLATE; ARCHITECTURE	Correct interpretations of depositional environments are fundamental for evaluating the geological history of a sedimentary basin. Palynofacies analyses are a valuable supplement to sedimentological and seismic studies. In order to develop a palynofacies reference dataset for fluvio-deltaic and shelfal successions, a study of the assemblages of sedimentary organic particles from seven different well-defined depositional environments within the uppermost Oligocene - lower Miocene succession onshore Denmark (eastern North Sea Basin) has been performed. The study deals with the following environments; floodplain, lagoon, washover-fan flat, prodelta, shoreface, offshore transition and shelf. The sedimentary organic particles were grouped into four major categories; 1) Structured wood particles, 2) Amorphous organic matter (AOM, in the present study mainly consisting of partly degraded vitrinite), 3) Cuticle and membranes and 4) Palynomorphs. The palynomorphs were grouped into eight subcategories; 1) Microspores, 2) Non-saccate pollen, 3) Bisaccate pollen, 4) Bonyococcus, 5) Other freshwater algae, 6) Fungal hyphae and -spores, 7) Acritarchs and 8) Organic-walled dinoflagellate cysts. A combination of a univariate box plots and a multivariate Principal Component Analysis (PCA) of the palynofacies data clear revealed the quantitative characteristics and variations within each discrete environment as well as their principal similarities and differences. In spite of some natural overlaps, for example between the lagoon and offshore transition environments, the data revealed distinct characteristics, e.g. a strong dominance of wood particles in the shoreface environment, a strong dominance of bisaccate pollen in the washover-fan flat environment and a near absence of dinocysts in the floodplain environment. An overall increase in relative abundances of dinocysts and a decrease in abundances of non-saccate pollen in the proximal-distal trend were also outlined. This study outlines a palynofacies reference dataset that can be used as a tool for interpreting depositional environments in equivalent settings, preferentially combined with other information such as seismic data, well logs, and/or lithology.	[Dybkjaer, Karen; Rasmussen, Erik S.; Sliwinska, Kasia K.; Esbensen, Kim H.; Mathiesen, Anders] Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Esbensen, Kim H.] KHE Consulting, Aldersrogade 8, DK-2100 Copenhagen, Denmark; [Esbensen, Kim H.] Aalborg Univ, Fredrik Bajers Vej 5, DK-9100 Aalborg, Denmark	Geological Survey Of Denmark & Greenland; Aalborg University	Dybkjær, K (通讯作者)，Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	kd@geus.dk	Dybkjær, Karen/G-5223-2018; Sliwinska, Kasia K./G-9097-2018	Sliwinska, Kasia K./0000-0001-5488-8832				[Anonymous], 1976, P 7 ANN M; Armstrong H. 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Pet. Geol.	FEB	2019	100						111	147		10.1016/j.marpetgeo.2018.08.012	http://dx.doi.org/10.1016/j.marpetgeo.2018.08.012			37	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	HK8EB		Green Submitted			2025-03-11	WOS:000458221100008
J	Bringué, M; Pospelova, V; Tappa, EJ; Thunell, RC				Bringue, Manuel; Pospelova, Vera; Tappa, Eric J.; Thunell, Robert C.			Dinoflagellate cyst production in the Cariaco Basin: A 12.5 year-long sediment trap study	PROGRESS IN OCEANOGRAPHY			English	Article						Southern Caribbean Sea; Upwelling; Seasonal variability; Interannual variability; Phytoplankton; Microzooplankton; El Nino	SEA-SURFACE TEMPERATURE; SANTA-BARBARA BASIN; SP-NOV DINOPHYCEAE; 1997-98 EL-NINO; ENVIRONMENTAL-CHANGE; THECA RELATIONSHIP; UPWELLING SYSTEM; CARIBBEAN SEA; PHYLOGENETIC POSITIONS; PALYNOLOGICAL EVIDENCE	Seasonal and interannual variability in dinoflagellate cyst production were assessed using a 12.5 year-long sediment trap time series from the Cariaco Basin (southern Caribbean Sea). This study constitutes the longest such time series published to date, providing robust patterns of variability for individual dinoflagellate cyst taxa as well as for major phytoplanktonic and (micro-)zooplanktonic groups at the site. Cyst production is interpreted in the context of physico-chemical properties measured in situ at the mooring site (primarily reflecting seasonal upwelling), and considering potential interactions with other major components of the pelagic food web (e.g., diatoms, ciliates, copepods). The time series consists in > 300 sediment trap samples, each representing similar to 14 days of sedimentation, collected at the CARIACO station between Nov. 8, 1996 and May 19, 2009. Mass fluxes of biogenic silica, calcium carbonate and organic carbon reflect dominantly the timing and strength of wind-driven, seasonal upwelling that brings colder, nutrient-rich waters to the surface, fostering primary productivity and the export of biogenous materials to the depths. On seasonal time scales, dinoflagellate cyst production is closely coupled with upwelling strength, with higher cyst fluxes consistently observed under active upwelling conditions (average of 50.5 x 10(3) cysts m(-2) day(-1)) compared to non-active upwelling intervals (29.0 x 10(3) cysts m(-2) day(-1)). Yearto-year variability is characterized by a large increase in cyst production observed over the last similar to 4 years of the time series (2006-2009) and minimum cyst fluxes recorded in the years 1998 and 1999, following the strong 1997/98 El Nino event. Dinoflagellate cyst assemblages are dominated by Brigantedinium spp. (59.1%), accompanied by Echinidinium delicatum (10.8%), Bitectatodinium spongium (8.4%), Spiny brown type A (2.9%) and Echinidinium spp. (2.4%). Cyst produced by both autotrophic and heterotrophic dinoflagellates generally respond positively to upwelling in the basin. Most cyst taxa are associated with active upwelling conditions (e.g., Bitectatodinium spongium, Brigantedinium spp., Echinidinium delicatum, Quinquecuspis concreta, Selenopemphix quanta, Spiny brown type C), with some showing higher fluxes under active but weak upwelling conditions (e.g., Echinidinium granulatum, Echinidinium spp., cyst of P. fukuyoi, Spiny brown type A). Other cyst taxa tend to show higher abundances at the onset of upwelling conditions (e.g., Echinidintum aculeatum, cyst of Protoperidinium steam) or following active upwelling intervals (e.g., Lejeunecysta marieae, Selenopemphix nephroides). The detailed response of each dinoflagellate cyst taxon to environmental variability is presented in the form of an atlas, providing photo-micrographs and detailing overall monthly production, contribution to the total trap assemblage as well as cyst production over the 12.5 years of the time series.	[Bringue, Manuel; Tappa, Eric J.; Thunell, Robert C.] Univ South Carolina, Sch Earth Ocean & Environm, 701 Sumter St,EWS 617, Columbia, SC 29208 USA; [Bringue, Manuel; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada; [Bringue, Manuel] Geol Survey Canada, 3303 33rd St NW, Calgary, AB T2L 2A7, Canada	University of South Carolina System; University of South Carolina Columbia; University of Victoria; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Bringué, M (通讯作者)，Univ South Carolina, Sch Earth Ocean & Environm, 701 Sumter St,EWS 617, Columbia, SC 29208 USA.; Bringué, M (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada.; Bringué, M (通讯作者)，Geol Survey Canada, 3303 33rd St NW, Calgary, AB T2L 2A7, Canada.	manuel.bringue@canada.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) Postdoctoral Fellowship (PDF); Advanced Support Program for Innovative Research Excellence (ASPIRE I - Track Lib) from the U. of South Carolina; NSERC; National Science Foundation (NSF) [OCE-9401537, OCE-9729697, OCE-0118349, OCE-0326313, OCE-0752037, OCE-1258991]	Natural Sciences and Engineering Research Council of Canada (NSERC) Postdoctoral Fellowship (PDF)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Advanced Support Program for Innovative Research Excellence (ASPIRE I - Track Lib) from the U. of South Carolina; NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); National Science Foundation (NSF)(National Science Foundation (NSF))	This research was funded by a Natural Sciences and Engineering Research Council of Canada (NSERC) Postdoctoral Fellowship (PDF) and an Advanced Support Program for Innovative Research Excellence (ASPIRE I - Track Lib) from the U. of South Carolina to MB, and an NSERC Discovery grant to VP. The CARIACO sediment trapping program was supported by National Science Foundation (NSF; grants OCE-9401537, OCE-9729697, OCE-0118349, OCE-0326313, OCE-0752037 and OCE-1258991). The authors wish to thank Claudia Benitez - Nelson and James L. Pinckney (U. of South Carolina) for providing mixed layer depth and HPLC data, and for constructive discussions on the basin's hydrology. The authors are grateful to Kenneth Mertens (IFREMER Concarneau) for his help in dinoflagellate cyst identification. We wish to thank Jon Liu (Geological Survey of Canada Calgary) for his help running the wavelet software in Matlab. The crew of the R/V Hermano Gines is also gratefully acknowledged for all operations at sea. The manuscript greatly benefited from constructive comments provided by two anonymous reviewers, for which the authors are grateful. 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J	Lira, B; Tavera, R				Lira, Beatriz; Tavera, Rosaluz			Life history and cell cycle of <i>Durinskia baltica</i> (Dinophyceae: Peridiniales) in culture	NOVA HEDWIGIA			English	Article						Dinophyceae; life cycle; ontogenesis; Peridiniales	SEXUAL REPRODUCTION; DINOFLAGELLATE; ENCYSTMENT; CYSTS; EXCYSTMENT	Durinskia baltica is a dinophyte whose presence has been reported over a wide ecological range (freshwater, brackish and marine environments) but has been studied mostly in temperate regions. Although there are some studies about its taxonomy, its life cycle is only partially known. Knowing the life cycle is important to understand various ecological aspects of dinophytes like bloom events, which have been reported recently in freshwater environments. In this study we describe the life cycle of a tropical freshwater strain of Durinskia baltica, identifying the different resting structures in asexual and sexual reproductive phases and the occurrence of meiosis. Cells were isolated from samples collected at a natural tropical freshwater site and maintained in culture. The photographic material was obtained with light and epifluorescence microscopy over alive culture material. We present the first description of the pellicle cyst that appears in the sexual phase of the life cycle and identify three alternative sexual routes: direct division of the planozygote by meiosis, temporary sexual encystment, and the formation of a hypnozygote with a short dormancy period. It was also found that the duration of the phases and meiosis timing are related directly to the route of the cycle that the organism follows. We conclude that, for D. baltica the presence of different routes after syngamy is a key response for the species' survival when short-term environmental changes (as in the studied water body) have more impact than seasonal transitions, as it occurs in temperate regions.	[Lira, Beatriz] Univ Nacl Autonoma Mexico, Posgrad Ciencias Mar & Limnol, Univ City 04510, DF, Mexico; [Tavera, Rosaluz] Univ Nacl Autonoma Mexico, Sci Fac, Dept Ecol & Nat Resources, Univ City 04510, DF, Mexico	Universidad Nacional Autonoma de Mexico; Universidad Nacional Autonoma de Mexico	Lira, B (通讯作者)，Univ Nacl Autonoma Mexico, Posgrad Ciencias Mar & Limnol, Univ City 04510, DF, Mexico.	bealirah@ciencias.unam.mx	Lira, Beatriz/LQL-2090-2024		Consejo Nacional de Ciencia y Tecnologia (CONACYT) [368241]	Consejo Nacional de Ciencia y Tecnologia (CONACYT)(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	We thank Consejo Nacional de Ciencia y Tecnologia (CONACYT) for awarding BL the PhD degree grant No. 368241. We also appreciate the contribution of Dr. Karin Rengefors of Lund University in Sweden and Dr. Matthew W. Parrow from the Department of Biology of the University of North Carolina at Charlotte for their valuable guidance and advice for the development of this paper. We also extend our gratefulness to Editor and adaptor Diego Salazar for proofreading the manuscript, and to two anonymous reviewers for the revision and comments of this paper.	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J	Zonneveld, KAF; Gray, DD; Kuhn, G; Versteegh, GJM				Zonneveld, Karin A. F.; Gray, Daniel D.; Kuhn, Gerhard; Versteegh, Gerard J. M.			Postdepositional aerobic and anaerobic particulate organic matter degradation succession reflected by dinoflagellate cysts: The Madeira Abyssal Plain revisited	MARINE GEOLOGY			English	Article							SELECTIVE PRESERVATION; DEEP-SEA; OXIC DEGRADATION; MARINE-SEDIMENTS; RESTING CYSTS; RECORD; CARBON; WATER; DECOMPOSITION; ENVIRONMENTS	We report on the succession of selective degradation of dinoflagellate cyst species that can be considered representative for discrete particulate organic matter (POM) classes of different degradability. The effects of anaerobic and aerobic degradation as well as bioturbation in a natural setting are documented in high resolution by means of palynological and geochemical analyses on Madeira Abyssal Plain A- and F-turbidites. These turbidites are unique as their initial ungraded sediments are affected by a downward penetrating oxydation front. Geochemical analyses document the presence of an active downward penetrating oxidation front in the A turbidite, and a palaeo-oxidation front in the F-turbidite. In this latter turbidite, several zones can be distinguished from top to bottom: an oxidised bioturbated zone, an oxidised but not-bioturbated zone, a visible paleooxidation front, and a narrow nitrogenous zone overlying unoxidised sediments. We are the first to report that anaerobic degradation within the nitrogenous zones in both turbidites affects cysts of some heterotrophic dinoflagellates. The cyst species affected (Echinidinium aculeatum, Echinidinium spp., cysts of Protoperidinium monospinum and Brigantedinium spp.) exponentially decrease in this zone that is further characterised by a strong decrease in sulphur content due to sulphide oxidation. Degradation rates are different for each species. These cysts of heterotrophic dinoflagellates consist of a nitrogen-rich glycan in contrast to the cellulosic cysts walls of phototrophic dinoflagellates. Therefore, our observation supports the hypothesis that the quality of organic matter plays an important role in OM degradation in oxygen deficient environments with N-rich OM being more labile than other components in these environments. All heterotrophic species are strongly affected by aerobic degradation with their cyst concentrations exponentially decreasing with increasing oxygen exposure. Degradation rates vary between species and range von highly degradable to slightly degradable. Most strongly affected are cysts of Protoperidinium monospinum, Brigantedinium spp., and Echinidinium spp. Increasingly less affected are: Selenopemphix nephroides, Selenopemphix quanta, other Peridinioids and Echinidinium aculeatum. An effect of aerobic degradation on photosynthetic species could only be observed for Pentapharsodinium dalei. All Impagidinium species appeared to be resistant to aerobic degradation. Despite having analysed only a limited number of samples in the bioturbated zone of the F-turbidite, we have strong indications that the bioturbation can lead to the degradation of POM that is not affected by aerobic degradation alone. The cyst species Spiniferites ramosus, Impagidinium paradoxum, Lingulodinium machaerophorum, Nematosphaeropsis labyrinthus, Spiniferites spp., Impagidinium sphaericum, Spiniferites elongates and Spiniferites mirabilis do not show concentration changes in the non-bioturbated aerobic sediments but their concentrations are considerably decreased in the bioturbated part of the F-turbidite. This supports the hypothesis that bioturbation can increase the degradation of POM by e.g. increasing oxygen exposure time and/or by an alteration of aerobic and anaerobic conditions. We furthermore show that the degradation rates of POM components represented by individual cyst species differ between zones with different redox and biological conditions. This implies that POM degradation reaction rate coefficients are environment dependent. Our observation that dinoflagellate cyst species have different degradation rates ranging from extremely labile to extremely recalcitrant within the individual redox/bioturbation zones supports the hypothesis that cyst walls have a species specific molecular structure. Our results support continuum models of organic matter degradation that assume a continuous distribution of organic matter reactivity.	[Zonneveld, Karin A. F.; Gray, Daniel D.; Versteegh, Gerard J. M.] Univ Bremen, MARUM Zentrum Marine Umweltwissensch, Leobenerstr 8, D-28359 Bremen, Germany; [Kuhn, Gerhard; Versteegh, Gerard J. M.] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany	University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Zonneveld, KAF (通讯作者)，Univ Bremen, MARUM Zentrum Marine Umweltwissensch, Leobenerstr 8, D-28359 Bremen, Germany.	kzonneveld@marum.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776; Kuhn, Gerhard/0000-0001-6069-7485	German Science Foundation (DFG) [ZO 114/13-1]; DFG Senatskommision for Ozeanforschung [MSM48]	German Science Foundation (DFG)(German Research Foundation (DFG)); DFG Senatskommision for Ozeanforschung	This study was carried out as part of the German Science Foundation (DFG) grant ZO 114/13-1. We thank the DFG Senatskommision for Ozeanforschung for financial support for the research cruise MSM48. We thank to anonymous reviewers for their constructive comments than greatly improved the quality of this paper. We thank the Captain and crew of the RV. Maria S. Merian for the constructive support during collection of the MAP cores.	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J	Saburova, M; Chomérat, N				Saburova, Maria; Chomerat, Nicolas			<i>Laciniporus arabicus</i> gen. et sp. nov. (Dinophyceae, Peridiniales), a new thecate, marine, sand-dwelling dinoflagellate from the northern Indian Ocean (Arabian Sea)<SUP>1</SUP>	JOURNAL OF PHYCOLOGY			English	Article						Arabian Sea; benthic dinoflagellates; Dinophyceae; Laciniporus arabicus; molecular phylogeny; morphology; Oman; Peridiniales; taxonomy	FRESH-WATER DINOFLAGELLATE; RDNA-BASED PHYLOGENY; BENTHIC DINOFLAGELLATE; EMENDED DESCRIPTION; MOLECULAR CHARACTERIZATION; TAXONOMIC REVISION; COOLIA-MALAYENSIS; KOREA MORPHOLOGY; COASTAL WATERS; JEJU ISLAND	A new thecate, photosynthetic, sand-dwelling marine dinoflagellate, Laciniporus arabicus gen. et sp. nov., is described from the subtidal sediments of the Omani coast in the Arabian Sea, northern Indian Ocean, based on detailed morphological and molecular data. Cells of L. arabicus are small (16.2-30.1 mu m long and 13.1-23.2 mu m wide), dorsoventrally compressed, with a small apical flap-shaped projection pointing to the left. The thecal plate pattern is distinguished by minute first precingular plate and sulcus, which extends into the epitheca, with large anterior and right sulcal plates. The Kofoidian thecal tabulation is Po, X, 4 ', 2a, 7 '', 6c, 6s, 5 ''', 2 ''''. Morphologically, the revealed plate pattern has an affinity to the Peridiniales, and LSU rDNA based phylogenetic analyses placed L. arabicus within the Thoracosphaeraceae, close to calcareous-cyst producing scrippsielloids, predatory pfiesteriaceans, and photosynthetic freshwater peridinioids Chimonodinium lomnickii and Apocalathium spp. However, the thecal plate arrangement of L. arabicus differs noticeably from any currently described dinoflagellates, and the species stands out from closely related taxa by extensive differences in physiology and ecology.	[Saburova, Maria] Kuwait Inst Sci Res, Ecosyst Based Management Marine Resources Program, Environm & Life Sci Res Ctr, POB 1638, Salmiya 22017, Kuwait; [Chomerat, Nicolas] IFREMER, LER BO, Stn Biol Marine, Pl Croix, F-29900 Concarneau, France	Kuwait Institute for Scientific Research; Ifremer	Saburova, M (通讯作者)，Kuwait Inst Sci Res, Ecosyst Based Management Marine Resources Program, Environm & Life Sci Res Ctr, POB 1638, Salmiya 22017, Kuwait.	msaburova@gmail.com	Saburova, Maria/JPK-3666-2023	Saburova, Maria/0000-0002-2204-2485	Foreign Fellow Scientist Program at the French Research Institute for Exploitation of the Sea (IFREMER, LER BO, Station de Biologie Marine, Concarneau, France)	Foreign Fellow Scientist Program at the French Research Institute for Exploitation of the Sea (IFREMER, LER BO, Station de Biologie Marine, Concarneau, France)	We highly appreciate Igor Polikarpov (Kuwait Institute for Scientific Research, Kuwait) valuable help with sampling and kind support during this work. We also thank Mikhail Chesalin (Fisheries Research Center, Salalah, Oman) for help in field sampling and hospitality in Salalah. The authors thank Gwenael Bilien (IFREMER, LER BO, Station de Biologie Marine, Concarneau, France) for her assistance with the molecular work, and Andrey Sazhin (P.P. Shirshov Institute of Oceanology, Moscow, Russia) for providing the optical facilities. We acknowledge the help of Ahlam S. Al-Kadi and Mohammed T. Rajab (Nanoscopy Science Center, Kuwait University, Kuwait) and Viktor Karlov (P.P. Shirshov Institute of Oceanology, Moscow, Russia) for their skilful technical assistance with SEM. Thanks to Jacob Larsen (IOC Science and Communication Centre on Harmful Algae, University of Copenhagen, Denmark) for his comments on an earlier version of the manuscript. We are grateful to anonymous reviewers for their detailed and constructive comments. 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Phycol.	FEB	2019	55	1					84	103		10.1111/jpy.12783	http://dx.doi.org/10.1111/jpy.12783			20	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	HM4PG	30179255	Green Published			2025-03-11	WOS:000459455700008
J	Liow, GR; Lau, WLS; Law, IK; Hii, KS; Noor, NM; Leaw, CP; Lim, PT				Liow, Guat Ru; Lau, Winnie Lik Sing; Law, Ing Kuo; Hii, Kieng Soon; Noor, Normawaty Mohammad; Leaw, Chui Pin; Lim, Po Teen			Phytoplankton community changes in Kuantan Port (Malaysia), with emphasis on the paralytic-shellfish toxin-producing dinoflagellate <i>Alexandrium tamiyavanichii</i>	REGIONAL STUDIES IN MARINE SCIENCE			English	Article						Alexandrium; Harmful algal bloom; Paralytic shellfish poisoning; qPCR; Saxitoxins	SETO INLAND SEA; COASTAL WATERS; LIFE-CYCLE; DINOPHYCEAE; IDENTIFICATION; COHORTICULA; ENCYSTMENT; EXCYSTMENT; DIVERSITY; DYNAMICS	The Kuantan Port (Pahang, Malaysia, South China Sea) is a multi-cargo port located on the east coast of Peninsular Malaysia. The port has served as an important seaway to major ports in Asia-Pacific regions. In November 2013 and August 2014, two incidents of paralytic shellfish poisoning (PSP) have been consecutively reported in the Port. In this study, a field investigation was undertaken in the Port from April 2015 to May 2016 as an effort to continuously monitor the occurrence of HAB species following the PSP episodes in the year 2013-2014. Phytoplankton and hydrographic samples were collected for quantitative and qualitative assessments in a monthly interval. To precisely quantify the PSP-toxins producing species Alexandrium tamiyavanichii, a real-time quantitative PCR (qPCR) assay was applied to detect the motile cells and cysts. The results revealed the presence of A. tamiyavanichii but with extremely low cell abundances (<0.1% of the total abundances). The species was found co-existed with other Alexandrium species. Alexandrium abundance was associated with salinity and nitrogen to phosphorus ratios but negatively correlated with PO4-P and NH4-N as revealed in the canonical correspondence analysis. Low cell abundances of diarrhetic-shellfish toxins producing dinoflagellates (Dinophysis spp.) and fish-killing species (Prorocentrum sigmoides, Akashiwo sanguinea, Noctiluca scintillans, Chattonella spp.) were also encountered in the port. The results of this study would provide useful baseline information for the assessment and management of ballast water in Malaysian ports and its territorial waters. (C) 2019 Elsevier B.V. All rights reserved.	[Liow, Guat Ru; Lau, Winnie Lik Sing; Law, Ing Kuo; Hii, Kieng Soon; Leaw, Chui Pin; Lim, Po Teen] Univ Malaya, Inst Ocean & Earth Sci, Bachok Marine Res Stn, Bachok 16310, Kelantan, Malaysia; [Noor, Normawaty Mohammad] Int Islamic Univ Malaysia, Kulliyyah Sci, Dept Marine Sci, Jalan Sultan Ahmad Shah, Kuantan 252, Pahang, Malaysia	Universiti Malaya; International Islamic University Malaysia	Leaw, CP; Lim, PT (通讯作者)，Univ Malaya, Inst Ocean & Earth Sci, Bachok Marine Res Stn, Bachok 16310, Kelantan, Malaysia.	cpleaw@um.edu.my; ptlim@um.edu.my	Hii, Kieng/R-2176-2017; Lim, Po Teen/C-9758-2013; Leaw, Chui Pin/F-5220-2012	Lim, Po Teen/0000-0003-2823-0564; Hii, Kieng Soon/0000-0001-6905-3045; Leaw, Chui Pin/0000-0003-3336-1438	Malaysian government through Ministry of Energy, Science, Technology, Environment and Climate Change, Sciencefund [04-01-03-SF1011]; Ministry of Education HiCoE Fund [IOES-2014C]; UM RU Fund [TU001-2018]; International Science and Technology Innovation Cooperation, MOST, China; MoE MyBrain Scholarship	Malaysian government through Ministry of Energy, Science, Technology, Environment and Climate Change, Sciencefund; Ministry of Education HiCoE Fund; UM RU Fund; International Science and Technology Innovation Cooperation, MOST, China; MoE MyBrain Scholarship	This work was funded by the Malaysian government through the Ministry of Energy, Science, Technology, Environment and Climate Change, Sciencefund [04-01-03-SF1011]; Ministry of Education HiCoE Fund [IOES-2014C]; UM RU Fund [TU001-2018]; International Science and Technology Innovation Cooperation, MOST, China [IF029-2018] to PT Lim. 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FEB	2019	26								100504	10.1016/j.rsma.2019.100504	http://dx.doi.org/10.1016/j.rsma.2019.100504			10	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	HN0EJ		Green Accepted			2025-03-11	WOS:000459857800004
J	Mangerud, G; Paterson, NW; Riding, JB				Mangerud, Gunn; Paterson, Niall W.; Riding, James B.			The temporal and spatial distribution of Triassic dinoflagellate cysts	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						Biostratigraphy; Dinoflagellate cysts; Geographical and temporal distributions; Late Triassic	KAPP TOSCANA GROUP; JURASSIC BOUNDARY; TRIASSIC/JURASSIC BOUNDARY; SEQUENCE STRATIGRAPHY; SHUBLIK FORMATION; TATRA MOUNTAINS; UPWELLING ZONE; CLIMATE-CHANGE; ARCTIC ALASKA; BARENTS SEA	The records of fossil dinoflagellate cysts from the Late Triassic, the time during which they first appear abundantly in the geological record, are reviewed. Most of the Triassic palynological literature pertains to terrestrial palynomorphs, thus it is challenging to establish a global picture of the temporal and spatial distribution of Late Triassic dinoflagellate cyst around the Pangea supercontinent. Moreover, data on Late Triassic dinoflagellate cysts are dispersed, and there are currently no records of dinoflagellate cysts from many marine successions. With the exception of an Australian record of the dinoflagellate cyst Sahulidinium ottii from the upper Mid Triassic, and a possible early Carnian occurrence of, among others, Rhaetogonyaulax in the Swiss Alps, cyst-forming dinoflagellates first appeared relatively synchronously around Pangea from the late Carnian. There are 36 species of pre-Norian species globally, whereas species richness exceeded 25 by the end of the Norian. During the Rhaetian, marine seaways had gradually opened due to sustained continental breakup, allowing the expansion of dinoflagellates into many European basins. New species are present, some known only from restricted areas, whereas others like Dapcodinium appear to have a global distribution. The majority of Triassic dinoflagellate cyst taxa do not extend into the Jurassic. (C) 2018 Elsevier B.V. All rights reserved.	[Mangerud, Gunn; Paterson, Niall W.] Univ Bergen, Dept Earth Sci, Allegaten 41, N-5007 Bergen, Norway; [Riding, James B.] British Geol Survey, Nottingham NG12 5GG, England	University of Bergen; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Mangerud, G (通讯作者)，Univ Bergen, Dept Earth Sci, Allegaten 41, N-5007 Bergen, Norway.	gunn.mangerud@uib.no	Mangerud, Gunn/ABD-2588-2020	Paterson, Niall W./0000-0002-2645-2086	Meltzer Research Fund; Faculty of Mathematics and Natural Sciences, University of Bergen; NERC [bgs05017] Funding Source: UKRI	Meltzer Research Fund; Faculty of Mathematics and Natural Sciences, University of Bergen; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	Professor Jan Golonka (AGH University of Science and Technology in Krakow, Poland) is acknowledged for providing the files of the paleogeographical map. Eva Bjorseth (University of Bergen) drafted the figures. We also thank from Przemyslaw Gedl and Daniel Mantle for their very constructive reviews, which substantially improved the manuscript. Thanks also go to Stephen Stukins who, in the initial phase of this project, guided us through the John Williams Index of Palaeopalynology reprint collection at the Natural History Museum, London. GM acknowledges the Meltzer Research Fund and the Faculty of Mathematics and Natural Sciences, University of Bergen for financial support for a research sabbatical. This paper was compiled during GM's recent sabbatical at the Department of Earth Sciences, Universidad de Concepcion, Chile and at GEUS, Copenhagen; both institutions are greatly acknowledged for providing facilities to undertake this work. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC).	Adloff M. 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Palynology	FEB	2019	261						53	66		10.1016/j.revpalbo.2018.11.010	http://dx.doi.org/10.1016/j.revpalbo.2018.11.010			14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	HO1ZW		Green Accepted			2025-03-11	WOS:000460712200006
J	Suzuki, Y; Suzuki, T; Awai, K; Shioi, Y				Suzuki, Yuya; Suzuki, Tomohiro; Awai, Koichiro; Shioi, Yuzo			Isolation and characterization of a tandem-repeated cysteine protease from the symbiotic dinoflagellate <i>Symbiodinium</i> sp. KB8	PLOS ONE			English	Article							CELL-DEATH	A cysteine protease belonging to peptidase C1A superfamily from the eukaryotic, symbiotic dinoflagellate, Symbiodinium sp. strain KB8, was characterized. The protease was purified to near homogeneity (566-fold) by (NH4)(2)SO4 fractionation, ultrafiltration, and column chromatography using a fluorescent peptide, butyloxycarbonyl-Val-Leu-Lys-4-methylcoumaryl-7-amide (Boc-VLK-MCA), as a substrate for assay purposes. The enzyme was termed VLKP (VLK protease), and its activity was strongly inhibited by cysteine protease inhibitors and activated by reducing agents. Based on the results for the amino acid sequence determined by liquid chromatography-coupled tandem mass spectrometry, a cDNA encoding VLKP was synthesized. VLKP was classified into the peptidase C1A superfamily of cysteine proteases (C1AP). The predicted amino acid sequence of VLKP indicated a tandem array of highly conserved precursors of C1AP with a molecular mass of approximately 71 kDa. The results of gel-filtration chromatography and SDS-PAGE suggested that VLKP exists as a monomer of 31-32 kDa, indicating that the tandem array is likely divided into two mass-equivalent halves that undergo equivalent posttranslational modifications. The VLKP precursor contains an inhibitor prodomain that might become activated after acidic autoprocessing at approximately pH 4. Both purified and recombinant VLKPs had a similar substrate specificity and kinetic parameters for common C1AP substrates. Most C1APs reside in acidic organelles such as the vacuole and lysosomes, and indeed VLKP was most active at pH 4.5. Since VLKP exhibited maximum activity during the late logarithmic growth phase, these attributes suggest that, VLKP is involved in the metabolism of proteins in acidic organelles.	[Suzuki, Yuya; Awai, Koichiro; Shioi, Yuzo] Shizuoka Univ, Grad Sch Sci, Shizuoka, Japan; [Suzuki, Tomohiro] Shizuoka Univ, Res Inst Green Sci & Technol, Shizuoka, Japan; [Awai, Koichiro] Shizuoka Univ, Elect Res Inst, Hamamatsu, Shizuoka, Japan; [Awai, Koichiro] JST, PRESTO, Kawaguchi, Saitama, Japan; [Suzuki, Tomohiro] Utsunomiya Univ, Ctr Biosci Res & Educ, Utsunomiya, Tochigi, Japan	Shizuoka University; Shizuoka University; Shizuoka University; Japan Science & Technology Agency (JST); Utsunomiya University	Awai, K (通讯作者)，Shizuoka Univ, Grad Sch Sci, Shizuoka, Japan.; Awai, K (通讯作者)，Shizuoka Univ, Elect Res Inst, Hamamatsu, Shizuoka, Japan.; Awai, K (通讯作者)，JST, PRESTO, Kawaguchi, Saitama, Japan.	awai.koichiro@shizuoka.ac.jp	Awai, Koichiro/B-5119-2010	Awai, Koichiro/0000-0002-1731-7499; Suzuki, Tomohiro/0000-0002-2444-5288	Precursory Research for Embryonic Science and Technology program of the Japanese Science and Technology Agency	Precursory Research for Embryonic Science and Technology program of the Japanese Science and Technology Agency	This work was supported in part by the Precursory Research for Embryonic Science and Technology program of the Japanese Science and Technology Agency to KA, and there was no additional external funding received for this study. The funder had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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J	Clotten, C; Stein, R; Fahl, K; Schreck, M; Risebrobakken, B; De Schepper, S				Clotten, Caroline; Stein, Ruediger; Fahl, Kirsten; Schreck, Michael; Risebrobakken, Bjorg; De Schepper, Stijn			On the causes of Arctic sea ice in the warm Early Pliocene	SCIENTIFIC REPORTS			English	Article							DINOFLAGELLATE CYST; NORDIC SEAS; BARENTS SEA; OCEAN; CIRCULATION; GREENLAND; ICELAND; VARIABILITY; HISTORY; MARINE	Scattered and indirect evidence suggests that sea ice occurred as far south as the Iceland Sea during the Early Pliocene, when the global climate was warmer than present. However, conclusive evidence as well as potential mechanisms governing sea ice occurrence outside the Arctic Ocean during a time with elevated greenhouse gas concentrations are still elusive. Here we present a suite of organic biomarkers and palynological records from the Iceland Sea and Yermak Plateau. We show that sea ice appeared as early as similar to 4.5 Ma in the Iceland Sea. The sea ice either occurred seasonally or was transported southward with the East Greenland Current. The Yermak Plateau mostly remained free of sea ice and was influenced dominantly by Atlantic water. From similar to 4.0 Ma, occurrence of extended sea ice conditions at both the Yermak Plateau and Iceland Sea document a substantial expansion of sea ice in the Arctic. The expansion occurred contemporaneous with increased northward heat and moisture transport in the North Atlantic region, which likely led to a fresher Arctic Ocean that favors sea ice formation. This extensive sea ice cover along the pathway of the East Greenland Current gradually isolated Greenland from warmer Atlantic water in the Late Pliocene, providing a positive feedback for ice sheet expansion in Greenland.	[Clotten, Caroline] Bjerknes Ctr Climate Res, Uni Res Climate, Jahnebakken 5, N-5007 Bergen, Norway; [Stein, Ruediger; Fahl, Kirsten] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Am Alten Hafen 26, D-27568 Bremerhaven, Germany; [Stein, Ruediger] Univ Bremen, MARUM, POB 330440, D-28334 Bremen, Germany; [Stein, Ruediger] Univ Bremen, Fac Geosci, POB 330440, D-28334 Bremen, Germany; [Schreck, Michael] UiT Arctic Univ Norway Tromso, Dept Geosci, POB 6050, N-9037 Tromso, Norway; [Risebrobakken, Bjorg; De Schepper, Stijn] Bjerknes Ctr Climate Res, NORCE Norwegian Res Ctr, Bergen, Norway	Bjerknes Centre for Climate Research; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Bremen; University of Bremen; UiT The Arctic University of Tromso; Bjerknes Centre for Climate Research; Norwegian Research Centre (NORCE)	Clotten, C (通讯作者)，Bjerknes Ctr Climate Res, Uni Res Climate, Jahnebakken 5, N-5007 Bergen, Norway.	caroline.clotten@gmx.de	; Risebrobakken, Bjorg/Y-1551-2018; De Schepper, Stijn/A-2836-2011	Fahl, Dr., Kirsten/0000-0001-9317-4656; Risebrobakken, Bjorg/0000-0002-7206-2193; De Schepper, Stijn/0000-0002-6934-0914; Stein, Ruediger/0000-0002-4453-9564	Research Council of Norway [229819]; RCN grant [221712]	Research Council of Norway(Research Council of Norway); RCN grant	This research was supported by the Research Council of Norway grant 229819 (C.C., S.D.S.). B.R. acknowledges support from RCN grant 221712. We like to thank S. Belt (Biogeochemistry Research Centre, University of Plymouth, UK) for providing the 7-HND standard for IP<INF>25</INF> quantification. We thank W. Luttmer for lab assistance, and A. Wuelbers and W. Hale at the IODP Bremen Core Repository for their help during sampling.	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J	Morquecho, L				Morquecho, Lourdes			<i>Pyrodinium bahamense</i> One the Most Significant Harmful Dinoflagellate in Mexico	FRONTIERS IN MARINE SCIENCE			English	Review						Pyrodinium bahamense; Mexico; harmful blooms; saxitoxins; PSP	TODOS-SANTOS BAY; ALGAL BLOOMS; PACIFIC COAST; SUBTROPICAL LAGOON; CYST DISTRIBUTION; TROPICAL PACIFIC; RED TIDE; GULF; SEDIMENTS; PLATE	Pyrodinium bahamense produces saxitoxins and can cause paralytic shellfish poisoning (PSP). This species has caused more human illnesses and fatalities than any other toxic dinoflagellate in Mexico. The distribution of dinoflagellate cysts with their vegetative stage is broad, mainly along Mexican Pacific coasts from the central Gulf of California to Chiapas, as well as in the southern Gulf of Mexico and the Mexican Caribbean Sea on the Atlantic coast. In vitro germination of living cysts from the southern Gulf of California occurs under thermophilic (20-35 degrees C) and euryhaline (20-35 ups) conditions. Blooms occurred typically during summer rainy season (June through September), inside of restricted shallow lagoons surrounded by mangrove forests. The data obtained so far on P. bahamense spatial and population variability in Mexican Pacific and the Gulf of Mexico, suggest a seasonal and latitudinal pattern. Also, in these regions, the abundance, seasonality, and species distribution tend to decrease from tropical to subtropical areas. The local strain toxicity has only been corroborated in one isolate from the southern Gulf of California, which exhibited a high saxitoxin concentration of 95 pg STX eq cell(-1). PSP outbreaks linked with P. bahamense in the Gulf of Tehuantepec from 1989 to 2007, caused at least similar to 200 human cases, with 15 fatalities. This mini-review ends with a viewpoint of management and research strategies to better understand the factors that play essential roles in the bloom dynamics and toxicity of this species.	[Morquecho, Lourdes] Ctr Invest Biol Noroeste, La Paz, Mexico	Telefonica SA; CIBNOR - Centro de Investigaciones Biologicas del Noroeste	Morquecho, L (通讯作者)，Ctr Invest Biol Noroeste, La Paz, Mexico.	lamorquecho@cibnor.mx	Morquecho, Lourdes/JPY-0626-2023	Morquecho, Lourdes/0000-0003-2963-8836	CIBNOR project [20014]	CIBNOR project	This work was supported by the CIBNOR project 20014 (Coleccion de Dinoflagelados Marinos).	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Mar. Sci.	JAN 23	2019	6								1	10.3389/fmars.2019.00001	http://dx.doi.org/10.3389/fmars.2019.00001			8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	LR6VW		gold			2025-03-11	WOS:000535831200001
J	Khanolkar, S; Sharma, J				Khanolkar, Sonal; Sharma, Jyoti			Record of Early to Middle Eocene paleoenvironmental changes from lignite mines, western India	JOURNAL OF MICROPALAEONTOLOGY			English	Article							OLIGOCENE DINOFLAGELLATE CYSTS; THERMAL MAXIMUM; FORAMINIFERAL MORPHOGROUPS; VASTAN LIGNITE; PALEOCENE; KUTCH; CLIMATE; BASIN; AGE; BIOSTRATIGRAPHY	Various Eocene hyperthermal events have been recorded from lignite sections of western India in the past decade. To infer the paleoenvironment, during a warm paleotropical climate of India, we have assessed multiple microfossil groups like pollen/spores, dinoflagellates and foraminifera from Early Eocene lignite mine sections from the Cambay (Surkha) and Barmer (Giral) basins and Middle Eocene sections from the Kutch Basin (Matanomadh and Panandhro mines) of western India. The Surkha and Giral sections exhibit a dominance of rainforest elements (Arengapollenites achinatus, Longapertites retipilatus), thermophilic mangrove palm Nypa and (sub)tropical dinoflagellate cyst Apectodinium, Cordosphaeridium and Kenleyia. This palynomorph assemblage is indicative of a marginal marine setting within a hot and humid climate. During the Middle Eocene, the diversity of dinocyst assemblage increased and a decrease in percentage of mangrove elements was observed in the Matanomadh and Panandhro mine sections of the Kutch Basin as compared to the Early Eocene sections of western India. Bloom of triserial planktic (Jenkinsina columbiana) and rectilinear benthic (Brizalina sp., Trifarina advena rajasthanensis) foraminifera indicates eutrophic conditions of deposition during the Late Lutetian-Early Bartonian in the lignite sections of the Kutch Basin which later changed to oligotrophic, open marine conditions towards the Bartonian (planktic E12 zone). This change to oligotrophic conditions coincides with a drastic increase in diversity of planktic foraminifera in the top portion of lignite mines of the Kutch Basin which may be correlated with the Kirthar-Wilson Bluff transgression event in the Bartonian observed across basins in India, Pakistan and Australia potentially linked to sea level rise around the Middle Eocene Climatic Optimum.	[Khanolkar, Sonal] Indian Inst Technol Kanpur, Dept Earth Sci, Kanpur, Uttar Pradesh, India; [Sharma, Jyoti] Univ Mumbai, Dept Geol, KJ Somaiya Coll Sci & Commerce, Mumbai, India	Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Kanpur; University of Mumbai	Khanolkar, S (通讯作者)，Indian Inst Technol Kanpur, Dept Earth Sci, Kanpur, Uttar Pradesh, India.	sonal.k.12@gmail.com	Sharma, Jyoti/GLQ-9140-2022	Khanolkar, Sonal/0000-0002-7911-1699	Department of Science and Technology, India [DST/INSPIRE/04/2016/002525, DST-WOSA PSR/WOS A/ES_31/2011]	Department of Science and Technology, India(Department of Science & Technology (India))	Sonal Khanolkar and Jyoti Sharma thank the Department of Science and Technology, India (project nos. DST/INSPIRE/04/2016/002525 and DST-WOSA PSR/WOS A/ES_31/2011) for providing the funding for carrying out this research work. Jyoti Sharma and Sonal Khanolkar are grateful to the Indian Institute of Technology Bombay and Indian Institute of Technology Kanpur for providing the facilities to carry out this work. We are thankful to the two anonymous reviewers and the handling editor Francesca Sangiorgi for the constructive comments which helped us improve the manuscript. We would like to dedicate this paper to Pratul Kumar Saraswati, IIT Bombay, who has been a motivation for our work and has played an important role in revising the Paleogene biostratigraphy of western India. Sonal Khanolkar would like to thank Manudeo Singh for help with the preparation of figures.	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J	Warny, S; Kymes, CM; Askin, R; Krajewski, KP; Tatur, A				Warny, Sophie; Kymes, C. Madison; Askin, Rosemary; Krajewski, Krzysztof P.; Tatur, Andrzej			Terrestrial and marine floral response to latest Eocene and Oligocene events on the Antarctic Peninsula	PALYNOLOGY			English	Article						Antarctica; Seymour Island; King George Island; palynology; Eocene; Oligocene	KING-GEORGE-ISLAND; SOUTH SHETLAND ISLANDS; LA MESETA FORMATION; SEYMOUR-ISLAND; STABLE-ISOTOPE; CLIMATE; SEA; STRATIGRAPHY; FACIES; VEGETATION	Palynological results from opposite sides of the northernmost Antarctic Peninsula provide insight on terrestrial vegetation and sea-surface conditions immediately before the Eocene-Oligocene transition (EOT), through Early Oligocene glacial conditions and the subsequent Late Oligocene interglacial interval. A latest Eocene sample set from the uppermost La Meseta Formation on Seymour Island, James Ross (back-arc) Basin, records a low-diversity Nothofagus (southern beech)-dominated vegetation with some podocarp conifers similar to Valdivian-type forest found today in Chile and Argentina. Marine organic-walled phytoplankton include leiospheres and Eocene dinoflagellate cysts such as Vozzhennikovia rotunda, V. apertura, Senegalinium asymmetricum and Spinidinium macmurdoense. Immediately before the EOT near the top of the section the decrease in terrestrial palynomorphs, increase in reworked specimens, disappearance of key dinocysts, and overwhelming numbers of sea-ice-indicative leiospheres plus the small dinoflagellate cyst Impletosphaeridium signal the onset of glacial conditions in a subpolar climate. Early to Late Oligocene samples from the Polonez Cove and Boy Point formations on King George Island, South Shetland Islands (magmatic arc), yielded an extremely depauperate terrestrial flora, likely resulting in part from poor vegetation cover during the Polonez Glaciation but also because of destruction of vegetation due to continued regional volcanism. The prevalence of sea-ice-indicative leiospheres in the marine palynomorph component is consistent with polar to subpolar conditions during and following the Polonez Glaciation.	[Warny, Sophie; Kymes, C. Madison] LSU Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA; [Warny, Sophie] LSU Museum Nat Sci, 109 Foster Hall, Baton Rouge, LA 70803 USA; [Krajewski, Krzysztof P.] Polish Acad Sci, Inst Geol Sci, Twarda 51-55, PL-00818 Warsaw, Poland; [Tatur, Andrzej] Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland	Louisiana State University System; Louisiana State University; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; University of Warsaw	Warny, S (通讯作者)，LSU Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA.; Warny, S (通讯作者)，LSU Museum Nat Sci, 109 Foster Hall, Baton Rouge, LA 70803 USA.	swarny@lsu.edu	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X	Polish Ministry of Science and Higher Education [DWM/N8IPY/2008]; US National Science Foundation [ANT-1048343]; Office of Polar Programs (OPP); Directorate For Geosciences [1048343] Funding Source: National Science Foundation	Polish Ministry of Science and Higher Education(Ministry of Science and Higher Education, Poland); US National Science Foundation(National Science Foundation (NSF)); Office of Polar Programs (OPP); Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This work was supported by the Polish Ministry of Science and Higher Education (to KPK and AT) [grant number DWM/N8IPY/2008]; and the US National Science Foundation (to SW) [grant number ANT-1048343].	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J	Hartman, JD; Sangiorgi, F; Bijl, PK; Versteegh, GJM				Hartman, Julian D.; Sangiorgi, Francesca; Bijl, Peter K.; Versteegh, Gerard J. M.			<i>Nucicla umbiliphora</i> gen. et sp. nov.: a Quaternary peridinioid dinoflagellate cyst from the Antarctic margin	PALYNOLOGY			English	Article						protoperidinioid; dinoflagellate cyst; East Antarctica; Antarctic shelf; Quaternary	PRIMARY PRODUCTIVITY; SURFACE SEDIMENTS; SEASONAL CYCLE; WILKES LAND; ROSS SEA; PHYTOPLANKTON; COMMUNITY; NUTRIENTS; PACIFIC; SECTOR	In the southern high latitudes, dinoflagellate cysts are an important microfossil group for both biostratigraphic and palaeoenvironmental interpretations purposes. In light of this, the peridinioid dinoflagellate cyst Nucicla umbiliphora gen. et sp. nov. from the Antarctic margin is formally described. Nucicla is dorsoventrally compressed, has a rounded pentagonal outline in dorso-ventral view, an epicyst that is only half as high as the hypocyst, an unusual archaeopyle formed by the loss of the three anterior intercalary plates, and a posterior sulcal plate that is positioned at the antapex. The species N. umbiliphora is characterised by a scabrate cyst wall and possesses undulated and/or crenulated folds/ridges. It has been so far exclusively found in Quaternary sediments obtained from the East Antarctic continental shelf and the Ross Sea. Although the dinoflagellate producing this cyst is as yet unknown, its brown color and the lack of autofluorescence suggest that the motile cell is likely a heterotrophic Protoperidinium species. As such, N. umbiliphora might benefit from the phytoplankton blooms occurring close to the Antarctic margin after seasonal sea-ice retreat.	[Hartman, Julian D.; Sangiorgi, Francesca; Bijl, Peter K.] Univ Utrecht, Marine Palynol & Paleoceanog, Dept Earth Sci, Princetonlaan 6a, NL-3584 CB Utrecht, Netherlands; [Versteegh, Gerard J. M.] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany	Utrecht University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Hartman, JD (通讯作者)，Univ Utrecht, Marine Palynol & Paleoceanog, Dept Earth Sci, Princetonlaan 6a, NL-3584 CB Utrecht, Netherlands.	juulhartman@gmail.com	; Versteegh, Gerard J.M./H-2119-2011	Hartman, Julian/0000-0001-6256-9989; Bijl, Peter/0000-0002-1710-4012; Versteegh, Gerard J.M./0000-0002-9320-3776; Sangiorgi, Francesca/0000-0003-4233-6154	Nederlandse Organisatie voor Wetenschappelijk Onderzoek [866.10.110]	Nederlandse Organisatie voor Wetenschappelijk Onderzoek(Netherlands Organization for Scientific Research (NWO))	This work was supported by the Nederlandse Organisatie voor Wetenschappelijk Onderzoek [grant number 866.10.110].	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J	Riding, JB				Riding, James B.			The literature on Triassic, Jurassic and earliest Cretaceous dinoflagellate cysts: Supplement 3	PALYNOLOGY			English	Article						biostratigrapy; dinoflagellate cysts; literature analysis and compilation; Triassic, Jurassic and earliest Cretaceous; worldwide	KRAKOW-SILESIA HOMOCLINE; ORE-BEARING CLAYS; TERRESTRIAL ECOSYSTEM CHANGE; KAPP TOSCANA GROUP; DEPOSITIONAL ENVIRONMENT; AGARDHFJELLET FORMATION; SEQUENCE STRATIGRAPHY; WESTERN CARPATHIANS; LUSITANIAN BASIN; FALKLAND PLATEAU	Since the production of three literature compilations in 2012, 2013 and 2014, 266 further published contributions on Triassic, Jurassic and earliest Cretaceous (Berriasian) dinoflagellate cysts were issued between April 2014 and January 2018, or have been discovered. These 266 items are listed alphabetically herein with full details, including digital object identifier (doi) numbers where applicable. A full description of each publication as a string of keywords is given. These studies are placed in one or more of 14 global regions, and the most significant contributions are reviewed for all these areas except Central America. The region with the most studies is West Europe (37.2%), but sub-Arctic Russia (10.5%), the Arctic region (10.2%), East Europe (7.1%) and sub-Arctic North America (4.1%) are also well represented. The proportions of these publications over the Triassic, Early Jurassic, Middle Jurassic, Late Jurassic and Jurassic-Cretaceous transition intervals are relatively similar. However, the Middle Jurassic is best represented, and the Triassic has the smallest number of contributions.	[Riding, James B.] British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk			NERC [bgs05017] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Abbink O, 2001, GLOBAL PLANET CHANGE, V30, P231, DOI 10.1016/S0921-8181(01)00101-1; Abbink O.A., 1998, LAB PALAEOBOTANY PAL, V8, P192; ALBERT N R, 1984, Palynology, V8, P233; ALBERT NR, 1986, MICROPALEONTOLOGY, V32, P303, DOI 10.2307/1485724; [Anonymous], 1980, Palaeontology; [Anonymous], GOLD ANN M AASP NOTT; [Anonymous], SCI MAT JURASSIC SYS; [Anonymous], 9210 GEOL SURV CAN; [Anonymous], B CANADIAN PETROLEUM; [Anonymous], NEFTEGASOVAA GEOLOGI; [Anonymous], PALYNOLOGY; [Anonymous], 1996, DANMARKS GRONLANDS G; [Anonymous], PALYNOLOGY; [Anonymous], AUST PET PROD EXPLOR; [Anonymous], THESIS; [Anonymous], SEDIMENTOLOGY PARALI; [Anonymous], 1984, P YORKSHIRE GEOLOGIC; [Anonymous], SCI MAT 5 ALL RUSS M; [Anonymous], INITIAL REPORTS DEEP; [Anonymous], 4 INT C MOD FOSS DIN; [Anonymous], 2015, Archives des Sciences; [Anonymous], THIRD INTERNATIONAL; [Anonymous], GEOLOGICAL SURVEY DE; [Anonymous], DINO 7 7 INT C MOD F; [Anonymous], 2016, GEN STRATIGRAPHIC SC; [Anonymous], GEOSCIENCE MAN; [Anonymous], SCI MAT PHANEROZOIC; [Anonymous], 1998, GEOLOGIE FRANCE; [Anonymous], AMERICAN ASSOCIATION; [Anonymous], PALYNOLOGY; [Anonymous], 2012, ALGOLOGIA; [Anonymous], PALYNOLOGY; [Anonymous], RAPPORT BOTANISK SER; [Anonymous], 2016, B ASOC LATINOAM PALE; [Anonymous], PALYNOLOGY; [Anonymous], PALYNOLOGY; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], GOLDEN ANNIVERSARY M; [Anonymous], SCI MAT JURASSIC SYS; [Anonymous], DINO 7 7 INT C MOD F; [Anonymous], 2005, Micropalaeontology of the Qiangtang Basin; [Anonymous], THESIS; [Anonymous], 2154 GEOL SURV CAN; [Anonymous], SCI MAT JURASSIC SYS; [Anonymous], PALYNOLOGY; [Anonymous], 1988, DINOFLAGELLATE CYSTS; [Anonymous], PALYNOLOGY; [Anonymous], 1993, PETROLEUM GEOLOGY NW; [Anonymous], PALYNOLOGY; [Anonymous], HIGH RESOLUTION SEQU; [Anonymous], PALAEONTOLOGY STRATI; [Anonymous], B CANADIAN PETROLEUM; [Anonymous], NORTHERN CARNARVON B; [Anonymous], 35 TH INTERNATIONAL; [Anonymous], PALYNOLOGY; [Anonymous], THESIS; [Anonymous], 2012, THESIS AUSTR NATL U; [Anonymous], PALYNOLOGY; [Anonymous], 2016, 12 JUR C WORKSH ICS; [Anonymous], 1996, Palynology: principles and applications; [Anonymous], PALYNOLOGY; [Anonymous], HOUST 2016 JOINT M S; [Anonymous], THESIS; [Аркадьев Владимир Владимирович Arkadiev V.V.], 2015, [Вестник Санкт-Петербургского университета. 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J	Santos, A; Helenes, J; Carvalho, MD				Santos, Alessandra; Helenes, Javier; Carvalho, Marcelo de Araujo			Late Cretaceous (early Turonian) dinoflagellate cysts from the Sergipe Basin, northeastern Brazil	PALYNOLOGY			English	Article						dinoflagellate cysts; Turonian; Sergipe Basin; Brazil	ALBIAN-CENOMANIAN BOUNDARY; WESTERN INTERIOR BASIN; ANOXIC EVENT; DINOCYST; RECORD; DISTRIBUTIONS; STRATIGRAPHY; ASSEMBLAGES; TEMPERATURE; PALYNOLOGY	This paper presents the stratigraphic distribution and taxonomy of 62 dinoflagellate cyst species found in 85 samples from early Turonian strata exposed at Votorantim Quarry in northeastern Brazil. The early Turonian age assignment is based on calcareous nannofossils together with the organic-walled dinoflagellate cysts Cribroperidinium muderongense, Canningia reticulata, Florentinia resex, Impletosphaeridium williamsii, Kallosphaeridium? ringnesiorum, Trichodinium boltenhagenii and Xenascus plotei, which are commonly found in early Turonian strata. The genera Subtilisphaera and Palaeohystrichophora are emended, Palaeohystrichophora cheit is reassigned to Subtilisphaera cheit, and is considered a senior synonym of Palaeohystrichophora palaeoinfusa. Canningia reticulata is regarded as a senior synonym of Canningia senonica, and Subtilisphaera pirnaensis is regarded as a separate species from Subtilisphaera perlucida, because morphological characteristics can be used to distinguish them. In this study many cosmopolitan species were found, but we could also observe species with tethyan affinities, such as S. cheit and X. plotei. These species have restricted geographic distribution around the equator and are common in the Cenomanian to Turonian in both hemispheres.	[Santos, Alessandra] Univ Vale Rio Sinos UNISINOS, Inst Tecnol Micropaleontol Itt Fossil, Av Unisinos 950, BR-93022750 Sao Leopoldo, RS, Brazil; [Helenes, Javier] CICESE, Dept Geol, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico; [Carvalho, Marcelo de Araujo] 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	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; Universidade Federal do Rio de Janeiro	Santos, A (通讯作者)，Univ Vale Rio Sinos UNISINOS, Inst Tecnol Micropaleontol Itt Fossil, Av Unisinos 950, BR-93022750 Sao Leopoldo, RS, Brazil.	alessandrass@unisinos.br	Carvalho, Marcelo/G-8463-2015; Escamilla, Javier/J-5033-2016		Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [1762-21-2]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior 1762-21-2.	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S	Belmonte, G; Rubino, F		Alekseev, VR; PinelAlloul, B		Belmonte, Genuario; Rubino, Fernando			Cysts and Resting Eggs from Marine Zooplankton: Dimension of the Phenomenon, Physiology of Rest, and Ecological and Biogeographic Implications	DORMANCY IN AQUATIC ORGANISMS. THEORY, HUMAN USE AND MODELING	Monographiae Biologicae		English	Article; Book Chapter						Life cycles; Dormancy; Biogeography; Potential biodiversity; Resurrection ecology; Confined marine environments; Cyst banks; Zooplankton	LIFE-HISTORY TRAITS; BALTIC SEA-ICE; DIAPAUSE EGGS; EVOLUTIONARY CONSEQUENCES; SEASONAL FLUCTUATIONS; VERTICAL-DISTRIBUTION; DINOFLAGELLATE CYSTS; ACARTIIDAE CALANOIDA; MONOPOREIA-AFFINIS; THERMAIKOS GULF	Encystment is a common strategy adopted by coastal marine plankton species to avoid adverse conditions. Spiny cysts have been identified in marine sediments of more than 600 millions years ago, thus suggesting that this has been an original trait of metazoan life cycles. Protista, Chromista, and Metazoa share this trait which is not the result of a convergent evolution, but a plesiomorphy, probably dictated by low oxygen concentrations. During the evolution of life on the Earth, the morphology has been modified, and today some taxa show typical and recognizable patterns. The affirmation of parental cares (brood protection) is suspected to have provoked the disappearing of spiny covering of eggs and/or cysts. Cysts produced in the pelagos sink to the bottom sediments where their dormancy may extend for decades. In polar seas, cysts are suspected to be entrapped within sea ice and released with ice melting to refuel a new plankton community in the complex frame of the so-called resurrection ecology. Confined marine coastal areas accumulate cysts in sediments due to many drivers as (i) reduced water movement/hydrodynamics, (ii) concentration of cyst-producing species with high population densities, and (iii) absence and/or scarcity of possible cyst consumers in the benthos. The pelagic-benthic nexus, which affects both the sediments and the water column (and possibly sea ice), is still poorly understood. The presence of cysts in the life cycle is likely to have considerable consequences for the ecology of coastal plankton as well as the evolution and biogeography of species.	[Belmonte, Genuario] Univ Salento, Dept Biol & Environm Sci & Technol, Lecce, Italy; [Rubino, Fernando] CNR, Water Res Inst, Unit Talassog A Cerruti, Taranto, Italy	University of Salento; Consiglio Nazionale delle Ricerche (CNR); Istituto di Ricerca sulle Acque (IRSA-CNR)	Belmonte, G (通讯作者)，Univ Salento, Dept Biol & Environm Sci & Technol, Lecce, Italy.	genuario.belmonte@unisalento.it; rubino@irsa.cnr.it	BELMONTE, GENUARIO/AAG-4029-2020; Rubino, Fernando/GOP-0332-2022					Albertsson J, 2000, MAR BIOL, V136, P611, DOI 10.1007/s002270050721; Alekseev Victor R., 2007, Monographiae Biologicae, V84, P29; Alekseev VR, 1990, DIAPAUSA RAKOOBRAZHI; [Anonymous], 2009, PALYNOLOGY; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Bailey SA, 2003, LIMNOL OCEANOGR, V48, P1701, DOI 10.4319/lo.2003.48.4.1701; BAN S, 1994, HYDROBIOLOGIA, V293, P185, DOI 10.1007/BF00229940; Ban S, 1992, J CRUSTACEAN BIOL, V12, P361; Barnes R S K., 1999, An Introduction to Marine Ecology; Baumgartner MF, 2017, ANNU REV MAR SCI, V9, P387, DOI 10.1146/annurev-marine-010816-060505; Belmonte G, 1997, HYDROBIOLOGIA, V355, P159, DOI 10.1023/A:1003071205424; Belmonte G, 1997, CRUSTACEANA, V70, P114, DOI 10.1163/156854097X00401; Belmonte G, 1998, J MARINE SYST, V15, P35, DOI 10.1016/S0924-7963(97)00047-X; Belmonte G, 1998, J MARINE SYST, V15, P359, DOI 10.1016/S0924-7963(97)00087-0; Belmonte G, 1995, OLSEN INT S, P53; BELMONTE G, 1992, B ZOOL, V59, P363, DOI 10.1080/11250009209386694; Belmonte G, 1998, TRENDS ECOL EVOL, V13, P4, DOI 10.1016/S0169-5347(97)01234-2; Belmonte G, 2001, HYDROBIOLOGIA, V453, P171, DOI 10.1023/A:1013192623131; BELMONTE G, 1994, HYDROBIOLOGIA, V293, P131, DOI 10.1007/BF00229932; BELMONTE G, 1994, HYDROBIOLOGIA, V293, P9, DOI 10.1007/BF00229917; Belmonte G, 2018, EUR ZOOL J, V85, P274, DOI 10.1080/24750263.2018.1488005; Belmonte G, 2007, J PLANKTON RES, V29, pI39, DOI 10.1093/plankt/fbl064; Boero F, 2004, ECOL COMPLEX, V1, P101; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; BOERO F, 1994, MAR ECOL-P S Z N I, V15, P3, DOI 10.1111/j.1439-0485.1994.tb00038.x; Bohonak AJ, 2006, ARCH HYDROBIOL, V167, P183, DOI 10.1127/0003-9136/2006/0167-0183; Braiko VD, 1966, DOKL AKAD NAUK, V170, P681; Brierley AS, 2002, ADV MAR BIOL, V43, P171, DOI 10.1016/S0065-2881(02)43005-2; BRYLINSKI J M, 1981, Journal of Plankton Research, V3, P255, DOI 10.1093/plankt/3.2.255; BUCK KR, 1992, J PHYCOL, V28, P15, DOI 10.1111/j.0022-3646.1992.00015.x; Caceres CE, 2003, ECOLOGY, V84, P1189, DOI 10.1890/0012-9658(2003)084[1189:HLTRTE]2.0.CO;2; CARBONE C, 2019, MUSEOL SCI MEM   AUG, P57; CARLTON JT, 1993, SCIENCE, V261, P78, DOI 10.1126/science.261.5117.78; CHESSON PL, 1981, AM NAT, V117, P923, DOI 10.1086/283778; Clegg JS, 1997, J EXP BIOL, V200, P467; COHEN D, 1966, J THEOR BIOL, V12, P119, DOI 10.1016/0022-5193(66)90188-3; Cohen PA, 2009, P NATL ACAD SCI USA, V106, P6519, DOI 10.1073/pnas.0902322106; Dahms HU, 2006, ESTUAR COAST SHELF S, V67, P562, DOI 10.1016/j.ecss.2005.12.011; DAHMS HU, 1995, HYDROBIOLOGIA, V306, P199, DOI 10.1007/BF00017691; Dieffenbach H., 2007, DIAPAUSE AQUATIC INV, P11; Drillet G., 2014, J. 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Biol.		2019	92						71	94		10.1007/978-3-030-21213-1_5	http://dx.doi.org/10.1007/978-3-030-21213-1_5	10.1007/978-3-030-21213-1		24	Marine & Freshwater Biology	Book Citation Index– Science (BKCI-S)	Marine & Freshwater Biology	BP4KS					2025-03-11	WOS:000553031200006
S	Belmonte, G; Rubino, F		Hawkins, SJ; Allcock, AL; Bates, AE; Firth, LB; Smith, IP; Swearer, SE; Todd, PA		Belmonte, Genuario; Rubino, Fernando			RESTING CYSTS FROM COASTAL MARINE PLANKTON	OCEANOGRAPHY AND MARINE BIOLOGY: AN ANNUAL REVIEW, VOL 57	Oceanography and Marine Biology		English	Article; Book Chapter							SP-NOV DINOPHYCEAE; DIAPAUSE EGG-PRODUCTION; CALANOID COPEPOD EGGS; SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; MOTILE STAGE RELATIONSHIPS; RED-TIDE DINOFLAGELLATE; ACARTIA-TONSA DANA; DIATOM CHAETOCEROS-PSEUDOCURVISETUS; GYRODINIUM-INSTRIATUM FREUDENTHAL; ALEXANDRIUM-TAMARENSE DINOPHYCEAE	Coastal plankton show fluctuations in abundance and species composition. Resting stage (cyst) production is a common strategy adopted by hundreds of plankton species to ensure reproduction and to avoid adverse conditions. During the resting period, these species are normally absent from the water column, and cysts produced in the plankton accumulate in the sediment where they wait for the return of suitable conditions. A portion of the cyst bank does not hatch, instead undergoing a dormancy that may extend for decades. Confined coastal areas accumulate cysts in sediment due to one or more possibilities, including reduced water movement/hydrodynamics, high population density, abundance of cyst-producing species, and the absence or scarcity of possible cyst consumers in the benthos. The pelagic-benthic nexus, which affects both the sediment and the water column (and possibly sea ice) is still poorly understood. In fact, the presence of cysts in the life cycle of organisms is likely to have considerable consequences for the ecology of coastal plankton, as well as the evolution and biogeography of species. This review aims to depict the presence (and even abundance) of resting stages in marine environments and their impact on ecosystem functioning. The review starts with a description of encysted resting stages in all marine planktonic taxa, listing a total of 501 species with known cysts, and methods and tools for their collection and study. The physiology and timing of the rest period is then described for various taxa, followed by a discussion of the evolutionary implications of resting. The presence of encysted stages in different realms and phyla of plankton suggests an ancient origin and a successive diversification of morphologies that, today, roughly characterise each taxa. Ecological and biogeographical implications stem from this general framework and support the hypothesis of seasonal occurrences of planktonic life in ecosystems where productivity is suspended for a long time (e.g. in polar seas). The potential to suspend or resume life has implications for human activities, such as the risk of translocations through ship ballast water and contamination of water and seafood with toxins but also the benefit of cysts for the production of aquaculture feed. The review concludes with perspectives on present knowledge and outstanding questions to address in future studies.	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B	Gollasch, S; David, M		Sheppard, C		Gollasch, Stephan; David, Matej			Ballast Water: Problems and Management	WORLD SEAS: AN ENVIRONMENTAL EVALUATION, VOL III: ECOLOGICAL ISSUES AND ENVIRONMENTAL IMPACTS, 2ND EDITION			English	Article; Book Chapter							RISK-ASSESSMENT; DINOFLAGELLATE CYSTS; BIOLOGICAL INVASIONS; SPECIES INTRODUCTIONS; TANK SEDIMENTS; SHIPS; EXCHANGE; TRANSPORT; ORGANISMS; OCEAN		[Gollasch, Stephan] GoConsult, Grosse Brunnenstr, Hamburg, Germany; [David, Matej] Dr Matej David Consult Doo, Korte 13e, Izola 6310, Slovenia; [David, Matej] Univ Rijeka, Fac Maritime Studies, Rijeka, Croatia	University of Rijeka	Gollasch, S (通讯作者)，GoConsult, Grosse Brunnenstr, Hamburg, Germany.		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J	De Schepper, S; Head, MJ				De Schepper, S.; Head, M. J.			Age calibration of dinoflagellate cyst and acritarch events in the Pliocene-Pleistocene of the eastern North Atlantic (DSDP Hole 610A) (vol 5, pg 137, 2008)	STRATIGRAPHY			English	Correction																		De Schepper S, 2008, STRATIGRAPHY, V5, P137	1	0	0	0	1	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	1547-139X	2331-656X		STRATIGRAPHY	Stratigraphy		2019	16	4					282	282						1	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	KZ3UC					2025-03-11	WOS:000523189800002
J	Eidvin, T; Rasmussen, ES; Riis, F; Dybkjær, K; Grosfield, K				Eidvin, Tor; Rasmussen, Erik Skovbjerg; Riis, Fridtjof; Dybkjaer, Karen; Grosfield, Kari			Correlation of the Upper Oligocene-Miocene deltaic to shelfal succession onshore Denmark with similar deposits in the northern North Sea and Norwegian Sea shelf based on Sr isotope-, bio- and seismic stratigraphy-a review	NORWEGIAN JOURNAL OF GEOLOGY			English	Review						Sr isotope stratigraphy; foraminiferal stratigraphy; Bolboforma stratigraphy; upper Paleogene-Neogene correlation; Denmark; North Sea; Norwegian Sea shelf; Norwegian Sea	CENOZOIC GEOLOGICAL EVOLUTION; PLEISTOCENE SAND INTRUSION; CAINOZOIC STRATIGRAPHY; SEQUENCE STRATIGRAPHY; CONTINENTAL-SHELF; UTSIRA FORMATION; DIEST FORMATION; CENTRAL GRABEN; MOLO FORMATION; VIKING GRABEN	The almost complete, mainly deltaic, upper Paleogene and Neogene succession in Jylland, Denmark, was previously investigated for 87Sr/86Sr ratios in 143 samples from 18 localities. In the present paper, strontium-isotope data from the Upper Oligocene Lower Miocene parts and foraminiferal and pyritised diatoms data from 94 of these samples were used to correlate with previously published data from Norwegian wells and boreholes and one borehole in the British sector of the North Sea. For the Middle Upper Miocene parts of the succession the correlation is based mainly on Bolboforma data. The ages of the geological formations in the Danish succession correlate readily with lithological units in the Norwegian North Sea, the Norwegian Sea shelf and the East Shetland Platform, which have all been investigated applying similar methods. The Bolboforma assemblages have their origin in the North Atlantic and the Norwegian Sea and confirm the presence of an open strait in the northern North Sea. This strait was the only seaway passage into the North Sea Basin during the Miocene. The glauconitic Utsira Formation sand (approximately 5.7-4.2 Ma), in the threshold area close to the outlet to the Norwegian Sea, overlies erosional unconformities comprising hiati of 21 my in some areas and 13 my in other areas. We believe that the unconformity below the Utsira Formation was mainly related to a fall in sea level in the Late Miocene, contemporaneous with that partly responsible for the Messinian salinity crisis. Bolboforma and dinoflagellate cysts stratigraphy indicate that the base of the Mob Formation in its southern distribution area (Draugen Field, Trandelag Platform) is of Late Miocene age (close to 9 Ma). This part of the Mob Formation was contemporaneous with the middle/upper part of the Kai Formation.	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J. Geol.		2019	99	4								10.17850/njg99-4-1	http://dx.doi.org/10.17850/njg99-4-1			31	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KG3SN		gold			2025-03-11	WOS:000509862300001
J	Grosfjeld, K; Dybkjær, K; Eidvin, T; Riis, F; Rasmussen, ES; Knies, J				Grosfjeld, Kari; Dybkjaer, Karen; Eidvin, Tor; Riis, Fridtjof; Rasmussen, Erik Skovbjerg; Knies, Jochen			A Miocene age for the Molo Formation, Norwegian Sea shelf off Vestfjorden, based on marine palynology	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Molo Formation; Eastern Norwegian shelf; Biostratigraphy; Dinoflagellate cysts; Miocene	DINOFLAGELLATE CYST; CONTINENTAL-SHELF; NORTH-SEA; MAGNETOSTRATIGRAPHIC CALIBRATION; CENOZOIC STRATIGRAPHY; ACRITARCH EVENTS; PLIOCENE; PLEISTOCENE; OLIGOCENE; EOCENE	Seven side-wall core samples from the lower part of the Mob Formation in exploration well 6610/3-1 off Vestfjorden/Lofoten have been reanalysed for marine palynomorphs. Description of new species from other studies and access to reference successions from nearby sites with an independent chronostratigraphy have enabled a more reliable depositional age constraint for the Mob Formation in its northern distribution area than previously achieved. The new data (e.g., the lowest occurrence of the dinoflagellate cysts Barssidinium graminosum and Barssidinium pliocenicum and the highest occurrence of the dinoflagellate cysts Minisphaeridium latirictum and Operculodinium piaseckii) provide incontrovertible evidence for a Miocene age for the Mob Formation in well 6610/3-1. Our data suggest that the Mob Formation in well 6610/3-1 started to accumulate after erosional activity which took place between the late middle Miocene and the late Miocene. The data (especially the presence of the dinoflagellate cyst A. andalouisiensis andalousiensis, the co-occurrence of the dinoflagellate cysts Barssidiniuni evangelineae and M. latirictum and the presence of the acritarch L. lucifer) suggest that the Mob Formation in well 6610/3 1 started to accumulate at around 8.8 / 8.7 Ma. The sediments were deposited in a warm temperate, high-energy environment influenced by river discharge. During deposition, older sediments, particularly from the Paleogene, became extensively eroded. The erosion and rapid accumulation were probably associated with the combined effects of eustatic sea-level fall and uplift/updoming of the hinterland/coastal zone.	[Grosfjeld, Kari; Knies, Jochen] Geol Survey Norway, POB 6315, N-7491 Trondheim, Norway; [Dybkjaer, Karen; Rasmussen, Erik Skovbjerg] Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Eidvin, Tor; Riis, Fridtjof] NPD, Prof Olav Hanssens Vei 10, NO-4021 Stavanger, Norway; [Knies, Jochen] Univ Tromso, Ctr Arctic Gas Hydrate Environm & Climate, N-9037 Tromso, Norway	Geological Survey of Norway; Geological Survey Of Denmark & Greenland; UiT The Arctic University of Tromso	Grosfjeld, K (通讯作者)，Geol Survey Norway, POB 6315, N-7491 Trondheim, Norway.	kari.grosfjeld@ngu.no	Dybkjær, Karen/G-5223-2018		BASE (BASEment fracturing and weathering on-and offshore Norway - Genesis, age, and landscape development) project; Lundin Norway; AkerBP; Total Norway; Wintershall	BASE (BASEment fracturing and weathering on-and offshore Norway - Genesis, age, and landscape development) project; Lundin Norway; AkerBP; Total Norway; Wintershall	The study is funded by the BASE (BASEment fracturing and weathering on-and offshore Norway - Genesis, age, and landscape development) project through support from Lundin Norway, AkerBP, Wintershall and Maersk (now Total Norway). Sigrid Elvenes (NGU) provided the bathymetric map in Fig. 1. Stijn De Schepper (NORCE), Claus Heilmann-Clausen (Aarhus University), Stephen Louwye (University Bremen), Jens Matthiessen (AWI), Dirk Munsterman (TNO), Stefan Piasecki (GEUS), Michael Schreck (UiT) and Robert Williams (NPD) helped with identification of species. Harald Brekke (NPD) and Martin Head (Brock University) reviewed the manuscript. Helge Loseth (Equinor), Dag Ottesen (NGU), Leif Rise (NGU) and William Helland-Hansen (UiB) contributed in geological discussions. David Roberts (NGU) corrected the language. To all these geoscientists we express our gratitude. We acknowledge the NGU, NPD and GEUS for permission to publish this paper.	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J. Geol.		2019	99	3								10.17850/njg99-3-6	http://dx.doi.org/10.17850/njg99-3-6			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KG3SJ		Green Published, gold			2025-03-11	WOS:000509861900004
J	Munsterman, DK; ten Veen, JH; Menkovic, A; Deckers, J; Witmans, N; Verhaegen, J; Kerstholt-Boegehold, SJ; van de Ven, T; Busschers, FS				Munsterman, Dirk K.; ten Veen, Johan H.; Menkovic, Armin; Deckers, Jef; Witmans, Nora; Verhaegen, Jasper; Kerstholt-Boegehold, Susan J.; van de Ven, Tamara; Busschers, Freek S.			An updated and revised stratigraphic framework for the Miocene and earliest Pliocene strata of the Roer Valley Graben and adjacent blocks	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						dinoflagellate cysts; lithostratigraphy; Neogene; seismic; southern North Sea Basin; well-log correlation	NORTH-SEA BASIN; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; DIEST FORMATION; DUTCH OFFSHORE; BELGIUM; MIDDLE; AREA; NETHERLANDS; EVOLUTION; OLIGOCENE	In the Netherlands, the bulk of the Miocene to lowest Pliocene sedimentary succession is currently assigned to a single lithostratigraphical unit, the Breda Formation. Although the formation was introduced over 40 years ago, the definition of its lower and upper boundaries is still problematic. Well-log correlations show that the improved lecto-stratotype for the Breda Formation in well Groote Heide partly overlaps with the additional reference section of the older Veldhoven Formation in the nearby well Broekhuizenvorst. The distinction between the Breda and the overlying Oosterhout Formation, which was mainly based on quantitative differences in glauconite and molluscs, gives rise to ongoing discussion, in particular due to the varying concentrations of glauconitic content that occur within both formations. In addition, the Breda Formation lacks a regional-scale stratigraphic framework which relates its various regionally to locally defined shallow marine to continental members. In order to resolve these issues, we performed renewed analyses of material from several archived cores. The results of archived and new dinocyst analyses were combined with lithological descriptions and wire-line log correlations of multiple wells, including the wells Groote Heide and Broekhuizenvorst. In this process, the updated dinocyst zonation of Munsterman & Brinkhuis (2004), recalibrated to the Geological Time Scale of Ogg et al. (2016), was used. To establish regionally consistent lithostratigraphic boundaries, additional data was used along a transect across the Roer Valley Graben running from its central part (well St-Michielsgestel-1) towards the southern rift shoulders (well Goirle-1). Along this transect, chronostratigraphic and lithostratigraphic analyses were integrated with well-log correlation and the analyses of seismic reflection data to constrain geometrical/structural relationships as well. The results led to the differentiation of two distinct seismic sequences distinguished by three recognisable unconformities: the Early Miocene Unconformity (EMU), the Mid-Miocene Unconformity (MMU) and the Late Miocene Unconformity (LMU). The major regional hiatus, referred to as the Mid-Miocene Unconformity, occurs intercalated within the present Breda Formation and compels subdivision of this unit into two formations, viz. the here newly established Groote Heide and the younger Diessen formations. Pending further studies, the former Breda Formation will be temporally raised in rank to the newly established Hilvarenbeek subgroup, which comprises both the Groote Heide and Diessen formations. Whereas these two sequences were already locally defined, a third sequence overlying the LMU represents two newly defined lithostratigraphical units, named the Goirle and the Tilburg members, positioned in this study at the base of the Oosterhout Formation. Besides their unique lithological characteristics, in seismic reflection profiles the Goirle and the Tilburg members stand out because of their distinct seismic facies. Use of an integrated, multidisciplinary and regional approach, an improved southern North Sea framework and more comprehensive lithostratigraphic subdivision of Neogene successions is proposed for the Netherlands, to make (cross-border) correlations more straightforward in the future.	[Munsterman, Dirk K.; ten Veen, Johan H.; Menkovic, Armin; Witmans, Nora; Kerstholt-Boegehold, Susan J.; van de Ven, Tamara; Busschers, Freek S.] TNO Geol Survey Netherlands, POB 80015, NL-3508 TA Utrecht, Netherlands; [Deckers, Jef] Flemish Inst Technol Res, VITO, Boeretang 200, B-2400 Mol, Belgium; [Verhaegen, Jasper] Katholieke Univ Leuven, Dept Earth & Environm Sci, Celestijnenlaan 200E, B-3001 Heverlee, Belgium	Netherlands Organization Applied Science Research; VITO; KU Leuven	Munsterman, DK (通讯作者)，TNO Geol Survey Netherlands, POB 80015, NL-3508 TA Utrecht, Netherlands.	dirk.munsterman@tno.nl	Busschers, Freek/HLQ-6717-2023; Verhaegen, Jasper/S-5729-2019	Munsterman, Dirk/0000-0003-1774-4615; Verhaegen, Jasper/0000-0002-9629-2655; ten Veen, Johan/0000-0002-4925-4672				Amorosi A, 1997, SEDIMENT GEOL, V109, P135, DOI 10.1016/S0037-0738(96)00042-5; [Anonymous], NETH J GEOSCI, DOI [DOI 10.1017/50016774600021405, DOI 10.1017/S0016774600021405]; [Anonymous], 2008, Zeitschrift der Deutschen Gesellschaft fur Geowissenschaften, DOI [DOI 10.1127/1860-1804/2008/0159-0687, 10.1127/1860-1804/2008/0159-0687]; [Anonymous], 2017, STROKE, V48, pe78; [Anonymous], 2010, Journal of Low Temperature Physics, V161, P1, DOI DOI 10.1007/S10909-010-0219-Y; Anthonissen ED, 2012, NEWSL STRATIGR, V45, P281, DOI 10.1127/0078-0421/2012/0025; Benvenuti A, 2012, NETH J GEOSCI, V91, P591; Bogemans F, 2018, GEOLOGISCH HYDROGEOL; Bosch J.H.A., 2000, 00141A TNO NITG; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brinkhuis H., 1992, THESIS; Catuneanu O., 2006, PRINCIPLES SEQUENCE; De Schepper S, 2017, REV PALAEOBOT PALYNO, V236, P12, DOI 10.1016/j.revpalbo.2016.08.005; De Schepper S, 2015, NAT COMMUN, V6, DOI 10.1038/ncomms9659; De Schepper S, 2009, PALYNOLOGY, V33, P179; Deckers J., 2019, GEOL J, V54, P1, DOI 10/1002/gj.3438; Deckers J., 2014, VITO-rapport 2014/ETE/R/1. 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J. Geosci.		2019	98								e8	10.1017/njg.2019.10	http://dx.doi.org/10.1017/njg.2019.10			23	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KG4ZI		Green Published, gold			2025-03-11	WOS:000509956300001
J	Birkenmajer, K; Gedl, P				Birkenmajer, Krzysztof; Gedl, Przemyslaw			THE JURASSIC TO PALAEOGENE STRATA IN THE NORTHERN BOUNDARY FAULT ZONE IN DEEP BOREHOLE PD-9 AT SZCZAWNICA, PIENINY KLIPPEN BELT, WEST CARPATHIANS, POLAND: BIOSTRATIGRAPHY AND TECTONIC IMPLICATIONS	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						Carpathians; biostratigraphy; dinoflagellate cysts; lithostratigraphy; tectonics; Poland	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; GEOLOGICAL STRUCTURE; OUTER CARPATHIANS; BLACK FLYSCH; PALEOCENE; BAJOCIAN; STRATIGRAPHY; NAPPE; AREA; AGE	The Jurassic through Palaeogene stratigraphy and tectonic structure of the PD-9 borehole at Szczawnica, Pieniny Klippen Belt, West Carpathians, Poland, is revised. The borehole was drilled in the strongly tectonized northern boundary fault zone of the Pieniny Klippen Belt, of Miocene age. Age revision is given by dinoflagellate cysts. Late Cretaceous taxa are reported from the Haluszowa Fonnation. The Bryjarka Member (previously with the rank of formation) yielded rich Early Eocene (Ypresian) assemblages. Similar ones are reported from the Szczawnica Formation. A tectonic thrust sheet of the Jurassic Szlachtowa Formation (Grajcarek Unit) in the Palaeogene of the Magura Nappe is evidenced; it yielded late Toarcian-Aalenian dinollagellate cyst assemblages. The succession of strata recorded from the PD-9 borehole shows the steep, almost vertical attitude of the Grajcarek Main Dislocation at Szczawnica, separating the structures of the Magura Nappe (to the north) and the Pieniny Klippen Belt to the south.	[Birkenmajer, Krzysztof; Gedl, Przemyslaw] Polish Acad Sci, Res Ctr Krakow, 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, Res Ctr Krakow, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl						Alexandrowicz S. 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J	Suchocka, A; Barski, M; Bienkowska-Wasiluk, M				Suchocka, Arleta; Barski, Marcin; Bienkowska-Wasiluk, Malgorzata			Dinoflagellate cyst stratigraphy of the Popiele Member and Menilite Formation in the Boryslav-Pokuttya Nappe (Aksmanice, SE Poland)	GEOLOGICAL QUARTERLY			English	Article						dinoflagellate cysts; biostratigraphy; Oligocene; Menilite Formation; Outer Carpathians; flysch	EOCENE-OLIGOCENE TRANSITION; MAGURA NAPPE; PALEOENVIRONMENTAL CHANGES; WESTERN CARPATHIANS; TERMINAL EOCENE; BIOSTRATIGRAPHY; SKOLE; BASIN; ZONE; NANNOPLANKTON	In the Paratethys Sea, isolation, the development of anoxia and stratification of the water column resulted in deposition of organic-rich sediments. In the Western Carpathians (Central Paratethys) these sediments now lie within the Menilite Formation. Whereas the Eocene-Oligocene transition has been studied in the West ern Carpathians and is documented by dinoflagellate cyst assemblages, the dinoflagellate cyst stratigraphy of the Menilite Formation members has been uncertain. The Popiele Member and the Menilite Formation exposed at Aksmanice (Boryslav-Pokuttya Nappe, Western Outer Carpathians) reflect palaeogeographic changes at the beginning of the Oligocene. These previously studied deposits have been assigned to lithostratigraphic units, though without biostratigraphic documentation. The age of the Menilite Fm. in the Carpathian sedimentary succession is particularly interesting due to the diachronous character of the facies development. In this study we provide biostratigraphic data based on well-preserved organic-walled dinoflagellate cyst assemblages. The marker taxa recovered indicate a Rupelian age (Early Oligocene) for the Menilite Fm. A different assemblage occurs in the Popiele Member underlying the Menilite Fm. Here, the dinoflagellate cysts are more diverse and abundant, and represented by typical Eocene taxa at tributed to Areosphaeridium spp. and Charlesdowniea spp. The Popiele Member may be as signed to the Priabonian (Late Eocene).	[Suchocka, Arleta; Barski, Marcin; Bienkowska-Wasiluk, Malgorzata] Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland	University of Warsaw	Suchocka, A (通讯作者)，Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	arleta_suchocka@wp.pl	; Bienkowska-Wasiluk, Malgorzata/F-4714-2011	Barski, Marcin/0000-0002-4102-3538; Bienkowska-Wasiluk, Malgorzata/0000-0001-5397-363X				Andreeva-Grigorovich A. S., 1991, THESIS; Andreyeva-Grigorovich A. S., 1994, Geologica Carpathica, V45, P333; [Anonymous], 1988, Geol. 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Q.		2019	63	3					539	557		10.7306/gq.1486	http://dx.doi.org/10.7306/gq.1486			19	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	JK6YX					2025-03-11	WOS:000494989400008
J	Romero, E; Amenábar, CR; Zamaloa, MC; Concheyro, A				Romero, Edgardo; Amenabar, Cecilia R.; Zamaloa, Maria C.; Concheyro, Andrea			<i>Nothofagus</i> and the associated palynoflora from the Late Cretaceous of Vega Island, Antarctic Peninsula	POLISH POLAR RESEARCH			English	Article						Antarctica; Vega Island; Cretaceous; Nothofagaceae leaves; palynology	JAMES-ROSS-ISLAND; KING GEORGE ISLAND; CAPE LAMB; MARAMBIO GROUP; STRATIGRAPHY; PALEOECOLOGY; CLASSIFICATION; PALYNOLOGY; EVOLUTION; DINOSAUR	Nothofagaceae fossil leaves and an associated palynoflora from Late Cretaceous sediments of Vega Island, eastern Antarctic Peninsula, are presented. The leaves are described as Nothofagus sp. 1 and Morphotype LDB 1, and come from the Snow Hill Island (late Campanian-early Maas-trichtian) and the Lopez de Bertodano (late Maastrichtian) formations, respectively. The palynoflora obtainexi from levels immediately above and below the Nothofagus sp. 1 and in the same horizon as the Morphotype LDB 1, included terrestrial and marine elements. In the palynoflora associated with Nothofagus sp. 1, conifers are dominant and pollen grains with Nothofagus affinity are represented by four species: Nothofagidites kaitangataensis (Te Punga) Romero 1973 and Nothofagidites senectus Dettmann and Playford 1968, which belong to the ancestral pollen type, as well as Nothofagidites dorotensis Romero 1973 and Nothofagidites sp. of the brassii-type. Cryptogamic spores, marine dinoflagellate cysts and algae, among others, are part of the assemblage. The palynoflora associated with the Morphotype 1 also contains abundant conifer and angiosperm pollen grains with N. dorotensis as the only Nothofagus species recorded. Marine dinoflagellate cysts are scarce while fungi and phytodebris are common elements. The joint presence of marine and non-marine palynomorphs supports a probable nearshore environment at time of deposition for both units. Pollen and spore evidence suggests a mixed conifer and angiosperm forest, with Podocarpaceae and Nothofagus as the main components, and ferns, lycopods, and mosses in the understory. This forest developed under temperate and moist conditions during the middle Campanian-Maastrichtian.	[Romero, Edgardo] Museo Argentino Ciencias Nat Bernardino Rivadavia, Av A Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina; [Amenabar, Cecilia R.; Concheyro, Andrea] Univ Buenos Aires, IDEAN Inst Estudios Andinos Don Pablo Groeber, CONICET, Fac Ciencias Exactas & Nat, Intendente Guiraldes 2620,C1428EHA, Buenos Aires, DF, Argentina; [Amenabar, Cecilia R.; Concheyro, Andrea] Inst Antartico Argentine, 25 Mayo 1151,3 Piso, RA-1650 San Martin, Buenos Aires, Argentina; [Zamaloa, Maria C.] Univ Buenos Aires, Dept Ecol Genet & Evoluc, Intendente Guiraldes 2620,C1428EHA, Buenos Aires, DF, Argentina	Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Instituto Antartico Argentino; University of Buenos Aires	Amenábar, CR (通讯作者)，Univ Buenos Aires, IDEAN Inst Estudios Andinos Don Pablo Groeber, CONICET, Fac Ciencias Exactas & Nat, Intendente Guiraldes 2620,C1428EHA, Buenos Aires, DF, Argentina.; Amenábar, CR (通讯作者)，Inst Antartico Argentine, 25 Mayo 1151,3 Piso, RA-1650 San Martin, Buenos Aires, Argentina.	ejromero@macn.gov.ar; amenabar@gl.fcen.uba.ar; mzamaloa@ege.fcen.uba.ar; andrea@gl.fcen.uba.ar		AMENABAR, CECILIA R./0000-0003-1280-3903	 [PICT 2433/2014]		To Direccion Nacional del Antartico-Instituto Antartico Argentino and Fuerza Area Argentina for the logistic and scientific support. We are immensely grateful to Alfredo Ambrosio for collecting the fossil leaves. We also thank to Gustavo Holfeltz for the preparation of palynological samples and to Gaston Cornachione for his assistance in the field. We also acknowledge Rosemary Askin and an anonymous reviewer for their constructive comments that helped to improve the manuscript. This is the contribution R-269 of the Instituto de Estudios Andinos "Don Pablo Groeber" (IDEAN-CONICET). It was partially supported by grant PICT 2433/2014 to MCZ.	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Res.		2019	40	3					227	253		10.24425/ppr.2019.129672	http://dx.doi.org/10.24425/ppr.2019.129672			27	Ecology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	JA0SD		Green Published, gold			2025-03-11	WOS:000487521100003
J	Lee, SP; Jeong, HJ; Kim, SJ; Ha Lee, K; Jang, SH				Lee, Sung Peon; Jeong, Hae Jin; Kim, So Jin; Ha Lee, Kyung; Jang, Se Hyeon			<i>Scrippsiella masanensis sp. nov</i>. (Thoracosphaerales, Dinophyceae), a phototrophic dinoflagellate from the coastal waters of southern Korea	PHYCOLOGIA			English	Article						ITS; LSU; Morphology; Noncalcareous; SEM; Taxonomy	CYST-THECA RELATIONSHIP; HARMFUL ALGAL BLOOMS; TAXONOMIC CLARIFICATION; SPINIFERA PERIDINIALES; TROCHOIDEA; ULTRASTRUCTURE; IDENTIFICATION; PHYLOGENY; GEN.; CALCIODINELLOIDEAE	A phototrophic dinoflagellate belonging to the genus Scrippsiella was isolated from a water sample collected from Masan Bay, Korea. Using a clonal culture of this dinoflagellate, its morphology was analysed with light, scanning and transmission electron microscopy and small subunit (SSU), large subunit (LSU), and internal transcribed spacer ribosomal DNA (ITS rDNA) sequences were studied. The dinoflagellate plate formula was Po, x, 4', 3a, 7 '', 6c (5c + t), 5s, 5''', and 2 '''', consistent with Scrippsiella. The dinoflagellate had a rounded epitheca, unlike most Scrippsiella species, which have a conical epitheca. Furthermore, it had a narrow, symmetrical, and pentagonal 1' plate, unlike other Scrippsiella species. In addition, it had three intercalary plates of different sizes. This species had noncalcareous cysts, unlike most Scrippsiella species, which have calcareous cysts. The LSU rDNA sequence of the dinoflagellate was about 2% different from Scrippsiella enormis, the closest Scrippsiella species, and the ITS rDNA sequence was about 8% different from S. enormis. The sequence was identical to an unidentified Scrippsiella strain from Chinese waters (SSND14) and 0.55% different from an unidentified Scrippsiella strain from Norwegian waters (GeoB 277). On the basis of its unique morphological and molecular features, this species was named Scrippsiella masanensis sp. nov.	[Lee, Sung Peon; Jeong, Hae Jin; Kim, So Jin; Ha Lee, Kyung; Jang, Se Hyeon] Seoul Natl Univ, Coll Nat Sci, Sch Earth & Environm Sci, Seoul 08826, South Korea; [Jeong, Hae Jin] Adv Inst Convergence Technol, Suwon 16229, South Korea	Seoul National University (SNU)	Jeong, HJ (通讯作者)，Seoul Natl Univ, Coll Nat Sci, Sch Earth & Environm Sci, Seoul 08826, South Korea.; Jeong, HJ (通讯作者)，Adv Inst Convergence Technol, Suwon 16229, South Korea.	hjjeong@snu.ac.kr	Jeong, hae/B-8908-2009; Jang, Hyeon/AAO-6009-2020	Jeong, Hae Jin/0000-0003-3310-4335	Useful Dinoflagellate Programme of the Korea Institute of Marine Science and Technology Promotion (KIMST) - Ministry of Oceans and Fisheries (MOF); National Research Foundation (NRF) - Ministry of Science and ICT [NRF-2015M1A5A1041806, NRF-2017R1E1A1A01074419]	Useful Dinoflagellate Programme of the Korea Institute of Marine Science and Technology Promotion (KIMST) - Ministry of Oceans and Fisheries (MOF)(Korea Institute of Marine Science & Technology Promotion (KIMST)Ministry of Oceans & Fisheries (MOF), Republic of Korea); National Research Foundation (NRF) - Ministry of Science and ICT(National Research Foundation of Korea)	This research was supported by the Useful Dinoflagellate Programme of the Korea Institute of Marine Science and Technology Promotion (KIMST) funded by the Ministry of Oceans and Fisheries (MOF) and Management of Marine Organisms Causing Ecological Disturbance and Harmful Effect Programme of KIMST and the National Research Foundation (NRF) funded by the Ministry of Science and ICT (NRF-2015M1A5A1041806; NRF-2017R1E1A1A01074419) award to HJJ.	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J	Hughes, GW				Hughes, Geraint Wyn			Turonian microcrinoids from the lower Aruma Formation of Saudi Arabia	MICROPALEONTOLOGY			English	Article						Roveacrinus; foraminifera; dinoflagellate cysts; Turonian; Aruma Formation; Saudi Arabia; biostratigraphy; paleoenvironments	ROVEACRINIDS CRINOIDEA; ASSEMBLAGES CRINOIDEA; BOUNDARY INTERVAL; BIOSTRATIGRAPHY; BASIN; PALEOECOLOGY; MICROFACIES; MORPHOLOGY; PLATFORM; SHELF	Pelagic microcrinoids assigned to the genus Roveacrinus identified in thin-sections of carbonates of the Turonian lower Aruma Formation of Saudi Arabia provide the first documented occurrence of these microfossils in the Arabian Peninsula. The species include Roveacrinus cf. alatus Douglas 1908, Roveacrinus sp., Roveacrinus geinitzi Schneider 1989, Roveacrinus cf. geinitzi, Roveacrinus aff. rugosus Douglas 1908, Roveacrinus sp. A., Roveacrinus aff. geinitzi Schneider 1989 and Roveacrinus cf. derdereensis. The Turonian range is based on the presence of planktonic foraminifera Heterohelix moremanni, H. globulosa and Marginotruncana sigali in the absence of Rotalipora spp., although possible Cenomanian forms are present within one deep marine microfacies assemblage. The biofacies containing the often abundant Roveacrinus fragments consists typically of abundant calcareous dinoflagellate cysts Calcisphaerula innominata with less common Pithonella ovalis, and rare Bonitocardiella conica, rare to common planktonic foraminifera and rare benthonic foraminifera including Marssonella turris and Gavelinella spp. This assemblage, within very fine-grained packstones, suggests a deep marine depositional environment with low energy, normal salinity conditions. Deep marine sediments, that include Heterohelix moremanni and forms that may be transitional to H. globulosa, include roveacrinids that compare with the Cenomanian species R. derdereensis and these may prove to be supplementary useful age indicators in such environments. Although their association with pelagic microfossils would suggest a planktonic lifestyle, a definite paleoenvironmental interpretation seems elusive by most authors although there is a direct association between the roveacrinoid abundance and flooding surfaces and high-productivity events. Roveacrinid fragments have been recovered from calcareous mudstones of the Ruwaydha and Tuwayil members of the Aruma Formation that overlie upper Cenomanian grainstones of the Mishrif Member of the Wasia Formation. A regionally significant unconformity separates the Mishrif Formation from the Aruma Formation, of which the basal Aruma represents a significant deep marine transgression. The episodic microcrinoid distribution potentially provides regionally correlative bioevents in addition to their possible relationship with the oceanic anoxic event OAE 2.	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J	Li, Z; Shin, H				Li, Zhun; Shin, HyeonHo			Morphology, phylogeny and life cycle of <i>Fragilidium mexicanum</i> Balech (Gonyaulacales, Dinophyceae)	PHYCOLOGIA			English	Article						Dinoflagellate; Life history; Molecular; Pellicle cyst; Resting cyst	SP-NOV DINOPHYCEAE; MOLECULAR PHYLOGENY; RESTING CYST; DINOFLAGELLATE; HISTORY; DUPLOCAMPANAEFORME; STRATEGIES; SEDIMENTS; TOXICITY; LIGHT	We describe the life cycle, morphology and molecular phylogenetic position of Fragilidium mexicanum, based on vegetative cells established by incubation of resting cysts isolated from sediment trap samples collected at Jinhae-Masan Bay, Korea. Resting cysts of F. mexicanum were spherical and surrounded by transparent mucilage, similar to other Fragilidium species. Germinated vegetative cells were identified as F. mexicanum based on thecal morphology and tabulation; the plate formula was Po, Pc, 4', 8 '',10c, 6s, 7''', 1p, 2 ''''. Molecular phylogenetic analyses of sequence data for small and large subunits of ribosomal DNA genes revealed that Fragilidium species were monophyletic with high supports and that F. mexicanum formed a separate Glade with Fragilidium sp. (JQ317599). Time-lapse photography was used to clarify the life history. Isolated resting cysts germinated into an unarmoured planomeiocyte and directly formed the pellicle cyst, with an armoured planomeiocyte emerging from the pellicle cyst. The armoured planomeiocyte underwent ecdysis and formed a coccoid meiocyte, with a two-celled chain emerging from the coccoid meiocyte. Like the armoured planomeicyte, vegetative cells also underwent ecdysis and then divided into two daughter cells that eventually emerged as motile vegetative cells. The life cycle of F. mexicanum has nonmotile life history stages that regularly alternate with motile stages. The nonmotile stage consists of five forms: resting cyst, pellicle cyst, asexual coccoid stage, coccoid meiocyte, and zygote. The motile stage also has five forms: unarmoured and armoured planomeiocyte, planozygote, gamete and vegetative cell.	[Li, Zhun; Shin, HyeonHo] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea	Korea Institute of Ocean Science & Technology (KIOST)	Shin, H (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea.	shh961121@kiost.ac	LI, ZHUN/GLT-3478-2022	LI, ZHUN/0000-0001-8961-9966; Shin, Hyeon Ho/0000-0002-9711-6717	project titled 'Research center for fishery resource management based on the information and communication technology (ICT)'; Marine Biotechnology Programme of the Korea Institute of Marine Science and Technology Promotion (KIMST) - Ministry of Oceans and Fisheries (MOF) [20170431]; KIOST project [PE99721]	project titled 'Research center for fishery resource management based on the information and communication technology (ICT)'; Marine Biotechnology Programme of the Korea Institute of Marine Science and Technology Promotion (KIMST) - Ministry of Oceans and Fisheries (MOF); KIOST project	This research was supported by a part of the project titled 'Research center for fishery resource management based on the information and communication technology (ICT)' and the Marine Biotechnology Programme of the Korea Institute of Marine Science and Technology Promotion (KIMST) funded by the Ministry of Oceans and Fisheries (MOF; No. 20170431), and KIOST project (PE99721).	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J	Youssef, AH; Al-Sahlan, G; Kadar, AP; Karam, KA; Packer, S; Starkie, S; Stead, D				Youssef, Abdulkader H.; Al-Sahlan, Ghaida; Kadar, Adi P.; Karam, Khalaf A.; Packer, Stephen; Starkie, Stephen; Stead, Darrin			Sequence stratigraphic framework of the Wara and Ahmadi Formations, onshore Kuwait	STRATIGRAPHY			English	Article								High resolution biostratigraphic and palaeoenvironmental investigation has been integrated with sedimentology and wireline log data to establish a biostratigraphically-constrained depositional sequence stratigraphic framework for the Wara and Ahmadi Formations, onshore Kuwait. Five hundred core samples from 10 wells were used in this study, in addition to seven wells with wire line log data for regional correlation. The 200 ft thick Wara Formation consists of alternating sand bodies and shale interbeds. It was deposited during the late Albian to early Cenomanian, in an inner shelf to marginal marine environments. It represents a 3rd order sequence, and is subdivided into three 4th order sequences; WA101, WA102 and WA103. The WA101 maximum flooding surface at the base of the Wara, has been recognized by the presence of common calcareous nannofossil and foraminifera assemblages. The WA102 maximum flooding surface is recognized near the middle part of the formation based on the occurrence of marine dinoflagellate cysts. The WA103 maximum flooding surface is recognized near top of the formation, based on the occurrence of marine dinoflagellate cysts. The Wara Formation 4th order highstand systems tracts are composed mainly of three progradational deltaic clastic clinoforms, which are composed of shallowing upward, barren-of-marine-fossil intercalations of sandstones and non-calcareous shale, with thin coal layers particularly at the upper part of WA103. They thicken towards the south and are composed of channel elastics in the Burgan area where assemblages are dominated by the miospores Araucariacites australis, Cyathidites spp., and Inaperturopollenites limbatus indicating a transitional paleoenvironment; sediments thin towards the distal part of the delta. The Ahmadi Formation is composed of two members; the Tuba member which is a carbonate reservoir in northern Kuwait and the Ahmadi shale member, which is considered to be a regional seal. It was deposited during the late Albian to early Cenomanian, in an inner-middle neritic marine environment. Its thickness is between 200-400 ft and it is dominated by shale to the south and carbonate to the north. Three 4th order sequences have been identified; AH101, AH102 and AH103. The AH101 maximum flooding surface at the base of the Tuba member, is indicated by the presence of common foraminifers and nannofossil assemblages. The AH102 maximum flooding surface is recognized from the middle Tuba member and indicated by common foraminifera and nannofossil assemblages and the AH103 maximum flooding surface is recognized at the base of the Ahmadi Shale, by common foraminifers and nannofossil assemblages. The Warn and Ahmadi 3rd order sequences are equivalent to the TSC global 3rd order sequences Al10 and Al11, respectively. The identified 4th order sequence boundaries, transgressive systems tracts, maximum flooding surfaces, and highstand stystems tracts are regionally correlated using electric wireline logs. The Wara silisiclastic reservoirs are developed towards the south while the Tuba carbonate reservoirs are developed towards the north.	[Youssef, Abdulkader H.; Al-Sahlan, Ghaida; Kadar, Adi P.; Karam, Khalaf A.] Kuwait Oil Co, Explorat Grp, POB 9758, Ahmadi, Kuwait; [Packer, Stephen] Millennia SC Ltd, Unit 2B, Wingrave HP22 4LW, Bucks, England; [Starkie, Stephen] Datum Stratig Associates Ltd, 12 Meade, Manchester M21 8FA, Lancs, England; [Stead, Darrin] Wellstrat Serv Ltd, 1 Castle Grange, Wrexham LL12 9HL, Wales	Kuwait Oil Company	Youssef, AH (通讯作者)，Kuwait Oil Co, Explorat Grp, POB 9758, Ahmadi, Kuwait.	ahyoussef@kockw.com						ABDULKARIM I. A., 1987, STRATIGRAPHIC UNPUB; Adasani M., 1965, 5TH AR PETR C, P7; Al-Fares A., 1998, GeoArabia, V3, P543, DOI DOI 10.2113/GEOARABIA0304543; ALSHARHAN AS, 1993, AAPG MEMOIR, V56, P173; ASHTON BADLEY, 2010, CORE SEDIMENTO UNPUB; BATE, 1996, ENV INTERPRETA UNPUB; Bergen James A., 1994, Journal of Nannoplankton Research, V16, P59; Brennan P., 1990, Structural Traps I, Treatise of Petroleum Geology, Atlas of Oil and Gas Fields, P103; Burnett J.A., 1998, P132; CARMAN G. 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J	Duxbury, S				Duxbury, Stan			Organic-walled marine microplankton from the Barremian and Aptian of the North Sea Region - biostratigraphy and taxonomy	MICROPALEONTOLOGY			English	Article						Palynology; zonation; dinocysts; Barremian; Aptian; Speeton Clay; UK; Saxony	DINOFLAGELLATE CYSTS; BASIN; STRATIGRAPHY; PROPOSALS; ZONATION; MARGIN	Quantitative palynofloral analysis of 42 core chip samples from upper Barremian and Aptian sediments of the Heslerton No. 2 shallow borehole (Speeton Clay Formation, Eastern England) and Gannet Field well 22/26a-2 (Valhall Formation, United Kingdom Sector, Central North Sea) has yielded very rich and diverse marine assemblages composed largely of dinocysts and acritarchs. The high biostratigraphic resolution achieved has allowed detailed correlation between the sections analysed and with third-party data from the Wiechendorf 1/86 borehole (Lower Saxony Basin), a distance of approximately 700 km; the positions and extent of several hiatuses have been assessed within this framework. The Barremian/Aptian boundary has been discussed and "conventional" palynological criteria assessed with respect to contrary microfaunal and nannofloral evidence. Close spacing of samples has allowed some assessment of inter-and intra-species trends and, although palaeoenvironmental change profoundly influences assemblages, specific controls remain poorly understood. Over-prescriptive generic placement of taxa based on what are essentially subjective criteria is critically discussed. The zonation scheme proposed by Duxbury (2001) has been re-visited and significantly refined; recognition of additional marker events has allowed further sub-division of several zones to subzonal level, allowing a better understanding of late Barremian palynostratigraphy. Seventy-nine key palynofloral events have now been recognised between the late Barremian and "mid" Aptian, including many first occurrences. One genus, 23 species and 2 subspecies of dinocysts are described as new, nine new combinations have been effected and the diagnoses of two species have been emended; one species has been reduced to sub-species rank.	[Duxbury, Stan] Duxbury Stratig Consultants, Church Lane, Chester CH2 1DJ, Cheshire, England		Duxbury, S (通讯作者)，Duxbury Stratig Consultants, Church Lane, Chester CH2 1DJ, Cheshire, England.	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Pap.; Williams GL, 2016, PALYNOLOGY, V40, P137, DOI 10.1080/01916122.2015.1113209; WILPSHAAR M, 1994, REV PALAEOBOT PALYNO, V84, P121, DOI 10.1016/0034-6667(94)90046-9	145	6	6	2	5	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	0026-2803	1937-2795		MICROPALEONTOLOGY	Micropaleontology		2019	65	3					173	276						98	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	IA8WN					2025-03-11	WOS:000469839400001
J	Yurur, EE				Yurur, Emine Erdem			DINOFLAGELLATE CYST ASSEMBLAGES IN THE SURFACE SEDIMENTS FROM ISKENDERUN BAY, NORTHEASTERN MEDITERRANEAN	FRESENIUS ENVIRONMENTAL BULLETIN			English	Article						Dinoflagellate; cyst; sediment; Iskenderun Bay; Mediterranean	RECENT MARINE-SEDIMENTS; IZMIR BAY; COASTAL WATERS; AEGEAN SEA; PHYTOPLANKTON ASSEMBLAGES; ZOOPLANKTON ABUNDANCE; ECOSYSTEM; BIOMASS; GULF; EUTROPHICATION	To document and understand dinoflagellate cyst assemblages, 6 surface sediment samples were collected from Iskenderun Bay, in the northeastern Mediterranean. A total of 28 cyst types were identified and the cyst concentration was attained as 144 cysts g-' dry weight sediment in the bay. The cyst concentration was low when compared to other areas in the Mediterranean. Lingulodinium machaerophorum, SpiMferites bulloideus, and Brigantedinium spp. were the most abundant cysts in the sampling points. Three of the stations had a sandy sediment grain size, while the other stations had a muddy (silt + clay) sediment distribution. Only the clay exhibited a significantly strong positive correlation with the total and heterotrophic dinoflagellate cyst concentrations, whereas no other strong correlation was found between the sediment grain size and dinoflagellate cysts. The present study provides the first modern dinoflagellate cyst records from the surface sediments of Iskenderun Bay, in the northeastern Mediterranean.	[Yurur, Emine Erdem] Manisa Celal Bayar Univ, Biol Dept, Fac Sci & Arts, Martyr Ilhan Varank Campus, TR-45140 Manisa, Turkey	Celal Bayar University	Yurur, EE (通讯作者)，Manisa Celal Bayar Univ, Biol Dept, Fac Sci & Arts, Martyr Ilhan Varank Campus, TR-45140 Manisa, Turkey.	ehyurur@gmail.com.tr						Aktan Y, 2011, ESTUAR COAST SHELF S, V91, P551, DOI 10.1016/j.ecss.2010.12.010; Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; Aydin H, 2015, TURK J FISH AQUAT SC, V15, P543, DOI 10.4194/1303-2712-v15_2_42; Aydin H, 2015, FRESEN ENVIRON BULL, V24, P4789; Aydin H, 2015, MAR POLLUT BULL, V94, P144, DOI 10.1016/j.marpolbul.2015.02.038; 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; Balkis N, 2016, PHYCOLOGIA, V55, P187, DOI 10.2216/15-93.1; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; Elshanawany R, 2010, PALYNOLOGY, V34, P233, DOI 10.1080/01916121003711665; Ferrante M., 2013, EuroMediterranean Biomed. 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Bull.		2019	28	2A					1356	1365						10	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	HO9GW					2025-03-11	WOS:000461270800039
J	Gao, H; You, SP; Lei, XD; Xiao, YP; Gu, HF; Tong, MM				Gao, Han; You, Shengpao; Lei, Xiangdong; Xiao, Yunpu; Gu, Haifeng; Tong, Mengmeng			The impact of biotic and abiotic factors on the distribution of surface sediment dinoflagellate cyst assemblages on the Nanji Island in the East China Sea	ACTA OCEANOLOGICA SINICA			English	Article; Proceedings Paper	10th WESTPAC International Scientific Conference	APR 17-20, 2017	Qingdao, PEOPLES R CHINA	UNESCO, State Ocean Adm China & Intergovernmental Oceanog Commiss, IOC Sub commiss W Pacific, First Inst Oceanog China		dinoflagellate cyst; Nanji Island; nutrients; harmful algal blooms	RESTING CYSTS; ALEXANDRIUM-CATENELLA; NORTH-ATLANTIC; TOKYO-BAY; SCRIPPSIELLA; DYNAMICS; BLOOM; GULF; PRODUCTIVITY; MORPHOLOGY	The dinoflagellate cyst assemblages on the Nanji Island in the East China Sea, are documented at the first time to construct a quantitative overview of the cyst bank from 2014 to 2015. Thirty-four morphotypes from six groups are identified and quantified at eight sampling sites around the island, including a high proportion of potentially toxigenic species (14%). Autotrophic dinocysts constitute 74% of the total cyst counts, which is relatively low (two to thirty-three per millilitre sediment) compared with previous studies in adjacent areas. Scrippsiella trochoidea and Protoperidinium avellana are the most abundant autotrophic and heterotrophic species, respectively. A multivariate analysis is performed to assess associations between dinocysts and abiotic or biotic variables. Differentiation among seasons is evident in the detrended correspondence analysis (DCA) ordination plot, while a spatial pattern is not clearly revealed despite heterogeneity of the hydrodynamic conditions between sampling sites. Soluble reactive phosphate, the ratio of nitrogen to phosphorus concentrations and Karenia mikimotoi bloom are the three factors significantly (P<0.05) related to surface sediment cyst assemblage defined by the canonical correspondence analysis (CCA), highlighting the importance of nutrient regime to a dinocyst distribution in this area. Although attempts to address the origin of HAB events in recent years using seed banks have failed, knowledge can be valuable for further investigation of dinocyst dynamics and potential toxin threats on the Nanji Island.	[Gao, Han; Xiao, Yunpu; Tong, Mengmeng] Zhejiang Univ, Ocean Coll, Zhoushan 316000, Peoples R China; [You, Shengpao; Lei, Xiangdong] Minist Nat Resources, Nanji Marine Environm Monitoring Stn, Pingyang 325400, Peoples R China; [Xiao, Yunpu] Pingyang Cty Marine & Fisheries Bur, Pingyang 325400, Peoples R China; [Gu, Haifeng] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China	Zhejiang University; Ministry of Natural Resources of the People's Republic of China; Ministry of Natural Resources of the People's Republic of China; Third Institute of Oceanography, Ministry of Natural Resources	Tong, MM (通讯作者)，Zhejiang Univ, Ocean Coll, Zhoushan 316000, Peoples R China.	mengmengtong@zju.edu.cn	Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171	Zhejiang Public Welfare Technology Research and Social Development Project of 2013 of China [2013C33081, 2013C32040]; National Natural Science Foundation of China [41306095]; Doctoral Fund of Ministry of Education of China [J20130101]	Zhejiang Public Welfare Technology Research and Social Development Project of 2013 of China; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Doctoral Fund of Ministry of Education of China(Ministry of Education, China)	Foundation item: The Zhejiang Public Welfare Technology Research and Social Development Project of 2013 of China under contract Nos 2013C33081 and 2013C32040; the National Natural Science Foundation of China under contract No. 41306095; the Doctoral Fund of Ministry of Education of China under contract No. J20130101.	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Sin.	JAN	2019	38	1					160	171		10.1007/s13131-019-1375-9	http://dx.doi.org/10.1007/s13131-019-1375-9			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Oceanography	HM4UA					2025-03-11	WOS:000459469100021
J	Turner, HE; Batenburg, SJ; Gale, AS; Gradstein, FM				Turner, Holly E.; Batenburg, Sietske J.; Gale, Andy S.; Gradstein, Felix M.			The Kimmeridge Clay Formation (Upper Jurassic-Lower Cretaceous) of the Norwegian Continental Shelf and Dorset, UK: a chemostratigraphic correlation	NEWSLETTERS ON STRATIGRAPHY			English	Article						Kimmeridge Clay Formation; chemostratigraphy; Late Jurassic; Early Cretaceous; cyclostratigraphy; Greenland-Norwegian Seaway	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SEA-LEVEL CHANGES; ORGANIC-CARBON; JURASSIC/CRETACEOUS BOUNDARY; SEQUENCE STRATIGRAPHY; BASIN; HISTORY; CYCLOSTRATIGRAPHY; FRACTIONATION; PALYNOFACIES	The Late Jurassic and Early Cretaceous were characterised by a number of carbon cycle perturbations, of which the temporal and geographic extent are poorly understood. This is due to a scarcity of high-resolution records and difficulties in correlation because of faunal provincialism and insufficiently constrained chronostratigraphy. In the Boreal and Sub-boreal seas of north-western Europe, the Kimmeridge Clay Formation (KCF) was deposited, a source-rock for oil of great economic value. Precise correlation is critical for assessing the nature of widespread organic matter deposition. Here we compare biostratigraphically-constrained organic carbon-isotope records from the Norwegian Continental Shelf with the Kimmeridgian-Tithonian (Upper Jurassic) Kimmeridge Clay Formation of the Dorset type area and with upper Tithonian-Berriasian (Upper Jurassic-Lower Cretaceous) records of Svalbard and Siberia. A number of isotopic excursions have been correlated between the studied cores (four Lundin Norway cores and one Statoil core from the Norwegian Continental Shelf) and from KCF-coeval sections in the Tethyan and Boreal realms. We identify and correlate the Eudoxus Zone positive shift, Hudlestoni Zone short-term negative shift, Volgian Isotopic Carbon Excursion (VOICE) and J/K boundary negative isotope excursion. Whereas physical properties or biostratigraphic data alone usually do not allow precise correlation, our integrated approach enables us to identify and correlate synchronous events amongst interregional sections. In addition, time series analyses of TOC records from two wells reveal cycles that strongly resemble the short-term eccentricity component recorded in Dorset. Correlation to the cyclostratigraphic framework of Dorset provides independent support of our age model, which is based on C-isotope stratigraphy and biostratigraphy. Our regional-scale correlation reflects the consistency of the C-isotope signal in the seas of north-western Europe at the time of deposition, and a high correlation potential across significant distances. In particular, correlation of C-isotope signals in the Early Cretaceous attests to sufficiently open marine conditions in the Greenland-Norwegian Seaway to record global carbon cycle variations despite a sea level lowstand.	[Turner, Holly E.; Gale, Andy S.] Univ Portsmouth, Sch Earth & Environm Sci, Burnaby Bldg,Burnaby Rd, Portsmouth PO1 3QL, Hants, England; [Batenburg, Sietske J.] Univ Oxford, Dept Earth Sci, South Parks Rd, Oxford OX1 3AN, England; [Gradstein, Felix M.] Univ Oslo, Nat Hist Museum, Postboks 1172, N-0318 Oslo, Norway	University of Portsmouth; University of Oxford; University of Oslo	Turner, HE (通讯作者)，Univ Portsmouth, Sch Earth & Environm Sci, Burnaby Bldg,Burnaby Rd, Portsmouth PO1 3QL, Hants, England.	holly.tumer@port.ac.uk	Batenburg, Sietske/AAD-6896-2019	Turner, Holly/0000-0003-3807-9001; Batenburg, Sietske J./0000-0002-4076-1248	NORLEX studentship; Geologic TimeScale Foundation	NORLEX studentship; Geologic TimeScale Foundation	This work was carried out whilst in receipt of a NORLEX studentship supplemented by Lundin Norway and the Geologic TimeScale Foundation. Gratitude is owed to M. Charnock for organisation of core viewing and sampling, and D. G. Bell at APT for palynological training. Thanks to Alevtina Dorn for sampling well 6406/12-2. We are grateful for Dr B. Cox's assistance with ammonite identifications and to M. J. Koevoets and Drs O. Hammer and NI. Rogov for sharing of their published data. Thanks are extended to Drs S. Nicoara and M. Gilmour from the OU stable isotope lab, to Dr D. Loydell and Professor A. Gotz for helpful and constructive discussions, and to Professor Ian Jarvis and three anonymous reviewers whose valuable suggestions and comments greatly improved the manuscript.	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J	Soliman, A; Slimani, H				Soliman, Ali; Slimani, Hamid			<i>Pentadinium dababiyaense</i>: A new organic-walled dinoflagellate cyst from the Upper Cretaceous, Dababiya, Egypt	CRETACEOUS RESEARCH			English	Article						Pentadinium; Suturocavate; Lace-like perforations; Maastrichtian; Dababiya; Egypt	UPPER NILE VALLEY; QUARRY COREHOLE; BIOSTRATIGRAPHY; OLIGOCENE; LITHOSTRATIGRAPHY; SUCCESSION; PALEOCENE; GULF	Pentadinium dababiyaense is a new, organic-walled dinoflagellate cyst (dinocyst), described herein from Upper Cretaceous core material from the Dababiya borehole, Upper Nile Valley, Egypt. It is characterized by having a distinctive cavate apical horn and cavate sutural crests with lace-like perforations in the periphragm. The sutural crests, together with the precingular type P archeopyle indicate a gonyaulacoid tabulation. The species has a very short stratigraphic range within the latest Maastrichtian and may constitute a useful stratigraphic marker. (C) 2018 Elsevier Ltd. All rights reserved.	[Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Slimani, Hamid] Univ Mohammed V Rabat, Geobiodivers & Nat Patrimony Lab GEOBIO, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Sci Inst, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco	Egyptian Knowledge Bank (EKB); Tanta University; Mohammed V University in Rabat	Soliman, A (通讯作者)，Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt.	ali.soliman@science.tanta.edu.eg; h_slimani@yahoo.com	Slimani, Hamid/AAL-4055-2020; Soliman, Ali/R-1583-2018	Soliman, Ali/0000-0001-7366-4607; Slimani, Hamid/0000-0001-6392-1913				Aubry MP, 2012, STRATIGRAPHY, V9, P241; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; Berggren WA, 2012, AUSTRIAN J EARTH SCI, V105, P161; Dupuis C, 2003, MICROPALEONTOLOGY, V49, P41, DOI 10.2113/49.Suppl_1.41; Dupuis C, 2012, STRATIGRAPHY, V9, P205; EDWARDS L E, 1982, Palynology, V6, P105; Eisenack A., 1965, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V123, P149; Fensome RA, 2009, J SYST PALAEONTOL, V7, P1, DOI 10.1017/S1477201908002538; Gerlach E., 1961, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V112, P143; Goolaerts S, 2012, STRATIGRAPHY, V9, P261; HARDING I C, 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P1; Sancay RH, 2006, MICROPALEONTOLOGY, V52, P537, DOI 10.2113/gsmicropal.52.6.537; Morgenroth P., 1966, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V127, P1; Obaidalla N, 2012, STRATIGRAPHY, V9, P229; Quaijtaal W, 2012, REV PALAEOBOT PALYNO, V175, P47, DOI 10.1016/j.revpalbo.2012.03.002; Schioler P, 2005, J MICROPALAEONTOL, V24, P1, DOI 10.1144/jm.24.1.1; Soliman A., 2018, CRETACEOUS PAL UNPUB; Soliman A, 2012, PALYNOLOGY, V36, P38, DOI 10.1080/01916122.2011.633632; Soliman A, 2012, GEOL CARPATH, V63, P49, DOI 10.2478/v10096-012-0004-8; Stover L.E., 1978, ANAL PRE PLEISTOCENE, V15; Stover Lewis E., 1994, Bulletin de la Societe Belge de Geologie, V102, P5; Strauss Christoph, 1992, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V73, P159; Tabara D, 2017, CRETACEOUS RES, V77, P102, DOI 10.1016/j.cretres.2017.04.021; von Benedek P.N., 1982, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V162, P265; Williams Graham L., 2017, AASP Contributions Series, V48, P1; ZHAO YY, 1994, GEOBIOS-LYON, V27, P261, DOI 10.1016/S0016-6995(94)80172-X	26	2	2	0	4	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	JAN	2019	93						188	196		10.1016/j.cretres.2018.09.005	http://dx.doi.org/10.1016/j.cretres.2018.09.005			9	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	HE6FI					2025-03-11	WOS:000453498300018
J	Gupta, S; Kumar, K				Gupta, Smita; Kumar, Kishor			Precursors of the Paleocene-Eocene Thermal Maximum (PETM) in the Subathu Group, NW sub-Himalaya, India	JOURNAL OF ASIAN EARTH SCIENCES			English	Article						Paleocene - Eocene Thermal Maximum (PETM); Carbon Isotope Excursion (CIE); Apectodinium; Subathu Group; NW sub-Himalaya; India	DINOFLAGELLATE CYSTS; ISOTOPE EXCURSION; HIMACHAL-PRADESH; FORELAND BASIN; COMET IMPACT; SECTION; METHANE; BOUNDARY; SEA; ACIDIFICATION	The Paleocene-Eocene Thermal Maximum (PETM) is one of the most pronounced and widely documented global warming events in the geological history that occurred at the beginning of the Eocene (similar to 56 Ma) causing substantial changes in biota and geochemistry. It is marked worldwide by a negative isotopic excursion of delta C-13. The biotic changes associated with the PETM in marine realm include bloom of the dinoflagellate Apectodinium, turnover of larger foraminiferids, diversification of planktic foraminiferids, and carbonate dissolution of calcareous test shells, etc. while the geochemical changes include decrease in carbonates and increase in abundance of silicates and phyllosilicates, etc. Conspicuously, there has been no attempt to identify the PETM in the Himalaya even though some Himalayan sections are known to have Paleocene-Eocene transition beds. To fill this lacuna, we investigated the basal part of the late Paleocene-middle Eocene Subathu Group exposed at the village Kurla near Subathu in Himachal Pradesh (NW sub-Himalaya) for biotic, mineralogical, and geochemical signatures of this abrupt warming event. The significant results of this study include carbon isotope excursion (CIE) of 3.4 parts per thousand, occurrence of index di-noflagellate genus Apectodinium, and carbonate dissolution of the larger benthic foraminiferids. The mineralogical changes noted across the Paleocene - Eocene transition include increase in quartz and phyllosilicates and decrease in carbonates. The geochemical changes include (i) increase in SiO2, Al2O3, K2O, and Fe2O3, (ii) decrease in CaCO3, (iii) decreasing trend of Si/Al, Fe/Al, and Mg/Al ratios, (iv) increasing trend of K/Al, Ti/Al, and Zr/Al ratios, (v) changes in trace element abundance, (vi) maximum chemical index of alteration (CIA) of 85-89%, and (vii) increase in abundance of rare earth elements. The aforementioned dataset is clearly very close to the PETM and even reflects its probable onset and peak phases, however, it is insufficient to definitively identify the PETM in the studied section. Nevertheless, since this study is the first from a Himalayan section and brings out considerable new information, all results and interpretations are presented and discussed here.	[Gupta, Smita; Kumar, Kishor] Wadia Inst Himalayan Geol, 33 Gen Mahadeo Singh Rd, Dehra Dun 248001, India	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, India.	kishorsri@gmail.com	KUMAR, Kishor/H-7232-2013	Kumar, Kishor/0000-0003-0875-9735				Adatte K.H., 2014, RENDICONTI ONLINE SO, V31, P5; Afzal J, 2011, LETHAIA, V44, P299, DOI 10.1111/j.1502-3931.2010.00247.x; Anderson T.F., 1983, STABLE ISOTOPES SEDI, V10, p1.1, DOI 10.2110/scn.83.10; [Anonymous], 1988, Geol. 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Asian Earth Sci.	JAN	2019	169						21	46		10.1016/j.jseaes.2018.05.027	http://dx.doi.org/10.1016/j.jseaes.2018.05.027			26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	HE7LQ					2025-03-11	WOS:000453619400003
S	Hegseth, EN; Assmy, P; Wiktor, JM; Wiktor, J; Kristiansen, S; Leu, E; Tverberg, V; Gabrielsen, TM; Skogseth, R; Cottier, F		Hop, H; Wiencke, C		Hegseth, Else N.; Assmy, Philipp; Wiktor, Jozef M.; Wiktor, Jozef, Jr.; Kristiansen, Svein; Leu, Eva; Tverberg, Vigdis; Gabrielsen, Tove M.; Skogseth, Ragnheid; Cottier, Finlo			Phytoplankton Seasonal Dynamics in Kongsfjorden, Svalbard and the Adjacent Shelf	ECOSYSTEM OF KONGSFJORDEN, SVALBARD	Advances in Polar Ecology		English	Article; Book Chapter						Arctic; Kongsfjorden; Phytoplankton; Svalbard; Time-series	ARCTIC FJORD KONGSFJORDEN; MARINE MICROBIAL EUKARYOTES; ATLANTIC WATER INFLOW; SPRING BLOOM DYNAMICS; MARGINAL ICE-ZONE; ZOOPLANKTON COMMUNITY; PHAEOCYSTIS-POUCHETII; PHYSICAL-ENVIRONMENT; PARTICULATE MATTER; WEST SPITSBERGEN	Phytoplankton phenology is a key driver of biological and chemical processes in marine ecosystems because it directly affects cycling of nutrients, the strength of the biological carbon pump, and energy transfer to higher tropic levels. However, phytoplankton time-series from the Arctic are scant, thus limiting our ability to link phytoplankton phenology to environmental variability. Kongsfjorden on the west coast of Spitsbergen is an established coastal monitoring site at the entrance to the Arctic Ocean. In this review we have compiled previously published phytoplankton investigations, chlorophyll fluorescence time-series data and unpublished phytoplankton data covering the years 2002-2014 from Kongsfjorden and the shelf outside the fjord to elaborate the most pertinent environmental factors responsible for the seasonal and inter-annual variability in phytoplankton bloom dynamics, biomass and species composition. In general, phytoplankton dynamics in Kongsfjorden follow the classic spring-bloom paradigm, with the main biomass peak in April-May dominated by spore-forming diatom species and the colony-forming haptophyte Phaeocystis pouchetii, followed by a diverse, but low biomass community characterised by dinoflagellates and small flagellates and their protozoan grazers during summer. Despite this general trend, phytoplankton phenology is subject to large inter-annual variability with no clear long-term trend. This variability can be mainly attributed to variability in the magnitude and depth of Atlantic Water (AW) inflow, sea ice cover and glacier melt-water discharge. We have shown the impact of environmental variability on phytoplankton phenology, but high-resolution monitoring of annual cycles over many years is required to resolve the ephemeral variations of phytoplankton populations in space and time against the backdrop of climate change.	[Hegseth, Else N.; Kristiansen, Svein; Cottier, Finlo] UiT Arctic Univ Norway, Fac Biosci Fisheries & Econ, Dept Arctic & Marine Biol, Tromso, Norway; [Assmy, Philipp] Norwegian Polar Res Inst, Fram Ctr, Tromso, Norway; [Wiktor, Jozef M.; Wiktor, Jozef, Jr.] Polish Acad Sci, Inst Oceanol, Sopot, Poland; [Leu, Eva] Akvaplan Niva AS, Fram Ctr, Tromso, Norway; [Tverberg, Vigdis] Nord Univ, Fac Biosci & Aquaculture, Bodo, Norway; [Gabrielsen, Tove M.; Skogseth, Ragnheid] Univ Ctr Svalbard, Longyearbyen, Norway; [Cottier, Finlo] Scottish Assoc Marine Sci, Scottish Oceans Inst, Oban, Argyll, Scotland	UiT The Arctic University of Tromso; Norwegian Polar Institute; Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences; Akvaplan-niva; Nord University; University Centre Svalbard (UNIS); University of the Highlands & Islands	Hegseth, EN (通讯作者)，UiT Arctic Univ Norway, Fac Biosci Fisheries & Econ, Dept Arctic & Marine Biol, Tromso, Norway.	else.hegseth@uit.no	Tverberg, Vigdis/AAC-8801-2021; 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J	Correia, VF; Riding, JB; Henriques, MH; Fernandes, P; Pereira, Z; Wiggan, NJ				Correia, Vania F.; Riding, James B.; Henriques, Maria Helena; Fernandes, Paulo; Pereira, Zelia; Wiggan, Nickolas J.			The Middle Jurassic palynostratigraphy of the northern Lusitanian Basin, Portugal	NEWSLETTERS ON STRATIGRAPHY			English	Article						biostratigraphy; dinoflagellate cysts; Cabo Mondego and Sao Giao; Lusitanian Basin; Middle Jurassic; palaeobiology	DINOFLAGELLATE CYSTS; BENTHIC FORAMINIFERA; STRATOTYPE SECTION; EARLY BAJOCIAN; ALGARVE BASIN; CABO MONDEGO; POINT GSSP; WEST SHELF; PALYNOLOGY; ASSEMBLAGES	A composite largely Middle Jurassic succession spanning the Toarcian-Aalenian transition to the lowermost Bathonian exposed at Cabo Mondego and Sao Giao in the northern Lusitanian Basin, western Portugal, was examined palynologically. The 129 samples are correlated to ammonite biozones spanning Pleydellia aalensis to Zigzagiceras zigzag. The Cabo Mondego succession comprises the type section of the Cabo Mondego Formation and spans virtually the entire interval studied. This is a significant interval because it includes the Global Stratotype Section and Point (GSSP) and the Auxiliary Stratigraphical Section and Point (ASSP) for the Bajocian and Bathonian stages respectively. The Cabo Mondego Formation largely yielded relatively abundant palynomorph associations in the 68 productive samples recovered. By contrast, the Povoa da Lomba Formation at Sao Giao only includes the Toarcian-Aalenian transition; the 21 productive horizons produced sparse assemblages. The uppermost Toarcian to lowermost Bajocian is characterised by a low diversity dinoflagellate cyst association, typified by Nannoceratopsis. Above this is a markedly more diverse assemblage. This influx, in the Witchellia laeviuscula ammonite biozone AB, represents a global evolutionary radiation which may be linked to sea level rise. The trend of increasing dinoflagellate cyst diversity continued at the Bajocian-Bathonian transition. The Middle Jurassic dinoflagellate cyst assemblages of the Lusitanian Basin are significantly less diverse than coeval palynobiotas from eastern and northern Europe, and the Arctic. The Toarcian Oceanic Anoxic Event (T-OAE) profoundly inhibited cyst-forming dinoflagellates in this depocentre, and the recovery was protracted. Hence the T-OAE may have suppressed dinoflagellate cyst diversity well into the Middle Jurassic. This phenomenon may have been exacerbated by the absence of typically Arctic taxa through latitudinal controls and/or global cooling during the early Aalenian. These low levels of dinoflagellate cyst species richness may also be related to the palaeogeography of the Lusitanian Basin. This relatively isolated deepwater depocentre close to the Proto Atlantic, may have precluded extensive biotal exchange with the widespread shelfal areas of the western Tethys. The absence of Dissiliodinium giganteum in the Lusitanian Basin is consistent with this scenario. The pollen and spores observed in this study are typical of Middle Jurassic assemblages worldwide. Araucarian pollen, largely Callialasporites, diversified and became prominent during the Aalenian.	[Correia, Vania F.; Fernandes, Paulo] Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal; [Correia, Vania F.; Pereira, Zelia] LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal; [Riding, James B.; Wiggan, Nickolas J.] British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, England; [Henriques, Maria Helena] Univ Coimbra, Fac Sci & Technol, Dept Earth Sci, Rua Silvio Lima, P-3030790 Coimbra, Portugal; [Henriques, Maria Helena] Univ Coimbra, Fac Sci & Technol, Geosci Ctr, Rua Silvio Lima, P-3030790 Coimbra, Portugal; [Wiggan, Nickolas J.] Univ Cambridge, Dept Earth Sci, Downing St, Cambridge CB2 3EQ, England	Universidade do Algarve; Laboratorio Nacional de Energia e Geologia IP (LNEG); UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universidade de Coimbra; Universidade de Coimbra; University of Cambridge	Correia, VF (通讯作者)，Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal.; Correia, VF (通讯作者)，LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal.	mvania.correia@lneg.pt	Henriques, Maria/H-9356-2019; Pereira, Zelia/B-2740-2017; Fernandes, Paulo/J-6577-2014	Henriques, Maria Helena/0000-0001-7943-3148; Correia, Vania/0000-0001-5648-3185; Pereira, Zelia/0000-0003-3056-6219; Fernandes, Paulo/0000-0003-4888-0230	Portuguese Foundation for Science and Technology (FCT) [SFRH/BD/93950/2013]; FCT [UID/Multi/00073/2013]; Fundação para a Ciência e a Tecnologia [UID/Multi/00073/2013, SFRH/BD/93950/2013] Funding Source: FCT; NERC [bgs05017] Funding Source: UKRI	Portuguese Foundation for Science and Technology (FCT)(Fundacao para a Ciencia e a Tecnologia (FCT)); FCT(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The contribution of Vania F. Correia represents part of PhD scholarship SFRH/BD/93950/2013 awarded by the Portuguese Foundation for Science and Technology (FCT). James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). The contribution of M. Helena Henriques is supported by the FCT as part of research project UID/Multi/00073/2013. The authors are grateful to the two anonymous reviewers and to the journal editor, Prof. Jorg Pross.	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J	Smelror, M; Boe, R; Davidsen, B; Ottesen, D				Smelror, Morten; Boe, Reidulv; Davidsen, Borre; Ottesen, Dag			The Sortlandsundet Basin, Vesteralen, northern Norway: a Jurassic basin based on erratics, seismic mapping and regional correlations	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Jurassic basin; seismics; erratic rocks; correlations; Sortlandsundet	DINOFLAGELLATE CYSTS; CONTINENTAL-MARGIN; CRUSTAL STRUCTURE; VOLCANIC MARGIN; ICE-SHEET; LOFOTEN; STRATIGRAPHY; NORDLAND; EVOLUTION; OFFSHORE	The Sortlandsundet Basin is a half-graben with Mesozoic sediments located in Sortlandsundet between Langoya and Hinnoya in Vesteralen. The basin is defined by the Hadselfjord Fault Zone in the southeast and by unconformable boundaries to Archaean to Palaeoproterozoic basement rocks to the northeast, northwest and southwest. The basin may have originated as an extensional basin and evolved as a transtensional basin in the Jurassic-Early Cretaceous. Sedimentary strata of probable Jurassic age within the basin are more than 400 m thick, with seismic reflectors dipping slightly to the southeast. Glacial-transported erratic blocks, assumed to derive from the Sortlandsundet Basin, are found along the shores of Sortlandsundet. The blocks comprise quartz-rich sedimentary rocks, varying from conglomerates to tine sandstones, representing terrestrial to shallow-marine deposits. Many of the erratic blocks contain common macro- and microfossils of Middle and Late Jurassic age. A syn-tectonic depositional model for the Sortlandsundet Basin with correlations to the age-equivalent strata offshore Vesterfilen (Ribban Basin) and on Andoya is discussed.	[Smelror, Morten; Boe, Reidulv; Davidsen, Borre; Ottesen, Dag] Geol Survey Norway, POB 6315 Torgarden, NO-7491 Trondheim, Norway	Geological Survey of Norway	Smelror, M (通讯作者)，Geol Survey Norway, POB 6315 Torgarden, NO-7491 Trondheim, Norway.	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J. Geol.		2019	99	4					597	618		10.17850/njg99-4-4	http://dx.doi.org/10.17850/njg99-4-4			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	VJ5SU		gold			2025-03-11	WOS:000608713500002
J	Mahboub, I; Slimani, H; Toufiq, A; Chekar, M; Djeya, KL; Jbari, H; Chakir, S				Mahboub, Imane; Slimani, Hamid; Toufiq, Abdelkabir; Chekar, Mouna; Djeya, Kouame Leger; Jbari, Hassan; Chakir, Sara			Middle Eocene to early Oligocene dinoflagellate cyst biostratigraphy and paleoenvironmental interpretations of the Ben Attaya section at Taza, eastern External Rif, Morocco	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Bartonian-Rupelian; Dinocyst stratigraphy; Paleoenvironment; External Rif; Southern Mediterranean	CRETACEOUS-PALEOGENE BOUNDARY; OULED HADDOU; SEA-LEVEL; PALYNOLOGICAL APPROACH; NORTH; BASIN; TRANSITION; SUCCESSION; DEPOSITS; TUNISIA	The palynological study was carried out on middle Eocene to early Oligocene sediments from the Ben Aattaya section, located in the Taza region, eastern External Rif, northeastern Morocco. The palynological content is dominated by dinoflagellate cysts (dinocyst), while spores and pollen are rare. Very known dinocyst event markers were used for dating the Ben Attaya section. The first occurrences (FO) of Cerebrocysta bartonensis, Glaphyrocysta semitecta, Lentinia serrata, Operculodinium divergens indicate the Bartonian. The FOs of Defiandrea heterophlycta, Schematophora speciosa, Stoveracysta ornata were used to recognize the Priabonian. While the FOs of Chiropteridium lobospinosum and Wetzeliella gochtii, as well as the last occurrences (LO) of Achilleodinium biformoides, Charlesdowniea coleothrypta subsp. coleothrypta, Enneadocysta pectiniformis, Glaphyrocyst semitecta, Hemiplacophora semilunifera, Lentinia serrata, Operculodinium divergens, Rhombodinium perforatwn, Schematophora speciosa and Stoverocysta ornata highlight the Rupelian. The changes in relative abundances of selected dinocyst groups and sporomorphs (pollen and spores) suggest a lagoonal to coastal inner neritic marine environment during the Bartonian and Priabonian, which was interrupted by a short phase of outer neritic conditions at the basal part of the section and ended by a marked decrease in the sea level, probably due to a regression during the Priabonian. The Rupelian deposits indicate a middle neritic marine environment marked by a progressive rise during the transgression.	[Mahboub, Imane; Slimani, Hamid; Chekar, Mouna; Jbari, Hassan] Mohammed V Univ Rabat, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Sci Inst, Geobiodivers & Nat Patrimony Lab GEOBIO, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco; [Toufiq, Abdelkabir] Univ Chouaib Doukkali, Fac Sci, Lab Geosci & Tech Environm, El Jadida, Morocco; [Djeya, Kouame Leger] Univ Felix Houphouet Boigny Cocody, Dept Marine Geosci, Abidjan, Cote Ivoire; [Chakir, Sara] Univ Hassan II Casablanca, Fac Sci Ben Msik, BP 7955, Casablanca, Morocco	Mohammed V University in Rabat; Chouaib Doukkali University of El Jadida; Universite Felix Houphouet-Boigny; Hassan II University of Casablanca	Slimani, H (通讯作者)，Mohammed V Univ Rabat, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Sci Inst, Geobiodivers & Nat Patrimony Lab GEOBIO, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913	University Mohammed V in Rabat [SVT 11/09]; National Center for Scientific and Technical Research (Research Unit: URAC46) in Morocco	University Mohammed V in Rabat; National Center for Scientific and Technical Research (Research Unit: URAC46) in Morocco	We are grateful to the University Mohammed V in Rabat (Project SVT 11/09) and the National Center for Scientific and Technical Research (Research Unit: URAC46) in Morocco for their support. The journal editor Prof. Mohamed Abdelsalam and two anonymous reviewers are kindly thanked for their constructive reviews. The authors thank Obianuju P. Umeji of the University of Nigeria who checked the English.	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Afr. Earth Sci.	JAN	2019	149						154	169		10.1016/j.jafrearsci.2018.08.006	http://dx.doi.org/10.1016/j.jafrearsci.2018.08.006			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	HA0JN					2025-03-11	WOS:000449894400011
J	Deng, YY; Hu, ZX; Chai, ZY; Tang, YZ				Deng, Yunyan; Hu, Zhangxi; Chai, Zhaoyang; Tang, Ying Zhong			Molecular cloning of heat shock protein 60 (Hsp60) and 10 (Hsp10) genes from the cosmopolitan and harmful dinoflagellate <i>Scrippsiella trochoidea</i> and their differential transcriptions responding to temperature stress and alteration of life cycle	MARINE BIOLOGY			English	Article							HEAT-SHOCK PROTEINS; RED TIDE DINOFLAGELLATE; DROSOPHILA-MELANOGASTER; EXPRESSION ANALYSIS; AKASHIWO-SANGUINEA; HSP70 EXPRESSION; THERMAL-STRESS; BALLAST WATER; ALGAL BLOOMS; CHAPERONIN	Heat shock protein 60 (Hsp60) and Hsp10 are two chaperones important to both stress responses and cellular metabolisms in most organisms. In this study, the cosmopolitan Scrippsiella trochoidea was used as a model of HAB-forming dinoflagellates to explore the possible functional roles of Hsp60 and Hsp10 in the adaptation of dinoflagellates to temperature stress and life cycle transition. The full-length cDNAs of a Hsp60 and a Hsp10 gene from S. trochoidea (StHsp60 and StHsp10) were obtained via rapid amplification of cDNA ends (RACE) and their deduced amino acid sequences both included family-characteristic conservative structures and motifs, indicating a conserved function for both among different taxa. Real-time qPCR revealed that StHsp60 and StHsp10 exhibited highly similar mRNA accumulation patterns in response to temperature stresses. Their mRNA amounts, compared to that at 20 degrees C (control), were rapidly up-regulated upon exposure to both lower (15 degrees C, 10 degrees C, 5 degrees C) and higher (25 degrees C, 30 degrees C) temperatures and showed a clear time-dependent manner, suggesting a possible involvement of StHsp60 and StHsp10 in the urgent adaptation of S. trochoidea to drastic temperature stress. Furthermore, significantly elevated mRNA levels of both genes were detected in resting cysts (newly formed and that maintained in dormancy for different durations) relative to that in vegetative cells, suggesting that higher levels of StHsp60 and StHsp10 are demanded by S. trochoidea resting cysts. The results of this work, as the first investigation to characterize Hsp60 and Hsp10 genes from dinoflagellates, enrich the knowledge about Hsps and lay an important foundation for further probing their functions in dinoflagellate resting cysts.	[Deng, Yunyan; Hu, Zhangxi; Chai, Zhaoyang; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Deng, Yunyan; Hu, Zhangxi; Tang, Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Deng, Yunyan; Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences	Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China.; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023; Chai, Zhaoyang/F-7485-2017	Deng, Yunyan/0000-0001-5967-3611	National Science Foundation of China [41476142, 41506143, 61533011, U1301235]; NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences [U1606404]; Creative Team Project of the Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology [LMEES-CTSP-2018-1]	National Science Foundation of China(National Natural Science Foundation of China (NSFC)); NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences; Creative Team Project of the Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology	The authors acknowledge financial support from the National Science Foundation of China (Grant No. 41606126), the NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences (Grant No. U1606404), National Science Foundation of China (Grant Nos. 41476142, 41506143, 61533011, and U1301235), and Creative Team Project of the Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology (Grant No. LMEES-CTSP-2018-1).	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Biol.	JAN	2019	166	1							7	10.1007/s00227-018-3455-3	http://dx.doi.org/10.1007/s00227-018-3455-3			14	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	HE1PU					2025-03-11	WOS:000453045700001
J	Shin, HH; Li, Z; Lim, D; Lee, KW; Seo, MH; Lim, WA				Shin, Hyeon Ho; Li, Zhun; Lim, Dhongil; Lee, Kyun-Woo; Seo, Min Ho; Lim, Weol Ae			Seasonal production of dinoflagellate cysts in relation to environmental characteristics ih jiiihae-Masan Bay, Korea: One-year sedimerit trap observation	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Scrippsiella; Spiniferites; Alexandrium; Phytoplankton; Summer; Late autumn	SCRIPPSIELLA-TROCHOIDEA CYSTS; ALEXANDRIUM-FUNDYENSE; POPULATION-DYNAMICS; JINHAE BAY; EUTROPHICATION; DINOPHYCEAE; INDICATORS; GROWTH; VIABILITY; COMMUNITY	To investigate dinoflagellate cyst production and seasonality in relation to major environmental factors, such as water temperature, salinity, chlorophyll-a (chl-a) and dissolved nutrients, and to propose dinoflagellate cysts as possible biological indicators for the reconstruction of past environmental conditions, a sediment trap study was conducted for one year, from March 2011 to February 2012, in Jinhae-Masan Bay, Korea. Marked increases in dinoflagellate cyst production were documented in Jinhae-Masna Bay during two distinct seasons (summer and late autumn) characterized by different environmental conditions. Summer (July and August) was characterized by relatively high water temperature, dissolved inorganic nitrogen (DIN), and chl-a concentrations and low salinity, whereas late autumn (November and December) exhibited high dissolved inorganic phosphorus, low water temperature and high salinity, compared to those of the summer. Fourteen dinoflagellate cyst taxa were identified. These assemblages were dominated by Brigantedinium species (round brown cyst), cysts of Scrippsiella species, Spiniferites species and cysts of Alexandrium species (ellipsoidal cyst). The total flux of dinoflagellate cysts ranged from 781 cysts m(-2) day(-1) to 5602 cysts m(-2) day(-1), and the production of autotrophic dinoflagellate cysts was mainly restricted to the wannest months (July-September) and autumn. Multivariable analysis revealed that the production of major dinoflagellate cysts, excluding those of Brigantediniunt species, can be enhanced by environmental conditions during summer in Jinhae-Masan Bay. In particular, the increased production of cysts of Scrippsiella species was related to increased water temperature, and the increased production of Spiniferites species was associated with lower salinity. Two peaks in cyst production of Alexandrium species in August and November corresponded with significant increases in DIN and DIP; however, no significant relationship was found between the production of Brigantedinizun species and environmental factors in Jinhae-Masan Bay. These results suggest that the cysts of Scrippsiella species, Spiniferites species and cysts of Alexandrium species present in sediment samples from Jinhae-Masan Bay can be used as biological indicators to reconstruct past environmental conditions involving relatively high water temperature, low salinity and enhanced nutrient level.	[Shin, Hyeon Ho; Li, Zhun; Lim, Dhongil] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea; [Lee, Kyun-Woo] Korea Inst Ocean Sci & Technol, Marine Ecosyst & Biol Res Ctr, Ansan 425600, South Korea; [Seo, Min Ho] Marine Ecol Res Ctr, Yeosu 59697, South Korea; [Lim, Weol Ae] Natl Inst Fisheries Sci, Busan 619705, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); National Institute of Fisheries Science	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea.	shh961121@kiost.ac.kr	LI, ZHUN/GLT-3478-2022; Lim, Dhongil/ACH-3964-2022	Shin, Hyeon Ho/0000-0002-9711-6717; Lim, Dhongil/0000-0002-0832-2907; LI, ZHUN/0000-0001-8961-9966	Marine Biotechnology Program - Ministry of Ocean and Fisheries of the Korean government; NIFS; KIOST [PE99623]	Marine Biotechnology Program - Ministry of Ocean and Fisheries of the Korean government; NIFS(National Institutes of Natural Sciences (NINS) - JapanNational Institute for Fusion Science (NIFS) - Japan); KIOST	This work was supported by grants from the Marine Biotechnology Program funded by the Ministry of Ocean and Fisheries of the Korean government, and by NIFS and KIOST projects (PE99623).	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Coast. Shelf Sci.	DEC 31	2018	215						83	93		10.1016/j.ecss.2018.09.031	http://dx.doi.org/10.1016/j.ecss.2018.09.031			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	HE0FV					2025-03-11	WOS:000452943100009
J	Mertens, KN; Van Nieuwenhove, N; Gurdebeke, PR; Aydin, H; Bogus, K; Bringué, M; Dale, B; De Schepper, S; de Vernal, A; Ellegaard, M; Grothe, A; Gu, HF; Head, MJ; Heikkilä, M; Limoges, A; Londeix, L; Louwye, S; Marret, F; Masure, E; Matsuoka, K; Mudie, PJ; Penaud, A; Pospelova, V; Price, AM; Ribeiro, S; Rochon, A; Sangiorgi, F; Schreck, M; Torres, V; Uzar, S; Versteegh, GJM; Warny, S; Zonneveld, K				Mertens, Kenneth Neil; Van Nieuwenhove, Nicolas; Gurdebeke, Pieter R.; Aydin, Hilal; Bogus, Kara; Bringue, Manuel; Dale, Barrie; De Schepper, Stijn; de Vernal, Anne; Ellegaard, Marianne; Grothe, Arjen; Gu, Haifeng; Head, Martin J.; Heikkila, Maija; Limoges, Audrey; Londeix, Laurent; Louwye, Stephen; Marret, Fabienne; Masure, Edwige; Matsuoka, Kazumi; Mudie, Peta J.; Penaud, Aurelie; Pospelova, Vera; Price, Andrea Michelle; Ribeiro, Sofia; Rochon, Andre; Sangiorgi, Francesca; Schreck, Michael; Torres, Vladimir; Uzar, Serdar; Versteegh, Gerard J. M.; Warny, Sophie; Zonneveld, Karin			The dinoflagellate cyst genera <i>Achomosphaera</i> Evitt 1963 and <i>Spiniferites</i> Mantell 1850 in Pliocene to modern sediments: a summary of round table discussions	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Spiniferites; Achomosphaera; Hafniasphaera; Rottnestia; Pterocysta	EEMIAN HYDROGRAPHIC CONDITIONS; LATE QUATERNARY; CENOZOIC DINOFLAGELLATE; NORTHERN BELGIUM; BALTIC SEA; SP-NOV; DINOPHYCEAE; ASSEMBLAGES; MORPHOLOGY; PROPOSALS	We present a summary of two round-table discussions held during two subsequent workshops in Montreal (Canada) on 16 April 2014 and Ostend (Belgium) on 8 July 2015. Five species of the genus Achomosphaera Evitt 1963 and 33 of the genus Spiniferites Mantell 1850 emend. Sarjeant 1970 occuring in Pliocene to modern sediments are listed and briefly described along with remarks made by workshop participants. In addition, several holotypes and topotypes are reillustrated. Three species previously assigned to Spiniferites are here considered/accepted as belonging to other genera: Impagidinium inaequalis (Wall and Dale in Wall et al. 1973) Londeix et al. 2009, Spiniferites? rubinus (Rossignol 1962 ex Rossignol 1964) Sarjeant 1970, and Thalassiphora balcanica Baltes & 1971. This summary forms the basis for a set of papers that follows, where points raised during the workshops are explored in greater detail.	[Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Concarneau, France; [Van Nieuwenhove, Nicolas] Aarhus Univ, Dept Geosci, Aarhus, Denmark; [Gurdebeke, Pieter R.; Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium; [Aydin, Hilal; Uzar, Serdar] Celal Bayar Univ, Dept Biol, Fac Sci & Arts, Manisa, Turkey; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX USA; [Bringue, Manuel] Univ South Carolina, Sch Earth Ocean & Environm, Columbia, SC USA; [Bringue, Manuel; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC, Canada; [Dale, Barrie] Univ Oslo, Dept Geosci, Oslo, Norway; [De Schepper, Stijn] Bjerknes Ctr Climate Res, Uni Res Climate, Bergen, Norway; [de Vernal, Anne] Univ Quebec Montreal, Dept Sci Terre & Atmosphere, Montreal, PQ, Canada; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg C, Denmark; [Grothe, Arjen; Sangiorgi, Francesca] Univ Utrecht, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol, Dept Earth Sci,Fac Geosci, Utrecht, Netherlands; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen, Peoples R China; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON, Canada; [Heikkila, Maija] Univ Helsinki, Dept Environm Sci, Environm Change Res Unit, Helsinki, Finland; [Van Nieuwenhove, Nicolas; Limoges, Audrey; Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Copenhagen, Denmark; [Londeix, Laurent] Univ Bordeaux, UMR 5805 EPOC, Pessac, France; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool, Merseyside, England; [Masure, Edwige] UPMC, MNHN, CR2P, CNRS,UMR7207, Paris, France; [Matsuoka, Kazumi] Inst East China Sea Res ECSER, Nagasaki, Japan; [Mudie, Peta J.] Geol Survey Canada, Dartmouth, NS, Canada; [Penaud, Aurelie] IUEM UBO, UMR6538 Domaines Ocean, Plouzane, France; [Price, Andrea Michelle] McGill Univ, Dept Geog, Montreal, PQ, Canada; [Rochon, Andre] ISMER UQAR, 310 Allee Ursulines, Rimouski, PQ, Canada; [Schreck, Michael] Univ Tromso Arctic Univ, Dept Geol, Tromso, Langnes, Norway; [Torres, Vladimir] ExxonMobil Explorat Co, Biostratig Core Grp, Spring, TX USA; [Versteegh, Gerard J. M.] Helmholtz Zentrum Polar & Meeresforsch, Dept Marine Geochem, AWI, Bremerhaven, Germany; [Versteegh, Gerard J. M.; Zonneveld, Karin] Bremen Univ, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA; [Van Nieuwenhove, Nicolas; Limoges, Audrey] Univ New Brunswick, Dept Earth Sci, Fredericton, NB, Canada	Ifremer; Aarhus University; Ghent University; Celal Bayar University; Texas A&M University System; Texas A&M University College Station; University of South Carolina System; University of South Carolina Columbia; University of Victoria; University of Oslo; Bjerknes Centre for Climate Research; University of Quebec; University of Quebec Montreal; University of Copenhagen; Utrecht University; Third Institute of Oceanography, Ministry of Natural Resources; Brock University; University of Helsinki; Geological Survey Of Denmark & Greenland; Universite de Bordeaux; University of Liverpool; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Universite de Bretagne Occidentale; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Quebec; Universite du Quebec a Rimouski; UiT The Arctic University of Tromso; Exxon Mobil Corporation; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Bremen; Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University; University of New Brunswick	Mertens, KN (通讯作者)，IFREMER, LER BO, Stn Biol Marine, Concarneau, France.	kenneth.mertens@ifremer.fr	Mertens, Kenneth/AAO-9566-2020; Warny, Sophie/A-8226-2013; Uzar, Serdar/G-9956-2014; Ribeiro, Sofia/AAZ-2782-2021; Van Nieuwenhove, Nicolas/IAQ-1532-2023; Bringue, Manuel/KIH-8224-2024; Ellegaard, Marianne/H-6748-2014; de Vernal, Anne/D-5602-2013; Gurdebeke, Pieter/AAY-7059-2020; Louwye, Stephen/D-3856-2012; De Schepper, Stijn/A-2836-2011; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015; Heikkila, Maija/N-7659-2013; Penaud, Aurelie/F-2485-2011; Versteegh, Gerard J.M./H-2119-2011; Ribeiro, Sofia/G-9213-2018	Bringue, Manuel/0000-0003-4460-8344; Louwye, Stephen/0000-0003-4814-4313; Limoges, Audrey/0000-0002-4587-3417; De Schepper, Stijn/0000-0002-6934-0914; Gu, Haifeng/0000-0002-2350-9171; Mertens, Kenneth/0000-0003-2005-9483; Marret-Davies, Fabienne/0000-0003-4244-0437; Heikkila, Maija/0000-0003-3885-8670; Penaud, Aurelie/0000-0003-3578-4549; Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Bogus, Kara/0000-0003-4690-0576; Gurdebeke, Pieter R./0000-0003-1425-8515; Sangiorgi, Francesca/0000-0003-4233-6154; Versteegh, Gerard J.M./0000-0002-9320-3776; Pospelova, Vera/0000-0003-4049-8133; Ribeiro, Sofia/0000-0003-0672-9161; Warny, Sophie/0000-0002-3451-040X				[Anonymous], 1993, SPEC PUBL NUMBER; 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J	Londeix, L; Zonneveld, K; Masure, E				Londeix, Laurent; Zonneveld, Karin; Masure, Edwige			Taxonomy and operational identification of Quaternary species of <i>Spiniferites</i> and related genera	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Dinoflagellate cysts; Quaternary; Spiniferites complex; Identification key; taxonomy	DINOFLAGELLATE CYST DISTRIBUTION; EEMIAN HYDROGRAPHIC CONDITIONS; ROYAL-SOCIETY BOREHOLE; LAST 2000 YEARS; BLACK-SEA; RECENT SEDIMENTS; CENOZOIC DINOFLAGELLATE; MARINE-SEDIMENTS; SURFACE SEDIMENT; BALTIC SEA	In this article, we are proposing an Identification Key for recognition of Quaternary Spiniferites species and some morphologically close Quaternary taxa of some related genera. We summarize the morphological features of 43 taxa (including three subspecies and one variety) based on the original description of the holotypes and sometimes supplemented by our observations. In addition to the Identification Key, we refer to published illustrations that feature both typical and atypical specimens for each taxon. The compilation of this key gave us the opportunity to reconsider some taxonomic concepts, which resulted in two new combinations and an emendation: Hafniasphaera granulata (Mao 1989) comb. nov., emend. and Hafniasphaera multisphaera (Price and Pospelova 2014) comb. nov. In addition, we recommend that the names Spiniferites nodosus and Spiniferites pseudofurcatus subsp. obliquus be restricted to their holotype.	[Londeix, Laurent] Univ Bordeaux, UMR 5805 EPOC, CS50023,Allee Geoffroy St Hillaire, F-33615 Pessac, France; [Zonneveld, Karin] Univ Bremen, Bremen, Germany; [Masure, Edwige] Univ Pierre & Marie Curie Paris6, UMR CNRS 5143, Paris, France	Universite de Bordeaux; University of Bremen; Sorbonne Universite	Londeix, L (通讯作者)，Univ Bordeaux, UMR 5805 EPOC, CS50023,Allee Geoffroy St Hillaire, F-33615 Pessac, France.	laurent.londeix@u-bordeaux.fr						[Anonymous], 9210 GEOL SURV CAN; [Anonymous], [No title captured]; [Anonymous], 1977, CONTRIBUTIONS STRATI; [Anonymous], P YORKSHIRE GEOL SOC; [Anonymous], 1985, AM ASS STRATIGRAPHIC; Attaran-Fariman Gilan, 2012, Algological Studies, V140, P51, DOI 10.1127/1864-1318/2012/0048; Biebow N., 1996, 57 GEOM; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; Bujak J., 1986, AASP Contributions Series, P7; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Davey R.J., 1966, STUDIES MESOZOIC CAI, P28; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A, 2018, PALYNOLOGY; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DOWNIE C, 1969, Grana Palynologica, V9, P124; du Chene R.J., 1977, Revista Espanola de Micropaleontologia, V9, P97; DUANE A, 1990, REV PALAEOBOT PALYNO, V63, P1, DOI 10.1016/0034-6667(90)90002-Z; DUCHENE RJ, 1988, B CTR RECHERCHES EXP, V12, P237; Eaton GL, 1996, REV PALAEOBOT PALYNO, V91, P151, DOI 10.1016/0034-6667(95)00073-9; Ehrenberg CG, 1837, ABHANDLUNGEN KONIG P, V1, P109; Eisenack A., 1954, Palaeontographica A, V105, P49; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P158, DOI 10.1073/pnas.49.2.158; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42, P909; Fensome RA., 1991, EISENACK CATALOG FOS, V1; Fensome Robert A., 1995, Eisenack Catalog of Fossil Dinoflagellates New Series, V3, P1463; Gurdebeke PR, 2018, PALYNOLOGY; HABIB D, 1982, MICROPALEONTOLOGY, V28, P335, DOI 10.2307/1485449; Harland R., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P531; HARLAND R, 1986, Palynology, V10, P25; HARLAND R, 1988, NEW PHYTOL, V108, P111, DOI 10.1111/j.1469-8137.1988.tb00210.x; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HARLAND R, 1980, Grana, V19, P211; HARLAND R, 1973, REV PALAEOBOT PALYNO, V16, P229, DOI 10.1016/0034-6667(73)90021-3; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; Harland R, 1978, CONT SHELF I PUBL, V100, P7; He C.Q., 2009, FOSSIL DINOFLAGELLAT; Head MJ, 2007, GEOL MAG, V144, P987, DOI 10.1017/S0016756807003780; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Head MJ, 1999, J PALEONTOL, V73, P1; Head MJ, 2005, QUATERN INT, V130, P3, DOI 10.1016/j.quaint.2004.04.027; Head MJ., 1992, NEOGENE QUATERNARY D; Heikkilä M, 2014, MAR MICROPALEONTOL, V106, P79, DOI 10.1016/j.marmicro.2013.12.002; Kholeif SEA, 2009, PALYNOLOGY, V33, P1, DOI 10.2113/gspalynol.33.1.1; Klumpp B., 1953, Palaeontographica A, V103, P377; Kremp G., 1965, Morphologic Encyclopedia of Palynology; LENTIN J. 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J	Limoges, A; Londeix, L; Mertens, KN; Rochon, A; Pospelova, V; Cuéllar, T; de Vernal, A				Limoges, Audrey; Londeix, Laurent; Mertens, Kenneth Neil; Rochon, Andre; Pospelova, Vera; Cuellar, Tomasa; de Vernal, Anne			Identification key for Pliocene and Quaternary <i>Spiniferites</i> taxa bearing intergonal processes based on observations from estuarine and coastal environments	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Dinoflagellate cyst; taxonomy; description; morphological variability; emendations	CYST-THECA RELATIONSHIP; DINOFLAGELLATE CYST; SPATIAL-DISTRIBUTION; ASSEMBLAGES; MORPHOLOGY; SALINITY; BLACK	The use of dinoflagellate cyst assemblages as a tool for palaeo-environmental reconstructions strongly relies on the robustness of cyst identification and existing information on the distribution of the different species. To this purpose, we propose a functional key for the identification of Pliocene and Quaternary Spiniferites bearing intergonal processes and depict the range of morphological variation of the different species on the basis of new observations from estuarine and coastal regions. Accordingly, the description of Spiniferites mirabilis is emended to include the new subspecies Spiniferites mirabilis subsp. serratus. We also report the occasional presence of intergonal processes in Spiniferites bentorii and Spiniferites belerius. This key aims to facilitate identification of this group of Spiniferites bearing intergonal processes and standardize cyst identification among researchers.	[Limoges, Audrey] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Copenhagen, Denmark; [Limoges, Audrey] Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB E3B 5A3, Canada; [Londeix, Laurent] Univ Bordeaux, UMR 5805 EPOC, CS50023,Allee Geoffroy St Hillaire, Pessac, France; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, Ghent, Belgium; [Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Pl Croix, Concarneau, France; [Rochon, Andre] Univ Quebec Rimouski, Inst Sci Mer ISMER, Rimouski, PQ, Canada; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC, Canada; [Cuellar, Tomasa] Univ Nacl Autonoma Mexico, Posgrad Ciencias Mar & Limnol, Mexico City, DF, Mexico; [de Vernal, Anne] Univ Quebec Montreal, Dept Sci Terre & Atmosphere, Geotop, Montreal, PQ, Canada	Geological Survey Of Denmark & Greenland; University of New Brunswick; Universite de Bordeaux; Ghent University; Ifremer; University of Quebec; Universite du Quebec a Rimouski; University of Victoria; Universidad Nacional Autonoma de Mexico; University of Quebec; University of Quebec Montreal	Limoges, A (通讯作者)，Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB E3B 5A3, Canada.	Audrey.Limoges@unb.ca	de Vernal, Anne/D-5602-2013; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Cuellar Martinez, Tomasa/0000-0002-0460-6275; Limoges, Audrey/0000-0002-4587-3417; Pospelova, Vera/0000-0003-4049-8133; Mertens, Kenneth/0000-0003-2005-9483	Fonds de Recherche du Quebec - Nature et Technologies (FRQNT); Natural Sciences and Engineering Research Council (NSERC) of Canada	Fonds de Recherche du Quebec - Nature et Technologies (FRQNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	Financial support to AL and AdV from the Fonds de Recherche du Quebec - Nature et Technologies (FRQNT) and to AdV, VP and AR from Natural Sciences and Engineering Research Council (NSERC) of Canada are gratefully acknowledged.	Adl SM, 2005, J EUKARYOT MICROBIOL, V52, P399, DOI 10.1111/j.1550-7408.2005.00053.x; [Anonymous], 1993, SPEC PUBL NUMBER; [Anonymous], 1914, BER DTSCH BOT GES, DOI DOI 10.1111/J.1438-8677.1914.TB07573.X; [Anonymous], 1985, AM ASS STRATIGRAPHIC; Bertini A, 1998, MICROPALEONTOLOGY, V44, P413, DOI 10.2307/1486042; Bujak J., 1986, AASP Contributions Series, P7; Butschli O., 1885, ORDNUNGEN THIER REIC, P906; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 1999, CAHIERS GEOTOP, P1; de Vernal A, 2018, PALYNOLOGY, V42, P182, DOI 10.1080/01916122.2018.1465730; de Vernal A, 2013, QUATERNARY SCI REV, V79, P122, DOI 10.1016/j.quascirev.2013.06.022; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; 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; Engel ER, 1992, GEOLOGISCHES JB A, V125, P3; Gurdebeke PR, 2018, PALYNOLOGY, V42, P93, DOI 10.1080/01916122.2018.1465735; Harland R., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P531; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Kedves M, 1999, PLANT CELL BIODEVELO, V11, P19; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Kurita Hiroshi, 2003, Proceedings of the Ocean Drilling Program Scientific Results, V186, P1, DOI 10.2973/odp.proc.sr.186.105.2003; Lentin JK., 1989, American Association of Stratigraphic Palynologists, Contributions Ser, V20, P473; Lewis J, 2001, EUR J PHYCOL, V36, P137, DOI 10.1017/S0967026201003171; Lewis J, 1999, GRANA, V38, P113, DOI 10.1080/00173139908559220; Limoges A, 2015, ESTUAR COAST SHELF S, V167, P549, DOI 10.1016/j.ecss.2015.11.005; Limoges A, 2013, MAR MICROPALEONTOL, V102, P51, DOI 10.1016/j.marmicro.2013.06.002; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; Mantell G.A, 1850, A Pictorial Atlas of Fossil Remains Consisting of Coloured Illustrations Selected from Parkinson's "Organic Remains of a Former World", and Artis's "Antediluvian Phytology; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; Mao Shaozhi, 1993, Palynology, V17, P47; MATSUOKA K, 1983, Palaeontographica Abteilung B Palaeophytologie, V187, P89; McCarthy F. 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G., 1996, SCI RESULTS, V149, P241; Mertens KN, 2009, MAR MICROPALEONTOL, V70, P54, DOI 10.1016/j.marmicro.2008.10.004; Mertens KN, 2018, PALYNOLOGY, V42, P10, DOI 10.1080/01916122.2018.1465739; Mertens KN, 2012, QUATERNARY SCI REV, V39, P45, DOI 10.1016/j.quascirev.2012.01.026; Morzadec-Kerfourn Marie Therese, 2002, Quaternaire, V13, P111; Mudie P.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P587, DOI 10.2973/odp.proc.sr.104.174.1989; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; Pospelova V, 2010, MAR MICROPALEONTOL, V75, P17, DOI 10.1016/j.marmicro.2010.02.003; Price AM, 2014, PALYNOLOGY, V38, P101, DOI 10.1080/01916122.2013.864341; Reid P.C., 1974, Nova Hedwigia, V25, P579; Rochon A., 1999, AM ASS STRATIGR PALY, V35, P146; Rossignol M., 1964, Revue de Micropaleontologie, V7, P83; SARJEANT W A S, 1970, Grana, V10, P74; Song Z.-c., 1985, Cenozoic-Mesozoic Palaeontology and Stratigraphy of East China, V1, P1; SUN X-K, 1992, Acta Micropalaeontologica Sinica, V9, P45; Suzuki Akihiko, 1998, Journal of the Geological Society of Japan, V104, P143; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Van Nieuwenhove N, 2018, PALYNOLOGY, V42, P111, DOI 10.1080/01916122.2018.1465736; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; Williams GL, 1978, AASP CONTRIBUTION SE, V34; Yun H, 2000, J PALEONTOL SOC KOR, V16, P123; Yun H., 1999, J PALEONTOLOGICAL SO, V15, P43; Yun H., 1994, J PALEONTOLOGICAL SO, V10, P99; ZHAO YY, 1994, GEOBIOS-LYON, V27, P261, DOI 10.1016/S0016-6995(94)80172-X; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	59	13	13	0	4	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	DEC 20	2018	42			1	SI		72	88		10.1080/01916122.2018.1465733	http://dx.doi.org/10.1080/01916122.2018.1465733			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	HE5FC		Green Published, Bronze			2025-03-11	WOS:000453398000004
J	Marret, F; Mertens, KN				Marret, Fabienne; Mertens, Kenneth Neil			Additional observations of <i>Spiniferites alaskensis</i> from topotype material	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Gulf of Alaska; chorate; Spiniferites; processes; Eemian; ODP	DINOFLAGELLATE CYSTS	Here we present new observations of Spiniferites alaskensis, a relatively rare species described from the Eemian of the Gulf of Alaska. We show that the species shows a gonyaulacacean tabulation: Po, 4 ', 6 '', 6c,? s, 6 ''', 1p, 1 ''''. The surface is finely granulate to scabrate. The species bears characteristic processes: these are exclusively gonal, membranous, perforated and end distally in platforms with stumpy ends. We provide more detail as how this species compares to closely related species belonging to the genus Spiniferites.	[Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Dept Geog & Planning, Liverpool L69 7ZT, Merseyside, England; [Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Concarneau, France	University of Liverpool; Ifremer	Marret, F (通讯作者)，Univ Liverpool, Sch Environm Sci, Dept Geog & Planning, Liverpool L69 7ZT, Merseyside, England.	f.marret@liverpool.ac.uk	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Marret-Davies, Fabienne/0000-0003-4244-0437; Mertens, Kenneth/0000-0003-2005-9483				Fensome RA, 2004, CONTRIBUTIONS SERIES, V42; Head MJ, 2007, GEOL MAG, V144, P987, DOI 10.1017/S0016756807003780; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Marret F, 2001, CAN J EARTH SCI, V38, P373, DOI 10.1139/e00-092; Reid P.C., 1974, Nova Hedwigia, V25, P579; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5	6	3	3	1	1	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	DEC 20	2018	42			1	SI		89	92		10.1080/01916122.2018.1465734	http://dx.doi.org/10.1080/01916122.2018.1465734			4	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	HE5FC		Bronze			2025-03-11	WOS:000453398000005
J	Gurdebeke, PR; Mertens, KN; Bogus, K; Marret, F; Chomérat, N; Vrielinck, H; Louwye, S				Gurdebeke, Pieter R.; Mertens, Kenneth Neil; Bogus, Kara; Marret, Fabienne; Chomerat, Nicolas; Vrielinck, Henk; Louwye, Stephen			Taxonomic Re-Investigation and Geochemical Characterization of Reid's (1974) Species of <i>Spiniferites</i> from Holotype and Topotype Material	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Dinoflagellate cyst; redescription; taxonomy; geochemistry; cyst wall composition; FTIR; dinosporin	CYST-THECA RELATIONSHIP; DINOFLAGELLATE CYST; MORPHOLOGY; SALINITY; NORTH; SEA; TEMPERATURE; SEDIMENTS	The genus Spiniferites currently encompasses 142 dinoflagellate cyst species. Some Spiniferites species are difficult to identify because of an incomplete or doubtful description, and/or substandard iconography. This study re-describes and re-illustrates the Spiniferites holotypes first described by Reid in 1974. It also discusses topotype material from surface sediments recovered from British estuaries, and attempts to provide further constraints on the classification of species in this genus using the geochemical characterization of their cyst walls. Reid described four new Spiniferites species: Spiniferites belerius, Spiniferites delicatus, Spiniferites elongatus and Spiniferites lazus. New photomicrographs are presented here for the holotypes of Spiniferites delicatus and Spiniferites elongatus, and additional morphological observations based on newly processed topotype material are given. The geochemical characterization of the Spiniferites cyst walls showed overall consistency with a carbohydrate-based dinosporin. However, variability in the dinosporins suggests that, in this genus, the cyst wall composition may be species-specific. Analysis of the characteristic spectral regions for unclassified Spiniferites species showed that, in some cases, it may be possible to constrain the likely species affinity using the cyst wall chemistry. However, in most cases, the morphologically unspeciated cysts did not show sufficient similarity to an identified species' cyst wall chemistry to be more conclusive. This could either reflect an intermediate species that cannot be clearly characterized using morphology or dinosporin composition, or it represents a completely different species. In either case, both the morphological and geochemical evaluations highlight the difficulties in classifying species of this genus unequivocally.	[Gurdebeke, Pieter R.; Mertens, Kenneth Neil; Louwye, Stephen] Univ Ghent, Dept Geol, Krijgslaan 281,S8, B-9000 Ghent, Belgium; [Mertens, Kenneth Neil; Chomerat, Nicolas] IFREMER, LER BO, Stn Biol Marine, Concarneau, France; [Bogus, Kara] Univ Nottingham, Sch Geog, Ctr Environm Geochem, Nottingham, England; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77843 USA; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool, Merseyside, England; [Vrielinck, Henk] Univ Ghent, Dept Solid State Sci, Ghent, Belgium	Ghent University; Ifremer; University of Nottingham; Texas A&M University System; Texas A&M University College Station; University of Liverpool; Ghent University	Gurdebeke, PR (通讯作者)，Univ Ghent, Dept Geol, Krijgslaan 281,S8, B-9000 Ghent, Belgium.	pieter.gurdebeke@ugent.be	Gurdebeke, Pieter/AAY-7059-2020; Mertens, Kenneth/AAO-9566-2020; Vrielinck, Henk/M-8367-2016; Mertens, Kenneth/C-3386-2015; Louwye, Stephen/D-3856-2012	Mertens, Kenneth/0000-0003-2005-9483; Bogus, Kara/0000-0003-4690-0576; Marret-Davies, Fabienne/0000-0003-4244-0437; Chomerat, Nicolas/0000-0001-9691-6344; Gurdebeke, Pieter R./0000-0003-1425-8515; Louwye, Stephen/0000-0003-4814-4313	Hercules Foundation (Flanders) [AUGE/13/16]	Hercules Foundation (Flanders)	C. Wellman and P.C. Reid are thanked for permission to consult the holotype material in the University of Sheffield palaeontology collections. The Hercules Foundation (Flanders) is gratefully acknowledged for financial support (FT-IMAGER project AUGE/13/16).	Adl SM, 2005, J EUKARYOT MICROBIOL, V52, P399, DOI 10.1111/j.1550-7408.2005.00053.x; [Anonymous], 1993, SPEC PUBL NUMBER; [Anonymous], 1914, BER DTSCH BOT GES, DOI DOI 10.1111/J.1438-8677.1914.TB07573.X; Bogus K, 2014, J PHYCOL, V50, P254, DOI 10.1111/jpy.12170; Bogus K, 2012, REV PALAEOBOT PALYNO, V183, P21, DOI 10.1016/j.revpalbo.2012.07.001; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; 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 R.A., 2008, DINOFLAJ2, Version 1; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; Head MJ, 2007, GEOL MAG, V144, P987, DOI 10.1017/S0016756807003780; Kaurakova M., 2001, CARBOHYD POLYM, V44, P291, DOI [10.1016/S0144-8617(00)00245-9, DOI 10.1016/S0144-8617(00)00245-9]; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Lewis J, 2001, EUR J PHYCOL, V36, P137, DOI 10.1017/S0967026201003171; Limoges A, 2018, PALYNOLOGY, V42, P72, DOI 10.1080/01916122.2018.1465733; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; Londeix L, 2018, PALYNOLOGY, V42, P45, DOI 10.1080/01916122.2018.1465740; Mantell G.A., 1854, The Medals of Creation, Or, First Lessons in Geology and the Study of Organic Remains:In Two Vols, V2; Marret F, 2004, HOLOCENE, V14, P689, DOI 10.1191/0959683604hl747rp; Marshall AO, 2015, PALAEONTOLOGY, V58, P201, DOI 10.1111/pala.12144; Mertens KN, 2009, MAR MICROPALEONTOL, V70, P54, DOI 10.1016/j.marmicro.2008.10.004; Mertens KN, 2018, PALYNOLOGY, V42, P10, DOI 10.1080/01916122.2018.1465739; Mertens KN, 2017, PALYNOLOGY, V41, P183, DOI 10.1080/01916122.2016.1147219; Mertens KN, 2015, SYST BIODIVERS, V13, P829, DOI 10.1080/14772000.2015.1078855; Mertens KN, 2015, HARMFUL ALGAE, V41, P1, DOI 10.1016/j.hal.2014.09.010; Pandey KK, 1999, J APPL POLYM SCI, V71, P1969, DOI 10.1002/(SICI)1097-4628(19990321)71:12<1969::AID-APP6>3.0.CO;2-D; Pospelova V, 2010, MAR MICROPALEONTOL, V75, P17, DOI 10.1016/j.marmicro.2010.02.003; Reid P.C., 1974, Nova Hedwigia, V25, P579; Reid P.C., 1972, THESIS U SHEFFIELD; REID PC, 1978, NOVA HEDWIGIA, V29, P429; 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; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Van Nieuwenhove N, 2018, PALYNOLOGY, V42, P111, DOI 10.1080/01916122.2018.1465736; Versteegh GJM, 2007, ORG GEOCHEM, V38, P1643, DOI 10.1016/j.orggeochem.2007.06.007; Versteegh GJM, 2012, ORG GEOCHEM, V43, P92, DOI 10.1016/j.orggeochem.2011.10.007; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL D, 1970, Micropaleontology (New York), V16, P47, DOI 10.2307/1484846; Zonneveld KAF, 2007, REV PALAEOBOT PALYNO, V145, P77, DOI 10.1016/j.revpalbo.2006.09.001	44	21	21	1	8	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	DEC 20	2018	42			1	SI		93	110		10.1080/01916122.2018.1465735	http://dx.doi.org/10.1080/01916122.2018.1465735			18	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	HE5FC		Bronze, Green Published			2025-03-11	WOS:000453398000006
J	Van Nieuwenhove, N; Potvin, É; Heikkilä, M; Pospelova, V; Mertens, KN; Masure, E; Kucharska, M; Yang, EJ; Chomérat, N; Zajaczkowski, M				Van Nieuwenhove, Nicolas; Potvin, Eric; Heikkila, Maija; Pospelova, Vera; Mertens, Kenneth Neil; Masure, Edwige; Kucharska, Malgorzata; Yang, Eun Jin; Chomerat, Nicolas; Zajaczkowski, Marek			Taxonomic revision of <i>Spiniferites elongatus</i> (the resting stage of <i>Gonyaulax elongata</i>) based on morphological and molecular analyses	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Single-cell PCR; Spiniferites ellipsoideus; Spiniferites frigidus; Rottnestia amphicavata; morphologic variability; taxonomy	CYST-THECA RELATIONSHIP; DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; PROCESS LENGTH VARIATION; NORTH-ATLANTIC OCEAN; SP-NOV DINOPHYCEAE; SURFACE SEDIMENTS; SEA; SALINITY; PACIFIC; PERIDINIALES	We restudied the morphological complex comprising the cyst-based species Spiniferites elongatus/Spiniferites frigidus/Rottnestia amphicavata. We reviewed existing studies, and acquired new morphometric measurements of recent cysts from across the Northern Hemisphere, scanning electron microscopy (SEM) observations of cysts from Barents Sea surface sediments, and genetic analyses of cysts from the Beaufort Sea. The measurements suggest that populations and morphospecies cannot be distinguished based on morphometric criteria. Furthermore, sequential sediment trap samples from Hudson Bay reveal that morphological variation can occur at the same location over a few weeks, arguing against a uniform morphological response to environmental parameters. The SEM observations reveal a consistent gonyaulacacean tabulation (Po, 4 ', 6 '', 6c, 5 s, *6 ''', 1p, 1 ''''). The small and large subunit ribosomal RNA genes and the internal transcribed spacer sequences obtained from differing cysts from the Beaufort Sea with morphologies attributable to the complex, including forms that correspond to Rottnestia amphicavata, were all identical and conform to those of Gonyaulax elongata from the Orkney Islands. The molecular analyses thus support the conclusion that the morphological variability is not reflected genetically and occurs within one species. Based on arguments against the generic attribution of amphicavata to Rottnestia, the continuum between the extreme ends of the morphological range, and the molecular data, we suggest Rottnestia amphicavata to be conspecific with Spiniferites frigidus, and both to be junior synonyms of Spiniferites elongatus. The morphometric data further indicate that Spiniferites ellipsoideus, an elongate cyst from the Miocene, can also be considered a junior synonym of Spiniferites elongatus. It is recommended to use two informal types in census work (i.e. Spiniferites elongatus - Beaufort morphotype for morphologies formerly assignable to Spiniferites frigidus/Rottnestia amphicavata, and Spiniferites elongatus - Norwegian morphotype for cysts with strongly reduced processes) to separate specimens at both extreme ends of the morphological spectrum from typical specimens of Spiniferites elongatus.	[Van Nieuwenhove, Nicolas] Geol Survey Denmark & Greenland, Dept Glaciol & Climate, Copenhagen K, Denmark; [Potvin, Eric; Yang, Eun Jin] Aarhus Univ, Dept Geosci, Aarhus, Denmark; [Heikkila, Maija] Korea Polar Res Inst, Div Polar Ocean Environm, Incheon, South Korea; [Pospelova, Vera] Univ Helsinki, Dept Environm Sci, ECRU, Helsinki, Finland; [Mertens, Kenneth Neil; Chomerat, Nicolas] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC, Canada; [Masure, Edwige] IFREMER, LER BO, Stn Biol Marine, Pl Croix, Concarneau, France; [Van Nieuwenhove, Nicolas; Heikkila, Maija] Univ Pierre & Marie Curie Paris, UMR CNRS, Paris, France; [Kucharska, Malgorzata; Zajaczkowski, Marek] Polish Acad Sci, Inst Oceanol, Dept Marine Ecol, Sopot, Poland	Geological Survey Of Denmark & Greenland; Aarhus University; Korea Polar Research Institute (KOPRI); University of Helsinki; University of Victoria; Ifremer; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences	Van Nieuwenhove, N (通讯作者)，Univ New Brunswick, Dept Earth Sci, Fredericton, NB E3B 5A3, Canada.	nicolas.vannieuwenhove@unb.ca	Mertens, Kenneth/AAO-9566-2020; Van Nieuwenhove, Nicolas/IAQ-1532-2023; Mertens, Kenneth/C-3386-2015; Heikkila, Maija/N-7659-2013	Zajaczkowski, Marek/0000-0002-3823-7359; Mertens, Kenneth/0000-0003-2005-9483; Chomerat, Nicolas/0000-0001-9691-6344; Yang, Eun Jin/0000-0002-8639-5968; Kucharska, Malgorzata/0000-0001-9862-2753; Pospelova, Vera/0000-0003-4049-8133; Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Heikkila, Maija/0000-0003-3885-8670	Danish Council for Independent Research, Natural Science [12-126709/FNU]; K-PORT [Korea-Polar Ocean in Rapid Transition, KOPRI] project - Ministry of Oceans and Fisheries of Korea [PM15040]; K-POD [Korea-Polar Ocean Development, KOPRI] project - Ministry of Oceans and Fisheries of Korea [PM15050]; Natural Sciences and Engineering Research Council of Canada (NSERC); Academy of Finland [252512]; Villlum Foundation, Denmark [VKR 023454]; Academy of Finland (AKA) [252512] Funding Source: Academy of Finland (AKA)	Danish Council for Independent Research, Natural Science(Det Frie Forskningsrad (DFF)); K-PORT [Korea-Polar Ocean in Rapid Transition, KOPRI] project - Ministry of Oceans and Fisheries of Korea(Korea Polar Research Institute of Marine Research Placement (KOPRI)); K-POD [Korea-Polar Ocean Development, KOPRI] project - Ministry of Oceans and Fisheries of Korea(Korea Polar Research Institute of Marine Research Placement (KOPRI)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Academy of Finland(Research Council of Finland); Villlum Foundation, Denmark; Academy of Finland (AKA)(Research Council of Finland)	Funding to NVN was provided by the Danish Council for Independent Research, Natural Science [project no. 12-126709/FNU]. The genetic work by EP was supported by the K-PORT [Korea-Polar Ocean in Rapid Transition, KOPRI, PM15040] and K-POD [Korea-Polar Ocean Development, KOPRI, PM15050] projects funded by the Ministry of Oceans and Fisheries of Korea. This research was partially funded by the Natural Sciences and Engineering Research Council of Canada (NSERC) through a Discovery grant to VP. She is the Hanse-Wissenschaftskolleg (HWK) senior research fellow in marine and climate research at the Institute for Advanced Study (Germany). Funding for MH was provided by the Academy of Finland [grant 252512] and the Villlum Foundation, Denmark [VKR 023454].	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J	Mudie, P; Rochon, A; Richards, K; Ferguson, S; Warny, S				Mudie, Peta; Rochon, Andre; Richards, Keith; Ferguson, Shannon; Warny, Sophie			<i>Spiniferites cruciformis</i>, <i>Pterocysta cruciformis</i> and <i>Galeacysta etrusca</i>: morphology and palaeoecology	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Cruciform cyst; chronostratigraphy; palaeosalinity; Paratethys; Ponto-Caspian	LAST 2000 YEARS; DINOFLAGELLATE CYSTS; BLACK-SEA; CENTRAL PARATETHYS; LATE MIOCENE; NORTHERN APENNINES; ATLANTIC COAST; LAGO MARE; SALINITY; HOLOCENE	Miocene to modern sediments of the Ponto-Caspian basins and Mediterranean Sea are uniquely distinguished by presence of gonyaulacacean cysts with ellipsoid to cruciform endocysts and highly variable ectocystal features, including pterate (wing-like) and galeate (helmet-like) outer wall layers. The term cruciform is defined to indicate cysts with concave epicyst and hypocyst surfaces and moderate dorsoventral flattening. These features may be morphological responses to salinity stress and some biometrical studies conclude that the cruciform Ponto-Caspian species Spiniferites cruciformis of Wall and Dale 1973 and Pterocysta cruciformis Rochon et al. 2003 are morphotypes of the ellipsoidal-subpentagonal Miocene-Holocene species Galeacysta etrusca Corradini and Biffi 1988. We show that the holotypes of these cruciform and rhomboid-subpentagonal galeate taxa differ in endocyst shape, ectocyst structure and attachment points, process morphology, and sulcal plate expression, and we present new data on morphological variations, modern distribution and ecology. We list multiple criteria for distinguishing these taxa from Paratethyan dinoflagellates with shared features, including Thalassiphora spp., Lophocysta, Romanodinium, and Seriliodinium. Log transforms of endocyst:ectocyst (EN:EC) dimensions cannot fully capture cruciformness or galeate and pterate wall characteristics that distinguish the genera, and at DSDP Site 380, EN:EC values for Pleistocene populations of Spiniferites cruciformis and Galeacysta etrusca are significantly different. Re-examination of the history of studies on the Galeacysta etrusca complex and comparison with new studies of Pleistocene to recent cysts leads to the conclusion there is insufficient evidence to justify combining the cruciform species with Galeacysta etrusca and we provide criteria for distinguishing among the main components of the complex. Using multiple morphological features, it appears there is a replacement of large Palaeogene marine-brackish water camocavate-circumcavate taxa with elliptical endocysts first by the Miocene rhombo-subpentagonal galeate species Galeacysta etrusca and then by the Pliocene - Holocene semi-marine-brackish cruciform species Spiniferites cruciformis and stenohaline Pterocysta cruciformis.	[Mudie, Peta] Geol Survey Canada Atlantic, Dartmouth, NS, Canada; [Rochon, Andre] Univ Quebec Rimouski, ISMER, Rimouski, PQ, Canada; [Richards, Keith] KrA Stratig Ltd, Conwy, Wales; [Richards, Keith] Univ Amsterdam, IBED, Amsterdam, Netherlands; [Ferguson, Shannon; Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Ferguson, Shannon; Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Quebec; Universite du Quebec a Rimouski; University of Amsterdam; Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University	Mudie, P (通讯作者)，Geol Survey Canada Atlantic, Dartmouth, NS, Canada.	mudiep@ns.sympatico.ca	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X	Louisiana State University Museum of Natural Science; NSERC Discovery Grant Program [05609, 206522]; LSU Department of Geology and Geophysics	Louisiana State University Museum of Natural Science; NSERC Discovery Grant Program(Natural Sciences and Engineering Research Council of Canada (NSERC)); LSU Department of Geology and Geophysics	Shannon Ferguson's MSc thesis was funded by the Louisiana State University Museum of Natural Science and by the LSU Department of Geology and Geophysics. AR research is funded by NSERC Discovery Grant Program no. 05609; much of PM research was supported by NSERC Discovery Grant Program no. 206522 awarded while Adjunct Professor at MUN. This is ESS Contribution no. 20160016 of NRCan.	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J	Pospelova, V; Zonneveld, KAF; Heikkilä, M; Bringue, M; Price, AM; Esenkulova, S; Matsuoka, K				Pospelova, Vera; Zonneveld, Karin A. F.; Heikkila, Maija; Bringue, Manuel; Price, Andrea M.; Esenkulova, Svetlana; Matsuoka, Kazumi			Seasonal, annual, and inter-annual <i>Spiniferites</i> cyst production: a review of sediment trap studies	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Gonyaulax ecology; Omura Bay; Cape Blanc; Arabian Sea; Salish Sea; Santa Barbara Basin; Hudson Bay	WALLED DINOFLAGELLATE CYSTS; RECENT MARINE-SEDIMENTS; SEA-SURFACE CONDITIONS; SANTA-BARBARA BASIN; PALYNOLOGICAL EVIDENCE; CAPE-BLANC; NORTHERN-HEMISPHERE; ABSOLUTE ABUNDANCE; UPWELLING SYSTEM; ORGANIC-CARBON	Despite the fact that dinoflagellate cysts of the diverse genus Spiniferites are abundant in coastal and estuarine sediments worldwide, little is known about patterns of their seasonal or annual production. In this paper we review previously published data on Spiniferites cyst fluxes from eight sediment trap time series in estuarine (the Strait of Georgia, Saanich Inlet, Hudson Bay, Omura Bay), coastal (the Santa Barbara Basin, the Arabian Sea), and offshore (off Cape Blanc) environments. This is the first study that provides detailed inter-site comparison of dinoflagellate cysts in sediment traps and analyzes seasonal, annual, and inter-annual cyst production from different geographic regions. We identified that cyst fluxes of all Spiniferites species at a given location increased or decreased simultaneously in all studied sediment trap records. This indicates that different Spiniferites species react in a similar way to local environmental triggers at each site. Average daily total cyst fluxes recorded in the sediment trap time series and in the dated surface sediment samples are greater in coastal and estuarine waters where marine primary productivity is higher. This implies that nutrient availability might be an important factor stimulating Spiniferites production. There is no uniform seasonal pattern in Spiniferites fluxes, but the timing of elevated total Spiniferites fluxes coincided with intervals of local seasonal environmental change at each site. Analyses of all sediment traps revealed that intervals with the highest total Spiniferites fluxes correspond to the timing and intensity of local environmental change at the sea-surface when waters had: minimal turbidity, some water column stability or stratification, availability of nutrients, and sea-ice free conditions. The multi-year trap data record considerable inter-annual variability in Spiniferites fluxes and seasonality when environmental conditions between the years varied. A combination of factors and specific environmental conditions are required to enhance Spiniferites cyst production in each region.	[Pospelova, Vera; Bringue, Manuel] Univ Victoria, Sch Earth & Ocean Sci, POB 3065 STN CSC, Victoria, BC V8W 3V6, Canada; [Zonneveld, Karin A. F.] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Heikkila, Maija] Univ Helsinki, Dept Environm Sci, Helsinki, Finland; [Heikkila, Maija] Geol Survey Denmark & Greenland, Dept Glaciol & Climate, Copenhagen, Denmark; [Bringue, Manuel] Univ South Carolina, Dept Earth & Ocean Sci, Columbia, SC USA; [Price, Andrea M.] McGill Univ, Dept Geog, Montreal, PQ, Canada; [Esenkulova, Svetlana] Pacific Salmon Fdn, Vancouver, BC, Canada; [Matsuoka, Kazumi] Inst East China Sea Res ECSER, Nagasaki, Japan	University of Victoria; University of Bremen; University of Helsinki; Geological Survey Of Denmark & Greenland; University of South Carolina System; University of South Carolina Columbia	Pospelova, V (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, POB 3065 STN CSC, Victoria, BC V8W 3V6, Canada.	vpospe@uvic.ca	Bringue, Manuel/KIH-8224-2024; Heikkila, Maija/N-7659-2013	Pospelova, Vera/0000-0003-4049-8133; Heikkila, Maija/0000-0003-3885-8670; Esenkulova, Svetlana/0000-0003-3611-1944; Bringue, Manuel/0000-0003-4460-8344	Natural Sciences and Engineering Research Council of Canada (NSERC) [RGPIN/6388-2015]; NSERC; Academy of Finland [252512]; Villum Foundation (Denmark); Academy of Finland (AKA) [252512] Funding Source: Academy of Finland (AKA)	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Academy of Finland(Research Council of Finland); Villum Foundation (Denmark)(Villum Fonden); Academy of Finland (AKA)(Research Council of Finland)	This research was funded by the Natural Sciences and Engineering Research Council of Canada (NSERC) through a Discovery grant (RGPIN/6388-2015) to V. Pospelova. She is the Hanse-Wissenschaftskolleg (HWK) senior research fellow in marine and climate research at the Institute for Advanced Study (Germany). A. Price and M. Bringue were supported by NSERC graduate and postdoctoral fellowships. M. Heikkilea received funding from the Academy of Finland (grant 252512) and from the Villum Foundation (Denmark).	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J	de Vernal, A; Eynaud, F; Henry, M; Limoges, A; Londeix, L; Matthiessen, J; Marret, F; Pospelova, V; Radi, T; Rochon, A; Van Nieuwenhove, N; Zaragosi, S				de Vernal, Anne; Eynaud, Frederique; Henry, Maryse; Limoges, Audrey; Londeix, Laurent; Matthiessen, Jens; Marret, Fabienne; Pospelova, Vera; Radi, Taoufik; Rochon, Andre; Van Nieuwenhove, Nicolas; Zaragosi, Sebastien			Distribution and (palaeo)ecological affinities of the main <i>spiniferites</i> taxa in the mid-high latitudes of the Northern Hemisphere	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Dinocysts; Quaternary; palaeoceanography; temperature; salinity; sea-ice; productivity	SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYST DISTRIBUTION; HYDROGRAPHIC CONDITIONS; MARINE-SEDIMENTS; LATE PLEISTOCENE; LATE QUATERNARY; FRESH-WATER; ICE COVER; HOLOCENE; GULF	In marine sediments of late Cenozoic age, Spiniferites is a very common genus of dinoflagellate cysts (dinocysts). Despite some taxonomical ambiguities due to large range of morphological variations within given species and convergent morphologies between different species, the establishment of an operational taxonomy permitted to develop a standardized modern database of dinocysts for the mid-high latitudes of the Northern Hemisphere. In the database that includes 1490 surface sediment samples, Spiniferites mirabilis-hyperacanthus, Spiniferites ramosus and Spiniferites elongatus were counted in addition to Spiniferites belerius, Spiniferites bentorii, Spiniferites bulloideus, Spiniferites delicatus, Spiniferites lazus and Spiniferites membranaceus. Among these taxa, Spiniferites mirabilis-hyperacanthus, Spiniferites ramosus, and Spiniferites elongatus are easy to identify and are particularly common. Spiniferites bentorii and Spiniferites delicatus also are morphologically distinct and occur in relatively high percentages in many samples. Spiniferites lazus and Spiniferites membranaceus also bear distinctive features, but occur only in a few samples. The identification of other taxa (Spiniferites belerius, Spiniferites bulloideus, notably) may be equivocal and their reported distribution has to be used with caution. The spatial distribution of Spiniferites species, with emphasis on the five most common taxa, is documented here with reference to hydrography (salinity and temperature in winter and summer, sea ice cover), primary productivity and geographical setting (bathymetry, distance to the coastline). The results demonstrate distinct ecological affinities for Spiniferites elongatus, which has an Arctic-subarctic distribution and appears abundant in low productivity environments characterized by winter sea ice and large temperature contrast between winter and summer. Spiniferites mirabilis-hyperacanthus, which occurs in warm temperate water sites, is more abundant in high salinity environments. It shares its environmental domain with Spiniferites bentorii, which appears to have a narrower distribution towards the warm and high salinity end of the Spiniferites mirabilis-hyperacanthus distribution. In contrast, Spiniferites delicatus, which occurs in warm-temperate to tropical environments, shows preference for relatively low salinity and low seasonal contrasts of temperature. Spiniferites ramosus exhibits a particularly wide distribution that overlaps both cold and warm Spiniferites taxa. Its cosmopolitan occurrence and its long-ranging biostratigraphical distribution suggest a high plasticity of the species and/or co-occurrence of several cryptic species. Hence, whereas Spiniferites elongatus and Spiniferites mirabilis-hyperacanthus are useful palaeoecological indicators despite their large morphological variability, Spiniferites ramosus is a taxon with an unconstrained ecological significance.	[de Vernal, Anne; Henry, Maryse; Radi, Taoufik] Geotop Univ Quebec Montreal, Montreal, PQ, Canada; [Eynaud, Frederique; Londeix, Laurent; Zaragosi, Sebastien] Univ Bordeaux, UMR 5805 EPOC, Pessac, France; [Limoges, Audrey; Van Nieuwenhove, Nicolas] Geol Survey Denmark & Greenland GEUS, Copenhagen, Denmark; [Matthiessen, Jens] Alfred Wegener Inst, Bremerhaven, Germany; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool, Merseyside, England; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC, Canada; [Rochon, Andre] Univ Quebec Rimouski, Inst Sci Mer Rimouski ISMER, Rimouski, PQ, Canada; [Van Nieuwenhove, Nicolas] Aarhus Univ, Dept Geosci, Aarhus, Denmark; [Limoges, Audrey; Van Nieuwenhove, Nicolas] Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB E3B 5A3, Canada	Universite de Bordeaux; Geological Survey Of Denmark & Greenland; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Liverpool; University of Victoria; University of Quebec; Universite du Quebec a Rimouski; Aarhus University; University of New Brunswick	de Vernal, A (通讯作者)，Geotop Univ Quebec Montreal, Montreal, PQ, Canada.	devernal.anne@uqam.ca	ZARAGOSI, Sébastien/JXL-2488-2024; Van Nieuwenhove, Nicolas/IAQ-1532-2023; de Vernal, Anne/D-5602-2013	Pospelova, Vera/0000-0003-4049-8133; Zaragosi, Sebastien/0000-0002-1456-8129; Marret-Davies, Fabienne/0000-0003-4244-0437; Matthiessen, Jens/0000-0002-6952-2494; Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Limoges, Audrey/0000-0002-4587-3417	Natural Sciences and Engineering Council (NSERC) of Canada; Fonds de recherche du Quebec - Nature et technologies (FRQNT)	Natural Sciences and Engineering Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds de recherche du Quebec - Nature et technologies (FRQNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	We are grateful to the anonymous reviewer of the journal and to Karin Zonneveld who made a thorough examination of the original manuscript and provided useful comments. This study is a contribution supported by research funds from the Natural Sciences and Engineering Council (NSERC) of Canada and the Fonds de recherche du Quebec - Nature et technologies (FRQNT).	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J	Londeix, L				Londeix, Laurent			Quantitative biostratigraphical ranges of some late Cenozoic species of the dinoflagellate genus <i>Spiniferites</i> and taxonomic considerations	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Biostratigraphy; dinoflagellates; Gonyaulax spinifera complex; Neogene; Quaternary; Spiniferites	CRETACEOUS-TERTIARY BOUNDARY; EOCENE-OLIGOCENE TRANSITION; CYST STRATIGRAPHY; HYDROGRAPHIC CONDITIONS; CALCAREOUS NANNOFOSSIL; PALYNOLOGICAL EVIDENCE; DINOCYST STRATIGRAPHY; LATE QUATERNARY; MAGURA NAPPE; PLIOCENE	A new quantitative biostratigraphical method, based on an 'index of stratigraphical abundance' (ISA), has been used to refine the stratigraphical range of 50 dinoflagellate cyst taxa. Most of these correspond to Quaternary representatives of Achomosphaera or Spiniferites. Some extinct taxa are also discussed when their morphology is close to that of recent species (e.g. Spiniferites lenzii, S. twistringiensis and S. pseudofurcatus), as well as some species possibly related to the motile Gonyaulax spinifera complex. The ISAs of S. mirabilis and S. hyperacanthus are similar, as well as for S. elongatus and S. sphaericum. Although initially presumed as indicating morphotypes of a same taxon, it seems rather that the ISAs similarites must be interpreted as an indication of close ecological preferences. The emergence of forms of Spiniferites with low to absent septa appears relatively late (compared to the range of the genus), but the first occurrence of intergonal processes is relatively early, indicating that it is probably a character deeply rooted into the generic genome. The previously calculated phylogeny of some Gonyaulax motile cells shows a different tree pattern than the stratigraphical first appearance succession of their presumed cyst equivalents.	[Londeix, Laurent] Univ Bordeaux, UMR EPOC CNRS 5805, Allee Geoffroy St Hilaire,CS 50023, F-33615 Pessac, France	Universite de Bordeaux	Londeix, L (通讯作者)，Univ Bordeaux, UMR EPOC CNRS 5805, Allee Geoffroy St Hilaire,CS 50023, F-33615 Pessac, France.	laurent.londeix@u-bordeaux.fr						[Anonymous], 9210 GEOL SURV CAN; [Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1996, Palynology: principles and applications; Ashraf A.R., 1979, Palaeontographica Abteilung B Palaeophytologie, V169, P122; ASHRAF A R, 1986, Palaeontographica Abteilung B Palaeophytologie, V200, P111; Auffret J.-P., 1975, Bulletin de la Societe Geologique de France, V17, P641; Below Raimond, 1994, Palaeontographica Abteilung B Palaeophytologie, V232, P59; BERGGREN WA, 1995, SEPM SPECIAL PUBLICA, V54, P130; BRIDEAUX WW, 1977, GEOLOGICAL SURVEY CA, V281; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; Brinkhuis H, 1992, LATE EOCENE EARLY OL; Bujak J., 1986, AASP Contributions Series, P7; Bujak JP, 1973, THESIS; Chen Y., 1978, THESIS; Claparede E, 1857, MEMOIRES I GENEVOIS, V6, P392; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; Costa L.I., 1992, P99; Costa L.I., 1979, DEEP SEA DRILLING PR, V48, P228; Costa L.I., 1988, GEOL JB A, V100, P330; Davey R.J., 1966, STUDIES MESOZOIC CAI, P28; Davey R.J., 1982, GEOL SURV DENMARK, V6, P1; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; De Coninck J, 2001, 20012 GEOL SURV BELG, V294; De Coninck J., 1999, B SOC BELG GEOL, V105, P171; de Klasz I., 1987, CAHIERS MICROPALEONT, V2, P5; De Schepper S, 2009, GEOL MAG, V146, P92, DOI 10.1017/S0016756808005438; de Vernal A, 2018, PALYNOLOGY S, V42; de Vernal A., 1989, Proceedings of the Ocean Drilling Program Scientific results, V105, P401, DOI DOI 10.2973/0DP.PR0C.SR.105.134.1989; DEFLANDRE G, 1938, CR HEBD ACAD SCI, V206, P687; DIESING K.M., 1866, SITZUNGBERICHTE MATH, V52, P287; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; Downie C, 1970, GRANA PALYNOL, V9, P124; du Chene R.E. 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J	Ellegaard, M; Head, MJ; Versteegh, GJM				Ellegaard, Marianne; Head, Martin J.; Versteegh, Gerard J. M.			Linking biological and geological data on dinoflagellates using the genus <i>Spiniferites</i> as an example: the implications of species concepts, taxonomy and dual nomenclature	PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Gonyaulax Diesing 1866	JUL 06-09, 2015	Flanders Marine Inst, Oostend, BELGIUM	Res Unit Palaeontol	Flanders Marine Inst	Morphospecies; phylogenetic species; biological species; evolution; nomenclature; Dinoflagellata; cyst; motile	CYST-THECA RELATIONSHIP; SP-NOV; GONYAULAX-BALTICA; DINOPHYCEAE; DIVERSITY; IMPACTS; FUNGI; SEA	Dinoflagellates encompass two taxonomic systems (dual taxonomy) reflected by separate traditions of nomenclature: one based mainly on living motile stages, and the other mainly on fossil cysts (dual nomenclature). Modern cysts may therefore bear two names if their life cycle is known. There have been attempts to rationalize this duality, but at species and genus level this has been largely unfruitful. New and continuing developments call for a renewed evaluation of this duality: (1) the elucidation of multiple new cyst-motile stage relationships creating overlaps between cyst-based and motile-based systems, and (2) the advent of DNA sequence-based phylogenies, revealing evolutionary patterns (underlying the phenotypic differences) that disagree with trees obtained from the study of fossil cysts. We examine the background of dual nomenclature and discuss the implications of new advances in molecular phylogeny for dual taxonomy as well as briefly review earlier attempts to unite cyst/fossil and motile-/living-based nomenclatures. From this basis, we explore routes for bringing the separate taxonomic systems closer together. Our rationale for doing this lies in the challenges facing communication between the biologists and geologists who work on these different life cycle stages. These challenges encompass taxonomic issues, nomenclature, evolutionary interpretations, and the nature of what we perceive as a species. We use the motile/cyst pair Gonyaulax/Spiniferites as our example, as these, and related genera, provide a useful model for illustrating the difficulties in bridging the gap between biology and palaeontology because they are numerous, with regard to both species and specimens, and are ubiquitous in both time and space.	[Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Thorvaldsensvej 40, DK-1871 Frederiksberg, Denmark; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON, Canada; [Versteegh, Gerard J. M.] Helmholz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Bremerhaven, Germany	University of Copenhagen; Brock University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Ellegaard, M (通讯作者)，Univ Copenhagen, Dept Plant & Environm Sci, Thorvaldsensvej 40, DK-1871 Frederiksberg, Denmark.	me@plen.ku.dk	Versteegh, Gerard J.M./H-2119-2011; Ellegaard, Marianne/H-6748-2014	Versteegh, Gerard J.M./0000-0002-9320-3776; Ellegaard, Marianne/0000-0002-6032-3376; Head, Martin/0000-0003-3026-5483	Natural Sciences and Engineering Research Council of Canada Discovery Grant	Natural Sciences and Engineering Research Council of Canada Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC))	We warmly thank Kenneth Mertens, Willemijn Quaijtaal, Thomas Steeman, Pieter Gurdebeke and Stephen Louwye for organizing the excellent Spiniferites follow-up workshop in Ostend, Belgium in 2015. MJH acknowledges a Natural Sciences and Engineering Research Council of Canada Discovery Grant. We are grateful to Barrie Dale and Rob Fensome for critical and constructive reviews, and to Kenneth Mertens for his patience in editing this special issue.	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J	Mertens, KN; Carbonell-Moore, C				Mertens, Kenneth Neil; Carbonell-Moore, Consuelo			Introduction to <i>Spiniferites</i> Mantell 1850 special issue	PALYNOLOGY			English	Editorial Material						Spiniferites; Achomosphaera; Nematosphaeropsis; Gonyaulax	CYST-THECA RELATIONSHIP; DINOFLAGELLATE CYST; RECENT SEDIMENTS; GONYAULAX-SPINIFERA; SP-NOV; CLASSIFICATION; SEA; DINOPHYCEAE	The first chapter of this special issue introduces the proceedings of two workshops concerning the cyst-based genus Spiniferites Mantell 1850. The historical background of the cyst-based genus Spiniferites, its closely related genera and the theca-based genus Gonyaulax Diesing 1866 is presented here.	[Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France; [Carbonell-Moore, Consuelo] Oregon State Univ, Dept Bot & Plant Pathol, Coll Agr, Corvallis, OR 97331 USA	Ifremer; Oregon State University	Mertens, KN (通讯作者)，IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France.	kenneth.mertens@ifremer.fr	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Mertens, Kenneth/0000-0003-2005-9483				Agelopoulos J., 1964, Neues Jahrbuch fuer Geologie und Palaeontologie Monatshefte, V11, P673; [Anonymous], 1993, SPEC PUBL NUMBER; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], [No title captured]; [Anonymous], 1974, FOSSIL LIVING DINOFL; [Anonymous], 1883, ORGANISMUS INFUSIONS; Balech E, 1977, HIDROBIOLOGIA, V4, P1; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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J	Ruvindy, R; Bolch, CJ; MacKenzie, L; Smith, KF; Murray, SA				Ruvindy, Rendy; Bolch, Christopher J.; MacKenzie, Lincoln; Smith, Kirsty F.; Murray, Shauna A.			qPCR Assays for the Detection and Quantification of Multiple Paralytic Shellfish Toxin-Producing Species of <i>Alexandrium</i>	FRONTIERS IN MICROBIOLOGY			English	Article						paralytic shellfish toxin; Alexandrium; qPCR; ribosomal DNA; Dinoflagellate cysts	REAL-TIME PCR; NEW-SOUTH-WALES; DINOFLAGELLATE GENUS ALEXANDRIUM; HARMFUL ALGAL BLOOMS; OSTENFELDII DINOPHYCEAE; MINUTUM DINOPHYCEAE; MOLECULAR-DETECTION; COASTAL WATERS; GLOBAL CLADE; TAMARENSE	Paralytic shellfish toxin producing dinoflagellates have negatively impacted the shellfish aquaculture industry worldwide, including in Australia and New Zealand. Morphologically identical cryptic species of dinoflagellates that may differ in toxicity, in particular, species of the former Alexandrium tamarense species complex, co-occur in Australia, as they do in multiple regions in Asia and Europe. To understand the dynamics and the ecological drivers of the growth of each species in the field, accurate quantification at the species level is crucial. We have developed the first quantitative polymerase chain reaction (qPCR) primers for A. australiense, and new primers targeting A. ostenfeldii, A. catenella, and A. pacificum. We showed that our new primers for A. pacificum are more specific than previously published primer pairs. These assays can be used to quantify planktonic cells and cysts in the water column and in sediment samples with limits of detection of 2 cells/L for the A. catenella and A. australiense assays, 2 cells/L and 1 cyst/mg sediment for the A. pacificum assay, and 1 cells/L for the A. ostenfeldii assay, and efficiencies of >90%. We utilized these assays to discriminate and quantify co-occurring A. catenella, A. pacificum, and A. australiense in samples from the east coast of Tasmania, Australia.	[Ruvindy, Rendy; Murray, Shauna A.] Univ Technol Sydney, Climate Change Cluster, Sydney, NSW, Australia; [Bolch, Christopher J.] Univ Tasmania, Inst Marine & Antarctic Studies, Launceston, Tas, Australia; [MacKenzie, Lincoln; Smith, Kirsty F.] Cawthron Inst, Nelson, New Zealand	University of Technology Sydney; University of Tasmania; Cawthron Institute	Ruvindy, R; Murray, SA (通讯作者)，Univ Technol Sydney, Climate Change Cluster, Sydney, NSW, Australia.	rendy.ruvindy@uts.edu.au; shauna.murray@uts.edu.au	Bolch, Christopher/J-7619-2014; Murray, Shauna/JAN-6668-2023; Murray, Shauna A/K-5781-2015	Murray, Shauna A/0000-0001-7096-1307	National Science Challenge, Sustainable Seas Innovation Fund [C01X1515, CAWX1801]	National Science Challenge, Sustainable Seas Innovation Fund	The provision of A. pacificum plankton and cyst data from the Marlborough Sounds was made possible through funding from the National Science Challenge, Sustainable Seas Innovation Fund (contract C01X1515) and the Seafood Safety Platform (MBIE contract #CAWX1801).	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Microbiol.	DEC 18	2018	9								3153	10.3389/fmicb.2018.03153	http://dx.doi.org/10.3389/fmicb.2018.03153			12	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	HE7YM	30619217	gold, Green Published			2025-03-11	WOS:000453658000001
J	Richards, K; van Baak, CGC; Athersuch, J; Hoyle, TM; Stoica, M; Austin, WEN; Cage, AG; Wonders, AAH; Marret, F; Pinnington, CA				Richards, Keith; van Baak, Christiaan G. C.; Athersuch, John; Hoyle, Thomas M.; Stoica, Marius; Austin, William E. N.; Cage, Alix G.; Wonders, Antoine A. H.; Marret, Fabienne; Pinnington, Carmel A.			Palynology and micropalaeontology of the Pliocene - Pleistocene transition in outcrop from the western Caspian Sea, Azerbaijan: Potential links with the Mediterranean, Black Sea and the Arctic Ocean?	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Akchagyl; Apsheron; Dinoflagellate cysts; Pollen; Ostracods; Foraminifera	NEOGENE PRODUCTIVE SERIES; CYST-THECA RELATIONSHIP; DINOFLAGELLATE CYSTS; LATE MIOCENE; OSTRACOD ASSEMBLAGES; LATE QUATERNARY; BENTHIC FORAMINIFERA; GONYAULAX-BALTICA; VIENNA BASIN; HOLOCENE	New palynological, ostracod and foraminiferal data are presented from a long outcrop section in the Jeirankechmez river valley, Azerbaijan, near the western coast of the Caspian Sea. The interval studied includes the upper part of the Pliocene Productive Series and overlying Plio-Pleistocene Akchagylian (Akchagyl) and Apsheronian (Apsheron) regional stages. Productive Series sediments were deposited in a closed fluvio-lacustrine basin, isolated from any marine influence. The onset of Akchagyl deposition is marked by a lithological change associated with a significant flooding event that, at its maximum extent, reached the Sea of Azov and into present-day Iran, Kazakhstan, Turkmenistan and Russia. At the Jeirankechmez locality, the lowermost beds of the Akchagyl contain predominantly freshwater assemblages with very minimal marine or brackish content showing that the onset of Akchagyl deposition was not a marine induced event. Reworked Mesozoic palynomorphs occur frequently in this lowermost interval, including the reworked pollen taxa Aqtcdapollenites-Triprojerms that were eroded from the north or north-east. Significant marine influence is evident ca. 30 m above the base of the Akchagyl in the studied outcrop, marked by the 'Cassidulina Beds' which contain a distinct but low diversity assemblage of foraminifera that occurs widely and can be correlated in many parts of the greater Caspian region. Dinoflagellate cysts (dinocysts) in the marine interval include frequent specimens very similar to Algidasphaeridium capillatum (Matsuoka and Bujak), a species only previously recorded from the northern Bering Sea. The combined evidence from these dinocysts and foraminifera suggests that a marine (i.e. seaway) connection existed briefly between the Arctic Ocean and the Caspian Sea at the very end of the Pliocene. Re-examination of core material from the Adriatic Sea shows that Cassidulina reniforme (Norvang) was present in the Mediterranean during and shortly after the Last Glacial Maximum. The possibility that the end Pliocene marine incursion came from the Mediterranean via the Black Sea region to the Caspian Sea cannot be entirely ruled out but is considered unlikely. Biometric analyses are applied to obtain a better understanding of the palaeoenvironmental significance of the assemblages dominated by cassidulinids. An interval > 300 m thick is assigned to the Apsheron regional stage on the basis of predominantly brackish ostracod and dinocyst associations. The dinocysts are of 'Peri-Paratethyan' affinity and closely resemble species first described from Miocene and Pliocene sediments in the Pannonian and Dacic basins of Eastem Europe. Many similarities exist in the microplankton records (dinocysts and acritarchs) between the Caspian Sea, the Black Sea and Central Paratethys.	[Richards, Keith] KrA Stratig Ltd, 116 Albert Dr, Deganwy LL31 9YY, Conwy, Wales; [Richards, Keith] Univ Amsterdam, IBED, Amsterdam, Netherlands; [van Baak, Christiaan G. C.; Hoyle, Thomas M.; Stoica, Marius] Univ Utrecht, Paleomagnet Lab Ft Hoofddijk, Utrecht, Netherlands; [Athersuch, John; Wonders, Antoine A. H.] StrataData Ltd, Ottershaw, Chertsey, England; [Hoyle, Thomas M.] Univ Utrecht, Marine Palynol & Paleoceanog, Utrecht, Netherlands; [Stoica, Marius] Univ Bucharest, Dept Geol, Bucharest, Romania; [Austin, William E. N.] Univ St Andrews, Sch Geog & Geosci, St Andrews, Fife, Scotland; [Cage, Alix G.] Keele Univ, Sch Geog Geol & Environm, Keele, Staffs, England; [Marret, Fabienne; Pinnington, Carmel A.] Univ Liverpool, Sch Environm Sci, Liverpool, Merseyside, England	University of Amsterdam; Utrecht University; Utrecht University; University of Bucharest; University of St Andrews; Keele University; University of Liverpool	Richards, K (通讯作者)，KrA Stratig Ltd, 116 Albert Dr, Deganwy LL31 9YY, Conwy, Wales.	kr@paly.co.uk	Stoica, Marius/N-4941-2018; Cage, Alix/AAK-9555-2021	van Baak, Christiaan/0000-0002-2044-2872; Stoica, Marius/0000-0003-0126-4270; Cage, Alix/0000-0001-9992-9757; Marret-Davies, Fabienne/0000-0003-4244-0437; Hoyle, Thomas M./0000-0002-6611-2254	Netherlands Research Centre for Integrated Solid Earth Sciences (ISES); Netherlands Organization for Scientific Research (NWO) [865.10.011]; DARIUS programme; BP (Caspian Sea) Ltd.; StrataData Ltd.; KrA Stratigraphic Ltd.; NERC [NE/J024449/1]	Netherlands Research Centre for Integrated Solid Earth Sciences (ISES); Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); DARIUS programme; BP (Caspian Sea) Ltd.; StrataData Ltd.; KrA Stratigraphic Ltd.; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work was carried out in the frame of activities sponsored by Netherlands Research Centre for Integrated Solid Earth Sciences (ISES) and the Netherlands Organization for Scientific Research (NWO) under grant number 865.10.011 awarded to Utrecht University. We are grateful to the DARIUS programme and its sponsors for funding of multiple fieldworks in Azerbaijan. The cost of biostratigraphic preparations was funded by BP (Caspian Sea) Ltd. and biostratigraphic analyses funded by StrataData Ltd. (micropalaeontology) and KrA Stratigraphic Ltd. (palynology). Palynological preparations were made by Jonah Chitolie (GeoTechniques Research Ltd.) and microfaunal preparations by Malcolm Jones (PLS Ltd.) and Rebecca Lamb (PetroStrat Ltd.). Nannofossil analyses were carried out by Liam Gallagher (Network Stratigraphic Ltd.) and Jennie Bull (PetroStrat Ltd.). SEM analyses of palynomorphs were carried out in the EBSD-SEM laboratory in the Department of Earth, Ocean and Ecological Sciences, School of Environmental Sciences, University of Liverpool supported by NERC grant NE/J024449/1, with thanks to Elisabetta Mariani and Mike O'Connor. SEM analyses of foraminifera were carried out at Keele University and the University of St Andrews, and SEM analyses of ostracods at the University of Bucharest. The authors would like to extend special thanks to Peta Mudie (Geological Survey Canada-Atlantic, Dartmouth, Canada) and two anonymous reviewers, for extensive comments that have significantly improved this manuscript. Frans Jorissen (University de Angers, France) is thanked for providing unpublished biometric data of Mediterranean foraminifera and for text comments. 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DEC 15	2018	511						119	143		10.1016/j.palaeo.2018.07.018	http://dx.doi.org/10.1016/j.palaeo.2018.07.018			25	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	HD5PY		Green Accepted, Green Published			2025-03-11	WOS:000452583600007
J	Keutgen, N				Keutgen, Norbert			A bioclast-based astronomical timescale for the Maastrichtian in the type area (southeast Netherlands, northeast Belgium) and stratigraphic implications: the legacy of PJ Felder	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						bivalves; calcareous nannofossils; dinoflagellates; eccentricity cycles; echinoderms	CARBON-ISOTOPE STRATIGRAPHY; MEMBER GULPEN FORMATION; CRETACEOUS/TERTIARY BOUNDARY; BENTHIC FORAMINIFERA; NANNOFOSSIL BIOSTRATIGRAPHY; INTEGRATED STRATIGRAPHY; SCAPHITID AMMONITES; BASQUE COUNTRY; DANISH BASIN; SEA	The present paper, dedicated to the legacy of local geologist-engineer Peter Jozef (Sjeuf) Felder, who died in 2009, confirms his view that bioclasts constitute a valuable tool in the correlation of outcrops and borehole cores across the type area of the Maastrichtian Stage in the vicinity of Maastricht. His approach of interpreting changes in bioclast contents as having been influenced by Milankovitch cyclicity has here been applied successfully to the entire sedimentary complex of Maastrichtian (latest Cretaceous) age in the study area. In the present approach, results are corroborated by index fossils, mainly dinoflagellate cysts but also calcareous nannofossils, which allow correlation with the Stevns-1 core reference section in eastern Denmark. With the exception of local remnants of Belemnella obtusa Zone age, the Maastrichtian Stage in its type area encompasses the last 4.6 Ma of the Cretaceous Period (i.e. the Belemnella sumensis/Acanthoscaphites tridens Zone up to the K/Pg boundary). P.J. Felder's bioclast analyses have enabled the detection of twelve 400 kyr eccentricity cycles of Milankovitch cyclicity in the area. However, the section is not continuous; there is a hiatus of c. 700 kyr between the Gulpen and Maastricht formations at the ENCI-HeidelbergCement Group quarry. In addition, smaller hiatuses, usually in the range of several 20 kyr cycles, have been detected in the upper Maastricht Formation.	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J	Sánchez-Pellicer, R; Masure, E; Villier, L				Sanchez-Pellicer, R.; Masure, E.; Villier, L.			Distribution of Albian dinoflagellate cyst associations along a proximal-distal transect across the Iberian margin	CRETACEOUS RESEARCH			English	Article						Dinocyst; Cretaceous; Lusitanian Basin; DSDP Hole 398D; Paleoenvironment; Statistical significance	LUSITANIAN BASIN PORTUGAL; SEA-SURFACE TEMPERATURE; NORTH-ATLANTIC; PALEOENVIRONMENTAL ANALYSIS; HYDROGRAPHIC CONDITIONS; MARINE ENVIRONMENTS; ANGIOSPERM POLLEN; ORGANIC-MATTER; BOUNDARY EVENT; STRATIGRAPHY	The analysis of Albian dinoflagellate cysts, or dinocysts, along an inshore-offshore transect across the Iberian Margin reveals the environmental influence on the assemblages composition. Two biodiversity metrics are used to analyze changes in the assemblage structure. The stress associated to environmental instability is identified as the main factor influencing the dinocyst biodiversity. The relative frequency distribution of dinocysts is analyzed to identify associations of taxa sharing similar environmental preferences. Seven dinocyst associations are identified. The environmental affinities of the seven dinocyst associations are inferred from lithological data and assemblage structure. Association 1 dominated the most proximal and unstable environments. Associations 2 and 3 characterized inner-middle neritic environments. Taxa in the Association 2 preferred stable mesotrophic conditions, whereas, taxa in the Association 3 were tolerant to variations in salinity and nutrient input. Associations 4 and 5 are indicative of open marine distal environments. Taxa in the Association 4 were tolerant to limited environmental fluctuations. Taxa in the Association 5 were restricted to stable open marine conditions. The widespread distribution of taxa in the Association 6 is interpreted as revealing their ubiquitous character. The taxon in the Association 7 is considered as cosmopolitan because its widespread distribution was conditioned to nutrients availability. (C) 2018 Elsevier Ltd. All rights reserved.	[Sanchez-Pellicer, R.; Masure, E.; Villier, L.] Sorbonne Univ, Ctr Rech Paleobiodivers & Paleoenvironm, CNRS, MNHN,CR2P,UMR7207,Case 104, F-75252 Paris 05, France; [Sanchez-Pellicer, R.] Univ Zaragoza, Dept Ciencias Tierra, Area Paleontol, C Pedro Cerbuna 12, E-50009 Zaragoza, Spain	Sorbonne Universite; Museum National d'Histoire Naturelle (MNHN); Centre National de la Recherche Scientifique (CNRS); University of Zaragoza	Sánchez-Pellicer, R (通讯作者)，Sorbonne Univ, Ctr Rech Paleobiodivers & Paleoenvironm, CNRS, MNHN,CR2P,UMR7207,Case 104, F-75252 Paris 05, France.	raquel.sanchez.pellicer@gmail.com						Adrain JM, 2000, PALEOBIOLOGY, V26, P625, DOI 10.1666/0094-8373(2000)026<0625:STADAT>2.0.CO;2; Alves TM, 2009, TECTONICS, V28, DOI 10.1029/2008TC002337; Anderson MJ, 2001, AUSTRAL ECOL, V26, P32, DOI 10.1046/j.1442-9993.2001.01070.x; [Anonymous], 1989, P OCEAN DRILLING PRO, DOI DOI 10.2973/ODP.PROC.SR.105.134.1989; Arthur M.A., 1979, INIT REPTS DSOP, V47, P719; Balseiro D, 2014, PALAEOGEOGR PALAEOCL, V414, P133, DOI 10.1016/j.palaeo.2014.08.022; Bashforth AR, 2010, PALAEOGEOGR PALAEOCL, V292, P367, DOI 10.1016/j.palaeo.2010.03.037; BERTHOU P.-Y., 1982, CUADERNOS GEOLOG A I, V8, P761; BERTHOU PY, 1990, REV PALAEOBOT PALYNO, V66, P313, DOI 10.1016/0034-6667(90)90045-K; BERTHOU PY, 1979, CR ACAD SCI D NAT, V288, P591; BINT A N, 1986, Palynology, V10, P135; Blechschmidt G., 1979, Initial Reports of the Deep Sea Drilling Project, V47B., P327, DOI [DOI 10.2973/DSDP.PROC.47-2.106.1979, 10.2973/dsdp.proc.47-2.106.1979]; Boillot G., 1987, Proceedings of the Ocean Drilling Program, 103 Initial Reports; Bonnet S, 2012, MAR MICROPALEONTOL, V84-85, P87, DOI 10.1016/j.marmicro.2011.11.006; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Bulinski KV, 2007, PALAEOGEOGR PALAEOCL, V253, P490, DOI 10.1016/j.palaeo.2007.06.016; Burla S, 2008, PALAEOGEOGR PALAEOCL, V257, P38, DOI 10.1016/j.palaeo.2007.09.010; Cartes JE, 2017, DEEP-SEA RES PT I, V125, P52, DOI 10.1016/j.dsr.2017.04.016; Choffat P., 1885, Recueil de monographies stratigraphiques sur le systeme cretacique du Portugal; Choffat P., 1891, Communicacoes da Commissao dos Trabalhos Geologicos de Portugal, V2, P171; Choffat P., 1904, Le Cretacique dans L'Arrabida et dans la Contree D'Ericeira, VVI, P1; Coccioni R., 1993, PALAEOPELAGOS, V3, P195; Coimbra R, 2017, MAR PETROL GEOL, V86, P1029, DOI 10.1016/j.marpetgeo.2017.07.003; Crouch EM, 2005, MAR MICROPALEONTOL, V56, P138, DOI 10.1016/j.marmicro.2005.05.002; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; DE VERNAL A, 1993, GEOGR PHYS QUATERN, V47, P167, DOI 10.7202/032946ar; Deroo G., 1979, Initial Rep. 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J	Yñiguez, AT; Maister, J; Villanoy, CL; Deauna, JD; Peñaflor, E; Almo, A; David, LT; Benico, GA; Hibay, E; Mora, I; Arcamo, S; Relox, J; Azanza, RV				Yniguez, Aletta T.; Maister, Jennifer; Villanoy, Cesar L.; Deauna, Josephine Dianne; Penaflor, Eileen; Almo, Aldwin; David, Laura T.; Benico, Garry A.; Hibay, Ellen; Mora, Irmi; Arcamo, Sandra; Relox, Jun; Azanza, Rhodora V.			Insights into the dynamics of harmful algal blooms in a tropical estuary through an integrated hydrodynamic-<i>Pyrodinium</i>-shellfish model	HARMFUL ALGAE			English	Article						Harmful algal blooms; Pyrodinium bahamense; Life cycle; Biophysical model; Estuary; Seasonality	BAHAMENSE VAR. COMPRESSUM; ALEXANDRIUM-FUNDYENSE BLOOMS; HALF-SATURATION CONSTANTS; NITRATE UPTAKE; WESTERN GULF; MANILA BAY; TOXINS; CYST; TOXICITY; GROWTH	In contrast to temperate Harmful Algal Blooms (HABs), knowledge on the mechanisms driving tropical HABs are less well studied. The interaction of a seasonal temperature window, cysts (for certain species) and large-scale transport are some of the key processes in temperate HABs. In the Philippines, HABs occur not along long open coastlines, but in embayments that are highly influenced by run-off and stratification. These embayments are typically also the sites of cultured or wild harvest shellfish and other aquaculture activities. Sorsogon Bay in the northeastern Philippines has experienced prolonged shellfish-harvesting bans due to blooms by Pyrodinium bahamense var. compressum severely affecting the fisheries industry in this area, as well as leading to Paralytic Shellfish Poisoning illnesses and fatalities. A novel integrated model was developed that mechanistically captures the interactions between hydrodynamic conditions, nutrients, the life history (cells and cysts) of Pyrodinium, as well as the cultured shellfish within the bay and their ensuing toxicities due to ingestion of toxic Pyrodinium cells and cysts. This is the second model developed for HABs in the Philippines, and the first to integrate different components of Pyrodinium bloom dynamics. The model is modularly composed of a watershed nutrient and diffusion model, a 3D hydrodynamic model, a Pyrodinium population model and a shellfish toxin model. It was able to capture the observed temporal variations of Pyrodinium and shellfish toxicity. It was also able to represent some aspects of the spatial distribution in Sorsogon Bay though there were discrepancies. To explore the dynamics of blooms, the linkages between the bloom and decline of the Pyrodinium population with shellfish toxicity as affected by temperature, salinity and nutrients were investigated. Comparisons with field results showed the seasonality of blooms in Sorsogon Bay is driven by increased rainfall. The timing of these conditions is important in facilitating Pyrodinium excystment and reproduction. Model results showed as well the potential significance of shellfish grazing and dinoflagellate cell mortality in influencing the decline of the bloom, and toxicity levels. This approach is promising in helping to understand mechanisms for HABs more holistically, and the model can be further improved to provide more precise quantitative information.	[Yniguez, Aletta T.; Maister, Jennifer; Villanoy, Cesar L.; Deauna, Josephine Dianne; Penaflor, Eileen; Almo, Aldwin; David, Laura T.; Benico, Garry A.; Azanza, Rhodora V.] Univ Philippines, Inst Marine Sci, Quezon City, Philippines; [Hibay, Ellen; Mora, Irmi] Bur Fisheries & Aquat Resources Reg 5, San Agustin Pili, Camarines Sur, Philippines; [Arcamo, Sandra; Relox, Jun] Bur Fisheries & Aquat Resources Main, Quezon City, Philippines	University of the Philippines System; University of the Philippines Diliman	Yñiguez, AT (通讯作者)，Univ Philippines, Inst Marine Sci, Quezon City, Philippines.	atyniguez@msi.upd.edu.ph	Azanza, Rhodora/HGU-5811-2022; Benico, Garry/S-6313-2019	Benico, Garry/0000-0002-2617-0222	Philippine Council for Agriculture, Aquatic and Natural Resources Research and Development (PCAARRD), Department of Science and Technology	Philippine Council for Agriculture, Aquatic and Natural Resources Research and Development (PCAARRD), Department of Science and Technology	The development and analysis of this model was made by possible through the funding provided by the Philippine Council for Agriculture, Aquatic and Natural Resources Research and Development (PCAARRD), Department of Science and Technology for the projects Stratification and Algal Blooms in the Tropics and Development of a Harmful Algal Bloom Operational Predictive System for the Philippines. The contributions and support of the staff and researchers from the PhilHABS, HABTech and HABGen programs, as well as the Bureau of Fisheries and Aquatic Resources (BFAR) were also important in filling in information needed for the model. The administrative staff at the Marine Science Institute were vital in processing paperwork and conducting tasks that allowed the researchers to carry out their science. 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J	Faye, S; Rochon, A; St-Onge, G				Faye, Simon; Rochon, Andre; St-Onge, Guillaume			Distribution of Modern Dinoflagellate Cyst Assemblages in Surface Sediments of San Jorge Gulf (Patagonia, Argentina)	OCEANOGRAPHY			English	Article							SURFICIAL SEDIMENTS; FEEDING-BEHAVIOR; OCEAN; SEA; GROWTH; CHLOROPHYLL; VARIABILITY; HEMISPHERE; PACIFIC; NORTH	The presence of upwelling systems and oceanic fronts makes the Southwest Atlantic Ocean a region of high primary productivity. These same conditions are present in San Jorge Gulf (SJG) along the southern Argentinian coast, where dinoflagellates and diatoms dominate primary production. The distribution of these microorganisms, including the cysts produced by some dinoflagellates during their life cycles, is controlled in marine environments by oceanographic parameters that include salinity, surface water temperature, ice cover duration, and productivity. The objective of this study is to document the modern distribution of dinoflagellate cyst assemblages in surface sediments so that the environmental preferences of each taxon can be inferred and used to reconstruct paleoenvironmental conditions. The dinoflagellate cyst (dinocyst) assemblages of 52 surface samples collected in 2014 aboard R/V Coriolis II in the SJG were described and compared to surface oceanographic conditions and grain size data. The results indicate dinocyst concentrations vary between 64 cysts g(-1) and 45,848 cysts g(-1) dry sediment, with Spiniferites ramosus and Operculodinium centrocarpum the dominant species, accompanied by Spiniferites mirabilis, Dubridinium sp., cysts of Polykrikos kofoidii, and cysts of Brigantedinium simplex, Brigantedinium auranteum, and Brigantedinium spp. We have defined two spatial domains based on the distribution of dinocysts in and near the SJG: northern/southern-central gulf and offshore domains. We found an increase in dinocyst concentrations along a north-south gradient in the SJG and minimum concentrations at offshore sites. In addition, multivariate analyses reveal the relationships among the relative abundances of dinocysts, fine grain size data (< 63 mu m; silts and clays), and primary productivity, as well as offshore upwelling, which appear to control most of the distribution of dinocysts.	[Faye, Simon] Inst Sci Mer Rimouski ISMER, Quebec Ocean, PQ, Canada; [Faye, Simon; Rochon, Andre; St-Onge, Guillaume] Univ Quebec Rimouski, GEOTOP, Rimouski, PQ, Canada; [Rochon, Andre] Univ Quebec Rimouski, ISMER, Rimouski, PQ, Canada; [St-Onge, Guillaume] Univ Quebec Rimouski, ISMER, Marine Geol, Rimouski, PQ, Canada	University of Quebec; Universite du Quebec a Rimouski; University of Quebec; Universite du Quebec a Rimouski; University of Quebec; Universite du Quebec a Rimouski	Faye, S (通讯作者)，Inst Sci Mer Rimouski ISMER, Quebec Ocean, PQ, Canada.; Faye, S (通讯作者)，Univ Quebec Rimouski, GEOTOP, Rimouski, PQ, Canada.	simon.faye@uqar.ca	St-Onge, Guillaume/E-4828-2014	St-Onge, Guillaume/0000-0001-6958-4217	Ministerio de Cienca, Tecnologia e Innovacion Productiva (MINCyT); Provincia de Chubut; Consejo Nacional de Investigaciones Cientificas Tecnicas (CONICET); FRQNT (Fonds de recherche du Quebec - Nature et technologies); NSERC	Ministerio de Cienca, Tecnologia e Innovacion Productiva (MINCyT); Provincia de Chubut; Consejo Nacional de Investigaciones Cientificas Tecnicas (CONICET)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); FRQNT (Fonds de recherche du Quebec - Nature et technologies); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	The authors are grateful to the captain, officers, crew, and scientists of the MARGES expedition on board R/V Coriolis II. We are grateful for the financial support of the Ministerio de Cienca, Tecnologia e Innovacion Productiva (MINCyT), Provincia de Chubut and the Consejo Nacional de Investigaciones Cientificas Tecnicas (CONICET) for the MARES and MARGES expeditions. Special thanks to A. Rivas and Pierre-Arnaud Desiage, who provided chlorophyll-a and grain size data, respectively. We also thank the reviewers for their comments that helped improve this manuscript. This work was carried out with the financial support of FRQNT (Fonds de recherche du Quebec - Nature et technologies) to G. St-Onge and A. Rochon and NSERC Discovery grants to A. Rochon and G. St-Onge.	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BOX 1931, ROCKVILLE, MD USA	1042-8275			OCEANOGRAPHY	Oceanography	DEC	2018	31	4			SI		122	131		10.5670/oceanog.2018.416	http://dx.doi.org/10.5670/oceanog.2018.416			10	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	HE5JA		gold, Green Published			2025-03-11	WOS:000453412900016
J	Kumar, A				Kumar, Arun			First record of palynomorph assemblages from the Arshad Sandstone (Late Cretaceous), Sirte Basin, north-central Libya	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Arshad Sandstone; Sirte Basin; Libya; Campanian-Maastrichtian palynomorphs; Paleoenvironments	DINOFLAGELLATE CYSTS; PALEOGENE BOUNDARY; WESTERN DESERT; OULED HADDOU; PALYNOLOGY; SEDIMENTS; FORAMINIFERA; OASIS; WELL; AREA	This paper presents the first record of identifiable palynomorph assemblages from the Arshad Sandstone, Sirte Basin, north-central Libya. Ninety core samples from five different wells were macerated to isolate palynomorphs, but 78 samples turned out to be barren. Among the 12 productive samples, the preservation of palynomorphs was generally poor to fair, limiting identifications at species level. However, despite these limitations workable assemblages were recovered from a few productive samples. Since palynomorph preservation is poor, many forms could only be identified at the generic level and some were unidentifiable. A few stratigraphically significant dinoflagellate cysts were identified at the species level. Palynomorph diversity is fairly high including both terrestrial (angiosperm and gymnosperm pollen grains, spores, algal and fungal remains) and marine (dinoflagellate cysts, acritarchs and foraminiferal remains) forms. The lithology of the Arshad Sandstone is quite diverse; variables include very hard and silicified sandstones, massive shales, sandy dolomites, and dolomitic sandstones. Characteristically all these sediments are massive, very hard, and occasionally bioturbated. No identifiable or datable macro- or mega-fossils are known from this stratigraphic unit, and previous attempts to isolate palynomorphs have been unsuccessful. The present palynological study indicates that these sediments were deposited in diverse environments ranging from nearshore terrestrial to shallow marine (inner shelf). Dinoflagellate cyst species indicate that the Arshad Sandstone is of Campanian-Maastrichtian age.	[Kumar, Arun] Carleton Univ, Dept Earth Sci, 1125 Colonel Dr, Ottawa, ON K1S 5B6, Canada	Carleton University	Kumar, A (通讯作者)，Carleton Univ, Dept Earth Sci, 1125 Colonel Dr, Ottawa, ON K1S 5B6, Canada.	arunkumarlko@hotmail.com						Abubakar MB, 2011, J AFR EARTH SCI, V60, P19, DOI 10.1016/j.jafrearsci.2011.01.007; Ahlbrandt T.S., 2001, U. S. Geological Survey Bulletin, V2, P1; [Anonymous], 1996, GEOLOGY SIRT BASIN; Barr F., 1972, Stratigraphic Nomenclature of the Sirte Basin, Libya; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; Boltenhagen E, 1977, EDI CENT NAT RECH SC; Bu-Argoub F. 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J. Geosci.	DEC	2018	11	23							740	10.1007/s12517-018-4108-z	http://dx.doi.org/10.1007/s12517-018-4108-z			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	HC7ED					2025-03-11	WOS:000451962500004
J	Correia, VF; Riding, JB; Duarte, LV; Fernandes, P; Pereira, Z				Correia, Vania F.; Riding, James B.; Duarte, Luis, V; Fernandes, Paulo; Pereira, Zelia			The Early Jurassic palynostratigraphy of the Lusitanian Basin, western Portugal	GEOBIOS			English	Article; Proceedings Paper	1st Workshop on Iberian Palaeobotany and Palynology	FEB 22, 2017	Cordoba, SPAIN			Biostratigraphy; Palynomorphs; Dinoflagellate cysts; Lower Jurassic; Lusitanian Basin; Portugal	OCEANIC ANOXIC EVENT; MIDDLE TOARCIAN; CALCAREOUS NANNOFOSSILS; ORGANIC-MATTER; BIOSTRATIGRAPHY; STRATIGRAPHY; ASSEMBLAGES; PALYNOLOGY; PENICHE; SEQUENCE	A comprehensive investigation of the Early Jurassic stratigraphical palynology of the Lusitanian Basin in western Portugal was undertaken, with most emphasis placed on dinofiagellate cysts. A total of 214 samples from an upper Sinemurian to upper Toarcian composite section based on six successions were examined. The Sinemurian material examined was barren of dinoflagellate cysts; however, the Pliensbachian and Toarcian successions are characterised by relatively low diversities where Luehndea spinosa, Mancodinium semitabulatum, Mendicodinium microscabratum, Nannoceratopsis gracilis, Nannoceratopsis senex, and Scriniocassis priscus are relatively common and biostratigraphically significant. Luehndea spinosa dominates the lowermost Toarcian (Dactylioceras polymorphum ammonite Biozone), and is an index species. At the base of the Hildaites levisoni ammonite Biozone, the effects of the Toarcian Oceanic Anoxic Event (T-OAE) caused Luehndea spinosa to become extinct. At the same time, dinofiagellate cyst abundance and diversity markedly decreased. After the T-OAE, during the middle and late Toarcian, phytoplankton recovery was prolonged and slow in the Lusitanian Basin. The Luehndea spinosa and Mendicodinium microscabratum dinoflagellate cyst biozones are defined, both of which are subdivided into two dinofiagellate cyst subbiozones. (C) 2018 Elsevier Masson SAS. All rights reserved.	[Correia, Vania F.; Fernandes, Paulo] Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal; [Correia, Vania F.; Pereira, Zelia] LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal; [Riding, James B.] British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, England; [Duarte, Luis, V] Univ Coimbra, Fac Sci & Technol, MARE Marine & Environm Sci Ctr, Dept Earth Sci, Rua Silvio Lima, P-3030790 Coimbra, Portugal	Universidade do Algarve; Laboratorio Nacional de Energia e Geologia IP (LNEG); UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universidade de Coimbra	Correia, VF (通讯作者)，Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal.	vania.correia@lneg.pt	Fernandes, Paulo/J-6577-2014; Duarte, Luis/F-5282-2013; Pereira, Zelia/B-2740-2017	Fernandes, Paulo/0000-0003-4888-0230; Duarte, Luis/0000-0002-9025-5896; Correia, Vania/0000-0001-5648-3185; Pereira, Zelia/0000-0003-3056-6219	Portuguese Foundation for Science and Technology (FCT) [SFRH/BD/93950/2013]; FCT [UID/MAR/04292/2013]; Project TOAE: Toarcian Oceanic Anoxic Event: Impact on marine carbon cycle and ecosystems (UNESCO-IUGS) [IGCP 655]; NERC [bgs05017] Funding Source: UKRI; Fundação para a Ciência e a Tecnologia [SFRH/BD/93950/2013] Funding Source: FCT	Portuguese Foundation for Science and Technology (FCT)(Fundacao para a Ciencia e a Tecnologia (FCT)); FCT(Fundacao para a Ciencia e a Tecnologia (FCT)); Project TOAE: Toarcian Oceanic Anoxic Event: Impact on marine carbon cycle and ecosystems (UNESCO-IUGS); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	The contribution of VSnia F. Correia is part of her Ph.D. scholarship SFRH/BD/93950/2013, awarded by the Portuguese Foundation for Science and Technology (FCT). This work is also under the Project IGCP 655 -TOAE: Toarcian Oceanic Anoxic Event: Impact on marine carbon cycle and ecosystems (UNESCO-IUGS). James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). Luis V. Duarte was supported by FCT, through the strategic project UID/MAR/04292/2013 granted to the Marine and Environmental Sciences Centre (MARE). The authors are grateful to Dr. Niels Poulsen (GEUS), Dr. Daniel Michoux (Total), Dr. Jose B. Diez (Vigo University) and to the journal Editor, Dr. Gilles Escarguel, for the helpful comments which substantially improved this work.	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J	Meroni, L; Chiantore, M; Petrillo, M; Asnaghi, V				Meroni, L.; Chiantore, M.; Petrillo, M.; Asnaghi, V.			Habitat effects on <i>Ostreopsis</i> cf. <i>ovata</i> bloom dynamics	HARMFUL ALGAE			English	Article						Ostreopsis cf. ovata; Benthic dinoflagellates; Bloom dynamics; Urbanisation; Hydrodynamics; Substratum preference	MEDITERRANEAN SEA; GENUS OSTREOPSIS; COASTAL WATERS; COOLIA DINOPHYCEAE; PROLIFERATION; MANAGEMENT; ALGAE; GENOA; QUANTIFICATION; MICROALGAE	In the last few decades, Ostreopsis spp., toxic benthic dinolagellates of tropical origin, generated large interest in the Mediterranean Sea, where several bloom events have been observed. Ecology and proliferation dynamics of O. cf. ovata are driven by complex interactions among biotic and abiotic drivers, and understanding mechanisms triggering bloom events is still far from being complete. The aim of the present study is to highlight the role of different habitat conditions, elucidating the effects of i) exposure to hydrodynamic conditions, ii) macroalgal community and iii) urbanisation level, in driving O. cf. ovata bloom dynamics. A significant effect of hydrodynamics was observed only for cells in seawater, with higher abundances in sheltered zones, irrespective of the urbanisation level. Similarly, a significant effect of the dominant macroalgal community, with higher abundances in Corallinales and turf dominated communities, and lower ones in Cystoseira amentacea canopies, has been recorded, consistently in the differently urbanised sites. Additionally, stretches of the coast suffering from a more intense anthropic exploitation are in general more prone to the proliferation of potentially toxic benthic microalgae. All these results imply a larger risk exposure to toxic effects for humans in urban beaches and sheltered areas, usually more attended by swimmers and bathers. These findings underline the need to preserve, and eventually restore, canopy dominated assemblages, which presently are under regression because of human threats, providing a straightforward example that restoration of relevant habitats implies a cascading improvement of human welfare.	[Meroni, L.; Chiantore, M.; Petrillo, M.; Asnaghi, V.] Univ Genoa, DISTAV, Cso Europa 26, Genoa, Italy; [Asnaghi, V.] CoNISMa, Ple Flaminio 9, Rome, Italy; [Chiantore, M.] CNR IBF, Via De Marini 5, Genoa, Italy	University of Genoa; CoNISMa; Consiglio Nazionale delle Ricerche (CNR); Istituto di Biofisica (IBF-CNR)	Asnaghi, V (通讯作者)，Univ Genoa, DISTAV, Cso Europa 26, Genoa, Italy.	valentina.asnaghi@unige.it	Asnaghi, Valentina/AFT-8900-2022; Chiantore, Mariachiara/C-7070-2017	Chiantore, Mariachiara/0000-0002-5862-1470; Asnaghi, Valentina/0000-0003-1659-2613	European Union	European Union(European Union (EU))	This publication is a contribution to M3-HABs project funded by the European Union under the ENPI CBC Mediterranean Sea Basin Programme. Authors thank Dr. Anna Maria Rossi for her help in sample processing and cells identification and counting. 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J	McLachlan, SMS; Pospelova, V; Hebda, RJ				McLachlan, Sandy M. S.; Pospelova, Vera; Hebda, Richard J.			Dinoflagellate cysts from the upper Campanian (Upper Cretaceous) of Hornby Island, British Columbia, Canada, with implications for Nanaimo Group biostratigraphy and paleoenvironmental reconstructions	MARINE MICROPALEONTOLOGY			English	Article						Cretaceous; North Pacific; Northumberland Formation; Dinoflagellate cysts; Palynology; Palynomorphs; Pollen and spores	SEA-SURFACE TEMPERATURE; TERTIARY BOUNDARY; MAESTRICHTIAN FORAMINIFERA; CALCAREOUS NANNOFOSSIL; MOLECULAR FOSSILS; SEDIMENTARY-ROCKS; MARINE-SEDIMENTS; SPRAY FORMATIONS; SACCATE POLLEN; UPPER LAMBERT	Thirty mudstone samples from coastal exposures of the Northumberland Formation on Hornby Island, British Columbia, Canada, yielded diverse dinoflagellate cyst and terrestrial sporomorph assemblages. A late Campanian age for the formation has been well defined through magnetostratigraphy, macrofossil biostratigraphy, and geochemical studies of the Hornby Island section. Dinoflagellate cyst taxa corresponding to 61 genera are exceptionally well preserved and include specimens referable to at least 68 formally established species. The earliest occurrences of Canninginopsis maastrichtiensis, Druggidium cf. discretum, Phanerodinium belgicum, Renidinium cf. vitilaire, Senegalinium simplex, Spiniferella cornuta, and Xenicodinium delicatum sensu Slimani et al. are reported along with the most recent occurrence of Senoniasphaera protrusa, extending their stratigraphic ranges into the upper Campanian. The palynomorph assemblages support a late Campanian age. Two dinoflagellate cyst ecozones are recognized (ecozone 1 and ecozone 2). Assemblages suggest sediment deposition in an inner shelf environment with moderate to high nutrient input and primary productivity.	[McLachlan, Sandy M. S.; Pospelova, Vera; Hebda, Richard J.] Univ Victoria, Sch Earth & Ocean Sci, POB 1700, Victoria, BC V8W 2Y2, Canada; [Hebda, Richard J.] Royal BC Museum, 675 Belleville St, Victoria, BC V8W 9W2, Canada	University of Victoria	McLachlan, SMS (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, POB 1700, Victoria, BC V8W 2Y2, Canada.	sandymcl@uvic.ca	McLachlan, Sandy/ABD-2408-2021	Pospelova, Vera/0000-0003-4049-8133; McLachlan, Sandy/0000-0003-3902-7190	Natural Science and Engineering Research Council (NSERC)	Natural Science and Engineering Research Council (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	The authors wish to extend their gratitude to Dr. Rob Fensome of the Geological Survey of Canada, Bedford Institute of Oceanography, Nova Scotia for sharing his insights with respect to peridinioid cyst taxonomy and Dr. Dennis Braman of the Royal Tyrell Museum, Drumheller, Alberta for discussions pertaining to sporomorph taxonomic identification. This manuscript also benefited from highly constructive feedback provided by Dr. Martin A. Pearce of Evolution Applied Limited, Buckinghamshire, United Kingdom, Dr. Paul Dodsworth of StrataSolve Limited, Cheshire, United Kingdom, and two anonymous reviewers. Partial funding for this research was provided by the Natural Science and Engineering Research Council (NSERC) V.P. (Discovery Grant).	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J	Blanco, J; Martín-Morales, E; Alvarez, G				Blanco, Juan; Martin-Morales, Eva; Alvarez, Gonzalo			Stability of okadaic acid and 13-desmethyl spirolide C in seawater and sediment	MARINE CHEMISTRY			English	Article						Okadaic acid; Spirolide; Lipophilic toxins; Stability; Sediment; Seawater; Interstitial water	LIPOPHILIC MARINE TOXINS; DINOFLAGELLATE ALEXANDRIUM-OSTENFELDII; TANDEM MASS-SPECTROMETRY; ANAEROBIC BIODEGRADATION; DINOPHYSIS TOXINS; STEROLS; DEGRADATION; PERSISTENCE; BREVETOXIN; LIPIDS	Persistence of lipophilic toxins in different environmental compartments determines the way in which their concentrations can be used to evaluate temporal trends and associated risks. Short term stability of two lipophilic toxins, representing two chemically different groups of toxins - okadaic acid (OA) (Diarrhetic Shellfish Poisoning toxin) and 13-desmethyl spirolide C (13desmSPXC) (cyclic imine) - in seawater, interstitial water and sediment were analyzed. OA was found to be very stable in seawater, interstitial water and sediment, without significant changes over a 23-day period. Contrarily, 13desmSPXC was readily degraded, but faster in interstitial water than in seawater. In sediments, its degradation was also fast and dependent on the origin of the samples. 13desmSPXC was found in natural sediments, and this toxin was mostly associated to large particles (> 10 mu m) in the sediment, that are or include resting cysts of the producer species. Therefore, it appears that high concentrations of 13desmSPXC in seawater would indicate recent blooms of the producer species, while those of OA could be due to recent blooms or to others that took place long before detection. The absence of OA and 13desmSPXC indicates a low impact of those toxins in the study area.	[Blanco, Juan; Martin-Morales, Eva] Ctr Invest Marinas, Pedras de Coron S-N, Vilanova De Arousa 36620, Spain; [Alvarez, Gonzalo] Univ Catolica Norte, Dept Acuicultura, Fac Ciencias Mar, Larrondo 1281, Coquimbo, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, CIDTA, Fac Ciencias Mar, Larrondo 1281, Coquimbo, Chile	Universidad Catolica del Norte; Universidad Catolica del Norte	Blanco, J (通讯作者)，Ctr Invest Marinas, Pedras de Coron S-N, Vilanova De Arousa 36620, Spain.	juan.carlos.blanco.perez@xunta.gal	Alvarez, Gonzalo/W-1262-2017; Blanco, Juan/A-8000-2008	Alvarez Vergara, Gonzalo/0000-0001-5812-1559; Blanco, Juan/0000-0003-2123-7747	Xunta de Galicia [PGDIT-12/02]; Conselleria do Mar of the Xunta de Galicia; Chilean National Commission for Scientific and Technological Research (CONICYT + PAI/CONCURSO NACIONAL INSERCION EN LA ACADEMIA CONVOCATORIA 2015) [79,150,008]	Xunta de Galicia(Xunta de Galicia); Conselleria do Mar of the Xunta de Galicia; Chilean National Commission for Scientific and Technological Research (CONICYT + PAI/CONCURSO NACIONAL INSERCION EN LA ACADEMIA CONVOCATORIA 2015)	This research was funded by Xunta de Galicia through the Project PGDIT-12/02. The work of Eva Martin-Morales was supported by a doctoral fellowship of the Conselleria do Mar of the Xunta de Galicia. Gonzalo Alvarez was funded by the Chilean National Commission for Scientific and Technological Research (CONICYT + PAI/CONCURSO NACIONAL INSERCION EN LA ACADEMIA CONVOCATORIA 2015, 79,150,008). We acknowledge Carmen Marino and Helena Martin for their technical assistance, as well as the crew of the vessel Chasula for their help in obtaining the sediment samples.	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Chem.	NOV 20	2018	207						21	25		10.1016/j.marchem.2018.10.007	http://dx.doi.org/10.1016/j.marchem.2018.10.007			5	Chemistry, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Oceanography	HE0BV					2025-03-11	WOS:000452932700003
J	Zwiep, KL; Hennekam, R; Donders, TH; van Helmond, NAGM; de Lange, GJ; Sangiorgi, F				Zwiep, Karin L.; Hennekam, Rick; Donders, Timme H.; van Helmond, Niels A. G. M.; de Lange, Gert J.; Sangiorgi, Francesca			Marine productivity, water column processes and seafloor anoxia in relation to Nile discharge during sapropels S1 and S3	QUATERNARY SCIENCE REVIEWS			English	Article						Sapropel S1; Sapropel S3; Nile discharge; Pollen; Micropaleontology; Dinocysts; Geochemistry; Nile delta; Anoxia; Marine productivity	EASTERN MEDITERRANEAN SAPROPEL; ORGANIC-MATTER; AFRICAN MONSOON; POLLEN RECORD; PLANKTONIC-FORAMINIFERA; DINOFLAGELLATE CYSTS; LATE PLEISTOCENE; AEGEAN SEA; TIME-SCALE; SEDIMENTS	Eastern Mediterranean sapropels S1 (similar to 10.5-6.1 kyr BP) and S3 (similar to 85.8-80.8 kyr BP) formed respectively under full interglacial and glacial inception conditions. Consequently, the environmental factors preconditioning and leading to sapropel formation (e.g., global sea level and monsoonal forcing) were different. These factors must have differently influenced processes such as marine productivity, water column processes, and related seafloor anoxia. Here we investigate these differences through an interdisciplinary approach using dinoflagellate cyst and pollen/spore assemblages and sedimentary (redox-sensitive) trace-metal concentrations from a core in the central Nile delta area. Comparing S1 to S3, we demonstrate that (1) Nile discharge appears to be stronger during S3 than S1, as shown by delta O-18(residuals), higher ratio of pollen and spores, and the higher abundance of coastal dinocysts and freshwater palynomorphs, (2) Ba/Al, C-org, and dinocyst accumulation rates indicate that marine productivity was similar at least during the first phase of their deposition and started prior to the onset of both sapropels, (3) bottom water conditions were more reducing during S3, resulting in higher Mo/Al, S, and C-org/P-tot values, but preservation was high and similar for both sapropels, and (4) Sedimentary Mo-U covariation indicates that the depth of water-column ventilation during deposition of S3 was shallower than during S1 (similar to 1000 m versus similar to 1800m, respectively). We attribute the observed differences to slightly enhanced precessional-forced monsoon intensity and potentially lower global sea level, resulting not only in increased North-African run-off, but also in reduced ventilation during S3 compared to S1. (C) 2018 Elsevier Ltd. All rights reserved.	[Zwiep, Karin L.; Donders, Timme H.; van Helmond, Niels A. G. M.; Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, Fac Geosci, Marine Palynol & Paleoceanog, Princetonlaan 8, NL-3584 CB Utrecht, Netherlands; [Hennekam, Rick; van Helmond, Niels A. G. M.; de Lange, Gert J.] Univ Utrecht, Dept Earth Sci, Fac Geosci, Geochem, Princetonlaan 8, NL-3584 CB Utrecht, Netherlands; [Hennekam, Rick] NIOZ Royal Netherlands Inst Sea Res, Dept Ocean Syst, POB 59, NL-1790 AB Den Burg, Texel, Netherlands; [Hennekam, Rick] Univ Utrecht, POB 59, NL-1790 AB Den Burg, Texel, Netherlands; [Donders, Timme H.] Univ Utrecht, Fac Geosci, Dept Phys Geog, Palaeoecol, Princetonlaan 8, NL-3584 CB Utrecht, Netherlands	Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University; Utrecht University	Zwiep, KL (通讯作者)，Univ Utrecht, Dept Earth Sci, Fac Geosci, Marine Palynol & Paleoceanog, Princetonlaan 8, NL-3584 CB Utrecht, Netherlands.; Hennekam, R (通讯作者)，NIOZ Royal Netherlands Inst Sea Res, Dept Ocean Syst, POB 59, NL-1790 AB Den Burg, Texel, Netherlands.; Hennekam, R (通讯作者)，Univ Utrecht, POB 59, NL-1790 AB Den Burg, Texel, Netherlands.	k.l.zwiep@gmail.com; rickhennekam@gmail.com	Donders, Timme/J-5044-2012; De Lange, Gert/B-9639-2014	Hennekam, Rick/0000-0002-8823-4519; De Lange, Gert/0000-0002-9420-3022; Sangiorgi, Francesca/0000-0003-4233-6154; van Helmond, Niels/0000-0003-0024-7217; Donders, Timme/0000-0003-4698-3463	MEDIFLUX-project [835.20.018]; MIMES; NWO [820.01.005]	MEDIFLUX-project; MIMES; NWO(Netherlands Organization for Scientific Research (NWO))	The published data of sapropels S1 and S3 are archived in the Mendeley data repository. For analytical assistance at Utrecht University we thank Erik van Vilsteren (ICP-MS), Helen de Waard (ICP-MS), Ton Zalm (ICP-OES) and Natasja Welters (Palynological preparation). NWO financial support to the MEDIFLUX-project (835.20.018) was greatly appreciated, which financed the MIMES cruise where core material was obtained. We thank captain, crew, NIOZ-technicians, and scientific team for core recovery. Funding of the PALM-project (820.01.005) by NWO to Gert J. de Lange is acknowledged for financing the geochemical analyses.	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J	Dzhembekova, N; Moncheva, S; Ivanova, P; Slabakova, N; Nagai, S				Dzhembekova, Nina; Moncheva, Snejana; Ivanova, Petya; Slabakova, Nataliya; Nagai, Satoshi			Biodiversity of phytoplankton cyst assemblages in surface sediments of the Black Sea based on metabarcoding	BIOTECHNOLOGY & BIOTECHNOLOGICAL EQUIPMENT			English	Article						18S rDNA; resting stages; sediment eukaryotic biodiversity; high-throughput sequencing (HTS)	RESTING STAGES; ADRIATIC SEA; BAY; RAPHIDOPHYCEAE; GERMINATION	Resting stages are common for the life cycle of some phytoplankton species, including blooming and potentially toxic species. The "seed bank" accumulated in the sediments can initiate blooms in the water column and could be an early warning signal of harmful algal blooms (HABs). In order to identify the phytoplankton cyst assemblages, thirteen surface sediment samples were collected from different sites in the Black Sea. The diversity of the resting stages was assessed using high-throughput sequencing metabarcoding (V7-9 hypervariable region of the 18S rDNA). One hundred and eighty microalgal species were identified with high level of similarity to the reference sequences. Dinoflagellates were dominated by Biecheleria, Gymnodinium and Karlodinium. Within diatoms, Skeletonema, Chaetoceros and Thalassiosira were the most abundant genera. Sixteen of the detected operational taxonomic units (OTUs) were assigned to harmful microalgae (12 dinoflagellates species, 1 diatom, 1 haptophyte and 2 raphidophytes). No pattern of microalgal sequences depth distribution was discriminated. The results show that DNA metabarcoding has a great potential for assessment of the phytoplankton diversity in environmental sediments.	[Dzhembekova, Nina; Moncheva, Snejana; Ivanova, Petya; Slabakova, Nataliya] Bulgarian Acad Sci, Inst Oceanol, Marine Biol & Ecol Dept, Varna, Bulgaria; [Nagai, Satoshi] Japan Fisheries Res & Educ Agcy, Natl Res Inst Fisheries Sci, Res Ctr Aquat Genom, Yokohama, Kanagawa, Japan	Bulgarian Academy of Sciences; Japan Fisheries Research & Education Agency (FRA)	Ivanova, P (通讯作者)，Bulgarian Acad Sci, Inst Oceanol, Marine Biol & Ecol Dept, Varna, Bulgaria.	pavl_petya@yahoo.com	Slabakova, Nataliya/LHA-4700-2024; Ivanova, Petya/A-3217-2014; Nagai, Satoshi/HOA-8686-2023; Dzhembekova, Nina/HTN-3019-2023	Ivanova, Petya/0000-0002-7487-9033; Dzhembekova, Nina/0000-0001-9620-6422; Slabakova, Nataliya/0000-0002-3294-5346; Nagai, Satoshi/0000-0001-7510-0063	Ministry of Education and Science, Bulgaria under project "Phytoplankton cysts - an intricacy between a "memory" or a "potential" for Black sea biodiversity and algal blooms" [LH01/8]; Japan Society for the Promotion of Science [17H03855]; National Science Fund; Grants-in-Aid for Scientific Research [17H03855] Funding Source: KAKEN	Ministry of Education and Science, Bulgaria under project "Phytoplankton cysts - an intricacy between a "memory" or a "potential" for Black sea biodiversity and algal blooms"; Japan Society for the Promotion of Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); National Science Fund; Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	This work was supported by the National Science Fund, Ministry of Education and Science, Bulgaria under project "Phytoplankton cysts - an intricacy between a "memory" or a "potential" for Black sea biodiversity and algal blooms" (Grant number LH01/8, 16.12.2016) and the Japan Society for the Promotion of Science under a Grant-In-Aid for Scientific Research (Kiban-B) (grant number 17H03855).	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Biotechnol. Equip.	NOV 2	2018	32	6					1507	1513		10.1080/13102818.2018.1532816	http://dx.doi.org/10.1080/13102818.2018.1532816			7	Biotechnology & Applied Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology	HP1AX		gold			2025-03-11	WOS:000461398900018
J	Vieira, M; Mandi, S; Casas-Gallego, M; Fenton, J				Vieira, Manuel; Mandi, Salih; Casas-Gallego, Manuel; Fenton, Jim			Three new Paleocene dinoflagellate cysts from the North Sea and the Norwegian Sea	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Paleocene; Danian; Selandian; Biostratigraphy; Dinoflagellate cysts; Taxonomy	LOWER PALEOGENE; BIOSTRATIGRAPHY; BASIN	Three dinoflagellate cysts species are formally described from Selandian and Danian sedimentary rocks of the North Sea and Norwegian Sea. The taxa are well known within the regional biostratigraphy community as important age markers, but have never been formally described. Thalassiphora lacunata sp. nov. differs from Thalassiphora delicata by possessing large, subcircular openings on the dorsal surface of the periphragm. For Spiniferites magnificus sp. nov., the morphology of the processes and the development of high sutural crests are the main diagnostic features to distinguish this species from other species of the genus Spiniferites. Operculodinium magnum sp. nov. differs from other Operculodinium species by its larger size and thicker wall, but also the distinctive numerous solid, fibrous processes. Spiniferites magnificus sp. nov. and O. magnum sp. nov. have a stratigraphic range restricted to the Danian. Thalassiphora lacunata sp. nov. has a short strati graphic range mainly restricted to the early Selandian. (C) 2018 Elsevier B.V. All rights reserved.	[Vieira, Manuel] Shell UK Ltd, 1 Altens Farm Rd, Aberdeen AB12 3FY, Scotland; [Mandi, Salih] RPS Ichron Ltd, Gadbrook Business Ctr, Century House, Northwich CW9 7TL, Cheshire, England; [Casas-Gallego, Manuel; Fenton, Jim] Robertson UK Ltd, Llandudno LL30 1SA, Conwy, Wales	Royal Dutch Shell	Vieira, M (通讯作者)，Shell UK Ltd, 1 Altens Farm Rd, Aberdeen AB12 3FY, Scotland.	Manuel.Vieira@Shell.com	Gallego, Manuel/ABE-8307-2020; Vieira, Manuel/AAY-4474-2020	Casas Gallego, Manuel/0000-0002-9802-9762; Vieira, Manuel/0000-0002-2389-4583				Ahmadi Z.M., 2003, MILLENNIUM ATLAS PET, P235; [Anonymous], 1996, Palynology: principles and applications; BENEDEK P N, 1981, Palaeontographica Abteilung B Palaeophytologie, V180, P39; Butschli O, 1885, PROTOZOA HG BRONNS K, P865; Dalland A., 1988, A lithostratigraphic scheme for the Mesozoic and Cenozoic succession offshore mid- and northern Norway; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Eaton GL., 1976, B BRIT MUS NAT HIST, V26; Eisenack A., 1954, Palaeontographica A, V105, P49; Eisenack A., 1960, Neues Jahrb. Geol. P.-M., P511; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42, P909; Gradstein FM, 2010, NEWSL STRATIGR, V44, P73, DOI 10.1127/0078-0421/2010/0005; GRADSTEIN FM, 1992, MICROPALEONTOLOGY, V38, P101, DOI 10.2307/1485991; Harland R, 1992, LITHOSTRATIGRAPHIC N; Isaken D., 1989, B NORW PETROL DIRECT, V5; Islam M.A., 1983, Revue de Micropaleontologie, V25, P231; LIENGJARERN M, 1980, Palaeontology (Oxford), V23, P475; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; Mangerud G, 1999, SPECIAL PUBLICATIONS, V133, P167; Mantell GA, 1850, ORGANIC REMAINS FORM; MANUM SB, 1979, REV PALAEOBOT PALYNO, V28, P237, DOI 10.1016/0034-6667(79)90026-5; Matsuoka Kazumi, 1997, Palynology, V21, P19; 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; Nohr-Hansen H, 2012, REV PALAEOBOT PALYNO, V178, P59, DOI 10.1016/j.revpalbo.2012.03.009; Pascher A., 1914, Berlin Ber D bot Ges, V32; SARJEANT W A S, 1970, Grana, V10, P74; Schioler P, 2005, J MICROPALAEONTOL, V24, P1, DOI 10.1144/jm.24.1.1; Slimani H, 2011, REV PALAEOBOT PALYNO, V168, P41, DOI 10.1016/j.revpalbo.2011.09.009; Stover L.E., 1978, GEOL SCI, V15, P300; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; THOMSEN E, 1985, Bulletin of the Geological Society of Denmark, V33, P341; Vieira M, 2018, PALYNOLOGY, V42, P180, DOI 10.1080/01916122.2017.1314390; WALL D., 1967, PALAEONTOLOGY, V10, P95; Williams G.L., 1985, P847; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Williams G.L., 1998, Mesozoic and Cenozoic Sequence Stratigra Phy of European Basins, V60, P764; WILLIAMS GL, 1966, B BRIT MUSEUM NATU S, V3, P176; Williams GL., 2000, ASS STRATIGRAPHIC PA, V37, P370	39	13	13	0	2	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	NOV	2018	258						256	264		10.1016/j.revpalbo.2018.09.002	http://dx.doi.org/10.1016/j.revpalbo.2018.09.002			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	HE0GX					2025-03-11	WOS:000452945900021
J	Pinyol-Gallemí, A; Pedersen, LF; Koski, M				Pinyol-Gallemi, Aleix; Pedersen, Lars-Flemming; Koski, Marja			Towards control of unwanted cyst-forming dinoflagellates in aquaculture systems: Knockout and recovery of <i>Pfiesteria</i> sp after peracetic acid exposure	AQUACULTURE RESEARCH			English	Article						cyst formation; disinfection; HABs; PAA; RAS; staining method	WATER; DISINFECTION; DEGRADATION		[Pinyol-Gallemi, Aleix; Koski, Marja] Tech Univ Denmark, Natl Inst Aquat Resources, Sect Oceans & Arctic, Lyngby, Denmark; [Pedersen, Lars-Flemming] Tech Univ Denmark, Natl Inst Aquat Resources, Sect Aquaculture, North Sea Res Ctr, Hirtshals, Denmark	Technical University of Denmark; Technical University of Denmark	Pinyol-Gallemí, A (通讯作者)，PISCO Grp, DK-2100 Copenhagen O, Denmark.	apinyolgallemi@gmail.com	Pedersen, Lars-Flemming/D-9919-2011	Pinyol Gallemi, Aleix/0000-0003-3453-8629; Koski, Marja/0000-0002-1860-9768; Pedersen, Lars-Flemming/0000-0002-8361-9268	Danish EPA [MST-141-00416, 667-00199]	Danish EPA	Danish EPA, Grant/Award Number: MST-141-00416, 667-00199	Anderson D. M., 2016, GLOBAL AQUACULTURE A; Antonelli M, 2006, ENVIRON SCI TECHNOL, V40, P4771, DOI 10.1021/es060273f; Bravo Isabel, 2014, Microorganisms, V2, P11; Falsanisi D, 2006, WATER QUAL RES J CAN, V41, P398, DOI 10.2166/wqrj.2006.043; Fistarol GO, 2004, ENVIRON MICROBIOL, V6, P791, DOI 10.1111/j.1462-2920.2004.00609.x; Ganini D, 2013, HARMFUL ALGAE, V27, P121, DOI 10.1016/j.hal.2013.05.002; Kremp A, 2009, LIMNOL OCEANOGR, V54, P1125, DOI 10.4319/lo.2009.54.4.1125; Litaker R., 2002, J PHYCOL, V463, P442; Liu DB, 2016, AQUACULT REP, V4, P136, DOI 10.1016/j.aqrep.2016.09.002; Liu DB, 2014, AQUACULT ENG, V60, P35, DOI 10.1016/j.aquaeng.2014.03.006; Moestrup O, 2014, HARMFUL ALGAE, V32, P33, DOI 10.1016/j.hal.2013.12.002; Noble Alicia C., 1996, Annual Review of Fish Diseases, V6, P65, DOI 10.1016/S0959-8030(96)90006-X; Pedersen LF, 2013, AQUACULT ENG, V53, P65, DOI 10.1016/j.aquaeng.2012.11.011; Pedersen LF, 2009, AQUACULTURE, V296, P246, DOI 10.1016/j.aquaculture.2009.08.021; Subramani P. A., 2017, Fish diseases: prevention and control strategies, P81; Toth GB, 2004, P ROY SOC B-BIOL SCI, V271, P733, DOI 10.1098/rspb.2003.2654; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Whyte JNCI, 2001, PHYCOLOGIA, V40, P298, DOI 10.2216/i0031-8884-40-3-298.1	18	3	3	2	14	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1355-557X	1365-2109		AQUAC RES	Aquac. Res.	NOV	2018	49	11					3682	3685		10.1111/are.13815	http://dx.doi.org/10.1111/are.13815			4	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	GV9ZH		gold			2025-03-11	WOS:000446520500023
J	Potvin, É; Kim, SY; Yang, EJ; Head, MJ; Kim, HC; Nam, SI; Yim, JH; Kang, SH				Potvin, Eric; Kim, So-Young; Yang, Eun Jin; Head, Martin J.; Kim, Hyun-cheol; Nam, Seung-Il; Yim, Joung Han; Kang, Sung-Ho			<i>Islandinium minutum</i> subsp <i>barbatum</i> subsp nov (Dinoflagellata), a New Organic-Walled Dinoflagellate Cyst from the Western Arctic: Morphology, Phylogenetic Position Based on SSU rDNA and LSU rDNA, and Distribution	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Arctic Ocean; Echinidinium karaense; modern sediment; "Polykrikos quadratus"; Polykrikos sp Arctic morphotype; ribosomal DNA; round brown spiny cyst; single-cell PCR	SEA-SURFACE CONDITIONS; SAND-DWELLING DINOFLAGELLATE; NORTHERN NORTH-ATLANTIC; THECA RELATIONSHIP; HYDROGRAPHIC CONDITIONS; MOLECULAR PHYLOGENY; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; BAFFIN-BAY; ICE COVER	A study of modern sediment from the Western Arctic has revealed the presence of a distinctive brown-colored cyst with a spherical central body bearing unbranched processes that are usually solid with a small basal pericoel. Distinctive barbs project from some processes, and process tips are usually minutely expanded into conjoined barbs. The archeopyle is apical and saphopylic. This cyst corresponds to Islandinium? cezare morphotype 2 of Head et al. (2001, J. Quat. Sci., 16:621). Phylogenetic analyses based on the small and large subunit rRNA genes infer close relationship with Islandinium minutum, the type of which is that of the genus. Re-examination of specimens of I. minutum reveals the presence of minute barbs on its processes, but differences with Islandinium? cezare morphotype 2 remain based on size, process distribution, and barb development. Furthermore, the internal transcribed spacer shows I. minutum to be distinct from this morphotype. On the basis of these small but discrete differences, we propose the new subspecies Islandinium minutum subsp. barbatum subsp. nov. Molecular sequencing of other cysts encountered, namely Echinidinium karaense, an unidentified flattened cyst, and "Polykrikos quadratus", places them in the Monovela clade, the latter showing greater morphological variability than previously thought.	[Potvin, Eric; Kim, So-Young; Yang, Eun Jin; Kang, Sung-Ho] Korea Polar Res Inst, Div Polar Ocean Sci, 26 Songdomirae Ro, Incheon 406840, South Korea; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Kim, Hyun-cheol] Korea Polar Res Inst, Unit Arctic Sea Ice Predict, Incheon 406840, South Korea; [Nam, Seung-Il] Korea Polar Res Inst, Div Polar Paleoenvironm, Incheon 406840, South Korea; [Yim, Joung Han] Korea Polar Res Inst, Div Polar Life Sci, Incheon 406840, South Korea	Korea Polar Research Institute (KOPRI); Brock University; Korea Polar Research Institute (KOPRI); Korea Polar Research Institute (KOPRI); Korea Polar Research Institute (KOPRI)	Kang, SH (通讯作者)，Korea Polar Res Inst, Div Polar Ocean Sci, 26 Songdomirae Ro, Incheon 406840, South Korea.	shkang@kopri.re.kr	Kim, So-Young/JFS-7698-2023; Kim, Hyun-Cheol/AAP-1250-2020	Yang, Eun Jin/0000-0002-8639-5968; Kim, Hyun-Cheol/0000-0002-6831-9291; Head, Martin/0000-0003-3026-5483	Ministry of Oceans and Fisheries of Korea [PM17040]; program on the Commercialization of Useful Metabolites from Polar Organisms from the Korea Polar Research Institute [PE17100]; NRF of Korea - the Korean Government [NRF-2015M1A5A1037243]; Danish Council for Independent Research, Natural Science [12-126709/FNU]; Natural Sciences and Engineering Research Council of Canada	Ministry of Oceans and Fisheries of Korea; program on the Commercialization of Useful Metabolites from Polar Organisms from the Korea Polar Research Institute(Korea Polar Research Institute of Marine Research Placement (KOPRI)); NRF of Korea - the Korean Government; Danish Council for Independent Research, Natural Science(Det Frie Forskningsrad (DFF)); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	We are grateful to the anonymous reviewers for their valuable suggestions. We also thank Nicolas Van Nieuwenhove who provided sediment from the Labrador Sea. This research was part of the project "K-AOOS (KOPRI, PM17040)" funded by the Ministry of Oceans and Fisheries of Korea. This research was also supported by the program on the Commercialization of Useful Metabolites from Polar Organisms (PE17100) from the Korea Polar Research Institute, the NRF of Korea Grant funded by the Korean Government (NRF-2015M1A5A1037243), as well as the Danish Council for Independent Research, Natural Science (project 12-126709/FNU). Martin J. Head acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant.	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Eukaryot. Microbiol.	NOV-DEC	2018	65	6					750	772		10.1111/jeu.12518	http://dx.doi.org/10.1111/jeu.12518			23	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	HC4OR	29575394				2025-03-11	WOS:000451783600001
J	Tomasovych, A; Gallmetzer, I; Haselmair, A; Kaufman, DS; Kralj, M; Cassin, D; Zonta, R; Zuschin, M				Tomasovych, Adam; Gallmetzer, Ivo; Haselmair, Alexandra; Kaufman, Darrell S.; Kralj, Martina; Cassin, Daniele; Zonta, Roberto; Zuschin, Martin			Tracing the effects of eutrophication on molluscan communities in sediment cores: outbreaks of an opportunistic species coincide with reduced bioturbation and high frequency of hypoxia in the Adriatic Sea	PALEOBIOLOGY			English	Article							GULF-OF-TRIESTE; GREAT-BARRIER-REEF; LONG-TERM CHANGES; ORGANIC-MATTER; PO PLAIN; MARINE-SEDIMENTS; ENVIRONMENTAL-CHANGES; DINOFLAGELLATE CYSTS; TEMPORAL RESOLUTION; DEATH ASSEMBLAGES	Estimating the effects and timing of anthropogenic impacts on the composition of macrobenthic communities is challenging, because early twentieth-century surveys are sparse and the corresponding intervals in sedimentary sequences are mixed by bioturbation. Here, to assess the effects of eutrophication on macrobenthic communities in the northern Adriatic Sea, we account for mixing with dating of the bivalve Corbula gibba at two stations with high accumulation (Po prodelta) and one station with moderate accumulation (Isonzo prodelta). We find that, first, pervasively bioturbated muds typical of highstand conditions deposited in the early twentieth century were replaced by muds with relicts of flood layers and high content of total organic carbon (TOC) deposited in the late twentieth century at the Po prodelta. The twentieth century shelly muds at the Isonzo prodelta are amalgamated but also show an upward increase in TOC. Second, dating of C. gibba shells shows that the shift from the early to the late twentieth century is characterized by a decrease in stratigraphic disorder and by an increase in temporal resolution of assemblages from similar to 25-50 years to similar to 10-20 years in both regions. This shift reflects a decline in the depth of the fully mixed layer from more than 20 cm to a few centimeters. Third, the increase in abundance of the opportunistic species C. gibba and the loss of formerly abundant, hypoxia-sensitive species coincided with the decline in bioturbation, higher preservation of organic matter, and higher frequency of seasonal hypoxia in both regions. This depositional and ecosystem regime shift occurred in ca. a.d. 1950. Therefore, the effects of enhanced food supply on macrobenthic communities were overwhelmed by oxygen depletion, even when hypoxic conditions were limited to few weeks per year in the northern Adriatic Sea. Preservation of trends in molluscan abundance and flood events in cores was enhanced by higher frequency of hypoxia that reduced bioturbation in the late twentieth century.	[Tomasovych, Adam] Slovak Acad Sci, Earth Sci Inst, Dubravska Cesta 9, Bratislava 84005, Slovakia; [Gallmetzer, Ivo; Haselmair, Alexandra; Zuschin, Martin] Univ Vienna, Dept Palaeontol, Althanstr 14, A-1090 Vienna, Austria; [Kaufman, Darrell S.] No Arizona Univ, Sch Earth Sci & Environm Sustainabil, Campus Box 4099, Flagstaff, AZ 86011 USA; [Kralj, Martina] Ist Nazl Oceanog & Geofis Sperimentale, Via A Piccard 54, I-34014 Trieste, Italy; [Cassin, Daniele; Zonta, Roberto] CNR, Ist Sci Marine, Castello 2737-F, I-30122 Venice, Italy	Slovak Academy of Sciences; Earth Science Institute, SAS; University of Vienna; Northern Arizona University; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR)	Tomasovych, A (通讯作者)，Slovak Acad Sci, Earth Sci Inst, Dubravska Cesta 9, Bratislava 84005, Slovakia.	geoltoma@savba.sk; ivo.gallmetzer@univie.ac.at; alexandra.haselmair@univie.ac.at; Darrell.Kaufman@nau.edu; mkralj@inogs.it; daniele.cassin@ve.ismar.cnr.it; roberto.zonta@ve.ismar.cnr.it; martin.zuschin@univie.ac.at	Kaufman, Darrell/A-2471-2008; CASSIN, DANIELE/LXU-7801-2024; Zuschin, Martin/M-9951-2016; Tomasovych, Adam/C-9623-2010	Kralj, Martina/0000-0003-1544-5515; Zuschin, Martin/0000-0002-5235-0198; Tomasovych, Adam/0000-0002-0471-9480; CASSIN, DANIELE/0000-0001-7517-7597	Austrian Science Fund (FWF) [P24901]; Slovak Research and Development Agency [APVV 17-0555]; Slovak Grant Agency [VEGA 0136-15]; Austrian Science Fund (FWF) [P24901] Funding Source: Austrian Science Fund (FWF)	Austrian Science Fund (FWF)(Austrian Science Fund (FWF)); Slovak Research and Development Agency(Slovak Research and Development Agency); Slovak Grant Agency(Vedecka grantova agentura MSVVaS SR a SAV (VEGA)); Austrian Science Fund (FWF)(Austrian Science Fund (FWF))	We thank M. Aberhan, L. C. Anderson, and one anonymous reviewer for comments. This study was funded by the Austrian Science Fund (FWF project P24901), the Slovak Research and Development Agency (APVV 17-0555), and the Slovak Grant Agency (VEGA 0136-15). We thank J. Sedmak and F. Perco for help with sampling, D. A. Garcia Ramos for help with determination of trace fossils, and K. Whitacre for amino acid analyses. The authors would like to thank to M. Celio of ARPAFVG for onboard activities and hydrological data.	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J	Pestchevitskaya, EB				Pestchevitskaya, E. B.			Morphology, Systematics, and Stratigraphic Significance of the Dinocyst Genus <i>Dingodinium</i>	PALEONTOLOGICAL JOURNAL			English	Article						dinocysts; Dingodinium; morphology; systematics; Jurassic; Cretaceous	JURASSIC-CRETACEOUS BOUNDARY; DINOFLAGELLATE CYSTS; BIOSTRATIGRAPHY	New material from the Upper Kimmeridgian and Volgian of the Gorodishche section (Ulyanovsk Region, Russia) allows a more accurate definition of the tabulation formula and archeopyle morphology of the dinocyst genus Dingodinium. The partiform pattern of the antapex and morphological features of the epicyst indicate that the genus Dingodinium should be attributed to the family Cladopyxiaceae of the suborder Cladopyxiineae. The genus Dingodinium as well as the species D. albertii, D. jurassicum, and D. tuberosum are revised, and a new species, D. nequeas, is described. In addition, the published data on Jurassic and Cretaceous species of the genus Dingodinium are analyzed and morphological criteria allowing their identification are recognized. Many species have a wide geographic distribution. Some species can be regarded as stratigraphically important for certain intervals of the Jurassic and Cretaceous.	[Pestchevitskaya, E. B.] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences	Pestchevitskaya, EB (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia.	PeschevickayaEB@ipgg.sbras.ru		Pestchevitskaya, Ekaterina/0000-0001-8174-0737	Presidium of the Russian Academy of Sciences [IX.126.1.3]; RSF Project [18-17-00038]; IGSP Projects [608, 632]; Russian Foundation for Basic Research [18-17-00038]; Russian Science Foundation [18-17-00038] Funding Source: Russian Science Foundation	Presidium of the Russian Academy of Sciences(Russian Academy of Sciences); RSF Project(Russian Science Foundation (RSF)); IGSP Projects; Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Russian Science Foundation(Russian Science Foundation (RSF))	I am sincerely grateful to V.V. Mitta for his leadership in the fieldwork during a joint expedition of the A.A. Borissiak Paleontological Institute, Russian Academy of Sciences and Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences. I also thank the reviewers and the Editorial Office for attentive treatment of the manuscript, valuable comments and suggestions that helped to present the study and improve the paper. The study was supported by the Presidium of the Russian Academy of Sciences, project IX.126.1.3, RSF Project no. 18-17-00038, IGSP Projects 608 and 632, and the Russian Foundation for Basic Research, project no. 18-17-00038.	AARHUS N, 1986, NORSK GEOL TIDSSKR, V66, P17; Abbink OA, 2001, P YORKS GEOL SOC, V53, P275, DOI 10.1144/pygs.53.4.275; Alberti G., 1961, Palaeontographica, V116, P1; BALDUZZI A, 1992, J AFR EARTH SCI, V15, P405, DOI 10.1016/0899-5362(92)90025-8; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BRIDEAUX W., 1971, PALAEONTOGRAPHICA B, V135, P53; BURGER D, 1982, Palynology, V6, P161; Cookson I. C., 1958, Proceedings of the Royal Society of Victoria N S, V70, P19; DAVEY R. 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J	Steads, DT; Batten, DJ				Steads, Darrin T.; Batten, David J.			Palynology of the Lower Cretaceous Hundleby Clay Member of the Claxby Ironstone Formation in eastern England and its biostratigraphic and palaeoenvironmental significance	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article							DINOFLAGELLATE CYSTS; EISENACK 1958; BASIN	Palynomorph assemblages recovered from five samples of the Hundleby Clay Member of the Claxby Ironstone Formation contain abundant dinoflagellate cysts and miospores (spores and pollen grains). The cyst assemblages are sufficiently diverse to enable an age determination of early Valanginian for all five samples, although it is possible that evidence from the highest two samples indicates a younger age, but no younger than earliest Hauterivian. The miospore assemblage is consistent with these suggestions. A close comparison can be made with palynomorph assemblages from the Speeton Clay Formation at outcrop in East Yorkshire, and indicates a possible correlation with Beds D4-D3 (Paratollia-Polyptychites ammonite zones), supporting the age determination. The overall composition of the palynological matter recovered from each sample, i.e. their palynofacies, suggests that the whole of the sedimentary succession accumulated in a nearshore marine setting, with deposits at the base of the exposure (samples 1 and 2) reflecting a more distal shelf environment than those from higher up and at the top of the section examined (samples 4, 5 and 3).	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Yorks. Geol. Soc.	NOV	2018	62		2				133	141		10.1144/pygs2018-006	http://dx.doi.org/10.1144/pygs2018-006			9	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GZ0KR					2025-03-11	WOS:000449052100007
J	Smelror, M; Fossum, K; Dypvik, H; Hudson, W; Mweneinda, A				Smelror, Morten; Fossum, Katrine; Dypvik, Henning; Hudson, Wellington; Mweneinda, Amina			Late Jurassic-Early Cretaceous palynostratigraphy of the onshore Mandawa Basin, southeastern Tanzania	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article							ROVUMA BASIN; TENDAGURU BEDS; ASSEMBLAGES; HISTORY; POLLEN	New palynostratigraphic data are presented for Upper Jurassic and Lower Cretaceous formations of the Mandawa Basin, southeastern Tanzania. A Late Jurassic (Kimmeridgian-Tithonian) age is confirmed for the Kipatimu Formation, from which the terrestrial sporomorphs allow a rough correlation to the mid Oxfordian-Tithonian Classopollis-Araucariacites-Shanbeipollenits Assemblage Zone. A dinoflagellate cyst assemblage recorded in the Mitole Formation correlates to the Dingodinium jurassicum-Kilwocysta assemblage as described from the Tithonian Trigonia smeei Bed of the Tendaguru Hill, southeast Tanzania. Dinoflagellate cyst assemblages in the upper Nalwehe Formation contain species typical of the Hauterivian-Barremian, while the Kihuluhulu Formation contains marine microfloras of Aptian to Albian ages. The palynological records confirm the presence of sediments related to profound marine transgressions and subsequent sea-level high-stands in the Late Jurassic (Kimmeridgian-Tihonian) and in the late Early Cretaceous (Aptian-Albian). (C) 2018 Elsevier B.V. All rights reserved.	[Smelror, Morten] Geol Survey Norway, POB 6315, N-7491 Trondheim, Norway; [Fossum, Katrine; Dypvik, Henning] Univ Oslo, Dept Geosci, POB 1047, N-0316 Oslo, Norway; [Hudson, Wellington; Mweneinda, Amina] Tanzania Petr Dev Corp, POB 2774, Dar Es Salaam, Tanzania	Geological Survey of Norway; University of Oslo	Smelror, M (通讯作者)，Geol Survey Norway, POB 6315, N-7491 Trondheim, Norway.	Morten.Smelror@NGU.NO		Fossum, Katrine/0000-0003-3937-271X; Smelror, Morten/0000-0002-9593-648X	Tanzania Petroleum Development Corporation; Statoil (Tanzania)	Tanzania Petroleum Development Corporation; Statoil (Tanzania)	Thanks are due to Tanzania Petroleum Development Corporation and Statoil (Tanzania) for supporting the Mandawa Basin Project, the many team members of the Mandawa Basin project, and to Mufak Said Naoroz (UiO) for preparing the palynological slides. Constructive comments on the manuscript by Przemyslaw Gedl and an anonymous reviewer greatly improved the final paper.	Backhouse J., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P205; BALDUZZI A, 1992, J AFR EARTH SCI, V15, P405, DOI 10.1016/0899-5362(92)90025-8; Barss MS, 1973, GEOL SURV CANADA, V73, P22; Brink M., 2015, 1 EAGE E AFR PETR GE; Costa L.I., 1992, P99; Dypvik H, 2015, E AFR PETR C EXH 4 6; Hancox PJ, 2002, J AFR EARTH SCI, V34, P291, DOI 10.1016/S0899-5362(02)00028-3; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Hudson W.E., 2011, THESIS, P357; HUGHES NF, 1987, REV PALAEOBOT PALYNO, V50, P255, DOI 10.1016/0034-6667(87)90003-0; JARZEN D M, 1981, Pollen et Spores, V23, P149; Kapilima S., 2003, Tanzan. J. Sci., V29, P1, DOI DOI 10.4314/TJS.V29I1.18362; Kent P. E., 1971, NATURAL ENV RES COUN, P1; KENT PE, 1972, NATURE, V238, P147, DOI 10.1038/238147a0; Key RM, 2008, S AFR J GEOL, V111, P89, DOI 10.2113/gssajg.111.1.89; Lashin G. M. A., 2007, J APPL SCI, V7, P1304; MBEDE EI, 1991, J AFR EARTH SCI, V13, P291, DOI 10.1016/0899-5362(91)90092-D; Msaky Emma S., 2007, Paleontological Research, V11, P41, DOI 10.2517/1342-8144(2007)11[41:OODCGW]2.0.CO;2; Mweneinda, 2014, THESIS, P210; Riding J.B., 1992, P7; Said A, 2015, J AFR EARTH SCI, V111, P288, DOI 10.1016/j.jafrearsci.2015.08.012; Savelieva YN, 2017, GEOL CARPATH, V68, P517, DOI 10.1515/geoca-2017-0034; Schrank E, 2005, PALYNOLOGY, V29, P49, DOI 10.2113/29.1.49; Schrank E, 2010, PALYNOLOGY, V34, P3, DOI 10.1080/01916121003620106; Schrank Eckart, 1999, Mitteilungen aus dem Museum fuer Naturkunde in Berlin Geowissenschaftliche Reihe, V2, P171; Smelror M, 2008, PALYNOLOGY, V32, P63, DOI 10.1080/01916122.2008.9989650; SRIVASTAVA SK, 1987, GEOBIOS-LYON, V20, P5, DOI 10.1016/S0016-6995(87)80057-8; Srivastava V, 1999, PALAEOECO A, V26, P31; Stevens J., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P185; Williams G.L., 2017, AM ASS STRATIGRAPHIC, V2; [No title captured]; [No title captured]	32	7	7	0	6	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	NOV	2018	258						248	255		10.1016/j.revpalbo.2018.09.001	http://dx.doi.org/10.1016/j.revpalbo.2018.09.001			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	HE0GX					2025-03-11	WOS:000452945900020
J	Langgut, D; Almogi-Labin, A; Bar-Matthews, M; Pickarski, N; Weinstein-Evron, M				Langgut, Dafna; Almogi-Labin, Ahuva; Bar-Matthews, Miryam; Pickarski, Nadine; Weinstein-Evron, Mina			Evidence for a humid interval at ∼56-44 ka in the Levant and its potential link to modern humans dispersal out of Africa	JOURNAL OF HUMAN EVOLUTION			English	Article						Modern humans; Initial Upper Paleolithic; MIS 3; Levant; Pollen; Middle-Upper Paleolithic transition	EASTERN MEDITERRANEAN REGION; LAST GLACIAL PERIOD; SAPROPEL FORMATION; NORTH-ATLANTIC; SOREQ CAVE; SOUTHERN LEVANT; HEINRICH EVENTS; ISOTOPE RECORDS; CLIMATE CHANGES; ORGANIC-MATTER	This study provides a detailed reconstruction of the paleoenvironmental conditions that prevailed during one of the periods of modern human migration out of Africa and their occupation of the Eastern Mediterranean-Levant during the Late Middle Paleolithic-Early Upper Paleolithic. Tracing the past vegetation and climate within the Eastern Mediterranean-Levant region is largely based on a southeastern Mediterranean marine pollen record covering the last 90 kyr (core MD-9509). The various palynomorphs were linked to distinct vegetation zones that were correlated to the two climate systems affecting the study area: the low-latitude monsoon system and the North Atlantic-Mediterranean climate system. The bioprovince palynological markers show that during the period between similar to 56 and 44 ka, which covers the early part of Marine Isotope Stage 3 (MIS 3), there was an increase in transportation of pollen from Nilotic origin and a rise in dinoflagellate cyst ratios. These changes coincided with maximum insolation values at 65 degrees N, which led to an enhancement in Nile River discharge into the Eastern Mediterranean following the intensification of the African monsoonal system. At the same time, the rise in Mediterranean arboreal pollen values (broadleaved, coniferous and deciduous temperate trees) is most likely driven by increased precipitation related to the intensification of the North Atlantic-Mediterranean climate system. The similar to 56-44 ka wet event coincides with Dansgaard-Oeschger interstadials 14 and 12 and with a warming phase in the Levant, as evidenced by the melting of permafrost along the higher elevations of Mount Hermon. We suggest that African modern humans were able to cross the harsher arid areas due to the intensification of the monsoonal system during the first part of MIS 3, and inhabit the Eastern Mediterranean-Levant region where climatic conditions were favorable (wetter and warmer), even in the currently semiarid/steppe regions. (C) 2018 Elsevier Ltd. All rights reserved.	[Langgut, Dafna] Tel Aviv Univ, Steinhardt Museum Nat Hist, Inst Archaeol, Lab Archaeobot & Ancient Environm, POB 39040, IL-6997801 Tel Aviv, Israel; [Almogi-Labin, Ahuva; Bar-Matthews, Miryam] Geol Survey Israel, 30 Malkhe Israel St, IL-9550161 Jerusalem, Israel; [Pickarski, Nadine] Univ Bonn, Steinmann Inst Geol Mineral & Paleontol, Nussallee 8, D-53115 Bonn, Germany; [Weinstein-Evron, Mina] Univ Haifa, Zinman Inst Archaeol, Palynol Lab, IL-3498838 Haifa, Israel	Tel Aviv University; Geological Survey Israel; University of Bonn; University of Haifa	Langgut, D (通讯作者)，Tel Aviv Univ, Steinhardt Museum Nat Hist, Inst Archaeol, Lab Archaeobot & Ancient Environm, POB 39040, IL-6997801 Tel Aviv, Israel.	langgut@post.tau.ac.il		Almogi-Labin, Ahuva/0000-0002-4082-7120; Langgut, Dafna/0000-0002-4824-1044	Israel Science Foundation [20/01-13.0, 910/05]; Ministry of National Infrastructures	Israel Science Foundation(Israel Science Foundation); Ministry of National Infrastructures	The research was supported by grants no. 20/01-13.0 and 910/05 from the Israel Science Foundation and by the Ministry of National Infrastructures. We thank the master, crew and scientists aboard R/V 'Marion Dufresne' for their assistance, with special thanks to Dr. Martine Paterne from Gif sur Yvette, France. We gratefully acknowledge M. Kitin for his technical help with the preparation of the palynological samples and M. Cavanagh for drawing Figures 1 and 2. We also wish to thank Dr. O. Barzilai for his critical comments on an early draft, which helped to improve the manuscript, and the two anonymous reviewers for their suggestions and comments.	Adam D. 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Israel and Jordan	161	28	29	2	25	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0047-2484			J HUM EVOL	J. Hum. Evol.	NOV	2018	124						75	90		10.1016/j.jhevol.2018.08.002	http://dx.doi.org/10.1016/j.jhevol.2018.08.002			16	Anthropology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Anthropology; Evolutionary Biology	GX1MN	30177446				2025-03-11	WOS:000447481500007
J	Mansour, A; Tahoun, SS				Mansour, Ahmed; Tahoun, Sameh S.			Palynological and palaeoenvironmental analyses of the upper Albian-Cenomanian succession in Gindi Basin, Egypt: Implication for transgressive/regressive systems tracts	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynology; Palynofacies; Sequence stratigraphy; Albian; Cenomanian; Gindi Basin; Western desert; Egypt	NORTH-WESTERN DESERT; SEA-LEVEL CHANGES; CRETACEOUS TERTIARY BOUNDARY; SEQUENCE STRATIGRAPHY; OIL-FIELD; DINOFLAGELLATE STRATIGRAPHY; UNITED-STATES; PALYNOFACIES; WELL; SEDIMENTS	The current contribution illustrates the advantage of the use of quantitative palynological data to palaeoenvironmentally differentiate the similar-looking monotonous, thick clastic interval of the Kharita, Bahariya and Abu Roash "G" units in Gindi Basin, Egypt. The present study aims also to the utilization of the upper Albian-Cenomanian quantitative palynological and palynofacies data and their integral interpretation in a sequence stratigraphic context. The recovered palynomorph assemblages with moderately diverse sporomorphs and dinoflagellate cysts, show poor to fair preservation. Around 47 species of pollen grains, 37 of dinoflagellate cysts and 36 species of pteridophytic spores have been recorded from two sections encountered in El Sagha-1A and BRE 6-1 wells drilled in Gindi Basin; however, achritarchs, microforaminiferal test linings and freshwater algae are impoverished and sparsely documented through the studied intervals. Based on the first downhole appearances (FDAs) of the recovered marker taxa, the encountered Abu Roash "G", Bahariya and the upper Kharita units are palynologically dated as late Cenomanian, early-middle Cenomanian and late Albian, respectively. Relative sea level fluctuation is particularly relevant and deduced from various palynological parameters mainly the terrestrial:marine (T:M) ratio and the palynological marine index (PMI). Based on the vertical stratigraphic distribution of the palynofacies along with the relative variations of the terrestrial versus marine palynomorphs, five complete (SQ1-SQ5) third order transgressive-regressive sequences and incomplete one are defined in El Sagha-1A in comparison to six complete (SQ2-SQ7) and one incomplete (SQ1) are constructed in BRE 6-1. Reliance on distinctive palynofacies assemblages, differentiated based on the relative composition of particulate organic matter constituents, four depositional palaeoenvironments were interpreted for the studied intervals. The Kharita and Bahariya formations were elucidated to be deposited in fluctuating marginal-shallow and proximal inner neritic marine environments. However, the sea level remarkably showed a continued rising which brought the inner-middle neritic conditions of the Abu Roash "G" Member during late Cenomanian.	[Mansour, Ahmed] Menia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt; [Tahoun, Sameh S.] Cairo Univ, Fac Sci, Geol Dept, Giza 12613, Egypt	Egyptian Knowledge Bank (EKB); Minia University; Egyptian Knowledge Bank (EKB); Cairo University	Mansour, A (通讯作者)，Menia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt.	ahmedmans48@mu.edu.eg; stahoun@yahoo.com	Mansour, Ahmed/AAR-4969-2020	Tahoun, Sameh S./0000-0002-0425-8848; Mansour, Ahmed/0000-0003-2466-7494				Aadland A.I., 1972, P 8 AR PETR C ALG AL, P19; [Anonymous], 1987, EARTH SCI SERIES; [Anonymous], 1992, Western Desert, oil and gas fields (A comprehensive overview), P431; Arai M., 1992, B S CRETACEO BRASIL, V2, P27; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; Batten D. 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J	Fischer, AD; Brosnahan, ML; Anderson, DM				Fischer, Alexis D.; Brosnahan, Michael L.; Anderson, Donald M.			Quantitative Response of <i>Alexandrium catenella</i> Cyst Dormancy to Cold Exposure	PROTIST			English	Article						Resting cyst; dinoflagellate; dormancy; chilling; germination; endogenous clock	EASTERN BERING-SEA; LIFE-CYCLE EVENTS; GONYAULAX-TAMARENSIS; RESTING CYSTS; PUGET-SOUND; VERTICAL MIGRATION; SHELLFISH TOXICITY; DINOPHYCEAE CYSTS; BUD DORMANCY; CHUKCHI SEA	Many dinoflagellate cysts experience dormancy, a reversible state that prevents germination during unfavorable periods. Several of these species also cause harmful algal blooms (HABs), so a quantitative understanding of dormancy cycling is desired for better prediction and mitigation of bloom impacts. This study examines the effect of cold exposure on the duration of dormancy in Alexandrium catenella, a HAB dinoflagellate that causes paralytic shellfish poisoning (PSP). Mature, dormant cysts from Nauset Marsh (Cape Cod, MA USA) were stored at low but above freezing temperatures for up to six months. Dormancy status was then determined at regular intervals using a germination assay. Dormancy timing was variable among temperatures and was shorter in colder treatments, but the differences collapse when temperature and duration of storage are scaled by chilling-units (CU), a common horticultural predictor of plant and insect development in response to weather. Cysts within Nauset meet a well-defined chilling requirement by late January, after which they are poised to germinate with the onset of favorable conditions in spring. Cysts thus modulate their dormancy cycles in response to their temperature history, enhancing the potential for new blooms and improving this species' adaptability to both unseasonable weather and new habitats/climate regimes. (C) 2018 Elsevier GmbH. All rights reserved.	[Fischer, Alexis D.; Brosnahan, Michael L.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Fischer, Alexis D.] Univ Calif Santa Cruz, Ocean Sci Dept, Santa Cruz, CA 95064 USA	Woods Hole Oceanographic Institution; University of California System; University of California Santa Cruz	Fischer, AD (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.; Fischer, AD (通讯作者)，Univ Calif Santa Cruz, Ocean Sci Dept, Santa Cruz, CA 95064 USA.	adfische@ucsc.edu	Fischer, Alexis/M-4531-2019	Brosnahan, Michael/0000-0002-2620-7638; Fischer, Alexis/0000-0002-8028-487X	National Science Foundation [OCE-0430724, OCE-0911031]; National Institute of Environmental Health Sciences [1P50ES01274201, 1P01ES021923]; National Park Service Cooperative Agreement [H238015504]; Friends of Cape Cod National Seashore	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)); National Park Service Cooperative Agreement; Friends of Cape Cod National Seashore	We are grateful to F. Correia and D. Kulis for their assistance with experimental monitoring and setup and to the many members of the Anderson lab for their assistance with sampling trips to Nauset. Many thanks to A. Solow for his sage statistical advice and to D. Ralston for his feedback. This work was supported by the National Science Foundation [OCE-0430724, OCE-0911031]; the National Institute of Environmental Health Sciences [1P50ES01274201, 1P01ES021923]; the National Park Service Cooperative Agreement [H238015504]; and the Friends of Cape Cod National Seashore.	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J	Witts, JD; Landman, NH; Garb, MP; Boas, C; Larina, E; Rovelli, R; Edwards, LE; Sherrell, RM; Cochran, JK				Witts, James D.; Landman, Neil H.; Garb, Matthew P.; Boas, Caitlin; Larina, Ekaterina; Rovelli, Remy; Edwards, Lucy E.; Sherrell, Robert M.; Cochran, J. Kirk			A fossiliferous spherule-rich bed at the Cretaceous-Paleogene (K-Pg) boundary in Mississippi, USA: Implications for the K-Pg mass extinction event in the Mississippi Embayment and Eastern Gulf Coastal Plain	CRETACEOUS RESEARCH			English	Article						Cretaceous; Paleogene; Ammonite; Chicxulub; Impact spherule; Mass extinction	CARBON-ISOTOPE EXCURSIONS; DANIAN STAGE PALEOCENE; HIGHEST AMMONITE ZONES; TERTIARY BOUNDARY; CHICXULUB IMPACT; BRAZOS RIVER; OF-MEXICO; STRATOTYPE SECTION; MONMOUTH COUNTY; ASTEROID IMPACT	We describe an outcrop of the Cretaceous-Paleogene (K-Pg) boundary exposed due to construction near New Albany, Union County, Mississippi. It consists of the Owl Creek Formation and overlying Clayton Formation. The Owl Creek Formation is rich in the ammonites Discoscaphites iris and Eubaculites carinatus, which, along with biostratigraphically important dinoflagellate cysts and calcareous nannofossils, indicate deposition occurred within the last 1 million years, most likely last 500 kyrs, of the Cretaceous. The base of the overlying Clayton Formation marks the K-Pg boundary, and consists of a 15-30 cm thick muddy, poorly sorted quartz sand containing abundant spherules representing ejecta derived from the Chicxulub impact event. Impact spherules range in size from 0.5 mm to 1 mm in diameter and are hollow and well preserved, with details such as smaller vesicular spherules enclosed within. The spherules are altered to clay minerals such as smectite and are typical of those found at K-Pg boundary sites in the Gulf of Mexico and beyond. Spherules are scattered throughout the bed, and surface counts suggest an average of 4 spherules per cm(2). Macrofossils within the spherule bed represent a rich fauna of ammonites, benthic molluscs (bivalves and gastropods), echinoids, as well as crabs and sharks. Macrofossil preservation ranges from whole to fragmentary, with most fossils preserved as internal moulds. The infill of the fossils is lithologically identical to the matrix of the spherule bed, including impact ejecta preserved within phragmocones and body chambers of ammonites, and differs from the underlying Owl Creek Formation. This suggests that the animals were either alive or loosely scattered on the sea floor at the time of deposition. Grain size changes indicate multiple events were responsible for deposition, and together with taphonomic evidence are consistent with dynamic high energy post-impact processes. Later sea level change during the Paleocene is responsible for a sharp contact at the top of the spherule bed. Geochemical evidence from the Owl Creek and Clayton Formations at this locality indicate numerous local paleoenvironmental changes affected the Mississippi Embayment at the time of the K-Pg boundary and mass extinction event. (C) 2018 Elsevier Ltd. All rights reserved.	[Witts, James D.; Landman, Neil H.] Amer Museum Nat Hist, Div Paleontol Invertebrates, New York, NY 10024 USA; [Garb, Matthew P.; Boas, Caitlin] CUNY Brooklyn Coll, Dept Earth & Environm Sci, Brooklyn, NY 11210 USA; [Larina, Ekaterina] Univ Southern Calif, Dept Earth Sci, Los Angeles, CA 90018 USA; [Rovelli, Remy] Univ New Mexico, Dept Earth & Planetary Sci, Albuquerque, NM 87131 USA; [Edwards, Lucy E.] US Geol Survey, Mail Stop 926A, Reston, VA 20192 USA; [Sherrell, Robert M.] Rutgers State Univ, Dept Marine & Coastal Sci, Piscataway, NJ 08901 USA; [Sherrell, Robert M.] Rutgers State Univ, Dept Earth & Planetary Sci, Piscataway, NJ 08901 USA; [Cochran, J. Kirk] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA	American Museum of Natural History (AMNH); City University of New York (CUNY) System; Brooklyn College (CUNY); University of Southern California; University of New Mexico; United States Department of the Interior; United States Geological Survey; Rutgers University System; Rutgers University New Brunswick; Rutgers University System; Rutgers University New Brunswick; State University of New York (SUNY) System; Stony Brook University	Witts, JD (通讯作者)，Amer Museum Nat Hist, Div Paleontol Invertebrates, New York, NY 10024 USA.	jwitts@amnh.org		Witts, James/0000-0002-4002-415X; Edwards, Lucy/0000-0003-4075-3317	Lerner-Gray Fund for Marine Research; Richard Gilder Graduate School, American Museum of Natural History; Norman Newell Fund	Lerner-Gray Fund for Marine Research; Richard Gilder Graduate School, American Museum of Natural History; Norman Newell Fund	Thanks to W.C. Smallwood (owner of the site) and George Phillips (Museum of Natural Science, Mississippi) for providing and facilitating access to the field site at AMNH locality 3481, and for help with fossil identification. We thank Corinne Myers, Jone Naujokaityte, the late Susan Klofak, and others for assistance in the field. Morgan Hill and George Harlow (AMNH) are thanked for assistance with SEM imaging and XRD analyses, Steve Thurston (AMNH) for help with figures and photography, and Alexandra Malinina and Kaixuan Bu (Rutgers University) for assistance with iridium determinations. We thank the handling editor Dr. Eduardo Koutsoukos and two anonymous reviewers for their helpful comments and suggestions which greatly improved the manuscript. This research was supported by the Lerner-Gray Fund for Marine Research and the Richard Gilder Graduate School, American Museum of Natural History, via a fellowship to James Witts. Additional support was provided by the Norman Newell Fund. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.	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Res.	NOV	2018	91						147	167		10.1016/j.cretres.2018.06.002	http://dx.doi.org/10.1016/j.cretres.2018.06.002			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	GR8LY		Green Submitted			2025-03-11	WOS:000442976600014
J	Razmjooei, MJ; Thibault, N; Kani, A; Dinarès-Turell, J; Pucéat, E; Shahriari, S; Radmacher, W; Jamali, AM; Ullmann, CV; Voigt, S; Cocquerez, T				Razmjooei, Mohammad J.; Thibault, Nicolas; Kani, Anoshiravan; Dinares-Turell, Jaume; Puceat, Emmanuelle; Shahriari, Samira; Radmacher, Wieslawa; Jamali, Amir Mohammad; Ullmann, Clemens V.; Voigt, Silke; Cocquerez, Theophile			Integrated bio- and carbon-isotope stratigraphy of the Upper Cretaceous Gurpi Formation (Iran): A new reference for the eastern Tethys and its implications for large-scale correlation of stage boundaries	CRETACEOUS RESEARCH			English	Article						Coniacian-Maastrichtian; Calcareous nannofossils; Planktic foraminifera; Dinoflagellate cysts; Carbon isotopes; Tethyan realm; Zagros	CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; PLANKTONIC FORAMINIFERAL BIOEVENTS; WESTERN INTERIOR BASIN; LOWER MAASTRICHTIAN CYCLOSTRATIGRAPHY; SEA-LEVEL CHANGE; BASQUE COUNTRY; CONIACIAN/SANTONIAN BOUNDARY; ASTRONOMICAL CALIBRATION; INOCERAMID BIVALVES; GLOBAL CORRELATION	A high-resolution stratigraphic analysis of the Upper Cretaceous Gurpi Formation has been undertaken in the Shahneshin section (Zagros Basin, Iran). New results on calcareous nannofossils, planktic foraminifers, dinoflagellate cysts and high-resolution carbon and oxygen stable isotopes form the basis of a reference section for the eastern Tethys that spans the upper Coniacian to the late Danian. Carbon-isotope correlation to Gubbio, Italy and the NW German chalk allows for the identification of many isotopic events as well as for the definition of new events in the Campanian and Maastrichtian. Our results allow for a review of the accurate position of the Coniacian/Santonian, Santonian/Campanian, and Campanian/Maastrichtian stage boundaries relative to carbon isotopes and plankton bioevents. The reliability of Coniacian to Maastrichtian planktic foraminifer, dinoflagellate cysts and calcareous nannofossil biohorizons is assessed. (C) 2018 Elsevier Ltd. All rights reserved.	[Razmjooei, Mohammad J.; Kani, Anoshiravan; Shahriari, Samira] Shahid Beheshti Univ, Dept Geol, Fac Earth Sci, Tehran, Iran; [Razmjooei, Mohammad J.; Thibault, Nicolas] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen, Denmark; [Dinares-Turell, Jaume] Ist Nazl Geofis & Vulcanol, Via Vigna Murata 605, I-00143 Rome, Italy; [Puceat, Emmanuelle; Cocquerez, Theophile] Univ Burgundy Franche Comte, CNRS, UMR 6282, Biogeosci, 6 Blvd Gabriel, F-21000 Dijon, France; [Radmacher, Wieslawa] Polish Acad Sci, Res Ctr Cracow, Inst Geol Sci, St Senacka 1, PL-31002 Krakow, Poland; [Jamali, Amir Mohammad] Natl Iranian Oil Co, Explorat Directorate, Tehran, Iran; [Ullmann, Clemens V.] Univ Exeter, Camborne Sch Mines & Environm, Penryn TR10 9FE, England; [Ullmann, Clemens V.] Univ Exeter, Sustainabil Inst, Penryn TR10 9FE, England; [Voigt, Silke] Goethe Univ Frankfurt, Inst Geosci, Altenhoferallee 1, D-60438 Frankfurt, Germany	Shahid Beheshti University; University of Copenhagen; Istituto Nazionale Geofisica e Vulcanologia (INGV); Centre National de la Recherche Scientifique (CNRS); Universite de Bourgogne; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; National Iranian Oil Company (NIOC); University of Exeter; University of Exeter; Goethe University Frankfurt	Razmjooei, MJ (通讯作者)，Shahid Beheshti Univ, Dept Geol, Fac Earth Sci, Tehran, Iran.	mjr@ign.ku.dk	Javad, Mohammad/ABG-1180-2020; Ullmann, Clemens/I-3227-2019; Radmacher, Wiesława/ABH-7042-2020; Thibault, Nicolas/B-1106-2013; Dinares-Turell, Jaume/G-2852-2011; Voigt, Silke/G-7270-2017	Thibault, Nicolas/0000-0003-4147-5531; razmjooei, mohammad javad/0000-0002-1165-7660; Dinares-Turell, Jaume/0000-0002-5546-2291; Voigt, Silke/0000-0002-2560-5933; Radmacher, Wieslawa/0000-0001-7316-3693	Carlsberg Foundation [2013-01-0425, CF16-0457]	Carlsberg Foundation(Carlsberg Foundation)	Special thanks go to Peyman, Salman, Farshid, Mostafa and Aref Razmjooei my great relatives and my friend Afshin Hashemi for helping us in the field as well as Johannes Monkenbusch for helpful suggestions. We thank the director of the sedimentology laboratory (Morteza Sharafpour) and the staff of central laboratory at Shahid Beheshti University for providing the laboratory facilities. The authors are grateful to Mehdi Namjouyan for his help in the course of this research. NT acknowledges the Carlsberg Foundation for funding this study (Carlsbergfondet 2013-01-0425 and CF16-0457). We thank Peter Harries, Irek Walaszczyk and an anonymous reviewer for their constructive criticism and useful comments and suggestions.	Akbar J. N. 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Res.	NOV	2018	91						312	340		10.1016/j.cretres.2018.07.002	http://dx.doi.org/10.1016/j.cretres.2018.07.002			29	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	GR8LY					2025-03-11	WOS:000442976600028
J	Skarlato, S; Filatova, N; Knyazev, N; Berdieva, M; Telesh, I				Skarlato, Sergei; Filatova, Natalya; Knyazev, Nikolay; Berdieva, Mariia; Telesh, Irena			Salinity stress response of the invasive dinoflagellate <i>Prorocentrum minimum</i>	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article; Proceedings Paper	Estuarine-and-Coastal-Sciences-Association (ECSA) 56th Conference on Coastal Systems in Transition - From a Natural to and Anthropogenically-Modified State	SEP 04-07, 2016	Bremen, GERMANY	Estuarine & Coastal Sci Assoc		Cell cycle; Dinoflagellates; Invasions; Mortality; Prorocentrum minimum; Salinity stress	PROTISTAN SPECIES-MAXIMUM; BALTIC SEA; CELL-CYCLE; MARINE-PHYTOPLANKTON; GRADIENT; NITROGEN; BLOOMS; DINOPHYCEAE; DIVERSITY; IMPACTS	Estuarine and coastal environments are vulnerable to alien species invasions. Many nonindigenous organisms demonstrate high ecological plasticity, which is particularly well expressed in unicellular eukaryotes. In this study, responses of the potentially toxic invasive dinoflagellate Prorocentrum minimum, initially acclimated to salinity 17 (control), to short-term stress by salinities 4, 8 and 35 were investigated experimentally by determination of mortality, alterations in cell cycle and chromosome fine structure, RNA synthesis and DNA replication. The percentage of dead cells within the P. minimum population after stress by critical salinity 8 was lower compared to the other tested conditions. Salinity stress caused only moderate impact on the cell cycle pattern; changes of chromosome fine structure at salinities 4 and 8 were evident though reversible. We disclosed the elevated RNA synthesis and DNA replication which can play a 'compensational' role by speeding up the metabolic (synthetic) activity of these protists at the critical salinity conditions. The increased RNA synthesis in phase G1 and additional DNA replication in phase S of the cell cycle likely enhance salinity tolerance and cause relatively low mortality of these micro-eukaryotes at salinity 8. We infer that the enhanced synthesis of DNA and RNA can be one of the advanced ecological strategies of P. minimum which along with the other cellular and physiological characteristics (small body size, planktonic mode of life, fast reproduction, high evolution rates, mixotrophy, ability to form cysts, etc.) helps these dinoflagellates to invade successfully and populate permanently coastal ecosystems, remaining highly competitive in the unstable brackishwater environments. (C) 2017 Elsevier Ltd. All rights reserved.	[Skarlato, Sergei; Filatova, Natalya; Knyazev, Nikolay; Berdieva, Mariia; Telesh, Irena] Russian Acad Sci, Inst Cytol, St Petersburg 194064, Russia; [Knyazev, Nikolay] St Petersburg Acad Univ, Nanotechnol Res & Educ Ctr, St Petersburg 194021, Russia; [Telesh, Irena] Russian Acad Sci, Inst Zool, St Petersburg 199034, Russia	Russian Academy of Sciences; St. Petersburg Scientific Centre of the Russian Academy of Sciences; Institute of Cytology RAS; Russian Academy of Sciences; St. Petersburg Scientific Centre of the Russian Academy of Sciences; St Petersburg Academic University; Russian Academy of Sciences; Zoological Institute of the Russian Academy of Sciences	Telesh, I (通讯作者)，Russian Acad Sci, Inst Cytol, St Petersburg 194064, Russia.	Irena.Telesh@zin.ru	Skarlato, Sergei/W-4663-2017; Telesh, Irena/N-4342-2016; Filatova, Natalia/AAF-1414-2021; Berdieva, Mariia/V-6811-2018; Knyazev, Nickolay/E-1870-2014	Berdieva, Mariia/0000-0002-5467-2713; Telesh, Irena/0000-0002-4167-3821; Skarlato, Sergei/0000-0001-7579-7227; Filatova, Natalia/0000-0001-9955-6612; Knyazev, Nickolay/0000-0002-7507-8051	Russian Science Foundation (Institute of Cytology RAS) [16-14-10116]; Russian Science Foundation [16-14-10116] Funding Source: Russian Science Foundation	Russian Science Foundation (Institute of Cytology RAS); Russian Science Foundation(Russian Science Foundation (RSF))	Three anonymous reviewers are acknowledged for their valuable comments and suggestions that allowed improving the manuscript significantly. The study was funded by the Russian Science Foundation (project 16-14-10116 at the Institute of Cytology RAS).	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Coast. Shelf Sci.	OCT 31	2018	211				SI		199	207		10.1016/j.ecss.2017.07.007	http://dx.doi.org/10.1016/j.ecss.2017.07.007			9	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology; Oceanography	GV5NE					2025-03-11	WOS:000446148100018
J	Chekar, M; Slimani, H; Jbari, H; Guédé, KE; Mahboub, I; Asebriy, L; Aassoumi, H				Chekar, Mouna; Slimani, Hamid; Jbari, Hassan; Guede, Kore Elysee; Mahboub, Imane; Asebriy, Lahcen; Aassoumi, Habiba			Eocene to Oligocene dinoflagellate cysts from the Tattofte section, western External Rif, northwestern Morocco: Biostratigraphy, paleoenvironments and paleoclimate	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinocysts; Lutetian; Bartonian; Chattian; MECO; Late Oligocene warming; Mediterranean	NORTH-SEA BASIN; CRETACEOUS-PALEOGENE BOUNDARY; OULED HADDOU; MIDDLE EOCENE; NEW-JERSEY; PALYNOLOGICAL APPROACH; ENVIRONMENTAL-CHANGES; THERMAL MAXIMUM; LEVEL CHANGE; PLIOCENE	The palynological analysis of the Eocene-Oligocene succession from the Tattofte section in the western External Rif (northwestern Morocco) reveals the presence of well-preserved and diverse assemblage, rich in dinoflagellate cysts (dinocysts). Qualitative analyses, especially of the dinocysts, differentiate the individual stages of the deposits, while quantitative analyses permit paleoenvironmental and paleoclimatic interpretations. We assign the lower part of the Tattofte section to the Middle Eocene (Lutetian and Bartonian) and its upper part to the Upper Oligocene (Chattian), and define a hiatus spanning the Late Eocene (Priabonian) and Early Oligocene (Rupelian). The dinocyst marker events used for the biostratigraphic interpretations include the first and last occurrences of marker species, such as Batiacasphaera compta, Castellodinium compactum, Cerebrocysta bartonensis, Distatodinium biffii, Distatodinium paradoxum, Distatodinium ellipticum, Enneadocysta arcuata, Homotryblium floripes, Hystrichokolpoma bullatum, Impagidinium velorwn, Lentinia serrata, Pentadiniurn imaginatum, Rhombodiniwn spinula, Saturnodiniwn perforaturn and Ynezidinium brevisulcatum, as well as the Chiropteridium spp. acmes. And we equate the Chattian with the dinocyst Distatodinium biffii Zone of Brinkhuis et al. (1992). Changes in the relative abundances of selected dinocyst groups, spores and pollen lead to the distinction, from oldest to youngest, of four marine environments: 1) marginal marine to coastal inner neritic under relatively warm-water during the Middle Eocene; 2) outer neritic to oceanic during a transgressive regime in the early Chattian; 3) fluctuating restricted to open marine in the middle Chattian; and 4) shallow coastal to open marine due to sea-level fall at the top of the section in the latest Chattian, suggested by the Chiropteridium spp. acmes. The acmes of selected thermophilic dinocyst taxa, such as Polysphaeridium spp. and Homotryblium spp. suggest warm water marine conditions, which may be related to the Middle Eocene climatic optimum (MECO) and Late Oligocene warming.	[Chekar, Mouna; Slimani, Hamid; Jbari, Hassan; Mahboub, Imane; Asebriy, Lahcen] Mohammed V Univ Rabat, Geobiodivers & Nat Patrimony Lab GEOBIO, Inst Sci, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco; [Guede, Kore Elysee] Univ Man, UFR Geol & Min Sci, BP 20, Man, Cote Ivoire; [Aassoumi, Habiba] Univ Abdelmalek Essaadi, Fac Sci, Dept Earth Sci, Lab Cartog & Digital Technol, Tetouan, Morocco	Mohammed V University in Rabat; Universite de Man; Abdelmalek Essaadi University of Tetouan	Slimani, H (通讯作者)，Mohammed V Univ Rabat, Geobiodivers & Nat Patrimony Lab GEOBIO, Inst Sci, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma	Elysee, Guede/ABE-3209-2021; Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913; Kore Elysee, Guede/0000-0003-1393-5078	University Mohammed V of Rabat [SVT 11/09]; National Center of Scientific Research, Morocco [URAC46]	University Mohammed V of Rabat(Mohammed V University in Rabat); National Center of Scientific Research, Morocco	This work was supported by the University Mohammed V of Rabat (Project SVT 11/09) and the National Center of Scientific Research (URAC46), Morocco. The authors are indebted to Achiles Gautier of the Paleontology Research Unit, Ghent University and Graham Williams of the Geological Survey of Canada who checked the English. The journal editor Isabel Montanez and three anonymous reviewers are kindly thanked for corrections and constructive comments that improved considerably the manuscript.	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OCT 15	2018	507						97	114		10.1016/j.palaeo.2018.07.004	http://dx.doi.org/10.1016/j.palaeo.2018.07.004			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	GQ8ZO					2025-03-11	WOS:000442055900008
J	Hartman, JD; Bijl, PK; Sangiorgi, F				Hartman, Julian D.; Bijl, Peter K.; Sangiorgi, Francesca			A review of the ecological affinities of marine organic microfossils from a Holocene record offshore of Adelie Land (East Antarctica)	JOURNAL OF MICROPALAEONTOLOGY			English	Review							WALLED DINOFLAGELLATE CYSTS; SEA-SURFACE CONDITIONS; TERRA-NOVA BAY; NON-POLLEN PALYNOMORPHS; KING-GEORGE-ISLAND; TIERRA-DEL-FUEGO; SOUTHERN-OCEAN; GYMNODINIUM-CATENATUM; ROSS SEA; ENVIRONMENTAL-CHANGE	Integrated Ocean Drilling Program (IODP) Expedition 318 recovered a similar to 170m long Holocene organic-rich sedimentary sequence at Site U1357. Located within the narrow but deep Adelie Basin close to the Antarctic margin, the site accumulated sediments at exceptionally high sedimentation rates, which resulted in extraordinary preservation of the organic sedimentary component. Here, we present an overview of 74 different mainly marine microfossil taxa and/or types found within the organic component of the sediment, which include the remains of unicellular and higher organisms from three eukaryotic kingdoms (Chromista, Plantae, and Animalia). These remains include phytoplanktonic (phototrophic dinoflagellates and prasinophytes) and very diverse zooplanktonic (heterotrophic dinoflagellates, tintinnids, copepods) organisms. We illustrate each marine microfossil taxon or type identified by providing morphological details and photographic images, which will help with their identification in future studies. We also review their ecological preferences to aid future (palaeo) ecological and (palaeo) environmental studies. The planktonic assemblage shows a high degree of endemism related to the strong influence of the sea-ice system over Site U1357. In addition, we found the remains of various species of detritus feeders and bottom-dwelling scavengers (benthic foraminifers and annelid worms) indicative of high export productivity at Site U1357. This study shows the potential of organic microfossil remains for reconstructing past environmental conditions, such as sea-ice cover and (export) productivity.	[Hartman, Julian D.; Bijl, Peter K.; Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, Marine Palynol & Paleoceanog, POB 80-115, NL-3508 TC Utrecht, Netherlands	Utrecht University	Sangiorgi, F (通讯作者)，Univ Utrecht, Dept Earth Sci, Marine Palynol & Paleoceanog, POB 80-115, NL-3508 TC Utrecht, Netherlands.	f.sangiorgi@uu.nl		Sangiorgi, Francesca/0000-0003-4233-6154; Bijl, Peter/0000-0002-1710-4012; Hartman, Julian/0000-0001-6256-9989	NWO Netherlands Polar Program [866.10.110]; US National Science Foundation; Joined Oceanographic Institutions Inc.	NWO Netherlands Polar Program; US National Science Foundation(National Science Foundation (NSF)); Joined Oceanographic Institutions Inc.	Julian D. Hartman, Peter K. Bijl, and Francesca Sangiorgi acknowledge NWO Netherlands Polar Program project number 866.10.110. This research used samples from the Integrated Ocean Drilling Program (IODP). IODP was sponsored by the US National Science Foundation and participating countries under the management of Joined Oceanographic Institutions Inc. We thank Natasja Welters and Niels van Schoffelen for the preparation of part of the palynological slides. We thank Martin Head for useful discussions concerning the determination of dinoflagellate cyst species.	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Micropalaentol.	OCT 11	2018	37	2					445	497		10.5194/jm-37-445-2018	http://dx.doi.org/10.5194/jm-37-445-2018			53	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	GW6SU		Green Submitted, gold			2025-03-11	WOS:000447092800001
J	Gurdebeke, PR; Mertens, KN; Takano, Y; Yamaguchi, A; Bogus, K; Dunthorn, M; Matsuoka, K; Vrielinck, H; Louwye, S				Gurdebeke, Pieter R.; Mertens, Kenneth Neil; Takano, Yoshihito; Yamaguchi, Aika; Bogus, Kara; Dunthorn, Micah; Matsuoka, Kazumi; Vrielinck, Henk; Louwye, Stephen			The affiliation of <i>Hexasterias problematica</i> and <i>Halodinium verrucatum</i> sp. nov. to ciliate cysts based on molecular phylogeny and cyst wall composition	EUROPEAN JOURNAL OF PROTISTOLOGY			English	Article						Acritarch; Ciliate cyst; FTIR; LSU-SSU rDNA; Prostomatida; Taxonomy	DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; PROCESS LENGTH VARIATION; BRITISH MARINE-ALGAE; RESTING CYSTS; BLACK-SEA; SURFACE SEDIMENTS; CRYPTOCARYON-IRRITANS; NORTH PACIFIC; 1ST RECORD; CILIOPHORA	Species in the genera Hexasterias and Halodinium have been recorded over the last decades as acritarchs in palynological and/or plankton studies. In paleoenvironmental studies, these resting stages are often interpreted as indicators of freshwater input. The biological affinity of these genera has never been definitely established. Here, a new species, Halodinium verrucatum sp. nov., is described and molecular evidence (single specimen SSU and LSU rDNA sequencing) reveals that both this new species and Hexasterias problematica, collected from sediment samples in the Skagerrak and Baltic Sea, are resting stages of prorodontid ciliates. Additionally, infrared spectroscopic analysis (micro-FTIR) of Hexasterias problematica and Halodinium spp. specimens indicates a carbohydrate-based composition of the cyst wall with evidence for nitrogen-containing functional groups. A similar composition is recorded for tintinnid loricae, which further supports the placement of Hexasterias and Halodinium as ciliate cysts, and the composition is consistent with the heterotrophic nature of ciliates. The morphologically similar species Radiosperma corbiferum has a comparable composition, suggesting a similar ciliate affinity and indicating the utility of micro-FTIR in understanding acritarch affinity. Hexasterias problematica typically occurs in coastal waters from temperate to arctic regions. Halodinium verrucatum sp. nov. is observed in temperate estuarine sediments in the northern hemisphere. (C) 2018 Elsevier GmbH. All rights reserved.	[Gurdebeke, Pieter R.; Louwye, Stephen] Univ Ghent, Dept Geol, Krijgslaan 281, B-9000 Ghent, Belgium; [Mertens, Kenneth Neil] Ifremer, Stn Biol Marine, LER BO, Pl Croix,BP40537, F-29185 Concarneau, France; [Takano, Yoshihito; Matsuoka, Kazumi] Inst East China Sea Res ECSER, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan; [Yamaguchi, Aika] Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 6578501, Japan; [Bogus, Kara] Univ Nottingham, Sch Geog, Ctr Environm Geochem, Nottingham NG7 2RD, England; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA; [Dunthorn, Micah] Univ Kaiserslautern, Dept Ecol, Erwin Schrodinger St, D-67663 Kaiserslautern, Germany; [Vrielinck, Henk] Univ Ghent, Dept Solid State Sci, Krijgslaan 281,S1, B-9000 Ghent, Belgium	Ghent University; Ifremer; Kobe University; University of Nottingham; Texas A&M University System; Texas A&M University College Station; University of Kaiserslautern; Ghent University	Gurdebeke, PR (通讯作者)，Univ Ghent, Dept Geol, Krijgslaan 281, B-9000 Ghent, Belgium.	pieter.gurdebeke@ugent.be	Gurdebeke, Pieter/AAY-7059-2020; Mertens, Kenneth/AAO-9566-2020; Vrielinck, Henk/M-8367-2016; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015	Louwye, Stephen/0000-0003-4814-4313; Dunthorn, Micah/0000-0003-1376-4109; Vrielinck, Henk/0000-0003-4861-9630; Mertens, Kenneth/0000-0003-2005-9483; Bogus, Kara/0000-0003-4690-0576; Gurdebeke, Pieter R./0000-0003-1425-8515	Hercules Foundation (FWO, Flanders) [AUGE/13/16]; National Science Foundation [OCE - 1326927]	Hercules Foundation (FWO, Flanders); National Science Foundation(National Science Foundation (NSF))	This work was supported by the Hercules Foundation (FWO, Flanders) [FT-IMAGER project - AUGE/13/16] and the National Science Foundation [OCE - 1326927].	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J. Protistol.	OCT	2018	66						115	135		10.1016/j.ejop.2018.09.002	http://dx.doi.org/10.1016/j.ejop.2018.09.002			21	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	HD2NP	30261410	Green Submitted			2025-03-11	WOS:000452347600012
J	Luo, ZH; Hu, ZX; Tang, YZ; Mertens, KN; Leaw, CP; Lim, PT; Teng, ST; Wang, L; Gu, HF				Luo, Zhaohe; Hu, Zhangxi; Tang, Yingzhong; Mertens, Kenneth Neil; Leaw, Chui Pin; Lim, Po Teen; Teng, Sing Tung; Wang, Lei; Gu, Haifeng			MORPHOLOGY, ULTRASTRUCTURE, AND MOLECULAR PHYLOGENY OF <i>WANGODINIUM SINENSE</i> GEN. ET SP NOV (GYMNODINIALES, DINOPHYCEAE) AND REVISITING OF <i>GYMNODINIUM DORSALISULCUM</i> AND <i>GYMNODINIUM IMPUDICUM</i>	JOURNAL OF PHYCOLOGY			English	Article						apical structure complex; cyst; dinoflagellate; Lepidodinium; nuclear chambers; pigment; pyrenoid; ultrastructure	WESTERN KOREA MORPHOLOGY; BLOOM-FORMING DINOFLAGELLATE; NW MEDITERRANEAN SEA; SHIWHAENSE N. GEN.; LSU RDNA SEQUENCE; COASTAL WATERS; COMB. NOV; RIBOSOMAL DNA; ALEXANDRIUM DINOPHYCEAE; UNARMORED DINOPHYCEAE	The genus Gymnodinium includes many morphologically similar species, but molecular phylogenies show that it is polyphyletic. Eight strains of Gymnodinium impudicum, Gymnodinium dorsalisulcum and a novel Gymnodinium-like species from Chinese and Malaysian waters and the Mediterranean Sea were established. All of these strains were examined with light microscopy, scanning electron microscopy and transmission electron microscopy. SSU, LSU and internal transcribed spacers rDNA sequences were obtained. A new genus, Wangodinium, was erected to incorporate strains with a loop-shaped apical structure complex (ASC) comprising two rows of amphiesmal vesicles, here referred to as a new type of ASC. The chloroplasts of Wangodinium sinense are enveloped by two membranes. Pigment analysis shows that peridinin is the main accessory pigment in W. sinense. Wangodinium differs from other genera mainly in its unique ASC, and additionally differs from Gymnodinium in the absence of nuclear chambers, and from Lepidodinium in the absence of Chl b and nuclear chambers. New morphological information was provided for G. dorsalisulcum and G. impudicum, e.g., a short sulcal intrusion in G. dorsalisulcum; nuclear chambers in G. impudicum and G. dorsalisulcum; and a chloroplast enveloped by two membranes in G. impudicum. Molecular phylogeny was inferred using maximum likelihood and Bayesian inference with independent SSU and LSU rDNA sequences. Our results support the classification of Wangodinium within the Gymnodiniales sensu stricto clade and it is close to Lepidodinium. Our results also support the close relationship among G. dorsalisulcum, G. impudicum, and Barrufeta. Further research is needed to assign these Gymnodinium species to Barrufeta or to erect new genera.	[Luo, Zhaohe; Wang, Lei; Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Hu, Zhangxi; Tang, Yingzhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France; [Leaw, Chui Pin; Lim, Po Teen] Univ Malaya, Inst Ocean & Earth Sci, Bachok Marine Res Stn, Bachok 16310, Kelantan, Malaysia; [Teng, Sing Tung] Univ Malaysia Sarawak, Fac Resource Sci & Technol, Kota Samarahan 94300, Sarawak, Malaysia	Third Institute of Oceanography, Ministry of Natural Resources; Chinese Academy of Sciences; Institute of Oceanology, CAS; Ifremer; Universiti Malaya; University of Malaysia Sarawak	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Teng, SingTung/E-8281-2015; ZHANG, hui jie/HTN-1690-2023; Mertens, Kenneth/AAO-9566-2020; Luo, Zhaohe/ITT-7163-2023; Leaw, Chui Pin/F-5220-2012; Mertens, Kenneth/C-3386-2015; Lim, Po Teen/C-9758-2013; Gu, Haifeng/ADN-4528-2022	Mertens, Kenneth/0000-0003-2005-9483; Teng, Sing Tung/0000-0002-8872-0963; Lim, Po Teen/0000-0003-2823-0564; Luo, Zhaohe/0000-0001-8662-2414; Hu, Zhangxi/0000-0002-4742-4973; Gu, Haifeng/0000-0002-2350-9171	National Natural Science Foundation of China [41676117]; NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences [U1606404]; Qingdao National Laboratory for Marine Science [2016ASKJ02]; MOSTI; Scientific and Technological Innovation Project	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences; Qingdao National Laboratory for Marine Science; MOSTI(Ministry of Energy, Science, Technology, Environment and Climate Change (MESTECC), Malaysia); Scientific and Technological Innovation Project	We thank two anonymous reviewers for constructive suggestions that improved the manuscript greatly. This work was supported by the National Natural Science Foundation of China (41676117), the NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences (U1606404), and the Scientific and Technological Innovation Project supported by the Qingdao National Laboratory for Marine Science (2016ASKJ02). Research permission was given by Marine Park of Malaysia and fund from MOSTI for sampling in Perhentian Island.	Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Al-Qassab S, 2002, ACTA PROTOZOOL, V41, P91; Alix B, 2012, NUCLEIC ACIDS RES, V40, pW573, DOI 10.1093/nar/gks485; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P644, DOI 10.2216/07-05.1; Biecheler B., 1952, Bull. Biol. Fr. Belg., V36, P1; BRADBURY PC, 1983, J ULTRA MOL STRUCT R, V85, P24, DOI 10.1016/S0022-5320(83)90113-2; Campbell P. 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Phycol.	OCT	2018	54	5					744	761		10.1111/jpy.12780	http://dx.doi.org/10.1111/jpy.12780			18	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	GV5VD	30144373	Green Published, Green Accepted			2025-03-11	WOS:000446171600014
J	Wu, HY; Luan, QS; Guo, MM; Gu, HF; Zhai, YX; Tan, ZJ				Wu, Hai-Yan; Luan, Qing-Shan; Guo, Meng-Meng; Gu, Hai-Feng; Zhai, Yu-Xiu; Tan, Zhi-Jun			Phycotoxins in scallops (<i>Patinopecten yessoensis</i>) in relation to source, composition and temporal variation of phytoplankton and cysts in North Yellow Sea, China	MARINE POLLUTION BULLETIN			English	Article						Phycotoxins; Phytoplankton; Cyst; Risk assessment	PARALYTIC SHELLFISH TOXINS; AZADINIUM-POPORUM DINOPHYCEAE; SOLID-PHASE EXTRACTION; HARMFUL ALGAL BLOOMS; LIQUID-CHROMATOGRAPHY; MASS-SPECTROMETRY; BIVALVE MOLLUSKS; MARINE BIOTOXINS; VARIABILITY; PHYLOGENY	The North Yellow Sea is a major aquaculture production area for the scallop Patinopecten yessoensis. In this study, the temporal and spatial variation of phycotoxins in scallops, phytoplankton, and their cysts were analyzed during a survey conducted from June 2011 to April 2012 around Zhangzi Island. The study area is a semi enclosed epicontinental sea surrounded by the Shandong Peninsula, the Liaodong Peninsula and the Korean Peninsula. The three main results of the study were as follows: (1) The saxitoxin-group toxins, okadaic acid and analogues, and pectenotoxins were the major phycotoxin residues found in scallops; (2) Six kinds of toxic microalgae were identified, Protoperidinium spp., Gonyatdax spp., and Alexandriurn spp. were the dominant taxa; Seven types of potential marine toxin-producing dinoflagellates, A. tamarense, A. catenella, Dinophysis forth, G. catenatum, Gambierdiscus toxicus, Azadinturn poporwn, and Pseudo-nitzschia pungen were identified as the primary source of phycotoxins and were present at relatively high density from June to October; and (3) azaspiracids and domoic acid might be new potential sources of toxin pollution. This study represents the first assessment to phycotoxins around Zhangzi Island in the North Yellow Sea.	[Wu, Hai-Yan; Luan, Qing-Shan; Guo, Meng-Meng; Zhai, Yu-Xiu; Tan, Zhi-Jun] Minist Agr, Key Lab Testing & Evaluat Aquat Product Safety &, Qingdao 266071, Peoples R China; [Wu, Hai-Yan; Luan, Qing-Shan; Guo, Meng-Meng; Zhai, Yu-Xiu; Tan, Zhi-Jun] Chinese Acad Fishery Sci, Yellow Sea Fisheries Res Inst, Qingdao 266071, Peoples R China; [Wu, Hai-Yan; Luan, Qing-Shan; Guo, Meng-Meng; Zhai, Yu-Xiu; Tan, Zhi-Jun] Carbon Sink Fisheries Lab, Qingdao 266071, Peoples R China; [Gu, Hai-Feng] Third Inst Oceanog, SOA, Xiamen 361005, Peoples R China	Ministry of Agriculture & Rural Affairs; Chinese Academy of Fishery Sciences; Yellow Sea Fisheries Research Institute, CAFS; Third Institute of Oceanography, Ministry of Natural Resources	Tan, ZJ (通讯作者)，106 Nanjing Ave, Qingdao, Shandong, Peoples R China.	wuhy@ysfri.ac.cn; qingsl@ysfri.ac.cn; guomm@ysfri.ac.cn; zhaiyx@ysfri.ac.cn; tanzj@ysfri.ac.cn	Luan, Qingshan/LXW-4416-2024; Gu, Haifeng/ADN-4528-2022	WU, Haiyan/0000-0001-5880-3998; Gu, Haifeng/0000-0002-2350-9171	National Key R&D Program of China [2017YFC1600701]; National Natural Science Foundation of China [31772075]	National Key R&D Program of China; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This work was supported by the National Key R&D Program of China (grant No. 2017YFC1600701) and the National Natural Science Foundation of China (grant No. 31772075).	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OCT	2018	135						1198	1204		10.1016/j.marpolbul.2018.08.045	http://dx.doi.org/10.1016/j.marpolbul.2018.08.045			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	GX9BT	30301019				2025-03-11	WOS:000448094200131
J	Frieling, J; Sluijs, A				Frieling, Joost; Sluijs, Appy			Towards quantitative environmental reconstructions from ancient non-analogue microfossil assemblages: Ecological preferences of Paleocene - Eocene dinoflagellates	EARTH-SCIENCE REVIEWS			English	Article							PALAEOCENE/EOCENE THERMAL MAXIMUM; CRETACEOUS-TERTIARY BOUNDARY; LAST GLACIAL MAXIMUM; SEA-LEVEL; NORTHERN-HEMISPHERE; VERTICAL-DISTRIBUTION; ARCTIC HYDROLOGY; CYST ASSEMBLAGES; MARINE-SEDIMENTS; CARBON INJECTION	We explore a novel approach towards quantification of paleo-ecological signals from non-analogue microfossil assemblages by quantifying relations between assemblages and high-quality geochemical and sedimentological data from sedimentary archives. We test this approach using one group of microfossils, the organic cysts of dinoflagellates (dinocysts), which are widely used in shelf and open marine settings for biostratigraphy and reconstructions of past environments and environmental change. Similar to other microfossil groups, dinocysts can be used to reconstruct environments with relatively high confidence for recent time periods, as species affinities can be derived from observational and instrumental data. In the absence of such data, the ecology of extinct species is much less certain and as a result reconstructions in deep time are often limited to qualitative interpretations. To explore if quantitative empirical relations between extinct dinocysts and high-quality geochemical data can be established, we study a major event of climate change, the Paleocene-Eocene Thermal Maximum (PETM; similar to 56 Ma ago). The PETM is a particularly suitable period for this exercise as there is a multitude of large environmental perturbations associated with the transient global warming, such as deoxygenation, sea level rise and an accelerated hydrological cycle. The synthesized published dataset exhibits better spatial and temporal coverage compared to any other period in deep time. We extract empirical relations for the abundance of previously proposed paleoecological groups as a function of independent environmental proxies for example, sea surface temperature and terrestrial organic matter input. The results unequivocally illustrate that many dinocysts show relations to several of the reconstructed environmental variables. Notably, we show that one genus (Apectodinium) and an ecogroup (epicystal Goniodomidae) required sea surface temperatures in excess of 20 degrees C, and 25 degrees C, respectively, while one species (Florentinia reichartii) was only abundant between 30 and 35 degrees C. Other groups apparently favored either a limited (Spiniferites) or high (Senegalinium) terrestrial input to the study site, relating to salinity, nutrient levels or suspended sediment load (i.e. murkiness). Crucially, our work shows that the validation and quantification of ecological signals by independent environmental proxy data provides the opportunity to extract more quantitative information from a wide range of (non-analogue) microfossil assemblages. While this approach is not limited to any specific group of microfossils (or macrofossils), we stress that proper calibration datasets, high-quality sedimentological and geochemical proxy records, are needed and should ideally have decent geographical coverage and include one or more environmental perturbations. Using this approach such empirical relations can be established for a wide range of microfossil groups that have highly complementary geological records, which increases the value of existing data and ensures future application of microfossil-based paleoecology.	[Frieling, Joost; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleoceo, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands	Utrecht University	Frieling, J (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleoceo, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands.	j.frieling1@uu.nl	Sluijs, Appy/B-3726-2009	Sluijs, Appy/0000-0003-2382-0215	European Research Council (ERC) [259627]; Netherlands Organization for Scientific Research (NWO) [ALWOP.223]; Dutch Ministry of Education, Culture and Science	European Research Council (ERC)(European Research Council (ERC)); Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); Dutch Ministry of Education, Culture and Science	We used samples and data provided by the International Ocean Discovery Program (IODP) and its predecessor, the Ocean Drilling Program. This contribution was funded through European Research Council (ERC) starting grant #259627 and Netherlands Organization for Scientific Research (NWO) grant #ALWOP.223, both to AS. This work was carried out under the program of the Netherlands Earth System Science Centre (NESSC), financially supported by the Dutch Ministry of Education, Culture and Science.	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J	Dawut, M; Sym, SD; Horiguchi, T				Dawut, Mahmutjan; Sym, Stuart D.; Horiguchi, Takeo			Re-investigation of <i>Gymnodinium natalense</i> (Dinophyceae), a tidal pool dinoflagellate from South Africa and the proposal of a new combination <i>Ansanella natalensis</i>	PHYCOLOGICAL RESEARCH			English	Article						amphiesmal vesicle; phylogeny; small subunit rDNA; taxonomy; ultrastructure	SP-NOV DINOPHYCEAE; BIECHELERIOPSIS-ADRIATICA; WOLOSZYNSKIA-CINCTA; COASTAL WATERS; GEN.; ULTRASTRUCTURE; INFERENCE; MRBAYES; MODELS	A small tidal pool bloom-forming dinoflagellate, Gymnodinium natalense T. Horiguchi & Pienaar, sampled from its type locality in South Africa, was re-investigated and a new combination Ansanella natalensis (T. Horiguchi & Pienaar) Dawut, Sym T. Horiguchi comb. nov. was proposed. The species was originally described as a new species of the genus Gymnodinium, and later, Moestrup et al. (2009a) transferred it to their new genus Biecheleria based on morphological resemblance. However, no molecular data were available at that time, making confirmation of its phylogenetic affinities impossible. An organism more-recently isolated from the type locality was confirmed as G. natalense based on its morphological features. In addition, we were able to characterize details of its surface structure, which were lacking in the original description. Cells were covered with small, mostly hexagonal, amphiesmal vesicles (AV) arranged in 11-13 latitudinal rows. The episome contained an elongated amphiesmal vesicle (EAV) enclosing approximately 25 knobs in linear array. A phylogenetic analysis based on SSU rDNA sequences revealed that this dinoflagellate was closely related to Ansanella granifera the only member of the genus. The G. natalense shared numerous characteristics with A. granifera, such as the arrangement of AVs in a similar number of latitudinal rows, the shape and position of the EAV, the possession of a type E eyespot, a similar type of pyrenoid, the absence of a peduncle and nuclear chambers, the lack of a nuclear fibrous connective and no resting cyst-like cells. Yet, it also showed some morphological differences, i.e. the possession of a single chloroplast that lacks grana-like thylakoids, which separate it from A. granifera. These morphological features, along with its highly supported molecular affinity with A. granifera, led to the conclusion that this dinoflagellate represents a new member of this genus, i.e. A. natalensis comb. nov. The phylogenetic analysis showed no support for a close relationship with members of the genus Biecheleria.	[Dawut, Mahmutjan] Hokkaido Univ, Grad Sch Sci, Dept Nat Hist Sci, Sapporo, Hokkaido, Japan; [Sym, Stuart D.] Univ Witwatersrand, Sch Anim Plant & Environm Sci, Johannesburg, South Africa; [Horiguchi, Takeo] Hokkaido Univ, Fac Sci, Dept Biol Sci, Sapporo, Hokkaido, Japan	Hokkaido University; University of Witwatersrand; Hokkaido University	Horiguchi, T (通讯作者)，Hokkaido Univ, Fac Sci, Dept Biol Sci, Sapporo, Hokkaido, Japan.	horig@sci.hokudai.ac.jp	Horiguchi, Takeo/D-7612-2012	Horiguchi, Takeo/0000-0002-6118-8460	Japan Science and Technology Agency; National Research Foundation (South Africa); JSPS [24370034]	Japan Science and Technology Agency(Japan Science & Technology Agency (JST)); National Research Foundation (South Africa)(National Research Foundation - South Africa); JSPS(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science)	The strains used in this study were collected on one of the field trips for a project entitled 'Biodiversity and evolution of algae in the Indo-Pacific: a Japan/South Africa comparison' (Strategic International Research Cooperative Program) supported by the Japan Science and Technology Agency and the National Research Foundation (South Africa). This research was also partly supported by the Grant-in-Aid by JSPS (No. 24370034).	Balzano S, 2012, BIOGEOSCIENCES, V9, P4553, DOI 10.5194/bg-9-4553-2012; Biecheler B., 1952, Bull. Biol. Fr. 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Res.	OCT	2018	66	4					300	309		10.1111/pre.12329	http://dx.doi.org/10.1111/pre.12329			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	GY8KQ					2025-03-11	WOS:000448876000006
J	Li, Z; Pospelova, V; Lin, HL; Liu, LJ; Song, B; Gong, WP				Li, Zhen; Pospelova, Vera; Lin, Hui-Ling; Liu, Lejun; Song, Bing; Gong, Wenping			Seasonal dinoflagellate cyst production and terrestrial palynomorph deposition in the East Asian Monsoon influenced South China Sea: A sediment trap study from the Southwest Taiwan waters	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palynology; Dinollagellate cysts; East Asian monsoon; South China Sea; Sediment trap; Seasonal change	MODERN POLLEN DISTRIBUTION; SMALL MOUNTAINOUS RIVERS; RECENT MARINE-SEDIMENTS; LAST GLACIAL MAXIMUM; SURFACE SEDIMENTS; ENVIRONMENTAL-CHANGE; CLIMATE-CHANGE; PALYNOLOGICAL EVIDENCE; BRITISH-COLUMBIA; NORTH-ATLANTIC	The South China Sea (SCS), influenced by the tropical East Asian Monsoon (EAM), experiences winter monsoon and summer monsoon shifts in near-surface wind, air temperature, sea-surface temperature, salinity, primary productivity, and other oceanographic conditions. To understand how monsoon seasons influence palynological dynamics and which palynological index could be a reliable indicator of winter or summer monsoons, we studied palynological records of sediment trap samples collected in March-April (winter monsoon season) and July August (summer monsoon season). Fluxes and assemblages of terrestrial pollen and spores, as well as marine dinoflagellate cysts, were investigated using sediment traps in the southwest Taiwan waters of the SCS. The pollen and spores of 109 taxa and dinoflagellate cysts of 53 taxa were identified in 24 sediment trap samples that were collected at 3-day intervals. The average abundance of Pinus pollen was notably higher in March-April at similar to 40%, which was double that in July-August. This trend was associated with transport by the northwest wind in March-April when Pinus pollen are produced by the coniferous vegetation in the South China and Taiwan Island. The pollen abundances of Chenopodiaceae/Amaranthaceae and Compositae seemed to be greatly reduced in July-August, with an opposite pattern observed for Poaceae, Artemisia, Cyperaceae, Typha, and fern spores. Fluvial transport is likely the controlling factor since river runoff intensifies in summer. High relative abundances and fluxes of Poaceae pollen are not indicators of summer monsoons but related to cultivated activities. Dinoflagellate cyst assemblages were dominated by cysts produced by heterotrophic taxa, especially Brigantedinium spp. at 68-91%. Proportionally higher increases than those of cysts produced by autotrophic dinoflagellates resulted in lower heterotrophic to autotrophic ratios in July-August. The highest total cyst fluxes occurred in late July of similar to 20,000 cysts m(-2) d(-1) together with the highest fluxes of autotrophic Operculodinium centrocarpum, Spiniferites spp., and Lingulodinium hemicystum. The increased fluxes of almost all dinoflagellate cyst taxa during July-August were related to the decreased sea-surface salinity (SSS) due to the greater river water inputs and nutrients. (C) 2018 Elsevier B.V. All rights reserved.	[Li, Zhen; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada; [Lin, Hui-Ling] Natl Sun Yat Sen Univ, Dept Oceanog, Kaohsiung 804, Taiwan; [Liu, Lejun] SOA, Inst Oceanog 1, 6 Xianxialing Rd, Qingdao 266061, Peoples R China; [Song, Bing] Korea Inst Geosci & Mineral Resources, Quaternary Geol Dept, Geol Res Div, Daejeon 305350, South Korea; [Gong, Wenping] SunYat Sen Univ, Sch Marine Sci, Guangzhou 510275, Guangdong, Peoples R China	University of Victoria; National Sun Yat Sen University; First Institute of Oceanography, Ministry of Natural Resources; Korea Institute of Geoscience & Mineral Resources (KIGAM); Sun Yat Sen University	Li, Z (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada.	imlizhen@hotmail.com	Li, Zhen/G-7667-2012; Song, Bing/I-3464-2019; LIN, HUI-LING/HJB-4015-2022	Pospelova, Vera/0000-0003-4049-8133; Li, Zhen/0000-0003-3989-7233	Natural Sciences and Engineering Research Council of Canada (NSERC) CGS D3 fellowship [CGSD3-475098-2015]; Montalbano scholarship; NSERC [RGPIN/6388-2015]; Ministry of Science and Technology Grants of Taiwan [NSC 98-3114-E-006-014, NSC 99-2611-M-110-006]; National Program on Global Change and Air-Sea Interaction from the State Oceanography Administration of China [GASI-GEOGE-05]; Chinese Natural Science Foundation [41506103, 51761135021]	Natural Sciences and Engineering Research Council of Canada (NSERC) CGS D3 fellowship(Natural Sciences and Engineering Research Council of Canada (NSERC)); Montalbano scholarship; NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Ministry of Science and Technology Grants of Taiwan; National Program on Global Change and Air-Sea Interaction from the State Oceanography Administration of China; Chinese Natural Science Foundation(National Natural Science Foundation of China (NSFC))	The Natural Sciences and Engineering Research Council of Canada (NSERC) CGS D3 fellowship (CGSD3-475098-2015) and Montalbano scholarship provided partial funding for this research to Z. Li. This work was also funded by NSERC through a Discovery grant (RGPIN/6388-2015) to V. Pospelova. She is the Hanse-Wissenschaftskolleg (HWK) senior research fellow in marine and climate research at the institute for Advanced Study (Germany). H.-L. Lin was supported by the Ministry of Science and Technology Grants of Taiwan (NSC 98-3114-E-006-014 and NSC 99-2611-M-110-006). L. Liu was partially supported by the National Program on Global Change and Air-Sea Interaction (GASI-GEOGE-05) from the State Oceanography Administration of China in this work, and B. Song and W. Gong were supported by Chinese Natural Science Foundation Projects of No. 41506103 and No. 51761135021, respectively.	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Palaeobot. Palynology	OCT	2018	257						117	139		10.1016/j.revpalbo.2018.07.007	http://dx.doi.org/10.1016/j.revpalbo.2018.07.007			23	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	GW6VF					2025-03-11	WOS:000447101200010
J	Lewis, AM; Coates, LN; Turner, AD; Percy, L; Lewis, J				Lewis, Adam Michael; Coates, Lewis Nicholas; Turner, Andrew D.; Percy, Linda; Lewis, Jane			A REVIEW OF THE GLOBAL DISTRIBUTION OF <i>ALEXANDRIUM MINUTUM</i> (DINOPHYCEAE) AND COMMENTS ON ECOLOGY AND ASSOCIATED PARALYTIC SHELLFISH TOXIN PROFILES, WITH A FOCUS ON NORTHERN EUROPE	JOURNAL OF PHYCOLOGY			English	Review						Alexandrium minutum; ecology; geographic distribution; paralytic shellfish toxins; toxin profiling	RECENT MARINE-SEDIMENTS; HARMFUL ALGAL BLOOMS; IRISH COASTAL WATERS; REAL-TIME PCR; DINOFLAGELLATE CYST ASSEMBLAGES; GENUS ALEXANDRIUM; ENVIRONMENTAL-FACTORS; MEDITERRANEAN LAGOON; POISONING TOXINS; CORK HARBOR	Alexandrium minutum is a globally distributed harmful algal bloom species with many strains that areknown to produce paralytic shellfish toxins (PSTs) and consequently represent a concern to human andecosystem health. This review highlightsthat A.minutum typically occurs in sheltered locations, with cell growth occurring during periods of stable water conditions. Sediment characteristics are important in the persistence of this species within a location, with fine sediments providing cyst deposits for ongoing inoculation to the water column. Toxic strains of A.minutum do not produce a consistent toxin profile, different populations produce a range of PSTs in differing quantities. Novel cluster analysis of published A.minutum toxin profiles indicates five PST profile clusters globally. Some clusters are grouped geographically (Northern Europe) while others are widely spread. Isolates from Taiwan have arange of toxin profile clusters and this area appears to have the most diverse set of PST producing A.minutum populations. These toxin profiles indicate that within the United Kingdom there are two populations of A.minutum grouping with strains from Northern France and Southern Ireland. There is a degree of interconnectivity in this region due tooceanic circulation and a high level of shipping andrecreational boating. Further research into theinterrelationships between the A.minutum populations in this global region would be of value.	[Lewis, Adam Michael; Coates, Lewis Nicholas; Turner, Andrew D.] Cefas, Barrack Rd, Weymouth DT48UB, Dorset, England; [Lewis, Adam Michael; Percy, Linda; Lewis, Jane] Univ Westminster, Fac Sci & Technol, 115 New Cavendish St, London W1W6UW, England	Centre for Environment Fisheries & Aquaculture Science; University of Westminster	Lewis, AM (通讯作者)，Cefas, Barrack Rd, Weymouth DT48UB, Dorset, England.; Lewis, AM (通讯作者)，Univ Westminster, Fac Sci & Technol, 115 New Cavendish St, London W1W6UW, England.	adam.lewis@cefas.co.uk	Turner, Andrew/J-5658-2015	Turner, Andrew/0000-0003-1390-0924; Lewis, Adam/0000-0001-7761-6266	Cefas Seedcorn	Cefas Seedcorn	We would like to acknowledge Cefas Seedcorn for funding this work.	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Phycol.	OCT	2018	54	5					581	598		10.1111/jpy.12768	http://dx.doi.org/10.1111/jpy.12768			18	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	GV5VD	30047623	Green Accepted			2025-03-11	WOS:000446171600001
J	Candel, MS; Borromei, AM; Louwye, S				Candel, Maria Soledad; Borromei, Ana M.; Louwye, Stephen			Early to middle Holocene palaeoenvironmental reconstruction of the Beagle Channel (southernmost Argentina) based on terrestrial and marine palynomorphs	BOREAS			English	Article							TIERRA-DEL-FUEGO; WALLED DINOFLAGELLATE CYSTS; POSTGLACIAL VEGETATION; PALYNOFACIES ANALYSIS; SOUTH-AMERICA; QUATERNARY; EVOLUTION; SEDIMENTS; COAST; PALEOECOLOGY	This paper presents the main palaeoenvironmental results obtained from a site located in the western sector of the Beagle Channel, Isla Grande de Tierra del Fuego, southernmost Argentina. The palynological analysis performed on marine sediments from Aserradero-Lapataia 2 (latitude 54 degrees 5122.7S, longitude 68 degrees 3422.8W) allowed us to document the evolution of palaeoenvironmental conditions during the beginning of the Holocene marine transgression into the Beagle Channel. The results indicate that, prior to the marine incursion, the coastal areas were characterized by the presence of open-grown shrubs and herbs along with woodland palaeocommunities. The aquatic environments were dominated exclusively by freshwater taxa. Around 8300cal. a BP, seawater gradually flooded the channel while cold and high effective moisture conditions favoured the development of an arboreal vegetation with dominance of Nothofagus forest and scarcity of shrub and herbaceous communities. Gradually increasing salinities allowed the development of freshwater/marine transitional environments indicated by aquatic palynomorphs able to tolerate stressed conditions under fluctuating salinities. The increasing dinocyst diversification with dominance of heterotrophic taxa corroborates the establishment of a fully marine environment during the middle-late Holocene in the Beagle Channel.	[Candel, Maria Soledad] Ctr Austral Invest Cient CADIC CONICET, Lab Geomorfol & Cuaternario, B Houssay 200, RA-9410 Ushuaia, Argentina; [Borromei, Ana M.] Univ Nacl Sur CONICET, Inst Geol Sur INGEOSUR, Ave Alem 1253 CuerpoB,Piso 2,B8000ICPB, Bahia Blanca, Buenos Aires, Argentina; [Louwye, Stephen] Univ Ghent, Dept Geol, Krijgslaan 281, B-9000 Ghent, Belgium	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Ghent University	Candel, MS (通讯作者)，Ctr Austral Invest Cient CADIC CONICET, Lab Geomorfol & Cuaternario, B Houssay 200, RA-9410 Ushuaia, Argentina.	soledadcandel@cadic-conicet.gob.ar	Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313	Erasmus Mundus (Euro TANGO II Project) Postdoctoral Fellowship; CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas) [PIP 112-201301-00323]	Erasmus Mundus (Euro TANGO II Project) Postdoctoral Fellowship; CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET))	This research was carried out by the lead author at Ghent University, Belgium, thanks to an Erasmus Mundus (Euro TANGO II Project) Postdoctoral Fellowship. This study was also supported by a CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas, PIP 112-201301-00323) grant to Ana Maria Borromei. We are grateful to Marcelo A. Martinez and Lorena L. Musotto (INGEOSUR-CONICET, Universidad Nacional del Sur, Argentina), Juan Federico Ponce and Andrea Coronato (CADIC-CONICET, Ushuaia, Argentina) for field assistance and contributing resources for the fieldwork. Our thanks are also extended to Sabine Van Cauwenberghe (Research Unit Palaeontology of Ghent University, Belgium) for her assistance in the laboratory. We thank Prof. Jan A. Piotrowski and two anonymous reviewers for their constructive comments that helped to improve our manuscript.	[Anonymous], 1986, INT S SEA LEV CHANG; Batten D., 1996, Palynology: principles and applications, P1011; Bentley MJ, 2009, HOLOCENE, V19, P51, DOI 10.1177/0959683608096603; Boessenkool K. 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J	Yang, Q; Jiang, ZW; Huang, CH; Zhang, RN; Li, LZ; Yang, G; Feng, LJ; Yang, GF; Zhang, H; Zhang, XL; Mu, J				Yang, Qiao; Jiang, Zhi-Wei; Huang, Cheng-Hui; Zhang, Ruo-Nan; Li, Ling-Zhi; Yang, Guang; Feng, Li-Juan; Yang, Guang-Feng; Zhang, Heng; Zhang, Xiao-Ling; Mu, Jun			<i>Hoeflea prorocentri</i> sp nov., isolated from a culture of the marine dinoflagellate <i>Prorocentrum mexicanum</i> PM01	ANTONIE VAN LEEUWENHOEK INTERNATIONAL JOURNAL OF GENERAL AND MOLECULAR MICROBIOLOGY			English	Article						Hoeflea prorocentri sp; nov; Novel species; Prorocentrum mexicanum; Algal-associated bacterium	DEOXYRIBONUCLEIC-ACID; GEN. NOV.; SEQUENCES; RECLASSIFICATION; TREES	A Gram-stain negative, aerobic, rod-shaped, non-motile, yellow-pigmented and non-spore-forming bacterial strain, designated PM5-8(T), was isolated from a culture of a marine toxigenic dinoflagellate Prorocentrum mexicanum PM01. Strain PM5-8(T) grew at 15-35 degrees C (optimum, 25-30 degrees C) and pH 6-11 (optimum, 7.5-8). Cells required at least 1.5% (w/v) NaCl for growth, and can tolerate up to 7.0% with the optimum of 4%. Phylogenetic analysis based on 16S rRNA gene sequence revealed that the strain PM5-8(T) is closely related to members of the genus Hoeflea, with high sequence similarities with Hoeflea halophila JG120-1(T) (97.06%) and Hoeflea alexandrii AM1V30(T) (97.01%). DNA-DNA hybridization values between the isolate and other type strains of recognized species of the genus Hoeflea were between 11.8 and 25.2%, which is far below the value of 70% thresholdfor species delineation. The DNA G+C content was 50.3mol%. The predominant cellular fatty acids of the strain wereidentified assummed feature 8 (C(16:1)7c and/or C(16:1)6c; 51.5%), C(18:1)7c 11-methyl (20.7%), C-16:0 (17.2%) and C-18:0 (5.7%). The major respiratory quinone was Q-10. Polar lipids profiles contained phosphatidylcholine, phosphatidylglycerol, sulfoquinovosyl diacylglycerol, phosphatidylmono- methylethanolamine, phosphatidylethanolamine and four unidentified lipids. On the basis of the polyphasic taxonomic datapresented, strain PM5-8(T) (=CCTCC AB 2016294(T)=KCTC 62490(T)) represents a novel species of the genus Hoeflea, for which the name Hoeflea prorocentri sp. nov. is proposed.	[Yang, Qiao; Jiang, Zhi-Wei; Huang, Cheng-Hui; Feng, Li-Juan; Yang, Guang-Feng; Zhang, Xiao-Ling; Mu, Jun] Zhejiang Ocean Univ, Lab Marine Environm & Ecol, Coll Marine Sci & Technol, Zhoushan 316022, Peoples R China; [Zhang, Ruo-Nan] Harbin Univ Commerce, Ctr Res Life Sci & Environm Sci, Harbin 150076, Heilongjiang, Peoples R China; [Li, Ling-Zhi; Zhang, Heng] Chinese Acad Fishery Sci, East China Sea Fisheries Res Inst, Shanghai 200090, Peoples R China; [Yang, Guang-Feng] Chinese Acad Sci, Key Lab Marine Ecol & Environm Sci, Inst Oceanol, Qingdao 266071, Peoples R China	Zhejiang Ocean University; Harbin University of Commerce; Chinese Academy of Fishery Sciences; East China Sea Fisheries Research Institute, CAFS; Chinese Academy of Sciences; Institute of Oceanology, CAS	Zhang, XL; Mu, J (通讯作者)，Zhejiang Ocean Univ, Lab Marine Environm & Ecol, Coll Marine Sci & Technol, Zhoushan 316022, Peoples R China.	zhangxiaoling@zjou.edu.cn; mujun@zjou.edu.cn	阳, 广凤/ABC-9925-2022; Zhang, Heng/JXL-3857-2024	Yang, Guang-feng/0000-0002-4320-2193	Talent Introduction Foundation of Zhejiang Ocean University; National Natural Science Foundation of China [41206093, 31470540]; Zhejiang Provincial Natural Science Foundation of China [LY18D060007]; Scientific Instrument and Chemical Reagents Project of Shanghai Science and Technology Committee [15142201600]; Municipal Public Welfare Project of Zhoushan [2017C32083]	Talent Introduction Foundation of Zhejiang Ocean University; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Zhejiang Provincial Natural Science Foundation of China(Natural Science Foundation of Zhejiang Province); Scientific Instrument and Chemical Reagents Project of Shanghai Science and Technology Committee; Municipal Public Welfare Project of Zhoushan	This work was supported by Talent Introduction Foundation of Zhejiang Ocean University (for Qiao Y.), the National Natural Science Foundation of China (41206093 and 31470540), the Zhejiang Provincial Natural Science Foundation of China (LY18D060007), Scientific Instrument and Chemical Reagents Project of Shanghai Science and Technology Committee (15142201600), and Municipal Public Welfare Project of Zhoushan (2017C32083). The authors also sincerely thank Prof. Hong-Nong Chou at Institute of Fisheries Science, National Taiwan University, for kindly providing Prorocentrum mexicanum PM01.	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J	Liu, DY; Wang, YN; Wang, YQ; Keesing, JK				Liu, Dongyan; Wang, Yanna; Wang, Yueqi; Keesing, John K.			Ocean fronts construct spatial zonation in microfossil assemblages	GLOBAL ECOLOGY AND BIOGEOGRAPHY			English	Article						Chinese seas; continental shelf; cyst; diatom; marine sediment; mesoscale fronts; palaeoecology; remote sensing; two-way indicator species analysis	BOTTOM BOUNDARY-LAYER; SURFACE SEDIMENTS; DIATOM DISTRIBUTION; SOUTHERN-OCEAN; YELLOW SEA; DYE TRACER; CHINA; PHYTOPLANKTON; FLOW; CLIMATOLOGY	Aim Integration of macroecology and palaeoecology is an important trend in understanding rapidly changing marine ecosystems. However, the spatial mismatch between these two data types has led to difficulties in interpretation, particularly for short-lived phytoplankton and their microfossils. Fronts are narrow transition zones between distinct water masses and play an essential role in partitioning phytoplankton assemblages in the ocean. Whether they also delimit microfossil assemblages deposited at the sea floor is unclear. We examined the correlation between quasi-stationary mesoscale fronts and the spatial distribution of microfossils (diatoms, dinoflagellates and silicoflagellates) in the Bohai, Yellow and East China Seas, to establish a causal link between microfossil assemblages and the factors controlling pelagic species assemblages on continental shelves. Location Time period China. 2003-2015. Major taxa studied Methods Phytoplankton. Front locations were determined using gradient analysis of monthly satellite sea surface temperature (SST) for 2003-2015. Microfossil assemblages were classified using two-way indicator species analysis of the relative abundance of 345 species collected from surface sediments at 126 sites. The relationships between frontal patterns and microfossil assemblages were evaluated by superimposing maps of front location, microfossil distribution and environmental features in the main water masses and by canonical correspondence analysis. Results Main conclusions Ten major fronts and four primary microfossil assemblages were identified. Analyses of the spatial patterns of fronts, microfossil assemblages, SST, salinity and nutrients revealed that the fronts partitioned the microfossils into assemblage types corresponding to the physicochemical features of the water masses. Microfossil species assemblages and their indicator species are separated by mesoscale fronts and are correlated with water properties. Producing base maps of microfossil assemblages in relationship to SST fronts enables examination of the importance of quasi-stationary mesoscale fronts in constructing microfossil patterns on continental shelves. The results displayed potential for the interpretation sediment core data and their integration with the macroecological context.	[Liu, Dongyan; Wang, Yanna] East China Normal Univ, State Key Lab Estuarine & Coastal Res, North Zhongshan Rd 3663, Shanghai 200062, Peoples R China; [Wang, Yueqi] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Key Lab Coastal Zone Environm Proc & Ecol Remedia, Beijing 100864, Shandong, Peoples R China; [Keesing, John K.] Univ Western Australia, Oceans Inst, Indian Ocean Marine Res Ctr, CSIRO Oceans & Atmosphere Res, Crawley, WA, Australia	East China Normal University; Chinese Academy of Sciences; Yantai Institute of Coastal Zone Research, CAS; University of Western Australia; Commonwealth Scientific & Industrial Research Organisation (CSIRO)	Liu, DY (通讯作者)，East China Normal Univ, State Key Lab Estuarine & Coastal Res, North Zhongshan Rd 3663, Shanghai 200062, Peoples R China.	dyliu@sklec.ecnu.edu.cn	wang, yq/F-3244-2012; Keesing, John/B-1955-2009	Liu, Dongyan/0000-0003-3606-9846; Keesing, John/0000-0002-0876-2144	Natural Science Foundation of China [41376121]; Chinese Academy of Sciences [XDA11020405]; Ministry of Science and Technology [2016YFE0133700]	Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Chinese Academy of Sciences(Chinese Academy of Sciences); Ministry of Science and Technology(Spanish Government)	Natural Science Foundation of China, Grant/Award Number: 41376121; Chinese Academy of Sciences, Grant/Award Number: XDA11020405; Ministry of Science and Technology, Grant/Award Number: 2016YFE0133700.	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Ecol. Biogeogr.	OCT	2018	27	10					1225	1237		10.1111/geb.12779	http://dx.doi.org/10.1111/geb.12779			13	Ecology; Geography, Physical	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography	GZ6RJ		Green Published			2025-03-11	WOS:000449568800008
J	Lammertsma, EI; Troelstra, SR; Flores, JA; Sangiorgi, F; Chemale, F; do Carmo, DA; Hoorn, C				Lammertsma, E. I.; Troelstra, S. R.; Flores, J. -A.; Sangiorgi, F.; Chemale, F., Jr.; do Carmo, D. A.; Hoorn, C.			Primary productivity in the western tropical Atlantic follows Neogene Amazon River evolution	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Amazon Fan; Brazilian Equatorial Margin; Neogene; Foraminifera; Organic-walled dinoflagellate cysts	WALLED DINOFLAGELLATE CYSTS; LATE MIOCENE ONSET; SEA FAN EVIDENCE; MARINE-SEDIMENTS; NORTH; DISPERSAL; PLUME; FOZ; DISCHARGE; HISTORY	The Amazon River nutrient-rich plume currently triggers large-scale phytoplankton blooms in the otherwise oligotrophic western tropical Atlantic Ocean. Little is known about the onset and development of this high productivity system, although a direct link to the transcontinental Amazon River evolution can be expected. The Amazon submarine fan, located on the Brazilian Equatorial Margin (BEM), contains a unique sediment archive of the river's history and associated environmental changes in the marine realm. This study represents the first marine microfossil multi-proxy approach applied to any sedimentary record in the submarine fan area for the time interval encompassing the onset and development of the transcontinental Amazon River system. To reconstruct Miocene to Pleistocene changes in surface- and bottom water conditions we analyzed organic-walled dinoflagellate cyst- and benthic foraminiferal assemblages, respectively. Moreover, terrestrial- and freshwater palynomorph abundances were studied to provide a link between fluvial input and marine environmental changes. In addition, a planktonic foraminiferal biostratigraphy is constructed to verify the available calcareous nannofossil-based age model. Our data show that in the early- mid Miocene up to similar to 13 Ma limited fluvial input reached the BEM and primary productivity was elevated, after which distinctly low productivity conditions prevailed. After the birth of the transcontinental Amazon at 9 Ma surface water productivity initially increased slightly. Consistently high surface water productivity and decreased bottom water oxygenation followed increasing terrestrial input after the (early) Pliocene. The temporal consistency between records from the Amazon Fan and the more distant Ceara Rise reflects large-scale marine environmental changes followed the development of the Amazon River, likely related to increased climatic variability in the Amazon Basin during the Plio-Pleistocene.	[Lammertsma, E. I.; Hoorn, C.] Univ Amsterdam, IBED, POB 94248, NL-1090 GE Amsterdam, Netherlands; [Lammertsma, E. I.; Chemale, F., Jr.; do Carmo, D. A.] Univ Brasilia, Inst Geosci, BR-70297400 Brasilia, DF, Brazil; [Troelstra, S. R.] Vrije Univ Amsterdam, Cluster Earth & Climate, Boelelaan 1085, NL-1081 HV Amsterdam, Netherlands; [Troelstra, S. R.] NBC Naturalis, Darwinweg 2, NL-2333 CR Leiden, Netherlands; [Flores, J. -A.] Univ Salamanca, Dept Geol, Grp Geociencias Ocean, Cardenal Pla y Deniel 22, E-37008 Salamanca, Spain; [Sangiorgi, F.] Univ Utrecht, Dept Earth Sci Marine Palynol & Paleoceanog, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands	University of Amsterdam; Universidade de Brasilia; Vrije Universiteit Amsterdam; Naturalis Biodiversity Center; University of Salamanca; Utrecht University	Lammertsma, EI (通讯作者)，Univ Amsterdam, IBED, POB 94248, NL-1090 GE Amsterdam, Netherlands.	emmylam@gmail.com; s.r.troelstra@vu.nl; flores@usal.es; f.sangiorgi@uu.nl; faridcj@unisinos.br; delei1998@gmail.com; m.c.hoorn@uva.nl	Flores, José-Abel/D-4218-2009; Troelstra, Simon/O-2355-2019; Do Carmo, Dermeval/AAL-9767-2020; Chemale, Farid/D-1798-2013; Hoorn, Carina/A-9372-2015	Hoorn, Carina/0000-0001-5402-6191; Chemale Junior, Farid/0000-0001-5003-5824; Sangiorgi, Francesca/0000-0003-4233-6154; DO CARMO, DERMEVAL APARECIDO/0000-0002-1613-7242	CLIM-AMAZON European Union's Seventh Framework Program (FP7/2007-2013); Universidade de Brasilia [295091]	CLIM-AMAZON European Union's Seventh Framework Program (FP7/2007-2013)(European Union (EU)); Universidade de Brasilia	CLIM-AMAZON European Union's Seventh Framework Program (FP7/2007-2013) and the Universidade de Brasilia funded E.L. 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Paleoclimatol. Paleoecol.	OCT 1	2018	506						12	21		10.1016/j.palaeo.2018.05.048	http://dx.doi.org/10.1016/j.palaeo.2018.05.048			10	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	GP6AU		Green Published			2025-03-11	WOS:000440960100002
J	Guo, RY; Liang, YT; Xing, Y; Wang, L; Mou, SL; Cao, CJ; Xie, RZ; Zhang, CL; Tian, JW; Zhang, YY				Guo, Ruoyu; Liang, Yantao; Xing, Yu; Wang, Long; Mou, Shanli; Cao, Chunjie; Xie, Ruize; Zhang, Chuanlun; Tian, Jiwei; Zhang, Yongyu			Insight Into the Pico- and Nano-Phytoplankton Communities in the Deepest Biosphere, the Mariana Trench	FRONTIERS IN MICROBIOLOGY			English	Article						pico- and nano-phytoplankton; 18S rRNA; plastid 23S rRNA; Mariana Trench; deep sea	RIBOSOMAL-RNA GENE; DISTRIBUTION PATTERNS; CHALLENGER DEEP; MARINE CYANOBACTERIA; EUKARYOTIC ALGAE; FECAL PELLETS; GROWTH-RATE; OCEAN; DIVERSITY; PROCHLOROCOCCUS	As photoautotrophs, phytoplankton are generally present in the euphotic zone of the ocean, however, recently healthy phytoplankton cells were found to be also ubiquitous in the dark deep sea, i.e., at water depths between 2000 and 4000 m. The distributions of phytoplankton communities in much deeper waters, such as the hadal zone, are unclear. In this study, the vertical distribution of the pico- and nano-phytoplankton (PN) communities from the surface to 8320 m, including the epipelagic, mesopelagic, bathypelagic, and hadal zones, were investigated via both 18S and p23S rRNA gene analysis in the Challenger Deep of the Mariana Trench. The results showed that Dinoflagellata, Chrysophyceae, Haptophyta, Chlorophyta, Prochloraceae, Pseudanabaenaceae, Synechococcaceae, and Eustigmatophyceae, etc., were the predominant PN in the Mariana Trench. Redundancy analyses revealed that depth, followed by temperature, was the most important environmental factors correlated with vertical distribution of PN community. In the hadal zone, the PN community structure was considerably different from those in the shallower zones. Some PN communities, e.g., Eustigmatophyceae and Chrysophyceae, which have the heterotrophic characteristics, were sparse in shallower waters, while they were identified with high relative abundance (94.1% and 20.1%, respectively) at the depth of 8320 m. However, the dinoflagellates and Prochloraceae Prochlorococcus were detected throughout the entire water column. We proposed that vertical sinking, heterotrophic metabolism, and/or the transition to resting stage of phytoplankton might contribute to the presence of phytoplankton in the hadal zone. This study provided insight into the PN community in the Mariana Trench, implied the significance of phytoplankton in exporting organic matters from the euphotic to the hadal zone, and also hinted the possible existence of some undetermined energy metabolism (e.g., heterotrophy) of phytoplankton making themselves adapt and survive in the hadal environment.	[Guo, Ruoyu; Liang, Yantao; Wang, Long; Mou, Shanli; Cao, Chunjie; Xie, Ruize; Zhang, Yongyu] Chinese Acad Sci, Qingdao Inst Bioenergy & Bioproc Technol, Key Lab Biofuels, Shandong Prov Key Lab Energy Genet, Qingdao, Peoples R China; [Xing, Yu; Tian, Jiwei] Ocean Univ China, Qingdao Collaborat Innovat Ctr Marine Sci & Techn, Key Lab Marine Chem Theory & Engn, Phys Oceanog Lab, Qingdao, Peoples R China; [Zhang, Chuanlun] Southern Univ Sci & Technol, Dept Ocean Sci & Engn, Shenzhen, Peoples R China	Chinese Academy of Sciences; Qingdao Institute of Bioenergy & Bioprocess Technology, CAS; Ocean University of China; Southern University of Science & Technology	Zhang, YY (通讯作者)，Chinese Acad Sci, Qingdao Inst Bioenergy & Bioproc Technol, Key Lab Biofuels, Shandong Prov Key Lab Energy Genet, Qingdao, Peoples R China.; Tian, JW (通讯作者)，Ocean Univ China, Qingdao Collaborat Innovat Ctr Marine Sci & Techn, Key Lab Marine Chem Theory & Engn, Phys Oceanog Lab, Qingdao, Peoples R China.	tianjw@ouc.edu.cn; zhangyy@qibebt.ac.cn	Xing, Yu/HOF-0285-2023; Guo, Ruoyu/HTS-1354-2023	Xie, Ruize/0000-0002-9105-9141; Guo, Ruoyu/0000-0002-3625-5983	National Key Research and Development Program of China [2016YFA0601402]; Fourth Polar Observation Program (Deep Sea Exploration Program, Qingdao National Laboratory for Marine Science and Technology); open task of Qingdao National Laboratory for Marine Science and Technology [QNLM2016ORP0311]; China Postdoctoral Science Foundation [2017M610452]; Natural Science Foundation of China [41606153, 41673073, 41806172]; CNOOC Tianjin project [CNOOC-KJ 125 FZDXM 00TJ 001-2014]; senior user's project of RV KEXUE [KEXUE2018G02]; "One Three Five" research project of QIBEBT	National Key Research and Development Program of China(National Key Research & Development Program of China); Fourth Polar Observation Program (Deep Sea Exploration Program, Qingdao National Laboratory for Marine Science and Technology); open task of Qingdao National Laboratory for Marine Science and Technology; China Postdoctoral Science Foundation(China Postdoctoral Science Foundation); Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); CNOOC Tianjin project; senior user's project of RV KEXUE; "One Three Five" research project of QIBEBT	This work was supported by the National Key Research and Development Program of China (2016YFA0601402), the Fourth Polar Observation Program (i.e., Deep Sea Exploration Program, Qingdao National Laboratory for Marine Science and Technology), the open task of Qingdao National Laboratory for Marine Science and Technology (QNLM2016ORP0311), the China Postdoctoral Science Foundation funded project (2017M610452), the Natural Science Foundation of China (41606153, 41673073, and 41806172), the CNOOC Tianjin project (CNOOC-KJ 125 FZDXM 00TJ 001-2014), the senior user's project of RV KEXUE (KEXUE2018G02), and the "One Three Five" research project of QIBEBT. This study was a contribution to the international IMBER project.	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Microbiol.	SEP 26	2018	9								2289	10.3389/fmicb.2018.02289	http://dx.doi.org/10.3389/fmicb.2018.02289			14	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	GU9CF	30319587	Green Published, gold			2025-03-11	WOS:000445641400001
J	Spilling, K; Olli, K; Lehtoranta, J; Kremp, A; Tedesco, L; Tamelander, T; Klais, R; Peltonen, H; Tamminen, T				Spilling, Kristian; Olli, Kalle; Lehtoranta, Jouni; Kremp, Anke; Tedesco, Letizia; Tamelander, Tobias; Klais, Riina; Peltonen, Heikki; Tamminen, Timo			Shifting Diatom-Dinoflagellate Dominance During Spring Bloom in the Baltic Sea and its Potential Effects on Biogeochemical Cycling	FRONTIERS IN MARINE SCIENCE			English	Review						eutrophication; pelagic-benthic coupling; ecosystem functioning; community composition; plankton sedimentation; carbon sink	DISSOLVED ORGANIC-MATTER; PERIDINIELLA-CATENATA DINOPHYCEAE; PHYTOPLANKTON COMMUNITY STRUCTURE; BASIN-SCALE CHANGES; SCRIPPSIELLA-HANGOEI; CLIMATE-CHANGE; VERNAL BLOOM; MARINE DINOFLAGELLATE; VERTICAL-DISTRIBUTION; CYANOBACTERIA BLOOMS	The Baltic Sea is affected by a range of human induced environmental pressures such as eutrophication. Here we synthesize the ongoing shift from diatom dominance toward more dinoflagellates in parts of the Baltic Sea during the spring bloom and its potential effects on biogeochemical cycling of key elements (e.g., C, N, and P). The spring bloom is the period with the highest annual primary production and sinking of organic matter to the sediment. The fate of this organic matter is a key driver for material fluxes, affecting ecosystem functioning and eutrophication feedback loops. The dominant diatoms and dinoflagellates appear to be functionally surrogates as both groups are able to effectively exhaust the wintertime accumulation of inorganic nutrients and produce bloom level biomass that contribute to vertical export of organic matter. However, the groups have very different sedimentation patterns, and the seafloor has variable potential to mineralize the settled biomass in the different sub-basins. While diatoms sink quickly out of the euphotic zone, dinoflagellates sink as inert resting cysts, or lyse in the water column contributing to slowly settling phyto-detritus. The dominance by either phytoplankton group thus directly affects both the summertime nutrient pools of the water column and the input of organic matter to the sediment but to contrasting directions. The proliferation of dinoflagellates with high encystment efficiency could increase sediment retention and burial of organic matter, alleviating the eutrophication problem and improve the environmental status of the Baltic Sea.	[Spilling, Kristian; Lehtoranta, Jouni; Kremp, Anke; Tedesco, Letizia; Peltonen, Heikki; Tamminen, Timo] Finnish Environm Inst SYKE, Helsinki, Finland; [Spilling, Kristian; Tamelander, Tobias] Univ Helsinki, Fac Biol & Environm Sci, Tvarminne Zool Stn, Hango, Finland; [Olli, Kalle; Klais, Riina] Univ Tartu, Inst Ecol & Earth Sci, Tartu, Estonia; [Olli, Kalle] Estonian Univ Life Sci, Inst Agr & Environm Sci, Tartu, Estonia	Finnish Environment Institute; University of Helsinki; University of Tartu; Tartu University Institute of Ecology & Earth Sciences; Estonian University of Life Sciences	Spilling, K (通讯作者)，Finnish Environm Inst SYKE, Helsinki, Finland.; Spilling, K (通讯作者)，Univ Helsinki, Fac Biol & Environm Sci, Tvarminne Zool Stn, Hango, Finland.	kristian.spilling@environment.fi	Olli, Kalle/G-5389-2010; Spilling, Kristian/KEH-0764-2024; Tedesco, Letizia/B-2884-2013	Peltonen, Heikki/0000-0001-9056-8342; Lehtoranta, Jouni/0000-0003-0853-7331; Tedesco, Letizia/0000-0001-9051-8177	Academy of Finland [259164, 263376]; Estonian Research Council [1575P]; Walter and Andree de Nottbeck Foundation; Swedish Cultural Heritage; COCOA-Nutrient cocktail in coastal zones of the Baltic Sea-EU BONUS project; Academy of Finland (AKA) [263376, 259164] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); Estonian Research Council(Estonian Research Council); Walter and Andree de Nottbeck Foundation; Swedish Cultural Heritage; COCOA-Nutrient cocktail in coastal zones of the Baltic Sea-EU BONUS project; Academy of Finland (AKA)(Research Council of Finland)	This study was supported by the Academy of Finland (decisions no 259164 and 263376) and Estonian Research Council (no 1575P, KO). Further funding came from Walter and Andree de Nottbeck Foundation (KS and ToT) and the Swedish Cultural Heritage (ToT). LT acknowledges support also from COCOA-Nutrient cocktail in coastal zones of the Baltic Sea-EU BONUS project.	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J	Hardy, W; Marret, F; Penaud, A; Le Mézo, P; Droz, L; Marsset, T; Kageyama, M				Hardy, William; Marret, Fabienne; Penaud, Aurelie; Le Mezo, Priscilla; Droz, Laurence; Marsset, Tania; Kageyama, Masa			Quantification of last glacial-Holocene net primary productivity and upwelling activity in the equatorial eastern Atlantic with a revised modern dinocyst database	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Transfer function; West Equatorial Africa; Orbital forcing; Carbon cycle	SEA-SURFACE-TEMPERATURE; DINOFLAGELLATE CYST DISTRIBUTION; ORGANIC-CARBON ACCUMULATION; OCEANIC PRIMARY PRODUCTION; SOUTH-ATLANTIC; NORTH-ATLANTIC; PLANKTONIC-FORAMINIFERA; SEASONAL VARIABILITY; CLIMATE CHANGES; HIGH-LATITUDES	In order to better explore quantitative reconstructions of net primary productivity (NPP) conditions using a dinoflagellate cyst (dinocyst)-based transfer function method, we revised the tropical Atlantic modern dinocyst database n = 208 (Marret et al., 2008). Modern assemblages from the worldwide dinocyst atlas (Zonneveld et al., 2013) were added to provide a better geographical coverage of the South Atlantic Ocean. The environmental dataset was updated using the World Ocean Atlas 2013 for sea-surface temperature (SST) and sea-surface salinity (SSS) data, as well as for 1997-2017 mean NPP values recorded during SeaWifs and MODIS spatial programs. New environmental datasets were tested using anomalies regarding mean latitudinal SST as a potential index to track past upwelling activity. Finally, preindustrial NPP values, simulated with the IPSL-CM5A-LR model developed at the Institut Pierre Simon Laplace (IPSL) have been added to the dinocyst environmental database to provide NPP values consistent with the mean age of "modern" dinocyst assemblages. The transfer function method using the updated modern database was then applied to fossil dinocyst assemblages of core KZAI-01, retrieved off the Congo River mouth and covering the last 43.2 kyr. Our results indicate a dominant orbital forcing, with higher primary productivity values reconstructed during precession minima (MIS 3 and the last deglaciation) and enhanced by a maximum of obliquity during the last deglaciation and the Holocene. The synchronicity between high upwelling intensity and high terrigenous inputs during high NPP period (e.g. during the last Deglaciation) highlighted the prevalent role of river-induced upwelling activity, which is specific to the Congo River. These results have improved our understanding of the environmental forcing leading to major trophic changes in the intertropical area.	[Hardy, William; Penaud, Aurelie; Droz, Laurence] IUEM UBO, UMR CNRS 6538, LGO, F-29280 Plouzane, France; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Le Mezo, Priscilla] ICTA, Barcelona, Spain; [Marsset, Tania] IFREMER, Geosci Marines, BP 70, F-29280 Plouzane, France; [Kageyama, Masa] CEA CNRS UVSQ, Ctr CEA Saclay, UMR CNRS 8112, LSCE IPSL, F-91191 Gif Sur Yvette, France	Universite de Bretagne Occidentale; University of Liverpool; Autonomous University of Barcelona; Universite Paris Cite; Ifremer; CEA; Universite Paris Saclay; Sorbonne Universite	Hardy, W (通讯作者)，IUEM UBO, UMR CNRS 6538, LGO, F-29280 Plouzane, France.	william.hardy@univ-brest.fr; F.Marret@liverpool.ac.uk	Marsset, Tania/A-4163-2012; KAGEYAMA, Masa/F-2389-2010; Droz, Laurence/P-8209-2019; Penaud, Aurelie/F-2485-2011	Droz, Laurence/0000-0002-6694-1247; Le Mezo, Priscilla K./0000-0002-5695-4845; Marsset, Tania/0000-0002-5245-6566; Penaud, Aurelie/0000-0003-3578-4549; Marret-Davies, Fabienne/0000-0003-4244-0437	Brittany Region [ANR-10-LABX-19]; French government under the program "Investissements d'Avenir"; "Laboratoire d'Excellence" LabexMER [ANR-10-LABX-19]	Brittany Region(Region Bretagne); French government under the program "Investissements d'Avenir"(Agence Nationale de la Recherche (ANR)); "Laboratoire d'Excellence" LabexMER	William Hardy's PhD was funded by the Brittany Region and this work was supported by the "Laboratoire d'Excellence" LabexMER (ANR-10-LABX-19) and co-funded by a grant from the French government under the program "Investissements d'Avenir". We thank B. Dennielou (Ifremer, Brest) for access to core KZAI-01. We are very grateful for the constructive comments from two anonymous reviewers that helped to greatly improve this manuscript.	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Paleoclimatol. Paleoecol.	SEP 15	2018	505						410	427		10.1016/j.palaeo.2018.06.025	http://dx.doi.org/10.1016/j.palaeo.2018.06.025			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	GM8KO					2025-03-11	WOS:000438477700035
J	Hartman, JD; Sangiorgi, F; Salabarnada, A; Peterse, F; Houben, AJP; Schouten, S; Brinkhuis, H; Escutia, C; Bijl, PK				Hartman, Julian D.; Sangiorgi, Francesca; Salabarnada, Ariadna; Peterse, Francien; Houben, Alexander J. P.; Schouten, Stefan; Brinkhuis, Henk; Escutia, Carlota; Bijl, Peter K.			Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica - Part 3: Insights from Oligocene-Miocene TEX<sub>86</sub>-based sea surface temperature reconstructions	CLIMATE OF THE PAST			English	Article							ISOPRENOID TETRAETHER LIPIDS; WALLED DINOFLAGELLATE CYSTS; OCEAN CIRCULATION CHANGES; STABLE-ISOTOPE RECORDS; CIRCUMPOLAR CURRENT; MEMBRANE-LIPIDS; CARBON-CYCLE; SINKING PARTICLES; DRILLING-PROJECT; ATMOSPHERIC CO2	The volume of the Antarctic continental ice sheet(s) varied substantially during the Oligocene and Miocene (similar to 34-5 Ma) from smaller to substantially larger than today, both on million-year and on orbital timescales. However, reproduction through physical modeling of a dynamic response of the ice sheets to climate forcing remains problematic, suggesting the existence of complex feedback mechanisms between the cryosphere, ocean, and atmosphere systems. There is therefore an urgent need to improve the models for better predictions of these systems, including resulting potential future sea level change. To assess the interactions between the cryosphere, ocean, and atmosphere, knowledge of ancient sea surface conditions close to the Antarctic margin is essential. Here, we present a new TEX86-based sea surface water paleotemperature record measured on Oligocene sediments from Integrated Ocean Drilling Program (IODP) Site U1356, offshore Wilkes Land, East Antarctica. The new data are presented along with previously published Miocene temperatures from the same site. Together the data cover the interval between similar to 34 and similar to 11 Ma and encompasses two hiatuses. This record allows us to accurately reconstruct the magnitude of sea surface temperature (SST) variability and trends on both million-year and glacial-interglacial timescales. On average, TEX86 values indicate SSTs ranging between 10 and 21 degrees C during the Oligocene and Miocene, which is on the upper end of the few existing reconstructions from other high-latitude Southern Ocean sites. SST maxima occur around 30.5, 25, and 17 Ma. Our record suggests generally warm to temperate ocean offshore Wilkes Land. Based on lithological alternations detected in the sedimentary record, which are assigned to glacial-interglacial deposits, a SST variability of 1.5-3.1 degrees C at glacial-interglacial timescales can be established. This variability is slightly larger than that of deep-sea temperatures recorded in Mg/Ca data. Our reconstructed Oligocene temperature variability has implications for Oligocene ice volume estimates based on benthic delta O-18 records. If the long-term and orbital-scale SST variability at Site U1356 mirrors that of the nearby region of deep-water formation, we argue that a substantial portion of the variability and trends contained in long-term delta O-18 records can be explained by variability in Southern high-latitude temperature and that the Antarctic ice volume may have been less dynamic than previously thought. Importantly, our temperature record suggests that Oligocene-Miocene Antarctic ice sheets were generally of smaller size compared to today.	[Hartman, Julian D.; Sangiorgi, Francesca; Peterse, Francien; Brinkhuis, Henk; Bijl, Peter K.] Univ Utrecht, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol, Dept Earth Sci, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands; [Salabarnada, Ariadna; Escutia, Carlota] Univ Granada, CSIC, Inst Andaluz Ciencias Tierra, Ave Palmeras 4, Granada 18100, Spain; [Houben, Alexander J. P.] Netherlands Org Appl Sci Res TNO, Appl Geosci Team, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [Schouten, Stefan; Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, Landsdiep 4, NL-1797 SZ T Horntje, Texel, Netherlands; [Schouten, Stefan; Brinkhuis, Henk] Univ Utrecht, Landsdiep 4, NL-1797 SZ T Horntje, Texel, Netherlands	Utrecht University; University of Granada; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT); Netherlands Organization Applied Science Research; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Hartman, JD (通讯作者)，Univ Utrecht, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol, Dept Earth Sci, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands.	juulhartman@gmail.com	Brinkhuis, Henk/IUO-8165-2023; Schouten, Stefan/P-4380-2016; Roset, Ariadna/L-8798-2014; Peterse, Francien/AAY-1473-2021; Escutia, Carlota/B-8614-2015; Peterse, Francien/H-5627-2011	Hartman, Julian/0000-0001-6256-9989; Escutia, Carlota/0000-0002-4932-8619; Brinkhuis, Henk/0000-0003-0253-6610; Bijl, Peter/0000-0002-1710-4012; Salabarnada, Ariadna/0000-0003-2239-2538; Peterse, Francien/0000-0001-8781-2826; Houben, Alexander/0000-0002-9497-1048; Salabarnada, Ariadna/0000-0003-0858-8083; Sangiorgi, Francesca/0000-0003-4233-6154	NWO Netherlands Polar Program [866.10.110]; Netherlands Earth System Science Centre (NESSC) - Dutch Ministry of Education, Culture and Science (OCW); NWO-ALW VENI grant [863.13.002, 863.13.016]; Spanish Ministerio de Econimia y Competitividad [CTM2014-60451-C2-1-P]; US National Science Foundation	NWO Netherlands Polar Program; Netherlands Earth System Science Centre (NESSC) - Dutch Ministry of Education, Culture and Science (OCW); NWO-ALW VENI grant; Spanish Ministerio de Econimia y Competitividad; US National Science Foundation(National Science Foundation (NSF))	Julian D. Hartman, Francesca Sangiorgi, Henk Brinkhuis, and Peter K. Bijl acknowledge the NWO Netherlands Polar Program project number 866.10.110. Stefan Schouten was supported by the Netherlands Earth System Science Centre (NESSC), funded by the Dutch Ministry of Education, Culture and Science (OCW). Peter K. Bijl and Francien Peterse received funding through NWO-ALW VENI grant nos. 863.13.002 and 863.13.016, respectively. Carlota Escutia and Ariadna Salabarnada thank the Spanish Ministerio de Econimia y Competitividad for grant CTM2014-60451-C2-1-P. We thank Alexander Ebbing and Anja Bruls for GDGT sample preparation during their MSc research. This research used samples from the Integrated Ocean Drilling Program (IODP). IODP was sponsored by the US National Science Foundation and participating countries under management of Joined Oceanographic Institutions Inc. This research is a contribution to the SCAR PAIS program. We thank Stephen Gallagher and the two anonymous reviewers for their thorough review and constructive comments, which helped improve this paper.	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J	Mohamed, ZA				Mohamed, Zakaria A.			Potentially harmful microalgae and algal blooms in the Red Sea: Current knowledge and research needs	MARINE ENVIRONMENTAL RESEARCH			English	Article						Harmful algae; Cyanobacteria; Red sea; Phycotoxins; Blooms	YEMENI COASTAL WATERS; 1ST RECORDED BLOOM; DINOFLAGELLATE CYSTS; MARINE-SEDIMENTS; SAUDI-ARABIA; PHYTOPLANKTON; GULF; CHLOROPHYLL; AQABA; CYANOBACTERIA	Harmful algal blooms (HABs) have increased throughout the world's coastal oceans during the last century mostly due to water eutrophication and climate change. These blooms are often accompanied by extreme extensive negative impacts to fisheries, coastal resources, public health and local economies, However, limited studies have reported HAB events in Red Sea coastal waters. This article reviews potentially harmful microalgae in the Red Sea, based on available published information during the last 3 decades. Five harmful algal blooms were recorded in the Red Sea; of which 3 blooms are formed by dinoflagellates (Noctiluca scintillans, Pyrodinuium bahamense, Protoperidinium quinquecorne), one by raphidophytes (Heterosigma akashiwo) and one by cyanobacteria (Trichodesmium erythraeum). Additionally, mangrove swamps in the Red Sea were occupied by cyanobacterial mats, which contain microcystin and saxitoxin-producing species. The existing data in this review could be a catalyst for the establishment of monitoring and management program for HABs and their toxins in Red Sea coastal waters. This review also identifies current research gaps and suggests future research directions.	[Mohamed, Zakaria A.] Sohag Univ, Fac Sci, Dept Bot & Microbiol, Sohag 82524, Egypt	Egyptian Knowledge Bank (EKB); Sohag University	Mohamed, ZA (通讯作者)，Sohag Univ, Fac Sci, Dept Bot & Microbiol, Sohag 82524, Egypt.	mzakaria_99@yahoo.com						Abd-Elhaleem Z. 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J	Gurdebeke, PR; Pospelova, V; Mertens, KN; Dallimore, A; Chana, J; Louwye, S				Gurdebeke, Pieter R.; Pospelova, Vera; Mertens, Kenneth Neil; Dallimore, Audrey; Chana, Jasmin; Louwye, Stephen			Diversity and distribution of dinoflagellate cysts in surface sediments from fjords of western Vancouver Island (British Columbia, Canada)	MARINE MICROPALEONTOLOGY			English	Article						Process length of Protoceratium reticulatum cysts; Biogenic silica; Total organic carbon; Dinoflagellate cyst diversity; Testate amoebae; Estuary	RECENT MARINE-SEDIMENTS; EFFINGHAM INLET; PROTOCERATIUM-RETICULATUM; ENVIRONMENTAL-FACTORS; SPATIAL-DISTRIBUTION; ABSOLUTE ABUNDANCE; THECA RELATIONSHIP; ORGANIC-MATTER; ANOXIC FJORD; SP NOV.	A total of 31 surface sediment samples from 16 coastal inlets in five sounds of western Vancouver Island were investigated for dinoflagellate cysts and other palynomorphs. Well-preserved and abundant dinoflagellate cysts were recovered, including a total of 32 cyst taxa belonging to four families. Total dinoflagellate cyst concentrations vary two orders of magnitude, with concentrations between 2267 and 918,584 cysts g(-1). The highest values were observed in samples from Tofino Inlet. Southern sites are characterized by cysts of autotrophic dinoflagellates, mainly Operculochnium centrocarpum sensu Wall & Dale 1966. Other abundant cysts of autotrophic dinoflagellates are Spiniferites spp. and cysts of Pentapharsodinium dalei. In general, other inlets in Quatsino, Kyuquot-Nootka and Clayoquot Sounds have lower total concentrations but have more cysts of heterotrophic dinoflagellates, mainly Round brown cysts, Brigantedinium spp., and Spiny brown cysts. Neroutsos Inlet is characterized by high concentrations of Arcellacean testate amoebae. Within inlets, cyst concentrations and assemblages vary. Near the heads of the inlets, concentrations are generally lower and assemblages are dominated by cysts of autotrophic dinoflagellates, mostly O. centroccupum sensu Wall & Dale 1966. Concentrations of cysts produced by heterotrophic dinoflagellates and their proportions in the assemblages generally increase from the head to the mouth of each inlet. Measured sedimentary biogenic silica abundances (%Opal) have consistently higher values in Clayoquot Sound and lower values in Quatsino Sound. Within individual inlets, biogenic silica generally increases in the head to mouth direction. The trend in heterotrophic cyst abundances is similar. Correlations between total organic carbon (TOC), total nitrogen (TN) and terrestrial palynomorph concentrations in the sediments indicate that the organic material at sites near inlet heads are mainly derived from terrestrial input. A significant negative correlation between biogenic silica and TOC/TN ratio was observed in the dataset, but not between the total heterotrophic cyst concentrations and relative abundances of biogenic silica. Statistical analyses (PCA, RDA) indicate that the assemblages of dinoflagellate cysts and other palynomorphs, their spatial distributions, and sedimentary geochemical measurements are related to the regional environmental setting (e.g., latitudinal trends in weather, primary productivity, and upwelling) and local characteristics of the inlets (e.g., site location relative to freshwater input, inlet morphology and bathymetry, as well as possible anthropogenic influences). Process length variation of O. centroccupurn sensu Wall & Dale 1966 was measured and it is comparable to previous measurements in similar environmental settings, allowing seawater densities to be inferred. Cysts of Alexandriurn spp. were found in most of the samples, with the highest abundance in the inlet heads of Kyuquot and Quatsino Sounds.	[Gurdebeke, Pieter R.; Louwye, Stephen] Univ Ghent, Dept Geol, Krijgslaan 281 S8, B-9000 Ghent, Belgium; [Pospelova, Vera; Chana, Jasmin] Univ Victoria, Sch Earth Sci, Bob Wright Ctr A405, POB 1700,STN CSC, Victoria, BC, Canada; [Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France; [Dallimore, Audrey] Royal Rd Univ, Sch Environm & Sustainabil, 2005 Sooke Rd, Victoria, BC V9B 5Y2, Canada	Ghent University; University of Victoria; Ifremer	Gurdebeke, PR (通讯作者)，Univ Ghent, Dept Geol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	pieter.gurdebeke@ugent.be	Mertens, Kenneth/AAO-9566-2020; Gurdebeke, Pieter/AAY-7059-2020; Mertens, Kenneth/C-3386-2015; Louwye, Stephen/D-3856-2012	Mertens, Kenneth/0000-0003-2005-9483; Gurdebeke, Pieter R./0000-0003-1425-8515; Pospelova, Vera/0000-0003-4049-8133; Louwye, Stephen/0000-0003-4814-4313	Natural Sciences and Engineering Research Council of Canada (NSERC) [RGPIN/6388-2015]	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	The Natural Sciences and Engineering Research Council of Canada (NSERC) provided funding (Discovery and Ship-time Grants) for this work to Vera Pospelova (grant number RGPIN/6388-2015) and Audrey Dallimore. We thank the officers and the crew of the CCGS Vector. Maureen Soon and Alice Chang are thanked for completing the geo-chemical analysis at the University of British Columbia. The constructive remarks by two anonymous reviewers are acknowledged.	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J	Fu, HP; Hu, XMA; Crouch, EM; An, W; Wang, JG; Garzanti, E				Fu, Hanpu; Hu, Xiumian; Crouch, Erica M.; An, Wei; Wang, Jiangang; Garzanti, Eduardo			Upper Cretaceous trench deposits of the Neo-Tethyan subduction zone: Jiachala Formation from Yarlung Zangbo suture zone in Tibet, China	SCIENCE CHINA-EARTH SCIENCES			English	Article						Provenance analysis; Trench deposits; Late Cretaceous; Neo-Tethyan oceanic subduction; Yarlung Zangbo suture zone; Tibet of China	FORE-ARC BASIN; ZIRCON U-PB; HF ISOTOPIC CONSTRAINTS; ASIA COLLISION ONSET; OCEANIC RED BEDS; SOUTHERN TIBET; FACIES ARCHITECTURE; PROVENANCE ANALYSIS; TECTONIC EVOLUTION; GANGDESE BATHOLITH	The history of convergence between the India and the Asia plates, and of their subsequent collision which triggered the Himalayan orogeny is recorded in the Yarlung Zangbo suture zone. Exposed along the southern side of the suture, turbidites of the the Jiachala Formation fed largely from the Gangdese arc have long been considered as post-collisional foreland-basin deposits based on the reported occurrence of Paleocene-early Eocene dinoflagellate cysts and pollen assemblages. Because magmatic activity in the Gangdese arc continued through the Late Cretaceous and Paleogene, this scenario is incompatible with U-Pb ages of detrital zircons invariably older than the latest Cretaceous. To solve this conundrum, we carried out detailed stratigraphic, sedimentological, paleontological, and provenance analyses in the Gyangze and Sajia areas of southern Tibet, China. The Jiachala Formation consists of submarine fan deposits that lie in fault contact with the Zongzhuo Formation. Sandstone petrography together with U-Pb ages and Hf isotope ratios of detrital zircons indicate provenance from the Gangdese arc and central Lhasa terrane. Well preserved pollen or dinoflagellate cysts microfossils were not found in spite of careful research, and the youngest age obtained from zircon grain was similar to 84 Ma. Based on sedimentary facies, provenance analysis and tectonic position, we suggest that the Jiachala Formation was deposited during the Late Cretaceous (similar to 88-84 Ma) in the trench formed along the southern edge of Asia during subduction of Neo-Tethyan oceanic lithosphere.	[Fu, Hanpu; Hu, Xiumian; An, Wei] Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China; [Crouch, Erica M.] GNS Sci, POB 30368, Lower Hutt 5040, New Zealand; [An, Wei] Hefei Univ Technol, Sch Resources & Environm Engn, Hefei 230009, Anhui, Peoples R China; [Wang, Jiangang] Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China; [Garzanti, Eduardo] Univ Milano Bicocca, Dept Earth & Environm Sci, I-20126 Milan, Italy	Nanjing University; GNS Science - New Zealand; Hefei University of Technology; Chinese Academy of Sciences; Institute of Geology & Geophysics, CAS; University of Milano-Bicocca	Hu, XMA (通讯作者)，Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China.	huxm@nju.edu.cn	Crouch, Erica/C-2820-2013		National Natural Science Foundation of China [41525007, 41602115]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank Wang Chengshan, Wu Fuyuan, Li Xianghui, Wan Xiaoqiao and Li Jianguo for constructive discussion and suggestions, Bian Lizeng and Roger Tremain for help in palynological processing, Zhou Bo for assistance in the field, and Lai Wen and Xue Weiwei for help in Hf isotopic analysis. We are grateful to the reviewers for their constructive comments. This work was supported by the National Natural Science Foundation of China (Grant Nos. 41525007, 41602115).	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China-Earth Sci.	SEP	2018	61	9					1204	1220		10.1007/s11430-017-9223-5	http://dx.doi.org/10.1007/s11430-017-9223-5			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GR0RK					2025-03-11	WOS:000442228800005
J	García-Moreiras, I; Pospelova, V; García-Gil, S; Sobrino, CM				Garcia-Moreiras, Iria; Pospelova, Vera; Garcia-Gil, Soledad; Munoz Sobrino, Castor			Climatic and anthropogenic impacts on the Ria de Vigo (NW Iberia) over the last two centuries: A high-resolution dinoflagellate cyst sedimentary record	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Coastal palaeoenvironments; Sea level; Lingulodinium polyedrum; Eutrophication; North Atlantic Oscillation (NAO), Atlantic; Iberian margin	NORTH-ATLANTIC OSCILLATION; SAN-SIMON BAY; ESTUARINE UPWELLING ECOSYSTEM; SEA-SURFACE-TEMPERATURE; DE-VIGO; PALYNOLOGICAL EVIDENCE; ENVIRONMENTAL-CHANGE; PHYTOPLANKTON ASSEMBLAGES; TELECONNECTION PATTERNS; FRESH-WATER	A high-resolution dinoflagellate cyst record spanning the period of similar to 1830-2012 CE from Ria de Vigo (Atlantic margin of NW Iberia) is presented. Changes in concentrations and percentages of dinoflagellate cysts and freshwater algal spores reflect climatic and anthropogenic influences on the ria, i.e. coastal inlet formed by the partial submergence of a river valley. Statistical analyses (PCA and clustering) were used to identify the main patterns of change in the cyst assemblages. The cyst record was compared with reconstructed and measured instrumental environmental data (NAO, temperatures, mean sea level, etc.) to support (palaeo)reconstructions. Four main phases were identified: the first phase (similar to 1830-1855 CE) of lower relative sea level (RSL), temperatures and precipitations represents the last stages of the LIA (Little Ice Age); the second phase (similar to 1855-1910 CE) is interpreted as a transition between the colder LIA and the wetter and warmer conditions that prevailed through the 20th century; the third phase (similar to 1910-1975 CE) is characterized by strong river inputs and water stratification in the ria; and the fourth phase (similar to 1975-2012 CE) reflects impacts of anthropogenic warming and pollution. The anthropogenic signal consists of increases in heterotrophic cyst proportions and cysts diversity, as well as of a marked decline of potentially toxic Lingulodinium machaerophorum. Increasing organic matter content, nutrients and industrial wastes have likely caused detrimental impacts on the autotrophic dinoflagellates, by increasing turbidity and toxicity. The B5-cyst record and its comparison with previously published data suggest that increased concentrations of L. machaerophorum in the 20th century were mainly related to river flow variations, that in turn were primarily driven by NAO changes, rather than cultural eutrophication. We also report high abundances of Peridinium ponticum in our record, determining that this species is not exclusive to the Black and Marmara Seas and has much wider natural distribution.	[Garcia-Moreiras, Iria; Garcia-Gil, Soledad; Munoz Sobrino, Castor] Univ Vigo, Marine Sci Stn Toralla, ECIMAT, Illa Toralla S-N, E-36331 Vigo, Spain; [Garcia-Moreiras, Iria; Munoz Sobrino, Castor] Univ Vigo, Sci Fac, Dept Plant Biol & Soil Sci, Campus Marcosende S-N, E-36310 Vigo, Spain; [Pospelova, Vera] OEASB A405 Univ Victoria, SEOS, 3800 Finnerty Rd, Victoria, BC V8P5C2, Canada; [Garcia-Gil, Soledad] Univ Vigo, Sci Fac, Dept Marine Geosci, Campus Marcosende S-N, E-36310 Vigo, Spain	Universidade de Vigo; CIM UVIGO; Universidade de Vigo; Universidade de Vigo	García-Moreiras, I (通讯作者)，Univ Vigo, Fac Biol, Dept Biol Vexetal & Ciencias Solo, Palynol & Paleobot Lab, Campus Lagoas Marcosende, E-36310 Vigo, Spain.	iriagamo@uvigo.es	Gil, Soledad/H-4460-2015; GARCIA-MOREIRAS, IRIA/H-4627-2015; Munoz Sobrino, Castor/H-2948-2015	GARCIA-MOREIRAS, IRIA/0000-0001-8713-0374; Pospelova, Vera/0000-0003-4049-8133; Munoz Sobrino, Castor/0000-0001-8191-3001	Spanish Ministry of Education and Science - EFRD funds [CGL2012-33584]; Xunta de Galicia [GRC2015/020, PRE/2013/404]; Natural Science and Engineering Research Council of Canada (NSERC); Fundacion Barrie	Spanish Ministry of Education and Science - EFRD funds(German Research Foundation (DFG)); Xunta de Galicia(Xunta de Galicia); Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fundacion Barrie	This work was funded by the Spanish Ministry of Education and Science CGL2012-33584 (co-financed with EFRD funds) and the Xunta de Galicia GRC2015/020 projects. Iria Garcia-Moreiras was supported by a research fellowship from Xunta de Galicia (PRE/2013/404). The authors thank Natalia Martinez Carreno for her contribution with grain size and elemental data. Partial funding for this research was provided by the Natural Science and Engineering Research Council of Canada (NSERC) to Vera Pospelova (Discovery Grant program). The collaboration between the XM-3 group from the University of Vigo and the SEOS department from the University of Victoria was possible thanks to the International Postgraduate Scholarship Programme of the Fundacion Barrie conceded to Iria Garcia Moreiras in 2015. Finally, we would like to thank the editor and three anonymous reviewers for their valuable comments that improved the manuscript.	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Paleoclimatol. Paleoecol.	SEP 1	2018	504						201	218		10.1016/j.palaeo.2018.05.032	http://dx.doi.org/10.1016/j.palaeo.2018.05.032			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	GV6ZJ					2025-03-11	WOS:000446269900015
J	Zonneveld, KAF; Ebersbach, F; Maeke, M; Versteegh, GJM				Zonneveld, Karin A. F.; Ebersbach, Friederike; Maeke, Mara; Versteegh, Gerard J. M.			Transport of organic-walled dinoflagellate cysts in nepheloid layers off Cape Blanc (N-W Africa)	DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS			English	Article						Dinoflagellate cysts; Particle transport; Nepheloid layer	SANTA-BARBARA BASIN; SEDIMENT RESUSPENSION; ENVIRONMENTAL-CHANGE; AEROBIC DEGRADATION; CLIMATE VARIABILITY; UPWELLING SYSTEM; NORTH-ATLANTIC; MATTER; RECORD; OCEAN	Many aspects of to the vertical and lateral transport of organic matter particles produced in the upper ocean are still not clear. This study documents the production, vertical and lateral displacement of the particulate organic matter fraction formed by dinoflagellate cysts in nepheloid layers present off Cape Blanc in November 2015. The position and extent of cyst production in the upper water column has been assessed by collecting the export rain of cysts with floating sediment traps. This has been compared to cyst associations in different intermediate nepheloid layers in the water column along two onshore-offshore transects. We document that highest cyst export production took place at the rim of a newly formed upwelling eddy/filament. We observed lateral transport up to 130 km off the shelf break into the deeper ocean in the bottom nepheloid layers (BNL) and in intermediate nepheloid layer (INL). The depth of the INL gradually increased from 600 m closest to the shelf break to 1300 m at the most offshore station. Transport in the BNL was observed in the more onshore part between 750 and 2300 m water depth. Cyst associations in both layers were comparable, indicating a common source. The large abundance of living cysts in these layers suggest that this source had a recent origin rather than being the result of resuspension of older sediment. The cyst associations of these samples differed from those of a second INL deeper in the water column as well as from samples from the more offshore part of the BNL. This indicates that the particles in this deeper INL and the offshore part of the BNL had a different origin. This origin could not be identified therefore no conclusions were drawn with respect to the extent to which these particles have been transported vertically or laterally. The cyst associations in the surface sediments differed from those of the nepholoid layers and the upper water column and did not reflect the effects of lateral transport as registered from the water column. The surface sediments contained a higher proportion of cysts that are highly resistant to aerobic degradation than the samples from the water column. This indicates that the former were modified predominantly by species-specific post depositional degradation. Selective degradation altering the cyst associations was not observed for the nepheloid layers.	[Zonneveld, Karin A. F.; Ebersbach, Friederike; Maeke, Mara] Univ Bremen, MARUM Fachbereich Geowissensch 5, Leobener Str 15, D-28334 Bremen, Germany; [Versteegh, Gerard J. M.] Heimholz Zentrum Polar & Meeresforschung, Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany	University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Zonneveld, KAF (通讯作者)，Univ Bremen, MARUM Fachbereich Geowissensch 5, Leobener Str 15, D-28334 Bremen, Germany.	zonnev@uni-bremen.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776	Senatskomission for Ozeanographie (DFG Germany)	Senatskomission for Ozeanographie (DFG Germany)	This study has been performed with financial support of the Senatskomission for Ozeanographie (DFG Germany). Captain Ralf Schmidt and his crew of the RV. Maria S. Merian are thanked for the professional and constructive cooperation that greatly contributed to the success of this cruise. Dr. Barbara Donner and Dr. Morten Iversen are greatly thanked for the critical reading of earlier versions of this manuscript, their general support and helpful suggestions during and after the cruise. We thank also the associated editor and two anonymous reviewers for their constructive comments on an earlier version of this manuscript.	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J	Palzer-Khomenko, MP; Wagreich, M; Kallanxhi, ME; Soliman, A; Knierzinger, W; Meszar, M; Gier, S				Palzer-Khomenko, Markus; Wagreich, Michael; Kallanxhi, Madalina-Elena; Soliman, Ali; Knierzinger, Wolfgang; Meszar, Maria; Gier, Susanne			Facies, palaeogeography and stratigraphy of the lower Miocene Traisen Formation and Wildendurnbach Formation (former "Oncophora Beds") in the Molasse Zone of Lower Austria	AUSTRIAN JOURNAL OF EARTH SCIENCES			English	Article						Molasse Basin; Calcite Minimum Interval; upper Ottnangian; Karpatian; Rzehakia Lake System; stratigraphy	ALPINE FORELAND BASIN; CENTRAL PARATETHYS; MIDDLE MIOCENE; SEQUENCE STRATIGRAPHY; DINOFLAGELLATE CYSTS; CENTRAL-EUROPE; FOREDEEP; STRATOTYPE; BOREHOLE; GERMANY	A detailed study of OMV wells throughout the Lower Austrian Molasse Basin demonstrates the existence of a distinct and synchronous upper Ottnangian (lower Miocene) stratigraphic signal, the Calcite Minimum Interval (CMI). It corresponds to the depositional phase of the Rzehakia Lake System. This signal is interpreted to be of chronostratigraphic importance as an expression of palaeoclimate and related sea-level change. It is represented by the brackish Traisen Formation, which crops out south of the Danube. The Traisen Formation correlates with sands and shales in OMV wells to the north, termed Wildendurnbach Formation. However, the CMI underlies a marine unit, the so-called "Oncophora Beds" (also known as Rzehakia Beds) as reported from OMV wells in the north at the border to the Czech Republic. We demonstrate that these former "Oncophora Beds" are younger, i.e. of Karpatian age, than originally assumed. Therefore, these deposits cannot be correlated to the late Ottnangian Traisen Formation. This may solve the problem of contradicting interpretations concerning the depositional environment of both units, which were correlated to each other in the past. As no Rzehakia bivalves (formerly Oncophora) are described from these former"Oncophora Beds", we recommend to avoid using the term for these turbiditic sands. Instead, we attribute these deposits to the fully marine Karpatian Laa Formation. These new findings, which are in accordance with published data from the Czech Republic, indicate two (in time and space) independent sedimentary systems and sand deposition centres for the Traisen Formation and the massive sands attributed as "Oncophora Beds"around Wildendurnbach. A late Ottnangian system in the south delivered the material of the Traisen Formation from the Alps and a Karpatian system delivered the clastic material of the massive sands of the Laa Formation from the east.	[Palzer-Khomenko, Markus; Wagreich, Michael; Knierzinger, Wolfgang; Meszar, Maria; Gier, Susanne] Univ Vienna, Dept Geodynam & Sedimentol, Althanstr 14, A-1090 Vienna, Austria; [Kallanxhi, Madalina-Elena] Babes Bolyai Univ, Dept Geol, Fac Biol & Geol, Str Mihail Kogalniceanu 1, Cluj Napoca 400084, Romania; [Soliman, Ali] Tanta Univ, Fac Sci, Geol Dept, Tanta 31527, Egypt	University of Vienna; Babes Bolyai University from Cluj; Egyptian Knowledge Bank (EKB); Tanta University	Palzer-Khomenko, MP (通讯作者)，Univ Vienna, Dept Geodynam & Sedimentol, Althanstr 14, A-1090 Vienna, Austria.	markus.palzer@gmx.at	Soliman, Ali/R-1583-2018; Wagreich, Michael/D-2279-2013	Wagreich, Michael/0000-0002-8828-0857	OMV [FA536022]	OMV	We would like to thank the OMV for funding the Project in the course of a University of Vienna-OMV cooperation project (grant number FA536022) and for providing the investigated drill cores and archive data, as well as the Geological Survey of Austria for providing the drill core of Schaubing. Special thanks go to Gebhardt Holger for his support. Further on, we thank Stjepan Coric, Reinhard Roetzel, Mathias Harzhauser, Dorte Theobalt, Philipp Strauss and Thomas Kuffner for fruitful discussions and for their support.	Aniwandter A, 1990, 30 YEARS GEOLOGICAL, P186; Beidinger A, 2014, TECTONICS, V33, P222, DOI 10.1002/2012TC003250; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; Bieg U., 2005, THESIS; Bujak J.P., 1980, SPEC PAP PALAEONTOL, V24, P100; Burnett J. 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F., 1983, GEOLOGIE KRISTALLINS; Strauss Christoph, 2001, Geologisches Jahrbuch Reihe A, V152, P395; Vazquez Pena FR, 2007, THESIS; von Benedek P.N., 1982, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V162, P265; Wagner LR, 1998, GEOL SOC SPEC PUBL, V134, P339, DOI 10.1144/GSL.SP.1998.134.01.16; WALL D., 1967, PALAEONTOLOGY, V10, P95; Wessely G., 2006, NIEDEROSTERREICH; Wimmer-Frey I., 2013, ARBEITSTAGUNG 2013 G, V13, P138	72	5	5	0	0	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.	SEP	2018	111	1					75	91		10.17738/ajes.2018.0006	http://dx.doi.org/10.17738/ajes.2018.0006			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GU7HZ		Green Published, gold			2025-03-11	WOS:000445493200006
J	Mitta, VV; Savelieva, YN; Fedorova, A; Shurekova, OV				Mitta, V. V.; Savelieva, Yu. N.; Fedorova, A. A.; Shurekova, O. V.			Ammonites, Microfauna, and Palynomorphs from the Lower Part of the Upper Bajocian Parkinsoni Zone of the Basin of the Bolshoi Zelenchuk River, Northern Caucasus	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						upper Bajocian; biostratigraphy; ammonites; foraminifers; ostracodes; dinocycsts; spores; pollen; Northern Caucasus	OSTRACODS	This paper contains the results of a comprehensive study of the standard Rarecostites subarietis Subzone of the upper Bajocian Parkinsonia parkinsoni Zone in sections on the Kyafar River (a tributary of the Bolshoi Zelenchuk River, Karachay-Cherkessia, Russia). The subzone is represented by shales with marl interbeds and sideritic concretions of the upper member of the Djangura Formation. The taxonomic composition and distribution of ammonites, foraminifers, ostracodes, dinoflagellate cysts, and miospores are established. The characteristic assemblages recognized of microfauna and palynomorphs enabled the recognition of foraminiferal and dinocyst biostratigraphic units for this Middle Jurassic interval. The index fossils are illustrated.	[Mitta, V. V.] Russian Acad Sci, Borissiak Paleontol Inst, Profsoyuznaya Ul 123, Moscow 117647, Russia; [Mitta, V. V.] Cherepovets State Univ, Pr Lunacharskogo 5, Cherepovets 162600, Vologda Oblast, Russia; [Savelieva, Yu. N.; Fedorova, A. A.; Shurekova, O. V.] AO Geologorazvedka, Ul Fayansovaya 20,Block 1,Lit 2, St Petersburg 191019, Russia	Russian Academy of Sciences; Paleontological Institute of the Russian Academy of Sciences; Cherepovets State University	Mitta, VV (通讯作者)，Russian Acad Sci, Borissiak Paleontol Inst, Profsoyuznaya Ul 123, Moscow 117647, Russia.; Mitta, VV (通讯作者)，Cherepovets State Univ, Pr Lunacharskogo 5, Cherepovets 162600, Vologda Oblast, Russia.	mitta@paleo.ru	Shurekova, Olga/MFH-8558-2025; Mitta, Vasily/O-2682-2018	Mitta, Vasily/0000-0001-7041-2295; Shurekova, Olga/0000-0002-0446-9637	Program of the Presidium of the Russian Academy of Sciences [17]	Program of the Presidium of the Russian Academy of Sciences(Russian Academy of Sciences)	M.P. Sherstyukov (Stavropol) provided friendly help with fieldwork. E.M. Tesakova (Moscow State University) and M. Franz (Freiburg, Germany) helped with identification of ostracodes. S.V. Bagirov (Paleontological Institute, Russian Academy of Sciences) provided ammonite photography. Photographs of ostracodes were provided by L.A. Kartseva (Botanical Institute, Russian Academy of Sciences) and by Yu.N. Savelieva at the Paleontological Institute of Russian Academy of Sciences. E.S. Platonov (AO Geologorazvedka) provided technical help in photographing foraminifers. A.A. Goryacheva (Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences) and V.A. Zakharov and M.A. Rogov (Geological Institute, Russian Academy of Sciences) helpfully advised on the manuscript. We are grateful to all those who helped with the preparation and publication of this research. This study was supported by the Program of the Presidium of the Russian Academy of Sciences, no. 17.	[Anonymous], 1992, T MEZHV STRAT KOM, V22; Antonova Z. A., 1958, T VSES NEFTEGAZ NAUC, VXVII, P41; Azbel' A.Ya., 1991, PRAKTICHESKOE RUKOVO, V5; Bate RH, 2009, MICROPALEAEONTOLOGIC, P199; Beher Elke, 2010, Palaeodiversity, P43; Beznosov N. 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J	Piasecki, S; Nohr-Hansen, H; Dalhoff, F				Piasecki, Stefan; Nohr-Hansen, Henrik; Dalhoff, Finn			Revised stratigraphy of Kap Rigsdagen beds, Wandel Sea Basin, North Greenland	NEWSLETTERS ON STRATIGRAPHY			English	Article						Kap Rigsdagen beds; Wandel Sea Basin; North Greenland; dinoflagellate cysts; stratigraphy	EOCENE; BIOSTRATIGRAPHY	The Wandel Sea Basin in eastern North Greenland comprises Upper Palaeozoic-Paleogene sediments. Most stratigraphic units are well dated but new palynological analyses of the 85-100 m thick succession at Kap Rigsdagen, North Greenland have revealed two stratigraphically significant dinoflagellate cyst assemblages which change the earlier age assignment of the succession. The lower assemblage suggests a late Barremian age for the sediments. These sediments and the underlying, coarse-grained sediments (barren of dinoflagellate cysts) show similarities to the upper LadegArdsfien Formation in Peary Land, also of late Barremian age. Consequently, this part of the Kap Rigsdagen succession is herein referred to the LadegArdsaen Formation. The upper part of the Kap Rigsdagen succession yielded a diverse dinoflagellate cyst assemblage dominated by reworked Lower and Upper Cretaceous species but includes Lower to Middle Eocene taxa. Alterbidinium? aff. . bicellulum is the only abundant Eocene species in these strata. This part of the succession is referred to the Thyra empty set Formation based on lithology and paralic depositional environment of Early to Middle Eocene age. Similar rich reworked Cretaceous dinoflagellate cyst assemblages in Paleogene deposits have previously been reported from North and East Greenland. In all cases, this magnitude of reworking responds to regional uplift events in connection with the North Atlantic break-up and sea-floor spreading.	[Piasecki, Stefan] Nat Hist Museum Denmark, Oster Voldgade 5-7, DK-1350 Copenhagen K, Denmark; [Piasecki, Stefan; Nohr-Hansen, Henrik] Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Dalhoff, Finn] Danish Environm Protect Agcy, Gillelejevej 2B, DK-3230 Ostrupgard, Graested, Denmark	Geological Survey Of Denmark & Greenland	Piasecki, S (通讯作者)，Nat Hist Museum Denmark, Oster Voldgade 5-7, DK-1350 Copenhagen K, Denmark.; Piasecki, S (通讯作者)，Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	sp@geus.dk	Nohr-Hansen, Henrik/G-9058-2018	Nohr-Hansen, Henrik/0000-0002-9291-8104				[Anonymous], B GRONLANDS GEOL UND; [Anonymous], 2003, THESIS; [Anonymous], 1990, RAPPORT GRONLANDS GE, DOI DOI 10.34194/RAPGGU.V148.8108; [Anonymous], B AM PALEONTOLOGY; [Anonymous], 1980, Special Papers in Palaeontology; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1979, RAPP GRONL GEOL UNDE, DOI DOI 10.34194/RAPGGU.V88.7558; [Anonymous], RAPP GRONLANDS GEOL; [Anonymous], 1993, GRONL GEOL UNDERS B; [Anonymous], 2010, Geological Survey of Denmark and Greenland Bulletin; [Anonymous], 1981, Rapport Gronlands Geologiske Undersogelse, DOI DOI 10.34194/RAPGGU.V106.7766; ARHUS N, 1991, CRETACEOUS RES, V12, P209; BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; Birkelund T., 1983, ZITTELIANA, V10, P7; Dam G, 1998, GEOLOGY, V26, P207, DOI 10.1130/0091-7613(1998)026<0207:SRTMPI>2.3.CO;2; Dawes P.R., 1973, ARCTIC GEOLOGY AAPG, V19, P117, DOI DOI 10.1306/M19375C10; EATON G L, 1976, Bulletin of the British Museum (Natural History) Geology, V26, P227; Fensome RA, 2016, GEOL SURV DEN GREENL, V36, P143; HAKANSSON E, 1989, GEOLOGY, V17, P683, DOI 10.1130/0091-7613(1989)017<0683:WSBANS>2.3.CO;2; Iakovleva AI, 2010, PALYNOLOGY, V34, P195, DOI 10.1080/01916121003629974; ISLAM MA, 1983, MICROPALEONTOLOGY, V29, P328, DOI 10.2307/1485740; Larsen LM, 2014, J GEOL SOC LONDON, V171, P539, DOI 10.1144/jgs2013-118; Lyck Jens M., 2000, Geology of Greenland Survey Bulletin, V187, P21; Nohr-Hansen H, 2016, GEOL SURV DEN GREENL, P9; Nohr-Hansen H, 2011, GEOL SURV DEN GREENL, P61; Nohr-Hansen Henrik, 2002, Geology of Greenland Survey Bulletin, V191, P111; STANLEY EDWARD A., 1965, BULL AMER PALEONTOL, V49, P179; Svennevig K, 2016, TECTONICS, V35, P2896, DOI 10.1002/2016TC004152	28	10	10	0	7	GEBRUDER BORNTRAEGER	STUTTGART	JOHANNESSTR 3A, D-70176 STUTTGART, GERMANY	0078-0421			NEWSL STRATIGR	Newsl. Stratigr.	SEP	2018	51	4					411	425		10.1127/nos/2018/0444	http://dx.doi.org/10.1127/nos/2018/0444			15	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GT8FH					2025-03-11	WOS:000444771600002
J	Bojanowski, MJ; Ciurej, A; Haczewski, G; Jokubauskas, P; Schouten, S; Tyszka, J; Bijl, PK				Bojanowski, Maciej J.; Ciurej, Agnieszka; Haczewski, Grzegorz; Jokubauskas, Petras; Schouten, Stefan; Tyszka, Jaroslaw; Bijl, Peter K.			The Central Paratethys during Oligocene as an ancient counterpart of the present-day Black Sea: Unique records from the coccolith limestones	MARINE GEOLOGY			English	Article						Pelagic sediments; Marginal basins; Paleoceanography; Salinity; Redox conditions; Methane venting	ANAEROBIC METHANE OXIDATION; SULFUR ISOTOPE FRACTIONATION; WALLED DINOFLAGELLATE CYSTS; REGIONAL MARKER HORIZON; OXIC ANOXIC INTERFACE; ORGANIC-MATTER; STABLE-ISOTOPE; WATER-COLUMN; PALEOENVIRONMENTAL CHANGES; WESTERN CARPATHIANS	Four isochronous Oligocene coccolith limestone horizons from the Carpathians were examined in order to reconstruct paleoceanographic conditions in the Central Paratethys. The dominance of small and size-uniform pyrite framboids, the occurrence of low-diversity dinoflagellate cysts and coccolithophorids and the presence of biomarker molecule 28,30-dinorhopane indicate that the water column was stratified with the upper water column being relatively well-oxygenated, but the bottom water being anoxic. The latter is confirmed by the fine and consistent horizontal laminations in various parts of the basin, scarcity of benthic organisms and their trace fossils. The limestones exhibit typical marine delta C-13 values, but are significantly depleted in O-18 and enriched in Sr-87 relative to contemporaneous ocean water. These isotopic compositions result from a decreased salinity of the surface waters caused by an increased riverine input. This is confirmed by the lack or impoverishment of planktonic foraminifers, presence to abundance of goniodomid dinoflagellate cysts and massive occurrence of low-diversity nannoplankton assemblages, which indicates decreased salinities as low as 17 parts per thousand and high productivity in the upper water column. These observations indicate that the limestones were formed during periods when connection of the Central Paratethys with the global ocean was limited, which impeded water exchange causing the development of low-salinity conditions of surface water and bottom-water anoxia. During the deposition of the oldest Tylawa horizon, primary productivity was enhanced and chemocline was positioned exceptionally high in the water column. Moreover, decreased delta C-13 values in both carbonates and organic matter of this horizon suggest that widespread methane venting took place in the basin during NP23. All these data show that during the Oligocene the Central Paratethys experienced similar conditions to those of the current Black Sea, which can be used as a modem analogue, especially for the Tylawa horizon. Therefore, the Tylawa horizon can be perceived as a potential effect of future post-depositional processes of coccolith marls analogous to those having been deposited in the Black Sea for 2.7 kyr.	[Bojanowski, Maciej J.] Polish Acad Sci, ING PAN Inst Geol Sci, Twarda 51-55, PL-00818 Warsaw, Poland; [Ciurej, Agnieszka; Haczewski, Grzegorz; Tyszka, Jaroslaw] Polish Acad Sci, ING PAN Inst Geol Sci, Res Ctr Cracow, Senacka 1, PL-31002 Krakow, Poland; [Ciurej, Agnieszka] Pedag Univ Cracow, Inst Geog, Podchorazych 2, PL-30084 Krakow, Poland; [Jokubauskas, Petras] Univ Warsaw, Inst Geochem Mineral & Petrol, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland; [Schouten, Stefan] N1OZ Royal Netherlands Inst Sea Res, Dept Marine Microbiol & Biogeochem, Landsdiep 4, NL-1797 SZ Thorntje, Texel, Netherlands; [Bijl, Peter K.] Univ Utrecht, Marine Palynol & Palaeoceanog, Lab Palaeobot & Palynol, Dept Earth Sci,Fac Geosci, Princetonlaan 8A, NL-3584 CB Utrecht, Netherlands; [Schouten, Stefan] Univ Utrecht, Dept Earth Sci, Fac Geosci, Budapestlaan 4, NL-3584 CB Utrecht, Netherlands	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; University of the National Education Commission; University of Warsaw; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University; Utrecht University	Bojanowski, MJ (通讯作者)，Polish Acad Sci, ING PAN Inst Geol Sci, Twarda 51-55, PL-00818 Warsaw, Poland.	mbojan@twarda.pan.pl; aciurej@up.krakow.pl; p.jokubauskas@student.uw.edu.pl; stefan.schouten@nioz.nl; ndtyszka@cyf-kr.edu.pl; p.k.bijl@uu.nl	Jokubauskas, Petras/AAP-3593-2021; Bojanowski, Maciej/H-1352-2012; Schouten, Stefan/P-4380-2016; Ciurej, Agnieszka/HNS-7682-2023	Jokubauskas, Petras/0000-0002-1099-4497; Bijl, Peter/0000-0002-1710-4012; Ciurej, Agnieszka/0000-0002-2383-7562; Bojanowski, Maciej/0000-0002-4735-1938	National Science Centre [2011/01/D/ST10/04617]; Ministry of Science and Higher Education [N N307 2744 33]; NWO-ALW VENI grant [v]; Netherlands Earth Science Center; Ministry of Education, Culture and Science, Netherlands (OCW) [NWO 024.002.001]; EU 7FP ATLAB Project [285989]	National Science Centre(National Science Centre, Poland); Ministry of Science and Higher Education; NWO-ALW VENI grant; Netherlands Earth Science Center; Ministry of Education, Culture and Science, Netherlands (OCW); EU 7FP ATLAB Project	We are grateful to Gert-Jan Reichart (Utrecht University) for his supervision during A. Ciurej research stay at Utrecht. Anchelique Mets (NIOZ) is thanked for analytical support with the organic geochemical analysis. This work was supported by the National Science Centre (grant no. 2011/01/D/ST10/04617) and by the Ministry of Science and Higher Education (grant no. N N307 2744 33). P.K.B. acknowledges funding through NWO-ALW VENI grant no. 863.13.002. S.S. was supported by the Netherlands Earth Science Center, funded by Ministry of Education, Culture and Science, Netherlands (OCW; grant no. NWO 024.002.001). AC, JT and MB were partly supported by the EU 7FP ATLAB Project no. 285989 coordinated by ING PAN. We appreciate constructive comments on the earlier version of the manuscript by Stephen Barker (Cardiff University).	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Geol.	SEP 1	2018	403						301	328		10.1016/j.margeo.2018.06.011	http://dx.doi.org/10.1016/j.margeo.2018.06.011			28	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	GS5BB		Green Published			2025-03-11	WOS:000443670500024
J	Ayu-Lana-Nafisyah; Endang-Dewi-Masithah; Matsuoka, K; Mirni-Lamid; Mochammad-Amin-Alamsjah; O-hara, S; Koike, K				Ayu-Lana-Nafisyah; Endang-Dewi-Masithah; Matsuoka, Kazumi; Mirni-Lamid; Mochammad-Amin-Alamsjah; O-hara, Shizuka; Koike, Kazuhiko			Cryptic occurrence of <i>Chattonella marina</i> var. <i>marina</i> in mangrove sediments in Probolinggo, East Java Province, Indonesia	FISHERIES SCIENCE			English	Article						Resting cysts; Temperature tolerance; Salinity tolerance; Raphidophyte; Ribosomal RNA; Red tide	DINOFLAGELLATE COCHLODINIUM-POLYKRIKOIDES; OVATA RAPHIDOPHYCEAE; MASS MORTALITY; DINOPHYCEAE; ESTUARY; BLOOM; BAY; PHYTOPLANKTON; GYMNODINIALES; PHILIPPINES	Mangrove forests and adjacent creeks are known to be highly productive estuaries, which are partly supported by benthic microalgae that grow on the sediments. During surveys investigating the microalgal floras of mangrove swamps in the eastern part of Java Island, a mud sample unexpectedly included large numbers of a notorious fish killer, Chattonella-like motile cells, and its resting cysts. These motile cells were established as clonal cultures for further identification and physiological tests. The cysts were examined through palynological and molecular biological means. Identification based on light microscopy and ribosomal RNA gene sequences confirmed that these cells and cysts were Chattonella marina var. marina. While the strains were genetically identical to the temperate strains isolated from Japan and China, temperature experiments showed that the Indonesian strains possessed a high maximum quantum yield of photosystem II even after exposure to 34 degrees C, a temperature at which the Japanese strain could not survive. Salinity experiments showed adaptation of the strains to a salinity of 15. These findings, together with the discovery of populations of cysts in the mangrove sediment, highlight the tough and unique nature of the Indonesian strains, which are likely adapted to wide fluctuations of temperature and salinity in mangrove swamps, and pose a potential risk to fisheries in Indonesia.	[Ayu-Lana-Nafisyah; O-hara, Shizuka; Koike, Kazuhiko] Hiroshima Univ, Grad Sch Biosphere Sci, Kagamiyama 1-4-4, Higashihiroshima, Hiroshima 7398528, Japan; [Ayu-Lana-Nafisyah; Endang-Dewi-Masithah; Mirni-Lamid; Mochammad-Amin-Alamsjah] Univ Airlangga, Fac Fisheries & Marine, Campus C UNAIR Mulyorejo, Surabaya 60115, East Java, Indonesia; [Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, Takaracho 1551-7, Nagasaki 8512213, Japan	Hiroshima University; Airlangga University; Nagasaki University	Koike, K (通讯作者)，Hiroshima Univ, Grad Sch Biosphere Sci, Kagamiyama 1-4-4, Higashihiroshima, Hiroshima 7398528, Japan.	kazkoike@hiroshima-u.ac.jp	Nafisyah, Ayu Lana/AAC-3815-2021; Koike, Kazuhiko/A-3392-2019	Lana Nafisyah, Ayu/0000-0001-7354-3821; Kazuhiko, Koike/0000-0001-5380-5839; Ohara, Shizuka/0000-0002-1207-6921	Ministry of Education, Culture, Sports, Science and Technology of Japan [17H04625]; Grants-in-Aid for Scientific Research [17H04625] Funding Source: KAKEN	Ministry of Education, Culture, Sports, Science and Technology of Japan(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	This work was supported by a Grant-in-Aid (KAKENHI no. 17H04625) for Scientific Research from the Ministry of Education, Culture, Sports, Science and Technology of Japan to K. K. The authors express their sincere gratitude to Ms. Tomoe Hikosaka-Katayama and Ms. Kanae Koike (Natural Science Center for Basic Research and Development, Hiroshima University) for assisting with the DNA analysis, as well as to Prof. Soetjipto, Dr., Ph.D., Institute of Tropical Disease Universitas Airlangga, who gave us information on transferring samples. We also thank Mr. Daniel Onny Setiyoko (Fisheries and Marine Faculty, Universitas Airlangga) for assisting with the specimen collection.	ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; Adesalu T. 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Sci.	SEP	2018	84	5					877	887		10.1007/s12562-018-1219-0	http://dx.doi.org/10.1007/s12562-018-1219-0			11	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	GR5JD					2025-03-11	WOS:000442664800015
J	Tahoun, SS; Deaf, AS; Ied, IM				Tahoun, Sameh S.; Deaf, Amr S.; Ied, Ibrahim M.			The use of cyclic stratigraphic pattern of peridinioid and gonyaulacoid dinoflagellate cysts in differentiating potential thick monotonous carbonate reservoirs: A possible ecostratigraphic tool under test	MARINE AND PETROLEUM GEOLOGY			English	Article						Upper Cretaceous; Dinoflagellate cysts; Biozones; Ecozones; Reservoir; Stratigraphy; Eastern Desert; Egypt	NORTHERN WESTERN-DESERT; TUNIS 1X BOREHOLE; CRETACEOUS PALYNOSTRATIGRAPHY; DEPOSITIONAL-ENVIRONMENTS; MARINE-SEDIMENTS; EASTERN DESERT; OIL-FIELD; SEQUENCE; EGYPT; BASIN	The current work used the conventional peridinioid-gonyaulacoid ratio (P/G) to devise a new concept of dinoflagellate cyst zonation called the dinoflagellate ecological zone (DEZ), which is based here on the peridinioid ecological zone (PEZ) and gonyaulacoid ecological zone (GEZ). The PEZ and GEZ were used successfully to further divide the thick monotonous carbonate succession (mid-Cenomanian to Campanian) in Q-72-1X well in the Eastern Desert of Egypt into smaller ecozones. PEZ and GEZ are practical and easy to use in subdividing large conventional biozones of the carbonate reservoirs into distinguishable, smaller ecozones when a finer resolution is necessary on a reservoir scale for production demands. This tool is suggested to be used in the hydrocarbon exploration industry with minimum knowledge of the taxonomy of the dinoflagellate cysts. The proposed PEZ and GEZ are related to local ecological conditions within the basin/hydrocarbon field (i.e. can be traced out laterally in an infra-basinal scale). This tool can be applied to any carbonate reservoirs in any petroliferous basin worldwide. Moreover, the P/G ratio, the relative abundances of the dinoflagellate cyst assemblages and other palyno-logical parameters were used successfully to reveal the palaeodepositional settings of the identified PEZ and GEZ. Alternating, transgressive and regressive phases were identified, although a dissimilar species composition is observed in each of these ecozones. Environments were interchanging between the regressive, marginal marine to proximal inner neritic and the transgressive, distal inner to middle shelf settings. Three peridiniacean dinoflagellate cyst peaks were recorded, the middle Cenomanian Subtilisphaera peak, the middle Coniacian Isabelidinium, Chatangiella, and Manumiella peak, and the middle Santonian Isabelidinium peak.	[Tahoun, Sameh S.] Cairo Univ, Fac Sci, Geol Dept, POB 12613, Giza, Egypt; [Deaf, Amr S.] Assiut Univ, Fac Sci, Geol Dept, POB 71516, Assiut, Egypt; [Ied, Ibrahim M.] Zagazig Univ, Fac Sci, Geol Dept, Zagazig, Egypt	Egyptian Knowledge Bank (EKB); Cairo University; Egyptian Knowledge Bank (EKB); Assiut University; Egyptian Knowledge Bank (EKB); Zagazig University	Tahoun, SS (通讯作者)，Cairo Univ, Fac Sci, Geol Dept, POB 12613, Giza, Egypt.	stahoun@cu.edu.eg	Deaf, Amr/AAF-6269-2020	Deaf, Amr/0000-0002-5073-7911; Tahoun, Sameh S./0000-0002-0425-8848				AbdelKireem MR, 1996, J AFR EARTH SCI, V22, P93, DOI 10.1016/0899-5362(95)00125-5; Aboul Ela N. M, 1992, N JB EOL PALAONT MH, P595; Aboul Ela N.M., 2013, 2 S GEOL RES TETH RE, P149; Al-Ameri TK, 1997, CRETACEOUS RES, V18, P789, DOI 10.1006/cres.1997.0087; [Anonymous], 1997, THESIS; [Anonymous], 1996, Palynology: principles and applications; Barss M.S., 1979, Geol. Surv. 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Pet. Geol.	SEP	2018	96						240	253		10.1016/j.marpetgeo.2018.05.030	http://dx.doi.org/10.1016/j.marpetgeo.2018.05.030			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GQ9AN					2025-03-11	WOS:000442058400016
J	Falardeau, J; de Vernal, A; Spielhagen, RF				Falardeau, Jade; de Vernal, Anne; Spielhagen, Robert F.			Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes	QUATERNARY SCIENCE REVIEWS			English	Article						Fram strait; Last glacial maximum (LGM); Late and post-glacial; Holocene; Temperature; Salinity; Sea ice; Dinocysts	SEA-SURFACE CONDITIONS; NORTHERN NORTH-ATLANTIC; DINOFLAGELLATE CYST ASSEMBLAGES; ORGANIC-WALLED MICROFOSSILS; HIGH-RESOLUTION RECORD; ARCTIC-OCEAN; NORDIC SEAS; BARENTS SEA; ICE COVER; CARBONATE DISSOLUTION	Sea-surface conditions in northeastern Fram Strait since the last glacial maximum (LGM) were reconstructed from cores MSM5/5-712-2 and PS2863/1-2 based on palynological assemblages, ecological preferences of dinocysts and application of the modern analog technique. Dinocyst in LGM sediments are sparse, but their assemblages reflect mild summer conditions. Given the regional context and evidence from other tracers, the dinocyst assemblages of the LGM could relate to regional fluxes of dinocysts during exceptional mild summers. From 19 to 14.7 ka, dinocyst data suggest very cold conditions with extensive sea-ice cover, while abundant reworked palynomorphs indicate intense glacial erosion. An abrupt transition at 14.7-14.5 ka was marked by a peak in summer temperatures coinciding with a rapidly deposited sediment layer related to a regional meltwater plume event in western Svalbard. From 14.7 to 12.6 ka, large seasonal temperature contrasts with mild summers and cold winters together with low salinity indicate continuous melting of the Svalbard Barents Sea ice sheet fostered by warm climate. At 12.6 ka, the regional onset of the Younger Dryas was marked by cooling and increased salinity. On a regional scale, the 12.6-12 ka interval corresponds to an important transition involving enhanced circulation of Arctic waters around Svalbard and establishment of coastal fronts along its northern and western margins. Modern-like oceanic conditions with relatively high salinity and low seasonal temperature contrast developed at about 7.6 ka. Since then, a slight cooling is observed, especially in winter. This study offers a comprehensive picture of the deglacial phases in eastern Fram Strait with unique data on the sea-surface salinity, which controls surface water stratification and plays an important role in ocean circulation. (C) 2018 Elsevier Ltd. All rights reserved.	[Falardeau, Jade; de Vernal, Anne] GEOTOP UQAM, CP 8888, Montreal, PQ H3C 3P8, Canada; [Spielhagen, Robert F.] GEOMAR Helmholtz Ctr Ocean Res, D-24148 Kiel, Germany; [Spielhagen, Robert F.] Acad Sci Humanities & Literature, D-55131 Mainz, Germany	University of Quebec; University of Quebec Montreal; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Falardeau, J (通讯作者)，GEOTOP UQAM, CP 8888, Montreal, PQ H3C 3P8, Canada.	falardeau.jade@courrier.uqam.ca	de Vernal, Anne/D-5602-2013; Spielhagen, Robert/HMD-2002-2023	Falardeau, Jade/0000-0002-4773-6731	Fonds de recherche du Quebec Nature et technologies (FRQNT); Natural Sciences and Engineering Research Council (NSERC) of Canada [38340]; NSERC-CREATE grant [432295]; Academy of Sciences, Humanities and Literature Mainz through the Akademienprogramm; National Science Foundation [OCE-1239667]	Fonds de recherche du Quebec Nature et technologies (FRQNT); Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); NSERC-CREATE grant; Academy of Sciences, Humanities and Literature Mainz through the Akademienprogramm; National Science Foundation(National Science Foundation (NSF))	This study was supported by the Fonds de recherche du Quebec Nature et technologies (FRQNT) to JF through scholarship and to GEOTOP Research Center through the Strategic Clusters program, the Natural Sciences and Engineering Research Council (NSERC) of Canada through discovery grant to AdV (38340) and the NSERC-CREATE grant to ArcTrain (432295), and the Academy of Sciences, Humanities and Literature Mainz through the Akademienprogramm. The laboratory analyses have been made in the micropaleontology and laboratory of GEOTOP at UQAM. The sediment samples from cores PS2863-1 and PS2832-2BC were made available through the ARK-XIII/2 expedition of the RV Polarstern and through the MSM05/5b expedition of the RV Maria S. Merian for core MSM5/5-712-2. A <SUP>14</SUP>C age was operated by the NOSAMS facility at the Woods Hole Oceanographic Institution with National Science Foundation sponsorship (OCE-1239667). Special thanks go to Maryse Henry and Sophie Bonnet for the palynological analysis of the first 315 cm of the MSM5/5-712-2 core. We thank Simon Van Bellen for his help in developing the age models from the Bacon software. We are grateful to the three anonymous reviewers of the journal for their critical comments on the original manuscript.	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J	Pedersen, GK; Lauridsen, BW; Svennevig, K; Bojesen-Koefoed, JA; Nohr-Hansen, H; Alsen, P				Pedersen, Gunver K.; Lauridsen, Bodil W.; Svennevig, Kristian; Bojesen-Koefoed, Jurgen A.; Nohr-Hansen, Henrik; Alsen, Peter			Burial history of a folded Cretaceous succession - A case study from the southern part of Kilen, eastern North Greenland	CRETACEOUS RESEARCH			English	Article						Burial temperatures; Palynomorphs; Macrofossils; Structural geology; Wandel sea basin	WANDEL SEA BASIN; PLATE BOUNDARY; THRUST BELT; MODEL; DEFORMATION; SPITSBERGEN; WESTERN	Kilen is a semi-nunatak in the Flade Isblink icecap in eastern North Greenland with exposures of Mesozoic sedimentary rocks, which are part of the Wandel Sea Basin. Cretaceous marine mudstones and interbedded sandstones of the Galadriel Fjeld and Solverbaek formations are thrusted and folded in large open folds at GAseslette in the southeastern part of Kilen. Steeply dipping strata, reflecting parasitic folds and small-scale thrusts, are exposed in low cliffs along a c. 9 km NNW-SSE stretch of the Solverbaek river. The present study is a case study of the thermal history of these outcrops, called the Solverbaek section. The burial temperatures are calculated from vitrinite reflectance (R-o) values. T-max -measurements from Rock-Eval type pyrolysis correlate with the R-o-values. The latter reflects the large-scale folds with higher temperatures in anticlines and lower in synclines. The sedimentary successions are dated on basis of dinoflagellate cysts, inoceramid bivalves and ammonites. The dataset demonstrate a correlation between the T-max-measurements, maximum burial temperatures, and the preservation of dinoflagellate cysts. The burial temperature at the boundary between the Kangoq Ryg Member and the Solverbaek Formation varies laterally through a restored section and suggest that the northern part of the section was c. 30 degrees hotter than the southern part prior to folding. Five events are distinguished in the thermal history of the Solverbaek section: (1) Deposition, (2) rotation of the succession, (3) thermal imprinting, (4) uplift, folding and thrusting, (5) final uplift and erosion up to present day. Following a recent structural model for Kilen events 1-3 are interpreted to be caused by Late Cretaceous rifting where (3) represents maximum burial during rifting. Event 4 is explained by basin inversion of presumed Paleocene-Eocene age. (C) 2018 Elsevier Ltd. All rights reserved.	[Pedersen, Gunver K.; Lauridsen, Bodil W.; Svennevig, Kristian; Bojesen-Koefoed, Jurgen A.; Nohr-Hansen, Henrik; Alsen, Peter] Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Lauridsen, Bodil W.] Univ Copenhagen, Nat Hist Museum Denmark, Earth & Planetary Syst Sci, Oster Voldgade 5-7, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland; University of Copenhagen	Pedersen, GK (通讯作者)，Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	gkp@geus.dk	Bojesen-Koefoed, Jørgen/AAH-5501-2020; Svennevig, Kristian/AAB-1969-2021; Alsen, Peter/F-4849-2017; Nohr-Hansen, Henrik/G-9058-2018; Svennevig, Kristian/H-1313-2018; Pedersen, Gunver Krarup/G-9411-2018; Lauridsen, Bodil Wesenberg/N-9879-2016	Alsen, Peter/0000-0001-6218-9054; Nohr-Hansen, Henrik/0000-0002-9291-8104; Svennevig, Kristian/0000-0003-3863-8096; Pedersen, Gunver Krarup/0000-0002-0792-2257; Bojesen-Koefoed, Jorgen Albert/0000-0001-5647-2769; Lauridsen, Bodil Wesenberg/0000-0002-4060-746X				[Anonymous], MONOGRAPH AMMONOID 2; [Anonymous], 1961, United States Geological Survey Professional Paper; [Anonymous], EARLY CRETACEOUS ZON; [Anonymous], SHORT COURSE NOTES G; [Anonymous], 2014, Tectonostratigraphic Atlas of the North-East Atlantic Region; [Anonymous], GEOLOGICAL SURVEY CA; [Anonymous], 1970, NORSK POLARINSTITUTT; [Anonymous], RAPP GRONLANDS GEOL; [Anonymous], B BRIT MUSEUM NATU S; [Anonymous], GEOLOGY INNUITIAN OR; [Anonymous], RAPP GRONLANDS GEOL; [Anonymous], 1991, Rapport Gronlands geologiske Undersogelse, DOI DOI 10.34194/BULLGGU.V160.6716; [Anonymous], 1999, POLARFORSCHUNG; [Anonymous], 1993, GRONL GEOL UNDERS B; [Anonymous], 1994, WANDEL SEA BASIN BAS; [Anonymous], 1991, B GRONLANDS GEOLOGIS; BARKER CE, 1994, ACS SYM SER, V570, P216; Bergh SG, 1997, AAPG BULL, V81, P637; Birkelund T., 1983, ZITTELIANA, V10, P7; Bordenave M., 1993, Applied Petroleum Geochemistry, P217; Braathen A, 1999, GEOL SOC AM BULL, V111, P1468, DOI 10.1130/0016-7606(1999)111<1468:AOACWT>2.3.CO;2; Brekke T, 2014, NPD-BULL, V11, P111; Chlalmers JA, 2001, GEOL SOC SPEC PUBL, V187, P77; Corradini D., 1973, B SOC PALEONTOL ITAL, V11, P119; Costa L.I., 1992, P99; Dam G., 1998, GEOLOGY GREENLAND SU, V180, P128, DOI DOI 10.34194/GGUB.V180.5096; Dam G., 2009, GEOL SURV DEN GREENL, V19, P171, DOI [10.34194/geusb.v19.4886, DOI 10.34194/GEUSB.V19.4886]; DHONDT AV, 1992, PALAEOGEOGR PALAEOCL, V92, P217, DOI 10.1016/0031-0182(92)90083-H; Donovan DT., 1957, MEDDELELSER GRONLAND, V155, P214; Dypvik H, 2002, POLAR RES, V21, P91, DOI 10.1111/j.1751-8369.2002.tb00069.x; HAKANSSON E, 1989, GEOLOGY, V17, P683, DOI 10.1130/0091-7613(1989)017<0683:WSBANS>2.3.CO;2; Håkansson E, 2001, B GEOL SOC DENMARK, V48, P149; Hakansson E., 1982, CAN SOC PET GEOL MEM, V8, P331; Håkansson E, 1993, B GEOL SOC DENMARK, V40, P9; Håkansson E, 2015, GEOL SOC SPEC PUBL, V413, P143, DOI 10.1144/SP413.10; Harries Peter J., 1996, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V77, P641; Hovikoski J, 2018, B GEOL SOC DENMARK, V66, P61; Nohr-Hansen H, 2016, GEOL SURV DEN GREENL, P9; Oakey GN, 2012, J GEOPHYS RES-SOL EA, V117, DOI 10.1029/2011JB008942; Olde K, 2015, REV PALAEOBOT PALYNO, V213, P1, DOI 10.1016/j.revpalbo.2014.10.006; OWEN H G, 1984, Bulletin of the Geological Society of Denmark, V33, P183; OWEN HG, 1984, CRETACEOUS RES, V5, P329, DOI 10.1016/S0195-6671(84)80028-2; Owen Hugh G., 1999, Scripta Geologica Special Issue, V3, P129; Pearce MA, 2009, PALAEOGEOGR PALAEOCL, V280, P207, DOI 10.1016/j.palaeo.2009.06.012; Piepjohn K, 2001, GEOL MAG, V138, P407, DOI 10.1017/S0016756801005660; Piepjohn K., 2015, Arktos, V1, P1, DOI DOI 10.1007/S41063-015-0015-7; Piepjohn K, 2016, J GEOL SOC LONDON, V173, P1007, DOI 10.1144/jgs2016-081; Serck CS, 2017, MAR PETROL GEOL, V86, P874, DOI 10.1016/j.marpetgeo.2017.06.044; Soper N.J., 1982, NARES STRAIT DRIFT G, V8, P205; Spath LF, 1946, MEDDELELSER GRONLAND, V132, P12; STELCK CR, 1995, CAN J EARTH SCI, V32, P977, DOI 10.1139/e95-082; Stemmerik L, 2005, NORW J GEOL, V85, P151; Surlyk F., 1991, Bull. 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J	Cruz-López, R; Maske, H; Yarimizu, K; Holland, NA				Cruz-Lopez, Ricardo; Maske, Helmut; Yarimizu, Kyoko; Holland, Neal A.			The B-Vitamin Mutualism Between the Dinoflagellate <i>Lingulodinium polyedrum</i> and the Bacterium <i>Dinoroseobacter shibae</i>	FRONTIERS IN MARINE SCIENCE			English	Article						B vitamin auxotrophy; growth limitation; Dinoflagellate-bacteria interactions; dissolved B-12; particulate B-12; particulate B-7	CYST FORMATION; SP-NOV.; BLOOM DYNAMICS; HIROSHIMA BAY; DINOPHYCEAE; B-12; PHYTOPLANKTON; ALGAE; GROWTH; CYANOBACTERIA	Recent research has shown that in aquatic systems pairs of prokaryote and eukaryote species exercise symbiotic exchanges of metabolites that are essential for the proliferation of either species. Using dinoflagellate Lingulodinium polyedrum cultures and a factorial design, we examined its growth at different concentrations of vitamin B-1 (thiamine) and B-12 (cobalamin). When both vitamins were at their lowest concentrations tested, 0.033 pM of B1 and 0.053 pM of B-12 the growth was limited. When axenic L. polyedrum was co-cultured with the bacterium Dinoroseobacter shibae, a known B-1 and B-12 producer, then L. polyedrum grew at the same rate as in culture media supplemented with B-1 and B-12. In the L. polyedrum vitamin-limited culture (V-L), the abundance of attached and free-living D. shibae was higher than in the vitamin-replete (V-R) culture. In the V-R and V-L co-cultures the measured particulate B-12 (PB12) concentration of attached and free-living D. shibae were in the range of 4.7 x 10(-18) to 3 x 10(-18) and 8.4 x 10(-21) to1.2 x 10(-19) (mol cell(-1)), respectively. Without B-12 or B-7 (biotin) added to the culture medium of a co-culture of L. polyedrum and D. shibae, the measured dissolved B-12 (dB(12)) concentration was more than 60 pM higher than necessary for un-limited growth rates of L. polyedrum. In the same culture we measured B-7 in the L. polyedrum particulate fraction (pB7; 4.7 x 10(-19) to 9.4 x 10(-19) mol cell(-1)). We suggest that in response to the production of B-1 and B-12 by D. shibae to supply L. polyedrum requeriments, the latter produced B-7, which is required by D. shibae, and in our culture was only produced by L. polyedrum when D. shibae was present. We propose that D. shibae can control L. polyedrum through the release of B-1 and B-12, and L. polyedrum can control D. shibae through the release of B-7. D. shibae is also auxotroph for niacin and 4-amino-benzoic acid, not provided by the culture medium. Therefore, L. polyedrum might affect a similar control through the release of these specific compounds and organic substrate necessary for the growth of D. shibae.	[Cruz-Lopez, Ricardo; Maske, Helmut] CICESE, Oceanog Biol, Ensenada, Baja California, Mexico; [Cruz-Lopez, Ricardo; Yarimizu, Kyoko; Holland, Neal A.] San Diego State Univ, Dept Chem & Biochem, San Diego, CA 92182 USA	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; California State University System; San Diego State University	Cruz-López, R (通讯作者)，CICESE, Oceanog Biol, Ensenada, Baja California, Mexico.; Cruz-López, R (通讯作者)，San Diego State Univ, Dept Chem & Biochem, San Diego, CA 92182 USA.	ricardo.crlp@gmail.com	Yarimizu, Kyoko/GPX-1849-2022	Yarimizu, Kyoko/0000-0001-7492-6592; Cruz-Lopez, Ricardo/0000-0002-4782-7625	National Council of Science and Technology (CONACyT-Mexico) [CB-2008-01 106003]	National Council of Science and Technology (CONACyT-Mexico)(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	This work was partially supported by the National Council of Science and Technology (CONACyT-Mexico) project CB-2008-01 106003 (to HM), a Ph.D. scholarship, and a Postdoctoral fellowship for overseas to RCL (CONACyT-Mexico). Additionally, we would like to thank Avery O. Tatters (University of Southern California) for kindly providing the L. polyedrum strain and Prof. Carl J. Carrano (San Diego State University) for allowing us to use his laboratory to prepare samples. We would like to show our gratitude to Sharon and Christopher A. Rhodes, the owners of Drug Delivery Experts LLC., for allowing us to use their facility to generate LC-MS data. Finally, we would like to thank the reviewers for constructive comments and suggestions.	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Mar. Sci.	AUG 28	2018	5								274	10.3389/fmars.2018.00274	http://dx.doi.org/10.3389/fmars.2018.00274			12	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	HJ7GX		gold			2025-03-11	WOS:000457365000001
J	More, KD; Orsi, WD; Galy, V; Giosan, L; He, LJ; Grice, K; Coolen, MJL				More, Kuldeep D.; Orsi, William D.; Galy, Valier; Giosan, Liviu; He, Lijun; Grice, Kliti; Coolen, Marco J. L.			A 43 kyr record of protist communities and their response to oxygen minimum zone variability in the Northeastern Arabian Sea	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Northeast Arabian Sea; oxygen minimum zone; protist ecology; sedimentary ancient DNA; paleogenomics; glacial-interglacial cycle	SEDIMENTS; PAKISTAN; MONSOON; OCEAN; LIFE; MICROZOOPLANKTON; OSCILLATIONS; PRODUCTIVITY; EVOLUTION; HEINRICH	An extensive oxygen minimum zone (OMZ) occurs in the northeastern (NE) Arabian Sea where sedimentary records show evidence of alternating strong and weak OMZs that correlate with North Atlantic climate variability during the last glacial-interglacial cycle. OMZs are expanding world-wide, but information on long-term OMZ-ecosystem interactions is mainly limited to fossilized species, notably foraminifera. Here, we provide a first comprehensive ancient sedimentary DNA record of both fossilizing and non-fossilizing protists and their response to OMZ variability in the NE Arabian Sea over the last 43 ka. Protist communities changed significantly during strong vs. weak OMZ conditions coincident with interstadials and stadials respectively. Dinoflagellates were identified as significant indicator taxa for strong OMZs during glacial as well as interglacial interstadials, whereas diatoms were significant indicators for strong OMZs only during glacial interstadials. The chlorophyte Chlorella was found to be the main phototrophic protist in nutrient-depleted surface waters during glacial stadials. Notably, strong OMZ conditions shaped past protist communities by creating isolated habitats for those capable of sustaining oxygen depletion either by adapting a parasitic life cycle (e.g. apicomplexans) or by establishing mutualistic connections with others (e.g. radiolarians and mixotrophic dinoflagellates) or by forming cysts (e.g. colpodeans). Notably, a long-term increase in eutrophication and a decrease in the diatom/dinoflagellate ratio was observed during the late Holocene favoring the pelagic component of the marine food web. A similar scenario could be expected in the context of predicted worldwide expansion of coastal OMZs associated with global climate change. (C) 2018 Elsevier B.V. All rights reserved.	[More, Kuldeep D.] Curtin Univ, Sch Mol & Life Sci MLS, Dept Agr & Environm, Bentley, WA 6102, Australia; [More, Kuldeep D.; Grice, Kliti; Coolen, Marco J. L.] Curtin Univ, Sch Earth & Planetary Sci EPS, Inst Geosci Res TIGeR, WAOIGC, Bentley, WA 6102, Australia; [Orsi, William D.] Ludwig Maximilians Univ Munchen, Dept Earth & Environm Sci Paleontol & Geobiol, D-80333 Munich, Germany; [Orsi, William D.] Ludwig Maximilians Univ Munchen, Geobioctr LMU, D-80333 Munich, Germany; [Galy, Valier] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA; [Giosan, Liviu] Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA; [He, Lijun] East China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China	Curtin University; Curtin University; University of Munich; University of Munich; Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; East China Normal University	More, KD (通讯作者)，Curtin Univ, Sch Mol & Life Sci MLS, Dept Agr & Environm, Bentley, WA 6102, Australia.; More, KD; Coolen, MJL (通讯作者)，Curtin Univ, Sch Earth & Planetary Sci EPS, Inst Geosci Res TIGeR, WAOIGC, Bentley, WA 6102, Australia.	k.more@postgrad.curtin.edu.au; marco.coolen@curtin.edu.au	Giosan, Liviu/F-1809-2010; He, Lijun/I-4996-2013; Coolen, Marco/B-8263-2015; Galy, valier/I-6185-2012	More, Kuldeep Dilip/0000-0002-8278-8086; Coolen, Marco/0000-0002-0417-920X; Grice, Kliti/0000-0003-2136-3508; Galy, valier/0000-0003-0385-8443	NSF MGG Grant [1357017]; C-DEBI grant [OCE-0939564]; Curtin Office for Research and Development (ORD); NSF OCE Grant [0634731]; NCBI under Bio project [PRJNA397489 (SRP148586)]	NSF MGG Grant; C-DEBI grant; Curtin Office for Research and Development (ORD); NSF OCE Grant(National Science Foundation (NSF)); NCBI under Bio project	This work was primarily supported by NSF MGG Grant #1357017 to MJLC, VG, and LG. Additional financial support was provided via a C-DEBI grant #OCE-0939564 to WDO. We also thank the Curtin Office for Research and Development (ORD) for funding a PhD stipend to K.D.M. This is C-DEBI contribution #358. Core collection was supported by NSF OCE Grant #0634731 to LG. We thank the co-chiefs Peter Clift and Tim Henstock as well as the scientific participants, captain and crew of the R/V Pelagia. We thank Dr. Cornelia Wuchter and Dr. Alisson Blyth for helpful discussions. Data has been deposited to SRA (Sequence Read Archive) NCBI under Bio project: PRJNA397489 (SRP148586). We thank Dr. Christopher Somes (GEOMAR Helmholtz Centre for Ocean Research) and two anonymous reviewers and Editor Prof. Derek Vance for their constructive feedback.	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AUG 15	2018	496						248	256		10.1016/j.epsl.2018.05.045	http://dx.doi.org/10.1016/j.epsl.2018.05.045			9	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	GM5LR					2025-03-11	WOS:000438179400025
J	Lozano-Cobo, H; Gómez-Gutiérrez, J; Franco-Gordo, C; del Prado-Rosas, MDG; Plascencia-Palomera, V; Ambriz-Arreola, I				Lozano-Cobo, Horacio; Gomez-Gutierrez, Jaime; Franco-Gordo, Carmen; del Carmen Gomez del Prado-Rosas, Maria; Plascencia-Palomera, Viridiana; Ambriz-Arreola, Israel			Changes in parasite-chaetognath species assemblages in the Mexican Central Pacific before and during El Nino 1997-1998	DISEASES OF AQUATIC ORGANISMS			English	Article						Protists; Platyhelminthes; Acanthocephalans; Nematodes; Larval stages; Infracommunity; Component community	GULF-OF-CALIFORNIA; WATER MASSES; 1ST RECORD; COAST; ABUNDANCE; ASSOCIATION; TREMATODES; EVOLUTION	We investigated the seasonal and interannual changes in diversity, abundance, and prevalence of chaetognaths and their parasites collected monthly during 1996-1998 in the Mexican Central Pacific. We tested the hypothesis of a positive relationship between abundance and species richness of chaetognaths and their parasites, and investigated the influence of the 19971998 El Nino event on this host-parasite interaction. Of the 9 chaetognath species collected in the present study, only 7 were found to be parasitized. Of 78 154 chaetognath specimens collected, 790 were parasitized (1% prevalence) with at least 1 type of epibiont (cysts, perhaps protists) and 6 types of endoparasites: protists (apicomplexans, dinoflagellates, and ciliates), digeneans, cestodes, acanthocephalans, nematodes, and other unidentified endoparasites. Cysts, digeneans, and cestodes were the most abundant parasites. Mean intensity ranged from 1-4 endoparasites and from 1-21 epibionts host(-1). Zonosagitta bedoti and Flaccisagitta enflata were the most abundant chae-tognath species and had the highest parasite diversity. Mesosagitta minima and Para sagitta euneritica had the highest parasite prevalence (>2%). A 2-way cluster analysis defined sampling month groups as before, during, and after the 1997-1998 El Nino. The highest abundances of chaetognaths and parasites were associated with a high thermal stratification index, salinity, and mixed layer depth. We conclude that there is a positive, non-linear correlation between the abundance of chaetognaths and their parasites. Although El Nino decreased the abundance and diversity of chaetognaths throughout the time series, the abundance and diversity of their parasites were not significantly different among hydro-climatic periods, suggesting that host abundance must decrease orders of magnitude to influence host availability for parasites.	[Lozano-Cobo, Horacio; Gomez-Gutierrez, Jaime] Inst Politecn Nacl, Dept Plancton & Ecol Marina, Ctr Interdisciplinario Ciencias Marinas, Av IPN S-N, La Paz 23096, Bcs, Mexico; [Franco-Gordo, Carmen; Plascencia-Palomera, Viridiana; Ambriz-Arreola, Israel] Univ Guadalajara, Dept Estudios Desarrollo Sustentable Zonas Coster, Ctr Univ Costa Sur, Gomez Farias 82, San Patricio Melaque 48980, Jalisco, Mexico; [del Carmen Gomez del Prado-Rosas, Maria] Univ Autonoma Baja California Sur, Dept Acad Ciencias Mar & Tierra, Lab Parasitol, Apdo Postal 19-B, La Paz 23080, Bcs, Mexico	Instituto Politecnico Nacional - Mexico; Universidad de Guadalajara; Universidad Autonoma de Baja California	Gómez-Gutiérrez, J (通讯作者)，Inst Politecn Nacl, Dept Plancton & Ecol Marina, Ctr Interdisciplinario Ciencias Marinas, Av IPN S-N, La Paz 23096, Bcs, Mexico.	jgomezgu@gmail.com		Lozano-Cobo, Horacio/0000-0002-2461-3042; Carmen, Franco-Gordo/0000-0001-9274-4020	University of Guadalajara; Consejo Nacional de Ciencia y Tecnologia (CONACYT) [A140618]; PIFI-IPN [SIP20110012]; BEIFI-IPN [SIP20140497, 20150113, 20171275]; SIP-IPN annual grants [20150113, 20171275, 20110012, 20120948, 20130224, 20140497, 20160495]; SEP-CONACyT Ciencia Basica [2012-01-178615, 2016-01-284201]	University of Guadalajara; Consejo Nacional de Ciencia y Tecnologia (CONACYT)(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); PIFI-IPN; BEIFI-IPN; SIP-IPN annual grants; SEP-CONACyT Ciencia Basica	The University of Guadalajara provided research funds. We thank Ariel Cruz-Villacorta (CIBNOR) for his technical help with the SEM observations. Consejo Nacional de Ciencia y Tecnologia (CONACYT) (A140618), PIFI-IPN (SIP20110012), BEIFI-IPN (SIP20140497, 20150113, 20171275) provided PhD financial support to H.L.C. Funding for zooplankton analysis was provided by SIP-IPN annual grants (20110012, 20120948, 20130224, 20140497, 20150113, 20160495, 20171275) and SEP-CONACyT Ciencia Basica 2012-01-178615, 2016-01-284201. C.F.G., I.A.A., and J.G.G. are SNI fellows, and J.G.G. is also a COFFA-IPN and EDI-IPN fellow. We thank Eva Kozak for English editorial help on an earlier version of the manuscript.	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Aquat. Org.	AUG 14	2018	129	3					215	238		10.3354/dao03245	http://dx.doi.org/10.3354/dao03245			24	Fisheries; Veterinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Veterinary Sciences	GV8DS	30154282	Bronze			2025-03-11	WOS:000446367300007
J	Padmakumar, KB; Thomas, LC; Salini, TC; Vijayan, A; Sudhakar, M				Padmakumar, K. B.; Thomas, Lathika Cicily; Salini, T. C.; Vijayan, Anilkumar; Sudhakar, M.			Subsurface bloom of dinoflagellate <i>Gonyaulax polygramma</i> Stein in the shelf waters off Mangalore-South Eastern Arabian Sea	INDIAN JOURNAL OF GEO-MARINE SCIENCES			English	Article						Gonyaulax polygramma; Harmful Algal Blooms; Ecdysis cysts; Water column stability; South Eastern Arabian Sea	RED-TIDE; WEST-COAST; PHYTOPLANKTON; MORTALITY; FISH	A monospecific bloom of thecate dinoflagellate Gonyaulax polygramma (5x 10(8) cells L-1) was observed from the shelf waters off Mangalore (South Eastern Arabian Sea) during late summer monsoon. The bloom was observed to be subsurface (similar to 5m depth) with chlorophyll a maxima of 13.15 mu g L-1 The species observed to be photosynthetic and no visible food vacuoles were observed within the cell. Water column stability with sufficient inorganic nutrients during the fag end of summer monsoon might have favoured the bloom species. The region observed complete exclusion of zooplankton and can suggestively due to unpalatability of the bloom species.	[Padmakumar, K. B.; Salini, T. C.; Vijayan, Anilkumar; Sudhakar, M.] Minist Earth Sci, Ctr Marine Living Resources & Ecol, Kochi 37, Kerala, India; [Padmakumar, K. B.; Thomas, Lathika Cicily] CUSAT, Sch Marine Sci, Dept Marine Biol Microbiol & Biochem, Kochi 16, Kerala, India	Ministry of Earth Sciences (MoES) - India; Centre for Marine Living Resources & Ecology (CMLRE); Cochin University Science & Technology	Padmakumar, KB (通讯作者)，Minist Earth Sci, Ctr Marine Living Resources & Ecol, Kochi 37, Kerala, India.; Padmakumar, KB (通讯作者)，CUSAT, Sch Marine Sci, Dept Marine Biol Microbiol & Biochem, Kochi 16, Kerala, India.	kbpadmakumar@gmail.com	Vijayan, Anil/V-9755-2019; KB, Padmakumar/AAJ-1065-2021					ALLEN WINFRED EMORY, 1935, ANN LARD BOT BUITENZORG, V44, P101; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1994, IOC MAN GUID 29 UNES; BHIMACHAR B. S., 1950, PROC INDIAN ACAD SCI SECT B, V31, P339; Bravo Isabel, 2014, Microorganisms, V2, P11; 조은섭, 2011, [JOURNAL OF ENVIRONMENTAL SCIENCE INTERNATIONAL, 한국환경과학회지], V20, P1521; Eppley R. W, 1974, P 1 INT C TOX DIN BL, P11; Goswami SC., 2004, Zooplankton methodology, collection and identification a field maual NIO, P16; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Jeong HJ, 2005, AQUAT MICROB ECOL, V38, P249, DOI 10.3354/ame038249; Jugnu R, 2008, MARINE FISHERIES INF; Karlson B., 2010, IOC manuals and guides no 55; Karunasagar Iddya, 1992, Journal of Shellfish Research, V11, P477; KATTI RJ, 1988, CURR SCI INDIA, V57, P380; Koizumi Y, 1996, NIPPON SUISAN GAKK, V62, P217; Krishnakumar PK, 2008, FISH OCEANOGR, V17, P45, DOI 10.1111/j.1365-2419.2007.00455.x; Kudela Raphael, 2005, Oceanography, V18, P184; Lewis E. J., 1965, PROCEEDING SEMINAR S, P224; MARGALEF R, 1978, OCEANOL ACTA, V1, P493; Naqvi SWA, 1998, CURR SCI INDIA, V75, P543; Nayak BB, 2000, INDIAN J MAR SCI, V29, P139; Nishikawa T., 1901, ANNOT ZOOL JAPON, V4, P31, DOI 10.34434/za000041; Padmakumar K. B., 2011, International Journal of Biosciences (IJB), V1, P57; Padmakumar K.B., 2012, INT J OCEANOGR, V2012, P1, DOI [10.1155/2012/263946, DOI 10.1155/2012/263946]; Padmakumar K. B., 2010, THESIS; PAERL HW, 1988, LIMNOL OCEANOGR, V33, P823, DOI 10.4319/lo.1988.33.4_part_2.0823; Parsons R.T., 1984, A manual of chemical and biological methods for seawater analysis, V1st, P173; Pitcher GC, 1998, MAR ECOL PROG SER, V172, P253, DOI 10.3354/meps172253; Pond S., 1993, INTRO DYNAMIC OCEANO, P240; PRAKASH A, 1964, CURR SCI INDIA, V33, P168; Reid F. M. H, 1970, Bull. Scripps Instn Oceanogr. tech. Ser., V17, P51; Silva MSD, 2011, INDIAN J GEO-MAR SCI, V40, P697; Smayda Theodore J., 2002, Harmful Algae, V1, P95, DOI 10.1016/S1568-9883(02)00010-0; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; THRONDSEN J, 1973, Norwegian Journal of Zoology, V21, P193; TOMAS C.R., 1997, IDENTIFYING MARINE P, P858; Winkler L.W., 1988, BER DTSCHE CHEM GES, V21, P2843, DOI DOI 10.1002/CBER.188802102122; Wyatt T, 2014, DEEP-SEA RES PT II, V101, P32, DOI 10.1016/j.dsr2.2012.12.006; Yamamoto Tamiji, 1997, Bulletin of the Japanese Society of Fisheries Oceanography, V61, P114	39	11	11	0	6	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.	AUG	2018	47	8					1658	1664						7	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	HC4QQ					2025-03-11	WOS:000451789700018
J	Van Nieuwenhove, N; Pearce, C; Knudsen, MF; Roy, H; Seidenkrantz, MS				Van Nieuwenhove, Nicolas; Pearce, Christof; Knudsen, Mads Faurschou; Roy, Hans; Seidenkrantz, Marit-Solveig			Meltwater and seasonality influence on Subpolar Gyre circulation during the Holocene	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						North Atlantic Ocean; Sea surface temperature; Sea surface salinity; Dinoflagellate cysts; Periodicity	LAURENTIDE ICE-SHEET; ICELAND-SCOTLAND OVERFLOW; NORTH-ATLANTIC CLIMATE; SEA-SURFACE CONDITIONS; LAST GLACIAL MAXIMUM; DINOFLAGELLATE CYSTS; SPATIAL AUTOCORRELATION; OVERTURNING CIRCULATION; MARINE-SEDIMENTS; HEAT-TRANSPORT	Dinoflagellate cyst assemblages in a marine sediment core from the Iceland Basin were used to carry out qualitative and quantitative assessments of upper ocean conditions in the northern branch of the Subpolar Gyre (SPG) during the Holocene. The data revealed that the early Holocene, i.e. prior to similar to 6.8 kyr B.P., experienced elevated summer sea surface temperatures (SST). In contrast, winter SST was lower compared to modern conditions. This stronger-than-present seasonality revealed by our data thus shows the influence of the early Holocene insolation forcing. Higher seasonality also dominated the reconstructed sea surface salinity (SSS) in the same period, with lower salinity during both summers and winters. The lower SSS suggests freshwater advection into the SPG, and the dinoflagellate cyst content from this interval indicates a dominant sourcing from the Canadian Labrador coast, and thus the eastern margin of the Laurentide Ice Sheet. Within this interval of low SSS, the onset of the Holocene Climate Optimum stands out by its distinct "marine" assemblage components and associated high summer SST and relative SSS increase between 9.3 and 7.8 kyr B.P. A prominent shift in the overall assemblage composition occurs at 6.8 kyr B.P., with lower seasonality in sea surface conditions from that time onwards. Increased summer and winter SSS suggest that this change is linked to the halted influence of meltwater from the Laurentide Ice Sheet, a westward shift of the subpolar front and a contracted SPG allowing an easier northward movement of southern-sourced North Atlantic waters, contributing to and consequently sustained by the spin-up of the overturning circulation. The subpolar front appears to gradually have moved slightly eastward again between 2.8 and 1.9 kyr B.P. towards its modern-day position, with a subtle increase of elements characterized by a typical East Greenland Current signature in the Iceland Basin. Finally, spectral analyses indicate that a range of periodicities may be present in the new SSS and SST records, most notably a 2000-yr periodicity in SSS changes, although none of the periodicities are dominant in both records or throughout the time interval covered by the records.	[Van Nieuwenhove, Nicolas] Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB, Canada; [Van Nieuwenhove, Nicolas; Pearce, Christof; Knudsen, Mads Faurschou; Seidenkrantz, Marit-Solveig] Aarhus Univ, Dept Geosci, iClimate, Arctic Res Ctr,Ctr Past Climate Studies, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Roy, Hans] Aarhus Univ, Dept Biosci, Ctr Geomicrobiol, Ny Munkegade 116, DK-8000 Aarhus C, Denmark	University of New Brunswick; Aarhus University; Aarhus University	Van Nieuwenhove, N (通讯作者)，Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB, Canada.	nicolas.vannieuwenhove@unb.ca	Van Nieuwenhove, Nicolas/IAQ-1532-2023; Knudsen, Mads/H-4842-2012; Pearce, Christof/M-4852-2013; Roy, Hans/G-3842-2010; Seidenkrantz, Marit-Solveig/A-3451-2012	Pearce, Christof/0000-0002-4866-3204; Roy, Hans/0000-0002-6477-3091; Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969	Danish Council for Independent Research, Natural Science [12-126709/0602-02361B]; Independent Research Fund Denmark/Natural Science [7014-00113B]; Danish Centre for Marine Sciences (Dansk Center for Havforskning)	Danish Council for Independent Research, Natural Science(Det Frie Forskningsrad (DFF)); Independent Research Fund Denmark/Natural Science; Danish Centre for Marine Sciences (Dansk Center for Havforskning)	We would like to thank the captain, crew and participants of the DA12-11/2 expedition onboard R/V Dana for their work and efforts in recovering the core. We thank Kirsten Rosendal, Aarhus University, for preparing the dinocyst samples. The Aarhus AMS Centre at the Department of Physics and Astronomy, Aarhus University, is acknowledged for producing the radiocarbon dates. We thank Sandrine Solignac and Matthias Moros for sharing raw data. We appreciate the time and efforts invested by two anonymous reviewers and editor Thierry Correge to provide valuable constructive comments. The research cruise was funded by the Danish Centre for Marine Sciences (Dansk Center for Havforskning) as part of a PhD course "Benthic Research at Sea" taking place in September 24-30, 2012. The project was funded by the Danish Council for Independent Research, Natural Science (project nos. 12-126709/0602-02361B) and the Independent Research Fund Denmark/Natural Science (G-Ice project no 7014-00113B).	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Paleoclimatol. Paleoecol.	AUG 1	2018	502						104	118		10.1016/j.palaeo.2018.05.002	http://dx.doi.org/10.1016/j.palaeo.2018.05.002			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	GI8AZ					2025-03-11	WOS:000434745500008
J	Kingsley, OK; Umeji, OP				Kingsley, Okeke Kachikwulu; Umeji, Obianuju P.			Palynofacies, Organic Thermal Maturation and Source Rock Evaluation of Nanka and Ogwashi Formations in Updip Niger Delta Basin, Southeastern Nigeria	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article							SEDIMENTS; MATTER	The oil and gas prospects in the Nigerian inland basins necessitated the palynofacies characterization, thermal maturation and source rock evaluation of the Nanka and Ogwashi formations of the Niger delta basin. The Nanka Formation has dominant terrestrial microflora, brown structured phytoclasts and amorphous organic matter, opaque debris accompanied by dinoflagellate cysts. The Ogwashi Formation has maximum terrestrial microflora, medium to large brown structured phytoclasts, opaque debris with abundance of dark brown amorphous organic matter and a few marine taxa. Palynofacies constituents of the Nanka Formation reflect Kerogen Type II / III which are Gas / Oil prone shown by abundance of marine species, amorphous organic matter in conjunction with terrestrial phytoclasts and non-marine palynomorphs assemblage. The spore/pollen colour range from light brown to dark brown which suggest oil generation to production of wet gas. This corresponds to thermal alteration index (TAI) 2+ to 3+ and vitrinite reflectance index (%R-o) 0.5% to 1.3%. Palynofacies of the Ogwashi Formation has Kerogen Type III (gas prone) linked with overwhelming abundant terrestrial phytoclasts palynomorphs and large amorphous organic matter of terrestrial origin. Spore/pollen thermal alteration colour ranges from light medium brown to dark brown indicative of mature oil generation and transition to dry gas phase. The thermal alteration index and vitrinite reflectance index (%R-o) values of the Ogwashi Formation is consistent with that of the Nanka Formation.	[Kingsley, Okeke Kachikwulu; Umeji, Obianuju P.] Univ Nigeria, Dept Geol, Nsukka, Nigeria	University of Nigeria	Kingsley, OK (通讯作者)，Univ Nigeria, Dept Geol, Nsukka, Nigeria.	okekekingsleyk@gmad.com; obianuju.umeji@unn.edu.ng						[Anonymous], J MICROPALAEONTOLOGY; Avbovbo AA., 1978, Bull. Can. Petrol. Geol., V26, P268; Batten D.J., 1999, FOSSIL PLANTS SPORES, P15; BUSTIN RM, 1988, AAPG BULL, V72, P277; Claret J., 1981, B RECH SNEA P, V5, P383; COMBAZ A., 1964, REV MICROPALDONTOL, V7, P205; EVAMY BD, 1978, AAPG BULL, V62, P1; Ezeofor A.O., 2004, THESIS, P51; GERMERAAD JH, 1968, REV PALAEOBOT PALYNO, V6, P189, DOI 10.1016/0034-6667(68)90051-1; Hayes J.M., 1983, Precambrian organic geochemistry - Preservation of the record; Jan du Chene R.E., 1978, Compte Rendu des Seances de la SPHN Geneve, V13, P5; Mehrotra N.C., 2002, MEM GEOL SOC INDIA, V61; Mude O., 2014, NIG ASS PETR EXPL C, pA13; NWACHUKWU JI, 1986, AAPG BULL, V70, P48; Nwajide C.S., 1996, NAPE B, V12, P75; Nwajide C. S., 1980, GEOLOGY, V25, P189; Nwajide CS, 2013, GEOLOGY NIGERIAS SED, P347; Oboh Francisca E., 1992, Palaios, V7, P559, DOI 10.2307/3514869; Oboh-Ikuenobe FE, 2005, J AFR EARTH SCI, V41, P79, DOI 10.1016/j.jafrearsci.2005.02.002; Okeke K. K., ALAKIRI FIELD NIGER, P7; Okeke KK, 2016, J AFR EARTH SCI, V120, P102, DOI 10.1016/j.jafrearsci.2016.04.020; Okezie C.N., 1985, Geol. Surv. Nigeria Occ. Pap., V10; Pearson DL., 1984, PALEOPALYNOLOGY, P581; Samuel N., 2014, GEOLOGY OKIGWE UNPUB, P94; Short K.C., 1967, AAPG AM ASS PET GEOL, V54, P750; Thomas B.M., 1982, Journal of Australian Petroleum Exploration Association, V22, P164, DOI [10.1071/AJ81012, DOI 10.1071/AJ81012]; Traverse A, 2007, Paleopalynology, V28, P615, DOI DOI 10.1007/978-1-4020-5610-9; 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]; Umeji OP., 2002, J MIN GEOL, V38, P111, DOI DOI 10.4314/JMG.V38I2.18781; Umeji OP, 2003, J MIN GEOL39, P95; van Hoeken-Klinkenberg P.M. J., 1966, Leidse geologische Mededelingen, V38, P37; Whitaker F, 1982, PALYNOFACIES INVEST, V31/2-4, P1; Whitaker M.F., 1992, GEOLOGY BRENT GROUP, V61, P169; Whitaker MF, 1984, PALYNOLOGICAL RESULT, P1	35	2	2	0	11	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	AUG	2018	92	2					215	226		10.1007/s12594-018-0984-9	http://dx.doi.org/10.1007/s12594-018-0984-9			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GQ3VR					2025-03-11	WOS:000441596000013
J	Tesson, SVM; Weissbach, A; Kremp, A; Lindström, Å; Rengefors, K				Tesson, Sylvie V. M.; Weissbach, Astrid; Kremp, Anke; Lindstrom, Ake; Rengefors, Karin			The potential for dispersal of microalgal resting cysts by migratory birds	JOURNAL OF PHYCOLOGY			English	Article						Apocalathium malmogiense; dinoflagellate cysts; endozoochory; microorganism dispersal; Peridiniopsis borgei	FRESH-WATER ALGAE; AQUATIC ORGANISMS; DINOFLAGELLATE CYSTS; SPRING BLOOM; GREEN-ALGAE; VIABILITY; MARINE; GERMINATION; DUCKS; FLOW	Most microalgal species are geographically widespread, but little is known about how they are dispersed. One potential mechanism for long-distance dispersal is through birds, which may transport cells internally (endozoochory) and deposit them during, or in-between, their migratory stopovers. We hypothesize that dinoflagellates, in particular resting stages, can tolerate bird digestion; that bird temperature, acidity, and retention time negatively affect dinoflagellate viability; and that recovered cysts can germinate after passage through the birds' gut, contributing to species-specific dispersal of the dinoflagellates across scales. Tolerance of two dinoflagellate species (Peridiniopsis borgei, a warm-water species and Apocalathium malmogiense, a cold-water species) to Mallard gut passage was investigated using invitro experiments simulating the gizzard and caeca conditions. The effect of invitro digestion and retention time on cell integrity, cell viability, and germination capacity of the dinoflagellate species was examined targeting both their vegetative and resting stages. Resting stages (cysts) of both species were able to survive simulated bird gut passage, even if their survival rate and germination were negatively affected by exposure to acidic condition and bird internal temperature. Cysts of A.malmogiense were more sensitive than P.borgei to treatments and to the presence of digestive enzymes. Vegetative cells did not survive conditions of bird internal temperature and formed pellicle cysts when exposed to gizzard-like acid conditions. We show that dinoflagellate resting cysts serve as dispersal propagules through migratory birds. Assuming a retention time of viable cysts of 2-12h to duck stomach conditions, cysts could be dispersed 150-800km and beyond.	[Tesson, Sylvie V. M.; Weissbach, Astrid; Lindstrom, Ake; Rengefors, Karin] Lund Univ, Dept Biol, SE-22362 Lund, Sweden; [Kremp, Anke] Finnish Environm Inst, Marine Res Ctr, FI-00560 Helsinki, Finland	Lund University; Finnish Environment Institute	Tesson, SVM (通讯作者)，Lund Univ, Dept Biol, SE-22362 Lund, Sweden.	tesson.sylvie.vm@gmail.com	Rengefors, Karin/K-5873-2019; Tesson, Sylvie VM/D-9018-2015	Tesson, Sylvie VM/0000-0002-0751-6953; Rengefors, Karin/0000-0001-6297-9734	Ebba och Sven Schwarz Stiftelse; Walter and Andree de Nottbeck Foundation; Sven och Lilly Lawski Foundation	Ebba och Sven Schwarz Stiftelse; Walter and Andree de Nottbeck Foundation; Sven och Lilly Lawski Foundation	Economic support was provided by Ebba och Sven Schwarz Stiftelse to K.R., by Walter and Andree de Nottbeck Foundation to A.K. and by Sven och Lilly Lawski Foundation to S.T. The authors declare no conflict of interest.	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Phycol.	AUG	2018	54	4					518	528		10.1111/jpy.12756	http://dx.doi.org/10.1111/jpy.12756			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	GQ6UC	29889985				2025-03-11	WOS:000441860300009
J	Kubiszyn, AM; Svensen, C				Kubiszyn, Anna M.; Svensen, Camilla			First record of a rare species, <i>Polyasterias problematica</i> (Prasinophyceae), in Balsfjord, northern Norway	BOTANICA MARINA			English	Article						Balsfjord; northern Norway; planktonic protists; Polyasterias problematica; Prasinophyceae	DINOFLAGELLATE CYSTS; BLACK-SEA; PHYTOPLANKTON 1976-1978; PLANKTON COMMUNITY; SEDIMENTS; ASSEMBLAGES; ABUNDANCE; DYNAMICS; SUMMER; QUEBEC	Polyasterias problematica is a poorly investigated prasinophyte species, practically known only from a few, primarily historical studies. Fragmentary information on the species indicates that P. problematica is mainly distributed in the euphotic zone of the Canadian and Russian Arctic, Atlantic Canada, the mid-Atlantic and some European seas. Here, we present the first record of this species in the Balsfjord waters, northern Norway. A detailed morphological description, with line drawings and microscopy-based photographs, as well as information on its up-to-date geographical distribution and possible explanations for its extraordinary scarcity are provided.	[Kubiszyn, Anna M.] Polish Acad Sci, Ctr Polar Studies KNOW, Leading Natl Res Ctr, Dept Marine Ecol,Inst Oceanol, Powstancow Warszawy 55, PL-81712 Sopot, Poland; [Svensen, Camilla] UiT Arctic Univ Tromso, Fac Biosci Fisheries & Econ, Dept Arctic & Marine Biol, N-9037 Tromso, Norway	Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences; UiT The Arctic University of Tromso	Kubiszyn, AM (通讯作者)，Polish Acad Sci, Ctr Polar Studies KNOW, Leading Natl Res Ctr, Dept Marine Ecol,Inst Oceanol, Powstancow Warszawy 55, PL-81712 Sopot, Poland.	aniak@iopan.gda.pl	Svensen, Camilla/AAH-3234-2020	Dabrowska (Kubiszyn), Anna/0000-0002-0911-3082	Fram Centre flagship "Fjord and Coast"; Let's Sea project [2015/17/N/NZ8/01642]; AREX project [W12/Norway/2016]; Leading National Research Centre (KNOW)	Fram Centre flagship "Fjord and Coast"; Let's Sea project; AREX project; Leading National Research Centre (KNOW)	We would like to thank two anonymous reviewers for their constructive comments and the editor Dr. Michel Poulin for his thorough review of the manuscript. We also thank professor Jozef Maria Wiktor (Institute of Oceanology Polish Academy of Sciences) for protist taxonomic consultations and comments on the manuscript, as well as Wiola Rasmus (Max Planck Institute for Evolutionary Biology) for preparing the line drawings. This study was funded by The Fram Centre flagship "Fjord and Coast" and was implemented with the support of the Let's Sea (2015/17/N/NZ8/01642) and AREX (W12/Norway/2016) projects. The publication has been financed from the funds of the Leading National Research Centre (KNOW) received by the Centre for Polar Studies for the period 2014-2018.	ANDERSON JT, 1980, CAN J FISH AQUAT SCI, V37, P2242, DOI 10.1139/f80-269; [Anonymous], 1958, Mitt. Int. Ver. Theor. Angew. Limnol., DOI DOI 10.1080/05384680.1958.11904091; Bech P. A., 1982, THESIS, P130; Berard-Therriault L., 1999, Publ spec can sci halieut aquat, V128, P1; Bergins B. V. A., 1932, Folia Zoologica et Hydrobiologica Riga, V4, P68; Bringue M. 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Marina	AUG	2018	61	4					421	428		10.1515/bot-2017-0123	http://dx.doi.org/10.1515/bot-2017-0123			8	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	GO4WF		Green Submitted			2025-03-11	WOS:000440017400011
J	Schneider, AC; Heimhofer, U; Heunisch, C; Mutterlose, J				Schneider, Anton Christoph; Heimhofer, Ulrich; Heunisch, Carmen; Mutterlose, Joerg			From arid to humid - The Jurassic-Cretaceous boundary interval in northern Germany	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palynology; Lower Saxony Basin; Climate change; Jurassic-Cretaceous boundary; Berriasian; Wealden	PURBECK LIMESTONE GROUP; LOWER SAXONY BASIN; MUNDER FORMATION; HILS SYNCLINE; SPORES INSITU; IN-SITU; CLIMATE; DORSET; SEDIMENTS; WEALDEN	The Jurassic-Cretaceous boundary interval in northwest Europe is characterised by a distinctive climatic change from pronounced aridity toward more humid conditions. In order to better understand the timing and evolution of the environmental dynamics related to this climatic change, terrestrial and aquatic palynomorphs (spores, pollen, dinoflagellate cysts, freshwater algae) have been studied from two recently drilled cores. The cores, which are both located in the Lower Saxony Basin (northern Germany), provide two 139 m and 134 m thick non marine successions embedded in a high-resolution biostratigraphic framework. The lower part of the cores can be attributed to the Winder Formation (upper Tithonian-middle Berriasian), the upper part to the Buckeberg Group (middle-upper Berriasian). For reconstructing the arid to humid climate transition 110 samples have been analysed for their palynological content. In the Lower Saxony Basin, the late Jurassic-earliest Berriasian vegetation was dominated by cheirolepidiacean conifer forests growing under arid conditions along a coastal belt. A marked decline in cheirolepidiacean pollen and the spread of pioneering plants records an increase in seasonal humidity in the early-mid Berriasian. In the mid-late Berriasian the presence of highly diverse floras reflects even more humid and warm conditions. Fluvio-deltaic mixed swamp forests, which grew landwards behind the coastal belt were composed of conifers, ferns, lycopods, horsetails, bryophytes, ginkgos, cycads and Bennettitales. Cheirolepidiaceans, probably forming part of mangrove-type plant communities, remained an important component of the coastal flora. The climatic shift correlates to the upper Subcraspedites lamplughi-middle Heteroceras kochi ammonite zones of the marine Boreal zonation scheme and is synchronous to the early-mid Berriasian shift from arid to humid recorded from southern England. (C) 2018 Elsevier B.V. All rights reserved.	[Schneider, Anton Christoph; Mutterlose, Joerg] Ruhr Univ Bochum, Inst Geol Mineral & Geophys, Univ Str 150, D-44801 Bochum, Germany; [Heimhofer, Ulrich] Leibniz Univ Hannover, Inst Geol, Callinstr 30, D-30167 Hannover, Germany; [Heunisch, Carmen] Landesamt Bergbau Energie & Geol, Stilleweg 2, D-30655 Hannover, Germany	Ruhr University Bochum; Leibniz University Hannover	Schneider, AC (通讯作者)，Ruhr Univ Bochum, Inst Geol Mineral & Geophys, Univ Str 150, D-44801 Bochum, Germany.	christoph.schneider@rub.de; heimhofer@geowi.uni-hannover.de; Carmen.Heunisch@lbeg.niedersachsen.de; joerg.mutterlose@rub.de	Mutterlose, Joerg/IYJ-0031-2023	Mutterlose, Joerg/0000-0003-3449-4507				Abbink O, 2001, GLOBAL PLANET CHANGE, V30, P231, DOI 10.1016/S0921-8181(01)00101-1; Abbink O.A., 1998, LAB PALAEOBOT PALYNO, V8, P1; Abbink OA, 2004, NETH J GEOSCI, V83, P17, DOI 10.1017/S0016774600020436; Abbink OA, 2001, P YORKS GEOL SOC, V53, P275, DOI 10.1144/pygs.53.4.275; Allen P, 1998, P GEOLOGIST ASSOC, V109, P197, DOI 10.1016/S0016-7878(98)80066-7; ANDERSON FW, 1964, NATURE, V201, P907, DOI 10.1038/201907a0; [Anonymous], 1994, AM ASS PETROLEUM GEO, DOI DOI 10.1306/M60585C34; [Anonymous], 1980, MEM MUS NAT HIST NAT; [Anonymous], 1997, Zeitschrift der Deutschen Geologischen Gesellschaft, DOI DOI 10.1127/ZDGG; [Anonymous], 1979, YORKSHIRE JURASSIC F; Arp G, 2008, SEDIMENTOLOGY, V55, P1227, DOI 10.1111/j.1365-3091.2007.00944.x; Arp G, 2008, PALAEOGEOGR PALAEOCL, V264, P230, DOI 10.1016/j.palaeo.2007.02.051; BALME BE, 1995, REV PALAEOBOT PALYNO, V87, P85; Batten D.J., 1984, FOSSILS CLIMATE, P127; BATTEN D.J., 1975, P GEOL ASS, V85, P433; Batten DJ, 2002, SPEC PAP PALAEONTOL, P13; BATTEN DJ, 1985, REV PALAEOBOT PALYNO, V44, P233, DOI 10.1016/0034-6667(85)90018-1; Beck CB, 1988, Origin and evolution of gymnosperms, P382; Bischoff G., 1963, ERDOEL Z, V10, P445; Boulter M., 1993, Special Papers in Palaeontology, V49, P125; BURGER D., 1966, LEID GEOL MEDED, V35, P209; Bush ABG, 1997, SCIENCE, V275, P807, DOI 10.1126/science.275.5301.807; Chaloner W.G., 1968, Coal and Coal-bearing Strata; CLEMENTS R.G., 1993, PROC DORSET NAT HIST, V114, P181; COUPER R.A., 1958, PALAEONTOGRAPHICA, V103, P75; DETTMANN M.E., 1963, P ROY SOC VICTORIA, V77, P1; Dorhofer G., 1977, Geologisches Jahrbuch A, V42, P3; Dorhofer G., 1977, NEUES JB GEOLOGIE PA, V153, P50; DORING H., 1965, GEOLOGIE 14 BEIH, V47, P1; Elstner F, 1996, CRETACEOUS RES, V17, P119, DOI 10.1006/cres.1996.0010; Elstner F., 1993, ZITTELIANA, V20, P389; Erbacher J., 2014, Litholex; Filatoff J., 1975, Palaeontographica Abteilung B Palaeophytologie, V154, P1; FRANCIS JE, 1983, PALAEONTOLOGY, V26, P277; FRANCIS JE, 1984, PALAEOGEOGR PALAEOCL, V48, P285, DOI 10.1016/0031-0182(84)90049-X; Galloway JM, 2013, MAR PETROL GEOL, V44, P240, DOI 10.1016/j.marpetgeo.2013.01.001; Gray J., 1965, Handbook of paleontological techniques, P530; GRIMM E.C., 1991, Tilia and TiliaGraph. 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J	Cramwinckel, MJ; Huber, M; Kocken, IJ; Agnini, C; Bijl, PK; Bohaty, SM; Frieling, J; Goldner, A; Hilgen, FJ; Kip, EL; Peterse, F; van der Ploeg, R; Röhl, U; Schouten, S; Sluijs, A				Cramwinckel, Margot J.; Huber, Matthew; Kocken, Ilja J.; Agnini, Claudia; Bijl, Peter K.; Bohaty, Steven M.; Frieling, Joost; Goldner, Aaron; Hilgen, Frederik J.; Kip, Elizabeth L.; Peterse, Francien; van der Ploeg, Robin; Roehl, Ursula; Schouten, Stefan; Sluijs, Appy			Synchronous tropical and polar temperature evolution in the Eocene	NATURE			English	Article							TETRAETHER MEMBRANE-LIPIDS; ODP SITE 1263; DINOFLAGELLATE CYSTS; SOUTHWEST PACIFIC; ATMOSPHERIC CO2; SOUTHERN-OCEAN; CLIMATE; TEX86; GREENHOUSE; MARINE	Palaeoclimate reconstructions of periods with warm climates and high atmospheric CO2 concentrations are crucial for developing better projections of future climate change. Deep-ocean(1,2) and high-latitude(3) palaeotemperature proxies demonstrate that the Eocene epoch (56 to 34 million years ago) encompasses the warmest interval of the past 66 million years, followed by cooling towards the eventual establishment of ice caps on Antarctica. Eocene polar warmth is well established, so the main obstacle in quantifying the evolution of key climate parameters, such as global average temperature change and its polar amplification, is the lack of continuous high-quality tropical temperature reconstructions. Here we present a continuous Eocene equatorial sea surface temperature record, based on biomarker palaeothermometry applied on Atlantic Ocean sediments. We combine this record with the sparse existing data(4-6) to construct a 26-million-year multi-proxy, multi-site stack of Eocene tropical climate evolution. We find that tropical and deep-ocean temperatures changed in parallel, under the influence of both long-term climate trends and short-lived events. This is consistent with the hypothesis that greenhouse gas forcing(7,8), rather than changes in ocean circulation(9,10), was the main driver of Eocene climate. Moreover, we observe a strong linear relationship between tropical and deep-ocean temperatures, which implies a constant polar amplification factor throughout the generally ice-free Eocene. Quantitative comparison with fully coupled climate model simulations indicates that global average temperatures were about 29, 26, 23 and 19 degrees Celsius in the early, early middle, late middle and late Eocene, respectively, compared to the preindustrial temperature of 14.4 degrees Celsius. Finally, combining proxy- and model-based temperature estimates with available CO2 reconstructions(8 )yields estimates of an Eocene Earth system sensitivity of 0.9 to 2.3 kelvin per watt per square metre at 68 per cent probability, consistent with the high end of previous estimates(11).	[Cramwinckel, Margot J.; Kocken, Ilja J.; Bijl, Peter K.; Frieling, Joost; Hilgen, Frederik J.; Kip, Elizabeth L.; Peterse, Francien; van der Ploeg, Robin; Schouten, Stefan; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands; [Huber, Matthew; Goldner, Aaron] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA; [Agnini, Claudia] Univ Padua, Dept Geosci, Padua, Italy; [Bohaty, Steven M.] Univ Southampton, Natl Oceanog Ctr Southampton, Ocean & Earth Sci, Southampton, Hants, England; [Roehl, Ursula] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Schouten, Stefan] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Microbiol & Biogeochem, Den Burg, Netherlands; [Schouten, Stefan] Univ Utrecht, Den Burg, Netherlands	Utrecht University; Purdue University System; Purdue University; University of Padua; NERC National Oceanography Centre; University of Southampton; University of Bremen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Cramwinckel, MJ (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands.	m.j.cramwinckel@uu.nl	Röhl, Ursula/G-5986-2011; Peterse, Francien/AAY-1473-2021; Agnini, Claudia/AAB-9971-2020; Schouten, Stefan/P-4380-2016; Peterse, Francien/H-5627-2011; Huber, Matthew/A-7677-2008; Sluijs, Appy/B-3726-2009	Cramwinckel, Marlow Julius/0000-0002-6063-836X; Peterse, Francien/0000-0001-8781-2826; van der Ploeg, Robin/0000-0001-5096-7496; Huber, Matthew/0000-0002-2771-9977; Sluijs, Appy/0000-0003-2382-0215; Agnini, Claudia/0000-0001-9749-6003; Bijl, Peter/0000-0002-1710-4012; Hilgen, Frits/0000-0002-5683-259X; Kocken, Ilja Japhir/0000-0003-2196-8718	Dutch Ministry of Education, Culture and Science; European Research Council (ERC) [259627]; Netherlands Organisation for Scientific Research (NWO) [834.11.006]; NWO-ALW Veni grants [863.13.002, 863.13.016]; US National Science Foundation (NSF) [OCE-0902882]; NSF; University of Padova [BIRD161002]	Dutch Ministry of Education, Culture and Science; European Research Council (ERC)(European Research Council (ERC)); Netherlands Organisation for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); NWO-ALW Veni grants; US National Science Foundation (NSF)(National Science Foundation (NSF)); NSF(National Science Foundation (NSF)); University of Padova	In this research, we used samples and data provided by the International Ocean Discovery Program (IODP) and its predecessor, the Ocean Drilling Program. This work was carried out under the programme of the Netherlands Earth System Science Centre (NESSC), financially supported by the Dutch Ministry of Education, Culture and Science. A.S. thanks the European Research Council (ERC) for ERG Starting Grant number 259627 under the European Union Seventh Framework Program. This study was made possible by the Netherlands Organisation for Scientific Research (NWO) grant number 834.11.006, which enabled the purchase of the UHPLC-MS system used for GDGT analyses. P.K.B. and F.P. acknowledge NWO-ALW Veni grants number 863.13.002 and number 863.13.016, respectively. M.H. was funded by the US National Science Foundation (NSF) grant OCE-0902882; the CESM model is also supported by the NSF. C.A. acknowledges the University of Padova grant number BIRD161002. We thank B. Wade (University College London) for converting the Eocene TDP data to GTS2012, P. Sexton (The Open University) for converting the middle Eocene Site 1258 data to GTS2012, J. Kiehl and C. Shields for providing their simulation data, G.-J. Reichart (Royal NIOZ and Utrecht University) for discussions, L. van der Heijden (Utrecht University, now at University of La Rochelle, France), M. Nicolai (Utrecht University), A. Mets (NIOZ), N. Welters, A. van Dijk and D. Kasjaniuk (Utrecht Geolab) for analytical support.	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J	Matthiessen, J; Schreck, M; De Schepper, S; Zorzi, C; de Vernal, A				Matthiessen, Jens; Schreck, Michael; De Schepper, Stijn; Zorzi, Coralie; de Vernal, Anne			Quaternary dinoflagellate cysts in the Arctic Ocean: Potential and limitations for stratigraphy and paleoenvironmental reconstructions	QUATERNARY SCIENCE REVIEWS			English	Review						Arctic Ocean; Quaternary; Dinoflagellate cysts; Biostratigraphy; Bioevents; Lithostratigraphy; Composite chronostratigraphy	SEA-SURFACE CONDITIONS; NORTHERN-HEMISPHERE GLACIATIONS; EURASIAN CONTINENTAL-MARGIN; BEAUFORT-MACKENZIE BASIN; AMINO-ACID EPIMERIZATION; NORWEGIAN-GREENLAND SEA; ATLANTIC WATER INFLOW; ICE-SHEET; YERMAK PLATEAU; PLIOCENE-PLEISTOCENE	The Arctic Ocean is a siliciclastic depositional environment which lacks any rock-forming biogenic calcareous and siliceous components during large parts of its Quaternary history. These hemipelagic sediments are nevertheless suitable for the study of organic-walled microfossils of which the fossil remains of dinoflagellates - dinoflagellate cysts - are the most important group. Dinoflagellate cysts have become an important tool in paleoceanography of the high northern latitudes, but their potential for Quaternary biostratigraphy has remained largely unexplored. Dinoflagellate cysts are the dominant marine palynomorph group which is more continuously present in the marginal seas (e.g. Barents Sea, Bering Sea) than in the Arctic Ocean itself throughout the Quaternary. Most species have long stratigraphic ranges, are temporary absent and show abundance variations on glacial-interglacial timescales. Of the more than 30 taxa recorded, only Habibacysta tectata and Filisphaera filifera became extinct in the Pleistocene. The highest persistent occurrence of H. tectata at ca. 2.0 Ma and the top of E filifera acme at ca. 1.8 Ma can be used for supra-regional stratigraphic correlation between the Arctic Ocean and adjacent basins. These events corroborate a slow sedimentation rate model for the Quaternary section on the central Lomonosov Ridge, but a combination of different methods will have to be applied to provide a detailed chronostratigraphy. The occurrence of cysts of phototrophic dinoflagellates in certain stratigraphic intervals on Lomonosov Ridge supports published evidence of episodic opening of the multiyear Arctic sea ice cover during the Quaternary probably related to a stronger inflow of Atlantic water. This contradicts the hypothesis of a permanently ice covered central Arctic Ocean in the Quaternary. (C) 2018 Elsevier Ltd. All rights reserved.	[Matthiessen, Jens] Alfred Wegener Inst, Helmholtz Ctr Polar & Marine Res, D-27568 Bremerhaven, Germany; [Schreck, Michael] Arctic Univ, Univ Tromso, Dept Geosci, N-9037 Tromso, Norway; [De Schepper, Stijn] Bjerknes Ctr Climate Res, Uni Res Climate, Jahnebakken 5, N-5007 Bergen, Norway; [Zorzi, Coralie; de Vernal, Anne] Univ Quebec Montreal, Ctr GEOTOP, Montreal, PQ H3C 3P8, Canada	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; UiT The Arctic University of Tromso; Bjerknes Centre for Climate Research; University of Quebec; University of Quebec Montreal	Matthiessen, J (通讯作者)，Alfred Wegener Inst, Helmholtz Ctr Polar & Marine Res, D-27568 Bremerhaven, Germany.	jens.matthiessen@awi.de	de Vernal, Anne/D-5602-2013; De Schepper, Stijn/A-2836-2011	Matthiessen, Jens/0000-0002-6952-2494; De Schepper, Stijn/0000-0002-6934-0914; Zorzi, Coralie/0000-0002-4910-5255	US National Science Foundation (NSF); Deutsche Forschungsgemeinschaft DFG [Ma3913/1, Ma3913/3]; Research Council of Norway [229819]; Natural Science and Engineering Research Council (NSERC) of Canada	US National Science Foundation (NSF)(National Science Foundation (NSF)); Deutsche Forschungsgemeinschaft DFG(German Research Foundation (DFG)); Research Council of Norway(Research Council of Norway); Natural Science and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	This research used samples and data provided by the Alfred Wegener Institute in Bremerhaven, and the Ocean Drilling Program (ODP) and Integrated Ocean Drilling Program (IODP) sponsored by the US National Science Foundation (NSF) and participating countries. Anja Bartels is thanked for assistance in the laboratory. We sincerely thank Stephen Louwye and Jens De Clercq for sharing with us their unpublished stratigraphic data from Site U1341. Ali Aksu is acknowledged for providing the original planktonic foraminifer and stable isotope data of sediment core CESAR 83-102. The constructive comments and suggestions of Martin Head and an anonymous reviewer helped to improve the manuscript. J.M. acknowledges financial support from the Deutsche Forschungsgemeinschaft DFG (Ma3913/1, Ma3913/3), and S.D.S from the Research Council of Norway (Project 229819). A.d.V and C.Z. are grateful for support from the Natural Science and Engineering Research Council (NSERC) of Canada.	Adler RE, 2009, GLOBAL PLANET CHANGE, V68, P18, DOI 10.1016/j.gloplacha.2009.03.026; Aksu AE, 1988, PALEOCEANOGRAPHY, V3, P519, DOI 10.1029/PA003i005p00519; Aksu A.E., 1985, Geological Survey of Canada Paper, V84, P115; Aksu A. 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J	Bijl, PK; Houben, AJP; Hartman, JD; Pross, J; Salabarnada, A; Escutia, C; Sangiorgi, F				Bijl, Peter K.; Houben, Alexander J. P.; Hartman, Julian D.; Pross, Jorg; Salabarnada, Ariadna; Escutia, Carlota; Sangiorgi, Francesca			Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica - Part 2: Insights from Oligocene-Miocene dinoflagellate cyst assemblages	CLIMATE OF THE PAST			English	Article							STABLE-ISOTOPE RECORDS; SOUTHERN-OCEAN; SEA-LEVEL; SURFACE SEDIMENTS; CARBON-CYCLE; CONTINENTAL-MARGIN; SUBTROPICAL FRONT; EAST ANTARCTICA; ATLANTIC SECTOR; CLIMATE	Next to atmospheric CO2 concentrations, iceproximal oceanographic conditions are a critical factor for the stability of Antarctic marine-terminating ice sheets. The Oligocene and Miocene epochs (similar to 34-5 Myr ago) were time intervals with atmospheric CO2 concentrations between those of present-day and those expected for the near future. As such, these past analogues may provide insights into ice-sheet volume stability under warmer-than-presentday climates. We present organic-walled dinoflagellate cyst (dinocyst) assemblages from chronostratigraphically well-constrained Oligocene to mid-Miocene sediments from Integrated Ocean Drilling Program (IODP) Site U1356. Situated offshore the Wilkes Land continental margin, East Antarctica, the sediments from Site U1356 have archived the dynamics of an ice sheet that is today mostly grounded below sea level. We interpret dinocyst assemblages in terms of paleoceanographic change on different timescales, i.e. with regard to both glacial-interglacial and long-term variability. Our record shows that a sea-ice-related dinocyst species, Selenopemphix antarctica, occurs only for the first 1.5 Myr of the early Oligocene, following the onset of full continental glaciation on Antarctica, and after the Mid-Miocene Climatic Optimum. Dinocysts suggest a weaker-than-modern sea-ice season for the remainder of the Oligocene and Miocene. The assemblages generally bear strong similarity to presentday open-ocean, high-nutrient settings north of the sea-ice edge, with episodic dominance of temperate species similar to those found in the present-day subtropical front. Oligotrophic and temperate surface waters prevailed over the site notably during interglacial times, suggesting that the positions of the (subpolar) oceanic frontal systems have varied in concordance with Oligocene-Miocene glacial-interglacial climate variability.	[Bijl, Peter K.; Hartman, Julian D.; Sangiorgi, Francesca] Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Palaeobot & Paly, POB 80-115, NL-3508 TC Utrecht, Netherlands; [Houben, Alexander J. P.] Netherlands Org Appl Sci Res TNO, Geol Survey Netherlands, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [Pross, Jorg] Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, Neuenheimer Feld 234, D-69120 Heidelberg, Germany; [Salabarnada, Ariadna; Escutia, Carlota] UGR, Inst Andaluz Ciencias Tierra, CSIC, Armilla 18100, Spain	Utrecht University; Netherlands Organization Applied Science Research; Ruprecht Karls University Heidelberg; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT); University of Granada	Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Palaeobot & Paly, POB 80-115, NL-3508 TC Utrecht, Netherlands.	p.k.bijl@uu.nl	Roset, Ariadna/L-8798-2014; Escutia, Carlota/B-8614-2015	Salabarnada, Ariadna/0000-0003-0858-8083; Escutia, Carlota/0000-0002-4932-8619; Hartman, Julian/0000-0001-6256-9989; Houben, Alexander/0000-0002-9497-1048; Bijl, Peter/0000-0002-1710-4012; Sangiorgi, Francesca/0000-0003-4233-6154; Salabarnada, Ariadna/0000-0003-2239-2538	US National Science Foundation; NWO-NNPP [866.10.110]; NWO-ALW VENI [863.13.002]; IODP priority program of the German Research Foundation (DFG); Spanish Ministerio de Economia y Competitividad [CTM2014-60451-C2-1-P]; Joined Oceanographic Institutions Inc.	US National Science Foundation(National Science Foundation (NSF)); NWO-NNPP; NWO-ALW VENI(Netherlands Organization for Scientific Research (NWO)); IODP priority program of the German Research Foundation (DFG); Spanish Ministerio de Economia y Competitividad(Spanish Government); Joined Oceanographic Institutions Inc.	This research used data and samples from the Integrated Ocean Drilling Program (IODP). IODP was sponsored by the US National Science Foundation and participating countries under management of Joined Oceanographic Institutions Inc. Peter K. Bijl and Francesca Sangiorgi thank NWO-NNPP grant no. 866.10.110 and NWO-ALW VENI grant no. 863.13.002 for funding and Natasja Welters for technical support. Jorg Pross acknowledges support through the IODP priority program of the German Research Foundation (DFG). Carlota Escutia and Ariadna Salabarnada thank the Spanish Ministerio de Economia y Competitividad for grant CTM2014-60451-C2-1-P. 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Past.	JUL 11	2018	14	7					1015	1033		10.5194/cp-14-1015-2018	http://dx.doi.org/10.5194/cp-14-1015-2018			19	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	GM6RX		Green Submitted, gold			2025-03-11	WOS:000438301300001
J	Quaijtaal, W; Tesseur, S; Donders, TH; Claeys, P; Louwye, S				Quaijtaal, Willemijn; Tesseur, Steven; Donders, Timme H.; Claeys, Philippe; Louwye, Stephen			A revised and improved age model for the middle Miocene part of IODP Site U1318 (Porcupine Basin, offshore southwestern Ireland)	GEOLOGICAL MAGAZINE			English	Article						North Atlantic; isotope stratigraphy; magnetostratigraphy; dinoflagellate cysts; Neogene	GLOBAL SEA-LEVEL; ISOTOPE STRATIGRAPHY; DINOFLAGELLATE CYST; OCEAN CIRCULATION; CARBON ISOTOPES; OXYGEN; SEQUENCES; EVENTS; SLOPE; MOUND	Integrated Ocean Drilling Program Leg 307 Site U1318 is one of the few relatively complete middle Miocene drillcores from the North Atlantic (Porcupine Basin, offshore southwestern Ireland). Using benthic foraminiferal stable carbon and oxygen isotopes, the existing age model for Site U1318 was improved. The stable isotope record displays globally recognized isotope events, used to revise the existing magnetostratigraphy-based age model. Two intervals contained misidentified magnetochrons which were corrected. The sampled interval now has a refined age of 12.75-16.60 Ma with a temporal resolution of c. 29 ka.	[Quaijtaal, Willemijn; Tesseur, Steven; Louwye, Stephen] Univ Ghent, Dept Geol, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium; [Donders, Timme H.] Univ Utrecht, Fac Geosci, Dept Phys Geog, Palaeoecol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands; [Donders, Timme H.] Geol Survey Netherlands, TNO B&O, POB 80015, NL-3508 TA Utrecht, Netherlands; [Claeys, Philippe] Vrije Univ Brussel, Earth Syst Sci, Pl Laan 2, B-1050 Brussels, Belgium	Ghent University; Utrecht University; Netherlands Organization Applied Science Research; Vrije Universiteit Brussel	Quaijtaal, W (通讯作者)，Univ Ghent, Dept Geol, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	willemijn.quaijtaal@ugent.be	Quaijtaal, Willemijn/HNB-5108-2023; Donders, Timme/J-5044-2012; Louwye, Stephen/D-3856-2012; Claeys, Philippe/B-4895-2008	Quaijtaal, Willemijn/0000-0001-6016-0194; Donders, Timme/0000-0003-4698-3463; Louwye, Stephen/0000-0003-4814-4313; Claeys, Philippe/0000-0002-4585-7687	Research Foundation-Flanders (FWO) [G.0179.11N]	Research Foundation-Flanders (FWO)(FWO)	The data used for this study can be found in online Supplementary Table S1 (available at http://journals.cambridge.org/geo). The samples for this study were provided by the Integrated Ocean Drilling Program. This work was supported by the Research Foundation-Flanders (FWO) under project number G.0179.11N. Ph.C. thanks the Hercules Foundation Flanders for support of the Stable Isotope facility. The advice of Dr An Holbourn on Miocene stable oxygen isotopes was very valuable for the improvement of the age model. Niels de Winter is thanked for his support during the isotopic measurements in Brussels. Walter Hale and Alex Wulbers kindly supported W.Q. and S.L. during sampling at the Bremen Core Repository. The authors thank Dirk Munsterman and one anonymous reviewer for their useful comments, which have improved the manuscript.	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Mag.	JUL	2018	155	5					1105	1116		10.1017/S0016756816001278	http://dx.doi.org/10.1017/S0016756816001278			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GI5PE		Green Submitted			2025-03-11	WOS:000434422300006
J	Jiang, HS; Kulis, DM; Brosnahan, ML; Anderson, DM				Jiang, Houshuo; Kulis, David M.; Brosnahan, Michael L.; Anderson, Donald M.			Behavioral and mechanistic characteristics of the predator-prey interaction between the dinoflagellate <i>Dinophysis acuminata</i> and the ciliate <i>Mesodinium rubrum</i>	HARMFUL ALGAE			English	Article						Dinophysis acuminate; Mesodinium rubrum; Predator-prey interaction behavior; High-speed microscale imaging system (HSMIS); Quantitative microvideography; Diarrhetic shellfish poisoning (DSP)	THIN-LAYERS; CAPTURE; CULTURE; TOXINS; BLOOM; FATE; SPP.	Predator-prey interactions of planktonic protists are fundamental to plankton dynamics and include prey selection, detection, and capture as well as predator detection and avoidance. Propulsive, morphology-specific behaviors modulate these interactions and therefore bloom dynamics. Here, interactions between the mixo-trophic, harmful algal bloom (HAB) dinoflagellate Dinophysis acuminata and its ciliate prey Mesodinium rubrwn were investigated through quantitative microvideography using a high-speed microscale imaging system (HSMIS). The dinoflagellate D. acuminate is shown to detect its M. rubrwn prey via chemoreception while M. rubrum is alerted to D. acurninata via mechanoreception at much shorter distances (89 +/- 39 mu m versus 41 +/- 32 mu m). On detection, D. acuminata approaches M. rubrum with reduced speed. The ciliate M. rubrum responds through escape jumps that are long enough to detach its chemical trail from its surface, thereby disorienting the predator. To prevail, D. acuminata uses capture filaments and/or releases mucus to slow and eventually immobilize M. rubrum cells for easier capture. Mechanistically, results support the notion that the desmokont flagellar arrangement of D. acuminata lends itself to phagotrophy. In particular, the longitudinal flagellum plays a dominant role in generating thrust for the cell to swim forward, while at other times, it beats to supply a tethering or anchoring force to aid the generation of a posteriorly-directed, cone-shaped scanning current by the transverse flagellum. The latter is strategically positioned to generate flow for enhanced chemoreception and hydrodynamic camouflage, such that D. acuminata can detect and stealthily approach resting M. rubrum cells in the water column.	[Jiang, Houshuo] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA; [Kulis, David M.; Brosnahan, Michael L.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution	Jiang, HS (通讯作者)，Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA.	hsjiang@whoi.edu		Brosnahan, Michael/0000-0002-2620-7638	National Science Foundation (NSF) [OCE-1559062]; Woods Hole Oceanographic Institution; NSF [OCE-1433979, OCE-1129496]; National Science Foundation [OCE-0850421, 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 Science Foundation (NSF)(National Science Foundation (NSF)); Woods Hole Oceanographic Institution; NSF(National Science Foundation (NSF)); National Science Foundation(National Science Foundation (NSF)); National Institutes of Health through the Woods Hole Center for Oceans and Human Health	This work was financially supported by National Science Foundation (NSF) grant OCE-1559062 and a Woods Hole Oceanographic Institution - 2014 Interdisciplinary Study Award. H.J. was also supported by NSF grants OCE-1433979 and OCE-1129496. D.M.A. and M.L.B. were also supported by National Science Foundation (Grants OCE-0850421, 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. The authors gratefully acknowledge these funding sources. Many thanks are extended to Satoshi Nagai for generously providing the M. rubrum and T. amphioxeia cultures used in this study. 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J	Qiu, JB; Meng, FP; Ding, L; Che, YJ; McCarron, P; Beach, DG; Li, AF				Qiu, Jiangbing; Meng, Fanping; Ding, Ling; Che, Yijia; McCarron, Pearse; Beach, Daniel G.; Li, Aifeng			Dynamics of paralytic shellfish toxins and their metabolites during timecourse exposure of scallops <i>Chlamys farreri</i> and mussels <i>Mytilus galloprovincialis</i> to <i>Alexandrium pacificum</i>	AQUATIC TOXICOLOGY			English	Article						Paralytic shellfish toxins; Metabolites; Chlamys farreri; Mytilus galloprovincialis; Alexandrium pacificum; Alexandrium tamarense	ACID ESTER METABOLITES; POISONING TOXINS; GYMNODINIUM-CATENATUM; DETOXIFICATION KINETICS; PATINOPECTEN-YESSOENSIS; SAXITOXIN ANALOGS; MASS-SPECTROMETRY; TRANSFORMATION; DEPURATION; ACCUMULATION	New C-11 hydroxyl metabolites of paralytic shellfish toxins (PSTs) have been reported in shellfish. To gain further information on these metabolites, as well as the potential for formation of phase-II metabolites and acyl esters of PSTs, bivalves were fed with the PSTs-producing dinoflagellate Alexandrium pacificum (strain ATHK). Through independent experiments, scallops (Chlamys farreri) were fed for 9 days and mussels (Mytilus galloprovincialis) for 5 days plus an additional 5 days of depuration, with representative samples taken throughout. Several common PSTs (C1-4, GTX1-6 and NEO) and metabolites including Ml, M3, M5, M7, M9, M2 and M8 were detected in the hepatopancreas of scallops during toxin accumulation and in the hepatopancreas of mussels during both toxin accumulation and elimination periods. The relative molar ratio of metabolites to precursor molecules was used to estimate relative metabolic conversion rates. Conversion rates of C1/2 and GTX2/3 were higher than those of C3/4 and GTX1/4, in scallops and mussels. The first metabolites observed in both bivalve species investigated were M1/3, which are formed from C1/2. However, the conversion of GTX2/3 to M2 was more complete than other biotransformation reactions in both mussels and scallops. In general, metabolic conversion of PSTs was observed after a shorter time and to a greater extent in mussels than in scallops in the exposure period. No acyl esters or conjugation products of PSTs with glucuronic acid, glutathione, cysteine and taurine were detected by liquid chromatography with high resolution tandem mass spectrometry in the samples investigated. Additionally, only GTX1/4 and GTX2/3 were detected in the kidney of scallops, which demonstrates that PSTs are mainly metabolized through the hepatic metabolism pathway in bivalves. This work improves the understanding of PST metabolism during toxin accumulation and depuration in commercially harvested shellfish.	[Qiu, Jiangbing; Meng, Fanping; Ding, Ling; Che, Yijia; Li, Aifeng] Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Peoples R China; [Meng, Fanping; Li, Aifeng] Ocean Univ China, Key Lab Marine Environm & Ecol, Minist Educ, Qingdao 266100, Peoples R China; [McCarron, Pearse; Beach, Daniel G.] Natl Res Council Canada, Measurement Sci & Stand, 1411 Oxford St, Halifax, NS B3H 3Z1, Canada	Ocean University of China; Ocean University of China; National Research Council Canada; International Business Machines (IBM); IBM Canada	Li, AF (通讯作者)，Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Peoples R China.	lafouc@ouc.edu.cn	Li, Aifeng/AFZ-2242-2022; Qiu, Jiangbing/M-4390-2019; Beach, Daniel/A-8286-2013; Qiu, Jiangbing/J-4852-2018	Beach, Daniel/0000-0002-5680-2112; Qiu, Jiangbing/0000-0002-0973-1809	National Natural Science Foundation of China [41376122]; State Scholarship Fund by the China Scholarship Council [201606330051]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); State Scholarship Fund by the China Scholarship Council	This work was funded by the National Natural Science Foundation of China (41376122) and supported by the State Scholarship Fund by the China Scholarship Council (201606330051). 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Toxicol.	JUL	2018	200						233	240		10.1016/j.aquatox.2018.05.003	http://dx.doi.org/10.1016/j.aquatox.2018.05.003			8	Marine & Freshwater Biology; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Toxicology	GM5ME	29778932				2025-03-11	WOS:000438180700024
J	Price, AM; Baustian, MM; Turner, RE; Rabalais, NN; Chmura, GL				Price, Andrea M.; Baustian, Melissa M.; Turner, R. Eugene; Rabalais, Nancy N.; Chmura, Gail L.			Dinoflagellate Cysts Track Eutrophication in the Northern Gulf of Mexico	ESTUARIES AND COASTS			English	Article						Sediments; Nutrients; Mississippi River; Atchafalaya River; Plankton; Hypoxia; Dead zone	LOUISIANA CONTINENTAL-SHELF; MISSISSIPPI RIVER; COASTAL WATERS; SEDIMENTARY RECORD; ECOLOGICAL ROLES; TOKYO-BAY; HYPOXIA; ASSEMBLAGES; INDICATORS; MICROPHYTOBENTHOS	We examined organic-walled dinoflagellate cysts from one Pb-210-dated sediment core and 39 surface sediment samples from the northern Gulf of Mexico to determine the relationship between nutrient enrichment and cyst assemblages in this region characterized by oxygen deficiency. The core spans from 1962 to 1997 and its sampling location is directly influenced by the Mississippi River plume. Surface sediments were collected in 2006, 2007, 2008, and 2014 and represent approximately 1 to 4 years of accumulation. A total of 57 cyst taxa were recorded, and four heterotrophic taxa in particular were found to increase in the top section (1986-1997) of the core-Brigantedinium spp., cysts of Archaeperidinium minutum, cysts of Polykrikos kofoidii, and Quinquecuspis concreta. These taxa show a similar increasing trend with variations in US fertilizer consumption and Mississippi River nitrate concentrations, both of which increased substantially in the 1970s and 1980s. The same four heterotrophic taxa dominated dinoflagellate cyst assemblages collected near the Mississippi River Bird's Foot Delta where nutrient concentrations were higher, especially in 2014. We propose that these cyst taxa can be used as indicators of eutrophication in the Gulf of Mexico. A canonical correspondence analysis (CCA) supports this proposition. The CCA identified sea-surface nutrient concentrations, sea-surface temperature, and sea-surface salinity as the most important factors influencing the cyst assemblages. In addition, cysts produced by the potentially toxic dinoflagellates Pyrodinium bahamense and Lingulodinium polyedrum were documented, but did not appear to have increased over the past 50 years.	[Price, Andrea M.; Chmura, Gail L.] McGill Univ, Dept Geog, Burnside Hall Bldg,805 Sherbrooke St West, Montreal, PQ H3A 0B9, Canada; [Price, Andrea M.; Turner, R. Eugene; Rabalais, Nancy N.] Louisiana State Univ, Dept Oceanog & Coastal Sci, 1002 Q Energy,Coast & Environm Bldg, Baton Rouge, LA 70803 USA; [Baustian, Melissa M.] Water Inst Gulf, One Amer Pl,301 N Main St,Suite 2000, Baton Rouge, LA 70825 USA; [Rabalais, Nancy N.] Louisiana Univ Marine Consortium, 8124 Highway 56, Chauvin, LA 70344 USA	Louisiana State University System; Louisiana State University	Price, AM (通讯作者)，McGill Univ, Dept Geog, Burnside Hall Bldg,805 Sherbrooke St West, Montreal, PQ H3A 0B9, Canada.; Price, AM (通讯作者)，Louisiana State Univ, Dept Oceanog & Coastal Sci, 1002 Q Energy,Coast & Environm Bldg, Baton Rouge, LA 70803 USA.	andrea.price@mail.mcgill.ca	Baustian, Melissa/ITT-2982-2023; Chmura, Gail/LNI-4648-2024; Rabalais, Nancy/GQA-6087-2022	Rabalais, Nancy N./0000-0002-1514-837X; Chmura, Gail/0000-0001-7163-3903	Natural Science and Engineering Research Council of Canada (NSERC) [CGS-D3]; Geological Society of America research; McGill's work study program; National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research [NA06OP0528, NA09NOS4780204, NA06OP0529, NA09NOS4780230, NGOMEX06]	Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Geological Society of America research; McGill's work study program; National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research(National Oceanic Atmospheric Admin (NOAA) - USA)	The Natural Science and Engineering Research Council of Canada (NSERC) is acknowledged for providing partial funding via a graduate scholarship (CGS- D3) to AMP and a Discovery Grant to GLC. This work was supported by a Geological Society of America research grant awarded to AMP. We thank Zingyi Zhang and Wonjun Cho for their lab assistance and McGill's work study program that funded them, Wendy Morrison (LUMCON) for her assistance at LUMCON, Charles Milan (Louisiana State University) for his role in dating the sediment core, and Vera Pospelova (University of Victoria), Raja Sengupta (McGill University), and Suzanne Leroy (Brunel University) for their comments on an earlier draft of this manuscript. Support for ship time was provided by the National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research, under awards NA06OP0528 and NA09NOS4780204 to Louisiana Universities Marine Consortium, awards NA06OP0529 and NA09NOS4780230 to Louisiana State University, and NGOMEX06 funding to NNR and RET. The crew of the R/V Pelican is thanked for assistance with sample collection. 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J	Quattrocchio, ME; Olivera, DE; Martínez, MA; Ponce, JJ; Carmona, NB				Quattrocchio, Mirta E.; Olivera, Daniela E.; Martinez, Marcelo A.; Ponce, Juan J.; Carmona, Noelia B.			Palynofacies associated to hyperpycnite deposits of the Miocene, Cabo Viamonte Beds, Austral Basin, Argentina	FACIES			English	Article						Hyperpycnites; Palynofacies; Miocene; Cabo Viamonte Beds; Austral Basin; Argentina	FUEGIAN ANDES; ORGANIC-MATTER; SE FRANCE; STRATIGRAPHY; RIVER; TURBIDITES; INITIATION; SYSTEMS; EVENTS	The Miocene deposits in the Punta Basilica locality, southernmost Argentina, are included within the Cabo Viamonte Beds, Cabo Domingo Group, in the Austral foreland basin of Tierra del Fuego province. The prograding clinoform systems were accumulated during a weak compressional tectonic regime that allowed the development of a narrow shelf. Paleoenvironmental reconstructions suggest that these clinoforms comprise two dominant architectural elements, channel-levee and lobe complexes, formed mainly by density hyperpycnal currents in outer shelf to depositional slope environments. The transitional and recurrent (vertical and lateral) alternation between sedimentary structures without rheologic boundaries associated with the co-occurrence of plant remains (Nothofagus) are diagnostic criteria for the recognition of hyperpycnites. This type of density flow typically transports large volumes of sediment and organic matter from proximal to deep-marine settings. Four palynofacies types were recognized in a cluster analysis. In general, the palynofacies show predominance of spores and pollen grains, tissues, cuticles, and spongy to fibrous amorphous organic matter (plant and/or freshwater to brackish algae derived), which reflect different positions within the depositional system (e.g., levee-channel and lobe deposits). The co-occurrence of inshore (Batiacasphaera spp., Lingulodinium sp.) with relatively more oceanic (Operculodinium centrocarpum, Spiniferites spp.) dinoflagellates is a strong indication that shallow-water assemblages have been displaced into deep-water settings. Due to the presence of Lingulodinium hemicystum (first appearance data: 23.0 Ma.) and Pentadinium laticinctum (last appearance data: 11.6 Ma.) an age not older than Miocene and not younger than the Serravallian/Tortorian boundary for the Punta Basilica section is proposed.	[Quattrocchio, Mirta E.; Olivera, Daniela E.; Martinez, Marcelo A.] UNS, CONICET, Inst Geol Sur, Dept Geol, San Juan 670,B8000ICN, Buenos Aires, DF, Argentina; [Quattrocchio, Mirta E.; Olivera, Daniela E.; Martinez, Marcelo A.] Univ Nacl Sur, Dept Geol, San Juan 670,B8000ICN, Buenos Aires, DF, Argentina; [Ponce, Juan J.; Carmona, Noelia B.] Univ Nacl Rio Negro, CONICET, Inst Invest Paleobiol & Geol, RA-8332 Gen 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)	Martínez, MA (通讯作者)，UNS, CONICET, Inst Geol Sur, Dept Geol, San Juan 670,B8000ICN, Buenos Aires, DF, Argentina.; Martínez, MA (通讯作者)，Univ Nacl Sur, Dept Geol, San Juan 670,B8000ICN, Buenos Aires, DF, Argentina.	mquattro@criba.edu.ar; daniela.olivera@uns.edu.ar; martinez@criba.edu.ar; jponce@unrn.edu.ar; ncarmona@unrn.edu.ar		Martinez, Marcelo/0000-0003-0538-4739	Consejo Nacional de Investigaciones Cientificas y Tecnicas following Research Project [PIP 417]; Agencia Nacional de Promocion Cientifica y Tecnologica [PICT 2011-1373]; Agencia Nacional de Promocion Cientifica y Tecnologica-Universidad Nacional de Rio Negro [PICTO-UNRN 2010-0199]; Secretaria General de Ciencia y Tecnologia de la Universidad Nacional del Sur [PGI-24/H142]	Consejo Nacional de Investigaciones Cientificas y Tecnicas following Research Project; Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); Agencia Nacional de Promocion Cientifica y Tecnologica-Universidad Nacional de Rio Negro; Secretaria General de Ciencia y Tecnologia de la Universidad Nacional del Sur	We thank S. Candel, F. Ponce and M. Espie for their assistance during field work. The authors kindly acknowledge the reviews of Hartmut Jager and George R. Dix and the comments of Editor-in-Chief Axel Munnecke, which improved the final version of the manuscript. Financial support was provided by Consejo Nacional de Investigaciones Cientificas y Tecnicas following Research Project: (PIP 417); Agencia Nacional de Promocion Cientifica y Tecnologica (PICT 2011-1373); Agencia Nacional de Promocion Cientifica y Tecnologica-Universidad Nacional de Rio Negro (PICTO-UNRN 2010-0199) and Secretaria General de Ciencia y Tecnologia de la Universidad Nacional del Sur (PGI-24/H142).	Barreda V., 2014, Paleobotany and Biogeography: A Festschrift for Alan Graham in His 80th Year, P1; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1983, PETROLEUM GEOCHEMIST, P275; Biddle K., 1986, Assoc. 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J	Schneider, AC; Heimhofer, U; Heunisch, C; Mutterlose, J				Schneider, Anton Christoph; Heimhofer, Ulrich; Heunisch, Carmen; Mutterlose, Joerg			The Jurassic-Cretaceous boundary interval in non-marine strata of northwest Europe - New light on an old problem	CRETACEOUS RESEARCH			English	Article						Lower Cretaceous; Dinoflagellates; Palynology; Ostracods; Correlations	PURBECK; TETHYAN; BIOSTRATIGRAPHY; WEALDEN; TRANSITION; SEDIMENTS; PATTERNS; NORTHERN; PORTLAND; DORSET	The non-marine Purbeck- and Wealden-type sediments of latest Jurassic (Tithonian) and earliest Cretaceous (Berriasian) age in northern Germany were deposited in a restricted intercontinental basin. They mark an interval of strong faunal and floral provincialism which makes correlation of the non marine strata across northwest Europe difficult. The position of the Jurassic-Cretaceous boundary has therefore been debated for decades. Our integrated stratigraphy of four sections in northern Germany, based on palynology (spores, pollen, dinoflagellate cysts) and ostracods, provides new evidence for a precise correlation with contemporaneous strata of other non-marine basins in northwest Europe. Correlation with the marine Boreal Realm and the Tethys is achieved via the Purbeck type section in England. A stratigraphic subdivision of the non-marine Berriasian succession in Germany is possible by using seven short-lived marine flooding events, which are documented by ceratioid dinoflagellate cysts and foraminifera. Our data suggest that a first major transgression took place close to the base of the Boreal Surites stenomphalus ammonite Zone. This level corresponds to a contemporaneous flooding event in southern England (Scallop Beds, Purbeck Group) and in southern Sweden (Annero Formation), thereby providing an excellent marker horizon for interbasinal correlation. (C) 2017 Elsevier Ltd. All rights reserved.	[Schneider, Anton Christoph; Mutterlose, Joerg] Ruhr Univ Bochum, Inst Geol Mineral & Geophys, Univ Str 150, D-44801 Bochum, Germany; [Heimhofer, Ulrich] Leibniz Univ Hannover, Inst Geol, Callinstr 30, D-30167 Hannover, Germany; [Heunisch, Carmen] LBEG, Stilleweg 2, D-30655 Hannover, Germany	Ruhr University Bochum; Leibniz University Hannover	Schneider, AC (通讯作者)，Ruhr Univ Bochum, Inst Geol Mineral & Geophys, Univ Str 150, D-44801 Bochum, Germany.	christoph.schneider@rub.de	Mutterlose, Joerg/IYJ-0031-2023	Mutterlose, Joerg/0000-0003-3449-4507				Abbink OA, 2001, P YORKS GEOL SOC, V53, P275, DOI 10.1144/pygs.53.4.275; Alberti G., 1961, Palaeontographica, V116, P1; ALLEN P, 1991, CRETACEOUS RES, V12, P511, DOI 10.1016/0195-6671(91)90005-W; Anderson F.W., 1973, Geological J Special Issue, VNo. 5, P101; Anderson F.W., 1985, Journal of Micropalaeontology, V4, P1; Anderson F. 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J	Wiese, F; Zobel, K; Mortimore, RN				Wiese, Frank; Zobel, Kerstin; Mortimore, Rory N.			Intrinsic processes control late Turonian calcareous dinoflagellate cyst assemblages - A case study from the Sussex chalk (England)	CRETACEOUS RESEARCH			English	Article						Oligotrophy; Intermediate disturbance hypotheses; Intrinsic triggering mechanisms; Calcareous dinoflagellate cysts	BOHEMIAN CRETACEOUS BASIN; LOWER SAXONY BASIN; NORTHERN GERMANY; SEQUENCE STRATIGRAPHY; SPECIES-DIVERSITY; SEDIMENT RESUSPENSION; OLIGOTROPHIC WATERS; CARBON ISOTOPES; ATLANTIC-OCEAN; NW GERMANY	Changes in late Turonian calcareous dinoflagellate cyst assemblages (c. 6400 specimens from 45 samples of the 27 m-thick Bridgewick section; Sussex, southern England) were plotted against four sedimentary sequences to test its response to eurybatic sea level changes. Only seven taxa occur, and Pithonella sphaerica, P. ovalis and P. spiralis dominate the flora (c. 98%). Pithonella cardiiformis, P. discoidea, N. circumperforata and Pirumella sp. are rare. The composition is identical to that of Salzgitter-Salder (NW Germany). The ratio P. sphaerica/P. ovalis (Ps/Po ratio) shows positive peaks during eurybatic sea level lows (max. 1.6) and negative peaks during maximum flooding (min. 0.2). The cumulative c-dinocysts composition, CCC (P. sphaerica, P. ovalis, P. spiralis, others), shows a proportional decrease of P. sphaerica and P. ovalis during eurybatic sea level falls and predominance of P. ovalis during sea level high. The species richness curve shows lowest species numbers in the context of peak transgression. Higher species numbers are associated with lower eurybatic sea levels. In conclusion, the Ps/Po ratio, the CCC and species richness in conjunction aid the recognition of eurybatic sea level changes. Due to the remote position of the working area on the well-oxygenated, drowned Turonian shelf, we exclude variations of external nutrient input, salinity, temperature and oxygen changes as a possible trigger for the observed floral changes. Instead, we suggest that intrinsic mechanisms drive the floral dynamics. In the sense of the intermediate disturbance hypotheses, the progressive increase of P. sphaerica, P. spiralis and other during progressive eurybatic sea level fall is triggered by higher disturbance frequencies (episodic water turbulence, resuspension events, increased internal cycling rate of C-org); vice versa, maximum flooding is characterized by lower disturbance frequencies (decrease of episodic turbulences, less internal cycling) and the progressive predominance of the optimal competitor, which is P. ovalis. The presence of seafloor topography (intra-shelf depressions and swells) could have created downslope currents where parautochthonous assemblages would be expected and could explain the offset of depositional dynamics at the seafloor leading to changes in the floral assemblages. (C) 2017 Elsevier Ltd. All rights reserved.	[Wiese, Frank] Georg August Univ Gottingen, Geosci Ctr Univ, Dept Geobiol, Goldschmidtstr 3, Gottingen, Germany; [Zobel, Kerstin] Siemensstr 26, D-14482 Potsdam, Germany; [Mortimore, Rory N.] ChalkRock Ltd, 32 Prince Edwards Rd, Lewes BN7 1BE, Sussex, England	University of Gottingen	Wiese, F (通讯作者)，Georg August Univ Gottingen, Geosci Ctr Univ, Dept Geobiol, Goldschmidtstr 3, Gottingen, Germany.	fwiese1@gwdg.de		Wiese, Frank/0000-0002-6910-2166	German Research Foundation [DFG Wi 1656/7-1]	German Research Foundation(German Research Foundation (DFG))	Financial support was provided by the German Research Foundation (DFG Wi 1656/7-1). We thank G. 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J	FitzPatrick, MEJ; Forber, DA; Hart, MB				FitzPatrick, Meriel E. J.; Forber, David A.; Hart, Malcolm B.			Dinocyst stratigraphy and palaeoenvironmental interpretation of the Cretaceous/Paleogene boundary at Stevns Klint, Denmark	CRETACEOUS RESEARCH			English	Article						K/Pg boundary; Dinoflagellate cysts; Biostratigraphy; Fiskeler member	TERTIARY BOUNDARY; DINOFLAGELLATE CYSTS; PALEOGENE BOUNDARY; CALCAREOUS NANNOFOSSIL; EL KEF; CRETACEOUS/TERTIARY BOUNDARY; PLANKTONIC FORAMINIFERS; NORTHWEST TUNISIA; STABLE-ISOTOPE; NEW-JERSEY	A re-examination of the uppermost Maastrichtian chalks and an expanded section of the Fish Clay (Fiskeler Member) undertaken at Stevns Klint, Denmark, one of the classic outcrops of the Cretaceous/Paleogene boundary, has identified diverse and abundant dinoflagellate cyst assemblages, which are compared with earlier dinoflagellate cyst (dinocyst) studies. The uppermost part of the white coccolith chalk (Sigerslev Member) of the uppermost Maastrichtian is placed in the Palynodinium grallator Zone. The overlying 'Grey Chalk' (Hojerup Member) represents a shallower-water marine succession that is characterised by a series of dune-like structures. The last common occurrence of P. grallator is within the Hojerup Member, confirming the Danian age for the Fish Clay (Fiskeler Member) and a latest Maastrichtian age for the P grallator Zone. Within the Fiskeler Member, Damassadinium californicum (previously known as Danea californica), a key biostratigraphical marker, is only intermittently present, while the distributions of Senoniasphaera inomata and Xenicodinium reticulatum provide useful biostratigraphic control. The well-preserved dinocysts of the Fiskeler Member are replaced by reduced assemblages in the Cerithium Limestone Member with only pollen grains recorded. (C) 2017 Elsevier Ltd. All rights reserved.	[FitzPatrick, Meriel E. J.; Hart, Malcolm B.] Plymouth Univ, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England; [Forber, David A.] Univ Exeter, Coll Engn Math & Phys Sci, Harrison Bldg,Streatham Campus, Exeter EX4 4QF, Devon, England	University of Plymouth; University of Exeter	FitzPatrick, MEJ (通讯作者)，Plymouth Univ, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England.	me.fitzpatrick@plymouth.ac.uk	Hart, Malcolm/KMD-8444-2024					ABILDGAARD S, 1759, BESKRIVELSE STEVNS K; ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; [Anonymous], 1847, B SOC GEOLOGIQUE FRA; Aydin T, 2013, THESIS; Batten D.J., 1999, FOSSIL PLANTS SPORES, P15; Beiranvand B, 2014, CR PALEVOL, V13, P235, DOI 10.1016/j.crpv.2013.10.003; Bernecker M, 2005, ERLANGEN EARTH C SER, P3, DOI 10.1007/3-540-27673-4_1; Bernecker M., 1990, Facies, V22, P103, DOI 10.1007/BF02536947; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; BRINKHUIS H, 1988, REV PALAEOBOT PALYNO, V56, P5, DOI 10.1016/0034-6667(88)90071-1; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Bromley R.G., 1979, CRETACEOUS TERTIARY, P16; Christensen LE., 1973, GEOLOGICAL SOC DENMA, V22, P193; DAMASSA S P, 1988, Palynology, V12, P167; Damholt T., 2012, NOMINATION STEVNS KL; DECONINCK J, 1982, GEOL MIJNBOUW, V61, P173; Donze P, 1997, CR ACAD SCI II A, V325, P961, DOI 10.1016/S1251-8050(97)82376-2; Fensome R.A., 2008, DINOFLAJ2, Version 1; FIRTH J V, 1987, Palynology, V11, P199; FIRTH JV, 1993, REV PALAEOBOT PALYNO, V79, P179, DOI 10.1016/0034-6667(93)90022-M; Fitzpatrick M.E, 1992, THESIS; Gedl P, 2004, GEOL SOC SPEC PUBL, V230, P257, DOI 10.1144/GSL.SP.2004.230.01.13; Gravesen Palle, 2001, Geologisk Tidsskrift, V2, P1; HABIB D, 1992, GEOLOGY, V20, P165, DOI 10.1130/0091-7613(1992)020<0165:DACNRT>2.3.CO;2; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; Hansen J.M., 1979, P136; Harland R., 1973, PALEONTOL, V16, P665; Hart M.B., 2014, Trans. 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J	Gussone, N; Friedrich, O				Gussone, Nikolaus; Friedrich, Oliver			Cretaceous calcareous dinoflagellate cysts as recorder of δ<SUP>44/40</SUP>Ca<sub>seawater</sub> and paleo-temperature using Sr/Ca thermometry	CHEMICAL GEOLOGY			English	Article						Sr/Ca; Mg/Ca; delta Ca-44/40; Calcareous dinoflagellates; Cretaceous; Campanian; Maastrichtian; Temperature proxy; Pirumella krasheninnikovii; Orthopithonella globosa; Nuttallides truempyi; Archaeoglobigerina australis	CALCIUM-ISOTOPE FRACTIONATION; THORACOSPHAERA-HEIMII DINOPHYCEAE; SEAWATER CHEMISTRY; CARBONATE; CA; RATIOS; ATLANTIC; FORAMINIFERA; EVOLUTION; PRODUCTIVITY	We evaluate the potential of calcareous dinoflagellates as archives for Sr/Ca-based paleo-temperature reconstructions and delta Ca-44/40(seawater) fluctuations on sediments from Ocean Drilling Program Expedition 113 (Hole 690C, Weddell Sea, Southern Ocean). Between 73 and 68 Ma, Sr/Ca ratios of two Cretaceous dinoflagellate species, Pirumella krasheninnikovii and Orthopithonella globosa show a pronounced decrease, consistent with a significant drop in sea-surface temperature as reflected by the delta O-18 of planktic foraminifers. The apparent temperature sensitivity of the dinoflagellate cysts' Sr/Ca is similar to 0.06 and similar to 0.08 mmol/ mol degrees C-1, using delta O-18-derived paleo sea-surface temperatures, which is significant and large enough to resolve paleoenvironmental temperature changes at current analytical precision. As the chemical composition of the cyst calcite appears to have a good preservation, the Sr/Ca of calcareous dinoflagellates has a potential to serve as paleo-temperature proxy, although the chemical composition of the Cretaceous seawater and potential impacts on the cyst geo-chemistry is pending further inspection. The Ca isotope composition of the two dinoflagellate species shows identical trends of increasing delta Ca-44/ 40 between 73 and 67 Ma. The planktic foraminifer Archaeoglobigerina australis and the benthic foraminifer Nuttallides truempyi reveal the same increase of about 0.parts per thousand but are offset relative to the dinoflagellates by about +0.5 parts per thousand, presumably due to species-specific Ca isotope fractionation. Bulk carbonate sediment shows significant scatter, likely caused by changes in faunal composition and does not reproduce the trend revealed by the dinoflagellate and foraminifer records. These observations demonstrate the importance of taxon-specific records and careful determination of fractionation factors of selected archives and highlight complications arising from utilizing less suitable archives, such as bulk sediments, for delta Ca-44/ 40(seawater) reconstructions. Our records indicate strong changes in the marine Ca cycle associated with the global temperature decrease towards the end of the Cretaceous.	[Gussone, Nikolaus] Westfalische Wilhelms Univ Munster, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany; [Friedrich, Oliver] Heidelberg Univ, Inst Geowissensch, Neuenheimer Feld 234-236, D-69120 Heidelberg, Germany	University of Munster; Ruprecht Karls University Heidelberg	Gussone, N (通讯作者)，Westfalische Wilhelms Univ Munster, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany.	nikolaus.gussone@uni-muenster.de		, Nikolaus/0000-0002-3390-1118	Deutsche Forschungsgemeinschaft (DFG) [GU 1035/2, 1035/3, FR 2544/2]	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	For support in the laboratory, we would like to thank Heidi Bayer, Frank Deipenwisch and Veronika Rapelius. We thank Stephanie Pabich and Mirjam Koch for assistance with sample preparation. We thank three anonymous reviewers for their constructive comments and Michael Bottcher for the editorial handling. This study was supported by the Deutsche Forschungsgemeinschaft (DFG) by grants GU 1035/2 and 1035/3 to NG and grant FR 2544/2 to OF. Microfossil samples and sediments were provided by the Integrated Ocean Drilling Program.	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JUN 5	2018	488						138	148		10.1016/j.chemgeo.2018.04.020	http://dx.doi.org/10.1016/j.chemgeo.2018.04.020			11	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	GG2MY					2025-03-11	WOS:000432528200011
J	Uddandam, PR; Prasad, V; Thakur, B; Manoj, MC				Uddandam, Prem Raj; Prasad, Vandana; Thakur, Biswajeet; Manoj, M. C.			<i>CRISTADINIUM</i> <i>STRIATISERRATUM</i>: A DINOFLAGELLATE CYST FROM THE TROPICAL REGION	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Cristadinium; non tabular striations; parasutural crest; Peridiniaceae; Eastern Arabian Sea	RECENT SEDIMENTS; EAST-COAST; WEST-COAST; ASSEMBLAGES	A new organic-walled dinoflagellate cyst Cristadinium striatiserratum sp. nov., has been reported from the modem sediments of the northern Indian Ocean. C. striatiserratum sp. nov., exhibit paratabulation in the form of parasutural crests that are septate and possess a serrated distal margin. The autophragm is surmounted with non tabular striations, and the archeopyle occupies a mid-dorsal anterior intercalary position (Type 2a). Similar forms have been reported earlier under different generic names viz. Selenopemphix (Benedeck, 1972), Lejeunecysta (Artzner and Dorhofer, 1978), and Protoperidinium (Bergh, 1881) from low latitudes. Taxonomic standardisation of the species that consist crests has been proposed here by describing it under genus Cristadinium that is earlier restricted to the Miocene. The study extends the geological range of the peridinioid species that consist of complete paratabulation from the Neogene to Holocene	[Uddandam, Prem Raj; Prasad, Vandana; Thakur, Biswajeet; Manoj, M. C.] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Uddandam, PR (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	premrajuddandam@gmail.com	Manoj, M/AAR-1882-2020		MoES [MoES/SIBER/NIO(RN)/11]	MoES	The authors are grateful to the Director, Prof. Sunil Bajpai, Birbal Sahni Institute of Palaeosciences for providing the facilities to carry out the present study. Some of the samples utilised in the study are part of MoES funded project entitled "High resolution paleoclimatic studies" No. MoES/SIBER/NIO(RN)/11. Dr. Rajiv Nigam, Dr. Rajeev Saraswat are duly acknowledged for their help. We thank Lucy Edwards for his constructive comments which helped improve this manuscript. This is BSIP contribution No 24-2017-2018.	[Anonymous], PALYNOLOGY; [Anonymous], 1989, P OC DRIL PROGR SCI; D'Silva MS, 2013, MAR POLLUT BULL, V66, P59, DOI 10.1016/j.marpolbul.2012.11.012; D'Silva MS, 2012, J SEA RES, V73, P86, DOI 10.1016/j.seares.2012.06.013; De Verteuil L., 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs, P391; González C, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2008PA001602; Gu HF, 2015, PHYCOLOGIA, V54, P49, DOI 10.2216/14-047.1; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; LENTIN JK, 1994, CAN J EARTH SCI, V31, P567, DOI 10.1139/e94-050; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; Matsuoka K, 2013, MICROPALEAEONTOLOGIC, P275; Mertens KN, 2009, BOREAS, V38, P647, DOI 10.1111/j.1502-3885.2009.00095.x; Narale DD, 2017, MAR POLLUT BULL, V115, P498, DOI 10.1016/j.marpolbul.2016.11.035; Narale DD, 2013, OCEANOLOGIA, V55, P979, DOI 10.5697/oc.55-4.979; Schlitzer R., 2015, OCEAN DATA VIEW; Silva MSD, 2011, INDIAN J GEO-MAR SCI, V40, P697; Su-Myat, 2012, FISHERIES SCI, V78, P1091, DOI 10.1007/s12562-012-0534-0; Uddandam PR, 2017, PALAEOGEOGR PALAEOCL, V483, P31, DOI 10.1016/j.palaeo.2017.01.013; Uddandam P, 2015, J PALAEONTOL SOC IND, V60, P11; Williams G.L., 2017, DATA SERIES, V2; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	21	5	5	0	0	SAGE PUBLICATIONS INDIA  PVT LTD	NEW DELHI	B-1-I-1 MOHAN CO-OPERATIVE INDUSTRIAL AREA, MATHURA RD, POST BAG NO 7, NEW DELHI 110 044, INDIA	0552-9360			J PALAEONTOL SOC IND	J. Palaeontol. Soc. India	JUN	2018	63	1					73	80						8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	GN2OP					2025-03-11	WOS:000438837700005
J	Janssen, R; Doppler, G; Grimm, K; Grimm, M; Haas, U; Hiss, M; Köthe, A; Radtke, G; Reichenbacher, B; Salamon, M; Standke, G; Teipel, U; Thomas, M; Uffenorde, H; Wielandt-Schuster, U				Janssen, Ronald; Doppler, Gerhard; Grimm, Kirsten; Grimm, Matthias; Haas, Ulrich; Hiss, Martin; Koethe, Angelika; Radtke, Gudrun; Reichenbacher, Bettina; Salamon, Martin; Standke, Gerda; Teipel, Ulrich; Thomas, Melanie; Uffenorde, Henning; Wielandt-Schuster, Ulrike		Subkommission Tertiar-	The Tertiary in the Stratigraphic Table of Germany 2016 (STG 2016)	ZEITSCHRIFT DER DEUTSCHEN GESELLSCHAFT FUR GEOWISSENSCHAFTEN			English	Article						Tertiary; geologic time scale; lithostratigraphy; correlation; facies; North Sea Basin; Rhine Graben System; Molasse Basin; Alps	ALPINE FORELAND BASIN; UPPER MARINE MOLASSE; UPPER RHINE GRABEN; NORTH-SEA BASIN; CENTRAL PARATETHYS; LOWER-MIOCENE; EASTERN ALPS; CALCAREOUS NANNOPLANKTON; DINOFLAGELLATE CYSTS; MIDDLE MIOCENE	The regional and stratigraphic subdivision of the Tertiary as part of the Stratigraphic Table of Germany 2016 (STD 2016) is summarised. Primarily, changes compared to STD 2002 are commented. Concerning more detailed explanations, the reader is referred to the respective literature and corresponding definitions in LithoLex (https://litholex.bgr.de). The STD 2016 has not only practical significance, but is also a working basis for (1) the further development of the stratigraphic terminology of the German Tertiary, (2) the correlations of regional units and (3) an improved correlation of the regional stages of the North Sea Basin and the Central Paratethys with the Global Stratigraphic Scale.	[Janssen, Ronald] Senckenberg Forschungsinst & Nat Museum, Senckenberganlage 25, D-60325 Frankfurt, Germany; [Doppler, Gerhard; Haas, Ulrich; Teipel, Ulrich] Bayer Landesamt Umwelt, Geol Dienst, Bgm Ulrich Str 160, D-86179 Augsburg, Germany; [Grimm, Kirsten] Nat Hist Museum, Landessammlung Nat Kunde Rheinland Pfalz, Reichklarastr 10, D-55116 Mainz, Germany; [Grimm, Matthias] Eduard Frank Str 12, D-55122 Mainz, Germany; [Hiss, Martin; Salamon, Martin] Geol Dienst Nordrhein Westfalen, De Greiff Str 195, D-47803 Krefeld, Germany; [Koethe, Angelika] Bundesanstalt Geowissensch & Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany; [Radtke, Gudrun] Hess Landesamt Nat Schutz Umwelt & Geol, Rheingaustr 186, D-65203 Wiesbaden, Germany; [Reichenbacher, Bettina] Ludwig Maximilians Univ Munchen, Dept Geo & Umweltwissensch Palaontol & Geobiol, Richard Wagner Str 10, D-80333 Munich, Germany; [Standke, Gerda] Johann Sebastian Bach Str 2, D-09599 Freiberg, Germany; [Thomas, Melanie] Landesamt Bergbau Energie & Geol, Stilleweg 2, D-30655 Hannover, Germany; [Uffenorde, Henning] Univ Gottingen, Geowissensch Zentrum, Goldschmidt Str 3, D-37077 Gottingen, Germany; [Wielandt-Schuster, Ulrike] Regierungsprasidium Freiburg, Landesamt Geol Rohstoffe & Bergbau, Albertstr 5, D-79104 Freiburg, Germany	Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); University of Munich; University of Gottingen	Janssen, R (通讯作者)，Senckenberg Forschungsinst & Nat Museum, Senckenberganlage 25, D-60325 Frankfurt, Germany.	ronald.janssen@senckenberg.de; gerhard.doppler@lfu.bayern.de; kgrimm@uni-mainz.de; UDL.Dr.Grimm@t-online.de; ulrich.haas@lfu.bayern.de; martin.hiss@gd.nrw.de; angelika.koethe@bgr.de; gudrun.radtke@hlnug.hessen.de; b.reichenbacher@lrz.uni-muenchen.de; martin.salamon@gd.nrw.de; gbstandke@t-online.de; ulrich.teipel@lfu.bayern.de; Melanie.Thomas@lbeg.niedersachsen.de; huffeno@gwdg.de; ulrike.wielandt-schuster@rpf.bwl.de	Reichenbacher, Bettina/AAM-9684-2020					Ahrendt H., 1995, Z DTSCH GEOLOGISCHEN, V146, P450, DOI [DOI 10.1127/ZDGG/146/1995/450, 10.1127/zdgg/146/1995/450]; Anderle H.-J., 2001, SCHRIFTENR DT GES 1, V75, P344; Anderson H.-J, 1977, Geologica Palaeontologica, V11, P197; Anderson H.-J., 1986, BEITRAGE REGIONALEN, V18, P650; [Anonymous], 1981, 2523408 TGL, P1; [Anonymous], 2012, GEOLOGIC TIME SCALE; [Anonymous], 1996, GEOLOGICAL SOC LONDO, DOI DOI 10.1144/GSL.SP.1996.101.01.02; [Anonymous], 2001, 219193 DIN; [Anonymous], INT J EARTH SCI; Bayerisches Geologisches Landesamt, 2004, GEOBAVARIA 600 MILL; Behrmann JH, 2005, INT J EARTH SCI, V94, P505, DOI 10.1007/s00531-005-0513-0; Benda L., 1990, GEOL JB A, V111, P1; Benedek P. 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J	Prasad, V; Farooqui, A; Murthy, S; Sarate, OS; Bajpai, S				Prasad, Vandana; Farooqui, Anjum; Murthy, Srikanta; Sarate, Omprakash S.; Bajpai, Sunil			Palynological assemblage from the Deccan Volcanic Province, central India: Insights into early history of angiosperms and the terminal Cretaceous paleogeography of peninsular India	CRETACEOUS RESEARCH			English	Article						Cretaceous; Deccan volcanic province; Infratrappean; Paleotropics; Palynology	KRISHNA-GODAVARI BASIN; CHHINDWARA DISTRICT; MADHYA-PRADESH; INTERTRAPPEAN BEDS; TERTIARY BOUNDARY; LAMETA FORMATIONS; MASS EXTINCTION; EARLY PALEOCENE; K/T BOUNDARY; POLLEN	Sedimentary deposits of the Deccan Volcanic Province (DVP), of central India are rich in fossil flora and fauna. Based on a new palynological study of Infratrappean deposits from a borehole succession located in the Ashtona village, Yeotmal District, Maharashtra (Wardha Basin), this paper attempts a reconstruction of the Late Cretaceous paleovegetation, paleoecology, depositional environment and paleogeography of central India prior to Deccan volcanism, and also seeks to evaluate the early history and timing of the angiosperm diversification relative to the Cretaceous-Paleogene (K-Pg) transition. The stratigraphic age of the Infratrappean sequence was determined on the basis of several index palynomorphs (Aquilapollenites, Jigansupollis), Azolla cretacea, Gabonisporis sp, Scollardia conferta of Maastrichtian age. Two new pollen species (Dipterocarpuspollenites cretacea sp. nov., Retiacolpites pigafettaensis sp. nov., and one new dinoflagellate species (Pierceites deccanensis sp. nov.) are described in this study. The numerical abundance of the mangrove pollen Spinizonocolpites pollen (Nypa), combined with the dinoflagellate cyst Pierceites deccanensis, indicates a brackish marine depositional setting close to low-lying coastal forests in central India during the Late Cretaceous. Furthermore, the new evidence presented here from an inland location in the Deccan province strongly suggests the existence of a shallow marine embayment in central India during the late Maastrichtian, which extended from the east coast through the Godavari rift zone, thus adding significantly to the previously described marine signatures from the Upper Cretaceous sequence of Rajahmundry area on the south-eastern coast of peninsular India. The Late Cretaceous fossil pollen of Dipterocarpaceae documented here provides compelling evidence for the evolution of these tropical rain forest elements in the insular India and their dispersal to south east Asia after the initiation of India-Asia collision, consistent with the Out of India hypothesis. The new palynomorph assemblage also has significant implications for our understanding of the floral response to the initiation of Deccan volcanism. (C) 2018 Elsevier Ltd. All rights reserved.	[Prasad, Vandana; Farooqui, Anjum; Murthy, Srikanta; Sarate, Omprakash S.; Bajpai, Sunil] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India; [Bajpai, Sunil] Indian Inst Technol Roorkee, Dept Earth Sci, Roorkee 247667, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Roorkee	Prasad, V; Bajpai, S (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.; Bajpai, S (通讯作者)，Indian Inst Technol Roorkee, Dept Earth Sci, Roorkee 247667, Uttar Pradesh, India.	prasad.van@gmail.com; sunilbajpai2001@yahoo.corn	Bajpai, Sunil/E-8416-2010					ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; [Anonymous], 1984, S EOV BOT BIOSTR CAL; [Anonymous], 1995, P INT C GLOB ENV DIV; Badve RM, 2003, CURR SCI INDIA, V85, P1407; Badve RM, 1977, Recent Researches in Geology, V4, P388; Barboni D, 2003, J VEG SCI, V14, P551, DOI 10.1111/j.1654-1103.2003.tb02182.x; Barreda VD, 2015, P NATL ACAD SCI USA, V112, P10989, DOI 10.1073/pnas.1423653112; Bhandari A., 1995, Indian Journal of Petroleum Geology, V4, P89; Bhattacharya A., 1966, J GEOL SOC INDIA, V7, P92; BLASCO F, 1975, SCI TECHNIQUE, V14, P1; Boyce CK, 2010, ANN MO BOT GARD, V97, P527, DOI 10.3417/2009143; Chanda S. 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Res.	JUN	2018	86						186	198		10.1016/j.cretres.2018.03.004	http://dx.doi.org/10.1016/j.cretres.2018.03.004			13	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	GE4CA					2025-03-11	WOS:000431160700017
J	Crampton-Flood, ED; Peterse, F; Munsterman, D; Damsté, JSS				Crampton-Flood, Emily Dearing; Peterse, Francien; Munsterman, Dirk; Damste, Jaap S. Sinninghe			Using tetraether lipids archived in North Sea Basin sediments to extract North Western European Pliocene continental air temperatures	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						paleoclimate; brGDGTs; coastal sediments; air temperature; Pliocene	DIALKYL GLYCEROL TETRAETHERS; DINOFLAGELLATE CYST STRATIGRAPHY; TERRESTRIAL ORGANIC-MATTER; BIOME RECONSTRUCTION; ACRITARCH EVENTS; MIDDLE MIOCENE; YENISEI RIVER; PLEISTOCENE; CLIMATE; MARINE	The Pliocene is often regarded as a suitable analogue for future climate, due to an overall warmer climate (2-3 degrees C) coupled with atmospheric CO2 concentrations largely similar to present values (-400 ppmv). Numerous Pliocene sea surface temperature (SST) records are available, however, little is known about climate in the terrestrial realm. Here we generated a Pliocene continental temperature record for Northwestern Europe based on branched glycerol dialkyl glycerol tetraether (brGDGT) membrane lipids stored in a marine sedimentary record from the western Netherlands. The total organic carbon (TOC) content of the sediments and its stable carbon isotopic composition (delta C-13(org)) indicate a strong transition from primarily marine derived organic matter (OM) during the Pliocene, to predominantly terrestrially derived OM after the transition into the Pleistocene. This trend is supported by the ratio of branched and isoprenoid tetraethers (BIT index). The marine-terrestrial transition indicates a likely change in brGDGT sources in the core, which may complicate the applicability of the brGDGT paleotemperature proxy in this setting. Currently, the application of the brGDGT-based paleothermometer on coastal marine sediments has been hampered by a marine overprint. Here, we propose a method to disentangle terrestrial and marine sources based on the degree of cyclization of tetramethylated brGDGTs (#rings) using a linear mixing model based on the global soil calibration set and a newly developed coastal marine temperature transfer function. Application of this method on our brGDGT record resulted in a 'corrected' terrestrial temperature record (MAT(terr)). This latter record indicates that continental temperatures were similar to 12-14 degrees C during the Early Pliocene, and 10.5-12 degrees C during the Mid Pliocene, confirming other Pliocene pollen based terrestrial temperature estimates from Northern and Central Europe. Furthermore, two colder (Delta 5-7 degrees C) periods in the Pliocene MAT(terr) record show that the influence of Pliocene glacials reached well into NW Europe. (C) 2018 The Authors. Published by Elsevier B.V.	[Crampton-Flood, Emily Dearing; Peterse, Francien; Damste, Jaap S. Sinninghe] Univ Utrecht, Fac Geosci, Dept Earth Sci, POB 80-012, NL-3508 TA Utrecht, Netherlands; [Munsterman, Dirk] Geol Survey Netherlands, Netherlands Org Appl Sci Res, Toegepast Nat Wetenschappelijk Onderzoek, POB 80015, NL-3508 TA Utrecht, Netherlands; [Damste, Jaap S. Sinninghe] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Microbiol & Biogeochem, POB 59, NL-1790 AB Den Burg, Texel, Netherlands; [Damste, Jaap S. Sinninghe] Univ Utrecht, POB 59, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; Netherlands Organization Applied Science Research; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Crampton-Flood, ED (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, POB 80-012, NL-3508 TA Utrecht, Netherlands.	e.dearingcramptonflood@uu.nl	Peterse, Francien/AAY-1473-2021; Peterse, Francien/H-5627-2011; Sinninghe Damste, Jaap/F-6128-2011	Peterse, Francien/0000-0001-8781-2826; Sinninghe Damste, Jaap/0000-0002-8683-1854	Netherlands Earth System Science Center (NESSC) from the Dutch Ministry for Education, Culture and Science [NWO 024.002.001]; NWO [834.11.006]	Netherlands Earth System Science Center (NESSC) from the Dutch Ministry for Education, Culture and Science; NWO(Netherlands Organization for Scientific Research (NWO))	We like to thank Dr. Stijn De Schepper and an anonymous reviewer for their comments, which greatly helped to improve this manuscript. The authors thank Natasja Welters and Arnold van Dijk for assistance with TOC and 813Corg analyses, and Denise Dorhout for re -analysis of the Portuguese margin samples. The work was supported by funding from the Netherlands Earth System Science Center (NESSC) through a gravitation grant (NWO 024.002.001) from the Dutch Ministry for Education, Culture and Science to JSSD. NWO grant #834.11.006 enabled the purchase of the UHPLCMS system used for GDGT analyses.	BALDAUF JG, 1987, INITIAL REP DEEP SEA, V94, P1159; Boogaert H.V. A., 1993, Stratigraphic Nomenclature of the Netherlands: Revision and Update by RGD and NOGEPA; Boyer T. 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J	Prasad, V; Utescher, T; Sharma, A; Singh, IB; Garg, R; Gogoi, B; Srivastava, J; Uddandam, PR; Joachimski, MM				Prasad, V.; Utescher, T.; Sharma, A.; Singh, I. B.; Garg, R.; Gogoi, B.; Srivastava, J.; Uddandam, P. R.; Joachimski, M. M.			Low-latitude vegetation and climate dynamics at the Paleocene-Eocene transition - A study based on multiple proxies from the Jathang section in northeastern India	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Paleotropics; PETM; Precipitation; Palynology; Climate change; Rainforest	SOUTH SHILLONG PLATEAU; COEXISTENCE APPROACH; APECTODINIUM ACME; TROPICAL FORESTS; FUTURE CLIMATE; MODERN POLLEN; DIVERSITY; RAIN; SEASONALITY; AMPLIFICATION	We present a multi-proxy study of an upper Paleocene-lower Eocene succession from the paleo-equatorial region. The study is carried out on a coal-bearing, shallow-marine succession exposed at Jathang, east Khasi hills, Meghalaya, northeastern India. The succession was deposited in a low-energy, coastal marsh-bay complex. Dinoflagellate cyst biostratigraphy yields a late Paleocene to early Eocene age for the section. The deposits of the lower part of the succession represent a transgressive systems tract (TST) defined by seven parasequences, each starting with bay sediments deposited during transgression, followed by a shallowing-upward bay fill-marsh deposit. In the vertical succession, each parasequence acquires an increasingly marine character, culminating in a maximum flooding surface at the Paleocene-Eocene boundary. It is followed by four shallowing upward parasequences deposited in a highstand systems tract (HST). Enhanced chemical weathering and high terrestrial supply are testified by raised SiO2 and Al2O3, contents and high percentages of terrestrial palynomorphs. The pollen flora recovered from the Jathang section was used for quantitative paleoclimate and vegetation reconstructions. The Coexistence Approach was applied based on Nearest Living Relatives (NLRB) of sixty fossil species recorded at different stratigraphic levels. Seven climate variables were determined for the fossil assemblages, and, as a measure of the seasonality of climate, the number of dry months was estimated. Our study shows that during the Paleocene there existed warm, seasonally dry tropical climate conditions with mean annual temperature at ca. 24-26 degrees C and mean annual precipitation at ca. 700-1800 mm, and with a dry season of 5-6 months. Particularly warm and wet, perhumid climate conditions with 26-27 degrees C and 2200-3200 mm mean annual precipitation with a dry period of 2-3 months were reconstructed for the latest Paleocene-earliest Eocene interval. The study shows a distinct vegetational turnover from palm-dominated, seasonally dry tropical forest during the Paleocene to highly diversified dicotyledonous megathermal rainforest during the latest Paleocene early Eocene. The present study demonstrates that the reduced duration of the dry period during the latest Paleocene-earliest Eocene, due to a more active hydrological cycle, played a major role in determining the climate and shaping the vegetation cover in the paleo-equatorial region. There is evidence from our data that seasonality of rainfall is the determining factor for the tropical forest vegetation pattern of the equatorial region rather than mean annual rainfall condition. As the main trigger for the observed step-wise changes of the hydrology along the studied succession, the fast northward movement of the Indian Plate is inferred.	[Prasad, V.; Sharma, A.; Garg, R.; Srivastava, J.; Uddandam, P. R.] BirbalSahni Inst Palaeosci, Lucknow 226007, Uttar Pradesh, India; [Utescher, T.] Senckenberg Res Inst, Frankfurt, Germany; [Utescher, T.] Univ Bonn, Steinmann Inst, Nussallee 8, D-53115 Bonn, Germany; [Singh, I. B.] 17-11-2C Metro City Nishat Ganj, Lucknow 226007, Uttar Pradesh, India; [Gogoi, B.] Guwahati Univ, Dept Geol Sci, Gauhati, India; [Joachimski, M. M.] Inst Geol & Mineral, D-91054 Erlangen, Germany	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); University of Bonn; Gauhati University; University of Erlangen Nuremberg	Prasad, V (通讯作者)，BirbalSahni Inst Palaeosci, Lucknow 226007, Uttar Pradesh, India.	prasad.van@gmail.com	Srivastava, Jyoti/AAB-1612-2020; Gogoi, Bikash/AAY-2636-2021; Joachimski, Michael/B-9477-2011	Joachimski, Michael/0000-0001-6088-3261; Srivastava, Jyoti/0000-0002-5264-7995	Indian National Science Academy (Intl/CAS), New Delhi; German Science Foundation [GZ: UT 27/2-1]	Indian National Science Academy (Intl/CAS), New Delhi; German Science Foundation(German Research Foundation (DFG))	VP, AS, JS, RG and PU thank the director of BSIP for providing all necessary facilities and permission to publish the manuscript (BSIP publication No 11, 2015-2016). VP and TU thank the Indian National Science Academy (Intl/CAS/2014), New Delhi, and the German Science Foundation (GZ: UT 27/2-1) for providing financial assistance. We thank our reviewers Dr. Carlos Jaramillo, Professor R. A. Spicer and an anonymous reviewer for their careful revision and helpful comments which greatly helped to improve this manuscript. This study is a contribution to the BSIP project and NECLIME (www.neclime.de). IBS is thankful to INSA Honorary Scientist position.	Allen MR, 2002, NATURE, V419, P224, DOI 10.1038/nature01092; [Anonymous], 2014, PALAEOFLORA DATABASE; [Anonymous], 2008, GENERA PALMARUM; [Anonymous], 2007, CLIMATE CHANGE 2007; [Anonymous], PALAEONTOGR ABT B; [Anonymous], P R SOC; [Anonymous], 1988, Geol. 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Petrol, V6, P119; Wing SL, 2005, SCIENCE, V310, P993, DOI 10.1126/science.1116913; Zachos JC, 2008, NATURE, V451, P279, DOI 10.1038/nature06588	86	23	25	0	41	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	MAY 15	2018	497						139	156		10.1016/j.palaeo.2018.02.013	http://dx.doi.org/10.1016/j.palaeo.2018.02.013			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	GC1CF					2025-03-11	WOS:000429513500012
J	Jung, SW; Kang, D; Kim, HJ; Shin, HH; Park, JS; Park, SY; Lee, TK				Jung, Seung Won; Kang, Donhyug; Kim, Hyun-Jung; Shin, Hyeon Ho; Park, Joon Sang; Park, So Yun; Lee, Taek-Kyun			Mapping distribution of cysts of recent dinoflagellate and <i>Cochlodinium polykrikoides</i> using next-generation sequencing and morphological approaches in South Sea, Korea	SCIENTIFIC REPORTS			English	Article							ENVIRONMENTAL DNA; COASTAL WATERS; DINOPHYCEAE; SCRIPPSIELLA; PHYLOGENY; COMMUNITY; MARGALEF; REVEALS	The total dinoflagellate cyst community and the cysts of Cochlodinium polykrikoides in the surface sediments of South Sea (Tongyeong coast), South Korea, were analysed using next-generation sequencing (NGS) and morphological approaches. Dinoflagellate cysts can be highly abundant (1114,087 cysts g(-1) dry weight) and have diverse species composition. A total of 35 taxa of dinoflagellate cysts representing 16 genera, 21 species (including four unconfirmed species), and 14 complex species were identified by NGS analysis. Cysts of Scrippsiella spp (mostly Scrippsiella trochoidea) were the most dominant and Polykrikos schwartzii, Pentapharsodinium dalei, Ensiculifera carinata, and Alexandrium catenella/tamarense were common. Thus, a combination of NGS and morphological analysis is effective for studying the cyst communities present in a given environment. Although C. polykrikoides developed massive blooms during 2013-2014, microscopy revealed low density of their cysts, whereas no cysts were detected by NGS. However, the vegetative C. polykrikoides not appeared during 2015-2017 in spite of the observation of C. polykrikoides cysts. This suggests that the C. polykrikoides blooms were not due to development of their cysts but to other factors such as currents transporting them to a marine environment suitable for their growth.	[Jung, Seung Won; Kim, Hyun-Jung; Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea; [Kang, Donhyug] Korea Inst Ocean Sci & Technol, Maritime Secur Res Ctr, Busan 49111, South Korea; [Park, Joon Sang] Korea Inst Ocean Sci & Technol, Marine Ecosyst & Biol Res Ctr, Busan 49111, South Korea; [Park, So Yun; Lee, Taek-Kyun] Korea Inst Ocean Sci & Technol, South Sea Environm Res Ctr, Geoje 53201, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST)	Lee, TK (通讯作者)，Korea Inst Ocean Sci & Technol, South Sea Environm Res Ctr, Geoje 53201, South Korea.	diatoms@kiost.ac.kr; tklee@kiost.ac.kr	Lee, Hak/Q-7386-2019	Shin, Hyeon Ho/0000-0002-9711-6717; Kim, Hyun-Jung/0000-0002-7961-9943; Lee, Taek-Kyun/0000-0001-6090-507X	Public Welfare & Safety Research Program through the National Research Foundation of Korea (NRF) - Ministry of Science and ICT of Republic of Korea [NRF-2013M3A2A1067529]; Research Program of Korea Institute of Marine Science & Technology (KIMST) - Ministry of Oceans and Fisheries of Republic of Korea [PM 60650]; Research Program of Korea Institute of Ocean Science and Technology [PE99628]	Public Welfare & Safety Research Program through the National Research Foundation of Korea (NRF) - Ministry of Science and ICT of Republic of Korea(National Research Foundation of Korea); Research Program of Korea Institute of Marine Science & Technology (KIMST) - Ministry of Oceans and Fisheries of Republic of Korea(Korea Institute of Marine Science & Technology Promotion (KIMST)); Research Program of Korea Institute of Ocean Science and Technology	The stored genomic DNA samples and fixed phytoplankton samples were obtained from the Library of Marine Samples, Korea Institute of Ocean Science & Technology, South Korea. This work was supported by the Public Welfare & Safety Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Science and ICT of Republic of Korea (Development of autonomous microalgal identification system and feasibility analyses of developed HAB control technologies: NRF-2013M3A2A1067529), supported by the Research Program of Korea Institute of Marine Science & Technology (KIMST) funded by the Ministry of Oceans and Fisheries of Republic of Korea (Establishment and demonstration of red tide detection and prediction system for minimizing red tide damage: PM 60650), and supported by the Research Program of Korea Institute of Ocean Science and Technology (Development of marine cold water layer-based multi-culture technology for marine biological resources: PE99628).	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J	Abadie, E; Chiantella, C; Crottier, A; Rhodes, L; Masseret, E; Berteaux, T; Laabir, M				Abadie, Eric; Chiantella, Claude; Crottier, Anais; Rhodes, Lesley; Masseret, Estelle; Berteaux, Tom; Laabir, Mohamed			What are the main environmental factors driving the development of the neurotoxic dinoflagellate <i>Vulcanodinium rugosum </i>in a Mediterranean ecosystem (Ingril lagoon, France)?	HARMFUL ALGAE			English	Article						Vulcanodinium rugosum; Neurotoxins; Ingril lagoon; Environmental factors; Development dynamic	OSTREOPSIS CF. OVATA; BIVALVE PINNA-MURICATA; NORTHERN ADRIATIC SEA; HARMFUL ALGAL BLOOMS; ALEXANDRIUM-CATENELLA; THAU LAGOON; TEMPORARY CYSTS; SOUTHERN FRANCE; COASTAL WATERS; NEW-ZEALAND	Vulcanodinium rugosum, a dinofiagellate developing in Ingril Lagoon (Mediterranean, France) is responsible for shellfish intoxications due to the neurotoxin pinnatoxin G. A one year survey (March 2012-April 2013) was conducted in this oligotrophic shallow lagoon and key environmental parameters were recorded (temperature, salinity and nutrients). The spatio-temporal distribution of V. rugosum in water column and on macrophytes was also determined. Planktonic cells of V. rugosum were observed at all sampling stations, but in relatively low concentrations (maximum of 1000 cell/L). The highest abundances were observed from June to September 2012. There was a positive correlation between cell densities and both temperature and salinity. Non-motile cells were detected on macrophytes, with a maximum concentration of 6300 cells/g wet weight. Nitrite and ammonium were negatively related to V. rugosum abundance whereas total nitrogen, total phosphorus and phosphates showed a positive correlation. Altogether, in situ results suggest that V. rugosum is rather thermophilic and that organic nutrients should be considered when studying the nutrition requirements for this noxious expanding dinoflagellate. (C) 2018 Elsevier B.V. All rights reserved.	[Abadie, Eric; Chiantella, Claude; Crottier, Anais; Berteaux, Tom] Univ Montpellier, IFREMER, Lab Environm Ressources Languedoc Roussillon,IRD, Ctr Marine Biodivers Exploitat & Conservat MARBEC, CS30171, Sete 03, France; [Rhodes, Lesley] Cawthron Inst, 98 Halifax St East,Private Bag 2, Nelson 7042, New Zealand; [Masseret, Estelle; Laabir, Mohamed] Univ Montpellier, Ctr Marine Biodivers Exploitat & Conservat MARBEC, CNRS, IRD,Ifremer, Pl E Bataillon,CC93, F-34095 Montpellier 5, France	Universite de Montpellier; Ifremer; Institut de Recherche pour le Developpement (IRD); Cawthron Institute; Universite de Montpellier; Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); Ifremer	Abadie, E (通讯作者)，Univ Montpellier, IFREMER, Lab Environm Ressources Languedoc Roussillon,IRD, Ctr Marine Biodivers Exploitat & Conservat MARBEC, CS30171, Sete 03, France.	Eric.abadie@ifremen.fr		ABADIE, Eric/0000-0001-9431-2010	TOTAL Foundation; Agence de l'Eau Rhone Mediterranee Corse (AERMC the Rhone-Mediterranean); Agence de l'Eau Rhone Mediterranee Corse (Corsica Water Agency); IRD (Institut National pour la Recherche et le Developpement National Institute for Research and Development)	TOTAL Foundation(Total SA); Agence de l'Eau Rhone Mediterranee Corse (AERMC the Rhone-Mediterranean); Agence de l'Eau Rhone Mediterranee Corse (Corsica Water Agency); IRD (Institut National pour la Recherche et le Developpement National Institute for Research and Development)	This work was backed by the LAGUNOTOX project funded by TOTAL Foundation. We would also to thank the Agence de l'Eau Rhone Mediterranee Corse (AERMC the Rhone-Mediterranean and Corsica Water Agency) for their financial help. 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J	Duque-Herrera, AF; Helenes, J; Pardo-Trujillo, A; Flores-Villarejo, JA; Sierro-Sáncheza, FJ				Duque-Herrera, Andres-Felipe; Helenes, Javier; Pardo-Trujillo, Andres; Flores-Villarejo, Jose-Abel; Sierro-Sancheza, Francisco-Javier			Miocene biostratigraphy and paleoecology from dinoflagellates, benthic foraminifera and calcareous nannofossils on the Colombian Pacific coast	MARINE MICROPALEONTOLOGY			English	Article						Biostratigraphy; Paleoecology; Dinoflagellates; Calcareous microfossils; Miocene; Western Colombia	NORTHWESTERN SOUTH-AMERICA; MIDDLE MIOCENE; SURFACE SEDIMENTS; STRATIGRAPHY; BASIN; PRODUCTIVITY; EVOLUTION; SEAWAY; PANAMA; CYSTS	We present dinoflagellate assemblages contained in samples from the exploratory well Buenaventura 1-ST-P, located on the Colombian Pacific coast. The biostratigraphic model includes data from calcareous nannofossils and dinoflagellates studied from the same samples. The paleobathymetric evolution for the stratigraphic column is interpreted from its lithology, and content of benthic foraminifera and palynomorphs. We propose a chronostratigraphic framework based on the correlation of the integrated biostratigraphy, and this framework allows identification of regional tectonic and paleoceanographic events in the section studied. Our results indicate that the studied interval was deposited from early to late Miocene times (< 17.9-5.33 Ma). The basal conglomeratic portion of the section was deposited between < 17.9 and 13.4 Ma, and may reflect the collision of the Choco Block with northwestern South America. These conglomerates contain very few dinoflagellates, calcareous nannofossils and benthic foraminifera. Overlying these conglomerates, similar to 1500 m of mainly shales, represent three complete transgressive-regressive (T-R) sedimentary cycles with environments ranging from transitional to upper bathyal. Autotrophic gonyaulacoid dinoflagellates dominate the lowest T-R cycle (similar to 14.18 to < 10.9 Ma), indicating warm and stratified superficial waters. The second T-R cycle (< 10.9 to < 9.53 Ma) is characterized by the lowest presence of marine microfossils, indicating low primary productivity. This cycle coincides with the Carbonate Crash event in the eastern tropical Pacific. Finally, the youngest T-R, from < 9.53 to similar to 5.33 Ma, shows an increase in marine microfossils, and a dominance of heterotrophic peridinioid dinoflagellates, which indicate high productivity in cooler superficial waters. This cycle coincides with the late Miocene Global Biogenic Bloom event.	[Duque-Herrera, Andres-Felipe; Helenes, Javier] CICESE, Dept Geol, Fracc Zona Playitas, Baja California, Mexico; [Pardo-Trujillo, Andres] Univ Caldas, Inst Invest Estratig, Manizales, Colombia; [Flores-Villarejo, Jose-Abel; Sierro-Sancheza, Francisco-Javier] Univ Salamanca, Dept Geol, Salamanca, Spain	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; Universidad de Caldas; University of Salamanca	Helenes, J (通讯作者)，Ctr Estudios Cient & Educ Super Ensenada, Dept Geol, Carretera Ensenada Tijuana 3918, Fracc Zona Playitas 22860, Baja California, Mexico.	jhelenes@cicese.mx	Escamilla, Javier/J-5033-2016; Sierro, Francisco/A-4714-2008	Pardo-Trujillo, Andres/0000-0001-9678-6818; Sierro, Francisco/0000-0002-8647-456X	CONACYT - CICESE [300334]	CONACYT - CICESE	Thanks to CONACYT - CICESE, for their financial support to the first author (scholarship number 300334) throughout this study. Also thanks to the Institute de Investigaciones en Estratigrafia (IIES-Universidad de Caldas, Colombia) and Agencia Nacional de Hidrocarburos (ANHColombia), for making available samples and data for the analyses, and for the permission to publish these results.	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Micropaleontol.	MAY	2018	141						42	54		10.1016/j.marmicro.2018.05.002	http://dx.doi.org/10.1016/j.marmicro.2018.05.002			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	GL2AI		hybrid			2025-03-11	WOS:000436915000005
J	Dewaele, L; Lambert, O; Louwye, S				Dewaele, Leonard; Lambert, Olivier; Louwye, Stephen			A critical revision of the fossil record, stratigraphy and diversity of the Neogene seal genus <i>Monotherium</i> (Carnivora, Phocidae)	ROYAL SOCIETY OPEN SCIENCE			English	Article						Phocidae; Monotherium; Neogene; North Atlantic; North Sea Basin	DINOFLAGELLATE CYST STRATIGRAPHY; BASIN NORTHERN BELGIUM; MIDDLE MIOCENE; ACRITARCH EVENTS; MARINE MAMMALS; SOUTHERN; PLIOCENE; PHYLOGENY; EVOLUTION; BIOGEOGRAPHY	Historically, Monotherium had been one of the few genera of extinct Phocidae (true seals) that served as a wastebin taxon. Consequently, it did neither aid in understanding phylogenetic relationships of extinct Phocidae, nor in understanding seal diversity in deep time. This urged the reassessment of the genus. Before our review, Monotherium included five different species: Monotherium aberratum, Monotherium affine, and Monotherium delognii from Belgium; Monotherium gaudini from Italy; and Monotherium? wymani from the east coast USA. In this work we redescribe the fossil record of the genus, retaining the type species M. delognii. Monotherium aberratum and M. affine are reassigned to the new phocine genus Frisiphoca. Monotherium gaudini is renamed and considered a stem-monachine (Noriphoca gaudini). The holotype of the monachine M.? wymani requires further study pending the discovery of new fossil material that could be attributed to the same taxon. Reinvestigating the stratigraphic context reveals that N. gaudini most likely represents one of the two oldest named phocid seals, or even the oldest, dated to the late Oligocene-earliest Miocene. Our results allow questioning the widespread idea that Phocidae originated in the western Atlantic and better appreciate their palaeobiogeography during the late Oligocene-Miocene interval in the North Atlantic realm.	[Dewaele, Leonard; Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium; [Dewaele, Leonard; Lambert, Olivier] Royal Belgian Inst Nat Sci, Earth & Hist Life, Brussels, Belgium	Ghent University; Royal Belgian Institute of Natural Sciences	Dewaele, L (通讯作者)，Univ Ghent, Dept Geol, Ghent, Belgium.; Dewaele, L (通讯作者)，Royal Belgian Inst Nat Sci, Earth & Hist Life, Brussels, Belgium.	leonard.dewaele@ugent.be	Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Lambert, Olivier/0000-0003-0740-5791; Dewaele, Leonard/0000-0003-1188-2515; Louwye, Stephen/0000-0003-4814-4313	FWO PhD Fellowship [11V9115N]; FWO [V411116N]	FWO PhD Fellowship; FWO(FWO)	Funding is provided as an FWO PhD Fellowship for L.D. (grant no. 11V9115N). Additional funding for a research visit to the National Museum of Natural History, Washington, DC, USA, by L.D., was provided as an FWO long stay travel grant (grant no. V411116N). There was no additional funding received for this study. Funders played no role in study design, data collection, analysis, publishing decisions or preparation of the manuscript.	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Soc. Open Sci.	MAY	2018	5	5							171669	10.1098/rsos.171669	http://dx.doi.org/10.1098/rsos.171669			31	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	GH5TA	29892365	gold, Green Published			2025-03-11	WOS:000433498000025
J	Soliman, A; Lucas-Clark, J				Soliman, Ali; Lucas-Clark, Joyce			<i>Sphaeripilosa wernerpilleri</i>, a new peridinioid dinoflagellate genus and species from the late Miocene of Lake Pannon, Austria	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Hennersdorf; Vienna Basin; Biostratigraphy; Paleoecology; Low-salinity; Nutrient-rich; Dinoflagellate evolution	MIDDLE MIOCENE; VIENNA BASIN; CYST GENUS; SEA; SALINITY; PALEOGEOGRAPHY; ISLANDINIUM; PARATETHYS; EVOLUTION; SEDIMENTS	Sediments of the late Miocene of Lake Pannon have been studied extensively for preserved fauna and flora. Processed samples have yielded many well-preserved species of dinoflagellate cysts. Ultra-high-resolution core samples (sampled at 0.5 cm intervals) from Hennersdorf, in the Vienna Basin, and nearby outcrop samples contain, in some parts, abundant specimens of a new genus and species of dinoflagellate cyst, Sphaeripilosa wernerpilleri. The new species is a thin-walled, acavate cyst, spherical to subspherical with a distinctive dense surface ornamentation consisting of short, hair-like, solid, evexate processes. The new genus is evidently peridinioid. Interpretation of the tabulation is based almost entirely on the shape of the archeopyle, which we studied in detail. We considered three hypotheses for archeopyle interpretation and concluded, mainly by elimination, that it is mesoepicystal (3A3I), making it ovoidinioid. Sphaeripilosa wernerpilleri appears to be an indicator of low salinity and high nutrient environments as well as a stratigraphic indicator for the late Miocene (Tortonian), Pannonian Regional Stage. It may also represent a transition in peridinioid evolution to a tabulation pattern that is common in the Miocene marine calcareous calciodinelloids, in this case as an organic-walled cyst living in fresh to brackish water. (C) 2018 Elsevier B.V. All rights reserved.	[Soliman, Ali] Tanta Univ, Fac Sci, Geol Dept, Tanta 31527, Egypt; [Lucas-Clark, Joyce] Clark Geol, 6420 Becker Dr, Loomis, CA 95650 USA	Egyptian Knowledge Bank (EKB); Tanta University	Lucas-Clark, J (通讯作者)，Clark Geol, 6420 Becker Dr, Loomis, CA 95650 USA.	ali.soliman@science.tanta.edu.eg; jluclark@gmail.com	Soliman, Ali/R-1583-2018	Soliman, Ali/0000-0001-7366-4607	Commission for Stratigraphical and Paleontological Research of the Austrian Academy of Science; FWF [P21414-B16]	Commission for Stratigraphical and Paleontological Research of the Austrian Academy of Science; FWF(Austrian Science Fund (FWF))	The lab work for this study was supported by the Commission for Stratigraphical and Paleontological Research of the Austrian Academy of Science and partly by FWF-project P21414-B16. A. Soliman would like to thank Professor Werner Piller of Graz University, Professor Matthias Harzhauser of the Natural History Museum of Vienna and Dr. Andrea Kern of the University of Sao Paulo, Brazil for their significant help. The authors would like to thank the Editor-in-Chief Prof. Mike Stephenson, R. Fensome (Canada) and L. E. Edwards (USA) for their constructive comments that greatly improved the manuscript.	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Palaeobot. Palynology	MAY	2018	252						29	40		10.1016/j.revpalbo.2018.02.005	http://dx.doi.org/10.1016/j.revpalbo.2018.02.005			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	GG9IW					2025-03-11	WOS:000433015200004
J	Wang, ZH; Ryves, DB; Lei, S; Nian, XM; Lv, Y; Tang, L; Wang, L; Wang, JH; Chen, J				Wang, Zhanghua; Ryves, David B.; Lei, Shao; Nian, Xiaomei; Lv, Ye; Tang, Liang; Wang, Long; Wang, Jiehua; Chen, Jie			Middle Holocene marine flooding and human response in the south Yangtze coastal plain, East China	QUATERNARY SCIENCE REVIEWS			English	Article						Palaeo-typhoon event; Sea-level rise; Coastal flooding; Neolithic	SEA-LEVEL FLUCTUATIONS; ENVIRONMENTAL-CHANGES; RICE CULTIVATION; DELTA; SITE; INDICATORS; MANAGEMENT; SALINITY; CHARCOAL; WETLANDS	Coastal flooding catastrophes have affected human societies on coastal plains around the world on several occasions in the past, and are threatening 21st century societies under global warming and sea level rise. However, the role of coastal flooding in the interruption of the Neolithic Liangzhu culture in the lower Yangtze valley, East China coast has been long contested. In this study, we used a well-dated Neolithic site (the Yushan site) close to the present coastline to demonstrate a marine drowning event at the terminal stage of the Liangzhu culture and discuss its linkage to relative sea-level rise. We analysed sedimentology, chronology, organic elemental composition, diatoms and dinoflagellate cysts for several typical profiles at the Yushan site. The field and sedimentary data provided clear evidence of a palaeo-typhoon event that overwhelmed the Yushan site at similar to 2560 BCE, which heralded a period of marine inundation and ecological deterioration at the site. We also infer an acceleration in sea-level rise at 2560-2440 BCE from the sedimentary records at Yushan, which explains the widespread signatures of coastal flooding across the south Yangtze coastal plain at that time. The timing of this mid-Holocene coastal flooding coincided with the sudden disappearance of the advanced and widespread Liangzhu culture along the lower Yangtze valley. We infer that extreme events and flooding accompanying accelerated sea-level rise were major causes of vulnerability for prehistoric coastal societies. (C) 2018 Elsevier Ltd. All rights reserved.	[Wang, Zhanghua; Nian, Xiaomei; Lv, Ye; Tang, Liang; Wang, Long] East China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China; [Ryves, David B.] Loughborough Univ, Dept Geog, Ctr Hydrol & Ecosyst Sci CHES, Loughborough LE11 3TU, Leics, England; [Lei, Shao; Wang, Jiehua] Ningbo Municipal Inst Cultural Rel & Archaeol, Ningbo 315000, Zhejiang, Peoples R China; [Chen, Jie] Shanghai Museum, Shanghai 200003, Peoples R China	East China Normal University; Loughborough University	Wang, ZH (通讯作者)，East China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.	zhwang@geo.ecnu.edu.cn		Tang, Liang/0000-0002-1230-965X; Nian, Xiaomei/0000-0002-3164-9254; Wang, Zhanghua/0000-0003-1374-8328	National Natural Science Foundation of China [41576042]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This study was supported by the National Natural Science Foundation of China (Grant No. 41576042). We are grateful to two anonymous reviewers for their helpful comments.	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J	Wiggan, NJ; Riding, JB; Fensome, RA; Mattioli, E				Wiggan, Nickolas J.; Riding, James B.; Fensome, Robert A.; Mattioli, Emanuela			The Bajocian (Middle Jurassic): A key interval in the early Mesozoic phytoplankton radiation	EARTH-SCIENCE REVIEWS			English	Review						Dinoflagellates; Coccolithophores; Radiation; Mesozoic marine revolution	OCEANIC ANOXIC EVENT; CARBON-ISOTOPE STRATIGRAPHY; NORTH-WEST SHELF; PALEOENVIRONMENTAL CHANGES; DINOFLAGELLATE CYSTS; MARINE REVOLUTION; LUSITANIAN BASIN; CLAY MINERALOGY; PALYNOLOGY; EVOLUTION	Dinoflagellates and coccolithophores are two of the most important groups of phytoplankton in the modern oceans. These groups originated in the Triassic and radiated through the early Mesozoic, rising to ecological prominence. Within this long-term radiation, important short-term intervals of evolutionary and ecological change can be recognised. The Bajocian (Middle Jurassic,similar to 170-168 Ma) was characterised by an important ecological transition within the coccolithophores, and the radiation of one of the principal families of cyst forming dinoflagellates, the Gonyaulacaceae. During the Early Bajocian, the coccolith genus WahZnatteria diversified and expanded ecologically to dominate coccolith floras, a situation which continued for the remainder of the Mesozoic. This pattern was paralleled within dinoflagellate cyst floras by the ecological dominance of the genus Dissiliodiniun in the mid-palaeolatitudes. These phenomena appear to be linked to a positive carbon isotope shift, and an interval of enhanced productivity driven by a shift to a more humid climate, enhanced continental weathering and nutrient flux, or by changes in ocean circulation and upwelling. The latest Early Bajocian to earliest Bathonian was then characterised by the rapid increase in diversity of dinoflagellate cysts within the family Gonyaulacaceae. Through this interval, the Gonyaulacaceae transitioned from being a relatively minor component of dinoflagellate cyst floras, to becoming one of the prominent groups of cyst-forming dinoflagellates, which has persisted to the Holocene. In Europe, the pattern of this radiation was strongly influenced by sea level, with the increase in gonyaulacacean diversity reflecting a major second-order transgression. On a finer scale, the main pulses of first appearances correlate with third-order transgressive episodes. A rise in sea level, coupled with changes in the tectonic configuration of ocean gateways, appears to have controlled the pattern of plankton diversification in Europe. These palaeoceanographic changes may have enhanced water-mass transfer between Europe, the northwest Tethys Ocean and the Hispanic Corridor, which promoted the floral interchange of dinoflagellates. Whilst sea-level rise and associated large-scale palaeoenvironmental shifts appear to have controlled the pattern of dinoflagellate cyst appearances in several regions outside Europe, there is no direct correlation between dinoflagellate cyst diversity and sea-level rise on a global scale. Although the Bajocian was transgressive in several regions, widespread flooded continental area was also present throughout the preceding Aalenian, an interval of low gonyaulacacean diversity. Moreover, although the Middle Jurassic was an interval of major climatic cooling, there was a similar to 5 myr gap between the onset of cooling and the radiation of gonyaulacaceans during the Bajocian. The Bajocian was, however, marked by a major evolutionary radiation in the pelagic realm, including ammonites, giant suspension feeding fishes and planktonic foraminifera. These phenomena may indicate an underlying ecological driver to the radiation of dinoflagellates during the Bajocian evolutionary explosion which could represent an extension of the Mesozoic Marine Revolution.	[Wiggan, Nickolas J.] Univ Cambridge, Dept Earth Sci, Downing St, Cambridge CB2 3EQ, England; [Wiggan, Nickolas J.; Riding, James B.] British Geol Survey, Environm Sci Ctr, Nicker Hill, Nottingham NG12 5GG, England; [Fensome, Robert A.] Geol Survey Canada Atlantic, Nat Resources Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; [Mattioli, Emanuela] Univ Claude Bernard Lyon 1, Lab CNRS UMR 5125, Campus Doua, F-69622 Villeurbanne, France	University of Cambridge; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Universite Claude Bernard Lyon 1	Wiggan, NJ (通讯作者)，Univ Cambridge, Dept Earth Sci, Downing St, Cambridge CB2 3EQ, England.	njw56@cantab.net	Mattioli, Emanuela/D-7951-2012	Mattioli, Emanuela/0000-0003-0990-1641	NERC BGS DTG award [BUFI 5246]; British Geological Survey and the University of Cambridge; Geological Survey of Canada (Natural Resource Canada); NRCan [20170383]; NERC [bgs05017] Funding Source: UKRI	NERC BGS DTG award; British Geological Survey and the University of Cambridge; Geological Survey of Canada (Natural Resource Canada); NRCan(Natural Resources Canada); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work has arisen from the PhD project of Nickolas J. Wiggan which was supported by NERC BGS DTG award reference BUFI 5246, entitled The mid Jurassic plankton explosion. This was funded jointly between the British Geological Survey and the University of Cambridge. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). We thank the Review Papers Coordinator, Tim Horscroft, for inviting this contribution. Nick Butterfield (Cambridge) is thanked for discussions and suggestions during NJW's PhD project. We also thank Daniel Mantle and Fabienne Giraud, whose insightful reviews greatly improved the quality of this manuscript. Rob Fensome acknowledges support from the Geological Survey of Canada (Natural Resource Canada), and thanks Nikole Bingham-Kozlowski for providing an internal review; this is NRCan Contribution number 20170383.	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Rev.	MAY	2018	180						126	146		10.1016/j.earscirev.2018.03.009	http://dx.doi.org/10.1016/j.earscirev.2018.03.009			21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GH7PM		Green Accepted, Green Submitted			2025-03-11	WOS:000433645900006
J	Gu, F; Chiessi, CM; Zonneveld, KAF; Behling, H				Gu, Fang; Chiessi, Cristiano M.; Zonneveld, Karin A. F.; Behling, Hermann			Late Quaternary environmental dynamics inferred from marine sediment core GeoB6211-2 off southern Brazil	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						South Atlantic; Pollen; Dinollagellate cysts; Environmental change; Vegetation history; Ocean currents	WALLED DINOFLAGELLATE CYSTS; CLIMATE DYNAMICS; SELECTIVE PRESERVATION; MULTIVARIATE-ANALYSIS; DISTRIBUTION PATTERNS; CAMPOS REGION; SAO FRANCISCO; MID-HOLOCENE; ATLANTIC; VARIABILITY	Vegetation and climate changes in southern Brazil, as well as the dynamics of the adjacent South Atlantic were investigated through the analyses of pollen, spores and dinocysts from marine sediment core GeoB6211-2 that covers the last 19.3 kyr. The pollen record indicates the dominance of grassland (campos) in southeastern South America (SESA), reflecting cold and/or dry conditions during the Last Glacial Maximum. Forests, mainly gallery forests, expanded slightly during Heinrich Stadial 1, suggesting slightly wetter conditions. A stronger expansion of the Atlantic lowland rainforest is noticed in the record after ca. 5.5 cal kyr BP, likely due to wetter conditions. The relatively high amount of exotic Nothofagus pollen, transported by wind, rivers and then by oceanic currents northwards to the study site, as well as the dinocyst Brigantedinium spp., indicate a noticeable influence of the Brazilian Coastal Current from the south between 19.3 and 14.8 cal kyr BP. After that, the decrease in Nothofagus and Brigantedinium spp. together with the increase in dinocyst Operculodinium centrocarpum indicate that the Brazil Current from the north dominated the coring site. The abundance of freshwater algae between ca. 19.3 and 17.0 cal kyr BP suggests that the Rio de la Plata mouth was located close to the coring site during this period, and its discharge of nutrient-rich freshwaters strongly affected the upper water column. Sea level rise decreased this impact during the late glacial phase by moving the coastline further away from the core site. The presence of the Brazil Current at the core site became stronger after ca. 15 cal kyr BP and strongest after 9 cal kyr BP. In summary, the pollen, spores and dinocyst records from core GeoB6211-2 provide important climatic records to reconstruct the environmental changes in SESA.	[Gu, Fang; Behling, Hermann] Univ Goettingen, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany; [Chiessi, Cristiano M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Rua Arlindo Bettio 1000, BR-3828000 Sao Paulo, Brazil; [Zonneveld, Karin A. F.] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany	University of Gottingen; Universidade de Sao Paulo; University of Bremen	Gu, F (通讯作者)，Univ Goettingen, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany.	Fang.Gu@biologie.uni-goettingen.de	Chiessi, Cristiano/JAZ-0806-2023; Chiessi, Cristiano/E-1916-2012; Fapesp, Biota/F-8655-2017	Chiessi, Cristiano/0000-0003-3318-8022; Fapesp, Biota/0000-0002-9887-8449; Gu, Fang/0000-0002-8181-2822	China Scholarship Council (CSC); FAPESP [2012/17517-3, 2013/50297-0]; CAPES [1976/2014, 564/2015]; CNPq [302607/2016-1, 422255/2016-5]; Division Of Environmental Biology; Direct For Biological Sciences [1343578] Funding Source: National Science Foundation; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [13/50297-0] Funding Source: FAPESP	China Scholarship Council (CSC)(China Scholarship Council); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Division Of Environmental Biology; Direct For Biological Sciences(National Science Foundation (NSF)NSF - Directorate for Biological Sciences (BIO)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	We thank Vera Markgraf, Henry Hooghiemstra and one anonymous reviewer for valuable and constructive comments on the manuscript. We would like to thank all crew members from RV Meteor cruise M46/2 for the recovery of the studied sediment core. We thank Jurgen Patzold for the help with the sample material, which has been provided by the GeoB Core Repository at the MARUM - Center for Marine Environmental Sciences, University of Bremen, Germany. Vera Bender is thanked for her help sampling the core and Jorg Christiansen for computer technical support. The first author thanks the financial support from China Scholarship Council (CSC). Cristiano M. Chiessi acknowledges the financial support from FAPESP (grants 2012/17517-3 and 2013/50297-0), CAPES (grants 1976/2014 and 564/2015) and CNPq (grants 302607/2016-1 and 422255/2016-5). The data reported in this paper will be archived in Pangaea (www.pangaea.de).	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Paleoclimatol. Paleoecol.	MAY 1	2018	496						48	61		10.1016/j.palaeo.2018.01.015	http://dx.doi.org/10.1016/j.palaeo.2018.01.015			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	GB3QR					2025-03-11	WOS:000428973000004
J	Wang, H; Park, BS; Lim, WA; Ki, JS				Wang, Hui; Park, Bum Soo; Lim, Weol-Ae; Ki, Jang-Seu			<i>CpMCA</i>, a novel metacaspase gene from the harmful dinoflagellate <i>Cochlodinium polykrikoides</i> and its expression during cell death	GENE			English	Article						Cochlodinium polykrikoides; CpMCA; Algicide; HGT; Transcriptional response; PCD	GENOME-WIDE ANALYSIS; PROROCENTRUM-DONGHAIENSE; REVEALS; FAMILY	Metacaspases (MCAs) are cysteine proteases that share sequence homology with caspases, and may play roles in programmed cell death (PCD). In the present study, we identified a novel MCA gene (CpMCA) from the red tide dinoflagellate Cochlodinium polykrikoides, and examined its molecular characteristics and gene expression in response to algicide-induced cell death. CpMCA cDNA is 1164 bp in length, containing a dinoflagellate spliced leader sequence (dinoSL), an 879-bp open reading frame (ORF), which codes for a 293-aa protein, and a poly (A) tail. Multi-sequence comparison indicated that CpMCA belongs to type I MCA, but it has a different structure at the N-terminal. Phylogenetic analysis showed that C. poly. krikoides may have acquired the MCA gene from bacteria by means of horizontal gene transfer (HGT). In addition, expressions of CpMCA significantly increased following exposure to the common algicides copper sulfate and oxidizing chlorine, which trigger cell death in dinoflagellates, suggesting that CpMCA may be involved in cell death.	[Wang, Hui; Ki, Jang-Seu] Sangmyung Univ, Dept Biotechnol, Seoul 03016, South Korea; [Park, Bum Soo] Sangmyung Univ, Inst Nat Sci, Seoul 03016, South Korea; [Lim, Weol-Ae] Natl Inst Fisheries Sci, Ocean Climate & Ecol Res Div, Busan 46083, South Korea	Sangmyung University; Sangmyung University; National Institute of Fisheries Science	Ki, JS (通讯作者)，Sangmyung Univ, Dept Biotechnol, Seoul 03016, South Korea.	kijs@smu.ac.kr	Wang, Hui/AFD-3905-2022; PARK, Bum Soo/W-3178-2017	PARK, Bum Soo/0000-0002-5441-6779; Wang, Hui/0000-0002-4121-1838	National Research Foundation of Korea Grant - Korean Government [2015M1A5A1041805, 2016R1D1A1A09920198]; National Fisheries Research and Development [R2018043]	National Research Foundation of Korea Grant - Korean Government(National Research Foundation of Korea); National Fisheries Research and Development	This work was supported by the National Research Foundation of Korea Grant funded by the Korean Government (2015M1A5A1041805 and 2016R1D1A1A09920198), and by a grant from the National Fisheries Research and Development (R2018043) funded to J.-S. Ki.	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J	Bringué, M; Thunell, RC; Pospelova, V; Pinckney, JL; Romero, OE; Tappa, EJ				Bringue, Manuel; Thunell, Robert C.; Pospelova, Vera; Pinckney, James L.; Romero, Oscar E.; Tappa, Eric J.			Physico-chemical and biological factors influencing dinoflagellate cyst production in the Cariaco Basin	BIOGEOSCIENCES			English	Article							SEA-SURFACE TEMPERATURE; RECENT MARINE-SEDIMENTS; SANTA-BARBARA BASIN; 1997-98 EL-NINO; THECA RELATIONSHIP; TROPICAL ATLANTIC; NORTH-ATLANTIC; CARIBBEAN SEA; ENVIRONMENTAL-CHANGE; ABSOLUTE ABUNDANCE	We present a 2.5-year-long sediment trap record of dinoflagellate cyst production in the Cariaco Basin, off Venezuela (southern Caribbean Sea). The site lies under the influence of wind-driven, seasonal upwelling which promotes high levels of primary productivity during boreal winter and spring. Changes in dinoflagellate cyst production is documented between November 1996 and May 1999 at similar to 14-day intervals and interpreted in the context of in situ observations of physico-chemical and biological parameters measured at the mooring site.& para;& para;Dinoflagellate cyst assemblages are diverse (57 taxa) and dominated by cyst taxa of heterotrophic affinity, primarily Brigantedinium spp. (51 % of the total trap assemblage). Average cyst fluxes to the trap are high (17.1 x 10(3) cysts m(-2) day(-1)) and show great seasonal and interannual variability. On seasonal timescales, dinoflagellate cyst production responds closely to variations in upwelling strength, with increases in cyst fluxes of several protoperidinioid taxa observed during active upwelling intervals, predominantly Brigantedinium spp. Cyst taxa produced by autotrophic dinoflagellates, in particular Bitectatodinium spongium, also respond positively to upwelling. Several "spiny brown" cysts contribute substantially to the assemblages, including Echinidinium delicatum (9.7 %) and Echinidinium granulatum (7.3 %), and show a closer affinity to weaker upwelling conditions. The strong El Nino event of 1997/98 appears to have negatively impacted cyst production in the basin with a 1-year lag, and may have contributed to the unusually high fluxes of cysts type "Cp" (possibly the cysts of the toxic dinoflagellate Cochlodinium polykrikoides sensu Li et al., 2015), with cyst type Cp fluxes up to 11.8 x 10(3) cysts m(-2) day(-1) observed during the weak upwelling event of February-May 1999.& para;& para;Possible trophic interactions between dinoflagellates and other major planktonic groups are also investigated by comparing the timing and magnitude of cyst production with proxies for phytoplanktonic communities (from photopigment data) and micro- to macrozooplankton abundance indicators (from palynological data) at the site. This work provides new, detailed insights into the ecology of cystproducing dinoflagellates and will allow for more detailed interpretations of fossil assemblages extracted from sedimentary records in the basin and elsewhere.	[Bringue, Manuel; Thunell, Robert C.; Pinckney, James L.; Tappa, Eric J.] Univ South Carolina, Sch Earth Ocean & Environm, 701 Sumter St,EWS 617, Columbia, SC 29208 USA; [Bringue, Manuel; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada; [Pinckney, James L.] Univ South Carolina, Belle W Baruch Inst Marine & Coastal Sci, 700 Sumter St,EWS 604, Columbia, SC 29208 USA; [Romero, Oscar E.] Univ Bremen, Ctr Marine Environm Sci, MARUM, Leobenerstr, D-28359 Bremen, Germany; [Bringue, Manuel] Geol Survey Canada, 3303 33rd St NW, Calgary, AB T2L 2A7, Canada	University of South Carolina System; University of South Carolina Columbia; University of Victoria; University of South Carolina System; University of South Carolina Columbia; University of Bremen; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Bringué, M (通讯作者)，Univ South Carolina, Sch Earth Ocean & Environm, 701 Sumter St,EWS 617, Columbia, SC 29208 USA.; Bringué, M (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada.; Bringué, M (通讯作者)，Geol Survey Canada, 3303 33rd St NW, Calgary, AB T2L 2A7, Canada.	manuel.bringue@canada.ca	Romero, Oscar/T-9717-2019; Bringue, Manuel/KIH-8224-2024	Pospelova, Vera/0000-0003-4049-8133; Romero, Oscar/0000-0003-0209-3258; Bringue, Manuel/0000-0003-4460-8344; Pinckney, James/0000-0002-6056-6511	Natural Sciences and Engineering Research Council of Canada (NSERC) Postdoctoral Fellowship (PDF); Advanced Support Program for Innovative Research Excellence (ASPIRE I - Track IIb) from the U. of South Carolina to Manuel Bringue; NSERC Discovery grant; National Science Foundation (NSF) [OCE 9401537, OCE 9729697, OCE 1258991]	Natural Sciences and Engineering Research Council of Canada (NSERC) Postdoctoral Fellowship (PDF)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Advanced Support Program for Innovative Research Excellence (ASPIRE I - Track IIb) from the U. of South Carolina to Manuel Bringue; NSERC Discovery grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); National Science Foundation (NSF)(National Science Foundation (NSF))	This work was funded by a Natural Sciences and Engineering Research Council of Canada (NSERC) Postdoctoral Fellowship (PDF) and an Advanced Support Program for Innovative Research Excellence (ASPIRE I - Track IIb) from the U. of South Carolina to Manuel Bringue, and an NSERC Discovery grant to Vera Pospelova. The CARIACO sediment trapping program was supported by the National Science Foundation (NSF; grants OCE 9401537, OCE 9729697, and OCE 1258991). The authors wish to thank Claudia Benitez-Nelson (University of South Carolina) for providing mixed layer depth data and for helpful discussions on the hydrology of the basin. Kenneth Mertens (IFREMER - Concarneau) is kindly thanked for his help in dinoflagellate cyst identification. The crew of the R/V Hermano Gines is also gratefully acknowledged for all operations at sea. The authors are grateful to Barrie Dale (University of Oslo), Sofia Ribeiro (Geological Survey of Denmark and Greenland), and the anonymous reviewer for their helpful and constructive comments that helped improve the manuscript. NRCan Contribution number: 20180015.	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L., 2017, AM ASS STRATIGRAPHIC, V48; Zonneveld KAF, 1999, REV PALAEOBOT PALYNO, V106, P153, DOI 10.1016/S0034-6667(99)00007-X; Zonneveld KAF, 1997, REV PALAEOBOT PALYNO, V97, P319, DOI 10.1016/S0034-6667(97)00002-X; Zonneveld KAF, 2000, DEEP-SEA RES PT II, V47, P2229, DOI 10.1016/S0967-0645(00)00023-0; Zonneveld KAF, 2015, PALYNOLOGY, V39, P387, DOI 10.1080/01916122.2014.990115; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003; Zonneveld KAF, 2010, J PHYCOL, V46, P202, DOI 10.1111/j.1529-8817.2009.00799.x	128	16	17	0	9	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	1726-4170	1726-4189		BIOGEOSCIENCES	Biogeosciences	APR 19	2018	15	7					2325	2348		10.5194/bg-15-2325-2018	http://dx.doi.org/10.5194/bg-15-2325-2018			24	Ecology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	GD4PU		gold, Green Published			2025-03-11	WOS:000430485900003
J	Cuellar-Martinez, T; Alonso-Rodríguez, R; Ruiz-Fernández, AC; de Vernal, A; Morquecho, L; Limoges, A; Henry, M; Sanchez-Cabeza, JA				Cuellar-Martinez, Tomasa; Alonso-Rodriguez, Rosalba; Carolina Ruiz-Fernandez, Ana; de Vernal, Anne; Morquecho, Lourdes; Limoges, Audrey; Henry, Maryse; Sanchez-Cabeza, Joan-Albert			Environmental forcing on the flux of organic-walled dinoflagellate cysts in recent sediments from a subtropical lagoon in the Gulf of California	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Sediment; Dinocyst; San Jose Island; Polysphaeridium zoharyi; Lingulodinium machaerophorum; Climatic variability	HARMFUL ALGAL BLOOMS; SEA-SURFACE CONDITIONS; TODOS-SANTOS BAY; LINGULODINIUM-POLYEDRUM; PYRODINIUM-BAHAMENSE; BAJA-CALIFORNIA; SPATIAL-DISTRIBUTION; ACCUMULATION RATES; CLIMATE-CHANGE; MARINE	To evaluate the relationship of changes in organic-walled dinoflagellate cyst (dinocyst) fluxes to sediments with environmental variables (air and sea surface temperatures, El Nino conditions, rainfall, and terrigenous index), cyst assemblages were analyzed in a Pb-210-dated sediment core (similar to 100 years) from the pristine San Jose Lagoon (San Jose Island, SWGulf of California). The dinocyst abundance ranged from3784 to 25,108 cysts g(-1) and fluxes were of the order of 103-104 cysts cm(-2) yr(-1). Lingulodinium machaerophorum, Polysphaeridium zoharyi and Spiniferites taxa accounted for 96% of the total dinocyst assemblages, and the abundances of these species increased towards the core surface. P. zoharyi fluxes increased from about 1965 onwards. Redundancy analyses, showed that mean minimum air temperature and terrigenous index were the key factors governing dinocyst fluxes. In this study, dinocyst fluxes of dominant taxa had responded to changes in climate-dependent environmental variables during the past similar to 20 years; this may also be the case in other subtropical coastal lagoons. (C) 2017 Elsevier B. V. All rights reserved.	[Cuellar-Martinez, Tomasa] Univ Nacl Autonoma Mexico, Posgrad Ciencias Mar & Limnol, Av Ciudad Univ 3000, Mexico City 04510, DF, Mexico; [Alonso-Rodriguez, Rosalba; Carolina Ruiz-Fernandez, Ana] Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Unidad Acad Mazatlan, Mazatlan 82040, Sinaloa, Mexico; [de Vernal, Anne; Henry, Maryse] Univ Quebec Montreal, Geotop, CP 8888,Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada; [Morquecho, Lourdes] Ctr Invest Biol Noroeste CIBNOR, Av IPN 195, La Paz 23096, Baja California, Mexico; [Limoges, Audrey] Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB E3B 5A3, Canada; [Sanchez-Cabeza, Joan-Albert] Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Unidad Acad Proc Ocean & Costeros, Ciudad Univ, Mexico City 04510, DF, Mexico	Universidad Nacional Autonoma de Mexico; Universidad Nacional Autonoma de Mexico; University of Quebec; University of Quebec Montreal; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; University of New Brunswick; Universidad Nacional Autonoma de Mexico	Alonso-Rodríguez, R (通讯作者)，Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Unidad Acad Mazatlan, Mazatlan 82040, Sinaloa, Mexico.	rosalba@ola.icmyl.unam.mx	Morquecho, Lourdes/JPY-0626-2023; de Vernal, Anne/D-5602-2013; Ruiz-Fernández, Ana Carolina/ABG-6985-2020; Sanchez-Cabeza, Joan-Albert/Q-2394-2016; Alonso-Rodriguez, Rosalba/U-9896-2017	Sanchez-Cabeza, Joan-Albert/0000-0002-3540-1168; Alonso-Rodriguez, Rosalba/0000-0001-7716-3869; Cuellar Martinez, Tomasa/0000-0002-0460-6275; Limoges, Audrey/0000-0002-4587-3417; Morquecho, Lourdes/0000-0003-2963-8836; RUIZ-FERNANDEZ, ANA CAROLINA/0000-0002-2515-1249	Posgrado en Ciencias del Mar y Limnologia, UNAM; CONACYT [307783];  [CONACYT 196813];  [PAPIIT-UNAM IN112914];  [PROMEP/103.5/13/9335];  [IAEA-ARCAL RLA 7014]	Posgrado en Ciencias del Mar y Limnologia, UNAM(Universidad Nacional Autonoma de Mexico); CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); ; ; ; 	This work was supported by the grants CONACYT 196813, PAPIIT-UNAM IN112914 and PROMEP/103.5/13/9335, IAEA-ARCAL RLA 7014. TCM thanks to Posgrado en Ciencias del Mar y Limnologia, UNAM and CONACYT which provided the Ph.D. fellowship (307783). The authors thank E. Calvillo-Espinoza, J. Angulo-Calvillo, A. Gonzalez-Peralta for their help provided in field work; M. Hernandez-Vazquez and L. H. Perez-Bernal for laboratory analysis; G. Ramirez-Resendiz, C. Suarez, E. Cruz-Acevedo for data management and artwork; and D. Oviedo and H. Rojas for bibliographic research assistance. M. E. Sanchez-Salazar and A. Grant contributed to the edition of the English manuscript. We also appreciate to anonymous reviewers for their thorough and constructive reviews.	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Total Environ.	APR 15	2018	621						548	557		10.1016/j.scitotenv.2017.11.269	http://dx.doi.org/10.1016/j.scitotenv.2017.11.269			10	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	FU9SJ	29195203				2025-03-11	WOS:000424196800057
J	van Soelen, EE; Twitchett, RJ; Kürschner, WM				van Soelen, Elsbeth E.; Twitchett, Richard J.; Kurschner, Wolfram M.			Salinity changes and anoxia resulting from enhanced run-off during the late Permian global warming and mass extinction event	CLIMATE OF THE PAST			English	Article							DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; PROCESS LENGTH VARIATION; NORTHERN NORTH-ATLANTIC; TRIASSIC BOUNDARY; SOUTH CHINA; SURFACE SEDIMENTS; CYST ASSEMBLAGES; EAST GREENLAND; BIOTIC CRISIS; BALTIC SEA	The late Permian biotic crisis had a major impact on marine and terrestrial environments. Rising CO2 levels following Siberian Trap volcanic activity were likely responsible for expanding marine anoxia and elevated water temperatures. This study focuses on one of the stratigraphically most expanded Permian-Triassic records known, from Jameson Land, East Greenland. High-resolution sampling allows for a detailed reconstruction of the changing environmental conditions during the extinction event and the development of anoxic water conditions. Since very little is known about how salinity was affected during the extinction event, we especially focus on the aquatic palynomorphs and infer changes in salinity from changes in the assemblage and morphology. The start of the extinction event, here defined by a peak in spore : pollen, indicating disturbance and vegetation destruction in the terrestrial environment, postdates a negative excursion in the total organic carbon, but predates the development of anoxia in the basin. Based on the newest estimations for sedimentation rates, the marine and terrestrial ecosystem collapse took between 1.6 and 8 kyr, a much shorter interval than previously estimated. The palyno-facies and palynomorph records show that the environmental changes can be explained by enhanced run-off and increased primary productivity and water column stratification. A lowering in salinity is supported by changes in the acritarch morphology. The length of the processes of the acritarchs becomes shorter during the extinction event and we propose that these changes are evidence for a reduction in salinity in the shallow marine setting of the study site. This inference is supported by changes in acritarch distribution, which suggest a change in palaeoenvironment from open marine conditions before the start of the extinction event to more nearshore conditions during and after the crisis. In a period of sea-level rise, such a reduction in salinity can only be explained by increased run-off. High amounts of both terrestrial and marine organic fragments in the first anoxic layers suggest that high run-off, increased nutrient availability, possibly in combination with soil erosion, are responsible for the development of anoxia in the basin. Enhanced run-off could result from changes in the hydrological cycle during the late Permian extinction event, which is a likely consequence of global warming. In addition, vegetation destruction and soil erosion may also have resulted in enhanced run-off. Salinity stratification could potentially explain the development of anoxia in other shallow marine sites. The input of freshwater and related changes in coastal salinity could also have implications for the interpretation of oxygen isotope records and seawater temperature reconstructions at some sites.	[van Soelen, Elsbeth E.; Kurschner, Wolfram M.] Univ Oslo, Dept Geosci, POB 1047 Blindern, N-0316 Oslo, Norway; [Twitchett, Richard J.] Nat Hist Museum, Earth Sci Dept, London SW7 5BD, England	University of Oslo; Natural History Museum London	van Soelen, EE (通讯作者)，Univ Oslo, Dept Geosci, POB 1047 Blindern, N-0316 Oslo, Norway.	evansoelen@gmail.com	Kürschner, Wolfram/B-4724-2009	Kurschner, Wolfram Michael/0000-0001-6883-6486	Norwegian Research Council [234005]; Permian/Triassic evolution of the Timan-Pechora; Danish National Research Foundation	Norwegian Research Council(Research Council of Norway); Permian/Triassic evolution of the Timan-Pechora; Danish National Research Foundation(Danmarks Grundforskningsfond)	This work was funded by the Norwegian Research Council, project 234005, The Permian/Triassic evolution of the Timan-Pechora and Barents Sea Basins. We thank Berit L. Berg and Mufak S. Naoroz for technical support. Samples were collected by Richard J. 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Past.	APR 9	2018	14	4					441	453		10.5194/cp-14-441-2018	http://dx.doi.org/10.5194/cp-14-441-2018			13	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	GB9AU		gold, Green Submitted			2025-03-11	WOS:000429367200001
J	Kitchen, SA; Bourdelais, AJ; Taylor, AR				Kitchen, Sheila A.; Bourdelais, Andrea J.; Taylor, Alison R.			Interaction of a dinoflagellate neurotoxin with voltage-activated ion channels in a marine diatom	PEERJ			English	Article						Brevetoxin; Karenia brevis; Action potential; Sodium channel; Dinoflagellate; Diatom	GATED SODIUM-CHANNELS; RED-TIDE DINOFLAGELLATE; HARMFUL ALGAL BLOOMS; BREVETOXIN-PRODUCING DINOFLAGELLATE; KARENIA-BREVIS BLOOMS; NA+-CHANNEL; POLYKETIDE SYNTHASES; MOLECULAR-MECHANISMS; SENSORY NEURONS; PHYTOPLANKTON	Background, The potent neurotoxins produced by the harmful algal bloom species Karenict brevis are activators of sodium voltage-gated channels (VGC) in animals, resulting in altered channel kinetics and membrane hyperexcitability. Recent biophysical and genomic evidence supports widespread presence of homologous sodium (Na+) and calcium (Ca2+) permeable VGCs in unicellular algae,including marine phytoplankton. We therefore hypothesized that VGCs of these phytoplankton may be an allelopathic target for waterborne neurotoxins produced by K. brevis blooms that could lead to ion channel dysfunction and disruption of signaling in a similar manner to animal Na+ VGCs. Methods. We examined the interaction of brevetoxin-3 (PbTx-3), a K. brevis neurotoxin with the Na+/Ca2+ VGC of the non-toxic diatom Odontella sinensis using electrophysiology, Single electrode current-and voltage-clamp recordings from O. sinensis in the presence of PbTx-3 were used to examine the toxin's effect on voltage gated Na+/Ca2+ currents. In silco analysis was used to identify the putative PbTx binding site in the diatoms. We identified Na+/Ca2+ ATCG homologs from the. transcriptomes and genomes of 12 diatoms, including three transcriptsfrom O. sinensts and aligned them with site-5 of Na+ VGCs, previously identified as the PbTx binding site in animals. Results. Up to 1 mu M PbTx had no effect on diatom resting membrane potential or membrane excitability. The kinetics of fast inward Na+/Ca2+ currents that underlie diatom action potentials were also unaffected. However, the peak inward current was inhibited by 33%, delayed outward current was inhibited by 25%, and reversal potential of the currents shifted positive, indicating a change in permeability of the underlying channels. Sequence analysis showed a lack of conservation of the PbTx binding site in diatom VGC homologs, many of which share molecular features more similar to single-domain bacterial Na+/Ca2+ VGCs than the 4-domain eukaryote channels. Discussion. Although membrane excitability and the kinetics of action potential currents were unaffected, the permeation of the channels underlying the diatom action potential was significantly altered in the presence of PbTx-3. However, at environmentally relevant concentrations the effects of PbTx-on diatom voltage activated currents and interference of cell signaling through this pathway may be limited. The relative insensitivity of phytoplankton VGCs may be due to divergence of site-5 (the putative PbTx binding site), and in some cases, such as a sinensis, resistance	[Kitchen, Sheila A.; Taylor, Alison R.] Univ North Carolina Wilmington, Dept Biol & Marine Biol, Wilmington, NC 28403 USA; [Bourdelais, Andrea J.] Univ North Carolina Wilmington, Ctr Marine Sci, Wilmington, NC USA	University of North Carolina; University of North Carolina Wilmington; University of North Carolina; University of North Carolina Wilmington	Taylor, AR (通讯作者)，Univ North Carolina Wilmington, Dept Biol & Marine Biol, Wilmington, NC 28403 USA.	taylora@uncw.edu		Kitchen, Sheila/0000-0003-4402-8139	University of North Carolina Wilmington Center for Marine Science Pilot Grant; National Science Foundation [IOS 0949744]	University of North Carolina Wilmington Center for Marine Science Pilot Grant; National Science Foundation(National Science Foundation (NSF))	This work was supported by a University of North Carolina Wilmington Center for Marine Science Pilot Grant and by the National Science Foundation (IOS 0949744). 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	Miao, YF; Warny, S; Clift, PD; Gregory, M; Liu, C				Miao, Yunfa; Warny, Sophie; Clift, Peter D.; Gregory, Mitch; Liu, Chang			Climatic or tectonic control on organic matter deposition in the South China Sea? A lesson learned from a comprehensive Neogene palynological study of IODP Site U1433	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article; Proceedings Paper	1st Joint Meeting of the 33rd Annual Meeting of the Society-for-Organic-Petrology (TSOP) / Meeting of the Palynological-Society (AASP) / Meeting of the International-Committee-for-Coal-and-Organic-Petrology (ICCP)	SEP 18-23, 2016	Houston, TX	Soc Organ Petrol, Palynol Soc, Int Comm Coal & Organ Petrol		Organic matters; Tectonics; Monsoon; Driving forces; Neogene	ASIAN SUMMER MONSOON; WESTERN QAIDAM BASIN; TIBETAN PLATEAU; MIDDLE MIOCENE; EXPEDITION 349; POLLEN RECORD; 20 MA; EVOLUTION; OLIGOCENE; PALYNOFACIES	Palynomorphs and other organic particles are basic key components of palynofacies, yet quantitative analyses of all types are rarely used together to investigate organic matter assemblage changes and evaluate the driving forces behind the observed changes. In this paper, eight organic-walled microfossil and particle morphologies (sporopollen, Pediastrum, Concentricystes, fungi, dinoflagellate cysts, structured/amorphous organic matters, stomatal apparatus and scolecodonts) are tabulated and their concentrations and fluxes are evaluated over the past 17 million years (Ma) in sediments recovered from the South China Sea at International Ocean Discovery Program (IODP) Site U1433. Overall, these morphologies show roughly similar increasing trends but with different levels of fluctuations. The uniform increase in all morphologies at 8 Ma (named the 8 Ma event) is the most notable feature of the past 17 Ma. To explain the trend, and because these various organic matters reflect various environmental conditions, we argue that the uniformity of the signal implies that tectonically-driven basin and drainage evolution played the key role, rather than paleoclimate (Asian summer monsoon). The similar to 8 Ma event was likely triggered by the onset of the Mekong River in its present location, although the role of monsoon evolution cannot be excluded completely.	[Miao, Yunfa; Warny, Sophie; Clift, Peter D.; Gregory, Mitch; Liu, Chang] Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA; [Miao, Yunfa] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Gansu, Peoples R China; [Warny, Sophie; Gregory, Mitch] Louisiana State Univ, Museum Nat Sci, 109 Foster Hall, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University; Chinese Academy of Sciences; Cold & Arid Regions Environmental & Engineering Research Institute, CAS; Louisiana State University System; Louisiana State University	Miao, YF; Warny, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA.	yunfine2000@sina.com; swarny@lsu.edu	Warny, Sophie/A-8226-2013; Clift, Peter/JWO-3915-2024	Warny, Sophie/0000-0002-3451-040X	U.S. Science Support Program to Louisiana State University; NSFC [41290252, 41772181]; Chinese Academy of Sciences; CENEX; Charles T. McCord Jr. Chair in Petroleum Geology; USSAC	U.S. Science Support Program to Louisiana State University; NSFC(National Natural Science Foundation of China (NSFC)); Chinese Academy of Sciences(Chinese Academy of Sciences); CENEX; Charles T. McCord Jr. Chair in Petroleum Geology; USSAC	This research used samples and/or data provided by the International Ocean Discovery Program (IODP). Funding for this research was provided by the U.S. Science Support Program to Louisiana State University as well as by the NSFC Grants (41290252, 41772181). The research was carried out at the Center for Excellence in Palynology (CENEX) in Baton Rouge, Louisiana. The visiting scholar fellowship to Yunfa Miao is funded by the Chinese Academy of Sciences through a partnership with CENEX. PC thanks the Charles T. McCord Jr. Chair in Petroleum Geology and USSAC for support during this study.	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J. Coal Geol.	APR 1	2018	190				SI		166	177		10.1016/j.coal.2017.10.003	http://dx.doi.org/10.1016/j.coal.2017.10.003			12	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Energy & Fuels; Geology	GE4BQ					2025-03-11	WOS:000431159700011
J	Plachno, BJ; Jurkowska, A; Pacyna, G; Worobiec, E; Gedl, P; Swierczewska-Gladysz, E				Plachno, Bartosz J.; Jurkowska, Agata; Pacyna, Grzegorz; Worobiec, Elzbieta; Gedl, Przemyslaw; Swierczewska-Gladysz, Ewa			Plant assemblage from Opole, southern Poland: New data on Late Cretaceous vegetation of the northern part of the European Province	PROCEEDINGS OF THE GEOLOGISTS ASSOCIATION			English	Article						Cretaceous; Upper Turonian; Geinitzia; Palynomorphs; Palaeoenvironment; Poland	TURONIAN-CONIACIAN; WESTERN; PRESERVATION; CUTICLES; TROUGH; ISLAND; BASIN	This paper presents the results of studies on plant macroremains found in the upper Turonian of the Folwark Quarry, Opole, Poland, associated with palynological studies of the host rocks. In addition to a few macrofossils (gymnosperm wood, conifer Geinitzia reichenbachii and fern ?Didymosorus) rich sporomorphs (bryophyte, lycopod and fern spores, conifer and angiosperm pollen grains) and marine palynomorphs (mainly dinoflagellate cysts) were recorded. The palynological analysis revealed that the vegetation on the neighbouring land (the East Sudetic Island) in the late Turonian was much more diverse than could be reconstructed based on only macrofossil remains. The latter are taxonomically restricted and dominated by one gymnosperm species (Geinitzia reichenbachii), which make them similar to most neighbouring, coeval Central European assemblages. Its over representation is, thus, a result of taphonomy. (C) 2018 The Geologists' Association. Published by Elsevier Ltd. All rights reserved.	[Plachno, Bartosz J.] Jagiellonian Univ Krakow, Dept Plant Cytol & Embryol, Gronostajowa 9 St, PL-30387 Krakow, Poland; [Jurkowska, Agata] AGH Univ Sci & Technol Krakow, Fac Geol Geophys & Environm Protect, Mickiewicza 30 St, PL-30059 Krakow, Poland; [Pacyna, Grzegorz] Jagiellonian Univ Krakow, Inst Bot, Dept Taxon Phytogeog & Palaeobot, Kopernika 27 St, PL-31501 Krakow, Poland; [Worobiec, Elzbieta] Polish Acad Sci, W Szafer Inst Bot, Lubicz 46 St, PL-31512 Krakow, Poland; [Gedl, Przemyslaw] Polish Acad Sci, Res Ctr Krakow, Inst Geol Sci, Senacka 1 St, PL-31002 Krakow, Poland; [Swierczewska-Gladysz, Ewa] Univ Lodz, Inst Earth Sci, Narutowicza 88 St, I-90139 Lodz, Poland	Jagiellonian University; AGH University of Krakow; Jagiellonian University; 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; University of Lodz	Jurkowska, A (通讯作者)，AGH Univ Sci & Technol Krakow, Fac Geol Geophys & Environm Protect, Mickiewicza 30 St, PL-30059 Krakow, Poland.	bartosz.plachno@uj.edu.pl; jurkowska.a@gmail.com; grzegorz.pacyna@uj.edu.pl; e.worobiec@botany.pl; ndgedl@cyf-kr.edu.pl; ewa.swierczewska@geo.uni.lodz.pl	; Jurkowska, Agata/A-9734-2016; Plachno, Bartosz/AAJ-6128-2021	Worobiec, Elzbieta/0000-0001-5997-9602; Jurkowska, Agata/0000-0001-5457-9968; Plachno, Bartosz/0000-0001-5579-5101; Swierczewska-Gladysz, Ewa/0000-0003-4628-2712; Pacyna, Grzegorz/0000-0003-4365-3549	AGH University of Science and Technology, Statutory Founding [11.11.140.626]; Ministry of Science and Higher Education of Poland; Department of Taxonomy, Phytogeography and Palaeobotany, Institute of Botany at the Jagiellonian University in Krakow [K/ZDS/006305]	AGH University of Science and Technology, Statutory Founding; Ministry of Science and Higher Education of Poland(Ministry of Science and Higher Education, Poland); Department of Taxonomy, Phytogeography and Palaeobotany, Institute of Botany at the Jagiellonian University in Krakow	Dr. Jadwiga Ziaja (W. Szafer Institute of Botany, Polish Academy of Sciences, Krakow) is kindly acknowledged for her help in taking photographs of pollen grains and spores and Tadeusz Jurkowski for support during the fieldwork. We thank Dr. Marc Philippe (Universite Lyon 1 and CNRS UMR 5276, France) for his suggestion regarding wood remains. Thanks to Kyle Freeman for linguistic corrections. Warmly thanks to Prof. Malcolm Hart (University of Plymouth) for fruitful discussion of the article. We thank two journal reviewers: Prof. David Batten (The University of Manchester) and Dr Alexei Herman (Russian Academy of Sciences) for their valuable comments and suggestions. Additional support was provided to (A. Jurkowska) by the AGH University of Science and Technology, Statutory Founding (11.11.140.626). This research was supported financially by the Ministry of Science and Higher Education of Poland as part of the statutory activities of the Department of Plant Cytology and Embryology (B.J. Plachno) and Department of Taxonomy, Phytogeography and Palaeobotany (G. Pacyna, funds number K/ZDS/006305), Institute of Botany at the Jagiellonian University in Krakow.	Alexandrowicz S. 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Geol. Assoc.	APR	2018	129	2					159	170		10.1016/j.pgeola.2018.01.008	http://dx.doi.org/10.1016/j.pgeola.2018.01.008			12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	GH3AC					2025-03-11	WOS:000433272100005
J	Deaf, AS; Tahoun, SS				Deaf, Amr S.; Tahoun, Sameh S.			Integrated palynological, organic geochemical, and sequence stratigraphic analyses of the middle to upper Cenomanian hydrocarbon reservoir/source Abu Roash "G" Member: A depositional model in northwestern Egypt	MARINE AND PETROLEUM GEOLOGY			English	Article						Palynology; Palaeoenvironments; Organic geochemistry; Sequence stratigraphy; Hydrocarbon potential; Abu Roash "G"; North Western Desert; Egypt	NORTH-WESTERN DESERT; SEA-LEVEL CHANGES; MARINE CARBONATE PLATFORM; DINOFLAGELLATE CYSTS; CENTRAL SINAI; CRETACEOUS STRATIGRAPHY; TURONIAN FORAMINIFERA; MIXED CARBONATE; VOCONTIAN BASIN; EASTERN DESERT	The current investigation provides further insight into the petroliferous characteristics of the Abu Roash "G" Member, which is regarded as an important rock unit for the Egyptian oil industry. Forty-seven samples covering the "G" Member were selected from the BED 14-1 and BED 2-4 wells in the Abu Gharadig Basin and from the Abu Tunis IX well in the Matruh Basin, both of which are located in the north Western Desert. An independent dating of the "G" rocks of BED 2-4 by benthic foraminifera and ostracods, in addition to palynological dating, suggests a middle-late Cenomanian age and provides the biochronostratigraphic framework for the sequence stratigraphic analysis. Analysis of the vertical distribution of particulate organic matter defines three palynofacies types (PF). PF-1 represents the basal "G", where shales of the BED wells and calcareous shale of Abu Tunis IX were deposited during a relative sea level rise in an outer middle shelf environment that experienced a notable high primary productivity. Prevailing reducing (suboxic-anoxic) conditions supported preservation of very high amounts of amorphous organic matter (AOM) in PF-1. PF-2 is equated to shales of the middle "G" of BED 14-1 and BED 2-4 and to calcareous shales and limestone of the upper "G" in Abu Tunis IX. PF-2 was deposited during a relative sea level fall in an inner middle shelf setting under better-developed suboxic-anoxic conditions. PF-3 corresponds to the upper "G" of BED 14-1 and BED 2-4 and represents the shallowest setting, where sandy and silty shales were deposited during a pronounced sea level fall in an inner shelf environment. The same suboxic-anoxic conditions were prevailing during deposition of PF-3. Three bioevents were recorded, which could be of palaeoecological and/or biostratigraphic significance. These are Senegalinium aenigmaticum-Dinopterygium cladoides peak, Dinopterygium cladoides-Dinopterygium alatum peak, and an acme of ClassopoUis brasiliensis. Sequence stratigraphy of a transect of the four studied sections was carried out to understand the response of the particulate organic matter distribution and depositional system to the sea level changes. Three third-order, depositional genetic sequences were recognized and correlated with the global sea level curve (KCe 2, KCe 3, and KCe 4). The early highstand systems tract (eHST) of the genetically related KCe 3 in all wells is characterized by relatively rich organic matter, where combined remarkably low water circulation and insignificant dilution of organic matter with coarse terrigenous material probably supported good preservation of organic matter. Spatial distribution of the "G" rocks shows lateral facies changes. This was inferred from sedimentation of an organic-poor (avg. 0.8 TOC wt %), coarse clastic (sandy shales) facies in the studied area in Abu Gharadig Basin. Sedimentation changes laterally into a northeast and northwest organic-rich, finer clastic (shale, calcareous shales, and argillaceous limestone) facies in the western Matruh Basin. The robust anoxic conditions and very low dilution of organic matter by terrigenous influx enhanced the organic richness (avg. 2.4 TOC wt %) of these rocks, which resulted in the formation of promising hydrocarbon source rocks. Thus, for a successful hydrocarbon exploration in the north Western Desert, the promising source section of the "G" Member would be associated with shales, calcareous shales, and argillaceous limestone lithologies. Its depositional environment is mainly confined to outer middle and inner middle shelf settings that have widespread suboxic-anoxic conditions and show eHST pattern. In contrast, the regressive intervals that are denoted by the lowstand systems tract (LST) and/or the late HST (1HST) typify the relatively coarse elastics as good quality reservoir rocks that are characterized by poor organic richness due to dilution with terrigenous influx.	[Deaf, Amr S.] Assiut Univ, Dept Geol, Fac Sci, Assiut 71516, Egypt; [Tahoun, Sameh S.] Cairo Univ, Dept Geol, Fac Sci, Giza 12613, Egypt	Egyptian Knowledge Bank (EKB); Assiut University; Egyptian Knowledge Bank (EKB); Cairo University	Deaf, AS (通讯作者)，Assiut Univ, Dept Geol, Fac Sci, Assiut 71516, Egypt.	amr.daif@science.au.edu.eg	Deaf, Amr/AAF-6269-2020	Tahoun, Sameh S./0000-0002-0425-8848; Deaf, Amr/0000-0002-5073-7911				Abd-Elshafy E., 2002, Egyptian Journal of Paleontology, V2, P157; Al-Ameri TK, 1999, CRETACEOUS RES, V20, P359, DOI 10.1006/cres.1999.0157; Alaug AS, 2014, ARAB J GEOSCI, V7, P2515, DOI 10.1007/s12517-013-0961-y; Andreu B, 2002, ECLOGAE GEOL HELV, V95, P133; [Anonymous], 1993, SPECIAL PUBL INT ASS; [Anonymous], 1987, GEOLOGICAL SOC LONDO; [Anonymous], SEPM SOC SEDIMENTARY; [Anonymous], 1993, Source Rocks in a Sequence Stratigraphic Framework, V37, P67; [Anonymous], 1977, QUESTIONS PHYTOSTRAT; [Anonymous], 1961, COAL TYPOLOGY CHEM P; ARTHUR MA, 1990, NATO ADV SCI I C-MAT, V304, P75; ARTHUR MA, 1988, NATURE, V335, P714, DOI 10.1038/335714a0; BAPETCO, 1991, INT FIN REP CO UNPUB; BAPETCO, 1988, INT FIN REP CO UNPUB; Baskin DK, 1997, AAPG BULL, V81, P1437; Bassoullet J.P., 1969, R MICROPALEONTOL, V3, P130; Batten D. 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J	Taylor, KWR; Willumsen, PS; Hollis, CJ; Pancost, RD				Taylor, Kyle W. R.; Willumsen, Pi Suhr; Hollis, Christopher J.; Pancost, Richard D.			South Pacific evidence for the long-term climate impact of the Cretaceous/Paleogene boundary event	EARTH-SCIENCE REVIEWS			English	Article						TEX86; Cretaceous-Paleogene boundary; Paleoclimate; Paleoceanography; Geochemistry; Palynology; Organic geochemistry; Biostratigraphy; New Zealand; Southwest Pacific	GLYCEROL TETRAETHER LIPIDS; DINOFLAGELLATE CYST ZONATION; CHICXULUB ASTEROID IMPACT; TERTIARY BOUNDARY; CRETACEOUS/TERTIARY BOUNDARY; NEW-ZEALAND; WATER-COLUMN; PALEOGENE BOUNDARY; FLAXBOURNE RIVER; PALEOENVIRONMENTAL CHANGES	The Cretaceous/Paleogene (K/Pg) boundary is well-represented across a range of depositional settings in New Zealand. Trends in fossil assemblages and marine lithofacies indicate that the K/Pg event was followed by a pronounced and long-term (similar to 1 Myr) perturbation in climate and ocean conditions. These findings are supported by a TEX86-derived sea surface temperature (SST) reconstruction across the K/Pg boundary at mid-Waipara River, north Canterbury. The BAYSPAR calibration indicates that SST was very stable in the uppermost Cretaceous (similar to 020 degrees C), but abruptly warmed by similar to 4 degrees C in a 25 cm-thick lowermost Paleocene interval. This interval is overlain by a similar to 2 m thick interval in which SST abruptly cooled by similar to 10 degrees C and then progressively returned to similar to 20 degrees C. The basal Paleocene warm interval is associated with an acme in the dinoflagellate species Trithyrodiniwn evittii and the succeeding cool interval is associated with an acme in Palaeoperidinium pyrophorum. Biostratigraphic correlation of the shelfal mid-Waipara section to the pelagic K/Pg sections in Marlborough reveals that a significant unconformity separates these two acme events, with the T acme event occurring in the earliest Paleocene and the P. pyrophorum acme occurring similar to 1 Myr later and lasting similar to 200 kyr. A succession of dinoflagellate acme events within the intervening interval in the Marlborough sections implies unstable climatic and environmental conditions in the lead up to the P. pyrophorum acme and cooling event at similar to 65 Ma. This event also coincides with a peak in biogenic silica accumulation in the Marlborough sections. We suggest that disruption to biogeochemical pathways at the K/Pg boundary caused long-term climatic cooling in the southern Pacific region.	[Taylor, Kyle W. R.; Pancost, Richard D.] Univ Bristol, Cabot Inst, Organ Geochem Unit, Bristol BS8 1TS, Avon, England; [Taylor, Kyle W. R.; Pancost, Richard D.] Univ Bristol, Sch Chem, Bristol BS8 1TS, Avon, England; [Taylor, Kyle W. R.] Elementar UK Ltd, Isoprime House,Earl Rd, Cheadle SK8 6PT, England; [Willumsen, Pi Suhr] Aarhus Univ, Dept Geosci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Hollis, Christopher J.] GNS Sci, POB 30-368, Lower Hutt, New Zealand	University of Bristol; University of Bristol; Aarhus University; GNS Science - New Zealand	Taylor, KWR (通讯作者)，Univ Bristol, Cabot Inst, Organ Geochem Unit, Bristol BS8 1TS, Avon, England.; Taylor, KWR (通讯作者)，Univ Bristol, Sch Chem, Bristol BS8 1TS, Avon, England.; Taylor, KWR (通讯作者)，Elementar UK Ltd, Isoprime House,Earl Rd, Cheadle SK8 6PT, England.	kyle.taylor@elementar.co.uk	Hollis, Christopher/D-3560-2011	Hollis, Christopher John/0000-0001-8840-9852; Pancost, Richard/0000-0003-0298-4026	NERC; Royal Society Wolfson Research Merit Award; European Research Council (ERC) [340923]	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Royal Society Wolfson Research Merit Award(Royal Society); European Research Council (ERC)(European Research Council (ERC))	We thank Dr. Ian D. Bull of the Bristol Node of the Natural Environment Research Council (NERC) Life Sciences Mass Spectrometry Facility for technical assistance with respect to the instrumentation used for organic geochemical analysis. We thank James Eldrett, Yige Zhang, and Erica Crouch, whose critical comments contributed to a much improved manuscript. KWRT and RDP thank NERC for funding KWRT's PhD. CJH acknowledges the GNS Science Global Change through Time Programme. RDP acknowledges the Royal Society Wolfson Research Merit Award and funding from the European Research Council for T-GRES (FP/2007-2013 ERC Grant Agreement number 340923).	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J	Kang, W; Wang, ZH				Kang, Wei; Wang, Zhao-Hui			Identification of a marine woloszynskioid dinoflagellate <i>Biecheleriopsis adriatica</i> and germination of its cysts from southern Chinese coasts	JOURNAL OF ENVIRONMENTAL SCIENCES			English	Article						Biecheleriopsis adriatica; Cyst; Germination; Phylogeny; Southern China	SP-NOV; LAKE TOVEL; COMB. NOV; GEN. NOV.; DINOPHYCEAE; ULTRASTRUCTURE; SUESSIACEAE; AREAS	A strain of small-sized dinoflagellates, isolated from the culture of sediment incubation collected from the coastal areas in southern China, has been identified under microscopical observation and rDNA sequence. Surface sediments from two sea areas in the southern Chinese coastal waters were incubated for 20 and 40 days, and germinated vegetative cells were observed. The cells were identified as species in the Suessiaceae based on the morphological characteristics, ultrastructural features of the cell, as well as its swimming behavior. The studied strain clusters into a well-supported Glade together with six sequences of Biecheleriopsis adriatica in the phylogenetic tree based on the large subunit (LSU) rDNA sequence. Therefore, the strain has been identified as B. adriatica based on morphological observation and phylogenetic analysis. B. adriatica was the dominant dinoflagellate species in the germinated phytoplankton community from both sea areas, which contributed 50%-83% to the total germinated dinoflagellates averagely. However, B. adriatica has not been reported in previous phytoplankton surveys, and was probably ignored or misidentified due to its small size and thin wall. The frequent and abundant occurrence of B. adriatica in the germinated phytoplankton community of many sea areas of the southern Chinese coastal waters suggests its wide and abundant distribution in these sea areas. (C) 2017 The Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences. Published by Elsevier B.V.	[Kang, Wei] Chinese Acad Fishery Sci, East China Sea Fisheries Res Inst, Minist Agr China, Key & Open Lab Marina & Estuary Fisheries, Shanghai 200090, Peoples R China; [Wang, Zhao-Hui] Jinan Univ, Coll Life Sci & Technol, Key Lab Eutrophicat & Red Tide Prevent Guangdong, Guangzhou 510632, Guangdong, Peoples R China; [Wang, Zhao-Hui] Minist Educ, Engn Res Ctr Trop & Subtrop Aquat Ecol Engn, Guangzhou 510632, Guangdong, Peoples R China	Ministry of Agriculture & Rural Affairs; Chinese Academy of Fishery Sciences; East China Sea Fisheries Research Institute, CAFS; Jinan University	Wang, ZH (通讯作者)，Jinan Univ, Coll Life Sci & Technol, Key Lab Eutrophicat & Red Tide Prevent Guangdong, Guangzhou 510632, Guangdong, Peoples R China.; Wang, ZH (通讯作者)，Minist Educ, Engn Res Ctr Trop & Subtrop Aquat Ecol Engn, Guangzhou 510632, Guangdong, Peoples R China.	twzh@jnu.edu.cn	Kang, Wei/JUV-4778-2023	Chi, Hai/0000-0003-3072-511X	National Natural Foundation of China [41276154, 41476132]	National Natural Foundation of China(National Natural Science Foundation of China (NSFC))	The authors gratefully acknowledge Dr. Larry B. 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J	Gentzis, T; Carvajal-Ortiz, H; Deaf, A; Tahoun, SS				Gentzis, Thomas; Carvajal-Ortiz, Humberto; Deaf, Arnr; Tahoun, Sameh S.			Multi-proxy approach to screen the hydrocarbon potential of the Jurassic succession in the Matruh Basin, North Western Desert, Egypt	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article; Proceedings Paper	1st Joint Meeting of the 33rd Annual Meeting of the Society-for-Organic-Petrology (TSOP) / Meeting of the Palynological-Society (AASP) / Meeting of the International-Committee-for-Coal-and-Organic-Petrology (ICCP)	SEP 18-23, 2016	Houston, TX	Soc Organ Petrol, Palynol Soc, Int Comm Coal & Organ Petrol		Jurassic; Palynology; Vitrinite reflectance; Rock-Eval pyrolysis; Multi-proxy approach; Geochemical screening; Matruh Basin; Western Desert, Egypt	LOWER CRETACEOUS SEQUENCES; DINOFLAGELLATE CYST; EASTERN DESERT; SHOUSHAN BASIN; SHUSHAN BASIN; SOURCE ROCKS; STRATIGRAPHY; PETROLEUM; SYSTEM; PALYNOLOGY	This paper discusses the hydrocarbon potential of the Jurassic succession in a mature basin in Egypt as an important element of a larger petroleum system study. Prior to any organic petrographic and organic geo-chemical analyses, a palynological age dating of the originally undifferentiated Jurassic sequence was carried out to identify different formations under investigation. This was based on key bioevents of some recovered dinoflagellate cysts and the identified lithology. Palynological, TOC/Rock Eva] pyrolysis (including modified Rock-Eval methods), and vitrinite reflectance (VRo%) data from a total of 14 samples taken from the uppermost lower-upper Jurassic sequence represented by the Wadi Natrun (Toarcian-Aalenian), Khatatba (late Bathonian-Callovian), and Masajid (Oxfordian) formations in the Abu Tunis-1 x well, are presented. In addition, two samples from the Abu Tunis-1 x well and the proximal (similar to 32 km to the east) Siqueifa-1 x well, having the highest remaining hydrocarbon potential (S2 yields), were analyzed and their results were compared using modified pyrolysis programs. Although the data showed a good correlation between the TAI of the palynomorph assemblage, vitrinite reflectance, and Tmax from Rock-Eval pyrolysis in the shallower intervals, the correlation between VRo and Tmax was poor in the lower half of the studied succession (middle Khatatba and Wadi Natrun formations). The very low Tmax values indicate immature OM while VRo and TAI indicated middle stage of oil window to past peak oil generation. The reason for this discrepancy is that the deeper samples are reservoir rocks, not source rocks, and the majority of the organic matter is not composed of reactive kerogen but consists of migrated hydrocarbons and NSO compounds. Contamination due to oil-based mud (OBM) was eliminated because the Abu Tunis-1 x well was drilled in 1969, prior to the extensive use of OEM in drilling. This study showed that a multi-proxy approach is the best way to screen the hydrocarbon potential in a thick succession that contains interbedded source and reservoir rocks.	[Gentzis, Thomas; Carvajal-Ortiz, Humberto] Core Labs Inc, 6316 Windfern Rd, Houston, TX 77040 USA; [Deaf, Arnr] Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt; [Tahoun, Sameh S.] Cairo Univ, Fac Sci, Dept Geol, Giza 12613, Egypt	Egyptian Knowledge Bank (EKB); Assiut University; Egyptian Knowledge Bank (EKB); Cairo University	Gentzis, T (通讯作者)，Core Labs Inc, 6316 Windfern Rd, Houston, TX 77040 USA.	thomas.gentzis@corelab.com	Deaf, Amr/AAF-6269-2020	Tahoun, Sameh S./0000-0002-0425-8848; Carvajal, Humberto/0000-0002-8021-5954; Deaf, Amr/0000-0002-5073-7911				Aboul Ela N.M., 1990, EARTH SCI SER, V4, P95; Aboul Ela N.M., 2010, P 5 INT C GEOLOGY TE, P85; About Ela N. 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J. Coal Geol.	APR 1	2018	190				SI		29	41		10.1016/j.coal.2017.12.001	http://dx.doi.org/10.1016/j.coal.2017.12.001			13	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Energy & Fuels; Geology	GE4BQ					2025-03-11	WOS:000431159700003
J	Schneebeli-Hermann, E; Looser, N; Hochuli, PA; Furrer, H; Reisdorf, AG; Wetzel, A; Bernasconi, SM				Schneebeli-Hermann, Elke; Looser, Nathan; Hochuli, Peter A.; Furrer, Heinz; Reisdorf, Achim G.; Wetzel, Andreas; Bernasconi, Stefano M.			Palynology of Triassic-Jurassic boundary sections in northern Switzerland	SWISS JOURNAL OF GEOSCIENCES			English	Article						Triassic; Jurassic; Palynology; Palaeoenvironment; Switzerland	TERRESTRIAL ECOSYSTEM CHANGE; SEA-LEVEL CHANGES; MASS EXTINCTIONS; EUROPE; AUSTRIA; STRATIGRAPHY; TAPHONOMY; PATTERNS; RECORD; MIDDLE	A first palynostratigraphic scheme of Upper Triassic deposits in northern Switzerland was established based on spore-pollen associations and dinoflagellate cyst records from the upper part of the Upper Triassic Klettgau Formation and the lower part of the Lower Jurassic Staffelegg Formation. Drill cores from the Adlerberg region (Basel Tabular Jura) and from Weiach (northern part of Canton Zurich) as well as from an outcrop at the Chilchzimmersattel (Basel Folded Jura) were studied and five informal palynological associations are distinguished. These palynological associations correlate with palynological association of the Central European Epicontinental Basin and the Tethyan realm and provide a stratigraphic framework for the uppermost Triassic sediments in northern Switzerland. Throughout the uppermost Triassic to Jurassic palynological succession a remarkable prominence of Classopollis spp. is observed. Besides Classopollis spp. the three Rhaetian palynological associations A to C from the Upper Triassic Belchen Member include typical Rhaetian spore-pollen and dinoflagellate taxa (e.g., Rhaetipollis germanicus, Geopollis zwolinskae, Rhaetogonyaulax rhaetica, and Dapcodinium priscum). Association B differs from association A in a higher relative abundance of the sporomorph taxa Perinopollenites spp. and the consistent occurrence of Granuloperculatipollis rudis and Ricciisporites tuberculatus. Spore diversity is highest in the late Rhaetian palynological association C and includes Polypodiisporites polymicroforatus. A Rhaetian age for the Belchen Member is confirmed by palynological associations A-C, but there is no record of the latest Rhaetian and the earliest Jurassic. In contrast to the Rhaetian palynological associations the Early Jurassic associations W and D include Pinuspollenites spp., Trachysporites fuscus (in association W), and Ischyosporites variegatus. In the view of the end-Triassic mass extinction and contemporaneous environmental changes the described palynofloral succession represents the pre-extinction phase (associations A and B) including a distinct transgression, the extinction phase (association C) associated with a regression, and the post-extinction phase (association W).	[Schneebeli-Hermann, Elke; Hochuli, Peter A.; Furrer, Heinz] Univ Zurich, Inst & Museum Palaeontol, Karl Schmid Str 4, CH-8006 Zurich, Switzerland; [Looser, Nathan; Bernasconi, Stefano M.] Swiss Fed Inst Technol, Dept Earth Sci, Sonneggstr 5, CH-8092 Zurich, Switzerland; [Reisdorf, Achim G.; Wetzel, Andreas] Univ Basel, Geol Palaontol Inst, Bernoullistr 32, CH-4056 Basel, Switzerland	University of Zurich; Swiss Federal Institutes of Technology Domain; ETH Zurich; University of Basel	Schneebeli-Hermann, E (通讯作者)，Univ Zurich, Inst & Museum Palaeontol, Karl Schmid Str 4, CH-8006 Zurich, Switzerland.	Elke.Schneebeli@pim.uzh.ch	Schneebeli, Elke/F-4873-2011; Bernasconi, Stefano/E-5394-2010	Schneebeli, Elke/0000-0002-1552-4785; Bernasconi, Stefano/0000-0001-7672-8856				Abbink O.A., 1998, Palynological investigations in the Jurassic of the North Sea region, V8; Abbink OA, 2004, NETH J GEOSCI, V83, P17, DOI 10.1017/S0016774600020436; ACHILLES H, 1986, ECLOGAE GEOL HELV, V79, P149; Barbacka M, 2017, PALAEOGEOGR PALAEOCL, V480, P80, DOI 10.1016/j.palaeo.2017.05.024; Batten D.J., 1996, Palynology: principles and applications, V2, P795; Bonis NR, 2009, REV PALAEOBOT PALYNO, V156, P376, DOI 10.1016/j.revpalbo.2009.04.003; BRENNER W., 1986, Neues Jahrbuch fur Geologie und Paleontologie Abhandlungen, V173, P131; Etter W., 2016, SWISS GEOSC M ABSTR, P144; Etzold A., 2010, LGRB- Informationen, V25, P105; Felber P., 2006, KLASSISCHE FOSSILIEN; FISCHER H, 1964, TATIGKEITSBERICHTE N, V24, P93; Fischer J, 2012, PALAEOGEOGR PALAEOCL, V353, P60, DOI 10.1016/j.palaeo.2012.07.002; Galli MT, 2005, PALAEOGEOGR PALAEOCL, V216, P203, DOI 10.1016/j.palaeo.2004.11.009; Hallam A, 2001, PALAEOGEOGR PALAEOCL, V167, P23, DOI 10.1016/S0031-0182(00)00229-7; Hallam A, 1999, EARTH-SCI REV, V48, P217, DOI 10.1016/S0012-8252(99)00055-0; Heer O., 1865, NEUJAHRSBLATT NATURF; Hesselbo SP, 2004, J GEOL SOC LONDON, V161, P365, DOI 10.1144/0016-764903-033; Hesselbo SP, 2002, GEOLOGY, V30, P251, DOI 10.1130/0091-7613(2002)030<0251:TAMEAT>2.0.CO;2; Heunisch C., 1999, TRIAS GANZ ANDERE WE, P207; Heunisch Carmen, 1996, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V200, P87; Hillebrandt AV, 2013, EPISODES, V36, P162, DOI 10.18814/epiiugs/2013/v36i3/001; Hochuli P.A., 1989, CORRELATION HYDROCAR, P131; JORDAN P, 1983, ECLOGAE GEOL HELV, V76, P355; Jordan P, 2016, SWISS J GEOSCI, V109, P257, DOI 10.1007/s00015-016-0218-3; Krausel R., 1955, SCHWEIZER PALAONTOL, V71, P1; Krausel R., 1966, SCHWEIZERISCHE PAL O, V84, P1; Krausel R., 1959, ABHANDLUNGEN SCHWEIZ, V77, P1; Kürschner WM, 2010, GEOL SOC SPEC PUBL, V334, P263, DOI 10.1144/SP334.11; Leschik G., 1955, ABHANDLUNGEN SCHWEIZ, V72, P1; Leuthardt F., 1904, ABH SCHWEIZ PALAONTO, V31, P24; Leuthardt F., 1903, ABHANDLUNGEN SCHWEIZ, V30, P1; Lindström S, 2017, PALAEOGEOGR PALAEOCL, V478, P80, DOI 10.1016/j.palaeo.2016.12.025; Lindström S, 2016, GEOL MAG, V153, P223, DOI 10.1017/S0016756815000552; Lindström S, 2012, GEOLOGY, V40, P531, DOI 10.1130/G32928.1; Looser N., 2017, SWISS J GEOSCI UNPUB; Lund J.J., 1977, DANMARKS GEOLOGISKE, V109, P103, DOI DOI 10.34194/RAEKKE2.V109.6900; Maisch MW, 2008, SWISS J GEOSCI, V101, P617, DOI 10.1007/s00015-008-1299-4; Matter A., 1988, BEITRAGE ZH GEOLOGIE, V73, P1; Meyer CA, 1995, ECLOGAE GEOL HELV, V88, P711; Meyer M., 2001, Bulletin Fur Angewandte Geologie, V6, P199; Nagra, 2001, Nagra Technical Report NTB 00-01; Nitsch E, 2005, NEWSL STRATIGR, V41, P225, DOI 10.1127/0078-0421/2005/0041-0225; RAUP DM, 1982, SCIENCE, V215, P1501, DOI 10.1126/science.215.4539.1501; Reisdorf AG, 2011, SWISS J GEOSCI, V104, P97, DOI 10.1007/s00015-011-0057-1; Riding JB, 2010, REV PALAEOBOT PALYNO, V162, P543, DOI 10.1016/j.revpalbo.2010.07.008; Ruhl M, 2009, EARTH PLANET SC LETT, V281, P169, DOI 10.1016/j.epsl.2009.02.020; SANDER PM, 1992, PALAEOGEOGR PALAEOCL, V93, P255; SCHEURING B W, 1970, Schweizerische Palaeontologische Abhandlungen, V88, P1; Schlatter R., 1983, MITTEILUNGEN NATURFO, V32, P159; Schlatter R., 1975, GEOLOGISCHE PA UNPUB; SCHUURMAN WML, 1979, REV PALAEOBOT PALYNO, V27, P53, DOI 10.1016/0034-6667(79)90044-7; Stampfli GM, 2006, GEOL SOC MEM, V32, P57, DOI 10.1144/GSL.MEM.2006.032.01.04; Tanner KM, 1978, B SCHWEIZERISCHEN VE, V44, P13; Traverse A., 2007, NATURE GEOSCIENCE, V2, P589; Visscher H., 1980, P INT PALYN C 4 LUCK, V2, P281; WEISS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V215, P1; Woollam R., 1983, 832 I GEOL; Ziegler P.A., 1990, GEOLOGICAL ATLAS W C	58	9	11	0	11	SPRINGER BASEL AG	BASEL	PICASSOPLATZ 4, BASEL, 4052, SWITZERLAND	1661-8726	1661-8734		SWISS J GEOSCI	Swiss J. Geosci.	APR	2018	111	1-2					99	115		10.1007/s00015-017-0286-z	http://dx.doi.org/10.1007/s00015-017-0286-z			17	Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	GD7PX					2025-03-11	WOS:000430705600006
J	Matsuoka, K; Ikeda, Y; Kaga, S; Kaga, Y; Ogata, T				Matsuoka, Kazumi; Ikeda, Yuri; Kaga, Shinnosuke; Kaga, Yoshimasa; Ogata, Takehiko			Repercussions of the Great East Japan Earthquake tsunami on ellipsoidal <i>Alexandrium cysts</i> (Dinophyceae) in Ofunato Bay, Japan	MARINE ENVIRONMENTAL RESEARCH			English	Article						Alexandrium cyst; Great East Japan Earthquake; Ofunato Bay; Sediment; Paralytic shellfish poisoning; Chilean tsunami	SETO-INLAND SEA; TAMARENSE RESTING CYSTS; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; KESENNUMA BAY; TOXIC DINOFLAGELLATE; IWATE PREFECTURE; SPP. DINOPHYCEAE; DISASTER 3.11; MOUNE BAY	Shellfish aquaculture in Ofunato Bay, Northeast Japan, was seriously damaged by a tsunami generated by the Great East Japan Earthquake, March 11th, 2011, accompanied by paralytic shellfish poisoning (PSP) outbreaks caused by Alexandrium tamarense (Dinophyceae). To understand longer future trends of PSP, an investigation was made of the historical occurrence and causes of Alexandrium outbreaks after the tsunami. Vertical distributions of Alexandrium cysts in two sediment-cores from Ofunato Bay revealed that the sediments above ca. 25 cm were eroded, re-suspended and re-deposited, and they included unusually abundant Alexandrium cysts. This abundance of cysts was due to re-deposition of older sediments by the tsunami. The first Ofunato Bay PSP incident was in 1961 after the Chilean Earthquake tsunami and was probably caused by similar unusual blooms of Alexandrium germinated from older sediments as the Great East Japan tsunami, together with nutrient enrichment because of population increase at the start of shellfish aquaculture.	[Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan; [Ikeda, Yuri; Ogata, Takehiko] Kitasato Univ, Sch Marine Biosci, Minami Ku, 1-15-1 Kitasato, Sagamihara, Kanagawa 2520373, Japan; [Kaga, Shinnosuke] Iwate Prefectural Govt, 10-1 Uchimaru, Morioka, Iwate 0208570, Japan; [Kaga, Yoshimasa] Iwate Fisheries Technol Ctr, 3-75-3 Hirata, Kamaishi, Iwate 0260001, Japan; [Matsuoka, Kazumi] 1403,370-2 Kuzetakada Cho,Minami Ku, Kyoto 6018211, Japan	Nagasaki University; Kitasato University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst East China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.; Matsuoka, K (通讯作者)，1403,370-2 Kuzetakada Cho,Minami Ku, Kyoto 6018211, Japan.	kazu-mtk@nagasaki-u.ac.jp; yikeda@kitasato-u.ac.jp; s-kaga@pref.iwate.jp; y-kaga@pref.iwate.jp; t.ogata@kitasato-u.ac.jp		Kaga, Shinnosuke/0000-0001-7066-4142	Sustainable Aquatic Food and Environment Project in the East China Sea (SAFE) Project in Nagasaki University; research project funds, Tohoku Ecosystem-Associated Marine Science Project (Ministry of Education, Culture, Sports, Science, and Technology)	Sustainable Aquatic Food and Environment Project in the East China Sea (SAFE) Project in Nagasaki University; research project funds, Tohoku Ecosystem-Associated Marine Science Project (Ministry of Education, Culture, Sports, Science, and Technology)	We sincerely express our acknowledgements to Dr. Petra Mudie, Geological Survey, Canada for her constructive suggestion and comments to the earlier manuscript. This research was partly supported by the Sustainable Aquatic Food and Environment Project in the East China Sea (SAFE) Project in Nagasaki University and the research project funds, Tohoku Ecosystem-Associated Marine Science Project (Ministry of Education, Culture, Sports, Science, and Technology).	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J	McCarthy, FMG; Gu, HF; Mertens, KN; Carbonell-Moore, C; Krueger, AM; Takano, Y; Matsuoka, K				McCarthy, Francine M. G.; Gu, Haifeng; Mertens, Kenneth N.; Carbonell-Moore, Consuelo; Krueger, Andrea M.; Takano, Yoshihito; Matsuoka, Kazumi			Transferring the freshwater dinoflagellate <i>Peridinium wisconsinense</i> (Dinophyceae) to the family Thoracosphaeraceae, with the description of <i>Fusiperidinium</i> gen. nov.	PHYCOLOGICAL RESEARCH			English	Article						Fusiperidinium wisconsinense; internal transcribed spacer; Peridiniales; phylogeny; SSU and LSU rDNA; tabulation	MIXED MODELS; CYSTS; LAKE; MARINE; PHYLOGENY; PRESERVATION; EVOLUTION; TAXONOMY; GERMANY; CLARKIA	Distinctive spindle-shaped thecae first described by Samuel Eddy in 1930 and assigned to the genus Peridinium Ehrenberg are commonly reported from freshwater environments in eastern North America. We demonstrate that thecae incubated from cysts of Peridinium wisconsinense Eddy have six cingular plates and a protuberant apical pore complex characteristic of the family Thoracosphaeraceae Schiller 1930 emend. Tangen in Tangen et al. 1982. Small subunit ribosomal DNA (SSU rDNA) and internal transcribed spacer (ITS) sequences confirm the close genetic similarity with Chimonodinium lomnickii (Wooszyska) Craveiro, Calado, Daugbjerg, Gert Hansen & Moestrup and with species recently reassigned to the genus Apocalathium Craveiro, Daugbjerg, Moestrup & Calado that was inferred from previously published LSU rDNA analysis of cysts of P. wisconsinense. Despite sharing identical tabulation with the thoracosphaeracean genera Chimonodinium Craveiro, Calado, Daugbjerg, Gert Hansen & Moestrup and Apocalathium, substantial morphological differences in the morphology of both the thecate and cyst stages of P. wisconsinense led us to reassign this species to the genus Fusiperidinium gen. nov. The phylogenetic position of Fusiperidinium wisconsinense comb. nov., inferred from concatenated data of SSU and LSU sequences, suggests that it evolved from the brackish Scrippsiella lineage, independently of the transition that produced the family Peridiniaceae. Cysts described as Geiselodinium tyonekensis Engelhardt from nonmarine strata from Alaska are apparently identical to the resistant cysts produced by F. wisconsinense. The palynologically-constrained late Middle Miocene age for the Tyonek Formation provides a minimum age of 11.6Ma for the evolution of this lineage, coinciding with a rapid glacioeustatic decline in sea level. Our findings also call into question the inclusion of the family Thoracosphaeraceae within the order Peridiniales Haeckel.	[McCarthy, Francine M. G.] Brock Univ, Earth Sci, St Catharines, ON, Canada; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen, Peoples R China; [Mertens, Kenneth N.] IFREMER, LER BO, Concarneau, France; [Carbonell-Moore, Consuelo] Oregon State Univ, Dept Bot & Plant Pathol, Coll Agr Sci, Corvallis, OR 97331 USA; [Krueger, Andrea M.] Brock Univ, Biol Sci, St Catharines, ON, Canada; [Takano, Yoshihito; Matsuoka, Kazumi] Inst East China Sea Res ECSER, Nagasaki, Japan	Brock University; Third Institute of Oceanography, Ministry of Natural Resources; Ifremer; Oregon State University; Brock University	McCarthy, FMG (通讯作者)，Brock Univ, Earth Sci, St Catharines, ON, Canada.	fmccarthy@brocku.ca	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	NSERC Discovery Grant; Sigma 300 FE-SEM of the station of Marine Biology in Concarneau	NSERC Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); Sigma 300 FE-SEM of the station of Marine Biology in Concarneau	We thank M. Drljepan (Western U) for her photomicrograph of C. lomnickii, O. Volik (U Waterloo) and K. Michels (U Wisconsin - Madison) for assistance with photomicrographs and M. Lozon (Brock U.) for assistance with drafting. The input of N. Chomerat (Ifremer) regarding nomenclature is appreciated, as are suggestions of delegates at DINO11, notably K. Dybkjaer and R. Fensome. We are also grateful to AASP-The Palynological Society for allowing us to reproduce Plate 1 of Engelhardt (1976) in Appendix S2, Supporting Information. This work was funded in part by an NSERC Discovery Grant to FMGM and facilitated by staff at the Dorset Environmental Research Centre. The Regional Council of Brittany, the General Council of Finistere and the urban community of Concarneau-Cornouaille-Agglomeration are acknowledged for the funding of the Sigma 300 FE-SEM of the station of Marine Biology in Concarneau. 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J	Awad, WK; Oboh-Ikuenobe, FE				Awad, Walaa K.; Oboh-Ikuenobe, Francisca E.			Late Paleogene-early Neogene dinoflagellate cyst biostratigraphy of the eastern Equatorial Atlantic	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Dinoflagellate cysts; Late Paleogene-early Neogene; Biostratigraphy; West Africa	NORTH-SEA BASIN; MIDDLE MIOCENE; CALCAREOUS NANNOFOSSILS; OLIGOCENE; ZONATION; EOCENE; STRATIGRAPHY; CALIBRATION; TRANSITION; EVENTS	Six dinoflagellate cyst biozones (zone 1-zone 5, subzones 1a and 1b) are recognized in the late Paleogene-early Neogene interval of the Ocean Drilling Program (ODP) Site 959 (Hole 959 A), Cote d'Ivoire-Ghana Transform Margin in the eastern Equatorial Atlantic. The biozones are based on palynological analysis of 30 samples covering a 273.2-m interval with generally fair preservation and good to poor recovery. We propose a new age of Late Eocene (Priabonian) for subunit LIB as opposed to the previously published mid-Early Oligocene age (middle Rupelian). This age assignment is mainly based on the presence of Late Eocene marker taxa, such as Hemiplacophora semilunifera and Schematophora speciosa in the lower part of the studied interval. We also document for the first time a hiatus event within dinoflagellate cyst zone 3, based on the last occurrences of several taxa. This interval is assigned to an Early Miocene age and is barren of other microfossils. Furthermore, we propose new last occurrences for two species. The last occurrence of Cerebrocysta bartonensis is observed in the late Aquitanian-early Burdigalian in this study vs. Priabonian-early Rupelian in mid and high latitude regions. Also, the last occurrence of Chiropteridium galea extends to the latest Early Miocene (Burdigalian) in ODP Hole 959 A; this event was previously identified in other studies as Chattian in equatorial regions, and Aquitanian in the Northern Hemisphere mid-latitudes. We suspect that these differences are due to physical (offshore vs. nearshore) and latitudinal locations of the areas studied. (C) 2018 Elsevier Ltd. All rights reserved.	[Awad, Walaa K.; Oboh-Ikuenobe, Francisca E.] Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Geol & Geophys Program, 129 McNutt Hall, Rolla, MO 65409 USA	University of Missouri System; Missouri University of Science & Technology	Awad, WK (通讯作者)，Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Geol & Geophys Program, 129 McNutt Hall, Rolla, MO 65409 USA.	wka9tb@mst.edu			Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology	Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology	We would like to acknowledge the Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology for funding this study. We would like to thank Dr. Javier Helenes, an anonymous reviewer and the journal editor Prof. Mohamed Abdelsalam for the detailed comments and useful suggestions that improved the manuscript.	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J	Huang, XG; Li, SX; Liu, FJ; Lan, WR				Huang, Xu-Guang; Li, Shun-xing; Liu, Feng-Jiao; Lan, Wang-Rong			Regulated effects of <i>Prorocentrum donghaiense</i> Lu exudate on nickel bioavailability when cultured with different nitrogen sources	CHEMOSPHERE			English	Article						Nickel; Bioavailability; Toxicity; Exudation; Metal speciation	TOXIC DINOFLAGELLATE ALEXANDRIUM; DIFFERENT MARINE-ALGAE; EMILIANIA-HUXLEYI; GREEN-ALGA; SKELETONEMA-COSTATUM; ORGANIC-CARBON; ZINC UPTAKE; NI UPTAKE; PHYTOPLANKTON; COPPER	Exudates by marine phytoplankton and metals coexist in the seawater, but little is known about their interaction. In this study, cultures of Prorocentrum donghaiense Lu were grown in urea and ammonium, and then exposed to different Ni ion levels in order to study the effects of Ni ions on algal growth. The regulatory mechanisms of P. donghaiense Lu for coping with different Ni ion levels was investigating by characterizing dissolved organic carbon (DOC), carbohydrate and protein content released per cell, hydropathy properties (hydrophilic and hydrophobic fractions) and thiol compounds (cysteine-like or glutathione-like). Lower levels of Ni ions (pNi>10.0) significantly promoted the growth of P. donghaiense Lu when incubated in urea; however, the same was not true for P. donghaiense Lu cultivated in ammonium. An increased presence of hydrophobic fractions and thiol compounds (cysteine-like or glutathione-like compounds) induced by low Ni ions (pNi>10.0) in urea cultures suggest that the activation of cellular mechanisms in response to insufficient Ni ion stress enhances Ni bioavailability. Furthermore, the abundance of carbohydrates and proteins released by cells when exposed to higher Ni ions levels (from pNi = 10.0 to pNi = 8.0) both in urea and ammonium cultures suggests that algal cells may utilize exudate to complex Ni cations and reduce their toxicity. Therefore, it can be speculated that phytoplankton can produce large amounts of specific exudate, which may accelerate the metal bioavailability (insufficient levels) and reduce metal toxicity (excess levels) to maintain an equilibrium with metals in the environment. (C) 2018 Elsevier Ltd. All rights reserved.	[Huang, Xu-Guang; Li, Shun-xing; Lan, Wang-Rong] Minnan Normal Univ, Coll Chem & Environm Sci, Zhangzhou 363000, Peoples R China; [Huang, Xu-Guang; Li, Shun-xing] Minnan Normal Univ, Fujian Prov Key Lab Modern Analyt Sci & Separat T, Zhangzhou 363000, Peoples R China; [Li, Shun-xing; Liu, Feng-Jiao] Xiamen Univ, Minist Educ, Key Lab Coastal & Wetland Ecosyst, Xiamen 361005, Peoples R China	MinNan Normal University; MinNan Normal University; Xiamen University	Huang, XG (通讯作者)，Minnan Normal Univ, Coll Chem & Environm Sci, Zhangzhou 363000, Peoples R China.	huangxuguang@munu.edu.cn	Liu, Fengjiao/AAO-7998-2020		National Natural Science Foundation of China [41206096, 40506020]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This work was supported by the National Natural Science Foundation of China (41206096 and 40506020).	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J	Donders, TH; van Helmond, NAGM; Verreussel, R; Munsterman, D; ten Veen, J; Speijer, RP; Weijers, JH; Sangiorgi, F; Peterse, F; Reichart, GJ; Damsté, JSS; Lourens, L; Kuhlmann, G; Brinkhuis, H				Donders, Timme H.; van Helmond, Niels A. G. M.; Verreussel, Roel; Munsterman, Dirk; ten Veen, Johan; Speijer, Robert P.; Weijers, JohanW. H.; Sangiorgi, Francesca; Peterse, Francien; Reichart, Gert-Jan; Damste, Jaap S. Sinninghe; Lourens, Lucas; Kuhlmann, Gesa; Brinkhuis, Henk			Land-sea coupling of early Pleistocene glacial cycles in the southern North Sea exhibit dominant Northern Hemisphere forcing	CLIMATE OF THE PAST			English	Article							TERRESTRIAL ORGANIC-MATTER; DINOFLAGELLATE CYSTS; LATE PLIOCENE; LATE NEOGENE; ICE-SHEET; ISOTOPE STRATIGRAPHY; POLLEN TRANSPORT; ATLANTIC-OCEAN; CLIMATE; QUATERNARY	We assess the disputed phase relations between forcing and climatic response in the early Pleistocene with a spliced Gelasian (similar to 2.6-1.8 Ma) multi-proxy record from the southern North Sea basin. The cored sections couple climate evolution on both land and sea during the intensification of Northern Hemisphere glaciation (NHG) in NW Europe, providing the first well-constrained stratigraphic sequence of the classic terrestrial Praetiglian stage. Terrestrial signals were derived from the Eridanos paleoriver, a major fluvial system that contributed a large amount of freshwater to the northeast Atlantic. Due to its latitudinal position, the Eridanos catchment was likely affected by early Pleistocene NHG, leading to intermittent shutdown and reactivation of river flow and sediment transport. Here we apply organic geochemistry, palynology, carbonate isotope geochemistry, and seismostratigraphy to document both vegetation changes in the Eridanos catchment and regional surface water conditions and relate them to early Pleistocene glacial-interglacial cycles and relative sea level changes. Paleomagnetic and palynological data provide a solid integrated timeframe that ties the obliquity cycles, expressed in the borehole geophysical logs, to Marine Isotope Stages (MIS) 103 to 92, independently confirmed by a local benthic oxygen isotope record. Marine and terrestrial palynological and organic geochemical records provide high-resolution reconstructions of relative terrestrial and sea surface temperature (TT and SST), vegetation, relative sea level, and coastal influence. During the prominent cold stages MIS 98 and 96, as well as 94, the record indicates increased non-arboreal vegetation, low SST and TT, and low relative sea level. During the warm stages MIS 99, 97, and 95 we infer increased stratification of the water column together with a higher percentage of arboreal vegetation, high SST, and relative sea level maxima. The early Pleistocene distinct warm-cold alterations are synchronous between land and sea, but lead the relative sea level change by 3000-8000 years. The record provides evidence for a dominantly Northern Hemisphere-driven cooling that leads the glacial buildup and varies on the obliquity timescale. Southward migration of Arctic surface water masses during glacials, indicated by cool-water dinoflagellate cyst assemblages, is furthermore relevant for the discussion on the relation between the intensity of the Atlantic meridional overturning circulation and ice sheet growth.	[Donders, Timme H.] Univ Utrecht, Fac Geosci, Dept Phys Geog, Heidelberglaan 2, NL-3584 CD Utrecht, Netherlands; [Donders, Timme H.; Verreussel, Roel] Netherlands Org Appl Sci Res, TNO Appl Geosci, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [van Helmond, Niels A. G. M.; Weijers, JohanW. H.; Sangiorgi, Francesca; Peterse, Francien; Reichart, Gert-Jan; Damste, Jaap S. Sinninghe; Lourens, Lucas; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Munsterman, Dirk; ten Veen, Johan] Netherlands Org Appl Sci Res, TNO Geol Survey Netherlands, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [Speijer, Robert P.] Katholieke Univ Leuven, Dept Earth & Environm Sci, B-3001 Heverlee, Belgium; [Reichart, Gert-Jan; Damste, Jaap S. Sinninghe; Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands; [Kuhlmann, Gesa] Geozentrum Hannover, BGR Fed Inst Geosci & Nat Resources, Stilleweg 2, D-30655 Hannover, NH, Germany; [Weijers, JohanW. H.] Shell Global Solut Int BV, Grasweg 31, NL-1031 HW Amsterdam, Netherlands	Utrecht University; Netherlands Organization Applied Science Research; Utrecht University; Netherlands Organization Applied Science Research; KU Leuven; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Royal Dutch Shell	Donders, TH (通讯作者)，Univ Utrecht, Fac Geosci, Dept Phys Geog, Heidelberglaan 2, NL-3584 CD Utrecht, Netherlands.; Donders, TH (通讯作者)，Netherlands Org Appl Sci Res, TNO Appl Geosci, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands.	t.h.donders@uu.nl	Donders, Timme/J-5044-2012; Speijer, Robert/H-5073-2016; Brinkhuis, Henk/IUO-8165-2023; Peterse, Francien/AAY-1473-2021; Damste, Jaap/F-6128-2011; Peterse, Francien/H-5627-2011; Reichart, Gert-Jan/N-6308-2018	Sangiorgi, Francesca/0000-0003-4233-6154; van Helmond, Niels/0000-0003-0024-7217; Peterse, Francien/0000-0001-8781-2826; Reichart, Gert-Jan/0000-0002-7256-2243; Donders, Timme/0000-0003-4698-3463; Brinkhuis, Henk/0000-0003-0253-6610; Speijer, Robert/0000-0002-5873-7203	Chevron Exploration and Production Netherlands B.V.; Total E&P Nederland B.V.; Dana Petroleum Netherlands B.V.; Oranje-Nassau Energie B.V.; Energie Beheer Nederland (EBN); Netherlands Earth System Science Center (NESSC) from Dutch Ministry for Education, Culture, and Science [NWO 024.002.001]	Chevron Exploration and Production Netherlands B.V.; Total E&P Nederland B.V.; Dana Petroleum Netherlands B.V.; Oranje-Nassau Energie B.V.; Energie Beheer Nederland (EBN); Netherlands Earth System Science Center (NESSC) from Dutch Ministry for Education, Culture, and Science	We are grateful for the constructive comments of Stijn de Schepper and David Naafs and an anonymous referee that helped to improve the paper. We gratefully acknowledge the support in providing the offshore samples to this study and permission to publish from Wintershall Noordzee B.V. and project support from partners Chevron Exploration and Production Netherlands B.V., Total E&P Nederland B.V., Dana Petroleum Netherlands B.V., Oranje-Nassau Energie B.V., and Energie Beheer Nederland (EBN). Arnold van Dijk is thanked for running C / N and stable isotope analyses and Giovanni Dammers for processing palynological samples. The work was partly supported by funding from the Netherlands Earth System Science Center (NESSC) through a gravitation grant (NWO 024.002.001) from the Dutch Ministry for Education, Culture, and Science to Jaap S. Sinninghe Damste, Gert-Jan Reichart, and Lucas Lourens.	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MAR 23	2018	14	3					397	411		10.5194/cp-14-397-2018	http://dx.doi.org/10.5194/cp-14-397-2018			15	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	GA6TH		Green Published, gold, Green Submitted, Green Accepted			2025-03-11	WOS:000428466600001
J	Figueroa, RI; Estrada, M; Garcés, E				Isabel Figueroa, Rosa; Estrada, Marta; Garces, Esther			Life histories of microalgal species causing harmful blooms: Haploids, diploids and the relevance of benthic stages	HARMFUL ALGAE			English	Article						Harmful algal species; Life history; Harmful algal blooms; Environmental and physiological factors; Resting stages; Management; Models	DINOFLAGELLATE GYMNODINIUM-CATENATUM; HETEROSIGMA-AKASHIWO RAPHIDOPHYCEAE; FIBROCAPSA-JAPONICA RAPHIDOPHYCEAE; RESTING CYSTS; ALEXANDRIUM-TAMARENSE; ALGAL BLOOMS; COCHLODINIUM-POLYKRIKOIDES; AKINETE DIFFERENTIATION; POPULATION-DYNAMICS; SEXUAL REPRODUCTION	In coastal and offshore waters, Harmful Algal Blooms (HABs) currently threaten the well-being of coastal countries. These events, which can be localized or involve wide-ranging areas, pose risks to human health, marine ecosystems, and economic resources, such as tourism, fisheries, and aquaculture. Dynamics of HABs vary from one site to another, depending on the hydrographic and ecological conditions. The challenge in investigating HABs is that they are caused by organisms from multiple algal classes, each with its own unique features, including different life histories. The complete algal life cycle has been determined in <1% of the described species, although elucidation of the life cycles of bloom forming species is essential in developing preventative measures. The knowledge obtained thus far has confirmed the complexity of the algal life cycle, which is composed of discrete life stages whose morphology, ecological niche (plankton(benthos), function, and lifespan vary. The factors that trigger transitions between the different stages in nature are mostly unknown, but it is clear that an understanding of this process provides the key to effectively forecasting bloom recurrence, maintenance, and decline. Planktonic stages constitute an ephemeral phase of the life cycle of most species whereas resistant, benthic stages enable a species to withstand adverse conditions for prolonged periods, thus providing dormant reservoirs for eventual blooms and facilitating organismal dispersal. Here we review current knowledge of the life cycle strategies of major groups of HAB producers in marine and brackish waters. Rather than providing a comprehensive discussion, the objective was to highlight several of the research milestones that have changed our understanding of the plasticity and frequency of the different life cycle stages as well as the transitions between them. We also discuss the relevance of benthic and planktonic forms and their implications for HAB dynamics. (C) 2018 Published by Elsevier B.V.	[Isabel Figueroa, Rosa] CO Vigo, IEO, Vigo 36280, Spain; [Isabel Figueroa, Rosa] Lund Univ, Aquat Ecol Div, Dept Biol, S-22362 Lund, Sweden; [Estrada, Marta; Garces, Esther] CSIC, Inst Ciencies Mar, Dept Biol Marina & Oceanog, Pg Maritim Barceloneta 37-49, E-08003 Barcelona, Spain	Spanish Institute of Oceanography; Lund University; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Figueroa, RI (通讯作者)，CO Vigo, IEO, Vigo 36280, Spain.	rosa.figueroa@ieo.es	Estrada, Marta/L-6207-2014; Garces, Esther/C-5701-2011; Figueroa, Rosa/M-7598-2015	Garces, Esther/0000-0002-2712-501X; Figueroa, Rosa/0000-0001-9944-7993	FORMAS (Sweden) [Formas 215-2010-824]	FORMAS (Sweden)(Swedish Research Council Formas)	We thank A. Kremp for providing useful comments to the chapter. R.I. Figueroa was funded by a FORMAS (Sweden) project (Formas 215-2010-824). 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J	Yang, AA; Hu, ZX; Tang, YZ				Yang Aoao; Hu Zhangxi; Tang Yingzhong			Solid sand particle addition can enhance the production of resting cysts in dinoflagellates	JOURNAL OF OCEANOLOGY AND LIMNOLOGY			English	Article						sand; resting cyst; encystment; Scrippsiella trochoidea; Biecheleria brevisulcata; Levanderina fissa	HARMFUL ALGAL BLOOMS; SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; BALLAST WATER; GYMNODINIUM-CATENATUM; GYRODINIUM-INSTRIATUM; ENCYSTMENT; MORPHOLOGY; TEMPERATURE; CULTURE; SEA	Resting cysts are an important part of the life cycle for many harmful algal bloom-forming dinoflagellates, and play vital roles in the recurrence and geographical spread of harmful algal blooms. Numerous factors have been suggested to regulate the formation of resting cysts, although only a few have been proven to be significant. Cyst formation can be induced by adverse environmental conditions such as drastic changes in temperature, light, salinity, and nutrient levels, and by biological interactions. In this study, we evaluated the ability of an artificial factor (fine sand particles) to enhance the formation of resting cysts. Fine sand particles were added to cultures of dinoflagellates that are known to produce cysts. The addition of fine sand particles significantly increased both the production rate and final yield of cysts in cultures of Scrippsiella trochoidea, Biecheleria brevisulcata, and Levanderina fissa (=Gymnodinium fissum, Gyrodinium instriatum, Gyrodinium uncatenum). The largest increase in the final yield (107-fold) of cysts as a result of sand addition was in S. trochoidea. However, addition of fine sand particles did not induce cyst formation, or barely affected cyst formation, in Akashiwo sanguinea, Cochlodinium polykrikoides and Pheopolykrikos hartmannii, which are also known to be cyst-producing species. We speculated that addition of sand significantly increased the chances of cell collision, which triggered cyst formation. However, further research is required to test this idea. Importantly, our findings indicate that the addition of fine sand particles is a useful method to obtain a large quantity of cysts in a short time for laboratory studies or tests; for example, if a cyst viability test is being used to assess the effectiveness of ships' ballast water treatment.	[Yang Aoao; Hu Zhangxi; Tang Yingzhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Yang Aoao] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Tang Yingzhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Laoshan Laboratory	Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023		NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences [U1606404]; National Natural Science Foundation of China [41476142, 61533011, 41506143]; Scientific and Technological Innovation Project - Qingdao National Laboratory for Marine Science [2016ASKJ02]; NSFC-Guangdong Joint Fund [U1301235]	NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Scientific and Technological Innovation Project - Qingdao National Laboratory for Marine Science; NSFC-Guangdong Joint Fund	Supported by the NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences (No. U1606404), the National Natural Science Foundation of China (Nos. 41476142, 61533011, 41506143), the Scientific and Technological Innovation Project supported by the Qingdao National Laboratory for Marine Science (No. 2016ASKJ02), and the NSFC-Guangdong Joint Fund (No. U1301235)	ANDERSON DM, 1988, J PHYCOL, V24, P255; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1985, J PHYCOL, V21, P200; Anderson DM, 2009, OCEAN COAST MANAGE, V52, P342, DOI 10.1016/j.ocecoaman.2009.04.006; Balkis N, 2016, PHYCOLOGIA, V55, P187, DOI 10.2216/15-93.1; Bolch CJS, 2007, HARMFUL ALGAE, V6, P465, DOI 10.1016/j.hal.2006.12.008; Bravo Isabel, 2014, Microorganisms, V2, P11; Chambouvet A, 2011, PROTIST, V162, P637, DOI 10.1016/j.protis.2010.12.001; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; Gu HF, 2008, J PHYCOL, V44, P478, DOI 10.1111/j.1529-8817.2008.00478.x; Guillard R. 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Oceanol. Limnol.	MAR	2018	36	2					273	280		10.1007/s00343-018-6291-x	http://dx.doi.org/10.1007/s00343-018-6291-x			8	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	GF1AA					2025-03-11	WOS:000431662200008
J	Crawford, DW; Cefarelli, AO; Wrohan, IA; Wyatt, SN; Varela, DE				Crawford, David W.; Cefarelli, Adrian O.; Wrohan, Ian A.; Wyatt, Shea N.; Varela, Diana E.			Spatial patterns in abundance, taxonomic composition and carbon biomass of nano-and microphytoplankton in Subarctic and Arctic Seas	PROGRESS IN OCEANOGRAPHY			English	Article						Phytoplankton; Carbon; Taxonomy; Arctic; Subarctic; Marine; Ocean	PHYTOPLANKTON COMMUNITY STRUCTURE; NORTHERN BAFFIN-BAY; BEAUFORT SEA; SURFACE WATERS; PIGMENT SIGNATURES; NUTRIENT DYNAMICS; CHLOROPHYLL-A; OCEAN; DIATOMS; VARIABILITY	In the summers of 2007 and 2008, we studied assemblages of nano-and microphytoplankton from the subsurface chlorophyll maximum (SCM) across five broad oceanographic domains in the seas surrounding northern North America. These domains are the eastern Subarctic North Pacific (ESNP), Bering and Chukchi Seas (BE-CH), Beaufort Sea and Canada Basin (BS-CB), Canadian Arctic Archipelago (CAA), and Baffin Bay and Labrador Sea (BB-LS). Average abundance and total carbon biomass (C) of phytoplankton (> 2 mu m) varied 10-fold and -20-fold, respectively, across the five domains. In the BE-CH, CAA and BB-LS, diatoms averaged 35-70% and dinoflagellates 11-45% of total phytoplankton C (> 2 pm), whereas in the ESNP and BS-CB, unidentified flagellates/coccoids (2-8 mu m) represented a greater proportion of total C (27% and 39% respectively) than in the other domains. In the BE-CH and BB-LS, phytoplankton C (> 2 gm) was dominated by dinoflagellates of the genus Gymnodinium, centric diatoms including Thalassiosira spp. and Chaetoceros spp., unidentified flagellates/coccoids (2-8 gm), and cryptomonads. In contrast, diatoms such as Thalassiosira spp. and its resting spores dominated C in the CAA, with dinoflagellates being less significant than in the BE-CH and BB-LS. Unidentified flagellates/coccolds (2-8 pm), Gymnodinium spp., and cryptomonads dominated in the ESNP, and particularly in the BS-CB, where diatoms contributed only 18% of the very low levels of total phytoplankton C (> 2 mu m). Phytoplankton C (> 2 mu m) to chlorophyll a ratios (phyto C:chl a) averaged only 31 g C g chl alpha(-1) in the oligotrophic BS-CB domain, and 51-150 g C g chl alpha(-1) in the other domains, whereas ratios of biogenic silica to phytoplankton C (> 2 mu m) (bSi:phyto C) were lowest in the eastern domains. Estimates of phytoplankton C were highly sensitive to the choice of C to cell volume equations (C:vol) adopted in the calculations, particularly in diatom-rich areas. This study highlights how diatoms and dinoflagellates are the main drivers of large-scale variations in C biomass for phytoplankton (> 2 mu m), whereas unidentified flagellates/coccoids (2-8 mu m) make a significant contribution to C biomass in oligotrophic domains, such as BS-CB, where diatoms and dinoflagellates are less abundant. Reduced surface water density (sigma(T)) was associated with deeper SCM layers, and with decreased C biomass of unidentified flagellates/coccoids (2-8 mu m). These observations confirm recent studies highlighting the role of surface water stratification caused by melting sea ice in shaping nano-and microphytoplankton assemblages.	[Crawford, David W.; Cefarelli, Adrian O.; Wyatt, Shea N.; Varela, Diana E.] Univ Victoria, Dept Biol, POB 1700, Victoria, BC V8W 2Y2, Canada; [Wrohan, Ian A.; Varela, Diana E.] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada; [Cefarelli, Adrian O.] Consejo Nacl Invest Cient & Tecn, Ctr Invest & Transferencia Golfo San Jorge, RA-9000 Comodoro Rivadavia, Chubut, Argentina	University of Victoria; University of Victoria; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Varela, DE (通讯作者)，Univ Victoria, Dept Biol, POB 1700, Victoria, BC V8W 2Y2, Canada.	dvarela@uvic.ca	Crawford, David/AAS-9927-2020; Crawford, David W./B-5679-2012	Wyatt, Shea/0000-0002-4597-4517; Crawford, David W./0000-0003-2948-1007	Canadian IPY-C3O project; Natural Sciences and Engineering Research Council (NSERC) of Canada; University of Victoria Faculty of Graduate Studies; NSERC USRA scholarship; NSERC CGS-D scholarship; Emerging Leaders in the Americas program from Foreign Affairs, Trade and Development Canada	Canadian IPY-C3O project; Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); University of Victoria Faculty of Graduate Studies; NSERC USRA scholarship(Natural Sciences and Engineering Research Council of Canada (NSERC)); NSERC CGS-D scholarship(Natural Sciences and Engineering Research Council of Canada (NSERC)); Emerging Leaders in the Americas program from Foreign Affairs, Trade and Development Canada	We extend our appreciation to the scientists, officers, and crew members of the CCGS Louis S. St-Laurent and CCGS Sir Wilfrid Laurier. We specially thank Eddy Carmack, Jane Eert, R. John Nelson, Bon van Hardenberg, Sarah Zimmerman, Bill Williams and Svein Vagle from the Arctic group at the Institute of Ocean Sciences (Sidney, BC). We also thank Andrey Proshutinsky (PI, NSF Beaufort Gyre Exploration Project) and Fiona McLaughlin (PI, Canadian JOIS) for ship time in the Canada Basin. We thank Brent Gowen for his expertise and assistance with electron microscopy, and Karina Giesbrecht for help with graphics. Financial support was provided by the Canadian IPY-C3O project lead by Eddy Carmack (D.E.V., co-PI), and by Discovery Individual and Northern Research Supplement grants from the Natural Sciences and Engineering Research Council (NSERC) of Canada awarded to D.E.V. Additional support was provided by the University of Victoria Faculty of Graduate Studies to I.A.W., by NSERC USRA and CGS-D scholarships to S.N.W., and by the Emerging Leaders in the Americas program from Foreign Affairs, Trade and Development Canada to A.O.C. We would particularly like to extend our sincere appreciation to two anonymous reviewers who provided thoughtful and extensive comments and criticisms that significantly improved the manuscript.	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Oceanogr.	MAR	2018	162						132	159		10.1016/j.pocean.2018.01.006	http://dx.doi.org/10.1016/j.pocean.2018.01.006			28	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	GE4DD		Green Published			2025-03-11	WOS:000431163600010
J	Gleason, FH; Lilje, O; Lange, L				Gleason, Frank H.; Lilje, Osu; Lange, Lene			What has happened to the "aquatic phycomycetes" (sensu Sparrow)? Part II: Shared properties of zoosporic true fungi and fungus-like microorganisms	FUNGAL BIOLOGY REVIEWS			English	Review						Cell wall chemistry; Chytridiomycota; Labyrinthulomycota; Oomycota; Perkinsozoa; Phytomyxea; Zoospore ultrastructure	SP-NOV; WASTING DISEASE; PLASMODIOPHORA-BRASSICAE; LABYRINTHULA-TERRESTRIS; MOLECULAR PHYLOGENY; MARINE ECOSYSTEMS; ECOLOGICAL ROLES; ZOSTERA-MARINA; LIFE-CYCLE; THRAUSTOCHYTRIDS	Many species of zoosporic heterotrophic parasites, saprotrophs and mutualists in the Phyla Perkinsozoa (dinoflagellates), Oomycota, Hyphochytriomycota, Labyrinthulomycota and Phyomyxea share morphological characteristics with zoosporic true fungi especially with some of the Chytridiomycota and with fungus-like organisms in the Phyla Mesomycetozoea, Chytridiomycota and Aphelidae. These characteristics include chemotactic motile zoospores, zoosporangia which produce zoospores, thick walled resistant cysts, rhizoid like structures, hyphal-like structures and cell walls surrounding the cells in several phases of their life cycle. These assemblages also inhabit both marine and freshwater ecosystems in which aquatic fungi and fungus-like organisms are found, have similar life cycles, grow on similar substrates, use similar infection strategies and infect some of the same host plants and animals. Many of these species were once included in the aquatic phycomycetes, an ecological assemblage of microorganisms but not a valid taxonomic group. Some of the shared characteristics are discussed in this review. (C) 2017 British Mycological Society. Published by Elsevier Ltd. All rights reserved.	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J	McCarthy, FMG; Riddick, NL; Volik, O; Danesh, DC; Krueger, AM				McCarthy, Francine M. G.; Riddick, Nicholas L.; Volik, Olena; Danesh, Donya C.; Krueger, Andrea M.			Algal palynomorphs as proxies of human impact on freshwater resources in the Great Lakes region	ANTHROPOCENE			English	Article						Non-pollen palynomorphs; Desmids; Cultural eutrophication; Geoarchaeology; Wendat; Lake Simcoe; Crawford Lake	NON-POLLEN PALYNOMORPHS; AWENDA PROVINCIAL-PARK; CRAWFORD LAKE; CULTURAL EUTROPHICATION; DINOFLAGELLATE CYSTS; TESTATE AMEBAS; LAND-USE; ONTARIO; SIMCOE; INDICATORS	Management of freshwater resources requires an understanding of the response of lakes to human impact. The long sedimentary records in lake archives hold the key to accurate forecasting. The remains of algae in "pollen" slides record two distinct phases of cultural eutrophication and siltation/turbidity resulting from soil erosion in sediments from two lakes in southern Ontario, Canada: 1) agricultural settlements by Iroquoian (Wendat/Huron) people around the middle of the last millennium and 2) widespread land-clearing by European colonists in the mid-nineteenth century, followed by industrial expansion and urbanization in the Great Lakes watershed to the present day. The half-cells of benthic desmids were particularly sensitive to turbidity associated with land clearing. In contrast, planktonic algae adapted to eutrophic waters thrived in response to increased agricultural runoff and human and animal waste during both intervals in cores from Lake Simcoe and in the well-documented varved sediments from Crawford Lake. These under-utilized microfossils can be useful proxies of human impact, particularly where mineralized microfossils are sparse due to dissolution. (c) 2017 Elsevier Ltd. All rights reserved.	[McCarthy, Francine M. G.; Riddick, Nicholas L.; Volik, Olena; Danesh, Donya C.; Krueger, Andrea M.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Riddick, Nicholas L.] McMaster Univ, Sch Geog & Earth Sci, Hamilton, ON, Canada; [Volik, Olena] Univ Waterloo, Dept Geog & Environm Management, Waterloo, ON, Canada; [Danesh, Donya C.] Queens Univ, Dept Biol, Kingston, ON K7L 3N6, Canada	Brock University; McMaster University; University of Waterloo; Queens University - Canada	McCarthy, FMG (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	fmccarthy@brocku.ca	Volik, Olena/ABH-8956-2020	Volik, Olena/0000-0003-4949-1974; Riddick, Nicholas/0009-0005-1370-6365	NSERC	NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	We would like to acknowledge the assistance of Mike Lozon (Brock University) with drafting, and Bas van Geel and Peter Coesel (Universitaet Amsterdam) for generously giving their time and helping with desmid identification, and Jock McAndrews and Volodymyr Sivkov for assistance in coring. We are particularly indebted to Bas van Geel for his inspiration to pursue NPP analysis. This work was partly supported by NSERC funds awarded to F. McCarthy.	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J	Cheniti, R; Rochon, A; Frihi, H				Cheniti, Radhia; Rochon, Andre; Frihi, Hocine			Ship traffic and the introduction of diatoms and dinoflagellates via ballast water in the port of Annaba, Algeria	JOURNAL OF SEA RESEARCH			English	Article						Shipping; Ballast water; Diatom; Dinoflagellate; Harmful taxa; Annaba, Algeria	HARMFUL ALGAL BLOOMS; SOUTHERN MEDITERRANEAN SEA; BIZERTE LAGOON; PROPAGULE PRESSURE; MARINE; TRANSPORT; TUNISIA; MANAGEMENT; ORGANISMS; INVASIONS	We present here the first study on the role of ship traffic in the introduction of potentially harmful and/or non-indigenous species in the port of Annaba (Algeria). A total of 25 ships of two different types (general cargo and bulk carriers) were sampled and separated into two categories: oceanic and Mediterranean ships. We estimated propagule pressure of high-risk coastal phytoplankton delivered in ballast water to the port of Annaba. We identified 40 diatom and 38 dinoflagellate taxa, among which, 11 harmful/toxictaxa: Pseudo-nitzschia spp., Alexandrium tamarense, Alexandrium sp., Dinophysisacuminata, Dinophysisrotundata, Dinophysis sp., Gonyaulax spinifera, Gymnodinium catenatum, Lingulodinium polyedrum, Protoceratium reticulatum and cyst of Alexandrium sp. In addition, 8 taxa (5 diatoms, 1 dinoflagellate and 2 dinoflagellate cysts) never observed in the Annaba region were considered as potentially non-indigenous: Actinoptychus splendens, Coscinodiscus asteromphalus, Coscinodiscus lineatus, Odentella granulata, Thalassiosira cf. decipiens, Prorocentrum scutellum, cyst of Polykrikos kofoidii and Islandinium minutum. Several factors were examined, including ship routes, ballast water age and the volume of ballast water discharged. Our analyses revealed that diatom and dinoflagellate abundances decreased with ballast water age, possibly as a result of mortality of species due to voyage length and lack of light in ballast tanks. Estimates of actual propagule pressure, diatoms and dinoflagellates abundances varied from 1 to 4 x 10(8) cells/ship. The results of this study could serve as the baseline for the development and implementation of monitoring and ballast water management programs in ports of Algeria.	[Cheniti, Radhia; Frihi, Hocine] Annaba Univ Badji Mokhtar, Marine Bioresources Lab, Annaba, Algeria; [Rochon, Andre] ISMER UQAR, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada	University of Quebec; Universite du Quebec a Rimouski	Cheniti, R (通讯作者)，Annaba Univ Badji Mokhtar, Marine Bioresources Lab, Annaba, Algeria.; Rochon, A (通讯作者)，ISMER UQAR, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	radhia.cheniti@gmail.com; andre_rochon@uqar.ca	Hocine, FREHI/R-8856-2016	FRIHI, Hocine/0000-0001-8104-2875				[Anonymous], 2004, INT CONVENTION CONTR; Armi Z, 2011, AFR J AQUAT SCI, V36, P47, DOI 10.2989/16085914.2011.559688; Briand F., 2010, CIESM WORKSHOP MONOG, V40; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; *CIESM, 2002, CIESM WORKSH MON, V20; Colautti RI, 2004, DIVERS DISTRIB, V10, P135, DOI 10.1111/j.1366-9516.2004.00061.x; Daoudi M., 2012, Transitional Waters Bulletin, V6, P4; David M, 2007, MAR POLLUT BULL, V54, P53, DOI 10.1016/j.marpolbul.2006.08.041; Dickman M, 1999, MAR ECOL PROG SER, V176, P253, DOI 10.3354/meps176253; Dobler J.P., 2002, P ALIEN MARINE ORGAN, VVolume 20, P19; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; Endresen O, 2004, MAR POLLUT BULL, V48, P615, DOI 10.1016/j.marpolbul.2004.01.016; Endresen O., 2002, MARINE SCI TECHNOLOG, V2002; Fernandez-Tejedor Margarita, 2010, CIESM Workshop Monographs, V40, P83; Flagella MM, 2006, OCEAN COAST MANAGE, V49, P947, DOI 10.1016/j.ocecoaman.2006.08.009; Frehi H, 2007, CR BIOL, V330, P615, DOI 10.1016/j.crvi.2007.05.002; Gomez F., 2013, CICIMAR Oceanides, V28, P1; Gomez Fernando, 2001, Harmful Algae News, V22, P1; Gomoiu MT, 2002, INVASIVE AQUATIC SPECIES OF EUROPE: DISTRIBUTION, IMPACTS AND MANAGEMENT, P341; Guelorget O., 1992, AQUA REV, V41, P21; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Illoul H., 2014, THESIS; Illoul H, 2008, CRYPTOGAMIE ALGOL, V29, P261; *IMO, 2003, INT CONV CO IN PRESS; IMO, 2017, INT CONV CONTR MAN S; Ismael AA, 2000, P 9 INT C HARMF ALG, P141; Joutei LT, 1995, HARMFUL ALGAE NEWS, V7, P12; Khairy HM, 2014, REV BIOL MAR OCEANOG, V49, P267, DOI 10.4067/S0718-19572014000200007; Klein G, 2010, BIOL INVASIONS, V12, P1031, DOI 10.1007/s10530-009-9520-6; Lavoie DM, 1999, ESTUAR COAST SHELF S, V48, P551, DOI 10.1006/ecss.1999.0467; Lawrence DJ, 2010, BIOL CONSERV, V143, P700, DOI 10.1016/j.biocon.2009.12.008; Aguirre-Macedo ML, 2008, MAR POLLUT BULL, V56, P1570, DOI 10.1016/j.marpolbul.2008.05.022; Lockwood JL, 2005, TRENDS ECOL EVOL, V20, P223, DOI 10.1016/j.tree.2005.02.004; Lockwood JL, 2009, DIVERS DISTRIB, V15, P904, DOI 10.1111/j.1472-4642.2009.00594.x; MARGALEF R, 1987, Investigacion Pesquera (Barcelona), V51, P121; McGee S, 2006, MAR POLLUT BULL, V52, P1634, DOI 10.1016/j.marpolbul.2006.06.005; Meunier A., 1915, MEM B I R SCI NAT BE, V7; Mohamed-Cherif F. 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J	Mathews, RP; Singh, BD; Singh, H; Singh, VP; Singh, A				Mathews, R. P.; Singh, B. D.; Singh, Hukam; Singh, V. P.; Singh, Alpana			Characterization of Panandhro Lignite Deposits (Kachchh Basin), western India: Results from the Bulk Geochemical and Palynofloral Compositions	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article							SOURCE-ROCK; CAMBAY BASIN; KUTCH BASIN; INFRARED-SPECTROSCOPY; LIPTINITE MACERALS; THERMAL MATURITY; EOCENE LIGNITES; FT-IR; COAL; GUJARAT	Characterization of the Panandhro lignite deposits from western Indian state of Gujarat, based on the geochemical and palynological evidences, has been performed to assess the floral composition, maturity and hydrocarbon potential of the sequence. Elementally, the lignites consist of moderate carbon, low hydrogen and moderate sulfur contents. The samples are characterized by high TOC contents (lignite: av. 46.43 wt.%, resin: 62.47 wt.%). The average HI values for the lignite is 136 mg HC/g TOC, and that of the associated resin is 671 mg HC/g TOC. The highest T-max is recoded in lignite (422 degrees C) and lowest in the resin (39 degrees C) samples. The FTIR spectrum of lignite is characterized by highly intense OH stretching peak similar to 3350 cm(-1), aliphatic CHx stretching peaks between 3000-2800 cm(-1), aromatic C=O stretching and an aromatic C=C stretching. The spectrum of resin shows strongest absorption due to aliphatic CHx stretching between 2940-2915 cm(-1) and 2870-2850 cm(-1), and deformation by the medium peak between 1450 and 1650 cm(-1). The recovered palynofloral assemblage indicates the dominance of angiosperm pollen grains with maximum abundance of Arecaceae family, and subdominant pteridophytic spores. Marine influence is indicated by the presence of abundant dinoflagellate cysts. The occurrence of flora from a variety of ecological niches suggests a luxuriant diverse vegetation pattern existed in the vicinity of depositional site under humid tropical conditions. The overall characteristics of the lignite deposits point towards their ability to generate (upon maturation) hydrocarbons as they have types III-II admixed kerogen (organic matters).	[Mathews, R. P.; Singh, B. D.; Singh, Hukam; Singh, V. P.; Singh, Alpana] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Mathews, RP (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	runciepaulmathews@gmail.com	Singh, Anoop Kumar/IXR-0763-2023; Singh, Prakash/AAE-6396-2020	SINGH, VIKRAM PARTAP/0000-0002-0136-7918				Basile L. 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J	Egger, LM; Bahr, A; Friedrich, O; Wilson, PA; Norris, RD; van Peer, TE; Lippert, PC; Liebrand, D; Pross, J				Egger, Lisa M.; Bahr, Andre; Friedrich, Oliver; Wilson, Paul A.; Norris, Richard D.; van Peer, Tim E.; Lippert, Peter C.; Liebrand, Diederik; Pross, Joerg			Sea-level and surface-water change in the western North Atlantic across the Oligocene-Miocene Transition: A palynological perspective from IODP Site U1406 (Newfoundland margin)	MARINE MICROPALEONTOLOGY			English	Article						Oligocene-Miocene Transition; Dinoflagellate cysts; North Atlantic Ocean; Sea level; Integrated Ocean Drilling Program	WALLED DINOFLAGELLATE CYSTS; ANTARCTIC ICE-SHEET; MIDDLE MIOCENE; CARBON-CYCLE; LATE EOCENE; STABLE-ISOTOPES; SEDIMENT DRIFTS; LATE PLIOCENE; LEG 171B; PALEOECOLOGY	The Oligocene-Miocene transition (OMT; similar to 23.1 Ma) terminates the late Oligocene warming trend and is marked by a transient, large-amplitude expansion of Antarctic ice sheets. The associated glacial maximum, which is expressed by a similar to 1 positive shift in benthic foraminiferal oxygen-isotope values, is commonly referred to as the 'Mi-1 isotope event'. Whereas the causes for the glacial maximum at the OMT are intrinsically connected to Southern Hemisphere ice-sheet dynamics, the behavior of the surface ocean in the Northern Hemisphere during this time is poorly known. To contribute to a better understanding of the paleoceanographic evolution during the OMT in the higher-latitude North Atlantic, we have analysed both marine and terrestrial palynomorphs from Integrated Ocean Drilling Program (IODP) Site U1406 offshore Newfoundland; this site has yielded a complete OMT section and exhibits a high-quality magnetostratigraphy that provides precise age control and allows reliable correlation to other records beyond Newfoundland. Our palynological data, which span the interval from 23.3 to 22.5 Ma and have a mean temporal resolution of 11.9 kyrs, show strong similar to 110-kyr eccentricity-paced oscillations during the earliest Miocene; these oscillations are in phase with similar cyclicity identified in previously published benthic foraminiferal oxygen-isotope records. More specifically, a pronounced sea-level variability is documented by the abundances of neritic dinoflagellate cysts (dinocysts) and terrigenous palynomorphs, which both reach maxima during peak glacial intervals as inferred from previously published South Atlantic benthic oxygen-isotope data. A decline in the abundance of warmer-water dinocysts suggests a surface-water cooling offshore Newfoundland from the latest Oligocene onwards. Surface-water productivity (as derived from the ratio between heterotrophic and autotrophic dinocysts) remained generally low throughout the studied interval. Notably, this ratio does not exhibit any correlation with changes in surface-water temperature, which is estimated from the ratio of warm-water over cold-water dinocysts. Together with the consistently low surface-water productivity, the lack of a correlation between surface-water productivity and temperature makes it highly unlikely that the observed paleoceanographic change was caused by a southward migration of the Arctic Front. Instead, we argue that our data may document an enhanced influence of the (Proto-) Labrador Current on surface waters offshore Newfoundland during the earliest Miocene that suppressed the influence of the Gulf Stream in this region of the Northwest Atlantic. We speculate that the enhanced influence of the (Proto-) Labrador Current was triggered by cooling of the northern hemisphere and possibly modulated by high-latitude sea-ice expansion.	[Egger, Lisa M.; Bahr, Andre; Friedrich, Oliver; Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234-236, D-69120 Heidelberg, Germany; [Wilson, Paul A.; van Peer, Tim E.; Liebrand, Diederik] Univ Southampton, Natl Oceanog Ctr, Waterfront Campus,European Way, Southampton SO14 3ZH, Hants, England; [Norris, Richard D.] Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gilman Dr, La Jolla, CA 92093 USA; [Lippert, Peter C.] Univ Utah, Dept Geol & Geophys, Frederick A Sutton Bldg,115 S 1460 E, Salt Lake City, UT 84112 USA	Ruprecht Karls University Heidelberg; University of Southampton; NERC National Oceanography Centre; University of California System; University of California San Diego; Scripps Institution of Oceanography; Utah System of Higher Education; University of Utah	Egger, LM (通讯作者)，Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234-236, D-69120 Heidelberg, Germany.	lisa.egger@geow.uni-heidelberg.de	Liebrand, Diederik/AAT-2004-2021; van Peer, Tim/R-8157-2016	Liebrand, Diederik/0000-0002-6925-7889; van Peer, Tim/0000-0003-3516-4198; Wilson, Paul/0000-0001-6425-8906; Lippert, Peter C/0000-0003-1744-9982; Bahr, Andre/0000-0001-5890-8773	U.S. National Science Foundation; management of Joint Oceanographic Institutions Inc.; German Research Foundation (DFG) [PR 651/16, FR 2544/8]; Royal Society; NERC [NE/K006800/1, NE/K014137/1] Funding Source: UKRI	U.S. National Science Foundation(National Science Foundation (NSF)); management of Joint Oceanographic Institutions Inc.; German Research Foundation (DFG)(German Research Foundation (DFG)); Royal Society(Royal Society); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research used samples and data provided by the Integrated Ocean Drilling Program, which was sponsored by the U.S. National Science Foundation and participating countries under management of Joint Oceanographic Institutions Inc. Invaluable support of the members of the IODP Expedition 342 Science Party is gratefully acknowledged. Malcolm Jones is thanked for technical support. This study was funded through the German Research Foundation (DFG; grants PR 651/16 and FR 2544/8 to J.P. and O.F., respectively). P.A.W. acknowledges NERC-UK IODP and a Royal Society Wolfson Award.	Beddow HM, 2016, PALEOCEANOGRAPHY, V31, P81, DOI 10.1002/2015PA002820; Bijl PK, 2017, PALYNOLOGY, V41, P423, DOI 10.1080/01916122.2016.1235056; Bijl PK, 2011, PALEOCEANOGRAPHY, V26, DOI 10.1029/2009PA001905; Boyle PR, 2017, MAR GEOL, V385, P185, DOI 10.1016/j.margeo.2016.12.014; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P219; Crouch E. 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Micropaleontol.	MAR	2018	139						57	71		10.1016/j.marmicro.2017.11.003	http://dx.doi.org/10.1016/j.marmicro.2017.11.003			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	GA1TT		Green Accepted, Bronze			2025-03-11	WOS:000428101000004
J	King, C; Iakovleva, A; Heilmann-Clausen, C; Steurbaut, E				King, Chris; Iakovleva, Alina; Heilmann-Clausen, Claus; Steurbaut, Etienne			Ypresian (early Eocene) stratigraphy of the Suvlu-Kaya reference section in the Bakhchisaray area (Crimea)	NEWSLETTERS ON STRATIGRAPHY			English	Article						Ypresian; lithostratigraphy; biostratigraphy; depositional environments; sequence stratigraphy; Suvlu-Kaya; Crimea	NORTH-SEA BASIN; DINOFLAGELLATE CYST; PALEOCENE; BIOSTRATIGRAPHY; AKTULAGAY; KAZAKSTAN; BOREHOLE; SEQUENCE; PLATFORM; EECO	The Suvlu-Kaya section (Crimea) is historically considered as a reference section for the European mid-latitude Thanetian and Ypresian. The Ypresian (calcareous nannofossil Zones NP10 to NP13) comprises mid-neritic clays and marls, overlain by inner neritic limestones. This integrated multidisciplinary study, including dinoflagellate cysts (first record and full illustration), calcareous nannofossils, foraminifera, depositional environments and sequence stratigraphy, reinforces its status as a reference section. The calcareous nannofossil subdivision of NP11 and NP12 and the planktonic foraminiferal Subbotina influx, originally defined in the North Sea Basin, are recognized at Suvlu-Kaya. The biostratigraphic synthesis presented here enables detailed correlations with the Aktulagay section in Western Kazakhstan and the North Sea Basin. The strong biostratigraphic correspondence between these areas confirms previous suggestions of a direct marine connection between the Peri-Tethys and the North Sea Basin, at least during the early and middle Ypresian (interval from mid Biochron NP10 to late Biochron NP12). If this direct connection was maintained during the late Ypresian is difficult to evaluate on the basis of the currently available data.	[King, Chris] Russian Acad Sci, Geol Inst, Pyzhevsky Pereulok 7, Moscow 119017, Russia; [King, Chris] Univ Liege, Pal Lab 3, Batiment B18,Allee 6 Aout,14, B-4000 Liege, Belgium; [Heilmann-Clausen, Claus] Aarhus Univ, Dept Geosci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Steurbaut, Etienne] Royal Belgian Inst Nat Sci, Vautierstr 29, B-1000 Brussels, Belgium; [Steurbaut, Etienne] Katholieke Univ Leuven, Leuven, Belgium	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; University of Liege; Aarhus University; Royal Belgian Institute of Natural Sciences; KU Leuven	Steurbaut, E (通讯作者)，Royal Belgian Inst Nat Sci, Vautierstr 29, B-1000 Brussels, Belgium.; Steurbaut, E (通讯作者)，Katholieke Univ Leuven, Leuven, Belgium.	etienne.steurbaut@naturalsciences.be	IAKOVLEVA, ALINA/ABH-9243-2020; Heilmann-Clausen, Claus/A-4848-2012		Danish Natural Science Research Council [21-04-0298]; Geological Institute, Russian Academy of Sciences [0135-2016-0001]	Danish Natural Science Research Council(Danish Natural Science Research Council); Geological Institute, Russian Academy of Sciences	The authors are very grateful to Dr. V.N. Ben'yamovskii (Geological Institute Moscow) for having provided the photograph of the Suvlu-Kaya section. K. Rosendal (Aarhus) is thanked for the palynological processing of samples for the dinoflagellate cyst analysis, and S. B. Andersen (Aarhus) is thanked for technical preparation of the dinoflagellate cyst plates. A. Vandersypen (RBINS Brussels) is greatly acknowledged for his assistance in the finalization of the figures. We thank the two reviewers (anonymous) for their careful examination and their constructive comments, which led to significant improvements of the manuscript. The research of AI was supported by the Danish Natural Science Research Council (Grant no. 21-04-0298) and the Russian State program no. 0135-2016-0001 (Geological Institute, Russian Academy of Sciences).	Agnini C, 2007, MAR MICROPALEONTOL, V64, P215, DOI 10.1016/j.marmicro.2007.05.003; Akhmet'ev MA, 2006, STRATIGR GEO CORREL+, V14, P49, DOI 10.1134/S0869593806010047; Andreeva-Grigorovich A. 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MAR	2018	51	2					167	208		10.1127/nos/2017/0384	http://dx.doi.org/10.1127/nos/2017/0384			42	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FY7EY					2025-03-11	WOS:000427025600002
J	Couet, D; Pringault, O; Bancon-Montigny, C; Briant, N; Poulichet, FE; Delpoux, S; Kefi-Daly Yahia, O; Ben Gharbia, H; M'Rabet, C; Hervé, F; Rovillon, G; Amzil, Z; Laabir, M				Couet, Douglas; Pringault, Olivier; Bancon-Montigny, Chrystelle; Briant, Nicolas; Poulichet, Francoise Elbaz; Delpoux, Sophie; Kefi-Daly Yahia, Ons; Ben Gharbia, Hela; M'Rabet, Charaf; Herve, Fabienne; Rovillon, Georges; Amzil, Zouher; Laabir, Mohamed			Effects of copper and butyltin compounds on the growth, photosynthetic activity and toxin production of two HAB dinoflagellates: The planktonic <i>Alexandrium catenella</i> and the benthic <i>Ostreopsis</i> cf. <i>ovata</i>	AQUATIC TOXICOLOGY			English	Article						Alexandrium catenella; Ostreopsis cf. ovata; Cu; Butyltin; Photosynthesis; Toxins	HARMFUL ALGAL BLOOMS; ORGANOTIN COMPOUNDS; MARINE-ENVIRONMENT; CHLAMYDOMONAS-REINHARDTII; AMPHIDINIUM-CARTERAE; SKELETONEMA-COSTATUM; PHOTOSYSTEM-II; ACUTE TOXICITY; TRACE-METALS; FRESH-WATER	Controlled laboratory experiments were conducted to test the effects of copper (Cu2+) and butyltins (BuT) on the growth, photosynthetic activity and toxin content of two HABs (Harmful Algal Blooms) dinoflagellates, the planktonic Alexandrium catenella and the benthic Ostreopsis cf. ovata. Microalgae were exposed to increasing concentrations of Cu2+ (10(-4) to 31 nM) or BuT (0.084 to 84 nM) for seven days. When considering the growth, EC50 values were 0.16 (+/- 0.09) nM and 0.03 (+/- 0.02) nM of Cu2+ for A. catenella and O. cf. ovata, respectively. Regarding BuT, EC50 was 14.2 (+/- 6) nM for O. cf. ovata, while A. catenella growth inhibition appeared at BuT concentrations >= 27 nM. Photosynthetic activity of the studied dinoflagellates decreased with increasing Cu and BuT concentrations. For O. cf. ovata, the response of this physiological parameter to contamination was less sensitive than the biomass. Cu exposure induced the formation of temporary cysts in both organisms that could resist adverse conditions. The ovatoxin-a and-b concentrations in O. cf. ovata cells increased significantly in the presence of Cu. Altogether, the results suggest a better tolerance of the planktonic A. catenella to Cu and BuT. This could result in a differentiated selection pressure exerted by these metals on phytoplankton species in highly polluted waters. The over-production of toxins in response to Cu stress could pose supplementary health and socio-economic threats in the contaminated marine ecosystems where HABs develop.	[Couet, Douglas; Pringault, Olivier; Laabir, Mohamed] Montpellier Univ, CNRS, IFREMER,IRD, Ctr Marine Biodivers Exploitat & Conservat MARBEC, Pl Eugene Bataillon, F-34095 Montpellier, France; [Couet, Douglas; Kefi-Daly Yahia, Ons; Ben Gharbia, Hela; M'Rabet, Charaf] IRESA Carthage Univ, Tunisian Natl Inst Agron INAT, Res Grp Oceanog & Plankton Ecol, 43 Ave Charles Nicolle, Tunis 1082, Tunisia; [Bancon-Montigny, Chrystelle; Poulichet, Francoise Elbaz; Delpoux, Sophie] Univ Montpellier, CNRS, Hydrosci Montpellier, IRD, Montpellier, France; [Briant, Nicolas; Herve, Fabienne; Rovillon, Georges; Amzil, Zouher] IFREMER, Phycotoxins Lab, BP 21105, F-44311 Nantes, France	Ifremer; Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Ifremer	Laabir, M (通讯作者)，Montpellier Univ, CNRS, IFREMER,IRD, Ctr Marine Biodivers Exploitat & Conservat MARBEC, Pl Eugene Bataillon, F-34095 Montpellier, France.	mohamed.laabir@umontpellier.fr	Montigny, Chrystelle/ACN-3124-2022; Pringault, Olivier/A-7399-2008; MONTIGNY, Chrystelle/H-1993-2013	Ben Gharbia, Hela/0000-0002-9878-6915; DELPOUX, Sophie/0000-0003-0017-7423; Pringault, Olivier/0000-0003-2363-8376; Kefi Daly Yahia, Ons/0000-0001-9532-8989; MONTIGNY, Chrystelle/0000-0003-0734-7130; HERVE, Fabienne/0000-0002-5485-7611	LMI COSYSMED (Laboratoire Mixte International Contaminants et Ecosystemes Marins Sud Mediterraneens) belonging to IRD (Institut Francais de Recherche pour le Developpement); LAGUNOTOX project - Fondation TOTAL; IRD; French Ministry of Foreign Affairs	LMI COSYSMED (Laboratoire Mixte International Contaminants et Ecosystemes Marins Sud Mediterraneens) belonging to IRD (Institut Francais de Recherche pour le Developpement); LAGUNOTOX project - Fondation TOTAL; IRD; French Ministry of Foreign Affairs	This work was supported by the LMI COSYSMED (Laboratoire Mixte International Contaminants et Ecosystemes Marins Sud Mediterraneens) belonging to IRD (Institut Francais de Recherche pour le Developpement), and LAGUNOTOX project funded by Fondation TOTAL. We would also like to thank the IRD and French Ministry of Foreign Affairs for funding Douglas Couet in Tunisia in the framework of International Volunteers Program.	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Toxicol.	MAR	2018	196						154	167		10.1016/j.aquatox.2018.01.005	http://dx.doi.org/10.1016/j.aquatox.2018.01.005			14	Marine & Freshwater Biology; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Toxicology	FX9IJ	29407801	Green Published			2025-03-11	WOS:000426411600017
J	Lee, SY; Jeong, HJ; You, JH; Kim, SJ				Lee, Sung Yeon; Jeong, Hae Jin; You, Ji Hyun; Kim, So Jin			Morphological and genetic characterization and the nationwide distribution of the phototrophic dinoflagellate <i>Scrippsiella lachrymosa</i> in the Korean waters	ALGAE			English	Article						Calciodinelloideae; dinoflagellate; DNA; ITS; qPCR; taxonomy	RED TIDES; COCHLODINIUM-POLYKRIKOIDES; PLANKTONIC DIATOMS; SURFACE SEDIMENTS; WESTERN KOREA; RESTING CYSTS; NORTH-SEA; BAY; DINOPHYCEAE; IDENTIFICATION	The phototrophic dinoflagellate genus Scrippsiella is known to have a worldwide distribution. Here, we report for the first time, the occurrence of Scrippsiella lachrymosa in Korean waters. Unlike the other stains of S. lachrymosa whose cultures had been established from cysts in the sediments, the clonal culture of the Korean strain of S. lachrymosa was established from motile cells. When the sulcal plates of S. lachrymosa, which have not been fully described to date, were carefully examined using scanning electron microscopy, the Korean strain of S. lachrymosa clearly exhibited the anterior sulcal plate (s.a.), right sulcal plate (s.d.), left sulcal plate (s.s.), median sulcal plate (s.m.), and posterior sulcal plate (s.p.). When properly aligned, the large subunit (LSU) rDNA sequence of the Korean strain of S. lachrymosa was ca. 1% different from those of two Norwegian strains of S. lachrymosa, the only strains for which LSU sequences have been reported. The internal transcribed spacer (ITS) rDNA sequence of the Korean strain of S. lachrymosa was also ca. 1% different from those of the Scottish and Chinese strains and 3% different from those of the Canadian, German, Greek, and Portuguese strains. Thus, the Korean S. lachrymosa strain has unique LSU and ITS sequences. The abundances of S. lachrymosa in the waters of 28 stations, located in the East, West, and South Sea of Korea, were quantified in four seasons from January 2016 to October 2017, using quantitative real-time polymerase chain reaction method and newly designed specific primer-probe sets. Its abundances were > 0.1 cells mL(-1) at eight stations in January and March 2016 and March 2017, and its highest abundance in Korean waters was 26 cells mL(-1). Thus, S. lachrymosa has a nationwide distribution in Korean waters as motile cells.	[Lee, Sung Yeon; Jeong, Hae Jin; You, Ji Hyun; Kim, So Jin] Seoul Natl Univ, Sch Earth & Environm Sci, Coll Nat Sci, Seoul 08826, South Korea; [Jeong, Hae Jin] Adv Inst Convergence Technol, Suwon 16229, South Korea	Seoul National University (SNU)	Jeong, HJ (通讯作者)，Seoul Natl Univ, Sch Earth & Environm Sci, Coll Nat Sci, Seoul 08826, South Korea.; Jeong, HJ (通讯作者)，Adv Inst Convergence Technol, Suwon 16229, South Korea.	hjjeong@snu.ac.kr	Jeong, hae/B-8908-2009	Jeong, Hae Jin/0000-0003-3310-4335	Useful Dinoflagellate program of Korea Institute of Marine Science and Technology Promotion (KIMST) - Ministry of Oceans and Fisheries (MOF); KIMST, the National Research Foundation (NRF) - Ministry of Science and ICT [NRF-2015M1A5A1041806, NRF-2017R1E1A1A01074419]	Useful Dinoflagellate program of Korea Institute of Marine Science and Technology Promotion (KIMST) - Ministry of Oceans and Fisheries (MOF)(Korea Institute of Marine Science & Technology Promotion (KIMST)Ministry of Oceans & Fisheries (MOF), Republic of Korea); KIMST, the National Research Foundation (NRF) - Ministry of Science and ICT(Korea Institute of Marine Science & Technology Promotion (KIMST))	We thank Kyung Ha Lee, Jin Hee Ok, An Suk Lim, Hee Chang Kang, Se Hyeon Jang, Ji Eun Kwon, Jae Yeon Park, and Eun Young Yoon, for technical support. This research was supported by the Useful Dinoflagellate program of Korea Institute of Marine Science and Technology Promotion (KIMST) funded by the Ministry of Oceans and Fisheries (MOF) and Management of marine organisms causing ecological disturbance and harmful effect Program of KIMST, the National Research Foundation (NRF) funded by the Ministry of Science and ICT (NRF-2015M1A5A1041806; NRF-2017R1E1A1A01074419) award to HJJ.	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J	Limoges, A; Ribeiro, S; Weckström, K; Heikkilä, M; Zamelczyk, K; Andersen, TJ; Tallberg, P; Massé, G; Rysgaard, S; Norgaard-Pedersen, N; Seidenkrantz, MS				Limoges, Audrey; Ribeiro, Sofia; Weckstrom, Kaarina; Heikkila, Maija; Zamelczyk, Katarzyna; Andersen, Thorbjorn J.; Tallberg, Petra; Masse, Guillaume; Rysgaard, Soren; Norgaard-Pedersen, Niels; Seidenkrantz, Marit-Solveig			Linking the Modern Distribution of Biogenic Proxies in High Arctic Greenland Shelf Sediments to Sea Ice, Primary Production, and Arctic-Atlantic Inflow	JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES			English	Article						Arctic sea ice; Greenland fjords; paleoclimate; microfossils; biomarkers	BENTHIC FORAMINIFERAL ASSEMBLAGES; CASSIDULINA-TERETIS TAPPAN; NORTHERN NORTH-ATLANTIC; CARBON-ISOTOPE RATIOS; FRESH-WATER; FRAM STRAIT; ORGANIC-MATTER; MICROHABITAT PREFERENCES; THERMOHALINE CIRCULATION; TROPHIC RELATIONSHIPS	The eastern north coast of Greenland is considered to be highly sensitive to the ongoing Arctic warming, but there is a general lack of data on modern conditions and in particular on the modern distribution of climate and environmental proxies to provide a baseline and context for studies on past variability. Here we present a detailed investigation of 11 biogenic proxies preserved in surface sediments from the remote High Arctic Wandel Sea shelf, the entrance to the Independence, Hagen, and Danmark fjords. The composition of organic matter (organic carbon, C:N ratios, C-13, N-15, biogenic silica, and IP25) and microfossil assemblages revealed an overall low primary production dominated by benthic diatoms, especially at the shallow sites. While the benthic and planktic foraminiferal assemblages underline the intrusion of chilled Atlantic waters into the deeper parts of the study area, the distribution of organic-walled dinoflagellate cysts is controlled by the local bathymetry and sea ice conditions. The distribution of the dinoflagellate cyst Polarella glacialis matches that of seasonal sea ice and the specific biomarker IP25, highlighting the potential of this species for paleo sea ice studies. The information inferred from our multiproxy study has important implications for the interpretation of the biogenic-proxy signal preserved in sediments from circum-Arctic fjords and shelf regions and can serve as a baseline for future studies. This is the first study of its kind in this area.	[Limoges, Audrey; Ribeiro, Sofia; Weckstrom, Kaarina; Heikkila, Maija] Geol Survey Denmark & Greenland, Dept Glaciol & Climate, Copenhagen, Denmark; [Limoges, Audrey] Univ New Brunswick, Dept Earth Sci, Fredericton, NB, Canada; [Weckstrom, Kaarina; Heikkila, Maija; Tallberg, Petra] Univ Helsinki, Dept Environm Sci, Environm Change Res Unit, Helsinki, Finland; [Zamelczyk, Katarzyna] Arctic Univ Norway, Dept Geosci, Ctr Arctic Gas Hydrate Environm & Climate, Tromso, Norway; [Andersen, Thorbjorn J.] Univ Copenhagen, Dept Geosci & Nat Resource Management, CENPERM, Copenhagen, Denmark; [Masse, Guillaume] CNRS, Dept Biol, TAKUVIK UMI3376, Quebec City, PQ, Canada; [Masse, Guillaume] Univ Laval, Quebec City, PQ, Canada; [Rysgaard, Soren; Seidenkrantz, Marit-Solveig] Aarhus Univ, Arctic Res Ctr, Aarhus, Denmark; [Rysgaard, Soren] Univ Manitoba, Dept Geog & Environm, Ctr Earth Observat Sci, Winnipeg, MB, Canada; [Norgaard-Pedersen, Niels] Geol Survey Denmark & Greenland, Dept Marine Geol, Copenhagen, Denmark; [Seidenkrantz, Marit-Solveig] Aarhus Univ, Dept Geosci, Ctr Climate Studies, Aarhus, Denmark	Geological Survey Of Denmark & Greenland; University of New Brunswick; University of Helsinki; UiT The Arctic University of Tromso; University of Copenhagen; Laval University; Aarhus University; University of Manitoba; Geological Survey Of Denmark & Greenland; Aarhus University	Limoges, A (通讯作者)，Geol Survey Denmark & Greenland, Dept Glaciol & Climate, Copenhagen, Denmark.; Limoges, A (通讯作者)，Univ New Brunswick, Dept Earth Sci, Fredericton, NB, Canada.	audrey.limoges@unb.ca	Ribeiro, Sofia/AAZ-2782-2021; Rysgaard, Søren/K-6689-2013; Zamelczyk, Katarzyna/AGK-4975-2022; Andersen, Thorbjorn Joest/N-7560-2014; Ribeiro, Sofia/G-9213-2018; Heikkila, Maija/N-7659-2013; Seidenkrantz, Marit-Solveig/A-3451-2012	Andersen, Thorbjorn Joest/0000-0001-5032-9945; Ribeiro, Sofia/0000-0003-0672-9161; Heikkila, Maija/0000-0003-3885-8670; Rysgaard, Soren/0000-0003-1726-2958; Weckstrom, Kaarina/0000-0002-3889-0788; Limoges, Audrey/0000-0002-4587-3417; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969	Villum Foundation, Denmark [VKR023454]; Arctic Research Centre; Aarhus University; Villum Foundation; Fonds de Recherche du Quebec - Nature et technologies (FRQNT) [188947]; Academy of Finland [296895]; Canada Excellence Research Chair program (CERC) [214902]; Danish Council for Independent Research (DFF-FNU) [0602-02361B]; Independent Research Fund Denmark [7014-00113B]; Academy of Finland (AKA) [296895] Funding Source: Academy of Finland (AKA)	Villum Foundation, Denmark(Villum Fonden); Arctic Research Centre; Aarhus University; Villum Foundation(Villum Fonden); Fonds de Recherche du Quebec - Nature et technologies (FRQNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Academy of Finland(Research Council of Finland); Canada Excellence Research Chair program (CERC); Danish Council for Independent Research (DFF-FNU)(Det Frie Forskningsrad (DFF)); Independent Research Fund Denmark(Det Frie Forskningsrad (DFF)); Academy of Finland (AKA)(Research Council of Finland)	The raw data obtained in this study are available in the supporting information. This study received financial support from the Villum Foundation, Denmark (grant VKR023454 to SRi.). Field work was funded by the Arctic Research Centre, Aarhus University, and the Villum Foundation. The Department of Environmental Science, Aarhus University is acknowledged for providing logistics at Villum Research Station in North Greenland. A. L. was also funded by the Fonds de Recherche du Quebec - Nature et technologies (FRQNT grant 188947). M. H. was also funded by the Academy of Finland (grant 296895). SRy was funded by the Canada Excellence Research Chair program (CERC grant 214902). M. S. S. was funded through the Danish Council for Independent Research (DFF-FNU grants 0602-02361B, OceanHeat) and the Independent Research Fund Denmark (grant 7014-00113B, G-Ice). We thank Kunuk Lennert, Jesper Hofmann, and Egon R. Frandsen for technical and logistical assistance in the field. We also appreciate outstanding logistical support from the Station Nord Danish military personnel. We further thank Leonid Polyak and Steffen Aagaard Sorensen for useful advice on benthic foraminiferal identification, Andrzej Witkowski for help with diatom taxonomy, and Laurence Dyke for commenting on the manuscript. This work is a contribution to the Arctic Science Partnership (ASP) and the ArcticNet Networks of Centres of Excellence programs.	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Geophys. Res.-Biogeosci.	MAR	2018	123	3					760	786		10.1002/2017JG003840	http://dx.doi.org/10.1002/2017JG003840			27	Environmental Sciences; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	GD0HG		Green Published, hybrid			2025-03-11	WOS:000430181200002
J	Mansour, A; Mohamed, O; Tahoun, SS; Elewa, AMT				Mansour, Ahmed; Mohamed, Omar; Tahoun, Sameh S.; Elewa, Ashraf M. T.			Sequence stratigraphy of the Raha Formation, Bakr Oil Field, Gulf of Suez, Egypt: Insights from electrical well log and palynological data	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Raha Formation; Sequence stratigraphy; Gamma ray log; Palynofacies analysis; Gulf of Suez; Egypt	CRETACEOUS-TERTIARY BOUNDARY; SEDIMENTARY ORGANIC-MATTER; NORTH-WESTERN DESERT; SEA-LEVEL CHANGES; DINOFLAGELLATE CYSTS; BAHARIYA FORMATION; PALYNOFACIES; BASIN; SUCCESSION; BOREHOLE	The current paper provides a high resolution sequence stratigraphic study of the Raha Formation from the productive Bakr Oil Field, central Gulf of Suez, Egypt. Sixty cutting rock samples spanning the Cenomanian from three wells (Bakr-114, B-115 and B-109) in the Bakr Basin, were palynologically investigated. The documented palynomorphs assemblage of either terrestrially-derived sporomorphs or marine inhabited dinocysts, allowed two palynological zones as well as their encompassing depositional palaeoenvironment to be recognized. These zones are Afropollis jardinus-Crybelosporites pannuceus Assemblage Zone (early-middle Cenomanian) and Classopollis brasiliensis-Tricolpites sagax Assemblage Zone (late Cenomanian). Detailed analysis of the particulate organic matter compositions suggested that the depositional palaeoenvironment of the Raha Formation was fluctuating between supratidal and distal-inner neritic conditions, due to successive oscillations of the Neo-Tethyan Ocean during the Cenomanian. The pronounced peaks of particulate organic matter versus gamma ray are markedly used in delineating the depositional sequences of the Raha Formation and their bounding surfaces. The Raha Formation probably corresponds to a second-order depositional sequence, which can be further subdivided into eight third-order depositional sequences, of which six are complete and two are incomplete ones. These depositional sequences are significantly synchronized based on a simple 2-D correlation model between the three wells. According to the hierarchical duration system, the Cenomanian herein was approximately attributed to 6 Myr, each of which has lower order depositional sequences that took approximately 0.9 Myr. Based on the sequence stratigraphic approach together with palynofacies analysis and gamma ray data, a condensed section was defined in the B-115. (C) 2017 Elsevier Ltd. All rights reserved.	[Mansour, Ahmed; Mohamed, Omar; Elewa, Ashraf M. 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Afr. Earth Sci.	MAR	2018	139						205	221		10.1016/j.jafrearsci.2017.12.009	http://dx.doi.org/10.1016/j.jafrearsci.2017.12.009			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FV6XG					2025-03-11	WOS:000424724800015
J	Worobiec, E; Gedl, P				Worobiec, Elzbieta; Gedl, Przemyslaw			Upper Eocene palynoflora from Lukowa (SE Poland) and its palaeoenvironmental context	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palynology; Palaeovegetation; Palaeoclimate; Palaeogeography; Priabonian; Europe	BOREHOLE CARPATHIAN FOREDEEP; DINOFLAGELLATE CYSTS; COEXISTENCE APPROACH; NORTHWESTERN GERMANY; POLLEN DISTRIBUTION; MARINE-SEDIMENTS; PLANT FOSSILS; MIOCENE; RECONSTRUCTION; CLIMATE	This paper presents the results of a palynological investigation of the sands from upper Eocene (Priabonian) epicontinental marine strata at Lukowa, SE Poland. This locality represents an isolated spot of upper Eocene strata in the southern part of epicontinental Poland due to later uplift and erosion of this area. The sands studied yielded a well-preserved palynoflora, providing information about palaeovegetation and palaeoclimate after the Early Eocene Climate Optimum. During the study a total of 94 fossil species of palynomorphs were identified. The results indicate that the vicinity of the sedimentary basin was covered by vegetation with a significant portion of thermophilous taxa and containing many elements with East Asian affinities. The plant communities were composed of Platanus, Platyccuya, Engelhardioideae, members of the Hamamelidaceae, Sapotaceae, Fabaceae, Oleaceae, Fagaceae (probably evergreen Quercus and Castanoideae), and Betulaceae families, as well as Salix, Carya, and others. Members of the Pinaceae family and Sciadopitys were components of coniferous or mixed forests. Taxodium, and presumably Glyptostrobus, together with Nyssa, might have covered areas with a higher groundwater level. The pollen of Milfordia and Aglaoreidia cyclops can probably be considered as representing marsh/freshwater vegetation. Cryptogams are represented mainly by ferns (including members of the Lygodiaceae and Schizaeaceae, probably as well as Gleicheniaceae and Cyatheaceae families) and Lycopodiaceae (including Lycopodiella). The presence of frequent pollen and spores of the genera presently growing under tropical and subtropical climatic conditions and the presence of several taxa characteristic for swamps indicate that the climate during deposition of the sediments studied was warm and humid. The mean annual temperature of 17.2-23.1 degrees C was estimated on the basis of Coexistence Approach method.	[Worobiec, Elzbieta] Polish Acad Sci, W Szafer Inst Bot, Lubicz 46, PL-31512 Krakow, Poland; [Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, Senacka 1, PL-31002 Krakow, Poland	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	Worobiec, E (通讯作者)，Polish Acad Sci, W Szafer Inst Bot, Lubicz 46, PL-31512 Krakow, Poland.	e.worobiec@botany.pl; ndgedl@cyf-kr.edu.pl		Worobiec, Elzbieta/0000-0001-5997-9602	W. Szafer Institute of Botany, Polish Academy of Sciences	W. Szafer Institute of Botany, Polish Academy of Sciences	Authorities of the Polskie Gornictwo Naftowe i Gazownictwo SA (PGNiG) are kindly acknowledged for granted permission for use their samples and for publication of research results. The study was supported by the W. Szafer Institute of Botany, Polish Academy of Sciences, through statutory funds for E. Worobiec. We would like to thank Grzegorz Worobiec (W. Szafer Institute of Botany PAS) for his help in photographing palynomorphs as well as Torsten Utescher (Senckenberg Research Institute, Germany), Johannes M. Bouchal (Swedish Museum of Natural History) and one anonymous reviewer for critically reading the manuscript and for their valuable suggestions.	Akkiraz MS, 2006, TURK J EARTH SCI, V15, P155; [Anonymous], 1978, Geol. 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Paleoclimatol. Paleoecol.	MAR 1	2018	492						134	146		10.1016/j.palaeo.2017.12.019	http://dx.doi.org/10.1016/j.palaeo.2017.12.019			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	FW1PV					2025-03-11	WOS:000425072800011
J	Thomas, ML; Warny, S; Jarzen, DM; Bentley, SJ; Droxler, AW; Harper, BB; Nittrouer, CA; Xu, KH				Thomas, Marie L.; Warny, Sophie; Jarzen, David M.; Bentley, Samuel J., Sr.; Droxler, Andre W.; Harper, Brandon B.; Nittrouer, Charles A.; Xu, Kehui			Palynomorph evidence for tropical climate stability in the Gulf of Papua, Papua New Guinea, over the latest marine transgression and highstand (14,500 years BP to today)	QUATERNARY INTERNATIONAL			English	Article						Palynology; Gulf of Papua; Papua New Guinea; Climate; Dinoflagellate cyst; Pollen	LAST GLACIAL MAXIMUM; LATE QUATERNARY; POLLEN MORPHOLOGY; SEDIMENT DELIVERY; DINOFLAGELLATE CYSTS; VEGETATION CHANGE; HUON PENINSULA; NICARAGUA RISE; TORRES STRAIT; KUK SWAMP	Three sediment cores (MV-41, MV-46, and MD-50) from the Gulf of Papua (GoP), Papua New Guinea, were analyzed to assess changes in climatic, oceanographic, and sedimentological conditions over the last 14.5 kyr. Palynomorphs, which were isolated from sediment core samples, were collected at approximately 0.5-m intervals using a strong acid and oxidant (MD-50)/non-oxidant (MV-41, MV-46) procedure. Radiocarbon (C-14) stable isotope geochronology, magnetic susceptibility, stable isotope analysis (MD-50 only; Oxygen-18 [O-18] and Carbon-13 [C-13]), and clay mineral maturity analysis were also completed for each core. Palynological data indicate that climatic conditions at sea level have remained warm, wet, and stable for the past 14.5 kyr with sea surface temperatures in the GoP above 14 degrees C. Potential decreases in vegetative cover marked the Younger Dryas interval (12.5-11.5 kyr BP), as indicated by reduced pollen and spore recovery. The end of the latest marine transgression (and the subsequent return to eustatic sea level highstand) is clearly delineated by increases in marine palynomorph recovery and decreases in mangrove pollen at approximately 5 kyr BP. An increase in seasonality and potential El Nino Southern Oscillation variability is observed in MD-50's oxygen isotope results at similar to 5 kyr BP. This is not supported by the palynomorph record, likely because of the sampling interval and dilution by tropical pollen flora, which indicates stable climatic conditions throughout the last 14.5 kyr. Sediment transport pathways in the GoP remained fairly constant throughout the time interval, which is supported by the lack of major changes in palynomorph assemblage composition. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.	[Thomas, Marie L.; Warny, Sophie; Bentley, Samuel J., Sr.] Louisiana State Univ, Dept Geol & Geophys, E235 Howe Russell Geosci Complex, Baton Rouge, LA 70803 USA; [Thomas, Marie L.] Hess Corp, 1501 McKinney St, Houston, TX 77010 USA; [Warny, Sophie] Louisiana State Univ, LSU Museum Nat Sci, Baton Rouge, LA 70803 USA; [Jarzen, David M.] Cleveland Museum Nat Hist, Paleobot & Paleoecol, 1 Wade Oval Dr, Cleveland, OH 44106 USA; [Bentley, Samuel J., Sr.] Louisiana State Univ, Coastal Studies Inst, Baton Rouge, LA 70803 USA; [Droxler, Andre W.; Harper, Brandon B.] Rice Univ, Dept Earth Sci, 6100 Main St, Houston, TX 77005 USA; [Harper, Brandon B.] Conoco Phillips, 600 N Dairy Ashford Rd, Houston, TX 77079 USA; [Nittrouer, Charles A.] Univ Washington, Sch Oceanog, Box 357940,1503 NE Boat St, Seattle, WA 98195 USA; [Xu, Kehui] Louisiana State Univ, Dept Oceanog & Coastal Sci, 2165 Energy,Coast & Environm Bldg, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University; Hess Corporation; Louisiana State University System; Louisiana State University; Cleveland Museum of Natural History; Louisiana State University System; Louisiana State University; Rice University; ConocoPhillips; University of Washington; University of Washington Seattle; Louisiana State University System; Louisiana State University	Thomas, ML (通讯作者)，Hess Corp, 1501 McKinney St, Houston, TX 77010 USA.	mlthomas716@yahoo.com	Warny, Sophie/A-8226-2013; Xu, Kehui/D-5446-2009	Bentley, Samuel/0000-0001-5826-7689; Xu, Kehui/0000-0002-3696-6160; Warny, Sophie/0000-0002-3451-040X	National Science Foundation (NSF); Marathon GeoDE Fellowship; AASP - The Palynological Society; Encana; Mary Jo Klosterman Professorship	National Science Foundation (NSF)(National Science Foundation (NSF)); Marathon GeoDE Fellowship; AASP - The Palynological Society; Encana; Mary Jo Klosterman Professorship	Samples from MV-41 and MV-46 were collected on a National Science Foundation (NSF)-funded PANASH (Paleoclimates of the Northern and Southern Hemisphere) cruise on the R/V Melville in 2004. Samples from MD-50 were collected on a 2005 MD148-PECTEN (Past Equatorial Climate: Tracking El Nino) cruise on the R/V Marion Dufresne. Sample processing, collection from curation sites, and analysis were primarily funded by the Marathon GeoDE Fellowship. Hess Corporation provided the Stratabugs program and license for plotting data. AASP - The Palynological Society, Encana, and the Mary Jo Klosterman Professorship also provided financial support for this project.	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Int.	FEB 22	2018	467		B				277	291		10.1016/j.quaint.2017.12.035	http://dx.doi.org/10.1016/j.quaint.2017.12.035			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	FZ3AG		Bronze			2025-03-11	WOS:000427457000009
J	Prebble, JG; Hinojosa, JL; Moy, CM				Prebble, Joseph G.; Hinojosa, Jessica L.; Moy, Christopher M.			Palynofacies assemblages reflect sources of organic matter in New Zealand fjords	CONTINENTAL SHELF RESEARCH			English	Article						Fjords; Palynofacies; Dinoflagellate cysts; Organic carbon	WALLED DINOFLAGELLATE CYSTS; TIERRA-DEL-FUEGO; SURFACE SEDIMENTS; CARBON BURIAL; SOUTHERN-HEMISPHERE; HOLOCENE SEDIMENTS; BEAGLE CHANNEL; TERRESTRIAL; MARINE; RATES	Understanding sources and transport pathways of organic carbon in fjord systems is important to quantify carbon cycling in coastal settings. Provenance of surficial sediment organic carbon in Fiordland National Park (southwestern New Zealand) has previously been estimated using a range of techniques, including mixing models derived from stable isotopes and lipid biomarker distributions. Here, we present the first application of palynofacies to explore the sources of particulate organic carbon to five fjords along the SW margin of New Zealand, to further discriminate the provenance of organic carbon in the fjords. We find good correlation between isotopic-and biomarker-derived proxies for organic carbon provenance and our new palynofacies observations. We observe strong down-fjord gradients of decreasing terrestrially derived organic carbon further from the river inflow at fjord heads. Fjords with small catchments and minor fresh water inflow exhibit reversed gradients, indicating that volume of freshwater entering at the fjord head is a primary mechanism to transport particulates down fjord rather than local transport from fjord sides. The palynofacies data also confirmed previously recorded latitudinal trends (i.e. between fjords), of less frequent and more weathered terrestrially derived organic carbon in the southern fjords, consistent with enhanced marine inflow and longer transport times in the southern catchments. Dinocyst assemblages also exhibit a strong latitudinal gradient, with assemblages dominated by heterotrophic forms in the north. In addition to providing support for previous studies, this approach allows finer discrimination of terrestrial organic carbon than previously, for example variation of leaf material. This study demonstrates that visual palynofacies analysis is a valuable tool to pinpoint origins of organic carbon in fjord systems, providing different but complementary information to other proxies.	[Prebble, Joseph G.] GNS Sci, POB 30368, Lower Hutt 5040, New Zealand; [Hinojosa, Jessica L.] CALTECH, Div Geol & Planetary Sci, 1200 E Calif Blvd,MC 100-23, Pasadena, CA 91125 USA; [Moy, Christopher M.] Univ Otago, Dept Geol, POB 56, Dunedin 9054, New Zealand	GNS Science - New Zealand; California Institute of Technology; University of Otago	Prebble, JG (通讯作者)，GNS Sci, POB 30368, Lower Hutt 5040, New Zealand.	j.prebble@gns.cri.nz		Hinojosa, Jessica/0000-0002-8589-102X	Global Change Through Time programme - New Zealand government	Global Change Through Time programme - New Zealand government	JP was supported by the Global Change Through Time programme, funded by the New Zealand government. We thank the crew of the University of Otago research vessel, Polaris II, for collection of sediment samples analysed in this study. We thank E. Crouch and G. Cortese for commenting on an early version of this manuscript, and three journal reviewers for their comments.	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Shelf Res.	FEB 15	2018	154						19	25		10.1016/j.csr.2017.12.009	http://dx.doi.org/10.1016/j.csr.2017.12.009			7	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	FX9HS					2025-03-11	WOS:000426409800003
J	Frieling, J; Huurdeman, EP; Rem, CCM; Donders, TH; Pross, J; Bohaty, SM; Holdgate, GR; Gallagher, SJ; McGowran, B; Bijl, PK				Frieling, Joost; Huurdeman, Emiel P.; Rem, Charlotte C. M.; Donders, Timme H.; Pross, Joerg; Bohaty, Steven M.; Holdgate, Guy R.; Gallagher, Stephen J.; McGowran, Brian; Bijl, Peter K.			Identification of the Paleocene-Eocene boundary in coastal strata in the Otway Basin, Victoria, Australia	JOURNAL OF MICROPALAEONTOLOGY			English	Article							THERMAL MAXIMUM; NEW-ZEALAND; SOUTH-PACIFIC; CARBON-CYCLE; SEA-LEVEL; CLIMATE; MARGIN; EVOLUTION; OCEAN; TEMPERATURES	Detailed, stratigraphically well-constrained environmental reconstructions are available for Paleocene and Eocene strata at a range of sites in the southwest Pacific Ocean (New Zealand and East Tasman Plateau; ETP) and Integrated Ocean Discovery Program (IODP) Site U1356 in the south of the Australo-Antarctic Gulf (AAG). These reconstructions have revealed a large discrepancy between temperature proxy data and climate models in this region, suggesting a crucial error in model, proxy data or both. To resolve the origin of this discrepancy, detailed reconstructions are needed from both sides of the Tasmanian Gateway. Paleocene-Eocene sedimentary archives from the west of the Tasmanian Gateway have unfortunately remained scarce (only IODP Site U1356), and no well-dated successions are available for the northern sector of the AAG. Here we present new stratigraphic data for upper Paleocene and lower Eocene strata from the Otway Basin, southeast Australia, on the (north) west side of the Tasmanian Gateway. We analyzed sediments recovered from exploration drilling (Latrobe-1 drill core) and outcrop sampling (Point Margaret) and performed high-resolution carbon isotope geochemistry of bulk organic matter and dinoflagellate cyst (dinocyst) and pollen biostratigraphy on sediments from the regional lithostratigraphic units, including the Pebble Point Formation, Pember Mudstone and Dilwyn Formation. Pollen and dinocyst assemblages are assigned to previously established Australian pollen and dinocyst zonations and tied to available zonations for the SW Pacific. Based on our dinocyst stratigraphy and previously published planktic foraminifer biostratigraphy, the Pebble Point Formation at Point Margaret is dated to the latest Paleocene. The globally synchronous negative carbon isotope excursion that marks the Paleocene-Eocene boundary is identified within the top part of the Pember Mudstone in the Latrobe-1 borehole and at Point Margaret. However, the high abundances of the dinocyst Apectodinium prior to this negative carbon isotope excursion prohibit a direct correlation of this regional bio-event with the quasi-global Apectodinium acme at the Paleocene-Eocene Thermal Maximum (PETM; 56 Ma). Therefore, the first occurrence of the pollen species Spinizonocolpites prominatus and the dinocyst species Florentinia reichartii are here designated as regional markers for the PETM. In the Latrobe-1 drill core, dinocyst biostratigraphy further indicates that the early Eocene (similar to 56-51 Ma) sediments are truncated by a similar to 10 Myr long hiatus overlain by middle Eocene (similar to 40 Ma) strata. These sedimentary archives from southeast Australia may prove key in resolving the model-data discrepancy in this region, and the new stratigraphic data presented here allow for detailed comparisons between paleoclimate records on both sides of the Tasmanian Gateway.	[Frieling, Joost; Huurdeman, Emiel P.; Rem, Charlotte C. M.; Bijl, Peter K.] Univ Utrecht, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol, Dept Earth Sci,Fac Geosci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Donders, Timme H.] Univ Utrecht, Palaeoecol, Lab Palaeobot & Palynol, Dept Phys Geog,Fac Geosci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, Neuenheimer Feld 234, D-69120 Heidelberg, Germany; [Bohaty, Steven M.] Univ Southampton, Natl Oceanog Ctr Southampton, Ocean & Earth Sci, Southampton, Hants, England; [Holdgate, Guy R.; Gallagher, Stephen J.] Univ Melbourne, Sch Earth Sci, Melbourne, Vic, Australia; [McGowran, Brian] Univ Adelaide, Dept Earth Sci, Adelaide, SA, Australia	Utrecht University; Utrecht University; Ruprecht Karls University Heidelberg; University of Southampton; NERC National Oceanography Centre; University of Melbourne; University of Adelaide	Frieling, J (通讯作者)，Univ Utrecht, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol, Dept Earth Sci,Fac Geosci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands.	j.frieling1@uu.nl	Gallagher, Stephen/AFL-9448-2022; Donders, Timme/J-5044-2012	Bijl, Peter/0000-0002-1710-4012; Gallagher, Stephen/0000-0002-5593-2740; Frieling, Joost/0000-0002-5374-1625; Donders, Timme/0000-0003-4698-3463	NWO VENI [863.13.002]; Heidelberg University; ARC Basin Genesis Hub	NWO VENI(Netherlands Organization for Scientific Research (NWO)); Heidelberg University; ARC Basin Genesis Hub	This research was funded through NWO VENI grant no. 863.13.002 to Peter K. Bijl. Jorg Pross acknowledges financial support by Heidelberg University. Stephen J. Gallagher was partly funded by the ARC Basin Genesis Hub. We thank Natasja Welters, Giovanni Dammers and Arnold van Dijk (Utrecht University) and Rineke Gieles, Marcel van der Meer and Ronald van Bommel (Netherlands Institute for Sea Research (NIOZ)) for technical assistance. Wim Hoek (Utrecht University) and Marcel van der Linden and Johan van Heerwaarden (NIOZ) are thanked for help developing the casing technique of sampling. We thank Erica Crouch and an anonymous reviewer for their constructive comments.	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J	David, M; Gollasch, S				David, Matej; Gollasch, Stephan			How to approach ballast water management in European seas	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Ballast water management; Harbours; Risks; Introduced species; Decision support	PROPAGULE PRESSURE; COLONIZATION PRESSURE; DINOFLAGELLATE CYSTS; SHIPS; MARINE; SEDIMENTS; INVASIONS; DISPERSAL; MODEL	The latest research continues to show that the ballast water issue is very complex, which makes it very challenging to manage. In 2004, the International Convention for the Control and Management of Ships' Ballast Water and Sediments (BWM Convention) was adopted to globally harmonize action against the transfer of harmful aquatic organisms and pathogens via ships' ballast water and related sediments. Analyses of the BWM Convention requirements, conducted through different research projects mainly aiming to provide support for the implementation of the BWM Convention, have shown that there are different steps countries need to take and that there are still some open issues which need to be solved. This paper presents some of the main issues identified and the core theoretical and applied measures required to solve these issues, with the aim to support more efficient and coordinated implementation of the BWM Convention requirements in EU seas. The approaches recommended here for the EU may be universally interesting for similar application in other areas of the world. (C) 2016 Elsevier Ltd. All rights reserved.	[David, Matej] Dr Matej David Consult, Korte 13e, SI-6310 Izola, Slovenia; [Gollasch, Stephan] GoConsult, Grosse Brunnenstr 61, DE-22763 Hamburg, Germany		David, M (通讯作者)，Dr Matej David Consult, Korte 13e, SI-6310 Izola, Slovenia.	matej.david@siol.net	Gollasch, Stephan/AAI-2041-2021; David, Matej/IQR-6321-2023	Gollasch, Stephan/0000-0003-4410-6969; David, Matej/0000-0003-0650-1730	European Union [266445]	European Union(European Union (EU))	The research leading to these results has received funding from the European Union's Seventh Framework Programme for research, technological development and demonstration (FP7/2007-2013) within the Ocean of Tomorrow call under Grant Agreement No.266445 for the project Vectors of Change in Oceans and Seas Marine Life, Impact on Economic Sectors (VECTORS). We like to thank Sarah Bailey (Fisheries and Oceans Canada, Great Lakes Laboratory for Fisheries and Aquatic Sciences, Burlington, Canada) for language editing and constructive comments on this manuscript.	[Anonymous], 2004, INT CONVENTION CONTR; [Anonymous], THESIS; [Anonymous], 1959, Archivio di Oceanografia e Limnologia, V11, P243; Bailey SA, 2007, AQUAT ECOSYST HEALTH, V10, P93, DOI 10.1080/14634980701193870; Bleich S, 2006, THESIS U ROSTOCK GER; Briski E, 2012, BIOL INVASIONS, V14, P1843, DOI 10.1007/s10530-012-0194-0; Briski E, 2012, P ROY SOC B-BIOL SCI, V279, P2990, DOI 10.1098/rspb.2011.2671; Carlton J. T., 1995, 6 RES NAT SEA GRANT; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; Casale G. A., 2002, BALLAST WATER NEWS; Chan FT, 2015, P ROY SOC B-BIOL SCI, V282, DOI 10.1098/rspb.2014.1517; Colautti RI, 2006, BIOL INVASIONS, V8, P1023, DOI 10.1007/s10530-005-3735-y; Courts A. D. 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Coast. Shelf Sci.	FEB 5	2018	201				SI		248	255		10.1016/j.ecss.2016.10.018	http://dx.doi.org/10.1016/j.ecss.2016.10.018			8	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	FY9TP					2025-03-11	WOS:000427210100024
J	Boyd, JL; Riding, JB; Pound, MJ; De Schepper, S; Ivanovic, RF; Haywoo, AM; Wood, SEL				Boyd, Jamie L.; Riding, James B.; Pound, Matthew J.; De Schepper, Stijn; Ivanovic, Ruza F.; Haywoo, Alan M.; Wood, Stephanie E. L.			The relationship between Neogene dinoflagellate cysts and global climate dynamics	EARTH-SCIENCE REVIEWS			English	Article						Dinoflagellate cysts; Global distributions; Neogene; Palaeoclimate; Palaeoecology; Palaeotemperature	SEA-SURFACE TEMPERATURE; BASIN NORTHERN BELGIUM; LATE MIOCENE CLIMATE; CARBON-DIOXIDE CONCENTRATIONS; MIDDLE MIOCENE; LATE PLIOCENE; PALYNOLOGICAL EVIDENCE; MARINE PALYNOMORPHS; BENGUELA CURRENT; ATLANTIC OCEAN	The Neogene Period (23.03-2.58 Ma) underwent a long-term, relatively gradual cooling trend, culminating in the glacial-interglacial climate of the Quaternary. Palaeoclimate studies on the Neogene have provided important information for understanding how modern patterns of atmospheric and oceanic circulation developed, and how they may relate to wider environmental change. Here we use a newly created global database of Neogene dinoflagellate cysts (the Tertiary Oceanic Parameters Information System - TOPIS) to investigate how dinoflagellate cysts recorded the cooling of Neogene surface marine waters on a global scale. Species with warm and cold water preferences were determined from previously published literature and extracted from the database. Percentages of cold water species were calculated relative to the total number of species with known temperature preferences from each site and compared throughout the Neogene at differing latitudes. Overall, the percentage of cold water species increases gradually through the Neogene. This trend indicates a gradual global cooling that is comparable to that reported from other marine and terrestrial proxies. This also demonstrates the use of dinoflagellate cysts in determining temperature change on both extended temporal and wide geographical scales. The increase in the percentage of cold water species of dinoflagellate cysts recorded worldwide from the Early and Middle Miocene to the Late Pliocene indicates a global scale forcing agent on Neogene climate such as CO2.	[Boyd, Jamie L.; Ivanovic, Ruza F.; Haywoo, Alan M.] Univ Leeds, Sch Earth & Environm, Woodhouse Lane, Leeds LS1 9JT, W Yorkshire, England; [Riding, James B.] British Geol Survey, Environm Sci Ctr, Keyworth NG12 5GG, Notts, England; [Pound, Matthew J.] Northumbria Univ, Dept Geog & Environm Sci, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England; [De Schepper, Stijn] Bjerknes Ctr Climate Res, Uni Res Climate, POB 7801, N-5020 Bergen, Norway; [Wood, Stephanie E. L.] Univ Sheffield, Dept Anim & Plant Sci, Western Bank, Sheffield S10 2TN, S Yorkshire, England	University of Leeds; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Northumbria University; Bjerknes Centre for Climate Research; University of Sheffield	Riding, JB (通讯作者)，British Geol Survey, Environm Sci Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk	Ivanovic, Ruza/C-5941-2012; De Schepper, Stijn/A-2836-2011	Ivanovic, Ruza/0000-0002-7805-6018; Pound, Matthew/0000-0001-8029-9548; De Schepper, Stijn/0000-0002-6934-0914	British Geological Survey (BGS) University Funding Initiative (BUFI); University of Leeds; BGS [GA/12S/004]; BUFI [S227]; NERC [NE/K008536/1]; Norwegian Research Council [229819]; NERC [bgs05017, NE/K008536/1] Funding Source: UKRI	British Geological Survey (BGS) University Funding Initiative (BUFI)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); University of Leeds; BGS; BUFI; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Norwegian Research Council(Research Council of Norway); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research was jointly funded by the British Geological Survey (BGS) University Funding Initiative (BUFI) and the University of Leeds. The BGS contract number was GA/12S/004, and the BUFI reference was S227. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). Ruza F. Ivanovic is funded by a NERC Independent Research Fellowship (#NE/K008536/1). Stijn De Schepper is funded by the Norwegian Research Council (project 229819). Finally, we extend our sincere thanks to the journal editor and to two anonymous reviewers whose perceptive comments and critiques helped us to significantly improve the manuscript.	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Rev.	FEB	2018	177						366	385		10.1016/j.earscirev.2017.11.018	http://dx.doi.org/10.1016/j.earscirev.2017.11.018			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FX9HM		Green Accepted			2025-03-11	WOS:000426409200022
J	Trottet, A; Wilson, B; Xin, GSW; George, C; Casten, L; Schmoker, C; Rawi, NSBM; Siew, MC; Larsen, O; Eikaas, HS; Tun, K; Drillet, G				Trottet, Aurore; Wilson, Bryan; Xin, Genevieve Sew Wei; George, Christaline; Casten, Lemuel; Schmoker, Claire; Rawi, Nurul Syazana Binte Modh; Siew, Moon Chew; Larsen, Ole; Eikaas, Hans S.; Tun, Karenne; Drillet, Guillaume			Resting Stage of Plankton Diversity from Singapore Coastal Water: Implications for Harmful Algae Blooms and Coastal Management	ENVIRONMENTAL MANAGEMENT			English	Article						phytoplankton; zooplankton; bacteria; spores; cysts; dormancy	DINOFLAGELLATE CYST DISTRIBUTION; GRADIENT GEL-ELECTROPHORESIS; CALANOID COPEPOD EGGS; ACARTIA-TONSA DANA; RNA GENE DATABASE; 16S RIBOSOMAL-RNA; SEA-BOTTOM MUDS; BALLAST WATER; INLAND SEA; MORPHOLOGICAL-CHARACTERISTICS	Resting strategies of planktonic organisms are important for the ecological processes of coastal waters and their impacts should be taken into consideration in management of water bodies used by multiple industries. We combined different approaches to evaluate the importance of resting stages in Singapore coastal waters. We used molecular approaches to improve the knowledge on Singapore biodiversity, we sampled and extracted cysts from sediments to evaluate the density of resting stages in Johor Strait, and we compared systematically information on Singapore planktonic biodiversity to existing published information on resting stages from these reported organisms. This is the first study evaluating the importance of resting stages in Singapore waters. Above 120 species reported in Singapore are known to produce resting stages though no previous work has ever been done to evaluate the importance of these strategies in these waters. The results from the resting stage survey confirmed 0.66 to 5.34 cyst g(-1) dry weight sediment were present in the Johor Strait suggesting that cysts may be flushed by tidal currents into and out of the strait regularly. This also suggest that the blooms occurring in Singapore are likely due to secondary growth of Harmful Algae Bloom species in the water rather than from direct germination of cysts from sediment. Finally, we discuss the importance of these resting eggs for three main national industries in Singapore (shipping, marine aquaculture and provision of drinking water through seawater desalination). We argue that this study will serve as a baseline for some of the future management of Singapore waters.	[Trottet, Aurore; Xin, Genevieve Sew Wei; George, Christaline; Casten, Lemuel; Schmoker, Claire; Rawi, Nurul Syazana Binte Modh; Siew, Moon Chew; Larsen, Ole; Eikaas, Hans S.; Drillet, Guillaume] DHI Water & Environm Singapore, 1 CleanTech Loop,03-05 CleanTech One, Singapore 637141, Singapore; [Wilson, Bryan] Univ Bergen, Dept Biol, Marine Microbiol Res Grp, Thormohlensgate 53B, N-5020 Bergen, Norway; [Xin, Genevieve Sew Wei] Natl Univ Singapore, Dept Biol Sci, 14 Sci Dr 4, Singapore 117543, Singapore; [Tun, Karenne] Natl Pk Board, 1 Cluny Rd, Singapore 259569, Singapore	Danish Hydraulic Institute (DHI); University of Bergen; National University of Singapore	Trottet, A (通讯作者)，DHI Water & Environm Singapore, 1 CleanTech Loop,03-05 CleanTech One, Singapore 637141, Singapore.	auroretrottet@gmx.fr	Drillet, Guillaume/B-6608-2009; Trottet, Aurore/KIE-3763-2024; Trottet, Aurore/Y-2389-2018	Drillet, Guillaume/0000-0001-5908-0568; Wilson, Bryan/0000-0001-9000-2920; Trottet, Aurore/0000-0003-2628-6732	National Parks of Singapore; DHI-NTU Research Centre; Danish Agency for Science Technology and Innovation [10-093759, 10-094773]	National Parks of Singapore; DHI-NTU Research Centre; Danish Agency for Science Technology and Innovation	We thank the National Parks of Singapore, the DHI-NTU Research Centre for the financial support of the project "Made In Plankton". The work was also supported by Elite Forsk grants nb 10-093759 and 10-094773 from the Danish Agency for Science Technology and Innovation to Guillaume Drillet. Finally, we would like to thank the entire plankton team from the Environmental Laboratories in Singapore for their continuous support and attitude toward new challenges. The authors would like to thank the two anonymous reviewers provided helpful comments on previous versions of the manuscript.	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Manage.	FEB	2018	61	2					275	290		10.1007/s00267-017-0966-5	http://dx.doi.org/10.1007/s00267-017-0966-5			16	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	FV0UB	29204675				2025-03-11	WOS:000424273700009
J	Zhang, Y; Yu, ZM; Song, XX; Yuan, YQ; Cao, XH				Zhang, Yue; Yu, Zhiming; Song, Xiuxian; Yuan, Yongquan; Cao, Xihua			Effects of modified clay used for the control of harmful algal blooms on <i>Alexandrium pacificum</i> cysts	HARMFUL ALGAE			English	Article						Modified clay; Alexandrium pacificum; Cyst; Encystment; Germination	SPECIES COMPLEX DINOPHYCEAE; TAMARENSE DINOPHYCEAE; TOXIC DINOFLAGELLATE; RESTING CYSTS; GONYAULAX-TAMARENSIS; SHELLFISH TOXICITY; FUNDYENSE CYST; RED TIDE; GERMINATION; GULF	Cyst formation plays an important role in the resistance of dinofiagellates to adverse environments, and cyst germination is considered one of the causes of harmful algal blooms (HABs). Among the methods for mitigating HABs, modified clay (MC) is considered a promising strategy because of its high efficiency and low environmental impacts. The typical HAB species Alexandrium pacificum was focused on in this study to clarify the effects of MC on cyst formation and germination. The results showed that more than 90% of the vegetative cells were removed under the 0.6 g/L. MC treatment. The vegetative cell density was monitored over 90 d and increased slightly to the peak at 10 d after the cell removal experiment, but persistent growth was not observed. The amount of cysts was maximal at 20 d after removal, however, most of the cysts were temporary cysts that subsequently disappeared. After 80 d, all the remaining cysts were resting ones. The total density of resting cysts was higher under MC concentrations of 0.2 and 0.4 g/L and lower under concentrations of 0.6, 0.8 and 1.0 g/L compared with that in the control. The total formation rate of resting cysts was 29.6% in the control group, and the lowest formation rate in the experimental groups was 15.5% at 0.6 g/L. MC. The total germination rate of resting cyst decreased as the MC concentration increased, and approximately 68.0% of the resting cysts in the control group germinated successfully, whereas the addition of MC reduced the germination rate to as low as 12.4%. Our results indicated that the application of appropriate MC concentrations may provide an effective mitigation strategy for A. pacificum blooms because it does not leave more residual cysts, which can act as "seeds" for the initiation of HABs. (C) 2017 Elsevier B.V. All rights reserved.	[Zhang, Yue; Yu, Zhiming; Song, Xiuxian; Yuan, Yongquan; Cao, Xihua] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Zhang, Yue; Yu, Zhiming; Song, Xiuxian] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Zhang, Yue; Yu, Zhiming; Song, Xiuxian; Yuan, Yongquan; Cao, Xihua] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Song, XX (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	songxx@qdio.ac.cn		Zhang, Yue/0000-0002-4427-6127; YUAN, Yongquan/0000-0002-1337-4744; Yu, Zhiming/0000-0003-0377-1129	National Key R&D Program of China [2017YFC1404300]; Programs of the Qingdao National Laboratory for Marine Science and Technology [2016ASKJ02-3]; National Natural Science Foundation of China [41276115]	National Key R&D Program of China; Programs of the Qingdao National Laboratory for Marine Science and Technology; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	The authors would like to thank Dr. Zhangxi Hu for his kind help during the experiment. 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J	Zastrozhnov, D; Gernigon, L; Gogin, I; Abdelmalak, MM; Planke, S; Faleide, JI; Eide, S; Myklebust, R				Zastrozhnov, D.; Gernigon, L.; Gogin, I.; Abdelmalak, M. M.; Planke, S.; Faleide, J. I.; Eide, S.; Myklebust, R.			Cretaceous-Paleocene Evolution and Crustal Structure of the Northern VOring Margin (Offshore Mid-Norway): Results from Integrated Geological and Geophysical Study	TECTONICS			English	Article							DINOFLAGELLATE CYST BIOSTRATIGRAPHY; VOLCANIC CONTINENTAL MARGINS; RIFTED MARGINS; NORWEGIAN SEA; NE ATLANTIC; LOFOTEN-VESTERALEN; LITHOSPHERIC EXTENSION; CENOZOIC EVOLUTION; TECTONIC EVOLUTION; PASSIVE MARGINS	We present results of a multidisciplinary study of the northern segment of the VOring volcanic rifted margin, offshore mid-Norway. This segment represents a transitional margin domain that is less investigated compared to the adjacent segments of the margin. In order to understand the geological evolution of the study area, we performed an integrated interpretation of an extensive geological and geophysical data set. This data set includes recently acquired and reprocessed 2-D reflection seismic, published refraction data and potential field data, as well as new borehole data. Two-dimensional potential field modeling was performed to better assess the crustal architecture and evolution of the northern VOring Margin. We then consider how crustal-scale structures and processes affected the basin formation. The outer and distal northern VOring Margin represents a series of deep Cretaceous (Traena Basin and Nagrind Syncline) and Cretaceous-Paleocene (Hel Graben) sag subbasins underlain by a significantly thinned continental crust. These subbasins developed in between structural highs (Utgard, Nyk, and Grimm Highs), which are underlain by a thicker crust and interpreted as a series of rigid continental blocks (buffers). In addition to the regional Late Jurassic-Early Cretaceous rifting events, we found structural evidence of local Neocomian and mid-Cretaceous extensional reactivation affecting the northern segment of the VOring Basin. During the mid-Late Cretaceous-Paleocene, the extensional axis within the VOring Basin province migrated sequentially northwestward to the present-day continent-ocean boundary. We also show fundamental differences between the volcanic rifted mid-Norwegian Margin and nonvolcanic (Iberian-type) margins and how preexisting structures events can shape the evolution and architecture of the margin.	[Zastrozhnov, D.; Abdelmalak, M. M.; Planke, S.; Faleide, J. I.] Univ Oslo, Ctr Earth Evolut & Dynam, Oslo, Norway; [Zastrozhnov, D.; Abdelmalak, M. M.; Planke, S.] VBPR, Oslo Sci Pk, Oslo, Norway; [Gernigon, L.] Geol Survey Norway NGU, Trondheim, Norway; [Gogin, I.] RPS Ichron, Northwich, England; [Eide, S.] First Geo AS, Skoyen, Norway; [Myklebust, R.] TGS, Asker, Norway	University of Oslo; Geological Survey of Norway	Zastrozhnov, D (通讯作者)，Univ Oslo, Ctr Earth Evolut & Dynam, Oslo, Norway.; Zastrozhnov, D (通讯作者)，VBPR, Oslo Sci Pk, Oslo, Norway.	zastrozhe@gmail.com	Planke, Sverre/AAE-1721-2021; Zastrozhnov, Dmitry/AAM-9704-2020; Eide, Sigurd/HNP-2355-2023	Planke, Sverre/0000-0001-6128-2193; Zastrozhnov, Dmitry/0000-0003-2354-4708; Eide, Sigurd/0000-0003-0061-1867	OMNIS Project: Offshore Mid-Norwegian: Integrated Margin and Basin Studies - Norwegian Research Council through its Centre of Excellence CEED (Centre for Earth Evolution and Dynamics) [210429/E30]	OMNIS Project: Offshore Mid-Norwegian: Integrated Margin and Basin Studies - Norwegian Research Council through its Centre of Excellence CEED (Centre for Earth Evolution and Dynamics)	Funding for this work came from OMNIS Project: Offshore Mid-Norwegian: Integrated Margin and Basin Studies (project: 210429/E30) funded by the Norwegian Research Council through its Centre of Excellence CEED (Centre for Earth Evolution and Dynamics). The seismic, magnetic, and gravity data presented in this study were provided by TGS. RPS Ichron is acknowledged for performing biostratigraphic analysis of well 6608/2-1S. Seismic interpretation was done using IHS Kingdom software. Grid interpolations and map compilations were established using Geosoft Oasis Montaj and ArcGIS softwares. We would like to acknowledge First Geo AS and TGS for the use of hiQbe T regional velocity cube employed in depth conversion. We thank GeoModelling Solutions for providing an academic license for TecMod 2-D software. The seismic and well data used in this study are available through the Diskos National Data Repository (NDR). Well formation tops are also available at the NPD factpages (www.npd.no) and the NORLEX team website (www.nhm2.uio.no/norlex/). We are grateful to Jolante van Wijk (New Mexico Tech), Daniel Schmid (PGP, University of Oslo), and Sergei Medvedev (CEED, University of Oslo) for their help and fruitful discussions that improved the paper, and we thank Ben Manton (VBPR) for the linguistic remarks. We also would like to thank Christopher Jackson, Philip Ball, and the Editor Nathan Niemi for their constructive and helpful reviews.	Abdelmalak MM, 2017, TECTONICS, V36, P2497, DOI 10.1002/2017TC004617; Abdelmalak MM, 2016, J GEOPHYS RES-SOL EA, V121, P5212, DOI 10.1002/2015JB012788; Abdelmalak MM, 2016, TECTONOPHYSICS, V675, P258, DOI 10.1016/j.tecto.2016.02.037; Abdelmalak MM, 2015, GEOLOGY, V43, P1011, DOI 10.1130/G37086.1; Ainsworth NR, 2000, PETROL GEOSCI, V6, P345, DOI 10.1144/petgeo.6.4.345; Allen P.A., 2013, Basin analysis. Principles and Application to Petroleum Play Assessment, V3, P642; Anderson J. 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G., 1999, Petroleum Geology of Northwest Europe: Proceedings of the 5th Conference, V1, P325; Xie X, 2009, GEOL SOC AM BULL, V121, P55, DOI 10.1130/B26398.1; Yamasaki T, 2010, J GEOL SOC LONDON, V167, P961, DOI 10.1144/0016-76492010-027; Yamasaki T, 2009, TECTONOPHYSICS, V468, P169, DOI 10.1016/j.tecto.2008.04.024	148	35	35	0	26	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0278-7407	1944-9194		TECTONICS	Tectonics	FEB	2018	37	2					497	528		10.1002/2017TC004655	http://dx.doi.org/10.1002/2017TC004655			32	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	GA6TE		Green Submitted			2025-03-11	WOS:000428466300005
J	Salgado, P; Fraga, S; Rodríguez, F; Bravo, I				Salgado, Pablo; Fraga, Santiago; Rodriguez, Francisco; Bravo, Isabel			Benthic flattened cells of the phylogenetically related marine dinoflagellates <i>Protoceratium reticulatum</i> and <i>Ceratocorys mariaovidiorum</i> (Gonyaulacales): a new type of cyst?	JOURNAL OF PHYCOLOGY			English	Article						benthic; Ceratocorys mariaovidiorum; Dinoflagellate; flattened cell; planktonic-benthic coupling; Protoceratium reticulatum; thin non-reticulated plates	ALEXANDRIUM-TAYLORI DINOPHYCEAE; LIFE-HISTORY; PFIESTERIA-PISCICIDA; BLOOM; CYCLES; ENCYSTMENT; SEXUALITY; RECURRENT; DYNAMICS; STRAINS	A planktonic-benthic relationship has been described for many dinoflagellate species as part of their ecological strategy to overcome highly variable aquatic environments. Here, the phylogenetically and morphologically related marine dinoflagellates Protoceratium reticulatum and Ceratocorys mariaovidiorum were studied in relation to an unknown benthic life form. In vivo and fixed samples from cultures were analyzed in detail by light and scanning electron microscopy. In both species, a cell type with a morphology different from that of vegetative cells was observed in cultures grown until stationary phase. This cell type was always benthic, swimming sporadically only when it was disturbed. Its main feature included a strong dorsoventral compression. These cells originated from vegetative cells whose protoplasm underwent a progressive flattening, resulting in a gradual detachment of the reticulate and thick thecal plates and the formation of very thin non-reticulated new plates with pores. When returned to fresh full-strength medium, the cells recovered their spherical vegetative-like morphology, including new reticulated thick plates and subsequent cell divisions. The kinetics of flattened cell formation showed that in both species, this cell type increased exponentially until the onset of the culture stationary phase and then decreased. The results of this study are discussed in the context of the planktonic-benthic coupling in dinoflagellate life cycles, including those newly appreciated to be well adapted to the benthic environment.	[Salgado, Pablo] Inst Fomento Pesquero IFOP, Dept Medio Ambiente, Div Invest Acuicultura, Enrique Abello 0552,Casilla 101, Punta Arenas, Chile; [Salgado, Pablo; Fraga, Santiago; Rodriguez, Francisco; Bravo, Isabel] IEO, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain	Instituto de Fomento Pesquero (Valparaiso); Spanish Institute of Oceanography	Salgado, P (通讯作者)，Inst Fomento Pesquero IFOP, Dept Medio Ambiente, Div Invest Acuicultura, Enrique Abello 0552,Casilla 101, Punta Arenas, Chile.; Salgado, P (通讯作者)，IEO, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain.	pablo.salgado@ifop.cl	Salgado, Pablo/KMA-0636-2024; Bravo, Isabel/D-3147-2012; Fraga, Santiago/AAA-3760-2020; Rodriguez, Francisco/A-5934-2019	Bravo, Isabel/0000-0003-3764-745X; Rodriguez, Francisco/0000-0002-6918-4771; Salgado, Pablo/0000-0002-4168-3675	CCVIEO project; Spanish National Project CICAN [CGL2013-40671-R]; Instituto de Fomento Pesquero (IFOP)	CCVIEO project; Spanish National Project CICAN; Instituto de Fomento Pesquero (IFOP)	We thank Isabel Ramilo and Pilar Rial for technical support. The present work was funded by the CCVIEO project and the Spanish National Project CICAN (CGL2013-40671-R). This article is going to be part of the thesis of Pablo Salgado that is attached to the framework of the doctoral program "Marine Science, Technology and Management" (DO*MAR) of the University of Vigo. P. Salgado is a researcher at the Instituto de Fomento Pesquero (IFOP), which has provided financial support for his doctoral stay at the Instituto Espanol de Oceanografia (IEO) in Vigo.	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A., 1973, BRIT PHYCOL J, V8, P105, DOI DOI 10.1080/00071617300650141; Zohary T, 1998, LIMNOL OCEANOGR, V43, P175, DOI 10.4319/lo.1998.43.2.0175	53	6	6	0	14	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	2018	54	1					138	149		10.1111/jpy.12611	http://dx.doi.org/10.1111/jpy.12611			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	FU8HN	29194636	Green Published			2025-03-11	WOS:000424094000014
J	Lewis, J; Taylor, JD; Neale, K; Leroy, SAG				Lewis, Jane; Taylor, Joe D.; Neale, Klaire; Leroy, Suzanne A. G.			Expanding known dinoflagellate distributions: investigations of slurry cultures from Caspian Sea sediment	BOTANICA MARINA			English	Article						Caspian Sea; Gonyaulax baltica; Gymnodinium aureolum; Kryptoperidinium foliaceum	CYST-THECA RELATIONSHIP; SP-NOV; COMB.-NOV; PHYLOGENETIC ANALYSIS; GYMNODINIUM-AUREOLUM; GONYAULAX-BALTICA; PHYTOPLANKTON; DINOPHYCEAE; CHECKLIST; SALINITY	To investigate the disparity between plankton and cyst records, sediment slurry cultures were used to isolate the motile stage of dinoflagellates from Caspian Sea sediment. This has resulted in new records for this area of Kryptoperidinium foliaceum, Gymnodinium aureolum and Woloszynskia sp. and for the cyst record, Scrippsiella acuminata. Two Gonyaulax species were isolated, one was identified as Gonyaulax baltica and the other an unknown species. Cultures of Lingulodinium polyedra were also isolated. The approach of using slurries was useful to provide cultures from sediments that were relatively poor in dinoflagellate cysts with contents.	[Lewis, Jane; Neale, Klaire] Univ Westminster, Fac Sci & Technol, Dept Life Sci, 115 New Cavendish St, London W1W 6UW, England; [Taylor, Joe D.] Univ Salford, Fac Sci & Technol, Dept Life Sci, 115 New Cavendish St, London W1W 6UW, England; [Taylor, Joe D.] Univ Salford, Sch Environm & Life Sci, Peel Bldg, Salford M5 4WT, Lancs, England; [Leroy, Suzanne A. G.] Ctr Europeen Rech & Enseignement Geosci Environm, Technopole Arbois, F-13545 Aix En Provence 4, France	University of Westminster; University of Salford; University of Salford; Aix-Marseille Universite	Lewis, J (通讯作者)，Univ Westminster, Fac Sci & Technol, Dept Life Sci, 115 New Cavendish St, London W1W 6UW, England.	lewisjm@westminster.ac.uk	Taylor, Joe/JCD-8107-2023; Taylor, Joe/F-2196-2015	Taylor, Joe/0000-0003-0095-0869				Bagheri S., 2014, Caspian Journal of Environmental Sciences, V12, P81; Bagheri Siamak, 2011, American Journal of Applied Sciences, V8, P1328, DOI 10.3844/ajassp.2011.1328.1336; Bagheri S, 2012, J MAR BIOL ASSOC UK, V92, P1243, DOI 10.1017/S0025315412000094; Bagheri S, 2012, EKOLOJI, V21, P32, DOI 10.5053/ekoloji.2012.834; Bagheri Siamak, 2010, World Journal of Fish and Marine Sciences, V2, P416; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; Dumont HJ, 1998, LIMNOL OCEANOGR, V43, P44, DOI 10.4319/lo.1998.43.1.0044; 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; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; Figueroa RI, 2009, PROTIST, V160, P285, DOI 10.1016/j.protis.2008.12.003; Ganjian A, 2010, IRAN J FISH SCI, V9, P382; Gogorev R., 2006, Caspian Sea Biodiversity Project; Gömez F, 2004, HYDROBIOLOGIA, V517, P43, DOI 10.1023/B:HYDR.0000027336.05452.07; Gómez F, 2003, BOT MAR, V46, P215, DOI 10.1515/BOT.2003.021; Guillard RRL., 1973, HDB PHYCOLOGICAL MET, P69; Hansen G, 2000, J PHYCOL, V36, P394, DOI 10.1046/j.1529-8817.2000.99172.x; Hoppenrath M., 2009, KL SENCKENBERG-REIHE, V49, P264; Kazanci N, 2004, J MARINE SYST, V46, P145, DOI 10.1016/j.jmarsys.2003.12.002; Kideys A. 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Marina	FEB	2018	61	1					21	31		10.1515/bot-2017-0041	http://dx.doi.org/10.1515/bot-2017-0041			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	FU2KU		Green Accepted, Green Submitted			2025-03-11	WOS:000423679800003
J	Ellegaard, M; Ribeiro, S				Ellegaard, Marianne; Ribeiro, Sofia			The long-term persistence of phytoplankton resting stages in aquatic 'seed banks'	BIOLOGICAL REVIEWS			English	Review						cyst; spore; microalgae; dinoflagellate; diatom; long-term viability; sediment record; seed bed	DIATOM CHAETOCEROS-PSEUDOCURVISETUS; MARINE PLANKTONIC DIATOM; BET-HEDGING GERMINATION; SEXUAL REPRODUCTION; SPORE FORMATION; LIFE-CYCLE; THALASSIOSIRA-ANTARCTICA; BIOCHEMICAL-COMPOSITION; GYMNODINIUM-CATENATUM; DINOFLAGELLATE CYST	In the past decade, research on long-term persistence of phytoplankton resting stages has intensified. Simultaneously, insight into life-cycle variability in the diverse groups of phytoplankton has also increased. Aquatic 'seed banks' have tremendous significance and show many interesting parallels to terrestrial seed beds of vascular plants, but are much less studied. It is therefore timely to review the phenomenon of long-term persistence of aquatic resting stages in sediment seed banks. Herein we compare function, morphology and physiology of phytoplankton resting stages to factors central for persistence of terrestrial seeds. We review the types of resting stages found in different groups of phytoplankton and focus on the groups for which long-term (multi-decadal) persistence has been shown: dinoflagellates, diatoms, green algae and cyanobacteria. We discuss the metabolism of long-term dormancy in phytoplankton resting stages and the ecological, evolutionary and management implications of this important trait. Phytoplankton resting stages exhibiting long-term viability are characterized by thick, often multi-layered walls and accumulation vesicles containing starch, lipids or other materials such as pigments, cyanophycin or unidentified granular materials. They are reported to play central roles in evolutionary resilience and survival of catastrophic events. Promising areas for future research include the role of hormones in mediating dormancy, elucidating the mechanisms behind metabolic shut-down and testing bet-hedging hypotheses.	[Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg 1871, Denmark; [Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Glaciol & Climate Dept, DK-1350 Copenhagen K, Denmark	University of Copenhagen; Geological Survey Of Denmark & Greenland	Ellegaard, M (通讯作者)，Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg 1871, Denmark.	me@plen.ku.dk	Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/AAZ-2782-2021; Ribeiro, Sofia/G-9213-2018	Ribeiro, Sofia/0000-0003-0672-9161	VILLUM Foundation, Denmark (VILLUM FONDEN) [VKR023454]	VILLUM Foundation, Denmark (VILLUM FONDEN)	We are grateful to Anna Godhe for helpful comments on an earlier draft, and to Anna Godhe and Nina Lundholm for collaboration on studies on long-term survival of marine diatoms and dinoflagellates. Atchaneey Boonprakob, Nina Lundholm, Ojvind Moestrup, Gertrud Cronberg and Karin Rengefors are thanked for their kind permission to reproduce micrographs in Fig. 3. We thank two anonymous reviewers for their insightful comments. S.R. received financial support from the VILLUM Foundation, Denmark (VILLUM FONDEN) (VKR023454).	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Rev.	FEB	2018	93	1					166	183		10.1111/brv.12338	http://dx.doi.org/10.1111/brv.12338			18	Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics	FS7GK	28474820	Green Published, hybrid			2025-03-11	WOS:000419965700009
J	Tian, C; Doblin, MA; Dafforn, KA; Johnston, EL; Pei, HY; Hu, WR				Tian, Chang; Doblin, Martina A.; Dafforn, Katherine A.; Johnston, Emma L.; Pei, Haiyan; Hu, Wenrong			Dinoflagellate cyst abundance is positively correlated to sediment organic carbon in Sydney Harbour and Botany Bay, NSW, Australia	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Dinoflagellate life cycle; Sydney Harbour; Risk management; Water quality; Redundancy analysis	HARMFUL ALGAL BLOOMS; NEW-SOUTH-WALES; SHIPS BALLAST WATER; SURFACE SEDIMENTS; SPATIAL-DISTRIBUTION; RESTING CYSTS; GENUS ALEXANDRIUM; EASTERN AUSTRALIA; INDIAN-OCEAN; NEW-ENGLAND	There is growing public concern about the global expansion of harmful algal bloom species (HABs), with dinoflagellate microalgae comprising the major portion of the harmful taxa. These motile, unicellular organisms have a lifecycle involving sexual reproduction and resting cyst formation whereby cysts can germinate from sediments and 'seed' planktonic populations. Thus, investigation of dinoflagellate cyst (dinocyst) distribution in sediments can provide significant insights into HAB dynamics and contribute to indices of habitat quality. Species composition and abundance of dinocysts in relation to sediment characteristics were studied at 18 stations in two densely populated temperate Australian estuaries, Sydney Harbour (Parramatta River/Port Jackson; PS) and Botany Bay (including Georges River; GB). Eighteen dinocyst taxa were identified, dominated by Protoceratium reticulatum and Gonyaulax sp.1 in the PS estuary, together with Archaeperidinium minutum and Gonyaulax sp.1 in the GB estuary. Cysts of Alexandrium catenella, which is one of the causative species of paralytic shellfish poisoning (PSP), were also detected in both estuaries. Out of the measured sediment characteristics (TOC, Cd, Cr, Cu, Fe, Pb, Mn, Ni, Zn and polycyclic aromatic hydrocarbons), TOC was the parameter explaining most of the variation in dinocyst assemblages and was positively correlated to most of the heavy metals. Given the significant relationship between sediment TOC and dinocyst abundance and heavy metal concentrations, this study suggests that sediment TOC could be broadly used in risk management for potential development of algal blooms and sediment contamination in these estuaries.	[Tian, Chang; Doblin, Martina A.] Univ Technol Sydney, Fac Sci, Climate Change Cluster, Sydney, NSW 2007, Australia; [Tian, Chang; Pei, Haiyan; Hu, Wenrong] Shandong Univ, Sch Environm Sci & Engn, Jinan 250061, Shandong, Peoples R China; [Tian, Chang; Dafforn, Katherine A.] Qilu Univ Technol, Sch Environm Sci & Engn, Jinan 250353, Shandong, Peoples R China; [Doblin, Martina A.; Johnston, Emma L.] Sydney Inst Marine Sci, Mosman, NSW 2088, Australia; [Dafforn, Katherine A.; Johnston, Emma L.] Univ New South Wales, Evolut & Ecol Res Ctr, Sch Biol Earth & Environm Sci, Sydney, NSW 2052, Australia; [Pei, Haiyan; Hu, Wenrong] Shandong Prov Engn Ctr Environm Sci & Technol, Jinan 250061, Shandong, Peoples R China	University of Technology Sydney; Shandong University; Qilu University of Technology; Sydney Institute of Marine Science; University of New South Wales Sydney	Doblin, MA (通讯作者)，Univ Technol Sydney, Fac Sci, Climate Change Cluster, Sydney, NSW 2007, Australia.; Pei, HY (通讯作者)，Shandong Univ, Sch Environm Sci & Engn, Jinan 250061, Shandong, Peoples R China.; Doblin, MA (通讯作者)，Sydney Inst Marine Sci, Mosman, NSW 2088, Australia.; Pei, HY (通讯作者)，Shandong Prov Engn Ctr Environm Sci & Technol, Jinan 250061, Shandong, Peoples R China.	martina.doblin@uts.edu.au; haiyanhup@126.com	Johnston, Emma/AAC-2878-2022; Doblin, Martina/E-8719-2013; Johnston, Emma/B-7210-2009; Dafforn, Katherine/J-9647-2013	Doblin, Martina/0000-0001-8750-3433; Johnston, Emma/0000-0002-2117-366X; Dafforn, Katherine/0000-0001-8848-377X	International Science and Technology Cooperation Program of China [2010DFA91150]; Shandong University; Plant Functional Biology and Climate Change Cluster, University of Technology Sydney	International Science and Technology Cooperation Program of China; Shandong University; Plant Functional Biology and Climate Change Cluster, University of Technology Sydney	The authors thank Marlene Zbinden for conducting the sediment organic carbon analyses and Gustaaf Hallegraeff for assistance with cyst identification. This study was supported by International Science and Technology Cooperation Program of China (No 2010DFA91150), a visiting fellowship from Shandong University and by the Plant Functional Biology and Climate Change Cluster, University of Technology Sydney.	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J	Allan, E; de Vernal, A; Knudsen, MF; Hillaire-Marcel, C; Moros, M; Ribeiro, S; Ouellet-Bernier, MM; Seidenkrantz, MS				Allan, Estelle; de Vernal, Anne; Knudsen, Mads Faurschou; Hillaire-Marcel, Claude; Moros, Matthias; Ribeiro, Sofia; Ouellet-Bernier, Marie-Michele; Seidenkrantz, Marit-Solveig			Late Holocene Sea Surface Instabilities in the Disko Bugt Area, West Greenland, in Phase With δ<SUP>18</SUP>O Oscillations at Camp Century	PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY			English	Article						Arctic sea ice reconstructions; West Greenland; Dinocyst database; late Holocene; Arctic climate change	JAKOBSHAVN ISBRAE; CLIMATE VARIABILITY; DINOFLAGELLATE CYSTS; OCEAN CIRCULATION; WATER ISOTOPES; ATLANTIC-OCEAN; MID-HOLOCENE; ICE; RECONSTRUCTION; RECORD	Palynological analyses of sediment core MSM343310 from Disko Bugt (68 degrees 38'861 degrees N, 53 degrees 49493 degrees W) document decadal- to centennial-scale variability of sea surface conditions during the last similar to 3,600years. Dinocyst fluxes (>10(4) cysts/cm(2)yr(-1)) indicate a very high productivity. Dinocyst assemblages dominated by Islandinium minutum, Brigantedinium spp., Islandinium? cezare, and the cyst of Pentapharsodinium dalei suggest low surface salinity and marked shifts in summer sea surface temperature. The application of the modern analog technique to dinocyst assemblages, using an updated reference data set with new sites from the West Greenland margin, led to reconstruct decadal-centennial-scale variations in sea surface salinity and temperature, in phase with the delta O-18 variations in the Camp Century ice core. At similar to 1.5ka BP, the seasonal sea ice cover records an important regime change, from winter-only sea ice to more unstable conditions marked by successive cooling pulses with sea ice cover of up to 8months/yr. The data suggest a close relationship between hydrographic conditions and regional climate over Greenland. Our record shows variations with a mean 200years periodicity until similar to 2ka BP, which supports the hypothesis of climate variations driven by solar variability. After 1.5ka BP, our data show a variability characterized by a 60-70year periodicity, which suggests linkages with the Atlantic Multidecadal Oscillation and southwestward migration of the atmospheric polar front. The most recent part of the record, from similar to 1900CE to 2007CE, is characterized by assemblages reflecting warmer surface conditions and reduced sea ice cover.	[Allan, Estelle; de Vernal, Anne; Hillaire-Marcel, Claude; Ouellet-Bernier, Marie-Michele] Univ Quebec, Ctr Rech Dynam Syst Terre Geotop, Montreal, PQ, Canada; [Knudsen, Mads Faurschou; Seidenkrantz, Marit-Solveig] Aarhus Univ, Ctr Past Climate Studies, Arctic Res Ctr, Aarhus, Denmark; [Knudsen, Mads Faurschou; Seidenkrantz, Marit-Solveig] Aarhus Univ, Dept Geosci, iClimate, Aarhus, Denmark; [Moros, Matthias] Leibniz Inst Balt Sea Res, Dept Marine Geol, Rostock, Germany; [Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Glaciol & Climate Dept, Copenhagen, Denmark	University of Quebec; University of Quebec Montreal; Aarhus University; Aarhus University; Leibniz Institut fur Ostseeforschung Warnemunde; Geological Survey Of Denmark & Greenland	Allan, E (通讯作者)，Univ Quebec, Ctr Rech Dynam Syst Terre Geotop, Montreal, PQ, Canada.	estelle.allan.56@gmail.com	Hillaire-Marcel, Claude/H-1441-2012; Ribeiro, Sofia/AAZ-2782-2021; Knudsen, Mads/H-4842-2012; de Vernal, Anne/D-5602-2013; Seidenkrantz, Marit-Solveig/A-3451-2012; Ribeiro, Sofia/G-9213-2018; Hillaire-Marcel, Claude/C-9153-2013	de Vernal, Anne/0000-0001-5656-724X; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969; Ribeiro, Sofia/0000-0003-0672-9161; Hillaire-Marcel, Claude/0000-0002-3733-4632; Allan, Estelle/0000-0003-0924-5808	Natural Science and Engineering Research Council (NSERC) of Canada; Fonds pour la Recherche du Quebec Nature et Technologie (FRQNT); Deutsche Forschungsgemeinschaft (DFG; project "Disco Climate") [MO1422/2-1]; Independent Research Fund Denmark/Natural Science (G-Ice project) [7014-00113B/FNU]	Natural Science and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds pour la Recherche du Quebec Nature et Technologie (FRQNT); Deutsche Forschungsgemeinschaft (DFG; project "Disco Climate")(German Research Foundation (DFG)); Independent Research Fund Denmark/Natural Science (G-Ice project)	We thank the Captain and crew of the R/V Maria S. Merian for the great work they did during the cruise MSM05/03. We acknowledge the financial support of the Natural Science and Engineering Research Council (NSERC) of Canada and the Fonds pour la Recherche du Quebec Nature et Technologie (FRQNT), the Deutsche Forschungsgemeinschaft (DFG; project "Disco Climate" MO1422/2-1), and the Independent Research Fund Denmark/Natural Science (G-Ice project 7014-00113B/FNU). This paper is a contribution to the Canada-Germany project ArcTrain and to the Canadian program VITALS. We thank Diana Krawczyk for providing the surface sediment samples from the West Greenland margin. We are also grateful to Maryse Henry and Taoufik Radi for their precious help with dinocyst identification and their works with the dinocyst database. The results of the new surface sediment samples from the West Greenland margin, the reconstructions of sea surface parameters from Disko Bugt, and the dinocyst database n = 1776 are available in the supporting information as tables.	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J	Lee, S; Hofmeister, R; Hense, I				Lee, Soonmi; Hofmeister, Richard; Hense, Inga			The role of life cycle processes on phytoplankton spring bloom composition: a modelling study applied to the Gulf of Finland	JOURNAL OF MARINE SYSTEMS			English	Article						Baltic Sea; Life cycle; Cold-water dinoflagellates; Diatoms; Resting stages; Seed pool; Spring bloom	DINOFLAGELLATE SCRIPPSIELLA-HANGOEI; BALTIC SEA; STRATEGIES; DYNAMICS; PATTERNS; DINOPHYCEAE; COMMUNITIES; MECHANISMS; ENCYSTMENT; SINKING	Diatoms are typical representatives of the spring bloom worldwide. In several parts of the Baltic Sea, however, cold-water dinoflagellates such as Biecheleria baltica have become dominant during the past decades. We have investigated the mechanisms behind this trend by using an ecosystem model which includes the life cycles of three main phytoplankton groups (diatoms, dinoflagellates and cyanobacteria). Coupled to a water column model we have applied the model system for the period 1981-2010 to the Gulf of Finland. In agreement with observations, the model results show an increasing trend in the proportion of dinoflagellates in the Gulf of Finland. Temperature and life cycle-related processes explain the relative increase of dinoflagellates and corresponding decrease of diatoms. Warming over the 30 years has enabled a head start of dinoflagellates by reducing the time lag between germination and growth of vegetative cells. Although diatoms have a much higher growth rate, they cannot compete with the high dinoflagellate concentrations that result from the inoculum. Diatoms will only dominate in years when the inoculum concentrations of dinoflagellates or the temperatures are low. Overall, the model results suggest that consideration of life cycle dynamics of competing phytoplankton groups may be crucial to understand trends and shifts in community composition.	[Lee, Soonmi; Hofmeister, Richard; Hense, Inga] Univ Hamburg, Ctr Earth Syst Res & Sustainabil, Inst Hydrobiol & Fisheries Sci, Hamburg, Germany; [Lee, Soonmi] CNRS, Ecol Networks & Global Change Grp, Theoret & Expt Ecol Stn, Moulis, France; [Lee, Soonmi] Paul Sabatier Univ, Moulis, France; [Hofmeister, Richard] Helmholtz Zentrum Geesthacht, Inst Coastal Res, Geesthacht, Germany	University of Hamburg; Centre National de la Recherche Scientifique (CNRS); Universite de Toulouse; Universite Toulouse III - Paul Sabatier; Helmholtz Association; Helmholtz-Zentrum Hereon	Lee, S (通讯作者)，Univ Hamburg, Ctr Earth Syst Res & Sustainabil, Inst Hydrobiol & Fisheries Sci, Hamburg, Germany.	soonmi.lee@sete.cnrs.fr		Hense, Inga/0000-0001-7322-680X	Cluster of Excellence "CliSAP", Universitat Hamburg through the German Science Foundation (DFG) [EXC177]	Cluster of Excellence "CliSAP", Universitat Hamburg through the German Science Foundation (DFG)	We thank two anonymous referees for their valuable comments, which helped to improve the manuscript. We are grateful to Riina Klais for making the observational data of diatoms and dinoflagellates available. We also thank ICES for the HELCOM monitoring data (temperature, salinity and nutrients) and ECMWF for the meteorological forcing data. This research was supported through the Cluster of Excellence "CliSAP" (EXC177), Universitat Hamburg, funded through the German Science Foundation (DFG).	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Mar. Syst.	FEB	2018	178						75	85		10.1016/j.jmarsys.2017.10.010	http://dx.doi.org/10.1016/j.jmarsys.2017.10.010			11	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	FQ2VB					2025-03-11	WOS:000418215000007
J	Ferguson, S; Warny, S; Escarguel, G; Mudie, PJ				Ferguson, Shannon; Warny, Sophie; Escarguel, Gilles; Mudie, Petra J.			MIS 5-1 dinoflagellate cyst analyses and morphometric evaluation of <i>Galeacysta</i> <i>etrusca</i> and <i>Spiniferites cruciformis</i> in southwestern Black Sea	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	4th Plenary Meeting of IGCP 610 - From the Caspian to Mediterranean - Environmental Change and Human Response during the Quaternary	2016	Tbilisi, REP OF GEORGIA	IGCP 610		Dinoflagellate cysts; DSDP Site 380; Brackish; Paleosalinity; Sea level	LAST 2000 YEARS; MARMARA SEA; SURFACE CONDITIONS; MEDITERRANEAN SEA; SALINITY CHANGES; ARAL SEA; HOLOCENE; WATER; ASSEMBLAGES; PLEISTOCENE	Here we evaluate the changes in dinoflagellate cyst assemblages and intraspecies morphometric variability in dominant Black Sea species during MIS 5-1 in sediment recovered from DSDP Site 380. Twenty-three taxa represent the majority of the 16,000 cysts tabulated. Qualitative assessment of assemblage composition indicates that the taxa are distributed in three ecological assemblages; marine stenohaline, marine euryhaline, and brackish Ponto-Caspian endemic species; the fluctuation of these assemblages provide evidence for changes in environmental conditions from the end of MIS 5e to MIS 1. Although some fluctuations in sea-surface salinity are highlighted by changes in dinoflagellate assemblages, the continuous presence of Pyxidinopsis psilata, Galeacysta etrusca and Spiniferites cruciformis likely indicate brackish conditions for most of the interval sampled at this site. Statistical analysis of measured morphometric changes in Galeacysta etrusca endocyst: ectocyst ratios indicate that the specimens recovered mostly belong to a smaller morphotype forming group 'b' of Popescu et al. (2009), interpreted as indicative of brackishemarine conditions after migration to the Mediterranean from the Paratethys. Although not fully conclusive because of sampling constraints and limited chronological control, the lack of sudden, large abundance changes in marine salinity-tolerant species the relatively low species diversity, and the sequence of sapropelic layers relative to banded clastic muds provides evidence against the occurrence of sustained marine flooding between ca. 0.07-0.007 Ma and it is not clear that the last interglacial marine highstand during MIS 5e was fully sampled at this site. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.	[Ferguson, Shannon; Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA; [Ferguson, Shannon; Warny, Sophie] Louisiana State Univ, Museum Nat Sci, E-235 Howe Russell, Baton Rouge, LA 70803 USA; [Escarguel, Gilles] Univ Claude Bernard Lyon 1, UMR CNRS 5023, Lab Ecol Hydrosyst Nat & Anthropises, Blvd 11 Novembre 1918, F-69622 Villeurbanne, France; [Mudie, Petra J.] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University; Centre National de la Recherche Scientifique (CNRS); Universite Claude Bernard Lyon 1; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Warny, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA.	swarny@lsu.edu	Warny, Sophie/A-8226-2013; Escarguel, Gilles/C-3297-2011	Escarguel, Gilles/0000-0003-0985-6369; Warny, Sophie/0000-0002-3451-040X	LSU Department of Geology and Geophysics	LSU Department of Geology and Geophysics	This paper is primarily a summary of S. Ferguson's M.S. thesis. Thanks are extended to Speranta Popescu for her substantial guidance and contribution during Ferguson's Master Thesis (Ferguson, 2012). She thanks her committee members for constructive remarks, and the LSU Department of Geology and Geophysics for financial assistance. Thanks are also extended to Martin Head (Brock University) for assistance with the identification of some dinoflagellate cyst species and ranges of reworked taxa, and to Crawford White for valuable figure and editing support. We also thank two anonymous reviewers for their constructive and helpful comments.	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Int.	JAN 20	2018	465		A				117	129		10.1016/j.quaint.2016.07.035	http://dx.doi.org/10.1016/j.quaint.2016.07.035			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	FW3UT					2025-03-11	WOS:000425237100012
J	Papadomanolaki, NM; Dijkstra, N; van Helmond, NAGM; Hagens, M; Bauersachs, T; Kotthoff, U; Sangiorgi, F; Slomp, CP				Papadomanolaki, Nina M.; Dijkstra, Nikki; van Helmond, Niels A. G. M.; Hagens, Mathilde; Bauersachs, Thorsten; Kotthoff, Ulrich; Sangiorgi, Francesca; Slomp, Caroline P.			Controls on the onset and termination of past hypoxia in the Baltic Sea	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Holocene; Temperature; Salinity; Stratification; Productivity; Recovery	DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; CYANOBACTERIAL BLOOMS; TETRAETHER LIPIDS; SURFACE SEDIMENTS; ORGANIC-MATTER; SALINITY; CLIMATE; CYSTS; IRON; BASIN	The Baltic Sea is currently the largest marine hypoxic (O-2 < 2 mg L-) 'dead zone' following excessive nutrient input from anthropogenic activities over the past century. Widespread hypoxia has previously developed in the Baltic Sea during the Holocene Thermal Maximum (HTM; 8-4 ka before present; BP) and the Medieval Climate Anomaly (MCA; 1.4-0.7 ka BP). Here we study the mechanisms that contributed to the onset and termination of this past hypoxia using geochemical and marine palynological data from a sediment record retrieved from the Landsort Deep during IODP Expedition 347 (Site M0063). Dinoflagellate cyst records and TEX86L-based sea surface temperature reconstructions indicate a major increase in salinity and temperature prior to and across the onset of the HTM hypoxic interval, underlining the importance of both temperature and salinity stratification in providing conditions conducive to the onset of hypoxia. Both salinity and temperature decline during the termination of the HTM hypoxic interval. In contrast, we find no evidence for significant changes in surface salinity during the MCA hypoxic interval and both the onset and termination of hypoxia appear to have been primarily driven by changes in temperature. Our results indicate that temperature and salinity changes were key drivers of past hypoxia in the Baltic Sea and imply that ongoing climate change will delay recovery from the modern, nutrient -driven hypoxic event in the Baltic Sea.	[Papadomanolaki, Nina M.; Dijkstra, Nikki; van Helmond, Niels A. G. M.; Hagens, Mathilde; Slomp, Caroline P.] Univ Utrecht, Dept Earth Sci, Geochem, POB 80021, NL-3508 TA Utrecht, Netherlands; [Bauersachs, Thorsten] Univ Kiel, Inst Geosci, Dept Organ Geochem, Ludewig Meyn Str 10, D-24118 Kiel, Germany; [Kotthoff, Ulrich] Hamburg Univ, Ctr Nat Hist, Inst Geol, Bundesstr 55, D-20146 Hamburg, Germany; [Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci Marine Palynol & Paleoceanog, POB 80115, NL-3508 TC Utrecht, Netherlands; [Hagens, Mathilde] Wageningen Univ & Res, Dept Soil Qual, Wageningen, Netherlands	Utrecht University; University of Kiel; University of Hamburg; Utrecht University; Wageningen University & Research	Papadomanolaki, NM (通讯作者)，Univ Utrecht, Dept Earth Sci, Geochem, POB 80021, NL-3508 TA Utrecht, Netherlands.	n.papadomanolaki@uu.nl	Bauersachs, Thorsten/AFY-5641-2022; Slomp, Caroline/A-9406-2012; Hagens, Mathilde/G-9756-2015	Sangiorgi, Francesca/0000-0003-4233-6154; Bauersachs, Thorsten/0000-0003-4858-9443; Hagens, Mathilde/0000-0003-3980-1043; van Helmond, Niels/0000-0003-0024-7217	ERC [278364]; NWO-Vici Grant [865.13.005]; DFG [BA 3841/ 5-1, BA 3841/5-2]; Ministry of Education, Culture and Science (OCW); European Research Council (ERC) [278364] Funding Source: European Research Council (ERC)	ERC(European Research Council (ERC)); NWO-Vici Grant(Netherlands Organization for Scientific Research (NWO)); DFG(German Research Foundation (DFG)); Ministry of Education, Culture and Science (OCW)(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)); European Research Council (ERC)(European Research Council (ERC))	Samples used in this study were provided by the Integrated Ocean Drilling Program (IODP). We thank the captain, crew and scientists of IODP Expedition 347 for their contribution to the sample collection. We also thank Ton Zalm, Helen de Waard and Arnold van Dijk for analytical assistance at Utrecht University. This research was funded by ERC Starting Grant 278364 and NWO-Vici Grant 865.13.005 to C. P. Slomp. T. Bauersachs received financial support through DFG grant BA 3841/ 5-1 and BA 3841/5-2. This work was carried out under the program of the Netherlands Earth System Science Centre (NESSC), financially supported by the Ministry of Education, Culture and Science (OCW).	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P., 2017, BOREAS; Wasmund N, 1997, INT REV GES HYDROBIO, V82, P169, DOI 10.1002/iroh.19970820205; Weijers JWH, 2006, ORG GEOCHEM, V37, P1680, DOI 10.1016/j.orggeochem.2006.07.018; Westman P, 2003, ESTUARIES, V26, P680, DOI 10.1007/BF02711979; Willumsen PS, 2013, BOREAS, V42, P210, DOI 10.1111/j.1502-3885.2012.00286.x; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zillén L, 2010, BIOGEOSCIENCES, V7, P2567, DOI 10.5194/bg-7-2567-2010; Zillén L, 2008, EARTH-SCI REV, V91, P77, DOI 10.1016/j.earscirev.2008.10.001; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	75	13	13	1	34	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	JAN 15	2018	490						347	354		10.1016/j.palaeo.2017.11.012	http://dx.doi.org/10.1016/j.palaeo.2017.11.012			8	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	FU1VP		Green Published			2025-03-11	WOS:000423637900024
J	Levac, E; Sandercombe, S; Chmura, GL				Levac, Elisabeth; Sandercombe, Simone; Chmura, Gail L.			The Younger Dryas in palynological records from the northern Northwest Atlantic: Does the terrestrial record lag the marine and air records?	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Pollen; Dinoflagellate cysts; Newfoundland; Climate reconstructions; Paleoceanography; Vegetation	AGE CALIBRATION CURVES; SEA-SURFACE CONDITIONS; RAPID CLIMATE-CHANGE; ST-LAWRENCE; LAKE TEMPERATURES; VEGETATION CHANGE; RESERVOIR AGES; MULTI-PROXY; CANADA; POLLEN	Major changes in both pollen and dinocyst assemblages are recorded during the Younger Dryas in Bay of Islands and are associated with large drops in air and sea surface temperatures, and sea surface salinity. The changes in vegetation are similar with those observed at other sites in Newfoundland. Dinoflagellate cyst assemblages also show similar species succession as nearby sites from the Gulf of St. Lawrence and Laurentian Channel. The amplitude of changes in air temperature (a 7 degrees C drop) is similar to those recorded in northeastern North America. In the sea-surface, temperature dropped by 7 degrees C, salinity by 4 psu and the sea ice cover duration increased by 7 months. Sea-surface and air temperatures started cooling 250 and 110 years before the start of the YD, hence there is a 140 years delay between ocean and atmosphere. A warming trend is seen in the marine record 310 years before the end of the YD, while vegetation and air temperatures started recovering after the end of the event, some 370 years later. The major lithological and vegetation changes observed during the YD period in eastern North America might actually represent the full impacts of the cooling associated with the YD, since the cooling trend actually started before the start of the YD period, as defined by radiocarbon dates and pollen zones.	[Levac, Elisabeth] Bishops Univ, Dept Geog & Environm, 2600 Coll St, Sherbrooke, PQ J1M 1Z7, Canada; [Sandercombe, Simone; Chmura, Gail L.] McGill Univ, Dept Geog, 805 Sherbrooke St W, Montreal, PQ H3A 0B9, Canada	Bishops University	Levac, E (通讯作者)，Bishops Univ, Dept Geog & Environm, 2600 Coll St, Sherbrooke, PQ J1M 1Z7, Canada.	elevac@ubishops.ca	Chmura, Gail/LNI-4648-2024	Chmura, Gail/0000-0001-7163-3903	NSERC [431997]; Global Environmental and Climate Change Centre at McGill University (FQRNT) [232172]	NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Global Environmental and Climate Change Centre at McGill University (FQRNT)	The authors thank Ali Aksu and Rick Hiscott for providing the samples from core MD99-2225 and some of the radiocarbon dates. This work was supported by a NSERC Discovery Grant (NSERC grant number 431997), and graduate stipends from the Global Environmental and Climate Change Centre at McGill University (FQRNT Regroupements Strategiques 232172). Help with the C2 software from Matt Peros was greatly appreciated. Comments by two anonymous reviewers are greatly acknowledged.	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Paleoclimatol. Paleoecol.	JAN 15	2018	490						269	279		10.1016/j.palaeo.2017.11.005	http://dx.doi.org/10.1016/j.palaeo.2017.11.005			11	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	FU1VP					2025-03-11	WOS:000423637900019
J	Ocakoglu, F; Yavuz, N; Aydln, A; Yilmaz, IÖ				Ocakoglu, Faruk; Yavuz, Nurdan; Aydln, Aysegul; Yilmaz, Ismail Omer			Orbitally-driven Mid-Burdigalian Coastal Sabkha cycles from the Sivas Basin: Sedimentological, paleontological, and geochemical data	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Evaporite cycles; Nannofossils; Paleoclimate; Palynology; Orbital forcing	CALCAREOUS NANNOPLANKTON BIOSTRATIGRAPHY; CENTRAL ANATOLIA; LATE OLIGOCENE; LACUSTRINE DEPOSITS; EASTERN ANATOLIA; ORGANIC-MATTER; UPPER MIOCENE; CLIMATE; EVOLUTION; FACIES	The Early to Middle Miocene period in the Sivas Basin is represented by a thick deposition of mud-dominated marine sediments (Karacaoren Formation) in an overall bay-like paleogeographic setting. Previous studies have suggested that halokinesis-induced local tectonics and orbital climatic fluctuations have been the primary controls on depositional evolution. In the present study, we investigated a 60-m-thick Karaman Gypsum Member (KGM), located at the base of the Karacaoren Formation, in terms of its sedimentological, paleontological; both palynology and nannofossil biostratigraphy, and geochemical/mineralogical aspects to better characterize climatic controls on its deposition. Nannofossil assemblages indicate that the studied member is confined within the Sphenolithus belemnos Zone (NN3; 18.92-17.97 Ma), and is mainly composed of rhythmic alternations of supratidal evaporites and lagoonal/marine mudstones. The palynological data demonstrate a minor, yet consistent, occurrence of megathermic taxa and numerous dinoflagellate cysts in mudstone intervals. The high chemical proxy of alteration (CPA) values and occurrence of kaolinites in the same mudstone intervals further prove deposition under warm and humid subtropical conditions. The perfect match between the environmental cyclicities in the KGM with a benthic delta O-18 curve justifies a strong control of obliquity/short eccentricity of a 40-100 kyr duration, and hints at radical precipitation changes throughout the individual orbital cycles. These precipitation changes are explained by extreme latitudinal precipitation gradients during relatively hot periods before the mid-Miocene Climatic Optimum.	[Ocakoglu, Faruk] Eskisehir Osmangazi Univ, Dept Geol Engn, TR-26480 Eskisehir, Turkey; [Yavuz, Nurdan; Aydln, Aysegul] Gen Directorate Mineral Res & Explorat, Dept Geol Res, TR-06800 Ankara, Turkey; [Yilmaz, Ismail Omer] Middle East Tech Univ, Dept Geol Engn, TR-06800 Ankara, Turkey	Eskisehir Osmangazi University; Ministry of Energy & Natural Resources - Turkey; Maden Tetkik ve Arama (MTA) - Turkey; Middle East Technical University	Ocakoglu, F (通讯作者)，Eskisehir Osmangazi Univ, Dept Geol Engn, TR-26480 Eskisehir, Turkey.	focak@ogu.edu.tr	, OMER/AAZ-9186-2020; Ocakoğlu, Faruk/HGB-7166-2022; Ocakoglu, Faruk/C-9485-2009	Ocakoglu, Faruk/0000-0002-4619-5865				Akgün F, 2007, PALAEOGEOGR PALAEOCL, V253, P56, DOI 10.1016/j.palaeo.2007.03.034; Akkiraz MS, 2011, PALAEOGEOGR PALAEOCL, V304, P276, DOI 10.1016/j.palaeo.2010.05.002; Alsharhan AS, 2003, EARTH-SCI REV, V61, P191, DOI 10.1016/S0012-8252(02)00110-1; Altunsoy M, 1998, J PETROL SCI ENG, V20, P73, DOI 10.1016/S0920-4105(97)00051-X; Andreychouk V, 2014, ANN SOC GEOL POL, V84, P297; [Anonymous], [No title captured]; [Anonymous], GEOCHEM GEOPHYS GEOS; [Anonymous], 1972, T P PALEONTOLOGICAL, DOI DOI 10.14825/PRPSJ1951.1972.87_429; ARTHUR MA, 1994, ANNU REV EARTH PL SC, V22, P499, DOI 10.1146/annurev.ea.22.050194.002435; Atalay Z, 1999, B MINER RES EXPLOR I, V121, P153; Aubry M.-P., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P471, DOI 10.2973/odp.proc.sr.120.149.1992; Aubry Marie-Pierre, 1992, P272; Aubry MP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P158; Bahadori A, 2011, J GEOCHEM EXPLOR, V111, P97, DOI 10.1016/j.gexplo.2011.02.007; Billups K, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2000PA000568; Billups K, 2004, EARTH PLANET SC LETT, V224, P33, DOI 10.1016/j.epsl.2004.05.004; Böhme M, 2011, PALAEOGEOGR PALAEOCL, V304, P212, DOI 10.1016/j.palaeo.2010.09.028; Boztug D, 2008, TURK J EARTH SCI, V17, P241; Bralower TJ, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2001PA000662; BRAMLETTE M. 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Paleoclimatol. Paleoecol.	JAN 15	2018	490						505	521		10.1016/j.palaeo.2017.11.035	http://dx.doi.org/10.1016/j.palaeo.2017.11.035			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	FU1VP					2025-03-11	WOS:000423637900035
J	Frieling, J; Reichart, GJ; Middelburg, JJ; Röhl, U; Westerhold, T; Bohaty, SM; Sluijs, A				Frieling, Joost; Reichart, Gert-Jan; Middelburg, Jack J.; Roehl, Ursula; Westerhold, Thomas; Bohaty, Steven M.; Sluijs, Appy			Tropical Atlantic climate and ecosystem regime shifts during the Paleocene-Eocene Thermal Maximum	CLIMATE OF THE PAST			English	Article							WALLED DINOFLAGELLATE CYSTS; TETRAETHER MEMBRANE-LIPIDS; SEA-SURFACE TEMPERATURE; GHANA TRANSFORM MARGIN; CARBON RELEASE; ENVIRONMENTAL-CHANGES; ARCTIC HYDROLOGY; METHANE RELEASE; OCEAN; MARINE	The Paleocene-Eocene Thermal Maximum (PETM, 56 Ma) was a phase of rapid global warming associated with massive carbon input into the ocean-atmosphere system from a C-13-depleted reservoir. Many midlatitude and high-latitude sections have been studied and document changes in salinity, hydrology and sedimentation, deoxygenation, biotic overturning, and migrations, but detailed records from tropical regions are lacking. Here, we study the PETM at Ocean Drilling Program (ODP) Site 959 in the equatorial Atlantic using a range of organic and inorganic proxies and couple these with dinoflagellate cyst (dinocyst) assemblage analysis. The PETM at Site 959 was previously found to be marked by a similar to 3.8% negative carbon isotope excursion (CIE) and a similar to 4 degrees C surface ocean warming from the uppermost Paleocene to peak PETM, of which similar to 1 degrees C occurs before the onset of the CIE. We record upper Paleocene dinocyst assemblages that are similar to PETM assemblages as found in extratropical regions, confirming poleward migrations of ecosystems during the PETM. The early stages of the PETM are marked by a typical acme of the tropical genus Apectodinium, which reaches abundances of up to 95 %. Subsequently, dinocyst abundances diminish greatly, as do carbonate and pyritized silicate microfossils. The combined paleoenvironmental information from Site 959 and a close-by shelf site in Nigeria implies the general absence of eukaryotic surface-dwelling microplankton during peak PETM warmth in the eastern equatorial Atlantic, most likely caused by heat stress. We hypothesize, based on a literature survey, that heat stress might have reduced calcification in more tropical regions, potentially contributing to reduced deep sea carbonate accumulation rates, and, by buffering acidification, also to biological carbonate compensation of the injected carbon during the PETM. Crucially, abundant organic benthic foraminiferal linings imply sustained export production, likely driven by prokaryotes. In sharp contrast, the recovery of the CIE yields rapid (<< 10 kyr) fluctuations in the abundance of several dinocyst groups, suggesting extreme ecosystem and environmental variability.	[Frieling, Joost; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Reichart, Gert-Jan; Middelburg, Jack J.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Princetonpl 9, NL-3584 CC Utrecht, Netherlands; [Reichart, Gert-Jan] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands; [Roehl, Ursula; Westerhold, Thomas] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany; [Bohaty, Steven M.] Univ Southampton, Natl Oceanog Ctr Southampton, Ocean & Earth Sci, Waterfront Campus European Way, Southampton SO14 3ZH, Hants, England	Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bremen; NERC National Oceanography Centre; University of Southampton	Frieling, J (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands.	j.frieling1@uu.nl	Westerhold, Thomas/D-4581-2011; Sluijs, Appy/B-3726-2009; Middelburg, Jack/B-4951-2011; Rohl, Ursula/G-5986-2011; Reichart, Gert-Jan/N-6308-2018	Westerhold, Thomas/0000-0001-8151-4684; Sluijs, Appy/0000-0003-2382-0215; Middelburg, Jack/0000-0003-3601-9072; Rohl, Ursula/0000-0001-9469-7053; Frieling, Joost/0000-0002-5374-1625; Reichart, Gert-Jan/0000-0002-7256-2243	European Research Council (ERC) under European Union; ERC [259627]; Netherlands Organization for Scientific Research (NWO) [834.11.006]; Deutsche Forschungsgemeinschaft; Ministry of Education, Culture and Science (OCW); European Research Council (ERC) [259627] Funding Source: European Research Council (ERC)	European Research Council (ERC) under European Union(European Research Council (ERC)); ERC(European Research Council (ERC)); Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); Ministry of Education, Culture and Science (OCW)(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)); European Research Council (ERC)(European Research Council (ERC))	We thank Natasja Welters, Arnold van Dijk, Ton Zalm, and Dominika Kasjaniuk (Utrecht University) for analytical support and Alex Wulbers and Walter Hale (IODP Bremen Core Repository) and Willem Schinkel (Erasmus University Rotterdam) for sampling assistance. The European Research Council (ERC) under the European Union Seventh Framework Program provided funding for this work with ERC starting grant 259627 to Appy Sluijs. The Netherlands Organization for Scientific Research (NWO) supported this work through grant no. 834.11.006 to Gert-Jan Reichart. The Deutsche Forschungsgemeinschaft supported Ursula Rohl and Thomas Westerhold. This work was carried out under the program of the Netherlands Earth System Science Centre (NESSC), financially supported by the Ministry of Education, Culture and Science (OCW). The International Ocean Discovery Program (IODP) is acknowledged for access to materials and data.	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Past.	JAN 15	2018	14	1					39	55		10.5194/cp-14-39-2018	http://dx.doi.org/10.5194/cp-14-39-2018			17	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	FS7PR		Green Published, Green Submitted, Green Accepted, gold			2025-03-11	WOS:000419990400001
J	Langgut, D				Langgut, D.			Late Quaternary Nile flows as recorded in the Levantine Basin: The palynological evidence	QUATERNARY INTERNATIONAL			English	Article						Nile; Sapropel; Levantine Basin; Heinrich events; Dinoflagellate cysts; Spores	EASTERN MEDITERRANEAN SAPROPELS; MARINE POLLEN RECORD; DEEP-SEA FAN; LATE PLEISTOCENE; NORTH-ATLANTIC; AFRICAN MONSOON; HEINRICH EVENTS; ISOTOPE RECORDS; CLIMATE CHANGES; ORGANIC-MATTER	This study aims to trace changes in the River Nile flows over the Late Quaternary and is based on palynomorphs which were embedded in the sea floor of the Levantine Basin. The palynomorphs were extracted from two marine sediment cores, which cover the last 86 ka and are located at the two ends of the Levantine Basin: MD-9509, at the southern part of the Levantine Basin, and MD-9501, at its northern part. Core MD-9509 was taken from the Nile cone and is characterized by high sedimentation rates and a good state of palynomorph preservation. The assemblages included palynomorphs which were transported via the Nile headwaters and therefore enabled the reconstruction of the River Nile flows. The results demonstrate that the last glacial period (similar to 75-16 ka) was characterized by a decrease in Nile water discharge and an increase in sediment influx, while opposite trends were observed prior to the last glacial period as well as during the deglaciation and the Holocene. Based on the study of the spores, it is suggested that during the last glacial, the main contributors of freshwater and sediment load to the Eastern Mediterranean Sea were the Blue Nile and the Atbara and only during interglacials was there a more significant contribution of the White Nile. Within the northern core, MD-9501, pollen was preserved only during the formation of sapropels S3 and S1. The comparison of the sapropelic palynological spectra in both core sites clearly indicates that during sapropel deposition, climate conditions were more humid in the Northern Levant, reflecting the north-south regional Mediterranean climatic moisture gradient. Sapropel formation was a result of the intensification of the monsoonal climate system which was most probably related to the maximum insolation values at 65 degrees N, while, currently, the Atlantic is the main influencing climate system in the region. One of the most interesting observations in this study is that during Heinrich Events H2-H6, which originated in the north Atlantic and were identified in MD-9509 based on minimum arboreal pollen percentages, pollen originating from tropical regions was not embedded in the Levantine Basin. These results lend support to the view that episodes of dryness in tropical/sub-tropical Eastern Africa were associated not only with low-latitude climate controls, but also with high-latitude glacial stress. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.	[Langgut, D.] Univ Haifa, Zinman Inst Archaeol, Lab Palynol, IL-3498838 Haifa, Israel; [Langgut, D.] Geol Survey Israel, 30 Malkhe Israel St, IL-95501 Jerusalem, Israel; [Langgut, D.] Tel Aviv Univ, Sonia & Marco Nadler Inst Archaeol, Lab Archaeobot & Ancient Environm, POB 39040, IL-6997801 Tel Aviv, Israel	University of Haifa; Geological Survey Israel; Tel Aviv University	Langgut, D (通讯作者)，Univ Haifa, Zinman Inst Archaeol, Lab Palynol, IL-3498838 Haifa, Israel.; Langgut, D (通讯作者)，Geol Survey Israel, 30 Malkhe Israel St, IL-95501 Jerusalem, Israel.; Langgut, D (通讯作者)，Tel Aviv Univ, Sonia & Marco Nadler Inst Archaeol, Lab Archaeobot & Ancient Environm, POB 39040, IL-6997801 Tel Aviv, Israel.	langgut@post.tau.ac.il		Langgut, Dafna/0000-0002-4824-1044	Ministry of National Infrastructures	Ministry of National Infrastructures	The study was supported by the Ministry of National Infrastructures. I am grateful to the master, crew and scientists aboard R/V Marion Dufresne for their assistance, with special thanks to Dr. Martine Paterne from Gif-sur-Yvette, France. My supervisors during my PhD studies - Prof. Mina Weinstein-Evron, Dr. Myriam Bar-Matthews and Dr. Ahuva Almogi-Labin, are gratefully appreciated for numerous discussions and suggestions, as well as for their support throughout the research. Michael Kitin, Silvia Chaim, and Allon Wagner are acknowledged for their technical help. Thanks also to M. Cavanagh and B. Laugomer for their assistance with the preparation of the figures. I wish to thank Prof. Mina Weinstein-Evron for her critical comments on an early draft which helped to improve the manuscript. Three anonymous reviewers are also acknowledged for their useful comments and suggestions. Thanks also to the Min -Te Chen - the Editor-in-Chief, and to the guest editors, Dr. Danny Rosenberg and Dr. Reuven Yeshurun for handling the manuscript.	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Int.	JAN 10	2018	464		A				273	284		10.1016/j.quaint.2017.07.006	http://dx.doi.org/10.1016/j.quaint.2017.07.006			12	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	FW3TR					2025-03-11	WOS:000425233900020
J	Kim, SY; Roh, YH; Shin, HH; Huh, S; Kang, SH; Lim, D				Kim, So-Young; Roh, Youn Ho; Shin, Hyeon Ho; Huh, Sik; Kang, Sung-Ho; Lim, Dhongil			Decadal-scale variations of sedimentary dinoflagellate cyst records from the Yellow Sea over the last 400 years	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Eutrophication; Dinoflagellate cyst; Alexandrium bloom; Mud deposits; Yellow Sea	HARMFUL ALGAL BLOOMS; EAST CHINA SEA; COASTAL WATERS; SPATIAL-DISTRIBUTION; METAL CONTAMINATION; SURFACE SEDIMENTS; MARINE-SEDIMENTS; GROWTH-RATES; BALTIC SEA; BOHAI SEA	In recent decades, the Yellow Sea has experienced severe environmental deterioration due to increasing input of anthropogenic pollutants and consequently accelerated eutrophication. Whilst there have been significant advances in documenting historical records of metal pollution in the Yellow Sea region, changes in phytoplankton community structures affected by eutrophication remain understudied. Here, we present a new record of dinoflagellate cyst-based signals in age-dated sediment cores from the Yellow Sea mud deposits to provide better insight into eutrophication history and identification of associated responses of the regional phytoplankton community. It is worthy of note that there were significant variations in abundances and community structures of dinoflagellate cysts in three historical stages in association with increasing anthropogenic activity over the last 400 years. Pervasive effects of human interference altering the Yellow Sea environments are recognized by: 1) an abrupt increase of organic matter, including the diatom-produced biogenic opal concentrations (similar to 1850); 2) a distinct shift in phytoplankton composition towards dinoflagellate dominance (similar to 1940), and 3) recent acceleration of dinoflagellate cyst accumulation (similar to 1990). Particularly in the central Yellow Sea shelf, the anomalously high deposition of dinoflagellate cysts (especially Alexandrium species) is suggested to be a potentially important source of inoculum cells serving as a seed population for localized and recurrent blooms in coastal areas around the Yellow Sea. (C) 2017 Elsevier Ltd. All rights reserved.	[Kim, So-Young; Kang, Sung-Ho] Korea Polar Res Inst, Div Polar Ocean Sci, Incheon 406840, South Korea; [Roh, Youn Ho] Korea Polar Res Inst, Div Polar Paleoenvironm, Incheon 406840, South Korea; [Roh, Youn Ho; Lim, Dhongil] Univ Sci & Technol, Daejeon 34113, South Korea; [Shin, Hyeon Ho; Lim, Dhongil] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea; [Huh, Sik] Korea Inst Ocean Sci & Technol, Dept Geol & Geophys, Ansan, South Korea	Korea Polar Research Institute (KOPRI); Korea Polar Research Institute (KOPRI); University of Science & Technology (UST); Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST)	Lim, D (通讯作者)，Univ Sci & Technol, Daejeon 34113, South Korea.	oceanlim@kiost.ac.kr	Lim, Dhongil/ACH-3964-2022; Kim, So-Young/JFS-7698-2023	Shin, Hyeon Ho/0000-0002-9711-6717; Lim, Dhongil/0000-0002-0832-2907	Ministry of Oceans and Fisheries, Korea [PE99537, PM17040]	Ministry of Oceans and Fisheries, Korea	This study is a contribution to the Korea Institute of Ocean Sciences & Technology research program (grant no. PE99537), and the K-AOOS Program (KOPRI; PM17040) funded by the Ministry of Oceans and Fisheries, Korea. We thank the Library of Marine Samples (LiMS), the Korea Institute of Ocean Sciences & Technology, for supplying the sediment samples for biogenic silicate analysis. The authors are grateful to the editor and three anonymous reviewers for their comments and suggestions that improved the manuscript.	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JAN 5	2018	200						91	98		10.1016/j.ecss.2017.10.006	http://dx.doi.org/10.1016/j.ecss.2017.10.006			8	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	FV1GE					2025-03-11	WOS:000424308600008
J	Pearce, MA				Pearce, Martin A.			Additional new organic-walled dinoflagellate cysts from two onshore UK Chalk boreholes	JOURNAL OF MICROPALAEONTOLOGY			English	Article							SOUTHERN ENGLAND; BIOSTRATIGRAPHY	Beautifully preserved dinoflagellate cysts continue to be discovered in UK Cretaceous chalks and provide important new biostratigraphic information. Five new species - Conosphaeridium norfolkense sp. nov., Glaphyrocysta coniacia sp. nov., Impletosphaeridium banterwickense sp. nov., Sentusidinium devonense sp. nov., Sentusidinium spinosum sp. nov. and the new subspecies Spiniferites ramosus subsp. ginakrogiae subsp. nov. - are described from Upper Cretaceous strata of the British Geological Survey (BGS) Banterwick Barn and Trunch boreholes (onshore UK). An emended diagnosis for Odontochitina diducta Pearce is also provided to broaden the morphological variability in the type material.	[Pearce, Martin A.] Evolut Appl Ltd, 50 Mitchell Way, Cheltenham GL54 2PL, Glos, England		Pearce, MA (通讯作者)，Evolut Appl Ltd, 50 Mitchell Way, Cheltenham GL54 2PL, Glos, England.	info@evolutionapplied.com		Pearce, Martin/0000-0001-7856-1076				Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], VERHANDELINGEN KONIN; [Anonymous], HIMAL GEOL; [Anonymous], P 2 PLANKT C; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1971, P 2 PLANKT C; [Anonymous], 1885, HG BRONNS KLASSEN OR; Benson D.G. Jr., 1976, Tulane Stud Geol Paleont, V12, P169; Boltenhagen E., 1977, P1; Brideaux W.W., 1975, BULLETIN, V252, P1; BUJAK JP, 1976, MAR MICROPALEONTOL, V1, P101, DOI 10.1016/0377-8398(76)90007-4; Burger D., 1980, Alcheringa, V4, P263, DOI 10.1080/03115518008558971; BURGER D., 1980, BUREAU MINERAL RESOU, V189, P1; Clarke R. F. A., 1967, Verb K ned Akad Wet Amst, V24, P1; COOKSON I C, 1968, Journal of the Royal Society of Western Australia, V51, P110; Cookson I. 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JAN 5	2018	37	1					73	86		10.5194/jm-37-73-2018	http://dx.doi.org/10.5194/jm-37-73-2018			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	FS5EK		gold			2025-03-11	WOS:000419816200006
J	Bijl, PK; Houben, AJP; Bruls, A; Pross, J; Sangiorgi, F				Bijl, Peter K.; Houben, Alexander J. P.; Bruls, Anja; Pross, Joerg; Sangiorgi, Francesca			Stratigraphic calibration of Oligocene-Miocene organic-walled dinoflagellate cysts from offshore Wilkes Land, East Antarctica, and a zonation proposal	JOURNAL OF MICROPALAEONTOLOGY			English	Article							SOUTHERN-OCEAN; MIDDLE MIOCENE; MAGNETOSTRATIGRAPHIC CALIBRATION; EOCENE; PACIFIC; BASIN; BIOSTRATIGRAPHY; GLACIATION; PALYNOLOGY; EXPEDITION	There is growing interest in the scientific community in reconstructing the paleoceanography of the Southern Ocean during the Oligocene-Miocene because these time intervals experienced atmospheric CO2 concentrations with relevance to our future. However, it has remained notoriously difficult to put the sedimentary archives used in these efforts into a temporal framework. This is at least partially due to the fact that the bioevents recorded in organic-walled dinoflagellate cysts (dinocysts), which often represent the only microfossil group preserved, have not yet been calibrated to the international timescale. Here we present dinocyst ranges from Oligocene-Miocene sediments drilled offshore the Wilkes Land continental margin, East Antarctica (Integrated Ocean Drilling Program (IODP) Hole U1356A). In addition, we apply statistical means to test a priori assumptions about whether the recorded taxa were deposited in situ or were reworked from older strata. Moreover, we describe two new dinocyst species, Selenopemphix brinkhuisii sp. nov. and Lejeunecysta adeliensis sp. nov., which are identified as important markers for regional stratigraphic analysis. Finally, we calibrate all identified dinocyst events to the international timescale using independent age control from calcareous nanoplankton and magnetostratigraphy from IODP Hole U1356A, and we propose a provisional dinoflagellate cyst zonation scheme for the Oligocene-Miocene of the Southern Ocean.	[Bijl, Peter K.; Bruls, Anja; Sangiorgi, Francesca] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, POB 80-115, NL-3508 TC Utrecht, Netherlands; [Houben, Alexander J. P.] Netherlands Org Appl Sci Res TNO, Appl Geosci Team, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, Neuenheimer Feld 234, D-69120 Heidelberg, Germany	Utrecht University; Netherlands Organization Applied Science Research; Ruprecht Karls University Heidelberg	Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, POB 80-115, NL-3508 TC Utrecht, Netherlands.	p.k.bijl@uu.nl		Bijl, Peter/0000-0002-1710-4012; Sangiorgi, Francesca/0000-0003-4233-6154; Houben, Alexander/0000-0002-9497-1048	US National Science Foundation; NWO-NNPP [866.10.110]; NWO-ALW VENI [863.13.002]	US National Science Foundation(National Science Foundation (NSF)); NWO-NNPP; NWO-ALW VENI(Netherlands Organization for Scientific Research (NWO))	We thank the constructive reviews of Michael J. Hannah and Kasia S. Sliwinska, which really improved our paper. This research used samples and data from the Integrated Ocean Drilling Program. IODP was sponsored by the US National Science Foundation and participating countries under management of Joined Oceanographic Institutions Inc. PKB and FS thank NWO-NNPP grant no. 866.10.110, NWO-ALW VENI grant no. 863.13.002 for funding and Natasja Welters for technical support. We thank Margot Cramwinckel for producing the illustrations in Fig. 5.	[Anonymous], 2001, TERRA ANTARTICA; [Anonymous], 2001, Terra Antartica, V8, P615; [Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1885, HG BRONNS KLASSEN OR; ARTZNER DG, 1978, CAN J BOT, V56, P1381, DOI 10.1139/b78-158; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; Bijl P. 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J	Smelror, M; Larssen, GB; Olaussen, S; Romuld, A; Williams, R				Smelror, Morten; Larssen, Geir Birger; Olaussen, Snorre; Romuld, Arnfinn; Williams, Robert			Late Triassic to Early Cretaceous palynostratigraphy of Kong Karls Land, Svalbard, Arctic Norway, with correlations to Franz Josef Land, Arctic Russia	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Mesozoic; stratigraphy; palynology; Svalbard	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; VOLGIAN-RYAZANIAN BOUNDARY; KAPP TOSCANA GROUP; BARENTS SEA; AGARDHFJELLET FORMATION; CENTRAL SPITSBERGEN; MESOZOIC MAGMATISM; NORDKAPP BASIN; SP-NOV; HOPEN	The Upper Triassic, Jurassic and Lower Cretaceous succession on Kong Karls Land contains common to abundant, well preserved, marine and terrestrial palynomorphs. The palynological assemblages suggest a Norian age for the Flatsalen Formation, which comprises the oldest deposits exposed on the islands. The overlying Svenskoya Formation is dated as Norian/?Rhaetian to Early Toarcian. There are possible depositional breaks at the base of and within this formation. The overlying Kongsoya Formation is dated as Late Toarcian-Aalenian. There is no evidence of exposed Bajocian deposits on Kong Karls Land. The oldest, transgressive deposits of the Agardhfjellet Formation are dated as Bathonian, while the youngest part of this formation is of Kimmeridgian age. The oldest Cretaceous deposits exposed on Kong Karls Land are ValanginianHauterivian condensed carbonates assigned to the Tordenskjoldberget Member (Klippfisk Formation). Directly overlying the condensed unit are Upper Barremian, or possibly lowermost Aptian, marine shales of the Kolje Formation equivalent. The youngest rocks preserved on Kong Karls Land are fluvial deposits of the Harfagrehaugen Member (Helvetiafjellet Formation) and the Kong Karls Land basaltic lava flows. The terrestrial palynomorphs found in the Hafagrehaugen Member support a latest Barremian to Aptian age for the Helvetiafjellet Formation, as suggested by the U-Pb geochronology.	[Smelror, Morten] Geol Survey Norway, POB 6315 Torgarden, NO-7491 Trondheim, Norway; [Larssen, Geir Birger] Lundin Norway AS, POB 794, NO-9488 Harstad, Norway; [Olaussen, Snorre] Univ Ctr Svalbard UNIS, Dept Arctic Geol, POB 156, NO-9171 Longyearbyen, Norway; [Romuld, Arnfinn] Equinor ASA, Forusbeen 50, NO-4035 Stavanger, Norway; [Williams, Robert] Norwegian Petr Directorate, POB 600, NO-4003 Stavanger, Norway	Geological Survey of Norway; University Centre Svalbard (UNIS); Equinor	Smelror, M (通讯作者)，Geol Survey Norway, POB 6315 Torgarden, NO-7491 Trondheim, Norway.	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J	Alsen, P; Piasecki, S				Alsen, Peter; Piasecki, Stefan			Biostratigraphy of the Hareelv Formation (Upper Jurassic) in the Blokelv-1 core, Jameson Land, central East Greenland	GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN			English	Article						Jameson Land Basin; East Greenland; ammonites; dinoflagellate cysts; biostratigraphy; chronostratigraphy; Oxfordian; Kimmeridgian; Volgian	SUCCESSION	The Hareelv Formation in the Blokelv-1 core is biostratigraphically subdivided by means of ammonite and dinoflagellate cyst stratigraphy. The succession ranges from the Oxfordian C. densiplicatum Chronozone to the Volgian P. elegans Chronozone. The mudstones of the Blokelv-1 core are characterised by large amounts of amorphous organic matter. This hampers the preparation and identification of dinoflagellate cysts, which are also commonly degraded and corroded. Ammonites, on the other hand, are common and well-preserved in the core, contrasting with that observed in the equivalent facies and stratigraphic interval at outcrop. Integration of the ammonite and dinoflagellate cyst biostratigraphical data yields a robust chronostratigraphic subdivision of the middle Oxfordian - lowermost Volgian cored section.	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S, 1996, FORMATION SOURCE RES, VII; Nohr-Hansen Henrik, 2002, Geology of Greenland Survey Bulletin, V191, P111; Page Kevin N., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P23; PIASECKI S, 1979, Bulletin of the Geological Society of Denmark, V28, P31; Piasecki S., 2004, GEOLOGICAL SURVEY DE, V5, P87; Piasecki S., 1996, FORMATION SOURCE RES, V1; Piasecki S, 1981, THESIS; Piasecki Stefan, 2004, Geological Survey of Denmark and Greenland Bulletin, V5, P99; Piasecki Stefan, 2004, Geological Survey of Denmark and Greenland Bulletin, V5, P73; Poulsen N.E., 1985, Arsskrift for Dansk Geologisk Forening, V1984, P133; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; Riding J.B., 1992, P7; Rosenkrantz A., 1929, Meddelelser om Gronland, V83, P135; Smelror M., 1988, Gronlands Geologiske Undersogelse Rapport, V137, P135, DOI [DOI 10.34194/RAPGGU.V137.8019, 10.34194/rapggu.v137.8019]; Spath L., 1935, MEDD GRONLAND, V99, P82; Spath L.F., 1936, MEDDELELSER GRONLAND, V99; SURLYK F, 1991, AAPG BULL, V75, P1468; Surlyk F, 2001, B GEOL SOC DENMARK, V48, P169; Surlyk F., 1973, B GRONLANDS GEOLOGIS, V105; Surlyk F., 1978, B GR NLANDS GEOLOGIS, V128, DOI [10.34194/bullggu.v128.6670, DOI 10.34194/BULLGGU.V128.6670]; Surlyk F., 2003, The Jurassic of Denmark and Greenland. Geological Survey of Denmark and Greenland Bulletin, V1, P659, DOI DOI 10.34194/GEUSB.V1.4674; SYKES R M, 1979, Palaeontology (Oxford), V22, P839; SYKES RM, 1976, LETHAIA, V9, P421, DOI 10.1111/j.1502-3931.1976.tb00984.x; Vosgerau H., 2004, GEOL SURV DEN GREENL, V5, P51, DOI [10.34194/geusb.v5.4807, DOI 10.34194/GEUSB.V5.4807]; Wierzbowski A, 2002, NEUES JAHRB GEOL P-A, V226, P145, DOI 10.1127/njgpa/226/2002/145; Woollam R., 1983, 832 I GEOL SCI; Zeiss Arnold, 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P75; Ziegler P.A., 1982, GEOLOGICAL ATLAS W C	55	13	13	0	0	GEOLOGICAL SURVEY DENMARK & GREENLAND	COPENHAGEN K	OSTER VOLDGADE 10, COPENHAGEN K, DK-1350, DENMARK	1604-8156			GEOL SURV DEN GREENL	Geol. Surv. Den. Greenl. Bull.		2018		42					15	37						23	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	IE1GG					2025-03-11	WOS:000472133400003
S	Verreussel, RMCH; Bouroullec, R; Munsterman, DK; Dybkjær, K; Geel, CR; Houben, AJP; Johannessen, PN; Kerstholt-Boegehold, SJ		Kilhams, B; Kukla, PA; Mazur, S; Mckie, T; Mijnlieff, HF; VanOjik, K		Verreussel, R. M. C. H.; Bouroullec, R.; Munsterman, D. K.; Dybkjaer, K.; Geel, C. R.; Houben, A. J. P.; Johannessen, P. N.; Kerstholt-Boegehold, S. J.			Stepwise basin evolution of the Middle Jurassic-Early Cretaceous rift phase in the Central Graben area of Denmark, Germany and The Netherlands	MESOZOIC RESOURCE POTENTIAL IN THE SOUTHERN PERMIAN BASIN	Geological Society Special Publication		English	Article; Book Chapter							DANISH CENTRAL GRABEN; RESERVOIR SANDSTONES; DINOFLAGELLATE CYSTS; TERSCHELLING BASIN; DUTCH OFFSHORE; BIOSTRATIGRAPHY; STRATIGRAPHY; GREENHOUSE; REVISION; BOUNDARY	This paper presents the results of a cross-border study of the Middle Jurassic-Early Cretaceous rift phase in the Danish-German-Dutch Central Graben area. Based on long-distance correlations of palynologically interpreted wells, a stepwise basin evolution pattern was determined. Four phases are defined and described as tectonostratigraphic mega-sequences (TMS). The TMS are governed by changes in the tectonic regime. TMS-1 reflects the onset of rifting, triggered by regional east-west extension. Rift climax was reached during TMS-1, reflected by thick mudstone accumulations. TMS-2 reflects a change in the tectonic regime from east-west to NE-SWextension. NW-SE-trending normal faults became active during this phase, switching the depocentres from the graben axis into adjacent basins. TMS-3 displays divergent basin development. In the Dutch Central Graben area, it is characterized by a basal unconformity and widespread sandstone deposition, indicating continued salt and fault activity. Organic-rich mudstone deposition prevails in the Danish and German Central Graben area, indicating sediment starvation and water-mass stratification. With TMS-4 the rift phase ended, reflected by regionally uniform mudstone deposition. The basin evolution model presented here coherently places the lithostratigraphic units occurring in a stratigraphic framework and provides a valuable basis for hydrocarbon exploration activities in the region.	[Verreussel, R. M. C. H.; Munsterman, D. K.; Houben, A. J. P.] TNO Netherlands Org Appl Sci Res, Geol Survey Netherlands, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [Bouroullec, R.; Geel, C. R.; Kerstholt-Boegehold, S. J.] TNO Netherlands Org Appl Sci Res, Appl Geosci, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [Dybkjaer, K.; Johannessen, P. N.] GEUS Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark	Netherlands Organization Applied Science Research; Netherlands Organization Applied Science Research; Geological Survey Of Denmark & Greenland	Verreussel, RMCH (通讯作者)，TNO Netherlands Org Appl Sci Res, Geol Survey Netherlands, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands.	roel.verreussel@tno.nl	Johannessen, Peter/G-9912-2018; Bouroullec, Renaud/AAE-1874-2019; Dybkjær, Karen/G-5223-2018	Houben, Alexander/0000-0002-9497-1048				Abbink OA, 2006, NETH J GEOSCI, V85, P221, DOI 10.1017/S001677460002148X; ABBINK O. 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Soc. Spec. Publ.		2018	469						305	340		10.1144/SP469.23	http://dx.doi.org/10.1144/SP469.23			36	Geology	Book Citation Index– Science (BKCI-S)	Geology	BM7EZ		hybrid			2025-03-11	WOS:000467836000016
S	Gogoi, B; Prasad, V; Garg, R; Singh, I		Bajpai, S; Tripathi, SC; Prasad, V		Gogoi, Bikash; Prasad, Vandana; Garg, Rahul; Singh, Indrabir			Palynofacies Study of Lakadong Limestone (Late Paleocene) of Mawsynram Area, Shillong Plateau, India: Implications for Sequence Stratigraphy	INDIAN PALEOGENE	Society of Earth Scientists Series		English	Article; Book Chapter						Sedimentary organic matter; Biostratigraphy; Carbonate facies; Palaeoenvironment; High Stand Systems Tract (HST)	SEDIMENTARY ORGANIC-MATTER; FORAMINIFERAL BIOSTRATIGRAPHY; VOCONTIAN TROUGH; CARBONATES; FACIES	Subtle paleoenvironmental fluctuations are difficult to detect in sedimentologically uniform carbonate rocks, however, study of relative increase and decrease of marine and terrestrial organic matter content provides a useful tool for deciphering the deepening and shallowing cycles in these successions. Lakadong Limestone Member in Khasi and Jaintia hills in South Shillong Plateau is late Paleocene in age and forms part of the carbonate platform. It represents deposition during High Stand Systems Tract. In the present study palynofacies analysis were carried out in two Lakadong Limestone sections i.e., Dohsniang (Kurtinsiang) (KPL) and Laitmowksing (LTL) from Khasi hills for detailed palaeoenvironmental interpretations, for the correlation and for the identification of higher order sea level cycles. Both the sections have been dated as late Paleocene based on the characteristic larger benthic foraminiferal assemblages belonging to the Tethyan Shallow Benthic Zones SBZ 3. For palynofacies analysis various type of organic matter were characterized and counted. The study shows cyclicity pattern in the organic matter types in both the sections which may be linked to the sea level changes of higher order cycles. Based on the variation in the organic matter content both the sections were subdivided into distinct palynofacies units. Each palynofacies unitsstart with high proportion of black oxidized palynomaceral along with dinoflagellate cysts representing a transgressive surface, followed by high quantity of degraded brown and cuticle organic matter from terrestrial source. Each palynofacies unit thus represent progradational deposit of High Stand Systems Tract starting with the deepening facies followed by shallowing facies of more terrestrial origin. Four progradational sequences have been identified in the KPL and three in the LTL section that can be correlated. Palynofacies study thus offers a logical approach for the study of uniform carbonate facies. Based on the present palynofacies criteria it has been possible to identify higher order sea level cycles in the Lakadong Limestone exposed at KPL and LTL section in Khasi Hills.	[Gogoi, Bikash] Gauhati Univ, Dept Geol Sci, Gauhati 781014, India; [Prasad, Vandana; Garg, Rahul] Birbal Sahni Inst Palaeosci, Lucknow 226007, Uttar Pradesh, India; [Singh, Indrabir] 17-11-2C Metro City Nishat Ganj, Lucknow 226007, Uttar Pradesh, India	Gauhati University; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Prasad, V (通讯作者)，Birbal Sahni Inst Palaeosci, Lucknow 226007, Uttar Pradesh, India.	prasad.van@gmail.com	Gogoi, Bikash/AAY-2636-2021					[Anonymous], 1987, GEOLOGICAL SOC LONDO; [Anonymous], 1962, Bulletin of the Geological Mining and Metallurgical Society of India, V25, P1; [Anonymous], PALYNOLOGY; [Anonymous], 2006, DELTA SEDIMENTATION; Aubry MP, 1998, LATE PALAEOCENE EARL; Bombardiere L, 1998, SEDIMENTOLOGY, V45, P771, DOI 10.1046/j.1365-3091.1998.00177.x; BOULTER MC, 1986, SEDIMENTOLOGY, V33, P871, DOI 10.1111/j.1365-3091.1986.tb00988.x; BRYANT ID, 1988, MAR PETROL GEOL, V5, P108; BUSTIN RM, 1988, AAPG BULL, V72, P277; COMBAZ A., 1964, REV MICROPALDONTOL, V7, P205; COMBAZ A., 1980, KEROGEN INSOLUBLE OR, P55; Dickens GR, 2000, B SOC GEOL FR, V171, P37; Downie C., 1971, Geoscience Man, V3, P29; Evans P., 1932, Trans Mining Geol. 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K., 1988, IAP PUBLICATION, V4, P34; Jauhri AK, 2001, PALAEOGEOGR PALAEOCL, V168, P187, DOI 10.1016/S0031-0182(00)00255-8; Kiessling W, 2003, LETHAIA, V36, P195, DOI 10.1080/00241160310004648; Loutit T.S., 1988, SEA LEVEL CHANGES IN, P183, DOI DOI 10.2110/PEC.88.01.0183; Mathur LP, 1964, INT GEOL C 22 SESS I, P88; Medlicott H. B., 1869, MEMOIRS GEOLOGICAL S, V7, P151; MULLER JAN, 1959, MICROPALEONTOLOGY, V5, P1, DOI 10.2307/1484153; MURTHY M. V. N., 1976, Records of the Geological Survey of India, V107, P80; NAGAPPA YEDATORE, 1959, MICROPALEONTOLOGY, V5, P145, DOI 10.2307/1484208; Parry C.C., 1981, Petroleum geology of the continental shelf of Northwest Europe, P205; Pittet B, 1997, SEDIMENTOLOGY, V44, P915, DOI 10.1046/j.1365-3091.1997.d01-58.x; Pocock SAJ, 1982, SEPM SHORT COURSE, V7, P7; Prasad V, 2013, FACIES, V59, P737, DOI 10.1007/s10347-012-0355-8; Prasad Vandana, 2006, Journal of the Palaeontological Society of India, V51, P75; PRATT LM, 1984, AAPG BULL, V68, P1146; Raja Rao C.S., 1981, COALFIELDS N E INDIA, V45, P1; Serra-Kiel J, 1998, B SOC GEOL FR, V169, P281; Smelror M., 1989, Palynology, V13, P121; STANLEY DJ, 1986, MAR GEOL, V70, P85, DOI 10.1016/0025-3227(86)90090-3; STEFFEN D, 1993, B CENT RECH EXPL, V17, P235; STROHMENGER C, 1993, B CENT RECH EXPL, V17, P183; Summerhayes C.P., 1987, MARINE PETROLEUM SOU, P301; Tappan H.N., 1980, PALEOBIOLOGY PLANT P, P1028; TISSOT B, 1979, NATURE, V277, P463, DOI 10.1038/277463a0; Tissot B.P., 1984, Petroleum formation and occurrence, Vsecond, P538; Tyson R. V., 1996, SEQUENCE STRATIGRAPH, V103, P75; 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]; VANDERZWAN CJ, 1990, REV PALAEOBOT PALYNO, V62, P157, DOI 10.1016/0034-6667(90)90021-A; WALL DAVID, 1965, MICRO PALEONTOLOGY, V11, P151, DOI 10.2307/1484516; Whitaker MF, 1984, OFFSHORE NO SEAS RED, P6; WILSON g f, 1953, Sci. Petrol, V6, P119	58	3	3	0	1	SPRINGER INTERNATIONAL PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2194-9204		978-3-319-77443-5; 978-3-319-77442-8	SOC EARTH SCI SER			2018							187	207		10.1007/978-3-319-77443-5_7	http://dx.doi.org/10.1007/978-3-319-77443-5_7	10.1007/978-3-319-77443-5		21	Geology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Paleontology	BM3EI					2025-03-11	WOS:000461946200008
J	Paolillo, MA; Guler, MV; Lazo, DG; Pazos, PJ; Ottone, EG; Aguirre-Urreta, B				Paolillo, Melisa A.; Veronica Guler, M.; Lazo, Dario G.; Pazos, Pablo J.; Ottone, Eduardo G.; Aguirre-Urreta, Beatriz			EARLY CRETACEOUS DINOFLAGELLATE CYSTS FROM THE AGRIO FORMATION AT ITS TYPE LOCALITY (NEUQUEN. BASIN, ARGENTINA) AND THEIR BIOSTRATIGRAPHIC IMPLICATIONS	AMEGHINIANA			English	Article						Dinocysts; Biostratigraphy; Valanginian; Hauterivian; South America	WEST-CENTRAL ARGENTINA; STRATIGRAPHY; AMMONITES; MEMBER; PALYNOSTRATIGRAPHY; INVERTEBRATES; PALEOECOLOGY; TRIGONIOIDA; ASSEMBLAGES; BIVALVIA	The Early Cretaceous marine deposits of the Agrio Formation are widely distributed in southern Mendoza and Neuquen provinces, Argentina. The stratigraphic distribution of upper Valanginian to upper Hauterivian organic-walled dinoflagellate cysts was evaluated at the Agrio Formation, at Bajada del Agrio locality. The assemblages exhibit a relatively moderate to low diversity and those with greater abundance are dominated by a small number of species such as Circulodinium distinctum, Cribroperidinium spp., Exochosphaeridium spp., Florentinia mantellii, Kiokansium unituberculatum, and Oligosphaeridium complex. Three diagnostic bioevents of lowest (LO) and highest (HO) stratigraphic occurrences of taxa calibrated with the local ammonoid zonation were identified for the Early Cretaceous of the Neuquen Basin: the LO of Callaiosphaeridium sp. (base of Holcoptychites neuquensis Zone, earliest Hauterivian), the LO of Cymososphaeridium validum (uppermost Hoplitocrioceras gentilii Zone, upper early Hauterivian) and the HO of Cymososphaeridium validum (lowermost Crioceratites diamantensis Zone, late Hauterivian). The studied assemblages are compared with Early Cretaceous assemblages from the Northern Hemisphere. In general, the association of dinoflagellate cysts together with the selected diagnostic species exhibit a clear affinity with those of the Mediterranean region.	[Paolillo, Melisa A.; Veronica Guler, M.] UNS, Dept Geol, Inst Geol Sur, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Lazo, Dario G.; Pazos, Pablo J.; Ottone, Eduardo G.; Aguirre-Urreta, Beatriz] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Inst Estudios Andinos Don Pablo Groeber, Pabellon 2,Ciudad Univ,Intendente Guiraldes 2160, Buenos Aires, DF, Argentina; [Lazo, Dario G.; Pazos, Pablo J.; Ottone, Eduardo G.; Aguirre-Urreta, Beatriz] Consejo Nacl Invest Cient & Tecn, Ave Godoy Cruz 2290,C1425FQB, Buenos Aires, DF, Argentina	National University of the South; University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Paolillo, MA (通讯作者)，UNS, Dept Geol, Inst Geol Sur, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	mpaolillo@ingeosur-conicet.gob.ar; vguler@criba.edu.ar	Pazos, Pablo/D-5973-2014; Lazo, Dario/AAT-9498-2021	Lazo, Dario G./0000-0002-8270-1577	PICT [2015-1381]	PICT(ANPCyT)	We are grateful to G. 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J	Sluijs, A; van Roij, L; Frieling, J; Laks, J; Reichart, GJ				Sluijs, Appy; van Roij, Linda; Frieling, Joost; Laks, Jelmer; Reichart, Gert-Jan			Single-species dinoflagellate cyst carbon isotope ecology across the Paleocene-Eocene Thermal Maximum	GEOLOGY			English	Article							FRACTIONATION	We present the first ever species-specific fossil dinoflagellate cyst stable carbon isotope (delta C-13) records, from the Bass River Paleocene-Eocene Thermal Maximum (PETM) section in New Jersey (USA), established using a novel coupled laser ablation-isotope ratio mass spectrometer setup. Correspondence with carbonate delta C-13 records across the characteristic negative carbon isotope excursion indicates that the delta C-13 of dissolved inorganic carbon exerts a major control on dinocyst delta C-13. Pronounced and consistent differences between species, however, reflect different habitats or life cycle processes and different response to pCO(2). Decreased interspecimen variability during the PETM in a species that also drops in abundance suggests a more limited niche, either in time (seasonal) or space. This opens a new approach for ecological and evolutionary reconstructions based on organic microfossils.	[Sluijs, Appy; van Roij, Linda; Frieling, Joost; Laks, Jelmer; Reichart, Gert-Jan] Univ Utrecht, Fac Geosci, Dept Earth Sci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Reichart, Gert-Jan] Univ Utrecht, NIOZ Royal Netherlands Inst Sea Res, Dept Ocean Syst, POB 59, NL-1790 AB Den Burg, Netherlands; [Reichart, Gert-Jan] Univ Utrecht, POB 59, NL-1790 AB Den Burg, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Sluijs, A (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands.		Reichart, Gert-Jan/N-6308-2018; Sluijs, Appy/B-3726-2009	Reichart, Gert-Jan/0000-0002-7256-2243; Sluijs, Appy/0000-0003-2382-0215	European Research Council [259627]; Dutch Ministry of Education, Culture, and Science; European Research Council (ERC) [259627] Funding Source: European Research Council (ERC)	European Research Council(European Research Council (ERC)); Dutch Ministry of Education, Culture, and Science; European Research Council (ERC)(European Research Council (ERC))	We thank Niels Waarlo for analytical support. Sluijs thanks the European Research Council for Starting Grant 259627. This work was carried out under the program of the Netherlands Earth System Science Centre, financially supported by the Dutch Ministry of Education, Culture, and Science. We thank Erica Crouch and an anonymous reviewer for thoughtful reviews.	BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Cramer BS, 1999, B SOC GEOL FR, V170, P883; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; Dickens GR, 1997, GEOLOGY, V25, P259, DOI 10.1130/0091-7613(1997)025<0259:ABOGIT>2.3.CO;2; Dunkley Jones T, 2013, EARTH-SCI REV, V125, P123, DOI 10.1016/j.earscirev.2013.07.004; Frieling J, 2017, SCI ADV, V3, DOI 10.1126/sciadv.1600891; Gibbs SJ, 2012, BIOGEOSCIENCES, V9, P4679, DOI 10.5194/bg-9-4679-2012; Hayes JM, 1999, CHEM GEOL, V161, P103, DOI 10.1016/S0009-2541(99)00083-2; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Hoins M, 2016, J EXP MAR BIOL ECOL, V481, P9, DOI 10.1016/j.jembe.2016.04.001; Hoins M, 2016, PLOS ONE, V11, DOI 10.1371/journal.pone.0154370; Hoins M, 2015, GEOCHIM COSMOCHIM AC, V160, P267, DOI 10.1016/j.gca.2015.04.001; John CM, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2007PA001465; Kopp RE, 2009, PALEOCEANOGRAPHY, V24, DOI 10.1029/2009PA001783; Matthiessen Jens, 2005, Palaeontologische Zeitschrift, V79, P3; McLean D.M., 1976, Micropaleontology, V22, P347, DOI 10.2307/1485256; MOOK WG, 1974, EARTH PLANET SC LETT, V22, P169, DOI 10.1016/0012-821X(74)90078-8; Rost B, 2006, PLANT CELL ENVIRON, V29, P810, DOI 10.1111/j.1365-3040.2005.01450.x; Sharkey T. D., 1985, Am. Soc. Plant Physiol., P389; 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; Sluijs A, 2007, NATURE, V450, P1218, DOI 10.1038/nature06400; Sluijs A, 2012, GLOBAL BIOGEOCHEM CY, V26, DOI 10.1029/2011GB004224; Van de Waal DB, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0065987; van Roij L, 2017, RAPID COMMUN MASS SP, V31, P47, DOI 10.1002/rcm.7769; Zachos JC, 2005, SCIENCE, V308, P1611, DOI 10.1126/science.1109004	26	20	22	1	14	GEOLOGICAL SOC AMER, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0091-7613	1943-2682		GEOLOGY	Geology	JAN	2018	46	1					79	82		10.1130/G39598.1	http://dx.doi.org/10.1130/G39598.1			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FQ8CD		hybrid, Green Published, Green Submitted			2025-03-11	WOS:000418589600020
J	Lambert, C; Penaud, A; Vidal, M; Klouch, K; Gregoire, G; Ehrhold, A; Eynaud, F; Schmidt, S; Ragueneau, O; Siano, R				Lambert, Clement; Penaud, Aurelie; Vidal, Muriel; Klouch, Khadidja; Gregoire, Gwendoline; Ehrhold, Axel; Eynaud, Frederique; Schmidt, Sabine; Ragueneau, Olivier; Siano, Raffaele			Human-induced river runoff overlapping natural climate variability over the last 150 years: Palynological evidence (Bay of Brest, NW France)	GLOBAL AND PLANETARY CHANGE			English	Article						Pollen grains; Dinoflagellate cysts; Estuarine dynamics; River runoff; Climate variability	NORTH-ATLANTIC OSCILLATION; DINOFLAGELLATE CYSTS; WESTERN-EUROPE; MULTIDECADAL VARIABILITY; ARMORICAN MASSIF; POLLEN; HOLOCENE; RECORD; SEA; EUTROPHICATION	For the first time a very high resolution palynological study (mean resolution of 1 to 5 years) was carried out over the last 150 years in a French estuarine environment (Bay of Brest; NW France), allowing direct comparison between the evolution of landscapes, surface water, and human practices on Bay of Brest watersheds, through continental (especially pollen grains) and marine (phytoplanktonic microalgae: cysts of dinoflagellates or dinocysts) microfossils. Thanks to the small size of the watersheds and the close proximity of the depositional environment to the mainland, the Bay of Brest represents an ideal case study for palynological investigations. Palynological data were then compared to published palaeo-genetic analyses conducted on the same core and to various available instrumental data, allowing us to better characterize past environmental variability since the second half of the 19th century in Western Brittany. We provide evidence of some clues of recent eutrophication and/or pollution that affected phytoplankton communities and which appears linked with increased runoff (higher precipitations, higher percentages of riparian forest pollen, decline of salt marsh-type indicators, and higher values of the XRF Ti/Ca signal), mainly explained by the evolution of agricultural practices since 1945 superimposed on the warming climate trend. We assume that the significant relay observed between dinocyst taxa: Lingulodinium machaerophorum and Spiniferites bentorii around 1965 then followed by Spiniferites membranaceus after 1985, attests to a strong and recent eutrophication of Bay of Brest surface waters induced by high river runoff combined with abnormally elevated air temperatures, especially obvious in the data from 1990. The structure of the dinocyst community has thus been deeply altered, accompanied by an unprecedented increase of Alexandrium minutum toxic form at the same period, as confirmed by the genetic quantification. Despite this recent major anthropogenic forcing, the fossil pollen sequence also records natural climate variability. We highlight, for the first time, a possible connection between climate (AMO modes) and fossil pollen records (especially tree pollination rates) in coastal sediments using tree percentage fluctuations as an indirect proxy for past sea surface and atmospheric temperatures.	[Lambert, Clement; Penaud, Aurelie; Vidal, Muriel; Gregoire, Gwendoline] UBO, IUEM, LGO, UMR CNRS 6538, F-29280 Plouzane, France; [Lambert, Clement; Ragueneau, Olivier] UBO, IUEM, Lab Sci Environm MARin LEMAR, UMR CNRS 6539, F-29280 Plouzane, France; [Klouch, Khadidja; Siano, Raffaele] DYNECO PELAGOS, Ctr Brest, IFREMER, F-29280 Plouzane, France; [Gregoire, Gwendoline; Ehrhold, Axel] IFREMER, Ctr Brest, Geosci Marines, F-29280 Plouzane, France; [Eynaud, Frederique; Schmidt, Sabine] Univ Bordeaux, EPOC UMR5805, F-33615 Pessac, France	Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Ifremer; Ifremer; Universite Paris Cite; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Penaud, A (通讯作者)，UBO, IUEM, LGO, UMR CNRS 6538, F-29280 Plouzane, France.	clement.lambert@univ-brest.fr; aurelie.penaud@univ-brest.fr	Lambert, Clément/ABF-5691-2020; ehrhold, axel/KHY-3754-2024; Schmidt, Sabine/G-1193-2013; Ragueneau, Olivier/H-6021-2017; Vidal, Muriel/B-7856-2014; Penaud, Aurelie/F-2485-2011	Lambert, Clement/0000-0002-7746-8504; Schmidt, Sabine/0000-0002-5985-9747; Ragueneau, Olivier/0000-0001-8598-1730; Ehrhold, Axel/0000-0001-7207-0831; Vidal, Muriel/0000-0003-3699-2083; Penaud, Aurelie/0000-0003-3578-4549	French CNRS; "Laboratoire d'Excellence" LabexMER [ANR-10-LABX-19]; French government under the program "Investissements d'Avenir"	French CNRS(Centre National de la Recherche Scientifique (CNRS)); "Laboratoire d'Excellence" LabexMER; French government under the program "Investissements d'Avenir"(Agence Nationale de la Recherche (ANR))	This study was supported by the French CNRS and is a contribution to the 2015-2016 INSU project EC2CO-LEFE: "CAMOMI: Convergences/Approches croisees des signaux MOleculaires et MIcropaleontologiques pour decrypter les forgages anthropiques et climatiques en milieu coder (Rade de Brest)". This work was supported by the "Laboratoire d'Excellence" LabexMER (ANR-10-LABX-19) and co-funded by a grant from the French government under the program "Investissements d'Avenir". We thank the UMR CNRS 5805 EPOC (Talence) for palynological laboratory procedures (Muriel Georget) and radionuclide measurements, the laboratory IFREMER-Marine Geosciences (Plouzane) for having set out the means for recovering the sediment core (SERABEQ cruises; G. Gregoire PhD thesis, 2016), and the laboratory IFREMER-DYNECO (Plouzane) for having provided samples necessary for the study. Finally, we would like to thank Katalin Kovacs for the English editing of the manuscript, as well as Michel Aidonidis (Head of the Weather Station at Brest) and the National Botanical Conservatory of Brest for constructive exchanges.	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Planet. Change	JAN	2018	160						109	122		10.1016/j.gloplacha.2017.11.004	http://dx.doi.org/10.1016/j.gloplacha.2017.11.004			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	FU9OU		Green Published			2025-03-11	WOS:000424186200008
S	Roy, S; Montresor, M; Cembella, A		Glibert, PM; Berdalet, E; Burford, MA; Pitcher, GC; Zhou, M		Roy, Suzanne; Montresor, Marina; Cembella, Allan			Key Questions and Recent Research Advances on Harmful Algal Blooms in Fjords and Coastal Embayments	GLOBAL ECOLOGY AND OCEANOGRAPHY OF HARMFUL ALGAL BLOOMS	Ecological Studies-Analysis and Synthesis		English	Article; Book Chapter							DISSOLVED ORGANIC NITROGEN; ALEXANDRIUM-MINUTUM; LIFE-CYCLE; AUREOCOCCUS-ANOPHAGEFFERENS; DINOFLAGELLATE BLOOMS; FUTURE PROJECTIONS; PRYMNESIUM-PARVUM; PHOSPHORUS LOADS; CLIMATE-CHANGE; RESTING CYSTS		[Roy, Suzanne] Univ Quebec Rimouski, Inst Sci Mer, Rimouski, PQ, Canada; [Montresor, Marina] Stn Zool Anton Dohrn, Naples, Italy; [Cembella, Allan] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Bremerhaven, Germany	University of Quebec; Universite du Quebec a Rimouski; Stazione Zoologica Anton Dohrn; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Roy, S (通讯作者)，Univ Quebec Rimouski, Inst Sci Mer, Rimouski, PQ, Canada.	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Stud.		2018	232						187	203		10.1007/978-3-319-70069-4_10	http://dx.doi.org/10.1007/978-3-319-70069-4_10	10.1007/978-3-319-70069-4		17	Ecology; Oceanography	Book Citation Index– Science (BKCI-S)	Environmental Sciences & Ecology; Oceanography	BL4ET					2025-03-11	WOS:000450291100011
J	Hehenberger, E; James, ER; del Campo, J; Buckland-Nicks, JA; Reimchen, TE; Keeling, PJ				Hehenberger, Elisabeth; James, Erick R.; del Campo, Javier; Buckland-Nicks, John A.; Reimchen, Thomas E.; Keeling, Patrick J.			Fish Parasite Dinoflagellates <i>Haidadinium ichthyophilum</i> and <i>Piscinoodinium</i> Share a Recent Common Ancestor	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Dinophyceae; endemic stickleback; refugium; SSU rRNA; taxonomy	QUEEN-CHARLOTTE-ISLANDS; MULTIPLE SEQUENCE ALIGNMENT; ENDEMIC STICKLEBACK; HAIDA GWAII; MOLECULAR PHYLOGENY; LIFE-CYCLE; ASSOCIATION; MITOCHONDRIAL; DINOPHYCEAE; MORPHOLOGY	The dinoflagellate Haidadinium ichthyophilum Buckland-Nicks, Reimchen and Garbary 1997 is an ectoparasite of the spine-deficient, three-spine stickleback Gasterosteus aculeatus L. Reimchen 1984, a fish endemic to Rouge Lake, Haida Gwaii. Haidadinium ichthyophilum proved difficult to assign taxonomically because its morphology and complex life cycle exhibited defining characteristics of both autotrophic and heterotrophic dinoflagellates, and was tentatively assigned to the Phytodiniales. Here, we characterized a 492bp fragment of the small subunit ribosomal RNA (SSU rRNA) from preserved H.ichthyophilum cysts. In SSU phylogeny, H.ichthyophilum branches with the fish parasites, Piscinoodinium sp., strongly supporting the inclusion of H.ichthyophilum within the Suessiales.	[Hehenberger, Elisabeth; James, Erick R.; del Campo, Javier; Keeling, Patrick J.] Univ British Columbia, Dept Bot, Canadian Inst Adv Res, 3529-6270 Univ Blvd, Vancouver, BC V6T 1Z4, Canada; [Buckland-Nicks, John A.] St Francis Xavier Univ, Dept Biol, 2320 Notre Dame Ave, Antigonish, NS B2G 2W5, Canada; [Reimchen, Thomas E.] Univ Victoria, Dept Biol, POB 3020, Victoria, BC V8W 3N5, Canada	University of British Columbia; Canadian Institute for Advanced Research (CIFAR); Saint Francis Xavier University - Canada; University of Victoria	Hehenberger, E (通讯作者)，Univ British Columbia, Dept Bot, 3529-6270 Univ Blvd, Vancouver, BC V6T 1Z4, Canada.	helisabe@mail.ubc.ca	James, Erick/D-4725-2012; Hehenberger, Elisabeth/AAG-3123-2021; del Campo, Javier/B-5233-2008	Keeling, Patrick/0000-0002-7644-0745; del Campo, Javier/0000-0002-5292-1421; Hehenberger, Elisabeth/0000-0001-7810-1336	NSERC [227301, 46205, 2354]; Tula Foundation; Marie Curie International Outgoing Fellowship grant [FP7-PEOPLE-2012-IOF - 331450 CAARL]	NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Tula Foundation; Marie Curie International Outgoing Fellowship grant(European Union (EU))	We are grateful to Dr. Rob Fensome and Dr. Juan Saldarriaga for connecting our laboratories. This work was supported by NSERC Discovery grants to PJK (#227301), JB-N (#46205) and TER (#2354). EH and JdC were supported by a grant to the Centre for Microbial Diversity and Evolution from the Tula Foundation. JdC was supported by Marie Curie International Outgoing Fellowship grant (FP7-PEOPLE-2012-IOF - 331450 CAARL). PJK is a Senior Fellow of the Canadian Institute for Advanced Research.	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Eukaryot. Microbiol.	JAN-FEB	2018	65	1					127	131		10.1111/jeu.12430	http://dx.doi.org/10.1111/jeu.12430			5	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	FS6ZC	28544317				2025-03-11	WOS:000419945900012
J	Wang, ZH; Liang, WB; Guo, X; Liu, L				Wang, Zhaohui; Liang, Weibiao; Guo, Xin; Liu, Lei			Inactivation of <i>Scrippsiella</i> <i>trochoidea</i> cysts by different physical and chemical methods: Application to the treatment of ballast water	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cysts; Germination; Ballast water treatment; Heating; Ultraviolet; Ultrasound	SHIPS BALLAST; HYDROGEN-PEROXIDE; MARINE ORGANISMS; GLOBAL TRANSPORT; TREATMENT SYSTEM; ARTEMIA-SALINA; PHYTOPLANKTON; RISK; ZOOPLANKTON; SONICATION	Effects of heating, ultraviolet (UV), ultrasound (US), hydrogen peroxide (H2O2) and freshwater, and the combined treatments on inactivation of cysts of Scrippsiella trochoidea and cysts in sediment suspension were studied. Heating was the most efficient way to inactivate cyst germination, and cysts were completely inactivated at 38 degrees C for 5 h. UV, US, and freshwater efficiently inhibited but could not completely inactivate cyst germination. Effects of heating, UV, and US on cyst germination decreased for cysts in sediment, and germination rates increased by 6.7-48% compared to the same treatment for cysts without sediment. H2O2 significantly inhibited cyst germination, but complete inactivation occurred at high concentration for long duration (100 mg/L, 6d). The combined treatments were more effective, especially the combinations of heating and UV. The results suggested that heating might be a feasible way for ballast water treatment especially after combined with filtration and UV.	[Wang, Zhaohui; Liang, Weibiao; Guo, Xin; Liu, Lei] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China	Jinan University	Wang, ZH (通讯作者)，Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Guangdong, Peoples R China.	twzh@jnu.edu.cn			National Natural Foundation of China [131301235, 41476132]	National Natural Foundation of China(National Natural Science Foundation of China (NSFC))	This work was supported by the National Natural Foundation of China (Nos. 131301235, 41476132).	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Pollut. Bull.	JAN	2018	126						150	158		10.1016/j.marpolbul.2017.11.002	http://dx.doi.org/10.1016/j.marpolbul.2017.11.002			9	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	FW8GQ	29421082				2025-03-11	WOS:000425569400018
J	Grothe, A; Sangiorgi, F; Brinkhuis, H; Stoica, M; Krijgsman, W				Grothe, Arjen; Sangiorgi, Francesca; Brinkhuis, Henk; Stoica, Marius; Krijgsman, Wout			Migration of the dinoflagellate <i>Galeacysta etrusca</i> and its implications for the Messinian Salinity Crisis	NEWSLETTERS ON STRATIGRAPHY			English	Article; Proceedings Paper	Strati Conference	JUL, 2015	Graz, AUSTRIA			Paratethys; Messinian Salinity Crisis; Lago Mare; Pontian; Galeacysta etrusca; dinocyst	SECTION MARCHE PROVINCE; MEDITERRANEAN SEA-LEVEL; EARLIEST ZANCLEAN AGE; DI-TETTO FORMATIONS; LATE MIOCENE; BLACK-SEA; LAGO-MARE; EASTERN PARATETHYS; NORTHERN APENNINES; DACIAN BASIN	The First Occurrence of the cysts of the dinoflagellate Galeacysta etrusca is a well-known marker for the final stage of the Messinian Salinity Crisis in the Mediterranean Basin. This taxon originated from the Paratethys in the north and migrated in a stepwise fashion towards the Mediterranean. Using the First Occurrence of this species throughout different Paratethyan basins and the Mediterranean, we here update and revise its migration path. We show that G. etrusca rapidly migrated from the Pannonian Basin into the Dacian, Black Sea and Caspian basins after the Pontian flooding at similar to 6.1 Ma. During the final stage of the Messinian Salinity Crisis (5.37-5.33 Million year ago), G. etrusca simultaneously appeared in the Mediterranean, indicating a single phase of Paratethyan water spilling into the Mediterranean. We propose to reimpose this single brackish water dominated unit/phase at the end of the MSC as the only valid 'Lago Mare' event.	[Grothe, Arjen; Sangiorgi, Francesca; Brinkhuis, Henk] Univ Utrecht, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol, Dept Earth Sci,Fac Geosci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, NL-1790 AB Den Burg, Texel, Netherlands; [Stoica, Marius] Univ Bucharest, Fac Geol & Geophys, Dept Geol, Balcescu Bd 1, Bucharest 010041, Romania; [Krijgsman, Wout] Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bucharest; Utrecht University	Grothe, A (通讯作者)，Univ Utrecht, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol, Dept Earth Sci,Fac Geosci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands.	a.grothe@uu.nl	Stoica, Marius/N-4941-2018; Brinkhuis, Henk/IUO-8165-2023	Stoica, Marius/0000-0003-0126-4270; Sangiorgi, Francesca/0000-0003-4233-6154; Brinkhuis, Henk/0000-0003-0253-6610; Krijgsman, Wout/0000-0002-1472-1074	Netherlands Geosciences Foundation (ALW); Netherlands Organization for Scientific Research (NWO)	Netherlands Geosciences Foundation (ALW); Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO))	We thank J. van Tongeren and N. Welters for their technical support in the lab. This work was financially supported by the Netherlands Geosciences Foundation (ALW) with support from the Netherlands Organization for Scientific Research (NWO) through the VICI grant of WK. We thank A. Bertini and O. Mandic for their constructive reviews.	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Stratigr.	JAN	2018	51	1			SI		73	91		10.1127/nos/2016/0340	http://dx.doi.org/10.1127/nos/2016/0340			19	Geology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology	FY7EK					2025-03-11	WOS:000427024200005
J	Türkecan, AT; Munsterman, D; Isik, U; Altiner, D; Pinar, M; Çevik, T; Alay, Z				Turkecan, Aksel Tugba; Munsterman, Dirk; Isik, Ugras; Altiner, Demir; Pinar, Mehtap; Cevik, Tugba; Alay, Zeynep			Dinoflagellate cyst biostratigraphy of Miocene strata in the Adana Basin, Eastern Mediterranean, Turkey	PALYNOLOGY			English	Article						dinoflagellate cysts; Mediterranean; Turkey; Adana; Miocene	NORTH-SEA BASIN; OLIGOCENE LOWER MIOCENE; UPPERMOST OLIGOCENE; MIDDLE MIOCENE; NEOGENE EVOLUTION; TRIPLE JUNCTION; SUBMARINE FANS; STRATIGRAPHY; SEQUENCE; JYLLAND	The Adana Basin is one of the major Neogene basins situated in SW Turkey with sedimentary successions providing good records of the paleoenvironmental changes that affected the Mediterranean area. Since a detailed biochronostratigraphic framework has not been properly established in the Adana Basin yet, this study will be the first multidisciplinary approach carried out in this region. In addition, a detailed biozonation based on marine palynomorphs was the first ever documented from the Kopekli Formation deposited during the Miocene (from late Burdigalian to Langhian) and the established biozones were correlated with those of planktonic foraminifera and calcareous nannofossils. According to the first occurrences (FOs) and the last occurrences (LOs) of selected taxa, five biozones (P-1, P-2, P-3, P-4 and P-5) based on dinoflagellate cysts; five biozones (M4a, M4b, M5a, M5b and M6) based on planktonic foraminifera; and two biozones (NN4 and NN5) based on calcareous nannofossils were established in the Miocene Kopekli Formation. In order to achieve a worldwide biostratigraphic perspective based on dinoflagellate cysts, the present biozones were compared with those described from NW Europe (Denmark, Germany, the Netherlands), the East Coast of the US and Egypt. After calibration to the established Turkish foraminifera and nannofossils standard, the palynological analysis shows that the recorded dinoflagellate cysts events (e.g. FO of Labyrinthodinium truncatum, Cerebrocysta poulsenii and Unipontidinium aquaeductus and LO of Palaeocystodinium ventricosum) occurred chronostratigraphically earlier in SE Turkey than in NW Europe and on the East Coast of the US.	[Turkecan, Aksel Tugba; Isik, Ugras; Pinar, Mehtap; Cevik, Tugba] TP, Res & Dev Ctr, TR-06100 Ankara, Turkey; [Alay, Zeynep] TP, TR-06100 Ankara, Turkey; [Munsterman, Dirk] Earth Life & Social Sci Geol Survey Netherlands, Netherlands Org Appl Sci Res TNO, Princetonlaan 6,POB 80015, NL-3508 TA Utrecht, Netherlands; [Altiner, Demir] Middle East Tech Univ, Dept Geol Engn, TR-06531 Ankara, Turkey	Netherlands Organization Applied Science Research; Middle East Technical University	Türkecan, AT (通讯作者)，TP, Res & Dev Ctr, TR-06100 Ankara, Turkey.	atdinc@tp.gov.tr	ALTINER, Demir/ABA-3163-2020		Turkish Petroleum (TP) Research Center	Turkish Petroleum (TP) Research Center	The data presented in this study partly cover the first author's PhD thesis. This study was supported by Turkish Petroleum (TP) Research Center. We would like to thank them for permissions and financial support. 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J	Edwards, LE; Weems, RE; Carter, MW; Spears, DB; Powars, DS				Edwards, Lucy E.; Weems, Robert E.; Carter, Mark W.; Spears, David B.; Powars, David S.			The significance of dinoflagellates in the Miocene Choptank Formation beneath the Midlothian gravels in the southeastern Virginia Piedmont	STRATIGRAPHY			English	Article							ATLANTIC COASTAL-PLAIN; PASSIVE-MARGIN; UNITED-STATES; STRATIGRAPHY; PLIOCENE; ZONATION; DIATOMS; ORIGIN	The Fall Line (formally "Tidewater Fall Line") separates the more resistant igneous, metamorphic, and consolidated sedimentary rocks of the Piedmont from the typically unconsolidated deposits of the Coastal Plain of Virginia. Widespread but now discontinuous patches of a deeply weathered sand and gravel are found west of the Fall Line, capping the highest hilltops. Near the community of Midlothian, Virginia, the gravels are underlain by fine-grained marine silts that bear an informative assemblage of fossil dinoflagellate cysts (dinocysts). In situ dinocysts belong to middle Miocene zone DN7, which is calibrated to similar to 12-13 Ma. These deposits are assigned to the upper part of the Choptank Formation, which crops out similar to 25 km(15 mi) to the east at an elevation similar to 60m(200 ft) lower. The dinocyst assemblage suggests that the maximum extent of this Choptank transgression probably covered a significant expanse of the Virginia Piedmont. The Choptank marine silts constrain the age of the unconformably overlying Midlothian gravels to younger than the latter part of the middle Miocene. Previous work has indicated that these gravels also are older than the Pliocene Yorktown Formation. Rare, reworked dinocysts in these Choptank outcrops west of the Fall Line are sourced from older deposits of more than one age. The source could be older updip strata of the lower Eocene Nanjemoy Formation, now erosionally removed. Alternatively, the source could be material referable to the upper Eocene Exmore Formation that resulted from the Chesapeake Bay impact event.	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C	Supono; Bolch, C; Knowles, G		Arisuryanti, T; Maryani; Rohmah, Z; Hidayati, L; Aristya, GR		Supono; Bolch, Christopher; Knowles, Graeme			Pathological Alteration of Digestive Tissues in Blue Mussel (<i>Mytillus galloprovincialis</i>) Larvae Induced by <i>Alexandrium fundyense</i> Lysates	INVENTING PROSPEROUS FUTURE THROUGH BIOLOGICAL RESEARCH AND TROPICAL BIODIVERSITY MANAGEMENT	AIP Conference Proceedings		English	Proceedings Paper	5th International Conference on Biological Science (ICBS)	SEP 15-16, 2017	Univ Gadjah Mada, Fac Biol, Yogyakarta, INDONESIA	Univ Tun Hussein Onn Malaysia	Univ Gadjah Mada, Fac Biol	Alexandrium fundyense; blue mussel larvae; HAB; lysate; pathology	TOXIC DINOFLAGELLATE; HETEROCAPSA-CIRCULARISQUAMA; TAMARENSE; SCALLOP; CATENELLA; CULTURES; GROWTH; CYSTS	Bloom of toxic dinoflagellate, Alexandrium fundyense has inflicted significant economic loss of both wild fisheries and aquaculture farming. This toxic dinoflagellate is capable of producing extracellular (exudates) and intracellular toxic compound (lysates), causing mass mortality of shellfish in hatchery operation. Despite its significant impacts, there is lack of study to understand the toxicity mechanism and cellular effect of A. fundyense lysates on shellfish larvae. This study aimed to investigate pathological changes of digestive tissues in blue mussel (Mytilus galloprovincialis) larvae exposed to A. fundyense lysates. Blue mussel larvae were exposed to A. fundyense lysates at a bloom concentration of 1 500 cells ml(-1) and sampled for histological assessment at every 0 h, 3 h, 15 h, 24 h, and 48 h after exposure. This study found that pathological changes in digestive tissues occurred as early as 3 h after exposure. Pathological changes included cell vacuolation, necrosis, and cilial exfoliation of style sac. Of these changes, only the prevalence and intensity of cell necrosis increases with increasing exposure duration (from low at 3 h to 15 h to intermediate at 24 h to 48 h). The finding of this study suggests that early detection and appropriate mitigation of A. fundyense bloom is needed to minimize its impact on shellfish hatchery.	[Supono] Indonesian Inst Sci, Res Ctr Oceanog, LKBL Bitung LIPI, Sulawesi Utara, Indonesia; [Bolch, Christopher] Univ Tasmania, Inst Marine & Antarctic Studies, Launceston, Tas, Australia; [Knowles, Graeme] Dept Primary Ind Pk Waters & Environm, Anim Hlth Lab, Launceston, Tas, Australia	National Research & Innovation Agency of Indonesia (BRIN); Indonesian Institute of Sciences (LIPI); University of Tasmania	Supono (通讯作者)，Indonesian Inst Sci, Res Ctr Oceanog, LKBL Bitung LIPI, Sulawesi Utara, Indonesia.	supono@lipi.go.id	Bolch, Christopher/J-7619-2014; Knowles, Graeme/HNQ-4536-2023; Supono, Supono/JOJ-7375-2023	Supono, Supono/0000-0002-2747-3049	Australia Awards Scholarship; LKBL Bitung-LIPI	Australia Awards Scholarship; LKBL Bitung-LIPI	We would like to thank Australia Awards Scholarship for research funding support, LKBL Bitung-LIPI for travel fund support for the conference, spring bay seafood for providing larvae, and Institute for Marine and Antarctic Studies (IMAS) for providing space and equipment set up during the experiment.	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J	Wainman, CC; Hannaford, C; Mantle, D; McCabe, PJ				Wainman, C. C.; Hannaford, C.; Mantle, D.; McCabe, P. J.			Utilizing U-Pb CA-TIMS dating to calibrate the Middle to Late Jurassic spore-pollen zonation of the Surat Basin, Australia to the geological time-scale	ALCHERINGA			English	Article						U-Pb CA-TIMS; tuffs; palynostratigraphy; Surat Basin; Jurassic	SOUTHERN-HEMISPHERE; ZIRCON; BIOSTRATIGRAPHY; AGE; GEOCHRONOLOGY; QUEENSLAND; PRECISION; MARINE	Spore-pollen palynostratigraphy is commonly used to subdivide and correlate Jurassic continental successions in eastern Australia and thus aid the construction of geological models for the petroleum and coal industries. However, the current spore-pollen framework has only been tenuously calibrated to the geological time-scale. Age determinations are reliant on indirect correlations of ammonite and dinoflagellate assemblages from New Zealand, the North West Shelf of Australia and Southeast Asia to the standard European stages. New uranium-lead chemical abrasion thermal ionization mass spectrometry (U-Pb CA-TIMS) dates from 19 tuff beds in the Middle-Upper Jurassic Injune Creek Group of the Surat Basin enables regional spore-pollen palynostratigraphic zones to be precisely dated for the first time. These results show the base of the APJ4.2 and APJ4.3 subzones are similar in age to previous estimates (Middle Jurassic, Bathonian) from indirect palynostratigraphic correlation. However, the base of the APJ5 Zone and the APJ6.1 Subzone may be somewhat younger than previously estimated, possibly by as much as 2.5 and 4.2 Myrs, respectively. The continued utilization of U-Pb CA-TIMS dates will further refine the absolute ages of these zones, improve the inter- and intra-basinal correlation of Middle-Upper Jurassic strata in eastern Australian basins and greatly enhance intercontinental correlations.	[Wainman, C. C.; McCabe, P. J.] Univ Adelaide, Australian Sch Petr, Adelaide, SA 5005, Australia; [Hannaford, C.; Mantle, D.] MGPalaeo Pty Ltd, 5 Arvida St, Malaga, WA 6090, Australia	University of Adelaide	Wainman, CC (通讯作者)，Univ Adelaide, Australian Sch Petr, Adelaide, SA 5005, Australia.	carmine.wainman@adelaide.edu.au; carey.hannaford@mgpalaeo.com.au; dan.mantle@mgpalaeo.com.au; peter.mccabe@adelaide.edu.au		Wainman, Carmine/0000-0001-6375-1520	University of Adelaide	University of Adelaide	Carmine Wainman received a PhD scholarship from the University of Adelaide that covered most of the travel and analytical costs. Geoff Wood from Santos Limited kindly provided palynological summaries and range charts for the Pleasant Hills 25 well. We thank Robert Nicoll of Geoscience Australia for reviewing the manuscript prior to submission and John Backhouse for insightful discussions regarding the identification of thin-walled brackish-marginal marine dinoflagellate cysts. Jesse Vitacca from MGPalaeo kindly assisted with palynological processing. Stratabugs was used under licence to produce the palynological plots in the appendices.	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J	Akkiraz, MS; Kangal, Ö; Özgen Erdem, N; Büyükmeriç, Y; Dogruöz, C				Akkiraz, Mehmet Serkan; Kangal, Ozgen; Ozgen Erdem, Nazire; Buyukmeric, Yesim; Dogruoz, Cihan			Palaeontological evidence and sedimentary facies in a lower Miocene (Aquitanian) succession from the Bingol minibasin (Sivas Basin), Central Anatolia	TURKISH JOURNAL OF EARTH SCIENCES			English	Article						Sivas Basin; Miocene; palaeoecology; Central Anatolia; palynology; Mollusca	CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; TERTIARY ULUKISLA BASIN; MIDDLE MIOCENE; CENTRAL TURKEY; REGIONAL IMPLICATIONS; COEXISTENCE APPROACH; SOUTHERN TURKEY; ORGANIC FACIES; EVOLUTION; OLIGOCENE	The results of palaeontological (palynological and mollusc) and sedimentological analyses of the lower Miocene deposits from the Bingol minibasin, a part of the Sivas Basin, are exhibited to define the vertical shifts in sedimentation environments and plant covers, linking to eustasy. The presence of index species Corbulomya (Lentidium) aquitanica suggests an Aquitanian age for the studied succession, which can be divided into three informal units: a lower unit, a middle unit, and an upper unit. Fine-grained sediments of the lower unit were deposited in a low sea-level setting due to high quantities of terrestrial palynomorphs. This unit is overlain by the middle unit, coralgal limestone, which marks the first initiation of Aquitanian transgression. Continuing shallow marine settings in the upper unit gave rise to deposition of coarse to fine-grained sediments. Palynological data were recovered from the fine-grained sediments of the lower and upper units. A total of 35 spore and pollen taxa were recorded, including 2 spores from ferns, 5 gymnosperms, 26 angiosperms, 1 group of undifferentiated dinoflagellate cysts, and 1 fresh water alga of Botryococcus sp. The pollen spectrum is dominated by coniferous forest, mainly undifferentiated Pinaceae, and herbaceous communities including high quantities of Poaceae and Chenopodiaceae-Amaranthaceae, with minor contributions of Ephedra sp., Caryophyllaceae, and Asteraceae subf. Asteroidae. High sea-level conditions, which started with sedimentation of the middle unit, survived during the deposition of the upper unit due to being overwhelmingly dominated by dinocysts. Thermophile plants including Avicennia sp., Engelhardia sp., Myrica sp., Sapotaceae, Cyrillaceae-Clethraceae, and Reveesia sp. along with relatively high quantities of xerophytes and the quantitative palaeoclimate values imply a subtropical and dry palaeoclimate.	[Akkiraz, Mehmet Serkan] Dumlupinar Univ, Fac Engn, Dept Geol Engn, Kutahya, Turkey; [Kangal, Ozgen; Ozgen Erdem, Nazire] Cumhuriyet Univ, Dept Geol Engn, Fac Engn, Sivas, Turkey; [Buyukmeric, Yesim] Bulent Ecevit Univ, Dept Geol Engn, Fac Engn, Zonguldak, Turkey; [Dogruoz, Cihan] Dumlupinar Univ, Dept Min Engn, Fac Engn, Kutahya, Turkey	Dumlupinar University; Cumhuriyet University; Zonguldak Bulent Ecevit University; Dumlupinar University	Akkiraz, MS (通讯作者)，Dumlupinar Univ, Fac Engn, Dept Geol Engn, Kutahya, Turkey.	sakkiraz73@gmail.com	akkiraz, mehmet/ADP-2366-2022; dogruoz, cihan/KCJ-5619-2024	Buyukmeric, Yesim/0000-0003-2678-3907; dogruoz, cihan/0000-0002-7487-4822	Scientific and Technological Research Council of Turkey (TUBITAK) [109Y041]	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 No. 109Y041). The assistance provided by Mehmet Can Diyarbakirli, who took part in the fieldwork, is acknowledged. The authors would like to thank Ali Gurel, two anonymous reviewers, and the manuscript editor, Aysegul Yildiz, for their helpful comments.	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J. Earth Sci.		2018	27	5					329	348		10.3906/yer-1710-20	http://dx.doi.org/10.3906/yer-1710-20			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GV3AD		Bronze			2025-03-11	WOS:000445963200001
J	Gürgey, K; Bati, Z				Gurgey, Kadir; Bati, Zuhtu			Palynological and petroleum geochemical assessment of the Lower Oligocene Mezardere Formation, Thrace Basin, NW Turkey	TURKISH JOURNAL OF EARTH SCIENCES			English	Article						Thrace Basin; Lower Oligocene; Wetzeliella gochtii; transgression; regression; source rock	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; DEPOSITIONAL ENVIRONMENT; LOWER MIOCENE; EASTERN PARATETHYS; ORGANIC-MATTER; BLACK-SEA; SEQUENCE STRATIGRAPHY; MAIKOP SERIES; MOLASSE BASIN; SOURCE ROCKS	The Oligocene clastic sequence of the Mezardere Formation (MF) with laterally variable organic richness has long been known as a proven source of gas with minor oil accumulations across the Thrace Basin of northwest Turkey. However, based on well data for the thick MF, neither detailed work in relation to age dating and stratigraphy nor a close linkage between the depositional facies/ environments, organic richness/organic proxies, and cyclicity has been established yet. In the present study, the MF was informally subdivided into Lower MF (LMF) and Upper MF (UMF) based on the distinct differences in palynological and geochemical data. Based on the common occurrences of Glaphyrocysta cf. semitecta and absence of Wetzeliella gochtii, the LMF is considered to be deposited during the earliest Oligocene (? Pshekian) under the prevailing marine conditions. The UMF is characterized by a very rich and diverse dinocyst assemblage having abundant occurrences of age-diagnostic Wetzeliella gochtii and a Solenovian age is assigned. Common Pediastrum occurrences in the UMF may suggest fresh water input as is the case for many source rocks of the Central and Eastern Paratethys. The UMF shows the geochemical characteristics of a typical transgressive sequence such as higher TOC, hydrogen index (HI), and relative hydrocarbon potential (RHP) values than those for the regressive LMF. On the RHP basis, three short-term transgressive to regressive cycles are recognized in the entire MF in the wells studied. The early mature UMF samples showed a fair to good source rock potential (average TOC = 1.14 wt. %; HI = 283 mg oil/g TOC) and low to moderate genetic petroleum potential (GP = 3.65 mg oil/g rock) and source potential index (SPI = 1.44 t oil/m(2)). The LMF samples were not evaluated due to their apparently low TOC, HI, and S2 values. Better understanding of the MF will eventually aid a better understanding of the paleoenvironment of the Eastern Paratethys.	[Gurgey, Kadir] Near East Univ, Dept Petr & Nat Gas Engn, Mersin 10, Nicosia, Turkey; [Bati, Zuhtu] Turkish Petr Corp TPAO, Res & Dev Ctr, Ankara, Turkey	Near East University; Ministry of Energy & Natural Resources - Turkey; Turkish Petroleum Corporation (TPAO)	Bati, Z (通讯作者)，Turkish Petr Corp TPAO, Res & Dev Ctr, Ankara, Turkey.	bati@tpao.gov.tr		Bati, Zuhtu/0000-0002-4773-0663				Abouelresh MO, 2012, AAPG BULL, V96, P1, DOI 10.1306/04261110116; [Anonymous], 1990, GULF COAST ASS GEOL; BARKER C, 1974, AAPG BULL, V58, P2349; Barski M, 2010, GEOL CARPATH, V61, P121, DOI 10.2478/v10096-010-0005-4; BATI Z, 1996, PALYNOSTRATIGRAPHY C; Bati Z, 1993, 1947 TPAO; Bati Z, 2007, TURK STRAT COMM WORK, P14; Bati Z, 2007, MICROPALEONTOLOGY, V53, P249, DOI 10.2113/gsmicropal.53.4.249; Bati Z, 2015, REV PALAEOBOT PALYNO, V217, P9, DOI 10.1016/j.revpalbo.2015.03.002; 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, V56, P51, DOI 10.1016/j.orggeochem.2012.12.005; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; BURKAN K, 1992, P 9 PETR C TURK, P34; Coccioni R, 2008, GEOL SOC AM BULL, V120, P487, DOI 10.1130/B25988.1; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; CREANEY S, 1993, AAPG BULL, V77, P386; CURIALE JA, 1992, ORG GEOCHEM, V19, P53, DOI 10.1016/0146-6380(92)90027-U; Demaison G, 1994, AAPG MEMOIR, V60, P73; DEMAISON GJ, 1980, AAPG BULL, V64, P1179; Dybkjær K, 2004, REV PALAEOBOT PALYNO, V131, P201, DOI 10.1016/j.revpalbo.2004.03.006; Ediger V. 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J. Earth Sci.		2018	27	5					349	383		10.3906/yer-1710-24	http://dx.doi.org/10.3906/yer-1710-24			35	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	GV3AD		Bronze			2025-03-11	WOS:000445963200002
J	Duxbury, S				Duxbury, Stan			Berriasian to lower Hauterivian palynostratigraphy, UK onshore and Outer Moray Firth	MICROPALEONTOLOGY			English	Article						Palynological zonation; dinocysts; Berriasian; Valanginian; Hauterivian; Speeton; UKCS Outer Moray Firth	DINOFLAGELLATE CYSTS; NORTH-SEA; EISENACK 1958; NOV; SYSTEMATICS; AREA	Detailed palynofloral analysis of Lower Cretaceous sections at Speeton (northeast England) and in the UKCS Outer Moray Firth has involved 31 outcrop samples and over 1100 well samples from Golden Eagle Field (UKCS blocks 14/26a and 20/01), including extensive conventional core. Very close sampling, particularly within the Valanginian, has allowed some assessment of inter- and intra-species trends, some very short-lived and others of longer duration and the possible origins of several species are discussed. Paleoenvironmental change is seen as a possible stimulus to these evolutionary trends. The zonation scheme proposed by Duxbury (2001) has been re-visited and significantly refined. Recognition of additional marker events has allowed the further subdivision of several zones to sub-zonal level, allowing a better understanding of the stratigraphy, particularly of the Valanginian. Over 100 key palynofloral events have now been recognised between the top Berriasian and lower Hauterivian, including many first occurrences. One genus and twenty-one species of stratigraphically significant dinollagellate cysts are described as new. Eight new combinations have been effected and the diagnoses of one genus and three species have been emended. The very high resolution achievable by applying the relined scheme is clearly demonstrated in two transects across the Golden Eagle Field.	[Duxbury, Stan] Duxbury Stratig Consultants, Church Lane, Chester CH2 1DJ, Cheshire, England		Duxbury, S (通讯作者)，Duxbury Stratig Consultants, Church Lane, Chester CH2 1DJ, Cheshire, England.	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J	Milàn, J; Rasmussen, ES; Dybkær, K				Milan, Jesper; Rasmussen, Erik Skovbjerg; Dybkaer, Karen			A crocodilian coprolite from the lower Oligocene Viborg Formation of Sofienlund Lergrav, Denmark	BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK			English	Article						Coprolite; Palaeogene; Oligocene; vertebrate fauna; Denmark; Crocodilian	VERTEBRATE COPROLITE; INTERNAL ARCHITECTURE; DINOSAUR COPROLITES; PREY REMAINS; STEVNS KLINT; MORPHOLOGY; CLASSIFICATION; NEOGENE; BASIN; LAND	A large, well-preserved vertebrate coprolite found in the clay pit Sofienlund Lergrav, Jylland, is identified as crocodilian due to its size and morphology. The coprolite consists of several concentric layers wrapped around a more homogeneous core. Weak constriction marks are present on the surface. Dinoflagellate cyst contents of the coprolite indicate a mid-Lutetian to earliest Rupelian (middle Eocene to earliest Oligocene) age, which at Sofienlund Lergrav places it within the lower Oligocene Viborg Formation. The coprolite can thus be dated as approximately 33-34 Ma old. The Viborg Formation in Denmark represents a period with deposition of hemipelagic marine clay and formation of glaucony. The nearest shoreline was located c. 200 km north of the location of the present day Sofienlund Lergrav, and the climate was humid, warm-temperate to sub-tropical. The presence of a crocodilian coprolite is an important addition to the sparse Oligocene vertebrate fauna of Denmark, which previously only consisted of sharks and cetaceans.	[Milan, Jesper] Ostsjaellands Museum, Geomuseum Faxe, Ostervej 2, DK-4640 Faxe, Denmark; [Milan, Jesper] Nat Hist Museum Denmark, Oster Voldgade 5-7, DK-1465 Copenhagen K, Denmark; [Rasmussen, Erik Skovbjerg; Dybkaer, Karen] Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Milàn, J (通讯作者)，Ostsjaellands Museum, Geomuseum Faxe, Ostervej 2, DK-4640 Faxe, Denmark.	jesperm@oesm.dk; esr@geus.dk; kd@geus.dk	Dybkjær, Karen/G-5223-2018					Adolfssen JS, 2017, B GEOL SOC DENMARK, V65; Bennett MR, 1996, PALAEOGEOGR PALAEOCL, V121, P331, DOI 10.1016/0031-0182(95)00071-2; Bonde N., 2008, DANEKRAE DANMARKS BE; Buckland William., 1835, T GEOLOGICAL SOC LON, V3, P223; Campbell HA, 2010, J ANIM ECOL, V79, P955, DOI 10.1111/j.1365-2656.2010.01709.x; Chame M, 2003, MEM I OSWALDO CRUZ, V98, P71, DOI 10.1590/S0074-02762003000900014; Chin K, 2007, PALAIOS, V22, P554, DOI 10.2110/palo.2006.p06-087r; Chin Karen, 2002, Paleontological Society Papers, V8, P43; CHRISTENSEN L, 1973, Bulletin of the Geological Society of Denmark, V22, P283; Eriksson ME, 2011, LETHAIA, V44, P455, DOI 10.1111/j.1502-3931.2010.00257.x; FISHER DC, 1981, PALEOBIOLOGY, V7, P262, DOI 10.1017/S0094837300004048; Hakansson E., 1992, GEOLOGISK KORT DANSK; Hansen BB, 2016, GEOL SOC SPEC PUBL, V434, P49, DOI 10.1144/SP434.12; Hansen J.P.V., 2004, GEOLOGICAL SOC MEMOI, V29, P83; HEILMANN-CLAUSEN C, 1985, Bulletin of the Geological Society of Denmark, V33, P287; Heilmann-Clausen C, 1997, Tertiary Research, V18, P31; Hoch Ella, 2000, Historical Biology, V14, P67; Hunt Adrian P., 2012, Bulletin of the New Mexico Museum of Natural History and Science, P137; Hunt Adrian P., 1994, P221; Hunt Adrian R., 2012, Bulletin of the New Mexico Museum of Natural History and Science, P5; Japsen P, 2010, PETROL GEOL CONF P, P979, DOI 10.1144/0070979; Jarsve EM, 2014, INT AS SED, V46, P417; Larsson LM, 2011, PALAEOGEOGR PALAEOCL, V309, P161, DOI 10.1016/j.palaeo.2011.05.003; Lewin RalphA., 1999, MERDE EXCURSIONS SCI; MCALLISTER J A, 1985, University of Kansas Paleontological Contributions Paper, P1; Milan J., 2010, CROCODILE TRACKS TRA, V51, P15; Milan Jesper, 2016, Bulletin of the New Mexico Museum of Natural History and Science, P159; Milan Jesper, 2015, Bulletin of the New Mexico Museum of Natural History and Science, P227; Milan Jesper, 2012, Bulletin of the New Mexico Museum of Natural History and Science, P235; Milan Jesper, 2012, Bulletin of the New Mexico Museum of Natural History and Science, P65; Milan Jesper, 2012, Bulletin of the New Mexico Museum of Natural History and Science, P99; Milan Jesper, 2010, Bulletin of the New Mexico Museum of Natural History and Science, V51, P215; Nielsen OB, 2015, J SEDIMENT RES, V85, P562, DOI 10.2110/jsr.2015.40; Northwood C, 2005, PALAEONTOLOGY, V48, P49, DOI 10.1111/j.1475-4983.2004.00432.x; PEDERSEN G K, 1983, Bulletin of the Geological Society of Denmark, V32, P43; Prasad V, 2005, SCIENCE, V310, P1177, DOI 10.1126/science.1118806; Rasmussen E. 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J	Luo, ZH; Lim, ZF; Mertens, KN; Gurdebeke, P; Bogus, K; Carbonell-Moore, MC; Vrielinck, H; Leaw, CP; Lim, PT; Chomérat, N; Li, XT; Gu, HF				Luo, Zhaohe; Lim, Zhen Fei; Mertens, Kenneth Neil; Gurdebeke, Pieter; Bogus, Kara; Carbonell-Moore, M. Consuelo; Vrielinck, Henk; Leaw, Chui Pin; Lim, Po Teen; Chomerat, Nicolas; Li, Xintian; Gu, Haifeng			Morpho-molecular diversity and phylogeny of <i>Bysmatrum</i> (Dinophyceae) from the South China Sea and France	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						benthic dinoflagellate; biogeography; Bysmatrum granulosum; Bysmatrum gregarium; Bysmatrum subsalsum; eyespot; molecular phylogeny	TIDAL POOL DINOFLAGELLATE; SP. NOV. DINOPHYCEAE; RDNA-BASED PHYLOGENY; GULF-OF-MEXICO; ALEXANDRIUM DINOPHYCEAE; BENTHIC DINOFLAGELLATE; SUBSALSUM DINOPHYCEAE; PERIDINIUM-GREGARIUM; ELECTRON-MICROSCOPY; SEQUENCE DATA	The dinoflagellate genus Bysmatrum encompasses five epibenthic or tide-pool species and has been characterized by separated anterior intercalary plates. In the present study, we obtained six strains of Bysmatrum from the South China Sea and French Atlantic coast by isolating single cells/cysts from plankton and sediment samples. All strains were examined with light microscopy and scanning electron microscopy. Based on morphological observations, three strains were identified as Bysmatrum subsalsum, characterized by the elongated and rectangular first and a hexagonal second anterior intercalary plate. They differ from each other in the number of sulcal lists and the configuration of the first anterior intercalary plate. One strain was identified as Bysmatrum gregarium and the other two as Bysmatrum granulosum. The cyst-theca relationship of B. subsalsum from the French Atlantic was established by incubation of the cyst, and the geochemical composition of the cyst wall was measured through micro-Fourier transform infrared spectroscopy. Bysmatrum subsalsum from Malaysia shows a bright red stigma in the sulcal area under light microscopy, which was confirmed with transmission electron microscopy: it was identified as a type B eyespot. Small subunit ribosomal DNA (SSU rDNA), partial large subunit ribosomal DNA (LSU rDNA) and internal transcribed spacer (ITS) sequences were obtained from all six strains. The maximum likelihood and Bayesian inference analysis based on concatenated SSU, ITS and LSU sequences revealed that Bysmatrum is monophyletic and nested within Peridiniales. Our strains of B. subsalsum form a new ribotype in the molecular phylogeny (designated as ribotype B). The genetic distance based on ITS sequences among Bysmatrum species ranged from 0.34 to 0.47 and those genetic distances at the intraspecific level of B. subsalsum could reach 0.41, supporting the possibility ofhidden crypticity within B. subsalsum.	[Luo, Zhaohe; Li, Xintian; Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Lim, Zhen Fei; Leaw, Chui Pin; Lim, Po Teen] Univ Malaya, Inst Ocean & Earth Sci, Bachok 16310, Kelantan, Malaysia; [Mertens, Kenneth Neil; Chomerat, Nicolas] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France; [Gurdebeke, Pieter] Univ Ghent, Dept Geol, Res Unit Palaeontol, Krijgslaan 281,S8, B-9000 Ghent, Belgium; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA; [Carbonell-Moore, M. Consuelo] Oregon State Univ, Coll Agr Sci, Dept Bot & Plant Pathol, 2082 Cordley Hall, Corvallis, OR 97331 USA; [Vrielinck, Henk] Univ Ghent, Dept Solid State Sci, Krijgslaan 281,S1, B-9000 Ghent, Belgium	Third Institute of Oceanography, Ministry of Natural Resources; Universiti Malaya; Ifremer; Ghent University; Texas A&M University System; Texas A&M University College Station; Oregon State University; Ghent University	Gu, HF (通讯作者)，SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China.; Mertens, KN (通讯作者)，IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France.	kenneth.mertens@ifremer.fr; guhaifeng@tio.org.cn	Luo, Zhaohe/ITT-7163-2023; Vrielinck, Henk/M-8367-2016; Mertens, Kenneth/AAO-9566-2020; Li, Xintian/HGA-0346-2022; Leaw, Chui Pin/F-5220-2012; Gurdebeke, Pieter/AAY-7059-2020; Lim, Po Teen/C-9758-2013; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Lim, Po Teen/0000-0003-2823-0564; Luo, Zhaohe/0000-0001-8662-2414; Vrielinck, Henk/0000-0003-4861-9630; Gurdebeke, Pieter R./0000-0003-1425-8515; Gu, Haifeng/0000-0002-2350-9171; Mertens, Kenneth/0000-0003-2005-9483; Chomerat, Nicolas/0000-0001-9691-6344; Bogus, Kara/0000-0003-4690-0576	National Key Research and Development Program of China [2016YFE0202100]; National Natural Science Foundation of China [41676117]; National Science Foundation [OCE - 1326927]; China-ASEAN Maritime Cooperation Fund	National Key Research and Development Program of China(National Key Research & Development Program of China); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); National Science Foundation(National Science Foundation (NSF)); China-ASEAN Maritime Cooperation Fund	This work was supported by the National Key Research and Development Program of China (2016YFE0202100), National Natural Science Foundation of China (41676117) and China-ASEAN Maritime Cooperation Fund. 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J. Phycol.		2018	53	3					318	335		10.1080/09670262.2018.1449014	http://dx.doi.org/10.1080/09670262.2018.1449014			18	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	GQ7TI		Green Published			2025-03-11	WOS:000441948900007
J	Moestrup, O; Nicholls, KH; Daugbjerg, N				Moestrup, Ojvind; Nicholls, Kenneth H.; Daugbjerg, Niels			Studies on woloszynskioid dinoflagellates IX: ultrastructure, cyst formation and phylogeny of the "red-snow' alga <i>Borghiella pascheri</i> (Suchlandt) Moestrup (= <i>Glenodinium pascheri, Woloszynskia pascheri, Gyrodinium nivalis</i>)	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Borghiella pascheri; "red snow' dinoflagellates; phylogeny; taxonomy; ultrastructure	FRESH-WATER DINOFLAGELLATE; LSU RDNA; SP NOV.; ELECTRON-MICROSCOPY; LAKE TOVEL; GEN.; DINOPHYCEAE; LIGHT; SANGUINEA	Red snow caused by dinoflagellates is a phenomenon rarely reported, described from the European Alps from 1914 onwards, and subsequently observed outside Europe on several occasions in Ontario, Canada. Considerable taxonomic confusion exists regarding the identity of the organism(s) causing red snow, but the most recent occurrence in 2016 in Ontario has now allowed detailed studies, including LM, SEM, TEM and molecular sequencing of the causative species. We conclude that the two species originally described as the cause of red snow, Glenodinium pascheri and Gyrodinium nivale, are synonymous and that the appropriate name for the organism is Borghiella pascheri (syn. Woloszynskia pascheri) as suggested by Moestrup & Calado in the recent volume of the Susswasserflora. The central part of Borghiella pascheri cells is tomato red and filled with numerous organelles, whose ultrastructure indicates modified chloroplasts. Lack of cultures has prevented chemical characterization of the red pigment. Formation of temporary cysts was common in the samples. Transformation of the motile cells into temporary cysts was followed in detail, and the cysts were shown to be surrounded by the fused inner membranes of the amphiesmal vesicles, which became the cell membrane of the cysts, covered by the fused pellicle precursors. The cell membrane from the motile cell was discarded together with the outer amphiesmal vesicle membrane and the thin thecal plates, and the temporary cysts were therefore not surrounded by any pattern of vesicles. Sexual reproduction resulted in the formation of hypnozygotes. Although the species possessed several unusual features, DNA sequencing showed it to belong to Borghiella. The culture established in 1965 from the Botanical Garden in Gottingen, Germany and generally identified as Woloszynskia pascheri belongs to a separate species of Borghiella, to be described separately.The occurrence of red snow caused by dinoflagellates is discussed.	[Moestrup, Ojvind; Daugbjerg, Niels] Univ Copenhagen, Dept Biol, Univ Pk 4, DK-2100 Copenhagen O, Denmark; [Nicholls, Kenneth H.] S 15 Concess 1, RR 1, Sunderland, ON LOC 1HO, Canada	University of Copenhagen	Moestrup, O (通讯作者)，Univ Copenhagen, Dept Biol, Univ Pk 4, DK-2100 Copenhagen O, Denmark.	moestrup@bio.ku.dk	Daugbjerg, Niels/D-3521-2014	Daugbjerg, Niels/0000-0002-0397-3073	Villum-Kann Rasmussen Foundation; Carlsberg Foundation [2012_01_0509]; Brodrene Hartmann [A22920]	Villum-Kann Rasmussen Foundation; Carlsberg Foundation(Carlsberg Foundation); Brodrene Hartmann	This work was supported by the Villum-Kann Rasmussen Foundation [Number no longer available]; Carlsberg Foundation [2012_01_0509]; Brodrene Hartmann [A22920];	Boutrup PV, 2016, PHYCOLOGIA, V55, P147, DOI 10.2216/15-138.1; Craveiro SC, 2013, PHYCOLOGIA, V52, P488, DOI 10.2216/13-152.1; Daugbjerg N, 2014, EUR J PHYCOL, V49, P436, DOI 10.1080/09670262.2014.969781; DODGE J D, 1970, Botanical Journal of the Linnean Society, V63, P53, DOI 10.1111/j.1095-8339.1970.tb02302.x; Doyle JJ., 1987, PHYTOCHEM B BOT SOC, V19, P11, DOI DOI 10.1016/0031-9422(80)85004-7; Flaim G, 2004, PHYCOLOGIA, V43, P737, DOI 10.2216/i0031-8884-43-6-737.1; Frassanito R, 2006, BIOCHEM SYST ECOL, V34, P843, DOI 10.1016/j.bse.2006.05.013; GERRATH JF, 1974, CAN J BOT, V52, P683, DOI 10.1139/b74-086; Gunning B.E.S., 1975, PLANT CELL BIOL ULTR; Hansen G, 2003, HARMFUL ALGAE, V2, P317, DOI 10.1016/S1568-9883(03)00060-X; Hansen G, 2018, PROTIST, V169, P280, DOI 10.1016/j.protis.2018.02.003; Hansen G, 2011, PHYCOLOGIA, V50, P583, DOI 10.2216/11-11.1; Kusel-Fetzmann E., 1979, Monographiae Biologicae, V37, P171; Lindberg K, 2005, PHYCOLOGIA, V44, P416, DOI 10.2216/0031-8884(2005)44[416:SOWDIW]2.0.CO;2; LINDEMANN E., 1928, ARCH PROTISTENK, V63, P259; Lindemann E., 1929, Archiv fuer Protistenkunde Jena, V68, P1; Loeblich A.R. 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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.			Species diversity and abundance of dinoflagellate resting cysts seven months after a bloom of <i>Alexandrium catenella</i> in two contrasting coastal systems of the Chilean Inland Sea	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Alexandrium catenella; dinoflagellate cysts; Chilean Inland Sea; cyst beds; oceanic and estuarine systems; Protoceratium reticulatum	SOUTHERN CHILE; KOFOID BALECH; MICROSATELLITE MARKERS; SPATIAL-DISTRIBUTION; COMPLEX DINOPHYCEAE; GENETIC DIVERSITY; SEDIMENTS; GERMINATION; TAMARENSE; DYNAMICS	In Chile, 90% of the fish farms and major natural shellfish beds are located in the region surrounding the Inland Sea, where over the last few decades harmful phytoplankton blooms have often been observed. The onset and recurrence of bloom events are often related to the resuspension and germination of resting cysts that have accumulated in the sediments. The degree of cyst settling, accumulation and germination is highly variable between areas and depends on physical and environmental factors. To learn how differences in oceanographic exposure, amount of river runoff and bathymetry affect dinoflagellate cyst deposition, we examined the diversity and abundance of dinoflagellate resting cysts from two hydrographically contrasting coastal areas (oceanic Guaitecas Archipelago and estuarine Pitipalena Fjord) of the Chilean Inland Sea in September 2006, seven months after a bloom of Alexandrium catenella, a producer of paralytic shellfish toxin. Cyst species diversity consisted of 18 taxa, including A. catenella and the noxious species Protoceratium reticulatum, both of which have caused blooms in the study area. Our results revealed significant differences between the two study sites in terms of the abundance and diversity of resting cysts, suggesting that in the specific case of A. catenella, only Guaitecas stations have potential for cyst accumulation and successful growth of cells. However, there was no evidence of long-term resting cyst beds of A. catenella at either study site.	[Diaz, Patricio A.] Univ Los Lagos, Ctr I Mar, Puerto Montt 557, Chile; [Diaz, Patricio A.; Molinet, Carlos; Diaz, Manuel] Univ Austral Chile, Programa Invest Pesquera, POB 1327,Los Pinos S-N, Balneario Pelluco, Puerto Montt, Chile; [Diaz, Patricio A.; Molinet, Carlos; Diaz, Manuel] Univ Austral Chile, Inst Acuicultura, POB 1327,Los Pinos S-N, Balneario Pelluco, Puerto Montt, Chile; [Seguel, Miriam; Labra, Gissela] Univ Austral Chile, Ctr Reg Anal Recursos & Medio Ambiente CERAM, Los Pinos S-N, Balneario Pelluco, Puerto Montt, Chile; [Labra, Gissela] Inst Fomento Pesquero IFOP, Balmaceda 252, Puerto Montt, Chile; [Figueroa, Rosa I.] Ctr Oceanog Vigo, IEO, Subida Radio Faro 50, Vigo 36390, Spain; [Figueroa, Rosa I.] Lund Univ, Dept Biol, Aquat Ecol, S-22362 Lund, Sweden	Universidad de Los Lagos; Universidad Austral de Chile; Universidad Austral de Chile; Universidad Austral de Chile; Instituto de Fomento Pesquero (Valparaiso); Spanish Institute of Oceanography; Lund University	Díaz, PA (通讯作者)，Univ Los Lagos, Ctr I Mar, Puerto Montt 557, Chile.; Díaz, PA (通讯作者)，Univ Austral Chile, Programa Invest Pesquera, POB 1327,Los Pinos S-N, Balneario Pelluco, Puerto Montt, Chile.; Díaz, PA (通讯作者)，Univ Austral Chile, Inst Acuicultura, POB 1327,Los Pinos S-N, Balneario Pelluco, Puerto Montt, Chile.	patricio.diaz@ulagos.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	Chilean National Commission for Scientific and Technological Research (CONICYT + PAI/CONCURSO NACIONAL INSERCION EN LA ACADEMIA CONVOCATORIA 2016) [79160065]; FORMAS (Sweden)	Chilean National Commission for Scientific and Technological Research (CONICYT + PAI/CONCURSO NACIONAL INSERCION EN LA ACADEMIA CONVOCATORIA 2016); FORMAS (Sweden)(Swedish Research Council Formas)	Patricio A. Diaz is funded by the Chilean National Commission for Scientific and Technological Research (CONICYT + PAI/CONCURSO NACIONAL INSERCION EN LA ACADEMIA CONVOCATORIA 2016, 79160065). Rosa I. Figueroa is funded by FORMAS (Sweden).	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Nelson, 1995, Revista de Biologia Marina, V30, P207; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; Varela D, 2012, HARMFUL ALGAE, V15, P8, DOI 10.1016/j.hal.2011.10.029	50	17	17	3	17	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0967-0262	1469-4433		EUR J PHYCOL	Eur. J. Phycol.		2018	53	3					410	421		10.1080/09670262.2018.1455111	http://dx.doi.org/10.1080/09670262.2018.1455111			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	GQ7TI		Bronze			2025-03-11	WOS:000441948900013
J	Riding, JB; Head, MJ				Riding, James B.; Head, Martin J.			Preparing photographic plates of palynomorphs in the digital age	PALYNOLOGY			English	Article						Imaging; microscopy; photographic plates; photography; presentation of images; production guide	RAYNAUD 1978 LENTIN; DINOFLAGELLATE CYST; PHASE-CONTRAST; MIDDLE MIOCENE; FOSSILS; MORPHOLOGY; REVISION; PLIOCENE; LESCHIK; INDEX	It is essential that palynologists adequately and effectively illustrate the specimens they study. The best way to do this for formal publication is to prepare plates' (montages) of photomicrographs. This now somewhat arcane term originated as a reference to the use of copper/steel and then glass plates in pre-film photography. In order to maximise visual impact and information, plates of palynomorphs should be prepared with utmost care. If assembled so that, for example, the images are arranged neatly with consistent orientations, and depict the best preserved and most representative specimens available with minimum extraneous palynodebris, the plate will have enhanced aesthetic appeal and, crucially, the scientific significance of the association being illustrated will be greatly enhanced. Specifically, the material will be effective as an identification guide, and facilitate further interpretations. Plates today are assembled digitally; accordingly, the user must have access to suitable software, and be able to use it effectively.	[Riding, James B.] British Geol Survey, Environm Sci Ctr, Keyworth NG12 5GG, Notts, England; [Head, Martin J.] Brock Univ, Dept Earth Sci, 1812 Sir Isaac Brock Way, St Catharines, ON L2S 3A1, Canada	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Brock University	Riding, JB (通讯作者)，British Geol Survey, Environm Sci Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk			Natural Sciences and Engineering Research Council of Canada; NERC [bgs05017] Funding Source: UKRI	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	Robert A. Fensome (Geological Survey of Canada, Dartmouth, Nova Scotia), Clinton B. Foster (Geoscience Australia, Canberra, ACT, Australia), Jan A.I. Hennissen (British Geological Survey, Nottingham, UK) and Geoffrey Playford (University of Queensland, Brisbane, Queensland, Australia) are all warmly thanked for their incisive and perceptive comments on early drafts of this article. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). Martin J. Head acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant.	Abramowitz M, 2017, THE MICROSCOPY; ANDERSON ROGER Y., 1958, MICROPALEONTOLOGY, V4, P205, DOI 10.2307/1484306; [Anonymous], VERHANDELINGEN KONIN; [Anonymous], 1963, Palaeontology; [Anonymous], 1980, Special Papers in Palaeontology; [Anonymous], 1999, Fossil Plants and spores: modern techniques; [Anonymous], 1965, HDB PALEONTOLOGICAL; [Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1996, Palynology: principles and applications; [Anonymous], 1977, J AUSTR GEOLOGY GEOP; Balme B.E., 1957, Coal Research Section T.C. 25; Barss M. 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D., 1976, Geoscience and Man, V15, P51; Williams GL, 2015, PALYNOLOGY, V39, P289, DOI 10.1080/01916122.2014.993888; Wilson GJ., 1988, NZ GEOLOGICAL SURVEY, V57, P96; Wilson L. R., 1960, Oklahoma Geology Notes, V20, P101; WILSON L. R., 1965, OKLA GEOL NOTES, V25, P130; Wood Gordon D., 1996, Palynology, V20, P177; Wood Gordon D., 1994, Palynology, V18, P195; Wood Gordon D., 1991, Palynology, V15, P181; Zernike F, 1942, PHYSICA, V9, P686, DOI 10.1016/S0031-8914(42)80035-X; Zernike F, 1942, PHYSICA, V9, P974, DOI 10.1016/S0031-8914(42)80079-8	116	15	16	0	3	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2018	42	3					354	365		10.1080/01916122.2017.1364052	http://dx.doi.org/10.1080/01916122.2017.1364052			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	GO5JO					2025-03-11	WOS:000440057100005
J	Nohr-Hansen, H; Costa, LI; Pearce, MA; Alsen, P				Nohr-Hansen, Henrik; Costa, Lucy I.; Pearce, Martin A.; Alsen, Peter			New Albian to Cenomanian (Cretaceous) dinoflagellate cyst taxa of ovoidinioid affinities from East Greenland, the Barents Sea and England	PALYNOLOGY			English	Article						Upper Albian; Lower Cenomanian; dinoflagellate cysts; Ovoidinioideae; new species; new genera; systematics		Palyno-biostratigraphical studies of upper Albian-Lower Cenomanian successions from East Greenland, the south-western Barents Sea and south-eastern England have revealed new dinoflagellate cyst taxa of clear or questioned ovoidinioid affinities. This paper describes the new genus Sindridinium, four new species - Ovoidinium epelidosphaeroides sp. nov., Epelidosphaeridia manifesta sp. nov., Sindridinium borealis gen. et sp. nov. and Sindridinium anaanae gen. et sp. nov. - and proposes a new combination, Sindridinium? torulosa comb. nov. (formerly Canningia torulosa). The genus Epelidosphaeridia is emended based on features seen in E.manifesta sp. nov., which demonstrate peridiniacean affinities and support inclusion in the Ovoidinioideae. Morphological gradations between Epelidosphaeridia spinosa, E. manifesta sp. nov. and Ovoidinium epelidosphaeroides sp. nov., suggest close phylogenetic relationships, also postulated between Sindridinium? torulosa comb. nov., S. borealis gen. et sp. nov. and S. anaanae gen. et sp. nov. The stratigraphic ranges of the taxa described are calibrated to known dinoflagellate markers and mid-Cretaceous ammonites.	[Nohr-Hansen, Henrik; Alsen, Peter] Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Pearce, Martin A.] Evolut Appl Ltd, Farringdon GL7 3QQ, Glos, England	Geological Survey Of Denmark & Greenland	Nohr-Hansen, H (通讯作者)，Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	hnh@geus.dk	Nohr-Hansen, Henrik/G-9058-2018; Alsen, Peter/F-4849-2017	Nohr-Hansen, Henrik/0000-0002-9291-8104; Alsen, Peter/0000-0001-6218-9054; Pearce, Martin/0000-0001-7856-1076				[Anonymous], REPORT SERIES; [Anonymous], 2014, B CAN PETROL GEOL, DOI DOI 10.2113/GSCPGBULL.62.4.261; [Anonymous], 1981, Report Series BI-R-81-12; [Anonymous], 1985, Canadian Technical Report of Hydrography and Ocean Sciences; [Anonymous], 1993, GRONL GEOL UNDERS B; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; Bujak J.P, 1983, AM ASS STRATIGRAPHIC, V13, P203; Cookson I. C., 1964, Palaeontology, V1, P37; Cookson I. C., 1961, Proceedings of the Royal Society of Victoria N S, V74, P69; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; Costa L.I., 1992, P99; Costa LI, 1985, 3 INT C MOD FOSS DIN; Davey R.J., 1973, REV ESP MICROPALEONT, V5, P173; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; DAVEY R.J., 1969, B BRIT MUS NAT HIST, V17, P103, DOI DOI 10.5962/P.313834; Evitt W.R., 1985, Sporopollenin dinoflagellate cysts: their morphology and interpretation, P333; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R.A., 2008, DINOFLAJ2, Version 1; Fensome RA, 2009, J SYST PALAEONTOL, V7, P1, DOI 10.1017/S1477201908002538; Hansen G, 2007, J LIMNOL, V66, P107, DOI 10.4081/jlimnol.2007.107; HELENES J, 1983, MICROPALEONTOLOGY, V29, P255, DOI 10.2307/1485733; Jarvis I, 2006, GEOL MAG, V143, P561, DOI 10.1017/S0016756806002421; Lentin JK., 1989, American Association of Stratigraphic Palynologists, Contributions Ser, V20, P473; MORGAN R., 1980, GEOLOGICAL SURVEY NE, V18, P1; Nohr-Hansen H, 2012, REV PALAEOBOT PALYNO, V178, P59, DOI 10.1016/j.revpalbo.2012.03.009; Norris G., 1978, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V156, P1; Ogg JG, 2016, CONCISE GEOLOGIC TIME SCALE 2016, P1; Radmacher W, 2014, MAR PETROL GEOL, V57, P109, DOI 10.1016/j.marpetgeo.2014.04.008; Singh C., 1983, ALBERTA RES COUNCIL, V44, P322; Stover L.E., 1978, Analyses of Pre-Pleistocene Organic-Walled Dinoflagellates, V15; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Williams G.L., 2017, AM ASS STRATIGRAPHIC, V2; ZIPPI PA, 1990, CAN J EARTH SCI, V27, P306, DOI 10.1139/e90-029	33	9	9	1	1	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2018	42	3					366	391		10.1080/01916122.2017.1351006	http://dx.doi.org/10.1080/01916122.2017.1351006			26	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	GO5JO					2025-03-11	WOS:000440057100006
J	Uzar, S; Aydin, H; Yurur, EE				Uzar, Serdar; Aydin, Hilal; Yurur, Emine Erdem			DINOFLAGELLATE CYST STUDIES IN THE SEDIMENTS OF TURKISH COASTAL WATERS AND FUTURE ASPECTS	FRESENIUS ENVIRONMENTAL BULLETIN			English	Article						Ecology; phytoplankton; dinoflagellate; resting cyst; sediment; biodiversity; indicator	RECENT MARINE-SEDIMENTS; HARMFUL ALGAL BLOOMS; BLACK-SEA CORRIDOR; SURFACE SEDIMENTS; IZMIR BAY; AEGEAN SEA; GONYAULAX-POLYEDRA; SP-NOV; ASSEMBLAGES; MARMARA	Marine organisms provide a valuable source of knowledge regarding how the marine ecosystem works. Studies of phytoplankton ecology and their dynamics offer a great opportunity for understanding these ecosystems. Dinoflagellates are a major part of marine phytoplankton and some dinoflagellates are able to produce resting cysts, which are composed of organic polymers that are highly resistant. These cysts are usually preserved very well in marine sediments. The number of studies on dinoflagellate cysts in the world's oceans is gradually increasing and these studies have become more detailed and multidisciplinary. Studies on dinoflagellate cysts in sediments have undergone a very important development in recent years, both in Turkish coastal waters as well as in the world's oceans. Here, we review the aims of the existing dinoflagellate cysts studies and summarise their results. We also give different future perspectives so as to contribute to the dinoflagellate cysts studies from Turkish coastal waters.	[Uzar, Serdar; Aydin, Hilal; Yurur, Emine Erdem] Manisa Celal Bayar Univ, Biol Dept, Fac Sci & Arts, Campus Martyr Prof Dr Ilhan Varank, TR-45140 Manisa, Turkey	Celal Bayar University	Uzar, S (通讯作者)，Manisa Celal Bayar Univ, Biol Dept, Fac Sci & Arts, Campus Martyr Prof Dr Ilhan Varank, TR-45140 Manisa, Turkey.	uzarserdar@yahoo.com.tr	Uzar, Serdar/G-9956-2014					Aydin H., 2013, Journal of Fisheries and Aquatic Sciences (Su Urunleri Dergisi), V30, P109, DOI 10.12714/egejfas.2013.30.3.04; Aydin H, 2015, TURK J FISH AQUAT SC, V15, P543, DOI 10.4194/1303-2712-v15_2_42; Aydin H, 2015, FRESEN ENVIRON BULL, V24, P4789; Aydin H, 2015, MAR POLLUT BULL, V94, P144, DOI 10.1016/j.marpolbul.2015.02.038; 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; Balkis N, 2016, PHYCOLOGIA, V55, P187, DOI 10.2216/15-93.1; Bringué M, 2013, MAR MICROPALEONTOL, V100, P34, DOI 10.1016/j.marmicro.2013.03.007; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; DALE B, 1978, OCEANUS, V21, P41; 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; Fujii R, 2006, J PLANKTON RES, V28, P131, DOI 10.1093/plankt/fbi106; Giannakourou A, 2005, CONT SHELF RES, V25, P2585, DOI 10.1016/j.csr.2005.08.003; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; Head M.J., 1996, Palynology: Principles and Applications, P1197; Joyce LB, 2005, HARMFUL ALGAE, V4, P309, DOI 10.1016/j.hal.2004.08.001; Koray T., 2004, HARMFUL ALGAE, P335; Lacasse O, 2013, MAR POLLUT BULL, V66, P230, DOI 10.1016/j.marpolbul.2012.10.016; Limoges A, 2015, J PHYCOL, V51, P211, DOI 10.1111/jpy.12257; Liu DY, 2013, MAR ECOL PROG SER, V475, P1, DOI 10.3354/meps10234; Liu DY, 2012, MAR MICROPALEONTOL, V84-85, P1, DOI 10.1016/j.marmicro.2011.11.001; Londeix L, 2009, REV PALAEOBOT PALYNO, V158, P52, DOI 10.1016/j.revpalbo.2009.07.004; Luo ZH, 2016, EUR J PHYCOL, V51, P188, DOI 10.1080/09670262.2015.1120348; Marret F, 2009, QUATERN INT, V197, P72, DOI 10.1016/j.quaint.2007.01.010; McCarthy FMG, 2011, REV PALAEOBOT PALYNO, V166, P46, DOI 10.1016/j.revpalbo.2011.04.008; Mertens KN, 2014, GEOLOGY, V42, P531, DOI 10.1130/G35456.1; Mertens KN, 2015, J PHYCOL, V51, P560, DOI 10.1111/jpy.12304; Mertens KN, 2012, QUATERNARY SCI REV, V39, P45, DOI 10.1016/j.quascirev.2012.01.026; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Mudie PJ, 2007, QUATERN INT, V167, P73, DOI 10.1016/j.quaint.2006.11.009; Mudie PJ, 2010, VEG HIST ARCHAEOBOT, V19, P531, DOI 10.1007/s00334-010-0268-9; 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; Okamoto OK, 1999, COMP BIOCHEM PHYS C, V123, P75, DOI 10.1016/S0742-8413(99)00013-4; Okamoto OK, 1998, COMP BIOCHEM PHYS C, V119, P67, DOI 10.1016/S0742-8413(97)00192-8; Pospelova V, 2005, MAR ECOL PROG SER, V292, P23, DOI 10.3354/meps292023; Pospelova V, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001251; Ribeiro S, 2008, MAR MICROPALEONTOL, V68, P156, DOI 10.1016/j.marmicro.2008.01.013; Rochon A, 2009, REV PALAEOBOT PALYNO, V155, P52, DOI 10.1016/j.revpalbo.2008.12.017; Ryan WBF, 2003, ANNU REV EARTH PL SC, V31, P525, DOI 10.1146/annurev.earth.31.100901.141249; Ryan WBF, 1997, MAR GEOL, V138, P119, DOI 10.1016/S0025-3227(97)00007-8; Ryan William., 1998, Noah's Flood: The New Scientific Discoveries About the Event that Changed History; Smayda TJ, 2003, J SEA RES, V49, P95, DOI 10.1016/S1385-1101(02)00219-8; Tardio M, 2006, J PALEOLIMNOL, V36, P315, DOI 10.1007/s10933-006-9001-1; Uzar S, 2010, SCI RES ESSAYS, V5, P285; Zonneveld KAF, 2012, MAR POLLUT BULL, V64, P114, DOI 10.1016/j.marpolbul.2011.10.012; Zonneveld KAF, 2009, J SEA RES, V62, P189, DOI 10.1016/j.seares.2009.02.003	50	2	2	0	6	PARLAR SCIENTIFIC PUBLICATIONS (P S P)	FREISING	ANGERSTR. 12, 85354 FREISING, GERMANY	1018-4619	1610-2304		FRESEN ENVIRON BULL	Fresenius Environ. Bull.		2018	27	5					2800	2808						9	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	GK8ZA					2025-03-11	WOS:000436522600023
J	Vieira, M; Mahdi, S; Osterloff, P				Vieira, Manuel; Mahdi, Salih; Osterloff, Peter			New Early Paleocene (Danian) dinoflagellate cyst species from the Ormen Lange Field, MOre Basin, Norwegian Continental Shelf	PALYNOLOGY			English	Article						Ormen Lange Field; Norway; Danian; biostratigraphy; palynology; dinoflagellate cysts; taxonomy	CENTRAL NORTH-SEA; WEST GREENLAND; BIOSTRATIGRAPHY; ACRITARCHS; EVOLUTION	A high-resolution palynological study of a recently acquired core from the southern part of the Ormen Lange field (Norway) over the Danian-aged reservoir interval revealed rich, diverse and well-preserved palynomorph assemblages. Review of these assemblages has allowed the opportunity to formally describe some dinoflagellate cysts previously left in open nomenclature and others recognised for the first time in this well. We propose in this paper the formal description of 10 new species: Achomosphaera eggadania sp. nov., Achomosphaera progranulata sp. nov., Areoligera constricta sp. nov., Areoligera pauciornata sp. nov., Deflandrea variabilis sp. nov., Eurydinium ovatum sp. nov., Glaphyrocysta pseudoreticulata sp. nov., Hystrichosphaeridium pachydermum sp. nov., Operculodinium runtata sp. nov. and Phthanoperidinium ormenlangei sp. nov. All the key diagnostic and morphological features of each species are discussed and compared with those of other forms outside and within the same genera. The new species presented all range throughout the Danian (Early Paleocene) and can be used in conjunction with other previously published markers to support and enhance the stratigraphic breakdown and subdivision of the reservoir interval across the Ormen Lange field, and potentially other areas in the North Sea basin.	[Vieira, Manuel] Shell UK Ltd, 1 Altens Farm Rd, Aberdeen AB12 3FY, Scotland; [Mahdi, Salih] RPS Ichron Ltd, Gadbrook Business Ctr, Century House, Northwich CW9 7TL, Cheshire, England; [Osterloff, Peter] Shell UK Ltd, 40 Bank St, London E14 5NR, England	Royal Dutch Shell; Royal Dutch Shell	Vieira, M (通讯作者)，Shell UK Ltd, 1 Altens Farm Rd, Aberdeen AB12 3FY, Scotland.	Manuel.Vieira@Shell.com	Mahdi, Saiful/S-3395-2017; Vieira, Manuel/AAY-4474-2020	Vieira, Manuel/0000-0002-2389-4583				[Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1914, BER DTSCH BOT GES, DOI DOI 10.1111/J.1438-8677.1914.TB07573.X; [Anonymous], 1996, Palynology: principles and applications; [Anonymous], 1847, B SOC GEOLOGIQUE FRA; Berggren WA, 2005, J FORAMIN RES, V35, P279, DOI 10.2113/35.4.279; Bujak JP., 1980, PALAEONTOLOGICAL ASS, V24, P36; BUJAK JP, 1983, AM ASS STRATIGRAPHIC, V13; Butschli O, 1885, PROTOZOA HG BRONNS K, P865; Dalland A., 1988, A lithostratigraphic scheme for the Mesozoic and Cenozoic succession offshore mid- and northern Norway; DAMASSA S P, 1979, Palynology, V3, P191; Davey R.J., 1966, STUDIES MESOZOIC CAI, P53; De Coninck J., 1975, Geologiska Foereningen i Stockholm Foerhandlingar, V97, P326; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Drugg W.S., 1967, Tulane Studies in Geology, V5, P181; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; Eaton GL., 1976, B BRIT MUS NAT HIST, V26; EDWARDS L E, 1981, Palynology, V5, P29; Eisenack A., 1954, Palaeontographica A, V105, P49; Eisenack A., 1938, Schriften der Physikalisch-Okonomischen Gesellschaft zu Konigsberg, V70, P181; Eldrett J, 2015, GEOL SOC SPEC PUBL, V403, P63, DOI 10.1144/SP403.9; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P158, DOI 10.1073/pnas.49.2.158; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42, P909; Fensome RA, 2009, J SYST PALAEONTOL, V7, P1, DOI 10.1017/S1477201908002538; FIRTH J V, 1987, Palynology, V11, P199; Gradstein FM, 2010, NEWSL STRATIGR, V44, P73, DOI 10.1127/0078-0421/2010/0005; GRADSTEIN FM, 1992, MICROPALEONTOLOGY, V38, P101, DOI 10.2307/1485991; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; Heilmann-Clausen C., 1988, GEOLOGISCHES JB A, V100, P339; Heilmann-Clausen C, 2005, PALYNOLOGY, V29, P143, DOI 10.2113/29.1.143; Holtedahl H, 1993, NORGES GEOLOGISKE UN, V6; Hultberg S.U., 1985, DINOFLAGELLATE STUDI, P33; Isaken D., 1989, B NORW PETROL DIRECT, V5; Islam M.A., 1983, Revue de Micropaleontologie, V25, P231; ISLAM MA, 1982, REV PALAEOBOT PALYNO, V36, P305, DOI 10.1016/0034-6667(82)90025-2; Lange D., 1969, BEITRAGE MEERESKUNDE, V24, P110; Lejeune-Carpentier M., 1938, ANN SOC GEOL BELG, V61, P163; Lentin J.K., 1981, BED I OCEANOG REP SE, V1981, P1; Lucas-Clark J, 2006, PALYNOLOGY, V30, P183, DOI 10.2113/gspalynol.30.1.183; Lund J.J., 2002, NO EUROPEAN CENOZOIC, P83; Mantell GA, 1850, PICTORIAL ATLAS FOSS, VXII; Mao S, 1992, P OCEAN DRILLING PRO, P120; Martini E., 1971, P 2 PLANKT C TECN RO, P739; Matsuoka Kazumi, 1997, Palynology, V21, P19; Möller NK, 2004, NORW J GEOL, V84, P169; Mudge DC, 1996, MAR PETROL GEOL, V13, P295, DOI 10.1016/0264-8172(95)00066-6; Nohr-Hansen H, 2002, GEOL SOC SPEC PUBL, V197, P111, DOI 10.1144/GSL.SP.2002.197.01.06; Nohr-Hansen H, 2001, NEUES JAHRB GEOL P-A, V219, P153, DOI 10.1127/njgpa/219/2001/153; Nohr-Hansen H, 1999, GRANA, V38, P125, DOI 10.1080/00173139908559221; Quattrocchio ME, 2003, AMEGHINIANA, V40, P129; Radmacher W, 2014, MAR PETROL GEOL, V57, P109, DOI 10.1016/j.marpetgeo.2014.04.008; Radmacher W, 2015, REV PALAEOBOT PALYNO, V216, P18, DOI 10.1016/j.revpalbo.2014.12.007; SARJEANT W A S, 1970, Grana, V10, P74; Schioler P, 2005, J MICROPALAEONTOL, V24, P1, DOI 10.1144/jm.24.1.1; Schioler Poul, 1993, Journal of Micropalaeontology, V12, P99; Schroder Theo, 1992, Journal of Micropalaeontology, V11, P113; Slimani H, 2001, J MICROPALAEONTOL, V20, P1, DOI 10.1144/jm.20.1.1; STOVER LE, 1974, GEOLOGICAL SOC AUSTR, V4, P167; THOMSEN E, 1985, Bulletin of the Geological Society of Denmark, V33, P341; Thorn VC, 2009, REV PALAEOBOT PALYNO, V156, P436, DOI 10.1016/j.revpalbo.2009.04.009; Vergara L, 2001, PETROL GEOSCI, V7, P395, DOI 10.1144/petgeo.7.4.395; Wade BS, 2011, EARTH-SCI REV, V104, P111, DOI 10.1016/j.earscirev.2010.09.003; WALL D., 1967, PALAEONTOLOGY, V10, P95; Williams G.L., 1985, P847; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Williams G.L., 1998, Mesozoic and Cenozoic Sequence Stratigra Phy of European Basins, V60, P764; Williams GL, 1966, B BRIT MUSEUM NAT S3, VSuppl. 3, P176	68	21	21	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2018	42	2					180	198		10.1080/01916122.2017.1314390	http://dx.doi.org/10.1080/01916122.2017.1314390			19	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	GC2IA					2025-03-11	WOS:000429604300004
J	Lebedeva, NK; Kuz'mina, OB				Lebedeva, N. K.; Kuz'mina, O. B.			Palynostratigraphy of the Upper Cretaceous and Paleogene Deposits in the South of Western Siberia by Example of Russkaya Polyana Boreholes, Omsk Trough	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						biostratigraphy; Upper Cretaceous; Paleogene; Omsk Trough; south of Western Siberia; palynology; dinocysts	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; PENINSULA KALININGRAD REGION; PALYNOLOGICAL CHARACTERISTICS; DINOCYST BIOSTRATIGRAPHY; CAMPANIAN BOUNDARY; MARINE PALEOGENE; BASIN; SEDIMENTARY; ZONATION; PART	The detailed study of Boreholes 8, 10, and 2 in the Russkaya Polyana district (Omsk Trough) made it possible to reveal the complex structure of the Upper Cretaceous sediments formed in unstable conditions of the marginal part of the Western Siberian basin. The Pokur, Kuznetsovo, Ipatovo, Slavgorod, and Gan'kino formations were subjected to palynological analysis and substantiation of their Late Cretaceous age. Eight biostratigraphic units with dinocysts and five units with spores and pollen from the Albian to the Maastrichtian were identified. The joint application of biostratigraphic and magnetostratigraphic methods made it possible to reveal the stratigraphic breaks in the studied sedimentary stratum and to estimate their scope. The age of the Lower Lyulinvor Subformation was specified in the marginal part of the Omsk Trough. The ingression traces of the Western Siberian basin in the Albian were found for the first time in the considered region.	[Lebedeva, N. K.; Kuz'mina, O. B.] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia; [Lebedeva, N. K.] Novosibirsk State Univ, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences; Novosibirsk State University	Lebedeva, NK (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia.; Lebedeva, NK (通讯作者)，Novosibirsk State Univ, Novosibirsk 630090, Russia.	LebedevaNK@ipgg.sbras.ru	Kuzmina, Olga/I-9547-2018; Natalia, Lebedeva/T-6040-2017	Natalia, Lebedeva/0000-0002-7192-8303	Comprehensive Program of the Siberian Branch of the Russian Academy of Sciences II. 2P "Integration and Development"; IGCP Project [608]	Comprehensive Program of the Siberian Branch of the Russian Academy of Sciences II. 2P "Integration and Development"; IGCP Project	This work was supported by the Comprehensive Program of the Siberian Branch of the Russian Academy of Sciences II. 2P "Integration and Development" and by the IGCP 608 Project.	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L., 1993, GEOL SURV CAN; ZAKHAROV VA, 2000, RUSS GEOL GEOPHYS, V41, P769	81	9	9	1	4	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	JAN	2018	26	1					80	108		10.1134/S0869593818010069	http://dx.doi.org/10.1134/S0869593818010069			29	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	FY8FH					2025-03-11	WOS:000427098600004
J	Davtalab, E; Vahidinia, M; Ghasemi-Nejad, E; Ashouri, A				Davtalab, Elham; Vahidinia, Mohammad; Ghasemi-Nejad, Ebrahim; Ashouri, Alireza			Planktonic foraminifera and dinoflagellate cysts from the Upper Cretaceous Abderaz Formation in the Koppeh-Dagh Basin, NE Iran	STRATIGRAPHY			English	Article						Planktonic Foraminifera; dinoflagellate cysts; biostratigraphy; Turonian-Campanian; Koppeh-Dagh Basin; Iran	GLOBAL BOUNDARY STRATOTYPE; SOUTH CASPIAN BASIN; NEW-ZEALAND; INTEGRATED BIOSTRATIGRAPHY; SHEMSHAK GROUP; NORTHERN IRAN; CONIACIAN; EVOLUTION; STRATIGRAPHY; ZONATION	Assemblages of planktonic foraminifera and dinoflagellate cysts were studied from the 359 m thick Padeha-Baghak composite section of the Abderaz Formation, eastern Koppeh-Dagh Basin, NE Iran. The formation consists mainly of light grey shales and marls with three chalky limestone beds in the upper part. Nine genera and 44 species of planktonic foraminifera and 39 genera and 85 species of dinoflagellate cysts are identified. Planktonic foraminifera are attributed to four biozones (Dicarinella primitiva-Marginotruncana sigali, Dicarinella concavata, Dicarinella asymetrica and Globotruncanita elevata zones). Two dinocyst superzones (Conosphaeridium striatoconum Superzone and the lower part of the Odontochitina porifera Superzone) with seven interval zones are recognized. These biozones suggest a late Turonian-early Campanian age for the Abderaz Formation in this part of the Koppeh-Dagh Basin.	[Davtalab, Elham; Vahidinia, Mohammad; Ashouri, Alireza] Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Azadi Sq,Univ Campus,POB 917751436, Mashhad 9177948953, Iran; [Ghasemi-Nejad, Ebrahim] Univ Tehran, Univ Coll Sci, Dept Geol, Enghelab Ave,POB 14155-6455, Tehran 1417614411, Iran	Ferdowsi University Mashhad; University of Tehran	Vahidinia, M (通讯作者)，Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Azadi Sq,Univ Campus,POB 917751436, Mashhad 9177948953, Iran.	Vahidinia@ferdowsi.um.ac.ir	Ghasemi-Nejad, Ebrahim/AAF-6087-2020; Vahidinia, Mohammad/AAB-7110-2020	Ashouri, Ali Reza/0000-0002-2913-4913	Department of Geology at Ferdowsi University of Mashhad, Iran [3/26723]	Department of Geology at Ferdowsi University of Mashhad, Iran	This work is a part of a Ph. D. thesis (#3/26723) of Elham Davtalab, which is supported by the Department of Geology at Ferdowsi University of Mashhad, Iran. The authors would like to acknowledge their logistical and financial support.	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J	Sharifi, M; Ghasemi-Nejad, E; Sarfi, M; Yazdi-Moghadam, M; Salehani, MT; Akhtari, M				Sharifi, Mohammad; Ghasemi-Nejad, Ebrahim; Sarfi, Mehdi; Yazdi-Moghadam, Mohsen; Salehani, Mostafa Tarjani; Akhtari, Maryam			Marine palynology and environmental interpretation of the Lower Cretaceous (Barremian?-Aptian) rock units in the Koppeh-Dagh Basin, NE Iran	GEOLOGICAL QUARTERLY			English	Article						Koppeh-Dagh; palynostratigraphy; palynofacies; palaeoecology; palaeoenvironment	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SEA-LEVEL CHANGES; ORGANIC-MATTER; SEQUENCE STRATIGRAPHY; PALYNOFACIES; SEDIMENTS; CARBONATES; EVOLUTION; FRANCE; FACIES	The Sarcheshmeh and Sanganeh formations are the Lower Cretaceous deep marine sequences of the Koppeh-Dagh sedimentary basin, which revealed a diverse assemblage of dinoflagellates. The paper discusses palynostratigraphy, palynofacies and palaeoenvironment of these rock units in a borehole drilled in the eastern part of this basin. Ninety-five ditch-cutting samples were prepared and studied palynologically, which resulted in recognition of 76 species of dinoflagellate cysts belonging to 29 genera. The recorded assemblages are in accordance with the Odontochitina operculata Zone suggesting a Barremian?-Aptian age for the formations. Palynological data extracted led to identification of five palynofacies types based on the categories of Tyson (1995). These indicate a marginal, proximal and distal shelf environment of deposition. The obtained data from calculated palaeoecological factors revealed a gradual sea level rise during the deposition of these rock units, resulting in replacement of the oxic/dysoxic Sarcheshmeh Formation by the dysoxic/anoxic Sanganeh Formation.	[Sharifi, Mohammad; Ghasemi-Nejad, Ebrahim; Salehani, Mostafa Tarjani] Univ Tehran, Univ Coll Sci, Dept Geol, Tehran, Iran; [Sarfi, Mehdi] Damghan Univ, Sch Earth Sci, Damghan, Iran; [Yazdi-Moghadam, Mohsen; Akhtari, Maryam] Natl Iranian Oil Co, Explorat Directorate, Sheikh Bahayi Sq, Tehran, Iran	University of Tehran; Damghan University; National Iranian Oil Company (NIOC)	Ghasemi-Nejad, E (通讯作者)，Univ Tehran, Univ Coll Sci, Dept Geol, Tehran, Iran.	eghaseminejad@gmail.com	Sharifi, Mohammad/AAG-7084-2019; Ghasemi-Nejad, Ebrahim/AAF-6087-2020; Moghadam, Mohsen/GSP-6543-2022	Yazdi-Moghadam, Mohsen/0000-0002-3495-8028; Sharifi, Mohammad/0000-0003-2351-7670	exploration directorate of the National Iranian Oil Company (NIOC); University of Tehran; Damghan University	exploration directorate of the National Iranian Oil Company (NIOC); University of Tehran(University of Tehran); Damghan University(Damghan University)	The authors thank the exploration directorate of the National Iranian Oil Company (NIOC), University of Tehran and Damghan University for their support. Prof. M. Fabianska and an Anonymous reviewer are thanked for reviewing the manuscript and giving many comments that improved quality of this paper.	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K., 2011, THESIS	66	3	3	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.		2018	62	1					90	99		10.7306/gq.1394	http://dx.doi.org/10.7306/gq.1394			10	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FX4KA		gold			2025-03-11	WOS:000426042600007
J	Raho, N; Fraga, S; Abad, JP; Marín, I				Raho, Nicolas; Fraga, Santiago; Abad, Jose P.; Marin, Irma			<i>Biecheleria tirezensis</i> sp nov (Dinophyceae, Suessiales), a new halotolerant dinoflagellate species isolated from the athalassohaline Tirez natural pond in Spain	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Athalassic; CBC; dinoflagellate; halotolerant; hypersaline; ITS2 secondary structure; phylogeny; Suessiaceae; taxonomy; Woloszynskioid	INTERNAL TRANSCRIBED SPACER; RIBOSOMAL-RNA; LAKE TOVEL; PHYLOGENETIC POSITION; WOLOSZYNSKIA-CINCTA; ELECTRON-MICROSCOPY; MOLECULAR ANALYSIS; COASTAL WATERS; COMB. NOV; GEN.	A new euryhaline and eurythermal dinoflagellate species, Biecheleria tirezensis sp. nov., is described based on samples taken from an extreme environment, the athalassohaline and particularly sulphate-rich Tirez natural pond (Spain). This species is able to survive in salinities from almost fresh water up to 56 and over a 5-25 degrees C temperature range. Thus, the ecological characteristics of this isolate differentiate it from other species of the same genus. Its morphology, as examined by light, scanning and transmission electron microscopy, shows that the cells are almost spherical, with several series of amphiesmal vesicles. It also has a single elongate amphiesmal vesicle (EAV) observed by SEM and the eyespot has a type E structure, typical of Biecheleria. Spherical and smooth cysts were observed in old cultures. The pigment composition is typical of a peridinin-containing dinoflagellate. Phylogeny inferred from nuclear rDNA SSU, ITS and LSU sequences showed the isolate belongs to the genus Biecheleria, closest to B. cincta and B. brevisulcata. Modelling and analysis of the secondary structure of its ITS2 region, and that of other species of the same genus and some representatives of the most closely related genera, indicated that the isolate represents a new species clearly separated from but related to B. cincta. The criterion of the presence of Compensatory Base Changes (CBCs) in the secondary structure of the ITS2 region as an indicator of species differentiation confirmed this, supporting the establishment of the Tirez pond isolate as a new species of Biecheleria.	[Raho, Nicolas; Abad, Jose P.; Marin, Irma] Univ Autonoma Madrid, Dept Biol Mol, E-28049 Madrid, Spain; [Fraga, Santiago] IEO, Ctr Oceanog Vigo, Vigo 36390, Spain; [Raho, Nicolas] MIT, Dept Civil & Environm Engn, 77 Massachusetts Ave, Cambridge, MA 02139 USA	Autonomous University of Madrid; Spanish Institute of Oceanography; Massachusetts Institute of Technology (MIT)	Abad, JP; Marín, I (通讯作者)，Univ Autonoma Madrid, Dept Biol Mol, E-28049 Madrid, Spain.	josep.abad@uam.es	Marin, Irma/Z-4231-2019; Lorenzo, Jose/Y-3871-2019; Fraga, Santiago/AAA-3760-2020	Abad Lorenzo, Jose Pascual/0000-0002-5284-5772	Universidad Autonoma de Madrid	Universidad Autonoma de Madrid	N. 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J. Phycol.		2018	53	1					99	113		10.1080/09670262.2017.1386328	http://dx.doi.org/10.1080/09670262.2017.1386328			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	FV7FW					2025-03-11	WOS:000424749900009
J	Matsuoka, K; Maung-Saw-Htoo-Thaw; Yurimoto, T; Koike, K				Matsuoka, Kazumi; Maung-Saw-Htoo-Thaw; Yurimoto, Tatsuya; Koike, Kazuhiko			Palynomorph Assemblages Dominated by Heterotrophic Marine Palynomorphs in Tropical Coastal Shallow-water Sediments from the Southern Myanmar Coast	JARQ-JAPAN AGRICULTURAL RESEARCH QUARTERLY			English	Article						coastal environment; dinoflagellate cyst; microbial loop; microforaminiferal lining; tinntinomorph	DINOFLAGELLATE CYST DISTRIBUTION; DIPLOPSALIS-LENTICULA; ENVIRONMENTAL-CHANGE; CERATIUM-FURCA; LATE HOLOCENE; FOOD WEBS; EUTROPHICATION; DINOPHYCEAE; MIXOTROPHY; POLLEN	The goal of this study was to characterize palynomorph assemblages in tropical marine coastal shallow-water sediments collected from the southern coast of Myanmar, and possibly find them as useful tools for reconstructing changes in the tropical coastal environment. These sediment samples were dominated by heterotrophic marine palynomorphs, particularly in microforaminiferal linings and heterotrophic dinoflagellate cysts. In addition, these tropical marine palynomorph assemblages were characterized by low cell/grain concentrations, especially in photo/mixotrophic dinoflagellate cysts. These marine palynomorph characteristics are common to other tropical coastal surface sediments collected from Southeast Asia. These assemblages may reflect a diagnostic food web that characterizes tropical coastal shallow waters. For example, benthic foraminifers (microforaminiferal linings) that are always dominated usually consume prey organisms composed of bacteria, diatoms, dinoflagellates and amorphous organic substances. And bacteria can utilize dissolved organic matter delivered from terrestrial and marine environments via various organisms that inhabit water and sediment surfaces. The dominance of microforaminiferal linings appears to result from both microbial and grazing food webs in tropical coastal shallow-water sediments.	[Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, Nagasaki, Nagasaki 8512213, Japan; [Maung-Saw-Htoo-Thaw; Koike, Kazuhiko] Hiroshima Univ, Grad Sch Biosphere Sci, Higashihiroshima, Hiroshima 7398528, Japan; [Yurimoto, Tatsuya] Japan Int Res Ctr Agr Sci, Tsukuba, Ibaraki 3058686, Japan; [Yurimoto, Tatsuya] FRA, Seikai Natl Fisheries Res Inst, Nagasaki, Nagasaki 8512213, Japan	Nagasaki University; Hiroshima University; Japan International Research Center for Agricultural Sciences; Japan Fisheries Research & Education Agency (FRA)	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst East China Sea Res, Nagasaki, Nagasaki 8512213, Japan.	kazu-mtk@nagasaki-u.ac.jp	Yurimoto, Tatsuya/AAS-1020-2020; Koike, Kazuhiko/A-3392-2019	Kazuhiko, Koike/0000-0001-5380-5839; Yurimoto, Tatsuya/0000-0002-7275-064X	MEXT/JSPS [26304031]; Grants-in-Aid for Scientific Research [26304031] Funding Source: KAKEN	MEXT/JSPS(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	The authors wish to express deep appreciation to officials of the Department of Fisheries (Myeik) and the staff from Myeik University in Myanmar for their assistance in our field work. The authors also wish to thank Myanmar Fisheries Federation (MFF) for their kind support of our visit to Myanmar. Finally, the authors wish to thank the two anonymous reviewers for their constructive and helpful comments toward improving this article. This work was partially supported by MEXT/JSPS-Grants-in-aid for Scientific Research (No: 26304031).	Armstrong H. 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M., 1993, GEOL ULTRIECTIN, V104, P242; Yamaguchi A, 2008, J PHYCOL, V44, P1090, DOI 10.1111/j.1529-8817.2008.00547.x; Yurimoto Tatsuya, 2015, International Aquatic Research, V7, P133, DOI 10.1007/s40071-015-0099-5	49	5	7	0	2	JAPAN INT RESEARCH CENTER AGRICULTURAL SCIENCES	IBARAKI	TSUKUBA, IBARAKI, 305-8686, JAPAN	0021-3551			JARQ-JPN AGR RES Q	Jarq - Jpn. Agric. Res. Q.		2018	52	1					77	89		10.6090/jarq.52.77	http://dx.doi.org/10.6090/jarq.52.77			13	Agriculture, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Agriculture	FU9XT		gold			2025-03-11	WOS:000424211200010
J	Pandey, S; Holt, K				Pandey, Shilpa; Holt, Katherine			Modern pollen distribution and its relationship to vegetation from the south-western part of the Ganges-Brahmaputra Delta, India	PALYNOLOGY			English	Article						Modern pollen distribution; mangroves; Pakhiralaya; Ganges-Brahmaputra Delta; India	HOLOCENE MANGROVE; SURFACE POLLEN; CHINA; RAIN; RECONSTRUCTION; AUSTRALIA; SEDIMENTS; PATTERNS; PLATEAU; FORESTS	Thirty surface samples collected from the Pakhiralaya area, south-western Ganges-Brahmaputra Delta, India, have been analysed for pollen in order to investigate modern pollen-vegetation relationships. Data on non-pollen palynomorphs (fungal spores, dinoflagellate cysts and algal cysts) were also obtained. There is currently a paucity of modern pollen studies from this region, which places limits on the interpretation of pollen data from other types of studies, for example studies aimed at understanding the Holocene vegetation history of this globally renowned tropical forest region. The local vegetation of the area is characterised by mangrove, marsh, herb and open land. The results of our study indicate that the pollen from locally growing taxa are the major components of modern pollen assemblages. Thus, pollen spectra show close linkages between modern pollen and local vegetation. Within the samples collected from the mangrove forest, the dominant mangrove taxa (Rhizophora mucronata, Bruguiera gymnorrhiza, Excoecaria agallocha, Sonneratia and Avicennia marina) are also the most frequently encountered pollen types, along with the mangrove associate taxa Thespesia sp., Pongamia pinnata and Phoenix paludosa. Thus, undisturbed mangrove forests are characterised mainly by a dominance of true mangrove and mangrove associate species in the pollen spectra. In contrast, pollen spectra from samples from open land' areas contained significant proportions of pollen from midland taxa. Anthropogenic impact on this area is captured in the samples through pollen of introduced plants such as Eucalyptus and Casuarina equisetifolia. The present study provides a basis for useful interpretation of Late Quaternary pollen sequences from the Ganges-Brahmaputra Delta, since modern pollen studies are still meagre in the poorly investigated delta region.	[Pandey, Shilpa] Birbal Sahni Inst Palaeosci, Quaternary Palynol Lab, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India; [Holt, Katherine] Massey Univ, Inst Agr & Environm, Private Bag 11222, Palmerston North, New Zealand	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Massey University	Pandey, S (通讯作者)，Birbal Sahni Inst Palaeosci, Quaternary Palynol Lab, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	shilpa.bsip@gmail.com			Birbal Sahni Institute of Palaeosciences, Lucknow, India	Birbal Sahni Institute of Palaeosciences, Lucknow, India	This work was supported by the Birbal Sahni Institute of Palaeosciences, Lucknow, India (in-house project).	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J	Mertens, KN; Carbonell-Moore, MC; Pospelova, V; Head, MJ; Highfield, A; Schroeder, D; Gu, HF; Andree, KB; Fernandez, M; Yamaguchi, A; Takano, Y; Matsuoka, K; Nézan, E; Bilien, G; Okolodkov, Y; Koike, K; Hoppenrath, M; Pfaff, M; Pitcher, G; Al-Muftah, A; Rochon, A; Lim, PT; Leaw, CP; Lim, ZF; Ellegaard, M				Mertens, Kenneth Neil; Carbonell-Moore, M. Consuelo; Pospelova, Vera; Head, Martin J.; Highfield, Andrea; Schroeder, Declan; Gu, Haifeng; Andree, Karl B.; Fernandez, Margarita; Yamaguchi, Aika; Takano, Yoshihito; Matsuoka, Kazumi; Nezan, Elisabeth; Bilien, Gwenael; Okolodkov, Yuri; Koike, Kazuhiko; Hoppenrath, Mona; Pfaff, Maya; Pitcher, Grant; Al-Muftah, Abdulrahman; Rochon, Andre; Lim, Po Teen; Leaw, Chui Pin; Lim, Zhen Fei; Ellegaard, Marianne			<i>Pentaplacodinium saltonense</i> gen. et sp nov (Dinophyceae) and its relationship to the cyst-defined genus <i>Operculodinium</i> and yessotoxin-producing <i>Protoceratium reticulatum</i>	HARMFUL ALGAE			English	Article						Pentaplacodinium; Protoceratium; Precingular plates; Salton Sea; Ceratocorys; Operculodinium; Cribroperidinioideae	PROCESS LENGTH VARIATION; ALEXANDRIUM DINOPHYCEAE; RIBOSOMAL DNA; SEQUENCE DATA; SEA; SALINITY; STRAINS; GENERA; LIGHT; ULTRASTRUCTURE	Strains of a dinoflagellate from the Salton Sea, previously identified as Protoceratium reticulatum and yessotoxin producing, have been reexamined morphologically and genetically and Pentaplacodinium saltonense n. gen. et sp. is erected to accommodate this species. Pentaplacodinium saltonense differs from Protoceratium reticulatum (Claparede et Lachmann 1859) Biltschli 1885 in the number of precingular plates (five vs. six), cingular displacement (two widths vs. one), and distinct cyst morphology. Incubation experiments (excystment and encystment) show that the resting cyst of Pentaplacodinium saltonense is morphologically most similar to the cyst-defined species Operculodinium israelianum (Rossignol, 1962) Wall (1967) and 0. psilatum Wall (1967). Collections of comparative material from around the globe (including Protoceratium reticulatum and the genus Ceratocorys) and single cell PCR were used to clarify molecular phylogenies. Variable regions in the LSU (three new sequences), SSU (12 new sequences) and intergenic ITS 1-2 (14 new sequences) were obtained. These show that Pentaplacodinium saltonense and Protoceratium reticulatum form two distinct clades. Pentaplacodinium saltonense forms a monophyletic Glade with several unidentified strains from Malaysia. LSU and SSU rDNA sequences of three species of Ceratocorys (C armata, C gourreti, C horrida) from the Mediterranean and several other unidentified strains from Malaysia form a well-supported sister clade. The unique phylogenetic position of an unidentified strain from Hawaii is also documented and requires further examination. In addition, based on the V9 SSU topology (bootstrap values >80%), specimens from Elands Bay (South Africa), originally described as Gonyaulax grindleyi by Reinecke (1967), cluster with Protoceratilim reticulatum. The known range of Pentaplacodinium saltonense is tropical to subtropical, and its cyst is recorded as a fossil in upper Cenozoic sediments. Protoceratium reticulatum and Pentaplacodiniutn saltonense seem to inhabit different niches: motile stages of these dinoflagellates have not been found in the same plankton sample. (C) 2017 Elsevier B.V. All rights reserved.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium; [Carbonell-Moore, M. Consuelo] Oregon State Univ, Coll Agr Sci, Dept Bot & Plant Pathol, 2082 Cordley Hall, Corvallis, OR 97331 USA; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB A405,POB 1700,Box 1700 STN CSC, Victoria, BC V8W 2Y2, Canada; [Head, Martin J.] Brock Univ, Dept Earth Sci, 1812 Sir Isaac Brock Way, St Catharines, ON L2S 3A1, Canada; [Highfield, Andrea; Schroeder, Declan] Marine Biol Assoc UK, Citadel Hill, Plymouth PL1 2PB, Devon, England; [Schroeder, Declan] Univ Reading, Sch Biol Sci, Reading RG6 6AJ, Berks, England; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Andree, Karl B.; Fernandez, Margarita] IRTA, Km 5-5, San Carlos de la Rapita 43540, Spain; [Yamaguchi, Aika] Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 6578501, Japan; [Takano, Yoshihito; Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res ECSER, 1551-7 Taira Machi, Nagasaki 8512213, Japan; [Nezan, Elisabeth; Bilien, Gwenael] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France; [Okolodkov, Yuri] Univ Veracruzana, Inst Ciencias Marinas & Pesquerias, Calle Hidalgo 617, Boca Del Rio 94290, Veracruz, Mexico; [Koike, Kazuhiko] Hiroshima Univ, Grad Sch Biosphere Sci, Kagamiyama 1-4-4, Higashihiroshima, Hiroshima 7398528, Japan; [Hoppenrath, Mona] Deutsch Zentrum Marine Biodivers Forsch DZMB, Sudstrand 44, D-26382 Wilhelmshaven, Germany; [Pfaff, Maya] Univ Cape Town, Ma RE Inst, Marine Biol Res Ctr, Zool Dept, ZA-7701 Rondebosch, South Africa; [Pitcher, Grant] Marine & Coastal Management, Private Bag X2, ZA-8012 Cape Town, South Africa; [Al-Muftah, Abdulrahman] Qatar Univ, Dept Biol & Environm Sci, Doha, Qatar; [Rochon, Andre] Univ Quebec Rimouski, Inst Sci Mer Rimouski ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada; [Lim, Po Teen; Leaw, Chui Pin; Lim, Zhen Fei] Univ Malaya, Inst Ocean & Earth Sci, Bachok 16310, Kelantan, Malaysia; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Thorvaldsensvej 40, DK-1871 Frederiksberg, Denmark	Ghent University; Oregon State University; University of Victoria; Brock University; Marine Biological Association United Kingdom; University of Reading; Third Institute of Oceanography, Ministry of Natural Resources; IRTA; Kobe University; Nagasaki University; Ifremer; Universidad Veracruzana; Hiroshima University; University of Cape Town; Qatar University; University of Quebec; Universite du Quebec a Rimouski; Universiti Malaya; University of Copenhagen	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.; Mertens, KN (通讯作者)，IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France.	kenneth.mertens29@gmail.com	Leaw, Chui Pin/F-5220-2012; Ellegaard, Marianne/H-6748-2014; Andree, Karl/L-7465-2014; Schroeder, Declan/O-9131-2019; Koike, Kazuhiko/A-3392-2019; Mertens, Kenneth/AAO-9566-2020; Gu, Haifeng/ADN-4528-2022; Fernandez-Tejedor, Margarita/J-9449-2013; Mertens, Kenneth/C-3386-2015; Lim, Po Teen/C-9758-2013	Kazuhiko, Koike/0000-0001-5380-5839; Gu, Haifeng/0000-0002-2350-9171; Fernandez-Tejedor, Margarita/0000-0002-2875-1135; Schroeder, Declan/0000-0001-5991-2838; Pospelova, Vera/0000-0003-4049-8133; Mertens, Kenneth/0000-0003-2005-9483; Lim, Po Teen/0000-0003-2823-0564	Natural Sciences and Engineering Research Council of Canada (NSERC); Institute Nacional de Investigacion y Tecnologia Agraria y Alimentaria of the Spanish Government [RTA2005-00109-00-00]; Natural Sciences and Engineering Research Council of Canada (NSERC); Institute Nacional de Investigacion y Tecnologia Agraria y Alimentaria of the Spanish Government [RTA2005-00109-00-00]	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Institute Nacional de Investigacion y Tecnologia Agraria y Alimentaria of the Spanish Government; Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Institute Nacional de Investigacion y Tecnologia Agraria y Alimentaria of the Spanish Government	V.P. and M.J.H. each acknowledge support from a Discovery Grant of the Natural Sciences and Engineering Research Council of Canada (NSERC). K.B.A. and M.F. were supported by the Institute Nacional de Investigacion y Tecnologia Agraria y Alimentaria of the Spanish Government (project RTA2005-00109-00-00). CINVESTAV, Merida is thanked for supplying information about the Yucatan samples. Beatriz Paz is acknowledged for interesting discussions on toxicity. Anke Kremp, Maija Hutunnen, Jacob Larsen, Paul Hargraves and Ximena Vivanco kindly provided plankton samples. Nancy Lewis and Margaret Beaton generously shared information on strains from Nova Scotia, Canada. Captain Brown, crew of the MSV Strickland, Ms. Sarah Thornton, and EOS313-2010 (University of Victoria) students are all thanked for their participation in sediment sample collection. Paul Hargraves kindly provided SEM images of P. saltonense from cultures established from the Indian River Lagoon.[SS]	Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; AI-Muftah A. 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J	Ferguson, S; Warny, S; Anderson, JB; Simms, AR; White, C				Ferguson, Shannon; Warny, Sophie; Anderson, John B.; Simms, Alexander R.; White, Crawford			Breaching of Mustang Island in response to the 8.2 ka sea-level event and impact on Corpus Christi Bay, Gulf of Mexico: Implications for future coastal change	HOLOCENE			English	Article						barrier island; dinoflagellates; Gulf of Mexico; Holocene; North America; sea-level changes	ICE-SHEET; RISE; CLIMATE; ENVIRONMENTS; HISTORY; CURVE	The results from an investigation of the coupled Mustang Island-Corpus Christi Bay complex, Gulf of Mexico, shows that the island was eliminated as an effective salinity barrier between 8.86 and 8.17 ka. This event is recorded by a 5-fold increase in dinoflagellate cysts within Corpus Christi Bay. During this time, the bay-head delta shifted 15 km landward and oyster reefs within the bay died off. Our age model indicates that this event most likely resulted from the most rapid period of eustatic rise of the Holocene, which peaked at 8.18-8.31 ka. This event is attributed to late-stage ice sheet disintegration, particularly in North America, by the rapid draining of Lake Agassiz-Ojibway. Local glacial-isostatic factors resulted in a sea-level rise of only 0.2-0.56 m in the western Gulf of Mexico, which was less than needed to submerge the barrier. Rather, it was the marked nature of this sea-level rise that led to the virtual destruction of Mustang Island as an effective salinity barrier. These results provide an analog for predicting coastal morphodynamic response to accelerated sea-level rise and emphasize the need for better understanding of barrier response to sea-level rise and developing improved numerical models for predicting future changes to coastal barrier shorelines.	[Ferguson, Shannon; Warny, Sophie; White, Crawford] Louisiana State Univ, Dept Geol & Geophys, E235 Howe Russell, Baton Rouge, LA 70803 USA; [Ferguson, Shannon; Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA; [Anderson, John B.] Rice Univ, Dept Earth Sci, Houston, TX 77251 USA; [Simms, Alexander R.] Univ Calif Santa Barbara, Dept Earth Sci, Santa Barbara, CA 93106 USA; [White, Crawford] Louisiana State Univ, Coastal Studies Inst, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University; Rice University; University of California System; University of California Santa Barbara; Louisiana State University System; Louisiana State University	Ferguson, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, E235 Howe Russell, Baton Rouge, LA 70803 USA.	ferg.shannon@gmail.com	Warny, Sophie/A-8226-2013; Simms, Alexander/E-5609-2012	Simms, Alexander/0000-0001-5034-2189; Warny, Sophie/0000-0002-3451-040X	LSU Museum of Natural Science; Shell Center for Sustainability, Rice University	LSU Museum of Natural Science; Shell Center for Sustainability, Rice University	This project was funded by a curatorial assistantship from the LSU Museum of Natural Science. Sample processing was funded by the Shell Center for Sustainability, Rice University.	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J	Ellegaard, M; Godhe, A; Ribeiro, S				Ellegaard, Marianne; Godhe, Anna; Ribeiro, Sofia			Time capsules in natural sediment archives-Tracking phytoplankton population genetic diversity and adaptation over multidecadal timescales in the face of environmental change	EVOLUTIONARY APPLICATIONS			English	Review						diatom; dinoflagellate; environmental change; marine; population genetics; resting stage; sediment record	SEED BANKS; FJORD; ACIDIFICATION; VIABILITY; EVOLUTION; LINKING	Undisturbed records of resting stages produced in the past and stored in coastal sediments are very valuable to science, because they may provide unique insights into past evolutionary and ecological trajectories. Within marine phytoplankton, multidecadal time series of monoclonal strains germinated from resting stages have been established for diatoms (Skeletonema marinoi) and dinoflagellates (Pentapharsodinium dalei), spanning ca. a century. Phenotypic and genotypic analyses of these time series have revealed effects of past environmental changes on population genetic structure. Future perspectives include direct comparisons of phenotypes and genotypic data of populations, for example, by genomewide assays that can correlate phenotypic trends with genotypes and allele frequencies in temporally separated strains. Besides their usefulness as historical records, "seed" banks of phytoplankton resting stages also have the potential to provide an inoculum that influences present populations through "dispersal from the past" (the storage effect) and are important for adaptation to future environments through their standing genetic diversity.	[Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg, Denmark; [Godhe, Anna] Univ Gothenburg, Dept Marine Sci, Gothenburg, Sweden; [Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Glaciol & Climate Dept, Copenhagen K, Denmark	University of Copenhagen; University of Gothenburg; Geological Survey Of Denmark & Greenland	Ellegaard, M (通讯作者)，Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg, Denmark.	me@plen.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Ribeiro, Sofia/G-9213-2018; Ellegaard, Marianne/H-6748-2014	Ribeiro, Sofia/0000-0003-0672-9161; Ellegaard, Marianne/0000-0002-6032-3376	Villum Foundation, Denmark [VKR23454]; Swedish Research Council Formas [219-2012-2070]	Villum Foundation, Denmark(Villum Fonden); Swedish Research Council Formas(Swedish Research Council Formas)	Villum Foundation, Denmark, Grant/Award Number: VKR23454; Swedish Research Council Formas, Grant/Award Number: 219-2012-2070	Almany GR, 2009, MOL ECOL RESOUR, V9, P1460, DOI 10.1111/j.1755-0998.2009.02759.x; ANDERSEN F, 1998, MARIAGER FJORD UDVIK; Andersen TJ, 2017, DEV PALEOENVIRON RES, V20, P121, DOI 10.1007/978-94-024-0990-1_6; Becks L, 2012, ECOL LETT, V15, P492, DOI 10.1111/j.1461-0248.2012.01763.x; Blomberg A., 2010, CURRENT OPINIONS BIO, V22, P1; De Meester L, 2014, J LIMNOL, V73, P193, DOI 10.4081/jlimnol.2014.831; Ellegaard M, 2013, MICROPALEAEONTOLOGIC, P149; Ellegaard M., 2017, BIOL REV; Ellegaard M, 2006, ESTUAR COAST SHELF S, V68, P567, DOI 10.1016/j.ecss.2006.03.013; Fallesen G, 2000, J MARINE SYST, V25, P313, DOI 10.1016/S0924-7963(00)00024-5; Feifel KM, 2015, HARMFUL ALGAE, V47, P56, DOI 10.1016/j.hal.2015.05.009; Godhe A, 2016, J BIOGEOGR, V43, P1130, DOI 10.1111/jbi.12722; Godhe A, 2010, MOL ECOL, V19, P4478, DOI 10.1111/j.1365-294X.2010.04841.x; Härnström K, 2011, P NATL ACAD SCI USA, V108, P4252, DOI 10.1073/pnas.1013528108; Hairston NG, 2002, INTEGR COMP BIOL, V42, P481, DOI 10.1093/icb/42.3.481; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; Kooistra WHCF, 2008, PROTIST, V159, P177, DOI 10.1016/j.protis.2007.09.004; Krehenwinkel H, 2015, GLOBAL CHANGE BIOL, V21, P4320, DOI 10.1111/gcb.13042; Kremp A, 2016, ENVIRON MICROBIOL, V18, P679, DOI 10.1111/1462-2920.13070; Lebret K, 2012, ENVIRON MICROBIOL, V14, P2395, DOI 10.1111/j.1462-2920.2012.02769.x; Lennon JT, 2011, NAT REV MICROBIOL, V9, P119, DOI 10.1038/nrmicro2504; Lohbeck KT, 2012, NAT GEOSCI, V5, P346, DOI [10.1038/ngeo1441, 10.1038/NGEO1441]; Lundholm N, 2017, ECOL EVOL, V7, P3132, DOI 10.1002/ece3.2906; Lundholm N, 2014, J APPL PHYCOL, V26, P417, DOI 10.1007/s10811-013-0123-3; Lundholm N, 2011, PHYCOLOGIA, V50, P629, DOI 10.2216/11-16.1; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; Miyazono A, 2012, HARMFUL ALGAE, V16, P81, DOI 10.1016/j.hal.2012.02.001; Narum SR, 2011, MOL ECOL RESOUR, V11, P184, DOI 10.1111/j.1755-0998.2011.02987.x; Ribeiro S, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0061184; Ribeiro S, 2011, NAT COMMUN, V2, DOI 10.1038/ncomms1314; Rochon A., 1999, AM ASS STRATIGR PALY, V35, P146; Schlüter L, 2014, NAT CLIM CHANGE, V4, P1024, DOI 10.1038/NCLIMATE2379; Sildever S, 2016, ENVIRON MICROBIOL, V18, P4403, DOI 10.1111/1462-2920.13372; STOCKNER JG, 1970, LIMNOL OCEANOGR, V15, P41; Tesson SVM, 2014, PLOS ONE, V9, DOI 10.1371/journal.pone.0114984; WARNER RR, 1985, AM NAT, V125, P769, DOI 10.1086/284379	36	12	15	1	22	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1752-4571			EVOL APPL	Evol. Appl.	JAN	2018	11	1			SI		11	16		10.1111/eva.12513	http://dx.doi.org/10.1111/eva.12513			6	Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Evolutionary Biology	FR4VI	29302268	Green Published, gold			2025-03-11	WOS:000419064100002
J	Ottone, EG; Lovecchio, JP; Pérez-Panera, JP; Ronchi, D				Ottone, Eduardo G.; Lovecchio, Juan P.; Perez-Panera, Juan P.; Ronchi, Diana			A NEW DINOFLAGELLATE FROM THE LATE CRETACEOUS OF THE COLORADO BASIN, OFF SHORE ARGENTINA	AMEGHINIANA			English	Editorial Material							BIOSTRATIGRAPHY; CYSTS		[Ottone, Eduardo G.] Univ Buenos Aires, CONICET, Inst Estudios Andinos Don Pablo Groeber IDEAN, Dept Ciencias Geol,Fac Ciencias Exactas & Nat, Pabellon 2 Ciudad Univ,C1428EHA, Buenos Aires, DF, Argentina; [Lovecchio, Juan P.] YPF SA, Gerencia Explorac Offshore, Ave Macacha Guemes 515,C1106BKK, Buenos Aires, DF, Argentina; [Perez-Panera, Juan P.] YPF Tecnol SA, CONICET, Lab Bioestratig, Gerencia Geociencias, Ave Petr Argentino S-N Entre 129 & 143, RA-1923 Buenos Aires, DF, Argentina; [Perez-Panera, Juan P.] Museo La Plata, Catedra Micropaleontol, Div Paleozool Invertebrados, Paseo Bosque S-N, RA-1900 La Plata, Buenos Aires, Argentina; [Ronchi, Diana] YPF Tecnol SA, Lab Bioestratig, GEMA SRL, Gerencia Geociencias, Ave Petr Argentino S-N Entre 129 & 143, RA-1923 Buenos Aires, DF, Argentina	University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of La Plata; Museo La Plata	Ottone, EG (通讯作者)，Univ Buenos Aires, CONICET, Inst Estudios Andinos Don Pablo Groeber IDEAN, Dept Ciencias Geol,Fac Ciencias Exactas & Nat, Pabellon 2 Ciudad Univ,C1428EHA, Buenos Aires, DF, Argentina.	ottone@gl.fcen.uba.ar; juan.lovecchio@ypf.com; juan.p.panera@ypftecnologia.com; dianaines.ronchi@set.ypf.com	Perez Panera, Juan/HSI-3366-2023	Lovecchio, Juan Pablo/0000-0002-0831-1829; Perez Panera, Juan Pablo/0000-0002-2326-0732	Consejo Nacional de Investigaciones Cientificas y Tecnicas [112 - 201501 - 00613 - CO]; YPF Tecnologia, Laboratorio de Bioestratigrafia [Y-TEC IB - 620]	Consejo Nacional de Investigaciones Cientificas y Tecnicas(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); YPF Tecnologia, Laboratorio de Bioestratigrafia	We express our gratitude to YPF S.A. and Y-TEC for allowing the publication of this work. The authors would also thank the suggestions of the editor D. Pol, the reviewer E. Masure and a second anonymous reviewer, who helped improve the quality of this contribution. This research was partially supported by the grants 112 - 201501 - 00613 - CO (Consejo Nacional de Investigaciones Cientificas y Tecnicas) and Y-TEC IB - 620 (YPF Tecnologia, Laboratorio de Bioestratigrafia). This is the contribution R-246 of the Instituto de Estudios Andinos Don Pablo Groeber.	Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], 1894, SYSTEMATISCHE PHYLOG, DOI DOI 10.3931/E-RARA-72554-XVI,[1]-400; [Anonymous], 1914, BER DTSCH BOT GES, DOI DOI 10.1111/J.1438-8677.1914.TB07573.X; [Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1885, HG BRONNS KLASSEN OR; Archangelsky S., 1996, GEOLOGIA RECURSOS NA, p67 72; Boltenhagen E, 1977, MICROPLANCTON CRETAC; Bujak J. 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W, 1977, Initial Rep Deep Sea Drilling Project, V36, P269	53	5	5	0	3	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana		2018	55	3					343	349		10.5710/AMGH.10.01.2018.3129	http://dx.doi.org/10.5710/AMGH.10.01.2018.3129			7	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	GO3BN		Green Published			2025-03-11	WOS:000439860900007
J	Kremp, A; Hinners, J; Klais, R; Leppänen, AP; Kallio, A				Kremp, Anke; Hinners, Jana; Klais, Riina; Leppaenen, Ari-Pekka; Kallio, Antti			Patterns of vertical cyst distribution and survival in 100-year-old sediment archives of three spring dinoflagellate species from the Northern Baltic Sea	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Baltic Sea; bloom expansion; dinoflagellate cysts; eutrophication; sediment archives	SCRIPPSIELLA-HANGOEI; PHYTOPLANKTON COMMUNITIES; RESTING CYST; DINOPHYCEAE; GERMINATION; ENCYSTMENT; BLOOM; NOV; ALEXANDRIUM; VIABILITY	The history of expansion of bloom-forming cold water dinoflagellates in the Northern Baltic Sea was studied using 100-year-old sediment archives of their resting cysts. Vertical cyst distributions of Biecheleria baltica and Apocalathium malmogiense, two dinoflagellates indistinguishable by light microscopy and not recognized as distinct species in monitoring, and chain-forming Peridiniella catenata were analysed in Pb-210 and Cs-137 dated layers of a sediment core from deep, hypoxic accumulation bottoms of the Gulf of Finland. Cyst profiles showed that B. baltica and A. malmogiense were already present in the Baltic spring phytoplankton community at the beginning of the 20th century. This confirms that B. baltica, which was only recognized in the late 1980s, is a native species in the area. A drastic increase in B. baltica cyst concentrations in the 1930s to 1960s coincided with the acceleration of anthropogenic eutrophication. Large cyst deposits accumulated over several decades in the sediment which, by the 1980s, amounted to the seed stock necessary to inoculate dominant blooms. In the cyst records A. malmogiense always contributed a minor fraction of the two species. P. catenata had a relatively short cyst record in Gulf of Finland sediments despite demonstrated long-term presence in the plankton, which emphasizes that cyst-based historic surveys are not suitable for all cyst-forming dinoflagellates. This was corroborated by correspondence analyses of long-term plankton and cyst records which validated the trends from the sediment archive for B. baltica and A. malmogiense, but failed to do so for P. catenata. Germination experiments with 100-year-old cysts revealed a remarkable long-term survival capacity of A. malmogiense, making this species a suitable model for resurrection studies testing adaptation in heavily impacted systems such as the Baltic Sea.	[Kremp, Anke] Finnish Environm Inst, Marine Res Ctr, Erik Palmenin Aukio 1, Helsinki 00560, Finland; [Hinners, Jana] Univ Hamburg, Ctr Earth Syst Res & Sustainabil, Inst Hydrobiol & Fisheries Sci, Grosse Elbstr 133, D-22767 Hamburg, Germany; [Klais, Riina] Tartu Univ, Estonian Marine Inst, Maealuse 14, EE-12618 Tallinn, Estonia; [Leppaenen, Ari-Pekka; Kallio, Antti] Radiat & Nucl Safety Author STUK, Environm Surveillance & Measurement, Lahteentie 2, FI-96400 Rovaniemi, Finland; [Leppaenen, Ari-Pekka] Preparatory Commiss Comprehens Nucl Test Ban Trea, Wagramerstr 5, A-1400 Vienna, Austria	Finnish Environment Institute; University of Hamburg; University of Tartu; Estonian Marine Institute; Radiation & Nuclear Safety Authority (STUK); International Atomic Energy Agency	Kremp, A (通讯作者)，Finnish Environm Inst, Marine Res Ctr, Erik Palmenin Aukio 1, Helsinki 00560, Finland.	anke.kremp@ymparisto.fi		Kallio, Antti/0000-0002-1466-3118; Hinners, Jana/0000-0002-5145-2539	Academy of Finland [251564, 283061]; Walter and Andre de Nottbeck Foundation; Landesforschungsforderung Hamburg [LFF-OS 20-2014]; Academy of Finland (AKA) [283061] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); Walter and Andre de Nottbeck Foundation; Landesforschungsforderung Hamburg; Academy of Finland (AKA)(Research Council of Finland)	Funding was provided by the Academy of Finland (grants 251564 and 283061) and the Walter and Andre de Nottbeck Foundation (to AK). J. Hinners acknowledges the support of Landesforschungsforderung Hamburg LFF-OS 20-2014. Radionuclide measurements were done as a part of the HELCOM-MORS cooperation.	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J. Phycol.		2018	53	2					135	145		10.1080/09670262.2017.1386330	http://dx.doi.org/10.1080/09670262.2017.1386330			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	GE9JN					2025-03-11	WOS:000431546100003
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J	Filipek, A; Wysocka, A; Barski, M				Filipek, Anna; Wysocka, Anna; Barski, Marcin			"Depositional setting of the Oligocene sequence of the Western Carpathians in the Polish Spisz region - a reinterpretation based on integrated palynofacies and sedimentological analyses" - Reply	GEOLOGICAL QUARTERLY			English	Editorial Material							HUMMOCKY CROSS-STRATIFICATION; WALLED DINOFLAGELLATE CYSTS; PODHALE BASIN; CONCRETIONS; TURBIDITES		[Filipek, Anna; Wysocka, Anna; Barski, Marcin] Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland	University of Warsaw	Filipek, A (通讯作者)，Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	anniafilipek@gmail.com	Filipek, Anna/KFT-3536-2024	Filipek, Anna/0000-0003-2861-4058; Wysocka, Anna/0000-0003-1015-5033; Barski, Marcin/0000-0002-4102-3538				Alexandrowicz WP, 2013, QUATERN INT, V293, P196, DOI 10.1016/j.quaint.2012.03.004; Alexandrowicz Witold Pawel, 2006, Folia Malacologica, V14, P191; [Anonymous], 1986, Prz. Geol.; [Anonymous], 2001, Sedimentology and Stratigraphy; [Anonymous], 2002, GEOLOGICAL SOC MEMOI; [Anonymous], 1985, LECT NOTES EARTH SCI; [Anonymous], 1996, Palynology: principles and applications; [Anonymous], 1960, Ann. Soc. Geol. Pol.; Barski M, 2014, REV PALAEOBOT PALYNO, V208, P50, DOI 10.1016/j.revpalbo.2014.05.002; Barski M, 2010, GEOL CARPATH, V61, P121, DOI 10.2478/v10096-010-0005-4; BROWNE GH, 1994, J SEDIMENT RES B, V64, P40; CHOWANIEC J, 2003, WSPOLCZESNE PROBLEMY, V11, P45; Chowaniec J, 2009, B PANSTWOWEGO I GEOL, V434; Cieszkowski M, 2009, 79 ZJAZD POLSK TOW G, P29; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; Day-Stirrat RJ, 2008, CLAY CLAY MINER, V56, P100, DOI 10.1346/CCMN.2008.0560109; DECELLES PG, 1992, J SEDIMENT PETROL, V62, P555; Dumas S, 2006, GEOLOGY, V34, P1073, DOI 10.1130/G22930A.1; Filipek A, 2017, GEOL Q, V61, P859, DOI 10.7306/gq.1382; Gedl P., 2000, Studia Geologica Polonica, V117, P69; Gedl P, 2018, GEOL Q, V62, P745, DOI 10.7306/gq.1422; Janocko J., 1998, SLOVAK GEOL MAG, V4, P281; Kothe A, 2008, STRATIGRAPHISCHES VO; Ksiazkiewicz M., 1977, Tectonics, Geology of Poland, V4, P476; Ludwiniak M, 2010, ACTA GEOL POL, V60, P283; Maecka D, 2002, B PANSTWOWEGO I GEOL, V404, P145; MASTELLA L, 1975, ROCZNIK POLSKIEGO TO, V45, P361; Mulder T, 2009, SEDIMENTOLOGY, V56, P997, DOI 10.1111/j.1365-3091.2008.01014.x; Myrow PM, 2002, J SEDIMENT RES, V72, P641, DOI 10.1306/022102720641; Oszczypko N., 2008, Przeglad Geologiczny, V56, P927; Oszczypko N., 2006, ROZWOJ PALEOTEKTONIC; PLINT AG, 1991, B CAN PETROL GEOL, V39, P18; Pomar L, 2012, EARTH-SCI REV, V111, P56, DOI 10.1016/j.earscirev.2011.12.005; Powell A.J., 1992, P155; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; Radomski A., 1958, ACTA GEOL POL, V8, P335; Reineck H., 1973, DEPOSITIONAL SEDIMEN, DOI [10.1007/978-3-642-96291-22, DOI 10.1007/978-3-642-96291-22]; Sotak J, 2001, MAR PETROL GEOL, V18, P87, DOI 10.1016/S0264-8172(00)00047-7; Sotak J., 2001, SEDIMENTARY SEQUENCE, P1; Starek D, 2012, GEOL Q, V56, P67; Tinterri R., 2011, GEOACTA-BOLOGNA, V10, P43; Tinterri R, 2011, MAR PETROL GEOL, V28, P629, DOI 10.1016/j.marpetgeo.2010.07.007; Unrug R., 1979, Annales Societatis Geologorum Poloniae, V49, P3; Vandenberghe N, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P855, DOI 10.1016/B978-0-444-59425-9.00028-7; WALKER RG, 1983, GEOL SOC AM BULL, V94, P1245, DOI 10.1130/0016-7606(1983)94<1245:HSSOIV>2.0.CO;2; Williams G.L., 1985, P847; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1	47	0	0	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.		2018	62	3					751	754		10.7306/gq.1424	http://dx.doi.org/10.7306/gq.1424			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	HC4QI		gold			2025-03-11	WOS:000451788200020
J	Rogelja, M; Cibic, T; Rubino, F; Belmonte, M; Del Negro, P				Rogelja, Manja; Cibic, Tamara; Rubino, Fernando; Belmonte, Manuela; Del Negro, Paola			Active and resting microbenthos in differently contaminated marine coastal areas: insights from the Gulf of Trieste (northern Adriatic, Mediterranean Sea)	HYDROBIOLOGIA			English	Article						Microphytobenthos; Plankton resting stages; Benthic primary production; Oxygen consumption	MICROPHYTOBENTHIC PRIMARY PRODUCTION; DINOFLAGELLATE CYST ASSEMBLAGES; SUBLITTORAL SEDIMENTS; INTEGRATED APPROACH; SPECIES COMPOSITION; SURFACE SEDIMENTS; ORGANIC-CARBON; POLLUTION; NITROGEN; ABUNDANCE	Marine benthic microalgae are a promising bioindicator of contamination. To date, however, investigations on the microbenthic communities subjected to multiple stressors in natural environments are still very rare. To assess whether the benthic processes of primary production and oxygen consumption, and the structure of active and resting microbenthos, were affected by sediment contamination, seven stations were sampled in different zones of the port of Trieste, subjected to multiple and diffuse contamination, and a reference site in the Marine Reserve of Miramare. No major differences in total abundance of active microbenthos were observed among sites, but the dominance of stress-resistant species and the reduction of more sensitive ones, were registered nearby the main productive activities. The densities of resting microbenthos were higher in polluted areas, and represented by key dinoflagellate species that were clearly linked to contamination. The analysis of similarity applied to both active and resting communities significantly separated the most contaminated stations from the other ones. The photosynthetic capability of active microbenthos did not seem to be affected by contamination. The maximum oxygen consumption rates observed in sediments nearby the productive activities were likely ascribable to high organic C contents and the presence of metals in reduced chemical form.	[Rogelja, Manja; Cibic, Tamara; Del Negro, Paola] Ist Nazl Oceanog & Geofis Sperimentale OGS, Sez Oceanog, I-34151 Trieste, Italy; [Rubino, Fernando; Belmonte, Manuela] CNR, Ist Ambiente Marino Costiero, Talassog A Cerruti, I-74123 Taranto, Italy; [Rogelja, Manja] Aquarium Piran Acad Elect & Maritime High Sch, Bolniska 11, Piran 6330, Slovenia	Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR)	Cibic, T (通讯作者)，Ist Nazl Oceanog & Geofis Sperimentale OGS, Sez Oceanog, I-34151 Trieste, Italy.	tcibic@inogs.it	Belmonte, Marisol/AAG-9759-2019; Rubino, Fernando/GOP-0332-2022	Cibic, Tamara/0000-0003-1519-4891; DEL NEGRO, Paola/0000-0003-2465-4896; Rubino, Fernando/0000-0003-2552-2510	Project Bandiera 'RITMARE-La Ricerca Italiana per il Mare'; Italian Ministry for Education, University and Research; 'Autorita' Portuale di Trieste' (Port Authority of Trieste)	Project Bandiera 'RITMARE-La Ricerca Italiana per il Mare'; Italian Ministry for Education, University and Research(Ministry of Education, Universities and Research (MIUR)); 'Autorita' Portuale di Trieste' (Port Authority of Trieste)	The activities described in this study were funded by the Project Bandiera 'RITMARE-La Ricerca Italiana per il Mare' coordinated by the National Research Council (C.N.R.) and funded by the Italian 'Ministry for Education, University and Research' within the National Research Programme 2011-2013. The activities carried out within the port of Trieste were funded by the 'Autorita' Portuale di Trieste' (Port Authority of Trieste). We are very grateful to C. Comici for grain size and TOC analyses and to F. Varisco for contaminant data.	Admirall W., 1984, Progress on Phycological Research, V3, P269; Agatz M, 1999, HELGOLAND MAR RES, V53, P92, DOI 10.1007/PL00012144; [Anonymous], 1958, Mitt. Int. Ver. Theor. Angew. 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J	Kotthoff, U; Groeneveld, J; Ash, JL; Fanget, AS; Krupinski, NQ; Peyron, O; Stepanova, A; Warnock, J; Van Helmond, NAGM; Passey, BH; Clausen, OR; Bennike, O; Andrén, E; Granoszewski, W; Andrén, T; Filipsson, HL; Seidenkrantz, MS; Slomp, CP; Bauersachs, T				Kotthoff, Ulrich; Groeneveld, Jeroen; Ash, Jeanine L.; Fanget, Anne-Sophie; Krupinski, Nadine Quintana; Peyron, Odile; Stepanova, Anna; Warnock, Jonathan; Van Helmond, Niels A. G. M.; Passey, Benjamin H.; Clausen, Ole Rono; Bennike, Ole; Andren, Elinor; Granoszewski, Wojciech; Andren, Thomas; Filipsson, Helena L.; Seidenkrantz, Marit-Solveig; Slomp, Caroline P.; Bauersachs, Thorsten			Reconstructing Holocene temperature and salinity variations in the western Baltic Sea region: a multi-proxy comparison from the Little Belt (IODP Expedition 347, Site M0059)	BIOGEOSCIENCES			English	Article							BENTHIC FORAMINIFERAL MG/CA; NORTH-ATLANTIC OSCILLATION; CLUMPED ISOTOPE; CLIMATE VARIABILITY; TETRAETHER LIPIDS; DINOFLAGELLATE CYSTS; CLEANING PROCEDURES; MEMBRANE-LIPIDS; ORGANIC-MATTER; COASTAL ZONE	Sediment records recovered from the Baltic Sea during Integrated Ocean Drilling Program Expedition 347 provide a unique opportunity to study paleoenvironmental and climate change in central and northern Europe. Such studies contribute to a better understanding of how environmental parameters change in continental shelf seas and enclosed basins. Here we present a multi-proxy-based reconstruction of paleotemperature (both marine and terrestrial), paleosalinity, and paleoecosystem changes from the Little Belt (Site M0059) over the past similar to 8000 years and evaluate the applicability of inorganic- and organic-based proxies in this particular setting. All salinity proxies (diatoms, aquatic palynomorphs, ostracods, diol index) show that lacustrine conditions occurred in the Little Belt until similar to 7400 cal yr BP. A connection to the Kattegat at this time can thus be excluded, but a direct connection to the Baltic Proper may have existed. The transition to the brackish-marine conditions of the Littorina Sea stage (more saline and warmer) occurred within similar to 200 years when the connection to the Kattegat became established after similar to 7400 cal yr BP. The different salinity proxies used here generally show similar trends in relative changes in salinity, but often do not allow quantitative estimates of salinity. The reconstruction of water temperatures is associated with particularly large uncertainties and variations in absolute values by up to 8 degrees C for bottom waters and up to 16 degrees C for surface waters. Concerning the reconstruction of temperature using foraminiferal Mg / Ca ratios, contamination by authigenic coatings in the deeper intervals may have led to an overestimation of temperatures. Differences in results based on the lipid paleothermometers (long chain diol index and TEX86L) can partly be explained by the application of modern-day proxy calibrations to intervals that experienced significant changes in depositional settings: in the case of our study, the change from freshwater to marine conditions. Our study shows that particular caution has to be taken when applying and interpreting proxies in coastal environments and marginal seas, where water mass conditions can experience more rapid and larger changes than in open ocean settings. Approaches using a multitude of independent proxies may thus allow a more robust paleoenvironmental assessment.	[Kotthoff, Ulrich] Univ Hamburg, Inst Geol, D-20146 Hamburg, Germany; [Kotthoff, Ulrich] Univ Hamburg, Ctr Nat Hist, D-20146 Hamburg, Germany; [Groeneveld, Jeroen] Univ Bremen, Ctr Marine Environm Sci, MARUM, D-28359 Bremen, Germany; [Ash, Jeanine L.] UCLA, Dept Earth Planetary & Space Sci, Los Angeles, CA 90024 USA; [Fanget, Anne-Sophie; Clausen, Ole Rono; Seidenkrantz, Marit-Solveig] Aarhus Univ, Ctr Climate Studies, Dept Geosci, DK-8000 Aarhus C, Denmark; [Fanget, Anne-Sophie] Univ Perpignan, Ctr Format & Rech Environm Mediterranees, F-66860 Perpignan, France; [Krupinski, Nadine Quintana; Filipsson, Helena L.] Lund Univ, Dept Geol, S-22362 Lund, Sweden; [Peyron, Odile] Univ Montpellier, Inst Evolutionary Sci, UMR 5554, F-34095 Montpellier 05, France; [Stepanova, Anna] Texas A&M Univ, Dept Comp Sci & Engn, College Stn, TX 77843 USA; [Warnock, Jonathan] Indiana Univ Penn, Dept Geosci, Indiana, PA 15705 USA; [Van Helmond, Niels A. G. M.; Slomp, Caroline P.] Univ Utrecht, Dept Earth Sci Geochem, Fac Geosci, POB 80021, NL-3508 TA Utrecht, Netherlands; [Passey, Benjamin H.] Univ Michigan, Dept Earth & Environm Sci, Ann Arbor, MI 48109 USA; [Bennike, Ole] Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark; [Andren, Elinor; Andren, Thomas] Sodertorn Univ, Sch Nat Sci Technol & Environm Studies, S-14189 Huddinge, Sweden; [Granoszewski, Wojciech] Natl Res Inst Krakow, Polish Geol Inst, PL-31560 Krakow, Poland; [Bauersachs, Thorsten] Univ Kiel, Inst Geosci, Dept Organ Geochem, D-24118 Kiel, Germany	University of Hamburg; University of Hamburg; University of Bremen; University of California System; University of California Los Angeles; Aarhus University; Universite Perpignan Via Domitia; Lund University; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Texas A&M University System; Texas A&M University College Station; Pennsylvania State System of Higher Education (PASSHE); Indiana University of Pennsylvania; Utrecht University; University of Michigan System; University of Michigan; Geological Survey Of Denmark & Greenland; Sodertorn University; Polish Geological Institute - National Research Institute; University of Kiel	Kotthoff, U (通讯作者)，Univ Hamburg, Inst Geol, D-20146 Hamburg, Germany.; Kotthoff, U (通讯作者)，Univ Hamburg, Ctr Nat Hist, D-20146 Hamburg, Germany.	ulrich.kotthoff@uni-hamburg.de	Slomp, Caroline/A-9406-2012; Fanget, Anne-Sophie/A-7555-2015; Clausen, Ole/A-5290-2012; Passey, Benjamin/F-9644-2010; Bauersachs, Thorsten/AFY-5641-2022; Seidenkrantz, Marit-Solveig/A-3451-2012; Bennike, Ole/G-7070-2018; Filipsson, Helena/F-7419-2011	Groeneveld, Jeroen/0000-0002-8382-8019; van Helmond, Niels/0000-0003-0024-7217; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969; Clausen, Ole Rono/0000-0002-6825-9065; Stepanova, Anna/0000-0001-5927-6536; Quintana Krupinski, Nadine B./0000-0002-8853-8432; Bennike, Ole/0000-0002-5486-9946; Bauersachs, Thorsten/0000-0003-4858-9443; Filipsson, Helena/0000-0001-7200-8608; Granoszewski, Wojciech/0000-0002-1615-6777	IODP; ESSAC; German Research Foundation [KO3944/6-1, BA3841/5-1]; Carlsberg Foundation; US National Science Foundation (NSF) [T347A13]; Swedish research council VR; Swedish research council FORMAS; LAM Foundation; Crafoord Foundation; Center for Environmental and Climate Research at Lund University; Foundation for Baltic and East European Studies [1562/3.1.1/2013, 2207/3.1.1/2014]; National Science Foundation [NSF-DGE-1144087, OCE-0652315]; European Research Council (ERC) [278364]; Netherlands Organisation for Scientific Research (NWO-Vici) [865.13.005]; Geocenter Denmark	IODP; ESSAC; German Research Foundation(German Research Foundation (DFG)); Carlsberg Foundation(Carlsberg Foundation); US National Science Foundation (NSF)(National Science Foundation (NSF)); Swedish research council VR(Swedish Research Council); Swedish research council FORMAS(Swedish Research Council Formas); LAM Foundation; Crafoord Foundation; Center for Environmental and Climate Research at Lund University; Foundation for Baltic and East European Studies(Foundation for Baltic and East European Studies); National Science Foundation(National Science Foundation (NSF)); European Research Council (ERC)(European Research Council (ERC)); Netherlands Organisation for Scientific Research (NWO-Vici)(Netherlands Organization for Scientific Research (NWO)); Geocenter Denmark	This investigation used samples from IODP Expedition 347, and we are very grateful to IODP and ESSAC for funding and organizing the expedition. Stephen Obrochta, Sofia Ribeiro, Ingo Feeser, and Walter Doerfler are gratefully acknowledged for insightful discussions and comments on the age model, dinoflagellate cyst taxonomy and ecology, and the Lake Belau pollen record. We thank the crew and scientific team of IODP Expedition 347 as well as the technical staff at MARUM, Bremen, for their support during the expedition's off-and onshore phases. We are grateful for technical support from the different laboratories involved in the study. We thank Audrey Limoges, Filipa Naughton, and the anonymous referee for their detailed input to the discussion paper, and we thank Markus Kienast for editing. This research was supported by the German Research Foundation (grants KO3944/6-1 to Ulrich Kotthoff and BA3841/5-1 to Thorsten Bauersachs), the Carlsberg Foundation and Geocenter Denmark (grants to MSS and ORC), and US National Science Foundation (NSF grant no. T347A13). Thomas Andren, Jeroen Groeneveld, Nadine Quintana Krupinski, Helena L. Filipsson thank the Swedish research councils VR and FORMAS, the LAM Foundation, the Crafoord Foundation and the Center for Environmental and Climate Research at Lund University for funding. Thomas Andren and Elinor Andren acknowledge funding from The Foundation for Baltic and East European Studies (grants 1562/3.1.1/2013 and 2207/3.1.1/2014). Jeanine L. Ash was supported by the National Science Foundation (NSF-DGE-1144087 and OCE-0652315). Caroline P. Slomp and Niels A. G. M. Van Helmond acknowledge funding from the European Research Council (ERC Starting Grant 278364) and the Netherlands Organisation for Scientific Research (NWO-Vici 865.13.005).	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J	Deng, YY; Hu, ZX; Shang, LX; Peng, QC; Tang, YZ				Deng, Yunyan; Hu, Zhangxi; Shang, Lixia; Peng, Quancai; Tang, Ying Zhong			Transcriptomic Analyses of <i>Scrippsiella trochoidea</i> Reveals Processes Regulating Encystment and Dormancy in the Life Cycle of a Dinoflagellate, with a Particular Attention to the Role of Abscisic Acid	FRONTIERS IN MICROBIOLOGY			English	Article						resting cyst; harmful algal blooms (HABs); dormancy; UHPLC-MS/MS; abscisicacid (ABA); dinoflagellate; Scrippsiella trochoidea	HARMFUL ALGAL BLOOMS; GENE-EXPRESSION; SEED DORMANCY; ZEAXANTHIN EPOXIDASE; AKASHIWO-SANGUINEA; CYST PRODUCTION; PHOTOSYSTEM-I; ORYZA-SATIVA; RNA-SEQ; BIOSYNTHESIS	Due to the vital importance of resting cysts in the biology and ecology of many dinoflagellates, a transcriptomic investigation on Scrippsiella trochoidea was conducted with the aim to reveal the molecular processes and relevant functional genes regulating encystment and dormancy in dinoflagellates. We identified via RNA-seq 3,874 (out of 166,575) differentially expressed genes (DEGs) between resting cysts and vegetative cells; a pause of photosynthesis (confirmed via direct measurement of photosynthetic efficiency); an active catabolism including beta-oxidation, glycolysis, glyoxylate pathway, and TCA in resting cysts (tested via measurements of respiration rate); 12 DEGs encoding meiotic recombination proteins and members of MEI2-like family potentially involved in sexual reproduction and encystment; elevated expressions in genes encoding enzymes responding to pathogens (chitin deacetylase) and ROS stress in cysts; and 134 unigenes specifically expressed in cysts. We paid particular attention to genes pertaining to phytohormone signaling and identified 4 key genes regulating abscisic acid (ABA) biosynthesis and catabolism, with further characterization based on their full-length cDNA obtained via RACE-PCR. The qPCR results demonstrated elevated biosynthesis and repressed catabolism of ABA during the courses of encystment and cyst dormancy, which was significantly enhanced by lower temperature (4 +/- 1 degrees C) and darkness. Direct measurements of ABA using UHPLC-MS/MS and ELISA in vegetative cells and cysts both fully supported qPCR results. These results collectively suggest a vital role of ABA in regulating encystment and maintenance of dormancy, akin to its function in seed dormancy of higher plants. Our results provided a critical advancement in understanding molecular processes in resting cysts of dinoflagellates.	[Deng, Yunyan; Hu, Zhangxi; Shang, Lixia; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Deng, Yunyan; Hu, Zhangxi; Tang, Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Peng, Quancai] Chinese Acad Sci, Inst Oceanol, Res Ctr Anal & Measurement, Qingdao, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Institute of Oceanology, CAS	Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China.; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023		NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences [U1606404]; National Science Foundation of China [41476142, 41606126, 61533011, 41506143, U1301235]; Scientific and Technological Innovation Project; Qingdao National Laboratory for Marine Science and Technology [2016ASKJ02]	NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences; National Science Foundation of China(National Natural Science Foundation of China (NSFC)); Scientific and Technological Innovation Project; Qingdao National Laboratory for Marine Science and Technology	This research was financially supported by the NSFC-Shandong Joint Fund for Marine Ecology and Environmental Sciences (Grant No. U1606404), National Science Foundation of China (Grant Nos. 41476142 and 41606126), the Scientific and Technological Innovation Project Financially Supported by Qingdao National Laboratory for Marine Science and Technology (Grant No. 2016ASKJ02), and National Science Foundation of China (Grant Nos. 61533011, 41506143, and U1301235).	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Microbiol.	DEC 11	2017	8								2450	10.3389/fmicb.2017.02450	http://dx.doi.org/10.3389/fmicb.2017.02450			19	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	FP4HK	29312167	Green Published, gold			2025-03-11	WOS:000417577500001
J	Lugliè, A; Giacobbe, MG; Riccardi, E; Bruno, M; Pigozzi, S; Mariani, MA; Satta, CT; Stacca, D; Bazzoni, AM; Caddeo, T; Farina, P; Padedda, BM; Pulina, S; Sechi, N; Milandri, A				Luglie, Antonella; Giacobbe, Maria Grazia; Riccardi, Elena; Bruno, Milena; Pigozzi, Silvia; Mariani, Maria Antonietta; Satta, Cecilia Teodora; Stacca, Daniela; Bazzoni, Anna Maria; Caddeo, Tiziana; Farina, Pasqualina; Padedda, Bachisio Mario; Pulina, Silvia; Sechi, Nicola; Milandri, Anna			Paralytic Shellfish Toxins and Cyanotoxins in the Mediterranean: New Data from Sardinia and Sicily (Italy)	MICROORGANISMS			English	Article						paralytic shellfish toxins; microcystins; BMAA; Alexandrium; artificial lakes; Mediterranean	METHYLAMINO-L-ALANINE; TAMARENSE SPECIES COMPLEX; HARMFUL ALGAL BLOOMS; DINOFLAGELLATE ALEXANDRIUM-CATENELLA; CYANOBACTERIAL GENUS ANABAENA; POISONING TOXINS; LIQUID-CHROMATOGRAPHY; FLUORESCENCE DETECTION; SUBG. DOLICHOSPERMUM; CYST ASSEMBLAGES	Harmful algal blooms represent a severe issue worldwide. They affect ecosystem functions and related services and goods, with consequences on human health and socio-economic activities. This study reports new data on paralytic shellfish toxins (PSTs) from Sardinia and Sicily (Italy), the largest Mediterranean islands where toxic events, mainly caused by Alexandrium species (Dinophyceae), have been ascertained in mussel farms since the 2000s. The toxicity of the A. minutum, A. tamarense and A. pacificum strains, established from the isolation of vegetative cells and resting cysts, was determined by high performance liquid chromatography (HPLC). The analyses indicated the highest toxicity for A. pacificum strains (total PSTs up to 17.811 fmol cell(-1)). The PSTs were also assessed in a strain of A. tamarense. The results encourage further investigation to increase the knowledge of toxic species still debated in the Mediterranean. This study also reports new data on microcystins (MCs) and beta-N-methylamino-L-alanine (BMAA) from a Sardinian artificial lake (Lake Bidighinzu). The presence of MCs and BMAA was assessed in natural samples and in cell cultures by enzyme-linked immunosorbent assay (ELISA). BMAA positives were found in all the analysed samples with a maximum of 17.84 mu g L-1. The obtained results added further information on cyanotoxins in Mediterranean reservoirs, particularly BMAA, which have not yet been thoroughly investigated.	[Luglie, Antonella; Mariani, Maria Antonietta; Satta, Cecilia Teodora; Stacca, Daniela; Caddeo, Tiziana; Farina, Pasqualina; Padedda, Bachisio Mario; Pulina, Silvia; Sechi, Nicola] Univ Sassari, Dipartimento Architettura Design & Urbanist, Via Piandanna 4, I-07100 Sassari, Italy; [Giacobbe, Maria Grazia] CNR, Ist Ambiente Marino Costiero, Spianata S Raineri 86, I-98122 Messina, Italy; [Riccardi, Elena; Pigozzi, Silvia; Milandri, Anna] Fdn Ctr Ric Marine, Natl Reference Lab Marine Biotoxins, Viale A Vespucci 2, I-47042 Cesenatico, FC, Italy; [Bruno, Milena] Ist Super Sanita, Environm Qual & Fish Farming, Environm & Primary Prevent, Vle Regina Elena 299, I-00161 Rome, Italy; [Satta, Cecilia Teodora] Agenzia Reg Ric Agr AGRIS, Serv Itt, SS Sassari Fertilia Km 18, I-07040 Bonassai, Olmedo, Italy; [Bazzoni, Anna Maria] Ist Zooprofilatt Sperimentale Sardegna G Pegreffi, Dipartimento Ispez Alimenti, Via Duca Abruzzi 8, I-07100 Sassari, Italy; [Pulina, Silvia] Univ Cagliari, Dept Life & Environm Sci, Via Fiorelli 1, I-09126 Cagliari, Italy	University of Sassari; Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR); Istituto Superiore di Sanita (ISS); IZS Della Sardegna; University of Cagliari	Satta, CT (通讯作者)，Univ Sassari, Dipartimento Architettura Design & Urbanist, Via Piandanna 4, I-07100 Sassari, Italy.; Satta, CT (通讯作者)，Agenzia Reg Ric Agr AGRIS, Serv Itt, SS Sassari Fertilia Km 18, I-07040 Bonassai, Olmedo, Italy.	luglie@uniss.it; mariagrazia.giacobbe@iamc.cnr.it; elena.riccardi@centroricerchemarine.it; milena.bruno@iss.it; silvia.pigozzi@centroricerchemarine.it; marianim@uniss.it; ctsatta@uniss.it; dstacca@uniss.it; bazzoni.annamaria@tiscali.it; tcaddeo@uniss.it; pasqui81@hotmail.it; bmpadedda@uniss.it; pulinasi@uniss.it; sechi@uniss.it; anna.milandri@centroricerchemarine.it	Satta, Cecilia Teodora/AAF-6417-2020; Luglie, Antonella/M-4321-2015; PULINA, Silvia/Q-2684-2017	SATTA, Cecilia Teodora/0000-0003-0130-9432; Luglie, Antonella/0000-0001-6382-4208; Bazzoni, Anna Maria/0000-0001-7236-3845; PULINA, Silvia/0000-0002-4861-4170				Adachi M, 1996, J PHYCOL, V32, P1049, DOI 10.1111/j.0022-3646.1996.01049.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; Anglès S, 2012, HARMFUL ALGAE, V16, P1, DOI 10.1016/j.hal.2011.12.006; [Anonymous], 2003, BOCCONEA; Balech E., 1995, GENUS ALEXANDRIUM HA, P1; Banack SA, 2015, TOXINS, V7, P322, DOI 10.3390/toxins7020322; Batoréu MCC, 2005, ENVIRON TOXICOL PHAR, V19, P401, DOI 10.1016/j.etap.2004.12.002; Bazzoni AM, 2015, ENVIRON MONIT ASSESS, V187, DOI 10.1007/s10661-014-4250-3; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; Borghero G, 2014, AGING-US, V35; Bravo I, 2008, HARMFUL ALGAE, V7, P515, DOI 10.1016/j.hal.2007.11.005; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Bricelj V. 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J	Szczepanik, P; Gize, A; Sawlowicz, Z				Szczepanik, Patrycja; Gize, Andrew; Sawlowicz, Zbigniew			Pyritization of dinoflagellate cysts: A case study from the Polish Middle Jurassic (Bathonian)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Pyrite; Pyritization; Dinoflagellate cysts; Ore-bearing clays; Middle Jurassic	ORE-BEARING CLAYS; KRAKOW-SILESIA HOMOCLINE; IRON II MONOSULFIDE; 125 DEGREES-C; PYRITE FORMATION; FRAMBOIDAL PYRITE; AQUEOUS-SOLUTIONS; ORGANIC-MATTER; PALEOENVIRONMENTAL RECONSTRUCTION; CZESTOCHOWA AREA	Bathonian mudstones and claystones were deposited in a shallow epicontinental sea of the Polish Basin (the Ore Bearing Czestochowa Clay Formation). They are represented by two units, differing in stratigraphical and facies development. Dinoflagellate cyst taxa are dominated by Ctenidodinium. The effects of the environment and sedimentation rate on pyritization intensity were compared using two locations. Where the sedimentation rate was probably faster and grey mudstones were deposited under dysoxic conditions, the extent of cyst pyritization was relatively minor. In contrast, where the deposition of black claystones was slower with deposition under more suboxic conditions, very intense pyritization led to complete infilling of cysts by pyrite. Pyritization required transport of iron, probably from microbial iron reduction, and sulphide, from bacterial sulphate reduction, from the surrounding sediment into the open dinoflagellate cysts. The supply of sulphur was the limiting factor. Controls on pyrite crystal habit by the organic composition of the dinoflagellate cysts walls and cells are inferred by the observation that dinoflagellate cysts uniquely contain mainly cuboid pyrite crystals. (C) 2017 Elsevier B.V. All rights reserved.	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Palaeobot. Palynology	DEC	2017	247						1	12		10.1016/j.revpalbo.2017.07.005	http://dx.doi.org/10.1016/j.revpalbo.2017.07.005			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FP5PL					2025-03-11	WOS:000417671300001
J	Gray, DD; Zonneveld, KAF; Versteegh, GJM				Gray, Daniel D.; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.			Species-specific sensitivity of dinoflagellate cysts to aerobic degradation: A five-year natural exposure experiment	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate; Aerobic degradation; Exposure experiment; Cap Blanc; Gotland Basin	ORGANIC-MATTER DECOMPOSITION; NORTHERN NORTH-ATLANTIC; MARINE-SEDIMENTS; SURFACE SEDIMENTS; SELECTIVE PRESERVATION; CARBON PRESERVATION; SEA; OCEAN; PRODUCTIVITY; RECORD	Post-depositional sedimentary dinofiagellate cyst associations undergo species-selective degradation tinder oxic conditions. However, there is little known about the temporal relationship between oxygen concentration and bulk dinocyst degradation rate over the time scale of several years, and if this degradation is mainly microbial or chemical. Whilst the overall sensitivity of heterotrophic dinofiagellate cysts is well documented, sensitivity differences within this group have not been studied. Here we examine the rates of cyst degradation of heterotrophic species over short temporal scales across an anoxic-oxic gradient. Sediment with a known dinoflagellate cyst association largely dominated by heterotrophic dinofiagellates, were connected to trap arrays at two different locations, Cap Blanc (NW Africa) and Gotland Basin (central Baltic Sea) and exposed to four different ambient oxygen concentrations representing a complete oxic gradient from 5.1 mL/L to sulphate bearing anoxic waters. Two treatments of either gauze or dialyse membrane in triplicate were established to investigate the effects of chemical or bacterial degradation. Cyst loss was significant at oxic settings, rapidly occurring within the first year of exposure (32%) whereas no significant degradation was observed for suboxic and anoxic exposures. Compiling the degradation rates of individual species under the different exposure settings reveals an overall species sensitivity ranking amongst cysts of heterotrophic species. Species of average resistance: Bitectatodinium spongium, Brigantediniurn spp., Echinidinium spp., Echinidinium aculeatum, and Gymnodinium trapeziforme. Species more resistant than average: Stelladinium robustum and Trinovantedinium applanatum. We observe that oxic degradation of cysts of heterotrophic dinofiagellates is fast and selective with maximal cyst association changes during the first year of oxic exposure. These aspects have to be taken into account in palaeoenvironmental and palaeoceanographic reconstructions where bottom/pore water conditions of the upper sediments are oxygenated. (C) 2017 Elsevier B.V. All rights reserved.	[Gray, Daniel D.; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.] Univ Bremen, MARUM Ctr Marine Environm Sci, Fachbereich Geowissensch 5, Bremen, Germany; [Versteegh, Gerard J. M.] Helmholtz Zentntm Polar & Meeresforsch, Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany	University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Gray, DD (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Fachbereich Geowissensch 5, Bremen, Germany.	dgray@marum.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776	German Research Foundation (DFG) [ZO 114/13-1]	German Research Foundation (DFG)(German Research Foundation (DFG))	This study was carried out as part of the German Research Foundation (DFG) grant ZO 114/13-1. We thank Wolfgang Roeder and Falk Pollehne (IOW Warnemunde) for logistic support and enabling the execution of the experiment in the Gotland Basin. We are grateful to Gerhard Fischer and the MARUM Logistic group (a.o. Gotz Ruhland, Marco Klann) for logistic support and sampling during the sediment trap service cruises. We thank the editor Prof. Stephenson and the reviewers Francesca Sangiorgi and Maija Heikkila for the constructive remarks that greatly improved the manuscript.	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Palaeobot. Palynology	DEC	2017	247						175	187		10.1016/j.revpalbo.2017.09.002	http://dx.doi.org/10.1016/j.revpalbo.2017.09.002			13	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FP5PL					2025-03-11	WOS:000417671300014
J	Savelieva, YN; Shurekova, OY; Feodorova, AA; Arkadiev, VV; Grishchenko, VA; Guzhikov, AY; Manikin, AG				Savelieva, Yuliya N.; Shurekova, Olga Y.; Feodorova, Anna A.; Arkadiev, Vladimir V.; Grishchenko, Vladimir A.; Guzhikov, Andrei Yu.; Manikin, Aleksey G.			Microbiostratigraphy of the Berriasian-Valanginian boundary in eastern Crimea: foraminifers, ostracods, organic-walled dinoflagellate cysts	GEOLOGICA CARPATHICA			English	Article						Eastern Crimea; Berriasian; Valanginian; biostratigraphy; foraminifers; ostracods; organic-walled dinoflagellate cysts	VOLGA BASIN; RUSSIA	Thorough study of foraminifers, ostracods and dinoflagellate remnants from the Zavodskaya Balka and Koklyuk sections helps to characterize the detailed biostratigraphic division of the Berriasian/Valanginian boundary sequence in the Feodosiya district of eastern Crimea. The foraminifer and dinocyst associations from the lower part of the sequence are clearly comparable with common Berriasian associations throughout all Mountain Crimea. On the other hand, foraminifer, ostracod and dinocyst associations from its upper part have been recorded only in eastern Crimea. The upper foraminifer level corresponds to the boreal ammonite zones from the Tauricum-Vcrrucosum (Upper Berriasian-Valanginian). Most of the ostracod species are endemic. The base of the uppermost dinocyst level correlates with the Lower Valanginian Paratollia zone from north-western Europe.	[Savelieva, Yuliya N.; Shurekova, Olga Y.; Feodorova, Anna A.] AO Geologorazvedka, Fayansovaya Str 20-10, St Petersburg 192019, Russia; [Arkadiev, Vladimir V.] St Petersburg State Univ, Univ Emb 7-9, St Petersburg 199034, Russia; [Grishchenko, Vladimir A.; Guzhikov, Andrei Yu.; Manikin, Aleksey G.] Saratov NG Chernyshevskii State Univ, Astrakhanskaya Str 83, Saratov 410012, Russia	Saint Petersburg State University; Saratov State University	Savelieva, YN (通讯作者)，AO Geologorazvedka, Fayansovaya Str 20-10, St Petersburg 192019, Russia.	julia-savelieva7@mail.ru; o.antonen@gmail.com; annafedoroff@yandex.ru; arkadievvv@mail.ru; grishenko-vladimir@bk.ru; aguzhikov@yandex.ru; agmanikin@mail.ru	Grishchenko, Vladimir/E-9247-2019; Vladimir, Arkadiev/N-2965-2013; Shurekova, Olga/MFH-8558-2025; Guzhikov, Andrey/Q-3515-2016; Manikin, Aleksey/M-5063-2016	Shurekova, Olga/0000-0002-0446-9637; Grisenko, Vladimir/0000-0002-0268-1917; Guzhikov, Andrey/0000-0002-0579-3981; Manikin, Aleksey/0000-0002-5727-3232				Alexandrov A. 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Saint Petersburg State Univ., Ser. Geol., Geogr., V7, P32; Shurekova O. V., 2016, P 2 PAL C I PETR GEO, P182; Slipper IJ, 2009, MICROPALEAEONTOLOGIC, P309; Smith GA, 2004, REV PALAEOBOT PALYNO, V128, P355, DOI 10.1016/S0034-6667(03)00155-6; Zhamoida A.I., 2006, STRATIGRAPHIC CODE R, P1	34	9	9	0	0	SLOVAK ACAD SCIENCES GEOLOGICAL  INST	BRATISLAVA	DUBRAVSKA CESTA 9, BRATISLAVA, 840 05, SLOVAKIA	1335-0552	1336-8052		GEOL CARPATH	Geol. Carpath.	DEC	2017	68	6					517	+		10.1515/geoca-2017-0034	http://dx.doi.org/10.1515/geoca-2017-0034			15	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FP4BC		gold			2025-03-11	WOS:000417560700002
J	Mertens, KN; Gu, HF; Pospelova, V; Chomérat, N; Nézan, E; Gurdebeke, PR; Bogus, K; Vrielinck, H; Rumebe, M; Meteigner, C				Mertens, Kenneth Neil; Gu, Haifeng; Pospelova, Vera; Chomerat, Nicolas; Nezan, Elisabeth; Gurdebeke, Pieter Roger; Bogus, Kara; Vrielinck, Henk; Rumebe, Myriam; Meteigner, Claire			First record of resting cysts of the benthic dinoflagellate <i>Prorocentrum leve</i> in a natural reservoir in Gujan-Mestras, Gironde, France	JOURNAL OF PHYCOLOGY			English	Article						cellulosic; micro-FTIR; palynology; Prorocentrales; resting stage	MOLECULAR PHYLOGENY; SP-NOV; COASTAL WATERS; MIXED MODELS; DINOPHYCEAE; MORPHOLOGY; LAGOON; SOUTH; SEDIMENTS; SEA	The resting cysts of the benthic dinoflagellate Prorocentrum leve from a natural reservoir in Gujan-Mestras (Gironde, France) were described in this study. The incubated urn-shaped cysts gave rise to cells of P.leve. Morphological observations through light microscopy and scanning electron microscopy, particularly of the periflagellar platelets, combined with large subunit ribosomal DNA sequences obtained through single-cell analysis confirm their affinity to the species P.leve. The cysts were characterized by a specific shape and the presence of an anterior plug. This is the first conclusive evidence for fossilizable resting stages within the Prorocentrales, one of the major orders within theDinophyceae. Palynological treatments show that the cysts and endospores withstand hydrochloric and hydrofluoric acids. Micro-Fourier transform infrared analysis on single specimens suggests that the composition of the endospore is cellulosic and the cyst wall a more robust, noncellulosic -glucan. The spectra overall are similar to other published spectra of resting cysts from autotrophic, planktonic dinoflagellates.	[Mertens, Kenneth Neil; Chomerat, Nicolas; Nezan, Elisabeth] IFREMER, Stn Biol Marine, LER BO, Pl Croix,BP40537, F-29185 Concarneau, France; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada; [Gurdebeke, Pieter Roger] Univ Ghent, Dept Geol, Krijgslaan 281,S8, B-9000 Ghent, Belgium; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA; [Vrielinck, Henk] Univ Ghent, Dept Solid State Sci, Krijgslaan 281,S1, B-9000 Ghent, Belgium; [Rumebe, Myriam; Meteigner, Claire] IFREMER, Stn Arcachon, LER AR, F-33120 Arcachon, France	Ifremer; Third Institute of Oceanography, Ministry of Natural Resources; University of Victoria; Ghent University; Texas A&M University System; Texas A&M University College Station; Ghent University; Ifremer	Mertens, KN (通讯作者)，IFREMER, Stn Biol Marine, LER BO, Pl Croix,BP40537, F-29185 Concarneau, France.	kenneth.mertens@ifremer.fr	Gurdebeke, Pieter/AAY-7059-2020; Mertens, Kenneth/AAO-9566-2020; Vrielinck, Henk/M-8367-2016; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022	Bogus, Kara/0000-0003-4690-0576; Mertens, Kenneth/0000-0003-2005-9483; Gurdebeke, Pieter R./0000-0003-1425-8515; Meteigner, Claire/0000-0003-0063-5615; Chomerat, Nicolas/0000-0001-9691-6344; Gu, Haifeng/0000-0002-2350-9171; Pospelova, Vera/0000-0003-4049-8133	Natural Sciences and Engineering Research Council of Canada (NSERC); Hercules Foundation (Flanders) [AUGE/13/16]	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Hercules Foundation (Flanders)	Rob Fensome, Graham Williams, and Jim Riding are thanked for useful discussions regarding the cyst morphology. N. Gayet is acknowledged for critical-point drying of the samples for SEM. This research was partly supported by the Natural Sciences and Engineering Research Council of Canada (NSERC) through a Discovery grant to VP. The Hercules Foundation (Flanders) is gratefully acknowledged for financial support (FT-IMAGER project - AUGE/13/16).	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Phycol.	DEC	2017	53	6					1193	1205		10.1111/jpy.12582	http://dx.doi.org/10.1111/jpy.12582			13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	FO9JS	28865145	Green Published			2025-03-11	WOS:000417204400007
J	Tahoun, SS; Deaf, AS; Mansour, A				Tahoun, Sameh S.; Deaf, Amr S.; Mansour, Ahmed			Palynological, palaeoenvironmental and sequence stratigraphical analyses of a Turonian-Coniacian sequence, Beni Suef Basin, Eastern Desert, Egypt: Implication of <i>Pediastrum</i> rhythmic signature	MARINE AND PETROLEUM GEOLOGY			English	Article						Palynology; Palaeoenvironment; Sequence stratigraphy; Pediastrum freshwater algae; Turonian; Coniacian; Abu Roash Formation; Beni Suef Basin; Eastern Desert; Egypt	NORTH-WESTERN DESERT; EARLY CRETACEOUS PALYNOSTRATIGRAPHY; SEDIMENTARY ORGANIC-MATTER; TUNIS 1X BOREHOLE; SEA-LEVEL CHANGES; DINOFLAGELLATE CYSTS; PALYNOFACIES ANALYSIS; OIL-FIELD; FORAMINIFERAL BIOSTRATIGRAPHY; REWORKED MICROFOSSILS	Sixteen samples from the "E" to "B" members of the Abu Roash Formation encountered in the Beni Suef Basin, Eastern Desert of Egypt were palynologically analyzed for palaeoenvironmental and sequence stratigraphic investigations. The integrated palynofacies and lithofacies analysis of the studied section indicates deposition of five alternating regressive and transgressive sequences in well-oxygenated, proximal shelf settings. The Abu Roash "E" and the upper "D" to the lower "C" members were deposited during pronounced regressive phases in oxic, shallow marginal marine settings. The upper "B" Member was deposited during a recurring regressive phase but of a lower magnitude in oxic, shallow inner neritic conditions. The lower "D" Member was deposited during a minor transgression phase in dysoxic, shallow inner neritic settings. While the upper "C" to the lower "B" section was deposited during a stronger transgressive episode in a relatively deep, inner neritic environment of prominent dysoxic conditions. This interchange in the depositional setting was documented by the pronounced and concurrent, cyclic nature of the freshwater algae, peridinioid dinoflagellate cysts, pteridophyte spores, and reworked sporomorphs with variable intensities. Their increasing and conversely their diminishing trends clearly reflect alternating regressive-transgressive periods of reduced and relatively normal salinity conditions, respectively. Overall, sedimentation of the studied Abu Roash section indicates a recurring rise in sea level, which accentuated during the earliest Santonian time. The analogous peaking in the Pediastrum signals with those of the pteridophyte spores and reworked taxa indicate a good connection between these Pediastrum signals and the pronounced fluviatile influxes of terrigenous sediments during regressive phases. Accordingly, this can be used to identify regressive sequence boundaries and hence the clastic reservoirs. Even with the small counts recorded herein, we believe high ratios of peridinioid/gonyalulacoid dinocysts are significantly paralleled by peaking signals of freshwater algae and regressive sedimentation phases. This must be preliminary documented here. Probably future palynological studies will be able to fully interpret and address this important Pediastrum rhythmic event in different sequence stratigraphic settings. The palynological parameters, age controlled sporomorph marker taxa, lithology, and gamma ray data were used to differentiate the Abu Roash members into three distinctive 3rd order depositional sequences (AR SQ1, AR SQ2, and AR SQ3). These sequences match well with the global stratigraphic sequences Tu 3, Tu 4, and Co 1 and connect the local rise in sea level to the global eustatic sea level rise. (C) 2017 Elsevier Ltd. All rights reserved.	[Tahoun, Sameh S.] Cairo Univ, Geol Dept, Fac Sci, Giza 12613, Egypt; [Deaf, Amr S.] Assiut Univ, Geol Dept, Fac Sci, Assiut 71516, Egypt; [Mansour, Ahmed] Minia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt	Egyptian Knowledge Bank (EKB); Cairo University; Egyptian Knowledge Bank (EKB); Assiut University; Egyptian Knowledge Bank (EKB); Minia University	Tahoun, SS (通讯作者)，Cairo Univ, Geol Dept, Fac Sci, Giza 12613, Egypt.	stahoun@yahoo.com	Deaf, Amr/AAF-6269-2020; Mansour, Ahmed/AAR-4969-2020	Mansour, Ahmed/0000-0003-2466-7494; Tahoun, Sameh S./0000-0002-0425-8848; Deaf, Amr/0000-0002-5073-7911				Abd-Elshafy E., 2002, Egyptian Journal of Paleontology, V2, P157; ABDALLAH H, 1995, CRETACEOUS RES, V16, P487, DOI 10.1006/cres.1995.1034; Abdel-Kireem M R., 1993, Geoscientific Research in Northeast Africa, P375; Abdel-Kireem M. 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J	Lau, WLS; Law, IK; Liow, GR; Hii, KS; Usup, G; Lim, PT; Leaw, CP				Lau, Winnie Lik Sing; Law, Ing Kuo; Liow, Guat Ru; Hii, Kieng Soon; Usup, Gires; Lim, Po Teen; Leaw, Chui Pin			Life-history stages of natural bloom populations and the bloom dynamics of a tropical Asian ribotype of <i>Alexandrium minuturn</i>	HARMFUL ALGAE			English	Article						HAB dynamics; Paralytic shellfish poisoning (PSP); Planozygote; Resting cyst; Saxitoxin	DINOFLAGELLATE GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE; CYST FORMATION; PHYLOGENETIC ANALYSIS; GYRODINIUM-UNCATENUM; CELL-CYCLE; DINOPHYCEAE; GROWTH; BAY; SEXUALITY	In 2015, a remarkably high density bloom of Alexandrium minutum occurred in Sungai Geting, a semi enclosed lagoon situated in the northeast of Peninsular Malaysia, causing severe discoloration and contaminated the benthic clams (Polymesoda). Plankton and water samples were collected to investigate the mechanisms of bloom development of this toxic species. Analysis of bloom samples using flow cytometry indicated that the bloom was initiated by the process of active excystment, as planomycetes (>4C cells) were observed in the early stage of the bloom. Increase in planozygotes (2C cells) was evident during the middle stage of the bloom, coinciding with an abrupt decrease in salinity and increase of temperature. The bloom was sustained through the combination of binary division of vegetative cells, division of planozygotes, and cyst germination through continuous excystment. Nutrient depletion followed by precipitation subsequently caused the bloom to terminate. This study provides the first continuous record of in situ life-cycle stages of a natural bloom population of A. minutum through a complete bloom cycle. The event has provided a fundamental understanding of the pelagic life-cycle stages of this tropical dinoflagellate, and demonstrated a unique bloom development characteristic shared among toxic Alexandrium species in coastal embayments. (C) 2017 Elsevier B.V. All rights reserved.	[Lau, Winnie Lik Sing; Law, Ing Kuo; Liow, Guat Ru; Hii, Kieng Soon; Lim, Po Teen; Leaw, Chui Pin] Univ Malaya, Inst Ocean & Earth Sci, Bachok 16310, Kelantan, Malaysia; [Usup, Gires] Univ Kebangsaan Malaysia, Fac Sci & Technol, Bangi 43600, Malaysia	Universiti Malaya; Universiti Kebangsaan Malaysia	Lim, PT; Leaw, CP (通讯作者)，Univ Malaya, Inst Ocean & Earth Sci, Bachok 16310, Kelantan, Malaysia.	ptlim@um.edu.my; chuipinleaw@gmail.com	Hii, Kieng/R-2176-2017; Leaw, Chui Pin/F-5220-2012; Lim, Po Teen/C-9758-2013	Leaw, Chui Pin/0000-0003-3336-1438; Hii, Kieng Soon/0000-0001-6905-3045; Lim, Po Teen/0000-0003-2823-0564	Malaysian government through the Ministry of Higher Education under HICoE Fund [IOES-2014C]; Ministry of Science, Technology and Innovation [04-01-03-SF1011]; JSPS Core-to-Core Program; Ministry of Higher Education MyBrain Scholarship	Malaysian government through the Ministry of Higher Education under HICoE Fund; Ministry of Science, Technology and Innovation(Ministry of Energy, Science, Technology, Environment and Climate Change (MESTECC), Malaysia); JSPS Core-to-Core Program(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Ministry of Higher Education MyBrain Scholarship	This work was funded by the Malaysian government through the Ministry of Higher Education under HICoE Fund [IOES-2014C]; and Ministry of Science, Technology and Innovation under Sciencefund [04-01-03-SF1011]. We acknowledged the research networking of JSPS Core-to-Core Program. WLS Lau was supported by the Ministry of Higher Education MyBrain Scholarship, and this work formed part of her MSc project. This work is dedicated to the memory of Prof. Paul J. Harrison (UBC).[SS]	ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; 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], 1998, PHYSL ECOLOGY HARMFU; Bajarias F. 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J	Santos, A; Carvalho, MD; de Oliveira, AD; Mendonça, JG				Santos, Alessandra; Carvalho, Marcelo de Araujo; de Oliveira, Antonio Donizeti; Mendonca Filho, Joao Graciano			Paleoenvironmental changes and influence on <i>Operculodinium centrocarpum</i> during the Quaternary in the Campos Basin, southwestern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Operculodinium centrocarpum; Dinoflagellate cysts; Quaternary; Campos Basin; Brazil	WALLED DINOFLAGELLATE CYSTS; NORTHERN NORTH-ATLANTIC; SEA-SURFACE CONDITIONS; BENTHIC FORAMINIFERA; CONTINENTAL-MARGIN; SOUTHERN BRAZIL; ADJACENT SEAS; SEDIMENTS; OCEAN; PLEISTOCENE	The purpose of this paper is to document the changes observed in the Quaternary dinoflagellate assemblages from 80 core samples from the Campos Basin. The Interglacial (Subzone X1), Glacial (Subzones Y5 to Y2), Last Glacial Maximum (Subzone Y1) and Post-Glacial (Zone Z) intervals were identified. High abundance of Operculodinium centrocarpum suggests the warm, high salinity and nutrient-poor water conditions dominated the upper water column of the Campos Basin. The climate and oceanic current dynamic of the continental slope of the Campos Basin appears to has been a significant controlling factor in the distribution of dinocysts, particularly of O. centrocarpum, during the Pleistocene/Holocene transition. (C) 2017 Elsevier Ltd. All rights reserved.	[Santos, Alessandra] Univ Vale Rio dos Sinos UNISINOS, Itt Fossil, Inst Tecnol Micropaleontol, Av Unisinos 950, BR-93022750 Sao Leopoldo, RS, Brazil; [Carvalho, Marcelo de Araujo] Univ Fed Rio de Janeiro, Museu Nacl, Lab Paleoecol Vegetal, Dept Geol & Paleontol, Quinta da Boa Vista S-N, BR-20940040 Sao Cristovao, RJ, Brazil; [de Oliveira, Antonio Donizeti; Mendonca Filho, Joao Graciano] Univ Fed Rio de Janeiro, Inst Geociencias, Dept Geol, Lab Palinofacies & Facies Organ LAFO, Av Athos da Silveira,274 Predio CCMN, BR-21949900 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro	Santos, A (通讯作者)，Univ Vale Rio dos Sinos UNISINOS, Itt Fossil, Inst Tecnol Micropaleontol, Av Unisinos 950, BR-93022750 Sao Leopoldo, RS, Brazil.	alessandrass@unisinos.br	Carvalho, Marcelo/G-8463-2015; Mendonca Filho, Joao Graciano/C-2098-2013	Mendonca Filho, Joao Graciano/0000-0001-8997-0270				[Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Caddah LFG, 1998, SEDIMENT GEOL, V115, P159, DOI 10.1016/S0037-0738(97)00091-2; CHANG YI-MAW, 1967, J PALEONTOL, V41, P500; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Mahiques MM, 2004, CONT SHELF RES, V24, P1685, DOI 10.1016/j.csr.2004.05.013; de Mahiques MM, 2002, MAR GEOL, V181, P387; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2007, DEV MARINE GEOL, V1, P371, DOI 10.1016/S1572-5480(07)01014-7; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; ERICSON DB, 1968, SCIENCE, V162, P1227, DOI 10.1126/science.162.3859.1227; Gu F, 2017, QUATERNARY SCI REV, V172, P55, DOI 10.1016/j.quascirev.2017.06.028; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Helenes J, 1998, AAPG BULL, V82, P1308; Iudice J.H., 1977, THESIS; Krebs CJ., 1989, ECOLOGICAL METHODOLO; Ledru MP, 1996, PALAEOGEOGR PALAEOCL, V123, P239, DOI 10.1016/0031-0182(96)00105-8; Machado L.C.R., 1998, INT C EXH TULS, V1, P408; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Mudie P.J., 1996, American Association of Stratigraphic Palynology Foundation, P843; Nagai RH, 2009, QUATERN INT, V206, P62, DOI 10.1016/j.quaint.2008.10.014; Oliveira A. 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J	Correia, VF; Riding, JB; Duarte, LV; Fernandes, P; Pereira, Z				Correia, Vania F.; Riding, James B.; Duarte, Luis V.; Fernandes, Paulo; Pereira, Zelia			The palynological response to the Toarcian Oceanic Anoxic Event (Early Jurassic) at Peniche, Lusitanian Basin, western Portugal	MARINE MICROPALEONTOLOGY			English	Article						Palaeobiology; Palynomorphs; Provincialism; Toarcian Oceanic Anoxic Event (T-OAE); Lusitanian Basin, Portugal	PLIENSBACHIAN-EARLY TOARCIAN; CARBON-ISOTOPE EXCURSION; MIDDLE TOARCIAN; PALEOENVIRONMENTAL CHANGE; CALCAREOUS NANNOFOSSILS; ENVIRONMENTAL-CHANGES; CYST PALEOECOLOGY; NEUQUEN BASIN; SEA-LEVEL; RECORD	The uppermost Pliensbachian and lower Toarcian (Lower Jurassic) succession exposed at Peniche in the central part of the Lusitanian Basin, western Portugal, was examined for palynomorphs. The 45 samples span the Emaciaticeras emaciatum, Dactylioceras polyrnorphum and Hildaites levisoni ammonite biozones (ABs), and the succession includes the Global boundary Stratotype Section and Point (GSSP) for the Toarcian Stage and the Toarcian Oceanic Anoxic Event (T-OAE). A low diversity dinoflagellate cyst flora, typical of the Sub-Boreal Realm, was recovered from the Emaciaticeras emaciatum and Dactylioceras polymotphum ABs. The dominant element is the cold water species Luehndea spinosa, which is an index for the Pliensbachian to earliest Toarcian, and is thought to have migrated from the more northerly Boreal Realm. Prior to the T-OAE, dinoflagellates thrived in the Lusitanian Basin, except during a brief warm period in the earliest Toarcian. Despite the latter, the recovery from this event was relatively rapid and was characterised by a return to relatively cool temperatures. The Hildaites levisoni AB at Peniche represents the T-OAE and the overlying strata, and is characterised by a profound reduction in dinoflagellate cyst relative abundances. This dinoflagellate cyst 'blackout', and the associated rise of prasinophytes, reflects significant environmental stress, such as marine anoxia, elevated temperatures and reduced salinity, with the former two probably being most important. The low proportions of dinoflagellate cysts following the T-OAE indicates a protracted recovery phase from the bottom and water column anoxia developed throughout the Lusitanian Basin.	[Correia, Vania F.; Fernandes, Paulo] Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal; [Correia, Vania F.; Pereira, Zelia] LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal; [Riding, James B.] British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, England; [Duarte, Luis V.] Univ Coimbra, Dept Earth Sci, Fac Sci & Technol, MARE Marine & Environm Sci Ctr, Rua Silvio Lima, P-3030790 Coimbra, Portugal	Universidade do Algarve; Laboratorio Nacional de Energia e Geologia IP (LNEG); UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universidade de Coimbra	Correia, VF (通讯作者)，Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal.	vania.correia@lneg.pt; jbri@bgs.ac.uk; lduarte@dct.uc.pt; pfernandes@ualg.pt; zelia.pereira@lneg.pt	Pereira, Zelia/B-2740-2017; Fernandes, Paulo/J-6577-2014; Duarte, Luis/F-5282-2013	Pereira, Zelia/0000-0003-3056-6219; Fernandes, Paulo/0000-0003-4888-0230; Correia, Vania/0000-0001-5648-3185; Duarte, Luis/0000-0002-9025-5896	Portuguese Foundation for Science and Technology (FCT) [SFRH/BD/93950/2013]; FCT [UID/MAR/04292/2013]; Fundação para a Ciência e a Tecnologia [UID/MAR/04292/2013, SFRH/BD/93950/2013] Funding Source: FCT; NERC [bgs05017] Funding Source: UKRI	Portuguese Foundation for Science and Technology (FCT)(Fundacao para a Ciencia e a Tecnologia (FCT)); FCT(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The contribution of Vania F. Correia is part of PhD scholarship number SFRH/BD/93950/2013 awarded by the Portuguese Foundation for Science and Technology (FCT). Luis V. Duarte was supported by FCT strategic project number UID/MAR/04292/2013 granted to the Marine and Environmental Sciences Centre, Coimbra, Portugal. We thank Filipe Barreira (LNEG) for his invaluable help with drafting the figures. Jan A.I. Hennissen (BGS) kindly reviewed an early draft of this contribution. The helpful comments of two anonymous reviewers and the editor, Professor Frans Jorissen (University of Angers, France), substantially improved this contribution. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC).	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Micropaleontol.	DEC	2017	137						46	63		10.1016/j.marmicro.2017.10.004	http://dx.doi.org/10.1016/j.marmicro.2017.10.004			18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	FP5PG		Green Accepted			2025-03-11	WOS:000417670800004
J	Panitz, S; De Schepper, S; Salzmann, U; Bachem, PE; Risebrobakken, B; Clotten, C; Hocking, EP				Panitz, Sina; De Schepper, Stijn; Salzmann, Ulrich; Bachem, Paul E.; Risebrobakken, Bjorg; Clotten, Caroline; Hocking, Emma P.			Mid-Piacenzian Variability of Nordic Seas Surface Circulation Linked to Terrestrial Climatic Change in Norway	PALEOCEANOGRAPHY			English	Article						dinoflagellate cysts; Norwegian Atlantic Current; Arctic Front; northward heat transport; obliquity forcing; late Pliocene	DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; PROCESS LENGTH VARIATION; LATE PLIOCENE; OVERTURNING CIRCULATION; MARINE-SEDIMENTS; NORWEGIAN SEA; NORTH PACIFIC; BLACK-SEA; CYSTS; PLEISTOCENE	During the mid-Piacenzian, Nordic Seas sea surface temperatures (SSTs) were higher than today. While SSTs provide crucial climatic information, on their own they do not allow a reconstruction of potential underlying changes in water masses and currents. A new dinoflagellate cyst record for Ocean Drilling Program (ODP) Site 642 is presented to evaluate changes in northward heat transport via the Norwegian Atlantic Current (NwAC) between 3.320 and 3.137Ma. The record is compared with vegetation and SST reconstructions from Site 642 and SSTs from Iceland Sea ODP Site 907 to identify links between SSTs, ocean currents, and vegetation changes. The dinocyst record shows that strong Atlantic water influence via the NwAC corresponds to higher-than-present SSTs and cool temperate vegetation during Marine Isotope Stage (MIS) transition M2-M1 and KM5. Reduced Atlantic water inflow relative to the warm stages coincides with near-modern SSTs and boreal vegetation during MIS M2, KM6, and KM4-KM2. During most of the studied interval, a strong SST gradient between Sites 642 and 907 indicates the presence of a proto-Arctic Front (AF). An absent gradient during the first half of MIS KM6, due to reduced Atlantic water influence at Site 642 and warm, presumably Atlantic water reaching Site 907, is indicative of a weakened NwAC and East Greenland Current. We conclude that repeated changes in Atlantic water influence directly affect terrestrial climate and that an active NwAC is needed for an AF to develop. Obliquity forcing may have played a role, but the correlation is not consistent. Plain Language Summary At present, northward heat transport via the Norwegian Atlantic Current (NwAC) is a major reason for the mild climate in Norway. For the warmer-than-present late Pliocene (approximately 3.0-3.3Ma), it is unclear if changes in northward heat transport affected the Norwegian Sea and Scandinavian climate. We analyzed fossil dinoflagellate cysts in Ocean Drilling Program Hole 642B to reconstruct changes in the influence of the NwAC during the late Pliocene. We found that strong NwAC influence and changes in insolation are responsible for warmer-than-present climatic conditions in Norway. In contrast, reduced NwAC influence is associated with similar-to-present climatic conditions on land. These results highlight that changes in northward heat transport via the NwAC and insolation changes control late Pliocene climate changes in Norway.	[Panitz, Sina; Salzmann, Ulrich; Hocking, Emma P.] Northumbria Univ, Fac Engn & Environm, Dept Geog, Newcastle Upon Tyne, Tyne & Wear, England; [De Schepper, Stijn; Bachem, Paul E.; Risebrobakken, Bjorg; Clotten, Caroline] Uni Res Climate, Bjerknes Ctr Climate Res, Bergen, Norway	Northumbria University; Bjerknes Centre for Climate Research	Panitz, S (通讯作者)，Northumbria Univ, Fac Engn & Environm, Dept Geog, Newcastle Upon Tyne, Tyne & Wear, England.	sina.panitz@gmail.com	Hocking, Emma/Q-6241-2019; Risebrobakken, Bjorg/Y-1551-2018; Salzmann, Ulrich/H-9929-2017; De Schepper, Stijn/A-2836-2011; Hocking, Emma/K-8292-2013	Risebrobakken, Bjorg/0000-0002-7206-2193; Salzmann, Ulrich/0000-0001-5598-5327; Bachem, Paul/0000-0002-6927-3934; De Schepper, Stijn/0000-0002-6934-0914; Hocking, Emma/0000-0002-8925-1695	Norwegian Research Council [221712, 229819]; European Consortium for Ocean Research Drilling (ECORD)	Norwegian Research Council(Research Council of Norway); European Consortium for Ocean Research Drilling (ECORD)	We acknowledge the International Ocean Drilling Program for providing the samples. We thank M. Jones (Palynological Laboratory Services LtD) and L. Dunlop (Northumbria University) for their help with the preparation of samples. The work is a contribution to the "Ocean Controls on high-latitude Climate sensitivity-a Pliocene case study" (OCCP) project funded by the Norwegian Research Council (project 221712). S. D. S. is grateful for support from the Norwegian Research Council (project 229819). S. P. acknowledges funding received from the European Consortium for Ocean Research Drilling (ECORD). The dinocyst data presented here are available in the supporting information and the alkenone SST for ODP Site 907 at https://doi.pangaea.de/10.1594/PANGAEA.877309. We thank J. Matthiessen and H. Dowsett for the constructive comments on the manuscript.	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F, 2013, CONTRIBUTION WORKING; STOCKMARR J, 1971, Pollen et Spores, V13, P615; Swift J., 1986, NORDIC SEAS, P129, DOI DOI 10.1007/978-1-4615-8035-5_5; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Verleye TJ, 2009, PALYNOLOGY, V33, P77; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Williams G.L., 2017, American Association of Stratigraphic Palynologists, Contribution series, V48, P1097; Zhang ZS, 2013, CLIM PAST, V9, P1495, DOI 10.5194/cp-9-1495-2013; Zhang ZS, 2013, NAT COMMUN, V4, DOI 10.1038/ncomms2521; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	91	4	4	0	28	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0883-8305	1944-9186		PALEOCEANOGRAPHY	Paleoceanography	DEC	2017	32	12					1336	1351		10.1002/2017PA003166	http://dx.doi.org/10.1002/2017PA003166			16	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	FR0PH		Green Accepted, Green Submitted, Green Published			2025-03-11	WOS:000418764600002
J	Nikitenko, BL; Devyatov, VP; Lebedeva, NK; Basov, VA; Goryacheva, AA; Pestchevitskaya, EB; Glinskikh, LA				Nikitenko, B. L.; Devyatov, V. P.; Lebedeva, N. K.; Basov, V. A.; Goryacheva, A. A.; Pestchevitskaya, E. B.; Glinskikh, L. A.			Jurassic and Cretaceous stratigraphy of the New Siberian Archipelago (<i>Laptev and East Siberian Seas</i>): facies zoning and lithostratigraphy	RUSSIAN GEOLOGY AND GEOPHYSICS			English	Article						Jurassic; Cretaceous; facies division; stratigraphy; foraminifera; ostracods; dinoflagellate cysts; spores and pollen; Arctic; New Siberian Islands	STOLBOVOI-ISLAND; SEDIMENTS	Mesozoic sections in the New Siberian Archipelago are important for understanding of the geology of underexplored shelf areas in the east of the Laptev Sea and in the west of the East Siberian Sea. They are reference sections for interpretation of seismic data in these regions. However, there are still many unresolved problems concerning the lithology, lateral extent, and age of Mesozoic deposits, as the sections have a complex structure and are heavily deformed. The performed research makes a basis for the first facies zoning of Jurassic and Cretaceous deposits in the New Siberian Islands and adjacent landmasses of continental Siberia at the junction of the Laptev and East Siberian Seas. The lithostratigraphic division of the Jurassic and Cretaceous is refined, being proposed for the first time for some stratigraphic intervals, and allows updating their lithostratigraphic division (or undertaking it for the first time for some stratigraphic intervals). Facies features of Jurassic and Cretaceous deposits allow the definition of three depositional series. (C) 2017, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.	[Nikitenko, B. L.; Lebedeva, N. K.; Goryacheva, A. A.; Pestchevitskaya, E. B.; Glinskikh, L. A.] Russian Acad Sci, Siberian Branch, AA Trofimuk Inst Petr Geol & Geophys, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia; [Nikitenko, B. L.; Lebedeva, N. K.; Goryacheva, A. A.] Novosibirsk State Univ, Ul Pirogova 2, Novosibirsk 630090, Russia; [Devyatov, V. P.] Siberian Res Inst Geol Geophys & Mineral Resource, Novosibirsk 630091, Russia; [Basov, V. A.] IS Gramberg Russian Res Inst Marine Geol & Minera, Angliiskii Pr 1, St Petersburg 190121, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences; Novosibirsk State University	Nikitenko, BL (通讯作者)，Russian Acad Sci, Siberian Branch, AA Trofimuk Inst Petr Geol & Geophys, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia.; Nikitenko, BL (通讯作者)，Novosibirsk State Univ, Ul Pirogova 2, Novosibirsk 630090, Russia.	NikitenkoBL@ipgg.sbras.ru	Nikitenko, Boris/S-9028-2017; Glinskikh, Larisa/Y-8646-2018; Natalia, Lebedeva/T-6040-2017; Anna, Goryacheva/T-5116-2017	Natalia, Lebedeva/0000-0002-7192-8303; Anna, Goryacheva/0000-0002-9012-7376; Glinskikh, Larisa/0000-0001-8241-188X; Pestchevitskaya, Ekaterina/0000-0001-8174-0737	Russian Science Foundation [14-37-00030]; Russian Science Foundation [14-37-00030] Funding Source: Russian Science Foundation	Russian Science Foundation(Russian Science Foundation (RSF)); Russian Science Foundation(Russian Science Foundation (RSF))	The study was supported by grant 14-37-00030 from the Russian Science Foundation.	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J	Martini, E; Schiller, W				Martini, Erlend; Schiller, Wolfgang			Contribution to the biodiversity of the lower Frankfurt Formation (Miocene) in the Hanau Basin (Germany): a new <i>Hymenomonas</i> (calcareous nannoplankton) and a new <i>Scrippsiella</i> (dinoflagellate) species	PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS			English	Article						Biodiversity; Calcareous Nannoplankton; Dinoflagellates; Miocene; Frankfurt Formation; Hanau Basin; Germany	SP-NOV; TAXONOMIC CLARIFICATION; MARINE DINOFLAGELLATE; PERIDINIALES; THORACOSPHAERACEAE; DINOPHYCEAE; TROCHOIDEA	Fine-grained calcareous sediments often contain mass occurrences of well-preserved micro- and nannofossils, providing a wide range for biodiversity studies and enable to establish index-fossils. In our research, we depicted very tiny nannofossils which might be easily overlooked. Two new species Hymenomonas kelleri (calcareous nannoplankton) and Scrippsiella francofurtana (dinoflagellate, calcareous resting stage) are described, representing ecologically important forms. Their stratigraphic occurrence is documented from the lower part of the Frankfurt Formation (Miocene, Upper Hydrobia Beds). The collected sediment samples were taken from the temporary excavation site "WestendDuo" tower in the city of Frankfurt/Main, Germany. Both extremely small species show exceptionally fine structures and only slight signs of diagenesis. Their association with remains of further dinoflagellates and other species of algae (S. francofurtana together with a mass occurrence of the calcareous nannoplankton species Coccolithus pelagicus) as well as stromatoliths, shells of gastropods (Hydrobia species) and skeletons of fishes (Gobius species) gives hints to a highly diversed former biocoenosis and to a characteristic Miocene thanatocoenosis. Furthermore, a new mass occurrence of nannoplankton named layer +21 is described.	[Martini, Erlend] Parkstr 40, D-61476 Kronberg, Germany; [Schiller, Wolfgang] Goethe Univ, Inst Geowissensch, Altenhoferallee 1, D-60438 Frankfurt, Germany	Goethe University Frankfurt	Schiller, W (通讯作者)，Goethe Univ, Inst Geowissensch, Altenhoferallee 1, D-60438 Frankfurt, Germany.	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J	Natsuike, M; Saito, R; Fujiwara, A; Matsuno, K; Yamaguchi, A; Shiga, N; Hirawake, T; Kikuchi, T; Nishino, S; Imai, I				Natsuike, Masafumi; Saito, Rui; Fujiwara, Amane; Matsuno, Kohei; Yamaguchi, Atsushi; Shiga, Naonobu; Hirawake, Toru; Kikuchi, Takashi; Nishino, Shigeto; Imai, Ichiro			Evidence of increased toxic <i>Alexandrium tamarense</i> dinoflagellate blooms in the eastern Bering Sea in the summers of 2004 and 2005	PLOS ONE			English	Article							LAWRENCE ESTUARY CANADA; CHUKCHI SEA; SHELF; WATER; ABUNDANCE; IMPACTS; CYSTS	The eastern Bering Sea has a vast continental shelf, which contains various endangered marine mammals and large fishery resources. Recently, high numbers of toxic A. tamarense resting cysts were found in the bottom sediment surface of the eastern Bering Sea shelf, suggesting that the blooms have recently occurred. However, little is known about the presence of A. tamarense vegetative cells in the eastern Bering Sea. This study's goals were to detect the occurrence of A. tamarense vegetative cells on the eastern Bering Sea shelf and to find a relationship between environmental factors and their presence. Inter-annual field surveys were conducted to detect A. tamarense cells and environmental factors, such as nutrients, salinity, chlorophyll a, and water temperature, along a transect line on the eastern Bering Sea shelf during the summers of 2004, 2005, 2006, 2009, 2012, and 2013. A. tamarense vegetative cells were detected during every sampling year, and their quantities varied greatly from year to year. The maximum cell densities of A. tamarense observed during the summers of 2004 and 2005 were much higher than the Paralytic shellfish poisoning warning levels, which are greater than 100-1,000 cells L-1, in other subarctic areas. Lower quantities of the species occurred during the summers of 2009, 2012, and 2013. A significant positive correlation between A. tamarense quantity and water temperature and significant negative correlations between A. tamarense quantity and nutrient concentrations (of phosphate, silicate, and nitrite and nitrate) were detected in every sampling period. The surface- and bottom-water temperatures varied significantly from year to year, suggesting that water temperatures, which have been known to affect the cell growth and cyst germination of A. tamarense, might have affected the cells' quantities in the eastern Bering Sea each summer. Thus, an increase in the Bering Sea shelf's water temperature during the summer will increase the frequency and scale of toxic blooms and the toxin contamination of plankton feeders. This poses serious threats to humans and the marine ecosystem.	[Natsuike, Masafumi; Matsuno, Kohei; Yamaguchi, Atsushi; Shiga, Naonobu; Hirawake, Toru; Imai, Ichiro] Hokkaido Univ, Grad Sch Fisheries Sci, Hakodate, Hokkaido, Japan; [Saito, Rui] Ehime Univ, Ctr Marine Environm Studies, Matsuyama, Ehime, Japan; [Fujiwara, Amane; Kikuchi, Takashi; Nishino, Shigeto] Japan Agcy Marine Earth Sci & Technol, Yokosuka, Kanagawa, Japan; [Natsuike, Masafumi] Tokyo Inst Technol, Sch Environm & Soc, Tokyo, Japan; [Shiga, Naonobu] Hakodate Jr Coll, Hakodate, Hokkaido, Japan	Hokkaido University; Ehime University; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); Institute of Science Tokyo; Tokyo Institute of Technology	Natsuike, M (通讯作者)，Hokkaido Univ, Grad Sch Fisheries Sci, Hakodate, Hokkaido, Japan.; Natsuike, M (通讯作者)，Tokyo Inst Technol, Sch Environm & Soc, Tokyo, Japan.	natsuike.m.aa@m.titech.ac.jp	Saito, Reiko/B-9410-2015; Matsuno, Kohei/AAJ-6510-2021; Yamaguchi, Atsushi/A-8613-2012	Hirawake, Toru/0000-0003-0274-6642; NISHINO, Shigeto/0000-0002-0560-241X; Matsuno, Kohei/0000-0001-9793-7622; Yamaguchi, Atsushi/0000-0002-5646-3608	Japan Society for the Promotion of Science (JSPS) [24248032, 24110005]; GRENE Arctic Climate Change Research Project; Grants-in-Aid for Scientific Research [17H01483, 15H05712, 15KK0268] 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); GRENE Arctic Climate Change Research 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))	This study was supported by Grant-in-Aid for Scientific Research (A) 24248032 to AY, Grant-in-Aid for Scientific Research on Innovative Areas 24110005 to AY from the Japan Society for the Promotion of Science (JSPS), and GRENE Arctic Climate Change Research Project to SN. 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	Mitta, VV; Savelieva, YN; Feodorova, AA; Shurekova, OV				Mitta, V. V.; Savelieva, Yu. N.; Feodorova, A. A.; Shurekova, O. V.			Biostratigraphy of the Bajocian-Bathonian Boundary Beds in the Basin of the Bolshoi Zelenchuk River (Northern Caucasus)	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Bajocian; Bathonian; biostratigraphy; ammonites; foraminifers; ostracodes; dinocysts; spores; pollen; Northern Caucasus	OSTRACODS; GERMANY; RUSSIA	The study of ammonites from the upper part of the upper Bajocian and lower part of the lower Bathonian in the sections of the basin of the Bolshoi Zelenchuk (Karachay-Cherkessia) allowed the recognition of Beds with Parkinsonia djanelidzei (approximate equivalent of the middle part of the Parkinsonia parkinsoni Chronozone) and Beds with Oraniceras scythicum (lower part of the Zigzagiceras zigzag Chronozone). The taxonomic composition and distribution of foraminifers, ostracodes, dinoflagellate cysts, and miospores were studied in the samples from these deposits (upper part of the upper member of Djangura Formation). The recognized characteristic assemblages of microfauna and palynomorphs allowed ostracode and dinocyst subdivisions to be proposed for the Bajocian-Bathonian boundary beds of the Northern Caucasus for the first time. The most important taxa, including ammonites, foraminifers, ostracodes, and dinocysts, are illustrated.	[Mitta, V. V.] Russian Acad Sci, Borissiak Paleontol Inst, Ul Profsoyuznaya 123, Moscow 117997, Russia; [Mitta, V. V.] Cherepovets State Univ, Pr Lunacharskogo 5, Cherepovets 162600, Russia; [Savelieva, Yu. N.; Feodorova, A. A.; Shurekova, O. V.] Geologorazvedka, Ul Knipovich 11-2, St Petersburg 192019, Russia	Russian Academy of Sciences; Paleontological Institute of the Russian Academy of Sciences; Cherepovets State University	Mitta, VV (通讯作者)，Russian Acad Sci, Borissiak Paleontol Inst, Ul Profsoyuznaya 123, Moscow 117997, Russia.; Mitta, VV (通讯作者)，Cherepovets State Univ, Pr Lunacharskogo 5, Cherepovets 162600, Russia.	mitta@paleo.ru	Shurekova, Olga/MFH-8558-2025; Mitta, Vasily/O-2682-2018	Shurekova, Olga/0000-0002-0446-9637; Mitta, Vasily/0000-0001-7041-2295	Presidium of the Russian Academy of Sciences [28]	Presidium of the Russian Academy of Sciences(Russian Academy of Sciences)	We are grateful to M.P. Sherstyukov (Stavropol) for friendly assistance during fieldwork; E.M. Tesakova (Moscow State University), who was consulted for the ostracode identification; S.V. Bagirov (Paleontological Institute, Russian Academy of Sciences) for ammonite photography; L.A. Kartseva (Botanical Institute, Russian Academy of Sciences) for ostracode photography; E.S. Platonov ("Geologorazvedka") for technical assistance in preparation and photography of foraminifers; and V.A. Basov (VNIIOkeangeologiya) and V.A. Zakharov and M.A. Rogov (Geological Institute, Russian Academy of Sciences) for helpful advice during the preparation of the manuscript. We are grateful to all those who helped with the preparation and publication of this research. This study was supported by the Program of the Presidium of the Russian Academy of Sciences, no. 28.	Antonova Z.A., 1975, T IGIG SO AN SSSR, V333, P214; Antonova Z.A., 1958, T VNIGNI PROC ALL RU, V12, P213; Antonova Z. A., 1958, T VSES NEFTEGAZ NAUC, VXVII, P41; Antonova Z.A, 1960, GEOL SB T KRASNODAR, V4, P191; Azbel' A.Ya., 1991, PRAKTICHESKOE RUKOVO, V5; Bate R. H., 1967, Bulletin of the British Museum (Natural History) Geology, V14, P21; Bate RH, 2009, MICROPALEAEONTOLOGIC, P199; Beher Elke, 2010, Palaeodiversity, P43; Besnosov N.V., 1958, YURSKIE AMMONITY SEV; Besnosov N.V., 1998, B KF VNIGNI, P1; Besnosov N.V., 1993, Late Bajocian and Bathonian Ammonites from the Northern Caucasus and Central Asia; Blaszyk J., 1967, Acta Palaeontologica Polonica, V12, P1; Borissjak A, 1908, MEMOIRES COMITE GEOL, V37, P1; Brand E, 1990, BIOSTRATIGRAPHISCHE, P119; DEPECHE F, 1985, B CTR RECHERCHES EXP, V9, P119; Depeche F, 1984, MEM SCI TERRE U PIER, P1; DODEKOVA L, 1990, Geologica Balcanica, V20, P3; Feist-Burkhardt S, 1997, B CENT RECH EXPL, V21, P31; Fernández-López SR, 2009, SWISS J GEOSCI, V102, P271, DOI 10.1007/s00015-009-1317-1; Franz M, 2014, NEUES JAHRB GEOL P-A, V274, P149, DOI 10.1127/0077-7749/2014/0431; Franz Matthias, 2009, Palaeodiversity, P119; Glinskikh L.A., 2015, Jurassic System of Russia: Problems of Stratigraphy and Paleogeography, P60; Gorbachik T. 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M., 1978, Foraminifers and Ostracods of the Jurassic of Ukraine; Riding J.B., 1992, P7; Shurekova O.V., 2015, YURSKAYA SISTEMA ROS, P309; Temirbekova U.T., 1985, TRIASOVYE YURSKIE MI; Temirbekova U.T., 1978, (Stratigraphy and Microfauna of the Bajocian and Bathonian Deposits of Dagestan (Miliolids and Biostratigraphy of the Bajocian and Bathonian Deposits of Dagestan)),; Tesakova Ekaterina M., 2008, Senckenbergiana Lethaea, V88, P55; Triebel E., 1951, Abhandlungen der Senckenbergischen Naturforschenden Gesellschaft, VNo. 485, P87; YAROSHENKO OP, 1965, T GEOL I AKAD NAUK S, V117; Zatwornitzky A.Ya., 1914, Izv. Geol. Kom, V33, P525	46	16	16	0	1	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	NOV	2017	25	6					607	626		10.1134/S0869593817060065	http://dx.doi.org/10.1134/S0869593817060065			20	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	FT6OT					2025-03-11	WOS:000423274200002
J	Brosnahan, ML; Ralston, DK; Fischer, AD; Solow, AR; Anderson, DM				Brosnahan, Michael L.; Ralston, David K.; Fischer, Alexis D.; Solow, Andrew R.; Anderson, Donald M.			Bloom termination of the toxic dinoflagellate <i>Alexandrium catenella</i>: Vertical migration behavior, sediment infiltration, and benthic cyst yield	LIMNOLOGY AND OCEANOGRAPHY			English	Article							GONYAULAX-TAMARENSIS; PHYTOPLANKTON BLOOMS; RESTING CYSTS; LIFE-CYCLE; CAPE-COD; DINOPHYCEAE; ENCYSTMENT; FUNDYENSE; ESTUARINE; DYNAMICS	New resting cyst production is crucial for the survival of many microbial eukaryotes including phytoplankton that cause harmful algal blooms. Production in situ has previously been estimated through sediment trap deployments, but here was instead assessed through estimation of the total number of planktonic cells and new resting cysts produced by a localized, inshore bloom of Alexandrium catenella, a dinoflagellate that is a globally important cause of paralytic shellfish poisoning. Our approach utilizes high frequency, automated water monitoring, weekly observation of new cyst production, and pre- and post-bloom spatial surveys of total resting cyst abundance. Through this approach, new cyst recruitment within the study area was shown to account for at least 10.9%+/- 2.6% (SE) of the bloom's decline, approximate to 5x greater than reported from comparable, sediment trap based studies. The observed distribution and timing of new cyst recruitment indicate that: (1) planozygotes, the immediate precursor to cysts in the life cycle, migrate nearer to the water surface than other planktonic stages and (2) encystment occurs after planozygote settlement on bottom sediments. Near surface localization by planozygotes explains the ephemerality of red surface water discoloration by A. catenella blooms, and also enhances the dispersal of new cysts. Following settlement, bioturbation and perhaps active swimming promote sediment infiltration by planozygotes, reducing the extent of cyst redistribution between blooms. The concerted nature of bloom sexual induction, especially in the context of an observed upper limit to A. catenella bloom intensities and heightened susceptibility of planozygotes to the parasite Amoebophrya, is also discussed.	[Brosnahan, Michael L.; Fischer, Alexis D.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Ralston, David K.] Woods Hole Oceanog Inst, Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA; [Solow, Andrew R.] Woods Hole Oceanog Inst, Marine Policy Ctr, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution	Brosnahan, ML (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	mbrosnahan@whoi.edu	Fischer, Alexis/M-4531-2019	Ralston, David/0000-0002-0774-3101; Brosnahan, Michael/0000-0002-2620-7638; Fischer, Alexis/0000-0002-8028-487X	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]; MIT Sea Grant [NA14OAR4170077]; Woods Hole Sea Grant [NA14OAR4170074, R/P-84]; National Park Service (NPS) [H238015504]; 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; MIT Sea Grant; Woods Hole Sea Grant; National Park Service (NPS); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	Special thanks to Robert Olson for assistance in modification of the Imaging FlowCytobot, Micheil Boesel for technical assistance in the development of the observatory raft and its profiling winch, Heidi Sosik for assistance with image analysis, David Kulis, Madeline McKenna, Jennifer Haskell, and other staff and student members of the Anderson lab for assistance in collection and analysis of field samples, to Sophia Fox and Krista Lee (National Park Service) for nutrient analyses, and to other National Park Service staff at the Cape Cod National Seashore and Michael O'Connor, Dick Hilmer, and others at the Eastham Department of Natural Resources for assistance at the Salt Pond study site. 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, MIT Sea Grant (NA14OAR4170077), Woods Hole Sea Grant (NA14OAR4170074, R/P-84), and National Park Service (NPS) Cooperative Agreement H238015504.	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A., 1973, BRIT PHYCOL J, V8, P105, DOI DOI 10.1080/00071617300650141; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	64	40	47	1	27	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0024-3590	1939-5590		LIMNOL OCEANOGR	Limnol. Oceanogr.	NOV	2017	62	6					2829	2849		10.1002/lno.10664	http://dx.doi.org/10.1002/lno.10664			21	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	FN3WB	29263558	hybrid, Green Published			2025-03-11	WOS:000415930800033
J	Mustapha, KA; Abdullah, WH; Konjing, Z; Gee, SS; Koraini, AM				Mustapha, Khairul Azlan; Abdullah, Wan Hasiah; Konjing, Zainey; Gee, Sia Say; Koraini, Ahmad Munif			Organic geochemistry and palynology of coals and coal-bearing mangrove sediments of the Neogene Sandakan Formation, Northeast Sabah, Malaysia	CATENA			English	Article						Mangrove sediments; Miocene; Sandakan Formation; Petroleum; Paleobiogeography	BIOSYNTHETIC PATHWAYS; MARINE INFLUENCE; SOURCE ROCKS; BASIN; BOTRYOCOCCUS; INDICATORS; EVOLUTION; STEROLS; BORNEO; MODEL	The coals and coal-bearing mangrove sediments of Sandakan Formation have been evaluated for their source rock potential, paleoredox conditions and source of organic input, as well as the age and paleovegetation distribution using geochemical and petrographical methods. The studied samples were generally rich in organic carbon, which varied from 0.60 (massive mudstone) to 62.37 wt% (coal). The studied samples have vitrinite reflectance (R-o) ranging from 0.31 to 0.49% and Tmax values ranging from 353 to 436 degrees C indicating an immature to very early mature stage for hydrocarbon generation. The sediments were dominated by Type III kerogen, with some Type II/Ill kerogen, suggesting a significant land plant contribution to the organic matter. The bimodal distribution displayed by gas chromatogram, with a clear odd/even carbon number and skewed to higher molecular weight carbon (nC(31)), Indicating a transitional depositional environment. The variation in pristane/phytane ratio, varied from 0.71 to 2.97, suggesting an alternating anoxic and oxic deposition conditions. The presence of marine dinoflagellate cyst in the mangrove and offshore mudstones were consistent with the relatively higher sulphur content in the studied samples which indicate marine inundations. Palynomorph recovered in this study, with abundant mangrove and freshwater types of pollen, suggesting a biogeographical distribution of ancient mangrove vegetation that expanded landward into the freshwater peat swamp setting and hinterland. The presence of marker species, viz. Florschuetzia levipoli, F. meridionalis and F. semilobata delineated an Early Miocene to Middle Miocene age for the Sandakan sediments.	[Mustapha, Khairul Azlan; Abdullah, Wan Hasiah; Gee, Sia Say] Univ Malaya, Fac Sci, Dept Geol, Kuala Lumpur 50603, Malaysia; [Konjing, Zainey; Koraini, Ahmad Munif] Biostratex Sdn Bhd, Unit 1A,Jalan Perusahaan 4, Selayang 68100, Selangor, Malaysia	Universiti Malaya	Mustapha, KA (通讯作者)，Univ Malaya, Fac Sci, Dept Geol, Kuala Lumpur 50603, Malaysia.	azian.geo@gmail.com	Konjing, Zainey/AAI-5894-2021; Mustapha, Khairul/H-4345-2011	MUSTAPHA, KHAIRUL AZLAN/0000-0001-9768-9219	University of Malaya; Ministry of Higher Education of Malaysia, under SLAB programme; University of Malaya through Center of Research Grant Management (PPGP);  [CG048-2013];  [BK085-2016]	University of Malaya(Universiti Malaya); Ministry of Higher Education of Malaysia, under SLAB programme; University of Malaya through Center of Research Grant Management (PPGP); ; 	This research is part of the first author's PhD project which was sponsored by University of Malaya and Ministry of Higher Education of Malaysia, under SLAB programme. University of Malaya is acknowledged for the research grant awarded through Center of Research Grant Management (PPGP). The research is partially funded by CG048-2013 and BK085-2016 research grants. The authors also would like to sincerely thank to Prof. Dr. Karl Stahr and anonymous reviewers for their critical reviews and constructive comments that improved the revised manuscript.	Abubaker T., 2004, MALAYS J SCI, V23, P165; Alongi DM, 2015, AGR FOREST METEOROL, V213, P266, DOI 10.1016/j.agrformet.2014.10.005; ANDERSON JAR, 1975, REV PALAEOBOT PALYNO, V19, P291, DOI 10.1016/0034-6667(75)90049-4; [Anonymous], 1992, THESIS; CALDER JH, 1991, B SOC GEOL FR, V162, P283; Clayton J L., 1993, Hydrocarbons from Coal. Am. Assoc. Petrol. Geol. 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J	Post, K; Louwye, S; Lambert, O				Post, Klass; Louwye, Stephen; Lambert, Oliver			<i>Scaldiporia vandokkumi</i>, a new pontoporiid (Mammalia, Cetacea, Odontoceti) from the Late Miocene to earliest Pliocene of the Westerschelde estuary (The Netherlands)	PEERJ			English	Article						Cetacea; Inioidea; Pontoporiidae; Westerschelde; The Netherlands; Late Miocene; earliest Pliocene	DINOFLAGELLATE CYST; DOLPHIN CETACEA; PISCO FORMATION; INIOID CETACEA; MIDDLE MIOCENE; NORTH; NEOGENE; RECORD; BRACHYDELPHIS; STRATIGRAPHY	Background. The family Pontoporiidae (Cetacea, Odontoceti Inioidea) is currently represented in our oceans by just one species of diminutive dolphin (Pontoporia blainvillei, franciscana). Although P. blainvillei is limited to coastal waters of the South Atlantic along Brazil, Uruguay and Argentina, multiple Miocene and Pliocene fossils indicate the past presence of members of the family in the South Atlantic, South Paciifc and North Atlantic oceans. Our comprehension of the origin and diversity of this clade and of the relationships of its members with other inioids is hampered by the fact that part of the described fossil specimens, especially from the North Atlantic realm, are cranial fragments often associated to limited stratigraphic information. Methods. Based on an almost complete fossil cranium of pontoporiid from the Westerschelde estuary, The Netherlands, whose preservation allows for detailed morphological observations, we describe a new genus and species. The latter is compared to other pontoporiids, as well as 'a few non-pontoporiid inioids. A phylogenetic analysis is performed to investigate the relationship of S. vandokkumi with the best-known extinct and extant inioids. Palynological analysis of the sediment associated to the holotype is used to assess its geological age. Results and discussion. The new genus and species Scaldiporia vandokkurni is characterized among others by greatly thickened premaxillary eminences reaching the level of the antorbital notch. Palynologically dated from the late Tortonian earliest Zanclean (7,6-5 Ma, Late Miocene earliest Pliocene), this new pontoporiid confirms the surprising past diversity of marine inioids in the North Atlantic area. Finally the content of the pontoporiid subfamily Brachydelphininae is briefly discussed,	[Post, Klass] Nat Hist Museum Rotterdam, Rotterdam, Netherlands; [Louwye, Stephen] Univ Ghent, Paleontol Res Unit, Ghent, Belgium; [Lambert, Oliver] Inst Royal Sci Nat Belgique, DO Terre & Hist Vie, Brussels, Belgium	Ghent University	Post, K (通讯作者)，Nat Hist Museum Rotterdam, Rotterdam, Netherlands.	klaaspost@fishcon.nl	Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Lambert, Olivier/0000-0003-0740-5791; Louwye, Stephen/0000-0003-4814-4313				Abel O., 1905, Memoires du Musee royal d'histoire naturelle de Belgique, V3, P1; Aguirre-Fernández G, 2017, J VERTEBR PALEONTOL, V37, DOI 10.1080/02724634.2017.1315817; Bianucci G, 2016, J MAPS, V12, P1037, DOI 10.1080/17445647.2015.1115785; Bianucci G, 2016, J MAPS, V12, P543, DOI 10.1080/17445647.2015.1048315; Bianucci G, 2013, J VERTEBR PALEONTOL, V33, P741, DOI 10.1080/02724634.2013.734888; Bianucci G, 2013, GEODIVERSITAS, V35, P105, DOI 10.5252/g2013n1a6; Brownell R.L. 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Jr, 2008, Virginia Museum of Natural History Special Publication, V14, P181	55	11	12	0	11	PEERJ INC	LONDON	341-345 OLD ST, THIRD FLR, LONDON, EC1V 9LL, ENGLAND	2167-8359			PEERJ	PeerJ	NOV 1	2017	5								e3991	10.7717/peerj.3991	http://dx.doi.org/10.7717/peerj.3991			29	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	FL4KX	29109917	Green Published, gold, Green Submitted			2025-03-11	WOS:000414199600005
J	Schrank, E				Schrank, Eckart			Palynology of the Albian Makhtesh Qatan site, northern Negev (Israel), with descriptions of two new pollen species	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Albian; Palynology; Pollen; Spores; Negev; Israel	EARLY CRETACEOUS TETRADS; WESTERN DESERT; ANGIOSPERM POLLEN; ZONASULCULATE POLLEN; WINTERACEOUS POLLEN; LUSITANIAN BASIN; SOUTHERN ISRAEL; POTOMAC GROUP; EGYPT; PALYNOSTRATIGRAPHY	Three levels of an independently dated Early Cretaceous succession in the northern Negev have yielded palynofloras of Albian age. The Afropollis jardinus-Tricolpites-Trisectoris-Qatanipollis Assemblage is from the lowermost level, a shale bed of about 60 cm thickness intercalated in the predominantly fluvial sandstones of the upper Hatira Formation at Makhtesh Qatan (IQ1 locality).The IQ1 palynoflora is dominated by psilatrilete spores, which are interpreted as influx from a fern bog. Altogether 46 formal and informal taxa were identified among the pteridophytic and bryophytic spores of this locality. The gymnosperms yielded 33 taxa including the new species Partitisporites krassilovii. The angiosperms are represented by 36 mono- and triaperturate species including Afropollis jardinus, the new species Foveomonocolpites ravnii and representatives of the genera Foveotricolpites, Qatanipollis, Rousea, Tricolpites and Trisectoris. A middle Albian age of this assemblage is supported by correlation of the IQ1 level with a marine intercalation, the Uza marine tongue of middle-late Albian age and by the strati graphic position of the IQ1 bed below the ammonite-dated late Albian lower Hazera (Hevyon) Formation at Makhtesh Ramon. Immediately above the dark grey palyniferous IQ1 shale, grey or light grey shales occur, which are either barren or yielded the remains of a weathered, residual palynoflora with freshwater algae such as Botryococcus and Ovoidites. The upper Hatira Formation discussed so far is overlain by the marine carbonates of the Hazera (= Hevyon Formation). The lower part of this formation yielded at Makhtesh Ramon a late Albian ammonite (Hypengonoceras, Lewy), which is associated with an elaterate pollen-bearing assemblage corresponding largely to the Afropollis jardinus-Elaterosporites klaszii Assemblage recovered by the author from the same formation and locality. In contrast to the spore-dominated IQ1 Assemblage, the late Albian palynoflora from Makhtesh Ramon (Miz7/6) is dominated by Classopollis, followed by psilatrilete spores and dinoflagellate cysts. The IQ1 palynoflora reflects high humidity and influence from a vegetation rich in ferns, while the abundance of Classopollis (Cheirolepidiaceae) in the late Albian sample may suggest a shift towards drier conditions. 2017 Elsevier B.V. All rights reserved.	[Schrank, Eckart] TU Berlin, Inst Angew Geowissensch, Sekr ACK 1-1,Ackerstr 76, D-13355 Berlin, Germany	Technical University of Berlin	Schrank, E (通讯作者)，TU Berlin, Inst Angew Geowissensch, Sekr ACK 1-1,Ackerstr 76, D-13355 Berlin, Germany.	e.schrank@tu-berlin.de			GIF (German-Israeli Foundation for Scientific Research and Development) [I-888-159.8/2005]	GIF (German-Israeli Foundation for Scientific Research and Development)(German-Israeli Foundation for Scientific Research and Development)	This article is dedicated to the memory of the late Professor Valentin Krassilov who invited me many years ago to join him and his team in a project on the fossil record of angiosperms in the Middle East. This project was supported by GIF (German-Israeli Foundation for Scientific Research and Development, no. I-888-159.8/2005) and included three field trips (2007 - 2009) under the guidance of Professor Krassilov, which enabled me to sample the Cretaceous sections in the Negev on which this paper is based.	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J	Mertens, KN; Takano, Y; Gu, HF; Bagheri, S; Pospelova, V; Pienkowski, AJ; Leroy, SAG; Matsuoka, K				Mertens, Kenneth N.; Takano, Yoshihito; Gu, Haifeng; Bagheri, Siamak; Pospelova, Vera; Pienkowski, Anna J.; Leroy, Suzanne A. G.; Matsuoka, Kazumi			Cyst-Theca Relationship and Phylogenetic Position of <i>Impagidinium caspienense</i> Incubated from Caspian Sea Surface Sediments: Relation to <i>Gonyaulax baltica</i> and Evidence for Heterospory within Gonyaulacoid Dinoflagellates	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Ataxiodinium choane; Baltic Sea; Impagidinium pallidum; Pyxidinopsis psilata; salinity; Spiniferites belerius; Spiniferites ramosus	MOTILE STAGE RELATIONSHIPS; LAST 2000 YEARS; PALYNOLOGICAL EVIDENCE; LATE PLEISTOCENE; SP-NOV; HOLOCENE; SALINITY; BLACK; DINOPHYCEAE; ASSEMBLAGES	We investigate the cyst-theca relationship of Impagidinium caspienense. Through an incubation experiment, we succeeded in examining the motile stage. Additional molecular analysis of single-cyst PCR (LSU and SSU rDNA) reveal that the cyst is related to the species Gonyaulax baltica Ellegaard et al. (2002). The ability of this species to belong to two types of cyst-based genera (spiniferate and impagidinioid) suggests that environmental (particularly salinity) and not genetic factors explain the formation of both morphotypes by G. baltica, which provides evidence for heterospory in this species. The affiliation to G. baltica demonstrates that I. caspienense is not endemic to the Caspian Sea. The phylogenetic position of several other gonyaulacoid species is also documented: Impagidinium pallidum, Ataxiodinium choane, Pyxidinopsis psilata, Spiniferites belerius, and Spiniferites ramosus. The LSU and SSU rDNA based phylogenies suggest that the genera Impagidinium and Spiniferites are not monophyletic, and that P. psilata and A. choane are close to Gonyaulax verior and Gonyaulax polygramma, respectively. In addition, this study accentuates the importance of cyst morphology in the classification of the Gonyaulacales.	[Mertens, Kenneth N.] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France; [Takano, Yoshihito; Matsuoka, Kazumi] Inst East China Sea Res ECSER, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Bagheri, Siamak] AREEO, Inland Waters Aquaculture Res Ctr, Iranian Fisheries Sci Inst, Anzali 66, Iran; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB A405,POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada; [Pienkowski, Anna J.] MacEwan Univ, Dept Phys Sci, Edmonton, AB T5J 4S2, Canada; [Pienkowski, Anna J.] Bangor Univ, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales; [Leroy, Suzanne A. G.] Brunel Univ London, Inst Environm, Uxbridge UB8 3PH, Middx, England	Ifremer; Third Institute of Oceanography, Ministry of Natural Resources; University of Victoria; Bangor University; Brunel University	Mertens, KN (通讯作者)，IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France.	kenneth.mertens@ifremer.fr	Mertens, Kenneth/AAO-9566-2020; Pieńkowski, Anna/AAL-1312-2020; Bagheri, Siamak/S-2035-2016; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022; Pienkowski, Anna/J-9339-2013	Mertens, Kenneth/0000-0003-2005-9483; Gu, Haifeng/0000-0002-2350-9171; Pospelova, Vera/0000-0003-4049-8133; Pienkowski, Anna/0000-0002-3606-7130	Natural Science and Engineering Research Council of Canada (NSERC); Marie Curie Integration Grant [FP7-PEOPLE-2011-CIG 304178]; NSERC (Discovery Grant)	Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Marie Curie Integration Grant(European Union (EU)Marie Curie Actions); NSERC (Discovery Grant)(Natural Sciences and Engineering Research Council of Canada (NSERC))	K.N.M. thanks Anna Godhe for providing surface sediment from Kattegat, Marianne Ellegaard for assistance with SEM during his stay in Copenhagen, and David Wall for discussions regarding Ataxiodinium. The Natural Science and Engineering Research Council of Canada (NSERC) is acknowledged for partial funding of this project to V.P. (Discovery Grant). The VENUS (Victoria Experimental Network Under the Sea), ONC (Ocean Networks Canada), R/V Thompson, and ROPOS (Remotely Operated Platform, Canadian Scientific Submersible Facility) teams are thanked for their assistance with sample collection in the Strait of Georgia. A.J.P. acknowledges funding by a Marie Curie Integration Grant (FP7-PEOPLE-2011-CIG 304178) and NSERC (Discovery Grant). Two anonymous reviewers and the associate editor are acknowledged for constructive comments that improved the manuscript.	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J	Björk, G; Nordberg, K; Arneborg, L; Bornmalm, L; Harland, R; Robijn, A; Ödalen, M				Bjork, Goran; Nordberg, Kjell; Arneborg, Lars; Bornmalm, Lennart; Harland, Rex; Robijn, Ardo; Odalen, Malin			Seasonal oxygen depletion in a shallow sill fjord on the Swedish west coast	JOURNAL OF MARINE SYSTEMS			English	Article						Oxygen conditions; Hypoxia; Shallow fjord; Swedish west coast	MARINE BENTHIC HYPOXIA; GULLMAR FJORD; RECENT SEDIMENTS; DINOFLAGELLATE CYSTS; HYDROGRAPHIC DATA; ALGAL MATS; SKAGERRAK; SWEDEN; WATERS; FORAMINIFERA	During the summer of 2008, oxygen depleted water, between 5 and 12 m depth, was discovered in Sannasfjord on the Swedish west coast. The resulting sediments were black, benthic macrofauna were absent and Beggiatoa bacterial mats were a characteristic feature. This phenomenon, which was observed several years in a row, appears to be a relatively new phenomenon starting in the mid-1980s. In this study we attempt to find the underlying causes by investigating climatic effects (temperature, wind and precipitation), the local supply of nutrients from land, ecosystem change and the supply of organic material from the open Skagerrak. An analysis of long meteorological time series indicates that climatic effects are contributory, but probably not a dominating factor leading to hypoxia. Results from an advection-diffusion model solving for oxygen show that the observed increase in the river supply of nutrients has a high potential to generate hypoxia. Although complex and more difficult to quantify, it appears that ecosystem changes, with higher abundance of filamentous algae, may have played an important role. It is also possible that an enhanced supply of organic material from the open Skagerrak has contributed. (C) 2017 Elsevier B.V. All rights reserved.	[Bjork, Goran; Nordberg, Kjell; Arneborg, Lars; Bornmalm, Lennart; Robijn, Ardo] Univ Gothenburg, Dept Marine Sci, POB 460, SE-40530 Gothenburg, Sweden; [Harland, Rex] 50 Long Acre, Nottingham NG13 BAH, England; [Odalen, Malin] Stockholm Univ, Dept Meteorol MISU, SE-10691 Stockholm, Sweden; [Arneborg, Lars] SMHI, Sven Kallfelts Gata 15, SE-42671 Vastra Frolunda, Sweden	University of Gothenburg; Stockholm University; Swedish Meteorological & Hydrological Institute	Björk, G (通讯作者)，Univ Gothenburg, Dept Marine Sci, POB 460, SE-40530 Gothenburg, Sweden.	goran.bjork@marine.gu.se		Nordberg, Kjell/0000-0003-0085-4607; Arneborg, Lars/0000-0003-0248-8110; Robijn, Ardo/0000-0002-1160-9992	Region Vastra Gotaland "RUN MN" [612-0125-08]; County Administrative Board O-Lan; Wahlstroms Foundation; Lars Hierta Memorial Foundation; Department of Earth Sciences; Tanum Community Administration; Department of Marine Sciences (University of Gothenburg)	Region Vastra Gotaland "RUN MN"; County Administrative Board O-Lan; Wahlstroms Foundation; Lars Hierta Memorial Foundation; Department of Earth Sciences; Tanum Community Administration; Department of Marine Sciences (University of Gothenburg)	The authors sincerely thank everyone who helped to perform this study. The crews of R/V Skagerak and R/V Nereus assisted during sampling campaigns 2008 and 2009. We acknowledge the funding by Region Vastra Gotaland "RUN & MN" (ref 612-0125-08) (KN), County Administrative Board O-Lan and Tanum Community Administration (KN). Also we gratefully acknowledge Wahlstroms Foundation and Lars Hierta Memorial Foundation (KN) and the Department of Earth Sciences and Department of Marine Sciences (from July I, 2015) (University of Gothenburg) for the PhD student (AR) fellowship. RH acknowledges the efficient palynological processing undertaken by Mr. David Bodman of the Palynological Laboratories at the University of Sheffield, UK.	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J	Hardeland, R				Hardeland, Ruediger			Taxon- and Site-Specific Melatonin Catabolism	MOLECULES			English	Review						5-methoxytryptamine; CNS; dinoflagellates; indole metabolism; kynuramines; plants; yeast	METABOLITE N-1-ACETYL-5-METHOXYKYNURAMINE AMK; PINEAL-GLAND; NITRIC-OXIDE; BRAIN METABOLITE; ARYL ACYLAMIDASE; INDOLEAMINE 2,3-DIOXYGENASE; CYCLIC 3-HYDROXYMELATONIN; CEREBROSPINAL-FLUID; FREE-RADICALS; 5-METHOXYTRYPTAMINE	Melatonin is catabolized both enzymatically and nonenzymatically. Nonenzymatic processes mediated by free radicals, singlet oxygen, other reactive intermediates such as HOCl and peroxynitrite, or pseudoenzymatic mechanisms are not species- or tissue-specific, but vary considerably in their extent. Higher rates of nonenzymatic melatonin metabolism can be expected upon UV exposure, e.g., in plants and in the human skin. Additionally, melatonin is more strongly nonenzymatically degraded at sites of inflammation. Typical products are several hydroxylated derivatives of melatonin and N-1-acetyl-N-2-formyl-5-methoxykynuramine (AFMK). Most of these products are also formed by enzymatic catalysis. Considerable taxon- and site-specific differences are observed in the main enzymatic routes of catabolism. Formation of 6-hydroxymelatonin by cytochrome P-450 subforms are prevailing in vertebrates, predominantly in the liver, but also in the brain. In pineal gland and non-mammalian retina, deacetylation to 5-methoxytryptamine (5-MT) plays a certain role. This pathway is quantitatively prevalent in dinoflagellates, in which 5-MT induces cyst formation and is further converted to 5-methoxyindole-3-acetic acid, an end product released to the water. In plants, the major route is catalyzed by melatonin 2-hydroxylase, whose product is tautomerized to 3-acetamidoethyl-3-hydroxy-5-methoxyindolin-2-one (AMIO), which exceeds the levels of melatonin. Formation and properties of various secondary products are discussed.	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K., 1999, STUDIES ANTIOXIDANTS, P136; Zsizsik BK, 2002, COMP BIOCHEM PHYS C, V133, P383, DOI 10.1016/S1532-0456(02)00126-6	144	45	45	2	19	MDPI	BASEL	ST ALBAN-ANLAGE 66, CH-4052 BASEL, SWITZERLAND		1420-3049		MOLECULES	Molecules	NOV	2017	22	11							2015	10.3390/molecules22112015	http://dx.doi.org/10.3390/molecules22112015			23	Biochemistry & Molecular Biology; Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Chemistry	FO1NJ	29160833	Green Published, Green Submitted, gold			2025-03-11	WOS:000416528400211
J	Hinners, J; Kremp, A; Hense, I				Hinners, Jana; Kremp, Anke; Hense, Inga			Evolution in temperature-dependent phytoplankton traits revealed from a sediment archive: do reaction norms tell the whole story?	PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES			English	Article						adaptation; global warming; phytoplankton; sediment archives; temperature-dependent traits	CLIMATE-CHANGE; MARINE DINOFLAGELLATE; SCRIPPSIELLA-HANGOEI; SIZE EVOLUTION; SOUTHERN-OCEAN; CYST FORMATION; GROWTH; DINOPHYCEAE; POPULATION; ENCYSTMENT	The high evolutionary potential of phytoplankton species allows them to rapidly adapt to global warming. Adaptations may occur in temperature-dependent traits, such as growth rate, cell size and life cycle processes. Using resurrection experiments with resting stages from living sediment archives, it is possible to investigate whether adaptation occurred. For this study, we revived resting cysts of the spring bloom dinoflagellate Apocalathium malmogiense from recent and 100-year-old sediment layers from the Gulf of Finland, and compared temperature-dependent traits of recent and historic strains along a temperature gradient. We detected no changes in growth rates and cell sizes but a significant difference between recent and historic strains regarding resting cyst formation. The encystment rate of recent strains was significantly lower compared with historic strains which we interpret as an indication of adaptation to higher and more rapidly increasing spring temperatures. Low encystment rates may allow for bloom formation even if the threshold temperature inducing a loss of actively growing cells through resting cyst formation is exceeded. Our findings reveal that phenotypic responses of phytoplankton to changing temperature conditions may include hidden traits such as life cycle processes and their regulation mechanisms. This study emphasizes the potential of living sediment archives to investigate plankton responses and adaptation to global warming.	[Hinners, Jana; Hense, Inga] Univ Hamburg, Inst Hydrobiol & Fisheries Sci, Ctr Earth Syst Res & Sustainabil, Grosse Elbstr 133, D-22767 Hamburg, Germany; [Kremp, Anke] Finnish Environm Inst SYKE, Ctr Marine Res, Erik Palmenin Aukio 1, Helsinki 00560, Finland	University of Hamburg; Finnish Environment Institute	Hinners, J (通讯作者)，Univ Hamburg, Inst Hydrobiol & Fisheries Sci, Ctr Earth Syst Res & Sustainabil, Grosse Elbstr 133, D-22767 Hamburg, Germany.	jana.hinners@uni-hamburg.de		Hinners, Jana/0000-0002-5145-2539; Kremp, Anke/0000-0001-9484-6899; Hense, Inga/0000-0001-7322-680X	Landesforschungsforderung Hamburg [LFF-OS 20-2014]; Academy of Finland [282061, 251564]; Walter and Andre de Nottbeck Foundation; Cluster of Excellence CliSAP (EXC177), University of Hamburg - German Science Foundation (DFG)	Landesforschungsforderung Hamburg; Academy of Finland(Research Council of Finland); Walter and Andre de Nottbeck Foundation; Cluster of Excellence CliSAP (EXC177), University of Hamburg - German Science Foundation (DFG)(German Research Foundation (DFG))	J.H. acknowledges the support of Landesforschungsforderung Hamburg LFF-OS 20-2014. Funding for A.K. was provided by the Academy of Finland grants 282061 and 251564 and the Walter and Andre de Nottbeck Foundation. I.H. was supported through the Cluster of Excellence CliSAP (EXC177), University of Hamburg, funded through the German Science Foundation (DFG).	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R. Soc. B-Biol. Sci.	OCT 11	2017	284	1864							20171888	10.1098/rspb.2017.1888	http://dx.doi.org/10.1098/rspb.2017.1888			8	Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Environmental Sciences & Ecology; Evolutionary Biology	VK1VD	29021182	Green Published, Bronze			2025-03-11	WOS:000662166400012
J	Kuhn, LA; Souza, PA; Cancelli, RR; Silva, WG; Macedo, RB				Kuhn, Lidia A.; Souza, Paulo A.; Cancelli, Rodrigo R.; Silva, Wagner G.; Macedo, Renato B.			Paleoenvironmental evolution of the coastal plain of Southern Brazil: palynological data from a Holocene core in Santa Catarina State	ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS			English	Article						coastal plain; environmental evolution; Holocene; palynology; Santa Catarina	GRANDE-DO-SUL; SEA-LEVEL FLUCTUATIONS; ENVIRONMENTAL-CHANGES; BUENOS-AIRES; PALYNOMORPHS; SEDIMENTS; ARGENTINA; DEPOSITS; CATALOG; RECORDS	This paper presents a paleoenvironmental reconstruction from palynological analyses of a sedimentary core of Holocene age, drilled at municipality of Garopaba (Santa Catarina), Southern Brazil. A total of 46 samples was collected for palynological analyses in the 450 cm-long core PCSC-3, as also three samples for radiocarbon dating and granulometric analyses. The palynological content includes 84 taxa related to pollen grains of angiosperms (38) and gimnosperm (3), spores of pteridophyta (16) and bryophyta (2), spores of fungi (8), algae (3), acritarchs (3), dinoflagellate cysts (2) and microforaminiferal linings (1). Three specimens of acritarchs are described and illustrated in detail. Three palynological phases were defined based on changes in assemblages: Phase I, Phase II and Phase III. The Phase I is characterized as a lagoonal paleoenvironment with marine influence from the beginning of the sedimentation (5390 cal yr BP), based on occurrences of acritarchs, dinoflagellate cysts and microforaminiferal linings. The Phase II (3032 yr BP until 858 cal yr BP) also is characterized by a lagoonal paleoenvironment, however, presented decrease in percentage of marine elements and increase in freshwater algae record, suggesting less marine influence in the lagoonal body. In Phase III (last 856 years), underwater sedimentation prevailed, under swamp-like conditions.	[Kuhn, Lidia A.; Souza, Paulo A.; Cancelli, Rodrigo R.; Silva, Wagner G.; Macedo, Renato B.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Inst Geociencias, Lab Palinol Marleni Marques Toigo,Dept Paleontol, Av Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil; [Silva, Wagner G.] Inst Fed Educ Ciencia & Tecnol Rio Grande do Sul, Campus Osorio,Rua Santos Dumont 2127, BR-95520000 Osorio, RS, Brazil	Universidade Federal do Rio Grande do Sul; Instituto Federal do Rio Grande do Sul (IFRS)	Kuhn, LA (通讯作者)，Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Inst Geociencias, Lab Palinol Marleni Marques Toigo,Dept Paleontol, Av Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil.	lidiaak.lak@gmail.com	; Alves de Souza, Paulo/O-9779-2018	Kuhn, Lidia/0000-0003-2120-1824; Alves de Souza, Paulo/0000-0001-9844-1530	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [132260/2015-8, 454804/2014-8]; Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [APG1012119]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); 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 thank Leo A. Hartmann for contributing with comments during the writing of the article, and Eduardo Barboza for making possible the particle size analysis. This contribution was performed with support grants from the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq proc. 132260/2015-8, 454804/2014-8) and Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS proc. APG1012119). The authors also thank reviewers for manuscript revision and suggestions.	Alvares CA, 2013, METEOROL Z, V22, P711, DOI 10.1127/0941-2948/2013/0507; Angulo RJ, 2006, QUATERNARY SCI REV, V25, P486, DOI 10.1016/j.quascirev.2005.03.008; Angulo RJ, 1999, MAR GEOL, V159, P323, DOI 10.1016/S0025-3227(98)00204-7; [Anonymous], 2012, Manual Tecnico da Vegetacao Brasileira; [Anonymous], 1996, Notas Tecnicas; [Anonymous], MACRODIAGNOSTICO ZON; Batten D., 1996, Palynology: principles and applications, P1011; Bauermann S. 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Acad. Bras. Cienc.	OCT-DEC	2017	89	4					2581	2595		10.1590/0001-3765201720160895	http://dx.doi.org/10.1590/0001-3765201720160895			15	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	FQ8XS	29069134	Green Published, Green Submitted, gold			2025-03-11	WOS:000418647100004
J	Wang, N; Luo, ZH; Mertens, KN; McCarthy, FMG; Gu, L; Gu, HF				Wang, Na; Luo, Zhaohe; Mertens, Kenneth N.; McCarthy, Francine M. G.; Gu, Li; Gu, Haifeng			Cyst-motile stage relationship and molecular phylogeny of a new freshwater dinoflagellate <i>Gymnodinium plasticum</i> from Plastic Lake, Canada	PHYCOLOGICAL RESEARCH			English	Article						apical structure complex; cyst; Gymnodiniales sensu stricto; Gymnodinium fuscum	WESTERN KOREA MORPHOLOGY; NW MEDITERRANEAN SEA; SHIWHAENSE N. GEN.; SP-NOV DINOPHYCEAE; RIBOSOMAL DNA; COASTAL WATERS; COMB. NOV.; ALEXANDRIUM DINOPHYCEAE; SEQUENCE DATA; ULTRASTRUCTURE	The dinophyceaen genus Gymnodinium was established with the freshwater species G. fuscum as type. According to Thessen et al. (2012), there are 268 species, with the majority marine species. In recently published molecular phylogenies based on ribosomal DNA sequences, Gymnodinium is polyphyletic. Here, a new freshwater Gymnodinium species, G. plasticum, is described from Plastic Lake, Ontario, Canada. Two strains were established by incubating single cysts, and their morphology was examined with light microscopy and scanning electron microscopy. The cyst had a rounded epicyst and hypocyst with a wide cingulum and smooth surface. Vegetative cells were characterized by an elongated nucleus running vertically and a deep sulcal intrusion. The apical structure complex was horseshoe-shaped and consisted of two pronounced ridges with a deep internal groove, encircling 80% of the apex. Small subunit ribosomal DNA (SSU rDNA), large subunit ribosomal DNA (LSU rDNA) and internal transcribed spacer (ITS) sequences were obtained from cultured strains. Molecular phylogeny based on concatenated SSU, LSU and ITS sequences supports the monophyly of the Gymnodiniales sensu stricto clade but our results suggest that many Gymnodinium species might need reclassification. Gymnodinium plasticum is closest to Dissodinium pseudolunula in our phylogeny but distant from the type species G. fuscum, as are the other gymnodiniacean taxa.	[Wang, Na; Luo, Zhaohe; Gu, Li; Gu, Haifeng] State Ocean Adm, Inst Oceanog 3, Xiamen, Peoples R China; [Mertens, Kenneth N.] IFREMER, Stn Biol Marine, LER BO, Concarneau, France; [McCarthy, Francine M. G.] Brock Univ, Earth Sci, St Catharines, ON, Canada	Third Institute of Oceanography, Ministry of Natural Resources; Ifremer; Brock University	Gu, HF (通讯作者)，State Ocean Adm, Inst Oceanog 3, Xiamen, Peoples R China.	guhaifeng@tio.org.cn	Luo, Zhaohe/ITT-7163-2023; Mertens, Kenneth/AAO-9566-2020; LI, QI/KHA-7880-2024; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Gu, Haifeng/0000-0002-2350-9171; Luo, Zhaohe/0000-0001-8662-2414; Mertens, Kenneth/0000-0003-2005-9483	National Natural Science Foundation of China [41676117]; Bilateral International Cooperation Project of SOA [HC170301]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Bilateral International Cooperation Project of SOA	We thank the responsible editor and two anonymous reviewers for constructive suggestions that improved the manuscript greatly. This work was supported by National Natural Science Foundation of China (41676117) and Bilateral International Cooperation Project of SOA (HC170301). We thank AM Krueger, Brock University, who assisted with field sampling.	Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Alix B, 2012, NUCLEIC ACIDS RES, V40, pW573, DOI 10.1093/nar/gks485; Allman G.J., 1855, QJ Microsc Sci, V3, P21; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P644, DOI 10.2216/07-05.1; Campbell P. 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OCT	2017	65	4					312	321		10.1111/pre.12190	http://dx.doi.org/10.1111/pre.12190			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	FI6IU		Green Published			2025-03-11	WOS:000412099200006
J	Uddandam, PR; Prasad, V; Rai, J				Uddandam, Prem Raj; Prasad, Vandana; Rai, Jyotsana			Dinoflagellate cyst distribution in sediments of western Bay of Bengal: Role of sea surface conditions	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinoflagellate cysts; Bay of Bengal; River discharge; Productivity; Upwelling	NORTHWESTERN INDIAN-OCEAN; ARABIAN SEA; PRODUCTIVITY CHARACTERISTICS; ENVIRONMENTAL-FACTORS; SEASONAL VARIABILITY; UPWELLING REGION; NORTHERN BAY; FRESH-WATER; TOKYO-BAY; SALINITY	Bay of Bengal is a shallow marine basin exposed to seasonal fluctuation in precipitation and run-off. Thus, salinity, temperature, nutrient and productivity vary along the latitudinal and onshore-offshore gradient in the Bay of Bengal. These parameters directly affect primary productivity, including that of dinoflagellate cysts. The spatial distribution of organic walled dinoflagellates cyst is studied in the 50 surface samples of eight transects from the western Bay of Bengal, to infer variation in the environmental conditions in the region. The cyst diversity consists of 40 taxa with an overall high dominance of protoperidinioid cysts over gonyalaucoides. Based on the study distinct onshore and offshore dinocyst assemblages are identified. The high productive coastal upwelling region is characterised by the dominance of gonyalaucoid dinocyst species Bitectatodinium spongium (Zonneveld 1997) Zonneveld and Jurkschat 1999 indicating its adaptability to the fluctuating salinity and high nutrient conditions. The outer shelf to middle slope regions of western Bay of Bengal is dominated by the protoperidinioid species. This is in contrast to the gonyalaucoid dinocyst assemblages of the outer shelf to middle slope regions in other oceans. Since protoperidinioids prefer high nutrient and reducing environmental conditions for growth and preservation, their presence suggest high nutrient availability due to the river discharge and low oxygen condition in the slope region in Bay of Bengal. Statistical analyses of the sea surface parameters and dinoflagellate cyst abundance data indicate that salinity and silicates as a major source of nutrient played a major role in the distribution of dinoflagellate cyst in the Bay of Bengal. (C) 2017 Elsevier B.V. All rights reserved.	[Uddandam, Prem Raj; Prasad, Vandana; Rai, Jyotsana] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Uddandam, PR (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	premrajuddandam@gmail.com			MoES [MoES/SIBER/NIO(RN)/11]	MoES	We are thankful to Director, BSIP for providing necessary facilities to carry out the present study. This study is carried out as a part of MoES funded project entitled "High resolution paleoclimatic studies" No. MoES/SIBER/NIO(RN)/11. We are also thankful to Dr. Rajiv Nigam and Dr. Rajeev Saraswat for their support during the sampling collection. The present publication bears a permission no. 36/2016-17 from the Birbal Sahni Institute of Paleosciences.	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Paleoclimatol. Paleoecol.	OCT 1	2017	483				SI		31	48		10.1016/j.palaeo.2017.01.013	http://dx.doi.org/10.1016/j.palaeo.2017.01.013			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	FH9QR					2025-03-11	WOS:000411547300004
J	Wary, M; Eynaud, F; Rossignol, L; Zaragosi, S; Sabine, M; Castera, MH; Billy, I				Wary, Melanie; Eynaud, Frederique; Rossignol, Linda; Zaragosi, Sebastien; Sabine, Marjolaine; Castera, Marie-Helene; Billy, Isabelle			The southern Norwegian Sea during the last 45 ka: hydrographical reorganizations under changing ice-sheet dynamics	JOURNAL OF QUATERNARY SCIENCE			English	Article						Dansgaard-Oeschger cycles; deep convection; Heinrich events; Holocene; sea-surface hydrographical conditions	NORTH-ATLANTIC OCEAN; RAPID CLIMATIC VARIATIONS; MARINE ISOTOPIC STAGE-3; NORDIC SEAS; GLACIAL PERIOD; NEOGLOBOQUADRINA-PACHYDERMA; DINOFLAGELLATE CYSTS; PALEOINTENSITY STACK; CIRCULATION CHANGES; ICEBERG DISCHARGES	The last glacial millennial Heinrich and Dansgaard-Oeschger events have been the subject of many studies in recent decades. However, significant uncertainties remain, notably regarding associated oceanic mechanisms. Here we investigate the evolution of hydrographical conditions in the 3-41 ka cal BP interval of core MD99-2285 located in the southern Norwegian Sea. Our results reveal an unusual scheme with: (i) warm Greenland interstadials marked by a relatively cold and homogeneous upper water column seasonally ice-covered and active deep water formation, (ii) cold Greenland and Heinrich stadials marked by a warm, low-salinity and nearly sea ice-free surface layer with iceberg calving, separated by a strong halocline from a colder and saltier subsurface layer, as well as strongly reduced deep convection, and (iii) close to modern Holocene oceanic conditions, but showing significant differences from interstadial conditions. Hence, our work strongly suggests different deep-water convection modes in the Nordic Seas, with, notably, interstadial deep water formation mainly forced by brine release. According to our results, the transition from the glacial mode of deep water formation to the modern open ocean convection mode might have occurred at the end of deglaciation/beginning of the Holocene, when both modes probably occurred. Copyright (C) 2017 John Wiley & Sons, Ltd.	[Wary, Melanie; Eynaud, Frederique; Rossignol, Linda; Zaragosi, Sebastien; Sabine, Marjolaine; Castera, Marie-Helene; Billy, Isabelle] Univ Bordeaux, EPOC Environm & Paleoenvironm Ocean & Continentau, UMR 5805, Pessac, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux	Wary, M (通讯作者)，Univ Bordeaux, EPOC Environm & Paleoenvironm Ocean & Continentau, UMR 5805, Pessac, France.	melanie.wary@u-bordeaux.fr	ZARAGOSI, Sébastien/JXL-2488-2024; WARY, Melanie/S-1121-2018	WARY, Melanie/0000-0001-5211-2168; Zaragosi, Sebastien/0000-0002-1456-8129	French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within EVE (Evolution et variabilite du climat a l'echelle globale); French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean); INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme; ARTEMIS 14C AMS French INSU; European Union's Seventh Framework Programme [243908]; French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within EVE (Evolution et variabilite du climat a l'echelle globale); French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean); INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme; ARTEMIS 14C AMS French INSU; European Union's Seventh Framework Programme [243908]	French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within EVE (Evolution et variabilite du climat a l'echelle globale); French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean); INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme; ARTEMIS 14C AMS French INSU; European Union's Seventh Framework Programme(European Union (EU)); French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within EVE (Evolution et variabilite du climat a l'echelle globale); French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean); INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme; ARTEMIS 14C AMS French INSU; European Union's Seventh Framework Programme(European Union (EU))	Analyses conducted on MD99-2285 were supported by the French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within the frame of the EVE (Evolution et variabilite du climat a l'echelle globale) 2009-2011 project 'RISCC: Role des Ice-Shelves dans le Changement Climatique' and of the IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean) 2013 project 'ICE-BIO- RAM: Impact des Changements Environnementaux sur la BIOdiversite marine lors des Rechauffements Abrupts du cliMat', this latter being also supported by the INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme. We also acknowledge financial support and facilities of the ARTEMIS <SUP>14</SUP>C AMS French INSU project. The research leading to these results also benefited from funding from the European Union's Seventh Framework Programme (FP7/2007-2013) under grant agreement No. 243908, 'Past4Future. Climate change - Learning from the past climate'. We warmly thank T. Richter and the Royal Netherlands Institute for Sea Research (NIOZ) for providing X-ray fluorescence data. We thank P. Lebleu and O. Ther for their assistance in core imagery. We also warmly thank L. Londeix, D. Swingedouw and M. Cremer for their advice and discussions which greatly contributed to the improvement of the present study. We would also like to express our gratitude to E. Georgiadis for proofreading the manuscript. We also thank M.-A. Sicre and the LOCEAN technician staff for the promising tests done with biomarkers. This is a U.M.R. EPOC 5805 (Universite de Bordeaux - C.N.R.S.) contribution.	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Quat. Sci.	OCT	2017	32	7					908	922		10.1002/jqs.2965	http://dx.doi.org/10.1002/jqs.2965			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	FI6MD					2025-03-11	WOS:000412109500002
J	Datema, M; Sangiorgi, F; de Vernal, A; Reichart, GJ; Lourens, LJ; Sluijs, A				Datema, Mariska; Sangiorgi, Francesca; de Vernal, Anne; Reichart, Gert-Jan; Lourens, Lucas J.; Sluijs, Appy			Comparison of qualitative and quantitative dinoflagellate cyst approaches in reconstructing glacial-interglacial climate variability at West Iberian Margin IODP 'Shackleton' Site U1385	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Shackleton Site; Integrated Ocean Drilling Program; Last glacial transition; Sea surface temperature and salinity; Modern analogue technique	SEA-SURFACE TEMPERATURE; NORTHERN NORTH-ATLANTIC; ORGANIC-MATTER; PLANKTONIC-FORAMINIFERA; HEINRICH EVENTS; ICE COVER; SELECTIVE PRESERVATION; HIGH-LATITUDES; TIME-SCALE; LAST	Dinoflagellate cysts (dinocysts) are commonly used to reconstruct past environmental conditions at the sea surface, such as primary production, temperature and salinity. Abundances of selected dinocyst taxa are used in qualitative indices, whereas the modern analogue technique (MAT) is used for quantitative reconstructions. Qualitative indices use process-based knowledge of present-day relations between the environmental variables and the distribution of dinocysts, whereas the MAT is based on the assumption that past assemblages have modern counterparts that correspond to similar sea-surface conditions. Here we explore the potential of both approaches to reconstruct sea surface temperature (SST), production (SSP), salinity (SSS) and seasonality during the last 22 thousand years along the West Iberian Margin (WIM), at Integrated Ocean Drilling Program (IODP) Site U1385. We compare results to published paleoclimatic reconstructions. Our SST and SSS reconstructions provide the first continuous dinocyst MAT-based SST and SSS records for this area and time interval. Qualitative and quantitative dinocyst-based SST estimates from the WIM are similar and resemble previous SST estimates from dinocysts, alkenones and foraminifers from nearby sites. The surface temperature trends and millennial-scale variations largely match_ those from the Greenland ice core records. Quantitative MAT-based SST estimates show increased seasonality in the glacial stage resulting from strong winter cooling. Dinocyst MAT-based salinity decreases concomitantly with cooling during the Younger Dryas and Heinrich Stadial 1 (HS1), likely related to the melting of icebergs that reached the region during HS1. Our qualitative and quantitative SSP estimates show higher values in the glacial stage compared to the Holocene, which is consistent with published records and supports the usefulness of both approaches. Small differences between SST tracer records may be explained by the limited number of modern analogues from warm ocean regions in the dinocyst reference dataset for MAT, the small number of dinocysts used in the qualitative estimates, the possible effect of a parameter other than temperature that might amplify noise, and/or seasonal biases of the tracer species. In any case, the advantage of the qualitative approach is to allow reconstructions in non-analogue situations. Regression of the qualitative index versus present-day SST also allows for a quantitative reconstruction, although over a limited range of SSTs (especially towards the lower end) and with quite some uncertainty, but produces reasonable values beyond the upper limit of the MAT. The MAT reconstructs more reliable SSTs, with a much smaller error of prediction, but only up to present-day WIM values, because it is based on the assumption that past assemblages have modern counterparts that correspond to similar sea-surface conditions, which is not always valid. The advantages of the MAT approach include its quantitative nature and insights into seasonality. Hence both approaches are complementary. At Site U1385, MAT can be used for reconstructions in the colder periods (YD, HS1 and glacial stage), with a small error of prediction and the quantified index can be used to estimate SST beyond the limit of the MAT (Holocene and B-A).	[Datema, Mariska; Sangiorgi, Francesca; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, Heidelberglaan 2,POB 80-115, NL-3508 TC Utrecht, Netherlands; [de Vernal, Anne] Univ Quebec, Ctr Rech Geochim & Geodynam Geotop, POB 8888, Montreal, PQ H3C 3P8, Canada; [Reichart, Gert-Jan; Lourens, Lucas J.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Heiderberglaan 2,POB 80-115, NL-3508 TC Utrecht, Netherlands; [Reichart, Gert-Jan] NIOZ Royal Netherlands Inst Sea Res, Dept Ocean Syst, POB 59, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; University of Quebec; University of Quebec Montreal; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Datema, M (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol,Marine Palynol & Paleocea, Heidelberglaan 2,POB 80-115, NL-3508 TC Utrecht, Netherlands.	M.C.Datema@uu.nl; F.Sangiorgi@uu.nl; devematanne@uqam.ca; G.J.Reichart@uu.nl; L.J.Lourens@uu.nl; A.Sluijs@uu.nl	de Vernal, Anne/D-5602-2013; Sluijs, Appy/B-3726-2009; Reichart, Gert-Jan/N-6308-2018	Sluijs, Appy/0000-0003-2382-0215; Sangiorgi, Francesca/0000-0003-4233-6154; Datema, Mariska/0000-0001-5963-3935; Reichart, Gert-Jan/0000-0002-7256-2243	ERC [259627]; European Research Council (ERC) [259627] Funding Source: European Research Council (ERC)	ERC(European Research Council (ERC)); European Research Council (ERC)(European Research Council (ERC))	This work used samples and data provided by the Integrated Ocean Drilling Program (IODP). We thank Walter Hale and Alex Wulbers from the IODP Core Repository in Bremen for curation of the sediment cores recovered at Site U1385. We acknowledge all shipboard participants of IODP Expedition 339 and particularly David Hodell for providing the age models. We thank Natasja Welters for laboratory assistance and Ton Markus (all Utrecht University) for illustration support. We gratefully acknowledge the reviewers and Frans Jorissen for their thoughtful comments that helped us to greatly improve this manuscript. The European Research Council (ERC) under the European Union Seventh Framework Program provided funding for this work by ERC Starting Grant 259627 to Sluijs. This work was carried out under the program of the Netherlands Earth System Science Centre (NESSC).	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Micropaleontol.	OCT	2017	136						14	29		10.1016/j.marmicro.2017.08.003	http://dx.doi.org/10.1016/j.marmicro.2017.08.003			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	FM3CP		Green Published			2025-03-11	WOS:000414882200002
J	Schreck, M; Nam, SI; Clotten, C; Fahl, K; De Schepper, S; Forwick, M; Matthiessen, J				Schreck, Michael; Nam, Seung-Il; Clotten, Caroline; Fahl, Kirsten; De Schepper, Stijn; Forwick, Matthias; Matthiessen, Jens			Neogene dinoflagellate cysts and acritarchs from the high northern latitudes and their relation to sea surface temperature	MARINE MICROPALEONTOLOGY			English	Article						Iceland Sea; Neogene; Dinoflagellate cyst; Acritarch; Alkenones; Paleotemperatures	NORWEGIAN-GREENLAND SEA; MIDDLE MIOCENE; LATE PLIOCENE; ASSEMBLAGES; ATLANTIC; RECONSTRUCTION; PLEISTOCENE; SEDIMENTS; BIOSTRATIGRAPHY; PALEOECOLOGY	Organic-walled dinoflagellate cysts and acritarchs are a vital tool for reconstructing past environmental change, in particular in the Neogene of the high northern latitudes where marine deposits are virtually barren of traditionally used calcareous microfossils. Yet only little is known about the paleoenvironmental value of fossil assemblages that do not have modem analogues, so that reconstructions remain qualitative. Thus, extracting their paleoecological signals still poses a major challenge, in particular on pre-Quatemary timescales. Here we unravel the relationship between species relative abundance and sea surface temperature for extinct dinoflagellate cyst and acritarch taxa from the Neogene of the Iceland Sea using palynological assemblages and organic geochemical (alkenone) data generated from the same set of samples. The reconstructed temperatures for the Miocene to Pliocene sequence of Ocean Drilling Program Site 907 range from 3 to 26 degrees C and our database consists of 68 dinoflagellate cyst and acritarch samples calibrated to alkenone data. The temperature range of five extant species co-occurring in the fossil assemblage agrees well with their present-day distribution providing confidence to inferred temperature ranges for extinct taxa. The 14 extinct dinoflagellate cyst and acritarch species clearly exhibit a temperature dependency in their occurrence throughout the analysed section. The dinoflagellate cyst species Batiacasphaera hirsuta, Labyrinthodinium truncatum, Cerebrocysta irregulare, Cordosphaeridium minimum, Impagidinium elongatum and Operculodinium centroccapum s.s., and the acritarch Lavradosphaera elongatum, which are confined to the Miocene, have highest relative abundances and restricted temperature ranges at the warn end of the reconstructed temperature spectrum. The latter five species disappear when Iceland Sea surface temperatures permanently drop below 20 degrees C, thus indicating a distinct threshold on their occurrence. In contrast, species occurring in both the Miocene and Pliocene interval (Batiacasphaera micropapillata, Habthacysta tectata, Reticulatosphaera actinocoronata, Cymatiosphaera? invaginata) show a broader temperature range and a tolerance towards cooler conditions. Operculodinium? eirilcianum may have a lower limit on its occurrence at around 10 degrees C. The calibration of species relative abundance versus reconstructed sea surface temperature provides a quantitative assessment of temperature ranges for extinct Miocene to Pliocene species indicating that temperature is a decisive ecological factor for regional extinctions that may explain the frequently observed asynchronous highest occurrences across different ocean basins. It demonstrates that qualitative assessments of ecological preferences solely based on (paleo) biogeographic distribution should be treated with caution. In addition to enhancing knowledge on marine palynomorph paleoecology, this study ultimately improves the application of palynomorphs for paleoenvironmental reconstructions in the Neogene of the Arctic and subarctic seas, a region essential for understanding past global climate.	[Schreck, Michael; Forwick, Matthias] UiT Arctic Univ Norway Tromso, Dept Geosci, POB 6050, N-9037 Tromso, Norway; [Schreck, Michael; Nam, Seung-Il] Korea Polar Res Inst, Div Polar Environm, 26 Songdomirae Ro, Incheon 21990, South Korea; [Clotten, Caroline; De Schepper, Stijn] Bjerknes Ctr Climate Res, Uni Res Climate, Jahnebakken 5, N-5007 Bergen, Norway; [Fahl, Kirsten; Matthiessen, Jens] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Alten Hafen 26, D-27568 Bremerhaven, Germany	UiT The Arctic University of Tromso; Korea Polar Research Institute (KOPRI); Bjerknes Centre for Climate Research; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Schreck, M (通讯作者)，UiT Arctic Univ Norway Tromso, Dept Geosci, POB 6050, N-9037 Tromso, Norway.	Michael.Schreck@uit.no	; De Schepper, Stijn/A-2836-2011	Fahl, Dr., Kirsten/0000-0001-9317-4656; De Schepper, Stijn/0000-0002-6934-0914; Matthiessen, Jens/0000-0002-6952-2494; Forwick, Matthias/0000-0001-6153-5891	German Research Foundation [DFG MA 3913/2]; Basic Research Program of the Korea Polar Research Institute [PE16062]; National Research Foundation of Korea from the Government of Korea (MSIT) [NRF-2015M1A5A1037243]; Norwegian Research Council [229819]	German Research Foundation(German Research Foundation (DFG)); Basic Research Program of the Korea Polar Research Institute(Korea Polar Research Institute of Marine Research Placement (KOPRI)); National Research Foundation of Korea from the Government of Korea (MSIT)(National Research Foundation of KoreaMinistry of Science & ICT (MSIT), Republic of Korea); Norwegian Research Council(Research Council of Norway)	This research uses samples and data provided by the Ocean Drilling Program. We gratefully thank W. Luttmer (AVVI-Bremerhaven) for technical support with the alkenone analyses and M. Jones (Palynological Laboratory Services Ltd., Holyhead, UK) for palynological preparation. MS and JM acknowledge financial support from the German Research Foundation (DFG MA 3913/2), and MS is additionally thankful to the Basic Research Program (No. PE16062) of the Korea Polar Research Institute, and a National Research Foundation of Korea grant from the Government of Korea (MSIT) (NRF-2015M1A5A1037243). SDS and CC acknowledge funding from the Norwegian Research Council (project 229819).	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J	Li, Z; Pospelova, V; Liu, LJ; Zhou, R; Song, B				Li, Zhen; Pospelova, Vera; Liu, Lejun; Zhou, Rui; Song, Bing			High-resolution palynological record of Holocene climatic and oceanographic changes in the northern South China Sea	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Asian monsoon; Holocene; Sea level change; Dinoflagellate cysts; Palynology; The South China Sea	WALLED DINOFLAGELLATE CYSTS; EAST-ASIAN MONSOON; LAST GLACIAL MAXIMUM; SANTA-BARBARA BASIN; RED-RIVER DELTA; SURFACE SEDIMENTS; POLLEN DISTRIBUTION; ATLANTIC-OCEAN; TAIWAN STRAIT; SUNDA SHELF	For the first time, palynological records of terrestrial palynomorphs and dinofiagellate cysts are investigated in a sediment core from the northern South China Sea (SCS) covering the last 12,500 years. Both terrestrial and marine palynomorph records show strong signals of the sea-level change during the studied interval. The highest herb pollen content was associated with extensive grasslands on the exposed shelf at the low sea-level stand during the Younger Dryas and early Holocene. The increase in fern spores and decrease in concentrations of dinofiagellate cysts and terrestrial palynomorphs was observed during the sea-level rise interval from 12,500 to similar to 6800 (or 6000) cal yr BP. Then, the sea level became stabilized and consistently low dinofiagellate cyst abundances and high abundances of fern spores were recorded. A high abundance of Impagidinium in the period similar to 12,000-10,400 cal yr BP possibly resulted from increased input of western Philippine Sea waters into the SCS and the branching of the Kuroshio Current. A short-term decrease of Impagidinium at similar to 11,700-11,000 cal yr BP corresponding to the MWP-1B event might be associated with input of the East China Sea waters through the Taiwan Strait. The relationship between the sedimentation rates and the concentrations of terrestrial palynomorphs indicates a water-dominant transport for pollen and spore dispersal prior to similar to 6300 cal yr BP, whereas wind transport became more prominent thereafter. The timing of this change corresponds to the highest sea-level stand at similar to 6800-6000 cal yr BP, when the present oceanographic setting was formed. The mid-Holocene Optimum can be seen by the highest abundance of subtropical-tropical broad-leaved arboreal pollen and by the highest abundances of Dapsilidinium pastielsii. Three strengthened winter monsoon intervals at similar to 5500 cal yr BP, 4000 cal yr BP, and 2500 cal yr BP are reflected by increases in Pinus pollen content after the present oceanographic condition formed. (C) 2017 Elsevier B.V. All rights reserved.	[Li, Zhen; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada; [Liu, Lejun] First Inst Oceanog, 6 Xianxialing Rd, Qingdao 266061, Shangdong, Peoples R China; [Zhou, Rui; Song, Bing] East China Normal Univ, State Key Lab Estuarine & Coastal Res, 3663 North Zhongshan Rd, Shanghai 200062, Peoples R China; [Song, Bing] Korea Inst Geosci & Mineral Resources, Geol Res Div, Quaternary Geol Dept, Daejeon 305350, South Korea	University of Victoria; First Institute of Oceanography, Ministry of Natural Resources; East China Normal University; Korea Institute of Geoscience & Mineral Resources (KIGAM)	Li, Z (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada.	imlizhen@hotmail.com	Li, Zhen/G-7667-2012; Song, Bing/AAA-9421-2020	Li, Zhen/0000-0003-3989-7233; Pospelova, Vera/0000-0003-4049-8133	Natural Sciences and Engineering Research Council of Canada (NSERC) CGS D3 fellowship; Montalbano scholarship; National Science and Technology Major Projects of China [2011ZX05056-001-02]; NSERC [312305]; National Key Project from the State Oceanography Administration of China [GASI-GEOGE-05]	Natural Sciences and Engineering Research Council of Canada (NSERC) CGS D3 fellowship; Montalbano scholarship; National Science and Technology Major Projects of China; NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); National Key Project from the State Oceanography Administration of China	The Natural Sciences and Engineering Research Council of Canada (NSERC) CGS D3 fellowship, Montalbano scholarship, and the National Science and Technology Major Projects of China grant (2011ZX05056-001-02) provided partial funding for this research to Z. Li. This work was also funded by NSERC through a Discovery grant (312305) to V. Pospelova. She is the Hanse-Wissenschaftskolleg (HWK) senior research fellow in marine and climate research at the Institute for Advanced Study (Germany). L. Liu was partially supported by the National Key Project (GASI-GEOGE-05) from the State Oceanography Administration of China in this work.	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Paleoclimatol. Paleoecol.	OCT 1	2017	483				SI		94	124		10.1016/j.palaeo.2017.03.009	http://dx.doi.org/10.1016/j.palaeo.2017.03.009			31	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	FH9QR					2025-03-11	WOS:000411547300009
J	Jurkowska, A; Barski, M				Jurkowska, Agata; Barski, Marcin			Maastrichtian island in the central European Basin-new data inferred from palynofacies analysis and inoceramid stratigraphy	FACIES			English	Article						Palynofacies; Inoceramid stratigraphy; Paleogeography; Late Cretaceous; Central European Basin	MID-POLISH TROUGH; DINOFLAGELLATE CYSTS; SEDIMENTS; POLAND; NORTH; ENVIRONMENT; DEPOSITION; INVERSION; ATLANTIC; MODEL	The palynological study and palynofacies analysis supported by size analysis of opaque phytoclasts and diversity indexes for particulate organic matter in stratigraphically well-constrained (inoceramid biostratigraphy) sections is applied in monotonous Upper Cretaceous carbonate- siliciclastic sediments of southern Poland. Integrated data allow for the estimation of the proximity of an uplifted area from the studied sections. For the first time in palynofacies analysis, both Simpson's Index of Diversity (1 - D) and Shannon's index are used for organic matter distribution providing a comprehensive understanding of a proximaldistal trend in a sedimentary basin. Cluster analysis allowed grouping the samples within proximal to distal shelf zones. The size analysis of opaque woody phytoclasts is used to extrapolate the distance from the source area. Palynofacies analysis indicates the existence of an uplifted area (probably connected with "Kukernitz Island") in the Holy Cross part of the Danish-Polish Trough during the Maastrichtian. The presented results improve contemporary paleogeographical interpretations for this part of the Late Cretaceous central European Basin. The youngest Maastrichtian deposits of the Miechow Synclinorium are described, based on inoceramids which are of early Late Maastrichtian age.	[Jurkowska, Agata] AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Mickiewicza 30, PL-30059 Krakow, Poland; [Barski, Marcin] Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland	AGH University of Krakow; University of Warsaw	Jurkowska, A (通讯作者)，AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Mickiewicza 30, PL-30059 Krakow, Poland.	jurkowska.a@gmail.com; marbar@uw.edu.pl	; Jurkowska, Agata/A-9734-2016	Barski, Marcin/0000-0002-4102-3538; Jurkowska, Agata/0000-0001-5457-9968	AGH statutory grants from the AGH University of Science and Technology [DS: 11.11.140.626]; Institute of Geology, Warsaw University	AGH statutory grants from the AGH University of Science and Technology; Institute of Geology, Warsaw University	This work was supported by AGH statutory grants from the AGH University of Science and Technology (DS: 11.11.140.626) and statutory grants of Institute of Geology, Warsaw University. We are very grateful to Prof. Marcin Machalski (Polish Academy of Sciences), Dr. Axel Munnecke (Friedrich-Alexander Universitat Erlangen-Nurnberg) and anonymous reviewer for constructive comments on the earlier version of the manuscript. The authors are greatly indebted to Marta Szczepanik and Kyle Freeman for linguistics corrections.	[Anonymous], 1834, SYNOPSIS ORGANIC REM; [Anonymous], 1983, Wetzel; [Anonymous], 2007, Paleopalynology; [Anonymous], 2000, Gottinger Arbeiten Zur Geologie Und Palaontologie; [Anonymous], 1980, PALEOBIOLOGY PLANT P; BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; Batten D.J., 1982, J. 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J	Triki, HZ; Laabir, M; Lafabrie, C; Malouche, D; Bancon-Montigny, C; Gonzalez, C; Deidun, A; Pringault, O; Daly-Yahia, OK				Triki, Habiba Zmerli; Laabir, Mohamed; Lafabrie, Celine; Malouche, Dhafer; Bancon-Montigny, Chrystelle; Gonzalez, Catherine; Deidun, Alan; Pringault, Olivier; Daly-Yahia, Ons Kefi			Do the levels of industrial pollutants influence the distribution and abundance of dinoflagellate cysts in the recently-deposited sediment of a Mediterranean coastal ecosystem?	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Dinocyst assemblage; Mediterranean Bizerte Lagoon; Spatial distribution; Toxic/noxious species; Organic/inorganic contaminants; Interaction pollutants/cysts	POLYCYCLIC AROMATIC-HYDROCARBONS; RECENT MARINE-SEDIMENTS; SURFACE SEDIMENTS; BIZERTE LAGOON; RESTING CYSTS; ALEXANDRIUM-PSEUDOGONYAULAX; ENVIRONMENTAL-FACTORS; SPATIAL-DISTRIBUTION; GONYAULAX-EXCAVATA; BENTHIC CYSTS	We studied the relationships between sediment industrial pollutants concentrations, sediment characteristics and the dinoflagellate cyst abundance within a coastal lagoon by investigating a total of 55 sampling stations within the Bizerte lagoon, a highly anthropized Mediterranean ecosystem. The sediment of Bizerte lagoon is characterized by a high dinocyst abundance, reaching a maximum value of 2742 cysts.g(-1) of dry sediment. The investigated cyst diversity was characterized by the presence of 22 dominant dinocyst morphotypes belonging to 11 genera. Two dinoflagellate species dominated the assemblage: Alexandrium pseudogonyaulax and Protoperidinium claudicans, representing 29 to 89% and 5 to 38% of the total cyst abundance, respectively, depending on the station. Seven morphotypes belonging to potentially toxic species were detected, including Alexandrium minutum, A. pseudogonyaulax, Alexandrium catenella/tamarense species complex, Lingulodinium polyedrum, Gonyaulax cf. spinifera complex, Prorocentrum micans and Protoceratium reticulatum. Pearson correlation values showed a positive correlation (alpha = 0.05) between cyst abundance and both water content and fine silt sediment content. Clustering revealed that the highest abundance of cysts corresponds to stations presenting the higher amounts of heavy metals. The simultaneous autoregressive model (SAM) highlighted a significant correlation (alpha = 0.05) between cyst accumulation and two main factors: sediment water content and sediment content for several heavy metals, including Hg, Cd, Cu, Ni and Cr. These results suggest that the degree of heavy metal pollution could influence cyst accumulation patterns. (C) 2017 Elsevier B.V. All rights reserved.	[Triki, Habiba Zmerli; Daly-Yahia, Ons Kefi] Univ Carthage, INAT, UR Biol Marine FST EL Manar 1, IRESA, 43 Ave Charles Nicolle, Tunis 1082, Tunisia; [Laabir, Mohamed] Univ Montpellier, Lab Ecol Syst Marins Cotiers ECOSYM, CNRS, UM2,IRD,IFREMER,UM1,UMR 5119, Pl Eugene Bataillon, F-34095 Montpellier, France; [Lafabrie, Celine; Pringault, Olivier] Univ Montpellier, CNRS, UMR 9190, MARBEC IRD,Ifremer, Pl Eugene Bataillon,Case 093, F-34095 Montpellier 5, France; [Lafabrie, Celine; Pringault, Olivier] Univ Carthage, Fac Sci Bizerte, Zarzouna 7021, Tunisia; [Malouche, Dhafer] Ecole Super Stat & Analy Informat, Zarzouna, Tunisia; [Bancon-Montigny, Chrystelle] Univ Montpellier, CNRS, UMR 5569 HydroSci IRD, 163 Rue Auguste Broussonnet, F-34090 Montpellier, France; [Gonzalez, Catherine] LGEI, Ecole Mines Ales, 6 Ave Clavieres, F-30319 Ales, France; [Deidun, Alan] Univ Malte, Dept Geosci, Msida, Malta	Universite de Carthage; Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); Ifremer; Universite de Montpellier; Universite de Carthage; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Montpellier; IMT - Institut Mines-Telecom; IMT Mines Ales	Triki, HZ (通讯作者)，Univ Carthage, INAT, UR Biol Marine FST EL Manar 1, IRESA, 43 Ave Charles Nicolle, Tunis 1082, Tunisia.	bibarouma@hotmail.fr	Malouche, Dhafer/HOF-7025-2023; Montigny, Chrystelle/ACN-3124-2022; GONZALEZ, Catherine/H-7105-2012; MONTIGNY, Chrystelle/H-1993-2013; Pringault, Olivier/A-7399-2008	Deidun, Alan/0000-0002-6919-5374; MONTIGNY, Chrystelle/0000-0003-0734-7130; Pringault, Olivier/0000-0003-2363-8376; Gonzalez, Catherine/0000-0002-2660-6559; Malouche, Dhafer/0000-0002-0494-7141	JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program; LAGUNOTOX project; TOTAL Foundation; IRD (Institut Francais pour la Recherche et le Developpement)	JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program; LAGUNOTOX project; TOTAL Foundation(Total SA); IRD (Institut Francais pour la Recherche et le Developpement)	This work benefitted from financial supports of the JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program funded in turn by IRD (Institut Francais pour la Recherche et le Developpement), as well as from the LAGUNOTOX project funded by TOTAL Foundation.	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Total Environ.	OCT 1	2017	595						380	392		10.1016/j.scitotenv.2017.03.183	http://dx.doi.org/10.1016/j.scitotenv.2017.03.183			13	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	EV2AZ	28391143	Green Published			2025-03-11	WOS:000401556800038
J	Agrawal, S; Verma, P; Rao, MR; Garg, R; Kapur, VV; Bajpai, S				Agrawal, Shailesh; Verma, Poonam; Rao, M. R.; Garg, Rahul; Kapur, Vivesh V.; Bajpai, Sunil			Lignite deposits of the Kutch Basin, western India: Carbon isotopic and palynological signatures of the early Eocene hyperthermal event ETM2	JOURNAL OF ASIAN EARTH SCIENCES			English	Article						Carbon isotope excursion; Dinoflagellate cysts; Eocene hyperthermal; Kutch Basin; India; Spore-pollen	THERMAL MAXIMUM 2; LATE PALEOCENE; DINOFLAGELLATE CYSTS; NAREDI FORMATION; WARMING EVENTS; MIDDLE EOCENE; NEW-ZEALAND; DEEP-SEA; AGE; EXCURSIONS	This study presents new results of combined palynological and stable carbon isotope (delta C-13) investigations carried out in the well known lignite sequence at Panandhro, District Kutch, in the Gujarat state of western India. Dinoflagellate cysts and associated spore-pollen assemblage assign an early Eocene (Ypresian) age to the lignitic succession at Panandhro. Furthermore, a pronounced negative Carbon Isotope Excursion (CIE) of about 2.7 parts per thousand, correlated to the Second Eocene Thermal Maximum (53.7 Ma), a globally recognized hyperthermal event, was discovered in the middle part of the succession, consistent with the palynological constraints. This is the first record of an Eocene hyperthermal event (ETM2) from the Kutch Basin. Our data has regional implications for the age of the lignitic sequences across western India as it demonstrates that there is no significant age difference between the lignite deposits of the Kutch and Cambay basins. Our results also support a Lutetian age for the previously described vertebrate fossils, including whales, from the Panandhro mine section.	[Agrawal, Shailesh; Verma, Poonam; Rao, M. R.; Garg, Rahul; Kapur, Vivesh V.; Bajpai, Sunil] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Luclmow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Agrawal, S; Bajpai, S (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Luclmow 226007, Uttar Pradesh, India.	as.shail@gmail.com; sunilbajpai2001@yahoo.com	Agrawal, Shailesh/O-6255-2015; Kapur, Vivesh/AAO-4885-2021; Bajpai, Sunil/E-8416-2010		Department of Science and Technology (DST), New Delhi [SR/FTP/ES-49/2012]	Department of Science and Technology (DST), New Delhi(Department of Science & Technology (India))	The authors would like to thankfully acknowledge the use of infrastructural facilities at Birbal Salmi Institute of Palaeosciences (BSIP) where this investigation was entirely carried out (BSIP/RDCC/201617/46). One of the authors (VVK) acknowledges financial support from Department of Science and Technology (DST), New Delhi (Project no. SR/FTP/ES-49/2012). We acknowledge Gujarat Mineral Development Corporation (GMDC), Gujarat for giving permission for field work and thank the staff of Panandhro Lignite Mine, Gujarat for the logistic support. We thank the Associate Editor, Dr. Zhonghui Liu, and the two anonymous reviewers for their constructive comments and suggestions.	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J	Gu, F; Zonneveld, KAF; Chiessi, CM; Arz, HW; Pätzold, J; Behling, H				Gu, Fang; Zonneveld, Karin A. F.; Chiessi, Cristiano M.; Arz, Helge W.; Paetzold, Juergen; Behling, Hermann			Long-term vegetation, climate and ocean dynamics inferred from a 73,500 years old marine sediment core (GeoB2107-3) off southern Brazil	QUATERNARY SCIENCE REVIEWS			English	Article						Southern Brazil; South Atlantic; Pollen; Spores; Dinoflagellate cysts; Environmental changes; Late Quaternary	DINOFLAGELLATE CYSTS; ATMOSPHERIC CIRCULATION; DISTRIBUTION PATTERNS; SEASONAL VARIABILITY; LATE PLEISTOCENE; RIVER DISCHARGE; RAIN-FOREST; ATLANTIC; INSOLATION; RECORD	Long-term changes in vegetation and climate of southern Brazil, as well as ocean dynamics of the adjacent South Atlantic, were studied by analyses of pollen, spores and organic-walled dinoflagellate cysts (dinocysts) in marine sediment core GeoB2107-3 collected offshore southern Brazil covering the last 73.5 cal kyr BP. The pollen record indicates that grasslands were much more frequent in the landscapes of southern Brazil during the last glacial period if compared to the late Holocene, reflecting relatively colder and/or less humid climatic conditions. Patches of forest occurred in the lowlands and probably also on the exposed continental shelf that was mainly covered by salt marshes. Interestingly, drought-susceptible Araucaria trees were frequent in the highlands (with a similar abundance as during the late Holocene) until 65 cal kyr BP, but were rare during the following glacial period. Atlantic rainforest was present in the northern lowlands of southern Brazil during the recorded last glacial period, but was strongly reduced from 38.5 until 13.0 cal kyr BP. The reduction was probably controlled by colder and/or less humid climatic conditions. Atlantic rainforest expanded to the south since the Lateglacial period, while Araucaria forests advanced in the highlands only during the late Holocene. Dinocysts data indicate that the Brazil Current (BC) with its warm, salty and nutrient-poor waters influenced the study area throughout the investigated period. However, variations in the proportion of dinocyst taxa indicating an eutrophic environment reflect the input of nutrients transported mainly by the Brazilian Coastal Current (BCC) and partly discharged by the Rio Itajal (the major river closest to the core site). This was strongly related to changes in sea level. A stronger influence of the BCC with nutrient rich waters occurred during Marine Isotope Stage (MIS) 4 and in particular during the late MIS 3 and MIS 2 under low sea level. Evidence of Nothofagus pollen grains from the southern Andes during late MIS 3 and MIS 2 suggests an efficient transport by the southern westerlies and Argentinean rivers, then by the Malvinas Current and finally by the BCC to the study site. Major changes in the pollen/spore and dinocyst assemblages occur with similar pacing, indicating strongly interlinked continental and marine environmental changes. Proxy comparisons suggest that the changes were driven by similar overarching factors, of which the most important was orbital obliquity. (C) 2017 Elsevier Ltd. All rights reserved.	[Gu, Fang; Behling, Hermann] Univ Goettingen, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany; [Zonneveld, Karin A. F.; Paetzold, Juergen] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany; [Chiessi, Cristiano M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Rua Arlindo Bettio 1000, BR-03828000 Sao Paulo, SP, Brazil; [Arz, Helge W.] Leibniz Inst Balt Sea Res Warnemilnde IOW, Marine Geol Dept, Seestr 15, D-18119 Rostock, Germany	University of Gottingen; University of Bremen; Universidade de Sao Paulo	Gu, F (通讯作者)，Univ Goettingen, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany.	Fang.Gu@biologie.uni-goettingen.de	Chiessi, Cristiano/JAZ-0806-2023; Arz, Helge/A-6659-2013; Chiessi, Cristiano/E-1916-2012; Fapesp, Biota/F-8655-2017; Patzold, Jurgen/D-5111-2017	Chiessi, Cristiano/0000-0003-3318-8022; Fapesp, Biota/0000-0002-9887-8449; Gu, Fang/0000-0002-8181-2822; Arz, Helge Wolfgang/0000-0002-1997-1718; Patzold, Jurgen/0000-0001-8074-4103	China Scholarship Council (CSC); FAPESP [2012/17517-3, 2013/50297-0]; CAPES [1976/2014, 564/2015]; CNPq [302607/2016-1, 422255/2016-5]; Gary Comer science and education foundation (GCSEF); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [13/50297-0] Funding Source: FAPESP	China Scholarship Council (CSC)(China Scholarship Council); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Gary Comer science and education foundation (GCSEF); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	We thank Henry Hooghiemstra and an anonymous Reviewer for the constructive comments that greatly improved the manuscript. The sample material has been provided by the GeoB Core Repository at the MARUM - Center for Marine Environmental Sciences, University of Bremen, Germany. We thank Vera Bender for her help sampling the core. The data reported in this paper are archived in Pangaea (www.pangaea.de). Anastasia Poliakova is thanked with the support of dinocyst identification and interpretation. Fabienne Marret is thanked for comments on the ecological distribution of dinocysts. The financial support for this study is given to the first author from China Scholarship Council (CSC). Cristiano M. Chiessi acknowledges the financial support from FAPESP (grants 2012/17517-3 and 2013/50297-0), CAPES (grants 1976/2014 and 564/2015) and CNPq (302607/2016-1 and 422255/2016-5). We thank the captain and crew of RV Meteor for the successful recovery of the sediment core and the Gary Comer science and education foundation (GCSEF) that funded the thesis of Gerrit Heil.	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Sci. Rev.	SEP 15	2017	172						55	71		10.1016/j.quascirev.2017.06.028	http://dx.doi.org/10.1016/j.quascirev.2017.06.028			17	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	FI2ND					2025-03-11	WOS:000411774700005
J	Povilauskas, L				Povilauskas, Leticia			PALYNOSTRATIGRAPHY OF THE CRETACEOUS-PALEOGENE IN THE AUSTRAL BASIN, SW SANTA CRUZ PROVINCE, ARGENTINA	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						palynostratigraphy; pollen grains; spores; Cretaceous; Paleogene; Santa Cruz Province	TERTIARY BOUNDARY; NEW-ZEALAND; POLLEN; PALYNOMORPHS; ANTARCTICA; SPORES; ISLAND	This paper analyses the palynological assemblages recovered from the Cerro Cazador and Monte Chico formations and is an exhaustive study of the spore-pollen assemblages from the Cerro Dorotea Formation; all units with outcrops out in southwestern Santa Cruz Province, Argentina. Six sections were sampled in two main areas: Estancia San Jose and Estancia Laguna Salada. The palynological assemblages yielded by the studied formations are integrated with elements of marine (dinoflagellate cysts and acritarchs) and continental (spores and pollen grains) origin, present in different proportions throughout these units. Forty one species of pollen grains and spores were recognized in the Cerro Cazador Formation, 74 genera and 127 species in the Monte Chico Formation and 64 genera and 107 species in the Cerro Dorotea Formation. On the basis of the stratigraphic distribution of the identified species, four palynological assemblages were recognized, which were defined by the exclusive presence of characteristic species and their similarities with other spore-pollen assemblages. The following ages were suggested: (i)Association 1, upper sections of the Cerro Cazador Formation: upper Campanian-lower Maastrichtian; (ii) Association 2, lower and middle levels of the Monte Chico Formation: Maastrichtian, probably upper Maastrichtian; (iii) Association 3, upper levels of the Monte Chico Formation: Maastrichtian-Danian; and (iv) Association 4, Cerro Dorotea Formation: Danian. Based on this analysis, the K/P boundary is located between Associations 2 and 3, within the Monte Chico Fonnation. These palynological assemblages indicate a near-shore marine depositional environment close to the coastline, with marginal conditions, and a progressive shallowing of the basin.	[Povilauskas, Leticia] UNLP, Div Paleobot, Museo La Plata, Paseo Bosque S-N,C1900DJR, La Plata, Buenos Aires, Argentina	National University of La Plata; Museo La Plata	Povilauskas, L (通讯作者)，UNLP, Div Paleobot, Museo La Plata, Paseo Bosque S-N,C1900DJR, La Plata, Buenos Aires, Argentina.	lepovilauskas@gmail.com		Povilauskas, Leticia/0000-0002-5241-0883	CONICET; National Agency for Promotion of Science and Technology [PICT 32320]	CONICET(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); National Agency for Promotion of Science and Technology(ANPCyT)	The author is deeply grateful to the CONICET and the National Agency for Promotion of Science and Technology for financial support (PICT 32320).	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J	Da Silva, WG; De Souza, PA; Van Waveren, I				Da Silva, Wagner Guimaraes; De Souza, Paulo Alves; Van Waveren, Isabel			NEW INSIGHTS ON THE SYSTEMATIC CLASSIFICATION OF CERTAIN PALYNOLOGICAL TAXA (TINTINNOMORPHS) FROM HOLOCENE DEPOSITS OF THE COASTAL PLAIN OF SOUTHERN BRAZIL	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						tintinnomorphs; tintinnids; Holocene; Coastal Plain of Santa Catarina	NON-POLLEN PALYNOMORPHS; SANTA-CATARINA STATE; SEA-LEVEL; DINOFLAGELLATE CYSTS; LATE QUATERNARY; ORGANIC-MATTER; SEDIMENTS; PRESERVATION; INDICATORS; INDONESIA	Tintinnomorphs is a term used for the grouping of palynomorphs resembling organic remains of tintinnids, which are not always identifiable as true lorica, cysts or pouch, being able to correspond to other protozoans and may even represent others structures of distinct organisms, such as rotifers and turbellarians. This paper presents tintinnomorphs recorded in Holocene sediments of the well PSC-03, drilled in the Coastal Plain of Santa Catarina, southern Brazil. A total of six tintinnomorphs types is described and illustrated (SPHERO-1, ELELNO-14, ESABNO-6, HEXANO-2, RECTNO-1, AROBNO-3), some of which are compared with specimens previously reported from Quaternary deposits of southern Brazil, southern South America and other regions of the world. Although tintinomorphs are associated to marine palynomorphs, they cannot be used as a conclusive paleoenvironmental evidence due to uncertainties about their biological affinity.	[Da Silva, Wagner Guimaraes] Inst Fed Educ Ciencia & Tecnol Rio Grande do Sul, IFRS, Campus Osorio,Rua Santos Dumont 2127, BR-95520000 Osorio, RS, Brazil; [De Souza, Paulo Alves] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Lab Palinol Marleni Marques Toigo, Av Bento Gonsalves 9500, BR-91540000 Porto Alegre, RS, Brazil; [Van Waveren, Isabel] Nat Biodivers Ctr, P0B 9517, Leiden, Netherlands	Instituto Federal do Rio Grande do Sul (IFRS); Universidade Federal do Rio Grande do Sul; Naturalis Biodiversity Center	Da Silva, WG (通讯作者)，Inst Fed Educ Ciencia & Tecnol Rio Grande do Sul, IFRS, Campus Osorio,Rua Santos Dumont 2127, BR-95520000 Osorio, RS, Brazil.	wagner.guimaraes.silva@gmail.com; paulo.aloes.souza@ufrgs.br; isabeLvanwaveren@naturalis.nl	Alves de Souza, Paulo/O-9779-2018	Alves de Souza, Paulo/0000-0001-9844-1530	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [1012119]; Instituto Federal do Rio Grande do Sul, through its Human Resources Training Program (IFRS) [233670022072015-50]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); 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)); Instituto Federal do Rio Grande do Sul, through its Human Resources Training Program (IFRS)	The authors would like to thank the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) for the basic research project funding; the Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS, proc. 1012119) for complementary funding; the support of the Instituto Federal do Rio Grande do Sul, through its Human Resources Training Program (IFRS proc. 233670022072015-50); and R.B. 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SEP-DEC	2017	20	3					321	332		10.4072/rbp.2017.3.04	http://dx.doi.org/10.4072/rbp.2017.3.04			12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	GJ2KH		Bronze			2025-03-11	WOS:000435098900004
J	Salgado, P; Figueroa, RI; Ramilo, I; Bravo, I				Salgado, Pablo; Figueroa, Rosa I.; Ramilo, Isabel; Bravo, Isabel			The life history of the toxic marine dinoflagellate <i>Protoceratium reticulatum</i> (Gonyaulacales) in culture	HARMFUL ALGAE			English	Article						Life history; Longitudinal biflagellation; Protoceratium reticulatum; Sexual cycle; Planozygote and germling division; Resting cyst	GYMNODINIUM-CATENATUM DINOPHYCEAE; SP-NOV DINOPHYCEAE; SEXUAL REPRODUCTION; LINGULODINIUM-POLYEDRUM; ALEXANDRIUM-TAMUTUM; YESSOTOXINS PROFILE; SURFACE SEDIMENTS; MATING-TYPE; CYCLE; CYST	Asexual and sexual life cycle events were studied in cultures of the toxic marine dinoflagellate Protoceratium reticulatum. Asexual division by desmoschisis was characterized morphologically and changes in DNA content were analyzed by flow cytometry. The results indicated that haploid cells with a C DNA content occurred only during the light period whereas a shift from a C to a 2C DNA content (indicative of S phase) took place only during darkness. The sexual life cycle was documented by examining the mating type as well as the morphology of the sexual stages and nuclei. Gamete fusion resulted in a planozygote with two longitudinal flagella, but longitudinally biflagellated cells arising from planozygote division were also observed, so one of the daughter cells retained two longitudinal flagella while the other daughter cell lacked them. Presumed planozygotes (identified by their longitudinally biflagellated form) followed two life-cycle routes: division and encystment (resting cyst formation). Both the division of longitudinally biflagellated cells and resting cyst formation are morphologically described herein. Resting cyst formation through sexual reproduction was observed in 6.1% of crosses and followed a complex heterothallic pattern. Clonal strains underwent sexuality (homothallism for planozygote formation and division) but without the production of resting cysts. Ornamental processes of resting cysts formed from the cyst wall under an outer balloon-shaped membrane and were fully developed in <1 h. Obligatory dormancy period was of 4 months. Excystment resulted in a large, rounded, pigmented, longitudinally biflagellated but motionless, thecate germling that divided by desmoschisis. Like the planozygote, the first division of the germling yielded one longitudinally biflagellated daughter cell and another without longitudinal flagella. The longitudinal biflagellation state of both sexual stages and of the first division products of these cells is discussed. (C) 2017 Elsevier B.V. All rights reserved.	[Salgado, Pablo] Inst Fomento Pesquero IFOP, Enrique Abello 0552,Casilla 101, Punta Arenas, Chile; [Salgado, Pablo; Figueroa, Rosa I.; Ramilo, Isabel; Bravo, Isabel] Ctr Oceanog Vigo, IEO, Subida Radio Faro 50, Vigo 36390, Spain	Instituto de Fomento Pesquero (Valparaiso); Spanish Institute of Oceanography	Salgado, P (通讯作者)，Inst Fomento Pesquero IFOP, Enrique Abello 0552,Casilla 101, Punta Arenas, Chile.	pablo.salgado@ifop.cl; rosa.figueroa@vi.ieo.es; isabel.ramilo@vi.ieo.es; isabel.bravo@vi.ieo.es	Salgado, Pablo/KMA-0636-2024; Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015	Figueroa, Rosa/0000-0001-9944-7993; Bravo, Isabel/0000-0003-3764-745X	CCVIEO project; Spanish National Project CICAN [CGL2013-40671-R]; Subsecretaria de Pesca y Acuicultura (SUBPESCA) of the Ministerio de Economia, Fomento y Turismo; Instituto Espanol de Oceanografia (IEO)	CCVIEO project; Spanish National Project CICAN; Subsecretaria de Pesca y Acuicultura (SUBPESCA) of the Ministerio de Economia, Fomento y Turismo; Instituto Espanol de Oceanografia (IEO)	The authors thank Pilar Rial and Elena Fagin for technical support. Gemita Pizarro from Instituto de Fomento Pesquero (IFOP) for providing the P. reticulatum strains. Ines Pazos from CACTI, University of Vigo, for SEM microscopy. The present work was funded by the CCVIEO project and the Spanish National Project CICAN (CGL2013-40671-R). The Red Tide Monitoring Program of Southern Chile during which strains were isolated, was funded by the Subsecretaria de Pesca y Acuicultura (SUBPESCA) of the Ministerio de Economia, Fomento y Turismo and carried out by IFOP. This article will be part of the doctoral thesis of Pablo Salgado and is within the doctoral program "Marine Science, Technology and Management" (DO*MAR) of the University of Vigo. 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J	Shcherbinina, EA; Iakovleva, AI; Zakrevskaya, EY				Shcherbinina, E. A.; Iakovleva, A. I.; Zakrevskaya, E. Yu.			Middle Eocene to early Oligocene nannofossils and palynomorphs from the Landzhar section, southern Armenia: Zonal stratigraphy and paleoecology	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						nannofossils; palynomorphs; dinocysts; Bartonian; Priabonian; Paleogene; Armenia	WALLED DINOFLAGELLATE CYSTS; BIOSTRATIGRAPHY	The results of the study of nannofossils and palynomorphs from the Landzhar section in southern Armenia were used to correlate bioevents of two groups of microorganisms, recognize zonal subdivisions, and identify variations in the assemblage compositions reflecting changes in the hydrology and sedimentation regime in the basin during the middle Eocene to early Oligocene.	[Shcherbinina, E. A.; Iakovleva, A. I.] Russian Acad Sci, Geol Inst, Moscow, Russia; [Zakrevskaya, E. Yu.] Russian Acad Sci, Vernadsky State Geol Museum, Moscow, Russia	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Russian Academy of Sciences	Shcherbinina, EA (通讯作者)，Russian Acad Sci, Geol Inst, Moscow, Russia.	katuniash@gmail.com	закревская, Елена/HKM-9062-2023; IAKOVLEVA, ALINA/ABH-9243-2020		A Just Russia; Russian Foundation for Basic Research [15-55-05102, 15-05-07556]; Geological Institute, Russian Academy of Sciences [0135-2014-0070, 01201459195, 0135-2016-0001]	A Just Russia; Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Geological Institute, Russian Academy of Sciences	We are grateful to M.A. Akhmetiev, A.Yu. Gladenkov, and Yu.B. Gladenkov for careful reading of the paper and fruitful discussion; G.N. Aleksandrova (Geological Institute, Russian Academy of Sciences) for chemical preparation of samples for palynological analysis; F.A. Airapetyan and A.G. Israelyan (Institute of Geological Sciences, National Academy of Sciences of the Republic of Armenia) for their assistance with field work; and A.S. Karakhanyan, director of the Institute of Geological Sciences, National Academy of Sciences of the Republic of Armenia, and the institute's staff for arrangement of field work. We also thank S.M. Mironov, leader of the party A Just Russia, for financial support of the 2014 field trip.This study was supported by the Russian Foundation for Basic Research (project nos. 15-55-05102 and 15-05-07556). The study of nannofossils and palynomorphs was performed as part of the government contracts with the Geological Institute, Russian Academy of Sciences (project nos. 0135-2014-0070, 01201459195, and 0135-2016-0001).	Agamalyan V.A., 2012, UCH ZAP YEREVAN STAT, P3; Agnini C, 2014, NEWSL STRATIGR, V47, P131, DOI 10.1127/0078-0421/2014/0042; Agnini C, 2011, GEOL SOC AM BULL, V123, P841, DOI 10.1130/B30158.1; Airapetyan F. 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SEP	2017	25	5					557	580		10.1134/S0869593817050069	http://dx.doi.org/10.1134/S0869593817050069			24	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	FJ2HY					2025-03-11	WOS:000412547000006
J	Mathewes, RW; Clague, JJ				Mathewes, Rolf W.; Clague, John J.			Paleoecology and ice limits of the early Fraser glaciation (Marine Isotope Stage 2) on Haida Gwaii, British Columbia, Canada	QUATERNARY RESEARCH			English	Article						Fraser glaciation; Glacial geology; Last glacial maximum; MIS 2; Stratigraphy; Paleoecology; Refugia; Geochronology; Haida Gwaii; British Columbia	QUEEN-CHARLOTTE-ISLANDS; LATE WISCONSIN GLACIATION; LATE QUATERNARY GEOLOGY; ALEXANDER ARCHIPELAGO; POLLEN MORPHOLOGY; CONTINENTAL-SHELF; QUADRA SAND; REFUGIUM	Our study combines new geological and paleoecological information to reconstruct the glacial history and terrestrial paleoenvironments on Haida Gwaii during the advance phase of the Fraser glaciation (Marine Isotope Stage 2). At Cape Ball on eastern Graham Island, five accelerator mass spectrometry radiocarbon ages ranging from 23,200 +/- 280 to 26,650 +/- 390 C-14 yr BP (ca. 27,000-31,400 cal yr BP) record the earliest approach of mainland glaciers to Haida Gwaii. Abundant marine dinoflagellate cysts indicate isostatic depression by glacial ice in Hecate Strait to the east. At Mary Point on the north coast of Graham Island, similar outwash of a piedmont lobe advancing westward along Dixon Entrance preserves plant remains dated from 19,270 +/- 360 to 23,740 +/- 300 C-14 yr BP (22,500-28,600 cal yr BP). These sediments also contain marine indicators. Plant macrofossils, pollen, and invertebrates support the geological evidence of a proglacial environment under a colder-than-present macroclimate. Although some trees were likely present on Graham Island at this time, tundra-like plant communities dominated low-lying areas. A large area that appears to have been ice-free during this time is a portion of the continental shelf off the east coast of Moresby Island, referred to provisionally as the "Hecate Refugium."	[Mathewes, Rolf W.] Simon Fraser Univ, Dept Biol Sci, 8888 Univ Dr, Burnaby, BC V5A 1S6, Canada; [Clague, John J.] Simon Fraser Univ, Dept Earth Sci, 8888 Univ Dr, Burnaby, BC V5A 1S6, Canada	Simon Fraser University; Simon Fraser University	Mathewes, RW (通讯作者)，Dept Biol Sci, 8888 Univ Dr, Burnaby, BC V5A 1S6, Canada.	mathewes@sfu.ca	Clague, John/L-3619-2019	MATHEWES, ROLF/0000-0001-7637-199X	Natural Sciences and Engineering Research Council of Canada [A3835, A24595]; Simon Fraser University	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Simon Fraser University	We thank Calvin J. Heusser (deceased), John V. Matthews Jr., Alice Telka, and Erle Nelson for field assistance at Mary Point. We also thank W.B. Schofield (deceased) for fossil moss identifications, Ian R. Walker for chironomid identification, and Vera Pospelova for confirming our dinoflagellate identifications. Erle Nelson provided the McMaster University (RIDDL) radiocarbon ages. Marlow Pellatt and Matt Huntley helped prepare some of the figures. Two anonymous reviewers helped to improve the manuscript. Funding was provided by the Natural Sciences and Engineering Research Council of Canada through Discovery Grants A3835 to RM and A24595 to JC, and from Simon Fraser University through Associate Dean research funds to RM.	[Anonymous], THE OUTER SHORES; [Anonymous], 1989, INDICATOR PLANTS COA; Barrie J. V., 1991, CONTINENTAL SHELF RE, V11, P710; Barrie JV, 2005, PACIF RIM ARCHAEOL, P7; Barrie JVaughan., 1993, QUATERN INT, V20, P123, DOI DOI 10.1016/1040-6182(93)90041-D; BLAISE B, 1990, QUATERNARY RES, V34, P282, DOI 10.1016/0033-5894(90)90041-I; Calder J. 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Res.	SEP	2017	88	2					277	292		10.1017/qua.2017.36	http://dx.doi.org/10.1017/qua.2017.36			16	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	FF5OB					2025-03-11	WOS:000409040600009
J	Ferraro, L; Rubino, F; Belmonte, M; Da Prato, S; Greco, M; Frontalini, F				Ferraro, L.; Rubino, F.; Belmonte, M.; Da Prato, S.; Greco, M.; Frontalini, F.			A multidisciplinary approach to study confined marine basins: the holobenthic and merobenthic assemblages in the Mar Piccolo of Taranto (Ionian Sea, Mediterranean)	MARINE BIODIVERSITY			English	Article						Holobenthos; Merobenthos; Foraminifera; Ostracods; Plankton resting stages; Confined marine areas; Mediterranean Sea	WALLED DINOFLAGELLATE CYSTS; BENTHIC FORAMINIFERAL FAUNAS; SOUTHERN ADRIATIC SEA; SURFACE SEDIMENTS; MARGINAL MARINE; HEAVY-METALS; MYTILUS-GALLOPROVINCIALIS; TAXONOMIC CLARIFICATION; ZOOPLANKTON COMPOSITION; ENVIRONMENTAL CONTROLS	Benthic foraminifera and ostracods, and resting stages (cysts) of plankton were analysed from surface sediment samples collected at 20 stations in the Mar Piccolo of Taranto (Ionian Sea, Mediterranean), with the aim to advance our knowledge on the biodiversity and ecological features of confined marine areas and to upgrade the autoecology of the species, and to have a more detailed and complete information to be applied as the baseline in future studies on environmental quality. In order to better assess the spatial distribution of the holobenthic and merobenthic species, we conceived a simple method of spatial analysis, based on all the identified taxa of foraminifera, ostracods and plankton cysts. Five groups were established on the basis of the number of sites per sub-basin where each taxon was registered, and this allowed us to recognise the preferential patterns of distribution for 150 species. The good correspondence between the results of the spatial analysis and those obtained from the analysis of the communities and the uni- and multivariate statistics showed a clear difference between the two sub-basins of the Mar Piccolo of Taranto.	[Ferraro, L.] CNR, Ist Ambiente Marino Costiero Calata Porta di Mass, I-80133 Naples, Italy; [Rubino, F.; Belmonte, M.] CNR, Ist Ambiente Marino Costiero, UOS Taranto, Via Roma 3, I-74123 Taranto, Italy; [Da Prato, S.] CNR, Ist Geosci & Georisorse, Via Moruzzi 1, I-56124 Pisa, Italy; [Greco, M.; Frontalini, F.] Univ Urbino Carlo Bo, Dipartimento Sci Pure & Applicate DiSPeA, I-61029 Urbino, Italy	Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR); Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR); Consiglio Nazionale delle Ricerche (CNR); Istituto di Geoscienze e Georisorse (IGG-CNR); University of Urbino	Rubino, F (通讯作者)，CNR, Ist Ambiente Marino Costiero, UOS Taranto, Via Roma 3, I-74123 Taranto, Italy.	rubino@iamc.cnr.it	Rubino, Fernando/GOP-0332-2022; Ferraro, Luciana/AAX-6983-2020; Belmonte, Marisol/AAG-9759-2019; Frontalini, Fabrizio/C-4819-2008; Greco, Mattia/HOF-9207-2023	Greco, Mattia/0000-0003-2416-6235; Rubino, Fernando/0000-0003-2552-2510; Ferraro, Luciana/0000-0002-6491-2274	CNR-Institute for Coastal Marine Environment of Taranto; Dipartimento di Scienze Pure e Applicate (DiSPeA); Universita degli Studi di Urbino "Carlo Bo"; CNR-Istituto di Geoscienze e Georisorse, Pisa, Italy	CNR-Institute for Coastal Marine Environment of Taranto; Dipartimento di Scienze Pure e Applicate (DiSPeA); Universita degli Studi di Urbino "Carlo Bo"; CNR-Istituto di Geoscienze e Georisorse, Pisa, Italy	The field and laboratory work was financially supported by the CNR-Institute for Coastal Marine Environment of Taranto, Dipartimento di Scienze Pure e Applicate (DiSPeA), Universita degli Studi di Urbino "Carlo Bo" and CNR-Istituto di Geoscienze e Georisorse, Pisa, Italy. Special thanks are owed to Mr. Cosimo Macripo for his technical assistance aboard the 'Aristocle.' The two anonymous reviewers contributed to improve the manuscript thanks to their very accurate comments.	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F., 2005, Palaeontologische Zeitschrift, V79, P61	140	11	11	2	20	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1867-1616	1867-1624		MAR BIODIVERS	Mar. Biodivers.	SEP	2017	47	3					887	911		10.1007/s12526-016-0523-0	http://dx.doi.org/10.1007/s12526-016-0523-0			25	Biodiversity Conservation; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Marine & Freshwater Biology	FF5DB					2025-03-11	WOS:000408993600028
J	Aktan, Y; Keskin, Ç				Aktan, Yelda; Keskin, Cetin			Second Habitat Record of <i>Polykrikos hartmannii</i> W. Zimm. (Dinophyceae) in the South Aegean Sea, Eastern Mediterranean	TURKISH JOURNAL OF FISHERIES AND AQUATIC SCIENCES			English	Article						Dinoflagellates; Ichthyotoxicity; Eastern Mediterrannean Sea; Aquaculture	GULF-OF-CALIFORNIA; DINOFLAGELLATE RESTING CYSTS; HARMFUL ALGAL BLOOMS; RECENT SEDIMENTS; LA-PAZ; BAY; SHALLOW; MARINE; BAHIA; USA	Polykrikos hartmannii, a harmful and ichthyotoxic marine dinoflageallate, has been widely distributed in temperate and tropical waters. In this study, P. hartmannii, previously recorded from fossil's, is recorded for the first time in the South Aegean Sea, Eastern Mediterranean from living cells. This study provides information on the new distribution areas of the species in the south-eastern Aegean Sea.	[Aktan, Yelda; Keskin, Cetin] Istanbul Univ, Fisheries Fac, Ordu St 200, TR-34470 Istanbul, Turkey	Istanbul University	Aktan, Y (通讯作者)，Istanbul Univ, Fisheries Fac, Ordu St 200, TR-34470 Istanbul, Turkey.	yaktan@istanbul.edu.tr	AKTAN TURAN, Yelda/AAD-1812-2020; Keskin, Cetin/LHA-5342-2024	Aktan Turan, Yelda/0000-0001-7920-8979; Keskin, Cetin/0000-0002-2434-0355				Aktan Yelda, 2011, Journal of the Black Sea Mediterranean Environment, V17, P159; Aktan Y, 2011, ESTUAR COAST SHELF S, V91, P551, DOI 10.1016/j.ecss.2010.12.010; Badylak S, 2004, J PLANKTON RES, V26, P1229, DOI 10.1093/plankt/fbh114; Balkis N, 2016, PHYCOLOGIA, V55, P187, DOI 10.2216/15-93.1; Balkis Neslihan, 2004, Journal of the Black Sea Mediterranean Environment, V10, P123; Basterretxea G, 2007, MAR ECOL PROG SER, V352, P53, DOI 10.3354/meps07168; Baula IU, 2011, HARMFUL ALGAE, V11, P33, DOI 10.1016/j.hal.2011.07.002; Birincioglu SS, 2013, KAFKAS UNIV VET FAK, V19, P343, DOI 10.9775/kvfd.2012.7847; CHATTON EDOUARD, 1933, BULL SOC ZOOL FRANCE, V58, P251; D'Costa PM, 2008, ESTUAR COAST SHELF S, V77, P77, DOI 10.1016/j.ecss.2007.09.002; Escobar-Morales S, 2015, BOT MAR, V58, P9, DOI 10.1515/bot-2014-0049; Ferrante M., 2013, HARMFUL ALGAL BLOOMS, V2, P587, DOI DOI 10.4172/SCIENTIFICREPORTS.587; Fujii R, 2006, J PLANKTON RES, V28, P131, DOI 10.1093/plankt/fbi106; Garate-Lizarraga I, 2014, CICIMAR Oceanides, V29, P25; Garate-Lizarraga I., 2008, Harmful Algae News, V37, P6; Gárate-Lizárraga I, 2013, MAR POLLUT BULL, V67, P217, DOI 10.1016/j.marpolbul.2012.11.031; Giacobbe MG, 2007, HYDROBIOLOGIA, V580, P125, DOI 10.1007/s10750-006-0459-7; Gómez F, 2006, J BIOGEOGR, V33, P261, DOI 10.1111/j.1365-2699.2005.01373.x; Gómez F, 2003, BOT MAR, V46, P215, DOI 10.1515/BOT.2003.021; Guiry MD., 2017, AlgaeBase; Hall NS, 2008, ESTUAR COAST, V31, P402, DOI 10.1007/s12237-008-9035-x; Hernández-Becerril DU, 2007, J ENVIRON SCI HEAL A, V42, P1349, DOI 10.1080/10934520701480219; Hoppenrath M, 2007, J PHYCOL, V43, P366, DOI 10.1111/j.1529-8817.2007.00319.x; Hoppenrath M, 2010, EUR J PROTISTOL, V46, P29, DOI 10.1016/j.ejop.2009.08.003; HULBURT EM, 1957, BIOL BULL-US, V112, P196, DOI 10.2307/1539198; Koray T., 2001, J FISHERIES AQUATIC, V18, P1; Larsen J., 2004, OPERA BOT, V140, P117; Lee Joon-Baek, 1998, Journal of Fisheries Science and Technology, V1, P283; MATSUOKA K, 1986, J PLANKTON RES, V8, P811, DOI 10.1093/plankt/8.4.811; Mizushima Koichiro, 2007, Plankton & Benthos Research, V2, P163, DOI 10.3800/pbr.2.163; Moncheva S., 2015, ABUNDANCE BIOMASS PH; Morquecho L, 2003, BOT MAR, V46, P132, DOI 10.1515/BOT.2003.014; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Okaichi T., 2003, RED TIDES, P7; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Peña-Manjarrez JL, 2005, CONT SHELF RES, V25, P1375, DOI 10.1016/j.csr.2005.02.002; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; Ruiz GM, 1997, AM ZOOL, V37, P621; Shin HH, 2011, ESTUAR COAST, V34, P712, DOI 10.1007/s12237-011-9373-y; Shin HH, 2010, MAR POLLUT BULL, V60, P1243, DOI 10.1016/j.marpolbul.2010.03.019; Srivilai Dusit, 2012, Coastal Marine Science, V35, P11; Steidinger Karen A., 1995, P387; Tang YZ, 2013, J PHYCOL, V49, P1084, DOI 10.1111/jpy.12114; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x; Yildirim O., 2004, E.U. Su Urunleri Dergisi, V21, P361; Yucel-Gier G, 2013, TURK J FISH AQUAT SC, V13, P737, DOI 10.4194/1303-2712-v13_4_19; ZIMMERMANN WALTER, 1930, ZEITSCHR BOT, V23, P419	48	4	4	3	19	CENTRAL FISHERIES RESEARCH INST	TRABZON	PO BOX 129, TRABZON, 61001, TURKEY	1303-2712			TURK J FISH AQUAT SC	Turk. J. Fish. Quat. Sci.	SEP	2017	17	5					1077	1081		10.4194/1303-2712-v17_5_25	http://dx.doi.org/10.4194/1303-2712-v17_5_25			5	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	FC3ZG		Bronze			2025-03-11	WOS:000406777500025
J	Estebenet, MSG; Guerstein, GR; Raising, MER; Ponce, JJ; Alperín, MI				Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.; Rodriguez Raising, Martin E.; Ponce, Juan J.; Alperin, Marta I.			Dinoflagellate cyst zonation for the middle to upper Eocene in the Austral Basin, southwestern Atlantic Ocean: implications for regional and global correlation	GEOLOGICAL MAGAZINE			English	Article						dinoflagellate cyst; Eocene; biostratigraphy; palaeoenvironment; Austral Basin; Argentina	SANTA-CRUZ PROVINCE; TIERRA-DEL-FUEGO; SOUTHERN-OCEAN; DRAKE PASSAGE; PALEOGENE; ARGENTINA; PATAGONIA; BIOSTRATIGRAPHY; AREA; RECONSTRUCTIONS	The well-exposed marine Eocene units from southwestern Patagonia, Argentina, contain useful information for reconstructing regional climate and oceanographic patterns in an area adjacent to the Drake Passage. The aim of this paper is to integrate dinoflagellate cyst data from three sections of the southwestern Austral Basin (Rio Turbio Formation) to propose a zonation scheme, which can be applied to other southwestern Atlantic Ocean sites. Assemblages of organic walled dinoflagellate cysts have been analysed in different cropping-out sections and cores, showing the high potential of this fossil group as biostratigraphic markers. Comparison of dinoflagellate cyst events of the upper member of the Rio Turbio Formation with calibrated biostratigraphic ranges in the Palaeogene South Pacific Ocean allowed us to date and correlate these sedimentary sections. The resulting zonation consists of four dinoflagellate cyst zones labelled RTF 1 to RTF 4, between the middle Lutetian and late Priabonian. As a final point, we applied dinoflagellate cyst species with importance as palaeoenvironmental markers to assess long-term climatic and oceanographic evolution for the area. This study shows that the endemic-Antarctic dinoflagellate cyst assemblage is dominant during the middle to late Eocene (RTF 1 to RTF 3), while a significant replacement of these taxa by cosmopolitan species characterizes the upper part of the upper member of the Rio Turbio Formation (RTF 4). This turnover seems to be a consequence of changes in the ocean circulation patterns forced by deepening of the southern Atlantic gateways (the Drake Passage and the Tasman Gateway).	[Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.] Univ Nacl Sur, Dept Geol, Inst Geol Sur, San Juan 670,B8000ICN, Bahia Blanca, Buenos Aires, Argentina; [Gonzalez Estebenet, M. Sol; Raquel Guerstein, G.; Ponce, Juan J.] Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina; [Rodriguez Raising, Martin E.] Yacimientos Petroliferos Fiscales SA, Oficinas Cent, Av Libertador 520, RA-9005 Comodoro Rivadavia, Chubut, Argentina; [Ponce, Juan J.] Univ Nacl Rio Negro, Inst Invest Paleobiol & Geol, Sede Alto Valle, Argentina; [Alperin, Marta I.] Univ Nacl La Plata, Fac Ciencias Nat & Museo, Calle 64 S-N E-Bv 120 & Diag 113, RA-1900 La Plata, Buenos Aires, Argentina	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	Estebenet, MSG (通讯作者)，Univ Nacl Sur, Dept Geol, Inst Geol Sur, San Juan 670,B8000ICN, Bahia Blanca, Buenos Aires, Argentina.; Estebenet, MSG (通讯作者)，Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina.	solge3@hotmail.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 O. Cardenas for palynological technical assistance, and J. Cornago for improving the language of the manuscript before submission. Rob Fensome and Peter Bijl are thanked for useful comments and suggestions that led to significant improvements to the new version of the manuscript. 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/H125).	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SEP	2017	154	5					1022	1036		10.1017/S0016756816000601	http://dx.doi.org/10.1017/S0016756816000601			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FE8GC		Green Published			2025-03-11	WOS:000408442600006
J	Lindström, S; Erlström, M; Piasecki, S; Nielsen, LH; Mathiesen, A				Lindstrom, Sofie; Erlstrom, Mikael; Piasecki, Stefan; Nielsen, Lars Henrik; Mathiesen, Anders			Palynology and terrestrial ecosystem change of the Middle Triassic to lowermost Jurassic succession of the eastern Danish Basin	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palynology; Spore-pollen; Paleoclimate; Triassic; Early Jurassic; End-Triassic event	TRIASSIC/JURASSIC BOUNDARY; DINOFLAGELLATE CYST; TRANSITION; MOUNTAINS; PALYNOFACIES; VEGETATION; PATTERNS; AFFINITY; CLIMATE; SCANIA	The pre-Rhaetian Triassic succession in the Danish Basin is generally dominated by red bed deposits unsuitable for preservation of organic material. However, during the late Middle Triassic a temporary change to wetter conditions resulted in preservation of diverse palynofloral assemblages, dominated by corystospermous seed fern pollen of Alisporites/Falcisporites and characterized by high abundances of the conifer pollen Protodiploxypinus gracilis, as well as common to abundant lycophyte spores assigned to Aratrisporites spp. A mid-Ladinian to early Camian (earliest Julian) age is inferred for this interval based on the presence of the probable gymnosperm pollen Staurosaccites quadrifidus, rare Retisulcites perforatus (of unknown affinity) and Enzonalasporites vigens of probably voltzialean affinity. No marine palynomorphs were recorded, only rare specimens of Ovoidites sp. and Plaesiodictyon mosellanum. Thus, together with previously recorded other fossils (a fish microfauna, an ostracod, plant remains and characeans) the recorded palynoflora indicates semi-arid conditions and deposition in a terrestrial to marginal fresh- or brackish water environment. After this, red bed deposition resumed in the area, and it is not until the mid-Rhaetian that well preserved and diverse palynofloras are again encountered in the succession. The Rhaetian palynofloras are significantly different to the Ladinian-early Carnian assemblages, being dominated by tree fern spores (Deltoidospora spp.), taxodiacean/cupressacean pollen (Perinopollenites elatoides), and the enigmatic gymnosperm pollen assigned to Ricciisporites tuberculatus. As much as 62% of the mid-Ladinian to Early Carnian spore-pollen taxa were not recorded in the Rhaetian, suggesting that major restructuring of the terrestrial ecosystem took place in this area during the Carnian and Norian. In comparison, 34% of the Rhaetian spore-pollen taxa recorded in this study, e.g. R. tuberculatus, Polypodiisporites polymicroforatus, Limbosporites lundbladiae and Cingulizonates rhaeticus, disappeared during the well-recognized end-Triassic event. The extinction interval is also characterized by a dramatic increase in the number of reworked palynomorphs, indicating erosion of the hinterland at this time. There is a marked drop in diversity from the Late Triassic to the earliest Jurassic. The palynology indicates that the established post-extinction vegetation was dominated by tree ferns (Deltoidospora) and pinacean conifers (Pinuspollenites minimus), along with common taxodiacean/cupressacean conifers, ginkgos/cycads and corystospermous seed ferns, and that it remained relatively stable during the Hettangian to early Sinemurian. (C) 2017 Elsevier B.V. All rights reserved.	[Lindstrom, Sofie; Piasecki, Stefan; Nielsen, Lars Henrik; Mathiesen, Anders] GEUS, Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Erlstrom, Mikael] SGU, Geol Survey Sweden, Kiliansgatan 10, SE-22350 Lund, Sweden; [Piasecki, Stefan] Nat Hist Museum Denmark, Geol Museum, Oster Voldgade 5-7, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Lindström, S (通讯作者)，GEUS, Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	sli@geus.dk	Lindström, Sofie/G-5481-2018; Mathiesen, Anders/H-3115-2018; Nielsen, Lars Henrik/G-7842-2018	Mathiesen, Anders/0000-0003-4345-7513; Nielsen, Lars Henrik/0000-0002-2078-7360; Lindstrom, Malin Sofie/0000-0001-8278-1055	Danish Council for Strategic Research	Danish Council for Strategic Research(Danske Strategiske Forskningsrad (DSF))	This paper is published with permission of the Geological Survey of Denmark and Greenland and is an outcome of the project "The geothermal energy potential in Denmark - reservoir properties, temperature distribution and models for utilization" under the "Sustainable Energy and Environment" program funded by the Danish Council for Strategic Research. Part of the work was performed within a Geocenter Denmark funded project to SL. Jette Halskov is acknowledged for help with the illustrations. The authors are greatful for helpful comments from two anonymous reviewers and editor Mike Stephenson.	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J	Hattenrath-Lehmann, TK; Gobler, CJ				Hattenrath-Lehmann, Theresa K.; Gobler, Christopher J.			Identification of unique microbiomes associated with harmful algal blooms caused by <i>Alexandrium fundyense</i> and <i>Dinophysis acuminata</i>	HARMFUL ALGAE			English	Article						Alexandrium; Bacteria; Dinophysis; HAB; Microbiome; Microbial; Sequencing	PSEUDO-NITZSCHIA-MULTISERIES; CYST FORMATION; TOXIC DINOFLAGELLATE; HIROSHIMA BAY; BACTERIAL COMMUNITIES; DIVERSITY; TAMARENSE; PARASITISM; GULF; ECOLOGY	Biotic interactions dominate plankton communities, yet the microbial consortia associated with harmful algal blooms (HABs) have not been well-described. Here, high-throughput amplicon sequencing of ribosomal genes was used to quantify the dynamics of bacterial (16S) and phytoplankton assemblages (18S) associated with blooms and cultures of two harmful algae, Alexandrium fundyense and Dinophysis acuminata. Experiments were performed to assess changes in natural bacterial and phytoplankton communities in response to the filtrate from cultures of these two harmful algae. Analysis of prokaryotic sequences from ecosystems, experiments, and cultures revealed statistically unique bacterial associations with each HAB. The dinoflagellate, Alexandrium, was strongly associated with multiple genera of Flavobacteria including Owenweeksia spp., Maribacter spp., and individuals within the NS5 marine group. While Flavobacteria also dominated Dinophysis-associated communities, the relative abundance of Alteromonadales bacteria strongly co-varied with Dinophysis abundances during blooms and Ulvibacter spp. (Flavobacteriales) and Arenicella spp. (Gammaproteobacteria) were associated with cells in culture. Eukaryotic sequencing facilitated the discovery of the endosymbiotic, parasitic dinoflagellate, Amoebophrya spp., that had not been regionally described but represented up to 17% of sequences during Alexandrium blooms. The presence of Alexandrium in field samples and in experiments significantly altered the relative abundances of bacterial and phytoplankton by both suppressing and promoting different taxa, while this effect was weaker in Dinophysis. Experiments specifically revealed a negative feedback loop during blooms whereby Alexandrium filtrate promoted the abundance of the parasite, Amoebophrya spp. Collectively, this study demonstrates that HABs formed by Alexandrium and Dinophysis harbor unique prokaryotic and eukaryotic microbiomes that are likely to, in turn, influence the dynamics of these HABs. (C) 2017 Elsevier B.V. All rights reserved.	[Hattenrath-Lehmann, Theresa K.; Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Southampton, NY 11968 USA	State University of New York (SUNY) System; Stony Brook University	Gobler, CJ (通讯作者)，SUNY Stony Brook, Sch Marine & Atmospher Sci, Southampton, NY 11968 USA.	christopher.gobler@stonybrook.edu	Gobler, Christopher/JOZ-2924-2023		NOAA's Monitoring and Event Response to Harmful Algal Blooms (MERHAB) [NA11NOS4780027]; Chicago Community Trust; Rauch Foundation	NOAA's Monitoring and Event Response to Harmful Algal Blooms (MERHAB); Chicago Community Trust; Rauch Foundation	We would like to thank Jennifer Jankowiak and Tony Walters for assistance with R code and QIIME troubleshooting, respectively. 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Zhuang YY, 2015, HARMFUL ALGAE, V42, P60, DOI 10.1016/j.hal.2014.12.006	98	43	45	3	83	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	SEP	2017	68						17	30		10.1016/j.hal.2017.07.003	http://dx.doi.org/10.1016/j.hal.2017.07.003			14	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	FJ7SE	28962978	Green Published			2025-03-11	WOS:000412958300002
J	Shin, HH; Li, Z; Kim, ES; Park, JW; Lim, WA				Shin, Hyeon Ho; Li, Zhun; Kim, Eun Song; Park, Jong -Woo; Lim, Weol Ae			Which species, <i>Alexandrium catenella</i> (Group I) or <i>A-pacificum</i> (Group IV), is really responsible for past paralytic shellfish poisoning outbreaks in Jinhae-Masan Bay, Korea?	HARMFUL ALGAE			English	Article						Paralytic shellfish poisoning; Alexandrium cyst; Alexandrium catenella (Group I); Alexandrium pacificum (Group IV); Large subunit ribosomal sequence; Korea	EAST CHINA SEA; COCHLODINIUM-POLYKRIKOIDES MARGALEF; RESTING CYSTS; TAMARENSE DINOPHYCEAE; COMPLEX DINOPHYCEAE; TOXIN COMPOSITION; VEGETATIVE CELLS; COASTAL WATERS; BALLAST WATER; SEDIMENT TRAP	Paralytic shellfish poisoning (PSP) caused the deaths of four people in coastal area of Korea, mainly Jinhae-Masan Bay and adjacent areas, in April 1986 and in 1996. The PSP outbreaks were caused by the consumption of mussels, Mytilus edulis. The organism that caused PSP was identified, from morphological data only, as Alexandrium tamarense which is recently renamed as A. catenella, however recent studies have shown that the morphological diagnostic characteristics used to identify Alexandrium species have uncertainties and molecular tools and other criteria should be considered as well. The organism that caused past PSP outbreaks and incidents in Korea therefore need to be carefully reconsidered. The aim of this study was to re-evaluate the species really responsible for past outbreaks of PSP in Jinhae-Masan Bay, Korea. The temporal production and fluxes of the resting cysts of Alexandrium species were investigated for one year (from March 2011 to February 2012) using a sediment trap, and the morphology and phylogeny of vegetative cells germinated from the resting cysts were analysed. The production of Alexandrium species peaked in August and November, when temporal discrepancies were found in the water temperature (22.4 and 22.7 degrees C in August, 19.1 and 19.6 degrees C in November) and salinity (29.5 and 26.1 psu in August, 30.5 and 31.8 psu in November). The morphological data revealed that Alexandrium species germinated from resting cysts collected in August have a ventral pore on the 1' plate, whereas the 1' plate in Alexandrium species germinated from resting cysts collected in November lacks a ventral pore. Molecular phylogenetic data for the vegetative cells from the germination experiments allowed the August and November peaks to be assigned to Alexandrium catenella (Group I) and A. pacificum (Group IV), respectively. This indicates that the production of resting cysts of A. catenella can be enhanced by relatively high water temperature. This result is not consistent with those of previous studies that A. catenella responsible for PSP outbreaks was found at relatively low water temperature. In addition, large subunit ribosomal sequences data revealed that A. pacificum isolates from Korea were closely related to those from Australia, Japan and New Zealand where the PSP toxicity of shellfish and blooms occurred in the 1990s, indicating that the introduction of toxic dinoflagellates were related to ballast water from bulk-cargo shipping. Based on these results, we concluded that past PSP outbreaks in Jinhae-Masan Bay of Korea could have been caused by A. pacificum rather than by A. catenella. (C) 2017 Elsevier B.V. All rights reserved.	[Shin, Hyeon Ho; Li, Zhun; Kim, Eun Song] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea; [Park, Jong -Woo; Lim, Weol Ae] Natl Inst Fisheries Sci, Busan 619705, South Korea	Korea Institute of Ocean Science & Technology (KIOST); National Institute of Fisheries Science	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea.; Lim, WA (通讯作者)，Natl Inst Fisheries Sci, Busan 619705, South Korea.	shh961121@kiost.ac.kr; limwa@korea.kr	LI, ZHUN/GLT-3478-2022	Shin, Hyeon Ho/0000-0002-9711-6717; LI, ZHUN/0000-0001-8961-9966	KIMST; NIFS [R2017047]; KIOST [PE99513, PE99515]	KIMST(Korea Institute of Marine Science & Technology Promotion (KIMST)); NIFS; KIOST	This work was supported by grants from KIMST, NIFS (R2017047) and KIOST (PE99513 and PE99515). 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J	Kim, ES; Li, Z; Oh, SJ; Yoon, YH; Shin, HH				Kim, Eun Song; Li, Zhun; Oh, Seok Jin; Yoon, Yang Ho; Shin, Hyeon Ho			Morphological Identification of <i>Alexandrium</i> Species (Dinophyceae) from Jinhae-Masan Bay, Korea	OCEAN SCIENCE JOURNAL			English	Article						Alexandrium; morphological identification; connecting pore; ventral pore; Jinhae-Masan Bay	DINOFLAGELLATE GENUS ALEXANDRIUM; OSTENFELDII DINOPHYCEAE; TAMARENSE DINOPHYCEAE; CAUSATIVE ORGANISM; RESTING CYSTS; TOXICITY; CATENELLA; COAST; BIOGEOGRAPHY; VARIABILITY	Outbreaks of paralytic shellfish poisoning (PSP) and dense blooms caused by Alexandrium species in Jinhae-Masan Bay, Korea have been nearly annual events for many years. However, excluding some Alexandrium species responsible for PSP, there are no critical reports on the morphology of Alexandrium species in this bay. To identify the Alexandrium species based on detailed morphological features, vegetative cells collected water samples and established by the incubation of resting cysts isolated from sediment trap samples were analyzed. Four species of Alexandrium were identified: Alexandrium affine, A. fundyense, A. catenella, and A. insuetum. Morphological features of these species were basically consistent with those outlined in previous studies. However, the ventral pore and the connecting pore on the sulcal plate, which have been accepted as diagnostic characteristics for the identification of A. fundyense and A. catenella, need to be reevaluated, indicating that useful morphological features for identifying these two species should be recommended to avoid confusion in the classification of species in genus Alexandrium.	[Kim, Eun Song; Li, Zhun; Shin, Hyeon Ho] KIOST, South Sea Res Inst, Lib Marine Samples, Geoje 53201, South Korea; [Oh, Seok Jin] Pukyong Natl Univ, Lab Coastal Environm & Ecol, Busan 48513, South Korea; [Yoon, Yang Ho] Chonnam Natl Univ, Sch Marine Technol, Coll Fisheries & Ocean Sci, Yeosu 59626, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Pukyong National University; Chonnam National University	Shin, HH (通讯作者)，KIOST, South Sea Res Inst, Lib Marine Samples, Geoje 53201, South Korea.	shh961121@kiost.ac.kr	LI, ZHUN/GLT-3478-2022	LI, ZHUN/0000-0001-8961-9966; Shin, Hyeon Ho/0000-0002-9711-6717	Korea Institute of Marine Science and Technology and KIOST project [PE99513, PE99515]	Korea Institute of Marine Science and Technology and KIOST project	This research was supported by a grant from Korea Institute of Marine Science and Technology and KIOST project (PE99513 and PE99515).	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J	Soliman, A; Riding, JB				Soliman, Ali; Riding, James B.			Late Miocene (Tortonian) gonyaulacacean dinoflagellate cysts from the Vienna Basin, Austria	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Late Miocene (Tortonian/Pannonian); Taxonomy; Central Paratethys; Vienna Basin; Austria	LAST 2000 YEARS; LAKE PANNON; EVOLUTION; CLIMATE; GULF	During the Late Miocene (Tortonian or Pannonian regional stage), at around 11.6 Ma, a glacioeustatically-driven sea-level fall caused the final closure of the Paratethys Ocean and Lake Pannon was formed in central Europe. Tile lake was initially brackish, but slowly freshened and became slightly alkaline. These unusual changes in water chemistry produced the radiation of a characteristic assemblage of gonyaulacacean dinoflagellate cysts. This study examined 94 samples from the Pannonian of Hennersdorf Clay Pit, south of Vienna, Austria. From this material, Achomosphaera brevis sp. nov., Seriliodinium? imperfecta sp. nov. and Spiniferites hennersdorfensis sp. nov. were apparently endemic to the Central Paratethys during the Late Miocene. Spiniferites bentorii (Rossignol 1964) Wall and Dale, 1970 subsp. oblongus Sutone-Szentai 1986 and Spiniferites bentorii (Rossignol, 1964) Wall and Dale 1970 subsp. pannonicus Sutone-Szentai 1986 are elevated to species status. The genus Spiniferites exhibited significant morphological variability especially in terms of general shape, apical boss development and process morphology. Supplementary descriptions and discussions of some other gonyaulacacean taxa which are present are provided. (C) 2017 Published by Elsevier B.V.	[Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Riding, James B.] British Geol Survey Keyworth, Nottingham NG12 5GG, England	Egyptian Knowledge Bank (EKB); Tanta University	Soliman, A (通讯作者)，Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt.	ali.soliman@science.tanta.edu.eg	Soliman, Ali/R-1583-2018	Soliman, Ali/0000-0001-7366-4607	FWF-project [P21414-B16]; Commission for Stratigraphical and Palaeontological Research of the Austrian Academy of Science; NERC [bgs05017] Funding Source: UKRI	FWF-project(Austrian Science Fund (FWF)); Commission for Stratigraphical and Palaeontological Research of the Austrian Academy of Science; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	Sample preparation was supported by the Commission for Stratigraphical and Palaeontological Research of the Austrian Academy of Science and by FWF-project P21414-B16. Ali Soliman would like to thank Professor Werner E. Piller of Graz University, Professor Mathias Harzhauser of the Natural History Museum of Vienna and Dr. Andrea Kern of the University of Sao Paulo, Brazil for their considerable help and microscope (LM and SEM) facilities. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). The authors would like to thank reviewers for their constructive comments that greatly improved the manuscript.	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Palaeobot. Palynology	SEP	2017	244						325	346		10.1016/j.revpalbo.2017.02.003	http://dx.doi.org/10.1016/j.revpalbo.2017.02.003			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FE5ZH		Green Accepted			2025-03-11	WOS:000408289300022
J	Tabara, D; Slimani, H; Mare, S; Chira, CM				Tabara, Daniel; Slimani, Hamid; Mare, Silvia; Chira, Carmen Mariana			Integrated biostratigraphy and palaeoenvironmental interpretation of the Upper Cretaceous to Paleocene succession in the northern Moldavidian Domain (Eastern Carpathians, Romania)	CRETACEOUS RESEARCH			English	Review						Dinocysts; Calcareous nannofossils; Foraminifera; Cretaceous-Paleogene (K-Pg) succession; Eastern Carpathians	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; ABATHOMPHALUS-MAYAROENSIS BOLLI; SEDIMENTARY ORGANIC-MATTER; WESTERN EXTERNAL RIF; PALEOGENE BOUNDARY; TERTIARY BOUNDARY; OULED HADDOU; CRETACEOUS/PALAEOGENE BOUNDARY; FORAMINIFERAL ASSEMBLAGES; AGGLUTINATED FORAMINIFERA	This study of the upper Maastrichtian to Danian sedimentary succession from the northern part of the Romanian Eastern Carpathians (Varnita section) aims to establish an integrated biostratigraphy based on calcareous nannofossils, organic-walled dinoflagellate cysts (dinocysts) and foraminiferal assemblages, and to reconstruct the depositional environments of the interval. The stratigraphic record across the studied section is incomplete, considering that an approximately 16 m thick strata interval from the top of the Maastrichtian to lowermost Danian cannot be analyzed due to a landslide covering the outcrop. The upper Maastrichtian is marked by a succession of biostratigraphic events, such as the First Appearance Datum (FAD) of the nannoplankton taxon Nephrolithus frequens and FAD of the dinocyst species Deflandrea galeata and Disphaerogena carposphaeropsis, and the Last Appearance Datum (LAD) of Isabelidinium cooksoniae in the lower part of the section. These bioevents are followed by the LAD of the Dinogymnium spp. and Palynodinium grallator dinocyst markers in the top of the Maastrichtian deposits analyzed. In terms of foraminiferal biostratigraphy, the upper Maastrichtian Abathomphalus mayaroensis Zone is documented in the lower part of the studied section. Some bioevents, such as the bloom of the calcareous dinoflagellate genus Thoracosphaera and the FAD of the organic-walled dinocysts Damassadinium californicum, Senoniasphaera inornata, Xenicodinium lubricum and X. reticulatum suggest an early Danian age for the middle part of the section. From the Danian deposits in the Varnita section, we describe a new organic-walled dinocyst species, Pentadinium darmirae sp. nov., which is until now the only species of the Pentadinium genus discovered in the Paleocene. The occurrence of the global Danian dinocyst marker Senoniasphaera inornata in the top of the section, suggests an age not younger than middle Danian (62.6 Ma) for the analyzed deposits. The palynofacies constituents, as well as the agglutinated foraminiferal morphogroups, used to reconstruct the depositional environments, show that the late Maastrichtian sediments were deposited in an outer shelf to distal (bathyal) environment, followed by a marine transgression during the Danian. (C) 2017 Elsevier Ltd. All rights reserved.	[Tabara, Daniel; Mare, Silvia] Alexandru Ioan Cuza Univ, Dept Geol, 20A Carol 1 Blv, Iasi 700505, Romania; [Slimani, Hamid] Univ Mohammed V Rabat, Sci Inst, Lab Geol & Remote Sensing, URAC 46,Ave Ibn Batouta,PB 703, Rabat 10106, Morocco; [Chira, Carmen Mariana] Babes Bolyai Univ, Dept Geol, M Kogalniceanu 1, Cluj Napoca 400084, Romania	Alexandru Ioan Cuza University; Mohammed V University in Rabat; Babes Bolyai University from Cluj	Tabara, D (通讯作者)，Alexandru Ioan Cuza Univ, Dept Geol, 20A Carol 1 Blv, Iasi 700505, Romania.	dan.tabara@yahoo.com; h_slimani@yahoo.com; silvia_mare@yahoo.com; carmen.chira@ubbcluj.ro	Tabara, Daniel/C-6630-2015; Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913				ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; [Anonymous], 1995, P 4 INT WORKSH AGGL; [Anonymous], 1980, CRETACEOUS RES; [Anonymous], 1977, QUESTIONS PHYTOSTRAT; Antonescu E., 1982, Dari de Seama ale Sedintelor Institutul de Geologie si Geofizica (Bucharest), V66, P61; Badescu D., 2005, TECTONIC STRATIGRAPH; Bak K, 2005, GEOL CARPATH, V56, P205; Batten D.J., 1999, FOSSIL PLANTS SPORES, P15; Bindiu Raluca, 2011, Studia Universitatis Babes-Bolyai Geologia, V56, P31; Bojar AV, 2013, GEOL SOC SPEC PUBL, V382, P105, DOI 10.1144/SP382.11; Bojar AV, 2009, SOC SEDIMENT GEOL SP, V91, P121; Bombardiere L, 2000, SEDIMENT GEOL, V132, P177, DOI 10.1016/S0037-0738(00)00006-3; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Burnett J.A., 1998, P132; Canfield D.E., 1991, Topics in Geobiology, V9, P337; Caron M., 1985, P17; Carvalho MD, 2013, SEDIMENT GEOL, V295, P53, DOI 10.1016/j.sedgeo.2013.08.002; Carvalho MD, 2006, SEDIMENT GEOL, V192, P57, DOI 10.1016/j.sedgeo.2006.03.017; Cetean CG, 2011, CRETACEOUS RES, V32, P575, DOI 10.1016/j.cretres.2010.11.001; Cieszkowski M, 2012, AUSTRIAN J EARTH SCI, V105, P240; Coccioni R, 2007, PALAEOGEOGR PALAEOCL, V255, P157, DOI 10.1016/j.palaeo.2007.02.046; CORLISS BH, 1985, NATURE, V314, P435, DOI 10.1038/314435a0; COURTILLOT V, 1990, GLOBAL PLANET CHANGE, V89, P291, DOI 10.1016/0921-8181(90)90025-8; COURTILLOT V, 1986, CR ACAD SCI II, V303, P863; Dastas NR, 2014, GEOSCIENCES, V4, P1, DOI 10.3390/geosciences4010001; Duringer P., 1985, SCI G OL B STRASBG, V38, P19; Fensome R.A., 2008, DINOFLAJ2, Version 1; Filho J.G.M., 2002, TECNICAS PROCEDIMENT, P20; FISHER IS, 1986, SEDIMENTOLOGY, V33, P575, DOI 10.1111/j.1365-3091.1986.tb00762.x; Gasinski MA, 2013, ACTA GEOL POL, V63, P515, DOI 10.2478/agp-2013-0022; Gasinski MA, 2009, GEOL CARPATH, V60, P283, DOI 10.2478/v10096-009-0020-5; Gedl P, 2004, GEOL SOC SPEC PUBL, V230, P257, DOI 10.1144/GSL.SP.2004.230.01.13; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P1; GRADSTEIN FM, 1981, MAR MICROPALEONTOL, V6, P211; Grasu C., 1988, CARPATHIAN FIYSCH PE; Guédé KE, 2014, GEOBIOS-LYON, V47, P291, DOI 10.1016/j.geobios.2014.06.006; Guerrera F, 2012, GEOL CARPATH, V63, P463, DOI 10.2478/v10096-012-0036-0; Habib D., 1982, NATURE ORIGIN CRETAC, P113; Habib Daniel, 1996, Geological Society of America Special Paper, V307, P243; Hammer O, 2006, PALEONTOLOGICAL DATA ANALYSIS, P1; Hammer Oyvind, 2001, Palaeontologia Electronica, V4, pUnpaginated; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; HARDENBOL J., 1998, Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, V60, P3; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; Hollis Christopher J., 1996, P173; Ion J., 1985, Dari de Seama ale Sedintelor Institutul de Geologie si Geofizica (Bucharest), V69, P117; Ionesi L., 1975, 14 EUR MICR C MICR G, P145; JONES R W, 1985, Revue de Paleobiologie, V4, P311; KAMINSKI M. 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Res.	SEP	2017	77						102	123		10.1016/j.cretres.2017.04.021	http://dx.doi.org/10.1016/j.cretres.2017.04.021			22	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	EZ4UG					2025-03-11	WOS:000404707400011
J	Oboh-Ikuenobe, FE; Antolinez-Delgado, H; Awad, WK				Oboh-Ikuenobe, Francisca E.; Antolinez-Delgado, Hernan; Awad, Walaa K.			Dinoflagellate cyst assemblages, biostratigraphy and paleoenvironment of a Paleocene-Early Eocene sedimentary succession in the northern Niger Delta Basin: Comparison with low, mid and high latitude regions	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Alo-1 Well; Imo Formation; Nsukka Formation; Paleocene-Early Eocene; Dinoflagellate cysts; Nigeria	THERMAL MAXIMUM; SEQUENCE STRATIGRAPHY; APECTODINIUM ACME; BIOTIC RESPONSE; CARBON-CYCLE; SEA-LEVEL; EL-KEF; MARGIN; CLIMATE; AFRICA	This study represents a contribution to the Late Paleocene-Early Eocene biostratigraphy in a low latitude strati graphic setting where, published studies are few in comparison with mid- and high latitude regions. We generated data for 62 dinoflagellate cysts from a comprehensive analysis of 33 samples covering a 713-m interval in the Alo-1 Well in the northern Niger Delta (Anambra) Basin, Nigeria. Dinoflagellate cyst recovery in the samples varies from very good to poor, and the specimens are commonly well preserved. We calibrate the dinoflagellate cyst data with recent biozonation schemes for ODP Hole 959D, Cote d'Ivoire-Ghana Transform Margin in the eastern Equatorial Atlantic, which allowed for a valid comparison with published studies in well-dated rock sections in northwestern Europe, the Mediterranean region, New Zealand, and Tasmania. Our observations show that there is better correlation between tropical and mid latitude dinoflagellate cyst assemblages compared to those in high latitude regions. We use the last occurrence and/or last abundance events of dinoflagellate cysts to identify four biostratigraphic zones (zone E to zone H) in the Alo-1 Well. Lithostratigraphic and biostratigraphic analyses suggest a late Selandian age for the contact between the Imo and Nsukka formations. Abundant thermophilic taxa that include the Cordosphaeridium group and Apectodinuim dominate the assemblage recovered in the depositional succession. The late Selandian to early Thanetian sediments are dominated by the Cordosphaeridium group, and are succeeded by abundant to superabundant marker species of Apectodinium in the late Thanetian to Ypresian. The superabundance of Apectodinium is significant because it is indicative of the global intense climatic warming that characterized the late Thanetian to early Ypresian. The Alo-1 Well dinoflagellate cyst data also suggest deposition under proximal, inner neritic conditions that preserved an assemblage dominated by species of Cordosphaeridium, Damassadinium, lfecysta and Polysphaeridium. Published by Elsevier B.V.	[Oboh-Ikuenobe, Francisca E.; Awad, Walaa K.] Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Geol & Geophys Program, 129 McNutt Hall, Rolla, MO 65409 USA; [Antolinez-Delgado, Hernan] Amerisur Explorat Colombia, Ayasha Bldg Tv 21 98-71 6th Floor, Bogota, Colombia	University of Missouri System; Missouri University of Science & Technology	Oboh-Ikuenobe, FE (通讯作者)，Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Geol & Geophys Program, 129 McNutt Hall, Rolla, MO 65409 USA.	ikuenobe@mst.edu		Oboh-Ikuenobe, Francisca/0000-0002-2223-9691	Petroleum Research Fund [34676-AC8]; Josephine Husbands Radcliffe Graduate Scholarship (Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology)	Petroleum Research Fund(American Chemical Society); Josephine Husbands Radcliffe Graduate Scholarship (Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology)	We acknowledge the Petroleum Research Fund (administered by the American Chemical Society, Grant 34676-AC8 to Francisca Oboh-Ikuenobe) and the Josephine Husbands Radcliffe Graduate Scholarship (Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology) for funding this study. We thank the Shell Petroleum Development Company of Nigeria for providing the Alo-1 ditch cutting samples for study. We also thank Onema Adojoh and Joel Edegbai for their detailed suggestions on an earlier draft of the manscript. We extend our appreciation to Prof. Hamid Slimani and two anonymous reviewers for taking the time and efforts to improve this paper.	Adegoke O.S., 1981, J. Min. Geol, V18, P141; Adegoke O.S., 1969, Colloque sur l' Eocene, V69, P22, DOI [10.1007/978-3-540-92685-6, DOI 10.1007/978-3-540-92685-6]; Antolinez-Delgado H., 2004, Dinoflagelados del intervalo Paleoceno Superior-Eoceno Inferior de Nigeria: Implicationes Paleoclimaticas; Antolinez-Delgado H, 2007, PALYNOLOGY, V31, P53, DOI 10.2113/gspalynol.31.1.53; ARUA I, 1982, PALAEOGEOGR PALAEOCL, V38, P269, DOI 10.1016/0031-0182(82)90007-4; Awad WK, 2016, J AFR EARTH SCI, V123, P123, DOI 10.1016/j.jafrearsci.2016.07.014; Barron A, 2017, GEOL SOC AM BULL, V129, P218, DOI 10.1130/B31559.1; Berggren W. 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SEP 1	2017	481						29	43		10.1016/j.palaeo.2017.05.020	http://dx.doi.org/10.1016/j.palaeo.2017.05.020			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	EY5BU					2025-03-11	WOS:000403993000003
J	Price, AM; Coffin, MRS; Pospelova, V; Latimer, JS; Chmura, GL				Price, Andrea M.; Coffin, Michael R. S.; Pospelova, Vera; Latimer, James S.; Chmura, Gail L.			Effect of nutrient pollution on dinoflagellate cyst assemblages across estuaries of the NW Atlantic	MARINE POLLUTION BULLETIN			English	Article						Nutrient loading; Plankton; Prince Edward Island; Environmental indicators; Water quality; Palynology	GULF-OF-MEXICO; COASTAL EUTROPHICATION; SPATIAL-DISTRIBUTION; WATER-QUALITY; TOKYO-BAY; NITROGEN; PRODUCTIVITY; NORTHEASTERN; INDICATORS; MASSACHUSETTS	We analyzed surface sediments from 23 northeast USA estuaries, from Maine to Delaware, and nine estuaries from Prince Edward Island (PEI, Canada), to determine how dinoflagellate cyst assemblages varied with nutrient loading. Overall the abundance of cysts of heterotrophic dinoflagellates correlates with modeled nitrogen loading, but there were also regional signals. On PEI cysts of Gymnodiniwn microreticulatum characterized estuaries with high nitrogen loading while the sediments of eutrophic Boston Harbor were characterized by high abundances of Spinifentes spp. In Delaware Bay and the Delaware Inland Bays Polysphaeridiwn zohatyi correlated with higher temperatures and nutrient loading. This is the first study to document the dinoflagellate cyst eutrophication signal at such a large geographic scale in estuaries, thus confirming their value as indicators of water quality change and anthropogenic impact.	[Price, Andrea M.; Chmura, Gail L.] McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ H3A 0B9, Canada; [Coffin, Michael R. S.] Univ Prince Edward Isl, Dept Biol, Charlottetown, PE C1A 4P3, Canada	University of Prince Edward Island	Price, AM (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ H3A 0B9, Canada.	andrea.price@mail.mcgill.ca	Chmura, Gail/LNI-4648-2024; Latimer, James/C-1632-2009; Coffin, Michael/AAE-1407-2022	Chmura, Gail/0000-0001-7163-3903; Pospelova, Vera/0000-0003-4049-8133	Natural Sciences and Engineering Research Council of Canada (NSERC); Canadian Association of Palynology (CAP); Geological Society of America (GSA); NSERC; NSERC CREATE (Collaborative Research and Training Experience) grant; Canadian Watershed Research Consortium	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Canadian Association of Palynology (CAP); Geological Society of America (GSA); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); NSERC CREATE (Collaborative Research and Training Experience) grant; Canadian Watershed Research Consortium	The Natural Sciences and Engineering Research Council of Canada (NSERC), the Canadian Association of Palynology (CAP) and the Geological Society of America (GSA) provided partial funding for this research through student research awards to AMP. This research was partially supported by NSERC Discovery grants to VP and GLC. IVIRSC was partially funded by an NSERC CREATE (Collaborative Research and Training Experience) grant to the Canadian Rivers Institute WATER (Watershed and Aquatics Training in Environmental Research) program and the Canadian Watershed Research Consortium. We thank Cindy Crane and the PEI Department of Communities, Land and Environment for providing nitrogen loads for PEI estuaries. We would also like to thank all those who provided information or water quality data from estuaries in this study: Alison Branco (Peconic Estuary Program, SCDHS South Shore Bays Water Quality), Barbara Warren (Salem Sound Coastwatch), Brad Hubeny (Salem State University - Geological Sciences), Ron Huber (Friends of Penobscot Bay), Christopher Deacutis (RIDEM Div. of Fish and Wildlife, Narragansett Bay Water Quality Monitoring Network), Jane Disney (Frenchman Bay Partners), Kevin Brinson (Delaware Environmental Observing System), Peter Milholland (Friends, of Casco Bay Citizen Stewards Water Quality Monitoring Program), Tony Williams (Buzzards Bay Coalition), Bebe Moulton (Friends of Blue Hill Bay), Mark Tedesco (EPA), William Hastback (NYSDEC - Bureau of Marine Resources), Matthew Sclafani (Cornell University), Pierce Rafferty (Henry L. Ferguson Museum), Warren Prell (Brown University). Chris Pickerell (Marine Program Director, Cornell), Jaime Vaudrey (University of Connecticut), Provincetown Center for Coastal Studies, Blue Hill Bay Coastal Monitoring Program - Marine Environmental Research Institute, and the many citizen scientists that are part of these organizations who volunteer their time to collect water quality measurements. The US grain size data used article were produced by the U.S. Environmental Protection Agency (EPA) through its Environmental Monitoring and Assessment Program (EMAP). The US samples were made available through the EPA's National Coastal Assessment program. We thank Jingyi Zhang and Artur Plis (McGill University) for assistance in biogenic silica sample preparation, Maureen Soon (University of British Columbia) for the biogenic silica analysis, and Lee van Ardenne (McGill University) for assistance with regression analyses.	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Pollut. Bull.	AUG 15	2017	121	1-2					339	351		10.1016/j.marpolbul.2017.06.024	http://dx.doi.org/10.1016/j.marpolbul.2017.06.024			13	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	FD4VB	28633948	Green Accepted			2025-03-11	WOS:000407529200049
J	Turner, HE; Gradstein, FM; Gale, AS; Watkins, DK				Turner, Holly E.; Gradstein, Felix M.; Gale, Andy S.; Watkins, David K.			The age of the Tojeira Formation (Late Jurassic, Early Kimmeridgian), of Montejunto, west-central Portugal	SWISS JOURNAL OF PALAEONTOLOGY			English	Article						Portugal; Jurassic; Kimmeridgian; Correlation; Biostratigraphy; Stable isotope stratigraphy	INTEGRATED STRATIGRAPHY; DINOFLAGELLATE CYSTS; CRETACEOUS BOUNDARY; RUSSIAN PLATFORM; NORTH YORKSHIRE; CLAY FORMATION; CARBON; CHEMOSTRATIGRAPHY; EVOLUTION; DORSET	Precise biostratigraphic dating of the Tojeira Formation (Late Jurassic, Early Kimmeridgian) of the Montejunto section of west-central Portugal, which has yielded important planktonic foraminiferal assemblages, is hindered by poor preservation in the upper part of the section as the lithology shifts from shale to coarser clastics. Assignment was previously made to the Idoceras planula and Sutneria platynota zones based on ammonites. Coccolith and dinoflagellate assemblages described here concur with the Early Kimmeridgian, yet, a finer age constraint is proposed by cyclo- and chemostratigraphical correlation. Peaks in delta C-13(org) and TOC, if equivalent to maxima in the envelope of clay/carbonate cycles in SE France, imply that the c. 50 m-thick section spans a 0.8-myr interval of the S. platynota through upper Ataxioceras hypselocyclum ammonite zones, with the approximate base of the A. hypselocyclum Zone at c. 15.4 m(level 13). Such stratigraphy provides new insights into the upper part of the formation by interbasinal correlation with other Tethyan records. An extended first occurrence of the dinoflagellate species Dichadogonyaulax? pannea in the S. platynota Zone is also proposed.	[Turner, Holly E.; Gradstein, Felix M.; Gale, Andy S.] Univ Portsmouth, Sch Earth & Environm Sci, Portsmouth PO1 3QL, Hants, England; [Gradstein, Felix M.] Univ Oslo, Nat Hist Museum, POB 1172, N-0318 Oslo, Norway; [Watkins, David K.] Univ Nebraska Lincoln, Dept Earth & Atmospher Sci, Lincoln, NE 68588 USA	University of Portsmouth; University of Oslo; University of Nebraska System; University of Nebraska Lincoln	Turner, HE (通讯作者)，Univ Portsmouth, Sch Earth & Environm Sci, Portsmouth PO1 3QL, Hants, England.	holly.turner@port.ac.uk	Watkins, David/AAJ-2571-2021	Turner, Holly/0000-0003-3807-9001	Norwegian Interactive Offshore Stratigraphic Lexicon (NOR-LEX); Lundin Petroleum, Norway; University of Portsmouth	Norwegian Interactive Offshore Stratigraphic Lexicon (NOR-LEX); Lundin Petroleum, Norway; University of Portsmouth	Fieldwork was carried out in receipt of funding by Norwegian Interactive Offshore Stratigraphic Lexicon (NOR-LEX). The senior author thanks Lundin Petroleum, Norway for providing a travel grant (and M. Charnock for the organization of such), the University of Portsmouth for a Placement Scheme Award, Dr S. Batenburg for Time Series Analysis training and support, G. Bell and N. Walasek for palynological training and support, and M.C. Blanc and others for a productive stay at the Applied Petroleum Technology facilities (APT), Oslo. Gratitude is extended to Dr. S. Nicoara at the Open University, UK for stable isotope and TOC measurements and Dr. D. Loydell for a useful discussion. We thank Profs. J. Ogg and D. Martill and Dr A. Waskowska whose reviews improved the manuscript.	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N., 1960, Bulletin of the Geological Society of India, V23, P1; Talib Abu, 2007, Revue de Paleobiologie, V26, P625; Taylor AM, 2014, GEOL J, V49, P143, DOI 10.1002/gj.2505; THOMAS JE, 1988, REV PALAEOBOT PALYNO, V56, P313, DOI 10.1016/0034-6667(88)90063-2; Vakhrameyev V.A., 1982, INT GEOL REV, V24, P1190, DOI [10.1080/00206818209451058, DOI 10.1080/00206818209451058, https://doi.org/10.1080/00206818209451058]; Wierzbowski A, 2002, NEUES JAHRB GEOL P-A, V226, P145, DOI 10.1127/njgpa/226/2002/145; Wimbledon WAP, 2008, EPISODES, V31, P423, DOI 10.18814/epiiugs/2008/v31i4/008	58	11	12	0	1	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1664-2376	1664-2384		SWISS J PALAEONTOL	Swiss J. Palaeontol.	AUG	2017	136	2					287	299		10.1007/s13358-017-0137-6	http://dx.doi.org/10.1007/s13358-017-0137-6			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	FT2KM		Green Published, hybrid			2025-03-11	WOS:000422970500006
J	Li, Z; Shin, HH				Li, Z.; Shin, H. H.			RESTING CYSTS OF POTENTIALLY HARMFUL DINOFLAGELLATES IN KOREAN COASTAL AREA	PHYCOLOGIA			English	Meeting Abstract									[Li, Z.; Shin, H. H.] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Ansan, South Korea	Korea Institute of Ocean Science & Technology (KIOST)		lizhun@kiost.ac.kr; shh961121@kiost.ac.kr							0	0	0	0	0	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	AUG	2017	56	4		S		245	117	117						1	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	FJ6TX					2025-03-11	WOS:000412892000246
J	El Atfy, H; El Diasty, WS; El Beialy, SY; Gheith, AM; Batten, DJ; Agha, NN				El Atfy, H.; El Diasty, W. Sh.; El Beialy, S. Y.; Gheith, A. M.; Batten, D. J.; Agha, N. N.			Palynofacies and geochemical analyses of the Upper Cretaceous-Eocene succession, western Sirte Basin, Libya: Palaeoenvironmental interpretation and implications for hydrocarbon generation potential	JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING			English	Article						Upper Cretaceous-Eocene; Palynology; Organic facies; Organic geochemistry; Concession 11; Sirte Basin; Libya	SOURCE-ROCK EVALUATION; ORGANIC FACIES; DINOFLAGELLATE CYST; EGYPT; CLASSIFICATION; CONCESSION; SUBSIDENCE; SEDIMENTS; EVOLUTION; DESERT	One hundred and thirty-six core and cuttings samples from Upper Cretaceous-Eocene deposits that are believed to include the most important source rocks in the Sirte Basin have been subjected to Rock-Eval pyrolysis, total organic carbon measurements, and palynofacies and microfacies analyses to determine palaeoenvironments and the thermal maturation history of the succession. It is apparent that the lower part of the Bahi Formation, the oldest rock unit examined, reflects a basin margin environment under the influence of freshwater input. Shallow marine, near-shore, inner shelf, suboxic-anoxic conditions, which are first suggested by the uppermost deposits of the Bahi Formation, prevailed for much of the time during deposition of the younger Cretaceous Etel, Rachmat, Sirte and Kalash formations. Shallow supratidal and intertidal sub-environments alternating with deeper environments of shelf embayments associated with a maximum rise in sea level are indicated by the Paleocene Farrud Member of the Beda Formation. The Zelten Formation consists of shallow intertidal and lagoonal facies, and the overlying Paleocene-Eocene Kheir Formation reflects relatively shallow marine sedimentation in mid to outer shelf environments alternating with short-lived, shallow, intertidal-lagoonal to supratidal conditions. The TOC content of the Upper Cretaceous samples examined is mostly moderate (up to 2.04%), the organic matter consisting of Types II and II/III kerogen. Differences in hydrocarbon generation potential are linked to varying proportions of aquatic versus terrigenous organic matter in the samples examined and hence to depositional conditions. Combined geochemical and palynofacies data reflect deposition mainly in weakly reducing to suboxic settings and suggest that immature to early mature gas-prone source rocks are within the Etel, Rachmat and some of the Sirte Formation, and mature oil/ gas-prone source rocks are within the Sirte and Kalash formations.	[El Atfy, H.; El Diasty, W. Sh.; El Beialy, S. Y.; Gheith, A. M.; Agha, N. N.] Mansoura Univ, Fac Sci, Geol Dept, Mansoura 35516, Egypt; [Batten, D. J.] Aberystwyth Univ, Dept Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales; [Batten, D. J.] Univ Manchester, Sch Earth Atmospher & Environm Sci, Oxford Rd, Manchester M13 9PL, Lancs, England	Egyptian Knowledge Bank (EKB); Mansoura University; Aberystwyth University; University of Manchester	El Diasty, WS (通讯作者)，Mansoura Univ, Fac Sci, Geol Dept, Mansoura 35516, Egypt.	awaleed@mans.edu.eg	Diasty, Waleed/AAG-7015-2019; Atfy, Haytham/AAT-2276-2021; Beialy, Salah/AAD-7329-2020	Shukry El Diasty, Waleed/0000-0002-3144-1189				Abadi AM, 2008, AAPG BULL, V92, P993, DOI 10.1306/03310806070; Ahlbrandt T.S., 2001, U. S. 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H., 2010, THESIS; Thorn VC, 2009, REV PALAEOBOT PALYNO, V156, P436, DOI 10.1016/j.revpalbo.2009.04.009; Thusu B., 1988, SUBSURFACE PALYNOSTR, P171; Traverse A., 2007, Paleopalynology, VSecond; 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]; Uwins F.J.R., 1988, SUBSURFACEPALYNOSTRA, P215; Waples D.W., 1985, GEOCHEMISTRY PETROLE	42	7	8	0	5	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0920-4105	1873-4715		J PETROL SCI ENG	J. Pet. Sci. Eng.	AUG	2017	157						148	163		10.1016/j.petrol.2017.07.021	http://dx.doi.org/10.1016/j.petrol.2017.07.021			16	Energy & Fuels; Engineering, Petroleum	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Engineering	FG7SR		Green Submitted			2025-03-11	WOS:000410624800013
J	Prebble, JG; Bostock, HC; Cortese, G; Lorrey, AM; Hayward, BW; Calvo, E; Northcote, LC; Scott, GH; Neil, HL				Prebble, J. G.; Bostock, H. C.; Cortese, G.; Lorrey, A. M.; Hayward, B. W.; Calvo, E.; Northcote, L. C.; Scott, G. H.; Neil, H. L.			Evidence for a Holocene Climatic Optimum in the southwest Pacific: A multiproxy study	PALEOCEANOGRAPHY			English	Article							SEA-SURFACE TEMPERATURE; SOUTHERN-OCEAN FRONTS; LAST GLACIAL PERIOD; NEW-ZEALAND; SUBTROPICAL FRONT; DINOFLAGELLATE CYSTS; CHATHAM RISE; ANTARCTIC PENINSULA; FORAMINIFERAL FLUX; SOUTHLAND CURRENT	The early Holocene sea surface temperature (SST) gradient across the subtropical front (STF) to the east of New Zealand was similar to 2 degrees C (measured between core sites MD97-2121 and MD97-2120): considerably less than the similar to 6 degrees C modern gradient between the two core sites. We document the surface ocean temperatures east and south of New Zealand during the early and middle Holocene, to test and expand upon this reconstruction. This new study samples a latitudinal transect of seven sediment cores from 37 degrees S to 60 degrees S in the southwest Pacific from subtropical waters north of New Zealand to polar waters in the Southern Ocean. Our compilation of SST proxies consists of 525 SST estimates from five different methods and includes 243 new data points. We confirm that an early Holocene warm peak in this region was mostly restricted to the area immediately south of the STF, which resulted in a lower temperature gradient across the STF than in modern times. However, there is no change in Holocene SST south of the polar front. Faunal assemblages suggest an early Holocene meridional expansion of fauna characteristic of the modern subtropical front in the Bounty Gyre. We suggest that such an expansion could be achieved by a reduced inflow of Subantarctic Surface Water into the Bounty Gyre. Results from a modern-analog matching platform called the Past Interpretation of Climate Tool (PICT) suggest that the early Holocene SST is most consistent with reduced westerly winds in the New Zealand sector of the Southern Ocean.	[Prebble, J. G.; Cortese, G.; Scott, G. H.] GNS Sci, Lower Hutt, New Zealand; [Bostock, H. C.; Lorrey, A. M.; Northcote, L. C.; Neil, H. L.] NIWA, Wellington, New Zealand; [Hayward, B. W.] Geomarine Res, Auckland, New Zealand; [Calvo, E.] Inst Marine Sci, Barcelona, Spain	GNS Science - New Zealand; National Institute of Water & Atmospheric Research (NIWA) - New Zealand; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Prebble, JG (通讯作者)，GNS Sci, Lower Hutt, New Zealand.	j.prebble@gns.cri.nz	HAYWARD, BRUCE/AAG-2597-2019; Cortese, Giuseppe/C-8281-2011; Calvo, Eva/C-2618-2014; Bostock, Helen/A-6834-2013	Hayward, Bruce W./0000-0003-1302-7686; Calvo, Eva/0000-0003-3659-4499; Bostock, Helen/0000-0002-8903-8958; Lorrey, Andrew/0000-0002-3923-3181; Cortese, Giuseppe/0000-0003-1780-3371; /0000-0002-2111-6817	New Zealand Antarctic Research Institute [NZARI 2014-2]; GNS Global Change Through Time Programme project 5; NIWA Coasts; Oceans Physical Resources (COPR) sediment processes project; NIWA "Regional Climate Modeling" core [CACV1702]	New Zealand Antarctic Research Institute; GNS Global Change Through Time Programme project 5; NIWA Coasts; Oceans Physical Resources (COPR) sediment processes project; NIWA "Regional Climate Modeling" core	We thank the scientists and crew who collected the suite of cores used in this study. The samples are currently archived at the National Institute of Water and Atmospheric Research (NIWA) and at the Integrated Ocean Drilling Program (IODP) core repositories. Funding for this project was provided by the New Zealand Antarctic Research Institute (NZARI 2014-2), the GNS Global Change Through Time Programme project 5 (J.P., G.C., and G.S.), the NIWA Coasts and Oceans Physical Resources (COPR) sediment processes project (H.B., H.N., and L.N.), and A.M.L. was supported by the NIWA "Regional Climate Modeling" core funded project contract CACV1702. We thank Marcus Vandergoes for comments on a draft. We thank journal Editors Ellen Thomas and Ryuji Tada, reviewer Stephen Gallagher, and an anonymous reviewer for comments that significantly improved the clarity of this manuscript. Data from this project are available in supporting information Tables S1-S6 from the journal website.	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J	Anglès, S; Reñé, A; Garcés, E; Lugliè, A; Sechi, N; Camp, J; Satta, CT				Angles, Silvia; Rene, Albert; Garces, Esther; Luglie, Antonella; Sechi, Nicola; Camp, Jordi; Satta, Cecilia Teodora			MORPHOLOGICAL AND MOLECULAR CHARACTERIZATION OF <i>BYSMATRUM SUBSALSUM</i> (DINOPHYCEAE) FROM THE WESTERN MEDITERRANEAN SEA REVEALS THE EXISTENCE OF CRYPTIC SPECIES	JOURNAL OF PHYCOLOGY			English	Article						5.8S-ITS; benthic; cyst; dinoflagellate; LSU; rRNA; SSU; taxonomy; transitional ecosystem	DINOFLAGELLATE CYST ASSEMBLAGES; BENTHIC DINOFLAGELLATE; PERIDINIUM-GREGARIUM; NOV DINOPHYCEAE; 1ST REPORT; SCRIPPSIELLA; THORACOSPHAERACEAE; AUSTRALIA; ECOLOGY	Bysmatrum subsalsum is a cosmopolitan dinoflagellate species that inhabits marine and transitional habitats. Despite its wide distribution, information on the morphological variability, phylogeny and ecology of B. subsalsum is scarce. In this study, we provide morphological and molecular data on B. subsalsum strains and wild cells from different locations in the Mediterranean Basin. The dynamics of cell abundances and the associated environmental conditions during a field bloom are also described. Genetic sequences of B. subsalsum obtained in this study showed large intraspecific differences, clustering in two well-differentiated clades. Despite a certain degree of variation with respect to cell size, apical pore complex (APC) morphology and size, and cingulum displacement, cells from the two clades showed similar morphological traits. These findings indicated the occurrence of cryptic species. Comparisons of the morphology of our B. subsalsum specimens with the few descriptions available in the literature revealed larger than previously known intraspecific morphological variability. Phylogenetic trees inferred from the concatenated SSU, 5.8S-ITS, and LSU rRNA and the individual 5.8S-ITS regions suggested the inclusion of Bysmatrum in the Peridiniales and a close phylogenetic relationship with Peridinium sensu stricto. However, the low statistical support prevented the assignment of Bysmatrum to a particular family of Peridiniales. Ecological data obtained from a bloom in La Pletera salt marshes (Catalan Coast, Spain) suggested the species reaches high cell abundances at water temperatures >20 degrees C and salinity levels >30. Our results add new information regarding the morphology, phylogeny, and ecology of B. subsalsum.	[Angles, Silvia] IMEDEA UIB CSIC, Inst Mediterrani Estudis Avancats, Dept Ecol & Recursos Marins, Miquel Marques 21, Esporles 07190, Spain; [Rene, Albert; Garces, Esther; Camp, Jordi] CSIC, Inst Ciencias Mar, Dept Biol Marina & Oceanog, Passeig Maritim Barceloneta 37-49, E-08003 Barcelona, Spain; [Luglie, Antonella; Sechi, Nicola; Satta, Cecilia Teodora] Univ Sassari, Dipartimento Architettura Design & Urbanist, Via Piandanna 4, I-090064 Sassari, Italy	Consejo Superior de Investigaciones Cientificas (CSIC); ATTITUS Educacao; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); University of Sassari	Satta, CT (通讯作者)，Univ Sassari, Dipartimento Architettura Design & Urbanist, Via Piandanna 4, I-090064 Sassari, Italy.	ctsatta@uniss.it	Satta, Cecilia Teodora/AAF-6417-2020; Anglès, Silvia/B-9469-2011; Luglie, Antonella/M-4321-2015; Garces, Esther/C-5701-2011; Rene, Albert/D-4560-2012	Luglie, Antonella/0000-0001-6382-4208; Garces, Esther/0000-0002-2712-501X; Rene, Albert/0000-0002-0488-3539; SATTA, Cecilia Teodora/0000-0003-0130-9432; Camp, Jordi/0000-0002-5202-9783	Marie Sklodowska Curie International Outgoing Fellowship within the 7th European Community Framework Programme (Project CONPLANK) [PIOF-GA-2011-302562]; Regione Sardegna; Zoumgest project; project DEVOTES; 7th European Community Framework Programme, "The Ocean for Tomorrow" [GA-308392]; Institut d'Ecologia Aquatica - UDG [LIFE 13 NAT/ES/001001]	Marie Sklodowska Curie International Outgoing Fellowship within the 7th European Community Framework Programme (Project CONPLANK); Regione Sardegna(Regione Sardegna); Zoumgest project; project DEVOTES; 7th European Community Framework Programme, "The Ocean for Tomorrow"; Institut d'Ecologia Aquatica - UDG	This research was supported by a Marie Sklodowska Curie International Outgoing Fellowship within the 7th European Community Framework Programme (Project CONPLANK, PIOF-GA-2011-302562). The Regione Sardegna funded Research Project "Master and Back" financed C. T. Satta's work. The Zoumgest project provided the financial support required for the Corru S'Ittiri Lagoon sampling. Financial support was also provided by the project DEVOTES, funded by the 7th European Community Framework Programme, "The Ocean for Tomorrow" (GA-308392). The authors thank X. Quintana (Institut d'Ecologia Aquatica - UDG) for providing physical-chemical data on PL (Project LIFE 13 NAT/ES/001001), J.M. Fortuno and the Servei de Microscopia Electronica (ICM-CSIC) and S. Marceddu (ISPA-CNR) for their assistance in the SEM observations, and V. Balague (ICM-CSIC) for technical assistance during the molecular analyses.	[Anonymous], 1958, Mitt. Int. Ver. Theor. Angew. Limnol., DOI DOI 10.1080/05384680.1958.11904091; Biecheler B., 1952, Bull. Biol. Fr. 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H., 1908, LIEFERUNG, V8, P123; Rhodes L, 2011, PHYCOLOGIA, V50, P624, DOI 10.2216/11-19.1; Satta CT, 2014, ESTUAR COAST, V37, P646, DOI 10.1007/s12237-013-9705-1; Satta CT, 2013, HARMFUL ALGAE, V24, P65, DOI 10.1016/j.hal.2013.01.007; STEIDINGER K A, 1977, Phycologia, V16, P69, DOI 10.2216/i0031-8884-16-1-69.1; Ten-Hage L, 2001, EUR J PHYCOL, V36, P129, DOI 10.1017/S0967026201003146; Zeng N, 2012, NEW ZEAL J MAR FRESH, V46, P511, DOI 10.1080/00288330.2012.719911	33	10	11	1	17	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	AUG	2017	53	4					833	847		10.1111/jpy.12546	http://dx.doi.org/10.1111/jpy.12546			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	FF8CF	28509342				2025-03-11	WOS:000409242000008
J	Stead, D; Eyers, J				Stead, Darrin; Eyers, Jill			The palynology and geology of the Lower Cretaceous (Aptian-Albian) of Munday's Hill Quarry, Bedfordshire, UK	PROCEEDINGS OF THE GEOLOGISTS ASSOCIATION			English	Article						Palynology; Lower Cretaceous; Albian; Aptian; Sporomorphs; Dinoflagellate cysts	ENGLAND; AFRICA; SANDS; SEA	Early Cretaceous sediments of Aptian-Albian age outcrop at Munday's Hill Quarry, Bedfordshire, England. Previous papers describing the section have resulted in different terminologies being applied. The Lower Cretaceous in Bedfordshire is represented by sediments belonging to the Lower Greensand Group and the Gault Clay Formation. Within the Lower Greensand Group in the study area the Woburn Sands Formation, are of Aptian-Albian age. Selected samples have been analysed for palynology. The analysis reveals diverse palynomorph assemblages, including well-preserved dinoflagellate cysts and sporomorphs. Comparison of the assemblages with published records indicates that the lower samples are of Late Aptian age. Forms recorded include common Kiokansium unituberculatum,Cerbia tabulata, Aptea polymorpha and Cyclonephelium inconspicuum. An Early Albian age is indicated for the uppermost sample. Crown Copyright (C) 2017 Published by Elsevier Ltd on behalf of The Geologists' Association. All rights reserved.	[Stead, Darrin] Wellstrat Serv Ltd, 1 Castle Grange, Caergwrle LL12 9HL, Wrexham, Wales; [Eyers, Jill] Chiltern Archaeol, 13 Pusey Way,Lane End, High Wycombe HP14 3LG, Bucks, England		Stead, D (通讯作者)，Wellstrat Serv Ltd, 1 Castle Grange, Caergwrle LL12 9HL, Wrexham, Wales.	dstead@wellstrat.com; chilternarchaeology@btopenworld.com						Alberti G., 1961, Palaeontographica, V116, P1; ALLEN JRL, 1981, NATURE, V289, P579, DOI 10.1038/289579a0; [Anonymous], 1836, Transactions of the Geological Society of London, DOI [10.1144/transgslb.4.2.103, DOI 10.1144/TRANSGSLB.4.2.103]; Batten D., 1996, Palynology: principles and applications, P1011; Batten DJ., 1980, P 4 INT PAL C, V2, P403; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BRIDEAUX W. W., 1975, GEOLOGICAL SURVEY CA, V252, P1; BUCK SG, 1985, J SEDIMENT PETROL, V55, P895; BUJAK JP, 1978, GEOLOGICAL SURVEY CA, V297, P1; Cameron A. C. G., 1892, P GEOLOGISTS ASS, P395; Casey R., 1961, Palaeontology, V3, P487; Costa L. 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F., 1984, 6 OFFSH NO SEAS C EX; Worssam B. C., 1969, MEMOIR GEOLOGICAL SU, P1	53	5	6	1	14	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND	0016-7878			P GEOLOGIST ASSOC	Proc. Geol. Assoc.	AUG	2017	128	4					599	612		10.1016/j.pgeola.2017.05.011	http://dx.doi.org/10.1016/j.pgeola.2017.05.011			14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	FF3GT					2025-03-11	WOS:000408784200007
J	Riding, JB; Garg, R; Rai, J				Riding, James B.; Garg, Rahul; Rai, Jyotsana			Dinoflagellate cyst biostratigraphy of the Patasar Shale Member (Upper Jurassic) of the Wagad Uplift, Kachchh, Gujarat, western India	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Biostratigraphy; Dinoflagellate cysts; Late Jurassic; Pollen and spores; Provincialism; Gujarat; Western India	AMMONITES; BASIN; NANNOFOSSILS; BOUNDARY; STRATA; SHELF; KUTCH; ZONE; PART	Two samples were analysed from the lowermost Patasar Shale Member of the Patasar Tank section on the western margin of the Wagad Uplift in the Kachchh Basin of Gujarat, western India. One of the samples produced an abundant, diverse and well-preserved palynobiota. The other sample produced a significantly sparser association, but of similar character. The overall assemblage is dominated by relatively long-rangingJurassic gymnospermous pollen grains, but also includes dinoflagellate cysts of definite Gondwanan affinity. The dinoflagellate cysts are confidently correlated to the Australian Dingodinium swanense Interval Zone, which is of Kimmeridgian (Late Jurassic) age. This indicates that the Australasian Jurassic dinoflagellate cyst biostratigraphical scheme can be applied in western India, and probably throughout the Indian subcontinent. Due to evidence from ammonites and calcareous nannofossils in the Patasar Shale Member, allied with other biostratigraphical evidence from New Zealand and Papua New Guinea, the age of the D. swanense Interval Zone is reinterpreted as being of Early Kimmeridgian age. The D. swanense Interval Zone was previously assigned to the Early to Late Kimmeridgian. Its refinement and revision to an older age are entirely consistent with recent reassessments of these dinoflagellate cyst biozones. Crown Copyright (C) 2017 Published by Elsevier B.V. All rights reserved.	[Riding, James B.] British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, England; [Garg, Rahul; Rai, Jyotsana] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Riding, JB (通讯作者)，British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk		Garg, Rahul/0000-0001-7479-6361	Science and Engineering Research Council (SERC) Division of the Department of Science and Technology (DST) of India [SR/S4/ES-521/2010(G)]; NERC [bgs05017] Funding Source: UKRI	Science and Engineering Research Council (SERC) Division of the Department of Science and Technology (DST) of India; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The Science and Engineering Research Council (SERC) Division of the Department of Science and Technology (DST) of India funded the participation of Jyotsana Rai in this project, which is number SR/S4/ES-521/2010(G). Rahul Garg and Jyotsana Rai both thank Dr. Sunil Bajpai, Director of the Birbal Sahni Institute of Palaeosciences, for the use of laboratory and office facilities. Dr. Bajpai is also thanked for granting permission to publish this article, which is number BSIP/RDCC/45/2016-17. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). The authors are grateful to Robert A. Fensome (Geological Survey of Canada) and an anonymous reviewer for their extremely helpful editorial comments.	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J	Ivanova, DK; Kietzmann, DA				Ivanova, Dania K.; Kietzmann, Diego A.			Calcareous dinoflagellate cysts from the Tithonian - Valanginian Vaca Muerta Formation in the southern Mendoza area of the Neuquen Basin, Argentina	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Calcareous dinoflagellate cysts; biostratigraphy; Upper jurassic; Lower cretaceous; Vaca Muerta Formation	JURASSIC-CRETACEOUS BOUNDARY; ANTARCTIC PENINSULA; CARBONATE RAMP; SOURCE-ROCK; BIOSTRATIGRAPHY; STRATIGRAPHY; CARPATHIANS; SUCCESSION; AMERICA; SECTION	The Late Jurassic - Early Cretaceous marine sediments of the Andean region show an excellent record of different calcareous microfossils, among which calcareous dinoflagellate cysts stand out. Detailed micropaleontological studies of Vaca Muerta Formation (Early Tithonian - Early Valanginian) in the southern Mendoza Neuquen Basin from three sections are conducted with the aim of establishing a major presence of microfossil representatives from different microfossil groups. The analysis of several thin sections from the outcrops reveals a relatively rich micropaleontological assemblage of calcareous dinoflagellate cysts, as well as levels with poor preserved calpionellids and benthic foraminifera. Particularly, calcareous dinoflagellate cyst includes 24 known species (two of them with two subspecies). Some species with biostratigraphic value of the Tethyan region have been identified also in the Andean region: 1) Committosphaera pulls (Borza) and Parastomiosphaera malmica (Borza) are species known only from Lower Tithonian; 2) Colomisphaera tenuis (Nagy) appears in the latest Early Tithonian; 3) Colomisphaera fords Rehanek and Stomiosphaerina proxima Rehanek are important markers for the latest Late Tithonian - middle Late Berriasian interval; 4) Stomiosphaera wanneri Borza appears in the middle Late Berriasian; 5) Colomisphaera conferta Rehanek and Colomisphaera vogleri (Borza) appear in the Late Berriasian and marked the Berriasian-Valanginian boundary interval; 6) Carpistomiosphaera valanginiana Borza is a marker for the Lower/Upper Valanginian. More detailed studies of these groups will allow their correlation with Tethyan biozones, and contribute to improve biostratigraphic schemes in the Neuquen Basin. (c) 2017 Elsevier Ltd. All rights reserved.	[Ivanova, Dania K.] Bulgarian Acad Sci, Dept Paleontol Stratig & Sedimentol, Geol Inst, BG-1113 Sofia, Bulgaria; [Kietzmann, Diego A.] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Ciudad Univ,Pabellon 2,Intendente Guiraldes 2160, Buenos Aires, DF, Argentina; [Kietzmann, Diego A.] Univ Buenos Aires, CONICET, Inst Geociencias Basicas Ambientales & Aplicadas, Buenos Aires, DF, Argentina	Bulgarian Academy of Sciences; University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires	Kietzmann, DA (通讯作者)，Univ Buenos Aires, CONICET, Inst Geociencias Basicas Ambientales & Aplicadas, Buenos Aires, DF, Argentina.	diegokietzmann@gl.fcen.uba.ar	Kietzmann, Diego/S-4549-2019; Ivanova, Daria/B-8443-2013	Kietzmann, Diego Alejandro/0000-0003-1222-7811	Agencia Nacional de Promocion Cientifica y Tecnologica [PICT-2015-0206]; University of Buenos Aires; UBACyT proyect [20020150200218BA]	Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); University of Buenos Aires(University of Buenos Aires); UBACyT proyect	This research has been done under the framework of the PICT-2015-0206 project supported by the Agencia Nacional de Promocion Cientifica y Tecnologica, and UBACyT 20020150200218BA proyect supported by the University of Buenos Aires. We are especially grateful to Dr. Alberto Riccardi (Universidad Nacional de La Plata y Museo, Argentina) for ammonite identification and discussion of Tithonian-Valanginian biostratigraphic data of the Neuquen over the years. Also, we thank Dr. H.A. Leanza (Museo de Ciencias Naturales Bernandino Rivadavia, Argentina) for his enriching conversations regarding the Neuquen Basin stratigraphy. We thank Dr. Mohamed Benzaggagh (Universite Moulay Ismail, Morocco), Dr. Rafael Lopez Martinez (Universidad Nacional Autonoma de Mexico, Mexico) and an anonymous reviewer, for their comments and suggestions that improved the original manuscript, as well as the editorial work of Dr. F. Vega (Regional Editor JSAES).	Aguirre-Urreta M. 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J	Lu, XX; Wang, ZH; Guo, X; Gu, YG; Liang, WB; Liu, L				Lu, Xinxin; Wang, Zhaohui; Guo, Xin; Gu, Yangguang; Liang, Weibiao; Liu, Lei			Impacts of metal contamination and eutrophication on dinoflagellate cyst assemblages along the Guangdong coast of southern China	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cysts; Metals; Biogenic elements; Sediments; South China Sea; Redundancy analysis	PEARL RIVER ESTUARY; INDUCED OXIDATIVE STRESS; HEAVY-METAL; SURFACE SEDIMENTS; MARINE-PHYTOPLANKTON; SPATIAL-DISTRIBUTION; ZHELIN BAY; INDUSTRIAL-POLLUTION; BIOGENIC ELEMENTS; YELLOW SEA	Fifty-one surface sediment samples were collected from eleven sea areas along the Guangdong coast in southern China. Biogenic elements, metals and dinoflagellate cysts were analyzed. Twenty-one cyst taxa in 12 genera were identified. The cyst concentrations ranged between 14 and 250 cysts/g, with an average of 69 cysts/g. The low cyst production was caused by coarse sediments, high sedimentation rates, and high anthropogenic disturbances. Biogenic elements were comparable with those reported. However, the metal concentrations were far lower than the sediment quality guidelines. Both biogenic elements and metals were higher in the Mid Coast and lower in the Western Coast. Eutrophication slightly enhanced the productivity of autotrophic dinocysts, and cysts of Scrippsiella indicated eutrophication. Cd had inhibitory effects on cyst production. Alexandrium and Diplopsalis cysts were sensitive to metal contamination; however, Gyrodiniwn, Pheopolykrikos, and Lingulodinium cysts had high resistance to metal contamination.	[Lu, Xinxin; Wang, Zhaohui; Guo, Xin; Gu, Yangguang; Liang, Weibiao; Liu, Lei] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China	Jinan University	Wang, ZH (通讯作者)，Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Guangdong, Peoples R China.	twzh@jnu.edu.cn	Gu, Yang-Guang/C-8275-2009	Gu, Yang-Guang/0000-0003-2314-0463	National Natural Science Foundation of China [41476132, 41276154, U1301235]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This work was supported by the National Natural Science Foundation of China (Nos. 41476132, 41276154, and U1301235).	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J	Eldrett, JS; Dodsworth, P; Bergman, SC; Wright, M; Minisini, D				Eldrett, James S.; Dodsworth, Paul; Bergman, Steven C.; Wright, Milly; Minisini, Daniel			Water-mass evolution in the Cretaceous Western Interior Seaway of North America and equatorial Atlantic	CLIMATE OF THE PAST			English	Article							OCEANIC ANOXIC EVENT; BOUNDARY EVENT; DINOFLAGELLATE CYSTS; DEMERARA RISE; STRATOTYPE SECTION; ORGANIC-MATTER; BLACK SHALES; LEVEL CHANGE; BASIN; CIRCULATION	The Late Cretaceous Epoch was characterized by major global perturbations in the carbon cycle, the most prominent occurring near the Cenomanian-Turonian (CT) transition marked by Oceanic Anoxic Event 2 (OAE-2) at 94.9-93.7 Ma. The Cretaceous Western Interior Seaway (KWIS) was one of several epicontinental seas in which a complex water-mass evolution was recorded in widespread sedimentary successions. This contribution integrates new data on the main components of organic matter, geochemistry, and stable isotopes along a north-south transect from the KWIS to the equatorial western Atlantic and Southern Ocean. In particular, cored sedimentary rocks from the Eagle Ford Group of west Texas (similar to 90-98 Ma) demonstrate subtle temporal and spatial variations in palaeoenvironmental conditions and provide an important geographic constraint for interpreting water-mass evolution. High-latitude (boreal-austral), equatorial Atlantic Tethyan and locally sourced Western Interior Seaway water masses are distinguished by distinct palynological assemblages and geochemical signatures. The northward migration of an equatorial Atlantic Tethyan water mass into the KWIS occurred during the early-middle Cenomanian (98-95 Ma) followed by a major re-organization during the latest Cenomanian-Turonian (95-94 Ma) as a full connection with a northerly boreal water mass was established during peak transgression. This oceanographic change promoted de-stratification of the water column and improved oxygenation throughout the KWIS and as far south as the Demerara Rise off Suriname. In addition, the recorded decline in redox-sensitive trace metals during the onset of OAE-2 likely reflects a genuine oxygenation event related to open water-mass exchange and may have been complicated by variable contribution of organic matter from different sources (e.g. refractory/terrigenous material), requiring further investigation.	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Past.	JUL 14	2017	13	7					855	878		10.5194/cp-13-855-2017	http://dx.doi.org/10.5194/cp-13-855-2017			24	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	FA7JS		gold, Green Submitted			2025-03-11	WOS:000405623600001
J	Hssaida, T; Benzaggagh, M; Riding, JB; Huault, V; Essamoud, R; Mouflih, M; Jaydawi, S; Chakir, S; Nahim, M				Hssaida, Touria; Benzaggagh, Mohamed; Riding, James B.; Huault, Vincent; Essamoud, Rachid; Mouflih, Mustapha; Jaydawi, Soukaina; Chakir, Sara; Nahim, Mohamed			Stratigraphical ranges and biozones of dinoflagellate cysts at the Middle-Late Jurassic transition (late Bathonian-early Oxfordian) from the Guercif Basin, northeastern Morocco	ANNALES DE PALEONTOLOGIE			French	Article						Biostratigraphy; Dinoflagellate cysts; Middle-Late Jurassic transition; Guercif Basin; Morocco	KIMMERIDGIAN PALYNOLOGY; SOUTHERN PORTUGAL; ALGARVE BASIN; NORTH; AREA	Despite the stratigraphical significance of dinoflagellate cysts as reliable markers for correlating and dating Jurassic-Cretaceous strata, investigations into this palynomorph group in the southern Tethyan Realm, specifically northwest Africa, are sparse and somewhat parochial. Most research on Jurassic dinoflagellate cysts is focussed on European depocentres in the Boreal and Sub-Boreal realms. This study is on biostratigraphical data from two petroleum boreholes (MSD1 and KDH1) drilled during 1985 in the Guercif Basin, northeast Morocco by ONAREP (Office National de Recherche et d'Exploitation Petrolier), now ONHYM (Office National des Hydrocarbures et des Mines). These boreholes penetrated a thick siliciclastic succession, attributed to the Middle and Upper Jurassic, below Miocene marls. Over sixty dinoflagellate cyst taxa were identified. Four dinoflagellate cyst biozones, named GI to GIV, are established for the late Bathonian to early Oxfordian interval. These biozones are defined on the basis of the first appearance datum (FAD) and/or the last appearance datum (LAD) of some biomarker taxa which have wide geographical distributions. These are: Ctenidodinium combazii and Ctenidodinium sellwoodii for the GI Biozone (late Bathonian-early Callovian); Ctenidodinium continuum and Meiourogonyaulax caytonensis for the GII Biozone (middle Callovian); Gonyaulacysta centriconnata and Wanaea thysanota for the GIII Biozone (late Callovian-earliest Oxfordian); and Liesbergia liesbergensis and Systematophora penicillata for the GIV Biozone (early Oxfordian). These biozones are correlated to those already established for the respective intervals in other palaeogeographic regions, such as the Boreal, Sub-boreal and Tethyan realms. (C) 2017 Elsevier Masson SAS. All rights reserved.	[Hssaida, Touria; Essamoud, Rachid; Mouflih, Mustapha; Jaydawi, Soukaina; Chakir, Sara] Univ Hassan II Mohammedia, Fac Sci Ben MSik, Ave Cdt Driss El Harti,BP 7955, Casablanca 20800, Morocco; [Benzaggagh, Mohamed] Univ Moulay Ismail, Fac Sci, Dept Geol, BP 11-201, Zitoune, Meknes, Morocco; [Riding, James B.] British Geol Survey, Environm Sci Ctr, Nottingham NG12 5GG, Royaume Uni, England; [Huault, Vincent] Univ Lorraine, Fac Sci & Technol, Dept Geosci, BP 70239,Blvd Aiguillettes, F-54506 Vandoeuvre Les Nancy, France; [Nahim, Mohamed] Off Natl Hydrocarbures & Mines ONHYM, Lab Petr Biostratig, Rabat, Morocco	Hassan II University of Casablanca; Moulay Ismail University of Meknes; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universite de Lorraine	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	Mouflih, Mustapha/AAA-9913-2019	Rachid, ESSAMOUD/0000-0003-1630-8053	NERC [bgs05017] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Aboul Ela N.M., 1990, EARTH SCI SER, V4, P95; [Anonymous], 1983, DINOFLAGELLATE OPPEL, DOI DOI 10.4095/119736; [Anonymous], 1983, GLOUCESTERSHIRE ENGL; Barski Marcin, 1999, Przeglad Geologiczny, V47, P718; 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; Ben Bouziane A., 1984, THESE TROISIEME CYCL; Benzaggagh M, 2016, BOL GEOL MIN, V127, P431; Benzaquen M., 1965, Etude stratigraphique preliminaire des formations dubasin de Guercif; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; 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; Bujak J.P., 1977, Developments in Palaeontology and Stratigraphy, V6, P321; Cattaneo G., 1987, THESIS; 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; Durr G., 1987, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V176, P67; Ehrenberg C.G., 1843, KONIGLICH PREUSSISCH, P61; El Beialy S.Y., 2002, Egypt. 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Paleontol.	JUL-SEP	2017	103	3					197	215		10.1016/j.annpal.2017.06.001	http://dx.doi.org/10.1016/j.annpal.2017.06.001			19	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	FL0FX		Green Accepted			2025-03-11	WOS:000413888100004
J	Yamamoto, K; Oikawa, H				Yamamoto, Keigo; Oikawa, Hiroshi			Temporal changes and differences in the toxin contents and the profiles between arc shell and Japanese cockle contaminated with paralytic shellfish toxin in Osaka Bay, eastern Seto Inland Sea, Japan	NIPPON SUISAN GAKKAISHI			Chinese	Article							ALEXANDRIUM-TAMARENSE; RESTING CYSTS; TRANSFORMATION; DINOPHYCEAE	The causative dinoflagellate blooms of paralytic shellfish toxins (PSTs) and changes in the toxin contents and the profiles in both arc shell Scapharca broughtonii and Japanese cockle Fulvia mutica in Osaka Bay for three years from 2013 to 2015 were investigated. During the investigation, the toxic dinoflagellate Alexandrium tamarense and A. catenella occurred in Osaka Bay. A. tamarense was the most important causative species in contamination of bivalves with PSTs. Contamination and detoxification in arc shell with PSTs were slower than those in Japanese cockle and slight amounts of PSTs remained in the arc shell throughout the year. On the other hand, PSTs in Japanese cockle were not detected after the end of bloom of A. tamarense. The dominant toxins of arc shell were GTX2 and GTX3 and relative ratio of STX in the arc shell increased with decontamination of toxins. In contrast, the dominant toxins in Japanese cockle were C1 and C2. In conclusion, the rate of GTX1 and GTX4 increased during the bloom of A. tamarense in both species. It was suggested that toxins in Japanese cockle were rapidly excreted without any in vivo conversions of toxins from the causative dinoflagellates.	[Yamamoto, Keigo] Res Inst Environm Agr & Fisheries, Marine Fisheries Res Ctr, Osaka, Osaka 5990311, Japan; [Oikawa, Hiroshi] Japan Fisheries Res & Educ Agcy, Natl Res Inst Fisheries Sci, Yokohama, Kanagawa 2368648, Japan	Japan Fisheries Research & Education Agency (FRA)	Yamamoto, K (通讯作者)，Res Inst Environm Agr & Fisheries, Marine Fisheries Res Ctr, Osaka, Osaka 5990311, Japan.	YamamotoK@o-suishi.zaqrs.jp						Fukuyo Y., 2002, PICES Science Report, V23, P7; Imai Ichiro, 2006, Plankton & Benthos Research, V1, P71; John U, 2014, PROTIST, V165, P779, DOI 10.1016/j.protis.2014.10.001; Kaga S, 2006, NIPPON SUISAN GAKK, V72, P1068, DOI 10.2331/suisan.72.1068; KVITEK RG, 1991, MAR ECOL PROG SER, V69, P47, DOI 10.3354/meps069047; Nagai S, 2016, HARMFUL ALGAE, V51, P97, DOI 10.1016/j.hal.2015.10.014; OSHIMA Y, 1992, TOXICON, V30, P1539, DOI 10.1016/0041-0101(92)90025-Z; OSHIMA Y, 1990, TOXIC MARINE PHYTOPLANKTON, P391; OSHIMA Y, 1995, J AOAC INT, V78, P528; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; Sato S, 2000, BIOORG MED CHEM LETT, V10, P1787, DOI 10.1016/S0960-894X(00)00332-2; Sato S, 2014, J AOAC INT, V97, P339, DOI 10.5740/jaoacint.SGESato; SHIMIZU Y, 1981, SCIENCE, V212, P547, DOI 10.1126/science.7209548; Twarog B.M., 1974, PROC 2 INT CORAL REE, P505; Uwe J, 2014, TAXON, V63, P932; Yamamoto K, 2010, NIPPON SUISAN GAKK, V76, P877, DOI 10.2331/suisan.76.877	16	6	6	1	4	JAPANESE SOC FISHERIES SCIENCE	TOKYO	C/O TOKYO UNIV FISHERIES, KONAN 4, MINATO, TOKYO, 108-8477, JAPAN	0021-5392	1349-998X		NIPPON SUISAN GAKK	Nippon Suisan Gakkaishi	JUL	2017	83	4					589	598		10.2331/suisan.17-00006	http://dx.doi.org/10.2331/suisan.17-00006			10	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	FI3ZK		gold			2025-03-11	WOS:000411908600005
J	Guallar, C; Bacher, C; Chapelle, A				Guallar, Carles; Bacher, Cedric; Chapelle, Annie			Global and local factors driving the phenology of <i>Alexandriurn minutum</i> (Halim) blooms and its toxicity	HARMFUL ALGAE			English	Article						Alexandrium minutum; PSP toxicity; HAB; Bloom phenology; Threshold analysis; Monitoring long time-series	HARMFUL ALGAL BLOOMS; NITZSCHIA SPP. BLOOMS; COASTAL WATERS; CLIMATE-CHANGE; TOXIN CONTENT; ENVIRONMENTAL-FACTORS; ENGLISH-CHANNEL; CYST FORMATION; OCEAN COLOR; CORK HARBOR	The dinoflagellate Alexandrium minutum is a toxic bloom-forming species distributed worldwide. The mechanisms driving and promoting the species blooms and their toxicity are studied and presented here. Most previously published work focuses on local and/or short-term scales. In this study, a broad temporal and spatial approach is addressed using time series covering several sites over several years and combining environmental variables and A. minutum abundances from the French English Channel - Atlantic coasts. Data were explored by means of phenology and threshold analysis. The A. minutum bloom characteristics are defined. Only one bloom per year is measured and it may reach more than a million of cells L-1. Bloom period extends from April to October and the bloom length ranges from two weeks to six months. In the ecosystems studied, water temperature and river flow, as regional and local factors respectively, are the main environmental drivers influencing the magnitude, growth rate and length of the blooms. Bloom toxicity is linked to the bloom maximum abundance and river flow. This work provides new knowledge for further managing tools for A. minutum blooms in the ecosystems studied. (C) 2017 Elsevier B.V. All rights reserved.	[Guallar, Carles; Chapelle, Annie] IFREMER, DYNECO PELAGOS, BP 70, F-29280 Plouzane, France; [Bacher, Cedric] IFREMER, DYNECO, BP 70, F-29280 Plouzane, France; [Guallar, Carles] Univ Barcelona, Fac Biol, Dept Biol Evolut Ecol & Ciencies Ambientals, Av Diagonal 643,5th Floor, E-08028 Barcelona, Spain	Ifremer; Ifremer; University of Barcelona	Guallar, C (通讯作者)，IFREMER, DYNECO PELAGOS, BP 70, F-29280 Plouzane, France.; Guallar, C (通讯作者)，Univ Barcelona, Fac Biol, Dept Biol Evolut Ecol & Ciencies Ambientals, Av Diagonal 643,5th Floor, E-08028 Barcelona, Spain.	carlesguallar@gmail.com; Cedric.Bacher@ifremer.fr; Annie.Chapelle@ifremer.fr		Bacher, Cedric/0000-0001-6090-4667; Guallar, Carles/0000-0001-7240-5873	Agence de l'Eau Loire Bretagne (AELB); AELB; IFREMER	Agence de l'Eau Loire Bretagne (AELB); AELB; IFREMER	This work was supported by the Agence de l'Eau Loire Bretagne (AELB) in the frame of the project PHYTORISK. Caries Guallar was funded by AELB and IFREMER.	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J	Kim, SY; Polyak, L; Delusina, I				Kim, So-Young; Polyak, Leonid; Delusina, Irina			Terrestrial and aquatic palynomorphs in Holocene sediments from the Chukchi-Alaskan margin, western Arctic Ocean: Implications for the history of marine circulation and climatic environments	HOLOCENE			English	Article						Chukchi Sea; Holocene; palynomorphs; pollen; sediment cores; western Arctic	DIFFUSE SPECTRAL REFLECTANCE; LAST GLACIAL MAXIMUM; BERING LAND-BRIDGE; SEA-ICE; LAPTEV SEA; NORTHERN CHUKOTKA; POLLEN RECORD; FRESH-WATER; VEGETATION; SHELF	Two sediment cores from the Chukchi Sea margin north of Alaska were analyzed for palynological composition including terrestrial and aquatic palynomorphs. Based on 13 radiocarbon ages, the investigated sedimentary record represents most of the Holocene with a century to multidecadal age resolution. Three palynological zones were discriminated based on the abundance of major palynomorph groups (terrestrial and freshwater palynomorphs and dinoflagellate cysts) and composition of spore and pollen assemblages. They are interpreted in terms of depositional and paleoclimatic changes including predominance of redeposition by meltwater or sea ice in the early-Holocene, a strong input of contemporaneous material related to Pacific water advection culminating after ca. 6000 yr BP, and more subtle changes in the late-Holocene. It is concluded that depositional environments, such as current transportation and mixing, have an overall major control on palynomorph distribution. The climatic factors may have also played an important role in palynomorph abundance and composition, especially in the middle-to late-Holocene, when circulation changes were less dramatic than during the flooding of the Bering Strait and the shallow Chukchi Sea shelf. Comprehending these linkages requires a better knowledge of the Holocene vegetation history in the coastal areas of Alaska and Chukchi Peninsula.	[Kim, So-Young] Korea Polar Res Inst, Div Polar Ocean Sci, 26 Songdomiraero, Incheon 21990, South Korea; [Polyak, Leonid] Ohio State Univ, Byrd Polar Res Ctr, Columbus, OH 43210 USA; [Delusina, Irina] Univ Calif Davis, Dept Earth & Planetary Sci, Davis, CA 95616 USA	Korea Polar Research Institute (KOPRI); University System of Ohio; Ohio State University; University of California System; University of California Davis	Kim, SY (通讯作者)，Korea Polar Res Inst, Div Polar Ocean Sci, 26 Songdomiraero, Incheon 21990, South Korea.	kimsy@kopri.re.kr	Kim, So-Young/JFS-7698-2023		Korea Polar Research Institute (KOPRI) [PE15062]; K-AOOS Program (KOPRI) - Ministry of Oceans and Fisheries, Korea [PM16040]	Korea Polar Research Institute (KOPRI); K-AOOS Program (KOPRI) - Ministry of Oceans and Fisheries, Korea	This study is a contribution to the Korea Polar Research Institute (KOPRI) research program under grant no. PE15062. 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J	Berezina, NA; Gubelit, YI; Polyak, YM; Sharov, AN; Kudryavtseva, VA; Lubimtsev, VA; Petukhov, VA; Shigaeva, TD				Berezina, Nadezhda A.; Gubelit, Yulia I.; Polyak, Yulia M.; Sharov, Andrey N.; Kudryavtseva, Valentina A.; Lubimtsev, Vasily A.; Petukhov, Vasily A.; Shigaeva, Tatyana D.			An integrated approach to the assessment of the eastern Gulf of Finland health: A case study of coastal habitats	JOURNAL OF MARINE SYSTEMS			English	Article						Environmental assessment; Indicators; Toxic pollution; Eutrophication; Coastal zone; Neva estuary	AMPHIPOD MONOPOREIA-AFFINIS; CLADOPHORA-GLOMERATA; BALTIC SEA; CYANOBACTERIAL BLOOMS; DINOFLAGELLATE CYSTS; ALGAL MATS; COMMUNITY; MACROALGAE; SEDIMENTS; MACROZOOBENTHOS	Eutrophication and chemical pollution are typical threats to the ecosystem of the Gulf of Finland. This paper aims to make a comprehensive assessment of the environmental status of coastal habitats in the easternmost Gulf of Finland (Neva River estuary) by using different physical, chemical and biotic variables to find cost-effective indicators for further monitoring. During summers of 2014 and 2015 we measured water salinity, phosphorus (eutrophication marker), biomass of harmful filamentous macroalgae (coastline hypoxia inductor), sediment hazardous substances (trace metals, polycyclic aromatic hydrocarbons) and other concomitant characters at 12 sites in the gulf. Also, we analyzed responses of the phytoplankton and benthic organisms, including metal tolerant and hydrocarbon-oxidizing bacteria, meio- and macrofauna, to these factors. We compared the indicative sensitivity and efficiency of several well-known biotic indices and methods, including a Saprobity system (basing on phytoplankton), Raffaelli and Mason index (meiobenthos), and two macrobenthic derived indices (Goodnight-Whitley Index and Benthic Quality Index). Also, we applied a new index - the embryo malformation frequency in benthic amphipods. To estimate the level of bottom hypoxia induced by the macroalgae blooms, we measured the algal cover and thickness of the algal mats. To verify our assessment, we tested correlations between all used variables. Biotic communities of these areas are subjected to high phosphorus and macroalgae blooms, toxic pollution, water salinity and other factors. We concluded that environmental state of coastal habitats at several southern sites (in Koporskaya Bay and near the developing port Bronka) and near port Primorsk in the north was bad, while the state of the rest of sites was moderate or good. The integrated approach for the assessment may be recommended for monitoring programs as an important tool for studying human-mediated and other effects on brackishwater coastal environments. (C) 2016 Elsevier B.V. All rights reserved.	[Berezina, Nadezhda A.; Gubelit, Yulia I.; Petukhov, Vasily A.] Russian Acad Sci, Zool Inst, Univ Skaya 1, St Petersburg 199034, Russia; [Polyak, Yulia M.; Sharov, Andrey N.; Kudryavtseva, Valentina A.; Lubimtsev, Vasily A.; Shigaeva, Tatyana D.] RAS, Sci Res Ctr Ecol Safety, Korpusnaya St 18, St Petersburg 197110, Russia	Russian Academy of Sciences; Zoological Institute of the Russian Academy of Sciences; Russian Academy of Sciences; St. Petersburg Federal Research Center of the Russian Academy of Sciences	Berezina, NA (通讯作者)，Russian Acad Sci, Zool Inst, Univ Skaya 1, St Petersburg 199034, Russia.	nadezhda.berezina@zin.ru	Kudryavtseva, Valentina/AAF-1374-2021; Petukhov, Vasily/U-4310-2017; Berezina, Nadezhda/R-1968-2016; Shigaeva, Tatiana/Q-5075-2016; Gubelit, Yulia/U-4874-2017; polyak, yulia/P-8505-2016; Sharov, Andrey/K-4222-2013	Gubelit, Yulia/0000-0002-7334-7844; Berezina, Nadezhda/0000-0003-3057-5596; shigaeva, tatiana/0000-0002-7548-6434; polyak, yulia/0000-0002-9490-2392; Sharov, Andrey/0000-0001-7581-2538	Russian Foundation for Basic Research [14-04-00207, 14-04-91721 BONUS_a]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	Authors cordially thank Lyudmila Umnova (ZIN RAS) for measurement of phosphates and two anonymous reviewers for valuable comments. This work was supported partially by the Russian Foundation for Basic Research (grants 14-04-00207 and 14-04-91721 BONUS_a) and a joint Programme between Finland, Estonia and Russia "The Gulf of Finland Year 2014".	Aleksandrov SV, 2010, MAR POLLUT BULL, V61, P205, DOI 10.1016/j.marpolbul.2010.02.015; Andersson A, 1996, MAR BIOL, V126, P791, DOI 10.1007/BF00351346; [Anonymous], 2012, F16122198 PND; [Anonymous], SCI TOTAL ENV; AUSTEN MC, 1989, ESTUAR COAST SHELF S, V29, P23, DOI 10.1016/0272-7714(89)90071-1; Back S., 2001, FINNISH ENV, V472, P71; Berezina N., 2016, J MAR BIOL ASS UK; Berezina N. 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JUL	2017	171				SI		159	171		10.1016/j.jmarsys.2016.08.013	http://dx.doi.org/10.1016/j.jmarsys.2016.08.013			13	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	EY5BJ					2025-03-11	WOS:000403991900018
J	Rezanka, T; Lukavsky, J; Nedbalová, L; Sigler, K				Rezanka, Tomas; Lukavsky, Jaromir; Nedbalova, Linda; Sigler, Karel			Lipidomic profile in three species of dinoflagellates (<i>Amphidinium carterae, Cystodinium</i> sp., and <i>Peridinium aciculiferum</i>) containing very long chain polyunsaturated fatty acids	PHYTOCHEMISTRY			English	Article						Dinoflagellates; Amphidinium carterae; Cystodinium sp.; Peridinium aciculiferum; Gymnodiniaceae; Phytodiniaceae; Peridiniaceae; Lipidomic analysis; Very long chain polyunsaturated fatty acids; Triacylglycerols; Phospholipids; Phosphatidylcholine	ELECTROSPRAY-IONIZATION; MASS-SPECTROMETRY; PHOSPHATIDYLCHOLINE; TRIACYLGLYCEROLS; IDENTIFICATION; REGIOISOMERS; MICROALGAE; DIACYLGLYCEROLS; DINOPHYCEAE; BIOMARKERS	This study describes the identification of very long chain polyunsaturated fatty acids (VLCPUFAs) in three strains of dinoflagellates (Amphidinium carterae, Cystodinium sp., and Peridinium aciculiferum). The strains were cultivated and their lipidomic profiles were obtained by high resolution mass spectrometry with the aid of positive and negative electrospray ionization (ESI) mode by Orbitrap apparatus. Hydrophilic interaction liquid chromatography (HILIC/ESI) was used to separate major lipid classes of the three genera of dinoflagellates by neutral loss scan showing the ion [M + H-28:8](+), where 28:8 was octacosaoctaenoic acid, and by precursor ion scanning of ions at m/z 407, which was an ion corresponding to the structure of acyl of 28:8 acid (C27H39COO-). Based on these analyzes, it was found that out of more than a dozen lipid classes present in the total lipids, only two classes of neutral lipids, i.e. major triacylglycerols and minor diacylglycerols contain VLCPUFAs. In polar lipids, VLCPUFAs were identified only in phosphatidic acid (PA) and phosphatidyl choline (PC) or in their lyso-forms (LPA and LPC). Further analysis of individual lipid classes by reversed-phase high-performance liquid chromatography (RPHPLC) showed the presence of triacylglycerols (TAGs) containing VLCPUFAs, i.e. molecular species of the sn-28:7/28:8/28:8, sn-26:7/28:7/28:8, or sn-26:7/28:8/28:8 types. These TAGs are the longest and most unsaturated TAGs isolated from a natural source that have yet been synthesized. In the case of PA and PC, tandem MS identified sn-28:8/16:0-PA and sn-28:8/16:0-PC and the corresponding lyso-forms (28:8-LPC and 28:8-LPA). All these results indicate that TAGs containing VLCPUFAs are biosynthesized in dinoflagellates in the same manner as in higher eukaryotic organisms, which means that the PA, after conversion to DAG, serves as a precursor in the biosynthesis of other phospholipids, e.g. PC, and, after further acylation, also of TAG. (C) 2017 Elsevier Ltd. All rights reserved.	[Rezanka, Tomas; Sigler, Karel] Inst Microbiol, Videnska 1083, Prague 14220, Czech Republic; [Lukavsky, Jaromir] Acad Sci Czech Republ, Inst Bot, Biorefinery Res Ctr Competence, Dukelska 135, CS-37982 Trebon, Czech Republic; [Nedbalova, Linda] Charles Univ Prague, Fac Sci, Dept Ecol, Vinicna 7, CR-12844 Prague, Czech Republic	Czech Academy of Sciences; Institute of Microbiology of the Czech Academy of Sciences; Czech Academy of Sciences; Institute of Botany of the Czech Academy of Sciences; Charles University Prague	Rezanka, T (通讯作者)，Inst Microbiol, Videnska 1083, Prague 14220, Czech Republic.	rezanka@biomed.cas.cz	Lukavský, Jaromír/H-1607-2014; Rezanka, Tomas/A-8399-2008; Nedbalova, Linda/D-2792-2009	Nedbalova, Linda/0000-0003-1800-714X; lukavsky, jaromir/0000-0002-8939-4725	Czech Science Foundation (GACR) [P503 17-00027S];  [RVO61388971];  [RVO67985939]	Czech Science Foundation (GACR)(Grant Agency of the Czech Republic); ; 	The research was supported by Czech Science Foundation (GACR) project P503 17-00027S and by Institutional Research Concepts RVO61388971 and RVO67985939.	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J	Vellekoop, J; Holwerda, F; Prámparo, MB; Willmott, V; Schouten, S; Cúneo, NR; Scasso, RA; Brinkhuis, H				Vellekoop, Johan; Holwerda, Femke; Pramparo, Mercedes B.; Willmott, Veronica; Schouten, Stefan; Cuneo, Nestor R.; Scasso, Roberto A.; Brinkhuis, Henk			Climate and sea-level changes across a shallow marine Cretaceous-Palaeogene boundary succession in Patagonia, Argentina	PALAEONTOLOGY			English	Article						Cretaceous; Palaeogene; Argentina; climate; sea level; dinocysts	TERRESTRIAL ORGANIC-MATTER; DINOFLAGELLATE CYSTS; TERTIARY BOUNDARY; TETRAETHER LIPIDS; SEQUENCE STRATIGRAPHY; CHICXULUB IMPACT; MEMBRANE-LIPIDS; NEUQUEN BASIN; NEW-JERSEY; PALEOCENE	Upper Maastrichtian to lower Paleocene, coarse-grained deposits of the Lefipan Formation in Chubut Province, (Patagonia, Argentina) provide an opportunity to study environmental changes across the Cretaceous-Palaeogene (K-Pg) boundary in a shallow marine depositional environment. Marine palynological and organic geochemical analyses were performed on the K-Pg boundary interval of the Lefipan Formation at the San Ramon section. The palynological and organic geochemical records from the San Ramon K-Pg boundary section are characteristic of a highly dynamic, nearshore setting. High abundances of terrestrial palynomorphs, high BIT-index values and the occasional presence of plant fossils are indicative of a large input of terrestrial organic material. The organic-walled dinoflagellate cyst (dinocyst) assemblage is generally dominated by Senegalinium and other peridinioid dinocyst taxa, indicative of high-nutrient conditions and decreased salinities, probably associated with a large fluvial input. The reconstructed sea surface temperatures range from 25 degrees C to 27 degrees C, in accordance with the tropical climate inferred by palynological and megafloral studies. As in the Bajada del Jaguel section, similar to 500km north-north-east of San Ramon, peaks of Senegalinium spp. were recorded below and above the K-Pg boundary, possibly related to enhanced runoff resulting from more humid climatic conditions. The lithological, palynological and organic geochemical records suggest the occurrence of a sea-level regression across the K-Pg boundary, resulting in a hiatus directly at the boundary in both sections, followed by a transgression in the Danian.	[Vellekoop, Johan; Brinkhuis, Henk] Univ Utrecht, Lab Palaeobot & Palynol, Dept Earth Sci, Marine Palynol & Palaeoceanog,Fac Geosci, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands; [Vellekoop, Johan] Katholieke Univ Leuven, Dept Earth & Environm Sci, Div Geol, Celestijnenlaan 200E, B-3001 Leuven, Belgium; [Holwerda, Femke] Bayer Staatssammlung Palaontol & Geol, SNSB, Richard Wagner Str 10, D-80333 Munich, Germany; [Holwerda, Femke] Univ Nova Lisboa, FCT, GeoBioTec, Campus Caparica, P-2829516 Caparica, Portugal; [Pramparo, Mercedes B.] CCT CONICET, Inst Argentino Nivol Glaciol & Ciencias Ambiental, CC 330, RA-5500 Mendoza, Argentina; [Willmott, Veronica; Schouten, Stefan] Royal Netherlands Inst Sea Res, Dept Marine Microbiol & Biogeochem, Texel, Netherlands; [Willmott, Veronica; Schouten, Stefan] Univ Utrecht, Royal Netherlands Inst Sea Res, Texel, Netherlands; [Schouten, Stefan] Univ Utrecht, Fac Geosci, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands; [Cuneo, Nestor R.] Consejo Nacl Invest Cient & Tecn, Museo Paleontol Egidio Feruglio, Ave Fontana 140, RA-9100 Trelew, Chubut, Argentina; [Scasso, Roberto A.] Univ Buenos Aires, CONICET, Inst Geociencias Basicas Aplicadas & Ambientales, Dept Ciencias Geol,Fac Ciencias Exactas & Nat, Pabellon 2, RA-1428 Buenos Aires, DF, Argentina; [Willmott, Veronica] Helmoltz Ctr Polar & Marine Res, Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany	Utrecht University; KU Leuven; Universidade Nova de Lisboa; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Vellekoop, J (通讯作者)，Univ Utrecht, Lab Palaeobot & Palynol, Dept Earth Sci, Marine Palynol & Palaeoceanog,Fac Geosci, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.; Vellekoop, J (通讯作者)，Katholieke Univ Leuven, Dept Earth & Environm Sci, Div Geol, Celestijnenlaan 200E, B-3001 Leuven, Belgium.	johan.vellekoop@kuleuven.be	Willmott Puig, Veronica/AGN-3478-2022; Brinkhuis, Henk/IUO-8165-2023; Vellekoop, Johan/L-1805-2019; Schouten, Stefan/P-4380-2016; Vellekoop, Johan/F-6466-2017	Holwerda, Femke/0000-0003-3446-5693; Vellekoop, Johan/0000-0001-6977-693X; Brinkhuis, Henk/0000-0003-0253-6610; Willmott Puig, Veronica/0000-0002-6552-8901	Utrecht University; Netherlands Organization for Scientific Research (NWO) [ALWPJ/09047, G.0B85.13]; Netherlands Earth System Science Center	Utrecht University; Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); Netherlands Earth System Science Center	We thank N. Welters, J. van Tongeren and J. Ossebaar for analytical assistance. Funding for this research was provided by Utrecht University and the Netherlands Organization for Scientific Research (NWO, open competition grant ALWPJ/09047 to H. Brinkhuis and VICI grant to S. Schouten) - FWO (Research Foundation Flanders) Grant ID: G.0B85.13. SS is funded by the Netherlands Earth System Science Center. We are grateful for the thoughtful revisions of editor John Jagt, reviewer Hamid Slimani, and technical editor Sally Thomas, which improved this paper.	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J	Wary, M; Eynaud, F; Swingedouw, D; Masson-Delmotte, V; Matthiessen, J; Kissel, C; Zumaque, J; Rossignol, L; Jouzel, J				Wary, Melanie; Eynaud, Frederique; Swingedouw, Didier; Masson-Delmotte, Valerie; Matthiessen, Jens; Kissel, Catherine; Zumaque, Jena; Rossignol, Linda; Jouzel, Jean			Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events	CLIMATE OF THE PAST			English	Article							MILLENNIAL-SCALE VARIABILITY; MARINE ISOTOPIC STAGE-3; NEOGLOBOQUADRINA-PACHYDERMA; SPATIAL AUTOCORRELATION; PLANKTIC FORAMINIFERS; DINOFLAGELLATE CYSTS; FRESH-WATER; ICE COVER; OCEAN; RECONSTRUCTION	Dansgaard-Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here, based on dinocyst analyses from the 48-30 ka interval of four sediment cores from the northern Northeast Atlantic and southern Norwegian Sea, we provide direct and quantitative evidence of a regional paradoxical seesaw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases. Combined with additional palaeorecords and multi-model hosing simulations, our results suggest that during cold Greenland phases, reduced Atlantic meridional overturning circulation and cold North Atlantic sea-surface conditions were accompanied by the subsurface propagation of warm Atlantic waters that re-emerged in the Nordic Seas and provided moisture towards Greenland summit.	[Wary, Melanie; Eynaud, Frederique; Swingedouw, Didier; Zumaque, Jena; Rossignol, Linda] Univ Bordeaux, EPHE, CNRS, UMR 5805,EPOC, F-33615 Pessac, France; [Masson-Delmotte, Valerie; Kissel, Catherine; Jouzel, Jean] UVSQ, INSU, CNRS, UMR8212,LSCE,IPSL,CEA, F-91191 Gif Sur Yvette, France; [Matthiessen, Jens] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, D-27568 Bremerhaven, Germany; [Zumaque, Jena] Univ Quebec Montreal, Geotop, Montreal, PQ H3C 3P8, Canada	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; Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); CEA; Universite Paris Cite; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Quebec; University of Quebec Montreal	Wary, M (通讯作者)，Univ Bordeaux, EPHE, CNRS, UMR 5805,EPOC, F-33615 Pessac, France.	melanie.wary@u-bordeaux.fr; frederique.eynaud@u-bordeaux.fr	Masson-Delmotte, Valerie/G-1995-2011; Catherine, Kissel/AAH-1647-2019; Swingedouw, Didier/D-1408-2010; WARY, Melanie/S-1121-2018	Swingedouw, Didier/0000-0002-0583-0850; Matthiessen, Jens/0000-0002-6952-2494; WARY, Melanie/0000-0001-5211-2168; Eynaud, Frederique/0000-0003-1283-7425	French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement); INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme; ARTEMIS 14C AMS French INSU project; European Union [243908]; Agence Nationale de la Recherche (ANR) [ANR-10-CEPL-0008]; Agence Nationale de la Recherche (ANR) [ANR-10-CEPL-0008] Funding Source: Agence Nationale de la Recherche (ANR)	French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement); INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme; ARTEMIS 14C AMS French INSU project; European Union(European Union (EU)); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR)); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	We thank Marie-Helene Castera for technical assistance, Didier Roche, Florian Ziemen, Uwe Mikolajewicz, Maria Fernanda Sanchez Goni, Masa Kageyama, Mary Elliot, Aurelie Penaud, and Fabienne Marret-Davies for discussions, and Sandrine Manthe for MD95-2009 and MD95-2010 planktonic foraminiferal counts. Analyses performed on MD99-2285 were supported by the French INSU (Institut National des Sciences de l'Univers) programme LEFE (Les enveloppes fluides et l'environnement) within the frame of the EVE (Evolution et variabilite du climat a l'echelle globale) 2009-2011 project "RISCC: Role des Ice-Shelves dans le Changement Climatique" and of the IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean) 2013 project "ICE-BIO-RAM: Impact des Changements Environnementaux sur la BIOdiversite marine lors des Rechauffements Abrupts du cliMat", this latter being also supported by the INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU programme. We also acknowledge financial supports and facilities of the ARTEMIS 14C AMS French INSU project. The research leading to these results also benefited from fundings from the European Union's Seventh Framework programme (FP7/2007-2013) under grant agreement no 243908, "Past4Future. 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Past.	JUN 30	2017	13	6					729	739		10.5194/cp-13-729-2017	http://dx.doi.org/10.5194/cp-13-729-2017			11	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	EZ5SH		Green Submitted, gold			2025-03-11	WOS:000404777800001
J	Bisconti, M; Lambert, O; Bosselaers, M				Bisconti, Michelangelo; Lambert, Olivier; Bosselaers, Mark			Revision of "<i>Balaena</i>" belgica reveals a new right whale species, the possible ancestry of the northern right whale, <i>Eubalaena glacialis</i>, and the ages of divergence for the living right whale species	PEERJ			English	Article						Cetacea; Balaenidae; Eubalaena ianitrix; Mysticeti; Phylogeny; Pliocene	DINOFLAGELLATE CYST STRATIGRAPHY; PHYLOGENETIC-RELATIONSHIPS; BALAENOPTERID WHALE; CETACEA MYSTICETI; BALEEN WHALES; LATE EOCENE; BODY-SIZE; PLIOCENE; GENUS; EVOLUTION	In 1941, Abel established Balaena belgica based on a series of fused cervical vertebrae and citing other cranial fragments from the late Neogene of the Antwerp harbor (northern Belgium). Later, Plisnier-Ladame & Quinet (1969) added a neurocranium and other skeletal remains from the same area to this species. Recently, the neurocranium was re-assigned to the genus Eubalaena thanks to newer phylogenetic analyses. Here, a new description is provided of materials previously assigned to "Balaena" belgica together with taxonomic revisions. Our work suggests that the cervical complex originally designated as the type of "Balaena" belgica is too poorly preserved to be used as such and is assigned to Balaenidae gen. et sp. indet., thus making "Balaena" belgica a nomen dubium. In addition to the neurocranium, the other remains consist in a fragment of maxilla assigned to Balaenidae gen. et sp. indet. and in a humerus assigned to Eubalaena sp. Discovered in the Kruisschans Sands Member of the Lillo Formation (3.2-2.8 Ma, Piacenzian, Late Pliocene), the neurocranium is designated as the holotype of the new species Eubalaena ianitrix. Our phylogenetic analysis supports a sister-group relationship of Eubalaena ianitrix and Eubalaena glacialis, and helps constraining the ages of origin for balaenid clades. Ecological and phylogenetic data suggest that Eubalaena ianitrix may represent the direct ancestor of Eubalaena glacialis, the latter having evolved through phyletic transformation including body size increase during the temperature decline of the Late Pliocene.	[Bisconti, Michelangelo] San Diego Nat Hist Museum, San Diego, CA 92101 USA; [Lambert, Olivier; Bosselaers, Mark] Royal Belgian Inst Nat Sci, Brussels, Belgium; [Bosselaers, Mark] Zeeland Royal Soc Sci, Middelburg, Netherlands	Royal Belgian Institute of Natural Sciences	Bisconti, M (通讯作者)，San Diego Nat Hist Museum, San Diego, CA 92101 USA.	michelangelobisconti@gmail.com	Bisconti, Michelangelo/ITR-9582-2023; Lambert, Olivier/AEN-2469-2022	Lambert, Olivier/0000-0003-0740-5791; Bisconti, Michelangelo/0000-0002-0281-4863	Collection Study Grant from AMNH; Natuurmuseum Rotterdam that financed travel and study of the IZIKO collection; three Synthesys 2 grants; European Community Research Infrastructure Action under the FP 7 [305, 1730, 3057]	Collection Study Grant from AMNH; Natuurmuseum Rotterdam that financed travel and study of the IZIKO collection; three Synthesys 2 grants; European Community Research Infrastructure Action under the FP 7	M.B. received support from a Collection Study Grant from AMNH (2005), from Natuurmuseum Rotterdam that financed travel and study of the IZIKO collection (2007), and from three Synthesys 2 grants (Synthesys Project: http://www.synthesys.info/), which were financed in 2010, 2012, and 2013 by the European Community Research Infrastructure Action under the FP 7 (BE-TAF project no. 305, NL-TAF project no. 1730 and BE-TAF project no. 3057). 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	Candel, MS; Louwye, S; Borromei, AM				Soledad Candel, Maria; Louwye, Stephen; Maria Borromei, Ana			Reconstruction of the late Holocene paleoenvironment of the western Beagle Channel (Argentina) based on a palynological analysis	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	6th Argentine Congress of Quaternary and Geomorphology	APR, 2015	Ushuaia, ARGENTINA			Marine palaeoenvironments; Late Holocene; Beagle channel; Tierra del Fuego	TIERRA-DEL-FUEGO; SOUTHERNMOST SOUTH-AMERICA; DINOFLAGELLATE CYSTS; QUATERNARY; GLACIER; FJORD; PALYNOFACIES; GLACIATIONS; EVOLUTION; PATAGONIA	Palynological analysis was performed on sediment samples from Arroyo Baliza site (54 degrees 51' S, 68 degrees 33' W), western sector of the Beagle Channel, Tierra del Fuego, Argentina, in order to reconstruct the palaeoenvironmental history during the Holocene marine transgressive-regressive cycle in the Beagle Channel. The palynological analysis reveals the presence of a closed-canopy Nothofagus forest development in the coastal areas under a cold, wet and variable climate conditions during the late Holocene. The marine assemblage composition shows similarities to those modern assemblages recorded in the surface samples from the Beagle Channel, characterised by the dominance of Peridiniales taxa, suggesting environmental conditions during the late Holocene comparable to today. The increasing salinity during middle Holocene was accompanied by an increase in number and diversity of the microplanktonic assemblages, suggesting the gradual installation of a marine environment as it exists today in the Beagle Channel. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.	[Soledad Candel, Maria] CADIC CONICET, Lab Geomorfol & Cuaternario, B Houssay 200, RA-9410 Ushuaia, Argentina; [Louwye, Stephen] Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, Krijgslaan 281 S8-WE13, B-9000 Ghent, Belgium; [Maria Borromei, Ana] Univ Nacl Sur, Dept Geog, INGEOSUR CONICET, San Juan 670,B8000ICN, Bahia Blanca, Buenos Aires, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Ghent University; 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)，CADIC CONICET, Lab Geomorfol & Cuaternario, B Houssay 200, RA-9410 Ushuaia, Argentina.	soledadcandel@cadic-conicet.gob.ar; louwye@ugent.be; borromei@criba.edu.ar	Louwye, Stephen/D-3856-2012		Erasmus Mundus (EuroTANGO II project) Postdoctoral fellowship; CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas) [PIP 11220100100041]	Erasmus Mundus (EuroTANGO II project) Postdoctoral fellowship; CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET))	This research was conducted by the lead author at Ghent University, Belgium thanks to an Erasmus Mundus (EuroTANGO II project) Postdoctoral fellowship. This study was also supported by CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas, PIP 11220100100041) grant to Ana Maria Borromei. We are grateful to Marcelo A. Martinez and Lorena L Musotto (INGEOSUR-CONICET, Universidad Nacional del Sur, Argentina), Juan Federico Ponce and Andrea Coronato (CADIC-CONICET, Ushuaia, Argentina) for field assistance and contributing resources in the field work. Our thanks are also extended to Sabine Van Cauwenberghe (RUP, UGent, Belgium) for her help in the laboratory. We thank to Dr. Min-Te Chen and two anonymous reviewers for their constructive comments that helped to improve our manuscript.	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Int.	JUN 23	2017	442		A				2	12		10.1016/j.quaint.2016.01.074	http://dx.doi.org/10.1016/j.quaint.2016.01.074			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	EZ9NG		Green Published			2025-03-11	WOS:000405056500002
J	Eichentopf, H; Böcker, J; Littke, R				Eichentopf, Hannah; Boecker, Johannes; Littke, Ralf			Source rock characterisation of the Rupelian Fish Shale (Bodenheim Fm. / Hochberg Sbfm.) - An organic geochemical profile from the clay pit "Unterfeld" (Rauenberg, Germany) in the Upper Rhine Graben	ZEITSCHRIFT DER DEUTSCHEN GESELLSCHAFT FUR GEOWISSENSCHAFTEN			English	Article						Fish Shale; Upper Rhine Graben; clay pit Unterfeld; source rock; shallow marine depositional environment; thermal maturity	POSIDONIA SHALE; LOWER TOARCIAN; MOLASSE BASIN; MATTER; OIL; QUANTIFICATION; PRESERVATION; PYROLYSIS; SEDIMENTS; MATURITY	Based on samples from a vertical profile in the clay pit "Unterfeld", located in the central part of the Upper Rhine Graben, this paper provides the first detailed organic geochemical characterisation of the Rupelian Fish Shale (Bodenheim Fm., Oligocene). The Fish Shale acts as an important source rock in the central and northern Upper Rhine Graben regarding the filling process of several oil fields. Mean TOC values of 4.0 % and mean hydrogen index (HI) values of 559 mg HC/g TOC are indicative of a high source rock potential for the Fish Shale with typical oil-prone type II kerogen. High mean sulphur contents (2.7 %) result from an anoxic depositional environment. Due to a vertically homogenous profile with respect to TOC, carbonate and sulphur content as well as hydrocarbon generation potential, lateral homogeneity can be assumed as well for the central Upper Rhine Graben. The occurrences of a highly branched C-25 isoprenoid as well as diatoms, dinoflagellate cysts and parts of fish bones are highly specific for this marine source rocks. Due to its unique geochemical character, biomarker data can be well used for oil to source rock correlation. A low vitrinite reflectance of 0.30 % indicates that the Fish Shale at this location has to be regarded as thermally immature with respect to oil generation. This finding is supported by low T-max values of about 417 degrees C and various molecular geochemical parameters, which were obtained for selected samples. In deeper settings of the Upper Rhine Graben, however, the oil window is reached by the Fish Shale.	[Eichentopf, Hannah; Boecker, Johannes; Littke, Ralf] Rhein Westfal TH Aachen, Energy & Mineral Resources Grp EMR, Inst Geol & Geochem Petr & Coal, Lochnerstr 4-20, D-52056 Aachen, Germany; [Boecker, Johannes] ENGIE E&P Deutschland GmbH, Waldstr 39, D-49808 Lingen, Ems, Germany	RWTH Aachen University	Littke, R (通讯作者)，Rhein Westfal TH Aachen, Energy & Mineral Resources Grp EMR, Inst Geol & Geochem Petr & Coal, Lochnerstr 4-20, D-52056 Aachen, Germany.	ralf.littke@emr.rwth-aachen.de	Littke, Ralf/A-6701-2016					[Anonymous], 1998, Carolinea; [Anonymous], BIOMARKER GUIDE; [Anonymous], 2005, GEOLOGIE RHEINLAND P; Battarbee R.W., 2001, TRACKING ENV CHANGES, P155, DOI DOI 10.1007/0-306-47668-1_8; Berger JP, 2005, INT J EARTH SCI, V94, P697, DOI 10.1007/s00531-005-0475-2; BERNER RA, 1984, GEOCHIM COSMOCHIM AC, V48, P605, DOI 10.1016/0016-7037(84)90089-9; Berner U., 2011, ERDOL ERDGAS KOHLE, V127, P303; Böcker J, 2017, INT J EARTH SCI, V106, P707, DOI 10.1007/s00531-016-1330-3; Böcker J, 2014, Z DTSCH GES GEOWISS, V165, P247, DOI 10.1127/1860-1804/2014/0063; Bou Daher S, 2015, MAR PETROL GEOL, V64, P304, DOI 10.1016/j.marpetgeo.2015.03.009; BROOKS JD, 1969, NATURE, V222, P257, DOI 10.1038/222257a0; Bruss D., 2000, BER FORSCHUNGSZ JULI, V3831; Di Primio R., 1995, BER FORSCHUNGSZ JULI, V3110; diPrimio R, 1996, ORG GEOCHEM, V24, P999, DOI 10.1016/S0146-6380(96)00116-7; Eisbacher G.H., 2010, SAMMLUNG GEOLOGISCHE, V103; ESPITALIE J, 1985, REV I FR PETROL, V40, P563, DOI 10.2516/ogst:1985035; ESPITALIE J, 1977, REV I FR PETROL, V32, P23, DOI 10.2516/ogst:1977002; Frimmel A., 2003, THESIS U TUBINGEN; Geyer OF., 2011, Geologie von Baden-Wurttemberg 5th edition, V5; Grimm Kirsten I., 2002, Courier Forschungsinstitut Senckenberg, V237, P229; Grimm M. 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Results, V157, P361; Littke R., 1993, LECT NOTES EARTH SCI, V47, P218; MARTINI E, 1971, ERD KOH ERDG PETR V, V24, P381; Marynowski L, 2011, CHEM GEOL, V285, P144, DOI 10.1016/j.chemgeo.2011.04.001; Micklich Norbert, 2005, Kaupia Darmstaedter Beitraege zur Naturgeschichte, V14, P113; Missbach H, 2016, INT J ASTROBIOL, V15, P165, DOI 10.1017/S1473550416000069; NICHOLS PD, 1988, J PHYCOL, V24, P90; Peters K.E., 1994, PETROLEUM SYSTEM SOU, P93, DOI DOI 10.1306/M60585C5; PETERS KE, 1986, AAPG BULL, V70, P318; Richter BE, 1996, ANAL CHEM, V68, P1033, DOI 10.1021/ac9508199; RIVA A, 1988, ORG GEOCHEM, V13, P671, DOI 10.1016/0146-6380(88)90088-5; Röhl HJ, 2001, PALAEOGEOGR PALAEOCL, V165, P27, DOI 10.1016/S0031-0182(00)00152-8; Ruckheim J., 1989, BER FORSCHUNGSZ JULI, V2307; Sachse VF, 2011, ORG GEOCHEM, V42, P209, DOI 10.1016/j.orggeochem.2010.12.004; Seifert W.K., 1980, PHYS CHEM EARTH, P229, DOI DOI 10.1016/0079-1946(79)90107-1; SHANMUGAM G, 1985, AAPG BULL, V69, P1241; Sissingh W, 1998, TECTONOPHYSICS, V300, P249, DOI 10.1016/S0040-1951(98)00243-1; Song JL, 2015, INT J COAL GEOL, V150, P127, DOI 10.1016/j.coal.2015.08.011; Tissot B. P., 1984, 2nd ed. Berlin: Springer; Volkman J.K., 1986, Biological markers in the sedimentary record, P1; VOLKMAN JK, 1994, ORG GEOCHEM, V21, P407, DOI 10.1016/0146-6380(94)90202-X; Weiss H.M., 2000, NIGOGA - The Norwegian Industry Guide to Organic Geochemical Analyses; ZIEGLER PA, 1992, TECTONOPHYSICS, V208, P91, DOI 10.1016/0040-1951(92)90338-7	55	2	2	0	6	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	1860-1804	1861-4094		Z DTSCH GES GEOWISS	Z. Dtsch. Ges. Geowiss.	JUN	2017	168	2					217	232		10.1127/zdgg/2017/0112	http://dx.doi.org/10.1127/zdgg/2017/0112			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FO4MD					2025-03-11	WOS:000416817400002
J	Zhao, XQ; Dupont, L; Schefuss, E; Bouimetarhan, I; Wefer, G				Zhao, Xueqin; Dupont, Lydie; Schefuss, Enno; Bouimetarhan, Ilham; Wefer, Gerold			Palynological evidence for Holocene climatic and oceanographic changes off western South Africa	QUATERNARY SCIENCE REVIEWS			English	Article						Dinoflagellate cysts; Paleoceanography; Paleoenvironment; West coast of South Africa; Holocene	WALLED DINOFLAGELLATE CYSTS; LATITUDE MARINE ENVIRONMENTS; BENGUELA UPWELLING REGION; SURFACE SEDIMENTS; AGULHAS LEAKAGE; LATE QUATERNARY; ATLANTIC-OCEAN; NORTH-ATLANTIC; INDIAN-OCEAN; ORANGE RIVER	Atmospheric and oceanographic interactions between the Atlantic and Indian Oceans influence up welling in the southern Benguela upwelling system. In order to obtain a better knowledge of paleoceanographic and paleoenvironmental changes in the southern Benguela region during the Holocene, 12 marine surface sediment samples and one gravity core GeoB8331-4 from the Namaqualand mudbelt off the west coast of South Africa have been studied for organic-walled dinoflagellate cysts in high temporal resolution. The results are compared with pollen and geochemical records from the same samples. Our study emphasizes significantly distinct histories in upwelling intensity as well as the influence of fluvial input during the Holocene. Three main phases were identified for the Holocene. High percentages of cysts produced by autotrophic taxa like Operculodinium centrocarpum and Spiniferites spp. indicate warmer and stratified conditions during the early Holocene (9900-8400 cal. yr BP), suggesting reduced upwelling likely due to a northward shift of the southern westerlies. In contrast, the middle Holocene (8400-3100 cal. yr BP) is characterized by a strong increase in heterotrophic taxa in particular Lejeunecysta paratenella and Echinidinium spp. at the expense of autotrophic taxa. This indicates cool and nutrient-rich waters with active upwelling probably caused by a southward shift of the southern westerlies. During the late Holocene (3100 cal. yr BP to modern), Brigantedinium spp. and other abundant taxa interpreted to indicate fluvial nutrient input such as cyst of Protoperidinium arnericanum and Lejeunecysta oliva imply strong river discharge with high nutrient supply between 3100 and 640 cal. yr BP. (C) 2017 Elsevier Ltd. All rights reserved.	[Zhao, Xueqin; Dupont, Lydie; Schefuss, Enno; Bouimetarhan, Ilham; Wefer, Gerold] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str, Bremen, Germany	University of Bremen	Zhao, XQ (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany.	xzhao@marum.de; dupont@uni-bremen.de; eschefuss@marum.de; ibouimetarhan@marum.de; gwefer@marum.de	Bouimetarhan, Ilham/D-2388-2011; Schefuss, Enno/A-7101-2015; Wefer, Gerold/S-2291-2016	Bouimetarhan, Ilham/0000-0003-3369-3811; Dupont, Lydie/0000-0001-9531-6793; Schefuss, Enno/0000-0002-5960-930X; Wefer, Gerold/0000-0002-6803-2020; Zhao, Xueqin/0000-0003-3354-3768	German Federal Ministry of Education and Research (BMBF) [03G0840A]; GLOMAR (Bremen International Graduate School for Marine Sciences)	German Federal Ministry of Education and Research (BMBF)(Federal Ministry of Education & Research (BMBF)); GLOMAR (Bremen International Graduate School for Marine Sciences)	This study was funded by the German Federal Ministry of Education and Research (BMBF) (Grant/Award Number: '03G0840A'). The investigations were conducted within the collaborative project 'Regional Archives for Integrated Investigations' (RAiN), which is embedded in the international research programme SPACES (Science Partnership for the Assessment of Complex Earth System Processes). We thank the captain, the crew, and the scientists of the Meteor cruise M57-1 for recovering the studied samples, and the GeoB core repository in MARUM (Center for Marine Environmental Sciences) for retaining the samples. Thanks to GLOMAR (Bremen International Graduate School for Marine Sciences) for supporting the first author's PhD project. We would like to thank Karin Zonneveld for her help with the dinoflagellate cyst identification. Gesine Mollenhauer and Nicole Herrmann are thanked for helpful discussion. We thank the two anonymous reviewers for their helpful and constructive comments.	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Sci. Rev.	JUN 1	2017	165						88	101		10.1016/j.quascirev.2017.04.022	http://dx.doi.org/10.1016/j.quascirev.2017.04.022			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	EX0YO					2025-03-11	WOS:000402946900007
J	Pellen, R; Popescu, SM; Suc, JP; Melinte-Dobrinescu, MC; Rubino, JL; Rabineau, M; Marabini, S; Loget, N; Casero, P; Cavazza, W; Head, MJ; Aslanian, D				Pellen, Romain; Popescu, Speranta-Maria; Suc, Jean-Pierre; Melinte-Dobrinescu, Mihaela Carmen; Rubino, Jean-Loup; Rabineau, Marina; Marabini, Stefano; Loget, Nicolas; Casero, Piero; Cavazza, William; Head, Martin J.; Aslanian, Daniel			The Apennine foredeep (Italy) during the latest Messinian: Lago Mare reflects competing brackish and marine conditions based on calcareous nannofossils and dinoflagellate cysts	GEOBIOS			English	Article						Dinoflagellate cysts; Calcareous nannoplankton; Lago Mare; Colombacci deposits; Apennine foredeep; Palaeo-sill	SECTION MARCHE PROVINCE; EARLIEST ZANCLEAN AGE; DI-TETTO FORMATIONS; TERTIARY PIEDMONT BASIN; NORTHERN APENNINES; SALINITY CRISIS; LATE MIOCENE; PALEOENVIRONMENTAL DATA; FORELAND BASIN; STRATIGRAPHIC EVOLUTION	Sediments deposited after the peak of the Messinian Salinity Crisis (MSC) in the Apennine foredeep of Italy embody a topic debated on both chronostratigraphic and palaeoenvironmental grounds. We performed micropalaeontological (calcareous nannofossil and dinoflagellate cyst) analyses on four stratigraphic sections (Monticino, Civitella del Tronto, Fonte dei Pulcini, Fonte la Casa) and reused those previously published from Maccarone. All sections belong to the p-ev(2) Fm. that includes the Colombacci deposits, usually considered emblematic of the Lago Mare in the area. Marine microfossils recorded in previous studies have often been neglected or considered reworked and hence discarded. We propose the occurrence of at least four marine inflows between 5.36 and 5.33 Ma, the first of which is reflected in the Apennine foredeep by marine dinoflagellates that are then replaced by Paratethyan (brackish) ones. Paratethyan species occupied favourable environments during intervals separating marine inflows while the marine species survived elsewhere. From this perspective, the Apennine foredeep was an isolated perched basin during most of the peak of the MSC (5.60-5.36 Ma), and was progressively and repeatedly invaded by marine waters overflowing a palaeo-sill before the beginning of the Zanclean (5.33 Ma) which itself reflects a continuing eustatic rise. The Gargano Peninsula and, offshore, the present-day Pelagosa sill may be regarded as the remnants of this Messinian sill. This interpretation provides new possibilities for ecostratigraphically correlating the sections with Lago Mare biofacies, the deposition of which unquestionably started prior to the deposition of Colombacci sediments and continued into the earliest Zanclean. The results of this study show that the Lago Mare facies cannot be restricted to a single brackish palaeoenvironment but included competing marine and brackish waters controlled by geographic and chronological factors. Deposits overlying the unconformity separating the regional p-ev(1), and p-ev(2) formations are considered to represent the first marine incursion into the Apennine foredeep. These results allow us to refine the palaeogeographic reconstruction of the Apennine foredeep during the peak of the MSC. Although this basin was deep, its history during the peak of the MSC did not parallel that of the central Mediterranean basins. (C) 2017 Elsevier Masson SAS. All rights reserved.	[Pellen, Romain; Rabineau, Marina] Univ Bretagne Occidentale, IUEM, UMR CNRS 6538, Domaines Ocean, 1 Pl Nicolas Copernic, F-29280 Plouzane, France; [Popescu, Speranta-Maria] GeoBioStratData Consulting, 385 Route Mas Rillier, F-69140 Rillieux La Pape, France; [Suc, Jean-Pierre; Loget, Nicolas] UPMC Univ Paris 06, Sorbonne Univ, CNRS, Inst Sci Terre Paris iSTeP,UMR 7193, 4 Pl Jussieu, F-75005 Paris, France; [Melinte-Dobrinescu, Mihaela Carmen] Natl Inst Marine Geol & Geoecol, 23-25 Dimitrie Onciul St,POB 34-51, Bucharest 70318, Romania; [Rubino, Jean-Loup] CSTTF, TOTAL, TG ISS, Ave Laribeau, F-64018 Pau, France; [Marabini, Stefano] Univ Bologna, Dip BiGeA, Muse Geol Giovanni Capellini, Via Zamboni 63, I-40126 Bologna, Italy; [Casero, Piero] Via Enrico di S Martino Valperga 57, Rome, Italy; [Cavazza, William] Univ Bologna, Dipartimento Sci Biol Geol & Ambientali, Piazza Porta San Donato 1, I-40126 Bologna, Italy; [Head, Martin J.] Brock Univ, Dept Earth Sci, 1812 Sir Isaac Brock Way, St Catharines, ON L2S 3A1, Canada; [Aslanian, Daniel] IFREMER, UR Geosci Marines, BP 70, F-29280 Plouzane, France	Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Total SA; University of Bologna; University of Bologna; Brock University; Ifremer	Pellen, R (通讯作者)，Univ Bretagne Occidentale, IUEM, UMR CNRS 6538, Domaines Ocean, 1 Pl Nicolas Copernic, F-29280 Plouzane, France.; Suc, JP (通讯作者)，UPMC Univ Paris 06, Sorbonne Univ, CNRS, Inst Sci Terre Paris iSTeP,UMR 7193, 4 Pl Jussieu, F-75005 Paris, France.	romin.pellen@gmail.com; jeanpierre.suc@gmail.com	Aslanian, Daniel/JWA-0851-2024; Mihaela, mihaela/AAF-5894-2021; Loget, Nicolas/A-9613-2011; Rabineau, Marina/E-3408-2010	Loget, Nicolas/0000-0001-6552-2238; Rabineau, Marina/0000-0001-8420-1587; Aslanian, Daniel/0000-0002-9394-606X	TerMex Program (MISTRALS) through the project AFAME for micropalaeontological analyses; CNRS-INSU `SYSTER'; 'Actions Marges' programs (projects 'Mouvements verticaux' and 'MEDOCC'); IFREMER; Laboratoire d'Excellence' LabexMER [ANR-10-LABX-19]; French government under the program 'Investissements d'Avenir'; Regional Council of Brittany; CNRS; UBO; French 'Actions Marges' program; GRI Mediterranee (Groupement Recherche et Industrie TOTAL-UPMC)	TerMex Program (MISTRALS) through the project AFAME for micropalaeontological analyses; CNRS-INSU `SYSTER'; 'Actions Marges' programs (projects 'Mouvements verticaux' and 'MEDOCC'); IFREMER; Laboratoire d'Excellence' LabexMER; French government under the program 'Investissements d'Avenir'(Agence Nationale de la Recherche (ANR)); Regional Council of Brittany(Region Bretagne); CNRS(Centre National de la Recherche Scientifique (CNRS)); UBO; French 'Actions Marges' program; GRI Mediterranee (Groupement Recherche et Industrie TOTAL-UPMC)	We particularly thank Prof. G.B. Vai, Director of the Monticino Geopark, for permitting our sampling. F. Lirer contributed to the sampling trips at Civitello del Tronto. The TerMex Program (MISTRALS) provided significant financial support through the project AFAME for micropalaeontological analyses and two field trips to Civitella del Tronto. The other field trips were supported by the CNRS-INSU `SYSTER' and 'Actions Marges' programs (projects 'Mouvements verticaux' and 'MEDOCC'), and by IFREMER. A scholarship to R. Pellen was provided by the 'Laboratoire d'Excellence' LabexMER (ANR-10-LABX-19), a French government-funded project under the program 'Investissements d'Avenir' and co-funded by a grant from the Regional Council of Brittany. It was further supported by IFREMER, CNRS and UBO with additional support from the French 'Actions Marges' program and the GRI Mediterranee (Groupement Recherche et Industrie TOTAL-UPMC). TOTAL is acknowledged for permission to publish the line drawings of seismic profiles NOSE05 and NOSE07. We are particularly grateful to three anonymous reviewers whose constructive comments led to significant improvements to our manuscript.	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J	Shin, HH; Li, Z; Yoon, YH; Oh, SJ; Lim, WA				Shin, Hyeon Ho; Li, Zhun; Yoon, Yang Ho; Oh, Seok Jin; Lim, Wol-Ae			Formation and germination of temporary cysts of <i>Cochlodinium polykrikoides</i> Margalef (Dinophyceae) and their ecological role in dense blooms	HARMFUL ALGAE			English	Article						Cochlodinium polykrikoides; Chain forming temporary cyst; Formation; Germination; Germling	HARMFUL ALGAL BLOOMS; ALEXANDRIUM-TAYLORI DINOPHYCEAE; RED TIDE; GONYAULAX-TAMARENSIS; COASTAL WATERS; NEW-YORK; DINOFLAGELLATE; GROWTH; PHYTOPLANKTON; GYMNODINIALES	While the initiation and development of dense bloom of Cochlodinium polykrikoides have been shown to be related to some environmental factors, little is known about the ecological role of the formation and germination of temporary cysts, nor of their significance for the rapid expansion of dense regional-scale blooms. This study examined the factors affecting the formation and germination of temporary cysts of C. polykrikoides, and provides details about the germination process. In the laboratory experiments, C. polykrikoides produced the chain-forming temporary cysts that are immobile and surrounded by a hyaline membrane. The encystment experiment indicated that darkness induces the formation of chain forming temporary cysts, consistent with field observation of morphology and fluxes of temporary cysts. Germination occurred twice from a single four-celled temporary cysts within 24 h after exposure to light, and the germlings appeared as two-celled chain-forming vegetative cells. The germination behavior of temporary cysts of C. polykrikoides differs from that of other dinoflagellates, and this may be a survival strategy for the maintenance of population size during dense blooms. (C) 2017 Elsevier B.V. All rights reserved.	[Shin, Hyeon Ho; Li, Zhun] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea; [Yoon, Yang Ho] Chonnam Natl Univ, Fac Marine Technol, Mipyeongro 386, Yeosu 550749, South Korea; [Oh, Seok Jin] Pukyong Natl Univ, Busan 608737, South Korea; [Lim, Wol-Ae] Natl Inst Fisheries Sci, Busan 619705, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Chonnam National University; Pukyong National University; National Institute of Fisheries Science	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea.	shh961121@kiost.ac.kr	LI, ZHUN/GLT-3478-2022	LI, ZHUN/0000-0001-8961-9966; Shin, Hyeon Ho/0000-0002-9711-6717	KIOST [PE99515]; NIFS [R2017047]; KIMST	KIOST; NIFS; KIMST(Korea Institute of Marine Science & Technology Promotion (KIMST))	This work was supported by grants from KIMST, KIOST (PE99515) and NIFS (R2017047).[CG]	ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anderson JT, 2003, MAR ECOL PROG SER, V246, P95, DOI 10.3354/meps246095; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Dale B., 1983, P69; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; Garces E., 2002, LIFEHAB, P46; Gobler CJ, 2012, HARMFUL ALGAE, V17, P64, DOI 10.1016/j.hal.2012.03.001; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; Kim DI, 2004, J PLANKTON RES, V26, P61, DOI 10.1093/plankt/fbh001; Lee CK, 2013, HARMFUL ALGAE, V30, pS3, DOI 10.1016/j.hal.2013.10.002; Lee YS, 2006, MAR POLLUT BULL, V52, P1249, DOI 10.1016/j.marpolbul.2006.02.024; Li Z, 2015, J PHYCOL, V51, P204, DOI 10.1111/jpy.12252; MANSINGH A, 1971, CAN ENTOMOL, V103, P983, DOI 10.4039/Ent103983-7; Matsuoka K, 2008, HARMFUL ALGAE, V7, P261, DOI 10.1016/j.hal.2007.12.002; Matsuzaki K, 2003, MATER SCI FORUM, V426-4, P563, DOI 10.4028/www.scientific.net/MSF.426-432.563; Nagasaki K, 2000, NIPPON SUISAN GAKK, V66, P666; Nehring S., 1993, P INT COAST C INT DI, P454; NFRDI, 2012, Annual Report of NFRDI on Red Tide of Korea; Oh S J, 2010, J KOREAN FISHERY AQU, V43, P715; Oh Seok Jin, 2006, Algae, V21, P311; Olli K, 2004, MAR BIOL, V145, P1, DOI 10.1007/s00227-004-1295-9; Omura T, 2012, MARINE PHYTOPLANKTON; Onitsuka G, 2010, HARMFUL ALGAE, V9, P390, DOI 10.1016/j.hal.2010.01.006; Park JG, 2001, PHYCOLOGIA, V40, P292, DOI 10.2216/i0031-8884-40-3-292.1; Rintala JM, 2007, MAR BIOL, V152, P57, DOI 10.1007/s00227-007-0652-x; Schmitter R.E., 1979, P123; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; Tang YZ, 2012, HARMFUL ALGAE, V20, P71, DOI 10.1016/j.hal.2012.08.001; Tang YZ, 2010, P NATL ACAD SCI USA, V107, P20756, DOI 10.1073/pnas.1009566107; Tang YZ, 2010, MAR ECOL PROG SER, V406, P19, DOI 10.3354/meps08537; Tomas CR, 2008, HARMFUL ALGAE, V7, P308, DOI 10.1016/j.hal.2007.12.005	34	18	20	1	28	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	JUN	2017	66						57	64		10.1016/j.hal.2017.05.002	http://dx.doi.org/10.1016/j.hal.2017.05.002			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	EY9FE	28602254				2025-03-11	WOS:000404303700007
J	Hoppenrath, M				Hoppenrath, Mona			Dinoflagellate taxonomy - a review and proposal of a revised classification	MARINE BIODIVERSITY			English	Review						Dinophytes; Dinozoa; Morphology; Phylogeny; Systematics	SAND-DWELLING DINOFLAGELLATE; CYST-THECA RELATIONSHIP; GEN. NOV DINOPHYCEAE; EARLY EVOLUTIONARY HISTORY; WESTERN KOREA MORPHOLOGY; SHIWHAENSE N. GEN.; MOLECULAR PHYLOGENY; RIBOSOMAL DNA; EMENDED DESCRIPTION; HETEROTROPHIC DINOFLAGELLATE	The knowledge about morphology-based taxonomy and classification as well as molecular phylogenetic hypotheses and character evolution of dinokaryotic dinoflagellates was summarized. Recommendations for future taxonomic work and character evaluations were given. A classification scheme based on nameless ranked systematics for dinoflagellate levels above genus was proposed. Higher ranks were based on the relative number of alveolae (Polyalveolate and Oligoalveolate) and their arrangement. Polyalveolate had alveolae arranged in series or not. Oligoalveolate had alveolae arranged in different tabulation patterns (Symmetricomorpha, Asymmetricomorpha, Sagittale). A group of taxa with unclear tabulation type (in-between peridinioid and gonyaulacoid) was separated and named Mesomorpha. A higher rank for taxa with a sagittal suture splitting only the hyposome in two lateral halves (extra tabulation pattern) was created, Pre-sagittale. The classification intended to highlight the unresolved relationships of higher ranks. Furthermore, the difficulties to define characters suitable for general higher rank circumscription should become visible. The study pinpointed what needs to be done to improve the current dinoflagellate taxonomy.	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Biodivers.	JUN	2017	47	2					381	403		10.1007/s12526-016-0471-8	http://dx.doi.org/10.1007/s12526-016-0471-8			23	Biodiversity Conservation; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Marine & Freshwater Biology	EX2MW					2025-03-11	WOS:000403061500017
J	Mudie, PJ; Marret, F; Mertens, KN; Shumilovskikh, L; Leroy, SAG				Mudie, Peta J.; Marret, Fabienne; Mertens, Kenneth N.; Shumilovskikh, Lyudmila; Leroy, Suzanne A. G.			Atlas of modern dinoflagellate cyst distributions in the Black Sea Corridor: from Aegean to Aral Seas, including Marmara, Black, Azov and Caspian Seas	MARINE MICROPALEONTOLOGY			English	Article						Phytoplankton; Harmful algae; Biodiversity; Paleoceanography; Surface samples	FRESH-WATER DINOFLAGELLATE; RECENT MARINE-SEDIMENTS; NORTH-ATLANTIC OCEAN; SP-NOV DINOPHYCEAE; SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; PROCESS LENGTH VARIATION; NON-POLLEN PALYNOMORPHS; LAST 2000 YEARS; SURFACE SEDIMENTS; THECA RELATIONSHIP	We present the first comprehensive taxonomic and environmental study of dinoflagellate cysts in 185 surface sediment samples from the Black Sea Corridor (BSC) which is a series of marine basins extending from the Aegean to the Aral Seas (including Marmara, Black, Azov and Caspian Seas). For decades, these low-salinity, semi-enclosed or endorheic basins have experienced large-scale changes because of intensive agriculture and industrialisation, with consequent eutrophication and increased algal blooms. The BSC atlas data provide a baseline for improved understanding of linkages between surface water conditions and dinoflagellate cyst (dinocyst) distribution, diversity and morphological variations. By cross-reference to dinocyst occurrences in sediment cores with radiocarbon ages covering the past c. 11,700 years, the history of recent biodiversity changes can be evaluated. The seabed cyst samples integrate seasonal and multi-year data which are not usually captured by plankton samples, and the cyst composition can point to presence of previously unrecorded motile dinoflagellate species in the BSC. Results show the presence of at least 71 dinocyst taxa of which 36% can be related to motile stages recorded in the plankton. Comparison with sediment core records shows that five new taxa appear to have entered or re-entered the region over the past century. Statistical analysis of the atlas data reveals the presence of four ecological assemblages which are primarily correlated with seasonal and annual surface water salinity and temperature; correlation with phosphate, nitrate and silicate nutrients, chlorophyll-alpha and bottom water oxygen is less clear but may be important for some taxa. Biodiversity indices reveal strong west east biogeographical differences among the basins that reflect the different histories of Mediterranean versus Ponto-Caspian connections. The atlas data provide a standardised taxonomy and regional database for interpreting downcore cyst variations in terms of quantitative oceanographic changes. The atlas also provides a baseline for monitoring further changes in the BSC dinocysts that may accompany the accelerating development of the region.	[Mudie, Peta J.] Geol Survey Canada, Box 1008, Dartmouth, NS B2Y 4A2, Canada; [Marret, Fabienne; Leroy, Suzanne A. G.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Mertens, Kenneth N.] Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium; [Shumilovskikh, Lyudmila] Univ Gottingen, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany; [Leroy, Suzanne A. G.] CEREGE, Technopole Arbois,BP 80, F-13545 Aix En Provence 4, France; [Mertens, Kenneth N.] LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Liverpool; Ghent University; University of Gottingen	Marret, F (通讯作者)，Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England.	f.marret@liverpool.ac.uk	Mertens, Kenneth/AAO-9566-2020; Shumilovskikh, Lyudmila/P-2493-2015; Mertens, Kenneth/C-3386-2015	Mertens, Kenneth/0000-0003-2005-9483; Marret-Davies, Fabienne/0000-0003-4244-0437	Leverhume Trust [F/00025/AN]; NSERC [RGPIN55408]	Leverhume Trust; NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	We are very grateful to Ali Aksu at Memorial University of Newfoundland (MUN) for providing over 50 surface samples and cores from Marmara and SW Black Sea, and to Helen Gillespie at the MUN CREAIT laboratory for palynological processing. We also sincerely thank Valentina Yanko-Hombach and Tatiana Kondaryuk of Odessa I.I. Mechnikov National University, Ukraine, for invaluable contribution of 74 samples from the Ukrainian (SH and HERMES samples) and Danube Shelves (MN samples). Gennady Matishov provided samples from the Sea of Azov. We also thank Helge W. Arz (Leibniz Institute for Baltic Sea Research Warnemiinde) for providing of 25 surface samples from the deep basin of the Black Sea. Charlotte Desmet is acknowledged for her contributions to the dataset. Thomas Verleye is thanked for loan of slides to photograph specimens. Lee Bradley and Eric Mousing are thanked for sharing their published data. Speranta Popescu is thanked for sharing palynological residues from the Black Sea, and Neslihan Balkis at Istanbul University for valuable information on cysts cultured from Marmara Sea plankton and surface sediment samples. We are grateful to the multiple contributors of surface samples in the Caspian and Aral Seas, including H. Lahijani and his group at INIOAS, Peter Zavialov and his group at the Shirshov Institute of Oceanology (SIO), Irina Muschik via Adventurers and Scientists for Conservation, Francois Gasse and the INCO-Copernicus project, A. Kakroodi (University of Tehran), H. Nazmllahzadeh and his group at the Caspian Sea Ecology Research Center, and H. Nazari and his colleagues at the Geological Survey of Iran. Suzanne Yee at the Liverpool University School of Environmental Sciences helped greatly with drafting of Fig. 1. Andre Rochon (ISMER) is thanked for his earlier SEM studies of Marmara Sea cysts. FMD would like to thank the Leverhume Trust (F/00025/AN) and the GNS-NZ for their hosting. PJM acknowledges NSERC funding support for Discovery Grant RGPIN55408) while at Memorial University 2008 2012. 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Micropaleontol.	JUN	2017	134						1	152		10.1016/j.marmicro.2017.05.004	http://dx.doi.org/10.1016/j.marmicro.2017.05.004			152	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	FP5LT					2025-03-11	WOS:000417661700001
J	Simo-Matchim, AG; Gosselin, M; Poulin, M; Ardyna, M; Lessard, S				Simo-Matchim, Armelle-Galine; Gosselin, Michel; Poulin, Michel; Ardyna, Mathieu; Lessard, Sylvie			Summer and fall distribution of phytoplankton in relation to environmental variables in Labrador fjords, with special emphasis on <i>Phaeocystis pouchetii</i>	MARINE ECOLOGY PROGRESS SERIES			English	Article						Taxonomic composition; Protists; Phytoplankton; Diatoms; Phaeocystis; Seasonal variability; Northeastern Canada; Labrador; Fjords	OCEAN SEA-ICE; COMMUNITY STRUCTURE; SPRING BLOOM; FOOD-WEB; SEASONAL-VARIATIONS; NORTHERN NORWAY; MARINE PLANKTON; COASTAL WATERS; CHLOROPHYLL-A; DYNAMICS	Protist (> 2 mu m) taxonomic composition was investigated for the first time in 4 Labrador fjords (Nachvak, Saglek, Okak and Anaktalak) during summers 2007 and 2013, early fall 2010 and late fall 2009. Protist composition was significantly different from one season to another. Significant spatial differences in protist composition were found only during summer 2013. During summer 2007, the community was characterized by diatoms and a mixed assemblage of flagellates. In summer 2013, flagellates largely dominated the community, and an intense Phaeocystis pouchetii bloom was observed in Nachvak Fjord (18 x 10(6) cells l(-1)). In autumn, the community was dominated by unidentified flagellates, prymnesiophytes and diatoms, in various proportions from early to late fall. From a summer situation characterized by stronger stratification, higher incident irradiance and depleted nutrients in surface waters, it evolved to an autumn situation characterized by decreasing air temperature and irradiance associated with an environmental forcing (e.g. weather) allowing cooling and greater vertical mixing of the water column. Combining our observations with those from the literature, we suggest the following annual succession in the Labrador fjord phytoplankton community: (winter) dinoflagellates and small flagellated cells-(spring) Fragilariopsis spp., Chaetoceros spp., Thalassiosira spp. and Phaeo cystis pouchetii-(summer) Chaetoceros spp., P. pouchetii and Chrysochromulina spp.-(fall) Gymnodinium/Gyrodinium spp., Chrysochromulina spp. and other flagellates. Overall, the protist richness was 2 times higher in fall than in summer, the highest richness being observed in early fall, with 201 taxonomic entries, 72 genera and 131 species identified.	[Simo-Matchim, Armelle-Galine; Gosselin, Michel; Lessard, Sylvie] Univ Quebec, Inst Sci Mer Rimouski, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada; [Poulin, Michel] Musee Canadien Nat, Rech & Collect, CP 3443,Succursale D, Ottawa, ON K1P 6P4, Canada; [Ardyna, Mathieu] Univ Laval, Takuvik Joint Int Lab, Quebec City, PQ, Canada; [Ardyna, Mathieu] CNRS, Paris, France; [Ardyna, Mathieu] Univ Laval, UMI3376, Dept Biol & Quebec Ocean, Quebec City, PQ G1V 0A6, Canada; [Ardyna, Mathieu] UPMC Univ Paris 06, Sorbonne Univ, INSU CNRS, Lab Oceanog Villefranche, 181 Chemin Lazaret, F-06230 Villefranche Sur Mer, France	University of Quebec; Laval University; Centre National de la Recherche Scientifique (CNRS); Laval University; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite	Simo-Matchim, AG (通讯作者)，Univ Quebec, Inst Sci Mer Rimouski, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	armellesimo@yahoo.fr	Gosselin, Michel/B-4477-2014; Ardyna, Mathieu/N-2027-2018	Gosselin, Michel/0000-0002-1044-0793; Ardyna, Mathieu/0000-0002-4703-6655	ArcticNet (Network of Centres of Excellence of Canada); Natural Sciences and Engineering Research Council of Canada (NSERC); Fonds de recherche du Quebec - Nature et technologies (FRQNT) through Quebec-Ocean; Canadian Museum of Nature; Institut des sciences de la mer de Rimouski (ISMER); Fondation de l'Universite du Quebec a Rimouski	ArcticNet (Network of Centres of Excellence of Canada); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds de recherche du Quebec - Nature et technologies (FRQNT) through Quebec-Ocean; Canadian Museum of Nature; Institut des sciences de la mer de Rimouski (ISMER); Fondation de l'Universite du Quebec a Rimouski	This project was supported by grants from ArcticNet (Network of Centres of Excellence of Canada) and the Natural Sciences and Engineering Research Council of Canada (NSERC). Partial funding was provided by the Fonds de recherche du Quebec - Nature et technologies (FRQNT) through Quebec-Ocean and by the Canadian Museum of Nature. A.G.S.M. received postgraduate scholar ships from the Institut des sciences de la mer de Rimouski (ISMER) and the Fondation de l'Universite du Quebec a Rimouski, and stipends from ArcticNet and Quebec-Ocean. We are thankful to the officers and crew of the CCGS 'Amundsen' for their invaluable support during expeditions. We are especially indebted to M. Blais, M. Simard, J. Ferland, J. Gara and T. Brown for sample collection and technical support; Y. Gratton and P. Guillot for providing and processing CTD data; J. E. Tremblay and J. Gagnon for providing the nutrient data; B. Else for data on CO<INF>2</INF> partial pressure; C. Jose for help during cell identification and enumeration; P. Archambault and M. Cusson for advice on statistical analysis; and 3 anonymous reviewers for their constructive comments. This is a contribution to the research programmes of ArcticNet, ISMER and QubecOcean.	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Ecol.-Prog. Ser.	MAY 31	2017	572						19	42		10.3354/meps12125	http://dx.doi.org/10.3354/meps12125			24	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	EX7RO		Bronze			2025-03-11	WOS:000403446100002
J	Dewaele, L; Amson, E; Lambert, O; Louwye, S				Dewaele, Leonard; Amson, Eli; Lambert, Olivier; Louwye, Stephen			Reappraisal of the extinct seal "<i>Phoca</i>" <i>vitulinoides</i> from the Neogene of the North Sea Basin, with bearing on its geological age, phylogenetic affinities, and locomotion	PEERJ			English	Article						Phocidae; Neogene; North Sea Basin; Belgium; Redescription; Taxonomy; Locomotion	MIDDLE MIOCENE; DINOFLAGELLATE CYST; BODY-SIZE; ATLANTIC REALM; SOUTH-AMERICA; CARNIVORA; PHOCIDAE; MAMMALIA; PINNIPEDS; STRATIGRAPHY	Background: Discovered on the southern margin of the North Sea Basin, "Phoca" vitulinoides represents one of the best-known extinct species of Phocidae. However, little attention has been given to the species ever since its original 19th century description. Newly discovered material, including the most complete specimen of fossil Phocidae from the North Sea Basin, prompted the redescription of the species. Also, the type material of "Phoca" vitulinoides is lost. Methods: "Phoca" vitulinoides is redescribed. Its phylogenetic position among Phocinae is assessed through phylogenetic analysis. Dinoflagellate cyst biostratigraphy is used to determine and reassess the geological age of the species. Myological descriptions of extant taxa are used to infer muscle attachments, and basic comparative anatomy of the gross morphology and biomechanics are applied to reconstruct locomotion. Results: Detailed redescription of "Phoca" vitulinoides indicates relatively little affinities with the genus Phoca, but rather asks for the establishment of a new genus: Nanophoca gen. nov. Hence, "Phoca" vitulinoides is recombined into Nanophoca vitulinoides. This reassignment is confirmed by the phylogenetic analysis, grouping the genus Nanophoca and other extinct phocine taxa as stem phocines. Biostratigraphy and lithostratigraphy expand the known stratigraphic range of N. vitulinoides from the late Langhian to the late Serravallian. The osteological anatomy of N. vitulinoides indicates a relatively strong development of muscles used for fore flipper propulsion and increased flexibility for the hind flipper. Discussion: The extended stratigraphic range of N. vitulinoides into the middle Miocene confirms relatively early diversification of Phocinae in the North Atlantic. Morphological features on the fore-and hindlimb of the species point toward an increased use of the fore flipper and greater flexibility of the hind flipper as compared to extant Phocinae, clearly indicating less derived locomotor strategies in this Miocene phocine species. Estimations of the overall body size indicate that N. vitulinoides is much smaller than Pusa, the smallest extant genus of Phocinae (and Phocidae), and than most extinct phocines.	[Dewaele, Leonard; Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium; [Dewaele, Leonard; Lambert, Olivier] Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Brussels, Belgium; [Amson, Eli] Humboldt Univ, Arbeitsgrp Morphol & Formengeschichte, Berlin, Germany; [Amson, Eli] Univ Zurich, Paldontol Inst & Museum, Zurich, Switzerland	Ghent University; Royal Belgian Institute of Natural Sciences; Humboldt University of Berlin; University of Zurich	Dewaele, L (通讯作者)，Univ Ghent, Dept Geol, Ghent, Belgium.; Dewaele, L (通讯作者)，Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Brussels, Belgium.	leonard.dewaele@ugent.be	Amson, Eli/I-4619-2019; Lambert, Olivier/AEN-2469-2022; Amson, Eli/M-3100-2013; Louwye, Stephen/D-3856-2012	Dewaele, Leonard/0000-0003-1188-2515; Amson, Eli/0000-0003-1474-9613; Lambert, Olivier/0000-0003-0740-5791; Louwye, Stephen/0000-0003-4814-4313	FWO Ph.D. Fellowship program; Swiss National Fund [SNF 31003A_149605]; Alexander von Humboldt Foundation	FWO Ph.D. Fellowship program(FWO); Swiss National Fund(Swiss National Science Foundation (SNSF)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation)	DL was financially supported through the FWO Ph.D. Fellowship program. EA was supported by the Swiss National Fund SNF 31003A_149605 granted to MR Sanchez-Villagra and subsequently by the Alexander von Humboldt Foundation. 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	Beleneva, IA; Skriptsova, AV; Svetashev, VI				Beleneva, I. A.; Skriptsova, A. V.; Svetashev, V. I.			Characterization of Biofilm-Forming Marine Bacteria and Their Effect on Attachment and Germination of Algal Spores	MICROBIOLOGY			English	Article						bacterial biofilms; antifouling activity; algal spores	ANTIFOULING ACTIVITY; MICROBIAL BIOFILMS; SP NOV.; ULVA; INHIBITION; SETTLEMENT; ZOOSPORES; IDENTIFICATION; SURFACE; MEMBER	In this work, 37 bacterial strains isolated from biofouling of marine organisms and from the Museum of Heterotrophic Bacteria of the National Scientific Center of Marine Biology were studied. The strains were identified based on their phenotypic characteristics and on the fatty acid composition of their cell wall lipids. Members of the genus Pseudoalteromonas prevailed both in associated microflora of two dinoflagellate clones and in the biofilms from marine hydrobionts. Associated microflora included also members of the CFB cluster, Bacillus, Sulfitobacter, Acinetobacter, Shewanella, and Psychrobacter. A considerable portion of strains (48.6%) exhibited antimicrobial activity. Antifouling activity against algal spores was studied using single-species bacterial biofilms and the spores of Ulva lactuca. Undaria pinnatifida, the algae most common in the Sea of Japan. Strong inhibitory effect on attachment of Ulva and Undaria spores was observed for 75 and 51% of the strains, respectively. Attached spores were, however, less sensitive to the inhibitory action of biofilms. Species specificity of algal response to bacteria was shown, with a strain having different effect on the spores of different algal species. Biotechnologically promising strains were determined, which exhibited high activity against the spores of macroalgae and could probably be used as producers of antifouling substances and as components of antifouling coatings. No relation was found between antifouling activity of bacteria and the source of their isolation. Our results indicate wide occurrence of bacteria with antifouling activity among associated microflora of marine hydrobionts and demonstrate the extent of complexity and diversity of relations between bacterial biofilms and algal spores.	[Beleneva, I. A.; Skriptsova, A. V.; Svetashev, V. I.] Russian Acad Sci, Far Eastern Branch, Natl Sci Ctr Marine Biol, Vladivostok, Russia	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Beleneva, IA (通讯作者)，Russian Acad Sci, Far Eastern Branch, Natl Sci Ctr Marine Biol, Vladivostok, Russia.	beleneva.vl@mail.ru	Svetashev, Vasily/K-3614-2016; Beleneva, Irina/AAR-8091-2021; Skriptsova, Anna/S-7365-2016	Skriptsova, Anna/0000-0001-5943-4522	Far Eastern Branch, Russian Academy of Sciences [15-I-6-059, A16-116101110096-3]	Far Eastern Branch, Russian Academy of Sciences(Russian Academy of Sciences)	This work was partly supported by the Far Eastern Branch, Russian Academy of Sciences (grant no. 15-I-6-059 and grant with registration no. A16-116101110096-3).	Alekseevna BI, 2013, JUNDISHAPUR J MICROB, V6, P166, DOI 10.5812/jjm.5039; Beleneva IA, 2014, MICROBIOLOGY+, V83, P220, DOI 10.1134/S0026261714030059; Beleneva IA, 2005, MICROBIOLOGY+, V74, P579, DOI 10.1007/s11021-005-0106-8; Bernbom N, 2011, APPL ENVIRON MICROB, V77, P8557, DOI 10.1128/AEM.06038-11; Bowman JP, 1997, SYST APPL MICROBIOL, V20, P209, DOI 10.1016/S0723-2020(97)80067-7; DILLON PS, 1989, MICROB ECOL, V17, P39, DOI 10.1007/BF02025592; Dobretsov S, 2006, BIOFOULING, V22, P43, DOI 10.1080/08927010500504784; Dobretsov S, 2013, BIOFOULING, V29, P423, DOI 10.1080/08927014.2013.776042; Egan S, 2002, APPL ENVIRON MICROB, V68, P372, DOI 10.1128/AEM.68.1.372-378.2002; Egan S, 2001, INT J SYST EVOL MICR, V51, P1499, DOI 10.1099/00207713-51-4-1499; Egan S, 2000, ENVIRON MICROBIOL, V2, P343, DOI 10.1046/j.1462-2920.2000.00107.x; FAUTZ E, 1979, J BACTERIOL, V140, P852, DOI 10.1128/JB.140.3.852-858.1979; Fenical William, 1993, Marine Biotechnology, V1, P419; Huang YL, 2008, AQUAT MICROB ECOL, V52, P185, DOI 10.3354/ame01215; Huang YL, 2011, BIOFOULING, V27, P287, DOI 10.1080/08927014.2011.562978; Ivanova EP, 2000, CURR MICROBIOL, V41, P341, DOI 10.1007/s002840010146; KAMPFER P, 1993, MED MICROBIOL LETT, V2, P394; Lee OO, 2006, INT J SYST EVOL MICR, V56, P2871, DOI 10.1099/ijs.0.64562-0; Li D, 2014, PLOS ONE, V9, DOI 10.1371/journal.pone.0091201; Long RA, 2001, APPL ENVIRON MICROB, V67, P4975, DOI 10.1128/AEM.67.11.4975-4983.2001; Lovejoy C, 1998, APPL ENVIRON MICROB, V64, P2806; Ma Yuexin, 2009, Acta Ecologica Sinica, V29, P222; MAKI JS, 1988, MAR BIOL, V97, P199, DOI 10.1007/BF00391303; Mieszkin S, 2013, BIOFOULING, V29, P1097, DOI 10.1080/08927014.2013.828712; Patel P, 2003, ENVIRON MICROBIOL, V5, P338, DOI 10.1046/j.1462-2920.2003.00407.x; Pukall R, 1999, INT J SYST BACTERIOL, V49, P513, DOI 10.1099/00207713-49-2-513; Qian PY, 2007, MAR BIOTECHNOL, V9, P399, DOI 10.1007/s10126-007-9001-9; Rao D, 2007, APPL ENVIRON MICROB, V73, P7844, DOI 10.1128/AEM.01543-07; SZEWZYK U, 1991, MAR ECOL PROG SER, V75, P259, DOI 10.3354/meps075259; Tait K, 2005, ENVIRON MICROBIOL, V7, P229, DOI 10.1111/j.1462-2920.2004.00706.x; Yang L, 2008, WOODHEAD PUBL MATER, P1; Yebra DM, 2006, BIOFOULING, V22, P33, DOI 10.1080/08927010500519097	32	3	3	2	51	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0026-2617	1608-3237		MICROBIOLOGY+	Microbiology	MAY	2017	86	3					317	329		10.1134/S0026261717030031	http://dx.doi.org/10.1134/S0026261717030031			13	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	EW9IB					2025-03-11	WOS:000402830500003
J	Pienkowski, AJ; Gill, NK; Furze, MFA; Mugo, SM; Marret, F; Perreaux, A				Pienkowski, Anna J.; Gill, Navpreet K.; Furze, Mark F. A.; Mugo, Samuel M.; Marret, Fabienne; Perreaux, Abbey			Arctic sea-ice proxies: Comparisons between biogeochemical and micropalaeontological reconstructions in a sediment archive from Arctic Canada	HOLOCENE			English	Article						biogenic silica; biomarkers; dinoflagellate cysts; IP25; modern analogue technique; PIP25	DINOFLAGELLATE CYSTS; BEAUFORT SHELF; SOUTHERN-OCEAN; BIOGENIC OPAL; FRAM STRAIT; FRESH-WATER; BIOMARKER; VARIABILITY; DIATOMS; FORAMINIFERA	Boxcore 99LSSL-001 from the southwest Canadian Arctic Archipelago (68.095 degrees N, 114.186 degrees W), studied by multiproxy approaches (sea-ice diatom biomarker IP25, phytoplankton-based biomarker brassicasterol, biogenic silica, total organic carbon, dinoflagellate cysts = dinocysts, diatoms) and their applications (sea-ice index PBIP25, modern analogue technique (MAT) transfer functions), provides a chronologically constrained (Pb-210, Cs-137, two C-14 dates) palaeoenvironmental archive spanning AD 1625-1999 with which to compare and evaluate proxies frequently used in sea-ice reconstructions. Whereas diatoms are rare, PBIP25, biogenic silica and qualitative dinocyst approaches show good agreement, suggesting that palaeo sea-ice histories based on biomarker and microfossil techniques are robust in this region. These combined approaches show fluctuating long open water to marginal ice zone conditions (AD 1625-1740), followed by high-amplitude oscillations between long open water and extended spring/summer sea ice (AD 1740-1870). Greater ice cover (AD 1870-1970) precedes recent reductions in seasonal sea ice (AD 1970-1999). Dinocyst-based MAT, however, produces a low-amplitude signal lacking the nuances of other proxies, with most probable sea-ice reconstructions poorly correlating with biomarker-based histories. Explanations for this disagreement may include limited spatial coverage in the modern dinocyst distribution database for MAT and the broad environmental tolerances of polar dinocysts. Overall, PBIP25 provides the most detailed palaeo sea-ice signal, although its use in a shallow polar archipelago downcore setting poses methodological challenges. This proxy comparison demonstrates the limitations of palaeo sea-ice reconstructions and emphasizes the need for calibration studies tying modern microfossil and biogeochemical proxies to directly measured oceanographic parameters, as a springboard for robust quantitative palaeo studies.	[Pienkowski, Anna J.; Gill, Navpreet K.; Furze, Mark F. A.; Mugo, Samuel M.; Perreaux, Abbey] MacEwan Univ, Dept Phys Sci, 10700 104th Ave, Edmonton, AB T5J 4S2, Canada; [Pienkowski, Anna J.] Bangor Univ, Sch Ocean Sci, Coll Nat Sci, Bangor, Gwynedd, Wales; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool, Merseyside, England	Bangor University; University of Liverpool	Pienkowski, AJ (通讯作者)，MacEwan Univ, Dept Phys Sci, 10700 104th Ave, Edmonton, AB T5J 4S2, Canada.	PienkowskiA@macewan.ca	Pieńkowski, Anna/AAL-1312-2020; Mugo, Samuel/J-2753-2013; Pienkowski, Anna/J-9339-2013	Marret-Davies, Fabienne/0000-0003-4244-0437; Mugo, Samuel/0000-0002-0015-1947; Furze, Mark/0000-0003-4636-6182; Pienkowski, Anna/0000-0002-3606-7130	Marie Curie Career Integration Grant [FP7-PEOPLE-2011-CIG 304178]; MacEwan University Undergraduate Student Research Initiative Fund	Marie Curie Career Integration Grant(Marie Curie Actions); MacEwan University Undergraduate Student Research Initiative Fund	This research was made possible by a Marie Curie Career Integration Grant awarded to A Pienkowski (FP7-PEOPLE-2011-CIG 304178 The Quaternary Environmental Evolution of the Northwest- Passage). We acknowledge the receipt of a MacEwan University Undergraduate Student Research Initiative Fund awarded to N. Gill. This paper is a contribution to the ArcticNet Phase IV project 'Mapping of Arctic Canada's Seafloor: Contributions to Global Change Science, Sustainable Resource Development, Safe Navigation of the Northwest Passage, Geohazards and Arctic Sovereignty'.	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J	Lundholm, N; Ribeiro, S; Godhe, A; Nielsen, LR; Ellegaard, M				Lundholm, Nina; Ribeiro, Sofia; Godhe, Anna; Nielsen, Lene Rostgaard; Ellegaard, Marianne			Exploring the impact of multidecadal environmental changes on the population genetic structure of a marine primary producer	ECOLOGY AND EVOLUTION			English	Article						dinoflagellate; environmental change; microsatellites; phytoplankton resting stage; population genetic structure; sediment core	DIATOM DITYLUM-BRIGHTWELLII; DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; NITZSCHIA-PUNGENS BACILLARIOPHYCEAE; PLANKTONIC DIATOM; PSEUDO-NITZSCHIA; COASTAL WATERS; SPRING-BLOOM; KOLJO-FJORD; NORTH-SEA; MICROSATELLITE MARKERS	Many marine protists form resting stages that can remain viable in coastal sediments for several decades. Their long-term survival offers the possibility to explore the impact of changes in environmental conditions on population dynamics over multidecadal time scales. Resting stages of the phototrophic dinoflagellate Pentapharsodinium dalei were isolated and germinated from five layers in dated sediment cores from Koljo fjord, Sweden, spanning ca. 1910-2006. This fjord has, during the last century, experienced environmental fluctuations linked to hydrographic variability mainly driven by the North Atlantic Oscillation. Population genetic analyses based on six microsatellite markers revealed high genetic diversity and suggested that samples belonged to two clusters of subpopulations that have persisted for nearly a century. We observed sub-population shifts coinciding with changes in hydrographic conditions. The large degree of genetic diversity and the potential for both fluctuation and recovery over longer time scales documented here, may help to explain the long-term success of aquatic protists that form resting stages.	[Lundholm, Nina] Univ Copenhagen, Nat Hist Museum Denmark, Solvgade 83, DK-1307 Copenhagen K, Denmark; [Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Glaciol & Climate Dept, Copenhagen K, Denmark; [Godhe, Anna] Univ Gothenburg, Dept Marine Sci, Gothenburg, Sweden; [Nielsen, Lene Rostgaard] Univ Copenhagen, Dept Geosci & Nat Resource Management, Frederiksberg, Denmark; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Frederiksberg, Denmark	University of Copenhagen; Geological Survey Of Denmark & Greenland; University of Gothenburg; University of Copenhagen; University of Copenhagen	Lundholm, N (通讯作者)，Univ Copenhagen, Nat Hist Museum Denmark, Solvgade 83, DK-1307 Copenhagen K, Denmark.	nlundholm@snm.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Lundholm, Nina/AAY-6249-2020; Ribeiro, Sofia/G-9213-2018; Nielsen, Lene/E-6769-2015; Ellegaard, Marianne/H-6748-2014; Lundholm, Nina/A-4856-2013	Ribeiro, Sofia/0000-0003-0672-9161; Nielsen, Lene/0000-0002-7214-8691; Ellegaard, Marianne/0000-0002-6032-3376; 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Evol.	MAY	2017	7	9					3132	3142		10.1002/ece3.2906	http://dx.doi.org/10.1002/ece3.2906			11	Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Evolutionary Biology	EW5LZ	28480012	Green Published, gold			2025-03-11	WOS:000402548900025
J	Lee, B; Park, MG				Lee, Bora; Park, Myung Gil			Different life cycle strategies of the dinoflagellates <i>Fragilidium duplocampanaeforme</i> and its prey <i>Dinophysis acuminata</i> may explain their different susceptibilities to the infection by the parasite <i>Parvilucifera infectans</i>	HARMFUL ALGAE			English	Article						Dinoflagellate; Defense mechanism; Parasite; Cyst formation; Food web dynamics	CILIATE MESODINIUM-RUBRUM; GYMNODINIUM-CATENATUM; CYST FORMATION; MARINE; TEMPERATURE; SPECIFICITY; DARKNESS; GROWTH	Some marine dinoflagellates form ecdysal cyst (=temporary cysts) as part of their life cycle or under unfavorable growth conditions. Whether the dinoflagellates form ecdysal cysts or not may influence susceptibility to parasitism. In this study, parasite prevalence relative to inoculum size of the parasitoid Parvilucifera infectans zoospores for two dinoflagellate hosts (i.e., Fragilidium duplocampanaeforme and Dinophysis acuminate), which have different life cycle strategies, was examined. Further, susceptibility of cysts to parasitism, encystment signal, duration of encystments, and effects of induced encystment on diel periodicity, using ecdysal cyst-forming F. duplocampanaeforme were explored. The percent hosts infected by P. infectans plotted as a function of inoculum size showed a sharp increase to a maximum in D. acuminata, but a gradual linear rise in F. duplocampanaeforme: while the parasite prevalence in D. acuminata increased to a maximum of 78.8 (+/- 2.4%) by a zoospore:host ratio of 20:1, it in F duplocampanaeforme only reached 8.9 (+/- 0.3%), even at a zoospore:host ratio of 120:1. In F duplocampanaeforme, infections were observed only in the vegetative cells and not observed in ecdysal cysts. When exposed to live, frozen, and sonicated zoospores and zoospore filtrate, F duplocampanaeforme formed ecdysal cysts only when exposed to live zoospores, suggesting that temporary cyst formation in the dinoflagellate resulted from direct contact with zoospores. When the Parvilucifera zoospores attacked and struggled to penetrate F duplocampanaeforme through its flagellar pore, the Fragilidium cell shed all thecal plates, forming a 'thecal cloud layer', in which the zoospores were caught and immobilized and thus could not penetrate anymore. The duration (35 +/- 1.8 h) of ecdysal cysts cysts (i.e., without addition of zoospores), thereby resulting in delayed growth as well as influencing the pattern of diel periodicity. The results from this study suggest that in addition to the classical predator prey interaction and allelopathic interaction, parasitism and its accompanying defense can make the food web dynamics much more complicated than previously thought. (C) 2017 Elsevier B.V. All rights reserved.	[Lee, Bora; Park, Myung Gil] Chonnam Natl Univ, Dept Oceanog, LOHABE, Gwangju 61186, South Korea	Chonnam National University	Park, MG (通讯作者)，Chonnam Natl Univ, Dept Oceanog, LOHABE, Gwangju 61186, South Korea.	mpark@chonnam.ac.kr			National Research Foundation of Korea [NRF-2016R1A6A1A03012647]; KIMST/MOF	National Research Foundation of Korea(National Research Foundation of Korea); KIMST/MOF(Korea Institute of Marine Science & Technology Promotion (KIMST)Ministry of Oceans & Fisheries (MOF), Republic of Korea)	The authors would like to thank D. Wayne Coats for valuable comments during the work. This work was supported by research grant funded by the National Research Foundation of Korea (NRF-2016R1A6A1A03012647) and a program entitled "Management of marine organisms causing ecological disturbance and harmful effects" funded by KIMST/MOF.[CG]	Alacid E, 2016, FRONT MICROBIOL, V7, DOI 10.3389/fmicb.2016.00769; Amorim A, 2013, MICROPALEAEONTOLOGIC, P223; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; 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; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; Bravo Isabel, 2014, Microorganisms, V2, P11; Chambouvet A, 2011, PROTIST, V162, P637, DOI 10.1016/j.protis.2010.12.001; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Garcés E, 2013, PROTIST, V164, P245, DOI 10.1016/j.protis.2012.11.004; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Guillard RRL., 1975, CULTURE MARINE INVER, P29, DOI [10.1007/978-1-4615-8714-93, DOI 10.1007/978-1-4615-8714-93, 10.1007/978-1-4615-8714-9_3]; Gustafson DE, 2000, NATURE, V405, P1049, DOI 10.1038/35016570; Johnson MD, 2005, AQUAT MICROB ECOL, V39, P303, DOI 10.3354/ame039303; Lundgren V, 2011, AQUAT MICROB ECOL, V63, P231, DOI 10.3354/ame01497; Nézan E, 2009, EUR J PROTISTOL, V45, P2, DOI 10.1016/j.ejop.2008.04.002; Norén F, 1999, EUR J PROTISTOL, V35, P233, DOI 10.1016/S0932-4739(99)80001-7; OWEN KC, 1985, J COASTAL RES, V1, P263; Park MG, 2004, J EUKARYOT MICROBIOL, V51, P145, DOI 10.1111/j.1550-7408.2004.tb00539.x; Park MG, 2006, AQUAT MICROB ECOL, V45, P101, DOI 10.3354/ame045101; Park MG, 2015, HARMFUL ALGAE, V43, P20, DOI 10.1016/j.hal.2015.02.001; Park MG, 2013, HARMFUL ALGAE, V30, pS62, DOI 10.1016/j.hal.2013.10.007; Park MG, 2010, J PHYCOL, V46, P424, DOI 10.1111/j.1529-8817.2010.00824.x; Rodríguez F, 2014, AQUAT MICROB ECOL, V72, P241, DOI 10.3354/ame01700; Smith M, 2007, MAR ECOL PROG SER, V338, P61, DOI 10.3354/meps338061; Toth GB, 2004, P ROY SOC B-BIOL SCI, V271, P733, DOI 10.1098/rspb.2003.2654; Yih W, 2004, AQUAT MICROB ECOL, V36, P165, DOI 10.3354/ame036165	28	8	8	1	30	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	MAY	2017	65						1	8		10.1016/j.hal.2017.04.002	http://dx.doi.org/10.1016/j.hal.2017.04.002			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	EW4AS	28526115				2025-03-11	WOS:000402445000001
J	Woelders, L; Vellekoop, J; Kroon, D; Smit, J; Casadío, S; Prámparo, MB; Dinarès-Turell, J; Peterse, F; Sluijs, A; Lenaerts, JTM; Speijer, RP				Woelders, L.; Vellekoop, J.; Kroon, D.; Smit, J.; Casadio, S.; Pramparo, M. B.; Dinares-Turell, J.; Peterse, F.; Sluijs, A.; Lenaerts, J. T. M.; Speijer, R. P.			Latest Cretaceous climatic and environmental change in the South Atlantic region	PALEOCEANOGRAPHY			English	Article						Maastrichtian; paleoclimate; paleoenvironment; South Atlantic; TEX86; oxygen isotopes	DINOFLAGELLATE CYSTS; BENTHIC FORAMINIFERA; ASTRONOMICAL CALIBRATION; SEQUENCE STRATIGRAPHY; TETRAETHER LIPIDS; CHICXULUB IMPACT; DECCAN VOLCANISM; MEMBRANE-LIPIDS; MASS EXTINCTION; NEUQUEN BASIN	Latest Maastrichtian climate change caused by Deccan volcanism has been invoked as a cause of mass extinction at the Cretaceous-Paleogene (K-Pg) boundary (66.0Ma). Yet late Maastrichtian climate and ecological changes are poorly documented, in particular on the Southern Hemisphere. Here we present upper Maastrichtian-lower Danian climate and biotic records from the Bajada del Jaguel (BJ) shelf site (Neuquen Basin, Argentina), employing the TEX86 paleothermometer, marine palynology (dinoflagellate cysts), and micropaleontology (foraminifera). These records are correlated to the astronomically tuned Ocean Drilling Program Site 1262 (Walvis Ridge). Collectively, we use these records to assess climatic and ecological effects of Deccan volcanism in the Southern Atlantic region. Both the TEX86-based sea surface temperature (SST) record at BJ and the bulk carbonate O-18-based SST record of Site 1262 show a latest Maastrichtian warming of 2.5-4 degrees C, at 450 to 150kyr before the K-Pg boundary, coinciding with the a large Deccan outpouring phase. Benthic foraminiferal and dinocyst assemblage changes indicate that this warming resulted in enhanced runoff and stratification of the water column, likely resulting from more humid climate conditions in the Neuquen Basin. These climate conditions could have been caused by an expanding and strengthening thermal low over the South American continent. Biotic changes in response to late Maastrichtian environmental changes are rather limited, when compared to the major turnovers observed at many K-Pg boundary sites worldwide. This suggests that environmental perturbations during the latest Maastrichtian warming event were less severe than those following the K-Pg boundary impact.	[Woelders, L.; Vellekoop, J.; Speijer, R. P.] Katholieke Univ Leuven, Dept Earth & Environm Sci, Leuven, Belgium; [Kroon, D.] Univ Edinburgh, Grant Inst, Sch GeoSci, Edinburgh, Midlothian, Scotland; [Smit, J.] Vrije Univ Amsterdam, Event Stratig, Amsterdam, Netherlands; [Casadio, S.] Univ Nacl Rio Negro, CONICET, General Roca, Argentina; [Pramparo, M. B.] IANIGLA CCT CONICET, Mendoza, Argentina; [Dinares-Turell, J.] Ist Nazl Geofis & Vulcanol, Rome, Italy; [Peterse, F.; Sluijs, A.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands; [Lenaerts, J. T. M.] Univ Utrecht, Inst Marine & Atmospher Res, Utrecht, Netherlands	KU Leuven; University of Edinburgh; Vrije Universiteit Amsterdam; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University Nacional Cuyo Mendoza; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Istituto Nazionale Geofisica e Vulcanologia (INGV); Utrecht University; Utrecht University	Woelders, L (通讯作者)，Katholieke Univ Leuven, Dept Earth & Environm Sci, Leuven, Belgium.	lineke.woelders@gmail.com	Speijer, Robert/H-5073-2016; Peterse, Francien/AAY-1473-2021; Vellekoop, Johan/L-1805-2019; Lenaerts, Jan/D-9423-2012; Dinares-Turell, Jaume/G-2852-2011; Vellekoop, Johan/F-6466-2017; Peterse, Francien/H-5627-2011; Sluijs, Appy/B-3726-2009	Lenaerts, Jan/0000-0003-4309-4011; Speijer, Robert/0000-0002-5873-7203; Dinares-Turell, Jaume/0000-0002-5546-2291; Vellekoop, Johan/0000-0001-6977-693X; Smit, Jan/0000-0002-6070-4865; Peterse, Francien/0000-0001-8781-2826; Woelders, Lineke/0000-0002-7091-2131; PRAMPARO, MERCEDES B./0000-0002-3955-8496; Sluijs, Appy/0000-0003-2382-0215	Research Foundation Flanders (FWO) [G.0B85.13]; Ministry of Education, Culture and Science (OCW); NWO [834.11.006]	Research Foundation Flanders (FWO)(FWO); Ministry of Education, Culture and Science (OCW)(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)); NWO(Netherlands Organization for Scientific Research (NWO))	Supporting data, texts, and figures are included in SI files; any additional data may be obtained from L.W. (e-mail: lineke.woelders@gmail.com). Data already published in literature are properly cited and referred to in the reference list. Samples and data provided by the Ocean Drilling Program (ODP) and International Ocean Discovery Program (IODP) were used. Universidad Nacional de Rio Negro and CONICET partially funded the field work at the BJ site. Funding to this project was provided by the Research Foundation Flanders (FWO) to R.P.S. (G.0B85.13). This work was also carried out within the theme of the Netherlands Earth System Science Centre (NESSC), financially supported by the Ministry of Education, Culture and Science (OCW). NWO grant 834.11.006 enabled the purchase of the UHPLC-MS system used for GDGT analyses at UU. Gert-Jan Reichart and two anonymous reviewers are thanked for their valuable comments. L. Woelders and J. Vellekoop contributed equally to the research and are both considered first authors.	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J	Jaramillo, C; Romero, I; D'Apolito, C; Bayona, G; Duarte, E; Louwye, S; Escobar, J; Luque, J; Carrillo-Briceño, JD; Zapata, V; Mora, A; Schouten, S; Zavada, M; Harrington, G; Ortiz, J; Wesselingh, FP				Jaramillo, Carlos; Romero, Ingrid; D'Apolito, Carlos; Bayona, German; Duarte, Edward; Louwye, Stephen; Escobar, Jaime; Luque, Javier; Carrillo-Briceno, Jorge D.; Zapata, Vladimir; Mora, Alejandro; Schouten, Stefan; Zavada, Michael; Harrington, Guy; Ortiz, John; Wesselingh, Frank P.			Miocene flooding events of western Amazonia	SCIENCE ADVANCES			English	Article							LLANOS FORELAND BASIN; EASTERN CORDILLERA; SOLIMOES FORMATION; MARINE INCURSION; MIDDLE MIOCENE; SEDIMENTARY ENVIRONMENTS; NORTHWESTERN AMAZONIA; SOUTHWESTERN AMAZONIA; DINOFLAGELLATE CYSTS; SOUTH-AMERICA	There is a considerable controversy about whether western Amazonia was ever covered by marine waters during the Miocene [23 to 5 Ma (million years ago)]. We investigated the possible occurrence of Miocene marine incursions in the Llanos and Amazonas/Solimoes basins, using sedimentological and palynological data fromtwo sediment cores taken in eastern Colombia and northwestern Brazil together with seismic information. We observed two distinctmarine intervals in the Llanos Basin, an early Miocene that lasted similar to 0.9My (million years) (18.1 to 17.2 Ma) and amiddleMiocene that lasted similar to 3.7 My (16.1 to 12.4Ma). These twomarine intervals are also seen in Amazonas/Solimoes Basin (northwestern Amazonia) but were much shorter in duration, similar to 0.2 My (18.0 to 17.8 Ma) and similar to 0.4 My (14.1 to 13.7 Ma), respectively. Our results indicate that shallow marine waters covered the region at least twice during the Miocene, but the events were shortlived, rather than a continuous full- marine occupancy of Amazonian landscape over millions of years.	[Jaramillo, Carlos; Romero, Ingrid; D'Apolito, Carlos; Ortiz, John] Smithsonian Trop Res Inst, Box 0843-03092, Balboa, Ancon, Panama; [Romero, Ingrid] Univ Illinois, Urbana, IL 61801 USA; [Romero, Ingrid; D'Apolito, Carlos; Bayona, German; Duarte, Edward] Corp Geol Ares, Calle 44A 53-96, Bogota, Colombia; [D'Apolito, Carlos; Harrington, Guy] Univ Birmingham, Birmingham, W Midlands, England; [Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium; [Escobar, Jaime] Univ Norte, Barranquilla, Colombia; [Luque, Javier] Univ Alberta, Dept Biol Sci, Edmonton, AB T6G 2E9, Canada; [Carrillo-Briceno, Jorge D.] Univ Zurich, Paleontol Inst & Museum, Karl Schmid Str 4, CH-8006 Zurich, Switzerland; [Zapata, Vladimir] Ecopetrol SA, Bogota, Colombia; [Mora, Alejandro] Hocol SA, Bogota, Colombia; [Schouten, Stefan] Univ Utrecht, Dept Marine Microbiol & Biogeochem, Royal Netherlands Inst Sea Res, POB 59, NL-1790 AB Den Burg, Texel, Netherlands; [Zavada, Michael] Univ Texas Permian Basin, Odessa, TX 79762 USA; [Wesselingh, Frank P.] Naturalis Biodivers Ctr, POB 9517,Darwinweg 2, NL-2300 RA Leiden, Netherlands	Smithsonian Institution; Smithsonian Tropical Research Institute; University of Illinois System; University of Illinois Urbana-Champaign; University of Birmingham; Ghent University; Universidad del Norte Colombia; University of Alberta; University of Zurich; Ecopetrol; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Texas System; Naturalis Biodiversity Center	Jaramillo, C (通讯作者)，Smithsonian Trop Res Inst, Box 0843-03092, Balboa, Ancon, Panama.	jaramilloc@si.edu	Schouten, Stefan/P-4380-2016; Romero, Ingrid/IUQ-7921-2023; Mora, Alejandro/LWH-7441-2024; Escobar, Jaime/HSE-4459-2023; Wesselingh, Frank/C-1367-2018; D'Apolito, Carlos/O-5496-2018; Louwye, Stephen/D-3856-2012	Luque, Javier/0000-0002-4391-5951; Romero, Ingrid C./0000-0003-1376-5830; Duarte, Edward/0000-0001-8788-909X; bayona, german/0000-0003-3860-5438; Wesselingh, Frank/0000-0003-3655-0701; jaramillo, carlos/0000-0002-2616-5079; Escobar, Jaime/0000-0001-7775-7130; Mora Bohorquez, Josue Alejandro/0000-0003-3667-3912; D'Apolito, Carlos/0000-0003-1602-0201; Louwye, Stephen/0000-0003-4814-4313	Smithsonian Institution; Anders Foundation; NSF Division of Earth Sciences [0957679]; Colciencias Jovenes Investigadores; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (Brazil) [BEX 0376/12-4]; "Plan de Fortalecimiento Institucional" Ares-Colciencias [COL0008512]; Palynological Society (United States); Division Of Earth Sciences; Directorate For Geosciences [0957679] Funding Source: National Science Foundation	Smithsonian Institution(Smithsonian Institution); Anders Foundation; NSF Division of Earth Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO)); Colciencias Jovenes Investigadores; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); "Plan de Fortalecimiento Institucional" Ares-Colciencias; Palynological Society (United States); Division Of Earth Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This study was supported by the Smithsonian Institution, Anders Foundation, NSF Division of Earth Sciences (grant 0957679), and Colciencias Jovenes Investigadores. 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Adv.	MAY	2017	3	5							e1601693	10.1126/sciadv.1601693	http://dx.doi.org/10.1126/sciadv.1601693			11	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	EV7KW	28508052	Green Published, Green Submitted, gold			2025-03-11	WOS:000401955300002
J	Gao, YC; Fang, HD; Dong, YH; Li, HT; Pu, CL; Zhan, AB				Gao, Yangchun; Fang, Hongda; Dong, Yanhong; Li, Haitao; Pu, Chuanliang; Zhan, Aibin			An improved method for the molecular identification of single dinoflagellate cysts	PEERJ			English	Article						Dinoflagellate cysts; Harmful algae; Ultrasonic cleaning; PCR inhibitor; Micropipette cleaning	RED-TIDE; COCHLODINIUM-POLYKRIKOIDES; RESTING CYSTS; GYMNODINIUM-CATENATUM; ALEXANDRIUM; DINOPHYCEAE; DIVERSITY; SEDIMENTS; TOXICITY; DYNAMICS	Background Dinoflagellate cysts (i.e., dinocysts) are biologically and ecologically important as they, can help dinoflagellate species survive harsh environments, facilitate their dispersal and serve as seeds for harmful algal blooms. In addition, dinocysts derived from some species can produce more toxins than vegetative forms, largely affecting species through their food webs and even human health. Consequently, accurate identification of dinocysts represents the first crucial step in many ecological studies. As dinocysts have limited or even no available taxonomic keys, molecular methods have become the first priority for dinocyst identification. However, molecular identification of dinocysts, particularly when using single cells, poses technical challenges. The most serious is the low success rate of PCR, especially for heterotrophic species. Methods. In this study, we aim to improve the success rate of single dinocyst identification for the chosen dinocyst species (Gonyaulax spinifera, Polykrikos kofoidii, Lingulodinium polyedrum, Pyrophacus steinii, Protoperidinium leonis and Protoperidinium oblongum) distributed in the South China Sea. We worked on two major technical issues: cleaning possible PCR inhibitors attached on the cyst surface and designing new dinoflagellate-specific PCR primers to improve the success of PCR amplification. Results. For the cleaning of single dinocysts separated from marine sediments, we used ultrasonic wave-based cleaning and optimized cleaning parameters. Our results showed that the optimized ultrasonic wave-based cleaning method largely improved the identification success rate and accuracy of both molecular and morphological identifications. For the molecular identification with the newly designed dinoflagellate-specific primers (185634F-18S634R), the success ratio was as high as 86.7% for single dinocysts across multiple taxa when using the optimized ultrasonic wave-based cleaning method, and much higher than that (16.7%) based on traditional micropipette-based cleaning. Discussion. The technically simple but robust method improved on in this study is expected to serve as a powerful tool in deep understanding of population dynamics of dinocysts and the causes and consequences of potential negative effects caused by dinocysts.	[Gao, Yangchun; Pu, Chuanliang; Zhan, Aibin] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, Beijing, Peoples R China; [Gao, Yangchun; Pu, Chuanliang; Zhan, Aibin] Univ Chinese Acad Sci, Chinese Acad Sci, Beijing, Peoples R China; [Fang, Hongda; Dong, Yanhong; Li, Haitao] State Ocean Adm, South China Sea Environm Monitoring Ctr, Guangzhou, Guangdong, Peoples R China	Chinese Academy of Sciences; Research Center for Eco-Environmental Sciences (RCEES); Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Zhan, AB (通讯作者)，Chinese Acad Sci, Res Ctr Ecoenvironm Sci, Beijing, Peoples R China.; Zhan, AB (通讯作者)，Univ Chinese Acad Sci, Chinese Acad Sci, Beijing, Peoples R China.	azhan@rcees.ac.cn	高, 养春/ITT-9176-2023; Zhan, Aibin/A-7240-2011		100-Talent Program of the Chinese Academy of Sciences; National Marine Public Welfare Research Program [201305010]	100-Talent Program of the Chinese Academy of Sciences(Chinese Academy of Sciences); National Marine Public Welfare Research Program	This work was supported by the 100-Talent Program of the Chinese Academy of Sciences to AZ, and by the National Marine Public Welfare Research Program (201305010). 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	Bolch, CJS; Bejoy, TA; Green, DH				Bolch, Christopher J. S.; Bejoy, Thaila A.; Green, David H.			Bacterial Associates Modify Growth Dynamics of the Dinoflagellate <i>Gymnodinium catenatum</i>	FRONTIERS IN MICROBIOLOGY			English	Article						dinoflagellate; bacteria; interaction; model; Gymnodinium catenatum; growth	CHLOROPHYLL-A FLUORESCENCE; MARINE-BACTERIA; CYST FORMATION; CELL-DEATH; SP-NOV.; PHYTOPLANKTON; DIVERSITY; COMMUNITY; DIATOMS; ALGAE	Marine phytoplankton cells grow in close association with a complex microbial associate community known to affect the growth, behavior, and physiology of the algal host. The relative scale and importance these effects compared to other major factors governing algal cell growth remain unclear. Using algal-bacteria co-culture models based on the toxic dinoflagellate Gymnodinium catenatum, we tested the hypothesis that associate bacteria exert an independent effect on host algal cell growth. Batch co-cultures of G. catenatum were grown under identical environmental conditions with simplified bacterial communities composed of one-, two-, or three-bacterial associates. Modification of the associate community membership and complexity induced up to four-fold changes in dinoflagellate growth rate, equivalent to the effect of a 5 ffi C change in temperature or an almost six-fold change in light intensity (20-115 moles photons PAR m(-2) s(-1)). Almost three-fold changes in both stationary phase cell concentration and death rate were also observed. Co-culture with Roseobacter sp. DG874 reduced dinoflagellate exponential growth rate and led to a more rapid death rate compared with mixed associate community controls or co-culture with either Marinobacter sp. DG879, Alcanivorax sp. DG881. In contrast, associate bacteria concentration was positively correlated with dinoflagellate cell concentration during the exponential growth phase, indicating growth was limited by supply of dinoflagellate-derived carbon. Bacterial growth increased rapidly at the onset of declining and stationary phases due to either increasing availability of algal-derived carbon induced by nutrient stress and autolysis, or at mid-log phase in Roseobacter co-cultures potentially due to the onset of bacterial-mediated cell lysis. Co-cultures with the three bacterial associates resulted in dinoflagellate and bacterial growth dynamics very similar to more complex mixed bacterial community controls, suggesting that three-way co-cultures are sufficient to model interaction and growth dynamics of more complex communities. This study demonstrates that algal associate bacteria independently modify the growth of the host cell under non-limiting growth conditions and supports the concept that algal-bacterial interactions are an important structuring mechanism in phytoplankton communities.	[Bolch, Christopher J. S.; Bejoy, Thaila A.] Univ Tasmania, Inst Marine & Antarctic Studies, Launceston, Tas, Australia; [Green, David H.] Scottish Marine Inst, Scottish Assoc Marine Sci, Oban, Argyll, Scotland; [Bejoy, Thaila A.] Curtin Univ, Sch Publ Hlth, Bentley, WA, Australia	University of Tasmania; University of the Highlands & Islands; Curtin University	Bolch, CJS (通讯作者)，Univ Tasmania, Inst Marine & Antarctic Studies, Launceston, Tas, Australia.	chris.bolch@utas.edu.au	Bolch, Christopher/J-7619-2014; Green, David/E-2533-2012	Green, David/0000-0001-7499-6021	University of Tasmania Internal Research Grant Scheme [B0015641]	University of Tasmania Internal Research Grant Scheme	This work was supported by University of Tasmania Internal Research Grant Scheme B0015641 awarded to CB.	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J., 1999, MICROBIAL BIOSYSTEMS	62	42	43	2	44	FRONTIERS MEDIA SA	LAUSANNE	AVENUE DU TRIBUNAL FEDERAL 34, LAUSANNE, CH-1015, SWITZERLAND	1664-302X			FRONT MICROBIOL	Front. Microbiol.	APR 19	2017	8								670	10.3389/fmicb.2017.00670	http://dx.doi.org/10.3389/fmicb.2017.00670			12	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	ES4TR	28469613	gold, Green Published, Green Accepted			2025-03-11	WOS:000399528400002
J	Patil, JS; Rodrigues, RV; Paul, P; Sathish, K; Rafi, M; Anil, AC				Patil, J. S.; Rodrigues, R. V.; Paul, P.; Sathish, K.; Rafi, M.; Anil, A. C.			Benthic dinoflagellate blooms in tropical intertidal rock pools: elucidation of photoprotection mechanisms	MARINE BIOLOGY			English	Article						Rockpools; Benthic dinoflagellates; Amphidinium carterae; Bysmatrum caponii; Blooms; Photoprotection	PHOTOSYNTHETIC ENERGY-CONVERSION; AMPHIDINIUM-CARTERAE HULBURT; COMMUNITY STRUCTURE; SP-NOV; PHYTOPLANKTON COMMUNITIES; MARINE DINOFLAGELLATE; CYTOTOXIC MACROLIDES; TOXIC DINOFLAGELLATE; CYST ASSEMBLAGES; DINOPHYCEAE	Intertidal rockpools (RPs), forming a ubiquitous component of rocky shores, are biologically rich ecosystems influenced by short-term (hours-days) and long-term (days-seasons) fluctuating environments. So far, studies on RP biology are scarce and received no attention in India. This study elucidates planktonic microalgal composition and photoprotection mechanisms [dynamic photoinhibition, non-photochemical-quenching (NPQ), and photoprotective pigments production)] from the RPs located at high tide (HT), mid tide (MT), and low tide (LT) zones on the rocky shores of Anjuna, Goa (India) facing the Arabian Sea. MT-RPs and LT-RPs were dominated by diatoms and HT-RPs by dinoflagellates due to the blooms of autotrophic benthic dinoflagellates belonging to Amphidinium sensu stricto and Bysmatrum. The detailed microscopic analysis of these dinoflagellates showed morphological and cellular features similar to Amphidinium carterae (known harmful algae of concern) and Bysmatrum caponii. This study reports B. caponii for the first time from India as well as from northern Indian Ocean. The fast-repetitionrate- fluorometer measurements of RP microalgae suggested lower quantum efficiency (F-v/F-m) and functional absorption cross section for HT-RPs followed by MT-RPs and LT-RPs. The observed differences can thus be attributed to the microalgal composition differences and to differences in experienced irradiance of these communities. Dynamic photoinhibition was more prominent in LT-RPs followed by MT-RPs and HT-RPs. The high accumulation of photoprotective pigments in HT-RPs (due to prolong exposure to solar radiation) could be the reason for the differences. The presence of reduced de-epoxidation state and the mid-day depression in F-v/F-m coupled with elevated sigma(PSII) confirmed dominance of NPQ of reaction centres in HT-RPs compared to other pools. This study concludes that RP planktonic microalgae are eurythermal, euryhaline, and euryphotic. Concerned with increasing harmful algal bloom events further studies on diverse aspects of RP microalgae (including chemical mediated interactions) needs attention.	[Patil, J. S.; Rodrigues, R. V.; Paul, P.; Sathish, K.; Rafi, M.; Anil, A. C.] CSIR, Natl Inst Oceanog, Panaji 403004, Goa, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO)	Patil, JS (通讯作者)，CSIR, Natl Inst Oceanog, Panaji 403004, Goa, India.	patilj@nio.org		Krishnan, Sathish/0009-0003-3905-871X; Paul, Pranoy/0000-0002-8234-0484	Council of Scientific and Industrial Research (CSIR) [PSC 0105]	Council of Scientific and Industrial Research (CSIR)(Council of Scientific & Industrial Research (CSIR) - India)	This study was supported by the Council of Scientific and Industrial Research (CSIR) funded project Ocean Finder PSC 0105.	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APR	2017	164	4							89	10.1007/s00227-017-3123-z	http://dx.doi.org/10.1007/s00227-017-3123-z			19	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	ER1UF					2025-03-11	WOS:000398579400028
J	Sildever, S; Kremp, A; Enke, A; Buschmann, F; Maljutenko, I; Lips, I				Sildever, Sirje; Kremp, Anke; Enke, Annely; Buschmann, Fred; Maljutenko, Iija; Lips, Inga			Spring bloom dinoflagellate cyst dynamics in three eastern sub-basins of the Baltic Sea	CONTINENTAL SHELF RESEARCH			English	Article						Biecheleria baltica; Peridiniella catenata; Cyst abundance; Resuspension; Cyst transport; Baltic Sea	PERIDINIELLA-CATENATA DINOPHYCEAE; SCRIPPSIELLA-HANGOEI DINOPHYCEAE; PHYTOPLANKTON COMMUNITIES; RESTING STAGES; RESUSPENSION EVENTS; RECENT SEDIMENTS; GULF; GERMINATION; ENCYSTMENT; FINLAND	Dinoflagellate cyst abundance and species composition were investigated before, during and after the spring bloom in the Gulf of Finland, north-eastern Baltic Proper and Gulf of Riga in order to detect spatial and temporal dynamics. Transport of newly formed cysts by currents was modelled to explore the possible distance travelled by cysts before sedimentation. The cyst community of the spring bloom dinoflagellates was dominated by the cysts of Biecheleria baltica in all basins, despite its marginal value in the planktonic spring bloom community in the Gulf of Riga. Dinofiagellate cyst abundance in the surface sediments displayed temporal dynamics in all basins, however, this appeared to be also influenced by physical processes. The model simulation showed that newly formed cysts are transported around 10-30 km from the point of origin before deposited. The latter suggests that transport of resting stages in the water column significantly affects spatial cyst distribution in the sediments and thus needs to be considered in the interpretation of temporal biological productivity patterns of a water body from cyst proxies.	[Sildever, Sirje; Buschmann, Fred; Maljutenko, Iija; Lips, Inga] Tallinn Univ Technol, Marine Syst Inst, Akad Tee 15A, EE-12618 Tallinn, Estonia; [Kremp, Anke] Finnish Environm Inst, Marine Res Ctr, Erik Palmenin Aukio 1, Helsinki 00560, Finland; [Enke, Annely] Univ Tartu, Estonian Marine Inst, Maealuse 14, EE-12618 Tallinn, Estonia	Tallinn University of Technology; Finnish Environment Institute; University of Tartu; Estonian Marine Institute	Sildever, S (通讯作者)，Tallinn Univ Technol, Marine Syst Inst, Akad Tee 15A, EE-12618 Tallinn, Estonia.	sirje.sildever@msi.ttu.ee	Lips, Inga/N-5000-2019; Buschmann, Fred/JMC-7316-2023; Maljutenko, Ilja/AAG-7459-2020; Sildever, Sirje/G-6674-2017	Maljutenko, Ilja/0000-0001-7655-3363; Lips, Inga/0000-0001-6556-6281; Sildever, Sirje/0000-0002-4847-936X	Estonian Ministry of Education and Research [IUT 19-6]; European Social Fund	Estonian Ministry of Education and Research(Ministry of Education & Research Tartu); European Social Fund(European Social Fund (ESF))	This work was supported by institutional research funding of the Estonian Ministry of Education and Research [IUT 19-6] and by a grant from European Social Fund, administered by the Doctoral School of Earth Sciences and Ecology.	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Shelf Res.	APR 1	2017	137						46	55		10.1016/j.csr.2016.11.012	http://dx.doi.org/10.1016/j.csr.2016.11.012			10	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	ES1DR					2025-03-11	WOS:000399268600005
J	Rubino, F; Belmonte, M; Gall, BS				Rubino, Fernando; Belmonte, Manuela; Gall, Bella S.			Plankton resting stages in recent sediments of Haifa port, Israel (Eastern Mediterranean) - Distribution, viability and potential environmental consequences	MARINE POLLUTION BULLETIN			English	Article						Resting stages; Germination; Surface sediments; Toxic species; Pollution; Eastem Mediterranean	DINOFLAGELLATE CYST ASSEMBLAGES; RECENT MARINE-SEDIMENTS; SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; SURFACE SEDIMENTS; COASTAL WATERS; IZMIR BAY; TAXONOMIC CLARIFICATION; DISTRIBUTION PATTERNS; INDUSTRIAL-POLLUTION; SHALLOW SEDIMENTS	Resting stages of plankton were sampled in the surficial sediments in the port of Haifa, Israel, on the eve of a major port enlargement project. We recorded the structure of the assemblages and examined their relationship with different environments within the port. Our findings reveal a remarkably high diversity coupled with low density and the highest number of oligotrich ciliate cyst types recorded from marine sediments. Near the eutrophic and highly polluted zone of the Kishon estuary ciliates were more abundant than elsewhere in the port, whereas dinoflagellates' abundance was reduced, and these trends held true both for full and empty cysts. Some harmful or potentially toxic species, such as Scrippsiella acuminata, were widespread in the port. The toxigenic species include Alexandrium minutum, Gymnodinium uncatenatum and Lingulodinium polyedrum. Active cells of the unarmoured, bloom-forming Akashiwo sanguinea were identified in the cultures obtained from the incubated sediments. (C) 2017 Elsevier Ltd. All rights reserved.	[Rubino, Fernando; Belmonte, Manuela] Inst Coastal Marine Environm, CNR, Talassografico A Cerruti, Via Roma 3, I-74123 Taranto, Italy; [Gall, Bella S.] Tel Aviv Univ, Steinhardt Museum Nat Hist, IL-6997811 Tel Aviv, Israel	Consiglio Nazionale delle Ricerche (CNR); Tel Aviv University	Rubino, F (通讯作者)，Inst Coastal Marine Environm, CNR, Talassografico A Cerruti, Via Roma 3, I-74123 Taranto, Italy.	rubino@iamc.cnr.it	Belmonte, Marisol/AAG-9759-2019; Rubino, Fernando/GOP-0332-2022	Rubino, Fernando/0000-0003-2552-2510	doctoral fellowship in Fundamental Ecology from the University of Salento, Lecce, Italy; CNR; IOLR; European Community's Seventh Framework Programme (FP7)	doctoral fellowship in Fundamental Ecology from the University of Salento, Lecce, Italy; CNR(Consiglio Nazionale delle Ricerche (CNR)); IOLR; European Community's Seventh Framework Programme (FP7)(European Union (EU))	We thank Young-Ok Kim and Sabine Agatha for useful discussion on the taxonomy of ciliate cysts, the crew of R/V "Etziona" for help with the sampling, Yaron Gertner, Chemistry Department, IOLR, for trace metals and TOC data. Esther Garces and Chris Reid commented helpfully on the manuscript. The work of M. Belmonte was supported by a doctoral fellowship in Fundamental Ecology from the University of Salento, Lecce, Italy (XXIV cycle). Support for this research was provided by CNR (FR), by IOLR, and by the European Community's Seventh Framework Programme (FP7/2007-2013) for the projects Vectors of Change in Oceans and Seas Marine Life, Impact on Economic Sectors (VECTORS) and Towards COast to COast NETworks of marine protected areas (from the shore to the high and deep sea), coupled with sea-based wind energy potential (COCONET) (BSG). The sampling took place while BSG worked in the National Institute of Oceanography, IOLR, Haifa.	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Pollut. Bull.	MAR 15	2017	116	1-2					258	269		10.1016/j.marpolbul.2016.12.078	http://dx.doi.org/10.1016/j.marpolbul.2016.12.078			12	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	ES4LU	28089552				2025-03-11	WOS:000399507600043
J	Hennissen, JAI; Head, MJ; De Schepper, S; Groeneveld, J				Hennissen, Jan A. I.; Head, Martin J.; De Schepper, Stijn; Groeneveld, Jeroen			Dinoflagellate cyst paleoecology during the Pliocene -Pleistocene climatic transition in the North Atlantic	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article							SEA-SURFACE CONDITIONS; CANONICAL CORRESPONDENCE-ANALYSIS; UPPER QUATERNARY SEDIMENTS; HEMISPHERE GLACIATIONS; MARINE ENVIRONMENTS; HIGH-LATITUDES; PRODUCTIVITY; ASSEMBLAGES; INTENSIFICATION; RECONSTRUCTION	Dinoflagellate cysts (dinocysts) are widely used as tracers of sea surface conditions in late Quaternary marine records. However, paleoenvironmental reconstructions across the Pliocene-Pleistocene climatic transition and beyond are limited because the hydrologic conditions influencing assemblage compositions may not have a modern analogue, and the ecological optima of extinct dinocyst species are not well known. From a study of two cored sites in the central and eastern North Atlantic, we bypass these issues by statistically analyzing the variations in dinocyst assemblage composition and comparing the results directly to paleoecological parameters (delta O-18(bulloides), Omega 18O(salinity), and geochemical proxies for sea surface temperature [SST]) derived from the planktonic foraminifer Globigerina bulloides recovered from the same samples as the dinocysts. Through canonical correspondence analysis we demonstrate the co-variation of seasonality and dinocyst paleoproductivity. We show that Pyxidinopsis braboi is a cold tolerant species with an optimum SST between 12 and 14 degrees C. We extend the use of Nematosphaeropsis labyrinthus as an indicator of transitional climatic conditions to the Pliocene, we offer evidence for the correlation of Bitectatodinium tepikiense and Filisphaera microornata to high seasonality, and we reiterate an apparent link between Spiniferites mirabilis and eastern North Atlantic water masses. Finally, we confirm that Habibacysta tectata is cold-tolerant rather than a strictly cold-water indicator, that Operculodinium? eirikianum is a cold-intolerant species favoring outer neritic environments, and that Ataxiodinium confusum and Invertocysta lacrymosa are both warm-water species. (C) 2017 Elsevier B.V. All rights reserved.	[Hennissen, Jan A. I.; Head, Martin J.] Univ Toronto, Dept Earth Sci, 22 Russell St, Toronto, ON M5S 3B1, Canada; [Hennissen, Jan A. I.] British Geol Survey, Nicker Hill, Keyworth NG12 5GG, Notts, England; [Head, Martin J.] Brock Univ, Dept Earth Sci, 1812 Sir Isaac Brock Way, St Catharines, ON L2S 3A1, Canada; [De Schepper, Stijn] Bjerknes Ctr Climate Res, Uni Res Climate, Nygardsgaten 112-114, N-5008 Bergen, Norway; [Groeneveld, Jeroen] Univ Bremen, MARUM Ctr Marine Environm Sci, Klagenfurter Str, D-28359 Bremen, Germany	University of Toronto; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Brock University; Bjerknes Centre for Climate Research; University of Bremen	Hennissen, JAI (通讯作者)，Univ Toronto, Dept Earth Sci, 22 Russell St, Toronto, ON M5S 3B1, Canada.; Hennissen, JAI (通讯作者)，British Geol Survey, Nicker Hill, 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; Research Council of Norway (RCN) [229819]; NERC [bgs05017] Funding Source: UKRI	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Research Council of Norway (RCN)(Research Council of Norway); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This contribution arose from the doctoral research of JH, which was supported by a Natural Sciences and Engineering Research Council of Canada Discovery grant to MJH. JH publishes with the approval of the Executive Director of the British Geological Survey. IODP is thanked for providing samples. SDS acknowledges funding from The Research Council of Norway (RCN project 229819). We are most grateful to J. Matthiessen and an anonymous reviewer for their helpful comments on the manuscript.	[Anonymous], P DSDP INIT REP; [Anonymous], 2003, MULTIVARIATE ANAL EC; [Anonymous], 1996, Am. Assoc. Strat. Palynol; [Anonymous], P IODP; [Anonymous], 1988, ADV ECOLOGICAL RES A; [Anonymous], 1989, P OC DRIL PROGR SCI; [Anonymous], TRACERS IN THE SEA; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; BAKKEN K, 1986, BOREAS, V15, P185; BAUMANN KH, 1992, MAR MICROPALEONTOL, V20, P129, DOI 10.1016/0377-8398(92)90003-3; Birks H.J.B., 1995, STAT MODELLING QUATE; Birks H. 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Paleoclimatol. Paleoecol.	MAR 15	2017	470						81	108		10.1016/j.palaeo.2016.12.023	http://dx.doi.org/10.1016/j.palaeo.2016.12.023			28	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	EN2MY		Green Accepted			2025-03-11	WOS:000395845800008
J	Poliakova, A; Zonneveld, KAF; Kwiatkowski, C; Suryoko, MA; Behling, H				Poliakova, Anastasia; Zonneveld, Karin A. F.; Kwiatkowski, Cornelia; Suryoko, Mustaba Ari; Behling, Hermann			Marine environment, vegetation and land use changes during the late Holocene in South Kalimantan and East Java reconstructed based on pollen and organic-walled dinoflagellate cysts analysis	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Late Holocene; Reconstruction of palaeoenvironment; Past vegetation; Anthropogenic influence; Marine sediment cores; Java Sea	INDIAN-OCEAN; CLIMATE VARIABILITY; BANDA SEA; WEST-JAVA; SURFACE SEDIMENTS; LATE PLEISTOCENE; MANGROVE POLLEN; MAKASSAR STRAIT; FIRE-HISTORY; SUNDA SHELF	The pollen, spore and organic-walled dinoflagellate cyst associations of two marine sediment cores from the Java Sea off the mouths of Jelai River (S Kalimantan) and Solo River (E Java) reflect environment and vegetation changes for the last ca 3500 years. A decline in primary forest taxa (e.g. Agathis, Allophylus, Dacrycarpus, Dacydium, Dipterocarpaceae, Phyllocladus and Podocarpus) suggest that the major change in vegetation is caused by forest canopy disturbance possibly as a consequence of human activity. The successive increase in pollen of pioneer tress/shrubs and herb taxa (e.g. Acalypha, Ficus, Macaranga/Mallotus, Trema, Pandanus) indicate the development of secondary vegetation. In Java these changes started much earlier (ca at 2950 cal yr BP) than in Kalimantan (ca at 910 cal yr BP) and seem to be more severe. Changes in the marine realm, reflected by the dinoflagellate cyst association, correspond to the changes in vegetation on land. They reflect a gradual change from relatively well ventilated to more hypoxic bottom/pore water conditions in a more eutrophic environment. Near the coast of Java, the shift of the water trophic status took place between ca 820 and 500 cal yr BP, while near the coast of Kalimantan it occurred as late as at the beginning of the 20th century. We observe an increasing amount of the cysts of Polykrikos schwartzii, P. kofoidii, Lingulodinium machaerophorum, Nematosphaeropsis labyrinthus and Selenopemphix nephroides at times of secondary vegetation development on land, suggesting that human induced terrestrial changes possibly affected the marine environment as well, most likely through increased eutrophication and pollution. (C) 2016 Elsevier B.V. All rights reserved.	[Poliakova, Anastasia; Behling, Hermann] Georg August Univ Gottingen, Albrecht von Haller Inst Plant Sci, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany; [Zonneveld, Karin A. F.] Univ Bremen, D-28334 Bremen, Germany; [Zonneveld, Karin A. F.; Kwiatkowski, Cornelia] Univ Bremen, Ctr Marine Environm Sci MARUM, Leobener Str, D-28359 Bremen, Germany; [Suryoko, Mustaba Ari] Marine Geol Inst ESDM, Jalan Dr Funjunan 236, Bandung 40174, Indonesia	University of Gottingen; University of Bremen; University of Bremen	Poliakova, A (通讯作者)，Georg August Univ Gottingen, Albrecht von Haller Inst Plant Sci, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany.	anastasia.poliakova@biologie.uni-goettingen.de		Poliakova, Anastasia/0000-0001-9824-2603	German Ministry of Education and Science (Bundesministerium fur Bildung and Forschung - BMBF), SPICE III - CAFINDO [03F0645C, 03F0645A]	German Ministry of Education and Science (Bundesministerium fur Bildung and Forschung - BMBF), SPICE III - CAFINDO	Field material for the present research was taken during the scientific cruises of the RV "Baruna Jaya" and unknown RV in 1995-1998. The authors express their gratitude to the crew, scientific and technical assistants for their help. We thank Uta Nusse-Hahne (University of Gottingen), Cornelia Roth and Mirijam Kiggen for the assistance in the laboratory. Dr. Mahyar Mohtadi (Center for Marine Environmental Sciences (MARUM), Bremen) is acknowledged for the help with C<SUP>14</SUP> dating. Prof. Dr. Dierk Hebbeln (MARUM, Bremen) is acknowledged for reading of the manuscript Dr. Haryadi Permana (Earth Dynamics and Geological Disaster Division Research Center for Geotechnology, Bandung, Indonesia) is acknowledged for the administrative support. All SPICE III - CAFINDO (Bremen-Gottingen) group is thanked for the discussion. Jorg Christiansen (University of Gottingen) has our regards for his computer assistance. The financial support by the German Ministry of Education and Science (Bundesministerium fur Bildung and Forschung - BMBF), SPICE III - CAFINDO, Grant No. 03F0645C and No. 03F0645A are gratefully acknowledged.	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Palaeobot. Palynology	MAR	2017	238						105	121		10.1016/j.revpalbo.2016.11.012	http://dx.doi.org/10.1016/j.revpalbo.2016.11.012			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ES5YS					2025-03-11	WOS:000399622900008
J	de Quay, GS; Roberts, GG; Watson, JS; Jackson, CAL				de Quay, G. Stucky; Roberts, G. G.; Watson, J. S.; Jackson, C. A. -L.			Incipient mantle plume evolution: Constraints from ancient landscapes buried beneath the North Sea	GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS			English	Article							ICELAND PLUME; PALEOGENE STRATIGRAPHY; MORAY FIRTH; UPLIFT; ATLANTIC; TEMPERATURE; SUBSIDENCE; SHETLAND; LEVEL; TOPOGRAPHY	Geological observations that constrain the history of mantle convection are sparse despite its importance in determining vertical and horizontal plate motions, plate rheology, and magmatism. We use a suite of geological and geophysical observations from the northern North Sea to constrain evolution of the incipient Paleocene-Eocene Icelandic plume. Well data and a three-dimensional seismic survey are used to reconstruct a 58-55 Ma landscape now buried similar to 1.5 km beneath the seabed in the Bressay region. Geochemical analyses of cuttings from wells that intersect the landscape indicate the presence of angiosperm debris. These observations, combined with presence of coarse clastic material, interpreted beach ridges, and a large dendritic drainage network, indicate that this landscape formed subaerially. Longitudinal profiles of paleo-rivers were extracted and inverted for an uplift rate history, indicating three distinct phases of uplift and total cumulative uplift of similar to 350 m. Dinoflagellate cysts in the surrounding marine stratigraphy indicate that this terrestrial landscape formed in < 3 Ma and was rapidly drowned. This uplift history is similar to that of a slightly older buried landscape in the Faeroe-Shetland basin similar to 400 km to the west. These records of vertical motion are consistent with pulses of anomalously hot asthenosphere spreading out from the incipient Icelandic plume. Using simple isostatic calculations, we estimate that the maximum thermal anomaly beneath Bressay was 50-100 degrees C. Our observations suggest that a thermal anomaly departed the Icelandic plume around 57.4 +/- 2.2 Ma at the latest and travelled with a velocity > similar to 150 km/Ma.	[de Quay, G. Stucky; Roberts, G. G.; Watson, J. S.; Jackson, C. A. -L.] Imperial Coll London, Dept Earth Sci & Engn, London, England	Imperial College London	de Quay, GS (通讯作者)，Imperial Coll London, Dept Earth Sci & Engn, London, England.	g.stucky-de-quay14@ic.ac.uk; gareth.roberts@imperial.ac.uk	Jackson, Christopher/AAY-4382-2021; Roberts, Gareth/H-5516-2015	Roberts, Gareth/0000-0002-6487-8117; Jackson, Christopher/0000-0002-8592-9032; Stucky de Quay, Gaia/0000-0002-8598-543X; Watson, Jonathan/0000-0003-0354-1729	National Environmental Research Council (NERC); London Petrophysical Society	National Environmental Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); London Petrophysical Society	This work was supported by a studentship from the National Environmental Research Council (NERC) and a grant from the London Petrophysical Society. We thank P.G.S. for permission to display seismic reflection profiles from the BBK data set. All seismic reflection and well data were made available through PGS and Statoil. We are grateful for core samples and photographic data which were obtained freely through the British Geological Survey at Keyworth. We thank R. Bell, P. Burgess, G. Hampson, L. Lonergan, M. Sephton, T. Weight, and N. White for helpful discussion. T. Becker, J. Chalmers, and an anonymous reviewer are thanked for their constructive comments. Data, input files, and source code necessary to reproduce uplift inversion model results are available from the authors upon request (g.stucky-de-quay14@imperial.ac.uk; gareth.roberts@imperial.ac.uk).	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Geophys. Geosyst.	MAR	2017	18	3					973	993		10.1002/2016GC006769	http://dx.doi.org/10.1002/2016GC006769			21	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	ES6RS		Green Submitted, hybrid			2025-03-11	WOS:000399677600009
J	Natsuike, M; Oikawa, H; Matsuno, K; Yamaguchi, A; Imai, I				Natsuike, Masafumi; Oikawa, Hiroshi; Matsuno, Kohei; Yamaguchi, Atsushi; Imai, Ichiro			The physiological adaptations and toxin profiles of the toxic <i>Alexandrium fundyense</i> on the eastern Bering Sea and Chukchi Sea shelves	HARMFUL ALGAE			English	Article						Alexandrium fundyense; Alexandrium tamarense (north American clade); Physiology; Chukchi Sea; Bering Sea; Cell growth; Cyst germination; Toxin profile; Water temperature; Salinity; Irradiance; Saxitoxin	TAMARENSE DINOPHYCEAE; GONYAULAX-TAMARENSIS; PROTOGONYAULAX-TAMARENSIS; RESTING CYSTS; COMPLEX DINOPHYCEAE; SPECIES COMPLEX; COASTAL WATERS; NORTHERN JAPAN; GERMINATION; GROWTH	Abundant cyst distributions of the toxic dinoflagellate Alexandrium fundyense (previous A. tamarense north American Glade) were recently observed on the north Chukchi Sea shelf and on the eastern Bering Sea shelf, suggesting that A. fundyense is both highly adapted to the local environments in the high latitude areas and might cause toxin contamination of plankton feeders. However, little is known about the physiological characteristics and toxin profiles of A. fundyense in these areas, which are characterized by low water temperatures, weak sunlight, and more or less permanent ice cover during winter. To clarify the physiological characteristics of A. fundyense, the effects of water temperature and light intensity on the vegetative growth and toxin profiles of this species were examined using A. fundyense strains isolated from one sediment sample collected from each area. Using the same sediments samples, seasonal changes of the cyst germination in different water temperatures were investigated. Vegetative cells grew at temperatures as low as 5 degrees C and survived at 1 degrees C under relatively low light intensity. They also grew at moderate water temperatures (10-15 degrees C). Their cysts could germinate at low temperatures (1 degrees C) and have an endogenous dormancy period from late summer to early spring, and warmer water temperatures (5-15 degrees C) increased germination success. These physiological characteristics suggest that A. fundyense in the Chukchi Sea and eastern Bering Sea is adapted to the environments of high latitude areas. In addition, the results suggest that in the study areas A. fundyense has the potential to germinate and grow when water temperatures increase. Cellular toxin amounts of A. fundyense strains from the eastern Bering Sea and Chukchi Sea were ranged from 7.2 to 38.2 fmol cell(-1). These toxin amounts are comparable with A. fundyense strains isolated from other areas where PSP toxin contamination of bivalves occurs. The dominant toxin of the strains isolated from the Chukchi Sea was saxitoxin, while mostA.fundyense strains from the eastern Bering Sea are dominated by the C2 toxin. Toxin profiles similar to those detected in Chukchi Sea have not been reported by any previous research. The dominance of a highly toxic PST variant in Chukchi A. fundyense suggests that presence of the species at low cell concentrations may cause toxin contamination of predators. This study revealed that abundant A. fundyense cysts deposited on the eastern Bering Sea and Chukchi Sea shelves potentially germinate and grow with PSP toxin contents in the local environments. In conclusion, a high risk of PSP occurrences exists on the eastern Bering Sea and Chukchi Sea shelves. (C) 2017 Elsevier B.V. All rights reserved.	[Natsuike, Masafumi; Yamaguchi, Atsushi; Imai, Ichiro] Hokkaido Univ, Grad Sch Fisheries Sci, 3-1-1 Minato Cho, Hakodate, Hokkaido 0418611, Japan; [Natsuike, Masafumi] Tokyo Inst Technol, Sch Environm & Soc, Meguro Ku, 2-12-1-M1-4 Ookayama, Tokyo 1528552, Japan; [Oikawa, Hiroshi] Natl Res Inst Fisheries Sci, 2-12-4 Fukuura, Kanazawa, Kanagawa 2368648, Japan; [Matsuno, Kohei] Australian Antarctic Div, 203 Channel Highway, Kingston, Tas 7050, Australia	Hokkaido University; Institute of Science Tokyo; Tokyo Institute of Technology; Japan Fisheries Research & Education Agency (FRA); Australian Antarctic Division	Natsuike, M (通讯作者)，Tokyo Inst Technol, Sch Environm & Soc, Meguro Ku, 2-12-1-M1-4 Ookayama, Tokyo 1528552, Japan.	natsuike.m.aa@m.titech.ac.jp	Matsuno, Kohei/AAJ-6510-2021; Yamaguchi, Atsushi/A-8613-2012	Matsuno, Kohei/0000-0001-9793-7622; Yamaguchi, Atsushi/0000-0002-5646-3608	Japan Society for the Promotion of Science (JSPS) [24248032, 24110005]; GRENE Arctic Climate Change Research Project	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); GRENE Arctic Climate Change Research Project	We are grateful to the captains and crews of the R/V Mirai and T/S Oshoro-Maru for assistance of the field observations. Professor Y. Oshima of Tohoku University, Professor M. Asakawa of Hiroshima University, and the Food Safety and Consumer Affairs Bureau in the Ministry of Agriculture, Forestry and Fisheries of Japan kindly supplied the PSP toxin standards. We thank the anonymous reviewers for their fruitful comments. This study was supported by Grant-in-Aid for Scientific Research (A) 24248032, Grant-in-Aid for Scientific Research on Innovative Areas 24110005 from the Japan Society for the Promotion of Science (JSPS), and GRENE Arctic Climate Change Research Project.[SS]	Anderson D.M., 1994, BIOGEOGRAPHY TOXIC D; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1990, TOXIC MARINE PHYTOPLANKTON, P41; ANDERSON DM, 1990, TOXICON, V28, P885, DOI 10.1016/0041-0101(90)90018-3; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Baggesen C, 2012, HARMFUL ALGAE, V19, P108, DOI 10.1016/j.hal.2012.06.005; BRAND L E, 1981, Journal of Plankton Research, V3, P193, DOI 10.1093/plankt/3.2.193; Burrell S, 2013, FOOD CONTROL, V31, P295, DOI 10.1016/j.foodcont.2012.10.002; BURSA ADAM, 1963, ARCTIC JOUR ARCTIC INST N AMER, V16, P239; CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; Collins C, 2009, J PHYCOL, V45, P692, DOI 10.1111/j.1529-8817.2009.00678.x; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1985, B MAR SCI, V37, P529; Grebmeier JM, 2012, ANNU REV MAR SCI, V4, P63, DOI 10.1146/annurev-marine-120710-100926; Gu T. 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J	Brandenburg, KM; Domis, LND; Wohlrab, S; Krock, B; John, U; van Scheppingen, Y; van Donk, E; Van de Waal, DB				Brandenburg, Karen M.; Domis, Lisette N. de Senerpont; Wohlrab, Sylke; Krock, Bernd; John, Uwe; van Scheppingen, Yvonne; van Donk, Ellen; Van de Waal, Dedmer B.			Combined physical, chemical and biological factors shape <i>Alexandrium ostenfeldii</i> blooms in the Netherlands	HARMFUL ALGAE			English	Article						Alexandrium; Nutrients; Grazing; Wind speed; Temperature; Salinity	HARMFUL ALGAL BLOOMS; PERUVIANUM BALECH; TOXIN PRODUCTION; MENDIOLA BALECH; THAU LAGOON; PHYTOPLANKTON COMMUNITIES; CLIMATE-CHANGE; GROWTH; DINOPHYCEAE; SALINITY	Harmful algal blooms (HABs) are globally expanding, compromising water quality worldwide. HAB dynamics are determined by a complex interplay of abiotic and biotic factors, and their emergence has often been linked to eutrophication, and more recently to climate change. The dinoflagellate Alexandrium is one of the most widespread HAB genera and its success is based on key functional traits like allelopathy, mixotrophy, cyst formation and nutrient retrieval migrations. Since 2012, dense Alexandrium ostenfeldii blooms (up to 4500 cells mL(-1)) have recurred annually in a creek located in the southwest of the Netherlands, an area characterized by intense agriculture and aquaculture. We investigated how physical, chemical and biological factors influenced A. ostenfeldii bloom dynamics over three consecutive years (2013-2015). Overall, we found a decrease in the magnitude of the bloom over the years that could largely be linked to changing weather conditions during summer. More specifically, low salinities due to excessive rainfall and increased wind speed corresponded to a delayed A. ostenfeldii bloom with reduced population densities in 2015. Within each year, highest population densities generally corresponded to high temperatures, low DIN:DIP ratios and low grazer densities. Together, our results demonstrate an important role of nutrient availability, absence of grazing, and particularly of the physical environment on the magnitude and duration of A. ostenfeldii blooms. Our results suggest that predicted changes in the physical environment may enhance bloom development in future coastal waters and embayments. (C) 2017 Elsevier B.V. All rights reserved.	[Brandenburg, Karen M.; Domis, Lisette N. de Senerpont; van Donk, Ellen; Van de Waal, Dedmer B.] Netherlands Inst Ecol, Dept Aquat Ecol, Wageningen, Netherlands; [Domis, Lisette N. de Senerpont] Wageningen Univ, Aquat Ecol & Water Qual Management Grp, Wageningen, Netherlands; [Wohlrab, Sylke; Krock, Bernd; John, Uwe] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Dept Ecol Chem, Bremerhaven, Germany; [van Scheppingen, Yvonne] Waterschap Scheldestromen, Middelburg, Netherlands	Royal Netherlands Academy of Arts & Sciences; Netherlands Institute of Ecology (NIOO-KNAW); Wageningen University & Research; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Brandenburg, KM (通讯作者)，Netherlands Inst Ecol, Dept Aquat Ecol, Wageningen, Netherlands.	k.brandenburg@nioo.knaw.nl	wohlrab, sylke/R-7435-2016; john, uwe/S-3009-2016; Krock, Bernd/ABB-7541-2020; Van de Waal, Dedmer/B-8002-2012; van Donk, Ellen/B-7272-2008; KNAW, NIOO-KNAW/A-4320-2012; De Senerpont Domis, Lisette Nicole/C-2902-2008	van Donk, Ellen/0000-0003-3279-4936; KNAW, NIOO-KNAW/0000-0002-3835-159X; Brandenburg, Karen/0000-0002-9342-3349; De Senerpont Domis, Lisette Nicole/0000-0001-7509-9541; Wohlrab, Sylke/0000-0003-3190-0880; Van de Waal, Dedmer/0000-0001-8803-1247	Gieskes-Strijbis Foundation; PACES research program of the Alfred-Wegener Institute; Helmholtz-Zentrum filr Polar- und Meeresforschung; German Research Foundation (DFG) Priority Programme DynaTrait [SPP1704, Jo 702/7-1]	Gieskes-Strijbis Foundation; PACES research program of the Alfred-Wegener Institute; Helmholtz-Zentrum filr Polar- und Meeresforschung; German Research Foundation (DFG) Priority Programme DynaTrait(German Research Foundation (DFG))	The authors thank Dennis Waasdorp, Nico Helmsing, Erik Reichman and Suzanne Naus-Wiezer for their assistance during the field work and technical support. We also thank Annegret Mailer for analyses of PSP toxins. Furthermore, we are grateful to Waterschap Scheldestromen for collecting a substantial part of the data over the past years and providing it to us. We would like to thank Ernst de Bola from Brachion-Idee for zooplankton counts and biovolume assessments. The work of KB is funded by the Gieskes-Strijbis Foundation. Financial support for BK and UJ was provided by the PACES research program of the Alfred-Wegener Institute, Helmholtz-Zentrum filr Polar- und Meeresforschung, and by the German Research Foundation (DFG) Priority Programme DynaTrait (SPP1704; Jo 702/7-1) for UJ and SW.	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J	Koutsodendris, A; Brauer, A; Reed, JM; Plessen, B; Friedrich, O; Hennrich, B; Zacharias, L; Pross, J				Koutsodendris, Andreas; Brauer, Achim; Reed, Jane M.; Plessen, Birgit; Friedrich, Oliver; Hennrich, Barbara; Zacharias, Lerotheos; Pross, Joerg			Climate variability in SE Europe since 1450 AD based on a varved sediment record from Etoliko Lagoon (Western Greece)	QUATERNARY SCIENCE REVIEWS			English	Article						Climate variability; Little Ice Age; Solar minimum; Varve microfacies; SE Europe; Balkan Peninsula; Etoliko Lagoon	NORTH-ATLANTIC OSCILLATION; ENVIRONMENTAL-CHANGE; TEMPERATURE VARIABILITY; MEDITERRANEAN REGION; ICE-AGE; LAKE; PRECIPITATION; RECONSTRUCTION; IMPACT; CONNECTION	To achieve deeper understanding of climate variability during the last millennium in SE Europe, we report new sedimentological and paleoecological data from Etoliko Lagoon, Western Greece. The record represents the southernmost annually laminated (i.e., varved) archive from the Balkan Peninsula spanning the Little Ice Age, allowing insights into critical time intervals of climate instability such as during the Maunder and Dalton solar minima. After developing a continuous, ca. 500-year-long varve chronology, high-resolution mu-XRF counts, stable-isotope data measured on ostracod shells, palynological (including pollen and dinoflagellate cysts), and diatom data are used to decipher the season-specific climate and ecosystem evolution at Etoliko Lagoon since 1450 AD. Our results show that the Etoliko varve record became more sensitive to climate change from 1740 AD onwards. We attribute this shift to the enhancement of primary productivity within the lagoon, which is documented by an up to threefold increase in varve thickness. This marked change in the lagoon's ecosystem was caused by: (i) increased terrestrial input of nutrients, (ii) a closer connection to the sea and human eutrophication particularly from 1850 AD onwards, and (iii) increasing summer temperatures. Integration of our data with those of previously published paleolake sediment records, tree-ring-based precipitation reconstructions, simulations of atmospheric circulation and instrumental precipitation data suggests that wet conditions in winter prevailed during 1740-1790 AD, whereas dry winters marked the periods 1790-1830 AD (Dalton Minimum) and 1830-1930 AD, the latter being sporadically interrupted by wet winters. This variability in precipitation can be explained by shifts in the large-scale atmospheric circulation patterns over the European continent that affected the Balkan Peninsula (e.g., North Atlantic Oscillation). The transition between dry and wet phases at Etoliko points to longitudinal shifts of the precipitation pattern in the Balkan Peninsula during the Little Ice Age. (C) 2017 Elsevier Ltd. All rights reserved.	[Koutsodendris, Andreas; Friedrich, Oliver; Hennrich, Barbara; Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany; [Brauer, Achim; Plessen, Birgit] German Res Ctr Geosci, Sect Climate Dynam & Landscape Evolut 5 2, D-14473 Potsdam, Germany; [Reed, Jane M.] Univ Hull, Dept Geog, Sch Environm Sci, Cottingham Rd, Kingston Upon Hull HU6 7RX, N Humberside, England; [Zacharias, Lerotheos] Univ Patras, Dept Environm & Nat Resources Management, Seferi 2, Agrinion 30100, Greece	Ruprecht Karls University Heidelberg; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; University of Hull; University of Patras	Koutsodendris, A (通讯作者)，Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany.	andreas.koutsodendris@geow.uni-heidelberg.de	; Koutsodendris, Andreas/G-8966-2013	Schroder, Birgit/0000-0003-4807-6357; Brauer, Achim/0000-0002-6655-9451; Koutsodendris, Andreas/0000-0003-4236-7508				Ahmed M, 2013, NAT GEOSCI, V6, P339, DOI [10.1038/NGEO1797, 10.1038/ngeo1797]; [Anonymous], 2001, EUROPEAN DIATOM DATA; [Anonymous], THESIS; Ariztegui D, 2010, GLOBAL PLANET CHANGE, V71, P183, DOI 10.1016/j.gloplacha.2009.11.016; ARSENIPAPADIMITRIOU A, 1991, THEOR APPL CLIMATOL, V43, P105, DOI 10.1007/BF00867467; Balkis N, 2016, PHYCOLOGIA, V55, P187, DOI 10.2216/15-93.1; Battarbee R.W., 2001, TRACKING ENV CHANGES, P155, DOI DOI 10.1007/0-306-47668-1_8; Bladé I, 2012, CLIM DYNAM, V39, P709, DOI 10.1007/s00382-011-1195-x; Brauer A, 2001, J PALEOLIMNOL, V25, P163, DOI 10.1023/A:1008136029735; Brauer A.H., 2004, The Climate in Historical Times. 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Sci. Rev.	MAR 1	2017	159						63	76		10.1016/j.quascirev.2017.01.010	http://dx.doi.org/10.1016/j.quascirev.2017.01.010			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	EM9CR		Green Accepted			2025-03-11	WOS:000395609300005
J	Wiggan, NJ; Riding, JB; Franz, M				Wiggan, Nickolas J.; Riding, James B.; Franz, Matthias			Resolving the Middle Jurassic dinoflagellate radiation: The palynology of the Bajocian of Swabia, southwest Germany	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Radiation; Middle Jurassic (Bajocian); Swabia; Germany; Biostratigraphy	KRAKOW-SILESIA HOMOCLINE; PIENINY KLIPPEN BELT; ORE-BEARING CLAYS; NORTH-WEST SHELF; CYSTS; STRATIGRAPHY; ASSEMBLAGES; AUSTRALIA; NORMANDY; GNASZYN	Dinoflagellates underwent a major radiation during the Bajocian (Middle Jurassic, similar to 170-168 Ma). The group originated in the Middle Triassic and dinoflagellate cysts were relatively low in diversity until the Bajocian, when over 100 species appeared. The Gonyaulacaceae expanded during this interval to become the dominant family of cyst-forming dinoflagellates, and has remained the principal dinofiagellate family throughout the Mesozoic and Cenozoic. However, Bajocian dinofiagellate cysts have received relatively little study. In order to unravel the pattern of the Bajocian dinofiagellate radiation, we have generated a high resolution, quantitative, palynological record through an expanded Middle Jurassic succession in Swabia, southwest Germany. Previous research has indicated a rapid, stepwise order of first appearances through the Bajocian. By contrast, we clearly demonstrate that there was a more gradual, continuous increase in diversity from the Late Aalenian to the Early Bathonian, although the number of first appearances was highest during the latest Early Bajocian to Late Bajocian. Major experimentation in excystment mode in the gonyaulacaceans occurred during the Late Aalenian and Early Bajocian, when multi-plate precingular, single-plate precingular and epicystal archaeopyle types first appeared. Through the integration of our data with published information from northwest Europe, we demonstrate that the appearance of dinofiagellate cyst taxa through the Late Aalenian-Early Bathonian appears to have been controlled by a major second-order transgression. Although the cause of this radiation is yet to be constrained, given the contemporaneous diversifications of other plankton groups, as well as ammonites, bivalves and fishes, it is likely that it formed part of the wider Mesozoic Marine Revolution. There is a prominent acme of Dissiliodinium giganteum in the Lower Bajocian which is a useful stratigraphical marker: Acanthaulax crispa is confirmed as a key index species for the Bajocian. One new species, Korystocysta aldridgeii sp. nov., is described. (C) 2016 The Authors. Published by Elsevier B.V.	[Wiggan, Nickolas J.] Univ Cambridge, Dept Earth Sci, Downing St, Cambridge CB2 3EQ, England; [Wiggan, Nickolas J.; Riding, James B.] British Geol Survey, Environm Sci Ctr, Nicker Hill, Nottingham NG12 5GG, England; [Franz, Matthias] State Author Geol, Mineral Resources & Min, Dept 9, Regierungsprasidium Freiburg, Albertstr 5, D-79104 Freiburg, Germany	University of Cambridge; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Wiggan, NJ (通讯作者)，Univ Cambridge, Dept Earth Sci, Downing St, Cambridge CB2 3EQ, England.	njw56@cam.ac.uk			NERC BGS DTG award [BUFI S246]; NERC [bgs05017] Funding Source: UKRI	NERC BGS DTG award; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work has arisen from the PhD project of Nickolas J. Wiggan which is supported by NERC BGS DTG award reference BUFI S246, entitled The mid Jurassic plankton explosion. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). Nick Butterfield is thanked for comments on earlier drafts of this manuscript. Michael Prauss is gratefully acknowledged for providing holotype photos of Dissiliodinium psilatum which assisted with this study. We also thank Jennie Bull for the databasing of literature range chart data. Marcin Barski and an anonymous reviewer are thanked for providing critical comments which improved this manuscript.	[Anonymous], 2008, GEOLOGY CENTRAL EURO, DOI DOI 10.1144/CEV2P; Bailey D., 1987, Journal of Micropalaeontology, V6, P89; BAILEY D A, 1990, Palynology, V14, P135; Barski M, 2014, REV PALAEOBOT PALYNO, V208, P50, DOI 10.1016/j.revpalbo.2014.05.002; Barski M, 2012, GEOL Q, V56, P391, DOI 10.7306/gq.1030; Butler N, 2005, MICROPALEAEONTOLOGIC, P43; Callomon John H., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P61; Davey R. 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Palaeobot. Palynology	MAR	2017	238						55	87		10.1016/j.revpalbo.2016.11.010	http://dx.doi.org/10.1016/j.revpalbo.2016.11.010			33	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ES5YS		hybrid, Green Published, Green Accepted			2025-03-11	WOS:000399622900006
J	Vellekoop, J; Woelders, L; Açikalin, S; Smit, J; van de Schootbrugge, B; Yilmaz, IÖ; Brinkhuis, H; Speijer, RP				Vellekoop, Johan; Woelders, Lineke; Acikalin, Sanem; Smit, Jan; van de Schootbrugge, Bas; Yilmaz, Ismail O.; Brinkhuis, Henk; Speijer, Robert P.			Ecological response to collapse of the biological pump following the mass extinction at the Cretaceous-Paleogene boundary	BIOGEOSCIENCES			English	Article							EOCENE THERMAL MAXIMUM; ORGANIC-CARBON FLUXES; K-T BOUNDARY; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; EL-KEF; TERTIARY BOUNDARY; SEA-LEVEL; CALCAREOUS NANNOFOSSIL; CHICXULUB IMPACT	It is commonly accepted that the mass extinction associated with the Cretaceous-Paleogene (K-Pg) boundary (similar to 66 Ma) is related to the environmental effects of a large extraterrestrial impact. The biological and oceanographic consequences of the mass extinction are, however, still poorly understood. According to the "Living Ocean" model, the biological crisis at the K-Pg boundary resulted in a long-term reduction of export productivity in the early Paleocene. Here, we combine organic-walled dinoflagellate cyst (dinocyst) and benthic foraminiferal analyses to provide new insights into changes in the coupling of pelagic and benthic ecosystems. To this end, we perform dinocyst and benthic foraminiferal analyses on the recently discovered Tethyan K-Pg boundary section at Okcular, Turkey, and compare the results with other K-Pg boundary sites in the Tethys. The post-impact dominance of epibenthic morphotypes and an increase of inferred heterotrophic dinocysts in the early Paleocene at Okcular are consistent with published records from other western Tethyan sites. Together, these records indicate that during the early Paleocene more nutrients remained available for the Tethyan planktonic community, whereas benthic communities were deprived of food. Hence, in the post-impact phase the reduction of export productivity likely resulted in enhanced recycling of nutrients in the upper part of the water column, all along the western Tethyan margins.	[Vellekoop, Johan; van de Schootbrugge, Bas; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Lab Palaeobot & Palynol, Marine Palynol, NL-3584 CD Utrecht, Netherlands; [Vellekoop, Johan; Woelders, Lineke; Speijer, Robert P.] Katholieke Univ Leuven, Dept Earth & Environm Sci, Div Geol, B-3001 Leuven Heverlee, Belgium; [Acikalin, Sanem] Newcastle Univ, Sch Civil Engn & Geosci, Newcastle Upon Tyne NE1 7RU, Tyne & Wear, England; [Smit, Jan] Vrije Univ Amsterdam, Fac Earth & Life Sci, Dept Sedimentol & Marine Geol, NL-1018 HV Amsterdam, Netherlands; [Yilmaz, Ismail O.] Middle East Tech Univ, Dept Geol Engn, Ankara, Turkey; [Yilmaz, Ismail O.] Univ Texas Austin, Dept Geol Sci, Austin, TX 78712 USA; [Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, Landsdiep 4, NL-1797 SZ Thorntje, Texel, Netherlands	Utrecht University; KU Leuven; Newcastle University - UK; Vrije Universiteit Amsterdam; Middle East Technical University; University of Texas System; University of Texas Austin; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Vellekoop, J (通讯作者)，Univ Utrecht, Fac Geosci, Lab Palaeobot & Palynol, Marine Palynol, NL-3584 CD Utrecht, Netherlands.; Vellekoop, J (通讯作者)，Katholieke Univ Leuven, Dept Earth & Environm Sci, Div Geol, B-3001 Leuven Heverlee, Belgium.	johan.vellekoop@kuleuven.be	Speijer, Robert/H-5073-2016; Vellekoop, Johan/L-1805-2019; Brinkhuis, Henk/IUO-8165-2023; , OMER/AAZ-9186-2020; Vellekoop, Johan/F-6466-2017	Smit, Jan/0000-0002-6070-4865; Vellekoop, Johan/0000-0001-6977-693X; Speijer, Robert/0000-0002-5873-7203; Brinkhuis, Henk/0000-0003-0253-6610; Acikalin, Sanem/0000-0001-7700-3363	Netherlands Organization for Scientific Research (NWO) Open Competition [ALWPJ/09047]; Research Foundation Flanders (FWO) [G.0B85.13]	Netherlands Organization for Scientific Research (NWO) Open Competition(Netherlands Organization for Scientific Research (NWO)); Research Foundation Flanders (FWO)(FWO)	This work was supported by the Netherlands Organization for Scientific Research (NWO) Open Competition Grant ALWPJ/09047 to H. Brinkhuis and the Research Foundation Flanders (FWO) grant G.0B85.13 to R.P. Speijer. We thank L. Kump, F. Boscolo Galazzo, P. Roopnarine and one anonymous referee for their suggestions.	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J	Zhao, Y; Tang, XX; Zhao, XW; Wang, Y				Zhao, Yan; Tang, Xuexi; Zhao, Xiaowei; Wang, You			Effect of various nitrogen conditions on population growth, temporary cysts and cellular biochemical compositions of <i>Karenia</i> <i>mikimotoi</i>	PLOS ONE			English	Article							HARMFUL ALGAL BLOOMS; RED TIDE; HETEROCAPSA-CIRCULARISQUAMA; PHAEODACTYLUM-TRICORNUTUM; PHOTOSYNTHETIC APPARATUS; DINOFLAGELLATE BLOOMS; MARINE-PHYTOPLANKTON; NUTRIENT; EUTROPHICATION; BAY	The harmful algal bloom (HAB)-forming dinoflagellate Karenia mikimotoi was exposed to different nitrogen (N) conditions, in order to study the population growth, temporary cyst production and cellular biochemical compositions in laboratory. The results indicated the population growth of K. mikimotoi was inhibited by different levels of N starvation but showed similar fast recovery after the resupplement of N, and temporary cysts were induced in the period of N starvation. K. mikimotoi grew well in inorganic (NO3-, NO2- and NH4+) and organic (urea) nitrogen sources, but the growth parameters (K, T-p, r) showed differences when simulated by Logistic model regressions. When the cellular organic compounds were measured simultaneously, K. mikimotoi cultured in urea produced more short-chained fatty acids while K. mikimotoi cultured in NH4+ produced more non-fatty acids compounds, indicating the potential change of toxins production cultured by various N sources. We concluded that K. mikimotoi could adapt to fluctuating N environments typical of coastal environments including total N concentration (deficiency or recovery) and relative compositions (different N sources).	[Zhao, Yan; Tang, Xuexi; Zhao, Xiaowei; Wang, You] Ocean Univ China, Dept Marine Ecol, Qingdao, Peoples R China	Ocean University of China	Wang, Y (通讯作者)，Ocean Univ China, Dept Marine Ecol, Qingdao, Peoples R China.	wangyou@ouc.edu.cn	Zhao, Xiaowei/LRB-5418-2024		National Science Foundation of China [U 1406403]	National Science Foundation of China(National Natural Science Foundation of China (NSFC))	This work was supported by the National Science Foundation of China, grant number: U 1406403, (http://wm.nsfc.gov.cn/). The funder had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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J	Dewaele, L; Lambert, O; Louwye, S				Dewaele, Leonard; Lambert, Olivier; Louwye, Stephen			On <i>Prophoca</i> and <i>Leptophoca</i> (Pinnipedia, Phocidae) from the Miocene of the North Atlantic realm: redescription, phylogenetic affinities and paleobiogeographic implications	PEERJ			English	Article						Phocidae; Prophoca; Leptophoca; Miocene; North Atlantic; Redescription; Biostratigraphy; Phylogeny; Biogeography	MIDDLE MIOCENE; DINOFLAGELLATE CYST; SOUTH-AFRICA; LATE NEOGENE; SEA LIONS; FUR SEALS; CARNIVORA; STRATIGRAPHY; PLIOCENE; ORIGIN	Background: Prophoca and Leptophoca represent the oldest known genera of phocine seals, dating from the latest early to middle Miocene. Originally, Prophoca rousseaui and Prophoca proxima were described based on fragmentary remains from the Miocene of Belgium. However, several researchers contested the union of Prophoca rousseaui and Prophoca proxima into one genus, without providing evidence. The stratigraphic context of Prophoca remained poorly constrained due to the lack of precise data associated with the original specimens collected in the area of Antwerp (north of Belgium). Methods: Prophoca and Leptophoca are redescribed and their phylogenetic position among Phocidae is reassessed using PAUP. Dinoflagellate biostratigraphy has been carried out on sediment samples associated with specimens from Prophoca and Leptophoca to elucidate their approximate ages. Results: Whereas the species Prophoca rousseaui is redescribed, Prophoca proxima is considered synonymous to Leptophoca lenis, with the proposal of a new combination Leptophoca proxima (Van Beneden, 1877). Sediment samples from specimens of both taxa have been dated to the late Langhian-early Serravallian (middle Miocene). Following a reinvestigation of Leptophoca amphiatlantica, characters from the original diagnosis are questioned and the specimens of Leptophoca amphiatlantica are considered Leptophoca cf. L. proxima. In a phylogenetic analysis, Prophoca rousseaui and Leptophoca proxima constitute early branching stem-phocines. Discussion: Leptophoca proxima from the North Sea Basin is younger than the oldest known find of Leptophoca proxima from North America, which does not contradict the hypothesis that Phocinae originated along the east coast of North America during the late early Miocene, followed by dispersal to Europe shortly after. Morphological features of the appendicular skeleton indicate that Prophoca rousseaui and Leptophoca proxima have archaic locomotory modes, retaining a more prominent use of the fore flipper for aquatic propulsion than extant Phocidae.	[Dewaele, Leonard; Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium; [Dewaele, Leonard; Lambert, Olivier] Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Brussels, Belgium	Ghent University; Royal Belgian Institute of Natural Sciences	Dewaele, L (通讯作者)，Univ Ghent, Dept Geol, Ghent, Belgium.; Dewaele, L (通讯作者)，Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Brussels, Belgium.	leonard.dewaele@ugent.be	Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Lambert, Olivier/0000-0003-0740-5791; Dewaele, Leonard/0000-0003-1188-2515	FWO Ph.D. Fellowship [11V9115N]; FWO [V411116N]	FWO Ph.D. Fellowship; FWO(FWO)	This publication is in partial fulfillment of the Ph.D. thesis of Leonard Dewaele, with funding provided as an FWO Ph.D. Fellowship (grant number 11V9115N). Additional funding for a research visit to the United States National Museum of Natural History, Washington, D.C., USA, by Leonard Dewaele, was provided as an FWO long stay travel grant (grant number V411116N). There was no additional funding received for this study. 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	Narale, DD; Anil, AC				Narale, Dhiraj Dhondiram; Anil, Arga Chandrashekar			Spatial distribution of dinoflagellates from the tropical coastal waters of the South Andaman, India: Implications for coastal pollution monitoring	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellates; Cyst; South Andaman region; Anthropogenic impact; Hannful algal bloom species	HARMFUL ALGAL BLOOMS; CYST ASSEMBLAGES; RECENT SEDIMENTS; CERATIUM-FURCA; PHYTOPLANKTON BLOOMS; SURFACE SEDIMENTS; EAST-COAST; PORT-BLAIR; CHINA SEA; DAYA BAY	Dinoflagellate community structure from two semi-enclosed areas along the South Andaman region, India, was investigated to assess the anthropogenic impact on coastal water quality. At the densely inhabited Port Blair Bay, the dominance of mixotrophs in water and Protoperidinoids in sediments was attributed to anthropogenic nutrient enrichment and prey availability. A significant decrease in dinoflagellate abundance from inner to outer bay emphasize the variation in nutrient availability. The dominance of autotrophs and Gonyaulacoid cysts at the North Bay highlight low nutrient conditions with less anthropogenic pressure. The occurrence of oceanic Omithocercus steinii and Diplopsalis sp. could evince the oceanic water intrusion into the North Bay. Nine potentially harmful and red-tide-forming species including Alexandrium tamarense complex, A. minutum were identified in this study. Although there are no harmful algal bloom (HABs) incidences in this region so far, increasing coastal pollution could support their candidature towards the future HABs initiation and development. (C) 2016 Elsevier Ltd. All rights reserved.	[Narale, Dhiraj Dhondiram; 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			CSIR; Indian XBT Program (CSIR-NIO) - INCOIS, Ministry of Earth Sciences, India [GAP2018]; Ballast Water Management Program (CSIR-NIO) - Ministry of Shipping, India [GAP2429]	CSIR(Council of Scientific & Industrial Research (CSIR) - India); Indian XBT Program (CSIR-NIO) - INCOIS, Ministry of Earth Sciences, India; Ballast Water Management Program (CSIR-NIO) - Ministry of Shipping, India	We are grateful to Director, CSIR-National Institute of Oceanography (NIO), Goa for his support. We thank Dr. V.V. Gopalkrishna, NIO for continuous support; Dr. Grenson George, CARL Port Blair for field sampling arrangements and lab facility. Acknowledge Mr. Chico Rebello for assistance during field work; Dr. Prakash Babu for sedimentary analysis. D.D.N. is grateful to CSIR for awarding the Senior Research Fellowship. This study was financially supported by the Indian XBT Program (GAP2018; CSIR-NIO) funded by INCOIS, Ministry of Earth Sciences, India and the Ballast Water Management Program (GAP2429; CSIR-NIO) funded by Ministry of Shipping, India. This is NIO contribution (No. 5968).	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Pollut. Bull.	FEB 15	2017	115	1-2					498	506		10.1016/j.marpolbul.2016.11.035	http://dx.doi.org/10.1016/j.marpolbul.2016.11.035			9	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	EL1RX	27988024				2025-03-11	WOS:000394399800073
J	Zumaque, J; Eynaud, F; de Vernal, A				Zumaque, Jena; Eynaud, Frederique; de Vernal, Anne			Holocene paleoceanography of the Bay of Biscay: Evidence for west -east linkages in the North Atlantic based on dinocyst data	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Holocene; Bay of Biscay; Dinocysts; Sea-surface conditions; Climatic optimum; Episodes of cooling	SEA-SURFACE; EUROPEAN DEGLACIATION; DINOFLAGELLATE CYSTS; CLIMATE; OCEAN; WATER; TEMPERATURE; FORAMINIFERA; CIRCULATION; OXYGEN	Paleoceanographical changes during the Holocene were reconstructed from the study of core MD95-2002 situated in the northern Bay of Biscay, which is marked by the direct influence of the northeastern return branch of the North Atlantic Drift. Palynological data, sea-surface condition estimates based on dinocyst assemblages and stable isotope measurements in planktic and benthic foraminifera reveal a strong influence of freshwater/meltwaters from both the proximal European sources and the more distal Laurentide Ice Sheet, which experienced delayed deglaciation. The data also indicate the setting of a climate optimum between 7 and 5.51 a followed by a cooling trend, which is consistent with insolation changes and other regional records of climate changes. Superimposed on the long term trends, the reconstructions of sea-surface conditions evidence large amplitude changes at centennial to millennial time-scales, with seven episodes of cooling and low salinity since 11 ka that generally match episodes of dense sea-ice cover in the Labrador Sea. The west to east transfer of the sea ice and/or meltwater signal across the North Atlantic evidenced from core MD95-2002 points to strong linkages between western and eastern North Atlantic, probably in relation to the North Atlantic Oscillation (NAO) mode of variability. (C) 2016 Elsevier B.V. All rights reserved.	[Zumaque, Jena; de Vernal, Anne] Univ Quebec, Geotop, CP 8888, Montreal, PQ H3C 3P8, Canada; [Eynaud, Frederique] Univ Bordeaux, EPOC, UMR 5805, F-33400 Talence, France	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	Zumaque, J (通讯作者)，Univ Quebec, Geotop, CP 8888, Montreal, PQ H3C 3P8, Canada.	zumaquej@gmail.com	de Vernal, Anne/D-5602-2013		MENRT; CNRS; IPEV; European Union MAST programme ENAM2; Natural Sciences and Engineering Research Council of Canada (NSERC) [38340]; Fonds de Recherche du Quebec - Nature et Technologies (FRQNT); French project: ANR HAMOC; French project: INSU TS/INTERRVIE & LEFE/IMA-GO ICE-BIO-RAM; French project: ARTEMIS 14C facilities; European Union [243908]	MENRT; CNRS(Centre National de la Recherche Scientifique (CNRS)); IPEV; European Union MAST programme ENAM2; Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds de Recherche du Quebec - Nature et Technologies (FRQNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); French project: ANR HAMOC(Agence Nationale de la Recherche (ANR)); French project: INSU TS/INTERRVIE & LEFE/IMA-GO ICE-BIO-RAM; French project: ARTEMIS 14C facilities; European Union(European Union (EU))	Core MD95-2002 was recovered thanks to financial support from MENRT, CNRS, IPEV and European Union MAST programme ENAM2. This work was supported by the funds from the Natural Sciences and Engineering Research Council of Canada (NSERC) (38340) and the Fonds de Recherche du Quebec - Nature et Technologies (FRQNT) and through French projects: ANR HAMOC, INSU TS/INTERRVIE & LEFE/IMA-GO ICE-BIO-RAM, ARTEMIS 14C facilities, and has benefited from the European Union's Seventh Framework programme (FP7/2007-2013) under grant 243908, "Past4Future - Climate change-Learning from the past climate". Thanks are due to Claude Hillaire-Marcel for his most valuable guidance and Maryse Henry and Jean-Francois Helie (GEOTOP) for their help in laboratory. We are grateful to the anonymous reviewers of the journal for their helpful and constructive comments on the manuscript.	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Paleoclimatol. Paleoecol.	FEB 15	2017	468						403	413		10.1016/j.palaeo.2016.12.031	http://dx.doi.org/10.1016/j.palaeo.2016.12.031			11	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	EL9DG					2025-03-11	WOS:000394919000028
J	Richards, K; Mudie, P; Rochon, A; Athersuch, J; Bolikhovskaya, N; Hoogendoorn, R; Verlinden, V				Richards, Keith; Mudie, Peta; Rochon, Andre; Athersuch, John; Bolikhovskaya, Nataliya; Hoogendoorn, Robert; Verlinden, Vincent			Late Pleistocene to Holocene evolution of the Emba Delta, Kazakhstan, and coastline of the north-eastern Caspian Sea: Sediment, ostracods, pollen and dinoflagellate cyst records	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Caspian Sea; Palynology; Ostracods; Stratigraphy; Pollen; Dinocysts	UPPER QUATERNARY DEPOSITS; LATE MIOCENE; ARAL SEA; BASIN; BLACK; PLIOCENE; MIDDLE; LEVEL; PLANT; AGE	Six cores, each approximately 10 m long, of late Pleistocene to Holocene age were studied from the Emba Delta region in the north-eastern Caspian Sea. Radiocarbon dates provide ages within the range of 47,820 to 12,020 cal BP for the middle sections, and for post-1950 close to surface. The ages fall within Marine Isotope Stage (MIS) 3, MIS 2 and MIS I (with MIS 4 also inferred). Four lithological units are present, each separated by an erosional contact. Unit 4 is equated with MIS 4 and consists of over-consolidated, east-west trending aeolian sands deposited during the late Pleistocene Atelian lowstand. Unit 3 is equated with MIS 3 and is a low energy, shallow open water or lagoonal deposit based on ostracod faunas. Pollen from mesophilic trees is common, confirming warm climatic conditions. Floristic elements such as Engelhardia and Carya were shared with East Asia. Frequent Taxodiaceae pollen occurs, derived from Glyptostrobus pensilis, a seasonal freshwater swamp tree, now found naturally only in isolated relict stands in East Asia. This suggests that the northeastern Caspian region was a 'refugium' supporting Glyptostrobus swamp vegetation during MIS 3. There is no evidence to indicate that these are reworked occurrences. Unit 2 consists of early Khvalynian transgressive barrier sands and Unit 1 of shoreface sands and muds of Holocene age. The late Khvalynian highstand and the Last Glacial Maximum (LGM) record are eroded by the Mangyshlak unconformity after ca. 12,500 cal BP. The Holocene interval contains frequent foraminifera and dinoflagellate cysts (dinocysts) of restricted 'marine' affinity (e.g. Lingulodinium machaerophorum). The dinocysts Pterocysta cruciformis and Impagidinium inaequalis are found commonly in the Caspian Sea for the first time. Results are compared with palynological and ostracod assemblages in surface samples from the eastern Caspian Sea coastal region. (C) 2017 Elsevier B.V. All rights reserved.	[Richards, Keith] KrA Stratig Ltd, 116 Albert Dr, Deganwy LL31 9YY, Conwy, Wales; [Richards, Keith] Univ Amsterdam, Inst Biodivers & Ecosyst Dynam, NL-1090 GE Amsterdam, Netherlands; [Mudie, Peta] Geol Survey Canada Atlantic, Box 2008, Dartmouth, NS B2Y 4A2, Canada; [Rochon, Andre] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada; [Athersuch, John] StrataData Ltd, 17 Bothy,Ottershaw Pk, Surrey KT16 0QG, England; [Bolikhovskaya, Nataliya] Lomonosov Moscow State Univ, Fac Geog, Moscow 119991, Russia; [Hoogendoorn, Robert; Verlinden, Vincent] Delft Univ Technol, NL-2600 GA Delft, Netherlands; [Hoogendoorn, Robert] Deltares, Princetonlaan 6, NL-3508 AL Utrecht, Netherlands; [Verlinden, Vincent] Centrica Energy E&P, Justice Mill Lane, Aberdeen AB11 6EQ, Scotland	University of Amsterdam; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Quebec; Lomonosov Moscow State University; Delft University of Technology; Deltares	Richards, K (通讯作者)，KrA Stratig Ltd, 116 Albert Dr, Deganwy LL31 9YY, Conwy, Wales.	kr@paly.co.uk		Verlinden, Vincent/0009-0006-2604-9621	Agip KCO [K00.00.000.AK.H.YS.0001.000 Rev P01]; Russian Science Foundation [16-17-10103]; UNESCO; IUGS; Russian Science Foundation [16-17-10103] Funding Source: Russian Science Foundation	Agip KCO; Russian Science Foundation(Russian Science Foundation (RSF)); UNESCO(Spanish Government); IUGS; Russian Science Foundation(Russian Science Foundation (RSF))	This project was partially funded by a research grant to Robert Hoogendoorn (Delft University of Technology, The Netherlands) by Agip KCO, under scope of work Document K00.00.000.AK.H.YS.0001.000 Rev P01. Project title: Sedimentary dynamics and coastal development of the eastern section of the North Caspian Sea (May 2008). In addition, the study of N.S. Bolikhovskaya for this paper was supported by the Russian Science Foundation (Grant No. 16-17-10103) 'The Caspian Sea system under the global climate change during the Quaternary'. This paper is a contribution to IGCP 610 'From the Caspian to the Mediterranean: Environmental Change and Human Response during the Quaternary' sponsored by UNESCO and IUGS.	Abdullayev NR., 2012, AAPG MEMOIR, V95, P71, DOI DOI 10.1306/13291385M953446; Abramova T.A., 1972, COMPREHENSIVE RES CA, V3, P134; Abramova T.A., 1985, Vestn. Mosk. 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Paleoclimatol. Paleoecol.	FEB 15	2017	468						427	452		10.1016/j.palaeo.2016.12.035	http://dx.doi.org/10.1016/j.palaeo.2016.12.035			26	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	EL9DG					2025-03-11	WOS:000394919000030
J	Corcoran, AA; Wolny, J; Leone, E; Ivey, J; Murasko, S				Corcoran, Alina A.; Wolny, Jennifer; Leone, Erin; Ivey, James; Murasko, Susan			Drivers of phytoplankton dynamics in old Tampa Bay, FL (USA), a subestuary lagging in ecosystem recovery	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Phytoplankton; Algal blooms; Community composition; Monitoring; Pyrodinium bahamense; USA; Florida; Tampa Bay	PYRODINIUM-BAHAMENSE; RESIDUAL CIRCULATION; FLORIDA; ESTUARY; GULF; DISTRIBUTIONS; WATERS; MAINE	In the past four decades, consistent and coordinated management actions led to the recovery of Tampa Bay, FL (USA) an estuary that was declared dead in the 1970s. An exception to this success story is Old Tampa Bay, the northernmost subestuary of the system. Compared to the other bay segments, Old Tampa Bay is characterized by poorer water quality and spring and summer blooms of cyanobacteria, pico-plankton, diatoms, and the saxitoxin-producing dinoflagellate Pyrodinium bahamense. Together, these blooms contribute to light attenuation and lagging recovery of seagrass beds. Yet, studies of phytoplankton dynamics within Old Tampa Bay have been limited both in number and in their spatiotemporal resolution. In this, study, we used field sampling and continuous monitoring to (1) characterize temporal and spatial variability in phytoplankton biomass and community composition and (2) identify key drivers of the different phytoplankton blooms in Old Tampa Bay. Overall, temporal variability in phytoplankton biomass (using chlorophyll a as a proxy) and community composition surpassed spatial variability of these parameters. We found a base community of small diatoms and flagellates, as well as certain dinoflagellates, that persisted year round in the system. Seasonally, freshwater runoff stimulated phytoplankton growth, specifically that of chlorophytes, cyanobacteria and other dinoflagellates consistent with predictions based on ecological theory. On shorter time scales, salinity, visibility, and freshwater inflows were important predictors of phytoplankton biomass. With respect to P. bahamense, environmental drivers including salinity, temperature and dissolved nutrient concentrations explained 24% of the variability in cell abundance, indicating missing explanatory parameters in our study for this taxon, such as cyst density and location of cyst beds. Spatially, we found differences in community trajectories across north south and west east gradients, with the northernmost sampling station being the most unique in the region. This work contributes to the knowledge of phytoplankton biomass and community composition in Tampa Bay by generating spatially and temporally rich phytoplankton community and environmental data for the Old Tampa Bay subestuary. Moreover, it enhances our understanding of bloom drivers and provides recommendations for ecosystem management. Specifically, our findings support continued nutrient reduction measures as a way to mitigate seasonal blooms of diatoms, cyanobacteria and chlorophytes, but not necessarily blooms of P. bahamense. Prediction and mitigation of P. bahamnese blooms should incorporate first order drivers such as cyst location and abundance. (C) 2016 Elsevier Ltd. All rights reserved.	[Corcoran, Alina A.; Wolny, Jennifer; Leone, Erin; Ivey, James; Murasko, Susan] Fish & Wildlife Res Inst, Florida Fish & Wildlife Conservat Commiss, 100 8th Ave SE, St Petersburg, FL 33701 USA; [Wolny, Jennifer] Maryland Dept Nat Resources, 1919 Lincoln Dr, Annapolis, MD 21401 USA; [Ivey, James] Univ S Florida, Dept Environm Sci Policy & Geog, 140 7th Ave 5, St Petersburg, FL 33701 USA	Florida Fish & Wildlife Conservation Commission; State University System of Florida; University of South Florida	Corcoran, AA (通讯作者)，Sapphire Energy, 9035 Adv Ave, Las Cruces, NM 88007 USA.	alina.corcoran@sapphireenergy.com		Wolny, Jennifer L./0000-0002-3556-5015; Ivey, James/0000-0003-3308-0193; , Alina Corcoran/0009-0001-3851-7668	Florida Fish and Wildlife Conservation Commission; Tampa Bay Environmental Fund through a National Fish and Wildlife Grant [1802-13-036518]	Florida Fish and Wildlife Conservation Commission; Tampa Bay Environmental Fund through a National Fish and Wildlife Grant	This work was supported by the Florida Fish and Wildlife Conservation Commission and the Tampa Bay Environmental Fund through a National Fish and Wildlife Grant (# 1802-13-036518). We acknowledge Mary Arnold, Julie Brame, Amber Bratcher, Matt Garrett, Karen Henschen, Cary Lopez, Laura Markley, Eric Muhlbach, Eric Robinson, and Ashley Yunker for their contributions to data collection and compilation. We also thank two anonymous reviewers who helped to improve this manuscript.	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Coast. Shelf Sci.	FEB 5	2017	185						130	140		10.1016/j.ecss.2016.11.009	http://dx.doi.org/10.1016/j.ecss.2016.11.009			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	EK0PJ					2025-03-11	WOS:000393628700012
J	Song, CH; Zeng, YY; Yan, MD; Fang, XM; Feng, Y; Pan, JQ; Liu, XF; Meng, QQ; Hu, CH; Zhong, SR				Song, Chunhui; Zeng, Yongyao; Yan, Maodu; Fang, Xiaomin; Feng, Ying; Pan, Jiaqiu; Liu, Xifang; Meng, Qingquan; Hu, Chunhua; Zhong, Sirui			Sedimentary Conditions of Evaporites in the Late Jurassic Xiali Formation, Qiangtang Basin: Evidence from Geochemistry Records	ACTA GEOLOGICA SINICA-ENGLISH EDITION			English	Article						Evaporites; geochemistry; Late Jurassic; Xiali Formation; Qiangtang Basin	STRONTIUM-ISOTOPE STRATIGRAPHY; QINGHAI-TIBET PLATEAU; SOURCE-ROCK KITCHENS; MARINE SOURCE ROCKS; DINOFLAGELLATE CYSTS; SEAWATER CHEMISTRY; SECULAR VARIATION; OXYGEN-ISOTOPE; EVOLUTION; GROWTH	The Qiangtang Basin (QB), located in the central Tibetan Plateau, is a Jurassic marine basin and one of the most important prospective salt resource belts in China. In recent decades, many outcrops of gypsiferous bed have been found in the Jurassic marine strata in the basin. Salt springs with abnormally high sodium (Na+) contents had been identified in the Late Jurassic Xiali Formation (Fm.) in the basin in the last years. However, to date, no potash or halite deposits have been identified in the QB. Gypsum outcrops and salt springs are very important signs in the investigation of halite and potash deposits. Therefore, the Xiali Fm. is a potentially valuable layer to evaluate for the possible presence of halite and potash deposits in the basin. However, few studies have explored the formation conditions of evaporites in the unit. Here, we present detailed geochemical records from the Yanshiping section related to the study of the formation conditions of evaporites in the Xiali Fm. of the QB. Climate proxies based on the obviously increased anion concentrations of SO42- and Cl- and the significant correlation coefficients of Ca2+-SO42- (R = 0.985) and Na+-Cl- (R = 0.8974) reveal that the upper member of the Xiali Fm. (the upper Xiali Fm.) formed under an arid climate and evolved into the sulfate phase or early chloride phase. Provenance proxies based on the obviously increased K+ and Na+ ion concentrations and the significant correlation coefficient of Na+-Cl- (R = 0.8974) suggest that the upper Xiali Fm. featured optimal provenance conditions for the possible formation of halite deposits. The regression and the semi-closed tidal flat environment in the upper Xiali Fm. were favorable for the formation of potash and halite deposits. The low Mg2+ /Ca2+ values (mean value = 1.82) and significant Na+-Cl- correlation coefficient (R = 0.8974) also suggest that the upper Xiali Fm. is the layer most likely to contain potential halite deposits. In addition, the macroscopic correlations of tectonism, provenance, paleoclimate, saliferous strata and sedimentary environment between the QB and the adjoining Amu Darya Basin in Central Asia reveal that the two basins shared similar geologic settings that were favorable for the formation of evaporites during the Late Jurassic. Therefore, the upper Xiali Fm. is a valuable layer to explore for halite deposit and may be potentially valuable in the future exploration for potash deposits in the QB.	[Song, Chunhui; Zeng, Yongyao; Feng, Ying; Pan, Jiaqiu; Meng, Qingquan; Hu, Chunhua; Zhong, Sirui] Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China; [Song, Chunhui; Zeng, Yongyao; Feng, Ying; Pan, Jiaqiu; Meng, Qingquan; Hu, Chunhua; Zhong, Sirui] Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou 730000, Peoples R China; [Yan, Maodu; Fang, Xiaomin] Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China; [Yan, Maodu; Fang, Xiaomin] Chinese Acad Sci, Key Lab Continental Collis & Plateau Uplift, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China; [Zeng, Yongyao] Lanzhou Resources & Environm Voc Tech Coll, Lanzhou, Peoples R China; [Liu, Xifang] Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China; [Liu, Xifang] Minist Land & Resources, Key Lab Saline Lake Resources & Environm, Beijing 100037, Peoples R China	Lanzhou University; Lanzhou University; Chinese Academy of Sciences; Chinese Academy of Sciences; Institute of Tibetan Plateau Research, CAS; Lanzhou Resources & Environment Voc-Tech University; China Geological Survey; Chinese Academy of Geological Sciences; Ministry of Natural Resources of the People's Republic of China	Song, CH (通讯作者)，Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China.; Song, CH (通讯作者)，Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou 730000, Peoples R China.	songchh@lzu.edu.cn	zeng, yongyao/GLR-7275-2022; Yan, Maodu/AAZ-4958-2021	Yan, Maodu/0000-0002-9257-5412	National Basic Research Program of China [2011CB403003, 2013CB956403]; "Strategic Priority Research Program" of the Chinese Academy of Sciences [XDB03020402]; National Natural Science Foundation of China [41272128]; College Research Program of Gansu Province [2016A-123]	National Basic Research Program of China(National Basic Research Program 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)); College Research Program of Gansu Province	This study was supported by the National Basic Research Program of China (Grant Nos. 2011CB403003 and 2013CB956403), "Strategic Priority Research Program" of the Chinese Academy of Sciences (Grant No. XDB03020402), the National Natural Science Foundation of China (Grant No. 41272128), the College Research Program of Gansu Province (Grant No. 2016A-123). Xiaohui Fang, Gang Niu, Sa Zhang, Song Wu, Jing Bao and Jiwei Yang are thanked for laboratory assistance and fieldwork assistance.	Abbink O, 2001, GLOBAL PLANET CHANGE, V30, P231, DOI 10.1016/S0921-8181(01)00101-1; 方小敏, 1997, 科学通报, V42, P2521; [Anonymous], SALT DEPOSITS THE OR; [Anonymous], CHINESE GEOLOGY; [Anonymous], J NW U; [Anonymous], EVOLUTION MESOZOIC S; [Anonymous], GEOLOGICAL B CHINA; [Anonymous], BILDUNG STEINSALZLAG; [Anonymous], 2010, SEDIMENT GEOLTETHYAN; [Anonymous], J JILIN U EARTH SCI; [Anonymous], ACTA GEOLOGICA SINIC; [Anonymous], TIBET GEOL CHINA; [Anonymous], PROGR REPORT POTASH; [Anonymous], INT PETR EXPL PROD D; [Anonymous], GEOSCIENCE; [Anonymous], STRATIGRAPHY QINGHAI; [Anonymous], 1965, GEOCHEMICAL REGULARI; Aurell M., 1994, GEOBIOS, V27, P549, DOI [10.1016/S0016-6995(94)80220-3, DOI 10.1016/S0016-6995(94)80220-3]; Bai S., 1989, GEOL REV, V35, P529; Barskov IS, 2000, DOKL EARTH SCI, V372, P643; Birch G., 1981, Trans. Geol. Soc. S. 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FEB	2017	91	1					156	174		10.1111/1755-6724.13069	http://dx.doi.org/10.1111/1755-6724.13069			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EN1KE					2025-03-11	WOS:000395768100011
J	Natsuike, M; Yokoyama, K; Nishitani, G; Yamada, Y; Yoshinaga, I; Ishikawa, A				Natsuike, Masafumi; Yokoyama, Katsuhide; Nishitani, Goh; Yamada, Yuichiro; Yoshinaga, Ikuo; Ishikawa, Akira			Germination fluctuation of toxic <i>Alexandrium</i> <i>fundyense</i> and <i>A</i>. <i>pacificum</i> cysts and the relationship with bloom occurrences in Kesennuma Bay, Japan	HARMFUL ALGAE			English	Article						Alexandrium fundyense; Alexandrium pacificum; Cyst; Germination; Mesocosm experiment; Toxic bloom	GREAT EAST JAPAN; SETO-INLAND-SEA; DINOFLAGELLATE GONYAULAX-TAMARENSIS; RESTING CYSTS; POPULATION-DYNAMICS; NORTHEAST JAPAN; HIROSHIMA-BAY; ONAGAWA BAY; SURFACE SEDIMENTS; SAMPLING DEVICE	While cyst germination may be an important factor for the initiation of harmful/toxic blooms, assessments of the fluctuation in phytoplankton cyst germination, from bottom sediments to water columns, are rare in situ due to lack of technology that can detect germinated cells in natural bottom sediments. This study introduces a simple mesocosm method, modeled after previous in situ methods, to measure the germination of plankton resting stage cells. Using this method, seasonal changes in germination fluxes of toxic dinoflagellates resting cysts, specifically Alexandrium fundyense (A. tamarense species complex Group I) and A. pacificurn (A. tamarense species complex Group IV), were investigated at a fixed station in Kesennuma Bay, northeast Japan, from April 2014 to April 2015. This investigation was conducted in addition to the typical samplings of seawater and bottom sediments to detect the dinoflagellates vegetative cells and resting cysts. Bloom occurrences of A. fundyense were observed June 2014 and February 2015 with maximum cell densities reaching 3.6 x 10(6) cells m(-2) and 1.4 x 10(7) cells m(-2), respectively. The maximum germination fluxes of A. fundyense cysts occurred in April 2014 and December 2014 and were 9.3 x 10(3) cells m(-2) day(-1) and 1.4 x 10(4) cells m(-2) day(-1), respectively. For A. pacificum, the highest cell density was 73 x 10(7) cells m(-2) during the month of August, and the maximum germination fluxes occurred in July and August, reaching 5.8 x 10(2) cells m(-2) day(-1). Thus, this study revealed the seasonal dynamics of A. fundyense and A. pacificurn cyst germination and their bloom occurrences in the water column. Blooms occurred one to two months after peak germination, which strongly suggests that both the formation of the initial population by cyst germination and its continuous growth in the water column most likely contributed to toxic bloom occurrences of A. fundyense and A. pacific -um in the bay. (C) 2016 Elsevier B.V. All rights reserved.	[Natsuike, Masafumi] Moune Inst Forest Sato Sea Studies, NPO Mori Wa Umi No Koibito, 212 Higashi Moune,Karakuwa Cho, Kesennuma, Miyagi 9880582, Japan; [Yokoyama, Katsuhide] Tokyo Metropolitan Univ, Grad Sch Urban Environm Sci, 1-1 Minami Osawa, Hachioji, Tokyo 1920397, Japan; [Nishitani, Goh] Tohoku Univ, Grad Sch Agr Sci, Aoba Ku, 1-1 Amamiya Machi, Sendai, Miyagi 9818555, Japan; [Yamada, Yuichiro] Kitasato Univ, Sch Marine Biosci, 1-15-1 Kitasato, Sagamihara, Kanagawa 2520373, Japan; [Yoshinaga, Ikuo] Tottori Univ Environm Sci, Grad Sch Environm Sci & Business Adm, 1-1-1 Wakabadai Kita, Tottori, Tottori 6891111, Japan; [Ishikawa, Akira] Mie Univ, Grad Sch Bioresources, 1577 Kurima Machiya Cho, Tsu, Mie 5148507, Japan; [Natsuike, Masafumi] Tokyo Inst Technol, Sch Environm & Soc, Meguro Ku, 2-12-1-M1-4 Ookayama, Tokyo 1528550, Japan	Tokyo Metropolitan University; Tohoku University; Kitasato University; Mie University; Institute of Science Tokyo; Tokyo Institute of Technology	Natsuike, M (通讯作者)，Moune Inst Forest Sato Sea Studies, NPO Mori Wa Umi No Koibito, 212 Higashi Moune,Karakuwa Cho, Kesennuma, Miyagi 9880582, Japan.; Natsuike, M (通讯作者)，Tokyo Inst Technol, Sch Environm & Soc, Meguro Ku, 2-12-1-M1-4 Ookayama, Tokyo 1528550, Japan.	natsuike.m.aa@m.titech.ac.jp	Yokoyama, Katsuhide/AAM-7655-2021	Yokoyama, Katsuhide/0000-0003-1576-6239	Japan Fund for Global Environment of the Environmental Restoration and Conservation Agency; JSPS KAKENHI [25249068]; Environment Fund of Mitsui Co. Ltd.; Grants-in-Aid for Scientific Research [25249068, 26340049, 16K07823] Funding Source: KAKEN	Japan Fund for Global Environment of the Environmental Restoration and Conservation Agency; JSPS KAKENHI(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); Environment Fund of Mitsui Co. Ltd.; Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We thank Dr. Tomoko Sakami of the Tohoku National Fisheries Research Institute, and Dr. Ichiro Imai of the Graduate School of Fisheries Science, Hokkaido University, for providing valuable comments to improve this manuscript. We are grateful to Makoto Hatakeyama of NPO Mori wa Umi no Koibito for helping with field sampling. This study was funded by the Japan Fund for Global Environment of the Environmental Restoration and Conservation Agency, JSPS KAKENHI Grant Number 25249068, and the Environment Fund of Mitsui & Co. Ltd.	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J	Taniuchi, Y; Watanabe, T; Kakehi, S; Sakami, T; Kuwata, A				Taniuchi, Yukiko; Watanabe, Tsuyoshi; Kakehi, Shigeho; Sakami, Tomoko; Kuwata, Akira			Seasonal dynamics of the phytoplankton community in Sendai Bay, northern Japan	JOURNAL OF OCEANOGRAPHY			English	Article						Sendai Bay; Diatom; Dinoflagellate; Picoeukaryote; Cyanobacteria	GREAT EAST JAPAN; FUNKA BAY; TSUNAMI; SYNECHOCOCCUS; EARTHQUAKE; ABUNDANCE; PACIFIC; IMPACTS; GROWTH; CYSTS	Sendai Bay is located on the Pacific coast of northern Japan and suffered serious damage following the 2011 off the Pacific coast of Tohoku earthquake and tsunami in March 2011. To assess the impact on the marine ecosystem, information was needed on the phytoplankton communities and their seasonal variation. However, such information was limited. Therefore, an intensive monitoring of the phytoplankton was carried out from March 2012 to April 2014. Seasonal variation of the phytoplankton community was similar at coastal and offshore stations. Total phytoplankton biomass, based on Chl a concentration, peaked in spring and then decreased to a minimum in summer, before gradually increasing during early winter and peaking again in the following spring. This seasonal pattern was consistent with previous studies conducted before the earthquake and tsunami. Also, size structure of the phytoplankton community and its four main groups was estimated from the size-fractioned samples of Chl a. Our results also showed that the spring bloom consisted of large diatoms, with their growth ceasing due to nitrogen depletion. The bloom was followed by a summer period where cyanobacteria and picoeukaryote became dominant, with high cell densities in spite of low nutrient concentrations. In addition, sporadic environmental changes, such as those following typhoons, were observed. These resulted in large increases/decreases in individual phytoplankton groups.	[Taniuchi, Yukiko; Watanabe, Tsuyoshi; Kakehi, Shigeho; Sakami, Tomoko; Kuwata, Akira] Tohoku Natl Fisheries Res Inst, Shinhama Cho, Shiogama, Miyagi 9850001, Japan; [Taniuchi, Yukiko] Hokkaido Natl Fisheries Res Inst, 116 Katsurakoi, Kushiro, Hokkaido, Japan	Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA)	Taniuchi, Y (通讯作者)，Tohoku Natl Fisheries Res Inst, Shinhama Cho, Shiogama, Miyagi 9850001, Japan.; Taniuchi, Y (通讯作者)，Hokkaido Natl Fisheries Res Inst, 116 Katsurakoi, Kushiro, Hokkaido, Japan.	taniuchi@affrc.go.jp	Kuwata, Akira/E-1121-2013		CREST (JST)	CREST (JST)(Japan Science & Technology Agency (JST)Core Research for Evolutional Science and Technology (CREST))	We particularly wish to thank Y. Sasaki and Dr. H. Saito for nutrient analyses and the captain and crews of Wakatakamaru and Dai5Taikai-maru for their cooperation. We also thank Dr. D. Jewson for his critical reading of the manuscript. This work was supported by CREST (JST).	Agawin NSR, 1998, MAR ECOL PROG SER, V170, P45, DOI 10.3354/meps170045; [Anonymous], J OCEANOGR UNPUB; [Anonymous], REPORTS SENDAI MUNIC; [Anonymous], 1971, INTERIM REPORT STUDI; [Anonymous], J OCEANOGR UNPUB; [Anonymous], J JAPAN SOC CIVIL SE; [Anonymous], REPORTS SENDAI MUNIC; [Anonymous], J OCEANOGR UNPUB; DAVIS JJ, 1958, ECOLOGY, V39, P530, DOI 10.2307/1931764; Falkowski P. 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Oceanogr.	FEB	2017	73	1					1	9		10.1007/s10872-015-0334-0	http://dx.doi.org/10.1007/s10872-015-0334-0			9	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	EJ1AZ					2025-03-11	WOS:000392943800001
J	Tachibana, A; Nishibe, Y; Fukuda, H; Kawanobe, K; Tsuda, A				Tachibana, Aiko; Nishibe, Yuichiro; Fukuda, Hideki; Kawanobe, Kyoko; Tsuda, Atsushi			Phytoplankton community structure in Otsuchi Bay, northeastern Japan, after the 2011 off the Pacific coast of Tohoku Earthquake and tsunami	JOURNAL OF OCEANOGRAPHY			English	Article						Phytoplankton; Diatom; Otsuchi Bay; Earthquake; Seasonality	PSEUDO-NITZSCHIA SPP.; GREAT EAST JAPAN; DYNAMICS; HOKKAIDO; IMPACTS; CYSTS	The tsunami caused by the 2011 off the Pacific coast of Tohoku Earthquake seriously damaged the Pacific coast of northeastern Japan. In addition to its direct disturbance, a tsunami can indirectly affect coastal pelagic ecosystems via topographical and environmental changes. We investigated seasonal changes in the phytoplankton community structure in Otsuchi Bay, northeastern Japan, from May 2011, which was 2 months after the tsunami, to May 2013. The phytoplankton species composition in May 2011 was similar to that observed in May 2012 and 2013. The present results are consistent with the dominant species and water-mass indicator species of phytoplankton in past records. These results suggest that there was no serious effect of the tsunami on the phytoplankton community in Otsuchi Bay. Community analysis revealed that two distinct seasonal communities appeared in each year of the study period. The spring-summer community was characterized by warm-water Chaetoceros species, and dinoflagellates appeared from May to September. The fall-winter community was characterized by cold neritic diatoms, which appeared from November to March. The succession from the spring-summer community to the fall-winter community took place within a particular water mass, and the fall-winter community appeared in both the surface water and the Oyashio water mass, suggesting that water-mass exchange is not the only factor that determines the phytoplankton community structure in Otsuchi Bay.	[Tachibana, Aiko; Nishibe, Yuichiro; Fukuda, Hideki; Tsuda, Atsushi] Univ Tokyo, Atmosphere & Ocean Res Inst, 5-1-5 Kashiwanoha, Kashiwa, Chiba 2778564, Japan; [Kawanobe, Kyoko] 7-83 Omotemachi, Aizuwakamatu, Fukushima 9650831, Japan	University of Tokyo	Tachibana, A (通讯作者)，Univ Tokyo, Atmosphere & Ocean Res Inst, 5-1-5 Kashiwanoha, Kashiwa, Chiba 2778564, Japan.	t.aiko@aori.u-tokyo.ac.jp	FUKUDA, Hideki/KVB-9846-2024	Tachibana, Aiko/0000-0002-6855-6297	Ministry of Education, Culture, Sports, Science and Technology; Grants-in-Aid for Scientific Research [15H04534] Funding Source: KAKEN	Ministry of Education, Culture, Sports, Science and Technology(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 T. Abe and M. Abe of Myoho-Maru and M. Kurosawa, M. Hirano, A. Yaguchi, T. Suzuki, and other members of the International Coastal Research Center, Atmosphere and Ocean Research Institute, University of Tokyo, for assistance with sampling in Otsuchi Bay after the 2011 tsunami. We are also grateful to the captain and crew of the R/V Tansei-Maru, the Japan Agency for Marine-Earth Science and Technology, for their support at sea. This study was supported through the research program 'Tohoku Ecosystem-Associated Marine Sciences' from the Ministry of Education, Culture, Sports, Science and Technology.	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FEB	2017	73	1					55	65		10.1007/s10872-016-0355-3	http://dx.doi.org/10.1007/s10872-016-0355-3			11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	EJ1AZ					2025-03-11	WOS:000392943800005
J	Kang, Y; Tang, YZ; Taylor, GT; Gobler, CJ				Kang, Yoonja; Tang, Ying-Zhong; Taylor, Gordon T.; Gobler, Christopher J.			DISCOVERY OF A RESTING STAGE IN THE HARMFUL, BROWN-TIDE-CAUSING PELAGOPHYTE, <i>AUREOUMBRA LAGUNENSIS</i>: A MECHANISM POTENTIALLY FACILITATING RECURRENT BLOOMS AND GEOGRAPHIC EXPANSION	JOURNAL OF PHYCOLOGY			English	Article						Aureoumbra; brown tide; cysts; harmful algal blooms; metabolism; resting stage	ALGA AUREOCOCCUS-ANOPHAGEFFERENS; CYST FORMATION; PHOTOSYNTHETIC APPARATUS; TOXIC DINOFLAGELLATE; NITROGEN LIMITATION; CLIMATE-CHANGE; DARK SURVIVAL; CELL-FORMATION; GROWTH-RATE; PHYTOPLANKTON	To date, the life stages of pelagophytes have been poorly described. This study describes the ability of Aureoumbra lagunensis to enter a resting stage in response to environmental stressors, including high temperature, nutrient depletion, and darkness, as well as their ability to revert from resting cells back to vegetative cells after exposure to optimal light, temperature, and nutrient conditions. Resting cells became round in shape and larger in size, filled with red accumulation bodies, had smaller and fewer plastids, more vacuolar space, contained lower concentrations of chl a and RNA, displayed reduced photosynthetic efficiency, and lower respiration rates relative to vegetative cells. Analysis of vegetative and resting cells using Raman microspectrometry indicated resting cells were enriched in sterols within red accumulation bodies and were depleted in pigments relative to vegetative cells. Upon reverting to vegetative cells, cells increased their chl a content, photosynthetic efficiency, respiration rate, and growth rate and lost accumulation bodies as they became smaller. The time required for resting cells to resume vegetative growth was proportional to both the duration and temperature of dark storage, possibly due to higher metabolic demands on stored energy (sterols) reserves during longer period of storage and/or storage at higher temperature (20 degrees C vs. 10 degrees C). Resting cells kept in the dark at 10 degrees C for 7 months readily reverted back to vegetative cells when transferred to optimal conditions. Thus, the ability of Aureoumbra to form a resting stage likely enables them to form annual blooms within subtropical ecosystems, resist temperature extremes, and may facilitate geographic expansion via anthropogenic transport.	[Kang, Yoonja; Taylor, Gordon T.; 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, 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	Kang, Yoonja/AAI-1725-2021; Gobler, Christopher/JOZ-2924-2023; Taylor, Gordon Thomas/A-6735-2009	Taylor, Gordon Thomas/0000-0002-6925-7571	ECOHAB [NA09NOS4780206, NA15NOS4780183]; NSF MRI grant [OCE-1336724]	ECOHAB; NSF MRI grant(National Science Foundation (NSF)NSF - Office of the Director (OD))	This study was supported by ECOHAB of NA09NOS4780206 and NA15NOS4780183. We acknowledge the Central Microscopy Imaging Center (C-MIC) at Stony Brook University, Stony Brook, New York 11794, for assistance with TEM images. We also express our gratitude to the staff of the Nano-Raman Molecular Imaging Laboratory (NARMIL), a service center of the School of Marine and Atmospheric Sciences (SoMAS) at Stony Brook University established with NSF MRI grant OCE-1336724. We also thank Jennifer Goleski for analytical assistance.	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Phycol.	FEB	2017	53	1					118	130		10.1111/jpy.12485	http://dx.doi.org/10.1111/jpy.12485			13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	EP3CJ	27779759				2025-03-11	WOS:000397259800012
J	Correia, VF; Riding, JB; Fernandes, P; Duarte, LV; Pereira, Z				Correia, Vania F.; Riding, James B.; Fernandes, Paulo; Duarte, Luis V.; Pereira, Zelia			The palynology of the lower and middle Toarcian (Lower Jurassic) in the northern Lusitanian Basin, western Portugal	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Biostratigraphy; Early Jurassic (Toarcian); Lusitanian Basin; Palaeobiology; Portugal; Toarcian Oceanic Anoxic Event	OCEANIC ANOXIC EVENT; REGRESSIVE FACIES CYCLES; ORGANIC-MATTER; RECORD; FRANCE; PHYTOPLANKTON; SUCCESSION; NORMANDY; BUILDUPS; ENGLAND	The lower and middle Toarcian (Lower Jurassic) successions of the northern Lusitanian Basin in western Portugal were examined for palynomorphs. Two localities, the Maria Pares and the Vale das Fontes sections, were sam-pled. The sections span the Dactylioceras polymorphum, Hildaites leyisoni and Hildoceras bifrons ammonite biozones. The samples produced relatively low diversity dinoflagellate cyst floras which are typical of those from coeval European successions; the most abundant species is Luehndea spinosa. The other forms encountered were Mancodinium semitabulatum, Mendicodinium microscabratum, M. spinosum subsp. spinosum, Mendicodinium sp., Nannoceratopsis ambonis, N. gracilis and N. senex. Dinoflagellate cysts typically dominate throughout the Dactylioceras polymorphum ammonite biozone; their abundance significantly decreased in the overlying Hildaites levisoni and Hildoceras bifrons ammonite biozones. The low diversity Luehndea-Nannoceratopsis dinoflagellate cyst flora of the northern Lusitanian Basin is characteristic of the Sub-Boreal region of Europe. This is a transitional region, intercalated between the Boreal and Tethyan realms. The Toarcian Oceanic Anoxic Event (T-OAE) in the northern Lusitanian Basin is characterised by a sudden decline in palynomorph abundance and diversity, including the virtual absence of acritarchs and dinoflagellate cysts. Following the T-OAE, Mancodinium semitabulatum and Mendicodinium spp. were the only dinoflagellate cysts recorded. This 'blackout' of dinoflagellate cysts during the T-OAE, and their partial recovery following the event, shows that dinoflagellate populations were responding to a major palaeoenvironmental change. (C) 2016 Elsevier B.V. All rights reserved.	[Correia, Vania F.; Fernandes, Paulo] Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal; [Correia, Vania F.; Pereira, Zelia] LNEG, Rua Amieira, P-4465955 Sao Mamede de Infesta, Portugal; [Riding, James B.] British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England; [Duarte, Luis V.] Univ Coimbra, MARE Marine & Environm Sci Ctr, Dept Earth Sci, Fac Sci & Technol, Rua Silvio Lima, P-3030790 Coimbra, Portugal	Universidade do Algarve; Laboratorio Nacional de Energia e Geologia IP (LNEG); UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universidade de Coimbra	Correia, VF (通讯作者)，Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal.	vania.correia@lneg.pt	Duarte, Luis/F-5282-2013; Pereira, Zelia/B-2740-2017; Fernandes, Paulo/J-6577-2014	Duarte, Luis/0000-0002-9025-5896; Pereira, Zelia/0000-0003-3056-6219; Correia, Vania/0000-0001-5648-3185; Fernandes, Paulo/0000-0003-4888-0230	Portuguese Foundation for Science and Technology [SFRH/BD/93950/2013]; Fundacao para a Ciencia e Tecnologia (FCT), through the strategic project [UID/MAR/04292/2013]; Fundação para a Ciência e a Tecnologia [UID/MAR/04292/2013, SFRH/BD/93950/2013] Funding Source: FCT; NERC [bgs05017] Funding Source: UKRI	Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundacao para a Ciencia e Tecnologia (FCT), through the strategic project(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The contribution of VAnia F. Correia to this paper is part of PhD scholarship SFRH/BD/93950/2013 awarded by the Portuguese Foundation for Science and Technology. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). LVD had the support of the Fundacao para a Ciencia e Tecnologia (FCT), through the strategic project UID/MAR/04292/2013 granted to MARE. The authors greatly appreciate the perceptive and incisive comments of Dr. Rob Fensome (Geological Survey of Canada) and an anonymous reviewer which significantly enriched this paper. The authors are also grateful to the jornal Editor, Prof. Mike Stephenson, for the useful suggestions for improvement of the manuscript.	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B., 2016, EPISODES, V39, P460; Rodrigues B, 2016, INT J COAL GEOL, V168, P35, DOI 10.1016/j.coal.2016.06.016; Smelror M., 1991, Revista Espanola de Micropaleontologia, V23, P47; SOARES AF, 1993, CR ACAD SCI II, V317, P1659; Srivastava SK, 2011, PALAEONTOGR ABT B, V285, P113, DOI 10.1127/palb/285/2011/113; SRIVASTAVA SK, 1976, LETHAIA, V9, P437, DOI 10.1111/j.1502-3931.1976.tb00985.x; SRIVASTAVA SK, 1987, GEOBIOS-LYON, V20, P5, DOI 10.1016/S0016-6995(87)80057-8; Suan G, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2007PA001459; Suan G, 2008, EARTH PLANET SC LETT, V267, P666, DOI 10.1016/j.epsl.2007.12.017; Suan G, 2011, EARTH PLANET SC LETT, V312, P102, DOI 10.1016/j.epsl.2011.09.050; Suan G, 2010, EARTH PLANET SC LETT, V290, P448, DOI 10.1016/j.epsl.2009.12.047; Svensen H, 2007, EARTH PLANET SC LETT, V256, P554, DOI 10.1016/j.epsl.2007.02.013; Terrinha P, 2002, J GEOL, V110, P101, DOI 10.1086/324206; Vakhrameev V.A., 1981, The Palaeobotanists, V28-29, P301, DOI DOI 10.54991/JOP.1981.1417; van Erve A., 1988, Neues Jahrbuch fur Geologie und Palaontologie Abhandlungen, V4, P256; Van Helden B.G.T., 1977, Geological Survey of Canada Paper, V77-1B, P163, DOI DOI 10.4095/102776; WEISS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V215, P1; Wille W., 1982, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V164, P74; Wille W., 1982, CYCLIC EVENT STRATIF, P505; Wilson R.C., 1989, AAPG Memoir, V46, P341; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Woollam R., 1983, 832 I GEOL SCI; Ziaja Jadwiga, 2006, Acta Palaeobotanica, V46, P3	112	20	22	1	15	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	FEB	2017	237						75	95		10.1016/j.revpalbo.2016.11.008	http://dx.doi.org/10.1016/j.revpalbo.2016.11.008			21	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	EI8TG		Green Accepted			2025-03-11	WOS:000392780400005
J	Lu, XX; Wang, ZH; Feng, J				Lu, Xin-Xin; Wang, Zhao-Hui; Feng, Jie			Sedimentary records of recent anthropogenic eutrophication and metal contamination in Zhelin Bay, an important mariculture area in Southern China	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cysts; Metals; Biogenic elements; Environmental changes; Zhelin Bay; South China Sea	DINOFLAGELLATE CYST ASSEMBLAGES; SURFACE SEDIMENTS; SPATIAL-DISTRIBUTION; EASTERN GUANGDONG; SEA; COAST; HOLOCENE; ESTUARY; WATERS; OCEAN	Dinoflagellate cysts (dinocysts), biogenic elements and metals were analyzed from sediment cores collected from Zhelin Bay of the South China Sea in December 2008 to understand the environmental changes over the past 50 years. Dinocyst concentrations ranged from 0 cysts/g to 770 cysts/g, and they were dominated by heterotrophic taxa. There was a clear increase trend upcore for biogenic elements, except for biogenic silica. Metals originated from both the lithogenic source and human activities, and significantly increased after 1985-1995. Environmental changes in the past 50 years can be divided into three stages: (1) before 1985, during which biogenic elements, cyst flux and metals were low; (2) from 1985 to the early 2000s, characterized by an obvious increase of dinocysts, TOC, TN and most metals, while TOC/TN and BSi decreased; and (3) after 2000, the period of rapid increase of dinocysts, TOC and TN but decrease of certain contamination metals. (C) 2016 Elsevier Ltd. All rights reserved.	[Lu, Xin-Xin; Wang, Zhao-Hui; Feng, Jie] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China	Jinan University	Wang, ZH (通讯作者)，Jinan Univ, Inst Hydrobiol, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China.	twzh@jnu.edu.cn			National Natural Science Foundation of China [41476132, 41276154]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This study was financially supported by the National Natural Science Foundation of China (grant numbers 41476132, 41276154).	[Anonymous], THESIS; Dai JC, 2007, ENVIRON POLLUT, V145, P656, DOI 10.1016/j.envpol.2006.10.005; Dale B., 1983, P69; de Vernal A, 2013, QUATERNARY SCI REV, V79, P111, DOI 10.1016/j.quascirev.2013.07.006; Gan Juli, 2001, J ZHEJIANG OCEAN U N, V20, P18; Gu YG, 2016, MAR POLLUT BULL, V113, P520, DOI 10.1016/j.marpolbul.2016.08.029; Gu YG, 2014, MAR POLLUT BULL, V81, P256, DOI 10.1016/j.marpolbul.2014.01.030; Guo YW, 2016, SCI TOTAL ENVIRON, V543, P105, DOI 10.1016/j.scitotenv.2015.11.012; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; Hu JF, 2008, MAR CHEM, V110, P7, DOI 10.1016/j.marchem.2008.02.001; [黄长江 Huang Changjiang], 2004, [海洋与湖沼, Oceanologia et Limnologia Sinica], V35, P21; Ip CCM, 2007, ENVIRON POLLUT, V147, P311, DOI 10.1016/j.envpol.2006.06.028; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; MEYERS PA, 1994, CHEM GEOL, V114, P289, DOI 10.1016/0009-2541(94)90059-0; MORTLOCK RA, 1989, DEEP-SEA RES, V36, P1415, DOI 10.1016/0198-0149(89)90092-7; 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, 2008, MAR MICROPALEONTOL, V68, P21, DOI 10.1016/j.marmicro.2008.01.008; Qi S, 2010, J MARINE SYST, V82, pS28, DOI 10.1016/j.jmarsys.2010.02.003; Qi YZ, 2004, HYDROBIOLOGIA, V512, P209, DOI 10.1023/B:HYDR.0000020329.06666.8c; Radi T, 2007, MAR MICROPALEONTOL, V62, P269, DOI 10.1016/j.marmicro.2006.09.002; Thibodeau B, 2006, MAR GEOL, V231, P37, DOI 10.1016/j.margeo.2006.05.010; USEPA, 1994, 600R94111 USEPA; Vásquez-Bedoya LF, 2008, MAR MICROPALEONTOL, V68, P49, DOI 10.1016/j.marmicro.2008.03.002; Wang C, 2008, ESTUAR COAST SHELF S, V76, P319, DOI 10.1016/j.ecss.2007.07.011; Wang ZH, 2004, MAR ECOL-P S Z N I, V25, P289, DOI 10.1111/j.1439-0485.2004.00035.x; Wang ZH, 2013, MAR POLLUT BULL, V76, P383, DOI 10.1016/j.marpolbul.2013.07.050; Zheng A.Z., 1994, J XIAMEN U NATURAL S, V33, P515	28	14	16	0	35	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 30	2017	114	2					1118	1124		10.1016/j.marpolbul.2016.10.036	http://dx.doi.org/10.1016/j.marpolbul.2016.10.036			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	EK4XR	27760714				2025-03-11	WOS:000393931700057
J	Yuan, H; Zhou, PL; Mei, N				Yuan, Han; Zhou, Peilin; Mei, Ning			Numerical and experimental investigation on the ballast flushing system	OCEAN ENGINEERING			English	Article						Ballast water; Sediments; Flushing; CFD	STIRRED TANKS PREDICTION; SOLID-LIQUID SUSPENSIONS; WATER MANAGEMENT; CFD SIMULATIONS; DINOFLAGELLATE CYSTS; DINOPHYCEAE; GERMINATION; SEDIMENTS; RISKS; SEA	The ballast sediments deposit not only provide the breeding ground for the survival organisms, but also affect the weight balance of the ship and even accelerate the corrosion of the ballast tank. In this work the performance of a ballast water flushing system for the 138,000 m(3) LNGC (Liquefied Natural Gas Carrier) double bottom cargo ship is studied. A simulation model of the ballast tank was made to conduct the numerical analysis. Besides, a scaled experimental setup was established on basis of the similarity principle. With different injecting velocities at the flushing inlet, the sediments distribution in the ballast tank is investigated and the energy consumption of the circulating pump is studied. The results show that by flushing the ballast water on the bottom, the sediments first accumulate at the far end, with the sediments volume fraction climbs up to 10-30%, before gradually getting removed over time. Further, higher inlet velocity leads to a more rapid decrease of average sediments proportion in the ballast tank over time, but the energy consumption in circulating pump significantly increases as well. The required power for this proposed ballast water flushing system is within the common range and thus applicable in the cargo ship.	[Yuan, Han; Mei, Ning] Ocean Univ China, Coll Engn, 238 Songling Rd, Qingdao 266100, Peoples R China; [Zhou, Peilin] Univ Strathclyde, Dept Naval Architecture & Marine Engn, Glasgow G4 0LZ, Lanark, Scotland	Ocean University of China; University of Strathclyde	Yuan, H (通讯作者)，Ocean Univ China, Coll Engn, 238 Songling Rd, Qingdao 266100, Peoples R China.	hanyuan@ouc.edu.cn	Mei, Ning/GLS-6203-2022; Yuan, Han/HKM-3093-2023	Yuan, Han/0000-0002-6521-9316	National Natural Science Foundation of China [51679225, 51276174]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	The authors acknowledge the support provided by the National Natural Science Foundation of China (NO. 51679225) and the National Natural Science Foundation of China (NO. 51276174).	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JAN 15	2017	130						188	198		10.1016/j.oceaneng.2016.12.003	http://dx.doi.org/10.1016/j.oceaneng.2016.12.003			11	Engineering, Marine; Engineering, Civil; Engineering, Ocean; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Oceanography	EJ1WJ		Green Accepted			2025-03-11	WOS:000393000700017
J	Steurbaut, E; King, C				Steurbaut, Etienne; King, Chris			The composite Kortrijk section (W Belgium): a key reference for mid-Ypresian (Early Eocene) stratigraphy in the southern North Sea Basin	GEOLOGICA BELGICA			English	Article						Integrated stratigraphy; microfossils; mid-Ypresian; key reference; southern North Sea Basin	BIOSTRATIGRAPHY; ASSEMBLAGES; AKTULAGAY; KAZAKSTAN	The upper part of the Kortrijk Clay Formation (the Roubaix Clay and Aalbeke Clay Members of mid-Ypresian age) has been exposed in road and canal cuttings and clay quarries in the Kortrijk area (western Belgium), and penetrated by several cored boreholes. It is overlain disconformably by the Mont-Panisel Sand Member of the Hyon Sand Formation (upper middle Ypresian). The Roubaix Clay Member contains diverse and well-preserved calcareous nannofossils, dinoflagellate cysts, foraminifera, ostracods and other calcitic microfossils, and less well-preserved mollusc assemblages, while the Aalbeke Clay Member is secondarily decalcified. The calcareous nannofossil subdivision of upper NP11 and lower NP12 has been recognised in the Kortrijk area, and calibrated with the NW European mid-Ypresian dinoflagellate cyst, ostracod and planktonic foraminiferal zones and datums (e.g. Subbotina influx). Several medium-scale depositional sequences, with an estimated duration of 400 kyr or less, have been recorded. Their respective boundaries coincide with the resistivity maxima identified on the majority of the wireline log profiles of the Belgian Ypresian. Integrated biostratigraphic, magnetostratigraphic and sequence stratigraphic analysis enables correlation with other areas in Belgium, with the London Clay Formation of southern England, and with the standard chronostratigraphic scale. A marine erosion surface has been identified at the base of Unit 20 in the Kortrijk area (mid-Ypresian, early Biochron NP12, middle C24n. 1n, -52.8 Ma), corresponding to the first occurrence of estuarine channel-fill units in southern England. This indicates a brief but profound sea-level fall, either eustatically or tectonically controlled. The composite Kortrijk section is proposed as a reference section for the middle Ypresian in the southern North Sea Basin, and for similar settings in mid-to high-latitudes of the Northern Hemisphere (e. g. Kazakhstan and Crimea).	[Steurbaut, Etienne] Royal Belgian Inst Nat Sci, Operat Directory Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium; [Steurbaut, Etienne] Katholieke Univ Leuven, Leuven, Belgium	Royal Belgian Institute of Natural Sciences; KU Leuven	Steurbaut, E (通讯作者)，Royal Belgian Inst Nat Sci, Operat Directory Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium.; Steurbaut, E (通讯作者)，Katholieke Univ Leuven, Leuven, Belgium.	etienne.steurbaut@naturalsciences.be						[Anonymous], VERHANDELINGEN KONIN; [Anonymous], B BELGISCHE VERENING; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], NEWSLETTERS STRATIGR; [Anonymous], 27 GEOL SOC; [Anonymous], 194 SERV GEOL BELG; [Anonymous], ANN U FERRARA SEZION; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], TERRAINS TERTIAIRES; [Anonymous], 1870, ETUDE GEOLOGIQUE COL; [Anonymous], P KONINKLIJKE NEDE B; [Anonymous], 1996, SPECIAL PUBLICATION; [Anonymous], THESIS; [Anonymous], BERICHTE GEOLOGISCHE; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], NATUURWETENSCHAPPELI; [Anonymous], 1991, B SOC BELGE GEOLOGIE; [Anonymous], BERICHTE GEOLOGISCHE; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], 1995, TERTIARY RES; [Anonymous], B SOC GEOLOGIQUE FRA; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], THESIS; [Anonymous], THESIS; [Anonymous], 1994, B SOC BELGE GEOLOGIE; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], THESIS; [Anonymous], 1991, B SOC BELGE GEOLOGIE; [Anonymous], 1996, GEOLOGICAL SOC LONDO, DOI DOI 10.1144/GSL.SP.1996.101.01.02; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], TREATISE INVERTEBR N; [Anonymous], THESIS; [Anonymous], PALAEOGENE FORAMINIF; [Anonymous], 1998, SEPM SOC SEDIMENTARY; [Anonymous], 1999, B SOC BELG GEOL; [Anonymous], 2016, UPDATE LITHOSTRATIGR; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], GEOLOGISCHES JB A; [Anonymous], 20092 GEOL SURV BELG; [Anonymous], MICROFOSSILES PAROI; [Anonymous], B SOC GEOLOGIQUE FRA; [Anonymous], 1993, SPECIAL PUBLICATIONS; [Anonymous], ANN SOC GEOLOGIQUE N; [Anonymous], 1991, THESIS; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], NW EUROPEAN TERTIARY; [Anonymous], MEMOIRES SERVIR EXPL; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], ATLAS EOCENE PLANKTO; AUBRY MP, 1986, PALAEOGEOGR PALAEOCL, V55, P267, DOI 10.1016/0031-0182(86)90154-9; AUBRY MP, 1986, J GEOL SOC LONDON, V143, P729, DOI 10.1144/gsjgs.143.5.0729; Australian Government, 2008, NAT CONTR PLAN EUR B; Berggren W. 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Belg.		2017	20	3-4					125	159		10.20341/gb.2017.008	http://dx.doi.org/10.20341/gb.2017.008			35	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FQ6YS		Green Published, Green Accepted, Green Submitted, gold			2025-03-11	WOS:000418510600003
J	Natsuike, M; Matsuno, K; Hirawake, T; Yamaguchi, A; Nishino, S; Imai, I				Natsuike, Masafumi; Matsuno, Kohei; Hirawake, Toru; Yamaguchi, Atsushi; Nishino, Shigeto; Imai, Ichiro			Possible spreading of toxic <i>Alexandrium tamarense</i> blooms on the Chukchi Sea shelf with the inflow of Pacific summer water due to climatic warming	HARMFUL ALGAE			English	Article						Alexandrium tamarense; Chukchi sea shelf; Climatic warming; Pacific summer water; Sea ice reduction; Spatial distribution; Temporal distribution	COASTAL WATERS; DINOPHYCEAE; LEBOUR; CYSTS; PHYTOPLANKTON; BIOGEOGRAPHY; ABUNDANCE; SEDIMENTS	A high abundance of resting cysts of the toxic dinoflagellate Alexandrium tamarense was recently reported in the vast continental shelf of the Chukchi Sea in the Arctic Ocean, suggesting that the species is widespread in the shelf. Nevertheless, little is known about the occurrence of A. tamarense vegetative cells in the water column of the arctic. Sea ice reduction and the inflow of Pacific summer water (PSW) through the Bering Strait have recently increased owing to warming in the shelf. To determine the spatial and temporal distributions of A. tamarense in the Chukchi Sea shelf and their relationship to the inflow of PSW, field samplings were conducted in the Chukchi Sea and north Bering Sea shelves three times during the summer of 2013 from July to October. Vegetative cells of A. tamarense was detected in both shelves at all sampling periods with a maximum density of 3.55 x 10(3) cells L-1. This species was also observed at the station at 73 degrees N, indicating the northernmost record of this species to date. The center of the A. tamarense distribution was between the north Bering and south Chukchi Sea shelf during the first collection period, and spread to the north Chukchi Sea shelf during the second and third collection periods. The species occurrences were mainly observed at stations affected by the PSW, especially Bering shelf water. Water structure of PSW was characterized by warmer surface and bottom water temperatures, and increased temperatures may have promoted the cell growth and cyst germination of A. tamarense. Therefore, it is suggested that an increase in the PSW inflow owing to warming promotes toxic A. tamarense occurrences on the Chukchi Sea shelf. (C) 2016 Elsevier B.V. All rights reserved.	[Natsuike, Masafumi; Hirawake, Toru; Yamaguchi, Atsushi; Imai, Ichiro] Hokkaido Univ, Grad Sch Fisheries Sci, 3-1-1 Minato Cho, Hakodate, Hokkaido 0418611, Japan; [Matsuno, Kohei] Australian Antarctic Div, 203 Channel Highway, Kingston, Tas 7050, Australia; [Nishino, Shigeto] Japan Agcy Marine Earth Sci & Technol, 2-15 Natsushima Cho, Yokosuka, Kanagawa 2370061, Japan; [Natsuike, Masafumi] Tokyo Inst Technol, Sch Environm Engn, Meguro Ku, 2-12-1-M1-4 Ookayama, Tokyo 1528552, Japan	Hokkaido University; Australian Antarctic Division; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); Institute of Science Tokyo; Tokyo Institute of Technology	Natsuike, M (通讯作者)，Hokkaido Univ, Grad Sch Fisheries Sci, 3-1-1 Minato Cho, Hakodate, Hokkaido 0418611, Japan.; Natsuike, M (通讯作者)，Tokyo Inst Technol, Sch Environm Engn, Meguro Ku, 2-12-1-M1-4 Ookayama, Tokyo 1528552, Japan.	natsuike.m.aa@m.titech.ac.jp	Matsuno, Kohei/AAJ-6510-2021; Yamaguchi, Atsushi/A-8613-2012	NISHINO, Shigeto/0000-0002-0560-241X; Matsuno, Kohei/0000-0001-9793-7622; Yamaguchi, Atsushi/0000-0002-5646-3608; Hirawake, Toru/0000-0003-0274-6642	GRENE Arctic Climate Change Research Project	GRENE Arctic Climate Change Research Project	The authors thank M. Yamaguchi for advice on the manuscript as well as the crews and captains of the VS Oshoro-Maru and the R/V Mirai for assistance with field sampling. This study was supported by the GRENE Arctic Climate Change Research Project.[SS]	ARMSTRONG IH, 1978, BRIT BIRDS, V71, P58; Baggesen C, 2012, HARMFUL ALGAE, V19, P108, DOI 10.1016/j.hal.2012.06.005; Blasco D, 2003, SCI MAR, V67, P261, DOI 10.3989/scimar.2003.67n3261; Burrell S, 2013, FOOD CONTROL, V31, P295, DOI 10.1016/j.foodcont.2012.10.002; BURSA ADAM, 1963, ARCTIC JOUR ARCTIC INST N AMER, V16, P239; Coachman L.K., 1975, Bering Strait: The Regional Physical Oceanography, P1; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1985, B MAR SCI, V37, P529; GERACI JR, 1989, CAN J FISH AQUAT SCI, V46, P1895, DOI 10.1139/f89-238; Grebmeier JM, 2006, PROG OCEANOGR, V71, P331, DOI 10.1016/j.pocean.2006.10.001; Gu HF, 2013, POLAR BIOL, V36, P427, DOI 10.1007/s00300-012-1273-5; Horner R., 1984, The Alaskan Beaufort Sea, P295; Ishikawa A, 2007, HARMFUL ALGAE, V6, P301, DOI 10.1016/j.hal.2006.04.005; Lilly EL, 2007, J PHYCOL, V43, P1329, DOI 10.1111/j.1529-8817.2007.00420.x; Miyazono Akira, 2002, Scientific Reports of Hokkaido Fisheries Experimental Station, V61, P1; Montoya Nora G., 1997, Revista de Investigacion y Desarrollo Pesquero, V11, P145; Natsuike M., 2016, HARMFUL ALG IN PRESS; Natsuike M, 2013, HARMFUL ALGAE, V27, P52, DOI 10.1016/j.hal.2013.04.006; Okolodkov YB, 1996, J EXP MAR BIOL ECOL, V202, P19, DOI 10.1016/0022-0981(96)00028-7; Orlova TY, 2004, BOT MAR, V47, P184, DOI 10.1515/BOT.2004.019; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Selina M.S., 2006, J MAR BIOL, V32, P321; Shimada H, 2012, FISHERIES SCI, V78, P865, DOI 10.1007/s12562-012-0513-5; Shimada K, 2006, GEOPHYS RES LETT, V33, DOI 10.1029/2005GL025624; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; Sukhanova IN, 2009, DEEP-SEA RES PT II, V56, P1223, DOI 10.1016/j.dsr2.2008.12.030; Tomas C., 1997, Identifying Marine Phytoplankton, P1, DOI DOI 10.1016/B978-0-12-693018-4.X5000-9; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Walsh JJ, 2011, PROG OCEANOGR, V91, P312, DOI 10.1016/j.pocean.2011.02.001; WATRAS CJ, 1982, J EXP MAR BIOL ECOL, V62, P25, DOI 10.1016/0022-0981(82)90214-3; Weingartner T, 2013, CONT SHELF RES, V67, P5, DOI 10.1016/j.csr.2013.03.012; WHITE AW, 1981, LIMNOL OCEANOGR, V26, P103, DOI 10.4319/lo.1981.26.1.0103; Woodgate RA, 2010, GEOPHYS RES LETT, V37, DOI 10.1029/2009GL041621	33	28	29	1	26	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	JAN	2017	61						80	86		10.1016/j.hal.2016.11.019	http://dx.doi.org/10.1016/j.hal.2016.11.019			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	EJ0HU					2025-03-11	WOS:000392890000009
J	Vento, B; Gandolfo, MA; Nixon, KC; Prámparo, M				Vento, Barbara; Gandolfo, Maria A.; Nixon, Kevin C.; Pramparo, Mercedes			Paleofloristic assemblage from the Paleogene Rio Guillermo Formation, Argentina: preliminary results of phylogenetic relationships of <i>Nothofagus</i> in South America	HISTORICAL BIOLOGY			English	Article						Paleofloristic composition; paleoclimate; paleoenvironmental; Nothofagus; phylogeny	SUBGENUS BRASSOSPORA; DINOFLAGELLATE CYSTS; PLANT DIVERSITY; SANTA-CRUZ; EOCENE; EVOLUTION; VEGETATION; PATAGONIA; CLIMATE; CLASSIFICATION	Hunicken's paleobotanical collection is one of the most important in South America because it was the first one to be related to a documented stratigraphic profile. This floristic assemblage (Oligocene) recovered from Rio Guillermo Formation, at Estancia Tres Marias, Rio Guillermo Valley, Santa Cruz, Argentina, is described by the first time in this paper. Five species of genus Nothofagus (N. subferruginea, N. serrulata, N. crenulata, N. elongata and N. variabilis) together with Myrcia bagualense are components of the assemblage. The presence of Acaena brandmayri is confirmed for the first time for the area. Paleoenviromental and paleoclimate implications are also discussed. Characteristic species from a temperate-cold climate such as the genus Nothofagus are present in the material studied. A phylogenetic study of the fossil species herein described and the extant South American species of Nothofagus is presented. The preliminary results support the hypothesis that fossil species of Nothogafus are closely related to the modern species.	[Vento, Barbara; Pramparo, Mercedes] CCT CONICET, Inst Argentino Glaciol Nivol & Ciencias Ambiental, Mendoza, Argentina; [Vento, Barbara; Gandolfo, Maria A.; Nixon, Kevin C.] Cornell Univ, Plant Biol Sect, LH Bailey Hortorium, Sch Integrat Plant Sci, Ithaca, NY 14853 USA	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Cornell University	Vento, B (通讯作者)，CCT CONICET, Inst Argentino Glaciol Nivol & Ciencias Ambiental, Mendoza, Argentina.; Vento, B (通讯作者)，Cornell Univ, Plant Biol Sect, LH Bailey Hortorium, Sch Integrat Plant Sci, Ithaca, NY 14853 USA.	bvento@mendoza-conicet.gov.ar			Williams Foundation; CONICET fellowship; National Science foundation [DEB-091832]; Direct For Biological Sciences; Division Of Environmental Biology [1556136] Funding Source: National Science Foundation	Williams Foundation; CONICET fellowship(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); National Science foundation(National Science Foundation (NSF)); Direct For Biological Sciences; Division Of Environmental Biology(National Science Foundation (NSF)NSF - Directorate for Biological Sciences (BIO))	This work was supported by The Williams Foundation, a CONICET fellowship to BV provided funds and by The National Science foundation award [DEB-091832] to MAG.	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Biol.		2017	29	1					93	107		10.1080/08912963.2015.1136930	http://dx.doi.org/10.1080/08912963.2015.1136930			15	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	EF3JX		Green Published			2025-03-11	WOS:000390221800010
J	De Schepper, S; Mangerud, G				De Schepper, Stijn; Mangerud, Gunn			Age and palaeoenvironment of the Utsira Formation in the northern North Sea based on marine palynology	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Dinoflagellate cysts; biostratigraphy; palaeoenvironment; Pliocene; Utsira Formation; carbon dioxide storage	DINOFLAGELLATE CYST STRATIGRAPHY; VIKING GRABEN; UPPER MIOCENE; SEQUENCE STRATIGRAPHY; PLIOCENE-PLEISTOCENE; CENOZOIC SEDIMENTS; ACRITARCH EVENTS; MIDDLE MIOCENE; BELGIUM; BASIN	The Utsira Formation is a major player in the carbon capture and storage on the Norwegian Shelf. Although this northern North Sea unit has been subjected to several geological and monitoring studies, its lateral distribution and stratigraphic position are still not fully understood. This unit was considered to be late Neogene and deposited in neritic environments on the Norwegian Shelf, in an area from the Viking Graben to the Tampen Spur. Here, we present marine palynomorph (dinoflagellate cysts, acritarchs) data extracted mainly from cutting samples of eight industry wells that cover the entire distribution area of the Utsira Formation to provide an age and palaeoenvironmental reconstruction for this unit. We conclude that deposits classified as Utsira Formation are Late Miocene/Early Pliocene to Early Pleistocene in age. Early Pliocene sediments are found mainly in the Viking Graben area, whereas sediments with an Early Pleistocene age occur over the entire distribution area of the Utsira Formation. All sediments were deposited in neritic environments that gradually became shallower from the Early Pliocene to the Pleistocene. At the same time, the dinoflagellate cysts also indicate a cooling that corresponds well with late Neogene global cooling. Precise dating of the Utsira Formation is difficult, but this can be improved by (1) using samples from cored section (in contrast to using cuttings), (2) a clear and unquestionable lithological definition of the Utsira Formation and (3) a continuous, calibrated reference section in the Neogene North Sea for comparison of the bioevents.	[De Schepper, Stijn; Mangerud, Gunn] Univ Bergen, Dept Earth Sci, POB 7803, N-5020 Bergen, Norway; [De Schepper, Stijn] Bjerknes Ctr Climate Res, Uni Res Climate, Jahnebakken 5, N-5007 Bergen, Norway	University of Bergen; Bjerknes Centre for Climate Research	De Schepper, S (通讯作者)，Univ Bergen, Dept Earth Sci, POB 7803, N-5020 Bergen, Norway.; De Schepper, S (通讯作者)，Bjerknes Ctr Climate Res, Uni Res Climate, Jahnebakken 5, N-5007 Bergen, Norway.	stijn.deschepper@uni.no	Mangerud, Gunn/ABD-2588-2020; De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914	Statoil ASA	Statoil ASA	Samples from wells 24/12-1, 25/2-10S, 30/6-3 and 34/4-6 were kindly provided by the Norwegian Petroleum Directorate and from wells 34/4-7, 34/7-2 and 34/7-4, by Statoil ASA. S. Piasecki (GEUS) kindly provided his palynological slides from well 15/9-A-23. Funding for sample preparations was provided by Statoil ASA. Malcolm J. Jones and Palynological Laboratory Services Ltd, Holyhead (UK) are thanked for the palynological preparations. A special thanks goes to Allex Cullum, Gitte V. Laursen, Bruce Tocher and Linn M. Johansen (Statoil ASA).	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J. Geol.		2017	97	4					305	325		10.17850/njg97-4-04	http://dx.doi.org/10.17850/njg97-4-04			21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FW1MG		Green Published, gold			2025-03-11	WOS:000425062500004
C	Józsa, S; Reháková, D		Kaminski, MA; Alegret, L		Jozsa, Stefan; Rehakova, Daniela			Deep-water agglutinated foraminifera and palaeoenvironmental implications of the upper Valanginian to Hauterivian Pieniny Limestone Formation (Nad Raztoky Quarry, Orava sector of the Pieniny Klippen Belt, Western Carpathians)	PROCEEDINGS OF THE NINTH INTERNATIONAL WORKSHOP ON AGGLUTINATED FORAMINIFERA	Grzybowski Foundation Special Publication		English	Proceedings Paper	9th International Workshop on Agglutinated Foraminifera	SEP 03-07, 2012	Univ Zaragoza, Zaragoza, SPAIN	Univ Zaragoza, Earth Sci Dept, Grzybowski Fdn	Univ Zaragoza	Maiolica limestones; black shales; deep-water agglutinated foraminifera; calcareous dinoflagellates; Valanginian; Hauterivian	CALCAREOUS DINOFLAGELLATE; BENTHIC FORAMINIFERA; EVENTS; BASIN; SEA; SEDIMENTARY; EVOLUTION; SECTION; RECORD; LEVEL	The upper member of the Pieniny Limestone Formation in the Western Carpathian Pieniny Klippen Belt represents a specific episode in the sedimentation of the Maiolica facies in the Mediterranean Tethys. Microfacies unusually rich in calcareous dinoflagellate cysts have been observed in the black shale intercalations. Among abundant cysts, dissolved samples yielded deep-water agglutinated foraminifera, calcareous benthic foraminifera and radiolaria. Data based on foraminiferal morphogroups and on the presence of other microfossil groups from the limestones and black shale alternations reveal microfaunal changes in this monotonous sequence. Palaeoenvironmental conditions are reflected by changes in the fossil record, influenced generally by nutrient availability and oxygen content.	[Jozsa, Stefan; Rehakova, Daniela] Comenius Univ, Fac Nat Sci, Dept Geol & Palaeontol, Ilkovieova 6,Mlynska Dolina G-1, Bratislava 84215, Slovakia	Comenius University Bratislava	Józsa, S (通讯作者)，Comenius Univ, Fac Nat Sci, Dept Geol & Palaeontol, Ilkovieova 6,Mlynska Dolina G-1, Bratislava 84215, Slovakia.		Reháková, Daniela/AAA-8694-2020		 [APVV 0212-12];  [VEGA 2/0094/14];  [APVV-14-0018];  [VEGA 2/0034/16]	; ; ; 	The authors are thankful for financial support of projects APVV 0212-12, VEGA 2/0094/14, APVV-14-0018, VEGA 2/0034/16. We gratefully acknowledge Eva Halasova and Marta Bak for their help and advice regarding calcareous nannoplankton and radiolaria. We are thankful to Roman Aubrecht for consultations regarding the geology and for providing digital photographs of the locality. Thanks go to Mike Kaminski and a second anonymous reviewer for reading draft of the manuscript and offering helpful suggestions.	Andrusov D., 1938, ROZPRAVY STATNIHO GE, V9; [Anonymous], 1994, Rivista Italiana di Paleontologia e Stratigrafia; [Anonymous], 1995, SPECIAL PUBLICATION; AUBRECHT R., 2004, Geolines, V17, P15; Bacelle L., 1965, ANNALI DELLUNIVERSIT, V1, P59; Bersezio R, 2002, PALAEOGEOGR PALAEOCL, V180, P253, DOI 10.1016/S0031-0182(01)00416-3; Birkenmajer K., 1977, Stud. Geol. 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Found. Spec. Publ.		2017	22						81	94						14	Geology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	BJ4JD					2025-03-11	WOS:000425069400008
J	De Schepper, S; Beck, KM; Mangerud, G				De Schepper, Stijn; Beck, Kristina M.; Mangerud, Gunn			Late Neogene dinoflagellate cyst and acritarch biostratigraphy for Ocean Drilling Program Hole 642B, Norwegian Sea	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Miocene; Pliocene; Palynology; Biozones; Nordic Seas; North Atlantic	NORTHERN BELGIUM; PLIOCENE-PLEISTOCENE; NORDIC SEAS; MIOCENE; STRATIGRAPHY; PALEOECOLOGY; CALIBRATION; ZONATION; ICELAND; EVENTS	The Arctic is a critical region in the current and past global climate system. One major challenge for investigating the geological history of the Arctic is the establishment of a rigorous chronology. To get better insights into the late Neogene history of oceanographic and climatic change in the region, well-calibrated ocean drill cores are essential. Nevertheless, detailed stratigraphy from (sub)Arctic ocean drill sites remains problematic due to the generally poor preservation of calcareous microfossils in high northern-latitude oceans. Here, organic-walled palynomorphs (dinoflagellate cysts and acritarchs) can compensate for the lack of calcareous microfossils because diverse and rich palynological assemblages can be recovered. We defined three magnetostratigraphically-calibrated dinoflagellate cyst and acritarch biozones in the Upper Miocene to Upper Pliocene of Norwegian Sea Ocean Drilling Program Hole 642B (Voring Plateau) that show potential for correlation within the Nordic Seas. It is also noted that several bioevents in the Nordic Seas are strongly diachronous with the North Atlantic, highlighting the limitations of applying North Atlantic bioevents directly to the Nordic Seas. For each of the three interval biozones (VP1 to VP3) we use the highest occurrences of acritarch and dinoflagellate cyst species ("Veriplicidium franklinii" of Anstey 1992, Reticulatosphaera actinocoronata, and Invertocysta lacrymosa) that are relatively synchronous across the Nordic Seas and North Atlantic and thus show potential for a North Atlantic Arctic reference stratigraphy. (C) 2016 Elsevier B.V. All rights reserved.	[De Schepper, Stijn; Beck, Kristina M.; Mangerud, Gunn] Univ Bergen, Dept Earth Sci, POB 7803, N-5020 Bergen, Norway; [De Schepper, Stijn] Uni Res Climate, Bjerknes Ctr Climate Res, POB 7810, N-5020 Bergen, Norway	University of Bergen; Bjerknes Centre for Climate Research	De Schepper, S (通讯作者)，Uni Res Climate, POB 7810, N-5020 Bergen, Norway.	smad2@cantab.net; kristina.mar.beck@gmail.com; Gunn.Mangerud@uib.no	Mangerud, Gunn/ABD-2588-2020; De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914	Norwegian Research Council [221712, 229819]	Norwegian Research Council(Research Council of Norway)	This work is based on the MSc thesis of Kristina Beck (University of Bergen, Norway). Malcolm J. Jones of Palynological Laboratory Services Ltd., Holyhead (UK) is thanked for the palynological preparations. Funding for sample preparations from Statoil ASA (via the Utsira Project) is appreciated. The Integrated Ocean Drilling Program provided the samples. B. Risebrobakken is thanked for making the samples available (Norwegian Research Council project 221712). SDS acknowledges funding from the Norwegian Research Council (project 229819). We are grateful for the constructive comments of K. Dybkjr and M.J. Head.	Anstey C. E., 1992, THESIS, P1; Anthonissen ED, 2009, NEWSL STRATIGR, V43, P91, DOI 10.1127/0078-0421/2009/0043-0091; Bachem PE, 2016, EARTH PLANET SC LETT, V446, P113, DOI 10.1016/j.epsl.2016.04.024; Beck K. 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Palaeobot. Palynology	JAN	2017	236						12	32		10.1016/j.revpalbo.2016.08.005	http://dx.doi.org/10.1016/j.revpalbo.2016.08.005			21	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	EG0TN		Green Accepted			2025-03-11	WOS:000390745200002
J	Pavlishina, P				Pavlishina, Polina			Palynostratigraphy and palaeoenvironments around the Albian-Cenomanian boundary interval (OAE1d), North Bulgaria	SCIENCE CHINA-EARTH SCIENCES			English	Article; Proceedings Paper	International Workshop on Climate and Environmental Evolution in the Mesozoic Greenhouse World / 3rd IGCP 609 Workshop on Cretaceous Sea-Level Change	SEP 05-11, 2015	Nanjing Univ, Nanjing, PEOPLES R CHINA	IGCP 60[	Nanjing Univ	Albian; Cenomanian; Dinoflagellate cysts; Biostratigraphy; Palaeoenvironments; OAE1d	SOUTHERN ALPS; SWITZERLAND; CLIMATE; EVENT; SEA	The palynological assemblages from two Albian-Cenomanian boundary sections in North Bulgaria are described. The samples analyzed yielded a diverse palynological content including dinoflagellate cysts and miospores. Based on dinocyst nutrient and productivity indices a phase of enhanced nutrient availability and high primary productivity is inferred for the latest Albian interval. The pronounced predominance of peridinioid dinocysts in this interval, namely O. verrucosum, O. scabrosum and especially P. infusorioides is considered to reflect eutrophic conditions. It coincides with the increased phosphorus mass accumulation occurring at the top part of the Upper Albian Dekov Formation. OAE 1d is indicated in the Tolovitsa karst spring section, based on palynofacies dominated by high amounts of granular amorphous organic matter (AOM) related to anoxic environmental conditions. These sections serve as evidence suggesting a relationship between Cretaceous peridinioid cysts (including Palaeohystichphora infusorioides, Ovoidinium verrucosum, O. scabrosum) and anoxic/suboxic conditions and/or high primary productivity. The pollen spectrum inferred relatively stable vegetation patterns of surrounding continental areas during and after the Albian/Cenomanian boundary interval and the times of OAE 1d formation. The hinterland vegetation integrated mainly pteridophyte spores and gymnosperms. The area was part of the Southern Laurasian floral province which was characterized by warm temperate to subtropical humid climate. Angiosperms were still minor part of this vegetation.	[Pavlishina, Polina] Univ Sofia, Dept Geol Palaeontol & Fossil Fuels, 15 Tzar Osvoboditel Bd, Sofia 1000, Bulgaria	University of Sofia	Pavlishina, P (通讯作者)，Univ Sofia, Dept Geol Palaeontol & Fossil Fuels, 15 Tzar Osvoboditel Bd, Sofia 1000, Bulgaria.	polina@gea.uni-sofia.bg	Pavlishina, Polina/AAL-5710-2021	Pavlishina, Polina/0000-0002-1172-9142	IGCP Project [609]	IGCP Project	I would like to express my gratitude to both reviewers for their constructive comments and useful suggestions. Special thanks are due to Michael Wagreich (University of Vienna) who made important suggestions for improving the manuscript and kindly corrected my English. I am also grateful to R. Scott (University of Tulsa) for his final support and valuable remarks. This work was carried out in the frame of the IGCP Project 609 "Climate-environmental deteriorations during greenhouse phases: Causes and consequences of short-term Cretaceous sea-level changes".	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China-Earth Sci.	JAN	2017	60	1					71	79		10.1007/s11430-016-0067-2	http://dx.doi.org/10.1007/s11430-016-0067-2			9	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology	EI1AN					2025-03-11	WOS:000392207400007
J	Wang, WH; Monnet, C; Servais, T				Wang, Wenhui; Monnet, Claude; Servais, Thomas			Quantitative methods used for understanding the taxonomy of acritarchs: a case study of the Middle Ordovician genus <i>Frankea</i> Burmann 1970	PALYNOLOGY			English	Article						Frankea; acritarchs; taxonomy; quantitative methods; intraspecific variation; morphometrics; ecophenotypism	DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; PROCESS LENGTH VARIATION; SEDIMENTS; SALINITY; CYST	The triangular-shaped acritarch genus Frankea, which displays characteristically branched appendices, has considerable stratigraphical and palaeobiogeographical significance in the Ordovician. High intraspecific variability of terminal processes (appendices) numbers and process lengths within Frankea suggest that the genus could be suitable for use in studying the relationship between morphological characters and environmental conditions. Quantitative multivariate exploratory analyses on Frankea indicate that the length of the appendices varies according to different localities and is most probably ecologically dependent and not age diagnostic as previously suggested. Principal components analyses and discriminant analyses are used to assess the original specific classification of Frankea. The morphometric analyses suggest that usage of quantitative characters, such as the process length, should be taken into consideration during the separation of species. A comprehensive discussion of qualitative and quantitative characters is carried out and suggests there are only three species of Frankea: F. hamata, F. hamulata and F. sartbernardensis.	[Wang, Wenhui] Cent South Univ, Sch Geosci & Infophys, Key Lab Metallogen Predict Nonferrous Met & Geol, Minist Educ, Changsha 410083, Hunan, Peoples R China; [Wang, Wenhui; Monnet, Claude; Servais, Thomas] Univ Lille, CNRS, UMR Evo Eco Paleo 8198, F-59000 Lille, France; [Servais, Thomas] Univ Durham, Van Mildert Coll, Cosins Hall, Durham DH1 3RL, England; [Servais, Thomas] Univ Durham, Inst Adv Study, Cosins Hall, Durham DH1 3RL, England; [Wang, Wenhui] Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen, Peoples R China	Central South University; Universite de Lille; Centre National de la Recherche Scientifique (CNRS); Durham University; Durham University; Xiamen University	Wang, WH (通讯作者)，Cent South Univ, Sch Geosci & Infophys, Key Lab Metallogen Predict Nonferrous Met & Geol, Minist Educ, Changsha 410083, Hunan, Peoples R China.; Wang, WH (通讯作者)，Univ Lille, CNRS, UMR Evo Eco Paleo 8198, F-59000 Lille, France.	wwhever@126.com	Wang, Wenhui/K-1512-2016; Monnet, Claude/F-8498-2010; Servais, Thomas/S-8045-2019; Servais, Thomas/I-2115-2018	Servais, Thomas/0000-0002-4089-7874	National Natural Science Foundation of China [41172001, 41402010]; MEL Visiting Fellowship [MELRS1709]; Youth Foundation of Jiangsu Province, China [BK20140602]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); MEL Visiting Fellowship; Youth Foundation of Jiangsu Province, China	Financial support from the National Natural Science Foundation of China [grant number 41172001], [grant number 41402010]; MEL Visiting Fellowship [grant number MELRS1709]; and Youth Foundation of Jiangsu Province, China [grant number BK20140602] is greatly acknowledged.	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J	Benson, DG; Miller, MA; Wood, GD				Benson, Don G., Jr.; Miller, Merrell A.; Wood, Gordon D.			A new Upper Jurassic species of <i>Scenedesmus</i> from the Bossier Formation, Texas, USA	PALYNOLOGY			English	Article						Scenedesmus; Upper Jurassic; Texas Gulf Coast; Bossier Formation	PEDIASTRUM; ACRITARCHS; SEDIMENTS; MEXICO; BASIN; ALGAE	Scenedesmus Meyen 1829 is an extant freshwater representative of the Chlorophyta (Order Chlorococcales, Family Scenedesmaceae). Fossil representatives have been conclusively identified from Lower Cretaceous lacustrine sediments and some are possibly as old as the Middle Jurassic. Specimens clearly attributable to Scenedesmus were encountered in Upper Jurassic Bossier Formation palynology preparations from a proprietary hydrocarbon exploration well in Wood County, Texas, USA. This alga, named Scenedesmus texanus sp. nov., is described herein. Also occurring with Scenedesmus are other freshwater representatives of the Chlorococcales, including Tetrastrum multifilorum and Pediastrum sp. The Bossier Formation Scenedesmus specimens occur in a mixed palynological assemblage consisting of freshwater algae, pollen, spores and a few dinoflagellate cysts. The combined occurrence of these palynomorphs indicates a marginal marine depositional setting with a freshwater influence.	[Benson, Don G., Jr.] Irf Grp Inc, 1522 Ehlinger Rd, Fayetteville, TX 78940 USA; [Miller, Merrell A.] Irf Grp Inc, 2753 East 23rd St, Tulsa, OK 74114 USA; [Miller, Merrell A.] Univ Tulsa, Dept Geosci, 800 South Tucker Dr, Tulsa, OK 74104 USA; [Wood, Gordon D.] Irf Grp Inc, Katy, TX USA	University of Tulsa	Benson, DG (通讯作者)，Irf Grp Inc, 1522 Ehlinger Rd, Fayetteville, TX 78940 USA.	dbenson308@gmail.com		Miller, Merrell/0000-0002-6046-4283				[Anonymous], 845 BUR EC GEOL; [Anonymous], 1980, PALEOBIOLOGY PLANT P; 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; Batten DJ., 1996, Palynology: principles and applications, P191; Benson Jr DG, 1999, PALYNOLOGY, V23, P248; Benson Jr DG, 2002, PALYNOLOGY, V26, P261; BRENNER W, 1994, REV PALAEOBOT PALYNO, V80, P209, DOI 10.1016/0034-6667(94)90002-7; Burgess W.J., 1976, Trans. 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D., 1997, AFRICA GEOSCIENCE RE, V4, P499; Wood GD, 1998, NORGES TEKNISK NATUR, P148; Wood GD, 1997, 9 C PER GEOL SOC GEO, V1, P597; Wood GD, 1996, ACRITARCHS PRAHA 199, V40, P703; Wood Gordon D., 2000, Palynology, V24, P9, DOI 10.2113/0240009; Zavattieri AM, 2008, J S AM EARTH SCI, V25, P227, DOI 10.1016/j.jsames.2007.06.006; Zippi Pierre A., 1998, Micropaleontology (New York), V44, P1, DOI 10.2307/1485998	45	3	3	0	3	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41			1	SI		262	270		10.1080/01916122.2017.1360632	http://dx.doi.org/10.1080/01916122.2017.1360632			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FX9TR					2025-03-11	WOS:000426450100017
J	Ravn, RL; Goodman, DK				Ravn, Robert L.; Goodman, David K.			Two new marine cyst genera from Upper Cretaceous Brookian megasequence strata in the North Slope of Alaska	PALYNOLOGY			English	Article						New dinoflagellate taxa; Alaska North Slope; Upper Cretaceous; biostratigraphy		Two new genera, comprising three new species, of marine algal cysts are described here. The extinction horizons of all three occur with a high degree of consistency in many petroleum wells in the Alaska North Slope region. These horizons provide useful correlation events within the overall progradational sediments which filled a large and complex depositional basin during Cenomanian-Turonian time. The newly described taxa are Paranelsoniella woodii gen. et sp. nov., P. minuta gen. et sp. nov. and Xanthocysta ovata gen. et sp. nov.	[Ravn, Robert L.] Irf Grp Inc, 2001 Shale Circle Anchorage, Anchorage, AK 99507 USA; [Ravn, Robert L.] Univ Alaska Anchorage, 2001 Shale Circle Anchorage, Anchorage, AK 99507 USA; [Goodman, David K.] Irf Grp Inc, 6720 Round Tree Dr, Anchorage, AK 99507 USA	University of Alaska System; University of Alaska Anchorage	Ravn, RL (通讯作者)，Irf Grp Inc, 2001 Shale Circle Anchorage, Anchorage, AK 99507 USA.; Ravn, RL (通讯作者)，Univ Alaska Anchorage, 2001 Shale Circle Anchorage, Anchorage, AK 99507 USA.	rraven777@hotmail.com						COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; Decker P., 2007, 20072 AL DIV GEOL GE, P1; DOERENKAMP A, 1976, Bulletin of Canadian Petroleum Geology, V24, P372; Evitt W.R., 1985, SPOROPOLLENIN DINOFL, P1; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Hubbard RJ, 1987, ALASKAN N SLOPE GEOL, V2, P797; McIntyre D.J., 1974, GEOLOGICAL SURVEY CA, P1; McIntyre D.J., 1975, Geoscience and Man, V11, P61, DOI DOI 10.1080/00721395.1975.9989756; Mull CG, 2004, US GEOLOGICAL SURVEY, P1	9	0	0	0	1	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41			1	SI		271	277		10.1080/01916122.2017.1360623	http://dx.doi.org/10.1080/01916122.2017.1360623			7	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FX9TR					2025-03-11	WOS:000426450100018
J	Goodman, DK				Goodman, David K.			Tabulation patterns in some fossil representatives of the dinoflagellate family Cladopyxiaceae Stein 1883	PALYNOLOGY			English	Article						Dinoflagellate; tabulation patterns; morphology	CYST	Several fossil dinoflagellates assignable to Microdinium, Histiocysta and Cladopyxidium are small, yet distinctive subspheroidal to ellipsoidal forms that share several discriminative morphological features. The epicyst is smaller than the hypocyst, and the cingulum, which is only slightly offset ventrally, is exceptionally wide. The specimens all have apical archeopyles and possess sutural features indicating a gonyaulacalean tabulation of 4', 3-5a, 7 '', 6c, 6''', 1p, 1'''', and 5-6s. However, the proportions and shapes of some plates and their relative positions differ significantly from plate relationships on other gonyaulacalean genera having similar tabulation formulas. The differences pertain mainly to the hypocyst, but on some forms modification of certain plates on the epicyst is also involved. Point-by-point comparison of comparable features emphasises the morphological similarities within this group, accentuates dissimilarities between them, and highlights the major differences between them and other fossil cysts having a similar tabulation formula. Extant cysts with a comparable tabulation are unknown.	[Goodman, David K.] Irf Grp Inc, 6721 Round Tree Dr, Anchorage, AK 99507 USA		Goodman, DK (通讯作者)，Irf Grp Inc, 6721 Round Tree Dr, Anchorage, AK 99507 USA.	theirfgroup@alaska.net						[Anonymous], 1985, SPOROPOLLENIN DINOFL; Balech E., 1967, Neotropica, V13, P105; Balech E., 1964, COMUNIC MUS ARG CS N, V1, P27; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; Clowes CD, 2013, PALYNOLOGY, V37, P316, DOI 10.1080/01916122.2013.775007; Cookson I.C., 1971, P ROY SOC VIC, V84, P217; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; Fensome R.A., 1993, Micropaleontology Press Special Paper; Goodman DK., 1979, Palynology, V3, P169; Lentin J.K., 1989, American Association of Stratigraphic Palynologists, Contributions Series, V20; MAY F E, 1980, Palaeontographica Abteilung B Palaeophytologie, V172, P10; McLean D.M., 1974, Geoscience Man, V9, P76; MCLEAN DM, 1972, J PALEONTOL, V46, P861; Slimani H, 2011, REV PALAEOBOT PALYNO, V168, P41, DOI 10.1016/j.revpalbo.2011.09.009; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4	18	4	4	1	1	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41			1	SI		290	308		10.1080/01916122.2017.1361246	http://dx.doi.org/10.1080/01916122.2017.1361246			19	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FX9TR					2025-03-11	WOS:000426450100020
J	Filipek, A; Wysocka, A; Barski, M				Filipek, Anna; Wysocka, Anna; Barski, Marcin			Depositional setting of the Oligocene sequence of the Western Carpathians in the Polish Spisz region - a reinterpretation based on integrated palynofacies and sedimentological analyses	GEOLOGICAL QUARTERLY			English	Article						wind-influenced turbidites; palynofacies; Oligocene; Central Carpathian Paleogene Basin; Carpathians	PIENINY KLIPPEN BELT; TURBIDITY CURRENTS; BASIN; POLAND; EVOLUTION; SLOVAKIA; HISTORY	The research on the Oligocene succession of the Central Carpathian Paleogene Basin (CCPB) in the Kacwin region focused on sedimentological and palynofacies analyses. Observations were carried out in natural exposures along three streams flowing in the Polish Spisz: Kacwinianka, Lapszanka and Kacwinski. Three main groups of lithofacies have been distinguished: coarse-grained, mixed and sandy-grained, and fine-grained. The lithofacies are characterized by variable sedimentary structures, e.g. massive structure, horizontal lamination, ripple cross-lamination, hummocky cross-stratification, deformation structure. Sedimentological analyses showed that structures typical for turbidity currents and those characteristic of relatively shallow deposition (HCS, wave ripples) could coexist in the investigated succession interpreted as typical for turbidity currents influenced by storm waves. This indicates relatively shallow-water environments. The palynofacies analysis enabled identification of the following components: black wood, brown wood, cortex, resin, sporomorphs, cuticle, algae, dinoflagellates and AOM. A high proportion of black wood and low diversity of components point to an origin related to turbidity currents. Furthermore, results of the palynofacies analysis have allowed determining that, during the deposition of the CCPB sediments in the Polish Spisz area, the distance between the deposition area and the source area became relatively large. The biostratigraphic analysis of dinoflagellate cysts from the Podhale Basin (Szaflary, Zakopane, and lower Chocholow beds) indicates an Early Rupelian age. Moreover, kerogen analysis in the UV was applied for the first time to study the CCPB succession. As a result, reworking was documented, so far unrecognized by other methods, and the mutual verification of the obtained results was possible.	[Filipek, Anna; Wysocka, Anna; Barski, Marcin] Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland	University of Warsaw	Filipek, A (通讯作者)，Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	anniafilipek@gmail.com	Filipek, Anna/KFT-3536-2024	Barski, Marcin/0000-0002-4102-3538; Filipek, Anna/0000-0003-2861-4058; Wysocka, Anna/0000-0003-1015-5033	National Science Centre (NCN) [2011/01/B/ST10/07591]	National Science Centre (NCN)	Cordial thanks are offered to the reviewers, Prof. J. Sotak (Geological Institute, Slovak Academy of Science, Banska Bystrica) and Anonymous Reviewer, whose constructive remarks have significantly improved the content of the paper. Furthermore, the authors thank M. Rogalski for help in field works. The study was financed by the National Science Centre (NCN) grant No. 2011/01/B/ST10/07591.	Alexandrowicz S. 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Q.		2017	61	4					859	876		10.7306/gq.1382	http://dx.doi.org/10.7306/gq.1382			18	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FU6AG		gold			2025-03-11	WOS:000423933500011
J	Ciurej, A; Bak, K; Bak, M				Ciurej, Agnieszka; Bak, Krzysztof; Bak, Marta			Late Albian calcareous dinocysts and calcitarchs record linked to environmental changes during the final phase of OAE 1d-a case study from the Tatra Mountains, Central Western Carpathians	GEOLOGICAL QUARTERLY			English	Article						calcareous dinocysts; calcitarchs; nutrient input and sea level fluctuations; Upper Albian; OAE 1d; Tatra Mountains	PIENINY KLIPPEN BELT; DINOFLAGELLATE CYSTS; BOUNDARY INTERVAL; PALEOENVIRONMENTAL CHANGES; CARBONATE PLATFORM; RECONSTRUCTION; STRATIGRAPHY; BASIN; EVENT; PALEOECOLOGY	Calcareous dinocysts and calcitarchs have been investigated for the first time within the Upper Albian limestone and marl succession of the Zabijak Formation from the High-Tatric Unit in the Tatra Mountains (Central Western Carpathians), related to the Oceanic Anoxic Event 1d (OAE 1d). Four groups of morphotaxa of calcareous dinocysts have been distinguished. They totally dominate the assemblages, and belong to the pithonellids. They are represented by Pithonella sphaerica (Kaufmann in Heer) and P. ovalis (Kaufmann in Heer), which dominate, as well as P. trejoi Bonet and P. lamellata Keupp in Keupp and Kienel, which are less abundant. Two other morphotaxa, Colomisphaera gigantea (Borza) and Cadosina oraviensis Borza, occur sporadically in the assemblages. Both forms represent the calcitarch group, which assembled calcispheres of unknown taxonomic affinity. The calcareous dinocyst and calcitarch diversity is low to moderate, compared to the general species richness known from Late Albian assemblages in other Western Tethyan sections. This is interpreted as a result of nutrient input fluctuations due to changes in the circulation pattern of surface and intermediate waters. The changes in the P. sphaerica/P. ovalis ratio along the Upper Albian section are here correlated with short-term (third-order) sea level fluctuations including transgressive and regressive events and a highstand. Pelletization processes might have influenced cyst abundance on the sea floor, especially during periods with oligotrophic surface waters.	[Ciurej, Agnieszka; Bak, Krzysztof] Pedag Univ Cracow, Inst Geog, Podchorazych 2, PL-30084 Krakow, Poland; [Bak, Marta] AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Al Mickiewicza 30, PL-30059 Krakow, Poland	University of the National Education Commission; AGH University of Krakow	Bak, K (通讯作者)，Pedag Univ Cracow, Inst Geog, Podchorazych 2, PL-30084 Krakow, Poland.	sgbak@cyf-kr.edu.pl	Ciurej, Agnieszka/HNS-7682-2023; Bak, Marta/A-5748-2017; Bak, Krzysztof/T-5842-2018	Ciurej, Agnieszka/0000-0002-2383-7562; Bak, Marta/0000-0001-9329-3540; Bak, Krzysztof/0000-0002-9199-3129	Ministry of Science and Higher Education [4n, 11.11.140.005]; National Science Centre [2011/01/B/ST10/07405]	Ministry of Science and Higher Education; National Science Centre(National Science Centre, Poland)	The study was supported by the Ministry of Science and Higher Education to A. Ciurej (Project DS-UP-WGB No. 4n), by the National Science Centre to K. Bak (grant 2011/01/B/ST10/07405), and by the Ministry of Science and Higher Education to M. Bak (Project DS-AGH University of Science and Technology, WGGiOS-KGOiG no. 11.11.140.005). The authors are grateful to J. Wendler, D. Rehakova and an anonymous reviewer for their helpful remarks. Special thanks go to K. Leszczynski for improving the English text.	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Q.		2017	61	4					887	895		10.7306/gq.1379	http://dx.doi.org/10.7306/gq.1379			9	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FU6AG		gold			2025-03-11	WOS:000423933500013
J	Gao, YC; Dong, YH; Li, HT; Zhan, AB				Gao, Yangchun; Dong, Yanhong; Li, Haitao; Zhan, Aibin			Harmful non-indigenous dinoflagellate cysts in China: A review	AQUATIC ECOSYSTEM HEALTH & MANAGEMENT			English	Article; Proceedings Paper	Conference on Marine and Freshwater Invasive Species - Ecology, Impact, and Management (MFIS)	MAY 02-04, 2016	Buenos Aires, ARGENTINA	Aquat Ecosyst Hlth & Management Soc, Argentine Consejo Nacl Investigaciones Cientifica & Tecnics, Canfornav Inc		biological invasion; metabarcoding; molecular identification; morphological identification	PHYLOGENETIC-RELATIONSHIPS; ALEXANDRIUM-TAMARENSE; DINOPHYCEAE; MORPHOLOGY; DIVERSITY; SEDIMENTS; COAST; TRANSPORT; ASSAY; SEA	Harmful dinoflagellate cysts (e.g. dinocysts) represent a great threat to marine and coastal ecosystems and even human health. As dinocysts have resistant cell walls that allow dinoflagellate species to successfully survive harsh environments, they can easily pass through multiple barriers during biological invasions and successfully colonize new locations. In introduced ranges, dinocysts often serve as seeds for harmful algal blooms, which can result in large-scale environmental disasters and economic losses. Correct identification of dinocysts represents the first step for both ecological studies and management programs. However, traditional methods, which are based on morphological observations, pose great technical challenges for dinocysts. Recent advances in molecular techniques, such as high-throughput sequencing-based metabarcoding, have tremendously revolutionized our abilities to detect marine biodiversity. Here, we summarize species composition of non-indigenous/cryptogenic dinocysts and their identification methods commonly used in China, discuss major problems in traditional morphological identification and technical issues of molecular identification, and finally propose future perspectives for the efficient identification of non-indigenous dinocysts using high-throughput sequencing-based metabarcoding. We also discuss technical issues that should be addressed before high-throughput sequencing-based metabarcoding can be widely used for dinocyst identification at large geographical scales.	[Gao, Yangchun; Zhan, Aibin] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, 18 Shuangqing Rd, Beijing 100085, Peoples R China; [Gao, Yangchun; Zhan, Aibin] Univ Chinese Acad Sci, Chinese Acad Sci, 19A Yuquan Rd, Beijing 100049, Peoples R China; [Dong, Yanhong; Li, Haitao] State Ocean Adm, South China Sea Environm Monitoring Ctr, 155 Xingang Rd West, Guangzhou 510300, Guangdong, Peoples R China	Chinese Academy of Sciences; Research Center for Eco-Environmental Sciences (RCEES); Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Zhan, AB (通讯作者)，Chinese Acad Sci, Res Ctr Ecoenvironm Sci, 18 Shuangqing Rd, Beijing 100085, Peoples R China.; Zhan, AB (通讯作者)，Univ Chinese Acad Sci, Chinese Acad Sci, 19A Yuquan Rd, Beijing 100049, Peoples R China.	zhanaibin@hotmail.com	Zhan, Aibin/A-7240-2011; 高, 养春/ITT-9176-2023		100-Talent Program of the Chinese Academy of Sciences (CAS); Key Laboratory of Environmental Biotechnology of the Chinese Academy of Sciences [Kf2013002]	100-Talent Program of the Chinese Academy of Sciences (CAS); Key Laboratory of Environmental Biotechnology of the Chinese Academy of Sciences	This work was supported by 100-Talent Program of the Chinese Academy of Sciences (CAS) to AZ and a special fund from the Key Laboratory of Environmental Biotechnology of the Chinese Academy of Sciences (Kf2013002) to HL.	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Ecosyst. Health Manag.		2017	20	4			SI		413	422		10.1080/14634988.2017.1403269	http://dx.doi.org/10.1080/14634988.2017.1403269			10	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	FT3ZO					2025-03-11	WOS:000423091000012
J	Estebenet, MSG; Cereceda, A; Guler, MV				Gonzalez Estebenet, M. Sol; Cereceda, Abril; Veronica Guler, M.			LATE CRETACEOUS ORGANIC-WALLED DINOFLAGELLATE CYSTS FROM THE ALTA VISTA FORMATION, AUSTRAL BASIN, ARGENTINA	AMEGHINIANA			English	Article						Paleomicroplankton; Biostratigraphy; Campanian; Patagonia; South America	ANTARCTIC PENINSULA; MAGALLANES BASIN; PATAGONIAN-ANDES; NEW-ZEALAND; ISLAND; STRATIGRAPHY; BIOSTRATIGRAPHY; SEDIMENTOLOGY; PALYNOLOGY; ZONATION	The Alta Vista Formation represents one of the first Late Cretaceous marine deposits accumulated during the foreland stage of the Austral Basin, Patagonia. All the analyzed samples contain dinoflagellate cysts denoting marine conditions throughout the unit and, despite the extremely poor preservation of the assemblages, diagnostic species were identified. The age of the Alta Vista Formation was assigned between the late Santonian and the late Campanian based on the invertebrate remains. Nevertheless, the age is still debatable and a detailed biostratigraphy has not been proposed for the unit so far. As in other Late Cretaceous Southern Hemisphere middle to high latitude successions, the dinoflagellate cysts from the Alta Vista Formation are useful for biostratigraphic interpretations. The co-occurrence of Odontochitina porifera, Palaeohystrichophora infusorioides, Nelsoniella aceras, Nelsoniella tuberculata and Xenikoon australis is consistent with a Campanian age, which in accordance with the age indicated by the invertebrates recorded in other localities in which the unit crops out. The occurrence of Xenikoon australis and Nelsoniella tuberculata constrains the age of the unit to the early-middle Campanian. Since the basal levels were not identified in the studied sections, the age herein suggested corresponds to the upper part of the Alta Vista Formation.	[Gonzalez Estebenet, M. Sol; Veronica Guler, M.] UNS, Dept Geol, Inst Geol Sur, Alem 1253 Cuerpo B 1 Piso,B8000CPB, Bahia Blanca, Buenos Aires, Argentina; [Cereceda, Abril] Univ Nacl La Plata, CONICET, Ctr Invest Geol, Diagonal 113 275, RA-1900 La Plata, Buenos Aires, Argentina	National University of the South; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of La Plata	Estebenet, MSG (通讯作者)，UNS, Dept Geol, Inst Geol Sur, Alem 1253 Cuerpo B 1 Piso,B8000CPB, Bahia Blanca, Buenos Aires, Argentina.	sol.gonzalezestebenet@uns.edu.ar; acereceda@cig.museo.unlp.edu.ar; vguler@criba.edu.ar			 [PIP-CONICET 02047]		The authors thank G. Holfeltz for his palynological technical assistance. The anonymous reviewers are thanked because their valuable suggestions improved the manuscript. This contribution was partially financed by grant PIP-CONICET 02047.	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J	Masure, E; Jha, N; Duarte, SG; Aggarwal, N; Arai, M; Joshi, H				Masure, Edwige; Jha, Neerja; Duarte, Sarah Goncalves; Aggarwal, Neha; Arai, Mitsuru; Joshi, Harinam			Influence of palaeoenvironmental factors on the encystment of Cretaceous dinoflagellate cysts (Ceratiaceae): a study from Godavari Graben, Southern India	PALYNOLOGY			English	Article						Dinoflagellate cysts; Ceratiaceae; Muderongia; India; Cretaceous	DINOPHYCEAE; REVISION	Muderongia staurota forms with long appendages at the distal end of the apical, lateral and antapical horns have been recovered from the Lower Cretaceous Gangapur Formation of Upper Gondwana sequence from the Chintalapudi Sub-Basin (India). The number of distal appendages reflects the number of plates forming the horns. We include these forms in the new species Muderongia gangapurensis sp. nov. The dinoflagellate cysts recovered suggest a late Berriasian to Valanginian for the lower part and a Hauterivian/Barremian age for the upper part of the studied interval of MJR-11 borehole. Unusual Muderongia and Odontochitina cysts bearing similar long appendages have only occasionally been described or illustrated in the literature from sediments rich in continental organic matter. We suggest that Cretaceous Ceratiaceae bearing such appendages are cysts of thecae that encysted in particular environments, where light, salinity, temperature and chemistry of water masses might have been key to their development. Our conclusion is supported by the high morphological variability of horns in modern Ceratiaceae, which reflects environmental factors. We discuss the plasticity of horns in the fossil record and note that such plasticity is recurring in Ceratiaceae, at least in the Early Cretaceous (145 Ma).	[Masure, Edwige] Univ Paris 06, CR2P, UMR 7207, MNHN,UPMC,CNRS, 4 Pl Jussieu, F-75005 Paris, France; [Jha, Neerja; Aggarwal, Neha; Joshi, Harinam] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow, Uttar Pradesh, India; [Duarte, Sarah Goncalves] Univ Fed Rio de Janeiro, Maths & Nat Sci Ctr, Dept Geol, 274 Av Athos da Silveira Ramos, BR-21949916 Rio de Janeiro, Ilha Do Fundao, Brazil; [Arai, Mitsuru] Sao Paulo State Univ, UNESP, IGCE, UNESPetro, BR-13501070 Rio Claro, SP, Brazil	Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Universidade Federal do Rio de Janeiro; Universidade Estadual Paulista	Masure, E (通讯作者)，Univ Paris 06, CR2P, UMR 7207, MNHN,UPMC,CNRS, 4 Pl Jussieu, F-75005 Paris, France.	edwige.masure@upmc.fr		Arai, Mitsuru/0000-0002-8932-0080				[Anonymous], 1980, Palaeontology; [Anonymous], 1982, PALAEOBOTANIST; [Anonymous], 1954, PUBL I BIOL APL; [Anonymous], 1885, HG BRONNS KLASSEN OR; Balech E., 1988, DINOFLAGELADOS ATL A, V1, P310; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; Bharadwaj D. C., 1964, The Palaeobotanist, V12, P181; BINT A N, 1986, Palynology, V10, P135; Cleve P T., 1900, KONGLIGA SVENSKA VET, V34, P1; Costa L.I., 1992, P99; DOWIDAR NM, 1972, MAR BIOL, V16, P138; Duane Ailbhe M., 1997, Palynology, V21, P123; El-Mehdawi AD, 1998, J MICROPALAEONTOL, V17, P173, DOI 10.1144/jm.17.2.173; Entz G, 1925, ARCH PROTISTENKD, V58, P131; Evitt W.R., 1985, Sporopollenin dinoflagellate cysts: their morphology and interpretation, P333; Fensome R.A., 1993, Micropaleontology Press Special Paper; Garg R, 1987, PALEOBOTANIST, V36, P257; Gómez F, 2010, PROTIST, V161, P35, DOI 10.1016/j.protis.2009.06.004; Gran H. H., 1902, Report Norwegian Fishery Investigations, Vii, P1; HARDING IC, 1990, REV PALAEOBOT PALYNO, V65, P311, DOI 10.1016/0034-6667(90)90081-S; Helby R., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P297; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Jain KP., 1977, PALEOBOTANIST, V24, P170; Jha N, 2016, PALAEOWORLD; Khowaja-Ateequzzaman, 1992, Geophytology, V22, P133; KOFOID CA, 2009, B MUS COMP ZOOL HARV, V52, P213; Kofoid Charles Atwood, 1907, Zoologischer Anzeiger Leipzig, V32; LAKSHMINARAYANA G, 1990, J GEOL SOC INDIA, V36, P13; Mao SZ, 1999, GRANA, V38, P144, DOI 10.1080/713786923; Monteil E, 1991, B CTR RECHERCHE EXPL, V15, P465; Muller OF, 1786, ANIMACULA INFUSORIA, P544; Nielsen J., 1956, Oikos, V7, P256, DOI 10.2307/3564926; Núñez-Betelu K, 1998, CAN J EARTH SCI, V35, P923, DOI 10.1139/e98-044; OSTENFELD C.H., 1903, BOT FAEROES PART 2 C, P558; Paulsen O., 1908, Botanischer Teil, V18, P1; Pizay MD, 2009, PROTIST, V160, P565, DOI 10.1016/j.protis.2009.04.003; SCHRANK F.VON PAULA., 1793, NATUFFORSCHER, V27, P26; SOURNIA A, 1984, PHYCOLOGIA, V23, P345, DOI 10.2216/i0031-8884-23-3-345.1; SOURNIA A, 1967, VIE MILIEU A BIOL MA, V18, P375; Sournia A., 1986, Introduction, Cyanophycees, Dictyophycees, Raphidophycees, P219; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; SUKH-DEV, 1988, Geophytology, V18, P1; Taylor F.J.R., 1987, Botanical Monographs (Oxford), V21, P24; Temponeras M, 2000, HYDROBIOLOGIA, V424, P101, DOI 10.1023/A:1003957129071; Tunin-Ley Alina, 2013, Microorganisms, V1, P58; Vanhoffen E., 1896, Zoologischer Anzeiger, Vxix, P134; Vijaya, 1999, CRETACEOUS RES, V20, P597, DOI 10.1006/cres.1999.0169; Wall D., 1975, Micropalaeontology, V21, P14, DOI 10.2307/1485153; Willey A., 1909, TREATISE ZOOLOGY 1, P154; WILLIAMS G.L., 1978, INITIAL REPORTT FHE, P783	50	5	5	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41	4					472	483		10.1080/01916122.2016.1262922	http://dx.doi.org/10.1080/01916122.2016.1262922			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FK5VW		Green Published			2025-03-11	WOS:000413571400004
J	McCarthy, FMG; Drljepan, M; Hubeny, JB; Krueger, AM; Pilkington, PM; Riddick, NL; MacKinnon, MD				McCarthy, Francine M. G.; Drljepan, Matea; Hubeny, J. Bradford; Krueger, Andrea M.; Pilkington, Paul Michael; Riddick, Nicholas L.; MacKinnon, Michael D.			The influence of dissolved oxygen on dinoflagellate cyst distribution across Sluice Pond, a meromictic lake in NE Massachusetts, USA	PALYNOLOGY			English	Article						Freshwater dinoflagellate cysts; meromixis; hypoxia; taphonomy; testate amoebae; tintinnid ciliates; Holocene	THECAMOEBIANS TESTATE AMEBAS; NON-POLLEN PALYNOMORPHS; PERIDINIUM-GATUNENSE; WATER-QUALITY; PRESERVATION; INDICATORS; SEDIMENTS; KINNERET; ECOLOGY; ONTARIO	Assemblages of dinoflagellate cysts in lakebed sediments across the deep, meromictic basin of Sluice Pond (Lynn, Massachusetts) were compared with measurements of water quality and sediment geochemistry and with testate amoeba and tintinnid assemblages. Lakebed sediments below oxygenated waters (DO > 2 mg/L) contain diverse testate amoebae, but sparse Peridinium willei-dominated dinoflagellate cyst assemblages. Sediments collected under hypoxic conditions (DO < 2 mg/L) showed higher preservation of organic carbon and nitrogen, and these deep basin sediments are characterised by diverse dinoflagellate cyst assemblages, but sieved microfossil assemblages are typically dominated by the planktonic Codonella cratera and the pseudo-planktonic Cucurbitella tricuspis. Strong inverse relationships of cysts of Peridinium willei (R-2 = 0.81) and Difflugia oblonga tests (R-2 = 0.7) with water depth are attributed to variations in bottom water oxygen concentrations. Both ecological and taphonomic factors must be considered when reconstructing palaeoenvironments from microfossil assemblages.	[McCarthy, Francine M. G.; Drljepan, Matea; Krueger, Andrea M.; Pilkington, Paul Michael; Riddick, Nicholas L.] Brock Univ, Earth Sci Dept, St Catharines, ON, Canada; [Hubeny, J. Bradford] Salem State Univ, Dept Geol Sci, Salem, MA USA; [MacKinnon, Michael D.] OSPM Solut, Hamilton, ON, Canada; [Drljepan, Matea] Western Univ, Dept Earth Sci, London, ON, Canada; [Riddick, Nicholas L.] McMaster Univ, Sch Geog & Earth Sci, Hamilton, ON, Canada	Brock University; Massachusetts System of Public Higher Education; Salem State University; Western University (University of Western Ontario); McMaster University	McCarthy, FMG (通讯作者)，Brock Univ, Earth Sci Dept, St Catharines, ON, Canada.	fmccarthy@brocku.ca		Riddick, Nicholas/0009-0005-1370-6365	Natural Sciences and Engineering Research Council of Canada [DDG-2015-00037]; National Science Foundation [EAR 1126128]	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); National Science Foundation(National Science Foundation (NSF))	This work was supported by the Natural Sciences and Engineering Research Council of Canada [grant number DDG-2015-00037], and the National Science Foundation [grant number EAR 1126128].	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J	Li, Z; Oh, SJ; Park, JW; Lim, WA; Shin, HH				Li, Zhun; Oh, Seok Jin; Park, Jong-Woo; Lim, Weol-Ae; Shin, Hyeon Ho			Cyst-motile stage relationship, morphology and phylogeny of a new chain-forming, marine dinoflagellate <i>Grammatodinium tongyeonginum gen. & sp nov</i>. from Korea	PHYCOLOGIA			English	Article						Cucumeridinium; Grammatodinium; Grammatodinium tongyeonginum; LSU rDNA; morphological characteristics; resting cyst; SSU rDNA	GYMNODINIUM-CATENATUM; MICRORETICULATE CYST; RESTING CYSTS; FLAGELLAR APPARATUS; THECA RELATIONSHIP; SEQUENCE DATA; COMB.-NOV; DINOPHYCEAE; SEDIMENTS; ULTRASTRUCTURE	A new phototrophic dinoflagellate, Grammatodinium tongyeonginum gen. & sp. nov., was established by incubating resting cysts collected from surface sediment samples from Tongyeong coastal area, Korea. The resting cysts were ovoid with a large reddish pigment body and surrounded with a thick mucous layer that incorporated attached detritus particles. The vegetative cells were 24.6-40.9 mu m long and 16.4-27.3 mu m wide. The cell surface was covered with prominent longitudinal equidistant furrows. The cingulum was narrow and descended two to eight times its width. The nucleus was located at the central part of the epicone. The peripheral chloroplasts were usually granular and yellow-green in culture and were distributed along the rim of the cingulum. The horseshoe-shaped apical groove ran from the end of the sulcal extension anticlockwise around the apex. The distal end of the apical groove was located next to the extension of the sulcus and more to the ventral side than the proximal end. Molecular phylogenetic analysis using small subunit ribosomal DNA (SSU rDNA) gene sequences revealed that G. tongyeonginum was allied with the Cucumeridinium species. Large subunit ribosomal DNA (LSU rDNA) sequences revealed that G. tongyeonginum formed a clade distantly related to the other genera of Gymnodiniales. The combination of morphological characteristics with molecular phylogenies distinguished the present species from other genera within Gymnodiniales.	[Li, Zhun; Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea; [Oh, Seok Jin] Pukyong Natl Univ, Busan 48513, South Korea; [Park, Jong-Woo; Lim, Weol-Ae] Natl Inst Fisheries Sci, Busan 46083, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Pukyong National University; National Institute of Fisheries Science	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea.	shh961121@kiost.ac.kr	LI, ZHUN/GLT-3478-2022	LI, ZHUN/0000-0001-8961-9966; Shin, Hyeon Ho/0000-0002-9711-6717	Marine Biotechnology Program - Ministry of Oceans and Fisheries of Korean Government, NIFS [PE99414]; Marine Biotechnology Program - Ministry of Oceans and Fisheries of Korean Government, KIOST [PE99414]	Marine Biotechnology Program - Ministry of Oceans and Fisheries of Korean Government, NIFS; Marine Biotechnology Program - Ministry of Oceans and Fisheries of Korean Government, KIOST	This research was supported by grants from Marine Biotechnology Program Funded by Ministry of Oceans and Fisheries of Korean Government, NIFS and KIOST (PE99414) projects	ANDERSON DM, 1988, J PHYCOL, V24, P255; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P644, DOI 10.2216/07-05.1; Balech E, 1988, DINOFLAGELADOS ATLAN; Balkis N, 2016, PHYCOLOGIA, V55, P187, DOI 10.2216/15-93.1; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Darriba D, 2012, NAT METHODS, V9, P772, DOI 10.1038/nmeth.2109; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; de Salas MF, 2003, J PHYCOL, V39, P1233, DOI 10.1111/j.0022-3646.2003.03-019.x; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; Ellegaard M, 1999, PHYCOLOGIA, V38, P289, DOI 10.2216/i0031-8884-38-4-289.1; Ellegaard M, 2001, PHYCOLOGIA, V40, P542, DOI 10.2216/i0031-8884-40-6-542.1; Fensome R.A., 1993, Micropaleontology Press Special Paper; Gómez F, 2015, J PHYCOL, V51, P1088, DOI 10.1111/jpy.12346; Gómez F, 2012, SYST BIODIVERS, V10, P267, DOI 10.1080/14772000.2012.721021; Gu HF, 2015, PHYCOLOGIA, V54, P49, DOI 10.2216/14-047.1; Gu HF, 2013, HARMFUL ALGAE, V28, P97, DOI 10.1016/j.hal.2013.06.001; Guindon S, 2010, SYST BIOL, V59, P307, DOI 10.1093/sysbio/syq010; Hansen G, 2000, J PHYCOL, V36, P394, DOI 10.1046/j.1529-8817.2000.99172.x; Head M.J., 1996, Palynology: Principles and Applications, P1197; Iwataki M, 2010, J EUKARYOT MICROBIOL, V57, P308, DOI 10.1111/j.1550-7408.2010.00491.x; Jeanmougin F, 1998, TRENDS BIOCHEM SCI, V23, P403, DOI 10.1016/S0968-0004(98)01285-7; Kobayashi Satoru, 2001, Phycological Research, V49, P61, DOI 10.1046/j.1440-1835.2001.00223.x; Kofoid Charles Atwood, 1921, FREE LIVING UNARMORE; KOJIMA N, 1992, REV PALAEOBOT PALYNO, V74, P239, DOI 10.1016/0034-6667(92)90009-6; Li Z, 2015, PHYCOLOGIA, V54, P566, DOI 10.2216/15-50.1; Li Z, 2015, PHYCOLOGIA, V54, P517, DOI 10.2216/15-47.1; Li Z, 2015, PHYCOLOGIA, V54, P67, DOI 10.2216/14-080.1; Li Z, 2015, J PHYCOL, V51, P204, DOI 10.1111/jpy.12252; Liu TT, 2015, PHYCOLOGIA, V54, P210, DOI 10.2216/14-94.1; LOEBLICH ALFRED R., 1968, J PALEONTOL, V42, P210; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; MATSUOKA K, 1986, J PLANKTON RES, V8, P811, DOI 10.1093/plankt/8.4.811; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Matsuoka K, 2009, REV PALAEOBOT PALYNO, V154, P79, DOI 10.1016/j.revpalbo.2008.12.013; Mertens KN, 2011, BOREAS, V40, P242, DOI 10.1111/j.1502-3885.2010.00193.x; ORLOVA T.Y., 2003, RUSSIAN J MARINE BIO, V29, P120; Page RDM, 1996, COMPUT APPL BIOSCI, V12, P357; Qiu DJ, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0071346; REES AJJ, 1991, PHYCOLOGIA, V30, P90, DOI 10.2216/i0031-8884-30-1-90.1; Ronquist F, 2012, SYST BIOL, V61, P539, DOI 10.1093/sysbio/sys029; Saunders GW, 1997, PLANT SYST EVOL, P237; Shin HH, 2014, HARMFUL ALGAE, V39, P175, DOI 10.1016/j.hal.2014.07.012; SOURNIA A., 1986, ATLAS PHYTOPLANCTON, VI; Takano Y, 2006, J PHYCOL, V42, P251, DOI 10.1111/j.1529-8817.2006.00177.x; TAKAYAMA H, 1985, Bulletin of Plankton Society of Japan, V32, P129; Tang YZ, 2013, J PHYCOL, V49, P1084, DOI 10.1111/jpy.12114; Taylor F.J.R., 1976, BIBLIOTHECA BOT, V132, P1; Yamaguchi A, 2005, PHYCOL RES, V53, P30	49	7	7	1	7	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia		2017	56	4					430	443		10.2216/16-88.1	http://dx.doi.org/10.2216/16-88.1			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	FJ6UF					2025-03-11	WOS:000412892800008
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 VIII: life cycle, resting cyst morphology and phylogeny of <i>Tovellia rinoi sp nov</i>. (Dinophyceae)	PHYCOLOGIA			English	Article						Dinoflagellates; Life cycle; LSU rDNA; Phylogeny; Resting cyst; Tovelliaceae	RDNA-BASED PHYLOGENY; CINCTUM-F-OVOPLANUM; LSU RDNA; SEXUAL REPRODUCTION; GEN. NOV; CRYPTOPERIDINIOPSOIDS DINOPHYCEAE; PFIESTERIA-PISCICIDA; ELECTRON-MICROSCOPY; ULTRASTRUCTURE; LIGHT	Tovellia rinoi nov. sp. is described on the basis of light microscopic and scanning electron microscopic examination of motile cells and resting cysts and the phylogenetic analysis of partial sequences of the large subunit ribosomal rRNA gene. The species was isolated from a flooded area near Aveiro, Portugal, and followed in culture through all stages of the life cycle, including formation of vegetative cells and gametes, sexual fusion, planozygote division through division cysts and the production of resting cysts. Motile cells had an ovate-conical epicone and a truncated or slightly excavated hypocone and were a little flattened dorsoventrally. Cell length was mostly 9-19 mu m, the smaller cells less pigmented and with the potential to act as gametes but also capable of vegetative multiplication. The amphiesma had three series of vesicles on the epicone, one in the cingulum and two on the hypocone and an apical line of plates (ALP) oriented almost dorsoventrally across the cell apex. One vesicle separated the ALP from the cingulum on the ventral side, two on the dorsal side. The resting cysts, showing an equatorial constriction and densely covered by hair-like spines, represented a new type within the family Tovelliaceae. The new species formed a well-supported sister group to the other Tovellia species in a LSU rDNA-derived phylogeny. Sexual fusion started with gametic contact within 'dancing groups' of small cells. The initial contact on the mid-ventral side of both gametes was often visible as a hyaline bridge, which apparently involved a globular structure protruding from the ventral ridge of one or both gametes. The two gametes in a fusing pair behaved differently, with one gamete rotating as it fused into its partner until gametic eyespots merged and the gametic longitudinal flagella assumed the position of the paired longitudinal flagella of the planozygote. Resting cysts developed from large cells morphologically identifiable as planozygotes, with cyst spines growing rapidly. Conversion of planozygotes into division cysts that produced motile cells was also observed. Germinating cysts produced regularly two motile cells, each apparently with a single longitudinal flagellum. Nuclear cyclosis was not detected at any stage of the life cycle.	[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, GeoBioTec Res Unit, P-3810193 Aveiro, Portugal; [Daugbjerg, Niels; Moestrup, Ojvind] Univ Copenhagen, Dept Biol, Marine Biol Sect, Univ Pk 4, 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.; Craveiro, SC (通讯作者)，Univ Aveiro, GeoBioTec Res Unit, P-3810193 Aveiro, Portugal.	scraveiro@ua.pt	Pandeirada, Mariana/AAF-7448-2019; Daugbjerg, Niels/D-3521-2014; Pandeirada, Mariana Sofia/E-8803-2015; Calado, Sandra Carla/A-6791-2016; Calado, Antonio Jose/D-6263-2015	Daugbjerg, Niels/0000-0002-0397-3073; Pandeirada, Mariana Sofia/0000-0001-5061-9029; Calado, Sandra Carla/0000-0002-2738-7626; Calado, Antonio Jose/0000-0002-9711-0593	program POCH (Programa Operacional Capital Humano) [SFRH/BD/109016/2015]; program QREN [SFRH/BPD/68537/2010]; POPH; Formacao Avancada; European Social Funding (FSE); Portuguese Ministry of Education and Science (MEC); GeoBioTec [UID/GEO/04035/2013]; Fundação para a Ciência e a Tecnologia [SFRH/BD/109016/2015] Funding Source: FCT	program POCH (Programa Operacional Capital Humano); program QREN; POPH; 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))	M.S.P. and S.C.C. were supported by grants SFRH/BD/109016/2015 and SFRH/BPD/68537/2010, respectively, from the financing programs POCH (Programa Operacional Capital Humano) and QREN, POPH, Tipologia 4.1, Formacao Avancada, and by the European Social Funding (FSE) and the Portuguese Ministry of Education and Science (MEC). GeoBioTec (UID/GEO/04035/2013) supported this project. For molecular work we used the facilities at the Laboratory of Molecular Studies for Marine Environments (LEMAM), Univ. Aveiro, Portugal.	Accoroni S, 2014, HARMFUL ALGAE, V34, P7, DOI 10.1016/j.hal.2014.02.003; BHAUD Y, 1988, J CELL SCI, V89, P197; Bibby B.T., 1972, British phycol J, V7, P85; Bravo Isabel, 2014, Microorganisms, V2, P11; 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	Hollis, CJ; Stickley, CE; Bijl, PK; Schioler, P; Clowes, CD; Li, X; Campbell, H				Hollis, Christopher J.; Stickley, Catherine E.; Bijl, Peter K.; Schioler, Poul; Clowes, Christopher D.; Li, Xun; Campbell, Hamish			The age of the Takatika Grit, Chatham Islands, New Zealand	ALCHERINGA			English	Article						Cretaceous; Paleocene; biostratigraphy; dinoflagellates; radiolarians; diatoms; K-Pg boundary	EASTERN NEW-ZEALAND; CRETACEOUS/TERTIARY BOUNDARY; SOUTHWEST PACIFIC; PALEOENVIRONMENTAL CHANGES; SOUTHEASTERN MARLBOROUGH; DINOFLAGELLATE CYST; TERTIARY BOUNDARY; FLAXBOURNE RIVER; WOODSIDE CREEK; 1ST RECORD	The oldest Paleogene strata on Chatham Islands, east of New Zealand, are the phosphatized conglomerates and sandstones of the Takatika Grit that crops out on the northeastern coast at Tioriori and unconformably overlies the Chatham Schist. An intact Cretaceous-Paleogene boundary transition is not preserved at this locality. New biostratigraphic analysis of dinoflagellate, diatom and radiolarian microfossil assemblages confirms that the Takatika Grit is of late early-middle Paleocene (New Zealand Teurian stage) age but contains reworked microfossils of early Campanian (Early Haumurian) age. Vertebrate fossils found in this unit are inferred to be a mixture of reworked Cretaceous and in situ Paleocene bones and teeth. The overlying Tutuiri Greensand is of middle-late Paleocene age in its lower part and also contains reworked Cretaceous microfossils.	[Hollis, Christopher J.; Clowes, Christopher D.; Li, Xun; Campbell, Hamish] GNS Sci, POB 30-368, Lower Hutt 5040, New Zealand; [Stickley, Catherine E.] Evolut Appl Ltd, 50 Mitchell Way, Cheltenham GL54 2PL, Glos, England; [Bijl, Peter K.] Univ Utrecht, Marine Palynol & Paleoceanog, Dept Earth Sci, NL-3584 CS Utrecht, Netherlands; [Schioler, Poul] Morgan Goodall Palaeo, Unit 1-5 Arvida St, Malaga, WA 6090, Australia	GNS Science - New Zealand; Utrecht University	Hollis, CJ (通讯作者)，GNS Sci, POB 30-368, Lower Hutt 5040, New Zealand.	c.hollis@gns.cri.nz; catherine.stickley@gmail.com; p.k.bijl@uu.nl; poul.schioler@mgpalaeo.com.au; c.clowes@gns.cri.nz; x.li@gns.cri.nz; h.campbell@gns.cri.nz	Hollis, Christopher/D-3560-2011	Hollis, Christopher John/0000-0001-8840-9852; Bijl, Peter/0000-0002-1710-4012	GNS Science Global Change through Time Programme [540GCT62]	GNS Science Global Change through Time Programme	This work was supported by GNS Science Global Change through Time Programme [grant number 540GCT62].	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J	Poliakova, A; Zonneveld, KAF; Herbeck, LS; Jennerjahn, TC; Permana, H; Kwiatkowski, C; Behling, H				Poliakova, Anastasia; Zonneveld, Karin A. F.; Herbeck, Lucia S.; Jennerjahn, Tim C.; Permana, Haryadi; Kwiatkowski, Cornelia; Behling, Hermann			High-resolution multi-proxy reconstruction of environmental changes in coastal waters of the Java Sea, Indonesia, during the late Holocene	PALYNOLOGY			English	Article						Late Holocene; organic-walled dinoflagellate cysts; marine biogeochemistry; palaeoenvironment; SE Kalimantan; Java Sea	DINOFLAGELLATE CYST DISTRIBUTION; RADIOCARBON AGE CALIBRATION; MALAY-THAI PENINSULA; INDIAN-OCEAN; LEVEL CHANGES; MARINE-SEDIMENTS; LATE PLEISTOCENE; WEST KALIMANTAN; SOUTHEAST-ASIA; SUNDA SHELF	To obtain insight into the natural variability of the coastal ecosystems off southern Kalimantan, late Holocene environmental conditions between ca. 2850 and 990 cal yr BP in the Java Sea were investigated. A 134-cm-long sediment core collected approximate to 50 km off the Pembuang River mouth was analysed for organic-walled dinoflagellate cysts, pollen/spores and biogeochemical parameters, e.g. organic carbon (C-org), total nitrogen (N) and calcium carbonate (CaCO3) as well as carbon and nitrogen stable isotope composition (C-13, N-15). Sediments consist of mixed terrestrial as well as marine organic matter, are characterised by low nutrient uptake and suggest generally low river discharge that is supported by very low pollen and spore concentrations (256 pollen grains cm(-3) and 20 spores cm(-3) at maximum, respectively). Foraminifera and coccolithophores dominated the plankton over cyst-producing dinoflagellates and diatoms. Dinoflagellate cyst assemblages are composed mainly of oxidation-resistant species of the genera Operculodinium and Spiniferites with a minor contribution of Impagidinium (mainly I. strialatum). The percentages of round brown and peridinioid cysts are low and decrease from the bottom of the core to the top. Palynological and biogeochemical data appear well correlated and synchronously reflect changes in the marine environment. It is reconstructed that after ca. 2480 cal yr BP, bottom waters became increasingly ventilated. A typical open-water dinoflagellate cyst association is gradually replaced by a more coastal association between ca. 2480 and 1530 cal yr BP that is most likely attributed to El Nino-induced seasonal differences between dry and wet periods of the year. After 1530 cal yr BP, a more pronounced influence of the Pembuang River is indicated by an increase in N-15 and decreased C-13 which is supported by the occurrence of nutrient-sensitive Lingulodinium machaerophorum and Nematosphaeropsis labyrinthus. The overall results indicate short-scale local environment fluctuations attributed to abiotic factors.	[Poliakova, Anastasia; Behling, Hermann] Georg August Univ Gottingen, Dept Palynol & Climate Dynam, Albrecht von Haller Inst Plant Sci, Untere Karspule 2a, D-37073 Gottingen, Germany; [Zonneveld, Karin A. F.; Kwiatkowski, Cornelia] Ctr Marine Environm Sci MARUM, D-28359 Bremen, Germany; [Herbeck, Lucia S.; Jennerjahn, Tim C.] Leibniz Ctr Trop Marine Ecol ZMT, D-28359 Bremen, Germany; [Permana, Haryadi] Indonesian Inst Sci, Earthquake & Geodynam Res Grp, Res Ctr Geotechnol, Bandung 40135, Indonesia	University of Gottingen; University of Bremen; Leibniz Association; Leibniz Zentrum fur Marine Tropenforschung (ZMT); National Research & Innovation Agency of Indonesia (BRIN); Indonesian Institute of Sciences (LIPI)	Poliakova, A (通讯作者)，Georg August Univ Gottingen, Dept Palynol & Climate Dynam, Albrecht von Haller Inst Plant Sci, Untere Karspule 2a, D-37073 Gottingen, Germany.	anastasia.poliakova@biologie.uni-goettingen.de	Jennerjahn, Tim/AAE-9146-2020; Permana, Haryadi/HGB-6201-2022	Poliakova, Anastasia/0000-0001-9824-2603	German Federal Ministry of Education and Research (Bundesministerium fur Bildung und Forschung - BMBF) [03F0645B, 03F0645C]	German Federal Ministry of Education and Research (Bundesministerium fur Bildung und Forschung - BMBF)(Federal Ministry of Education & Research (BMBF))	This work was supported by the German Federal Ministry of Education and Research (Bundesministerium fur Bildung und Forschung - BMBF) [grant numbers 03F0645B and 03F0645C] for the project SPICE III - CAFINDO.	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J	Iakovleva, AI				Iakovleva, Alina I.			Did the PETM trigger the first important radiation of wetzelielloideans? Evidence from France and northern Kazakhstan	PALYNOLOGY			English	Article						Dinoflagellate cysts; wetzelielloideans; taxonomy; earliest Eocene; France; Kazakhstan; PETM	EOCENE THERMAL MAXIMUM; EARLIEST EOCENE; BIOTIC RESPONSE; PALEOCENE; CARBON; STRATIGRAPHY; RELEASE; METHANE; MARINE	Until now it was presumed that the first major expansion of the dinoflagellate cyst subfamily Wetzelielloideae occurred during the Early Ypresian, with the appearance of Dracodinium (= Wetzeliella) astra at approximate to 55 Ma, i.e. approximate to 1 My after the Paleocene/Eocene boundary and after the onset of the negative Carbon Isotope Excursion (CIE), which is coeval with the Paleocene-Eocene Thermal Maximum (PETM) event. Palynological studies of lowest Eocene sections in northern Kazakhstan (former Turgay Strait) and France (southeastern part of the former North Sea Basin) indicate that the first strong radiation of the dinoflagellate cyst subfamily Wetzelielloideae occurred in two stages: the first major diversity corresponds to the late stage of the PETM (at least 16 new taxa from seven genera) at about 55.8 Ma and the second one a little later, after the PETM (three new taxa), but probably several hundred thousand years before the first appearance of Dracodinium astra. In both geographical areas, all newly described wetzelielloideans seem to disappear before the first occurrences of Dracodinium astra and Dracodinium lobiscum. Therefore, the first important radiation of the Wetzelielloideae occurred earlier (by about 800,000 y) than was previously postulated - thus closer to 56 than to 55 Ma. New wetzelielloidean taxa include 14 new formally described species, Axiodinium sparnacium, Dracodinium? modestum, Epelidinium brinkhuisii, Epelidinium leptotoichum, Epelidinium normandiense, Petalodinium lenisium, Stichodinium elegantulum, Stichodinium galliciense, Stichodinium parisiense, Stichodinium prostimus, Stichodinium sympagicum, Vallodinium heilmannii, Vallodinium picardicum and Wilsonidium modicum. The emended diagnosis of the genus Stichodinium is proposed.	[Iakovleva, Alina I.] Russian Acad Sci, Inst Geol, Pyzhevsky Pereulok 7, Moscow 119017, Russia; [Iakovleva, Alina I.] Univ Liege, Pal Lab 3, Batiment B18,Allee Six Aout 14, B-4000 Liege, Belgium	Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; University of Liege	Iakovleva, AI (通讯作者)，Russian Acad Sci, Inst Geol, Pyzhevsky Pereulok 7, Moscow 119017, Russia.; Iakovleva, AI (通讯作者)，Univ Liege, Pal Lab 3, Batiment B18,Allee Six Aout 14, B-4000 Liege, Belgium.	alina.iakovleva@gmail.com	IAKOVLEVA, ALINA/ABH-9243-2020		Geological Institute, Russian Academy of Sciences [01201459195]; BRGM PaleoScene and 'Paleosurface 'Eocene - PETM' research projects; BRGM Regolith Scientific Program	Geological Institute, Russian Academy of Sciences; BRGM PaleoScene and 'Paleosurface 'Eocene - PETM' research projects; BRGM Regolith Scientific Program	The research of the Turgay palynological material was supported by the State project no. 01201459195 (Geological Institute, Russian Academy of Sciences). Dinoflagellate cyst study from the Paris and Dieppe-Hampshire basins was financially supported by the BRGM PaleoScene and 'Paleosurface 'Eocene - PETM' research projects and the BRGM Regolith Scientific Program.	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Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FF2RG					2025-03-11	WOS:000408743900002
J	Price, AM; Baustian, MM; Turner, RE; Rabalais, NN; Chmura, GL				Price, Andrea M.; Baustian, Melissa M.; Turner, R. Eugene; Rabalais, Nancy N.; Chmura, Gail L.			<i>Melitasphaeridium choanophorum</i> - a living fossil dinoflagellate cyst in the Gulf of Mexico	PALYNOLOGY			English	Article						Biostratigraphy; dinoflagellate cysts; Gulf of Mexico; living fossil; modern sediment; refugium	CONTINENTAL-SHELF; LATE QUATERNARY; WARM POOL; OLIGOCENE; BIOSTRATIGRAPHY; SEDIMENTS; ATLANTIC; PLIOCENE; HYPOXIA; AREA	We show the first conclusive evidence that Melitasphaeridium choanophorum, a dinoflagellate cyst species until recently considered extinct, is still living in the northern Gulf of Mexico. This suggests the Gulf of Mexico may have acted as a refugium for some warm-water dinoflagellates during past glaciations. Melitasphaeridium choanophorum can be considered a living fossil because cysts with cell contents were found among 15 of the 39 surface sediment samples analyzed from the northern Gulf of Mexico, and from five of 12 samples from a dated core (1962-1997). Melitasphaeridium choanophorum comprises a minor component of the total dinoflagellate cyst assemblages, with a maximum of 1.4% or 15 cysts g(-1). It was found in surface sediments with overlying sea-surface temperatures of 16.6 to 31.2 degrees C (winter and summer), and summer sea-surface salinities of 21.0 to 31.7 psu. The relationship of M. choanophorum with modern sea-surface conditions can be used to infer past oceanographic conditions.	[Price, Andrea M.; Chmura, Gail L.] McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ, Canada; [Baustian, Melissa M.] Water Inst Gulf, Baton Rouge, LA USA; [Turner, R. Eugene] Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA; [Rabalais, Nancy N.] Louisiana Univ Marine Consortium, Chauvin, LA 70344 USA	Louisiana State University System; Louisiana State University	Price, AM (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ, Canada.	andrea.price@mail.mcgill.ca	Rabalais, Nancy/GQA-6087-2022; Chmura, Gail/LNI-4648-2024; Baustian, Melissa/ITT-2982-2023	Price, Andrea/0000-0002-5359-053X; Rabalais, Nancy N./0000-0002-1514-837X; Chmura, Gail/0000-0001-7163-3903	Center for Sponsored Coastal Ocean Research, National Oceanic and Atmospheric Administration [NA06OP0528, NGOMEX06, NA09NOS4780230, NA09NOS4780204, NA06OP0529]; Natural Science and Engineering Research Council of Canada	Center for Sponsored Coastal Ocean Research, National Oceanic and Atmospheric Administration; Natural Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work was funded by the Center for Sponsored Coastal Ocean Research, National Oceanic and Atmospheric Administration [grant numbers NA06OP0528, NGOMEX06, NA09NOS4780230, NA09NOS4780204, and NA06OP0529], and the Natural Science and Engineering Research Council of Canada.	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H., 1986, PAPERS 1 S NEOGENE D, V17, P169; Zachos JC, 2008, NATURE, V451, P279, DOI 10.1038/nature06588; Ziegler M, 2008, NAT GEOSCI, V1, P601, DOI 10.1038/ngeo277	38	9	9	0	7	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41	3					351	358		10.1080/01916122.2016.1205676	http://dx.doi.org/10.1080/01916122.2016.1205676			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FF2RG					2025-03-11	WOS:000408743900004
J	Bijl, PK; Brinkhuis, H; Egger, LM; Eldrett, JS; Frieling, J; Grothe, A; Houben, AJP; Pross, J; Sliwinska, KK; Sluijs, A				Bijl, Peter K.; Brinkhuis, Henk; Egger, Lisa M.; Eldrett, James S.; Frieling, Joost; Grothe, Arjen; Houben, Alexander J. P.; Pross, Joerg; Sliwinska, Kasia K.; Sluijs, Appy			Comment on "<i>Wetzeliella</i> and its allies - the "hole' story: a taxonomic revision of the Paleogene dinoflagellate subfamily Wetzelielloideae' by Williams et al. (2015)	PALYNOLOGY			English	Article						Comment; taxonomic revision; dinoflagellate cyst; Wetzelielloideae; stratigraphy	SOUTHWEST PACIFIC; BIOSTRATIGRAPHY; OLIGOCENE; CLIMATE; CYSTS	The taxonomic revision of the dinoflagellate cyst subfamily Wetzelielloideae by Williams et al. (2015) places primary emphasis on the type of archaeopyle, and secondarily on wall ornamentation. Williams et al. (2015) argues that this provides more clarity for taxonomic differentiation within the subfamily of Wetzelielloideae, and adds to the stratigraphical significance of species within. We find, however, that their proposed revision (1) introduces taxonomic criteria that divert drastically from these in other dinoflagellate cyst subfamilies, (2) unnecessarily erects and emends many new genera and species, and (3) poses serious practical limitations, which together (4) lead to profound reduction of the stratigraphical applicability of many marker species. In this contribution, we substantiate our concerns regarding the approach and criteria used by Williams et al. (2015). We propose to retain the generic definitions of Wetzelielloideae that existed prior to the revisions by Williams et al. (2015), until a revision supported by the community is available.	[Bijl, Peter K.; Brinkhuis, Henk; Frieling, Joost; Grothe, Arjen; Sluijs, Appy] Univ Utrecht, Fac Geosci, Lab Palaeobot & Palynol, Marine Palynol & Paleoceanog, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, Landsdiep 4, NL-1797 SZ T Horntje, Texel, Netherlands; [Egger, Lisa M.; Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Paleoenvironm Dynam Grp, Neuenheimer Feld 234, D-69120 Heidelberg, Germany; [Eldrett, James S.] Shell Int Explorat & Prod BV, Kesslerpk 1, NL-2288 GS Rijswijk, Netherlands; [Houben, Alexander J. P.] Netherlands Org Appl Sci Res TNO, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands; [Sliwinska, Kasia K.] Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Ruprecht Karls University Heidelberg; Royal Dutch Shell; Netherlands Organization Applied Science Research; Geological Survey Of Denmark & Greenland	Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci, Lab Palaeobot & Palynol, Marine Palynol & Paleoceanog, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands.	p.k.bijl@uu.nl	Brinkhuis, Henk/IUO-8165-2023; Sluijs, Appy/B-3726-2009; Sliwinska, Kasia K./G-9097-2018	Frieling, Joost/0000-0002-5374-1625; Eldrett, James/0000-0001-5196-3112; Sluijs, Appy/0000-0003-2382-0215; Sliwinska, Kasia K./0000-0001-5488-8832; Brinkhuis, Henk/0000-0003-0253-6610; Houben, Alexander/0000-0002-9497-1048; Bijl, Peter/0000-0002-1710-4012	NWO-ALW VENI [863.13.002]; IODP Priority Program of the German Research Foundation (DFG) [PR651-16]; AASP Student Research Grant	NWO-ALW VENI(Netherlands Organization for Scientific Research (NWO)); IODP Priority Program of the German Research Foundation (DFG); AASP Student Research Grant	This work was supported by the NWO-ALW VENI [grant number 863.13.002]. L. Egger and J. Pross acknowledge financial support through the IODP Priority Program of the German Research Foundation (DFG) [grant number PR651-16], granted to J. Pross. A. Grothe acknowledges funding through the AASP Student Research Grant 2015.	Bailey D., 1987, Journal of Micropalaeontology, V6, P89; Bijl PK, 2013, EARTH-SCI REV, V124, P1, DOI 10.1016/j.earscirev.2013.04.010; Bijl PK, 2013, P NATL ACAD SCI USA, V110, P9645, DOI 10.1073/pnas.1220872110; Crouch E.M., 2003, CAUSES CONSEQUENCES, V369, P113, DOI DOI 10.1130/0-8137-2369-8.113; Dallanave E, 2016, EARTH PLANET SC LETT, V433, P380, DOI 10.1016/j.epsl.2015.11.010; Egger LM, 2016, REV PALAEOBOT PALYNO, V234, P159, DOI 10.1016/j.revpalbo.2016.08.002; Eldrett JS, 2009, MAR MICROPALEONTOL, V73, P226, DOI 10.1016/j.marmicro.2009.10.004; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; Feist-Burkhardt S, 2001, NEUES JAHRB GEOL P-A, V219, P33, DOI 10.1127/njgpa/219/2001/33; Fensome R.A., 1993, CLASSIFICATION MODER; Fensome R.A., 2008, Atlantic Geology, V44, P93, DOI DOI 10.4138/6506; Firth JV, 2013, GEOL SOC SPEC PUBL, V373, P29, DOI 10.1144/SP373.9; GOODMAN D K, 1985, Palynology, V9, P61; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; Head M.J., 1996, Palynology: Principles and Applications, P1197; Hollis CJ, 2012, EARTH PLANET SC LETT, V349, P53, DOI 10.1016/j.epsl.2012.06.024; Hollis CJ, 2009, GEOLOGY, V37, P99, DOI 10.1130/G25200A.1; ISLAM MA, 1982, REV PALAEOBOT PALYNO, V36, P305, DOI 10.1016/0034-6667(82)90025-2; Pross J, 2001, NEUES JAHRB GEOL P-A, V219, P207, DOI 10.1127/njgpa/219/2001/207; Pross J, 2010, REV PALAEOBOT PALYNO, V158, P213, DOI 10.1016/j.revpalbo.2009.09.002; Sliwinska KK, 2012, REV PALAEOBOT PALYNO, V172, P48, DOI 10.1016/j.revpalbo.2012.01.008; Sluijs A, 2007, DEEP-TIME PERSPECTIVES ON CLIMATE CHANGE: MARRYING THE SIGNAL FROM COMPUTER MODELS AND BIOLOGICAL PROXIES, P323; Sluijs A, 2009, BIOGEOSCIENCES, V6, P1755, DOI 10.5194/bg-6-1755-2009; Sluijs A, 2009, REV PALAEOBOT PALYNO, V154, P34, DOI 10.1016/j.revpalbo.2008.11.006; WALL D., 1967, PALAEONTOLOGY, V10, P95; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Williams GL, 2015, PALYNOLOGY, V39, P289, DOI 10.1080/01916122.2014.993888	27	13	14	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41	3					423	429		10.1080/01916122.2016.1235056	http://dx.doi.org/10.1080/01916122.2016.1235056			7	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FF2RG		Green Published, hybrid			2025-03-11	WOS:000408743900010
J	Williams, GL; Damassa, SP; Fensome, RA; Guerstein, GR				Williams, Graham L.; Damassa, Sarah P.; Fensome, Robert A.; Raquel Guerstein, G.			A response to "Comment to <i>Wetzeliella</i> and its allies - the "hole' story: a taxonomic revision of the Paleogene dinoflagellate subfamily Wetzelielloideae by Williams etal. (2015)'	PALYNOLOGY			English	Article						Biostratigraphy; dinoflagellate cysts; evolution; Paleogene; taxonomy; wetzelielloideans	OFFSHORE EASTERN CANADA; SCOTIAN MARGIN	The paper by Williams etal. (2015) concerning a proposed taxonomic revision of the subfamily Wetzelielloideae has led to a comment by Bijl etal. (2016) that questions the validity of our assumptions regarding recognition of the equiepeliform, latiepeliform, hyperepeliform and soleiform archaeopyle types and their significance at the generic level. In this response we address the points that they raise, which are: the introduction of taxonomic criteria allegedly not followed in other fossil subfamilies; the erection of too many taxa; the unworkable nature of the proposed classification; and the reduction of stratigraphic applicability of many significant marker species. We have organised our response under the following topics: pragmatism versus theory; generic criteria: intergroup consistency; the genus Apectodinium and operculum attachment; stratigraphic utility; the number of taxa; and recognition problems. We also discuss specimens illustrated in the two plates included with the comment. The variations in archaeopyle shapes and types of attachment of the operculum (the latter concept has been modified following more recent research) that we have used in part to separate the genera within the Wetzelielloideae have been previously applied to other peridiniacean subfamilies, most notably the Deflandreoideae. As with that subfamily, we consider that our focus on archaeopyle shape and operculum attachment for differentiating wetzelielloidean genera introduces an approach that may help refine the stratigraphic ranges of individual species. While it is a fundamental truth that there are no correct' taxonomic ideas, we consider that new approaches should be tested with usage over time, not rejected out of hand prior to careful study.	[Williams, Graham L.; Fensome, Robert A.] Geol Survey Canada Atlantic, Nat Resources Canada, Bedford Inst Oceanog, POB 1006, Dartmouth, NS B2Y 4A2, Canada; [Damassa, Sarah P.] 119 South St, Rockport, MA 01966 USA; [Raquel Guerstein, G.] Univ Nacl Sur, Dept Geol, Lab Palinol INGEOSUR, Avda Alem 1253,Cuerpo B 2do Piso, 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)，Geol Survey Canada Atlantic, Nat Resources Canada, Bedford Inst Oceanog, POB 1006, Dartmouth, NS B2Y 4A2, Canada.	rob.fensome@canada.ca		Guerstein, G. Raquel/0000-0003-1623-1084				Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Bijl PK, 2016, PALYNOLOGY; BUJAK J P, 1979, Micropaleontology (New York), V25, P308, DOI 10.2307/1485305; Bujak J.P., 1980, SPEC PAP PALAEONTOL, V24, P100; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; Costa LI., 1979, P 4 INT PAL C LUCKN, P34; DAMASSA SP, 1979, J PALEONTOL, V53, P815; Deptuck ME, 2012, CAN J EARTH SCI, V49, P1567, DOI 10.1139/e2012-075; Dybkjær K, 2004, PALAEOGEOGR PALAEOCL, V206, P41, DOI 10.1016/j.palaeo.2003.12.021; Eisenack A., 1954, Palaeontographica A, V105, P49; Evitt W.R., 1981, INT COMM PALYNOL NEW, V4, P6; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R.A., 2008, Atlantic Geology, V44, P93, DOI DOI 10.4138/6506; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42, P909; Fensome RA, 2016, BULLETIN, V36; Fensome RA, 2009, J SYST PALAEONTOL, V7, P1, DOI 10.1017/S1477201908002538; Gocht H., 1955, MONATSHEFTE, P84; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; Iakovleva KI., 2016, PALYNOLOGY IN PRESS; Lentin J.K., 1989, American Association of Stratigraphic Palynologists, Contributions Series, V20; LENTIN JK, 1989, REV PALAEOBOT PALYNO, V58, P215, DOI 10.1016/0034-6667(89)90087-0; Lentin JK, 1976, SERIES; Lentin JK, 1977, SERIES, VBI-R-77-8; MONTEIL E, 1991, B CENT RECH EXPL, V15, P461; NOhr-Hansen H, GEOLOGICAL IN PRESS; Vozzhennikova T.F., 1967, Extinct Peridinieae from the Jurassic, Cretaceous, and Paleogene Beds of the USSR; Vozzhennikova TF., 1963, OSNOVY PALEONTOLOGII, V14, P171; Weston JF, 2012, CAN J EARTH SCI, V49, P1417, DOI 10.1139/e2012-070; WILEY EO, 1991, SPECIAL PUBLICATION, V19, P158; WILLIAMS GL, 1966, BRIT MUSEUM NATURAL, V3, P182; Williams GL, 2015, PALYNOLOGY, V39, P289, DOI 10.1080/01916122.2014.993888	33	7	10	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41	3					430	437		10.1080/01916122.2017.1283367	http://dx.doi.org/10.1080/01916122.2017.1283367			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	FF2RG		Green Published			2025-03-11	WOS:000408743900011
J	Mohamed, O; Piller, WE				Mohamed, Omar; Piller, Werner E.			A model of dinoflagellate cyst distribution around the K/Pg boundary and its paleoenvironmental implications (Eastern Alps)	AUSTRIAN JOURNAL OF EARTH SCIENCES			English	Article						Dinoflagellate cysts; palynofacies; Cretaceous/Paleogene; Eastern Alps	CRETACEOUS-PALEOGENE BOUNDARY; NORTHERN CALCAREOUS ALPS; PALYNOFACIES; STRATIGRAPHY; INDICATORS; SECTION; BASIN	A new model was developed for the paleogeographic distribution of dinoflagellate cysts across the Cretaceous/ Paleogene (K/Pg) boundary. Four sections in the Eastern Alps were studied. The Knappengraben and Gamsbach sections are located in the Gosau Basin of Gams, Austria. They are continuous across the boundary and represent a bathyal environment. The Waidach section north of Salzburg (Austria) contains neritic deposits of the Helvetic unit but shows a hiatus at the boundary. The Goppling section between Teisendorf and Oberteisendorf (Bavaria, Germany) belongs to a turbidite-rich, deep-water system (Ultrahelvetic unit), and is considered to be continuous across the boundary. The occurrence and distribution of dinoflagellate cysts in these sections suggests that Trabeculidinium, Adnatosphaeridium, Spiniferites, Pterodinium, Impagidinium, Achomosphaera and Codoniella are restricted to bathyal environments, whereas Areoligera, Manumiella and Trithyrodinium are restricted to the neritic environment. The abundance of Manumiella and Trithyrodinium indicate a high nutrient supply. Hystrichosphaeridium -dominated assemblages have been recorded in both neritic and bathyal environments. Two Manumiella spikes were recorded only at Waidach and interpreted to reflect slight coolings of oceanic surface waters. In the Danian, acme of Spongodinium delitiense are recorded similar to 1 m above the K/Pg boundary in the neritic and bathyal environments. These acmes could reflect a slight cooling of surface waters in the earliest Danian. The palynofacies analysis in the Gams Basin reveals a high abundance of amorphous organic matter in the Maastrichtian, and black phytoclasts in the Danian, which indicates intensified terrigenous run-off in the Danian with higher sea-floor oxygenation. In the Waidach section, palynomorphs are much more abundant, indicating a shelf to basin transitional area with dysoxic-anoxic conditions at the sea-floor.	[Mohamed, Omar] Menia Univ, Geol Dept, Fac Sci, El- Minia, Egypt; [Piller, Werner E.] Karl Franzens Univ Graz, Inst Earth Sci Geol & Palaeontol, Heinrichstr 26, A-8010 Graz, Austria	Egyptian Knowledge Bank (EKB); Minia University; University of Graz	Mohamed, O (通讯作者)，Menia Univ, Geol Dept, Fac Sci, El- Minia, Egypt.	omar.mohamed@mu.edu.eg		Mohamed, Omar/0000-0002-2817-1683				[Anonymous], 2008, BERICHTE GEOLOGISCHE; Berggren WA, 2000, PALAEOGEOGR PALAEOCL, V159, P1, DOI 10.1016/S0031-0182(00)00031-6; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Carvalho MD, 2013, SEDIMENT GEOL, V295, P53, DOI 10.1016/j.sedgeo.2013.08.002; Egger H, 2010, AUSTRIAN J EARTH SCI, V103, P121; Egger H, 2009, STRATIGRAPHY, V6, P333; Egger Hans, 2004, Annalen des Naturhistorischen Museums in Wien A Mineralogie Petrologie Geologie Palaeontologie Archaeozoologie Anthropologie Praehistorie, V106A, P281; Faupl P., 2000, Mitteilungen der O sterreichischen Geologischen Gesellschaft, V92, P79; Gedl P, 2004, GEOL SOC SPEC PUBL, V230, P257, DOI 10.1144/GSL.SP.2004.230.01.13; Gradstein F., 2004, A Geological Time Scale; Guasti E, 2005, MAR MICROPALEONTOL, V55, P1, DOI 10.1016/j.marmicro.2005.01.001; Habib D., 1982, NATURE ORIGIN CRETAC, P113; Hammer Oyvind, 2001, Palaeontologia Electronica, V4, pUnpaginated; Haubold H, 1999, PHYS CHEM EARTH PT A, V24, P697, DOI 10.1016/S1464-1895(99)00101-5; Herm D., 1981, GEOL BAVAR, V82, P319; Krenmayr HG, 1996, SEDIMENT GEOL, V101, P149, DOI 10.1016/0037-0738(95)00052-6; Lahodynsky R., 1988, REV ESPANOLA PALEONT, V1988; Mohamed O., 2010, THESIS; Mohamed O, 2013, REV PALAEOBOT PALYNO, V190, P85, DOI 10.1016/j.revpalbo.2012.11.002; Mohamed O, 2012, CRETACEOUS RES, V35, P143, DOI 10.1016/j.cretres.2011.12.007; Peryt D, 1997, PALAEOGEOGR PALAEOCL, V132, P287, DOI 10.1016/S0031-0182(97)00056-4; PERYT D, 1993, PALAEOGEOGR PALAEOCL, V104, P239, DOI 10.1016/0031-0182(93)90135-6; PREISINGER A, 1986, NATURE, V322, P794, DOI 10.1038/322794a0; Pueyo EL, 2007, TECTONICS, V26, DOI 10.1029/2006TC001965; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; Stampfli G.M., 2002, J VIRTUAL EXPLORER, V7, P75, DOI DOI 10.1016/S0012-821X; Stampfli GM, 2006, GEOL SOC MEM, V32, P57, DOI 10.1144/GSL.MEM.2006.032.01.04; Stradner H., 1987, TERRA COGNITA, V7, P212; Tabara D, 2017, GEOL Q, V61, P39, DOI 10.7306/gq.1302; TRAUB FRANZ, 1953, GEOL BAVARICA, V15, P1; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; WAGREICH M, 1993, GEOLOGY, V21, P941, DOI 10.1130/0091-7613(1993)021<0941:STEIOB>2.3.CO;2	32	2	2	0	8	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.		2017	110	1								10.17738/ajes.2017.0003	http://dx.doi.org/10.17738/ajes.2017.0003			7	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FA1ES		gold			2025-03-11	WOS:000405182700005
J	Riddick, NL; Volik, O; McCarthy, FMG; Danesh, DC				Riddick, Nicholas L.; Volik, Olena; McCarthy, Francine M. G.; Danesh, Donya C.			The effect of acetolysis on desmids	PALYNOLOGY			English	Article						Non-pollen palynomorphs; Lake Simcoe; anthropogenic impact; selective preservation; Cosmarium; Pediastrum	NON-POLLEN PALYNOMORPHS; RECENT MARINE-SEDIMENTS; CRAWFORD LAKE; WATER-QUALITY; ONTARIO; INDICATORS; ALGAE; EUTROPHICATION; PALYNOLOGY; CARBONATE	Acetolysis, an oxidising technique common in palynological preparation, is beneficial for pollen analysts who employ it to remove unwanted' organic matter from peat and lake samples. Since this technique was introduced by G. Erdtman in 1934, however, several researches have noted concerns, such as the destruction of thin-walled pollen grains in addition to non-sporopollenin pollen components, and selective destruction of protoperidinioid dinoflagellate cysts. Desmids are conjugate green algae with a wide range of environmental preferences whose half-cells are known from sediments dating back to at least the Neogene (possibly as far back as the Devonian), and they have proven useful in modern and palaeolimnological studies (e.g. as indicators of nutrient loading, anthropogenic impact and drought). Desmids are rarely mentioned in palynological studies, however, except to illustrate fluvial transport to nearshore marine settings. A diverse desmid flora was found in samples processed without acetolysis from Smith's Bay in Lake Simcoe, and desmid and thecamoebian (testate amoeba) assemblage changes record eutrophication up-core. Very low concentrations of both desmids and Pediastrum, another group of algal non-pollen palynomorphs (NPP), record siltation and inhibition of photosynthesis attributed to two phases of land-clearing and agriculture (Wendat/Huron and Euro-Canadian). After acetolysis, the desmid abundance in the same residues drops significantly (between 36 and 100%, mean = 87%) and the assemblage is skewed towards the most robust Cosmarium spp. However, other low-relief NPP, like Pediastrum, may be easier to observe after acetolysis as they are not obscured by amorphous organic matter. Because of the observed detrimental impact acetolysis has on the desmid assemblage, recommendations include: (i) not acetolysing, as pollen and Pediastrum can be observed either way, or (ii) using a two-pronged approach where susceptible microfossils are observed pre-acetolysis and resistant ones observed post-acetolysis.	[Riddick, Nicholas L.; McCarthy, Francine M. G.] Brock Univ, Dept Earth Sci, St Catharines, ON, Canada; [Volik, Olena] Univ Waterloo, Dept Geog & Environm Management, Waterloo, ON, Canada; [Danesh, Donya C.] Queens Univ, Dept Biol, Kingston, ON, Canada	Brock University; University of Waterloo; Queens University - Canada	Riddick, NL (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON, Canada.	riddick.nicholas@gmail.com	Volik, Olena/ABH-8956-2020	Volik, Olena/0000-0003-4949-1974; Riddick, Nicholas/0009-0005-1370-6365				Bennett KD., 2001, Tracking Environmental Change Using Lake Sediment. 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An introduction to phycology; van Geel B., 2001, TRACKING ENV CHANGE, P99, DOI DOI 10.1007/0-306-47668-1_6; Volik O., 2014, THESIS; Worobiec Elzbieta, 2014, Acta Palaeobotanica, V54, P113, DOI 10.2478/acpa-2014-0005; Zippi P., 1990, ENV RES TECHN TRANSF, P393	52	15	15	1	9	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2017	41	2					171	179		10.1080/01916122.2015.1113208	http://dx.doi.org/10.1080/01916122.2015.1113208			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ES5HV					2025-03-11	WOS:000399569900004
J	Mertens, KN; Gu, HF; Takano, Y; Price, AM; Pospelova, V; Bogus, K; Versteegh, GJM; Marret, F; Turner, RE; Rabalais, NN; Matsuoka, K				Mertens, Kenneth Neil; Gu, Haifeng; Takano, Yoshihito; Price, Andrea M.; Pospelova, Vera; Bogus, Kara; Versteegh, Gerard J. M.; Marret, Fabienne; Turner, R. Eugene; Rabalais, Nancy N.; Matsuoka, Kazumi			The cyst-theca relationship of the dinoflagellate cyst <i>Trinovantedinium pallidifulvum</i>, with erection of <i>Protoperidinium lousianensis</i> sp nov and their phylogenetic position within the <i>Conica</i> group	PALYNOLOGY			English	Article						Micro-FTIR; Selenopemphix undulata; Wadden Sea; Lake Saroma; Saanich Inlet; Gulf of Mexico	SURFACE SEDIMENTS; RESTING CYSTS; HETEROTROPHIC DINOFLAGELLATE; MOLECULAR PHYLOGENY; COASTAL WATERS; MIDDLE MIOCENE; NORTH PACIFIC; DINOPHYCEAE; PERIDINIALES; GENUS	We establish the cyst-theca relationship of the dinoflagellate cyst species Trinovantedinium pallidifulvum Matsuoka 1987 based on germination experiments of specimens isolated from the Gulf of Mexico. We show that the motile stage is a new species, designated as Protoperidinium louisianensis. We also determine its phylogenetic position based on single-cell polymerase chain reaction (PCR) of a single cell germinated from the Gulf of Mexico cysts. To further refine the phylogeny, we determined the large subunit (LSU) sequence through single-cell PCR of the cyst Selenopemphix undulata isolated from Brentwood Bay (Saanich Inlet, BC, Canada). The phylogeny shows that P. louisianensis is closest to P. shanghaiense, the motile stage of T. applanatum, and is consistent with the monophyly of the genus Trinovantedinium. Selenopemphix undulata belongs to a different clade than Selenopemphix quanta (alleged cyst of P. conicum), suggesting that the genus Selenopemphix is polyphyletic. Trinovantedinium pallidifulvum is widely distributed with occurrences in the Gulf of Mexico, the North Atlantic, the northeast Pacific and southeast Asia. In addition, we illustrate the two other extant species, Trinovantedinium applanatum and Trinovantedinium variabile, and two morphotypes of Trinovantedinium. Geochemical analyses of the cyst wall of T. pallidifulvum indicate the presence of amide groups in agreement with other heterotrophic dinoflagellate species, although the cyst wall of T. pallidifulvum also includes some unique features.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium; [Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Takano, Yoshihito; Matsuoka, Kazumi] Inst East China Sea Res ECSER, 1551-7 Taira Machi, Nagasaki 8512213, Japan; [Price, Andrea M.] McGill Univ, Dept Geog, Burnside Hall,805 Sherbrooke St West, Montreal, PQ H3A OB9, Canada; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB A405,POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada; [Bogus, Kara] Texas A&M Univ, Int Ocean Discovery Program, 1000 Discovery Dr, College Stn, TX 77845 USA; [Versteegh, Gerard J. M.] MARUM Ctr Marine Environm Sci, Leobener Str, D-28359 Bremen, Germany; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Turner, R. Eugene] Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA; [Rabalais, Nancy N.] Louisiana Univ Marine Consortium, Chauvin, LA 70344 USA; [Mertens, Kenneth Neil] IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France; [Versteegh, Gerard J. M.] Helmholtz Zentrum Polar & Meeresforsch, AWI, Handelshafen 12, D-27570 Bremerhaven, Germany	Ghent University; Third Institute of Oceanography, Ministry of Natural Resources; University of Victoria; Texas A&M University System; Texas A&M University College Station; University of Bremen; University of Liverpool; Louisiana State University System; Louisiana State University; Ifremer; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.; Mertens, KN (通讯作者)，IFREMER, LER BO, Stn Biol Marine, Pl Croix,BP40537, F-29185 Concarneau, France.	kenneth.mertens@ifremer.fr; gerard.versteegh@awi.de	Rabalais, Nancy/GQA-6087-2022; Mertens, Kenneth/AAO-9566-2020; Versteegh, Gerard J.M./H-2119-2011; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022	Versteegh, Gerard J.M./0000-0002-9320-3776; Marret-Davies, Fabienne/0000-0003-4244-0437; Mertens, Kenneth/0000-0003-2005-9483; Gu, Haifeng/0000-0002-2350-9171; Price, Andrea/0000-0002-5359-053X; Pospelova, Vera/0000-0003-4049-8133; Bogus, Kara/0000-0003-4690-0576; Rabalais, Nancy N./0000-0002-1514-837X	German Science Foundation [VE486/2]; Natural Sciences and Engineering Research Council of Canada (NSERC); National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research [NA06OP0528, NA09NOS4780204, NA06OP0529, NA09NOS4780230]	German Science Foundation(German Research Foundation (DFG)); Natural Sciences 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)	Kenneth Neil Mertens is a postdoctoral researcher of FWO Belgium. Martin J. Head is acknowledged for advice on the genus Trinovantedinium. Anna Godhe is thanked for providing a sample from the Kattegat. Evelyne Goubert is thanked for providing a sample from La Vilaine Bay, and Jean-Pierre Debenay for samples from the Vie River estuary. We acknowledge the Scripps Institution of Oceanography (SIO) Geological Collections and, in particular, Alex Hangsterfer for sediment samples from the Bay of Bengal. Pieter R. Gurdebeke is thanked for providing a nice specimen of Trinovantedinium variabile. KNM and AMP thank Anne de Vernal for letting us use the equipment to conduct germination experiments at Geotop. Sofia Ribeiro is thanked for the loan of slides from Portugal. GJMV acknowledges support by the German Science Foundation (Heisenberg fellowship VE486/2). AMP and VP acknowledge the support of the Natural Sciences and Engineering Research Council of Canada (NSERC). Support for ship time for Gulf of Mexico specimens was provided by the National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research, under awards NA06OP0528 and NA09NOS4780204 to Louisiana Universities Marine Consortium, and awards NA06OP0529 and NA09NOS4780230 to Louisiana State University. The crew of the R/V Pelican is thanked for assistance with sample collection. Martin J. Head and an anonymous reviewer are thanked for remarks that significantly improved the manuscript.	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J	Tabara, D; Slimani, H				Tabara, Daniel; Slimani, Hamid			Dinoflagellate cysts and palynofacies across the Cretaceous-Paleogene boundary interval of the Vrancea Nappe (Eastern Carpathians, Romania)	GEOLOGICAL QUARTERLY			English	Article						Vrancea Nappe; dinoflagellate cyst biostratigraphy; palynofacies; Cretaceous-Paleogene boundary interval	WESTERN EXTERNAL RIF; TERTIARY BOUNDARY; OULED HADDOU; CRETACEOUS/PALAEOGENE BOUNDARY; PLANKTONIC FORAMINIFERS; SEQUENCE STRATIGRAPHY; NORTHERN APENNINES; MOLDAVIDIAN BASIN; MASS EXTINCTION; NEW-ZEALAND	A palynological study of uppermost Maastrichtian to Lower Paleocene deposits from a stratigraphic section of the Vrancea Nappe (Eastern Carpathians), reveals the presence of diverse and well-preserved dinoflagellate cyst assemblages. The biostratigraphic interpretation of these dinocyst assemblages suggests that (1) the Cretaceous-Paleogene boundary lies within a similar to 8 m thick sedimentary interval, between the Lep a Formation (uppermost Maastrichtian) and Putna-Piatra Uscata Formation (Lower Danian), based on the Last Appearance Datum of latest Maastrichtian markers such as Pterodinium cretaceum and Palynodinium cf. grallator and on the First Appearance Datum of Danian markers such as Senoniasphaera inornata, Xenicodinium lubricum, Tectatodinium rugulaturn and Eisenackia circumtabulata, and (2) a discontinuity between the two formations. The palynofacies analysis from this geological section indicates an abundance of continental organic matter (mainly opaque phytoclasts), deposited in a distal setting of the sedimentary basin. The occurrences in the palynological assemblage of some oceanic dinocyst taxa such as Impagidinium and Pterodinium suggest the same depositional environment for the geological formations analysed.	[Tabara, Daniel] AI I Cuza Univ Iasi, Dept Geol, 20A Carol I Blv, Iasi 700505, Romania; [Slimani, Hamid] Univ Mohammed V Rabat, Inst Sci, Lab Geol & Remote Sensing, URAC 46, Ave Ibn Batouta,POB 703, Rabat 10106, Morocco	Alexandru Ioan Cuza University; Mohammed V University in Rabat	Tabara, D (通讯作者)，AI I Cuza Univ Iasi, Dept Geol, 20A Carol I Blv, Iasi 700505, Romania.	dan.tabara@yahoo.com	Slimani, Hamid/AAL-4055-2020; Tabara, Daniel/C-6630-2015	Slimani, Hamid/0000-0001-6392-1913				ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; Amadori ML, 2012, INT J EARTH SCI, V101, P1599, DOI 10.1007/s00531-011-0744-1; [Anonymous], 1990, PALAEOGEOGR PALAEOCL; [Anonymous], 1977, QUESTIONS PHYTOSTRAT; Batten D.J., 1999, FOSSIL PLANTS SPORES, P15; Benson D.G. 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L., 1993, GEOL SURV CANADA, P92; Willumsen PS, 2011, ALCHERINGA, V35, P199, DOI 10.1080/03115518.2010.494484; Willumsen PS, 2004, J MICROPALAEONTOL, V23, P119, DOI 10.1144/jm.23.2.119	70	15	15	0	8	POLISH GEOLOGICAL INST	WARSAW	RAKOWIECKA 4, BLDG A, ROOM 434, PL-00-975 WARSAW, POLAND	1641-7291	2082-5099		GEOL Q	Geol. Q.		2017	61	1					39	52		10.7306/gq.1302	http://dx.doi.org/10.7306/gq.1302			14	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EL4AY		gold			2025-03-11	WOS:000394563700003
J	Singh, YR; Singh, BP; Singh, AK; Devi, SR				Singh, Y. Raghumani; Singh, B. P.; Singh, A. K.; Devi, S. Ranjeeta			Palynology and Mineral Composition of the Upper Disang flyschoid sediments from the Southern Manipur, Northeast India: Age, Paleoenvironment and Provenance Reconstruction	HIMALAYAN GEOLOGY			English	Article						Palynology; Mineralogy; Age; Upper Disang Formation; Indo-Myanmar ranges	OLIGOCENE DINOFLAGELLATE CYSTS; IMPHAL VALLEY; EOCENE; NAGALAND; FOSSILS; OCEAN; ZONE	This paper describes palynology and mineral composition of the Upper Disang Formation from the southern part of Manipur, Northeast India to reconstruct age, paleoenvironment and provenance of this flyschoid sedimentary formation. The palynofossils suggest late Eocene age for the Upper Disang Formation. This formation has dinoflagellate cysts, viz., Homonyblium, Cordosphaeridium, Fibrocysta cf. axialis, Hystrichokolpoma cf. riguadiae and Operculodinium centrocarpum which indicate a shallow marine depositional environment. The lower part of the sequence (G-1 to G-22) characterised by Homonybliumfloripes, Operculodinium centrocarpum and Fibrocysta cf. axialis suggests deposition in nearshore (inner neritic) shallow marine environment, whereas, Cordosphaeridium and Hystrichokolpoma cf. rigaudiae present in the upper part of the formation (GT-1 to GT-22) suggests deposition in the nearshore, probably, outer neritic environment. Occurrence of Homotryblium floripes shows the drier period, where reduced runoff and strong evaporation led to increase salinity in nearshore restricted environment. This study suggests derivation of the sediments from a chlorite and mica- schist or gneiss or phyllite-bearing provenance. The field data along with the mineral compositions and available palynomorphs suggest that the Upper Disang shales and sandstones were deposited in a shallow marine basin during late Eocene and tropical warm humid climate condition, probably, with short time aridity, prevailed during their deposition.	[Singh, Y. Raghumani; Devi, S. Ranjeeta] Manipur Univ, Dept Earth Sci, Imphal 795003, Manipur, India; [Singh, B. P.] Banaras Hindu Univ, CAS Geol, Varanasi 221005, Uttar Pradesh, India; [Singh, A. K.] Wadia Inst Himalayan Geol, Dehra Dun 248001, Uttar Pradesh, India	Manipur University; Banaras Hindu University (BHU); Department of Science & Technology (India); Wadia Institute of Himalayan Geology (WIHG)	Singh, YR (通讯作者)，Manipur Univ, Dept Earth Sci, Imphal 795003, Manipur, India.	yengmani@gmail.com			Department of Science and Technology, Government of India [SR/S4/ES-576/2011]	Department of Science and Technology, Government of India(Department of Science & Technology (India))	The authors express thanks to the Head, Department of Earth Sciences, Manipur University, Imphal and the Director, WIHG, Dehradun for providing the necessary facilities. Two of the authors YRS and BPS gratefully acknowledge the Department of Science and Technology, Government of India for the financial support in from of a Research Project (No. SR/S4/ES-576/2011). We are thankful to Prof. Jianguo Li (Nanjing Institute of Geology and Paleontology, China), Shri Venus Guruaribam, Shri Krishna Mondal and Shri A. Patra (India) for their technical support during preparation of this manuscript.	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Geol.		2017	38	1					1	11						11	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EP6HR					2025-03-11	WOS:000397479700001
J	Miján, I; Louwye, S; Lambert, O				Mijan, Ismael; Louwye, Stephen; Lambert, Olivier			A new <i>Beneziphius</i> beaked whale from the ocean floor off Galicia, Spain and biostratigraphic reassessment of the type species	ACTA PALAEONTOLOGICA POLONICA			English	Article						Mammalia; Cetacea; Ziphiidae; Miocene; North Atlantic; North Sea; Iberian Peninsula	LATE MIOCENE; DINOFLAGELLATE CYST; CETACEA ODONTOCETI; ZIPHIIDAE CETACEA; MIDDLE MIOCENE; EVOLUTION; NORTH; BASIN; FORAMINIFERA; MORPHOLOGY	Although the fossil record of beaked whales (Cetacea, Odontoceti, Ziphiidae) is continuously improving, the geological age of new taxa is often poorly constrained. Based on a partial cranium from deep seafloor deposits off Galicia, Spain, we describe a new species of the stem beaked whale genus Beneziphius, B. cetariensis sp. nov. The latter differs from the type species B. brevirostris in the larger size, the rostrum being proportionally longer, the premaxillae being longer than the maxillae at the apex of the rostrum, the left premaxillary sac fossa being transversely concave, and the ascending process of the premaxilla reaching the vertical. Considering that the stratigraphic context of deep-sea deposits off the Iberian Peninsula is not precisely known, we provisionally propose an extended, middle Miocene to early Pliocene interval for the geological age of B. cetariensis. Nonetheless, the palynological analysis of sediment sampled from cavities in the cranium of the holotype of B. brevirostris, discovered during the second part of the nineteenth century in inland deposits of Antwerp (north of Belgium), yield an early to mid-Serravallian age (13.2-12.8 Ma, late middle Miocene). B. brevirostris is thus the oldest described species of the "Messapicetus clade", a large clade of stem ziphiids in which most species are dated from the late Miocene. The description of the Galician species B. cetariensis broadens the biogeographic distribution of Beneziphius and confirms the strong ziphiid faunal affinities between the eastern coast of the North Atlantic and the southern margin of the North Sea Basin.	[Mijan, Ismael] Soc Galega Hist Nat, Praza Canido S-N, E-15401 Ferrol, Spain; [Louwye, Stephen] Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, 281 Krijgslaan S8, B-9000 Ghent, Belgium; [Lambert, Olivier] Inst Royal Sci Nat Belgique, DO Terre & Hist Vie, Rue Vautier 29, 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.	ismaelmijan@gmail.com; stephen.louwye@ugent.be; olivier.lambert@naturalsciences.be	Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Lambert, Olivier/0000-0003-0740-5791				[Anonymous], 1997, PALAEONTOGRAPHIA ITA; Antunes MT, 2015, GEOL ACTA, V13, P181, DOI 10.1344/GeologicaActa2015.13.3.1; Bianucci G, 2007, GEODIVERSITAS, V29, P561; Bianucci G, 2016, PEERJ, V4, DOI 10.7717/peerj.2479; Bianucci G, 2013, GEODIVERSITAS, V35, P105, DOI 10.5252/g2013n1a6; Bianucci Giovanni, 2005, Deinsea (Rotterdam), P1; Brisson M. - J., 1762, REGNUM ANIMALE CLASS; Dalebout ML, 2014, MAR MAMMAL SCI, V30, P1081, DOI 10.1111/mms.12113; de Buffrenil V., 2000, Historical Biology, V14, P57; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; 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; Gol'din P, 2014, BIOL J LINN SOC, V113, P510, DOI 10.1111/bij.12337; GOLOBOFF PA, 1993, CLADISTICS, V9, P83, DOI 10.1111/j.1096-0031.1993.tb00209.x; Gray J.E., 1850, CATALOGUE SPECIMEN 1; Hassanin A, 2012, CR BIOL, V335, P32, DOI 10.1016/j.crvi.2011.11.002; HEYNING JE, 1984, CAN J ZOOL, V62, P1645, DOI 10.1139/z84-239; Kouwenhoven TJ, 2006, PALAEOGEOGR PALAEOCL, V238, P373, DOI 10.1016/j.palaeo.2006.03.035; Lambert O, 2005, GEODIVERSITAS, V27, P443; Lambert O, 2013, J VERTEBR PALEONTOL, V33, P709, DOI 10.1080/02724634.2013.743405; Lambert O, 2011, CR PALEVOL, V10, P453, DOI 10.1016/j.crpv.2011.03.012; Lambert O, 2010, J VERTEBR PALEONTOL, V30, P1645, DOI 10.1080/02724634.2010.501642; MacLeod CD, 2002, CAN J ZOOL, V80, P178, DOI 10.1139/Z01-188; McGowen MR, 2009, MOL PHYLOGENET EVOL, V53, P891, DOI 10.1016/j.ympev.2009.08.018; Mead James G., 2009, Smithsonian Contributions to Zoology, P1; Morin P.A., 2016, MARINE MAMMAL SCI; Quaijtaal W, 2014, PALAEOGEOGR PALAEOCL, V399, P140, DOI 10.1016/j.palaeo.2014.02.017; Ramassamy B, 2016, ZOOL J LINN SOC-LOND, V178, P381, DOI 10.1111/zoj.12418; Schreck M, 2012, REV PALAEOBOT PALYNO, V187, P66, DOI 10.1016/j.revpalbo.2012.08.006; Scotese C.R., 2014, Atlas of Phanerozoic Climatic Zones (Mollweide Projection), V1-6; Soliman A, 2009, PALYNOLOGY, V33, P73, DOI 10.1080/01916122.2009.9989685; Uhen MD, 2008, J VERTEBR PALEONTOL, V28, P589, DOI 10.1671/0272-4634(2008)28[589:NPWFAA]2.0.CO;2; Werth AJ, 2006, J MAMMAL, V87, P579, DOI 10.1644/05-MAMM-A-279R1.1; Wichura H, 2015, P NATL ACAD SCI USA, V112, P3910, DOI 10.1073/pnas.1421502112	34	5	6	0	10	INST PALEOBIOLOGII PAN	WARSAW	UL TWARDA 51/55, 00-818 WARSAW, POLAND	0567-7920	1732-2421		ACTA PALAEONTOL POL	Acta Palaeontol. Pol.		2017	62	1					211	220		10.4202/app.00309.2016	http://dx.doi.org/10.4202/app.00309.2016			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	EO4AI		gold, Green Published			2025-03-11	WOS:000396635800013
J	Galvn-Escobedo, IG; Ramírez-Arriaga, E; Valiente-Banuet, A; Uscanga-Mortera, E; García-Moya, E; Kohashi-Shibata, J				Galvn-Escobedo, Iris G.; Ramirez-Arriaga, Elia; Valiente-Banuet, Alfonso; Uscanga-Mortera, Ebandro; Garcia-Moya, Edmundo; Kohashi-Shibata, Josue			Paleopalinological record of the San Gregorio formation (Borehole B4), Baja California Sur, Mexico	BOLETIN DE LA SOCIEDAD GEOLOGICA MEXICANA			Spanish	Article						pollen-spores; dinoflagellates; diversity; paleovegetation; San Gregorio formation	WALLED DINOFLAGELLATE CYSTS; NEOTROPICAL PALEOBOTANY; CUAYUCA FORMATION; CLOUD FOREST; CHRONOSTRATIGRAPHY; PALYNOLOGY; EVOLUTION; OLIGOCENE; ECOLOGY; PUEBLA	In La Purnsima region, Comondu, Baja California Sur, the borehole B4 was extracted from the San Gregorio formation (upper Oligocene-lower Miocene). It contains continental and marine palynomorphs. The aim of this study was to examine the borehole palinomorphs and analyze their richness and a diversity. We propose the vegetation types in which these elements could develop based on continental microfossils. Also the deposition environment was interpreted based on the marine microfossils. The richness for pollen-spores and dinoflagellate cysts assemblages was n = 161 and n = 28 respectively. The total richness was n = 189. The a-diversity (H') of the pollen-spores assemblage was 2.61 and the evenness (J') was 0.51. The dinoflagellate cysts diversity H' was 2.33 and J' was 0.70. The total diversity H' was 3.02, and J' was 0.57. Using CONISS analysis (constrained incremental sum of squares clustering), three zones in the stratigraphic column of the borehole were defined. Zone A, was characterized by the presence of Operculodinium dinoflagellate cysts and a scarcity of pollen-spores. Zone B, was defined by continental palynomorphs, highlighting the presence of Chenopodipollis, Graminidites, Liliacidites pollen and Lusatisporis dettmannae spores, as well as Achomosphaera, Lingulodinium and Polysphaeridium dinoflagellates cysts. Zone C, was established by the Tubulifloridites pollen record. The chronostratigraphic pointers were: Corsinipollenites, Ephedripites claricristatus, Momipites coryloides and M. tenuipolus. The pollen-spore assemblages suggests the presence of two plant paleocommunities: a cloud forest in the highlands at the regional level, and a tropical deciduous forest at the local level near to the deposit basin. The presence of marine palynomorphs in the sequence suggest that these deposits correspond to a shallow marine environment near the coast.	[Galvn-Escobedo, Iris G.; Uscanga-Mortera, Ebandro; Garcia-Moya, Edmundo; Kohashi-Shibata, Josue] Colegio Postgrad, Posgrad Bot, Campus Montecillo,Carretera Mexico Texcoco, Texcoco 56230, Estado De Mexic, Mexico; [Ramirez-Arriaga, Elia] Univ Nacl Autonoma Mexico, Inst Geol, Dept Paleontol, Lab Palinol, Ciudad Univ, Mexico City 04510, DF, Mexico; [Valiente-Banuet, Alfonso] Univ Nacl Autonoma Mexico, Inst Ecol, Dept Ecol Biodiversidad, Ciudad Univ, Mexico City 04510, DF, Mexico	Colegio de Postgraduados - Mexico; Universidad Nacional Autonoma de Mexico; Universidad Nacional Autonoma de Mexico	Galvn-Escobedo, IG (通讯作者)，Colegio Postgrad, Posgrad Bot, Campus Montecillo,Carretera Mexico Texcoco, Texcoco 56230, Estado De Mexic, Mexico.	sirigales@gmail.com	Arriaga, Elia/AAG-4322-2020					ALATORRE AE, 1988, ECON GEOL, V83, P1918, DOI 10.2113/gsecongeo.83.8.1918; Alvarez-Zúñiga E, 2012, BOT SCI, V90, P163, DOI 10.17129/botsci.481; [Anonymous], 1994, ZENTRALBLATT GEOLO 1; [Anonymous], 2000, BOL SOC GEOL MEX; [Anonymous], 1989, DIVERSIDAD ECOLOGICA; [Anonymous], 1996, COMPOSITAE SYSTEMATI; [Anonymous], 2010, BOSQUE MESIFILO MONT; [Anonymous], 2014, Los tipos de vegetacion de Mexico y su clasificacion edicion conmemorativa 1963-2013; [Anonymous], REV INVEST CIENT; Applegate S.P., 1986, Revista do Instituto Geologico (Sao Paulo), V6, P145; Aranda-Gomez J.J., 2000, Boletin de la Sociedad Geologica Mexicana, V53, P59, DOI DOI 10.18268/BSGM2000V53N1A3; Barnett J., 1982, THESIS; Beal C.H, 1948, GEOLOGICAL SOC AM ME, V31, P138; Becerra JX, 2005, P NATL ACAD SCI USA, V102, P10919, DOI 10.1073/pnas.0409127102; BIAGGI R, 1978, THESIS; BRUIJNZEEL LA, 1993, J ECOL, V81, P145, DOI 10.2307/2261231; Carrasco-Velázquez Baldomero E., 2009, Bol. 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Soc. Geol. Mex.		2017	69	1					35	58		10.18268/BSGM2017v69n1a3	http://dx.doi.org/10.18268/BSGM2017v69n1a3			24	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EO3CD		gold, Green Published			2025-03-11	WOS:000396571600003
J	Sánchez-Pellicer, R; Masure, E; Villier, L				Sanchez-Pellicer, Raquel; Masure, Edwige; Villier, Loic			A new biostratigraphic correlation for Late Cretaceous-Paleocene strata of the Gulf of Guinea: Evidence from dinoflagellate cysts	COMPTES RENDUS GEOSCIENCE			English	Article						Upper Cretaceous/Palaeocene; Cote d'Ivoire-Ghana; ODP Hole 959D; Biostratigraphy; Dinoflagellate cysts	TERTIARY BOUNDARY; SEQUENCE; PALEOENVIRONMENTS; TRANSITION; ATLANTIC; DEPOSITS; GENUS; RIF	A new biostratigraphic correlation for Late Cretaceous and Palaeocene strata of the Cote d'Ivoire-Ghana continental margin has been developed from the identification of significant dinoflagellate cyst events in ODP Hole 959D. The Late Cretaceous stage boundaries are mostly consistent with previous studies. However, the Maastrichtian/Danian boundary is placed much lower than previously recognized on the basis of the first occurrences of Carpatella cornuta and Damassadinium californicum. The base of the Selandian is recognized from the last occurrence of Cerodinium diebelii and the first occurrence of Adnatosphaeridium multispinosum. The base of the Thanetian is recognized from the first occurrence of Areoligera gippingensis. The rarity of the age-marker taxa is the main reason for different age determinations among studies of the same section. (C) 2016 Academie des sciences. Published by Elsevier Masson SAS.	[Sanchez-Pellicer, Raquel; Masure, Edwige; Villier, Loic] Univ Paris 06, MNHN, CNRS CR2P UMR7207, Ctr Rech Paleobiodiversite & Paleoenvironm, Case 104, F-75252 Paris 05, France; [Sanchez-Pellicer, Raquel] Univ Zaragoza, Dept Ciencias Tierra, Area Paleontol, C Pedro Cerbuna 12, E-50009 Zaragoza, Spain	Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; University of Zaragoza	Sánchez-Pellicer, R (通讯作者)，Univ Paris 06, MNHN, CNRS CR2P UMR7207, Ctr Rech Paleobiodiversite & Paleoenvironm, Case 104, F-75252 Paris 05, France.	raquel.sanchez_pellicer@courriel.upmc.fr			TOTAL; U.S. National Science Foundation (NSF)	TOTAL(Total SA); U.S. National Science Foundation (NSF)(National Science Foundation (NSF))	R.S.P. thanks Daniel Michoux for his helps on dinoflagellate cyst systematic and taxonomy. and Jean Dejax for sharing his knowledge on restoring palynological slides. Funding for this research was provided by TOTAL. The samples were provided by the Ocean Drilling Program (ODP), an organization sponsored by the U.S. National Science Foundation (NSF) and participating countries under management of Joint Oceanographic Institutions (JOI), Inc. We would like to thank Robert Fensome and Peter Bijl for their useful and constructive comments on the manuscript.	ALLERTON S., 1998, PROC OCEAN DRILL SCI, V159, P199; Basile C., 1998, Proceedings of the Ocean Drilling Program, Scientific Results, V159, P101; Besse J, 2002, J GEOPHYS RES-SOL EA, V107, DOI 10.1029/2000JB000050; Boltenhagen E, 1977, MICROPLANCTON CRETAC; 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; Corradini D., 1973, B SOC PALEONTOL ITAL, V11, P119; du Chene R.E. 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JAN	2017	349	1					32	41		10.1016/j.crte.2016.11.001	http://dx.doi.org/10.1016/j.crte.2016.11.001			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EO1BE		Green Published, hybrid			2025-03-11	WOS:000396431800004
J	Grigorszky, I; Kiss, TK; Pór, G; Dévai, G; Nagy, AS; Somlyai, I; Berta, C; Duleba, M; Trábert, Z; Acs, E				Grigorszky, Istvan; Kiss, Tihamer Keve; Por, Gabriella; Devai, Gyorgy; Nagy, Alex Sandor; Somlyai, Imre; Berta, Csaba; Duleba, Monika; Trabert, Zsuzsa; Acs, Eva			Temperature and growth strategies as the essential factors influencing the occurrence of <i>Stephanodiscus minutulus</i> (Kutzing) Cleve & Moller and <i>Palatinus apiculatus</i> (Ehrenberg) Craveiro, Calado, Daugbjerg & Moestrup	FUNDAMENTAL AND APPLIED LIMNOLOGY			English	Article; Proceedings Paper	10th Central European Diatom Meeting (CE-DiatoM)	APR 20-23, 2016	Budapest, HUNGARY	MTA Ctr Ecol Res, Hungarian Nat Hist Mus		life cycle; Stephanodiscus minutulus; Palatinus apiculatus; spring bloom; excystment; encystment	LIFE-CYCLE; SEASONAL SUCCESSION; BLOOM FORMATION; ICE ALGAE; PHYTOPLANKTON; DIATOMS; ASSEMBLAGES; GERMINATION; ENCYSTMENT; DYNAMICS	The life cycle of diatoms and dinoflagellates enables them to produce interannually varying dominances. This variability results from life -cycle interactions, physical conditions, and inter-species competition for nutrients and light. In particular, the overall dominant species of the year can be linked to the abundances of resting stages and temperature in spring. The aim of this study was to investigate the effects of temperature and life cycle as biotic factors on spring phytoplankton blooms caused by Stephanodiscus minutulus (Ktitzing) Cleve & Moller and Palatinus apiculatus (Ehrenberg) Craveiro, Calado, Daugbjerg & Moestrup, in a Hungarian shallow backwater. The composition of plankton communities exhibited a marked interannual heterogeneity. Our results suggested that a slight decrease in temperature in spring favours a spring bloom of vegetative dinoflagellates before encystment begins. However, a rapid increase in temperature results in high abundances of dinoflagellate cysts, which, in turn, leads to the dominance of diatoms. In this case, encystment starts before a pronounced dinoflagellate spring bloom is established.	[Grigorszky, Istvan; Devai, Gyorgy; Nagy, Alex Sandor; Somlyai, Imre; Berta, Csaba] Univ Debrecen, Dept Hydrobiol, Egyet Ter 1, H-4032 Debrecen, Hungary; [Grigorszky, Istvan; Kiss, Tihamer Keve; Duleba, Monika; Trabert, Zsuzsa; Acs, Eva] Hungarian Acad Sci, Danube Res Inst, Ctr Ecol Res, Karolina Ut 29-31, H-1113 Budapest, Hungary; Paterson Johal Consulting, 203 B-10190 152A St, Surrey, BC V3A 1M8, Canada	University of Debrecen; HUN-REN; HUN-REN Centre for Ecological Research; Danube Research Institute; Hungarian Academy of Sciences	Grigorszky, I (通讯作者)，Univ Debrecen, Dept Hydrobiol, Egyet Ter 1, H-4032 Debrecen, Hungary.; Grigorszky, I (通讯作者)，Hungarian Acad Sci, Danube Res Inst, Ctr Ecol Res, Karolina Ut 29-31, H-1113 Budapest, Hungary.	grigorszky.istvan@science.unideb.hu	Csaba, Berta/AES-0541-2022; Ács, Éva/J-3252-2014; István, Grigorszky/Q-2245-2019	Somlyai, Imre/0009-0009-0379-4196	MOB-WATER-LAB [HURO/1101/142/1.3.2]	MOB-WATER-LAB	We would like to thank the two anonymous reviewers for their suggestions and comments. The study was financial supported by HURO/1101/142/1.3.2, MOB-WATER-LAB.	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Appl. Limnol.	JAN	2017	189	2			SI		167	175		10.1127/fal/2016/0941	http://dx.doi.org/10.1127/fal/2016/0941			9	Limnology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	EM3OC		Green Accepted			2025-03-11	WOS:000395223500007
J	Matsuoka, K; Yurimoto, T; Chong, VC; Man, A				Matsuoka, Kazumi; Yurimoto, Tatsuya; Chong, Ving Ching; Man, Alias			Marine palynomorphs dominated by heterotrophic organism remains in the tropical coastal shallow-water sediment; the case of Selangor coast and the estuary of the Manjung River in Malaysia	PALEONTOLOGICAL RESEARCH			English	Article						dinoflagellate cysts; food web; Malaysia; marine palynomorph; microforaminiferal linings; tintinnomorph	DINOFLAGELLATE CYST DISTRIBUTION; SEA-SURFACE CONDITIONS; NORTH-ATLANTIC; ASSEMBLAGES; EUTROPHICATION; RECONSTRUCTION	We aimed to clarify and quantify the abundance of palynomorphs of tropical coastal marine shallowwater sediments collected from Oman, Malaysia, Okinawa and also the Sanriku region of Japan for making a comparison with temperate areas. Palynomorphs in these samples contained phototrophic and heterotrophic dinoflagellate cysts, acritarchs, resting cells of Prasinophyceae and Chrysophyceae, tintinnomorphs, microforaminiferal linings, testate amoebae and resting eggs and body fragments of copepods. The sediment samples from Malaysia, Oman, and Okinawa were characterized by dominance of heterotrophic marine palynomorphs, in particular microforaminiferal linings and heterotrophic dinoflagellate cysts, while the samples from Sanriku were different and dominated by phototrophic and heterotrophic dinoflagellate cysts. In addition subtropicaltropical assemblages were characterized by low cell/grain concentrations, especially phototrophic dinoflagellate cysts. These characteristics of marine palynomorphs in tropical shallow-water sediments may reflect lower production of phytoplankton in water column as well as high sedimentation rates. Also, high densities of heterotrophic palynomorphs consisting of microforaminiferal linings, tintinnomorphs, crustacean remains and other elements are other characteristics for tropical coastal shallow-water marine sediments. It is difficult to explain the abundant occurrences of heterotrophic dinoflagellate cysts based on the grazing food web against the fact of low phytoplankton production.	[Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan; [Yurimoto, Tatsuya] Japan Int Res Ctr Agr Sci, 1-1 Owashi, Tsukuba, Ibaraki 3058686, Japan; [Chong, Ving Ching] Univ Malaya, Inst Ocean & Earth Sci, Kuala Lumpur 50603, Malaysia; [Man, Alias] FRI Kampung Ache, Fisheries Res Inst, Sitawan 32000, Perak, Malaysia	Nagasaki University; Japan International Research Center for Agricultural Sciences; Universiti Malaya	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	Yurimoto, Tatsuya/AAS-1020-2020; CHONG, VING/B-4645-2009	CHONG, VING/0000-0003-0331-768X; Yurimoto, Tatsuya/0000-0002-7275-064X	JIRCAS project "Development of aquaculture technologies for sustainable and equitable production of aquatic products in tropical coastal areas"; MEXT/JSPS [26304031]; Grants-in-Aid for Scientific Research [26304031] Funding Source: KAKEN	JIRCAS project "Development of aquaculture technologies for sustainable and equitable production of aquatic products in tropical coastal areas"; MEXT/JSPS(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We express sincere thanks to Aya Morinaga for her kind help in the preparation of sediment samples and to Kazuhiko Koike for his valuable discussion on primary production in Southeast Asian mangrove coastal waters. We also thank two anonymous reviewers for providing valuable suggestions and comments that were useful for improving an earlier manuscript. The FTU data of Ofunato Bay was kindly provided by Iwate Fisheries Technology Center. This work is partially supported by the JIRCAS project "Development of aquaculture technologies for sustainable and equitable production of aquatic products in tropical coastal areas" and MEXT/JSPS-Grants-in-aid for Scientific Research (No: 26304031).	Al Gheilani H. M., 2010, FINAL REPORT OF BLOO; [Anonymous], 2007, Paleopalynology; Armstrong H.A., 2007, MICROFOSSILS, V2nd Edn, pviii+296; Baula IU, 2011, HARMFUL ALGAE, V11, P33, DOI 10.1016/j.hal.2011.07.002; Bulos A. D. M., 2008, TERMINAL REPORT DEV, P14; Canini ND, 2013, TROP ECOL, V54, P331; Chong V.C., 1999, Productivity and Sustainable Utilisation of Brackish Water Mangrove Ecosystem. Proceedings of the 4th Seminar on Results for 1997/1998 Research Projects, P115; Chong V. 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JAN	2017	21	1					14	26		10.2517/2016PR006	http://dx.doi.org/10.2517/2016PR006			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	EL2GX					2025-03-11	WOS:000394439200004
J	Hoetzel, S; Dupont, LM; Marret, F; Jung, G; Wefer, G				Hoetzel, Sebastian; Dupont, Lydie M.; Marret, Fabienne; Jung, Gerlinde; Wefer, Gerold			Steps in the intensification of Benguela upwelling over the Walvis Ridge during Miocene and Pliocene	INTERNATIONAL JOURNAL OF EARTH SCIENCES			English	Article						Dinoflagellate cysts; Benguela upwelling; Miocene-Pliocene; Eastern South Atlantic	DINOFLAGELLATE CYST STRATIGRAPHY; MATUYAMA DIATOM MAXIMUM; MIDDLE MIOCENE; SURFACE SEDIMENTS; SOUTHERN-AFRICA; SW AFRICA; SYSTEM; CIRCULATION; EVENTS; NORTH	Upwelling is a significant part of the ocean circulation controlling largely the transport of nutrient-rich cold waters to the surface and therefore influencing ocean productivity and global climate. The Benguela upwelling system (BUS) is one of the major upwelling areas in the world. Previous reconstructions of the BUS mainly focused on the onset and intensification in southern and central parts, but changes of the northern part have been rarely investigated in detail. Using the Late Miocene to Pliocene organic-walled dinoflagellate cyst record of ODP Site 1081, we reconstruct and discuss the early upwelling history over the Walvis Ridge with a special focus on the movement of the Angola-Benguela Front (ABF). We suggest that during the Late Miocene the Angola Current flowed southwards over the Walvis Ridge more frequently than today because the ABF was probably located further south as a result of a weaker meridional temperature gradient. A possible strengthening of the meridional gradient during the latest Miocene to early Pliocene in combination with uplift of south-western Africa intensified the upwelling along the coast and increased the upwelling's filaments over the Walvis Ridge. An intermediate period from 6.2 to 5.5 Ma is shown by the dominance of Habibacysta tectata, cysts of a cool-tolerant dinoflagellate known from the northern Atlantic, indicating changing oceanic conditions contemporaneous with the Messinian Salinity Crisis. From 4.3 Ma on, the upwelling signal got stronger again and waters were well-mixed and nutrient-rich. Our results indicate a northward migration of the ABF as early as 7 Ma and the initial stepwise intensification of the BUS.	[Hoetzel, Sebastian; Dupont, Lydie M.; Jung, Gerlinde; Wefer, Gerold] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str, Bremen, Germany; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England	University of Bremen; University of Liverpool	Dupont, LM (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str, Bremen, Germany.	dupont@uni-bremen.de	; Wefer, Gerold/S-2291-2016	Marret-Davies, Fabienne/0000-0003-4244-0437; Dupont, Lydie/0000-0001-9531-6793; Wefer, Gerold/0000-0002-6803-2020	DFG Research Center/Cluster of Excellence 'MARUM-The Ocean in the Earth System'; DFG Research Center/Cluster of Excellence 'GLOMAR-Bremen International Graduate School for Marine Sciences'	DFG Research Center/Cluster of Excellence 'MARUM-The Ocean in the Earth System'(German Research Foundation (DFG)); DFG Research Center/Cluster of Excellence 'GLOMAR-Bremen International Graduate School for Marine Sciences'(German Research Foundation (DFG))	This work was supported by the DFG Research Center/Cluster of Excellence 'MARUM-The Ocean in the Earth System' and 'GLOMAR-Bremen International Graduate School for Marine Sciences'. The authors thank Michael Schreck and Jens Matthiessen for helping to identify unknown dinoflagellates and discussion about the Batiacasphaera complex. Florian Rommerskirchen is thanked for the biogeochemical measurements and Marta Witek for laboratory support. Data are accessible at Pangaea.de.	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J. Earth Sci.	JAN	2017	106	1					171	183		10.1007/s00531-016-1309-0	http://dx.doi.org/10.1007/s00531-016-1309-0			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EK0VU					2025-03-11	WOS:000393646000010
S	Ellegaard, M; Dale, B; Mertens, KN; Pospelova, V; Ribeiro, S		Weckstrom, K; Saunders, KM; Gell, PA; Skilbeck, CG		Ellegaard, Marianne; Dale, Barrie; Mertens, Kenneth N.; Pospelova, Vera; Ribeiro, Sofia			Dinoflagellate Cysts as Proxies for Holocene Environmental Change in Estuaries: Diversity, Abundance and Morphology	APPLICATIONS OF PALEOENVIRONMENTAL TECHNIQUES IN ESTUARINE STUDIES	Developments in Paleoenvironmental Research		English	Article; Book Chapter						Organic microfossils; Paleoecology; Nutrients; Salinity; Temperature; Life-cycle	NORTHERN NORTH-ATLANTIC; SEA-SURFACE TEMPERATURE; SANTA-BARBARA BASIN; BALTIC SEA; SPATIAL-DISTRIBUTION; ADJACENT SEAS; GULLMAR FJORD; RESTING CYSTS; TOKYO-BAY; SEDIMENTARY RECORD	Dinoflagellates are important components of marine plankton as both primary producers and predators on bacteria and microeukaryotes. About 200 species, most of these estuarine, form a resting stage, called a cyst, as part of their life- cycle. Dinoflagellate cysts are mostly organic, composed of a very resistant material called dinosporin, and are often very well preserved in sediments. Dinoflagellate cysts have in many cases provided excellent records of changes through time in salinity, temperature and nutrients, and have also been used to reconstruct changes in sea ice cover, industrial pollution and coastal proximity through time. These environmental changes can be reconstructed from: (1) changes in dinoflagellate cyst communities; (2) changes in abundance; and (3) morphological variations in individual species. The two main methods for concentrating dinoflagellate cysts from sediment samples are palynological processing with HCl and HF, and density separation. As dinoflagellate cysts are mostly organic, they may be preserved where microfossils composed of silica or calcium carbonate are missing because of dissolution.	[Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Fac Sci, Frederiksberg, Denmark; [Dale, Barrie] Univ Oslo, Dept Geosci, Oslo, Norway; [Mertens, Kenneth N.] Ifremer Stn Biol Marine, Concarneau, France; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC, Canada; [Ribeiro, Sofia] Geol Survey Denmark & Greenland, Dept Marine Geol & Glaciol, Copenhagen, Denmark	University of Copenhagen; University of Oslo; University of Victoria; Geological Survey Of Denmark & Greenland	Ellegaard, M (通讯作者)，Univ Copenhagen, Dept Plant & Environm Sci, Fac Sci, Frederiksberg, Denmark.	me@plen.ku.dk; barrie.dale@geo.uio.no; kenneth.mertens@ifremer.fr; vpospe@uvic.ca; sri@geus.dk	Ribeiro, Sofia/AAZ-2782-2021; Mertens, Kenneth/AAO-9566-2020; Ellegaard, Marianne/H-6748-2014; Mertens, Kenneth/C-3386-2015	Pospelova, Vera/0000-0003-4049-8133; Mertens, Kenneth/0000-0003-2005-9483				Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1985, J PHYCOL, V21, P200; 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J	Ning, WX; Andersson, PS; Ghosh, A; Khan, M; Filipsson, HL				Ning, Wenxin; Andersson, Per S.; Ghosh, Anupam; Khan, Mansoor; Filipsson, Helena L.			Quantitative salinity reconstructions of the Baltic Sea during the mid-Holocene	BOREAS			English	Article							DINOFLAGELLATE PROTOCERATIUM-RETICULATUM; PROCESS LENGTH VARIATION; LACUSTRINE CARBONATES; HYDROLOGICAL CHANGES; SURFACE SEDIMENTS; HOLOCENE HISTORY; ISOTOPE RECORDS; CYSTS; STRATIGRAPHY; TEMPERATURE	We reconstructed the past coastal environment of the Baltic Sea from c. 7300 to 3500cal. a BP, with a focus on sea surface salinity (SSS). To quantitatively determine the SSS, two methods were employed: measurements of Sr-87/Sr-86 ratios in mollusc shells (SSSSr) and process length variations of dinoflagellate cysts Operculodinium centrocarpum (SSSpl). The SSSSr was similar to 6-7 between 6800 and 6400cal. a BP, similar to modern conditions. Between 6000 and 3900cal. a BP, SSSSr was consistently higher, ranging between similar to 9 and 13. Microfossils sensitive to salinity variations, such as Radiosperma corbiforum and Spiniferites spp., support the SSSSr estimate. In comparison with the SSSSr, the SSSpl values were consistently higher, with an average of similar to 14. We suggest SSSpl tend to overestimate salinity and are not as reliable as SSSSr. A multi-proxy approach, including analysis of microfossil, organic carbon content, C/N ratios and grain-size, allowed for a division of the study period into three zones (Zones I-III). Zone I (7300-6400cal. a BP) is characterized by relatively O.centrocarpum and R.corbiforum concentrations, silt contents and C/N ratios, corresponding to the regional Littorina transgression maximum. Zone II (6400-3900cal. a BP) is characterized by increased Spiniferites spp. and decreased R.corbiforum abundances, and by lowered C/N ratios and silt contents relative to Zone I. Zone III (3900-3500cal. a BP) represents the start of the Post-Littorina Sea phase, indicating a shift to the modern Baltic Sea phase with decreased salinity.	[Ning, Wenxin; Ghosh, Anupam; Khan, Mansoor; Filipsson, Helena L.] Lund Univ, Dept Geol, Solvegatan 12, SE-22362 Lund, Sweden; [Andersson, Per S.] Swedish Museum Nat Hist, Dept Geosci, SE-10405 Stockholm, Sweden; [Ghosh, Anupam] Jadavpur Univ, Dept Geol Sci, Kolkata 700032, India	Lund University; Swedish Museum of Natural History; Jadavpur University	Ning, WX (通讯作者)，Lund Univ, Dept Geol, Solvegatan 12, SE-22362 Lund, Sweden.	wenxin.ning@geol.lu.se	Ghosh, Anupam/AAK-4306-2020; Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608	FORMAS Strong Research Environment: Managing Multiple Stressors in the Baltic Sea [217-2010-126]; Crafoord Foundation; Royal Physiographic Society in Lund; Swedish Agency for Marine and Water Management (SWAM)	FORMAS Strong Research Environment: Managing Multiple Stressors in the Baltic Sea; Crafoord Foundation; Royal Physiographic Society in Lund; Swedish Agency for Marine and Water Management (SWAM)	We thank the captain and crew of R/V 'Ocean Surveyor' for their help during sampling. We are grateful to Rex Harland and Karin Zonneveld for their guidance on the preparation and identification of the dinoflagellate cyst, and to Hubert Vonhof for the <SUP>13</SUP>C and <SUP>18</SUP>O analysis. Thanks are also due to Svante Bjorck and Bjorn E. Berglund for their discussion of the results. We thank Nathalie V. Putten and Asa Wallin for guidance during the grain-size analysis. We thank two anonymous reviewers and the Guest Editor Prof. Helge W. Arz for comments and improvement of the manuscript. The project was funded by FORMAS Strong Research Environment: Managing Multiple Stressors in the Baltic Sea (217-2010-126). We also acknowledge funding from the Crafoord Foundation and the Royal Physiographic Society in Lund. The hydrographic data used in the project are from SMHI's database - SHARK. The collection of data for SHARK is organized by the Swedish environmental monitoring program and funded by the Swedish Agency for Marine and Water Management (SWAM).	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J	Mousing, EA; Ribeiro, S; Chisholm, C; Kuijpers, A; Moros, M; Ellegaard, M				Mousing, Erik A.; Ribeiro, Sofia; Chisholm, Chelsea; Kuijpers, Antoon; Moros, Matthias; Ellegaard, Marianne			Size differences of Arctic marine protists between two climate periods-using the paleoecological record to assess the importance of within-species trait variation	ECOLOGY AND EVOLUTION			English	Article						cell size; dinoflagellate cysts; interspecific; intraspecific; paleoecology; temperature	INTRASPECIFIC VARIABILITY; WEST GREENLAND; CELL-SIZE; PHYTOPLANKTON; TEMPERATURE; SALINITY; PATTERNS; COMMUNITIES; REVEALS; FUTURE	Mean body size decreases with increasing temperature in a variety of organisms. This size-temperature relationship has generally been tested through space but rarely through time. We analyzed the sedimentary archive of dinoflagellate cysts in a sediment record taken from the West Greenland shelf and show that mean cell size decreased at both intra- and interspecific scales in a period of relatively warm temperatures, compared with a period of relatively cold temperatures. We further show that intraspecific changes accounted for more than 70% of the change in community mean size, whereas shifts in species composition only accounted for about 30% of the observed change. Literature values on size ranges and midpoints for individual taxa were in several cases not representative for the measured sizes, although changes in community mean size, calculated from literature values, did capture the direction of change. While the results show that intraspecific variation is necessary to accurately estimate the magnitude of change in protist community mean size, it may be possible to investigate general patterns, that is relative size differences, using interspecific-level estimates.	[Mousing, Erik A.; Chisholm, Chelsea] Univ Copenhagen, Ctr Macroecol Evolut & Climate, Nat Hist Museum Denmark, Copenhagen, Denmark; [Ribeiro, Sofia; Kuijpers, Antoon] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Copenhagen, Denmark; [Moros, Matthias] Leibniz Inst Baltic Sea Res Warnemunde IOW, Warnemunde, Germany; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci, Copenhagen, Denmark	University of Copenhagen; Geological Survey Of Denmark & Greenland; Leibniz Institut fur Ostseeforschung Warnemunde; University of Copenhagen	Mousing, EA (通讯作者)，Univ Copenhagen, Ctr Macroecol Evolut & Climate, Nat Hist Museum Denmark, Copenhagen, Denmark.	eamousing@snm.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Mousing, Erik Askov/C-4371-2015; Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/G-9213-2018	Mousing, Erik Askov/0000-0003-1663-2507; Ellegaard, Marianne/0000-0002-6032-3376; Ribeiro, Sofia/0000-0003-0672-9161	Danish National Research Foundation [DNRF96]; German Research Council; Villum Foundation, Denmark [VKR023454]	Danish National Research Foundation(Danmarks Grundforskningsfond); German Research Council(German Research Foundation (DFG)); Villum Foundation, Denmark(Villum Fonden)	Danish National Research Foundation, Grant/Award Number: DNRF96; German Research Council; The Villum Foundation, Denmark, Grant/Award Number: VKR023454	Adler PB, 2014, P NATL ACAD SCI USA, V111, P740, DOI 10.1073/pnas.1315179111; Albert CH, 2010, FUNCT ECOL, V24, P1192, DOI 10.1111/j.1365-2435.2010.01727.x; [Anonymous], 0503RV  BALT SEA RES; [Anonymous], 2015, GRIDEXTRA MISCELLANE; ATKINSON D, 1994, ADV ECOL RES, V25, P1, DOI 10.1016/S0065-2504(08)60212-3; ATKINSON D, 1995, J THERM BIOL, V20, P61, DOI 10.1016/0306-4565(94)00028-H; Atkinson D, 2003, P ROY SOC B-BIOL SCI, V270, P2605, DOI 10.1098/rspb.2003.2538; Barton AD, 2016, P NATL ACAD SCI USA, V113, P2964, DOI 10.1073/pnas.1519080113; Bland JM, 1998, BRIT MED J, V316, P129; Blois JL, 2013, P NATL ACAD SCI USA, V110, P9374, DOI 10.1073/pnas.1220228110; 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Evol.	JAN	2017	7	1					3	13		10.1002/ece3.2592	http://dx.doi.org/10.1002/ece3.2592			11	Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Evolutionary Biology	EH9CO	28070270	gold, Green Published			2025-03-11	WOS:000392069500001
J	Barron, A; Zobaa, MK; Oboh-Ikuenobe, FE				Barron, Adam; Zobaa, Mohamed K.; Oboh-Ikuenobe, Francisca E.			Palynological evidence for sustained deep-marine conditions during the Eocene-Miocene in the southern Gulf of Mexico distal continental margin	GEOLOGICAL SOCIETY OF AMERICA BULLETIN			English	Article							DINOFLAGELLATE CYST DISTRIBUTION; NORTH-WESTERN DESERT; POLLEN FLORAS; USA; PALYNOFACIES; MISSISSIPPI; PALEOCENE; BASIN; SEA; SEDIMENTS	The present study represents the first attempt to provide palynological data about the southern Gulf of Mexico distal continental margin during the Eocene-Miocene time interval. In addition to documenting the types of fossil palynomorphs preserved in these economically critical rock sequences, this study also provides important information about the accumulation and preservation of total sedimentary particulate organic matter along with their paleoenvironmental and paleoceanographic implications. This was accomplished through the analysis of cored sediments from the Deep Sea Drilling Project Site 94 north of the Yucatan Peninsula and Site 540 south of the Western Florida Escarpment. The present findings from the deep waters of southern Gulf of Mexico are expected to greatly assist hydrocarbon geo-scientists in their exploration and development efforts, reducing investment risk and drilling uncertainty. Two palynofacies assemblages were recognized based on particulate organic matter analysis: marine-dominated palynofacies A and terrestrially influenced palynofacies B. The organic compositions of these two palynofacies along with the recovered dino-flagellate cyst community suggest that while sustained oceanic depositional conditions were prevalent, occasional influxes of terrestrial organic material of variable magnitudes occurred. These short-term influxes were especially pronounced during the late Eocene and earliest Oligocene and appear to have happened in response to the cooling and slight global sea-level drop that occurred at ca. 38-33.5 Ma. The preserved terrestrial palynomorphs in the samples indicate coastal plain and estuarine vegetation sources in general, except during the Eocene-Oligocene transition, when anemophilous pollen specimens mostly derived from farther inland and montane sources were recovered.	[Barron, Adam; Zobaa, Mohamed K.; Oboh-Ikuenobe, Francisca E.] Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Rolla, MO 65409 USA; [Zobaa, Mohamed K.] Benha Univ, Dept Geol, Fac Sci, Banha 13518, Egypt	University of Missouri System; Missouri University of Science & Technology; Egyptian Knowledge Bank (EKB); Benha University	Zobaa, MK (通讯作者)，Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Rolla, MO 65409 USA.; Zobaa, MK (通讯作者)，Benha Univ, Dept Geol, Fac Sci, Banha 13518, Egypt.	apbhx5@mst.edu; mohamed.zobaa@mst.edu; ikuenobe@mst.edu	Zobaa, Mohamed/AAF-7062-2020; Zobaa, Mohamed/L-4058-2017	Zobaa, Mohamed/0000-0002-1592-5781; Oboh-Ikuenobe, Francisca/0000-0002-2223-9691	Josephine Husbands Radcliffe Fellowship	Josephine Husbands Radcliffe Fellowship	We wish to thank the staff at Integrated Ocean Drilling Program (IODP) repository at Texas A&M University for providing the samples used in this research. 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J	Yanchilina, AG; Ryan, WBF; McManus, JF; Dimitrov, P; Dimitrov, D; Slavova, K; Filipova-Marinova, M				Yanchilina, Anastasia G.; Ryan, William B. F.; McManus, Jerry F.; Dimitrov, Petko; Dimitrov, Dimitar; Slavova, Krasimira; Filipova-Marinova, Mariana			Compilation of geophysical, geochronological, and geochemical evidence indicates a rapid Mediterranean-derived submergence of the Black Sea's shelf and subsequent substantial salinification in the early Holocene	MARINE GEOLOGY			English	Article						Black Sea transgression; Isotope geochemistry; Black Sea; Marine-lake connections; Reflection profiles; Paleoceanography; Paleosalinity; Lake transgression	MARMARA SEA; DINOFLAGELLATE CYSTS; LEVEL CHANGES; ISOTOPE; SEDIMENTS; PLEISTOCENE; MORPHOLOGY; EVOLUTION; AGE; TRANSGRESSION	Our knowledge of rate and processes in which semi-enclosed environments alternate from lacustrine to marine is commonly limited because of the paucity of specific proxies for sea level and salinity. Here we investigate the timing, rate, and key mechanisms involved in the transformation of the previously isolated Black Sea-Lake to the modern partly-enclosed marine sea using a suite of geophysical, geochemical, and geochronological methods. Cores were collected in transects across shelves of Ukraine, Romania, Bulgaria, and Turkey. Biogenic carbonate from these cores was analyzed for radiocarbon and strontium, oxygen, and carbon isotopes. Strontium results indicate that the submergence of the Black Sea shelf at 9300 calendar years BP was caused by the ingress of Mediterranean water and was abrupt, taking <40 years. The seismic reflection profiles show a uniform drape of subsequent sediment over aeolian dunes indicating a drowning with no time for erosion accompanying the submergence. Moisture measurements beneath the uniform drape indicate that the shelf was dry before submergence and the shoreline of the Preboreal lake may have regressed to beyond 120 mbsl. Mollusks colonized the newly submerged substrate of the inner shelf at the same time as they colonized the outer shelf. The succession of mollusk species with shells whose strontium isotope composition has a marine component indicates a rising salinity. The transformation of the lake to a sea is affirmed by increases in the shells' strontium and oxygen isotopic ratios towards the external ocean value. Radiocarbon years are calibrated to calendar years by tuning the oxygen and carbon isotope composition of the mollusk record to that of the Uffh dated Sofular Cave stalagmites. The match shows a reduction of the lake's prior high reservoir age accompanying the inflow of the Mediterranean water. In 900 years the salinity reached a threshold that excluded all previous Black Sea lacustrine fauna. These results imply that any substantial postglacial submergence of the Black Sea shelves did not occur prior to entry of Mediterranean water. (C) 2016 The Authors. Published by Elsevier B.V.	[Yanchilina, Anastasia G.; Ryan, William B. F.; McManus, Jerry F.] Columbia Univ, Lamont Doherty Earth Observ, 61 Route 9W, New York, NY 10027 USA; [Dimitrov, Petko; Dimitrov, Dimitar; Slavova, Krasimira] Bulgarian Acad Sci, Inst Oceanol, Varna 9000, Bulgaria; [Filipova-Marinova, Mariana] Varna Reg Museum Hist, 41 Maria Louisa Blvd, Varna 9000, Bulgaria; [Yanchilina, Anastasia G.] Weizmann Inst Sci, 234 Herzl St, IL-7610001 Rehovot, Israel	Columbia University; Bulgarian Academy of Sciences; Weizmann Institute of Science	Yanchilina, AG (通讯作者)，Columbia Univ, Lamont Doherty Earth Observ, 61 Route 9W, New York, NY 10027 USA.; Yanchilina, AG (通讯作者)，Weizmann Inst Sci, 234 Herzl St, IL-7610001 Rehovot, Israel.	nyanchil@ldeo.columbia.edu; billr@ldeo.columbia.edu; jmcmanus@ldeo.columbia.edu; margeo@io-bas.bg; dimpetdim@io-bas.bg; marianafilipova@yahoo.com	Yanchilina, Anastasia/GQQ-2125-2022; Dimitrov, Petko/T-6909-2019; Dimitrov, Dimitar Petkov/B-7374-2017	mcmanus, jerry/0000-0002-7365-1600; Filipova-Marinova, Mariana/0000-0002-0786-9476; Ryan, William B F/0000-0002-9447-6610; Yanchilina, Anastasia Gennadyevna/0000-0003-3782-6343; Dimitrov, Petko/0000-0003-2280-2058; Dimitrov, Dimitar Petkov/0000-0001-8402-9529				Aksu AE, 2002, MAR GEOL, V190, P119, DOI 10.1016/S0025-3227(02)00345-6; Algan O., 2007, The Black Sea Flood Question: Changes in Coastline, Climate, and Human Settlement, P603; Apakidze A.M., 1987, Radiouglerodnoe datirovanie arkheologicheskikh i paleobotanicheskikh abraztzov Gruzii (Radiocarbon dating of archaeological and paleobotanical samples in georgia); Arkhangel'skiy A.D., 1938, Izv. 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M., 2007, MOSCOW U GEOLOGY B, V62; Soulet G, 2011, QUATERNARY SCI REV, V30, P1019, DOI 10.1016/j.quascirev.2011.03.001; Soulet G, 2010, EARTH PLANET SC LETT, V296, P57, DOI 10.1016/j.epsl.2010.04.045; Soulet G, 2011, EARTH PLANET SC LETT, V308, P245, DOI 10.1016/j.epsl.2011.06.002; Strakhov N.M., 1971, Lithology and Mineral Resources, V3, P263; Wall D., 1974, Dinoflagellates in Late Quaternary Deep-Water Sediments of Black Sea; Wesselingh F., 2015, COMMUNICATION; Yanko-Hombach V., 2011, Geologiya i poleznie iskopamye Mirovogo Okeana (Geology and mineral resources of the World Ocean), V2, P61; Yanko-Hombach V, 2007, QUATERN INT, V167, P91, DOI 10.1016/j.quaint.2006.08.004; Yanko-Hombach V, 2014, QUATERN INT, V345, P100, DOI 10.1016/j.quaint.2013.07.027; ZUBAKOV VA, 1988, QUATERNARY RES, V29, P1, DOI 10.1016/0033-5894(88)90067-1	101	51	55	1	36	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0025-3227	1872-6151		MAR GEOL	Mar. Geol.	JAN 1	2017	383						14	34		10.1016/j.margeo.2016.11.001	http://dx.doi.org/10.1016/j.margeo.2016.11.001			21	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	EI8VR		hybrid			2025-03-11	WOS:000392786800002
J	Nicholls, KH				Nicholls, Kenneth H.			Introduction to the biology and ecology of the freshwater cryophilic dinoflagellate <i>Woloszynskia pascheri</i> causing red ice	HYDROBIOLOGIA			English	Article						Woloszynskia pascheri; Freshwater red tide; Cryophilic; Psychrophily; Red ice; Extreme cold tolerance	LOW-TEMPERATURE RESISTANCE; SP-NOV DINOPHYCEAE; LAKE TOVEL; LIGHT; ULTRASTRUCTURE; GYMNODINIUM; PHYLOGENY; DIVERSITY; GEN.; ONTARIO	The rarely reported red pigmented dinoflagellate, Woloszynskia pascheri, is described from frozen surface waters in Ontario, Canada. New information based on light microscopy (LM) is provided on cell organelles (dinokaryon, chromosomes, pigment droplets and ectoplasmic vesicular layer), the thin-walled ice-bound pellicle cysts and thick-walled summer resting cysts. An earlier published suggestion that W. pascheri has morphology similar to that of Gymnodinium cryophilum (Wedemayer, Wilcox et Graham) G. Hansen et Moestrup is refuted. The process of red ice formation depends on a number of weather-related and other environmental factors. The most important of these being a mid-winter thaw that creates pathways (cracks and melted areas of ice) for passage of swimming cells from the water underlying the ice to water on the surface of the ice. In thin-walled ice-bound pellicle cysts, W. pascheri remained viable at ambient air temperatures lower than -20A degrees C for several days and suggests a unique biochemical physiology that needs research. A summary of the historical classification of this species reveals a tumultuous past and the continuing assignment of this species within the genus Woloszynskia appears doubtful, given the rapidly improving state of knowledge about the fine structure and molecular biology of many other similar species.	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Ges, V34, P242; Sundström AM, 2009, J PHYCOL, V45, P938, DOI 10.1111/j.1529-8817.2009.00712.x; Takahashi K, 2015, PROTIST, V166, P638, DOI 10.1016/j.protis.2015.10.003; Taylor FJR, 2008, BIODIVERS CONSERV, V17, P407, DOI 10.1007/s10531-007-9258-3; Thessen AE, 2012, PLOS ONE, V7, DOI 10.1371/journal.pone.0044015; Thomashow MF, 1998, PLANT PHYSIOL, V118, P1, DOI 10.1104/pp.118.1.1; Thompson R.H., 1951, Lloydia, V13, P277; Von Stosch HA., 1973, Br Phycol J, V8, P105; WEDEMAYER GJ, 1982, J PHYCOL, V18, P13, DOI 10.1111/j.1529-8817.1982.tb03152.x; WILCOX LW, 1989, J PHYCOL, V25, P785, DOI 10.1111/j.0022-3646.1989.00785.x; WILCOX LW, 1986, PROTOPLASMA, V135, P71, DOI 10.1007/BF01277000; Zhang J, 2010, APPL ENVIRON MICROB, V76, P2989, DOI 10.1128/AEM.00026-09	51	5	5	0	27	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0018-8158	1573-5117		HYDROBIOLOGIA	Hydrobiologia	JAN	2017	784	1					305	319		10.1007/s10750-016-2885-5	http://dx.doi.org/10.1007/s10750-016-2885-5			15	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	EB6IA					2025-03-11	WOS:000387484100022
J	Liu, Y; Sun, QL; Fan, DD; Lai, XH; Xu, LC; Finlayson, B; Chen, ZY				Liu, Yan; Sun, Qianli; Fan, Daidu; Lai, Xiaohe; Xu, Lichen; Finlayson, Brian; Chen, Zhongyuan			Pollen evidence to interpret the history of rice farming at the Hemudu site on the Ningshao coast, eastern China	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	Nagoya International Quaternary Science Meeting	2015	Nagoya, JAPAN			Pollen analysis; Environmental changes; Hemudu Culture; Rice farming; Ningshao coastal plain	HOLOCENE ENVIRONMENTAL-CHANGE; SEA-LEVEL HIGHSTAND; YANGTZE DELTA; PLAIN; DOMESTICATION; AGRICULTURE; CULTIVATION; CALIBRATION; FIELDS; FIRE	A 3.12-m sediment core named HMD was retrieved near the Hemudu archaeological site to decode the rice farming history and its connection to the environment change at the site since mid-Holocene. Microfossil results together with core lithology indicated a brackish supra-tidal flat deposition prior to ca. 6500 years ago, on which the Hemudu people settled. A desalinized environment indicated by abundant aquatic herbs and declined dinoflagellate at ca. 6500-6200 cal yr BP would have favored human occupation and rice farming assisted by clearing and firing. This then followed by a significant increase of Pinus pollen and fern spores, suggesting enhanced fluvial processes possibly under a cooler climate setting, which might have constrained the living space for the ancestors and weakened the rice farming activities at the site. Rice farming returned at ca. 5500-5200 cal yr BP with an ameliorated climate and suitable coastal environment as evidenced by increases of Poaceae pollen, charcoal remains and the emergence of more sites at the late Hemudu Culture stage. From ca. 5200 cal yr BP, fern spores and freshwater algae increased, implying an expanded waterbody probably associated with the migration of the Yaojiang River that made the Hemudu site no longer favorable for human occupation. (C) 2016 Elsevier Ltd and INQUA. All rights reserved.	[Liu, Yan; Sun, Qianli; Lai, Xiaohe; Xu, Lichen; Chen, Zhongyuan] East China Normal Univ, State Kay Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China; [Liu, Yan; Fan, Daidu] Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China; [Finlayson, Brian] Univ Melbourne, Sch Geog, Melbourne, Vic 3010, Australia	East China Normal University; Tongji University; University of Melbourne	Sun, QL (通讯作者)，East China Normal Univ, State Kay Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.	qlsun@sklec.ecnu.edu.cn	Chen, Zhong Yuan/JRW-5575-2023; Qianli, Sun/GYU-4636-2022; Finlayson, Brian/H-9638-2014; Lai, Xiaohe/AIE-1483-2022	Liu, Yan/0000-0003-3521-4650				[Anonymous], QUATERNARY INT; Chang Kwang-Chih., 1986, The Archaeology of Ancient China; Chen ZY, 1998, J COASTAL RES, V14, P360; Fang X. F., 2006, THESIS; Fuller D. 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DEC 28	2016	426						195	203		10.1016/j.quaint.2016.05.016	http://dx.doi.org/10.1016/j.quaint.2016.05.016			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Arts &amp; Humanities Citation Index (A&amp;HCI); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	EF7US					2025-03-11	WOS:000390535300024
J	Paterson, NW; Mangerud, G; Cetean, CG; Mork, A; Lord, GS; Klausen, TG; Morkved, PT				Paterson, Niall William; Mangerud, Gunn; Cetean, Claudia G.; Mork, Atle; Lord, Gareth Steven; Klausen, Tore Grane; Morkved, Pal Tore			A multidisciplinary biofacies characterisation of the Late Triassic (late Carnian-Rhaetian) Kapp Toscana Group on Hopen, Arctic Norway	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Late Triassic; Kapp Toscana Group; Palynology; Palynofacies; Micropaleontology; Svalbard	BARENTS SEA; PALYNOFACIES ANALYSIS; GEERDALEN FORMATION; SNADD FORMATION; SVALBARD; STRATIGRAPHY; PALYNOLOGY; RECORDS; SPORES; MIDDLE	A multidisciplinary study of the Kapp Toscana Group (De Geerdalen, Flatsalen and Svenskoya formations) on Hopen, Svalbard, provides an enhanced palaeoenvironmental interpretation for the Upper Triassic succession on the island. The biofacies of the formations were characterised using a combination of palynological, palynofacies and micropalaeontological analyses. Micropalaeontological, palynofacies and delta C-13(org) data are presented from Hopen for the first time. Six distinct biofacies assemblages were recognised: (I) Lower undifferentiated De Geerdalen Formation, characterised by a dominance of fern spores, and low abundance assemblages of foraminifera and ostracods, interpreted to reflect deposition in a deltaic environment during maximum marine regression; (II) Upper De Geerdalen Formation, Hopen Member, rich in bisaccate gymnosperm pollen and the alga Plaesiodictyon mosellaneum, consistent with deposition in a brackish marginal marine setting; (III) Lower Flatsalen Formation, characterised by microforaminiferal linings, marine phytoplankton and super-abundant agglutinated foraminifera, considered to reflect deposition in a shallow marine environment; (IV) Middle Flatsalen Formation, dominated by dinoflagellate cysts, radiolaria and ostracods, indicating deposition in a relatively distal, dysoxic-anoxic marine environment (a maximum flooding surface is inferred based on the acme of radiolarians and dominance of dinoflagellate cysts); (V) Upper Flatsalen Formation, corresponding to a decrease in marine palynomorphs, absence of radiolaria, agglutinated foraminifera and ostracods, and an increase in terrestrial organic matter; and (VI) Svenskoya Formation, characterised by a dominance of terrestrial palynomorphs and deposited in a fluvio-deltaic environment. The biofacies units are integrated with the established litho-, chrono- and palynostratigraphic framework for the island and contribute to an enhanced palaeogeographic understanding of the Barents Sea region during the Late Triassic. (C) 2015 Elsevier B.V. All rights reserved.	[Paterson, Niall William; Mangerud, Gunn; Klausen, Tore Grane; Morkved, Pal Tore] Univ Bergen, Dept Earth Sci, Allegaten 41, N-5020 Bergen, Norway; [Cetean, Claudia G.] CGG Serv UK Ltd, Llandudno LL30 1SA, Wales; [Mork, Atle] SINTEF Petr Res Geophys & Reservoir Technol, SP Andersens Veg 15A, N-7031 Trondheim, Norway; [Mork, Atle; Lord, Gareth Steven] Norwegian Univ Sci & Technol, Dept Geol & Mineral Resources Engn, N-7491 Trondheim, Norway; [Lord, Gareth Steven] Univ Ctr Svalbard UNIS, Longyearbyen, Norway	University of Bergen; SINTEF; Norwegian University of Science & Technology (NTNU); University Centre Svalbard (UNIS)	Paterson, NW (通讯作者)，Univ Bergen, Dept Earth Sci, Allegaten 41, N-5020 Bergen, Norway.	niall.paterson@uib.no; gunn.mangerud@uib.no; claudia.cetean@cgg.com; atlemork@ntnu.no; gareth.lord@ntnu.no; tore.klausen@uib.no; pal.morkved@uib.no	Mangerud, Gunn/ABD-2588-2020	Paterson, Niall W./0000-0002-2645-2086; Lord, Gareth Steven/0000-0002-4659-0080; Klausen, Tore Grane/0000-0003-2524-512X	FORCE industry consortium; Centrica; Chevron; ConocoPhillips; Det Norske; Dong; ENI; Lundin; Shell; Statoil	FORCE industry consortium; Centrica; Chevron; ConocoPhillips; Det Norske; Dong; ENI; Lundin; Shell(Royal Dutch Shell); Statoil	This research is funded by a FORCE industry consortium, consisting of: Centrica, Chevron, ConocoPhillips, Det Norske, Dong, ENI, Lundin, Shell and Statoil. We thank Malcolm Jones (PLS PalyLab) for preparation of palynological slides and Jordan Donn Holl (University of Bergen) for preparing samples for carbon isotope analyses. We thank the Norwegian Petroleum Directorate for the invitation to participate in the 2011 Hopen expedition. We also thank Prof. Vivi Vajda, Dr. Sofie Lindstrom and one anonymous reviewer for their constructive comments on this manuscript.	Abbink OA, 2004, NETH J GEOSCI, V83, P17, DOI 10.1017/S0016774600020436; Allen Sharon., 1991, Sequence Stratigraphy as an Exploration Tool, P11; [Anonymous], 1998, LPP Contributions Series; [Anonymous], 1977, NORSK POLARINSTITUTT; [Anonymous], 1975, Geosci. 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Paleoclimatol. Paleoecol.	DEC 15	2016	464				SI		16	42		10.1016/j.palaeo.2015.10.035	http://dx.doi.org/10.1016/j.palaeo.2015.10.035			27	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	ED8GI					2025-03-11	WOS:000389109600003
J	Park, TG; Kim, JJ; Kim, WJ; Won, KM				Park, Tae Gyu; Kim, Jin Joo; Kim, Won Jin; Won, Kyoung Mi			Development of real-time RT-PCR for detecting viable <i>Cochlodinium polykrikoides</i> (Dinophyceae) cysts in sediment	HARMFUL ALGAE			English	Article						Cochlodinium polykrikoides; Cyst; Dinoflagellate; Real-time RT-PCR; Red tide	POLYMERASE-CHAIN-REACTION; RED TIDE DINOFLAGELLATE; KOREAN COASTAL WATERS; MARINE-SEDIMENTS; HARMFUL DINOFLAGELLATE; ALEXANDRIUM-TAMARENSE; PFIESTERIA-PISCICIDA; PHYLOGENETIC-RELATIONSHIPS; ENVIRONMENTAL-SAMPLES; MARGALEF DINOPHYCEAE	Morphological observations have confirmed that cysts are produced by dinoflagellates. However, finding a seed bed or unknown cysts in field samples by microscopy is extremely time consuming. Real-time PCR has been used to facilitate the detection of dinoflagellate cysts in sediment. However, DNA from dead vegetative cells remaining on the surface sediment may persist for a long period of time, which can cause false positive DNA detection. In this study, a non-quantitative RNA targeted probe using real-time RT-PCR was developed for detection of viable cysts in sediment. Large-subunit rRNA was used to develop a species-specific RNA targeted probe for the ichthyotoxic dinoflagellate Cochlodinium polykrikoides. The sediment samples were sieved and incubated at 30 degrees C for 3 h prior to RNA extraction to remove RNA from dead cells remaining in the sediment. Nested-PCR was conducted to maximize assay sensitivity. A field survey to determine the distribution of cysts at 155 sampling stations in the western and southern part of the Korean peninsula showed that C polykrikoides cysts were detected at five sampling stations. (C) 2016 Elsevier B.V. All rights reserved.	[Park, Tae Gyu; Kim, Jin Joo; Kim, Won Jin; Won, Kyoung Mi] Natl Inst Fisheries Sci, Southeast Sea Fisheries Res Inst, Tongyeong 650943, South Korea	National Institute of Fisheries Science	Park, TG (通讯作者)，Natl Inst Fisheries Sci, Southeast Sea Fisheries Res Inst, Tongyeong 650943, South Korea.	taegyupark@korea.kr			National Institute of Fisheries Science [R2016046]	National Institute of Fisheries Science	We thank Drs. Mi Seon Park and Won Duk Yoon of the NIFS for their valuable comments and suggestions. We also thank Drs. Jong Woo Park and Seung Min Lee of the NIFS for the sediment samples from Yeosu and the Yellow Sea. This study was funded by a grant from the National Institute of Fisheries Science (R2016046).	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J	Ganne, A; Leroyer, C; Penaud, A; Mojtahid, M				Ganne, A.; Leroyer, C.; Penaud, A.; Mojtahid, M.			Present-day palynomorph deposits in an estuarine context: The case of the Loire Estuary	JOURNAL OF SEA RESEARCH			English	Article						Loire; Surface sediments; Pollen and dinoflagellate cysts; Estuarine dynamics	DINOFLAGELLATE CYST ASSEMBLAGES; RECENT MARINE-SEDIMENTS; SURFACE SEDIMENTS; POLLEN TRANSPORT; QUANTITATIVE RECONSTRUCTION; BRITISH-COLUMBIA; ORGANIC-MATTER; FRESH-WATER; BLACK-SEA; VEGETATION	Estuaries are dynamic systems that collect terrestrial, aerial, fluvial, and marine inputs, including organic micro fossils, which, when fossilized and observed on palynological slides, are also referred to as palynomorphs (pollen and non-pollen palynomorphs including dinoflagellate cysts or dinocysts). To understand these organic micro fossil deposit arrangements across the Loire estuary, palynomorph counts were undertaken in 31 surface sediments collected across longitudinal and perpendicular transects of the Loire active riverbed, from the upper inner estuary to the river mouth. Main results suggest a large homogeneity of the pollen content throughout the entire upstream-downstream transect, with a dominance of arboreal taxa (Pinus, Quercus, Alnus) and Poaceae. Also, perpendicular transects across the channel show a great similarity between the muddy surface layers and the underlying consolidated clay layers. This is probably due to: i) homogeneity of the landscape at a regional scale (large catchment area of the Loire River), and ii) complex hydrodynamic processes involving strong mixing of the palynological signal. Furthermore, despite scarce woodlands in the regional landscape, arboreal-pollen (especially Pinus and Quercus) represents >60% of the total pollen percentages. This could be explained by several factors: i) generally higher arboreal pollen production and dispersion as compared to herbaceous taxa, ii) distant inputs from marine areas downstream and/or forested regions far upstream, and iii) differential selection or inheritance from underlying sediments. Differentiation between the outer and inner estuarine environments was furthermore possible using a ratio of terrestrial versus marine palynological indicators. Among the dinocyst assemblages (marine realm), the euryhaline species Lingulodinium machaeropho rum predominates; this taxon being very sensitive to strong water column stratification. Also, total dinocyst concentration increased upstream, which may result from the tidal forcing pushing salinity upriver beneath outflowing river water, and thus signing the estuarine turbidity maximum influence within the Loire River. (C) 2016 Elsevier B.V. All rights reserved.	[Ganne, A.; Leroyer, C.] Univ Rennes 1, CNRS, UMR 6566, Lab Archeosci, Campus Beaulieu,263 Av Gen Leclerc,CS 74205, F-35042 Rennes, France; [Ganne, A.; Penaud, A.] Univ Brest, CNRS, UMR Domaines Ocean 6538, IUEM, F-29280 Plouzane, France; [Mojtahid, M.] Univ Angers, CNRS, UMR 6112, LPG,BIAF,UFR Sci, 2 Bd Lavoisier, F-49045 Angers 01, France	Universite de Rennes; Centre National de la Recherche Scientifique (CNRS); 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); Centre National de la Recherche Scientifique (CNRS); Universite d'Angers	Ganne, A (通讯作者)，Univ Rennes 1, CNRS, UMR 6566, Lab Archeosci, Campus Beaulieu,263 Av Gen Leclerc,CS 74205, F-35042 Rennes, France.	axelle.ganne@univ-rennes1.fr	Penaud, Aurelie/F-2485-2011	Penaud, Aurelie/0000-0003-3578-4549	European Regional Development Fund (FEDER)	European Regional Development Fund (FEDER)(European Union (EU))	This work is connected to the SEMHABEL project, financed by the European Regional Development Fund (FEDER). We are grateful to G. Maillet (BIAF laboratory, University of Angers) for connecting us with the SEMHABEL project, to L Charrieau (POLEN laboratory, University of Nantes) for processing the palynological treatments, to D. Aoustln (Archeosciences laboratory, University of Rennes 1, UMR 6566) for his help with plant and palynological identifications and to Marie Cachera (LEMAR, UMR 6539) for her advises in statistical treatments. The authors are also pleased to acknowledge the two anonymous reviewers and E. Metzger for their comments, M. Thibeaudon and G. Oliver (R.N.S.A.) for providing us Nantes city airborne pollen data, S. Cerisier (GIP Loire) for answering our questions about soil occupation data of the Loire estuary and finally Katalin Kovacs for her reread of this manuscript.	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Sea Res.	DEC	2016	118				SI		35	51		10.1016/j.seares.2016.10.006	http://dx.doi.org/10.1016/j.seares.2016.10.006			17	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	EG1WX					2025-03-11	WOS:000390826000003
J	Prioretti, L; Giordano, M				Prioretti, Laura; Giordano, Mario			DIRECT AND INDIRECT INFLUENCE OF SULFUR AVAILABILITY ON PHYTOPLANKTON EVOLUTIONARY TRAJECTORIES	JOURNAL OF PHYCOLOGY			English	Article						algae evolution; ATP sulfurylase; cell composition; elemental stoichiometry; sulfate assimilation; sulfur metabolism	TRANSFORM INFRARED-SPECTROSCOPY; MARINE-PHYTOPLANKTON; SULFATE ASSIMILATION; CYSTEINE SYNTHASE; ATP SULFURYLASE; SERINE ACETYLTRANSFERASE; ELEMENTAL STOICHIOMETRY; ARABIDOPSIS-THALIANA; CHLOROPHYLL-A; HIGHER-PLANTS	The sulfate facilitation hypothesis suggests that changes in ocean sulfate concentration influenced the rise to dominance of phytoplankton species of the red lineage. The mechanistic reasons for this phenomenon are not yet understood. We started to address this question by investigating the differences in S utilization by algae of the green and red lineages and in cyanobacteria cultured in the presence of either 5 mmol . L-1 (approximately equivalent to Paleozoic ocean concentrations) or 30 mmol . L-1 (corresponding to post-Mesozoic/extant concentrations) sulfate. The activities of the main enzymes involved in SO42- dassimilation changed in response to changes in growth sulfate concentration. ATP sulfurylase showed different kinetics in the various taxa, with an especially odd behavior for the dinoflagellate. Sulfate availability had a modest effect on cell organic composition. Species-specific differences in the use of some elements were instead obvious in algae grown in the presence of different sulfate concentrations, overall confirming that algae of the red lineage do better at high sulfate than algae of the green lineage. The increase in sulfate concentration may thus have had an impact on phytoplankton radiation both through changes in their enzymatic machinery and through indirect repercussion on elemental usage.	[Prioretti, Laura; Giordano, Mario] Univ Politecn Marche, Lab Algal & Plant Physiol, Dipartimento Sci Vita & Ambiente, Via Brecce Bianche, I-60131 Ancona, Italy; [Giordano, Mario] Acad Sci Czech Republic, Inst Microbiol, Algatech, Trebon, Czech Republic; [Giordano, Mario] CNR, Inst Marine Sci, Venice, Italy; [Prioretti, Laura] Aix Marseille Univ, Inst Microbiol Mediterranee, Lab Bioenerget & Ingn Prot, CNRS,UMR 7281, 31 Chemin Joseph Aiguier, F-13402 Marseille 20, France	Marche Polytechnic University; Czech Academy of Sciences; Institute of Microbiology of the Czech Academy of Sciences; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR); Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS)	Giordano, M (通讯作者)，Univ Politecn Marche, Lab Algal & Plant Physiol, Dipartimento Sci Vita & Ambiente, Via Brecce Bianche, I-60131 Ancona, Italy.; Giordano, M (通讯作者)，Acad Sci Czech Republic, Inst Microbiol, Algatech, Trebon, Czech Republic.; Giordano, M (通讯作者)，CNR, Inst Marine Sci, Venice, Italy.	m.giordano@univpm.it	Giordano, Mario/A-8949-2008					[Anonymous], PHYSL MICROALGAE; Behrenfeld MJ, 2008, PHILOS T R SOC B, V363, P2687, DOI 10.1098/rstb.2008.0019; Bochenek M, 2013, NEW PHYTOL, V199, P650, DOI 10.1111/nph.12303; Bromke MA, 2013, AMINO ACIDS, V44, P1253, DOI 10.1007/s00726-013-1462-8; BRUNOLD C, 1987, PHYSIOL PLANTARUM, V70, P168, DOI 10.1111/j.1399-3054.1987.tb06127.x; BURNELL JN, 1984, PLANT PHYSIOL, V75, P873, DOI 10.1104/pp.75.3.873; Butterfield ER, 2013, PROTIST, V164, P218, DOI 10.1016/j.protis.2012.09.001; DIXON GK, 1988, NEW PHYTOL, V109, P297, DOI 10.1111/j.1469-8137.1988.tb04198.x; Domenighini A, 2009, J PHYCOL, V45, P522, DOI 10.1111/j.1529-8817.2009.00662.x; Droux M, 1998, EUR J BIOCHEM, V255, P235, DOI 10.1046/j.1432-1327.1998.2550235.x; Falkowski PG, 2004, SCIENCE, V305, P354, DOI 10.1126/science.1095964; Fanesi A, 2014, PLANT CELL ENVIRON, V37, P512, DOI 10.1111/pce.12176; GAITONDE MK, 1967, BIOCHEM J, V104, P627, DOI 10.1042/bj1040627; Geider RJ, 2002, EUR J PHYCOL, V37, P1, DOI 10.1017/S0967026201003456; Giordano M, 2000, PLANT PHYSIOL, V124, P857, DOI 10.1104/pp.124.2.857; Giordano M, 2005, NEW PHYTOL, V166, P371, DOI 10.1111/j.1469-8137.2005.01335.x; Giordano M, 2001, J PHYCOL, V37, P271, DOI 10.1046/j.1529-8817.2001.037002271.x; Giordano M, 2015, PLANT CELL ENVIRON, V38, P2313, DOI 10.1111/pce.12551; Giordano M, 2014, AQUAT BOT, V118, P45, DOI 10.1016/j.aquabot.2014.06.012; Giordano M, 2013, PLANT SCI, V211, P92, DOI 10.1016/j.plantsci.2013.07.008; Hell Rudiger, 2011, Arabidopsis Book, V9, pe0154, DOI 10.1199/tab.0154; Ho TY, 2003, J PHYCOL, V39, P1145, DOI 10.1111/j.0022-3646.2003.03-090.x; JEFFREY SW, 1975, BIOCHEM PHYSIOL PFL, V167, P191, DOI 10.1016/s0015-3796(17)30778-3; Khan MS, 2010, PLANT CELL, V22, P1216, DOI 10.1105/tpc.110.074088; Logan HM, 1996, J BIOL CHEM, V271, P12227, DOI 10.1074/jbc.271.21.12227; MONOD J, 1949, ANNU REV MICROBIOL, V3, P371, DOI 10.1146/annurev.mi.03.100149.002103; Montechiaro F, 2010, J PLANT PHYSIOL, V167, P110, DOI 10.1016/j.jplph.2009.07.013; NAKAMURA K, 1987, PLANT CELL PHYSIOL, V28, P885, DOI 10.1093/oxfordjournals.pcp.a077370; Norici A, 2005, PHOTOSYNTH RES, V86, P409, DOI 10.1007/s11120-005-3250-0; Palmucci M, 2012, ENVIRON EXP BOT, V75, P220, DOI 10.1016/j.envexpbot.2011.07.005; Palmucci M, 2011, J PHYCOL, V47, P313, DOI 10.1111/j.1529-8817.2011.00963.x; Patron NJ, 2008, BMC EVOL BIOL, V8, DOI 10.1186/1471-2148-8-39; PETERSON GL, 1977, ANAL BIOCHEM, V83, P346, DOI 10.1016/0003-2697(77)90043-4; PORRA RJ, 1989, BIOCHIM BIOPHYS ACTA, V975, P384, DOI 10.1016/S0005-2728(89)80347-0; PORRA RJ, 1990, BIOCHIM BIOPHYS ACTA, V1019, P137, DOI 10.1016/0005-2728(90)90135-Q; Prioretti L, 2014, FRONT PLANT SCI, V5, DOI 10.3389/fpls.2014.00597; Quigg A, 2003, NATURE, V425, P291, DOI 10.1038/nature01953; Quigg A, 2011, P ROY SOC B-BIOL SCI, V278, P526, DOI 10.1098/rspb.2010.1356; Ratti S, 2011, GEOBIOLOGY, V9, P301, DOI 10.1111/j.1472-4669.2011.00284.x; Ratti S, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0077349; RAVEN JA, 1991, LIMNOL OCEANOGR, V36, P1701, DOI 10.4319/lo.1991.36.8.1701; Ravina CG, 2002, PLANT PHYSIOL, V130, P2076, DOI 10.1104/pp.012484; SAITO E, 1969, AGR BIOL CHEM TOKYO, V33, P860, DOI 10.1080/00021369.1969.10859391; Schobben M, 2015, P NATL ACAD SCI USA, V112, P10298, DOI 10.1073/pnas.1503755112; Schulze K, 2011, BMC BIOTECHNOL, V11, DOI 10.1186/1472-6750-11-118; van Creveld SG, 2015, ISME J, V9, P385, DOI 10.1038/ismej.2014.136; Wirtz M, 2006, J PLANT PHYSIOL, V163, P273, DOI 10.1016/j.jplph.2005.11.013; Yarmolinsky D, 2013, PLANT PHYSIOL, V161, P725, DOI 10.1104/pp.112.207712	48	11	12	3	21	WILEY-BLACKWELL	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	DEC	2016	52	6					1094	1102		10.1111/jpy.12468	http://dx.doi.org/10.1111/jpy.12468			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	EF5BB	27716928				2025-03-11	WOS:000390344600016
J	Yamaguchi, A; Yoshimatsu, S; Hoppenrath, M; Wakeman, KC; Kawai, H				Yamaguchi, Aika; Yoshimatsu, Sadaaki; Hoppenrath, Mona; Wakeman, Kevin C.; Kawai, Hiroshi			Molecular Phylogeny of the Benthic Dinoflagellate Genus <i>Amphidiniopsis</i> and its Relationships with the Family Protoperidiniaceae	PROTIST			English	Article						Amphidiniopsis; Archaeperidinium; Herdmania; heterotrophic dinoflagellate; molecular phylogeny; Protoperidiniaceae	SP-NOV DINOPHYCEAE; CYST-THECA RELATIONSHIP; SAND-DWELLING DINOFLAGELLATE; EMENDED DESCRIPTION; HETEROTROPHIC DINOFLAGELLATE; HERDMANIA-LITORALIS; PERIDINIALES; MORPHOLOGY; ULTRASTRUCTURE; TAXONOMY	The genus Amphidiniopsis is a benthic (sand-dwelling) lineage of thecate dinoflagellates, containing 19 morphologically diverse species. Past work has shown that some Amphidiniopsis species form a Glade with the sand-dwelling Herdmania litoralis as well as some planktonic species in the family Protoperidiniaceae (i.e. the Monovela group). Still, our contemporary knowledge regarding Amphidiniopsis is limited, compared to the Protoperidiniaceae. To this end, we obtained 18S rDNA data from seven Amphidiniopsis species and a part of the 28S rDNA from four Amphidiniopsis species, with the goal of improving our understanding of phylogenetic relationships among Amphidiniopsis and the Monovela group. Results from the molecular phylogenetic analyses showed that Amphidiniopsis spp., with the exception of A. cf. arenaria, H. litoralis, and members within the Monovela group formed a single Glade. Within the Glade, relationships among Amphidiniopsis spp. and the Monovela group were more complicated - some subclades contained both representatives of Amphidiniopsis and the Monovela group. Our study suggests that habitat (benthic or planktonic), as well as traditionally used, general morphological characteristics, do not reflect molecular phylogenetic relationships, and that the taxonomy of the sand-dwelling genus Amphidiniopsis, and the planktonic family Protoperidiniaceae, should be reconsidered simultaneously. (C) 2016 Elsevier GmbH. All rights reserved.	[Yamaguchi, Aika; Kawai, Hiroshi] Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 6578501, Japan; [Yoshimatsu, Sadaaki] 2298-28 Yashima Nishimachi, Takamatsu, Kagawa 7610113, Japan; [Hoppenrath, Mona] Senckenberg Meer, German Ctr Marine Biodivers Res, Sudstrand 44, D-26382 Wilhelmshaven, Germany; [Wakeman, Kevin C.] Hokkaido Univ, Fac Sci, Dept Biol Sci, North 10,West 8, Sapporo, Hokkaido 0600810, Japan	Kobe University; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Hokkaido University	Yamaguchi, A (通讯作者)，Kobe Univ, Res Ctr Inland Seas, Kobe, Hyogo 6578501, Japan.	aika@harbor.kobe-u.ac.jp	Wakeman, Kevin/P-8827-2019	Wakeman, Kevin/0000-0003-3501-7702	Supporting Positive Activities for Female Researchers on 'Revolution! Female Researcher Training "Kobe Style"' at Kobe University - Japan Science and Technology Agency, Japan	Supporting Positive Activities for Female Researchers on 'Revolution! Female Researcher Training "Kobe Style"' at Kobe University - Japan Science and Technology Agency, Japan	This work was supported by Supporting Positive Activities for Female Researchers on 'Revolution! Female Researcher Training "Kobe Style"' at Kobe University financed by Japan Science and Technology Agency, Japan.	Abe T. H., 1981, PUBLICATIONS SETO MA, V6, P1; Abe T. 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J	Klouch, ZK; Caradec, F; Plus, M; Hernández-Fariñas, T; Pineau-Guillou, L; Chapelle, A; Schmitt, S; Quéré, J; Guillou, L; Siano, R				Klouch, Z. K.; Caradec, F.; Plus, M.; Hernandez-Farinas, T.; Pineau-Guillou, L.; Chapelle, A.; Schmitt, S.; Quere, J.; Guillou, L.; Siano, R.			Heterogeneous distribution in sediments and dispersal in waters of <i>Alexandrium minutum</i> in a semi-enclosed coastal ecosystem	HARMFUL ALGAE			English	Article							TIME PCR ASSAY; RESTING CYSTS; SURFACE SEDIMENTS; DINOFLAGELLATE CYSTS; EXTRACELLULAR DNA; BREST FRANCE; BAY; BLOOMS; TAMARENSE; DYNAMICS	Within the framework of research aimed at using genetic methods to evaluate harmful species distribution and their impact on coastal ecosystems, a portion of the ITS1rDNA of Alexandrium minutum was amplified by real-time PCR from DNA extracts of superficial (1-3 cm) sediments of 30 subtidal and intertidal stations of the Bay of Brest (Brittany, France), during the winters of 2013 and 2015. Cell germinations and rDNA amplifications of A. minutum were obtained for sediments of all sampled stations, demonstrating that the whole bay is currently contaminated by this toxic species. Coherent estimations of ITS1rDNA copy numbers were obtained for the two sampling cruises, supporting the hypothesis of regular accumulation of A. minutum resting stages in the south-eastern, more confined embayments of the study area, where fine-muddy sediments are also more abundant. Higher ITS1rDNA copy numbers were detected in sediments of areas where blooms have been seasonally detected since 2012. This result suggests that specific genetic material estimations in superficial sediments of the bay may be a proxy of the cyst banks of A. minutum. The simulation of particle trajectory analyses by a Lagrangian physical model showed that blooms occurring in the south-eastern part of the bay are disconnected from those of the north-eastern zone. The heterogeneous distribution of A. minutum inferred from both water and sediment suggests the existence of potential barriers for the dispersal of this species in the Bay of Brest and encourages finer analyses at the population level for this species within semi-enclosed coastal ecosystems. (C) 2016 Elsevier B.V. All rights reserved.	[Klouch, Z. K.; Caradec, F.; Plus, M.; Hernandez-Farinas, T.; Chapelle, A.; Schmitt, S.; Quere, J.; Siano, R.] IFREMER, DYNECO PELAGOS, Ctr Brest, F-29280 Plouzane, France; [Klouch, Z. K.; Hernandez-Farinas, T.; Guillou, L.] Sorbonne Univ, UPMC Univ Paris 6, Stn Biol Roscoff,CNRS, Adaptat & Diversite Milieu Marin UMR 7144,Equipe, Pl Georges Teissier,CS90074, F-29688 Roscoff, France; [Pineau-Guillou, L.] IFREMER, Ctr Brest, LOPS OC, F-29280 Plouzane, France	Ifremer; Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; Ifremer	Siano, R (通讯作者)，IFREMER, DYNECO PELAGOS, Ctr Brest, F-29280 Plouzane, France.	raffaele.siano@ifremer.fr	Hernández-Fariñas, Tania/G-6550-2014; Plus, Martin/KII-5441-2024; Pineau-Guillou, Lucia/L-7883-2015	HERNANDEZ FARINAS, Tania/0000-0002-8453-7096; Pineau-Guillou, Lucia/0000-0001-8175-1735; Plus, Martin/0000-0001-9913-4233; Guillou, Laure/0000-0003-1032-7958	DAOULEX project - Region Bretagne; Ifremer; ECosphere Continentale et COtiere (EC2CO) initiative of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): PALMITO; Region Bretagne (Allocation de REcherche Doctorale (ARED) fellowship)	DAOULEX project - Region Bretagne; Ifremer; ECosphere Continentale et COtiere (EC2CO) initiative of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): PALMITO; Region Bretagne (Allocation de REcherche Doctorale (ARED) fellowship)	This work was financed by the DAOULEX project supported by the Region Bretagne. This research was carried out within the framework of K. Klouch's PhD funded by Ifremer and Region Bretagne (Allocation de REcherche Doctorale (ARED) fellowship) and by the project of the ECosphere Continentale et COtiere (EC2CO) initiative of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): PALMITO (2013-2015). The authors wish to thank all colleagues who helped with sample collection and Xavier Caisey for scuba diving sampling assistance. We wish to thank Dominique Hervio-Heath and members of the SG2M/LSEM laboratory of Ifremer for access to their laboratory facilities and all their technical suggestions. Pierre Bodenes is acknowledged for collaborating in the picture developments and Pascale Malestroit for helping with culture maintenance. This research falls within the scope of the French GDR (Groupement de Recherche) Phycotox (http://www.phycotox.fr) (2012-2018) on harmful microalgae and phycotoxins. 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J	Baranyi, V; Pálfy, J; Görög, A; Riding, JB; Raucsik, B				Baranyi, Viktoria; Palfy, Jozsef; Gorog, Agnes; Riding, James B.; Raucsik, Bela			Multiphase response of palynomorphs to the Toarcian Oceanic Anoxic Event (Early Jurassic) in the Reka Valley section, Hungary	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Early Jurassic; Mecsek Mountains; Hungary; Palynofacies; Prasinophytes; Toarcian Oceanic Anoxic Event (T-OAE)	DETRENDED CORRESPONDENCE-ANALYSIS; DINOFLAGELLATE CYST DISTRIBUTION; ORGANIC-WALLED PHYTOPLANKTON; FLOOD-BASALT VOLCANISM; EUKARYOTIC PHYTOPLANKTON; MASS EXTINCTIONS; BIOTIC CRISIS; SEA-LEVEL; BASIN; PALYNOFACIES	Major palaeoenvironmental and palaeoceanographical changes occurred during the Early Jurassic Toarcian Oceanic Anoxic Event (T-OAE), due to a perturbation of the global carbon cycle and a crisis in marine ecosystems. The sequence of environmental change and regional differences during the T-OAE are not yet fully understood and organic-walled phytoplankton and other palynomorphs are well-suited, but under-utilised, in research into this event. Based on quantitative palynological analyses from a black shale-bearing succession at Reka Valley in the Mecsek Mountains of southwest Hungary, five sequential palynomorph assemblages are distinguished. These reveal major shifts in organic-walled phytoplanlcton communities, driven by palaeoenvironmental changes. In addition, palynofacies analysis helped to document changes in the composition of sedimentary organic matter, and to quantify the terrestrial input. Assemblage 1 is characterised by a moderately diverse phytoplankton community and high levels of terrestrial palynomorphs. Assemblage 2 records a significant peak of the euryhaline dinoflagellate cyst Nannoceratopsis. Assemblage 3 is distinguished by dominance of highly opportunistic prasinophytes and the temporary disappearance of all dinoflagellate cyst taxa. Assemblages 4 and 5 represent distinctive phases of a prolonged recovery phase with low diversity phytoplankton assemblages and intermittently high levels of terrestrially-derived palynomorphs. The successive disappearance of phytoplankton taxa and the gradual takeover by opportunistic euryhaline species at the onset of the T-OAE were related to several phenomena. These include reduced salinity in the surface waters, establishment of a stable pycnocline and deterioration of nutrient recycling, followed by oxygen deficiency throughout much of the water column. The high amount of terrestrially-derived palynodebris indicates intense runoff and freshwater input, driven by the early Toarcian warming and the enhanced hydrological cycle. Comparison with coeval European successions proves that the palaeoenvironmental changes during the T-OAE were not entirely synchronous, and local factors played a crucial role in influencing phytoplankton communities. In the Mecsek Basin, regional freshening of the surface waters and increased terrestrial input due to the proximity of the hinterland had a greater influence on phytoplankton communities compared to the open oceanic setting of the Tethys to the south. (C) 2016 Elsevier B.V. All rights reserved.	[Baranyi, Viktoria; Gorog, Agnes] Eotvos Lorand Univ, Dept Palaeontol, Pazmany Peter Setany 1-C, H-1117 Budapest, Hungary; [Palfy, Jozsef] Eotvos Lorand Univ, Dept Phys & Appl Geol, Pazmany Peter Setany 1-C, H-1117 Budapest, Hungary; [Palfy, Jozsef] MTA MTM ELTE Res Grp Paleontol, POB 137, H-1431 Budapest, Hungary; [Riding, James B.] British Geol Survey, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England; [Raucsik, Bela] Univ Szeged, Dept Mineral Geochem & Petrol, Egyet Utca 2, H-6722 Szeged, Hungary	Eotvos Lorand University; Eotvos Lorand University; HUN-REN; Office for Supported Research Groups (ELKH); UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Szeged University	Baranyi, V (通讯作者)，Univ Oslo, Dept Geosci, POB 1047, N-0316 Oslo, Norway.	viktoria.baranyi@geo.uio.no	Palfy, Jozsef/A-3908-2009; Baranyi, Viktoria/HSI-1752-2023; Gorog, Agnes/K-9996-2018; Raucsik, Bela/L-8307-2018	Gorog, Agnes/0000-0002-0910-8822; Baranyi, Viktoria/0000-0002-1194-9903; Palfy, Jozsef/0000-0001-9686-1849; Raucsik, Bela/0000-0002-1951-5974	Hungarian Scientific Research Fund [K72633]; Hantken Miksa Foundation; AASP Student Scholarship; NERC [bgs05002, bgs05016] Funding Source: UKRI	Hungarian Scientific Research Fund(Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA)); Hantken Miksa Foundation; AASP Student Scholarship; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We thank Maria Barbacka (Hungarian Natural History Museum, Budapest), and Andras Galacz and Istvan Szente (Elitvos Lorand University, Budapest), for their helpful advice. Emese Reka Bodor (Geological and Geophysical Institute of Hungary, Budapest) is thanked for her assistance in the field, and help with data analysis. Elzbieta Witkowska (Jagiellonian University, Krakow, Poland) and Jadwiga Ziaja (Wladyslaw Szafer Institute of Botany, Krakow, Poland) are acknowledged for their help with taxonomy, and for obtaining literature. Emanuela Mattioli (Universite Claude Bernard Lyon 1, France) kindly undertook calcareous nannofossil analyses during an earlier project on the section studied. We thank Wolfram M. Kurschner (University of Oslo, Norway) for his constructive comments on an early draft of the manuscript. Two anonymous reviewers provided constructive comments and help in improving this article. The research was financed by the Hungarian Scientific Research Fund (project K72633) and the Hantken Miksa Foundation. Viktoria Baranyi was also supported by an AASP Student Scholarship in 2013. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). This is MTM-MTA-ELTE Palaeo contribution number 226.	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Palaeobot. Palynology	DEC	2016	235						51	70		10.1016/j.revpalbo.2016.09.011	http://dx.doi.org/10.1016/j.revpalbo.2016.09.011			20	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ED8IJ		Green Accepted, Green Published			2025-03-11	WOS:000389114900005
J	Dhib, A; Fertouna-Bellakhal, M; Turki, S; Aleya, L				Dhib, Amel; Fertouna-Bellakhal, Mouna; Turki, Souad; Aleya, Lotfi			Driving factors of dinoflagellate cyst distribution in surface sediments of a Mediterranean lagoon with limited access to the sea	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cysts; Phytoplankton; Abiotic factors; Ghar El Melh lagoon	HARMFUL ALGAL BLOOMS; NORTHWESTERN INDIAN-OCEAN; RESTING CYSTS; SPATIAL-DISTRIBUTION; BIZERTE LAGOON; ALEXANDRIUM-CATENELLA; ESTUARINE SEDIMENTS; VEGETATIVE CELLS; RUPPIA-CIRRHOSA; BENTHIC CYSTS	Seasonal distribution of dinoflagellate cysts were studied at five surface sediment study stations in Ghar El Melh Lagoon (GML) (Tunisia) in relation to physicochemical parameters and phytoplankton abundance in the water column. At least sixteen dinocyst types were identified, dominated mainly by Protoperidinium spp., Scrippsiella trochoidea complex, Lingulodinum machaerophorum, Alexandrium spp. and Gymnodinium spp., along with many round brown cysts. Cyst abundance ranged from 0 to 229 g(-1) dry sediment. No significant differences in cyst distribution were found among stations, though a significant variation was observed among seasons with cyst dominance in autumn. No significant variation was found between cyst abundance and the different abiotic factors monitored, neither in the water column (physicochemical parameters) nor in the sediment (% H2O). Low dinocyst abundance was consistent with the dominance of non-cyst-forming dinoflagellates in the GML water column. (C) 2016 Elsevier Ltd. All rights reserved.	[Dhib, Amel; Fertouna-Bellakhal, Mouna; Aleya, Lotfi] Univ Bourgogne Franche Comte, Lab Chronoenvironm, UMR CNRS 6249, Besancon, France; [Dhib, Amel; Fertouna-Bellakhal, Mouna; Turki, Souad] INSTM, Lab Milieu Marin, Ctr Goulette, Tunis, Tunisia; [Fertouna-Bellakhal, Mouna] Inst Super Peche & Aquaculture Bizerte, Unite Rech Exploitat Milieux Aquat, Errimel, Bizerte, Tunisia; [Fertouna-Bellakhal, Mouna] Fac Sci Bizerte, Bizerte, Tunisia	Universite de Franche-Comte; Institut National des Sciences et Technologies de la Mer; Universite de Carthage	Aleya, L (通讯作者)，Univ Bourgogne Franche Comte, Lab Chronoenvironm, UMR CNRS 6249, Besancon, France.	lotfi.aleya@univ-fcomte.fr						Abdenadher M, 2012, ESTUAR COAST SHELF S, V106, P102, DOI 10.1016/j.ecss.2012.04.029; Abid F, 2008, ESTUAR COAST SHELF S, V80, P391, DOI 10.1016/j.ecss.2008.09.007; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anderson Donald M., 1997, Limnology and Oceanography, V42, P1009; Anglès S, 2010, DEEP-SEA RES PT II, V57, P210, DOI 10.1016/j.dsr2.2009.09.002; [Anonymous], THESIS; [Anonymous], 1996, HARMFUL TOXIC ALGAL; [Anonymous], HARMFUL ALGAE NEWS; [Anonymous], LIST WETL INT IMP; APHA A. 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J	Neubauer, EF; Poole, AZ; Weis, VM; Davy, SK				Neubauer, Emilie F.; Poole, Angela Z.; Weis, Virginia M.; Davy, Simon K.			The scavenger receptor repertoire in six cnidarian species and its putative role in cnidarian-dinoflagellate symbiosis	PEERJ			English	Article						CD36; Aiptasia; CTLD; Sea anemone; Coral symbiosis; SRCR; Innate immunity; Coral; Scavenger receptor; Symbiodinium	IMMUNE GENE REPERTOIRE; C-TYPE LECTINS; B TYPE-I; TRANSCRIPTOME ANALYSIS; INNATE IMMUNITY; PROTEIN; RECOGNITION; ANCIENT; GENOME; DOMAIN	Many cnidarians engage in a mutualism with endosyrnbiotic photosynthetic dino-flagellates that forms the basis of the coral reef ecosystem. Interpartner interaction and regulation includes involvement of the host innate irnmune system. Basal metazoans, including cnidarians have diverse and complex innate immune repertoires that are just beginning to be described. Scavenger receptors (SR) area diverse superfarruly of innate immunity genes that. recognize microbes. The a broad array of microbial hgands and participate in phagocytosis of invading crobes. The superfarnily includes subclades named SR-A through SR-I that are categorized based on the arrangement of sequence domains including the scavenger receptor cysteine rich (SRCR), the C-type lectin (CTLD) and the CD36 domains. Previous fiinctional and gene expression studies on cnidarian-dinoflagellate symbiosis have implicated SR-like proteins in interpartner communication and regulation. IIn this study, we characterized the SR repertoire from a combination of genomic and Itranscriptomic resources from six l cnidarian species n the Class Anthozoa. We combined these bioinformatic analyses with functional experiments using the SR inhibitor fucoidan Ito explore a role fort SRs in cnidarian symbiosis and immunity. Bioinformatic searches revealed a large diversity of SR like genes that resembled SR-As, SR-Bs, SR-Es and SR-Is. SRCRs, CTLDs and CD36 domains were identified in multiple sequences in combinations that were highly homologous to vertebrate SRs as well as in proteins with novel domain combinations. Phylogenetic analyses of CD36 domains of the SR-B-like sequences from a diversity of metazoans grouped cnidarian with bilaterian sequences separate from other basal metazoans. All cnidarian sequences grouped together with moderate support in a subclade separately from bilaterian sequences. Functional experiments were carried out on the sea anemone Aiptasia pallida that engages in a symbiosis with Symbiodinium minutum (clade B1). Experimental blocking of the SR ligand binding site with the inhibitor fucoidan reduced the ability of S. minutum Ito colonize A. pallida suggesting that host SRs play a role in host-symbiont recognition. In addition, incubation of symbiotic anemones with fucoidan elicited an immune response, indicating that host SRs function in immune modulation that results in host tolerance of the symbionts.	[Neubauer, Emilie F.; Davy, Simon K.] Victoria Univ Wellington, Sch Biol Sci, Wellington, New Zealand; [Poole, Angela Z.] Western Oregon Univ, Dept Biol, Monmouth, OR USA; [Weis, Virginia M.] Oregon State Univ, Dept Integrat Biol, Corvallis, OR 97331 USA	Victoria University Wellington; Western Oregon University; Oregon State University	Weis, VM (通讯作者)，Oregon State Univ, Dept Integrat Biol, Corvallis, OR 97331 USA.	weis@oregolistate.edu	Weis, Virginia/T-5095-2019	Weis, Virginia/0000-0002-1826-2848; Detournay, Olivier/0009-0003-4965-438X; Davy, Simon/0000-0003-3584-5356	National Science Foundation [IOB0919073]; Commonwealth Doctoral Scholarship; Faculty of Science Strategic Research Grant from Victoria University of Wellington	National Science Foundation(National Science Foundation (NSF)); Commonwealth Doctoral Scholarship; Faculty of Science Strategic Research Grant from Victoria University of Wellington	This work was partially supported by a grant from the National Science Foundation to VMW (IOB0919073). EFN was supported by a Commonwealth Doctoral Scholarship and a Faculty of Science Strategic Research Grant from Victoria University of Wellington. 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	Powell, JH; Riding, JB				Powell, John H.; Riding, James B.			Stratigraphy, sedimentology and structure of the Jurassic (Callovian to Lower Oxfordian) succession at Castle Hill, Scarborough, North Yorkshire, UK	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article							RAYNAUD 1978 LENTIN; STAFFIN BAY; MIDDLE; ENGLAND; BASIN; SKYE	Site investigation borehole cores and temporary shaft exposures at the Toll House Pumping Station shaft site, Castle Hill, Scarborough, North Yorkshire, have revealed new data on the Callovian to Lower Oxfordian (Jurassic) succession. The condensed transgressive marine unit, the Lower Callovian Cornbrash Formation, rich in berthierine ooids and abundant shelly fossils, and the attenuated Cayton Clay Formation represent the Early Callovian marine transgression that flooded the low-gradient alluvial plain, which is represented by the underlying Scalby Formation. The Callovian Osgodby Formation (Red Cliff Rock and Langdale members) is an extensively bioturbated, silty sandstone with abundant berthierine-pyrite ooids in the lower part. It was deposited in lower-to upper-shoreface settings. Slow sedimentation rates, with long sediment residence time, resulted in a diverse ichnofauna and a high bioturbation index. Framboidal pyrite ooids in the lower Osgodby Formation sandstones are interpreted as being formed in anoxic lagoons in the nearshore zone; ooids were subsequently swept offshore during storm surge-ebb events. Cold water dinoflagellate cysts of Boreal affinity such as Gonyaulacysta dentata in the lower part of the Oxford Clay Formation indicate an Early Oxfordian age. This is confirmed by the presence of the zonal ammonite species Quenstedoceras mariae and is consistent with a relatively cold, but warming, palaeoclimate at this time. Shaft excavations revealed a new major fault, the Toll House Fault, which is interpreted to be a splay fault bifurcating off the main Castle Hill Fault. Together, the Toll House and Castle Hill faults form the western bounding faults of the Peak Trough, a grabenlike structure that extends northwards, offshore.	[Powell, John H.; Riding, James B.] British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Powell, JH (通讯作者)，British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England.	jhp@bgs.ac.uk						[Anonymous], GEOL SOC LONDON; [Anonymous], 1979, P YORKS GEOL SOC; [Anonymous], 1829, ILLUSTRATIONS GEOL 1; Arkell W.J., 1933, The Jurassic System in Great Britain; ARKELL WJ, 1945, P YORKS GEOL SOC, V25, P339; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; Brinkmann R, 1926, NACHRICHTEN GESEL MP, P199; Buckman S. 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S., 1959, Geological Magazine, V96, P329; Taylor A, 2003, EARTH-SCI REV, V60, P227, DOI 10.1016/S0012-8252(02)00105-8; Taylor KG, 2011, ELEMENTS, V7, P113, DOI 10.2113/gselements.7.2.113; TAYLOR KG, 1995, J SEDIMENT RES A, V65, P358, DOI 10.1306/D42680C2-2B26-11D7-8648000102C1865D; Taylor KG, 2000, SEDIMENT GEOL, V131, P77, DOI 10.1016/S0037-0738(00)00002-6; Whyte M.A., 2006, YORKSHIRE ROCKS LAND, P174; Williams ME, 2002, GEOL J, V37, P279, DOI 10.1002/gj.915; Woollam R., 1980, Journal of the University of Sheffield Geological Society, V7, P243; Wright J. K., 1968, Proceedings of the Geological Association, V79, P363; Wright J.K., 1983, Proceedings of the Yorkshire Geological Society, V44, P249; Wright J. 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J	Razumkova, ES				Razumkova, E. S.			New dinocyst species (family Ceratiaceae Willey et Hickson) from the Lower Cretaceous of Southwestern Western Siberia	PALEONTOLOGICAL JOURNAL			English	Article						nonmarine dinocyst; Aptian; Lower Cretaceous; Western Siberia		New species of Aptian dinoflagellate cyst of the family Ceratiaceae, Endoceratium immarinum sp. nov. and Nyktericysta (Hastodinium) sibirica sp. nov., are described. These taxa interpreted as nonmarine expand the palynological characteristics of the Vikulovo Formation of Western Siberia.	[Razumkova, E. S.] Res & Prod Enterprise Geologorazvedka, Ul Knipovicha 11-2, St Petersburg 192019, Russia		Razumkova, ES (通讯作者)，Res & Prod Enterprise Geologorazvedka, Ul Knipovicha 11-2, St Petersburg 192019, Russia.	elena.razumkova@gmail.com		Razumkova, Elena/0000-0003-1856-9492				BATTEN D J, 1988, Cretaceous Research, V9, P337, DOI 10.1016/0195-6671(88)90007-9; Harding IC, 1995, CRETACEOUS RES, V16, P727, DOI 10.1006/cres.1995.1046; Mao SZ, 1999, GRANA, V38, P144, DOI 10.1080/713786923; Nohr-Hansen Henrik, 1998, Palynology, V22, P143; Pedersen G. K., 2014, Bulletin of Canadian Petroleum Geology, V62, P261; Raevskaya E.G., 2011, PROBLEMY SOVREMENNOI, V1, P103; Zhamoid A.I., 2000, POSTANOVLENIYA MEZHV, V35, P1; Zippi Pierre A., 1998, Micropaleontology (New York), V44, P1, DOI 10.2307/1485998	8	2	2	0	2	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0031-0301	1555-6174		PALEONTOL J+	Paleontol. J.	NOV	2016	50	6					646	652		10.1134/S0031030116060125	http://dx.doi.org/10.1134/S0031030116060125			7	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	EE8ZB					2025-03-11	WOS:000389914200013
J	Wary, M; Eynaud, F; Rossignol, L; Lapuyade, J; Gasparotto, MC; Londeix, L; Malaizé, B; Castera, MH; Charlier, K				Wary, Melanie; Eynaud, Frederique; Rossignol, Linda; Lapuyade, Joanna; Gasparotto, Marie-Camille; Londeix, Laurent; Malaize, Bruno; Castera, Marie-Helene; Charlier, Karine			Norwegian Sea warm pulses during Dansgaard-Oeschger stadials: Zooming in on these anomalies over the 35-41 ka cal BP interval and their impacts on proximal European ice-sheet dynamics	QUATERNARY SCIENCE REVIEWS			English	Article						Dansgaard-Oeschger events; Heinrich events; Trigger mechanism; Sea ice; Surface/subsurface hydrological conditions; High resolution multiproxy approach	NORTH-ATLANTIC OCEAN; RAPID CLIMATIC VARIATIONS; DINOFLAGELLATE CYSTS; CONTINENTAL-SLOPE; NORDIC SEAS; CIRCULATION CHANGES; SURFACE CONDITIONS; FAEROE MARGIN; ARCTIC-OCEAN; GREENLAND	The last glacial millennial climatic events (i.e. Dansgaard-Oeschger and Heinrich events) constitute outstanding case studies of coupled atmosphere-ocean-cryosphere interactions. Here, we investigate the evolution of sea-surface and subsurface conditions, in terms of temperature, salinity and sea ice cover, at very high-resolution (mean resolution between 55 and 155 years depending on proxies) during the 35 -41 ka cal BP interval covering three Dansgaard-Oeschger cycles and including Heinrich event 4, in a new unpublished marine record, i.e. the MD99-2285 core (62.69 degrees N; -3.57s degrees E). We use a large panel of complementary tools, which notably includes dinocyst-derived sea-ice cover duration quantifications. The high temporal resolution and multiproxy approach of this work allows us to identify the sequence of processes and to assess ocean-cryosphere interactions occurring during these periodic ice-sheet collapse events. Our results evidence a paradoxical hydrological scheme where (i) Greenland interstadials are marked by a homogeneous and cold upper water column, with intensive winter sea ice formation and summer sea ice melting, and (ii) Greenland and Heinrich stadials are characterized by a very warm,and low saline surface layer with iceberg calving and reduced sea ice formation, separated by a strong haloclirie from a less warm and saltier subsurface layer. Our work also suggests that this stadial surface/subsurface warming started before massive iceberg release, in relation with warm Atlantic water advection. These findings thus support the theory that upper ocean warming might have triggered European ice-sheet destabilization. Besides, previous paleoceanographic studies conducted along the Atlantic inflow pathways close to the edge of European ice-sheets suggest that such a feature might have occurred in this whole area. Nonetheless, additional high resolution paleoreconstructions are required to confirm such a regional scheme. (C) 2016 Elsevier Ltd. All rights reserved.	[Wary, Melanie; Eynaud, Frederique; Rossignol, Linda; Lapuyade, Joanna; Gasparotto, Marie-Camille; Londeix, Laurent; Malaize, Bruno; Castera, Marie-Helene; Charlier, Karine] Univ Bordeaux, EPOC, UMR 5805, Bat B18,Allee Geoffroy St Hilaire, F-33615 Pessac, France; [Gasparotto, Marie-Camille] Univ Quebec, UQAM, Montreal, PQ H3C 3P8, Canada	Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Quebec; University of Quebec Montreal	Wary, M (通讯作者)，Univ Bordeaux, EPOC, UMR 5805, Bat B18,Allee Geoffroy St Hilaire, F-33615 Pessac, France.	melanie.wary@u-bordeaux.fr	; WARY, Melanie/S-1121-2018	Bruno, Malaize/0000-0002-5571-9990; WARY, Melanie/0000-0001-5211-2168	French INSU (Institut National des Sciences de l'Univers) program LEFE (Les enveloppes fluides et l'environnement); IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean) project "ICE-BIO-RAM: Impact des Changements Environnementaux sur la BIOdiversite marine lors des Rechauffements Abrupts du cliMat"; INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU program; ARTEMIS 14C AMS French INSU project; European Union [243908]	French INSU (Institut National des Sciences de l'Univers) program LEFE (Les enveloppes fluides et l'environnement); IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean) project "ICE-BIO-RAM: Impact des Changements Environnementaux sur la BIOdiversite marine lors des Rechauffements Abrupts du cliMat"; INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU program; ARTEMIS 14C AMS French INSU project; European Union(European Union (EU))	Analyses conducted on MD99-2285 were supported by the French INSU (Institut National des Sciences de l'Univers) program LEFE (Les enveloppes fluides et l'environnement) within the frame of the EVE (Evolution et variability du climat a lechelle globale) 2009-2011 project "RISCC: Role des Ice-Shelves dans le Changement Climatique" and the IMAGO (Interactions multiples dans l'atmosphere, la glace et l'ocean) 2013 project "ICE-BIO-RAM: Impact des Changements Environnementaux sur la BIOdiversite marine lors des Rechauffements Abrupts du cliMat", the latter being also supported by the INTERRVIE (Interactions Terre/Vie) - TS (Terre solide) INSU program. We also acknowledge financial support and use of the facilities of the ARTEMIS 14C AMS French INSU project. The research leading to these results also benefited from funding from the European Union's Seventh Framework Programme (FP7/2007-2013) under grant agreement no. 243908, "Past4Future. Climate change - Learning from the past climate".	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Sci. Rev.	NOV 1	2016	151						255	272		10.1016/j.quascirev.2016.09.011	http://dx.doi.org/10.1016/j.quascirev.2016.09.011			18	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	EA2DZ					2025-03-11	WOS:000386404300016
J	Awad, WK; Oboh-Ikuenobe, FE				Awad, Walaa K.; Oboh-Ikuenobe, Francisca E.			Early Paleogene dinoflagellate cysts from ODP Hole 959D, Cote d'Ivoire-Ghana Transform Margin, West Africa: New species, biostratigraphy and paleoenvironmental implications	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Dinoflagellate cysts; Biostratigraphy and paleoenvironment; Taxonomy; ODP Hole 959D; Cote d'Ivoire-Ghana Transform Margin; West Africa; Early Paleocene to Early Eocene	CRETACEOUS TERTIARY BOUNDARY; PALEOCENE-EOCENE BOUNDARY; SEA-LEVEL; CALCAREOUS NANNOFOSSIL; THERMAL MAXIMUM; EL-KEF; NORTH; SEDIMENTS; SOUTH; SECTION	A nearly continuous sedimentary record from Ocean Drilling Program (ODP) Site 959 (Hole 959D) in the Cote d'Ivoire-Ghana Transform Margin provides the opportunity to study Lower Paleogene palynology in this equatorial region. This paper presents data for 117 dinoflagellate cyst taxa recorded in 18 samples covering a 91-m interval from 867.60 mbsf to 77632 mbsf. Preservation of dinoflagellate cysts varied from poor to excellent, and recovery was almost superabundant. Based on last or first occurrence of dinoflagellate cyst events, five zones (zone 1 to zone 5) were identified. The concentration of several dinoflagellate cyst events in the Thanetian interval suggests the presence of hiatuses or condensed horizons as inferred in previous studies of nearby localities. Frequent to common abundance of Apectodinium in the upper Thanetian sediments apparently records the global episodes of intense climatic warming that characterized the latest Paleocene to earliest Eocene time. An assemblage dominated by species of Operculodinium, Spiniferites, and Tectatodinium confirms the outer neritic to oceanic depositional setting of the drill hole as previously inferred from lithologic characteristics. Finally, four new dinoflagellate cyst taxa, Adnatosphaeridium ivoriense, Diphyes digitum, Eocladopyxis furculum and Tectatodinium nigeriaense that were observed only in the Paleocene interval, have been formally identified and described in detail. (C) 2016 Elsevier Ltd. All rights reserved.	[Awad, Walaa K.; Oboh-Ikuenobe, Francisca E.] Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Geol & Geophys Program, 129 McNutt Hall, Rolla, MO 65409 USA	University of Missouri System; Missouri University of Science & Technology	Awad, WK (通讯作者)，Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Geol & Geophys Program, 129 McNutt Hall, Rolla, MO 65409 USA.	wka9tb@mst.edu		Oboh-Ikuenobe, Francisca/0000-0002-2223-9691	Petroleum Research Fund; Josephine Husbands Radcliffe Graduate Scholarship (Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology); American Chemical Society [34676-AC8]	Petroleum Research Fund(American Chemical Society); Josephine Husbands Radcliffe Graduate Scholarship (Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology); American Chemical Society(American Chemical Society)	We acknowledge the Petroleum Research Fund (administered by the American Chemical Society, Grant 34676-AC8 to Francisca Oboh-Ikuenobe) and the Josephine Husbands Radcliffe Graduate Scholarship (Department of Geosciences and Geological and Petroleum Engineering, Missouri University of Science and Technology) for funding this study. Discussions with Drs. Robert A. Fensome, Graham L. Williams and Lucy E. Edwards on the taxonomy and morphology of dinoflagellate cysts are gratefully appreciated. Constructive and critical reviews by Hamid Slimani and Ali Soliman greatly improved the manuscript.	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J	Wood, SEL; Riding, JB; Fensome, RA; Williams, GL				Wood, Stephanie E. L.; Riding, James B.; Fensome, Robert A.; Williams, Graham L.			A review of the <i>Sentusidinium</i> complex of dinoflagellate cysts	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						Dinoflagellate cysts; Mesozoic-Cenozoic; Morphology; Sentusidinium complex; Taxonomic review	NORTHERN BELGIUM; NEW-ZEALAND; PART 2; MIDDLE; SEA; MIOCENE; BIOSTRATIGRAPHY; STRATIGRAPHY; PALYNOLOGY; ACRITARCHS	The Jurassic to Neogene (Miocene) dinoflagellate cyst genus Sentusidinium has a relatively simple overall morphology. This genus, together with Batiacasphaera, Kallosphaeridium and Pentafidia, comprises the Sentusidinium complex. This is distinct from the superficially similar laterally asymmetrical and subspheroidal/lenticular Cyclonephelium complex. The genus Sentusidinium is an acavate, subcircular, proximate to proximochorate, sexiform gonyaulacacean genus with an apical archaeopyle and typically low relief ornamentation. Since the erection of Sentusidinium in 1978, three similar genera have been established, which we consider to be taxonomic junior synonyms of that genus: Barbatacysta, Escharisphaeridia and Pilosidinium. However, we deem the Early Cretaceous to Miocene genera Batiacasphaera, Kallosphaeridium and Pentafidia are deemed to be separate from Sentusidinium. We refine the definition of the Early Cretaceous to Miocene genus Batiacasphaera to circumscribe cysts with a reticulate to rugulate autophragm and an apical archaeopyle with a free operculum. By contrast, Kallosphaeridium has a ventrally attached apical archaeopyle with five plates that can be interpreted as type (4A1I)(@) or type (5A)(@); it also has a small operculum relative to the overall cyst diameter. The six accepted Kallosphaeridium species are confined to the Palaeogene. The Australian genus Pentafidia is unusual in appearing to only have five precingular plates; this comprises two species from the Jurassic-Cretaceous transition of Western Australia. Therefore, we emend Sentusidinium to restrict it to acavate, proximate or proximochorate dinoflagellate cysts with an autophragm devoid of, or covered with, highly variable, non-linear ornamentation and a type (tA) apical archaeopyle. Occasionally the elements of ornamentation may be connected, but rarely is a cingulum indicated, and the tabulation is never clearly evident. A kalyptra may be occasionally present. The operculum is free. Following a comprehensive literature review, we accept 17 species in Batiacasphaera. In Kallosphaeridium we accept six species confidently and consider six species to be problematical. We list 38 (34 accepted and four problematical) species of Sentusidinium. Kallosphaeridium? helbyi is here transferred to Cyclonephelium without question. The species Batiacasphaera angularis is occasionally tabulate and hence we transfer it, with question, to Meiourgonyaulax. The Sentusidinium complex is clearly polyphyletic, and all genera considered herein belong to the order Gonyaulacales. Batiacasphaera, Kallosphaeridium and Pentafidia cannot be confidently assigned to a family, whereas Sentusidinium belongs to the Gonyaulacaceae. The number of species within the complex has been reduced from 137 to 68; furthermore, all infraspecific taxa have been eliminated. Crown Copyright (C) 2016 Published by Elsevier B.V. All rights reserved.	[Wood, Stephanie E. L.] Univ Sheffield, Dept Anim & Plant Sci, Western Bank, Alfred Denny Bldg, Sheffield S10 2TN, S Yorkshire, England; [Riding, James B.] British Geol Survey, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England; [Fensome, Robert A.; Williams, Graham L.] Bedford Inst Oceanog, Geol Survey Canada Atlantic, Nat Resources Canada, POB 1006, Dartmouth, NS B2Y 4A2, Canada	University of Sheffield; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography	Wood, SEL (通讯作者)，Univ Sheffield, Dept Anim & Plant Sci, Western Bank, Alfred Denny Bldg, Sheffield S10 2TN, S Yorkshire, England.	selw89@gmail.com			NERC [NE/J016667/1]; NERC [bgs05017] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This contribution forms part of the PhD research of the first author, which is sponsored by a NERC open CASE Award with case partners Shell USA NE/J016667/1. 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J	Egger, LM; Sliwinska, KK; van Peer, TE; Liebrand, D; Lippert, PC; Friedrich, O; Wilson, PA; Norris, RD; Pross, J				Egger, Lisa M.; Sliwinska, Katarzyna K.; van Peer, Tim E.; Liebrand, Diederik; Lippert, Peter C.; Friedrich, Oliver; Wilson, Paul A.; Norris, Richard D.; Pross, Joerg			Magnetostratigraphically-calibrated dinoflagellate cyst bioevents for the uppermost Eocene to lowermost Miocene of the western North Atlantic (IODP Expedition 342, Paleogene Newfoundland sediment drifts)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Paleogene; Oligocene; Biostratigraphy; Dinoflagellates; North Atlantic; Integrated Ocean Drilling Program	MIDDLE EOCENE; OLIGOCENE TRANSITION; SEA BASIN; BIOSTRATIGRAPHY; ONSET; STRATIGRAPHY; FORAMINIFERA; ICE; GREENHOUSE; STRATOTYPE	The Oligocene epoch represents a somewhat neglected chapter in paleoclimate and paleoceanographic history, which is at least partially due to the scarcity of complete Oligocene sedimentary archives and poor biostratigraphic age control. Many of the biotic events registered in Oligocene microfossils are strongly diachronous across latitudes as a response to increased global cooling and enhanced meridional temperature gradients. To improve biostratigraphic age control for the Oligocene of the North Atlantic Ocean, we carried out a high-resolution study of dinoflagellate cysts from Integrated Ocean Drilling Program (IODP) Sites U1405, U1406 and U1411 off Newfoundland. Together the sites comprise an apparently complete uppermost Eocene (34.9 Ma) to lowermost Miocene (21.7 Ma) sequence with good magnetostratigraphic age control. This allows us to firmly tie identified dinoflagellate cyst bioevents to the geomagnetic polarity timescale. In the dinoflagellate cyst assemblages studied we have identified and magnetostratigraphically-calibrated ten first and 19 last appearance datums. Our magnetostratigraphically-calibrated dinocyst-based biostratigraphy, which is based on an average sample resolution of a sample every similar to 150 kyrs, will contribute to an improved age framework for future paleoceanographical studies in the higher-latitude North Atlantic. (C) 2016 Elsevier B.V. All rights reserved.	[Egger, Lisa M.; Friedrich, Oliver; Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany; [Sliwinska, Katarzyna K.] Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [van Peer, Tim E.; Liebrand, Diederik; Wilson, Paul A.] Univ Southampton, Natl Oceanog Ctr, Waterfront Campus,European Way, Southampton SO14 3ZH, Hants, England; [Lippert, Peter C.] Univ Utah, Dept Geol & Geophys, Frederick A Sutton Bldg,115 S 1460 E, Salt Lake City, UT 84112 USA; [Norris, Richard D.] Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gilman Dr, La Jolla, CA 92093 USA	Ruprecht Karls University Heidelberg; Geological Survey Of Denmark & Greenland; NERC National Oceanography Centre; University of Southampton; Utah System of Higher Education; University of Utah; University of California System; University of California San Diego; Scripps Institution of Oceanography	Egger, LM (通讯作者)，Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany.	lisa.egger@geow.uni-heidelberg.de	Sliwinska, Kasia K./G-9097-2018; van Peer, Tim/R-8157-2016; Liebrand, Diederik/AAT-2004-2021	Sliwinska, Kasia K./0000-0001-5488-8832; van Peer, Tim/0000-0003-3516-4198; Liebrand, Diederik/0000-0002-6925-7889; Lippert, Peter C/0000-0003-1744-9982; Wilson, Paul/0000-0001-6425-8906	US. National Science Foundation; German Research Foundation (DFG) [PR651/16-3, FR2544/8]; Danish Council for Independent Research/Natural Sciences (DFF/FNU) [11-107497]; NERC [NE/K006800/1, NE/K014137/1, NE/K008390/1] Funding Source: UKRI	US. National Science Foundation(National Science Foundation (NSF)); German Research Foundation (DFG)(German Research Foundation (DFG)); Danish Council for Independent Research/Natural Sciences (DFF/FNU); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research used samples and data provided by the Integrated Ocean Drilling Program, which was sponsored by the US. National Science Foundation and participating countries under management of Joint Oceanographic Institutions Inc. Invaluable support of the members of the IODP Expedition 342 Science Party is gratefully acknowledged. Andre Bahr and Martin Head are thanked for discussions, and Malcolm Jones is thanked for technical support. Financial support through the German Research Foundation (DFG; grants PR651/16-3 and FR2544/8 to J.P. and O.F., respectively) and the Danish Council for Independent Research/Natural Sciences (DFF/FNU; grant 11-107497 to K.K.S.) is gratefully acknowledged.	[Anonymous], 1980, Special Papers in Palaeontology; Backmann J., 1987, Abhandlungen der Geologischen Bundesanstalt (Vienna), V39, P21; BALDAUF JG, 1990, NATO ADV SCI I C-MAT, V308, P575; Beaudoin A. 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Palaeobot. Palynology	NOV	2016	234						159	185		10.1016/j.revpalbo.2016.08.002	http://dx.doi.org/10.1016/j.revpalbo.2016.08.002			27	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	EB6WP		Green Accepted, Bronze			2025-03-11	WOS:000387526600012
J	Frieling, J; Svensen, HH; Planke, S; Cramwinckel, MJ; Selnes, H; Sluijs, A				Frieling, Joost; Svensen, Henrik H.; Planke, Sverre; Cramwinckel, Margot J.; Selnes, Haavard; Sluijs, Appy			Thermogenic methane release as a cause for the long duration of the PETM	PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA			English	Article						carbon cycle; thermogenic methane; volcanism; climate change; PETM	EOCENE THERMAL MAXIMUM; CARBON-ISOTOPE EXCURSION; ORGANIC-MATTER; SEA-LEVEL; OCEAN; FRACTIONATION; CLIMATE; BASIN; CYCLE; ACIDIFICATION	The Paleocene-Eocene Thermal Maximum (PETM) (similar to 56 Ma) was a similar to 170,000-y (similar to 170-kyr) period of global warming associated with rapid and massive injections of C-13-depleted carbon into the ocean-atmosphere system, reflected in sedimentary components as a negative carbon isotope excursion (CIE). Carbon cycle modeling has indicated that the shape and magnitude of this CIE are generally explained by a large and rapid initial pulse, followed by similar to 50 kyr of C-13-depleted carbon injection. Suggested sources include submarine methane hydrates, terrigenous organic matter, and thermogenic methane and CO2 from hydrothermal vent complexes. Here, we test for the contribution of carbon release associated with volcanic intrusions in the North Atlantic Igneous Province. We use dinoflagellate cyst and stable carbon isotope stratigraphy to date the active phase of a hydrothermal vent system and find it to postdate massive carbon release at the onset of the PETM. Crucially, however, it correlates to the period within the PETM of longer-term C-13-depleted carbon release. This finding represents actual proof of PETM carbon release from a particular reservoir. Based on carbon cycle box model [i.e., Long-Term Ocean-Atmosphere-Sediment Carbon Cycle Reservoir (LOSCAR) model] experiments, we show that 4-12 pulses of carbon input from vent systems over 60 kyr with a total mass of 1,500 Pg of C, consistent with the vent literature, match the shape of the CIE and pattern of deep ocean carbonate dissolution as recorded in sediment records. We therefore conclude that CH4 from the Norwegian Sea vent complexes was likely the main source of carbon during the PETM, following its dramatic onset.	[Frieling, Joost; Cramwinckel, Margot J.; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Palaeobot & Paly, NL-3584 CS Utrecht, Netherlands; [Svensen, Henrik H.; Planke, Sverre] Univ Oslo, Ctr Earth Evolut & Dynam, N-0315 Oslo, Norway; [Planke, Sverre] Oslo Innovat Ctr, Volcan Basin Petr Res, N-0349 Oslo, Norway; [Selnes, Haavard] Appl Petr Technol, N-2027 Kjeller, Norway	Utrecht University; University of Oslo	Frieling, J (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Marine Palynol & Paleoceanog,Lab Palaeobot & Paly, NL-3584 CS Utrecht, Netherlands.	j.frieling1@uu.nl	Planke, Sverre/AAE-1721-2021; Sluijs, Appy/B-3726-2009	Cramwinckel, Marlow Julius/0000-0002-6063-836X; Sluijs, Appy/0000-0003-2382-0215; Planke, Sverre/0000-0001-6128-2193; Frieling, Joost/0000-0002-5374-1625	European Research Council (ERC) under the European Union [259627]; Norwegian Research Council for Centre of Excellence [223272]; Ministry of Education, Culture, and Science	European Research Council (ERC) under the European Union(European Research Council (ERC)); Norwegian Research Council for Centre of Excellence(Research Council of Norway); Ministry of Education, Culture, and Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT))	We thank N. Welters and A. van Dijk (Utrecht University) for analytical support and R. Zeebe for input and assistance with setting up the LOSCAR experiments. We thank the Norwegian Petroleum Directorate for access to samples and Tomlinson Geophysical Services for access to seismic reflection data. The European Research Council (ERC), under the European Union Seventh Framework Program, provided funding for this work through ERC Starting Grant 259627 (to A.S.). We thank the Norwegian Research Council for Centre of Excellence Grant 223272 (to the Centre for Earth Evolution and Dynamics, Oslo). This work was carried out under the program of the Netherlands Earth System Science Centre, financially supported by the Ministry of Education, Culture, and Science.	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Natl. Acad. Sci. U. S. A.	OCT 25	2016	113	43					12059	12064		10.1073/pnas.1603348113	http://dx.doi.org/10.1073/pnas.1603348113			6	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	DZ7ZI	27790990	Green Published, Bronze			2025-03-11	WOS:000386087100041
J	Gu, HF; Mertens, KN; Liu, TT				Gu, Haifeng; Mertens, Kenneth N.; Liu, Tingting			<i>Huia caspica</i> gen. & comb. nov., a dinoflagellate species that recently crossed the marine-freshwater boundary	PHYCOLOGICAL RESEARCH			English	Article						cyst-theca relationship; diplopsalioideans; Diplopsalis caspica; Glenodinium caspica; LSU rDNA	CYST-THECA RELATIONSHIP; OBLEA-ROTUNDA DIPLOPSALIDACEAE; PHYLOGENETIC POSITIONS; ADAPTIVE EVOLUTION; MIXED MODELS; DINOPHYCEAE; PERIDINIALES; GENERA; PROTOPERIDINIUM; ULTRASTRUCTURE	The dinoflagellate subfamily Diplopsalidoideae encompasses 11 genera whose plate patterns show a large diversity. In a recently published molecular phylogeny (Liu et al. 2015) some of these genera (e.g. Diplopsalis, Diplopelta) are polyphyletic, suggesting that further subdivision of these genera is needed. Here we established the cyst-theca relationship of Diplopsalis caspica by incubating cysts collected from the East China Sea. Cells of D. caspica display a plate formula of Po, X, 3', 1a, 6 '', 3c+t, ?4s, 5''', 1 '''', characterized by a small, parallelogrammic anterior intercalary plate (1a) located in the middle of the dorsal part of the epitheca. The cysts are spherical and smooth-walled with a theropylic archeopyle. In addition, we obtained four large subunit ribosomal DNA (LSU rDNA) sequences from the germinated motile cells by single-cell polymerase chain reaction. Strains of D. caspica from the marine environment of the East China Sea differ at 0-2 positions of LSU rDNA sequences from that of lacustrine strains from NE China. In the molecular phylogeny, D. caspica was close to Lebouraia pusilla but distant from D. lenticula, the type species of Diplopsalis. Our results support the systematic importance of plate 1a, and therefore D. caspica was transferred to a new genus, Huia. The conservative LSU rDNA sequences in H. caspica suggest that the marine-freshwater transition occurred recently.	[Gu, Haifeng; Liu, Tingting] Third Inst Oceanog, Dept Marine Biol & Ecol, Xiamen, Peoples R China; [Mertens, Kenneth N.] IFREMER, LER BO, Stn Biol Marine, Concarneau, France	Third Institute of Oceanography, Ministry of Natural Resources; Ifremer	Gu, HF (通讯作者)，Third Inst Oceanog, Dept Marine Biol & Ecol, Xiamen, 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, 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).	Abe T. H., 1941, REC OCEAN OGR WORKS JAPAN, V12, P121; Abe T. 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S, 1881, ORGANISMUS CILIOFLAG; BOLTOVSKOY A, 1975, Physis Seccion B las Aguas Continentales y sus Organismos, V34, P73; Calado AJ, 2011, PHYCOLOGIA, V50, P641, DOI 10.2216/11-21.1; CARTY S, 1986, PHYCOLOGIA, V25, P197, DOI 10.2216/i0031-8884-25-2-197.1; Chomérat N, 2004, EUR J PHYCOL, V39, P317, DOI 10.1080/09670260410001712590; Craveiro SC, 2010, J EUKARYOT MICROBIOL, V57, P568, DOI 10.1111/j.1550-7408.2010.00512.x; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; DODGE JD, 1993, BOT MAR, V36, P137, DOI 10.1515/botm.1993.36.2.137; DODGE JD, 1981, BOT J LINN SOC, V83, P15, DOI 10.1111/j.1095-8339.1981.tb00126.x; Ehrenberg C. 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A., NUCL ACIDS S SER, V41, P95; Hameed Hameed Abbas, 2015, Marine Biodiversity Records, V8, pe150, DOI 10.1017/S1755267215001281; Head M.J., 1996, Palynology: Principles and Applications, P1197; Imanian B, 2007, BMC EVOL BIOL, V7, DOI 10.1186/1471-2148-7-172; Jones FC, 2012, NATURE, V484, P55, DOI 10.1038/nature10944; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; Katoh K, 2005, NUCLEIC ACIDS RES, V33, P511, DOI 10.1093/nar/gki198; Kawami Hisae, 2006, Plankton & Benthos Research, V1, P183; Kremp A, 2006, J PHYCOL, V42, P400, DOI 10.1111/j.1529-8817.2006.00205.x; Kretschmann J, 2015, PHYTOTAXA, V220, P239, DOI 10.11646/phytotaxa.220.3.3; LEWIS J, 1990, BRIT PHYCOL J, V25, P339, DOI 10.1080/00071619000650381; LINDEMANN E., 1927, ARCH PROTISTENK, V59, P417; Liu TT, 2015, PHYCOLOGIA, V54, P210, DOI 10.2216/14-94.1; LOEBLICH AR, 1980, TAXON, V29, P321, DOI 10.2307/1220299; Logares R, 2007, MOL PHYLOGENET EVOL, V45, P887, DOI 10.1016/j.ympev.2007.08.005; Logares R, 2007, MICROB ECOL, V53, P549, DOI 10.1007/s00248-006-9088-y; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; Mertens KN, 2015, SYST BIODIVERS, V13, P829, DOI 10.1080/14772000.2015.1078855; Naustvoll LJ, 2000, PHYCOLOGIA, V39, P187, DOI 10.2216/i0031-8884-39-3-187.1; Naustvoll LJ, 1998, PHYCOLOGIA, V37, P1, DOI 10.2216/i0031-8884-37-1-1.1; Nie Dashu, 1943, SINENSIA, V14, P1; Orr MR, 1998, TRENDS ECOL EVOL, V13, P502, DOI 10.1016/S0169-5347(98)01511-0; Ostenfeld C.H., 1902, VIDENSK MEDDEL DANSK, V1901, P129; Ostenfeld C. H., 1908, WISSENSCHAFTLICHE ER, V8, P123; Posada D, 2008, MOL BIOL EVOL, V25, P1253, DOI 10.1093/molbev/msn083; Ronquist F, 2003, BIOINFORMATICS, V19, P1572, DOI 10.1093/bioinformatics/btg180; Schiller J., 1935, Rabenhorst's Kryptogamenflora von Deutschland, Osterreichs und der Schweiz, V10, P1; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Stamatakis A, 2006, BIOINFORMATICS, V22, P2688, DOI 10.1093/bioinformatics/btl446; STROM SL, 1993, LIMNOL OCEANOGR, V38, P965, DOI 10.4319/lo.1993.38.5.0965; Taylor FJR, 2008, BIODIVERS CONSERV, V17, P407, DOI 10.1007/s10531-007-9258-3; Wang S., 2001, SCI CHINA, V31, P760; WOLOSZYNSKA J., 1917, B INT ACAD SCI CRACO, V1917, P114; You XJ, 2015, NOVA HEDWIGIA, V101, P313, DOI 10.1127/nova_hedwigia/2015/0272; Zhang Q, 2015, J SYST EVOL, V53, P512, DOI 10.1111/jse.12151	58	11	12	1	21	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1322-0829	1440-1835		PHYCOL RES	Phycol. Res.	OCT	2016	64	4					251	258		10.1111/pre.12146	http://dx.doi.org/10.1111/pre.12146			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	EC7GK		Green Published			2025-03-11	WOS:000388304700006
J	Basavaraju, MH; Jaiprakash, BC; Chidambaram, L; Ayyadurai, M				Basavaraju, M. H.; Jaiprakash, B. C.; Chidambaram, L.; Ayyadurai, M.			Biostratigraphy and depositional environments of subsurface sediments in well Arani-A, Palar basin, Tamil Nadu	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						Biostratigraphy; Palynofossils; Albian; Palar basin; Tamil Nadu	NORTH-WEST SHELF; AUSTRALIA	The first exploratory well Arani-A was drilled in the Palar basin to a depth of 2400m and terminated within the granitic basement.This well offered the first ever opportunity to understand biostratigraphy, sedimentation history and depositional environment of the entire sedimentary column based on arenaceous foraminifera, spores, pollen and dinoflagellate cyst assemblages. Previous studies on few scattered outcrops around Sriperumbudur, Chengalpattu and Sathyavedu areas have documented palynofossil assemblage of Neocomian-Aptian age. The present study reveals the presence of middle Jurassic (Bajocian-Callovian) sediments (2360-1725 m) resting on the granitic basement. The sediments are interpreted to have deposited under lacustrine/estuarine conditions with high tides providing occasional marine influence. The middle Jurassic sediments are conformably overlain by late Jurassic (Oxfordian-Tithonian) sediments (1725 - 950 m). The late Jurassic sediments have been inferred to have got deposited under fluctuating near shoremarginal marine conditions. There is a 55m thick boulder bed (950 - 895 m) separating the overlying Valanginian sediments. Early Cretaceous (Valanginian-Early Albian) sediments are developed in the interval from 895-50m. The boulder bed possibly corresponds to the missing Berriasian stage of the earliest Cretaceous representing an unconformity of the order of similar to 5 Ma across Jurassic-Cretaceous boundary. These sediments are inferred to have deposited under shallow inner neritic conditions. The sediments from 50m to surface consist mainly of lateritic sandstone and alluvium. The sedimentary history of Palar basin began in Bajocian stage of middle Jurassic (170-168 Ma) and ended in early Albian stage of early Cretaceous (113-105 Ma). The late Albian marine transgression which facilitated huge sedimentation in Cauvery and Krishna-Godavari basins has bypassed the Palar basin thus adversely affecting the hydrocarbon potential.	[Basavaraju, M. H.; Jaiprakash, B. C.; Chidambaram, L.; Ayyadurai, M.] ONGC Ltd, Reg Geosci Lab, Madras 600049, Tamil Nadu, India		Basavaraju, MH (通讯作者)，ONGC Ltd, Reg Geosci Lab, Madras 600049, Tamil Nadu, India.	basavamh1955@gmail.com						Basavaraju M.H., 2014, PALYNOSTRATIGR UNPUB; Basavaraju M.H., 2014, UNPUB; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P1, DOI 10.1016/B978-0-444-59425-9.00001-9; Helby R., 2004, UPDATE JURASSIC EARL; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Mantle DJ, 2012, REV PALAEOBOT PALYNO, V180, P41, DOI 10.1016/j.revpalbo.2012.03.005; Mazumder S., 2013, ONGC B, V48, P112; Nagendra A., 2011, UNPUB; Rangaraju M. K., 1993, P 2 SEM PETR BAS IND, V1, P371; Riding JB, 2010, REV PALAEOBOT PALYNO, V162, P543, DOI 10.1016/j.revpalbo.2010.07.008; Sastri V.V., 1976, MINERAL RESOURCES DE, V42, P212; Stover L.E., 1987, PLANKTON STRATIGRAPH, P847; Tripathi A., 1997, Journal of the Palaeontological Society of India, V42, P101; Vairavan V., 1993, 2 SEM PETR BAS IND, P389; Venkatachala B.S., 1988, PALEOBOTANIST, V36, P183; Williams G.L., 1993, Geological Survey of Canada Paper, P1; Williams G.L., 1985, PLANKTON STRATIGRAPH, V2, P847; WILSON GJ, 1980, 92 NZ GEOL SURV, P1	18	3	3	0	2	SPRINGER INDIA	NEW DELHI	7TH FLOOR, VIJAYA BUILDING, 17, BARAKHAMBA ROAD, NEW DELHI, 110 001, INDIA	0016-7622	0974-6889		J GEOL SOC INDIA	J. Geol. Soc. India	OCT	2016	88	4					407	420		10.1007/s12594-016-0504-8	http://dx.doi.org/10.1007/s12594-016-0504-8			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EB7OV					2025-03-11	WOS:000387578900002
J	Volik, O; McCarthy, FMG; Riddick, NL				Volik, Olena; McCarthy, Francine M. G.; Riddick, Nicholas L.			Insights from pollen, non-pollen palynomorphs and testate amoebae into the evolution of Lake Simcoe	JOURNAL OF PALEOLIMNOLOGY			English	Article						Lake Simcoe; Non-pollen palynomorphs; Testate amoebae; Paleolimnology; Eutrophication	WATER-QUALITY CHANGES; CULTURAL EUTROPHICATION; SEDIMENTARY PHOSPHORUS; HURON BASIN; ONTARIO; INDICATORS; CANADA; PEDIASTRUM; PATTERNS; PROXIES	Comparing the distribution of little-known non-pollen palynomorphs (NPP) with pollen and testate amoebae (thecamoebians) in a long piston core from the main basin of Lake Simcoe illustrates their potential as paleolimnological indicators. Sediments rich in spruce and pine pollen in core LS07 PC5 contain sparse, low-diversity microfossil assemblages recording cold, oligotrophic waters (mainly the testate amoeba Difflugia oblonga, the desmid genus Cosmarium, andPediastrum integrum). Marked climate warming reconstructed from pollen data using transfer functions is associated with a sharp increase in algal NPP abundance and diversity, including Botryococcus spp., the desmid genus Staurastrum, and Pediastrum simplex. A Centropyxis-dominated testate amoeba fauna, and sparse, low-diversity NPP record slightly brackish conditions attributed to the early Holocene drought. Diverse benthic desmid and Pediastrum spp. (including P. brevicorne) floras, together with abundant Botryococcus, record warm, mesotrophic waters associated with a hemlock-maplebeech pollen assemblage from which January temperatures several degrees warmer than today were reconstructed. A decline in NPP abundance and diversity and the re-establishment of a Centropyxis-dominated testate amoeba fauna supports drought as a cause for the regional "hemlock decline''. The most marked change in aquatic microfossil assemblages coincides with anthropogenic impact. The appearance of dinoflagellate cysts and a marked increase in difflugiid testate amoebae (notably Cucurbitella tricuspis) records eutrophication below the ragweed rise that is attributed to the agricultural activities of the Wendat Nation. Two phases of anthropogenic impact are distinguishedwithin the ragweed zone: (1) an NPP assemblage nearly devoid of desmids but rich in Peridinium wisconsinense and Pediastrum boryanum, attributed to Euro-Canadian land clearing and agriculture, and (2) an assemblage rich in Botryococcus, Peridinium willei/P. volzii, Codonella cratera, and meso-eutrophic desmids with planktonic life habits, is attributed to urbanization and industrialization.	[Volik, Olena; McCarthy, Francine M. G.; Riddick, Nicholas L.] Brock Univ, Dept Earth Sci, 500 Glenridge Ave, St Catharines, ON L2S 3A1, Canada; [Volik, Olena] Univ Waterloo, Dept Geog & Environm Management, 200 Univ Ave W, Waterloo, ON N2L 3G1, Canada	Brock University; University of Waterloo	Volik, O (通讯作者)，Brock Univ, Dept Earth Sci, 500 Glenridge Ave, St Catharines, ON L2S 3A1, Canada.; Volik, O (通讯作者)，Univ Waterloo, Dept Geog & Environm Management, 200 Univ Ave W, Waterloo, ON N2L 3G1, Canada.	volik.olena@gmail.com	Volik, Olena/ABH-8956-2020	Volik, Olena/0000-0003-4949-1974; Riddick, Nicholas/0009-0005-1370-6365				Anderson TW, 2012, J PALEOLIMNOL, V47, P513, DOI 10.1007/s10933-011-9551-8; [Anonymous], 2015, National Climate Data and Information Archive; Bartlein P.J., 1993, Elk Lake, Minnesota, P275, DOI [10.1130/SPE276-p275, DOI 10.1130/SPE276-P275]; Birch J, 2015, J ANTHROPOL ARCHAEOL, V39, P139, DOI 10.1016/j.jaa.2015.03.004; BURDEN ET, 1986, CAN J EARTH SCI, V23, P43, DOI 10.1139/e86-005; Byrne R., 1998, IROQUOIAN PEOPLES LA, V1, P94; Chittenden R., 1990, The Origin of Wye Marsh; Coesel PFM., 2007, DESMIDS LOWLANDS MES; Danesh DC, 2013, PALYNOLOGY, V37, P231, DOI 10.1080/01916122.2013.782366; Drljepan M, 2014, HOLOCENE, V24, P1731, DOI 10.1177/0959683614551227; Duthie HC, 1996, J PALEOLIMNOL, V15, P79; Eimers MC, 2005, J GREAT LAKES RES, V31, P322; Ginn BK, 2012, J GREAT LAKES RES, V38, P825, DOI 10.1016/j.jglr.2012.09.002; GUYOHLSON D, 1992, REV PALAEOBOT PALYNO, V71, P1, DOI 10.1016/0034-6667(92)90155-A; Hall RI, 1996, CAN J FISH AQUAT SCI, V53, P1, DOI 10.1139/cjfas-53-1-1; Hammer Oyvind, 2001, Palaeontologia Electronica, V4, pUnpaginated; Hawryshyn J., 2010, THESIS; Hawryshyn J, 2012, CAN J FISH AQUAT SCI, V69, P24, DOI [10.1139/F2011-134, 10.1139/f2011-134]; Heidenreich C.E., 1971, Huronia: a history and geography of the Huron Indians, 1600-1650; Jankovská V, 2000, FOLIA GEOBOT, V35, P59, DOI 10.1007/BF02803087; Komarek J., 2001, REV GREEN ALGAL GENU; Kumar Arun, 1998, Palaeontologia Electronica, V1, pUnpaginated; Lewis CFM, 2008, AQUAT ECOSYST HEALTH, V11, P127, DOI 10.1080/14634980802095263; *LSEMS, 2003, STAT LAK SIMC WAT; [LSRCA] Lake Simcoe Region Conservation Authority, 2009, WAT REP CARD SUMM LA; McAndrews J.H., 1973, KEY QUATERNARY POLLE; McAndrews J.H., 1994, Great Lakes Archaeology and Paleoecology: Exploring Interdisciplinary Initiative for the Nineties, P179; McAndrews JH, 2010, VEG HIST ARCHAEOBOT, V19, P495, DOI 10.1007/s00334-010-0237-3; McCarthy FMG, 2013, MICROPALEAEONTOLOGIC, P133; MCCARTHY FMG, 1995, J PALEONTOL, V69, P980, DOI 10.1017/S0022336000035630; McCarthy F, 2012, J PALEOLIMNOL, V47, P411, DOI 10.1007/s10933-010-9410-z; McCarthy F, 2012, J PALEOLIMNOL, V47, P429, DOI 10.1007/s10933-010-9415-7; McCarthy FMG, 2007, J PALEOLIMNOL, V37, P453, DOI 10.1007/s10933-006-9050-5; McCarthy FMG, 2015, MEM MUS ANTHR UNIV M, V57, P13; McCarthy FMG, 2011, REV PALAEOBOT PALYNO, V166, P46, DOI 10.1016/j.revpalbo.2011.04.008; Mertens KN, 2012, PHYCOLOGIA, V51, P612, DOI 10.2216/11-89.1; Neville LA, 2011, J FORAMIN RES, V41, P230, DOI 10.2113/gsjfr.41.3.230; North RL, 2013, INLAND WATERS, V3, P51, DOI 10.5268/IW-3.1.529; OVERPECK JT, 1992, GEOLOGY, V20, P1071, DOI 10.1130/0091-7613(1992)020<1071:MENAVC>2.3.CO;2; Patterson RT, 2012, PALAEOGEOGR PALAEOCL, V348, P32, DOI 10.1016/j.palaeo.2012.05.028; PATTERSON RT, 1989, J PALEONTOL, V63, P245, DOI 10.1017/S0022336000019272; Payne RJ, 2012, REV PALAEOBOT PALYNO, V173, P68, DOI 10.1016/j.revpalbo.2011.09.006; Riddick NL, 2017, PALYNOLOGY, V41, P171, DOI 10.1080/01916122.2015.1113208; Riddick NL, 2016, 59 C GREAT LAK RES I; Rode D.L., 2009, THESIS; Roe HM, 2010, J PALEOLIMNOL, V43, P955, DOI 10.1007/s10933-009-9380-1; Schindler DW, 2012, P R SOC B, DOI [10.1098/rspb2012.1032, DOI 10.1098/RSPB2012.1032]; Shannon C. E., 1964, The theory of mathematical communication; Smol JohnP., 2009, Pollution of Lakes and Rivers: A Paleoenvironmental Perspective, V2nd; St Jacques JM, 2000, J PALEOLIMNOL, V23, P385, DOI 10.1023/A:1008178002326; Stastny J, 2010, FOTTEA, V10, P1, DOI 10.5507/fot.2010.001; Todd BJ, 2004, 4667 GEOL SURV CAN; Todd BJ, 2008, J PALEOLIMNOL, V39, P361, DOI 10.1007/s10933-007-9111-4; van Geel B., 2001, TRACKING ENV CHANGE, P99, DOI DOI 10.1007/0-306-47668-1_6; Volik O., 2014, THESIS; Watchorn MA, 2008, J PALEOLIMNOL, V39, P491, DOI 10.1007/s10933-007-9126-x; Whitney BS, 2012, J PALEOLIMNOL, V47, P601, DOI 10.1007/s10933-012-9583-8; Winter JG, 2007, J GREAT LAKES RES, V33, P381, DOI 10.3394/0380-1330(2007)33[381:PITLSF]2.0.CO;2; Young J.D., 2010, Lake Simcoe water quality update; Yu ZC, 1997, GEOLOGY, V25, P251, DOI 10.1130/0091-7613(1997)025<0251:MHDCCB>2.3.CO;2; Zippi P., 1990, ENV RES TECHN TRANSF, P393	61	10	11	2	40	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0921-2728	1573-0417		J PALEOLIMNOL	J. Paleolimn.	OCT	2016	56	2-3					137	152		10.1007/s10933-016-9900-8	http://dx.doi.org/10.1007/s10933-016-9900-8			16	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	DW9OC					2025-03-11	WOS:000383989300004
J	Shumilovskikh, LS; Seeliger, M; Feuser, S; Novenko, E; Schlütz, F; Pint, A; Pirson, F; Brückner, H				Shumilovskikh, Lyudmila S.; Seeliger, Martin; Feuser, Stefan; Novenko, Elena; Schluetz, Frank; Pint, Anna; Pirson, Felix; Brueckner, Helmut			The harbour of Elaia: A palynological archive for human environmental interactions during the last 7500 years	QUATERNARY SCIENCE REVIEWS			English	Article						Vegetation history; Maritime trade; Erosion; Non-pollen palynomorphs; Helminth eggs; Fungal spores; Dinoflagellate cysts; Pergamon; Turkey; Holocene	NON-POLLEN PALYNOMORPHS; BLACK-SEA; INTESTINAL PARASITES; POSIDONIA-OCEANICA; WESTERN TURKEY; HUMAN IMPACT; LAKE; VEGETATION; RECONSTRUCTION; NETHERLANDS	Elaia, the harbour city for ancient Pergamon (western Turkey), was investigated using geoarchaeological methods. The rise and fall of Elaia were closely linked to the flourishing period of Pergamon, which ruled wide parts of today's western Turkey in Hellenistic times. In the framework of this research, the palynological analysis of a 9 m sediment core, Ela-70, retrieved from the enclosed harbour of the city, was carried out to reconstruct the vegetation and environmental history of the wider Gulf of Elaia region. An age-depth model, based on 11 calibrated radiocarbon ages, starting from 7.5 ka BP, provides the basis for the high resolution study of sediments from the Hellenistic period, as well as before and after. The lower part of the pollen diagram is characterised by high percentages of deciduous oaks and pines, suggesting the dominance of open forests close to the coring site. The change from oak forests to a cultural landscape, with olive, pistachio, walnut, and grape, started around 850 BC, reaching a maximum ca. 250 BC, and continuing to ca. AD 800. This period is characterised by increase of fire activity, soil erosion intensity, and pastoral farming. Such long-lasting intensive land use likely led to the climax ecosystem turnover from open deciduous oak forests to pine stands, while salt marshes developed around the coring site. The discovery of the dinoflagellate cysts of Peridinium ponticum, a Black Sea endemic species, in the harbour of Elaia evidences maritime trade between the Aegean Sea and the Black Sea; its first occurrence coincides with the time of the Mithridatic Wars (1st century BC). In conclusion, palynological data, in addition to historical and archaeological records, provide a deeper insight into human environmental interactions, as derived from the geoarchaeological archive of the harbour of Elaia. (C) 2016 Elsevier Ltd. All rights reserved.	[Shumilovskikh, Lyudmila S.] Univ Gottingen, Dept Palynol & Climate Dynam, Wilhelm Weber Str 2a, D-37073 Gottingen, Germany; [Shumilovskikh, Lyudmila S.] Tomsk State Univ, Lab Taxon & Phylogeny Plants, Tomsk, Russia; [Seeliger, Martin; Pint, Anna; Brueckner, Helmut] Univ Cologne, Inst Geog, Cologne, Germany; [Feuser, Stefan] Univ Rostock, Heinrich Schliemann Inst Ancient Studies, Rostock, Germany; [Novenko, Elena] Lomonosov Moscow State Univ, Fac Geog, Moscow, Russia; [Schluetz, Frank] Lower Saxony Inst Hist Coastal Res, Wilhelmshaven, Germany; [Pirson, Felix] DAI Dept Istanbul, Istanbul, Turkey; [Novenko, Elena] Russian Acad Sci, Inst Geog, Moscow, Russia	University of Gottingen; Tomsk State University; University of Cologne; University of Rostock; Lomonosov Moscow State University; Russian Academy of Sciences; Institute of Geography, Russian Academy of Sciences	Shumilovskikh, LS (通讯作者)，Univ Gottingen, Dept Palynol & Climate Dynam, Wilhelm Weber Str 2a, D-37073 Gottingen, Germany.	shumilovskikh@gmail.com	Novenko, Elena/L-7934-2015; Brueckner, Helmut/O-3017-2015; Shumilovskikh, Lyudmila/P-2493-2015	Shumilovskikh, Lyudmila/0000-0002-7429-3163; Novenko, Elena/0000-0003-2174-8467; Schlutz, Frank/0000-0003-2114-8146; Feuser, Stefan/0000-0003-0625-3095	DFG priority program "The Hellenistic Polis as a Living Space - Urban Structures and Civic Identity between Tradition and Innovation" [(SPP) 1209]; German Research Foundation (DFG) [PI 740/1-3, BR 877/32-1]; D. I. Mendeleev Scientific Fund Program of Tomsk State University; Russian Foundation for Basic Research (RFBR) [16-35-60083, 16-36-00293]	DFG priority program "The Hellenistic Polis as a Living Space - Urban Structures and Civic Identity between Tradition and Innovation"; German Research Foundation (DFG)(German Research Foundation (DFG)); D. I. Mendeleev Scientific Fund Program of Tomsk State University; Russian Foundation for Basic Research (RFBR)(Russian Foundation for Basic Research (RFBR))	We thank Bas van Geel for valuable reviewing of the manuscript and Robert Spengler for polishing the English. The project presented here was conducted in the context of the DFG priority program (SPP) 1209 "The Hellenistic Polis as a Living Space - Urban Structures and Civic Identity between Tradition and Innovation" (2008-2011). Financial support by the German Research Foundation is gratefully acknowledged (DFG ref. nos. PI 740/1-3 and BR 877/32-1). The study was partially supported by the D. I. Mendeleev Scientific Fund Program of Tomsk State University and Russian Foundation for Basic Research (RFBR grants 16-35-60083 and 16-36-00293). The studies would not have been possible without the hospitality and support of the Pergamon excavation team. The Ministry of Culture and Tourism of the Republic of Turkey kindly granted the research permits.	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Sci. Rev.	OCT 1	2016	149						167	187		10.1016/j.quascirev.2016.07.014	http://dx.doi.org/10.1016/j.quascirev.2016.07.014			21	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Physical Geography; Geology	DW7IW					2025-03-11	WOS:000383825400011
J	Bowman, V; Ineson, J; Riding, J; Crame, J; Francis, J; Condon, D; Whittle, R; Ferraccioli, F				Bowman, V.; Ineson, J.; Riding, J.; Crame, J.; Francis, J.; Condon, D.; Whittle, R.; Ferraccioli, F.			The Paleocene of Antarctica: Dinoflagellate cyst biostratigraphy, chronostratigraphy and implications for the palaeo-Pacific margin of Gondwana	GONDWANA RESEARCH			English	Article						Cretaceous-Paleocene; Antarctic Peninsula; Gondwana; Biostratigraphy; Palaeogeography	K-T BOUNDARY; SEYMOUR-ISLAND; NEW-ZEALAND; TRANSANTARCTIC MOUNTAINS; TECTONIC RECONSTRUCTIONS; PALYNOLOGICAL EVIDENCE; WEST ANTARCTICA; MARAMBIO GROUP; PALEOGENE; EVOLUTION	The Paleocene (66-56 Ma) was a critical time interval for understanding recovery from mass extinction in high palaeolatitudeswhen global climate waswarmer than today. A unique sedimentary succession fromSeymour Island (Antarctic Peninsula) provides key referencematerial from this important phase of the early Cenozoic. Dinoflagellate cyst data froma 376mthick stratigraphical section, including the Cretaceous-Paleogene boundary, is correlatedwith biozones from New Zealand, the East Tasman Plateau and southeastern Australia. A detailed age model is suggested for the Lopez de Bertodano (LDBF) and Sobral (SF) formations based on dinoflagellate cyst biostratigraphy and U-Pb dating of zircons, supported by correlatedmagnetostratigraphy and strontium isotope values frommacrofossils. The top of the LDBF is confirmed as latest Maastrichtian to earliest Danian (similar to 66.2-65.65 Ma) in age. The overlying SF is mostly Danian in age, with an inferred hiatus near the top overlain by sediments dated as ? late Thanetian. Rare Apectodinium homomorphum first appear in the uppermost SF; the earliest in situ record from Antarctica. The distribution of marine and terrestrial fossils from uppermost Cretaceous to Eocene sediments in Patagonia, Antarctica, New Zealand and Australia required both sea and land connections between these fragments of Gondwana. Fossil evidence and reconstructions of Antarctic palaeogeography and palaeotopography reveal evidence for persistent embayments in the proto-Weddell and Ross Sea regions at this time. We conclude that a coastal dispersal route along the palaeo-Pacificmargin of Gondwana could explain the fossil distribution without requiring a transAntarctic strait or closely spaced archipelago. A region in the West to East Antarctic boundary zone, elevated until the early Paleogene, perhaps acted as a site for high elevation ice caps. This supports fossil, geochemical and sedimentological evidence for cold climate intervals and significant sea level falls during the Maastrichtian and Paleocene. (C) 2015 The Authors. Published by Elsevier B.V. on behalf of International Association for Gondwana Research.	[Bowman, V.; Crame, J.; Francis, J.; Whittle, R.; Ferraccioli, F.] British Antarctic Survey, Madingley Rd, Cambridge CB3 0ET, England; [Ineson, J.] Geol Survey Denmark & Greenland, Oster Volgade 10, DK-1350 Copenhagen K, Denmark; [Riding, J.; Condon, D.] British Geol Survey, Ctr Environm Sci, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; Geological Survey Of Denmark & Greenland; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Bowman, V (通讯作者)，British Antarctic Survey, Madingley Rd, Cambridge CB3 0ET, England.	vanessa.bowman@bas.ac.uk	; Condon, Daniel/A-4249-2008; Ineson, Jon/G-9800-2018	Bowman, Vanessa/0000-0002-4887-3949; Condon, Daniel/0000-0002-9082-3283; Ineson, Jon/0000-0003-0017-3705; Ferraccioli, Fausto/0000-0002-9347-4736	UK Natural Environment Research Council (NERC) [NE/I00582X/1, NE/C506399/1]; School of Earth and Environment, University of Leeds, UK; Environmental Change and Evolution programme of The British Antarctic Survey; NERC [bas0100036, NE/I00582X/2, bas0100029, NE/I005803/1, bas0100030, NE/I00582X/1] Funding Source: UKRI	UK Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); School of Earth and Environment, University of Leeds, UK; Environmental Change and Evolution programme of The British Antarctic Survey; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	UK Natural Environment Research Council (NERC) grants NE/I00582X/1 (PALEOPOLAR) and NE/C506399/1 (Antarctic Funding Initiative) funded this research. The authors thank the School of Earth and Environment, University of Leeds, UK, for support and use of their facilities where this work was initiated. The Environmental Change and Evolution programme of The British Antarctic Survey awarded additional funding to Bowman for STRATABUGS palynological software. The authors would like to thank the rest of the PALEOPOLAR team, particularly Stuart Robinson (University of Oxford) and Dave Kemp (University of Aberdeen), for useful discussions. Jette Halskov (GEUS) is thanked for drafting the sedimentological log. The British Antarctic Survey provided field logistics. James B. Riding publishes with the permission of the Executive Director, British Geological Survey (NERC), Jon R. Ineson with the permission of the Geological Survey of Denmark and Greenland (GEUS). 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OCT	2016	38						132	148		10.1016/j.gr.2015.10.018	http://dx.doi.org/10.1016/j.gr.2015.10.018			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EQ2BF		Green Accepted, hybrid			2025-03-11	WOS:000397872600009
J	Ichinomiya, M; dos Santos, AL; Gourvil, P; Yoshikawa, S; Kamiya, M; Ohki, K; Audic, S; de Vargas, C; Noël, MH; Vaulot, D; Kuwata, A				Ichinomiya, Mutsuo; dos Santos, Adriana Lopes; Gourvil, Priscillia; Yoshikawa, Shinya; Kamiya, Mitsunobu; Ohki, Kaori; Audic, Stephane; de Vargas, Colomban; Noel, Mary-Helene; Vaulot, Daniel; Kuwata, Akira			Diversity and oceanic distribution of the Parmales (Bolidophyceae), a picoplanktonic group closely related to diatoms	ISME JOURNAL			English	Article							NEWLY DISCOVERED CYSTS; OYASHIO REGION; LIFE-CYCLE; SILICEOUS NANOPLANKTON; GROWTH-CHARACTERISTICS; REFERENCE DATABASE; MARINE; CHRYSOPHYCEAE; COMMUNITY; ABUNDANCE	Bolidomonas is a genus of picoplanktonic flagellated algae that is closely related to diatoms. Triparma laevis, a species belonging to the Parmales, which are small cells with a siliceous covering, has been shown to form a monophyletic group with Bolidomonas. We isolated several novel strains of Bolidophyceae that have permitted further exploration of the diversity of this group using nuclear, plastidial and mitochondrial genes. The resulting phylogenetic data led us to formally emend the taxonomy of this group to include the Parmales within the Bolidophyceae, to combine Bolidomonas within Triparma and to define a novel species, Triparma eleuthera sp. nov. The global distribution of Bolidophyceae was then assessed using environmental sequences available in public databases, as well as a large 18S rRNA V9 metabarcode data set from the Tara Oceans expedition. Bolidophyceans appear ubiquitous throughout the sampled oceans but always constitute a minor component of the phytoplankton community, corresponding to at most similar to 4% of the metabarcodes from photosynthetic groups (excluding dinoflagellates). They are similar to 10 times more abundant in the small size fraction (0.8-5 mu m) than in larger size fractions. T. eleuthera sp. nov. constitutes the most abundant and most widespread operational taxonomic unit (OTU) followed by T. pacifica, T. mediterranea and the T. laevis clade. The T. mediterranea OTU is characteristic of Mediterranean Sea surface waters and the T. laevis clade OTU is most prevalent in colder waters, in particular off Antarctica.	[Ichinomiya, Mutsuo] Prefectural Univ Kumamoto, Kumamoto, Japan; [dos Santos, Adriana Lopes; Gourvil, Priscillia; Audic, Stephane; de Vargas, Colomban; Vaulot, Daniel] UPMC Univ Paris 06, Sorbonne Univ, CNRS, UMR 7144,Stn Biol Roscoff, Roscoff, France; [Yoshikawa, Shinya; Kamiya, Mitsunobu; Ohki, Kaori] Fukui Prefectural Univ, Obama, Fukui, Japan; [Noel, Mary-Helene] Natl Inst Environm Studies, Tsukuba, Ibaraki, Japan; [Kuwata, Akira] Fisheries Res Agcy, Tohoku Natl Fisheries Res Inst, 3-27-5 Shinhama Cho, Shiogama, Miyagi 9850001, Japan	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Sorbonne Universite; Fukui Prefectural University; National Institute for Environmental Studies - Japan; Japan Fisheries Research & Education Agency (FRA)	Kuwata, A (通讯作者)，Fisheries Res Agcy, Tohoku Natl Fisheries Res Inst, 3-27-5 Shinhama Cho, Shiogama, Miyagi 9850001, Japan.	akuwata@affrc.go.jp	Vaulot, Daniel/T-6649-2019; Kuwata, Akira/E-1121-2013; GOURVIL, PRISCILLIA/AAM-3903-2020; Lopes dos Santos, Adriana/B-7252-2018	Kamiya, Mitsunobu/0000-0002-2343-5547; Gourvil, Priscillia/0000-0003-0408-4988; Lopes dos Santos, Adriana/0000-0002-0736-4937; de Vargas, Colomban/0000-0002-6476-6019; Vaulot, Daniel/0000-0002-0717-5685	Japan Society for the Promotion of Science (JSPS) [22657027, 23370046, 26291085, 15K14784]; Canon Foundation; Core Research for Evolutional Science and Technology from Japan Science and Technology; European Union program MicroB3 [287589]; French 'Investissements d'Avenir' program OCEANOMICS [ANR-11-BTBR-0008]; French 'Investissements d'Avenir' program EMBRC-France; European Union program MaCuMBA [FP7-KBBE-2012-6-311975]; Grants-in-Aid for Scientific Research [16K07489, 26291085, 15K07194, 22657027, 15K14784, 23370046] 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); Canon Foundation(Canon Foundation); Core Research for Evolutional Science and Technology from Japan Science and Technology; European Union program MicroB3; French 'Investissements d'Avenir' program OCEANOMICS(Agence Nationale de la Recherche (ANR)); French 'Investissements d'Avenir' program EMBRC-France(Agence Nationale de la Recherche (ANR)); European Union program MaCuMBA; 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 Masanobu Kawachi for help with the SEM pictures and Yukiko Taniuchi for help in sequencing the nad1 gene. Two anonymous referees provided very useful comments. Ian Probert provided invaluable help and advice for the taxonomic treatment. Financial support for this work was provided by Grants-in-Aid for Scientific Research 22657027, 23370046, 26291085 and 15K14784 from the Japan Society for the Promotion of Science (JSPS), the Canon Foundation and Core Research for Evolutional Science and Technology from Japan Science and Technology as well as by the European Union programs MicroB3 (UE-contract-287589) and MaCuMBA (FP7-KBBE-2012-6-311975), and the French 'Investissements d'Avenir' programs OCEANOMICS (ANR-11-BTBR-0008) and EMBRC-France.	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OCT	2016	10	10					2419	2434		10.1038/ismej.2016.38	http://dx.doi.org/10.1038/ismej.2016.38			16	Ecology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Microbiology	EB0LN	27003244	Green Published, hybrid			2025-03-11	WOS:000387035400007
J	McArthur, AD; Jolley, DW; Hartley, AJ; Archer, SG; Lawrence, HM				McArthur, Adam D.; Jolley, David W.; Hartley, Adrian J.; Archer, Stuart G.; Lawrence, Hugo M.			Palaeoecology of syn-rift topography: A Late Jurassic footwall island on the Josephine Ridge, Central Graben, North Sea	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palynology; Horst palaeoecology; Upper Jurassic; Central North Sea; Source-to-sink	SUEZ RIFT; PALEOENVIRONMENTAL ANALYSIS; SEQUENCE STRATIGRAPHY; VIKING GRABEN; HUMBER GROUP; BASIN; EVOLUTION; MARINE; ASSEMBLAGES; POLLEN	Understanding rift topography is essential for determining source areas, sediment pathways, and the type of sediment delivered to a rift basin; factors essential for interpreting petroleum systems in ancient rifts. Here we investigate Upper Jurassic sediments from the Josephine Ridge region of the Central Graben, North Sea, by integrating geophysical, palynological, petrophysical and sedimentological datasets to analyse the palaeoenvironments of the Jade and Judy horsts, the tops of which are not preserved. Interpretation of geophysical and petrophysical data together with core descriptions shows study wells to step progressively away from the Josephine Ridge into adjacent grabens. One hundred and five palynological samples from six wells range from the Oxfordian to the Lower Tithonian, spanning the syn-rift period of the Central Graben. Samples from the adjacent grabens and the Jade Horst are rich in dinoflagellate cysts and possess <20% terrestrial palynomorphs. Samples from the Judy Horst contain a wide range of terrestrial palynomorphs, dominated by lycopsid, fern and moss spores, representing c.50% of the recovered palynomorphs. Correspondence analysis of the assemblages implies that Jade did not possess a terrestrial ecosystem; Judy samples define seven groupings of related miospores, all interpreted to represent very low lying, relatively early successional type environments. This implies subaerial exposure of the Judy Horst during the Late Jurassic, which is interpreted to have formed an isolated, low relief, footwall crest island. This study provides a new methodology for investigating rift topography, particularly in cases where the tops of horsts were subsequently removed by erosion. The Judy Island would have separated the Central Graben into its eastern and western arms earlier than previously predicted, in the Late Oxfordian, with consequences for distribution of shallow and deep-marine reservoir quality sediments. (C) 2016 Elsevier B.V. All rights reserved.	[McArthur, Adam D.; Jolley, David W.; Hartley, Adrian J.; Archer, Stuart G.] Univ Aberdeen, Kings Coll, Dept Geol & Petr Geol, Meston Bldg, Aberdeen AB24 3EU, Scotland; [Lawrence, Hugo M.] ConocoPhillips UK Ltd, Rubislaw House, Aberdeen, Scotland	University of Aberdeen; ConocoPhillips	McArthur, AD (通讯作者)，Univ Fed Rio Grande do Sul, Inst Geociencias, BR-91501970 Porto Alegre, RS, Brazil.	adam.mcarthur@ufrgs.br	Archer, Stuart/S-9039-2019	Jolley, David/0000-0003-0909-2952; McArthur, Adam/0000-0002-7245-9465	ConocoPhillips (U.K.) Limited	ConocoPhillips (U.K.) Limited	We thank ConocoPhillips (U.K.) Limited for providing the study data and financial support, along with co-ventures in the study area BG Group, ENI UK Ltd., Chevron and OMV UK Ltd. for permission to release data. Nick Schofield, Ben Kilhams and Rob Daly are thanked for the discussions, and Fiona Thompson for laboratory assistance. Two anonymous reviewers and Editor David Bottjer are thanked for their comments.	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Paleoclimatol. Paleoecol.	OCT 1	2016	459						63	75		10.1016/j.palaeo.2016.06.033	http://dx.doi.org/10.1016/j.palaeo.2016.06.033			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	DV0EU		Green Submitted			2025-03-11	WOS:000382591600006
J	Olde, K; Jarvis, I; Pearce, M; Walaszczyk, I; Tocher, B				Olde, Kate; Jarvis, Ian; Pearce, Martin; Walaszczyk, Ireneusz; Tocher, Bruce			Organic-walled dinoflagellate cyst records from a prospective Turonian - Coniacian (Upper Cretaceous) GSSP, Slupia Nadbrzezna, Poland	CRETACEOUS RESEARCH			English	Article						Turonian; Coniacian; GSSP; Palynology; Dinoflagellate cyst	CARBON-ISOTOPE STRATIGRAPHY; SEA-LEVEL; PALEOENVIRONMENTAL CHANGE; BOUNDARY; GERMANY; BIOSTRATIGRAPHY; PRESERVATION; DELTA-C-13; DINOCYST; CHALK	A river section at Slupia Nadbrzezna, central Poland, has been proposed as a candidate Turonian - Coniacian (Cretaceous) GSSP, in combination with the Salzgitter-Salder quarry section of Lower Saxony, Germany. Results of a high-resolution (25 cm) palynological study of the boundary interval in the Slupia Nadbrzezna section are presented. Terrestrial palynomorphs are rare; marine organic-walled dinoflagellate cysts dominate the palynological assemblage. The dinoflagellate cyst assemblage has a low species richness (5-11 per sample; total of 18 species recorded) and diversity (Shannon index H = 0.8-1.4), dominated by four taxa: Circulodinium distinctum subsp. distinctum; Oligosphaeridium complex; Spiniferites ramosus subsp. ramosus; Surculosphaeridium longifurcatum. Declining proportions of O. complex and S. ramosus subsp. ramosus characterise the uppermost Turonian, with an increased dominance of S. longifurcatum in the lower Coniacian. The Turonian - Coniacian boundary interval includes an acme of C. distinctum subsp. distinctum in the upper Mytiloides scupini Zone, a dinoflagellate cyst abundance maximum in the Cremnoceramus walterdorfensis walterdorfensis Zone, and the highest occurrence of Senoniasphaera turonica in the basal Coniacian lower Cremnoceramus deformis erectus Zone. Most previously reported Turonian - Coniacian boundary dinoflagellate cyst marker species are absent; a shallow-water oligotrophic epicontinental depositional setting, remote from terrestrial influence, likely limited species diversity and excluded many taxa of biostratigraphic value. (C) 2016 The Authors. Published by Elsevier Ltd.	[Olde, Kate; Jarvis, Ian; Pearce, Martin] Kingston Univ London, Dept Geog & Geol, Kingston Upon Thames KT1 2EE, Surrey, England; [Pearce, Martin] Evolut Appl Ltd, 50 Mitchell Way, Cheltenham GL54 2PL, Glos, England; [Walaszczyk, Ireneusz] Univ Warsaw, Fac Geol, Al Wirki & Wigury 93, PL-02089 Warsaw, Poland; [Tocher, Bruce] STATOIL, 6300 Bridge Point Pkwy,Bldg 2,Suite 500, Austin, TX 78730 USA	Kingston University; University of Warsaw; Equinor	Jarvis, I (通讯作者)，Kingston Univ London, Dept Geog & Geol, Kingston Upon Thames KT1 2EE, Surrey, England.	i.jarvis@kingston.ac.uk	Walaszczyk, Ireneusz/ABE-7229-2021; Jarvis, Ian/A-1637-2008	Jarvis, Ian/0000-0003-3184-3097; Walaszczyk, Ireneusz/0000-0002-6037-8860; Pearce, Martin/0000-0001-7856-1076	Kingston University London; Statoil Petroleum AS contract [4501936147]	Kingston University London; Statoil Petroleum AS contract	Kate Olde acknowledges receipt of a Kingston University London PhD studentship and support by Statoil Petroleum AS contract 4501936147. Przemyslaw Gedl (Polish Academy of Sciences), two anonymous referees, and editor Eduardo Koutsoukos provided valuable critical reviews.	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J	Penaud, A; Eynaud, F; Voelker, AHL; Turon, JL				Penaud, Aurelie; Eynaud, Frederique; Luise Voelker, Antje Helga; Turon, Jean-Louis			Palaeohydrological changes over the last 50 ky in the central Gulf of Cadiz: complex forcing mechanisms mixing multi-scale processes	BIOGEOSCIENCES			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; WESTERN MEDITERRANEAN SEA; COVERED CARBONATE MOUND; RECENT MARINE-SEDIMENTS; HIGH-RESOLUTION RECORD; FRONT-CURRENT SYSTEM; ICE-CORE RECORD; NORTH-ATLANTIC; IBERIAN MARGIN; GLACIAL MAXIMUM	New dinoflagellate cyst (dinocyst) analyses were carried out at high resolution in core MD99-2339, retrieved from a contouritic field in the central part of the Gulf of Cadiz, for the Marine Isotope Stage (MIS) 3 interval, allowing for discussion of palaeohydrological changes over the last 50 ky in the subtropical NE Atlantic Ocean. Some index dinocyst taxa, according to their (palaeo) ecological significance, shed light on significant sea-surface changes. Superimposed on the general decreasing pattern of dinocyst export to the seafloor over the last 50 ky, paralleling the general context of decreasing aeolian dust fertilization, a complex variability in dinocyst assemblages was detected at the millennial timescale. Enhanced fluvial discharges occurred during Greenland Interstadials (GIs), especially GI 1, 8 and 12, while enhanced upwelling cell dynamics were suggested during the Last Glacial Maximum and Heinrich Stadials. Finally, during the early Holocene, and more specifically during the Sapropel 1 interval (around 7-9 ka BP), we evidenced a strong decrease in dinocyst fluxes, which occurred synchronously to a strong reduction in Mediterranean Outflow Water strength and which we attributed to an advection of warm and nutrient-poor subtropical North Atlantic Central Waters. Over the last 50 ky, our study thus allows for capturing and documenting the fine tuning existing between terrestrial and marine realms in North Atlantic subtropical latitudes, in response to not only the regional climate pattern but also monsoonal forcing interfering during precession-driven Northern Hemisphere insolation maxima. This mechanism, well expressed during the Holocene, is superimposed on the pervasive role of the obliquity as a first major trigger for explaining migration of dinocyst productive centres in the NE Atlantic margin to the subtropical (temperate) latitudes during glacial (interglacial) periods.	[Penaud, Aurelie] Univ Brest, CNRS, Domaines Ocean UMR6538, IUEM, F-29280 Plouzane, France; [Eynaud, Frederique; Turon, Jean-Louis] Univ Bordeaux, CNRS, EPOC UMR5805, Allee Geoffroy St Hilaire, F-33615 Pessac, France; [Luise Voelker, Antje Helga] IPMA, Div Geol & Georecursos Marinhos, Rua Alfredo Magalhaes Ramalho 6, P-1495006 Lisbon, Portugal; [Luise Voelker, Antje Helga] Univ Algarve, Ctr Ciencias Mar, CCMAR, Campus Gambelas, P-8005139 Faro, Portugal	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Instituto Portugues do Mar e da Atmosfera; Universidade do Algarve	Penaud, A (通讯作者)，Univ Brest, CNRS, Domaines Ocean UMR6538, IUEM, F-29280 Plouzane, France.	aurelie.penaud@univ-brest.fr	Penaud, Aurelie/F-2485-2011; Voelker, Antje/C-5427-2012	Penaud, Aurelie/0000-0003-3578-4549; Eynaud, Frederique/0000-0003-1283-7425; Voelker, Antje/0000-0001-6465-6023	French CNRS; "Laboratoire d'Excellence" LabexMER [ANR-10-LABX-19]; French government through the programme "Investissements d'Avenir"; FCT (IF)	French CNRS(Centre National de la Recherche Scientifique (CNRS)); "Laboratoire d'Excellence" LabexMER; French government through the programme "Investissements d'Avenir"(Agence Nationale de la Recherche (ANR)); FCT (IF)(Fundacao para a Ciencia e a Tecnologia (FCT))	Thanks to the French polar institute (IPEV, Institut Paul Emile Victor), the captain and the crew of the Marion Dufresne, and the scientific teams of the IMAGES I and V cruises. We wish to thank M. Castera, M. Georget and O. Ther for invaluable technical assistance at the laboratory. This study was supported by the French CNRS and contributes to the 2013 INSU project "ICE-BIO-RAM: Impact des Changements Environnementaux sur la BIOdiversite marine lors des Rechauffements Abrupts du cliMat" (http://www.insu.cnrs.fr/files/ao_2013_-_eynaud_validee.pdf). This work was supported by the "Laboratoire d'Excellence" LabexMER (ANR-10-LABX-19) and co-funded by a grant from the French government through the programme "Investissements d'Avenir". Antje Voelker acknowledges her Investigador FCT (IF) development grant.	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J	Fersi, W; Bassinot, F; Lézine, AM				Fersi, Wiem; Bassinot, Franck; Lezine, Anne-Marie			PAST PRODUCTIVITY VARIATIONS AND ORGANIC CARBON BURIAL IN THE GULF OF ADEN SINCE THE LAST GLACIAL MAXIMUM	QUATERNAIRE			English	Article						Gulf of Aden; dinoflagellate cysts; productivity; organic carbon; monsoon	DINOFLAGELLATE CYST DISTRIBUTION; SEA-SURFACE CONDITIONS; SOUTHERN RED-SEA; ARABIAN SEA; INDIAN-OCEAN; LATE-QUATERNARY; NORTH-ATLANTIC; MONSOON VARIABILITY; MARINE-SEDIMENTS; HIGH-RESOLUTION	We reconstructed the evolution of marine primary productivity across the last deglaciation in the Gulf of Aden based on micro-paleontological and sedimentological data from marine core MD92-1002. Dinoflagellate cysts analysis suggests that the glacial period was characterized by weakened upwellings and well ventilated bottom water. Primary productivity increased from 14.5 ka with a maximum between 12.6 and 10.8 ka, then declined during the Holocene. Maximum of primary productivity in the Gulf of Aden took place about 3 ka earlier than the maximum of upwelling intensity off the Oman margin, and was not phase-locked with the maximum of boreal summer insolation. XRF-derived bromine contents mimic the variations of Total Organic Carbon (TOC) in core MD92-1002. Both records show a strong glacial/interglacial signal that is largely decoupled from our reconstruction of surface productivity, suggesting that total organic content in core MD92-1002 is mainly controlled by preservation at the sea floor.	[Fersi, Wiem; Bassinot, Franck] CEA Saclay, CEA CNRS UVSQ UMR8212, Lab Sci Climat & Environm IPSL, FR-91191 Gif Sur Yvette, France; [Fersi, Wiem; Lezine, Anne-Marie] UPMC Univ Paris 06, Sorbonne Univ, CNRS IRD MNHN, LOCEAN IPSL Lab, 4 Pl Jussieu, FR-75005 Paris, France	CEA; Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Institut de Recherche pour le Developpement (IRD); Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite	Fersi, W (通讯作者)，CEA Saclay, CEA CNRS UVSQ UMR8212, Lab Sci Climat & Environm IPSL, FR-91191 Gif Sur Yvette, France.; Fersi, W (通讯作者)，UPMC Univ Paris 06, Sorbonne Univ, CNRS IRD MNHN, LOCEAN IPSL Lab, 4 Pl Jussieu, FR-75005 Paris, France.	wiem.fersi@lsce.ipsl.fr; franck.bassinot@lsce.ipsl.fr; anne-marie.lezine@locean-ipsl.upmc.fr	Lézine, Anne-Marie/A-5618-2013	LEZINE, Anne-Marie/0000-0002-3555-5124; Fersi, Wiem/0000-0002-3541-3804	national research funding agency in France (ANR) [ANR-10-BLAN-0608, ANR-11-BS56-0024]; CEA (France); CNRS (France); Agence Nationale de la Recherche (ANR) [ANR-11-BS56-0024, ANR-10-BLAN-0608] Funding Source: Agence Nationale de la Recherche (ANR)	national research funding agency in France (ANR)(Agence Nationale de la Recherche (ANR)); CEA (France)(CEA); CNRS (France)(Centre National de la Recherche Scientifique (CNRS)); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	This research was funded by the national research funding agency in France (ANR) through the ELPASO project (ANR-10-BLAN-0608) and the MONOPOL project (ANR-11-BS56-0024). Thanks are due to K. Lemonnier (CNRS LOCEAN) for assistance with laboratory procedure and dinocyst identification and E. Moreno, who ensured the accessibility of samples (MNHN core repository, Paris). XRF analyses were performed at EPOC Laboratory (Bordeaux, France). AMS dating was provided by ARTEMIS, UMS 2572, Laboratoire de Mesure du Carbone 14 (LMC14) (Saclay, France). W.F. and F.B are supported by CEA (France) and A.-M.L. by CNRS (France). This is LSCE contribution 5739.	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J	Fraga, S; Rodríguez, F; Riobó, P; Bravo, I				Fraga, Santiago; Rodriguez, Francisco; Riobo, Pilar; Bravo, Isabel			<i>Gambierdiscus balechii</i> sp nov (Dinophyceae), a new benthic toxic dinoflagellate from the Celebes Sea (SW Pacific Ocean)	HARMFUL ALGAE			English	Article						Benthic dinoflagellates; Celebes Sea; Ciguatera; Cysts; Gambierdiscus balechii; rRNA	GENUS GAMBIERDISCUS; CIGUATERA; GONYAULACALES; MORPHOLOGY; TAXONOMY; AREAS	A new benthic toxic dinoflagellate is described from the Celebes Sea. Gambierdiscus balechii sp. nov. was isolated from seaweeds growing in tidal ponds. Its morphology was studied by means of LM and SEM; G. balechii has a very ornamented theca, a hatchet shaped second apical plate, a narrow second antapical plate and an asymmetrical third precigular plate, a unique combination of characters among Gambierdiscus species. It has a very wide size range with widths from 36 to mu m. Phylogenetic analyses of two G. balechii strains, based on LSU rRNA (D8-D10) and partial SSUrRNA sequences confirmed that these clustererd in its' own group, separated from the rest of Gambierdiscus species and with G. pacificus, G. belizeanus and G. scabrosus as its closest relatives. Thecate cysts are described from culture as non motile vegetative-like cells which germinated after being isolated and transferred to fresh medium. Mouse tests showed that this species is toxic and hence it is a potential cause of ciguatera in the Celebes Sea. (C) 2016 Elsevier B.V. All rights reserved.	[Fraga, Santiago; Rodriguez, Francisco; Bravo, Isabel] Inst Espanol Oceanog, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain; [Riobo, Pilar] CSIC, IIM, Eduardo Cabello 6, Vigo 36208, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM)	Fraga, S; Rodríguez, F (通讯作者)，Inst Espanol Oceanog, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain.	santi.fraga@vi.ieo.es; francisco.rodriguez@vi.ieo.es; pilarriobo@iim.csic.es; isabel.bravo@vi.ieo.es	Fraga, Santiago/AAA-3760-2020; Bravo, Isabel/D-3147-2012; Riobo, Pilar/K-1945-2017; Rodriguez, Francisco/A-5934-2019	Riobo, Pilar/0000-0002-1921-6229; Rodriguez, Francisco/0000-0002-6918-4771; Bravo, Isabel/0000-0003-3764-745X	CICAN; CCVIEO	CICAN; CCVIEO	The comments and suggestions provided by the critical review of anonymous reviewers greatly improved this manuscript. The authors thank Antonella Penna for providing the samples from Manado from which the G. balechi strains were isolated. Ines Pazos from CACTI, Universidade de Vigo, for SEM and confocal microscopy. Angel Sebastian from CACTI, Universidade de Vigo, for DNA sequencing. The authors thank Fabiola Arevalo from INTECMAR (Vilagarcia de Arousa, Spain) for her help with the mouse bioassay. Amelia Fernandez-Villamarin, Isabel Ramilo, Pilar Rial for technical assistance. This work was funded by projects CICAN and CCVIEO. This is a contribution of Unidad Asociada IEO-CSIC Microalgas Nocivas.[SS]	ADACHI R, 1979, B JPN SOC SCI FISH, V45, P67; [Anonymous], 2012, GLOB EC OC HARMF ALG; BESADA EG, 1982, B MAR SCI, V32, P723; Bravo I, 2014, HARMFUL ALGAE, V40, P1, DOI 10.1016/j.hal.2014.09.009; Bravo Isabel, 2014, Microorganisms, V2, P11; Chinain M, 1999, J PHYCOL, V35, P1282, DOI 10.1046/j.1529-8817.1999.3561282.x; De Fouw J.C., 1999, 388802021 IRVM; de Silva E., 1956, Bull. Inst. Fr. 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J	Aubry, AMR; de Vernal, A; Hillaire-Marcel, C				Aubry, A. M. R.; de Vernal, A.; Hillaire-Marcel, C.			The "warm" Marine Isotope Stage 31 in the Labrador Sea: Low surface salinities and cold subsurface waters prevented winter convection	PALEOCEANOGRAPHY			English	Article						water stratification; Jaramillo; Labrador Sea; MAT; dinocysts; foraminifera	FORAMINIFER NEOGLOBOQUADRINA-PACHYDERMA; NORTH-ATLANTIC; PLANKTONIC-FORAMINIFERA; DINOFLAGELLATE CYST; BENTHIC FORAMINIFERA; PLEISTOCENE; ICE; PLIOCENE; CIRCULATION; CALIBRATION	Surface and subsurface conditions in the Labrador Sea during Marine Isotope Stage (MIS) 31 at the Integrated Ocean Drilling Program Site U1305 off southwest Greenland are reconstructed based on dinocyst and foraminifer assemblages. Isotopic compositions of planktonic (Neogloboquadrina pachyderma, Np) and benthic (Cibicides wuellerstorfi, Cw, and Oridorsalis umbonatus, Ou) foraminifera provide further information about water properties in the mesopelagic layer as well as at the seafloor. Dinocyst proxy reconstructions indicate low salinities (32-34.5), cool winters (3-6 degrees C), and mild summers (10-15 degrees C) in the surface water layer during the MIS 31 optimum. However, planktonic foraminifer assemblages largely dominated by Np suggest relatively cold subsurface conditions in winter and summer (<4 degrees C). Lower C-13 values in Np versus Cw further suggest either a lesser-ventilated mesopelagic layer than the bottom one or high organic matter oxidation rates at Np habitat depth. The dinocyst and planktonic foraminifer records together suggest a strong stratification between the surface and subsurface water layers. Isotopic and micropaleontological data thus converge toward paleoceanographical conditions unsuitable for convection and intermediate or deep water formation in the Labrador Sea during the warm MIS 31 interglacial, a situation comparable to the one that prevailed during the warm MIS 5e.	[Aubry, A. M. R.; de Vernal, A.; Hillaire-Marcel, C.] Univ Quebec, Geotop, Montreal, PQ, Canada	University of Quebec; University of Quebec Montreal	Aubry, AMR (通讯作者)，Univ Quebec, Geotop, Montreal, PQ, Canada.	aurelieaubry@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	Integrated Ocean Drilling Program (IODP); Natural Sciences and Engineering Research Council of Canada; Fonds Quebecois de Recherche sur la Nature et les Technologies	Integrated Ocean Drilling Program (IODP); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Fonds Quebecois de Recherche sur la Nature et les Technologies(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	This research used samples provided by the Integrated Ocean Drilling Program (IODP, 2003-2013). Funding was granted from the Natural Sciences and Engineering Research Council of Canada (discovery grants to A. de Vernal and C. Hillaire-Marcel) and the Fonds Quebecois de Recherche sur la Nature et les Technologies (team awards to de Vernal et al.). We are grateful to Michal Kucera for providing the MARGO data and the corresponding temperatures at different water depths in the water column. We acknowledge the help of Jean-Francois Helie (GEOTOP-UQAM) for isotopic measurements in foraminifera. All the data set for this paper are available through the GEOTOP database http://www.geotop.ca/en/bases-de-donnees/paleoceanographiques.html. For any questions or requests about the data set, please contact me at aurelieaubry@gmail.com. We thank Antje Voelker and the anonymous reviewer for their helpful and constructive comments on the manuscript.	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J	Song, CH; Zeng, YY; Yan, MD; Wu, S; Fang, XM; Bao, J; Zan, JB; Liu, XF				Song, Chunhui; Zeng, Yongyao; Yan, Maodu; Wu, Song; Fang, Xiaomin; Bao, Jing; Zan, Jinbo; Liu, Xifang			Magnetostratigraphy of the middle-upper Jurassic sedimentary sequences at Yanshiping, Qiangtang Basin, China	GEOPHYSICAL JOURNAL INTERNATIONAL			English	Article						Magnetostratigraphy; Palaeomagnetism applied to tectonics; Rock and mineral magnetism; Asia	RESOLUTION MAGNETO STRATIGRAPHY; NE TIBETAN PLATEAU; TECTONIC EVOLUTION; DINOFLAGELLATE CYSTS; QINGHAI PROVINCE; NORTHERN TIBET; AREA; GROWTH; BIOSTRATIGRAPHY; DEFORMATION	A series of important geological events occurred in the Tibetan Plateau area during the Jurassic, such as the collision of the Lhasa and Qiangtang Terranes, the closure of the Meso-Tethyan Ocean, the opening of the Neo-Tethyan Ocean and the cessation of the mega-monsoon. The similar to 3000 m thick Jurassic sedimentary sequence in the Qiangtang Basin on the central Tibetan Plateau, which is called the Yanshiping (YSP) Group, recorded these geological events. However, the chronology of the sequence is surprisingly poorly constrained. Here, we perform a detailed palaeomagnetic analysis on the similar to 1060 m thick middle and upper portions of the YSP Group (the Xiali and Suowa Formations) in the YSP section of the eastern Qiangtang Basin. Three bivalve zones at stratigraphic intervals of similar to 40-140, 640-800 and 940-1040 m are identified, which yield a Bathonian-Callovian age for the Lower Xiali Fm., a Callovian-Oxfordian age for the Lower Suowa Fm. and an Oxfordian-Kimmeridgian age for the Upper Suowa Fm. A total of 544 oriented palaeomagnetic samples were collected from the section. By combining thermal and alternating field demagnetizations, clear characteristic remanent magnetization (ChRM) directions are isolated for most of the samples. The robust ChRM directions pass fold and reversals tests, which support the primary nature of the ChRMs and yield a palaeopole at 76.8A degrees N/297.2A degrees E (dp = 2.2A degrees, dm = 3.7A degrees). A total of 27 normal and 26 reversed polarity zones were successfully recorded in the section. Combined with fossil age constraints, results suggest that the section is plausibly composed of a Callovian-Early Kimmeridgian age sedimentary sequence.	[Song, Chunhui; Zeng, Yongyao; Wu, Song; Bao, Jing] Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China; [Song, Chunhui; Zeng, Yongyao; Wu, Song; Bao, Jing] Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou 730000, Peoples R China; [Yan, Maodu; Fang, Xiaomin; Zan, Jinbo] Chinese Acad Sci, Inst Tibetan Plateau Res, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China; [Yan, Maodu; Fang, Xiaomin; Zan, Jinbo] Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China; [Liu, Xifang] Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China; [Liu, Xifang] Minist Land & Resources, Key Lab Saline Lake Resources & Environm, Beijing 100037, Peoples R China	Lanzhou University; Lanzhou University; Chinese Academy of Sciences; Institute of Tibetan Plateau Research, CAS; Chinese Academy of Sciences; Institute of Tibetan Plateau Research, CAS; China Geological Survey; Chinese Academy of Geological Sciences; Ministry of Natural Resources of the People's Republic of China	Song, CH (通讯作者)，Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China.; Song, CH (通讯作者)，Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou 730000, Peoples R China.	songchh@lzu.edu.cn	Zan, Jinbo/AAI-4457-2020; Yan, Maodu/AAZ-4958-2021; zeng, yongyao/GLR-7275-2022	Yan, Maodu/0000-0002-9257-5412	National Basic Research Program of China [2011CB403000]; Chinese Academy of Sciences; National Natural Science Foundation of China [41272128, 41272185, 41321061]	National Basic Research Program of China(National Basic Research Program of China); Chinese Academy of Sciences(Chinese Academy of Sciences); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	This study was supported by the National Basic Research Program of China (Grant No. 2011CB403000) and programs of the Chinese Academy of Sciences and the National Natural Science Foundation of China (Grant Nos 41272128, 41272185 and 41321061). Prof Jingen Sha from Nanjing Institute of Geology and Palaeontology CAS is thanked for identifying the bivalve fossils, and Xiaohui Fang, Gang Niu, Sa Zhang, Dawen Zhang, Jiaqiu Pan, Lifang Ma and Jiwei Yang are thanked for laboratory and fieldwork assistance. Mark J. Dekkers, Luca Lanci, an anonymous reviewer and Editor Eduard Petrovsky are thanked for making many valuable suggestions to improve the manuscript.	ALLEGRE CJ, 1984, NATURE, V307, P17, DOI 10.1038/307017a0; [Anonymous], ADM MANAGEMENT CHINA; [Anonymous], EARTH PLANETARY SCI; [Anonymous], STRATIGRAPHY QINGHAI; [Anonymous], 1996, Palynology: principles and applications; Atrops Francois, 1993, Geobios Memoire Special (Villeurbanne), V15, P19; Bai S., 1989, GEOL REV, V35, P529; Callomon J.H., 2000, Advances in Jurassic Research 2000. 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J. Int.	SEP	2016	206	3					1847	1863		10.1093/gji/ggw199	http://dx.doi.org/10.1093/gji/ggw199			17	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	DX8PG		Bronze			2025-03-11	WOS:000384650400028
J	Fang, XM; Song, CH; Yan, MD; Zan, JB; Liu, CL; Sha, JG; Zhang, WL; Zeng, YY; Wu, S; Zhang, DW				Fang, Xiaomin; Song, Chunhui; Yan, Maodu; Zan, Jinbo; Liu, Chenglin; Sha, Jingeng; Zhang, Weilin; Zeng, Yongyao; Wu, Song; Zhang, Dawen			Mesozoic litho- and magneto-stratigraphic evidence from the central Tibetan Plateau for megamonsoon evolution and potential evaporites	GONDWANA RESEARCH			English	Article						Mesozoic magnetostratigraphy; Central Tibetan Plateau; Land-sea interaction climate model; Megamonsoon; Evaporite mineral sources	PALEOMAGNETIC CONSTRAINTS; DINOFLAGELLATE CYSTS; TECTONIC EVOLUTION; CHINA EVIDENCE; SOUTHERN ASIA; CLIMATE; QIANGTANG; MONSOON; UPLIFT; PALEOGEOGRAPHY	The megamonsoon was a striking event that profoundly impacted the climatic environment and related mineral sources (salts, coals and oil-gases) in the Mesozoic. How this event impacted Asia is unknown. Here, we firstly reported a Mesozoic stratigraphic sequence in the northern Qiangtang Basin, in the central Tibetan Plateau, based on lithofacies and chronologies of paleontology and magnetostratigraphy. Hpw the planetary and megamonsoon circulations controlled the Asian climate with time has been recorded. Using the basic principles of physical geography, present analogs and a newly developed model, the evolution of the stratigraphic sequence was interpreted to demonstrate that the Qiangtang Basin has been subjected to a megamonsoon climate with heavy precipitation during its northward movement since the Latest Permian but has been subjected to a dry environment due to moving into the northern hemisphere subtropic high zone in the Middle Triassic and monsoonal retreat in the early Late Jurassic (early Oxfordian) approximately 161 Ma. The coupling of the hot-dry climate and the close of the Meso-Tethys, along with sea retreat in the Late Jurassic, ensured a large potential time window for evaporite (potash) formation in the Qiangtang Basin, while the tropic megamonsoon rain forest in the Late Permian to the Early Triassic and in the Late Triassic to Middle Jurassic favored the formation of coal and hydrocarbon source rocks. (C) 2016 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[Fang, Xiaomin; Yan, Maodu; Zan, Jinbo; Zhang, Weilin; Zhang, Dawen] Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China; [Fang, Xiaomin; Yan, Maodu; Zan, Jinbo; Zhang, Weilin; Zhang, Dawen] Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China; [Song, Chunhui; Zeng, Yongyao; Wu, Song] Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China; [Song, Chunhui; Zeng, Yongyao; Wu, Song] Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou 730000, Peoples R China; [Liu, Chenglin] Chinese Acad Geol Sci, Inst Mineral Resources, MLR Key Lab Metallogeny & Mineral Assessment, Beijing 100037, Peoples R China; [Sha, Jingeng] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, 39 East Beijing Rd, Nanjing 210008, Jiangsu, Peoples R China	Chinese Academy of Sciences; Chinese Academy of Sciences; Institute of Tibetan Plateau Research, CAS; Lanzhou University; Lanzhou University; China Geological Survey; Chinese Academy of Geological Sciences; Chinese Academy of Sciences	Fang, XM (通讯作者)，Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China.; Fang, XM (通讯作者)，Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China.	fangxm@itpcas.ac.cn	Zan, Jinbo/AAI-4457-2020; zeng, yongyao/GLR-7275-2022; Yan, Maodu/AAZ-4958-2021	Yan, Maodu/0000-0002-9257-5412	National Basic Research Program of China [2011CB403000]; National Natural Science Foundation of China [41272128, 41321061, 41272185]	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))	This study was supported by the National Basic Research Program of China (Grant No. 2011CB403000) and National Natural Science Foundation of China (Grant No. 41272128, 41321061, 41272185). Fuli Wu, Xiaohui Fang, Gang Niu, Haidong Ren, Sa Zhang, and Jiwei Yang are thanked for their assistance in the laboratory and fieldwork. Cordial thanks are also given to Professor Xu Chen, Professor C. R. Scotese and Professor Rob Van der Voo for their encouragement and valuable discussions about continental drifting and allowing us to use their series maps of reconstructed global continents and climatic records for the Mesozoic.	[Anonymous], J CHENGDU COLL GEOLO; Arkell W.J., 1933, JURASSIC SYSTEM GREA, P681; Bai S., 1989, GEOL REV, V35, P529; BGMRXAR (Bureau of Geology Mineral Resources of Xizang Autonomous Region), 1993, REG GEOL XIZ TIB, P137; Boos WR, 2010, NATURE, V463, P218, DOI 10.1038/nature08707; Boucot A. 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SEP	2016	37						110	129		10.1016/j.gr.2016.05.012	http://dx.doi.org/10.1016/j.gr.2016.05.012			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DX9HC					2025-03-11	WOS:000384703200008
J	Cormier, MA; Rochon, A; de Vernal, A; Gélinas, Y				Cormier, Marc-Andre; Rochon, Andre; de Vernal, Anne; Gelinas, Yves			Multi-proxy study of primary production and paleoceanographical conditions in northern Baffin Bay during the last centuries	MARINE MICROPALEONTOLOGY			English	Article						Arctic; Quantitative reconstruction; Dinoflagellate; Isotopic composition; Transfer function; Biomarkers	SEA-ICE RECONSTRUCTIONS; LATE SUMMER CONDITIONS; SURFACE CONDITIONS; HOLOCENE CLIMATE; ORGANIC-MATTER; HIGH-LATITUDES; WATER POLYNYA; BEAUFORT SEA; MARINE; CARBON	As polynyas are often used around the globe as a window on tomorrow's marine polar ecosystems, this study presents reconstructions of primary production and sea-surface conditions near the North Water polynya, since similar to 1560 CE from palynological, isotopic and biomarker analyses of a sediment core. Quantitative reconstructions of sea-surface conditions (temperature, sea-ice cover and production) were derived from the Modern Analogue Technique (MAT) applied to dinoflagellate cyst assemblages. Production was also qualitatively estimated from the stable isotope composition of organic carbon and nitrogen and the concentration of organic biomarkers (IP25, dinosterols). The results show relatively stable oceanographic conditions but suggest a slight warming accompanied by an increase in productivity after 1860 CE. The comparison of MAT reconstructions and the organic biomarker data suggests that IP25 provides information about primary production associated with sea-ice but does not unequivocally reflect sea-ice concentration in this regional setting, which is marked by dense seasonal sea ice except during the short summer season. (C) 2016 Elsevier B.V. All rights reserved.	[Cormier, Marc-Andre; Rochon, Andre] Univ Quebec, Inst Sci Mer ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada; [de Vernal, Anne] Univ Quebec, Ctr GEOTOP, Montreal, PQ H3C 3P8, Canada; [Gelinas, Yves] Concordia Univ, Geotop, 7141 Sherbrooke St West,SP Bldg, Montreal, PQ H4B 1R6, Canada	University of Quebec; University of Quebec; University of Quebec Montreal; Concordia University - Canada	Cormier, MA (通讯作者)，ETH, Environm Syst Sci, LFW D13,Univ Str 2, CH-8092 Zurich, Switzerland.	ma_cormier@alumni.ethz.ch	de Vernal, Anne/D-5602-2013; Gélinas, Yves/K-4019-2013	Cormier, Marc-Andre, Francis/0000-0001-7645-1375	Natural Sciences and Engineering Research Council of Canada (NSERC); 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)); Fonds de recherche du Quebec - Nature et technologies (FRQNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	The authors are thankful to Dr. Guillaume Masse for the identification of the biomarker IP<INF>25</INF>, Dr. Bassam Ghaleb, Dr. Taoufik Radi and Mina Ibrahim for their laboratory assistance, Dr. Simon Belt, Dr. Maya Al-Sid-Cheikh and Dr. Christian Gagnon for their fruitful comments on the study. This work was supported by the Natural Sciences and Engineering Research Council of Canada (NSERC) and the Fonds de recherche du Quebec - Nature et technologies (FRQNT).	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J	Tahoun, SS; Deaf, AS				Tahoun, Sameh S.; Deaf, Amr S.			Could the conventionally known Abu Roash "G" reservoir (upper Cenomanian) be a promising active hydrocarbon source in the extreme northwestern part of Egypt? Palynofacies, palaeoenvironmental, and organic geochemical answers	MARINE AND PETROLEUM GEOLOGY			English	Article						Palynofacies; Palaeoenvironment; Organic geochemistry; Abu Roash "G"; Hydrocarbon potential; North Western Desert; Egypt	NORTH-WESTERN DESERT; SEA-LEVEL CHANGES; DINOFLAGELLATE CYSTS; VOCONTIAN BASIN; OIL-FIELD; MATTER; PALYNOLOGY; SEDIMENTS; WELL; STRATIGRAPHY	In different areas of the Western Desert of Egypt, the Abu Roash "G" Member exhibits either a reservoir or source affinity. Thus, thirteen cutting samples covering the Abu Roash "G" Member were selected from the Nest-1A well at Matruh Basin to investigate its hydrocarbon source potential. Palynological age dating of the section that is calibrated with foraminifera and ostracodes enabled a proper identification of the "G" Member. Detailed analysis of the vertical distribution of particulate organic matter of this member shows two palynofacies types. PF-1 reflects an outer middle shelf depositional environment of prevailed reducing (suboxic-anoxic) conditions for the organic-rich shales of the lower "G" Member (samples 1-8). While, PF-2 reflects a minor regression that resulted in deposition of another organic-rich shales of the upper "G" Member (samples 9-13) in an inner middle shelf setting under the same prevailing reducing (suboxic-anoxic) conditions. Organic geochemical analysis reveals good to very good potential of the "G" Member as a hydrocarbon source rock (1.8-2.41, avg. 2.15 total organic content wt %). It also shows good to very good petroleum potential (PP: 4.8-11, avg. 8 mg HC/g rock). Pyrolsis and palynofacies analyses show kerogen type II for the lower "G" Member (samples 1-8), which is characterized by high Hydrogen index (HI: 396 and 329 mg HC/g TOC at depths 1500 and 1560 m) and very high dominance of oil-prone material (amorphous organic matter "AOM", marine palynomorphs, and sporomorphs) and very rare occurrence of gas prone material (brown phytoclasts). The upper "G" Member (samples 9-13) shows kerogen type which is characterized by a lower HI value of 213 mg HC/g TOC at depth 1340 m and it contains fewer amounts of gas-prone material and relatively lower AOM and marine palynomorphs in comparison to the upper "G" Member. Maturation parameters T-max (430-433 degrees C), production index (PI: 0.1 mg HC/g rock), and thermal alteration index (TAI: 2+) indicate the lower "G" Member has already entered the early oil-window kitchen, and it is expected to produce oil. The upper "G" Member is expected to produce only oil with no gas shows, because it is marginally mature (T-max 426 degrees C, PI 0.2, TAI 2). The source potential index (SPI: 5.3 t HC/m(2)) of the "G" Member shows it as currently generating moderate quantities of oil in the area of Nest-1A well. Consequently, the organic-rich shales of the "G" Member are suggested here as a promising, active oil source rock in that extreme northwestern part of the Western Desert of Egypt. However, for commercial oil recovery from the Abu Roash "G" Member, it is highly recommended to explore the depocentre of Matruh Basin at about 150 km east the Nest-1A well. (C) 2016 Elsevier Ltd. All rights reserved.	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Pet. Geol.	SEP	2016	76						231	245		10.1016/j.marpetgeo.2016.05.025	http://dx.doi.org/10.1016/j.marpetgeo.2016.05.025			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DS2KR					2025-03-11	WOS:000380598900015
J	Hardy, W; Penaud, A; Marret, F; Bayon, G; Marsset, T; Droz, L				Hardy, William; Penaud, Aurelie; Marret, Fabienne; Bayon, Germain; Marsset, Tania; Droz, Laurence			Dinocyst assemblage constraints on oceanographic and atmospheric processes in the eastern equatorial Atlantic over the last 44 kyr	BIOGEOSCIENCES			English	Article							WEST-AFRICAN MONSOON; BENGUELA UPWELLING SYSTEM; HEINRICH STADIAL 1; DEEP-SEA FAN; DINOFLAGELLATE-CYST; GLACIAL MAXIMUM; ENVIRONMENTAL-CHANGE; VEGETATION CHANGE; CLIMATE CHANGES; ICE-CORE	A new 44 kyr long record of dinoflagellate (phytoplanktonic organisms) cysts (dinocysts) is presented from a marine sediment core collected on the Congolese margin with the aim of reconstructing past hydrological changes in the equatorial eastern Atlantic Ocean since Marine Isotopic Stage (MIS) 3. Our high-resolution dinocyst record indicates that significant temperature and moisture variations occurred across the glacial period, the last deglaciation and the Holocene. The use of specific dinocyst taxa, indicative of fluvial, upwelling and Benguela Current past environments for instance, provides insights into the main forcing mechanisms controlling palaeohydrological changes on orbital timescales. In particular, we are able, for the last 44 kyr, to correlate fluvial-sensitive taxa to monsoonal mechanisms related to precession minima-obliquity maxima combinations. While upwelling mechanisms appear as the main drivers for dinoflagellate productivity during MIS 2, dissolved nutrientenriched Congo River inputs to the ocean also played a significant role in promoting dinoflagellate productivity between approximately 15.5 and 5 ka BP. Finally, this highresolution dinocyst study permits us to precisely investigate the suborbital timing of the last glacial-interglacial termination, including an atypical warm and wet oceanic LGM signature, northern high-latitude abrupt climate change impacts in the equatorial eastern Atlantic, as well as a two-step decrease in moisture conditions during the Holocene at around 7-6 and 4-3.5 ka BP.	[Hardy, William; Penaud, Aurelie; Droz, Laurence] IUEM UBO, UMR Domaines Ocean 6538, F-29280 Plouzane, France; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Bayon, Germain; Marsset, Tania] IFREMER, UR Geosci Marines, BP 70, F-29280 Plouzane, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; University of Liverpool; Ifremer	Hardy, W (通讯作者)，IUEM UBO, UMR Domaines Ocean 6538, F-29280 Plouzane, France.	william.hardy@univ-brest.fr	Bayon, Germain/F-9754-2010; Droz, Laurence/P-8209-2019; Penaud, Aurélie/F-2485-2011; Marsset, Tania/A-4163-2012	Droz, Laurence/0000-0002-6694-1247; Marret-Davies, Fabienne/0000-0003-4244-0437; Bayon, Germain/0000-0002-6791-4953	Brittany Region; "Laboratoire d'Excellence" LabexMER [ANR-10-LABX-19]; French government under the program "Investissements d'Avenir"	Brittany Region(Region Bretagne); "Laboratoire d'Excellence" LabexMER; French government under the program "Investissements d'Avenir"(Agence Nationale de la Recherche (ANR))	William Hardy's PhD was funded by the Brittany Region and this work was supported by the "Laboratoire d'Excellence" LabexMER (ANR-10-LABX-19) and co-funded by a grant from the French government under the program "Investissements d'Avenir". We thank B. Dennielou (Ifremer, Brest) for access to core KZAI-01. We thank the two anonymous reviewers for their constructive comments that helped to improve this manuscript.	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J	Shcherbinina, E; Gavrilov, Y; Iakovleva, A; Pokrovsky, B; Golovanova, O; Aleksandrova, G				Shcherbinina, Ekaterina; Gavrilov, Yuri; Iakovleva, Alina; Pokrovsky, Boris; Golovanova, Olga; Aleksandrova, Galina			Environmental dynamics during the Paleocene-Eocene thermal maximum (PETM) in the northeastern Peri-Tethys revealed by high-resolution micropalaeontological and geochemical studies of a Caucasian key section	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Paleocene-Eocene-Thermal Maximum; Nannofossils; Dinocysts; Organic matter; Carbon and oxygen isotopes	CARBON-ISOTOPE EXCURSION; CALCAREOUS NANNOPLANKTON; DINOFLAGELLATE CYSTS; ARCTIC-OCEAN; NEW-ZEALAND; MARINE; ACIDIFICATION; DABABIYA; RECORDS; CLIMATE	The sedimentary record of the Paleocene-Eocene Thermal Maximum (PETM) in the wide epeiric sea of the NE Peri-Tethys contains a sapropelitic bed (SBD) characterized by a specific microfossil assemblage and negative oxygen and carbon isotope excursions (CIE). New results obtained from a high-resolution sampling of this interval in the Kheu section, central Caucasus, allows us to explore the succession, interrelationships and consequences of global and regional palaeoenvironmental events during the PETM. The CIE apparently lasted twice as long as the SBD accumulation period; thus, the SBD represents a response to the early and most dramatic phase of the PETM related to rapid transgression and greatly enhanced eutrophication of the basin. The lithological architecture of the SBD represents four bands, each of which consists of a dark, low-calcareous TOC-rich clay and relatively paler calcareous clays. The highest TOC concentrations are found in the lower and upper bands of the SBD; however, the lower band mostly consists of basinal organic matter, while the upper band represents mixed, basinal and terrestrial, organic matter. Pre-PETM events include the initial evolution of the Rhomboaster nannofossil lineage with the early first appearance of a short-arm species, relatively reduced calcareous plankton productivity, changes in the ratios of dinocyst ecological groups, and minor fluctuations in delta C-13 and delta O-18. The onset of the CIE corresponds to the base of the SBD, which exhibits a dramatic decrease in total nannofossil abundance and an increase in total dinoflagellate abundance, the occurrence of "excursion taxa" of nannofossils (rhomboasters, asymmetric discoasters) and dinocysts (Axiodinium augustum, Epelidinium pechoricum), and significant variations in the species ratios of both nannoplankton and dinoflagellate communities, with widespread dominance of warm-water and eutrophic species. Above the SBD but during the late phase of CIE, the nannofossil abundance and species composition show a slight recovery, but most Paleocene taxa become extinct during the CIE recovery. Apectodinium spp. significantly decrease in abundance above the SBD, but rare specimens of Ax. augustum persist higher in the section after the end of the CIE. Thus, the major extinction of the Paleocene nannofossil taxa occurs after the termination of the most critical conditions during the CIE recovery phase, while the dinocyst "excursion taxa" survive even later. (C) 2016 Elsevier B.V. All rights reserved.	[Shcherbinina, Ekaterina; Gavrilov, Yuri; Iakovleva, Alina; Pokrovsky, Boris; Golovanova, Olga; Aleksandrova, Galina] Russian Acad Sci, Inst Geol, Pyzhevsky 7, Moscow 119017, Russia	Russian Academy of Sciences	Shcherbinina, E (通讯作者)，Russian Acad Sci, Inst Geol, Pyzhevsky 7, Moscow 119017, Russia.	katuniash@gmail.com	Golovanova, Olga/ABC-5770-2021; IAKOVLEVA, ALINA/ABH-9243-2020; Galina, Aleksandrova/AAW-8215-2020	Golovanova, Olga/0000-0003-4995-7789; Galina, Aleksandrova/0000-0001-5402-6968; Pokrovsky, Boris/0000-0003-3112-5044	Russian Foundation of Basic Research [15-05-07556]; Geological Institute of Russian Academy of Sciences [0135-2014-0070, 0135-2014-0028, 0135-2014-0024]	Russian Foundation of Basic Research(Russian Foundation for Basic Research (RFBR)); Geological Institute of Russian Academy of Sciences	We are very thankful to Prof. Marie-Pierre Aubry for thorough revision and fruitful discussion helping to improve this paper.We thank Dr. Hans Egger for careful reading of the manuscript and important remarks. This research was supported by the Russian Foundation of Basic Research (Project no. 15-05-07556). This paper is written as a part of the research on the State Programmes nos. 0135-2014-0070, 0135-2014-0028 and 0135-2014-0024 of the Geological Institute of Russian Academy of Sciences.	Aarnes I, 2015, J GEOL SOC LONDON, V172, P588, DOI 10.1144/jgs2014-098; Agnini C, 2014, NEWSL STRATIGR, V47, P131, DOI 10.1127/0078-0421/2014/0042; AKHMETIEV M. A., 1996, FOSSIL MICROORGANISM, P55; Alegret L, 2010, GEOL SOC AM BULL, V122, P1616, DOI 10.1130/B30055.1; Alegret L, 2009, PALAIOS, V24, P318, DOI 10.2110/palo.2008.p08-057r; Angori E, 2007, GEOL SOC AM SPEC PAP, V424, P69, DOI 10.1130/2007.2424(04); [Anonymous], CLIMATE DISCUSSION; [Anonymous], 1981, SPECIAL PUBLICATION; [Anonymous], LITHOL MINER RESOUR; Aubry M. 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J	Price, AM; Pospelova, V; Coffin, MRS; Latimer, JS; Chmura, GL				Price, Andrea M.; Pospelova, Vera; Coffin, Michael R. S.; Latimer, James S.; Chmura, Gail L.			Biogeography of dinoflagellate cysts in northwest Atlantic estuaries	ECOLOGY AND EVOLUTION			English	Article						Coastal waters; estuary type; northeast USA; palynology; phytoplankton; Prince Edward Island; water quality	NORTHEASTERN UNITED-STATES; ENVIRONMENTAL-FACTORS; SPATIAL-DISTRIBUTION; NORTHERN-HEMISPHERE; SURFACE SEDIMENTS; WEST-COAST; PHYTOPLANKTON; BAY; ASSEMBLAGES; MASSACHUSETTS	Few biogeographic studies of dinoflagellate cysts include the near-shore estuarine environment. We determine the effect of estuary type, biogeography, and water quality on the spatial distribution of organic-walled dinoflagellate cysts from the Northeast USA (Maine to Delaware) and Canada (Prince Edward Island). A total of 69 surface sediment samples were collected from 27 estuaries, from sites with surface salinities > 20. Dinoflagellate cysts were examined microscopically and compared to environmental parameters using multivariate ordination techniques. The spatial distribution of cyst taxa reflects biogeographic provinces established by other marine organisms, with Cape Cod separating the northern Acadian Province from the southern Virginian Province. Species such as Lingulodinium machaerophorum and Polysphaeridinium zoharyi were found almost exclusively in the Virginian Province, while others such as Dubridinium spp. and Islandinium? cezare were more abundant in the Acadian Province. Tidal range, sea surface temperature (SST), and sea surface salinity (SSS) are statistically significant parameters influencing cyst assemblages. Samples from the same type of estuary cluster together in canonical correspondence analysis when the estuaries are within the same biogeographic province. The large geographic extent of this study, encompassing four main estuary types (riverine, lagoon, coastal embayment, and fjord), allowed us to determine that the type of estuary has an important influence on cyst assemblages. Due to greater seasonal variations in SSTs and SSSs in estuaries compared to the open ocean, cyst assemblages show distinct latitudinal trends. The estuarine context is important for understanding present-day species distribution, the factors controlling them, and to better predict how they may change in the future.	[Price, Andrea M.; Chmura, Gail L.] McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ H3A 0B9, Canada; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB A405,POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada; [Coffin, Michael R. S.] Univ Prince Edward Isl, Dept Biol, Charlottetown, PE C1A 4P3, Canada; [Latimer, James S.] US EPA, Off Res & Dev, Narragansett, RI 02882 USA	University of Victoria; University of Prince Edward Island; United States Environmental Protection Agency	Price, AM (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ H3A 0B9, Canada.	pricea@uvic.ca	Latimer, James/C-1632-2009; Coffin, Michael/AAE-1407-2022; Chmura, Gail/LNI-4648-2024	Chmura, Gail/0000-0001-7163-3903; Pospelova, Vera/0000-0003-4049-8133; Price, Andrea/0000-0002-5359-053X	Natural Sciences and Engineering Research Council of Canada	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	Natural Sciences and Engineering Research Council of Canada	ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Briggs JC, 2012, J BIOGEOGR, V39, P12, DOI 10.1111/j.1365-2699.2011.02613.x; CLOERN JE, 1985, HYDROBIOLOGIA, V129, P153, DOI 10.1007/BF00048693; Cooke R., 2007, MMR 2007: Mathematical methods in reliability, P1; 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, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A, 2013, QUATERNARY SCI REV, V79, P122, DOI 10.1016/j.quascirev.2013.06.022; de Vernal A, 2007, DEV MARINE GEOL, V1, P371, DOI 10.1016/S1572-5480(07)01014-7; DYER K.R., 1973, ESTUARIES PHYS INTRO, P1; Ekman S., 1953, Zoogeography of the Sea, P1; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Ellegaard M, 2006, ESTUAR COAST SHELF S, V68, P567, DOI 10.1016/j.ecss.2006.03.013; EPA, 2006, STAT LOC VIS INF NAT; Fitzgerald M. 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F., 1988, CANOCO REFERENCE MAN; Townsend DavidW., 2006, SEA VOLUME 14A, P119; Usup G, 2012, HARMFUL ALGAE, V14, P301, DOI 10.1016/j.hal.2011.10.026; Verardo S., 1999, MICROFOSSILS CHESAPE, p[72, 99]; Wake C., 2006, CROSS BORDER INDICAT; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wares JP, 2002, MOL ECOL, V11, P1131, DOI 10.1046/j.1365-294X.2002.01510.x; Zonneveld KAF, 2010, BIOGEOSCIENCES, V7, P483, DOI 10.5194/bg-7-483-2010; Zonneveld KAF, 2015, PALYNOLOGY, V39, P387, DOI 10.1080/01916122.2014.990115; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	77	29	29	0	7	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	2045-7758			ECOL EVOL	Ecol. Evol.	AUG	2016	6	16					5648	5662		10.1002/ece3.2262	http://dx.doi.org/10.1002/ece3.2262			15	Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Evolutionary Biology	DT6FF	27547344	gold, Green Published			2025-03-11	WOS:000381578400008
J	Deng, YY; Hu, ZX; Ma, ZP; Tang, YZ				Deng Yunyan; Hu Zhangxi; Ma Zhaopeng; Tang Ying Zhong			Validation of reference genes for gene expression studies in the dinoflagellate Akashiwo sanguinea by quantitative real-time RT-PCR	ACTA OCEANOLOGICA SINICA			English	Article						Akashiwo sanguinea; dinoflagellate; internal control; qRT-PCR; resting cyst; reference gene	INTERNAL CONTROL GENES; HOUSEKEEPING GENES; ALGAL BLOOMS; NORMALIZATION; SELECTION; PROGRESS; GROWTH; CYSTS; MODEL	The accurate measurement of gene expression via quantitative real-time reverse transcription PCR (qRT-PCR) heavily relies on the choice of valid reference gene(s) for data normalization. Resting cyst is the dormant stage in the life cycle of dinoflagellate, which plays crucial roles in HAB-forming dinoflagellate ecology. However, only limited investigations have been conducted on the reference gene selection in dinoflagellates. Gap remained in our knowledge about appropriate HKGs for normalizing gene expression in different life stages, which laid obstacles for the application of qRT-PCR to the HAB-forming group. In this study, six candidate reference genes, 18S ribosomal RNA (18S), glyceraldehyde-3-phosphate dehydrogenase (GAPDH), alpha-tubulin (TUA), beta-tubulin (TUB), actin (ACT) and cytochrome oxidase subunit 1 (COX1), were evaluated for their expression stability with qRT-PCR and three statistical algorithms (GeNorm, NormFinder, and BestKeeper) for the cosmopolitan, harmful algal bloom-forming dinoflagellate Akashiwo sanguinea. Expression patterns were observed across 18 biological samples, including cells at resting stages (resting cysts), different growth stages, in darkness, exposed to abscisic acid (ABA) and exposed to temperature stress. The results indicated that TUA,.18S,and GAPDH were relatively stable across all tested scenarios. While the best-recommended reference genes differed across experimental groups, the pairs of ACT and TUA, 18S and GAPDH were the most reliable for cells at different growth stages and darkness treatment. The combination of TUA and TUB was the best choice for normalization in resting cysts and in ABA treatment, respectively. The pair of ACT and COXI was suitable for temperature treatments. This study was the first to investigate the stable internal reference genes in dinoflagellates at different stages of life cycle, particularly in resting cysts. Our results provided useful information for selection of reference genes in dinoflagellates regarding quantification of gene expression at different experimental scenarios, which will facilitate more accurate and widespread use of qRT-PCR in gene analysis of dinoflagellates and help to design primers targeting orthologous genes in other algal species.	[Deng Yunyan; Hu Zhangxi; Ma Zhaopeng; Tang Ying Zhong] Chinese Acad Sci, Key Lab Marine Ecol & Environm Sci, Inst Oceanol, Qingdao 266071, Peoples R China; [Tang Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, 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; Laoshan Laboratory; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Tang, YZ (通讯作者)，Chinese Acad Sci, Key Lab Marine Ecol & Environm Sci, Inst Oceanol, Qingdao 266071, Peoples R China.; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023		National Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers [U1406403]; State Key Program of National Natural Science of China [61533011]; China Postdoctoral Science Foundation [2014M551969, 2015T80754]	National Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers; State Key Program of National Natural Science of China(National Natural Science Foundation of China (NSFC)); China Postdoctoral Science Foundation(China Postdoctoral Science Foundation)	Foundation item: The National Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers under contract No. U1406403; the State Key Program of National Natural Science of China under contract No. 61533011; China Postdoctoral Science Foundation under contract Nos 2014M551969 and 2015T80754.	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Sin.	AUG	2016	35	8					106	113		10.1007/s13131-016-0887-9	http://dx.doi.org/10.1007/s13131-016-0887-9			8	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	DT1NH					2025-03-11	WOS:000381248900015
J	Carreto, JI; Montoya, NG; Carignan, MO; Akselman, R; Acha, EM; Derisio, C				Carreto, Jose I.; Montoya, Nora G.; Carignan, Mario O.; Akselman, Rut; Marcelo Acha, E.; Derisio, Carla			Environmental and biological factors controlling the spring phytoplankton bloom at the Patagonian shelf-break front - Degraded fucoxanthin pigments and the importance of microzooplankton grazing	PROGRESS IN OCEANOGRAPHY			English	Review							WESTERN SOUTH-ATLANTIC; RESTING STAGE CELLS; CHLOROPHYLL-A; ARGENTINE SEA; EMILIANIA-HUXLEYI; PLANKTON COMMUNITIES; OITHONA-SIMILIS; CHLORIN ESTERS; MARINE FRONTS; DIATOM BLOOM	The aim of this study was to investigate the biotic and abiotic factors controlling the spring phytoplankton blooms at the Patagonian shelf-break front (PSBF). Using a CHEMTAX analysis of HPLC pigment data and other methods, the biomass and spatial variability of plankton communities were studied in four sections (39-48 S) across the PSBF during October 2005. Environmental factors and the biomass and composition of plankton communities exhibited a marked spatial heterogeneity. The latitudinal and cross-shelf progression in the timing of the spring bloom initiation and the nutritive properties of the water masses (Subantarctic Shelf Waters and Malvinas Current Waters) seemed to be the key factors. Three plankton regions were distinguished: (a) Outer shelf (OS), (b) Shelf-break front (SBF) and (c) Malvinas Current (MC). At the highly stratified OS region, the post-bloom community showed low-biomasshigh-phytoplankton diversity formed mainly by small cells (haptophytes 30-62%, diatoms 17-49%, chlorophytes 0-34%, and prasinophytes 0-21% of total Chl a). High amounts of degraded fucoxanthin were found associated with the heterotrophic dinoflagellate, Protoperidinium capurroi. Grazing by this microheterotroph on the diatom population seemed to be the most important factor for the spring bloom decay at the OS. A remarkable quasi monospecific bloom (similar to 90%) of a nanodiatom (Thalassiosira bioculata var. raripora) associated with high Chl a (up to 20 mg m(-3)) occurred along (1000 km) the SBF and in the most northern extension of the MC. In the southern region, the bloom was developed under absent or incipient density stratification, increasing solar irradiance, high nitrate and phosphate availability, and low numbers of phytoplankton grazers. The average mixedlayer PAR irradiance (<2.0 mol quanta PAR m(-2) d(-1)) and Si:N ratios (<0.2) were low, suggesting a diatom population limited by light and under progressive silicate limitation. The more stratified northern region of the SBF showed a later stage of the bloom development, but the large population of diatoms under Si limitation was not in senescence and losses from microzooplankton grazing were minor. The observed high proportion of Chl a below a shallow upper mixed layer (up to 85%) could directly reach the bed, favoring the development of epibenthic communities and the formation of seed diatom banks and organic iron-rich sediments. The upwelling along the SBF provides a large source of macronutrients and probably the dissolved iron needed to sustain the intense diatom bloom, but also diatom resting stages that could act as seeds for the next spring bloom. The macronutrient-rich MC region showed low chlorophyll (Chl a < 0.8 mg m(-3)) and a highly diverse phytoplankton community, mainly composed of small cells (diatoms 20-70%, haptophytes 20-40%, chlorophytes 2-25%, prasinophytes 2-18%, and cryptophytes 3-12% of total Chl a). (C) 2016 Elsevier Ltd. All rights reserved.	[Carreto, Jose I.; Montoya, Nora G.; Carignan, Mario O.; Akselman, Rut; Marcelo Acha, E.; Derisio, Carla] Inst Nacl Invest & Desarrollo Pesquero INIDEP, V Ocampo 1,B7602HSA, Mar Del Plata, Buenos Aires, Argentina; [Marcelo Acha, E.; Derisio, Carla] Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina; [Marcelo Acha, E.] Univ Nacl Mar del Plata, Fac Ciencias Exactas & Nat, IIMyC, Mar Del Plata, Buenos Aires, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National Fisheries Research & Development Institute (INIDEP); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of Mar del Plata	Carreto, JI (通讯作者)，Inst Nacl Invest & Desarrollo Pesquero INIDEP, Paseo Victoria Ocampo 1,B7602HSA, Mar Del Plata, Buenos Aires, Argentina.	jcarreto@inidep.edu.ar			INIDEP; Fundacion Antorchas [13900-13, PNUDARG02/018, BB23, BB33]; CONICET [PIP-112-201101-00892]; Inter-American Institute for Global Change Research (IAI) - US National Science Foundation [CRN 3070, GEO-0452325]; Directorate For Geosciences; ICER [1128040] Funding Source: National Science Foundation	INIDEP; Fundacion Antorchas; CONICET(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Inter-American Institute for Global Change Research (IAI) - US National Science Foundation; Directorate For Geosciences; ICER(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This work was facilitated by the contribution of many colleagues who provided us instruments, help on board, unpublished data, but mostly useful advices. Among them we wish to thank: A. Bianchi, A. Callone, E. Cozzolino, V. Lutz and A. Piola. We are also grateful to M.D. Makey for providing the computer program CHEMTAX. We are thankful for the constructive criticism of two anonymous reviewers, which greatly improved the manuscript. This work was financed by INIDEP and grants from: "Fundacion Antorchas" (Grant 13900-13), PNUDARG02/018) (BB23 and BB33), CONICET PIP-112-201101-00892, and the Inter-American Institute for Global Change Research (IAI) CRN 3070 sponsored by the US National Science Foundation Grant GEO-0452325. This is INIDEP contribution No 1983.	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Oceanogr.	AUG	2016	146						1	21		10.1016/j.pocean.2016.05.002	http://dx.doi.org/10.1016/j.pocean.2016.05.002			21	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	DU6RH		Bronze, Green Published			2025-03-11	WOS:000382341800001
J	Okeke, KK; Umeji, OP				Okeke, Kingsley K.; Umeji, Obianuju P.			Palynostratigraphy, palynofacies and palaeoenvironment of deposition of Selandian to Aquitanian sediments, southeastern Nigeria	JOURNAL OF AFRICAN EARTH SCIENCES			English	Review						Palynostratigraphy; Palynofacies; Palaeoenvironment; Dinoflagellate association	PALEOCENE THERMAL MAXIMUM; PALYNOLOGY; STRATIGRAPHY; BASIN	Investigation of outcrop sections along the Onitsha-Awka transect in the Niger Delta Basin southeastern Nigeria was undertaken to assess the palynological composition, palynofacies and palaeoenvironment of deposition. Stratigraphic ranges of palynomorphs suggest an age of Selandian to Aquitanian. The palynological composition is marked by abundance of dinoflagellate cysts in the Imo Formation (Selandian to Thanetian), dominance of spores and pollen over dinoflagellate cysts in the Nanka Formation (Ypresian to Bartonian), and overwhelming amounts of spore and pollen in the Ogwashi Formation (Pariabonian to Aquitanian). Palynofacies content shows dominance of structureless organic matter in the Imo Formation, few phytoclasts in the Nanka Formation and maximum phytoclast amounts in the Ogwashi Formation. Thanetian to Ypresian boundary was marked by the mixing of older Palaeocene and younger Eocene microfossils, decrease of microflora towards the end of Palaeocene and the evolution of abundant and more diverse Eocene taxa. The Imo Formation was deposited in middle to outer neritic zone based on abundance of gonyaulacacean cysts. However, peridiniacean and terrestrial microflora extend the deposition range to shallow waters of inner neritic and coastal zone. Increase in diversity and abundance of terrestrial palynomorphs over marine palynomorphs assemblages in the overlying Nanka Formation suggest deposition under alternating coastal and inner neritic conditions while the Ogwashi Formation records oscillating coastal plain and brackish water depositional conditions. The palaeoenvironments illustrate that general retrogradation was followed by progradation of the delta during the Cenozoic. (C) 2016 Elsevier Ltd. All rights reserved.	[Okeke, Kingsley K.; Umeji, Obianuju P.] Univ Nigeria, Dept Geol, Nsukka, Nigeria	University of Nigeria	Okeke, KK (通讯作者)，Univ Nigeria, Dept Geol, Nsukka, Nigeria.	okekekingsleyk@gmail.com; obianuju.umeji@unn.edu.ng						Adediran S. 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J	Juliao-Lemus, T; Carvalho, MD; Torres, D; Plata, A; Parra, C				Juliao-Lemus, Tatiana; Carvalho, Marcelo de Araujo; Torres, Diego; Plata, Angelo; Parra, Carlos			Paleoenvironmental reconstruction based on palynofacies analyses of the Cansona Formation (Late Cretaceous), Sinu-San Jacinto Basin, northwest Colombia	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Sedimentary organic matter; Santonian (?)-Maastrichtian; Northern South America; Continental-marine trends	ORGANIC-MATTER; CARBONATES; SEDIMENTS; STRATA; FACIES	To reconstruct the paleoenvironments of the Cansona Formation, a Cretaceous succession in Colombia that has controversial paleoenvironmental interpretation, occasionally deep marine and occasionally shallow marine, palynofacies analyses were conducted on 93 samples from four sections of the Sinu San Jacinto Basin in the north, midwest, and southwest sectors. For the palynofacies analyses, the kerogen categories were counted and subjected to cluster analyses. Four palynofacies associations were revealed for the four sections: Palynofacies Association I (PA I), which consisted of microforaminiferal linings, scolecodonts, dinoflagellate cysts, pollen grains, and fungi hyphae; PA II, which consisted of phytoclast translucent non-biostructured and biostructured, opaque phytoclasts (equidimensional and lath shaped); PA III, which consisted of pseudoamorphous particles, cuticles, resin, and fungal spores; and PA IV, which consisted of fluorescent and non-fluorescent amorphous organic matter and the fresh-water algae Botryococcus. In contrast to early studies that suggested a generalization of the depositional environment for the Cansona Formation (deep or shallow conditions), this study suggests that the formation reflects conspicuous stratigraphic and lateral changes and hence different depositional environments. The Cerro Cansona (CC4 section) and Chalan (AP section) areas are a more marine proximal settings (Early Campanian-Maastrichtian), and there is an intermediate setting for the Lorica area (SC section) and deeper conditions for the Monteria area (CP2 section). (C) 2016 Elsevier Ltd. All rights reserved.	[Juliao-Lemus, Tatiana] ECOPETROL ICP, Km 7 Via Piedecuesta, Santander, Colombia; [Carvalho, Marcelo de Araujo] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Lab Paleoecol Vegetal, Quinta Boa Vista S-N, BR-20940040 Sao Cristovao, RJ, Brazil; [Torres, Diego; Plata, Angelo; Parra, Carlos] EOS DTH Ltda, Santander, Colombia	Ecopetrol; Universidade Federal do Rio de Janeiro	Juliao-Lemus, T (通讯作者)，ECOPETROL ICP, Km 7 Via Piedecuesta, Santander, Colombia.	tatiana.juliao@ecopetrol.com.co	Carvalho, Marcelo/G-8463-2015	Plata-Torres, Angelo/0000-0001-8509-0567	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]; 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])(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq](Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the anonymous reviewer for their helpful comments and suggestions. This study was conducted at the Colombian Institute of Research (ICP)/ECOPETROL. We would like to express our thanks to ECOPETROL for giving us the opportunity to study the samples. We thank the geologist Freddy Nino for his belief in us and support during this study. MC thanks 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 and the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq] grant no. 302064/2010-9.	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South Am. Earth Sci.	AUG	2016	69						103	118		10.1016/j.jsames.2016.03.009	http://dx.doi.org/10.1016/j.jsames.2016.03.009			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DP3XU					2025-03-11	WOS:000378430200007
J	Zimmerman, KCK; Levitis, DA; Pringle, A				Zimmerman, K. C. K.; Levitis, D. A.; Pringle, A.			Beyond animals and plants: dynamic maternal effects in the fungus <i>Neurospora crassa</i>	JOURNAL OF EVOLUTIONARY BIOLOGY			English	Article						anisogamy; crossing distance; development; fungi; maternal effects; microbes; Neurospora crassa; population genetics; quantitative genetics	FLOW-CYTOMETRY DATA; REPRODUCTIVE ISOLATION; SPECIES RECOGNITION; MODEL EUKARYOTE; INHERITANCE; ADAPTATION; EVOLUTION; ORGANIZATION; POPULATIONS; METABOLISM	Maternal effects are widely documented in animals and plants, but not in fungi or other eukaryotes. A principal cause of maternal effects is asymmetrical parental investment in a zygote, creating greater maternal vs. paternal influence on offspring phenotypes. Asymmetrical investments are not limited to animals and plants, but are also prevalent in fungi and groups including apicomplexans, dinoflagellates and red algae. Evidence suggesting maternal effects among fungi is sparse and anecdotal. In an experiment designed to test for maternal effects across sexual reproduction in the model fungus Neurospora crassa, we measured offspring phenotypes from crosses of all possible pairs of 22 individuals. Crosses encompassed reciprocals of 11 mating-type 'A' and 11 mating-type 'a' wild strains. After controlling for the genetic and geographic distances between strains in any individual cross, we found strong evidence for maternal control of perithecia (sporocarp) production, as well as maternal effects on spore numbers and spore germination. However, both parents exert equal influence on the percentage of spores that are pigmented and size of pigmented spores. We propose a model linking the stage-specific presence or absence of maternal effects to cellular developmental processes: effects appear to be mediated primarily through the maternal cytoplasm, and, after spore cell walls form, maternal influence on spore development is limited. Maternal effects in fungi, thus far largely ignored, are likely to shape species' evolution and ecologies. Moreover, the association of anisogamy and maternal effects in a fungus suggests maternal effects may also influence the biology of other anisogamous eukaryotes.	[Zimmerman, K. C. K.] Harvard Univ, Dept Organism & Evolutionary Biol, Cambridge, MA 02138 USA; [Levitis, D. A.] Bates Coll, Dept Biol, Lewiston, ME 04240 USA; [Pringle, A.] Univ Wisconsin, Dept Bot, Madison, WI USA; [Pringle, A.] Univ Wisconsin, Dept Bacteriol, Madison, WI 53706 USA	Harvard University; University of Wisconsin System; University of Wisconsin Madison; University of Wisconsin System; University of Wisconsin Madison	Zimmerman, KCK (通讯作者)，Harvard Univ, Dept Organism & Evolutionary Biol, Biol Labs 2112, 16 Divinity Ave, Cambridge, MA 02138 USA.	kzimmerman@fas.harvard.edu	Pringle, Anne/ISV-5313-2023	Zimmerman, Kolea/0000-0001-6224-3364	FAS Division of Science, Research Computing Group at Harvard University; National Science Foundation [DGE0644491, DGE1144152]; Max Planck Institute for Demographic Research	FAS Division of Science, Research Computing Group at Harvard University; National Science Foundation(National Science Foundation (NSF)); Max Planck Institute for Demographic Research	We thank J. Paltseva for assistance in counting perithecia, P. Rogers for assistance with flow cytometry, R. Corbett-Detig for help with genetic distance calculations, J. Taylor for clarification of SNP data and M. Lalli for critical reading of this manuscript. We are also grateful for the resources provided by the Fungal Genetics Stock Center (Manhattan, Kansas, USA). Some of the computations in this manuscript were run on the Odyssey cluster supported by the FAS Division of Science, Research Computing Group at Harvard University. Our work is supported by the National Science Foundation Graduate Research Fellowship under Grant Nos. (DGE0644491 and DGE1144152) awarded to K.Z. and by other National Science Foundation grants awarded to the Pringle Laboratory. This work was also supported by funds from the Max Planck Institute for Demographic Research to K.Z., D.L. and A.P.	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Evol. Biol.	JUL	2016	29	7					1379	1393		10.1111/jeb.12878	http://dx.doi.org/10.1111/jeb.12878			15	Ecology; Evolutionary Biology; Genetics & Heredity	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Evolutionary Biology; Genetics & Heredity	DU8XS	27062053	Bronze, Green Submitted			2025-03-11	WOS:000382500100010
J	Klouch, KZ; Schmidt, S; Andrieux-Loyer, F; Le Gac, M; Hervio-Heath, D; Qui-Minet, ZN; Quéré, J; Bigeard, E; Guillou, L; Siano, R				Klouch, Khadidja Z.; Schmidt, Sabine; Andrieux-Loyer, Francoise; Le Gac, Mickael; Hervio-Heath, Dominique; Qui-Minet, Zujaila N.; Quere, Julien; Bigeard, Estelle; Guillou, Laure; Siano, Raffaele			Historical records from dated sediment cores reveal the multidecadal dynamic of the toxic dinoflagellate <i>Alexandrium minutum</i> in the Bay of Brest (France)	FEMS MICROBIOLOGY ECOLOGY			English	Article						paleoecology; ancient DNA; real-time PCR; harmful algal blooms (HAB); dinoflagellates; coastal ecology	REAL-TIME PCR; SEA-SURFACE CONDITIONS; HARMFUL ALGAL BLOOMS; ANCIENT DNA; BLACK-SEA; EXTRACELLULAR DNA; HOLOCENE CLIMATE; TEMPORAL TRENDS; RESTING STAGES; CYSTS	The multiannual dynamic of the cyst-forming and toxic marine dinoflagellate Alexandrium minutum was studied over a time scale of about 150 years by a paleoecological approach based on ancient DNA (aDNA) quantification and cyst revivification data obtained from two dated sediment cores of the Bay of Brest (Brittany, France). The first genetic traces of the species presence in the study area dated back to 1873 +/- 6. Specific aDNA could be quantified by a newly developed real-time PCR assay in the upper core layers, in which the germination of the species (in up to 17-19-year-old sediments) was also obtained. In both cores studied, our quantitative paleogenetic data showed a statistically significant increasing trend in the abundance of A. minutum ITS1 rDNA copies over time, corroborating three decades of local plankton data that have documented an increasing trend in the species cell abundance. By comparison, paleogenetic data of the dinoflagellate Scrippsiella donghaienis did not show a coherent trend between the cores studied, supporting the hypothesis of the existence of a species-specific dynamic of A. minutum in the study area. This work contributes to the development of paleoecological research, further showing its potential for biogeographical, ecological and evolutionary studies on marine microbes.	[Klouch, Khadidja Z.; Andrieux-Loyer, Francoise; Le Gac, Mickael; Qui-Minet, Zujaila N.; Quere, Julien; Siano, Raffaele] IFREMER, Ctr Brest, DYNECO PELAGOS, BP 70 ZI Pointe Diable, F-29280 Plouzane, France; [Klouch, Khadidja Z.; Bigeard, Estelle; Guillou, Laure] Univ Paris 06, Sorbonne Univ, CNRS, Equipe DIPO,Stn Biol Roscoff,Adaptat & Divers Mil, Pl Georges Teissier,CS90074, F-29688 Roscoff, France; [Schmidt, Sabine] Univ Bordeaux, EPOC UMR5805, F-33605 Pessac, France; [Hervio-Heath, Dominique] IFREMER, RBE, SG2M, Lab Sante Environm & Microbiol, F-29280 Plouzane, France	Ifremer; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Ifremer	Siano, R (通讯作者)，IFREMER, Ctr Brest, DYNECO PELAGOS, BP 70 ZI Pointe Diable, F-29280 Plouzane, France.	raffaele.siano@ifremer.fr	; Schmidt, Sabine/G-1193-2013	Guillou, Laure/0000-0003-1032-7958; Bigeard, Estelle/0000-0003-2256-8986; Schmidt, Sabine/0000-0002-5985-9747; Le Gac, Mickael/0000-0001-6451-5781; Qui Minet, Zujaila Nohemy/0000-0001-6002-5240; HERVIO HEATH, Dominique/0000-0001-7487-6361; ANDRIEUX-LOYER, Francoise/0000-0001-6433-012X	VEHSPA; KYNDER; 'Laboratoire d'Excellence' LabexMER (Agence Nationale de la Recherche (ANR)) [10-LABX-19]; French government under the program 'Investissements d'Avenir'; initiative ECosphere Continentale et COtiere (EC2CO) of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): PALMITO; initiative ECosphere Continentale et COtiere (EC2CO) of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): CA'MOMI; ANR HAPAR [20142019]	VEHSPA; KYNDER; 'Laboratoire d'Excellence' LabexMER (Agence Nationale de la Recherche (ANR))(Agence Nationale de la Recherche (ANR)); French government under the program 'Investissements d'Avenir'(Agence Nationale de la Recherche (ANR)); initiative ECosphere Continentale et COtiere (EC2CO) of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): PALMITO; initiative ECosphere Continentale et COtiere (EC2CO) of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): CA'MOMI; ANR HAPAR(Agence Nationale de la Recherche (ANR))	This work was financed by the exploratory projects VEHSPA (2012-2013) and KYNDER (2014-2015), supported by the 'Laboratoire d'Excellence' LabexMER (Agence Nationale de la Recherche (ANR) - 10-LABX-19) and co-funded by the French government under the program 'Investissements d'Avenir', by the projects of the initiative ECosphere Continentale et COtiere (EC2CO) of the Institut National des Sciences de l'Univers/Centre National de la Recherche Scientifique (INSU/CNRS): PALMITO (2013-2015) and CA'MOMI (2015-2017), and the ANR HAPAR project (20142019). This research was carried out within the framework of K. Klouch's PhD and funded by Ifremer and Region Bretagne (Allocation de REcherche Doctorale (ARED) fellowship).	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Ecol.	JUL	2016	92	7							fiw101	10.1093/femsec/fiw101	http://dx.doi.org/10.1093/femsec/fiw101			16	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	DR1VT	27162179	Green Published, Bronze			2025-03-11	WOS:000379693700012
J	Trigal, C; Ruete, A				Trigal, Cristina; Ruete, Alejandro			Asynchronous changes in abundance over large scales are explained by demographic variation rather than environmental stochasticity in an invasive flagellate	JOURNAL OF ECOLOGY			English	Article						aquatic plant ecology; biogeography; climate; demographic stochasticity; environmental stochasticity; Gonyostomum semen; invasive species; lakes; microalgae	GONYOSTOMUM-SEMEN RAPHIDOPHYCEAE; EARLY-WARNING SIGNALS; BLOOM FORMATION; CYLINDROSPERMOPSIS-RACIBORSKII; DIDYMOSPHENIA-GEMINATA; DINOFLAGELLATE CYSTS; GONYAULAX-TAMARENSIS; BOREAL LAKES; RESPONSES; DYNAMICS	Environmental stochasticity is important in explaining the persistence and establishment of invasive species, but the simultaneous effects of environmental and demographic factors are difficult to separate. Understanding how demography and environmental factors affect invasive species abundance over large temporal and spatial scales is essential to anticipate populations at risk of becoming established and setting appropriate management measures. Using a hierarchical mixed modelling approach, we analysed the spatial and interannual dynamics of the invasive raphidophyte Gonyostomum semen, a noxious flagellate which is spreading in northern Europe, in response to demographic and environmental variation. We used data from 76 lakes distributed across two biogeographical regions in Sweden (Central Plains in the south and Fennoscandian region in the north) and sampled during 14years. We found a strong asynchrony in the density dynamics of G. semen populations between the two regions. G. semen showed positive trends (i.e. increasing frequency of high density peaks) in most southern lakes, forming established populations with recurrent blooms in successive years in some of them. In contrast, G. semen populations were smaller and more stochastic in the north.G. semen previous year's abundance, a proxy for cyst production and recruitment, had a strong control on the dynamics, likely contributing to the stability of high density populations in southern lakes. Conversely, the effects of climate and habitat were weaker and their influence varied across regions. Temperature was the limiting factor in the north whereas local habitat was more important in the south.Synthesis. A full understanding of the mechanisms driving abundance changes across large scales can only be gained if endogenous and environmental factors are analysed together. For phytoplankton species, and specially, noxious microalgae, this implies that proxies for cyst production and recruitment, which are the inoculum for next year population, should be included in e.g. distribution, bloom formation and climate models, as these may modify establishment and population response to environmental variation. Asynchronous changes in abundance across regions also indicate that management plans should be developed for small regions, as inference at a large scale may obscure the mechanisms driving local population changes.	[Trigal, Cristina] Swedish Univ Agr Sci SLU, Swedish Species Informat Ctr, PO 7007, SE-75007 Uppsala, Sweden; [Ruete, Alejandro] Swedish Univ Agr Sci SLU, Dept Ecol, PO 7044, SE-75007 Uppsala, Sweden	Swedish University of Agricultural Sciences; Swedish University of Agricultural Sciences	Trigal, C (通讯作者)，Swedish Univ Agr Sci SLU, Swedish Species Informat Ctr, PO 7007, SE-75007 Uppsala, Sweden.	cristina.trigal@slu.se	Ruete, Alejandro/E-6024-2010					Acosta F, 2015, P NATL ACAD SCI USA, V112, P11594, DOI 10.1073/pnas.1505204112; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Angeler DG, 2013, HARMFUL ALGAE, V23, P60, DOI 10.1016/j.hal.2013.01.001; [Anonymous], 2011, Data Analysis Using Regression and Multilevel/Hierarchical Models; [Anonymous], RIKSINVENTERING 2000; [Anonymous], METHODS QUANTITATI 1; [Anonymous], 2012, JAGS PROGRAM ANAL BA; BERDALET E, 1993, DEV MAR BIO, V3, P737; Bernard C, 2003, ENVIRON TOXICOL, V18, P176, DOI 10.1002/tox.10112; Drake JM, 2010, NATURE, V467, P456, DOI 10.1038/nature09389; Ellison AM, 2004, ECOL LETT, V7, P509, DOI 10.1111/j.1461-0248.2004.00603.x; Falconer IR, 2006, ENVIRON TOXICOL, V21, P299, DOI 10.1002/tox.20194; 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; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; Gelman Andrew., 2007, Bayesian Data Analysis, V3rd; Genovesi B, 2009, J PLANKTON RES, V31, P1209, DOI 10.1093/plankt/fbp066; Hagman CHC, 2015, HYDROBIOLOGIA, V744, P1, DOI 10.1007/s10750-014-2050-y; Hansson LA, 2000, ECOLOGY, V81, P842, DOI 10.1890/0012-9658(2000)081[0842:SEOFCD]2.0.CO;2; Hobbs RJ, 2009, TRENDS ECOL EVOL, V24, P599, DOI 10.1016/j.tree.2009.05.012; HONGVE D, 1988, PROC INT ASSOC THE 1, V23, P430; Illies J., 1978, LIMNOFAUNA EUROPAEA; Figueroa RI, 2011, J PHYCOL, V47, P13, DOI 10.1111/j.1529-8817.2010.00937.x; Johansson KSL, 2013, AQUAT SCI, V75, P447, DOI 10.1007/s00027-013-0291-x; Jones R. 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Ecol.	JUL	2016	104	4					947	956		10.1111/1365-2745.12576	http://dx.doi.org/10.1111/1365-2745.12576			10	Plant Sciences; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Environmental Sciences & Ecology	DQ2ES		Bronze			2025-03-11	WOS:000379015400006
J	Rubino, F; Cibic, T; Belmonte, M; Rogelja, M				Rubino, F.; Cibic, T.; Belmonte, M.; Rogelja, M.			Microbenthic community structure and trophic status of sediments in the Mar Piccolo of Taranto (Mediterranean, Ionian Sea)	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Microphytobenthos; Plankton; Resting stages; Benthic primary production; Benthic respiration; Confined marine basin; Ionian sea	MICROPHYTOBENTHIC PRIMARY PRODUCTION; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; RESTING STAGES; SUBLITTORAL SEDIMENTS; GULF; BAY; PHYTOPLANKTON; PLANKTON; BIODIVERSITY	This study aimed to assess the benthic ecosystem trophic status in a heavily polluted marine area and the response of the microbenthic community to multiple and diffuse anthropogenic impacts, integrating information coming from the active and resting (plankton's cysts) components of microbenthos. Two sampling campaigns were carried out in the period 2013-2014 and four sampling sites at different levels of industrial contamination were chosen within the first and second inlet of the Mar Piccolo of Taranto. The chemical contamination affected to a higher extent the active microbenthos than the resting one. In the central part of the first inlet, characterised by more marine features, thrives a very rich and biodiverse microbenthic community. In contrast, at the polluted site near the military navy arsenal, extremely low densities (9576 +/- 1732 cells cm(-3)) were observed for active microbenthos, but not for the resting community. Here, the high level of contamination selected for tychopelagic diatom species, i.e., thriving just above the surface sediments, while the other life forms died or moved away. Following the adoption of a 10 mu m mesh, for the first time, resting spores produced by small diatoms of the genus Chaetoceros were found. Our results further indicate that although the Mar Piccolo is very shallow, the benthic system is scarcely productive, likely as a consequence of the accumulated contaminants in the surface sediments that probably interfere with the proper functioning of the benthic ecosystem.	[Rubino, F.; Belmonte, M.] UOS Talassog A Cerruti, CNR Inst Coastal Marine Environm, Taranto, Italy; [Cibic, T.; Rogelja, M.] OGS Ist Nazl Oceanog & Geofis Sperimentale, Trieste, Italy	Istituto Nazionale di Oceanografia e di Geofisica Sperimentale	Rubino, F (通讯作者)，UOS Talassog A Cerruti, CNR Inst Coastal Marine Environm, Taranto, Italy.	rubino@iamc.cnr.it	Belmonte, Marisol/AAG-9759-2019; Rubino, Fernando/GOP-0332-2022	Rubino, Fernando/0000-0003-2552-2510; Cibic, Tamara/0000-0003-1519-4891	Ministry for Education, University and Research within the National Research Programme	Ministry for Education, University and Research within the National Research Programme(Ministry of Education, Universities and Research (MIUR))	The activities described in this publication were founded by the Project Bandiera RITMARE - La Ricerca Italiana per il Mare coordinated by the National Research Council and funded by the Ministry for Education, University and Research within the National Research Programme 2011-2013.	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Sci. Pollut. Res.	JUL	2016	23	13					12624	12644		10.1007/s11356-015-5526-z	http://dx.doi.org/10.1007/s11356-015-5526-z			21	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	DP9LI	26511257				2025-03-11	WOS:000378817300011
J	Unida, S; Patruno, S				Unida, Stefania; Patruno, Stefano			The palynostratigraphy of the Upper Maiolica, Selli Level and the Lower Marne a Fucoidi units in the proposed Barremian/Aptian (Lower Cretaceous) GSSP stratotype at Gorgo a Cerbara, Umbria-Marche Basin, Italy	PALYNOLOGY			English	Article						Gorgo a Cerbara; Barremian/Aptian; Umbria-Marche Basin; palynostratigraphy; Selli Level; Maiolica Formation; Marne a Fucoidi Formation; Italy	DINOFLAGELLATE CYST STRATIGRAPHY; OCEANIC ANOXIC EVENT; GULF-OF-MEXICO; MAGNETIC STRATIGRAPHY; SOUTHERN ALPS; PLANKTONIC-FORAMINIFERA; SEDIMENTS; TETHYS; NANNOFOSSILS; SWITZERLAND	The section of Gorgo a Cerbara in Italy has been proposed as the Global Stratotype Section and Point (GSSP) for the Barremian/Aptian boundary (Lower Cretaceous). This section displays the transition between the white pelagic limestones of the Maiolica Formation (Tithonian-lowermost Aptian) and the polychrome marls of the Marne a Fucoidi Formation (Aptian-Albian). The Oceanic Anoxic Event 1a (OAE 1a) anoxic horizon (Selli Level) is located in the latter formation. Here, we report for the first time a palynostratigraphical assessment of this key section, with a very high resolution in the Selli Level. Palynomorph groups recorded include acritarchs, microforaminiferal test linings, 58 dinoflagellate cysts, 44 sporomorph taxa, and freshwater fungal and algal bodies. These include such biostratigraphical markers as Rhynchodiniopsis aptiana and Odontochitina operculata among the dinoflagellate cysts and Afropollis cf. jardinus among sporomorphs. Biostratigraphical events recognised allow comparisons with previously studied successions in other similar areas (e.g. Cismon apticore in the Southern Alps, Italy). The distribution of taxa recorded in the Gorgo a Cerbara section is generally consistent with published data, but several differences between the assemblages recorded in the Cismon apticore and in this study were noted. The best global markers for the Barremian/Aptian boundary are represented by the disappearance of R. aptiana and by the appearance of O. operculata, but in this section these occurred 0.65-1.35 Myr after the magnetostratigraphically defined boundary, within the Selli Level. The angiosperm pollen A. cf. jardinus is recorded only within the Selli Level (from 1.4 to 1.6 Myr after the Barremian/Aptian boundary), consistent with an Early Aptian age. A cluster of 10 extremely short-ranging dinoflagellate cyst excursion taxa appear in this section coincident with the Nannoconid Crisis event and its associated thermal peak, ca. 10-20 kyr before the onset of the OAE 1a. Several short-ranging Pteridophyta spore species are found only within the Selli Level itself.	[Unida, Stefania] RPS Energy, Goldvale House,27-41 Church St West, Woking GU21 6DH, Surrey, England; [Patruno, Stefano] Petr Geoserv, 4 Hts, Weybridge KT13 0NY, Surrey, England		Unida, S (通讯作者)，RPS Energy, Goldvale House,27-41 Church St West, Woking GU21 6DH, Surrey, England.	unidas@rpsgroup.com	Patruno, Stefano/ABA-2908-2020; Patruno, Stefano/G-7260-2017	Patruno, Stefano/0000-0002-6375-995X				ALVAREZ W, 1977, GEOL SOC AM BULL, V88, P383, DOI 10.1130/0016-7606(1977)88<383:UCMSAG>2.0.CO;2; Alvarez W., 1989, B SOC GEOL ITAL, V108, P3; [Anonymous], 1989, MEM DESCR CARTA GEOL; ARTHUR MA, 1990, NATO ADV SCI I C-MAT, V304, P75; Batten D.J., 1984, FOSSILS CLIMATE, P127; Batten D.J., 1979, INIT REPS DSDP, V48, P579; BRALOWER TJ, 1989, MAR MICROPALEONTOL, V14, P153, DOI 10.1016/0377-8398(89)90035-2; Brenner G.J., 1976, ORIGIN EARLY EVOLUTI, P23; CECCA F, 1994, CRETACEOUS RES, V15, P457, DOI 10.1006/cres.1994.1027; Cecca F., 1989, MEMORIE DESCRITTIVE, VXXXIX, P118; CHANNELL JET, 1995, EARTH PLANET SC LETT, V134, P125, DOI 10.1016/0012-821X(95)00111-O; Channell JET, 2000, GEOL SOC AM BULL, V112, P1430, DOI 10.1130/0016-7606(2000)112<1430:ECMSIT>2.0.CO;2; Coccioni R, 1989, 262 IGCP U URB, P16; Coccioni R., 1987, BOLLETTINO SOCIET GE, V106, P183; Coccioni R., 1992, CRETACEOUS RES, V13, P457; Coccioni R., 1989, ATT 2 CONV INT FOSS, P163; Coccioni R, 1989, CRETACEOUS W TETHYS, P563; DAVIES E H, 1985, Palynology, V9, P105; Doyle J.A., 1982, B CENT RECH EXPL, V6, P39; Doyle JA, 1999, PALAEOECO A, V26, P3; DOYLE JA, 1990, AM J BOT, V77, P1544, DOI 10.2307/2444487; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; ERBA E, 1994, PALEOCEANOGRAPHY, V9, P483, DOI 10.1029/94PA00258; Erba Elisabetta, 1996, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V66, P31; Erba E, 2010, SCIENCE, V329, P428, DOI 10.1126/science.1188886; Evitt W.R., 1967, Stanford University Publications, Geological Sciences, V10, P1; Evitt W.R., 1985, Sporopollenin dinoflagellate cysts: their morphology and interpretation, P333; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Fiet N, 2000, B SOC GEOL FR, V171, P103; Fiet N., 1998, THESIS, P283; Gradstein F., 2012, GEOLOGIC TIME SCALE, P1176, DOI DOI 10.1016/B978-0-444-59425-9.00005-6; Gradstein F.M., 2004, A Geologic Time Scale; HARDING I C, 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P1; HARKER SD, 1975, REV PALAEOBOT PALYNO, V20, P217, DOI 10.1016/0034-6667(75)90013-5; Heimhofer U, 2008, INT J EARTH SCI, V97, P785, DOI 10.1007/s00531-007-0186-y; Herbert T.D., 1995, Geochronology, Time Scales, and Global Stratigraphic Correlation: SEPM Special Publication, v, V54, P81; HERNGREEN G F W, 1981, Pollen et Spores, V23, P441; HOCHULI PA, 1981, REV PALAEOBOT PALYNO, V35, P337, DOI 10.1016/0034-6667(81)90116-0; Jenkyns HC, 2003, PHILOS T R SOC A, V361, P1885, DOI 10.1098/rsta.2003.1240; Keller CE, 2011, PALAEOGEOGR PALAEOCL, V305, P43, DOI 10.1016/j.palaeo.2011.02.011; Kelly DC, 1996, GEOLOGY, V24, P423; Koppelhus Eva B., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P777; Leereveld H, 1997, CRETACEOUS RES, V18, P385, DOI 10.1006/cres.1997.0070; Leereveld H., 1995, THESIS, VN2; Londeix L, 1996, REV PALAEOBOT PALYNO, V92, P367, DOI 10.1016/0034-6667(95)00097-6; LOWRIE W, 1984, EARTH PLANET SC LETT, V71, P315, DOI 10.1016/0012-821X(84)90096-7; Malinverno A, 2010, PALEOCEANOGRAPHY, V25, DOI 10.1029/2009PA001769; Malinverno A, 2012, J GEOPHYS RES SOLID, V117, pB6; Menegatti AP, 1998, PALEOCEANOGRAPHY, V13, P530, DOI 10.1029/98PA01793; Micarelli A., 1977, Studi Geologici Camerti, V3, P57; MILLIOUD ME, 1975, AM ASS STRATIGRAPHIC, V4, P65; Muller J., 1987, CONTRIBUTIONS SERIES, V19, P7; Orlansky R., 1971, UTAH GEOLOGICAL MINE, V89, P1; Patruno S., 2008, THESIS; Patruno S, 2015, PALAEOGEOGR PALAEOCL, V424, P147, DOI 10.1016/j.palaeo.2015.01.031; Patruno S, 2011, GRZYB FOUND SPEC PUB, V16, P191; Powell AJ, 1992, BRIT MICROPALAEONTOL, P7; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; Reneville P. 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J	Rembauville, M; Blain, S; Caparros, J; Salter, I				Rembauville, M.; Blain, S.; Caparros, J.; Salter, I.			Particulate matter stoichiometry driven by microplankton community structure in summer in the Indian sector of the Southern Ocean	LIMNOLOGY AND OCEANOGRAPHY			English	Article							NATURAL IRON-FERTILIZATION; SUBSURFACE CHLOROPHYLL MAXIMUM; ORGANIC-CARBON FLUX; PHYTOPLANKTON BLOOM; ELEMENTAL STOICHIOMETRY; MARINE-PHYTOPLANKTON; CROZET BASIN; FRONTAL ZONE; INTERANNUAL VARIABILITY; LIGHT INTERACTIONS	Microplankton community structure and particulate matter stoichiometry were investigated in a late summer survey across the Subantarctic and Polar Front in the Indian sector of the Southern Ocean. Microplankton community structure exerted a first order control on PON:POP stoichiometry with diatom-dominated samples exhibiting much lower ratios (4-6) than dinoflagellate and ciliate-dominated samples (10-21). A significant fraction of the total chlorophyll a (30-70%) was located beneath the euphotic zone and mixed layer and sub-surface chlorophyll features were associated to transition layers. Although micro-plankton community structure and biomass was similar between mixed and transition layers, the latter was characterized by elevated Chl:POC ratios indicating photoacclimation of mixed layer communities. Empty diatom frustules, in particular of Fragilariopsis kerguelensis and Pseudo-nitzschia, were found to accumulate in the Antarctic Zone transition layer and were associated to elevated BSi:POC ratios. Furthermore, high Si(OH) 4 diffusive fluxes (>1 mmol m(2) d(-1)) into the transition layer appeared likely to sustain silicification. We suggest transition layers as key areas of C and Si decoupling through (1) physiological constraints on carbon and silicon fixation (2) as active foraging sites for grazers that preferentially remineralize carbon. On the Kerguelen Plateau, the dominant contribution of Chaetoceros Hyalochaete resting spores to microplankton biomass resulted in a three-fold enhancement of POC concentration at 250 m, compared to other stations. These findings further highlight the importance of diatom resting spores as a significant vector of carbon export through the intense remineralization horizons characteristing Southern Ocean ecosystems.	[Rembauville, M.; Blain, S.; Caparros, J.; Salter, I.] UPMC Univ Paris 06, Sorbonne Univ, CNRS, Lab Oceanog Microbienne LOMIC,Observ Oceanol, Banyuls Sur Mer, France; [Salter, I.] Alfred Wegener Inst, Helmholtz Ctr Polar & Marine Res, Bremerhaven, Germany	Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Rembauville, M (通讯作者)，UPMC Univ Paris 06, Sorbonne Univ, CNRS, Lab Oceanog Microbienne LOMIC,Observ Oceanol, Banyuls Sur Mer, France.	rembauville@obs-banyuls.fr	Rembauville, Mathieu/LSK-7045-2024; Salter, Ian/AAI-1015-2021; blain, stephane/F-6917-2010	blain, stephane/0000-0002-5234-2446; Rembauville, Mathieu/0000-0003-0850-8565; Salter, Ian/0000-0002-4513-0314	French research program of INSU-CNRS LEFE-CYBER (EXPLAIN); French ANR (KEOPS2) [ANR-10-BLAN-0614]; French institute INSU; French institute IPEV; French program SOERE/Great-gases; European program FP7/Carbochange	French research program of INSU-CNRS LEFE-CYBER (EXPLAIN); French ANR (KEOPS2)(Agence Nationale de la Recherche (ANR)); French institute INSU; French institute IPEV; French program SOERE/Great-gases; European program FP7/Carbochange	We thank the captain Bernard Lassiette and crew of the R/V Marion Dufresne for their support aboard as well as the chief scientist Yves Cherel. We thank Claire Lo Monaco and Celine Ridame for the access to the CTD and chlorophyll a data and Isabelle Durand for the help in the Thorpe displacement calculation. We thank the three anonymous reviewers for their constructive comments, which helped us to improve the manuscript. This work was supported by grants from the French research program of INSU-CNRS LEFE-CYBER (EXPLAIN, Ian Salter) and the French ANR (KEOPS2, ANR-10-BLAN-0614, Stephane Blain). The OISO program is supported by the French institutes INSU and IPEV, the French program SOERE/Great-gases, and the European program FP7/Carbochange.	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J	Zhao, XQ; Dupont, L; Meadows, ME; Wefer, G				Zhao, Xueqin; Dupont, Lydie; Meadows, Michael E.; Wefer, Gerold			Pollen distribution in the marine surface sediments of the mudbelt along the west coast of South Africa	QUATERNARY INTERNATIONAL			English	Article						Pollen distribution; Pollen transport; Marine surface sediments; West coast of South Africa	WALLED DINOFLAGELLATE CYSTS; FECAL DEPOSITS HYRACEUM; VEGETATION HISTORY; ORGANIC-MATTER; CLIMATE-CHANGE; LATE HOLOCENE; ORANGE RIVER; CAPE; PRESERVATION; PALEOENVIRONMENTS	The distribution of pollen in marine surface sediments offshore of the west coast of South Africa has been investigated to aid in the interpretation of marine pollen records of onshore vegetation changes. A transect of sediment surface pollen samples retrieved from the Namaqualand mudbelt from just south of the Orange River mouth (29 degrees S) to St Helena Bay (33 degrees S) indicates distinctive pollen spectra reflecting vegetation communities on the adjacent continent. Pollen concentration increases southwards, partly in relation to greater pollen productivity due to higher biomass and density of fynbos vegetation and of sedimentary processes and low pollen concentrations consequent to dilution with silt and clay from the Orange River. The distribution of specific pollen taxa suggests that the Orange River is a major contributor of pollen to the northern mudbelt declining southwards, while the pollen distribution in the central mudbelt is largely attributable to seasonal inputs of pollen from offshore berg winds and local ephemeral Namaqualand rivers. The typical fynbos elements dominate in the southern mudbelt indicating a pollen source mainly in the fynbos vegetation types. These conclusions support a companion analysis of fossil pollen records of two marine sediment cores from the northern and southern mudbelt respectively. This study demonstrates that pollen records from marine sediment cores in the Namaqualand mudbelt have the potential to be a tool to reconstruct palaeovegetation on the adjacent continent. However, to better reconstruct the palaeoclimate of South Africa and fully understand the relations between terrestrial and marine deposits, more marine surface sediments along the western coast of South Africa as well as more terrestrial surface sediments need to be studied. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.	[Zhao, Xueqin; Dupont, Lydie; Wefer, Gerold] Univ Bremen, MARUM Ctr Marine Environm Sci, POB 330 440, D-28334 Bremen, Germany; [Meadows, Michael E.] Univ Cape Town, Dept Environm & Geog Sci, ZA-7701 Cape Town, South Africa	University of Bremen; University of Cape Town	Zhao, XQ (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, POB 330 440, D-28334 Bremen, Germany.	xzhao@marum.de; dupont@uni-bremen.de; mmeadows@mweb.co.za; gwefer@marum.de	Wefer, Gerold/S-2291-2016; Meadows, Michael/AAH-2461-2020	Wefer, Gerold/0000-0002-6803-2020; Dupont, Lydie/0000-0001-9531-6793; Zhao, Xueqin/0000-0003-3354-3768; Meadows, Michael/0000-0001-8322-3055	German Federal Ministry of Education and Research (BMBF)	German Federal Ministry of Education and Research (BMBF)(Federal Ministry of Education & Research (BMBF))	This study was funded by the German Federal Ministry of Education and Research (BMBF). The investigations were conducted within the collaborative project "Regional Archives for Intergrated Investigations" (RAiN) (03G0840A), which is embedded in the international research program SPACES (Science Partnership for the Assessment of Complex Earth System Processes). Thanks to the captain, the crew and scientists of the Meteor M57-1 cruise for recovering the studied material. We would like to thank Frank H. Neumann and an anonymous reviewer for their useful comments that have helped to improve the manuscript. We also thank Enno Schefuss for critical discussions and valuable suggestions.	[Anonymous], S AFR GEOGR J; [Anonymous], 1997, S. Afr. Geogr. 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Int.	JUN 6	2016	404		B				44	56		10.1016/j.quaint.2015.09.032	http://dx.doi.org/10.1016/j.quaint.2015.09.032			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	DM5PX					2025-03-11	WOS:000376403500005
J	Quijano-Scheggia, S; Barajas-Gonzalez, M; Lim, HC; Leaw, CP; Olivos-Ortiz, A; Gaviño-Rodriguez, J; Pérez, JB; Bates, SS				Quijano-Scheggia, Sonia; Barajas-Gonzalez, Maribel; Lim, Hong Chang; Leaw, Chui Pin; Olivos-Ortiz, Aramis; Gavino-Rodriguez, Juan; Blanco Perez, Juan; Bates, Stephen S.			The inhibitory effect of a non-yessotoxin-producing dinoflagellate, <i>Lingulodinium polyedrum</i> (Stein) Dodge, towards <i>Vibrio vulnificus</i> and <i>Staphylococcus aureus</i>	REVISTA DE BIOLOGIA TROPICAL			English	Article							RNA SECONDARY STRUCTURE; GULF-OF-CALIFORNIA; SEQUENCE ALIGNMENT; BAHIA CONCEPCION; CYST PRODUCTION; DATABASE; ANTIBACTERIAL; RETICULATUM; VARIABILITY; RESISTANCE	The increased bacterial resistance to antibiotics has caused global concern, prompting the search for new compounds. Because of their abundance and diversity, marine phytoplankton are an important potential source of such compounds. Research on dinoflagellates has led to the discovery of inhibitors of bacterial growth. The marine dinoflagellate Lingulodinium polyedrum blooms in different regions of the world, including Mexico, and is also known to regulate the growth of other species in coastal waters. Here, we investigated the taxonomy of this dinoflagellate and characterized the ability of its extracts to inhibit the growth of two bacteria of medical importance (Vibrio vulnificus and Staphylococcus aureus). Taxonomic characterization was performed by PCR and gene amplification of ITS, and confirmed that the species isolated off the Pacific coast of Mexico was L. polyedrum. To prove the inhibitory effect of L. polyedrum extracts, cultures were harvested by centrifugation. Pellets from three cellular abundances were extracted with water, methanol, hexane and chloroform. The experiments on V. vulnificus showed a high growth inhibition for the four extracts, ranging from 77 to 98 %. Surprisingly, the growth inhibition was lower when the extracts originated from a higher L. polyedrum cell abundance, ranging from 0 to 34 %. For S. aureus, the growth inhibition was also high, but not statistically different for all extracts and cell abundances, ranging from 62 to 99 %. This study obtained promising results for future pharmacological applications. Our Mexican strain of L. polyedrum did not produce any detectable yessotoxins.	[Quijano-Scheggia, Sonia; Barajas-Gonzalez, Maribel; Olivos-Ortiz, Aramis; Gavino-Rodriguez, Juan] Univ Colima, Ctr Univ Invest Oceanol, Carretera Manzanillo Barra Navidad Km 19-5, Manzanillo 28860, Colima, Mexico; [Lim, Hong Chang; Leaw, Chui Pin] Univ Malaya, Inst Ocean & Earth Sci, Bachok Marine Res Stn, Bachok 16310, Kelantan, Malaysia; [Blanco Perez, Juan] Ctr Invest Marinas, Pedras Coron S-N,Apdo 13, Vilanova De Arousa 36620, Spain; [Bates, Stephen S.] Fisheries & Oceans Canada, Gulf Fisheries Ctr, POB 5030, Moncton, NB E1C 9B6, Canada	Universidad de Colima; Universiti Malaya; Fisheries & Oceans Canada	Quijano-Scheggia, S (通讯作者)，Univ Colima, Ctr Univ Invest Oceanol, Carretera Manzanillo Barra Navidad Km 19-5, Manzanillo 28860, Colima, Mexico.	quijanosonia@gmail.com; maribel_barajas@ucol.mx; hclim24@gmail.com; chuipinleaw@gmail.com; aolivos@ucol.mx; gavinho@ucol.mx; juan.carlos.blanco.perez@xunta.es; stephen.bates@dfo-mpo.gc.ca	Leaw, Chui Pin/F-5220-2012; Lim, Hong/J-8761-2012	Olivos-Ortiz, Aramis/0000-0002-9886-9817; Quijano, Sonia/0000-0003-1499-8337; Lim, Hong Chang/0000-0003-0013-7819	University of Colima; Terminal KMS de GNL, S. de R.L. de C.V.	University of Colima; Terminal KMS de GNL, S. de R.L. de C.V.	We thank the University of Colima and Terminal KMS de GNL, S. de R.L. de C.V. for the funding provided for this research, Maria Rivera-Vilarelle for her onsite effort and invaluable lab work, and the Centro de Investigacion en Alimentacion y Desarrollo (Mazatlan, Sinaloa, Mexico) for providing the Vibrio vulnificus strain.	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Biol. Trop.	JUN	2016	64	2					805	816						12	Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics	DW2IT	29451969	Green Submitted, gold			2025-03-11	WOS:000383466800027
J	Clowes, CD; Hannah, MJ; Wilson, GJ; Wrenn, JH				Clowes, Christopher D.; Hannah, Michael J.; Wilson, Graeme J.; Wrenn, John H.			Marine palynostratigraphy and new species from the Cape Roberts drill-holes, Victoria land basin, Antarctica	MARINE MICROPALEONTOLOGY			English	Article						Acritarchs; Dinoflagellates; Cymatiosphaera; Lejeunecysta; New species; Biostratigraphy; Zonation; Cape Roberts drill-holes; Oligocene; Miocene; Antarctica	ORBITALLY-INDUCED OSCILLATIONS; ROSS SEA; ICE-SHEET; OLIGOCENE; BOUNDARY	Three research wells were cored near Cape Roberts, McMurdo Sound, during the summers of 1997, 1998 and 1999. Rich marine palynomorph assemblages were obtained from the early Miocene and Oligocene sediments, and almost immediately described at a reconnaissance level by the original on-site science team. In these studies, a number of undescribed species were reported, most strikingly of the distinctive dinoflagellate cyst genus Lejeunecysta. This report continues that work with the description of six new species: ?Cymatiosphaera robertsii, Lejeunecysta acuminata, Lejeunecysta attenuata, Lejeunecysta katatonos, Lejeunecysta rotunda, and Lejeunecysta striata. A new zonation comprising five marine palynomorph biozones is proposed, largely based upon the new taxa. The taxon ranges are derived from earlier published ranges with some minor updates. (C) 2016 Elsevier B.V. All rights reserved.	[Clowes, Christopher D.; Hannah, Michael J.; Wilson, Graeme J.; Wrenn, John H.] GNS Sci, POB 30 368, Lower Hutt 5040, New Zealand	GNS Science - New Zealand	Clowes, CD (通讯作者)，GNS Sci, POB 30 368, Lower Hutt 5040, New Zealand.	c.clowes@gns.cri.nz			Past Antarctic Climates (PAC) Programme; New Zealand Ministry of Business Innovation and Employment [C05X1001]; New Zealand Ministry of Business, Innovation & Employment (MBIE) [C05X1001] Funding Source: New Zealand Ministry of Business, Innovation & Employment (MBIE)	Past Antarctic Climates (PAC) Programme; New Zealand Ministry of Business Innovation and Employment(New Zealand Ministry of Business, Innovation and Employment (MBIE)); New Zealand Ministry of Business, Innovation & Employment (MBIE)(New Zealand Ministry of Business, Innovation and Employment (MBIE))	The authors thank Ian Raine for gathering together the materials from earlier studies; Joe Prebble for providing additional study materials; Peter Bijl and Francesca Sangiorgi for useful discussions and providing an early draft of the Wilkes Land manuscript; and Philip Carthew for drafting assistance. CDC completed the paper thanks to funding provided by the Past Antarctic Climates (PAC) Programme, led by Dr. Richard Levy, whose advice and encouragement is also gratefully acknowledged. The PAC Programme is supported by the New Zealand Ministry of Business Innovation and Employment contract C05X1001 to GNS Science.	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J	Agic, H; Moczydlowska, M; Canfield, DE				Agic, Heda; Moczydlowska, Malgorzata; Canfield, Donald E.			Reproductive cyst and operculum formation in the Cambrian-Ordovician galeate-plexus microfossils	GFF			English	Article						Baltica; Dasycladales; Estonia; galeate plexus; Ordovician; palaeobiology	GREEN-ALGA ACETABULARIA; BIOLOGICAL AFFINITIES; DINOFLAGELLATE CYSTS; LUKATI FORMATION; LIFE-CYCLE; ACRITARCHS; PHYTOPLANKTON; MARINE; MICROPHYTOPLANKTON; BIODIVERSIFICATION	Unicellular organic-walled microfossils from the Cambrian-Ordovician transition in Estonia (ca. 490-480million years ago) exhibit rare characters reflecting their function as reproductive algal cysts. The studied assemblages record the evolutionary history of phytoplankton in the early Palaeozoic Era: novel morphologies appearing through the Cambrian and subsequently diversifying in the Ordovician. Well-preserved specimens were extracted following a standard palynological method and studied by light-transmitted microscopy. The galeate plexus acritarchs Caldariola, Priscogalea and Stelliferidium have revealed exceptionally preserved morphological elements and a rare structure among both fossil and extant protists - an opening with operculum (lid) in reproductive cysts, in addition to lavish vesicle ornamentation and sculpture. Analogous morphology is observed in the living dasycladalean alga Acetabularia (Chlorophyta), which possesses an intrinsic lid-forming apparatus used during the organism's reproductive stage. Based on the observations on the fossil material and studies on the Acetabularia lid formation, we propose a model of operculum formation in the galeate plexus micro-organisms. Due to strong morphological and ecological similarities between galeate fossils and dasycladalean cysts, and the antiquity of this algal order, galeates may be positioned within green algae, more specifically Dasycladales. The unique morphology of the operculum-bearing microbiota would have required a high degree of intracellular complexity for its development, suggesting that advanced intracellular machinery was present already in the early Palaeozoic phytoplankton. Additionally, the minute prasinophyte microfossil Reticella corrugata is reported for the first time in the Upper Cambrian strata.	[Agic, Heda; Moczydlowska, Malgorzata] Uppsala Univ, Dept Earth Sci, Palaeobiol, Uppsala, Sweden; [Canfield, Donald E.] Univ Southern Denmark, Inst Biol, Nord Ctr Earth Evolut NordCEE, Odense, Denmark	Uppsala University; University of Southern Denmark	Agic, H (通讯作者)，Uppsala Univ, Dept Earth Sci, Palaeobiol, Uppsala, Sweden.	heda.agic@geo.uu.se; malgo.vidal@pal.uu.se	Agic, Heda/AAQ-9641-2021; Canfield, Don/C-1735-2012	Canfield, Don/0000-0001-7602-8366; Agic, Heda/0000-0002-4002-4141	Swedish Research Council (Vetenskapsradet, VR) [621-2012-1669]; Danish National Research Foundation [DNRF53]	Swedish Research Council (Vetenskapsradet, VR)(Swedish Research Council); Danish National Research Foundation(Danmarks Grundforskningsfond)	Research was supported by The Swedish Research Council (Vetenskapsradet, VR, grant number 621-2012-1669 to M.M.) and Danish National Research Foundation (grant number DNRF53 to D.E.C.). 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J	MacKenzie, AL; Webber, S; Watts, AM; Tonks, A				MacKenzie, A. L.; Webber, S.; Watts, A. M.; Tonks, A.			Historical deposits of <i>Alexandrium catenella</i> resting cysts in the sediments of Queen Charlotte Sound, New Zealand	NEW ZEALAND JOURNAL OF MARINE AND FRESHWATER RESEARCH			English	Article						Alexandrium catenella; Marlborough Sounds; New Zealand; resting cysts; sediment chronology	MARLBOROUGH SOUNDS; PUGET-SOUND; DINOPHYCEAE; CHRONOLOGY; DYNAMICS; PROPOSAL; REJECT; GULF	In 2011, a large repository of resting cysts of the toxic dinoflagellate Alexandrium catenella was discovered in the sediments of the Onapua/Opua inlet located off Tory Channel, Queen Charlotte Sound. The inlet is a potential source of infection for other areas, such as the major mussel-growing areas of Port Underwood and Pelorus Sound. This study aimed to establish whether the dinoflagellate was a new arrival in the Sounds or had existed unnoticed in this isolated embayment for some time. Alexandrium catenella cysts were identified to a depth of 20-21cm within the sediment cores, corresponding to a date estimated by radioisotope (Pb-210 and Cs-137) and Pinus radiata pollen distribution to at least the mid 1970s. Over this time span, resident populations of A. catenella have not become established beyond the confines of Queen Charlotte Sound, suggesting it does not pose an imminent threat of doing so unless increasingly intense and prolonged blooms result in more widespread cyst dispersal.	[MacKenzie, A. L.] Cawthron Inst, Nelson, New Zealand; [Webber, S.] Univ Victoria, Sch Geog Environm & Earth Sci, Wellington, New Zealand; [Watts, A. M.] Natl Inst Water & Atmosphere, Nelson, New Zealand; [Tonks, A.] Otago Sch Med Sci, Dept Anat, Dunedin, New Zealand	Cawthron Institute; Victoria University Wellington; National Institute of Water & Atmospheric Research (NIWA) - New Zealand; University of Otago	MacKenzie, AL (通讯作者)，Cawthron Inst, Nelson, New Zealand.	lincoln.mackenzie@cawthron.org.nz		Tonks, Alexandra/0000-0002-4851-6108; Webber, Sam/0000-0002-3981-5632	New Zealand Ministry for Business Innovation and Employment (MBIE) through the Cawthron Institute's Safe New Zealand Seafood programme [CAWX1317]; Bayer Boost environmental scholarships - Bayer New Zealand; Ministry for Science and Innovation undergraduate internship programme	New Zealand Ministry for Business Innovation and Employment (MBIE) through the Cawthron Institute's Safe New Zealand Seafood programme; Bayer Boost environmental scholarships - Bayer New Zealand; Ministry for Science and Innovation undergraduate internship programme	This research was principally funded by the New Zealand Ministry for Business Innovation and Employment (MBIE) through the Cawthron Institute's Safe New Zealand Seafood programme; MBIE contract CAWX1317. Sam Webber and Allie Tonks were supported through Bayer Boost environmental scholarships funded by Bayer New Zealand. Ashleigh Watts was supported via the Ministry for Science and Innovation undergraduate internship programme (2012).	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Z. J. Mar. Freshw. Res.	JUN	2016	50	2					195	208		10.1080/00288330.2015.1110187	http://dx.doi.org/10.1080/00288330.2015.1110187			14	Fisheries; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology; Oceanography	DP6RE					2025-03-11	WOS:000378625200002
J	Morozova, TV; Orlova, TY; Efimova, KV; Lazaryuk, AY; Burov, BA				Morozova, Tatiana V.; Orlova, Tatiana Yu.; Efimova, Kseniya V.; Lazaryuk, Alexander Yu.; Burov, Boris A.			<i>Scrippsiella trochoidea</i> cysts in recent sediments from Amur Bay, Sea of Japan: distribution and phylogeny	BOTANICA MARINA			English	Article						biomolecular study; dinoflagellate cyst; distribution; longevity; Scrippsiella trochoidea	RECENT MARINE-SEDIMENTS; WALLED DINOFLAGELLATE CYSTS; BOTTOM SEDIMENTS; YOKOHAMA-PORT; TOKYO-BAY; DINOPHYCEAE; GULF; EUTROPHICATION; MORPHOLOGY; PRESERVATION	A study of vertical distribution of dinoflagellate cysts in recent sediments was conducted for the first time in the Far Eastern seas of Russia. Dinoflagellate cysts were studied in sediment cores retrieved from five stations in Amur Bay (Peter the Great Bay, Sea of Japan) in 2010 and 2013. The Scrippsiella trochoidea complex was the dominant type of cyst, the average proportion of which (in the entire sediment cores) reached 39% of the total cyst abundance. The maximum abundance of S. trochoidea complex reached 5513 cysts g(-1) dry sediment. Cysts of the S. trochoidea complex were found to remain viable in the sediments after exposure to sub-zero temperatures. The identification of S. trochoidea in the Far Eastern seas of Russia was first confirmed by using biomolecular genetic analyses. The study of vertical distribution showed that cysts of this species dominate the upper sediment layers (0-10 cm). A tendency for abundance to increase from the shore toward the middle part of the bay was observed in the spatial distribution of cysts.	[Morozova, Tatiana V.; Orlova, Tatiana Yu.; Efimova, Kseniya V.] Russian Acad Sci, Far Eastern Branch, AV Zhirmunsky Inst Marine Biol, 17 Palchevskogo Str, Vladivostok 690041, Russia; [Efimova, Kseniya V.] Far Eastern Fed Univ, 8 Sukhanova Str, Vladivostok 690950, Russia; [Lazaryuk, Alexander Yu.; Burov, Boris A.] Russian Acad Sci, Far Eastern Branch, VI Ilichev Pacific Oceanol Inst, 43 Baltiiskaya Str, Vladivostok 690041, Russia	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences; Far Eastern Federal University; Ilichev Pacific Oceanological Institute; Russian Academy of Sciences	Morozova, TV (通讯作者)，Russian Acad Sci, Far Eastern Branch, AV Zhirmunsky Inst Marine Biol, 17 Palchevskogo Str, Vladivostok 690041, Russia.	tatiana_morozova@mail.ru	Morozova, Tatiana/G-4468-2018; Efimova, Kseniya/Q-3201-2016; Lazaryuk, Alexander/AAH-2203-2019; Orlova, Tatiana/AAU-8448-2020	Orlova, Tatiana/0000-0002-5246-6967; Efimova, Kseniya/0000-0002-6617-288X	Russian Foundation for Basic Research [15-04-05331]; Far Eastern Branch of Russian Academy of Sciences [12-III-A-06-093, 15-I-6-056, 15-I-6-059, 15-I-7-012, 15-I-6-014 o]; Russian Science Foundation [14-50-00034]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Far Eastern Branch of Russian Academy of Sciences(Russian Academy of Sciences); Russian Science Foundation(Russian Science Foundation (RSF))	The authors gratefully acknowledge the Russian Foundation for Basic Research (grant 15-04-05331), the Far Eastern Branch of Russian Academy of Sciences [grants 12-III-A-06-093, 15-I-6-056, 15-I-6-059, 15-I-7-012 (collection of biological material and culturing), 15-I-6-014 o (identification of microalgae)]. 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J	Ribeiro, S; Amorim, A; Abrantes, F; Ellegaard, M				Ribeiro, Sofia; Amorim, Ana; Abrantes, Fatima; Ellegaard, Marianne			Environmental change in the Western Iberia Upwelling Ecosystem since the preindustrial period revealed by dinoflagellate cyst records	HOLOCENE			English	Article						dinoflagellate cysts; Douro river; eutrophication; North Atlantic Oscillation; upwelling; Western Iberian Upwelling Ecosystem	NORTH-ATLANTIC OSCILLATION; SANTA-BARBARA BASIN; HYDROGRAPHIC CONDITIONS; GYMNODINIUM-CATENATUM; SEDIMENTARY RECORD; SURFACE SEDIMENTS; NORWEGIAN FJORD; GULLMAR FJORD; BALTIC SEA; EUTROPHICATION	We present the first multi-site study of dinoflagellate cyst records spanning ca. AD 1860-2000 from the west Iberian coast. Our aim was to reconstruct environmental changes in the Western Iberia Upwelling Ecosystem, one of the most biologically productive areas in the world, and an active fishery region. A major shift in cyst assemblages was recorded off the northwestern shelf sector between 1920 and 1950 towards autotrophic dominance, and consisted of a multi-fold increase in total cyst concentrations and cysts of Lingulodinium polyedrum, accompanied by an increase in Protoceratium reticulatum cysts. The observed changes pre-date the industrialization of agriculture in Portugal, and are concomitant with a shift in the North Atlantic Oscillation (NAO) towards negative indices (higher river input) and increasing sea-surface temperatures. The southernmost record, with reduced river- and human influence, showed only minor changes during the 20th century. Here, an increase in Protoperidinioid cysts after the 1980s is related to upwelling intensification. Our study indicates that the main changes recorded in the Western Iberian Upwelling system during the 20th century were driven by regional climate variability (warming, increased water stability and nutrient availability), possibly enhanced by anthropogenic nutrient input from the second half of the century. Our results highlight the complexity of the environmental drivers that may act upon dinoflagellate communities within the same region. The 20th-century environmental change in the Western Iberian Ecosystem has resulted in a shift towards marked autotrophic dominance of dinoflagellate cyst communities, and the northward expansion of species associated with Harmful Algal Blooms.	[Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, DK-1350 Copenhagen KBH K, Denmark; [Amorim, Ana] Univ Lisbon, Fac Ciencias, Marine & Environm Sci Ctr, P-1699 Lisbon, Portugal; [Amorim, Ana] Univ Lisbon, Fac Ciencias, Dept Biol Vegetal, P-1699 Lisbon, Portugal; [Abrantes, Fatima] IPMA, Unidade Geol Marinha, Lisbon, Portugal; [Ellegaard, Marianne] Univ Copenhagen, Dept Plant & Environm Sci PLEN, DK-1168 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland; Universidade de Lisboa; Universidade de Lisboa; Laboratorio Nacional de Energia e Geologia IP (LNEG); Instituto Portugues do Mar e da Atmosfera; University of Copenhagen	Ribeiro, S (通讯作者)，Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, DK-1350 Copenhagen KBH K, Denmark.	sri@geus.dk	Ribeiro, Sofia/AAZ-2782-2021; Abrantes, Fatima/N-7253-2019; Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/G-9213-2018; Abrantes, Fatima/B-5985-2013; Amorim, Ana/AAA-2615-2020	Ellegaard, Marianne/0000-0002-6032-3376; Ribeiro, Sofia/0000-0003-0672-9161; Abrantes, Fatima/0000-0002-9110-0212; Amorim, Ana/0000-0002-9612-4280	EU project HOLSMEER [EVK2-CT-2000-00060]; ESF EUROCORES EUROMARGINS project SEDPORT [PDCTM/40017/2003]; Portuguese Foundation for Science and Technology [UID/MAR/04292/2013]; project INSPECT [PTDC/MAR/73579/2006, SFRH/BD/30847/2006, PEst-OE/MAR/UI0199/2011]	EU project HOLSMEER; ESF EUROCORES EUROMARGINS project SEDPORT; Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); project INSPECT	Financial support was provided by the EU project HOLSMEER (EVK2-CT-2000-00060), the ESF EUROCORES EUROMARGINS project SEDPORT (PDCTM/40017/2003) and by the Portuguese Foundation for Science and Technology through UID/MAR/04292/2013, project INSPECT (PTDC/MAR/73579/2006), grant no. 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J	Gard, G; Backhouse, J; Crux, J				Gard, Gunilla; Backhouse, John; Crux, Jason			Calibration of Early Cretaceous dinoflagellate zones from the NWS of Australia to the global time scale through calcareous nannofossils	CRETACEOUS RESEARCH			English	Article						Biostratigraphy; Nannofossils; Palynology; Early Cretaceous; Australia		Palynomorphs and nannofossils were examined from the Lower Cretaceous interval of the well North Scarborough-1, drilled on the Exmouth Plateau, North West Shelf of Australia. Integration of the chronostratigraphic information from both fossil groups revealed discrepancies in the age information with the nannofossils suggesting a younger age than dinoflagellate cysts. The nannofossil events have a stronger tie to the global time scale than the dinoflagellate zones which are mainly local. The direct comparison of nannofossil and dinoflagellate events in the same section allows for improved strati graphic precision and a revised correlation of Australian dinoflagellate zonal ages to the global time scale, GTS12. Global nannofossil ages confirm a Barremian late Hauterivian age for the Muderongia australis Zone, but the Systematophora areolata to Dissimulidinium lobispinosum Zones appear to be 1-2 my younger than previously estimated. (C) 2016 Elsevier Ltd. All rights reserved.	[Gard, Gunilla; Crux, Jason] BHP Billiton Petr, 1360 Post Oak Blvd, Houston, TX 77056 USA; [Backhouse, John] Univ Western Australia, Sch Earth & Environm, UWA Ctr Energy Geosci, 35 Stirling Highway, Crawley, WA 6009, Australia	BHP Billiton; University of Western Australia	Gard, G (通讯作者)，BHP Billiton Petr, 1360 Post Oak Blvd, Houston, TX 77056 USA.	gunilla.gard@bhpbilliton.com; john.backhouse@uwa.edu.au; jason.crux@bhpbilliton.com						Backhouse J., 1999, COBURN 1 WELL COMPLE, P52; Backhouse J., 1988, W AUSTR GEOLOGICAL S, V135; Bergen J.A., 1994, J NANNOPLANKTON RES, P59; Bown P.R., 1998, P86; Davey R.J., 1966, STUDIES MESOZOIC CAI, P53; Geoscience Australia, 2013, AUSGEO NEWS, V111; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P43, DOI 10.1016/B978-0-444-59425-9.00003-2; HARDENBOL J., 1998, Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, V60, P3; Helby R., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V123, P407, DOI 10.2973/odp.proc.sr.123.121.1992; Helby R., 2004, Updated Jurassic and Early Cretaceous dinocyst zonation NWS Australia; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Howe R.W., 2000, 213 MERIWA; Jeremiah J, 2001, J MICROPALAEONTOL, V20, P45, DOI 10.1144/jm.20.1.45; Kaminski M.A., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V123, P717, DOI 10.2973/odp.proc.sr.123.115.1992; Kelman A.P., 2013, NO CARNORVON BASIC B; Longley I.M., 2002, SEDIMENTARY BASINS W, P27, DOI DOI 10.1017/CB09781107415324.004; Marshall N.G., 2013, NEW STRATIGRAPHIC FR; Metcalfe I, 2015, GONDWANA RES, V28, P61, DOI 10.1016/j.gr.2014.09.002; Mutterlose J., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V123, P343, DOI 10.2973/odp.proc.sr.123.124.1992; Ogg J., 2012, TIMESCALE CREATOR; Partridge A., 2006, AUSTR MESOZOIC CENOZ; Rawson P.F., 1995, B KNONKLINIK BELGISH, V66; Smith T., 2015, APPEA J, V2015, P105, DOI [DOI 10.1071/AJ14008, 10.1071/AJ14008]; Styzen Michael J., 1997, Journal of Nannoplankton Research, V19, P49	24	6	6	0	6	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	JUN	2016	61						180	187		10.1016/j.cretres.2016.01.001	http://dx.doi.org/10.1016/j.cretres.2016.01.001			8	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	DG2ZJ					2025-03-11	WOS:000371939000018
J	Filipova-Marinova, M; Pavlov, D; Giosan, L				Filipova-Marinova, Mariana; Pavlov, Danail; Giosan, Liviu			Multi-proxy records of Holocene palaeoenvironmental changes in the Varna Lake area, western Black Sea coast	QUATERNARY INTERNATIONAL			English	Article						Pollen; Dinocysts; Non-pollen palynomorphs; Human impact; Palaeoecology; Geoarchaeology	VEGETATION HISTORY; POLLEN ANALYSIS; 2 SEQUENCES; CALIBRATION; AGE	High-resolution spore-pollen analysis of laminated sediments of newly taken Core-3 (870 cm long) from Varna Lake (northeastern Bulgaria) is combined with multiproxy micropalaeontological 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 several submerged praehistorical sites and the Varna Chalcolithic Necropolis, and permits more precise palaeoecological correlations of obtained results with available archaeological and geochronological data. The established Age vs. Depth Model shows that the formation of the lake started after 7870 cal. BP due to a rise of the Black Sea level, also known as the First Phase of the Vityazevyan Black Sea Transgression. After ca. 94 y, the Second Phase of the Vityazevyan Black Sea Transgression is registered by a major change in the sedimentation and formation of molluscan shell hash layer of Mytilus galloprovincialis that covers the interval 7776 to 6183 cal. BP. Mixed oak and hornbeam forests dominated the vegetation cover during the Atlantic, Subboreal and Subatlantic chronozones of the Holocene. An important change in the forest composition occurs at ca. 5518 cal. BP, when Carpinus betulus reached its maximum spread due to a climate change. The high-resolution geoarchaeological reconstruction of palaeovegetation also reveals the extent of anthropogenic influence in the Varna Lake area, with deforestation and agricultural practice. Two periods of significant presence of pollen from cultivated cereals, and secondary anthropogenic indicators (weeds and ruderals) were identified. According to the available AMS-radiocarbon data, these periods correspond to the Late Eneolithic and Early Bronze Age. The Transitional period without human activities between these two archaeological periods lasted ca. 319 y and coincides with a rise of the Black Sea level, reflected by the increase of euryhaline marine dinoflagelate cysts Lingulodinium machaerophorum and Spiniferites belerius, and acritarchs Cymatiosphaera globulosa and Micrhystridium cf. ariakense during the First Phase of the Kalamitian Black Sea Transgression. The increased values of Corylus coincidently with decrease of Quercus and Ulmus suggest clearance of forests and enlargement of arable areas during the Late Eneolithic. The NPP-record of spores of coprophyllous fungi Cercophora, Sordaria, Podospora and Chaetomium indicates the presence of domestic animals during the Early Bronze Age. The maximum of Alnus, Ulmus, Fraxinus excelsior-type and Fagus pollen at 717 cal. BP suggests an increase of humidity and cooling of climate during the Subatlantic. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.	[Filipova-Marinova, Mariana] Museum Nat Hist Varna, 41 Maria Louisa Blvd, Varna 9000, Bulgaria; [Pavlov, Danail] Soc Innovat Ecologists Bulgaria, 10 Dr Bassanovich Str, Varna 9010, Bulgaria; [Giosan, Liviu] Woods Hole Oceanog Inst, Dept Geol & Geophys, 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; lgiosan@whoi.edu	Giosan, Liviu/F-1809-2010; Pavlov, Danail/N-7815-2013	Filipova-Marinova, Mariana/0000-0002-0786-9476; Pavlov, Danail/0000-0001-7382-2054	Bulgarian National Science Fund [DNTS02/11]; 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 bilateral project DNTS02/11 "Comparative paleoEcology and GeoArchaeology of Varna Lake (Bulgaria) and Mamaia Lake (Romania) - E.G.A.L." funded by the Bulgarian National Science Fund and Romanian National Authority for Scientific Research is greatly acknowledged.	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Int.	MAY 16	2016	401						99	108		10.1016/j.quaint.2015.05.009	http://dx.doi.org/10.1016/j.quaint.2015.05.009			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	DJ8QW					2025-03-11	WOS:000374478500008
J	Zonneveld, KAF; Siccha, M				Zonneveld, Karin A. F.; Siccha, Michael			Dinoflagellate cyst based modern analogue technique at test - A 300 year record from the Gulf of Taranto (Eastern Mediterranean)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinoflagellate cyst; Modern analogue technique; Eastern Mediterranean	SEA-SURFACE CONDITIONS; SW ADRIATIC SEA; DINOCYST ASSEMBLAGES; PRIMARY PRODUCTIVITY; CLIMATE VARIABILITY; RECONSTRUCTION; PHYTOPLANKTON; SEDIMENTS; WATER; EUTROPHICATION	To test the performance of dinoflagellate cyst based palaeoenvironmental reconstructions derived via the modern analogue technique (MAT) and a non-quantitative method, we have compared, reconstructions of mixed layer temperature, sea surface temperature and mixed layer salinity of a well dated site from the Gulf of Taranto, to instrumental data of air temperature, precipitation and river discharge. Two hypotheses are tested: the reconstructions of dinoflagellate cyst based MAT improve when a) a local reference dataset rather than an extra regional reference dataset is used, b) the reference and downcore datasets are corrected for species specific preservation prior to analysis. This is achieved by executing four experiments based on different reference datasets 1) a North Atlantic dataset including all species, 2) a North Atlantic dataset including degradation resistant species, 3) a Mediterranean dataset including all species, 4) a Mediterranean dataset including degradation resistant species only. We show that MAT based reconstructions improve when a local rather than an extra-regional reference dataset is used. Exclusively including species resistant to degradation improves the reconstruction if an extra-regional reference dataset is used, but leads to considerable loss of variability if the local reference dataset is used. Both MAT-based and qualitative reconstructions correlate to instrumental data for industrial times. For pre-industrial times, MAT reconstructions of variability in temperature and salinity do not co-vary with variability in the instrumental data, whereas qualitative reconstructions provide a relatively good fit. We suggest this to be a result of the anthropogenic influence on coastal marine ecosystems existing today at the majority of the coastal sample sites in the reference dataset. As a result, conditions at these sites do not correspond to pre-industrial conditions. We advise users of dinoflagellate cyst transfer functions to pay more attention to this aspect. (C) 2016 Elsevier B.V. All rights reserved.	[Zonneveld, Karin A. F.; Siccha, Michael] Univ Bremen, MARUM Fachbereich Geowissensch 5, Leobener Str, D-28334 Bremen, Germany	University of Bremen	Zonneveld, KAF (通讯作者)，Univ Bremen, MARUM Fachbereich Geowissensch 5, Leobener Str, D-28334 Bremen, Germany.	kzonneveld@marum.de		Siccha, Michael/0000-0002-2039-5535				[Anonymous], 1996, CLIMATIC VARIATIONS; Belmonte G., 2001, Biologia Marina Mediterranea, V8, P352; Bogus K, 2014, J PHYCOL, V50, P254, DOI 10.1111/jpy.12170; Boldrin A, 2005, MAR GEOL, V222, P135, DOI 10.1016/j.margeo.2005.06.010; Bonnet S, 2012, MAR MICROPALEONTOL, V84-85, P87, DOI 10.1016/j.marmicro.2011.11.006; Bringué M, 2013, MAR MICROPALEONTOL, V100, P34, DOI 10.1016/j.marmicro.2013.03.007; Bringué M, 2012, MAR GEOL, V291, P83, DOI 10.1016/j.margeo.2011.11.004; Camuffo D, 2013, CLIMATIC CHANGE, V117, P85, DOI 10.1007/s10584-012-0539-9; Camuffo D, 2014, CLIMATIC CHANGE, V122, P217, DOI 10.1007/s10584-013-0988-9; Camuffo D, 2012, CLIMATIC CHANGE, V111, P335, DOI 10.1007/s10584-011-0142-5; Camuffo D, 2012, PHYS CHEM EARTH, V40-41, P23, DOI 10.1016/j.pce.2010.02.002; 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Zonneveld KAF, 2009, J SEA RES, V62, P189, DOI 10.1016/j.seares.2009.02.003	83	7	8	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	MAY 15	2016	450						17	37		10.1016/j.palaeo.2016.02.045	http://dx.doi.org/10.1016/j.palaeo.2016.02.045			21	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	DK4VP					2025-03-11	WOS:000374918700002
J	Daners, G; Guerstein, GR; Amenábar, CR; Morales, E				Daners, Gloria; Raquel Guerstein, G.; Amenabar, Cecilia R.; Morales, Ethel			MIDDLE TO UPPER EOCENE DINOFLAGELLATE CYSTS FROM PUNTADEL ESTE AND COLORADO BASINS, MID LATITUDE SOUTHWEST ATLANTIC OCEAN	REVISTA BRASILEIRA DE PALEONTOLOGIA			Spanish	Article						dinoflagellate cysts; Eocene; Punta del Este Basin; Colorado Basin; biostratigraphy; paleoceanography	SANTA-CRUZ PROVINCE; SOUTHERN-OCEAN; DRAKE PASSAGE; CONTINENTAL-MARGIN; SCOTIA SEA; PALEOGENE; BIOSTRATIGRAPHY; ARGENTINA; EVOLUTION; PATAGONIA	The analysis of middle Eocene dinoflagellate cyst assemblages from sites at Punta del Este (similar to 36 degrees S, Uruguay) and Colorado (similar to 38 degrees S, Argentina) basins allows to interpret ocean circulation patterns on the South American Shelf prior to the opening of the Drake Passage. The assemblages contain endemic-Antarctic taxa such as Enneadocysta, Defiandrea, Vozzhennikovia and Spinidinium, which are also dominant in several circum-Antarctic sites, located southern 45 degrees S. Enneadocysta dictyostila is the most abundant species recorded from the studied sites and the unique member of the endemic assemblage apparently tolerant to warm surface waters. The presence of endemic taxa at mid latitudes has been related to a strong clockwise subpolar gyre favoured by the partial continental blockage of the Tasmanian Gateways and the Drake Passage. The distribution of the dinoflagellate cyst assemblages along the South Atlantic Ocean Shelf can be explained by a similar dynamical mechanism induced by a cyclonic subpolar gyre on the South Atlantic Ocean. The western boundary current of this gyre, starting on the west Antarctic continental slope, would follow a similar path to the present Malvinas Current on the Patagonian slope, which introduce cold oceanic waters to the shelf and intensifies the northward shelf transport. In the same way, during the middle Eocene the western boundary current of a proto-Weddell Gyre transported the circum-Antarctic waters and the endemic taxa northward along the Southwestern Atlantic Shelf. The opening and deepening of the Tasmanian Gateway and Drake Passage and the development of an incipient Antarctic Circumpolar Current during the latest Eocene Oligocene disrupted the subpolar gyres and promoted the extinction of the endemic species.	[Daners, Gloria] Univ Republica, Fac Ciencias, Inst Ciencias Geol, Dept Paleontol, Igua 4225, Montevideo 11400, Uruguay; [Raquel Guerstein, G.] Univ Nacl Sur, CONICET, Inst Geol Sur, Dept Geol, San Juan 670,B8000ICN, Bahia Blanca, Buenos Aires, Argentina; [Amenabar, Cecilia R.] Univ Buenos Aires, Inst Antartico Argentino, Inst Estudios Andinos Don Pablo Groeber, CONICET,Dept Ciencias Geol, Intendente Guiraldes 2160,C1428EGA, Buenos Aires, DF, Argentina; [Morales, Ethel] Univ Republica, Fac Ciencias, Inst Ciencias Geol, Dept Geol Sedimentaria & Aplicada, Igua 4225, Montevideo 11400, Uruguay	Universidad de la Republica, Uruguay; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Instituto Antartico Argentino; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; Universidad de la Republica, Uruguay	Daners, G (通讯作者)，Univ Republica, Fac Ciencias, Inst Ciencias Geol, Dept Paleontol, Igua 4225, Montevideo 11400, Uruguay.	glo@fcien.edu.uy; raquel.guerstein@uns.edu.ar; amenabar@gl.fcen.uba.ar; ethel@fcien.edu.uy						[Anonymous], 2013, THESIS; [Anonymous], 1971, P 2 PLANKT C; Archangelsky S., 1997, PEJERREY X 1 OFFSHOR; Barker PF, 2007, DEEP-SEA RES PT II, V54, P2293, DOI 10.1016/j.dsr2.2007.07.027; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; Bijl PK, 2013, EARTH-SCI REV, V124, P1, DOI 10.1016/j.earscirev.2013.04.010; Bijl PK, 2013, P NATL ACAD SCI USA, V110, P9645, DOI 10.1073/pnas.1220872110; 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; Bohaty SM, 2003, GEOLOGY, V31, P1017, DOI 10.1130/G19800.1; Bohaty SM, 2009, PALEOCEANOGRAPHY, V24, DOI 10.1029/2008PA001676; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; BUJAK J P, 1980, Special Papers in Palaeontology, P1; Casadío S, 2009, AMEGHINIANA, V46, P27; COCOZZA CD, 1992, ANTARCT SCI, V4, P355, DOI 10.1017/S0954102092000506; Combes V, 2014, J GEOPHYS RES-OCEANS, V119, P731, DOI 10.1002/2013JC009498; CONCHEYRO A, 1991, Ameghiniana, V28, P385; Conti B., 2015, THESIS; Cookson I. 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Bras. Paleontol.	MAY-AUG	2016	19	2					283	302		10.4072/rbp.2016.2.11	http://dx.doi.org/10.4072/rbp.2016.2.11			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DY9RD		Bronze, Green Published			2025-03-11	WOS:000385471900011
J	Fuentes, SN; Guler, MV; Cuitiño, JI; Palazzesi, L; Scasso, RA; Barreda, VD				Fuentes, Sabrina N.; Veronica Guler, M.; Cuitino, Jose I.; Palazzesi, Luis; Scasso, Roberto A.; Barreda, Viviana D.			BIOSTRATIGRAPHY BASED NEOGENE DINOFLAGELLATE CYSTS IN NORTHEAST OF PATAGONIA, ARGENTINA	REVISTA BRASILEIRA DE PALEONTOLOGIA			Spanish	Article						dinoflagellate cysts; Miocene; Northern Patagonia; Argentina	EASTERN PATAGONIA; MIOCENE; ASSEMBLAGES; CHUBUT; BASIN; BEDS	This paper presents the biostratigraphic results based on dinoflagellate cysts from two Neogene lithostratigraphic units cropping out in northeastern Patagonia. The Barranca Final Formation, located in the southwestern Colorado Basin, is exposed along the northern coast of San Matias Gulf, Rio Negro Province, and the Puerto Madryn Formation in the Peninsula Valdes, Chubut Province. The low-to-moderate diverse dinoflagellate cyst assemblages present are dominated by neritic taxa with subordinate oceanic indicators. Towards the top of both sections, the relative frequencies of the dinoflagellate cyts decrease, whereas acritarchs and continental palynomorphs proportions increase, indicating a shallowing upwards trend. The stratigraphic range of Labyrinthodinium truncatum truncatum in the lower part of the Barranca Final Formation indicate age between the late Burdigalian (ca. 16.5 Ma) and the late Tortonian (ca. 7.5 Ma) time interval. Labyrinthodinium truncatum truncatum and Habibacysta tectata constrain the age of the Puerto Madryn Formation to the Serravalian to Tortonian interval (late middle miocene to early late Miocene). Theses ages are consistent with the Sr-87/Sr-86 isotopic analysis of the oyster valves at 9.61 and 8.3 and with the Sr-87/Sr-86 ratios on calcitic shells at about 10 Ma, respectively.	[Fuentes, Sabrina N.] Museo Argentino Ciencias Nat Bernardino Rivadavia, Ave Angel Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina; [Veronica Guler, M.] Consejo Nacl Invest Cient & Tecn, Inst Geol Sur INGEOSUR, San Juan 670,B8000ICN, Buenos Aires, DF, Argentina; [Cuitino, Jose I.] Inst Patagon Geol & Paleontol CCT CENPAT CONICET, Blvd Brown 2915,U9120ACD, Puerto Madryn, Chubut, Argentina; [Palazzesi, Luis; Barreda, Viviana D.] Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat Bernardino Rivadavia, Ave Angel Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina; [Scasso, Roberto A.] Univ Buenos Aires, CONICET, Dept Ciencias Geol, FCEyN, C1428EHA, RA-1053 Buenos Aires, DF, Argentina	Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Centro Nacional Patagonico (CENPAT); Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires	Fuentes, SN (通讯作者)，Museo Argentino Ciencias Nat Bernardino Rivadavia, Ave Angel Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina.	sfuentes@macn.gov.ar; vguler@criba.edu.ar; jcuitino@cenpat-conicet.gob.ar; lpalazzesi@macn.gov.ar; rscasso@gl.fcen.uba.ar; vbarreda@macn.gov.ar	Cuitiño, José/HLQ-7475-2023	Cuitino, Jose Ignacio/0000-0002-4742-7920; Palazzesi, Luis/0000-0001-8026-4679; Barreda, Viviana Dora/0000-0002-1560-1277				Alberdi Maria T., 1997, Revista Espanola de Paleontologia, V12, P249; [Anonymous], 1965, ACTAS SEGUNDAS JORNA; [Anonymous], 1998, ANALES ACAD NACL CIE; [Anonymous], 1949, DESCRIPCION GEOLOGIC; [Anonymous], 1980, 2 S GEOL REG ARG; Caramés A, 2004, AMEGHINIANA, V41, P461; Cione AL, 2005, GEOBIOS-LYON, V38, P29, DOI 10.1016/j.geobios.2003.08.005; del Rio C.J., 1990, Anales de la Academia Nacional de Ciencias Exactas Fisicas y Naturales de Buenos Aires, V40, P231; del Río CJ, 2004, J PALEONTOL, V78, P1097, DOI 10.1666/0022-3360(2004)078<1097:TMMAOE>2.0.CO;2; Del Río CJ, 2001, PALAIOS, V16, P3, DOI 10.2307/3515550; Del Rio Claudia Julia, 2000, Serie Correlacion Geologica, V14, P77; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Fensome R.A., 2008, DINOFLAJ2, Version 1; Frenguelli J., 1921, B ACAD NACL CIENCIAS, V29, P191; Gelos E.M., 1993, REV ASOC GEOL ARGENT, V47, P365; Gradstein F.M., 2012, GEOLOGIC TIME SCALE, DOI [10.1016/B978-0-444-59425-9.11001-5, DOI 10.1016/B978-0-444-59425-9.11001-5]; GRIMM E., 1991, TILIA SOFTWARE; Guler M.V., 2002, REV MUSEO ARGENTINO, V5, P225; Haller M., 1979, C GEOLOGICO ARGENTIN, V7, P285; Head MJ, 1997, J PALEONTOL, V71, P165, DOI 10.1017/S0022336000039123; Kaasschieter J.P.H., 1963, TULSA GEOLOGICAL SOC, V31, P177; Louwye S, 2008, GEOL MAG, V145, P321, DOI 10.1017/S0016756807004244; Louwye S, 2007, GEOL MAG, V144, P33, DOI 10.1017/S0016756806002627; Malumian N., 1998, ACTAS X C LATINOAM G, V1, P125; Marengo H., 2015, CHACO PARANENSE BASI, DOI [10.1007/978-3-319-12814-6, DOI 10.1007/978-3-319-12814-6]; Masiuk V., 1976, 24 ARPEL; Palazzesi L, 2004, AMEGHINIANA, V41, P355; Palazzesi L, 2014, NAT COMMUN, V5, DOI 10.1038/ncomms4558; Parras A, 2012, J S AM EARTH SCI, V37, P122, DOI 10.1016/j.jsames.2012.02.007; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; Scasso R., 1987, Rev. 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MAY-AUG	2016	19	2					303	314		10.4072/rbp.2016.2.12	http://dx.doi.org/10.4072/rbp.2016.2.12			12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DY9RD		Bronze, Green Published			2025-03-11	WOS:000385471900012
J	Abadie, E; Muguet, A; Berteaux, T; Chomérat, N; Hess, P; D'OrbCastel, ER; Masseret, E; Laabir, M				Abadie, Eric; Muguet, Alexia; Berteaux, Tom; Chomerat, Nicolas; Hess, Philipp; D'OrbCastel, Emmanuelle Roque; Masseret, Estelle; Laabir, Mohamed			Toxin and Growth Responses of the Neurotoxic Dinoflagellate <i>Vulcanodinium rugosum</i> to Varying Temperature and Salinity	TOXINS			English	Article						Vulcanodinium rugosum; Mediterranean Ingril Lagoon; toxin production; growth conditions; temperature; salinity	HARMFUL ALGAL BLOOMS; GYMNODINIUM-CATENATUM DINOPHYCEAE; ALEXANDRIUM-TAMARENSE; MARINE DINOFLAGELLATE; ENVIRONMENTAL-FACTORS; PARALYTIC SHELLFISH; CLIMATE-CHANGE; HIROSHIMA BAY; RESTING CYSTS; PINNATOXINS E	Vulcanodinium rugosum, a recently described species, produces pinnatoxins. The IFR-VRU-01 strain, isolated from a French Mediterranean lagoon in 2010 and identified as the causative dinoflagellate contaminating mussels in the Ingril Lagoon (French Mediterranean) with pinnatoxin-G, was grown in an enriched natural seawater medium. We tested the effect of temperature and salinity on growth, pinnatoxin-G production and chlorophyll a levels of this dinoflagellate. These factors were tested in combinations of five temperatures (15, 20, 25, 30 and 35 degrees C) and five salinities (20, 25, 30, 35 and 40) at an irradiance of 100 mu mol photon m(-2) s(-1). V. rugosum can grow at temperatures and salinities ranging from 20 degrees C to 30 degrees C and 20 to 40, respectively. The optimal combination for growth (0.39 +/- 0.11 d(-1)) was a temperature of 25 degrees C and a salinity of 40. Results suggest that V. rugosum is euryhaline and thermophile which could explain why this dinoflagellate develops in situ only from June to September. V. rugosum growth rate and pinnatoxin-G production were highest at temperatures ranging between 25 and 30 degrees C. This suggests that the dinoflagellate may give rise to extensive blooms in the coming decades caused by the climate change-related increases in temperature expected in the Mediterranean coasts.	[Abadie, Eric; Muguet, Alexia; Berteaux, Tom; D'OrbCastel, Emmanuelle Roque] IFREMER, Ctr Marine Biodivers Exploitat & Conservat MARBEC, Lab Environm Ressources Languedoc Roussillon, CS30171, F-34200 Sete 03, France; [Chomerat, Nicolas] IFREMER, Lab Environm Ressources Bretagne Occidentale, Pl Croix, F-29900 Concarneau, France; [Hess, Philipp] IFREMER, Lab Phycotoxines DYNECO PHYC, Rue Ile Yeu,BP 21105, F-44311 Nantes 3, France; [Masseret, Estelle; Laabir, Mohamed] Univ Montpellier, Inst Dev Res, Ctr Marine Biodivers Exploitat & Conservat MARBEC, Ifremer,CNRS, Pl E Bataillon,CC93, F-34095 Montpellier 5, France	Ifremer; Ifremer; Ifremer; Universite de Montpellier; Institut de Recherche pour le Developpement (IRD); Ifremer; Centre National de la Recherche Scientifique (CNRS)	Abadie, E (通讯作者)，IFREMER, Ctr Marine Biodivers Exploitat & Conservat MARBEC, Lab Environm Ressources Languedoc Roussillon, CS30171, F-34200 Sete 03, France.	eric.abadie@ifremer.fr; alexia.muguet@hotmail.fr; tom.berteaux@ifremer.fr; nicolas.chomerat@ifremer.fr; philipp.hess@ifremer.fr; emmanuelle.roque@ifremer.fr; estelle.masseret@univ-montp2.fr; mohamed.laabir@univ-montp2.fr	; Hess, Philipp/G-1761-2010	Chomerat, Nicolas/0000-0001-9691-6344; roque d'orbcastel, emmanuelle/0000-0002-0954-0033; Hess, Philipp/0000-0002-9047-1345; ABADIE, Eric/0000-0001-9431-2010; Masseret, Estelle/0000-0001-6856-8637	EC2CO Ecosphere Continentale et Cotiere DRIL (VULCANO project); TOTAL Foundation (LAGUNOTOX project); Agence de l'Eau Rhone Mediterranee Corse (AERMC-Rhone Mediterranean Corsica Water Agency); IRD (Institut National pour la Recherche et le Developpement-National Institute for Research and Development)	EC2CO Ecosphere Continentale et Cotiere DRIL (VULCANO project); TOTAL Foundation (LAGUNOTOX project); Agence de l'Eau Rhone Mediterranee Corse (AERMC-Rhone Mediterranean Corsica Water Agency); IRD (Institut National pour la Recherche et le Developpement-National Institute for Research and Development)	Thanks to EC2CO Ecosphere Continentale et Cotiere DRIL (VULCANO project) and TOTAL Foundation (LAGUNOTOX project) for funding this work. We would also to thank the Agence de l'Eau Rhone Mediterranee Corse (AERMC-Rhone Mediterranean Corsica Water Agency) for their financial help. Thanks to the IRD (Institut National pour la Recherche et le Developpement-National Institute for Research and Development) for funding Mohamed Laabir's stay in Tunisia.	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J	Slimani, H; Guédé, KE; Williams, GL; Asebriy, L; Ahmamou, M				Slimani, Hamid; Elysee Guede, Kore; Williams, Graham L.; Asebriy, Lahcen; Ahmamou, M'Fedal			Campanian to Eocene dinoflagellate cyst biostratigraphy from the Tahar and Sekada sections at Arba Ayacha, western External Rif, Morocco	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Campanian-Ypresian dinoflagellate cysts; Biostratigraphy; Cretaceous-Paleogene boundary; Paleocene-Eocene boundary; Western External Rif; Morocco	CRETACEOUS-TERTIARY BOUNDARY; OULED HADDOU; PALEOGENE BOUNDARY; CRETACEOUS/PALAEOGENE BOUNDARY; CALCAREOUS NANNOPLANKTON; NORTHERN APENNINES; THERMAL MAXIMUM; CARBON-CYCLE; SEA-LEVEL; EL-KEF	Our detailed palynological study of the Upper Cretaceous-Lower Eocene manly succession from the Sekada and Tahar sections in southern Arba Ayacha, westernmost External Rif Chain (northwestern Morocco), has provided precise age determinations based on dinoflagellate cyst biostratigraphy. Dinoflagellate cysts (dinocysts), which are the dominant palynomorphs, allowed us to recognize the following ages: Late Campanian, Early and Late Maastrichtian, Danian, Selandian, Thanetian and Early Ypresien. Published studies on the western External Rif based on lithostratigraphy, show conflicting ages of Late Cretaceous (Senonian) and Early Eocene. Our age determinations are based on dinocyst events, which are more reliable. We recognize the Late Campanian on the First Occurrence (FO) and Last Occurrence (LO) of Exochosphaeridium? masureae, and the FO of Cerodinium spp., and the LOs of Cribroperidinium wilsonii subsp. wilsonii, Odontochitina porifera and Trithyrodinium suspectum. The Early Maastrichtian is denoted by the FOs of Alterbidinium varium and Palaeocystodinium golzowense and the LO of Alterbidinium acutulum. We define the Late Maastrichtian on the FOs of Disphaerogena carposphaeropsis and Glaphyrocysta perforata, and the LOs of Alisogymnium euclaense, Dinogymnium spp., Isabelidinium cooksoniae, and Pterodinium cretaceum, plus the worldwide latest Maastrichtian acme of Manumiella seelandica. Marking the Danian is the overall range of Senoniasphaera inomata, the FOs of Carpatella cornuta, Damassadinium californicum and Membranilarnacia? tenella. Species having LOs in the Selandian incude Cerodinium diebelii, Manumiella seelandica, Senoniasphaera inornata, Palaeocystodinium australinum and Cerodinium speciosum. We recognize the Thanetian mainly on the FO of Homotryblium tenuispinosum and based the worldwide terminal Thanetian acme of Apectodinium spp. The Early Ypresian is characterized by the FO of Deflandrea phosphoritica and a high abundance of Apectodinium spp. and Kenleyia spp. Thus, we now know that the rocks outcropping in the Sekada and Tahar sections are Late Campanian to Early Ypresian in age. (C) 2016 Elsevier B.V. All rights reserved.	[Slimani, Hamid; Elysee Guede, Kore; Asebriy, Lahcen] Mohammed V Univ Rabat, Inst Sci, Lab Geol & Remote Sensing, URAC46, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco; [Elysee Guede, Kore; Ahmamou, M'Fedal] Univ Mohammed V Rabat, Fac Sci, Lab Elect Signal Treatments & Geomat, Ave Ibn Batouta,PB 1014, Rabat 10106, Morocco; [Elysee Guede, Kore] Univ Felix Houphouet Boigny, UFR STRM, BP 582, Abidjan 22, Cote Ivoire; [Williams, Graham L.] Nat Resources Canada, Bedford Inst Oceanog, Geol Survey Canada Atlantic, POB 1006, Dartmouth, NS B2Y 4A2, Canada	Mohammed V University in Rabat; Mohammed V University in Rabat; Universite Felix Houphouet-Boigny; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography	Slimani, H (通讯作者)，Mohammed V Univ Rabat, Inst Sci, Lab Geol & Remote Sensing, URAC46, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020; Elysee, Guede/ABE-3209-2021	Kore Elysee, Guede/0000-0003-1393-5078; Slimani, Hamid/0000-0001-6392-1913	"Comite d'Entraide International" (CEI); "Direction de l'Orientation et des Bourses" (DOB) of Cote d'Ivoire; University Mohammed V of Rabat [SVT 11/09]; National Center of Scientific Research, Morocco [URAC46]	"Comite d'Entraide International" (CEI); "Direction de l'Orientation et des Bourses" (DOB) of Cote d'Ivoire; University Mohammed V of Rabat(Mohammed V University in Rabat); National Center of Scientific Research, Morocco	Authors would like to thank Dr. Stephen Louwye and Mrs. Sabine Van Cauwenberghe (Paleontology Research Unit, University of Gent, Belgium) for the palynological preparation of some of the studied samples. The second author thanks the "Comite d'Entraide International" (CEI) and the "Direction de l'Orientation et des Bourses" (DOB) of Cote d'Ivoire for financial support. This work is supported by the University Mohammed V of Rabat (Project SVT 11/09) and the National Center of Scientific Research (URAC46), Morocco. The journal reviewers Lucia Roncaglia and an anonymous are kindly thanked for their reviews that improved considerably the manuscript.	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Palaeobot. Palynology	MAY	2016	228						26	46		10.1016/j.revpalbo.2016.01.003	http://dx.doi.org/10.1016/j.revpalbo.2016.01.003			21	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	DJ7WV					2025-03-11	WOS:000374424800002
J	Van Nieuwenhove, N; Baumann, A; Matthiessen, J; Bonnet, S; de Vernal, A				Van Nieuwenhove, Nicolas; Baumann, Astrid; Matthiessen, Jens; Bonnet, Sophie; de Vernal, Anne			Sea surface conditions in the southern Nordic Seas during the Holocene based on dinoflagellate cyst assemblages	HOLOCENE			English	Article						dinocysts; Holocene; oceanography; phytoplankton; sea surface; seasonality	NORTH ICELANDIC SHELF; NORWEGIAN-GREENLAND SEA; LAURENTIDE ICE-SHEET; HIGH-RESOLUTION; PALEOCEANOGRAPHIC IMPLICATIONS; DINOCYST ASSEMBLAGES; PALEO-OCEANOGRAPHY; OCEAN CONDITIONS; ATLANTIC CURRENT; LIGHT-INTENSITY	Dinoflagellate cyst (dinocyst) records from the southern Nordic Seas were compiled in order to evaluate the evolution of upper ocean conditions, on a millennial timescale and supported by a highly resolved record from the Voring Plateau. After the transitional phase from the last deglaciation, three main phases define the Holocene. The early Holocene (>7.5 ka BP) features important numbers of cool-temperate species dominated by Nematosphaeropsis labyrinthus and Impagidinium pallidum in the west. The assemblage composition changes drastically at the transition from the early to the mid-Holocene, from when on Operculodinium centrocarpum dominates. The changeover is dated between similar to 6.1 and 7.5 ka BP, perhaps earlier closer to the Iceland-Scotland Ridge, and appears to be linked to the onset of a modern type of surface circulation. 'Warmest' assemblages occur at the Voring Plateau shortly after the transition, when Atlantic waters also appear to have spread farthest westward. The recurrence of colder elements can be linked to cooling from similar to 2.4 ka BP at the Voring Plateau and presumably earlier in the west but is difficult to date there because of the low sedimentation rates. This is a general issue in many areas of the Nordic Seas and appears to have an important effect on cyst concentrations and assemblage composition, with the possible loss of oxygenation-sensitive cysts in the older parts of the cores. Comparing dinocyst-based quantitative reconstructions with those retrieved from other plankton reveals a significantly different trend between proxies, linked to a differing autecological response to seasonal changes at their respective depth habitats.	[Van Nieuwenhove, Nicolas] Aarhus Univ, Dept Geosci, Hoegh Guldbergsgade 2, DK-8000 Aarhus C, Denmark; [Van Nieuwenhove, Nicolas; Bonnet, Sophie; de Vernal, Anne] Univ Quebec, Ctr Rech Geochim & Geodynam Geotop, Ste Foy, PQ G1V 2M3, Canada; [Baumann, Astrid; Matthiessen, Jens] Alfred Wegener Inst, Helmholtz Ctr Polar & Marine Res, Bremerhaven, Germany	Aarhus University; University of Quebec; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Van Nieuwenhove, N (通讯作者)，Aarhus Univ, Dept Geosci, Hoegh Guldbergsgade 2, DK-8000 Aarhus C, Denmark.	nvn@geo.au.dk	Van Nieuwenhove, Nicolas/IAQ-1532-2023; de Vernal, Anne/D-5602-2013	Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Matthiessen, Jens/0000-0002-6952-2494	German Research Foundation [NI1248]; European Union's Seventh Framework program [243908]; Ministere du Developpement Economique de l'innovation et de l'exportation du Quebec; ArcTrain-Canada	German Research Foundation(German Research Foundation (DFG)); European Union's Seventh Framework program(European Union (EU)); Ministere du Developpement Economique de l'innovation et de l'exportation du Quebec; ArcTrain-Canada	This work was supported by the German Research Foundation (Grant NI1248); the European Union's Seventh Framework program (Grant Agreement 243908 'Past4Future': climate change learning from the past climate); the Ministere du Developpement Economique de l'innovation et de l'exportation du Quebec; and ArcTrain-Canada.	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J	Mardones, JI; Bolch, C; Guzmán, L; Paredes, J; Varela, D; Hallegraeff, GM				Mardones, Jorge I.; Bolch, Chris; Guzman, Leonardo; Paredes, Javier; Varela, Daniel; Hallegraeff, Gustaaf M.			Role of resting cysts in Chilean <i>Alexandrium catenella</i> dinoflagellate blooms revisited	HARMFUL ALGAE			English	Article						Alexandrium catenella; Mating compatibility/encystment; Mandatory dormancy; Excystment; AFLPs; Chilean cysts field data	SPECIES COMPLEX DINOPHYCEAE; GENETIC DIVERSITY; TAMARENSE; EXCYSTMENT; DNA; GERMINATION; POPULATION; FRAGMENT; DORMANCY; FJORDS	The detection of sparse Alexandrium catenella-resting cysts in sediments of southern Chilean fjords has cast doubts on their importance in the recurrence of massive toxic dinoflagellate blooms in the region. The role of resting cysts and the existence of different regional Chilean populations was studied by culturing and genetic approaches to define: (1) cyst production; (2) dormancy period; (3) excystment success; (4) offspring viability and (5) strain mating compatibility. This study newly revealed a short cyst dormancy (minimum 69 days), the role of key abiotic factors (in decreasing order salinity, irradiance, temperature and nutrients) controlling cyst germination (max. 60%) and germling growth rates (up to 0.36-0.52 div. day(-1)). Amplified fragment length polymorphism (AFLP) characterization showed significant differences in genetic distances (GD) among A. catenella populations that were primarily determined by the geographical origin of isolates and most likely driven by oceanographic dispersal barriers. A complex heterothallic mating system pointed to variable reproductive compatibility (RCs) among Chilean strains that was high among northern (Los Lagos/North Aysen) and southern populations (Magallanes), but limited among the genetically differentiated central (South Aysen) populations. Field cyst surveys after a massive 2009 bloom event revealed the existence of exceptional high cyst densities in particular areas of the fjords (max. 14.627 cysts cm(-3)), which contrast with low cyst concentrations (<221.3 cysts cm(-3)) detected by previous oceanographic campaigns. In conclusion, the present study suggests that A. catenella resting cysts play a more important role in the success of this species in Chilean fjords than previously thought. Results from in vitro experiments suggest that pelagic-benthic processes can maintain year-round low vegetative cell concentrations in the water column, but also can explain the detection of high cysts aggregations after the 2009-bloom event. Regional drivers that lead to massive outbreaks, however, are still unknown but, potential scenarios are discussed. (C) 2016 Elsevier B.V. All rights reserved.	[Mardones, Jorge I.; Bolch, Chris; Hallegraeff, Gustaaf M.] Univ Tasmania, Inst Marine & Antarctic Studies IMAS, Private Bag 129, Hobart, Tas 7001, Australia; [Guzman, Leonardo] IFOP, Balmaceda 252, Puerto Montt 5480000, Chile; [Paredes, Javier; Varela, Daniel] Univ Lagos, Ctr I Mar, Casilla 557, Puerto Montt, Chile; [Paredes, Javier] Univ Catolica Norte, Fac Ciencias Mar, Dept Biol Marina, Programa Doctorado Biol & Ecol Aplicada, Antofagasta, Chile	University of Tasmania; Universidad de Los Lagos; Universidad Catolica del Norte	Mardones, JI (通讯作者)，Univ Tasmania, Inst Marine & Antarctic Studies IMAS, Private Bag 129, Hobart, Tas 7001, Australia.	jorge.mardones@utas.edu.au	Bolch, Christopher/J-7619-2014; Hallegraeff, Gustaaf/C-8351-2013; Varela, Daniel/D-7908-2013	Hallegraeff, Gustaaf/0000-0001-8464-7343; Varela, Daniel/0000-0003-4603-4970; Mardones, Jorge/0000-0003-3160-0415	BECAS-CHILE Program of the National Commission for Scientific and Technological Research (CONICYT); Chilean Ph.D student fellowship from CONICYT; FONDECYT [1130954]; Fisheries and Aquaculture Undersecretary-Instituto de Fomento Pesquero (IFOP)	BECAS-CHILE Program of the National Commission for Scientific and Technological Research (CONICYT); Chilean Ph.D student fellowship from CONICYT; FONDECYT(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDECYT); Fisheries and Aquaculture Undersecretary-Instituto de Fomento Pesquero (IFOP)	We thank Ludmilla Untari, Helen Bond, Sarah Ugalde and Andrea Zuniga for technical assistance. This research was supported by a Ph.D. student fellowship from BECAS-CHILE Program of the National Commission for Scientific and Technological Research (CONICYT) to J. Mardones and by a Chilean Ph.D student fellowship from CONICYT to J. Paredes. 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J	Heikkilä, M; Pospelova, V; Forest, A; Stern, GA; Fortier, L; Macdonald, RW				Heikkila, Maija; Pospelova, Vera; Forest, Alexandre; Stern, Gary A.; Fortier, Louis; Macdonald, Robie W.			Dinoflagellate cyst production over an annual cycle in seasonally ice-covered Hudson Bay	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cyst; Sea-ice; Hudson Bay; Arctic; Sediment trap; Phytoplankton dynamics; Tintinnid loricae; Ciliate	SEA-SURFACE CONDITIONS; RECENT MARINE-SEDIMENTS; FRESH-WATER; LIFE-CYCLE; MIXOTROPHIC DINOFLAGELLATE; PALYNOLOGICAL EVIDENCE; OCEANOGRAPHIC CHANGES; ENVIRONMENTAL-FACTORS; DINOCYST ASSEMBLAGES; SPATIAL-DISTRIBUTION	We present continuous bi-weekly to bi-monthly dinoflagellate cyst, tintinnid loricae and tintinnid cyst fluxes at two mooring sites in Hudson Bay (subarctic Canada) from October 2005 to September 2006. The total dinoflagellate cyst fluxes at the site on the western side of the bay ranged from 4600 to 53,600 cysts m(-2) day(-1) (average 20,000 cysts m(-2) day(-1)), while on average three times higher fluxes (average 62,300 cysts m(-2) day(-1)) were recorded at the site on the eastern side of the bay with a range from 2700 to 394,800 cysts m(-2) day(-1). These values are equivalent to the average fluxes calculated from the top 1-cm sediment layer of 210Pb-dated box cores at corresponding locations, and hence lend support to the use of sediment dinoflagellate cysts in palaeoceanography. Tintinnid fluxes ranged from 1200 to 80,000 specimens m(-2) day(-1) (average 32,100 tintinnids m(-2) day(-1)) in the west, and 1600 to 1,240,800 specimens m(-2) day(-1) (average 106,800 tintinnids m(-2) day(-1)) in the east, with the highest Salpingella sp. fluxes recorded during the sea-ice cover season. The dinoflagellate cyst species diversity recorded in the traps was similar at the two environmentally differing locations, with cold-water (e.g., Echinidinium karaense, Islandinium minutum, Islandinium? cezare, Polykrikos sp. var. arctica, Spiniferites elongates), cosmopolitan (e.g., Operculodinium centrocarpum, Spiniferites ramosus, Brigantedinium) and typical warmer-water (e.g., Echinidinium aculeatum, Islanidium brevispinosum) species present. Furthermore, the species-specific timing of cyst production behaved similarly relative to the seasonal sea-ice cycle at both locations. Cyst species proportions and species-specific flux quantities, however, differed between the two sites and corresponded to the quantities and species assemblages recorded in the surface sediment, with the exception of cysts of Polarella glacialis and cf. Biecheleria sp. that seem not to preserve well in sediment but were abundant in both traps. Otherwise, cyst assemblage at the western trap site was dominated by O. centrocarpum and S. elongates while at the eastern site very high quantities of cysts of Pentapharsodinium dalei were recorded. Our data do not lend support to the hypothesis that trophic status solely determines whether cyst production takes place under-ice or in the open water, since cysts of light-dependent (phototrophic) and light-independent (heterotrophic) dinoflagellates are recorded during both conditions. Most importantly, negligible under-ice cyst production is recorded during the deep arctic winter. (C) 2016 Elsevier B.V. All rights reserved.	[Heikkila, Maija] Univ Helsinki, Dept Environm Sci, Environm Change Res Unit, POB 65, FIN-00014 Helsinki, Finland; [Heikkila, Maija; Stern, Gary A.; Macdonald, Robie W.] Univ Manitoba, Ctr Earth Observat Sci, 496 Wallace Bldg, Winnipeg, MB R3T 2N2, Canada; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB A405,POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada; [Forest, Alexandre; Fortier, Louis] Univ Laval, Takuv Joint Lab, Pavillon Alexandre Vachon 1045, Quebec City, PQ G1V 0A6, Canada; [Macdonald, Robie W.] Inst Ocean Sci, Dept Fisheries & Oceans, 9860 W Saanich Rd,POB 6000, Sidney, BC V8L 4B2, Canada	University of Helsinki; University of Manitoba; University of Victoria; Laval University; Fisheries & Oceans Canada	Heikkilä, M (通讯作者)，Univ Helsinki, Dept Environm Sci, Environm Change Res Unit, POB 65, FIN-00014 Helsinki, Finland.	maija.heikkila@helsinki.fi	Macdonald, Robie/A-7896-2012; Heikkila, Maija/N-7659-2013	Forest, Alexandre/0000-0001-9002-947X; Macdonald, Robie/0000-0002-1141-8520; Heikkila, Maija/0000-0003-3885-8670; Pospelova, Vera/0000-0003-4049-8133; Stern, Gary/0000-0003-2160-0841	ArcticNet, a Network of Centres of Excellence of Canada; Academy of Finland [251, 212]; Natural Science and Engineering Research Council of Canada (NSERC)	ArcticNet, a Network of Centres of Excellence of Canada; Academy of Finland(Research Council of Finland); Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	We are grateful to the captains and crews of CCGS Amundsen and CCGS Pierre Radisson, and the mooring team technicians for the deployments and recoveries of the sediment traps. National Climate Services Canada is thanked for producing the missing CWEEDS data. We thank the Editor and two reviewers for their constructive comments on the manuscript. This study was supported by ArcticNet, a Network of Centres of Excellence of Canada, and the Academy of Finland (grant no. 251,212 to M.H.). This research was partially supported by the Natural Science and Engineering Research Council of Canada (NSERC Discovery grant to V.P.).	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Micropaleontol.	MAY	2016	125						1	24		10.1016/j.marmicro.2016.02.005	http://dx.doi.org/10.1016/j.marmicro.2016.02.005			24	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DO4EO		Green Published			2025-03-11	WOS:000377734800001
J	Reidhaar, PE; Lane, CS; Benitez-Nelson, CR; Gamble, DW				Reidhaar, Paula E.; Lane, Chad S.; Benitez-Nelson, Claudia R.; Gamble, Douglas W.			Spatial and Temporal Variations in <i>Pyrodinium bahamense</i> Cyst Concentrations in the Sediments of Bioluminescent Mangrove Lagoon, St. Croix, USVI	ESTUARIES AND COASTS			English	Article						Conservation; Dinoflagellate; Nutrients; Paleoenvironment; Radioisotope; Stable isotope	ISOTOPIC COMPOSITION; BAHIA FOSFORESCENTE; ORGANIC-MATTER; MANILA BAY; PHYTOPLANKTON; COASTAL; GEOCHEMISTRY; ACCUMULATION; ABUNDANCE; FLORIDA	Mangrove Lagoon, located on the island of St. Croix, US Virgin Islands (USVI), is one of few actively bioluminescent lagoons in a location experiencing significant anthropogenic impacts. The bioluminescence is due to an abundance of the dinoflagellate Pyrodinium bahamense in the water column. We recovered surface sediments and sediment cores from Mangrove Lagoon to analyze the spatial distribution and temporal variability of P. bahamense cysts in this system. Surface sediment P. bahamense cyst concentrations ranged from 0 to 466 cysts g(-1) dry sediment, with higher abundances associated with elevated surface water nutrient concentrations and a mixed terrestrial-marine organic matter source regime. In combination with available bioassay data, we hypothesize that phytoplankton utilize nutrients rapidly and subsequent decay of organic matter makes nutrients available for dinoflagellates at the sediment-water interface in the eastern and northern quadrants of the lagoon. However, the nutrients are rapidly exhausted during counterclockwise lagoon circulation resulting in the decline of primary productivity and dinoflagellate abundance in the western quadrants. Downcore profiles suggest that P. bahamense blooms have been occurring for decades, declining in recent years. No cysts were present in sediments predating dredging activities of the 1960s that created Mangrove Lagoon. Recent reductions in cyst abundance may be the result of limited primary productivity caused by restricted water exchange with Salt River Bay due to shallowing of a sill at the mouth of the lagoon. This research highlights the need for more comprehensive geochemical and fossil analyses to better understand long-term ecological variability and inform conservation efforts of these unique habitats.	[Reidhaar, Paula E.; Lane, Chad S.; Gamble, Douglas W.] Univ N Carolina, Dept Geog & Geol, Wilmington, NC 28403 USA; [Benitez-Nelson, Claudia R.] Univ S Carolina, Marine Sci Program, Columbia, SC 29208 USA; [Benitez-Nelson, Claudia R.] Univ S Carolina, Dept Earth & Ocean Sci, Columbia, SC 29208 USA	University of North Carolina; University of North Carolina Wilmington; University of South Carolina System; University of South Carolina Columbia; University of South Carolina System; University of South Carolina Columbia	Reidhaar, PE (通讯作者)，Univ N Carolina, Dept Geog & Geol, Wilmington, NC 28403 USA.	paulareidhaar@yahoo.com		Lane, Chad/0000-0001-8934-5379; Benitez-Nelson, Claudia/0000-0002-1004-5048	US Office of Insular Affairs; National Parks Service (NPS); University of North Carolina Wilmington (UNCW); University of North Carolina Wilmington Center for Marine Science	US Office of Insular Affairs; National Parks Service (NPS); University of North Carolina Wilmington (UNCW); University of North Carolina Wilmington Center for Marine Science	We would like to thank the US Office of Insular Affairs, the National Parks Service (NPS), the University of North Carolina Wilmington (UNCW), and the University of North Carolina Wilmington Center for Marine Science for funding this work. We also wish to thank M. Zimberlin and J. Pinckney at the University of South Carolina for sharing data. Thanks are also due to Z. Hillis-Starr (NPS), D. Goldstein (NPS), A. Wagner (UNCW), K. Duernberger (UNCW), M. Tedick (UNCW), J. Massoll (UNCW), B. Castillo (UVI), K. Reale-Munroe (UVI), and M. Taylor (UVI) for assistance in the field.	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J	Luo, ZH; Mertens, KN; Bagheri, S; Aydin, H; Takano, Y; Matsuoka, K; McCarthy, FMG; Gu, HF				Luo, Zhaohe; Mertens, Kenneth Neil; Bagheri, Siamak; Aydin, Hilal; Takano, Yoshihito; Matsuoka, Kazumi; McCarthy, Francine M. G.; Gu, Haifeng			Cyst-theca relationship and phylogenetic positions of <i>Scrippsiella plana</i> sp nov and <i>S-spinifera</i> (Peridiniales, Dinophyceae)	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						calcareous dinoflagellates; cysts; Duboscquodinium collinii; growth; ITS; Peridinium wisconsinense	CALCAREOUS CYSTS; SEQUENCE DATA; TAXONOMIC CLARIFICATION; ALEXANDRIUM DINOPHYCEAE; TROCHOIDEA DINOPHYCEAE; MARINE DINOFLAGELLATE; MEDITERRANEAN SEA; RIBOSOMAL DNA; MIXED MODELS; CHINA SEA	Species belonging to the dinophyte genus Scrippsiella are frequently reported in marine waters, but information on their distribution in brackish environments is limited. Here we describe a new species, S. plana, through incubation of non-calcified cysts from sediments collected in the South China Sea and Caspian Sea. The vegetative cells consist of a conical epitheca and a rounded hypotheca with the plate formula of Po, X, 4, 3a, 7, 5C+t, 5S, 5, 2. It differs from other Scrippsiella species by its flattened body in dorsoventral view and a small first anterior intercalary (1a) plate (half the size of plate 3a). Scrippsiellaplana strains from the South China Sea and Caspian Sea share identical internal transcribed spacer (ITS) sequences, and show phenotypic plasticity and local adaptation in growth rate at various salinities, consistent with the environments in which they originated. In addition, two strains of S. spinifera were obtained by incubating ellipsoid cysts with calcareous spines from sediments collected along the Turkish and Hawaiian coast. They also share identical ITS sequences and differ from Duboscquodinium collinii (a parasite of tintinnids) only at two base pair positions (in the ITS2 region). Molecular phylogeny based on ITS and large subunit ribosomal DNA (LSU rDNA) sequences revealed that S. plana was nested within the Calciodinellum (CAL) clade and S. spinifera within the S. trochoidea (STR) clade. The phylogenetic position of Peridinium' wisconsinense is reported for the first time, which supports multiple transitions of the Peridiniales to freshwater.	[Luo, Zhaohe; Gu, Haifeng] SOA, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium; [Bagheri, Siamak] AREEO, Iranian Fisheries Sci Inst, Inland Waters Aquaculture Res Ctr, Anzali 66, Iran; [Aydin, Hilal] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, Campus Muradiye, TR-45140 Manisa, Turkey; [Takano, Yoshihito; Matsuoka, Kazumi] Inst East China Sea Res ECSER, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan; [McCarthy, Francine M. G.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Third Institute of Oceanography, Ministry of Natural Resources; Ghent University; Celal Bayar University; Brock 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; Bagheri, Siamak/S-2035-2016; Luo, Zhaohe/ITT-7163-2023; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Gu, Haifeng/0000-0002-2350-9171; Luo, Zhaohe/0000-0001-8662-2414; Bagheri, Siamak/0000-0002-4645-7634; Mertens, Kenneth/0000-0003-2005-9483	National Natural Science Foundation of China [41376170]; public science and technology research funds projects of ocean [201305027]; Higher Education Council of Turkey	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); public science and technology research funds projects of ocean; Higher Education Council of Turkey(Ministry of National Education - Turkey)	Haifeng Gu was supported by the National Natural Science Foundation of China (41376170) and public science and technology research funds projects of ocean (201305027). Kenneth Neil Mertens is a postdoctoral fellow of FWO Belgium. Hilal Aydin was partly supported by Higher Education Council of Turkey.	Abe T.H., 1981, SETO MARINE BIOL LAB, V6, P1, DOI DOI 10.5134/176462; Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Alix B, 2012, NUCLEIC ACIDS RES, V40, pW573, DOI 10.1093/nar/gks485; [Anonymous], 1993, SPEC PUBL NUMBER; 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, NOTAS MUS LA PLATA ZOOL, V20, P111; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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J. Phycol.	MAY	2016	51	2					188	202		10.1080/09670262.2015.1120348	http://dx.doi.org/10.1080/09670262.2015.1120348			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	DI4VG		Bronze			2025-03-11	WOS:000373496900007
J	Abdelmalak, MM; Meyer, R; Planke, S; Faleide, JI; Gernigon, L; Frieling, D; Sluijs, A; Reichart, GJ; Zastrozhnov, D; Theissen-Krah, S; Said, A; Myklebust, R				Abdelmalak, M. M.; Meyer, R.; Planke, S.; Faleide, J. I.; Gernigon, L.; Frieling, Di.; Sluijs, A.; Reichart, G-J.; Zastrozhnov, D.; Theissen-Krah, S.; Said, A.; Myklebust, R.			Pre-breakup magmatism on the Vexing Margin: Insight from new sub-basalt imaging and results from Ocean Drilling Program Hole 642E	TECTONOPHYSICS			English	Article						Pre-breakup; Voring Margin; ODP Hole 642E; Lower Series Flows; Geochemistry-Biostratigraphy; Early Eocene; Emplacement model	ATLANTIC IGNEOUS PROVINCE; EOCENE THERMAL MAXIMUM; OUTER VORING BASIN; CONTINENTAL-MARGIN; CRUSTAL STRUCTURE; NORWEGIAN MARGIN; TECTONIC EVOLUTION; VOLCANIC MARGINS; FLOOD BASALTS; NE ATLANTIC	Improvements in sub-basalt imaging combined with petrological and geochemical observations from the Ocean Drilling Program (ODP) Hole 642E core provide new constraints on the initial breakup processes at the Voring Margin. New and reprocessed high-quality seismic data allow us to identify a new seismic fades unit which we define as the Lower Series Flows. This facies unit is seismically characterized by wavy to continuous subparallel reflections with an internal disrupted and hummocky shape. Drilled lithologies, which we correlate to this facies unit, have been interpreted as subaqueous flows extruding and intruding into wet sediments. Locally, the top boundary of this facies unit is defined as a negative in polarity reflection and referred as the K Reflection. This reflection can be correlated with the spatial extent of pyroclastic deposits, emplaced during transitional shallow marine to subaerial volcanic activities during the rift to drift transition. The drilled Lower Series Flows consist of peraluminous, cordierite bearing peperitic basaltic andesitic to dacitic flows interbedded with thick volcano-sedimentary deposits and intruded sills. The peraluminous geochemistry combined with available. C (from calcite which fills vesicles and fractures), Sr, Nd, and Pb isotopes data points toward upper crustal rock mantle magma interactions with a significant contribution of organic carbon rich pelagic sedimentary material during crustal anatexis. From biostratigraphic analyses, Apectodinium augustum was found in the Lower Series Flows. This dinoflagellate cyst species is a marker for the Paleocene - Eocene Thermal Maximum (PETM). However, based on very high stable carbon isotope ratios of bulk organic matter we exclude that these strata represent the PETM. This implies thatA. augustum was reworked into the early Eocene sediments of this facies unit. Crucially, this unit predates the breakup time of the Voring Margin. Finally, a conceptual emplacement model for the Lower Series Flows facies unit is proposed. This model comprises several stages: (1) the emplacement of subaqueous peperitic basaltic andesitic flows intruding and/or extruding wet sediments; (2) a subaerial to shallow marine volcanism and extrusion of dacitic flows; (3) a proto-breakup phase with intense shallow marine to subaerial explosive volcanism responsible for pyroclastic flow deposits, which can be correlated with the seismic K-Reflection; and (4) the main breakup stage with intense transitional tholeiitic MORB-type volcanism and large subsidence concomitant with the buildup of the Seaward-Dipping Reflector wedge. (C) 2016 Elsevier B.V. All rights reserved.	[Abdelmalak, M. M.; Planke, S.; Faleide, J. I.; Zastrozhnov, D.; Theissen-Krah, S.] Univ Oslo, CEED, N-0316 Oslo, Norway; [Meyer, R.] GFZ German Res Ctr Geosci, Sect Earth Surface Geochem 3 3, D-14473 Potsdam, Germany; [Planke, S.] VBPR, Oslo Sci Pk, N-0349 Oslo, Norway; [Gernigon, L.] Geol Survey Norway NGU, Leiv Erikssons Vei 39, Trondheim, Norway; [Frieling, Di.; Sluijs, A.] Univ Utrecht, Dept Earth Sci, Marine Palynol & Paleoceanog, Lab Palaeobot & Palynol,Fac Geosci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Reichart, G-J.] Univ Utrecht, Dept Earth Sci, Fac Geosci, Heidelberglaan 2, NL-3584 CS Utrecht, Netherlands; [Reichart, G-J.] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands; [Theissen-Krah, S.] GEOMAR Helmholtz Ctr Ocean Res Kiel, Wischhofstr 1-3, D-24148 Kiel, Germany; [Said, A.] Kalkulo AS, Simula Res Lab, Martin Linges Vei 25, N-1364 Fornebu, Norway; [Myklebust, R.] TGS, Lensmannslia 4, N-1386 Asker, Norway	University of Oslo; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; Geological Survey of Norway; Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Abdelmalak, MM (通讯作者)，Univ Oslo, CEED, N-0316 Oslo, Norway.	m.m.abdelmalak@geo.uio.no	Planke, Sverre/AAE-1721-2021; Zastrozhnov, Dmitry/AAM-9704-2020; Sluijs, Appy/B-3726-2009; Reichart, Gert-Jan/N-6308-2018	Frieling, Joost/0000-0002-5374-1625; Sluijs, Appy/0000-0003-2382-0215; Theissen-Krah, Sonja/0000-0002-6163-5515; Zastrozhnov, Dmitry/0000-0003-2354-4708; Reichart, Gert-Jan/0000-0002-7256-2243; Planke, Sverre/0000-0001-6128-2193	Norwegian Research Council through Centre of Excellence CEED (Centre for Earth Evolution and Dynamics) [210429/E30]; European Research Council (ERC) under European Union; ERC [259627]; European Research Council (ERC) [259627] Funding Source: European Research Council (ERC)	Norwegian Research Council through Centre of Excellence CEED (Centre for Earth Evolution and Dynamics); European Research Council (ERC) under European Union(European Research Council (ERC)); ERC(European Research Council (ERC)); European Research Council (ERC)(European Research Council (ERC))	Founding for this work came from the OMNIS Project: Offshore Mid Norwegian: Integrated Margin and Basin Studies (Project Number: 210429/E30) funded by the Norwegian Research Council through its Centre of Excellence CEED (Centre for Earth Evolution and Dynamics). The European Research Council (ERC) under the European Union Seventh Framework Program provided funding for this work by ERC Starting Grant 259627 to Sluijs. We thank Stella Heijnens and Arnold van Dijk for generating delta<SUP>13</SUP>C data and Natasja Welters for palynological sample preparation (all at Utrecht University). Seismic interpretation was done using HS: Kingdom software. Grid interpolations and map compilations were established using Geosoft Oasis Montaj and ArcGis software. We thank Jan. Hertogen, an anonymous reviewer, and the editor for useful comments that improved the paper.	Abdelmalak MM, 2012, TECTONOPHYSICS, V581, P132, DOI 10.1016/j.tecto.2011.11.020; Abdelmalak M.M., 2016, DEV ESCARPMENT UNPUB; Abdelmalak MM, 2015, GEOLOGY, V43, P1011, DOI 10.1130/G37086.1; [Anonymous], 2010, TRANSITION SPATIO TE; [Anonymous], 1999, PETROLEUM GEOLOGY C, DOI DOI 10.1144/0050041; [Anonymous], 1981, Geol. 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J	Cvetkovic, M; Grego, M; Turk, V				Cvetkovic, Martina; Grego, Mateja; Turk, Valentina			The efficiency of a new hydrodynamic cavitation pilot system on <i>Artemia salina</i> cysts and natural population of copepods and bacteria under controlled mesocosm conditions	MARINE POLLUTION BULLETIN			English	Article						Hydrodynamic cavitation; Ballast water; Copepods; Artemia salina cysts; Heterotrophic marine bacteria	BALLAST WATER MANAGEMENT; DINOFLAGELLATE CYSTS; MEDITERRANEAN SEA; PROTEIN-SYNTHESIS; BY-PRODUCTS; ZOOPLANKTON; SHIPS; OCEAN; PHYTOPLANKTON; ORGANISMS	A study of the efficiency of hydrodynamic cavitation and separation was carried out to evaluate an innovative, environmentally safe and acceptable system for ballast water treatment for reducing the risk of introducing non-native species worldwide. Mesocosm experiments were performed to assess the morphological changes and viability of zooplankton (copepods), Artemia salina cysts, and the growth potential of marine bacteria after the hydrodynamic cavitation treatment with a different number of cycles. Our preliminary results confirmed the significant efficiency of the treatment since more than 98% of the copepods and A. salina cysts were damaged, in comparison with the initial population. The efficiency increased with the number of the hydrodynamic cavitation cycles, or in combination with a separation technique for cysts. There was also a significant decrease in bacterial abundance and growth rate, compared to the initial number and growth potential. (C) 2016 Elsevier Ltd. All rights reserved.	[Cvetkovic, Martina] Univ Ljubljana, Fac Civil & Geodet Engn, Dept Environm Civil Engn, Hajdrihova 28, Ljubljana 1000, Slovenia; [Grego, Mateja; Turk, Valentina] Natl Inst Biol, Marine Biol Stn Piran, SI-6330 Piran, Slovenia	University of Ljubljana; National Institute of Biology - Slovenia	Cvetkovic, M (通讯作者)，Univ Ljubljana, Fac Civil & Geodet Engn, Dept Environm Civil Engn, Hajdrihova 28, Ljubljana 1000, Slovenia.	martina_cvetkovic@yahoo.com	turk, Valentina/AAV-8033-2020					Abatzopoulos TJ, 2003, BELG J ZOOL, V133, P103; [Anonymous], PRINCIPLES MODERN MI; [Anonymous], GUIDELINES APPL BALL; [Anonymous], ABS GUID BALL WAT EX; [Anonymous], EMERGING RISKS BALLA; [Anonymous], 2004, INT CONVENTION CONTR; [Anonymous], 2014, UND BALL WAT MAN GUI; [Anonymous], PHI75005 FAOUNDOBFAR; [Anonymous], CAV 2003 5 INT S CAV; [Anonymous], 55213 IMP MEPC; [Anonymous], THESIS TEXAS A M U T; [Anonymous], DISS ABSTR INT; [Anonymous], MANUAL HARMFUL MARIN; [Anonymous], 2001, Methods in microbiology; Bakalar G, 2014, SPRINGERPLUS, V3, DOI 10.1186/2193-1801-3-468; 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Zhang NH, 2013, CHEM ENG J, V231, P427, DOI 10.1016/j.cej.2013.07.055	83	5	5	2	21	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0025-326X	1879-3363		MAR POLLUT BULL	Mar. Pollut. Bull.	APR 15	2016	105	1					341	350		10.1016/j.marpolbul.2016.01.030	http://dx.doi.org/10.1016/j.marpolbul.2016.01.030			10	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	DL7JC	26902683				2025-03-11	WOS:000375816000053
J	Richlen, ML; Zielinski, O; Holinde, L; Tillmann, U; Cembella, A; Lyu, YH; Anderson, DM				Richlen, Mindy L.; Zielinski, Oliver; Holinde, Lars; Tillmann, Urban; Cembella, Allan; Lyu, Yihua; Anderson, Donald M.			Distribution of <i>Alexandrium fundyense</i> (Dinophyceae) cysts in Greenland and Iceland, with an emphasis on viability and growth in the Arctic	MARINE ECOLOGY PROGRESS SERIES			English	Article						Arctic; Alexandrium; Dinoflagellate; Cysts; Harmful algal bloom	DINOFLAGELLATE RESTING CYSTS; TAMARENSE LEBOUR BALECH; SPATIAL-DISTRIBUTION; DISKO BAY; SURFACE SEDIMENTS; PUGET-SOUND; RED TIDE; WEST; TEMPERATURE; GERMINATION	The bloom-forming dinoflagellate Alexandrium fundyense has been extensively studied due its toxin-producing capabilities and consequent impacts on human health and economies. This study investigated the prevalence of resting cysts of A. fundyense in western Greenland and Iceland, to assess the historical presence and magnitude of bloom populations in the region, and to characterize environmental conditions during summer, when bloom development may occur. Analysis of sediments collected from these locations showed that A. fundyense cysts were present at low to moderate densities in most areas surveyed, with highest densities observed in western Iceland. Additionally, laboratory experiments were conducted on clonal cultures established from isolated cysts or vegetative cells from Greenland, Iceland, and the Chukchi Sea (near Alaska) to examine the effects of photoperiod interval and irradiance levels on growth. Growth rates in response to the experimental treatments varied among isolates, but were generally highest under conditions that included both the shortest photoperiod interval (16 h light:8 h dark) and higher irradiance levels (similar to 146 to 366 mu mol photons m(-2) s(-1)), followed by growth under an extended photoperiod interval and low irradiance level (similar to 37 mu mol photons m-(2) s-(1)). Based on field and laboratory data, we hypothesize that blooms in Greenland are primarily derived from advected A. fundyense populations, as low bottom temperatures and limited light availability would likely preclude in situ bloom development. In contrast, the bays and fjords in Iceland may provide more favorable habitat for germling cell survival and growth and therefore may support indigenous, self-seeding blooms.	[Richlen, Mindy L.; Lyu, Yihua; Anderson, Donald M.] Woods Hole Oceanog Inst, 266 Woods Hole Rd,MS 32, Woods Hole, MA 02543 USA; [Zielinski, Oliver; Holinde, Lars] Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm, D-26111 Oldenburg, Germany; [Tillmann, Urban; Cembella, Allan] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Handelshafen 12, D-27570 Bremerhaven, Germany; [Lyu, Yihua] Xiamen Univ, Sch Life Sci, State Key Lab Marine Environm Sci, Xiamen 361102, Peoples R China	Woods Hole Oceanographic Institution; Carl von Ossietzky Universitat Oldenburg; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Xiamen University	Richlen, ML (通讯作者)，Woods Hole Oceanog Inst, 266 Woods Hole Rd,MS 32, Woods Hole, MA 02543 USA.	mrichlen@whoi.edu	Zielinski, Oliver/P-4643-2019	Zielinski, Oliver/0000-0002-6018-5030; Cembella, Allan/0000-0002-1297-2240	Helmholtz Institute initiative Earth and Environment under the PACES Program Topic 2 Coast; Alfred Wegener Institute; Woods Hole Center for Oceans and Human Health through National Science Foundation (NSF) Grant [OCE-1314642]; National Institute of Environmental Health Sciences (NIEHS) Grant [1-P01-ES021923-01]; Captain Klaus Bergman and crew; James M. and Ruth P. Clark Arctic Research Initiative; Directorate For Geosciences; Division Of Ocean Sciences [1314642] Funding Source: National Science Foundation	Helmholtz Institute initiative Earth and Environment under the PACES Program Topic 2 Coast; Alfred Wegener Institute; Woods Hole Center for Oceans and Human Health through National Science Foundation (NSF) Grant(National Science Foundation (NSF)); National Institute of Environmental Health Sciences (NIEHS) Grant; Captain Klaus Bergman and crew; James M. and Ruth P. Clark Arctic Research Initiative; Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	Funding for this study was provided by the James M. and Ruth P. Clark Arctic Research Initiative to D.M.A. and M.L.R., and for the ARCHEMHAB expedition via the Helmholtz Institute initiative Earth and Environment under the PACES Program Topic 2 Coast (Workpackage 3) of the Alfred Wegener Institute. The research is part of the SCOR/IOC GEOHAB Core Research Project on HABs in Fjords and Coastal Embayments. Additional support was provided by the Woods Hole Center for Oceans and Human Health through National Science Foundation (NSF) Grant OCE-1314642 and National Institute of Environmental Health Sciences (NIEHS) Grant 1-P01-ES021923-01. We are grateful to Daniela Voss, Daniela Meier, and Rohan Henkel for their assistance during the cruise, and for helping to prepare the figures. We also thank Prof. Haifeng Gu for providing sediments from the Chukchi Sea, and Kerry Norton, Dave Kulis, John Brinckerhoff, Bruce Keafer, Lauren Henry, Hovey Clifford, and Judy Kleindinst for logistical and laboratory support and assistance. Finally, we acknowledge the generous support and assistance provided by Captain Klaus Bergman and crew of the RV 'Maria S. Merian' throughout the cruise.	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Ecol.-Prog. Ser.	APR 7	2016	547						33	46		10.3354/meps11660	http://dx.doi.org/10.3354/meps11660			14	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	DJ5IT	27721528	Green Submitted, Green Accepted			2025-03-11	WOS:000374241200003
J	Chekar, M; Slimani, H; Guédé, KE; Aassoumi, H; Asebriy, L				Chekar, Mouna; Slimani, Hamid; Guede, Kore Elysee; Aassoumi, Habiba; Asebriy, Lahcen			Eocene dinoflagellate cyst biostratigraphy and paleoenvironments from the Ibn Batouta section, Tangier region, westernmost External Rif Morocco	ANNALES DE PALEONTOLOGIE			French	Article						Eocene; Dinoflagellate cysts; Biostratigraphy; Paleoenvironments; Ibn Batouta section; MECO; Morocco	CRETACEOUS-PALEOGENE BOUNDARY; SEA-LEVEL CHANGES; OULED HADDOU; TERTIARY BOUNDARY; MIDDLE EOCENE; EL-KEF; MIOCENE; STRATIGRAPHY; BASIN; GREENHOUSE	Palynological investigations of Eocene sediments from the Ibn Batouta section, located in the external Tangier Unit (western External Rif, northwestern Morocco), revealed the presence of well-preserved figured organic matter, rich in dinoflagellate cysts. Qualitative and quantitative analysis of palynological content, mainly dinoflagellate cysts, allowed a biostratigraphic subdivision and a paleoenvironmental reconstruction of these deposits. The dinoflagellate cyst events used for the characterization of the Middle Eocene (Lutetian and Bartonian) in the lower part of the Ibn Batouta section are: the first and last appearances of Castellodinium compactum, Distatodinium craterum, Distatodinium ellipticum, Distatodinium pilosum, Hystrichokolpoma salacia, Phthanoperidinium geminatum, Polysphaeridium biformum, Rhombodinium spinula, Ynezidinium brevisulcatum, the first appearance of Homonyblium floripes and the last appearance of Hystrichokolpoma bullatum. The disappearance of most of these species and the last appearance of Deflandrea phosphoritica are used for deduction of an Upper Eocene-Lower Oligocene age for the upper part of the section. Relative abundance changes of selected dinoflagellate cyst groups and continental palynomorphs (spores and pollen) allowed to highlight, in ascending order, five different marine environments: (1) neritic coastal with important nutrient availability at the base of the section; (2) outer neritic at the beginning of a transgressive phase in the Lutetian; (3) deeper outer neritic to oceanic in full transgressive phase in the Bartonian; (4) probably shallower outer neritic at the beginning of a regressive phase in the upper Bartonian; (5) coastal, probably estuarine in full regressive phase in the Upper Eocene-Lower Oligocene interval. These paleoenvironmental changes coincide with the global climate changes of the Middle Eocene Climatic Optimurn (MECO). (C) 2016 Elsevier Masson SAS. All rights reserved.	[Chekar, Mouna; Slimani, Hamid; Guede, Kore Elysee; Asebriy, Lahcen] Mohammed V Univ Rabat, Inst Sci, Dept Sci Terre, Lab Geol & Teledetect, Ave Ibn Batouta,BP 703, Rabat, Morocco; [Chekar, Mouna; Aassoumi, Habiba] Univ Abdelmalek Essaadi, Fac Sci, Dept Sci Terre, Lab Cartog & Technol Numer, Tetouan, Morocco; [Guede, Kore Elysee] Univ Felix Houphouet Boigny, UFR STRM, 22,BP 582, Abidjan, Cote Ivoire	Mohammed V University in Rabat; Abdelmalek Essaadi University of Tetouan; Universite Felix Houphouet-Boigny	Slimani, H (通讯作者)，Mohammed V Univ Rabat, Inst Sci, Dept Sci Terre, Lab Geol & Teledetect, Ave Ibn Batouta,BP 703, Rabat, Morocco.	h_slimani@yahoo.com	Elysee, Guede/ABE-3209-2021; Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913; Kore Elysee, Guede/0000-0003-1393-5078				ANDRIEUX J, 1971, EARTH PLANET SC LETT, V12, P191, DOI 10.1016/0012-821X(71)90077-X; [Anonymous], 9210 GEOL SURV CAN; [Anonymous], 1996, Palynology: principles and applications; Benyaich A., 1991, THESIS; Bijl PK, 2010, SCIENCE, V330, P819, DOI 10.1126/science.1193654; Bohaty SM, 2003, GEOLOGY, V31, P1017, DOI 10.1130/G19800.1; Bohaty SM, 2009, PALEOCEANOGRAPHY, V24, DOI 10.1029/2008PA001676; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; Brinkhuis H, 1994, GFF, V116, P46, DOI 10.1080/11035899409546146; Chalouan A, 2001, B SOC GEOL FR, V172, P603, DOI 10.2113/172.5.603; Crouch E.M., 2003, CAUSES CONSEQUENCES, V369, P113, DOI DOI 10.1130/0-8137-2369-8.113; Crouch EM, 2005, MAR MICROPALEONTOL, V56, P138, DOI 10.1016/j.marmicro.2005.05.002; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Durand-Delga M, 2000, CR ACAD SCI II A, V331, P29, DOI 10.1016/S1251-8050(00)01378-1; Durand-Delga M., 1980, Livre Jubilaire de la Societe geologique de France, V10, P203; ESHET Y, 1992, MAR MICROPALEONTOL, V18, P199, DOI 10.1016/0377-8398(92)90013-A; Fauconnier D., 2004, Les dinoflagelles fossile. 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J	Elshanawany, R; Zonneveld, KAF				Elshanawany, Rehab; Zonneveld, Karin A. F.			Dinoflagellate cyst distribution in the oligotrophic environments of the Gulf of Aqaba and northern Red Sea	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Gulf of Aqaba; Northern Red Sea; Oligotrophic environment	SURFACE SEDIMENTS; PHYTOPLANKTON DYNAMICS; MEDITERRANEAN-SEA; UPWELLING SYSTEM; BRITISH-COLUMBIA; HIGH-LATITUDES; FRESH-WATER; ASSEMBLAGES; MARINE; BAY	Oligotrophic environmental systems form a major part of the marine aquatic environments on earth. Compared to mesotrophic and eutrophic environments extremely little information is available about the relationship between the distribution of organic-walled dinoflagellate cysts and physical and biological gradients in the upper water column. Here we present the first comprehensive study of the modern geographic distribution of organic-walled dinoflagellate cysts in the oligotrophic environments of the northern Red Sea and Gulf of Aqaba. We show that sediments of both regions have characteristic dinoflagellate cyst associations consisting of both heterotrophic and phototrophic species of which the latter, including both autotrophic and mixotrophic species, form the major part of the associations in both regions. The upper water environment of the Gulf of Aqaba is characterized by slightly enhanced nutrient concentrations compared to the Red Sea, due to water column mixing in winter. Its phytoplankton composition is dominated by pico- and ultra-plankton and a slight higher amount of eukaryotes compared to northern Red Sea. Its sedimentary cyst associations are characterized by higher relative and absolute abundances of the species Brigantedinium spp., Votadinium calvum, Echinidinium spp., Lingulodinium machaerophorum, Spiniferites spp., Spiniferites bentorii, Spiniferites membranaceus and Spiniferites mirabilis. Sediments of the northern Red Sea are characterized by high relative abundances of Impagidinium aculeatum, Impagidinium sphaericum, Operculodinium israelianum, Operculodinium longispinigerum, Operculodinium centrocarpum, cysts of Pentapharsodinium dalei, and Selenopemphix nephroides. A positive relationship between the distribution of the heterotrophic species Brigantedinium spp., Echinidinium spp. and V. calvum with the occurrence of other eukaryotic groups such as e.g. diatoms is documented. The distribution of S. nephroides cannot be related to the presence of diatom occurrences and it is suggested that the distribution of food sources other than diatoms affects its distribution. We document a positive relationship between the sedimentary distribution of the phototrophic dinoflagellate species L machaeropho rum and Spiniferites species and the abundance of the cyanobacteria Synechococcus in the water column. Since Synechococcus is known to be a potential prey of Lingulodinium polyedrum and members of the Gonyaulax spinifera complex (the motile forms producing these cysts) we suggest a possible cyst distribution-prey relationship of mixotrophic dinoflagellates. (C) 2016 Elsevier B.V. All rights reserved.	[Elshanawany, Rehab; Zonneveld, Karin A. F.] Univ Bremen, MARUM, Leobener Str, D-28359 Bremen, Germany; [Elshanawany, Rehab] Univ Alexandria, Fac Sci, Baghdad St, Moharam Bey 21511, Egypt; [Zonneveld, Karin A. F.] Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany	University of Bremen; Egyptian Knowledge Bank (EKB); Alexandria University; University of Bremen	Zonneveld, KAF (通讯作者)，Univ Bremen, MARUM, Leobener Str, D-28359 Bremen, Germany.	rehab_shanawany@yahoo.com			German Science Foundation (DFG); Egyptian Cultural Affairs and Missions Sector	German Science Foundation (DFG)(German Research Foundation (DFG)); Egyptian Cultural Affairs and Missions Sector(Ministry of Higher Education & Scientific Research (MHESR))	This research is funded by the German Science Foundation (DFG) funded centre of excellence MARUM and the Egyptian Cultural Affairs and Missions Sector in form of a scholarship of Dr. R. Elshanawany.	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Micropaleontol.	APR	2016	124						29	44		10.1016/j.marmicro.2016.01.003	http://dx.doi.org/10.1016/j.marmicro.2016.01.003			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DL6GK					2025-03-11	WOS:000375737500003
J	Ning, WX; Ghosh, A; Jilbert, T; Slomp, CP; Khan, M; Nyberg, J; Conley, DJ; Filipsson, HL				Ning, Wenxin; Ghosh, Anupam; Jilbert, Tom; Slomp, Caroline P.; Khan, Mansoor; Nyberg, Johan; Conley, Daniel J.; Filipsson, Helena L.			Evolving coastal character of a Baltic Sea inlet during the Holocene shoreline regression: impact on coastal zone hypoxia	JOURNAL OF PALEOLIMNOLOGY			English	Article						Hypoxia; Baltic Sea; Holocene; Biogeochemistry; Dinoflagellate cyst; Coastal zone	DINOFLAGELLATE CYST RECORD; CLIMATE-CHANGE; LAND-USE; TEMPERATURE RECONSTRUCTION; CYANOBACTERIA BLOOMS; ENVIRONMENTAL-CHANGE; HYDROLOGICAL CHANGES; ORGANIC-MATTER; CENTRAL SWEDEN; VARIABILITY	Although bottom water hypoxia (O-2 < 2 mg L-1) is presently widespread in the Baltic Sea coastal zone, there is a lack of insight into past changes in bottom water oxygen in these areas on timescales of millennia, and the possible driving factors. Here, we present a sediment-based environmental reconstruction of surface water productivity, salinity and bottom water oxygen for the past 5400 years at GAyensfjarden, a coastal site in SE Sweden. As proxies, we use dinoflagellate cysts, benthic foraminifera, organic carbon (C-org), biogenic silica (BSi), C-org/N-tot, C-org/P-tot, Ti/Al, K/Al and grain size distribution. The chronology of the sediment sequence is well constrained, based on Pb-210, Cs-137 and AMS C-14 dates. Between 3400 and 2100 BCE, isostatic conditions favored enhanced deep water exchange between GAyensfjarden and the open Baltic Sea. At that time, GAyensfjarden was characterized by relatively high productivity and salinity, as well as frequently occurring hypoxic-anoxic bottom water, despite the relatively large connection with the Baltic Sea. The most severe interval of oxygen depletion is recorded between 2400 and 2100 BCE, and appears to coincide with a similar hypoxic event in the Gotland Basin in the open Baltic Sea. As regional climate became wetter and colder between 2100 BCE and 700 BCE, salinity declined and bottom water oxygen conditions improved. Throughout the record, grain size, Ti/Al and K/Al data indicate an evolution towards a more enclosed coastal system, as suggested by reconstructions of the post-glacial shoreline regression. GAyensfjarden shifted to close to modern conditions after 700 BCE, and was characterized by less hypoxia and lower salinity compared with 3400-700 BCE. The timing of the shift corresponds with the Sub-Boreal/Sub-Atlantic transition in Europe. Human-induced erosion in the catchment is observed as early as 600 CE, and is particularly prominent since regional copper mining activity increased around 1700 CE. A sharp increase in sediment C-org concentration is recorded since the 1950s, indicating significant anthropogenic impact on biogeochemical cycles in the coastal zone, as observed elsewhere in the Baltic Sea.	[Ning, Wenxin; Ghosh, Anupam; Khan, Mansoor; Conley, Daniel J.; Filipsson, Helena L.] Lund Univ, Dept Geol, Solvegatan12, S-22362 Lund, Sweden; [Ghosh, Anupam] Jadavpur Univ, Dept Geol Sci, Ctr Adv Study, Kolkata 700032, India; [Jilbert, Tom; Slomp, Caroline P.] Univ Utrecht, Fac Geosci, Dept Earth Sci, POB 80-021, NL-3508 TA Utrecht, Netherlands; [Jilbert, Tom] Univ Helsinki, Dept Environm Sci, POB 65, FIN-00014 Helsinki, Finland; [Nyberg, Johan] Geol Survey Sweden, Box 670, S-75128 Uppsala, Sweden	Lund University; Jadavpur University; Utrecht University; University of Helsinki	Ning, WX (通讯作者)，Lund Univ, Dept Geol, Solvegatan12, S-22362 Lund, Sweden.	wenxin.ning@geol.lu.se; anupam.ghosh@gmail.com; tom.jilbert@helsinki.fi; c.p.slomp@uu.nl; mansoorswati@yahoo.com; johan.nyberg@sgu.se; daniel.conley@geol.lu.se; helena.filipsson@geol.lu.se	Slomp, Caroline/A-9406-2012; Jilbert, Tom/AAL-2273-2021; Ghosh, Anupam/AAK-4306-2020; Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608; Conley, Daniel Joseph/0000-0001-9668-9284	FORMAS Strong Research Environment: Managing Multiple Stressors in the Baltic Sea [217-2010-126]; Crafoord Foundation; Royal Physiographic Society in Lund; Netherlands Organization for Scientific Research (NWO Vidi) [86405.004]; Netherlands Organization for Scientific Research (NWO ERC) [278364]; BONUS [Art 185]; EU; FORMAS; Swedish Agency for Marine and Water Management (SWAM)	FORMAS Strong Research Environment: Managing Multiple Stressors in the Baltic Sea(Swedish Research Council Formas); Crafoord Foundation; Royal Physiographic Society in Lund; Netherlands Organization for Scientific Research (NWO Vidi)(Netherlands Organization for Scientific Research (NWO)); Netherlands Organization for Scientific Research (NWO ERC); BONUS; EU(European Union (EU)); FORMAS(Swedish Research Council Formas); Swedish Agency for Marine and Water Management (SWAM)	We thank the captain and crew of R/V Ocean Surveyor for help during sampling. We thank Nathalie V. Putten and A Asa Wallin for guidance during grain size analysis. Anna Brostrom, Svante Bjorck, Anne Birgitte Nielsen and Conny Lenz are thanked for helpful discussions. Conny Lenz, Vincent Kofman and Leo de Jong assisted with sediment sampling and lab analysis. The project was funded by FORMAS Strong Research Environment: Managing Multiple Stressors in the Baltic Sea (217-2010-126). We also acknowledge funding from the Crafoord Foundation, the Royal Physiographic Society in Lund, and the Netherlands Organization for Scientific Research (NWO Vidi 86405.004 and ERC Starting Grant #278364). This work also resulted from the BONUS COCOA project supported by BONUS (Art 185), funded jointly by the EU and FORMAS. The hydrographic data used in the project were collected from SMHI's database-SHARK. The SHARK data collection is organized by the environmental monitoring program and funded by the Swedish Agency for Marine and Water Management (SWAM).	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Paleolimn.	APR	2016	55	4					319	338		10.1007/s10933-016-9882-6	http://dx.doi.org/10.1007/s10933-016-9882-6			20	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	DI2CW					2025-03-11	WOS:000373304300002
J	Han, M; Lee, H; Anderson, DM; Kim, B				Han, Myungsoo; Lee, Haeok; Anderson, Donald M.; Kim, Baikho			Paralytic shellfish toxin production by the dinoflagellate <i>Alexandrium pacificum</i> (Chinhae Bay, Korea) in axenic, nutrient-limited chemostat cultures and nutrient-enriched batch cultures	MARINE POLLUTION BULLETIN			English	Article						Alexandrium pacificum; Batch cultures; Chemostat; Dinoflagellate; Nutrient enrichment and limitation; PSP toxin	PROTOGONYAULAX-TAMARENSIS; PHOSPHORUS LIMITATION; ANTIBIOTIC TREATMENTS; GENUS ALEXANDRIUM; GENETIC-MARKERS; RESTING CYSTS; CELL-CYCLE; GROWTH; TOXICITY; FUNDYENSE	Blooms of Alexandrium pacificum (formerly Alexandrium tamarense) are common in Chinhae Bay (Korea), presumably linked to anthropogenic eutrophication. Here we examine PSP toxin content and composition in axenic chemostat and batch cultures of A. pacificum using growth conditions that differed according to dilution rate, nutrient limitations, and enrichments. Phosphate (P)-limited cells in chemostat cultures had higher toxin content and a toxin composition that differed from that of nitrogen (N)-limited cells at the highest growth rates. Therefore, toxin composition changes do occur in axenic cultures of A. pacificum following extended growth under steady state conditions. In nutrient -limited batch cultures that received N and P enrichment, the N-enriched cultures showed a more diverse toxin profile than the P-enriched cells; the toxin content of N-enriched cells was lower than in the P-enriched cultures. We infer the following order for the biosynthesis of individual toxins: C1, C2 > GTX3 > GTX1 > neoSTX. (C) 2016 Elsevier Ltd. All rights reserved.	[Han, Myungsoo; Lee, Haeok; Kim, Baikho] Hanyang Univ, Dept Life Sci, Seoul 04763, South Korea; [Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	Hanyang University; Woods Hole Oceanographic Institution	Kim, B (通讯作者)，Hanyang Univ, Dept Life Sci, Seoul 04763, South Korea.	tigerk@hanyang.ac.kr	Kim, Baik-Ho/D-9356-2011		Hanyang University [HY-201200000000731-N]; National Science Foundation [OCE-1314642]; National Institute of Environmental Health Sciences [1-P01-ES021923-01]; Woods Hole Center for Oceans and Human Health; Directorate For Geosciences; Division Of Ocean Sciences [1314642] Funding Source: National Science Foundation	Hanyang University; 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)); Woods Hole Center for Oceans and Human Health; Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This work was supported by the research fund of Hanyang University (HY-201200000000731-N). The authors would like to thank Prof. Omura of Tokyo University of Fisheries for his kind advice regarding the culture of axenic Alexandrium. Support for D. M. Anderson was provided 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.	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Pollut. Bull.	MAR 15	2016	104	1-2					34	43		10.1016/j.marpolbul.2016.01.057	http://dx.doi.org/10.1016/j.marpolbul.2016.01.057			10	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	DJ4SK	26874747	Green Accepted, Bronze			2025-03-11	WOS:000374198100017
J	Prebble, JG; Crouch, EM; Cortese, G; Carter, L; Neil, H; Bostock, H				Prebble, Joseph G.; Crouch, Erica M.; Cortese, Giuseppe; Carter, Lionel; Neil, Helen; Bostock, Helen			Southwest Pacific sea surface conditions during Marine Isotope Stage 11-Results from dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						MIS11; Dinoflagellate cysts; Sea surface temperature; Productivity; Subtropical Front; SW Pacific	EASTERN NEW-ZEALAND; SOUTHEASTERN NEW-ZEALAND; SOUTHERN-HEMISPHERE MIDLATITUDES; SUBTROPICAL CONVERGENCE REGION; RED-TIDE DINOFLAGELLATE; TASMAN SEA; AUSTRALIAN CURRENT; INDIAN-OCEAN; CHATHAM RISE; DEEP-OCEAN	Dinoflagellate cyst (dinocyst) assemblages are examined from three SW Pacific marine sediment cores covering Marine Isotope Stage 11 (MIS11, 423 Ica-380 Ica). MDO6-2988 and MDO6-2989 are in the east Tasman Sea, north of the Subtropical Front (STF), whilst DSDP594 is in Subantarctic surface waters (SAW) off eastern New Zealand. Sea surface temperature (SST) estimates from dinocyst assemblages indicate that the east Tasman Sea was similar to 2.5 degrees C warmer than present during the peak warmth of MIS11. In the east Tasman Sea, north of the STF, there is a two-step warming into MIS11 in cores MD06-2988 and MDOG-2989. East of New Zealand and south of the STF, at core site DSDP594, dinocyst SST estimates suggest that MIS11 was an extended warm period similar to, or slightly warmer than, present conditions, although data from the early phase (prior to 417 ka) may be compromised due to insufficient modern analogues. At all sites, glacial/interglacial climatic fluctuations were accompanied by large assemblage changes. Glacial intervals were characterised by higher abundances of assemblages typical of SAW (Nematosphaeropsis labyrinthus, Selenopemphix antarctica +/- Brigantedinium spp). Subtropical surface water (STW) assemblages dominated during the interglacial in the east Tasman Sea (including Impagidinium aculeatum, I. patulum, and Spiniferites mirabilis), whilst assemblages consistent with continued SAW influence remained during the interglacial at core site DSDP594, albeit with reduced cold water indicators such as S. antarctica. The changes are particularly pronounced in the east Tasman Sea, where the STF is inferred to have been located further north during glacials MIS12 and MIS10. The influence of STW at DSDP594 during MIS11 and the Holocene is inferred to have been less than during MIS5e. A qualitative dinocyst-based index likely reflecting primary productivity (also influenced by oxygen concentration on the sea floor) is broadly anti-phased with SST on glacial-interglacial timescales at all sites. (C) 2016 Elsevier B.V. All rights reserved.	[Prebble, Joseph G.; Crouch, Erica M.; Cortese, Giuseppe] GNS Sci, POB 30 368, Lower Hutt 5040, New Zealand; [Carter, Lionel] Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand; [Neil, Helen; Bostock, Helen] 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 30 368, Lower Hutt 5040, New Zealand.	j.prebble@gns.cri.nz	Crouch, Erica/C-2820-2013; Cortese, Giuseppe/C-8281-2011; Bostock, Helen/A-6834-2013	Bostock, Helen/0000-0002-8903-8958; Cortese, Giuseppe/0000-0003-1780-3371; Prebble, Joseph/0000-0002-7268-4187	New Zealand government "Bright Futures" graduate scholarship; GNS Science through its Global Change through Time (GCT) Programme; FRST funded Antarctica New Zealand Interglacial Climate Extremes (ANZICE) programme; Consequences of Earth, Ocean Change (CEOC) Programme; NIWA core funding	New Zealand government "Bright Futures" graduate scholarship; GNS Science through its Global Change through Time (GCT) Programme; FRST funded Antarctica New Zealand Interglacial Climate Extremes (ANZICE) programme; Consequences of Earth, Ocean Change (CEOC) Programme; NIWA core funding	We thank the crew and science party of the RN Marion Dufresne MD152 (MATACORE) cruise, and those involved with DSDP Leg 90. Sonja Fry and Roger Tremain at GNS Science assisted with palynological processing. Bruce Hayward shared five unpublished foraminifera census counts from MD06-2989, and Matt Ryan and Brent Alloway shared unpublished data on their identification of tephra at DSDP594. JP was supported by a New Zealand government "Bright Futures" graduate scholarship. JP, 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. HN and HB were supported by the Consequences of Earth, Ocean Change (CEOC) Programme and NIWA core funding. We thank the three anonymous reviewers for their constructive comments that have improved this manuscript.	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Paleoclimatol. Paleoecol.	MAR 15	2016	446						19	31		10.1016/j.palaeo.2016.01.007	http://dx.doi.org/10.1016/j.palaeo.2016.01.007			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	DF7QP					2025-03-11	WOS:000371553000003
J	Lambert, O; Louwye, S				Lambert, Olivier; Louwye, Stephen			A NEW EARLY PLIOCENE SPECIES OF <i>MESOPLODON</i>: A CALIBRATION MARK FOR THE RADIATION OF THIS SPECIES-RICH BEAKED WHALE GENUS	JOURNAL OF VERTEBRATE PALEONTOLOGY			English	Article							DINOFLAGELLATE CYST STRATIGRAPHY; BASIN NORTHERN BELGIUM; MIDDLE MIOCENE; CETACEA; ZIPHIIDAE; ODONTOCETI; PALEOECOLOGY; RESURRECTION; PLEISTOCENE; SYSTEMATICS	Including at least 15 extant species, the beaked whale genus Mesoplodon (Cetacea, Odontoceti, Ziphiidae) is by far the most species-rich cetacean genus. Such a high diversity reflects one or several pulses of radiation, most likely involving a sexual selection mechanism affecting shape, size, and position of mandibular tusks. However, the tempo of this diversification is currently poorly constrained due to the scarce fossil record. Based on the reassessment of five partial skulls discovered in Antwerp (north of Belgium), a new fossil species of the genus Mesoplodon, M. posti, sp. nov., is described. Only the second fossil species of the genus currently recognized, it is characterized (among other features) by: transverse sections of the rostrum higher than wide (a feature proposed to correspond to the presence of lower tusks more posterior than the apex of the mandibles); the presence of a basirostral groove at the rostrum base; pentagonal joined nasals; the posterior projection of the premaxilla in the vertex shorter than the nasal backward; and a strong transverse compression of the frontals behind the nasals. Our phylogenetic analysis results in M. posti being nested among extant species of Mesoplodon. Palynological study of the organic-walled phytoplankton from sediment retained in cranial cavities of several specimens indicates an age between 4.86 and 3.9Ma (Zanclean, early Pliocene). Constituting the first temporally well-constrained fossil species of Mesoplodon, M. posti provides an upper calibration point for the beginning of the radiation(s), having produced a surprisingly high number of extant species in this genus. http://zoobank.org/urn:lsid:zoobank.org:pub:7407D183-BC8A-466B-8934-F7BE05611ED6SUPPLEMENTAL DATASupplemental materials are available for this article for free at www.tandfonline.com/UJVPCitation for this article: Lambert, O., and S. Louwye. 2016. A new early Pliocene species of Mesoplodon: a calibration mark for the radiation of this species-rich beaked whale genus. Journal of Vertebrate Paleontology. DOI: 10.1080/02724634.2015.1055754.	[Lambert, Olivier] Inst Royal Sci Nat Belg, Rue Vautier 29, B-1000 Brussels, Belgium; [Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium	Ghent University	Lambert, O (通讯作者)，Inst Royal Sci Nat Belg, Rue Vautier 29, B-1000 Brussels, Belgium.	olivier.lambert@naturalsciences.be; stephen.louwye@rug.ac.be	Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Lambert, Olivier/0000-0003-0740-5791; Louwye, Stephen/0000-0003-4814-4313				Abel O., 1905, Memoires du Musee royal d'histoire naturelle de Belgique, V3, P1; Andrews RC, 1908, B AM MUS NAT HIST, V24, P203; [Anonymous], 1997, PALAEONTOGRAPHIA ITA; [Anonymous], 1972, The Scientific Reports of the Whales Research Institute; [Anonymous], T ZOOLOGICAL SOC LON, DOI DOI 10.1111/J.1096-3642.1878.TB00468.X; Bianucci G, 2007, GEODIVERSITAS, V29, P561; Bianucci G, 2013, GEODIVERSITAS, V35, P105, DOI 10.5252/g2013n1a6; Brisson M.J., 1762, QUADRUPEDUM SCILICET; Buono MR, 2013, J VERTEBR PALEONTOL, V33, P986, DOI 10.1080/02724634.2013.752377; Cuvier G.L.C.F.D., 1823, Recherches sur les ossements fossiles, V5; Dalebout ML, 2014, MAR MAMMAL SCI, V30, P1081, DOI 10.1111/mms.12113; Dalebout ML, 2008, SYST BIOL, V57, P857, DOI 10.1080/10635150802559257; Dalebout ML, 1998, MOL ECOL, V7, P687, DOI 10.1046/j.1365-294x.1998.00380.x; Dalebout ML, 2004, J HERED, V95, P459, DOI 10.1093/jhered/esh054; Dalebout ML, 2003, MAR MAMMAL SCI, V19, P421, DOI 10.1111/j.1748-7692.2003.tb01314.x; Dalebout ML, 2002, MAR MAMMAL SCI, V18, P577, DOI 10.1111/j.1748-7692.2002.tb01061.x; de Buffrenil V., 2000, Historical Biology, V14, P57; 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; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Fensome R.A., 2008, DINOFLAJ2, Version 1; 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 Ewan, 2001, P169; Gervais P., 1850, ZOOLOGIE, V14, P5; Glaessmer M. 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Vertebr. Paleontol.	MAR 3	2016	36	2							e1055754	10.1080/02724634.2015.1055754	http://dx.doi.org/10.1080/02724634.2015.1055754			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DH7EA					2025-03-11	WOS:000372953300009
J	Polyakova, YI; Novichkova, YA; Lisitzin, AP; Shevchenko, VP; Kravchishina, MD				Polyakova, Ye. I.; Novichkova, Ye. A.; Lisitzin, A. P.; Shevchenko, V. P.; Kravchishina, M. D.			Diatoms and aquatic palynomorphs in surface sediments of the White Sea bays as indicators of sedimentation in marginal filters of rivers	OCEANOLOGY			English	Article							SUSPENDED PARTICULATE MATTER; GRAIN-SIZE COMPOSITION; BOTTOM SEDIMENTS; KEM RIVER; DINOFLAGELLATE CYSTS; ESTUARY; LAPTEV	Diatom algae, aquatic palynomorphs, and the grain-size of surface sediments from bays of the White Sea were investigated in a program dedicated to the study of marginal filters (MF) in the Severnaya Dvina, Onega, and Kem rivers. Three microalgal assemblages are established in surface sediments, which replace each other successively with distance from river mouths and are characterized by a gradual decrease in a share of freshwater species of diatoms and Chlorophyceae algae, significantly varying concentrations of marine diatoms and dinocysts due to changes in water salinity, grain-size composition of sediments, quantitative distribution of suspended particulate matter (SPM), and water productivity at different marginal filter stages.	[Polyakova, Ye. I.] Moscow MV Lomonosov State Univ, Dept Geog, Moscow, Russia; [Novichkova, Ye. A.; Lisitzin, A. P.; Shevchenko, V. P.; Kravchishina, M. D.] Russian Acad Sci, Shirshov Inst Oceanol IO RAS, Moscow, Russia	Lomonosov Moscow State University; Russian Academy of Sciences	Polyakova, YI (通讯作者)，Moscow MV Lomonosov State Univ, Dept Geog, Moscow, Russia.; Novichkova, YA; Lisitzin, AP; Shevchenko, VP; Kravchishina, MD (通讯作者)，Russian Acad Sci, Shirshov Inst Oceanol IO RAS, Moscow, Russia.	ye.polyakova@mail.ru; enovichkova@mail.ru; lisitzin@ocean.ru; vshevch@ocean.ru; kravchishina@ocean.ru	Polyakova, Yelena/L-8889-2015; Shevchenko, Vladimir/C-2096-2014; Novichkova, Ekaterina/AAC-4726-2019; Lisitzin, Alexander/S-8300-2018; Novichkova, Ekaterina/B-5807-2017; Kravchishina, Marina/B-3741-2017	Novichkova, Ekaterina/0000-0001-5687-1719; Kravchishina, Marina/0000-0001-9967-2891	Basic Research Program of the Earth Sciences Division of the Russian Academy of Sciences "Nanoparticles: Formation Conditions, Analytical Methods, and Technique of Extraction from Mineral Raw Materials"; Russian Federation for state support of leading scientific schools [NSh-2493.2014.5)]; young Russian Scientists (Candidates of Science) [MK-6982.2015.5];  [0149-2014-0026]	Basic Research Program of the Earth Sciences Division of the Russian Academy of Sciences "Nanoparticles: Formation Conditions, Analytical Methods, and Technique of Extraction from Mineral Raw Materials"; Russian Federation for state support of leading scientific schools(Leading Scientific Schools Program); young Russian Scientists (Candidates of Science); 	This work was supported by Basic Research Program no. 5 of the Earth Sciences Division of the Russian Academy of Sciences "Nanoparticles: Formation Conditions, Analytical Methods, and Technique of Extraction from Mineral Raw Materials," grants of the President of the Russian Federation for state support of leading scientific schools (no. NSh-2493.2014.5), and young Russian Scientists (Candidates of Science) (no. MK-6982.2015.5). Materials were obtained under a state-guaranteed order for the Laboratory of Physical-Geology Research, project no. 0149-2014-0026 "Systemic Investigation of Sedimentation in Seas of Russia and the Arctic and Atlantic Oceans."	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P., 2004, Berichte zur Polar- und Meeresforschung, V482, P142; Shevchenko VP, 2005, HYDROL EARTH SYST SC, V9, P57, DOI 10.5194/hess-9-57-2005	40	4	4	0	10	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0001-4370	1531-8508		OCEANOLOGY+	Oceanology	MAR	2016	56	2					289	300		10.1134/S000143701602017X	http://dx.doi.org/10.1134/S000143701602017X			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	DM1OE					2025-03-11	WOS:000376114400014
J	Van Nieuwenhove, N; Hillaire-Marcel, C; Bauch, HA; de Vernal, A				Van Nieuwenhove, Nicolas; Hillaire-Marcel, Claude; Bauch, Henning A.; de Vernal, Anne			Sea surface density gradients in the Nordic Seas during the Holocene as revealed by paired microfossil and isotope proxies	PALEOCEANOGRAPHY			English	Article						Holocene; Nordic Seas; deep water formation; sea surface density gradient	EQUATION-OF-STATE; NORTH-ATLANTIC; DEEP-WATER; HIGH-RESOLUTION; PALEOCEANOGRAPHIC CHANGES; DELTA-O-18 RECORDS; ICE VARIABILITY; NORWEGIAN SEA; ARCTIC-OCEAN; FRAM STRAIT	We attempt to assess the Holocene surface-subsurface seawater density gradient on millennial time scale based on the reconstruction of potential density (sigma) by combining data from dinoflagellate cyst assemblages and planktic foraminiferal (Neogloboquadrina pachyderma (s)) stable oxygen isotopes (O-18(c)). Following several calibration exercises, the likeliness of favorable seasonal preconditioning to open ocean convection is evaluated. The reconstructed sigma values reveal unfavorable conditions for vertical convection in the western Nordic Seas prior to similar to 7-6.5kaB.P., with a westward increase and persistence of surface water buoyancy. Active overturning became more likely after 6.5kaB.P. as suggested by a reduced and recurrently inverted vertical sigma gradient, while intermittent eastward spreading of lower density surface waters continued to modulate the area of potential overturning. Despite some reservation regarding the accuracy of the sigma values reconstructed, the documentation of relative changes of sigma gradients through time and space is suggested as a helpful tool for the appraisal of past overturning likeliness.	[Van Nieuwenhove, Nicolas; Hillaire-Marcel, Claude; de Vernal, Anne] Univ Quebec, Ctr Rech Geochim & Geodynam, Montreal, PQ H3C 3P8, Canada; [Van Nieuwenhove, Nicolas] Aarhus Univ, Dept Geosci, Aarhus, Denmark; [Bauch, Henning A.] Acad Sci Humanities & Literature, Mainz, Germany; [Bauch, Henning A.] Helmholtz Ctr Ocean Res, GEOMAR, Kiel, Germany	University of Quebec; University of Quebec Montreal; Aarhus University; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Van Nieuwenhove, N (通讯作者)，Univ Quebec, Ctr Rech Geochim & Geodynam, Montreal, PQ H3C 3P8, Canada.; Van Nieuwenhove, N (通讯作者)，Aarhus Univ, Dept Geosci, Aarhus, Denmark.	nvn@geo.au.dk	de Vernal, Anne/D-5602-2013; Van Nieuwenhove, Nicolas/IAQ-1532-2023; Hillaire-Marcel, Claude/H-1441-2012; Hillaire-Marcel, Claude/C-9153-2013	Hillaire-Marcel, Claude/0000-0002-3733-4632; Van Nieuwenhove, Nicolas/0000-0001-6369-2751	European Union [243908]; Ministere du Developpement Economique de l'innovation et de l'exportation (MDEIE) du Quebec; Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant; German Research Foundation (DFG) [NI 1248/1]; Danish Council for Independent Research, Natural Science [12-126709/FNU]	European Union(European Union (EU)); Ministere du Developpement Economique de l'innovation et de l'exportation (MDEIE) du Quebec; Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); German Research Foundation (DFG)(German Research Foundation (DFG)); Danish Council for Independent Research, Natural Science(Det Frie Forskningsrad (DFF))	We acknowledge the valuable feedback from Editors C. Charles and E. Thomas and insightful anonymous comments. Raw data and transfer function results used in this manuscript can be accessed through the Geotop database at www.geotop.ca. This study is a contribution to the project "Past4Future Climate change-Learning from the past climate" of the European Union's Seventh Framework program (FP7/2007-2013) under grant agreement 243908. Participation of N.V.N., C.H.M., and A.d.V. to Past4Future has been supported by the Ministere du Developpement Economique de l'innovation et de l'exportation (MDEIE) du Quebec. Additional financial support to C.H.M. was provided by the Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant, to A.d.V. and N.V.N. by ArcTrain-Canada, to N.V.N. and H.A.B. by the German Research Foundation (DFG grant NI 1248/1), and to N.V.N. by the Danish Council for Independent Research, Natural Science (project 12-126709/FNU).	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J	Hayashi, A; Crombie, A; Lacey, E; Richardson, AJ; Vuong, D; Piggott, AM; Hallegraeff, G				Hayashi, Aiko; Crombie, Andrew; Lacey, Ernest; Richardson, Anthony J.; Vuong, Daniel; Piggott, Andrew M.; Hallegraeff, Gustaaf			<i>Aspergillus Sydowii</i> Marine Fungal Bloom in Australian Coastal Waters, Its Metabolites and Potential Impact on <i>Symbiodinium</i> Dinoflagellates	MARINE DRUGS			English	Article						secondary metabolites; Aspergillus sydowii; coral disease; Symbiodinium; maximum quantum yield (F-v/F-m); sydowinol; sydowinin; sydonic acid; sydonol	GORGONIA-VENTALINA; SEA FANS; PATHOGEN; ZOOXANTHELLAE; TEMPERATURE; DIVERSITY; HEALTHY; DUST	Dust has been widely recognised as an important source of nutrients in the marine environment and as a vector for transporting pathogenic microorganisms. Disturbingly, in the wake of a dust storm event along the eastern Australian coast line in 2009, the Continuous Plankton Recorder collected masses of fungal spores and mycelia (~150,000 spores/m(3)) forming a floating raft that covered a coastal area equivalent to 25 times the surface of England. Cultured A. sydowii strains exhibited varying metabolite profiles, but all produced sydonic acid, a chemotaxonomic marker for A. sydowii. The Australian marine fungal strains share major metabolites and display comparable metabolic diversity to Australian terrestrial strains and to strains pathogenic to Caribbean coral. Secondary colonisation of the rafts by other fungi, including strains of Cladosporium, Penicillium and other Aspergillus species with distinct secondary metabolite profiles, was also encountered. Our bioassays revealed that the dust-derived marine fungal extracts and known A. sydowii metabolites such as sydowic acid, sydowinol and sydowinin A adversely affect photophysiological performance (F-v/F-m) of the coral reef dinoflagellate endosymbiont Symbiodinium. Different Symbiodinium clades exhibited varying sensitivities, mimicking sensitivity to coral bleaching phenomena. The detection of such large amounts of A. sydowii following this dust storm event has potential implications for the health of coral environments such as the Great Barrier Reef.	[Hayashi, Aiko; Hallegraeff, Gustaaf] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas 7004, Australia; [Crombie, Andrew; Lacey, Ernest; Vuong, Daniel] Microbial Screening Technol, Bldg A,28-54 Percival Rd, Smithfield, NSW 2164, Australia; [Richardson, Anthony J.] CSIRO Marine & Atmospher Res, Ecosci Precinct, Brisbane, Qld 4102, Australia; [Richardson, Anthony J.] Univ Queensland, Sch Math & Phys, Ctr Applicat Nat Resource Math, St Lucia, Qld 4072, Australia; [Piggott, Andrew M.] Macquarie Univ, Dept Chem & Biomol Sci, Sydney, NSW 2109, Australia	University of Tasmania; Commonwealth Scientific & Industrial Research Organisation (CSIRO); University of Queensland; Macquarie University	Hallegraeff, G (通讯作者)，Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas 7004, Australia.	aiko.hayashi@utas.edu.au; acrombie@microbialscreening.com; elacey@microbialscreening.com; anthony.richardson@csiro.au; dvuong@microbialscreening.com; andrew.piggott@mq.edu.au; gustaaf.hallegraeff@utas.edu.au	; Piggott, Andrew/G-9259-2012; Hallegraeff, Gustaaf/C-8351-2013; Richardson, Anthony/B-3649-2010	Vuong, Daniel/0000-0002-2451-3148; Piggott, Andrew/0000-0002-5308-5314; Crombie, Andrew/0000-0003-3985-1681; Hallegraeff, Gustaaf/0000-0001-8464-7343; Richardson, Anthony/0000-0002-9289-7366; Hayashi, Aiko/0000-0002-7348-9682	Australian Research Council [DP130102725, FT130100142]	Australian Research Council(Australian Research Council)	Hiromitsu Nakajia, Tottori University, Japan, kindly provided us with four typical A. sydowii metabolites. Drew Harvell, Cornell University, USA, provided us with two pathogenic Caribbean A. sydowii strains. John Pitt and Ailsa Hocking for the provision of A. sydowii strains from the CSIRO FRR collection. This work was funded by the Australian Research Council (DP130102725, FT130100142).	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Drugs	MAR	2016	14	3								10.3390/md14030059	http://dx.doi.org/10.3390/md14030059			14	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	DI7SB	26999164	Green Published, Green Accepted, gold, Green Submitted			2025-03-11	WOS:000373701200011
J	Allameh, M; Nejad, EG				Allameh, Mohsen; Nejad, Ebrahim Ghasemi			Palynology and Palynofacies of Santonian-Maastrichtian strata (Abtalkh Fm.) in eastern Koppeh-Dagh Basin, NE of Iran	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Koppeh-Dagh; Abtalkh Formation; Upper Cretaceous; Dinoflagellate cyst; Palynofacies	DINOFLAGELLATE CYSTS; NORTHERN APENNINES; ORGANIC-MATTER; SEDIMENTS; FIELD	The Abtalkh Formation is one of the Upper Cretaceous rock units in the Koppeh-Dagh sedimentary basin which is considered to be of Campanian-Maastrichtian in age. The current study addresses age determination, Palynozonation, and Palynofacies of this formation in eastern Koppeh-Dagh Basin in northeastern Iran based on dinoflagellate cyst species. Accordingly, 65 rock samples were collected from the 923 thick formation and prepared and studied palynologically. The study yielded 28 genera and 45 species of dinoflagellate cysts which confirm the age of Santonian-Maastrichtian for the formation. Moreover, four zones, belonging to a superzone and one subzone, were differentiated based on the first and last appearance of index species. Furthermore, five palynofacies indicative of marginal to highly shelf basin environments were differentiated. Abundance of warm water dinocysts and the presence of fungal hyphae indicate dominance of a warm climate during sedimentation period of the formation. The study of organic matter preservation indicates a relatively low oxygen content and low rate of sedimentation.	[Allameh, Mohsen] Islamic Azad Univ, Mashhad Branch, Dept Geol, Mashhad, Iran; [Nejad, Ebrahim Ghasemi] Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran	Islamic Azad University; University of Tehran	Allameh, M (通讯作者)，Islamic Azad Univ, Mashhad Branch, Dept Geol, Mashhad, Iran.	allameh0277@mshdiau.ac.ir	Allameh, Mohsen/AAW-2163-2021	Allameh, Mohsen/0000-0002-1994-1914				Afshar Harb A., 1969, B IRAN PET I, V37, P86; Afshar-Harb A, 1994, GEOLOGY KOPEH DAGH; Aghanabati A, 2004, GEOLOGY IRAN GEOLOGI; Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P253; Bombardiere L, 2000, SEDIMENT GEOL, V132, P177, DOI 10.1016/S0037-0738(00)00006-3; COMBAZ A., 1964, REV MICROPALDONTOL, V7, P205; Foucher J-C., 1975, Annales scient Univ Reims ARERS, V13, P8; Garzon S, 2012, PALYNOLOGY, V36, P112, DOI 10.1080/01916122.2012.675147; Ghasemi-Nejad E, 2009, STRATIGR SEDIMENTOL, V25, P53; Ghourchaei S, 2015, ARAB J GEOSCI, V8, P2153, DOI 10.1007/s12517-014-1276-3; Hadavi Fatemeh, 2004, Journal of Nannoplankton Research, V26, P63; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; IOANNIDES N.S., 1986, B GEOLOGICAL SURVEY, V371, P1; Kirsch K.H., 1991, GEOLOGIE PALAONTOLOG, V22, P1; Lebedeva NK, 2006, PALEONTOL J+, V40, pS604, DOI 10.1134/S0031030106110086; Lentin J.K., 1980, AASP CONTR SER; Marheinecke Uwe, 1992, Palaeontographica Abteilung B Palaeophytologie, V227, P1; MARSHALL NG, 1990, ALCHERINGA, V14, P1, DOI 10.1080/03115519008619004; Mehrotra NC, 1991, PALEOBOTANIST, V47, P50; Pavlishina P, 2004, ANN NATURHIST MUS A, V106, P1; Roncaglia L, 1997, REV PALAEOBOT PALYNO, V97, P177, DOI 10.1016/S0034-6667(96)00070-X; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; Roncaglia L, 2002, CRETACEOUS RES, V23, P65, DOI 10.1006/cres.2002.0298; Roncaglia L, 1997, SCI REP, V97, P1; SCHIOLER P, 1993, REV PALAEOBOT PALYNO, V78, P321, DOI 10.1016/0034-6667(93)90070-B; Schrank E., 1987, BERLINER GEOWISS ABH, V75, P249, DOI DOI 10.1016/0195-6671(92)90040-W; Skupien P, 2008, B GEOSCI, V83, P207, DOI 10.3140/bull.geosci.2008.02.207; Soliman Ali, 2008, Annalen des Naturhistorischen Museums in Wien A Mineralogie Petrologie Geologie Palaeontologie Archaeozoologie Anthropologie Praehistorie, V110A, P401; SONCINI MJ, 1990, B CENT RECH EXPL, V14, P583; Traverse A, 1998, PALAEOPALYNOLOGY; Traverse A., 2007, Topics in Geobiology, Vsecond; Tyson R.V., 1993, Applied Micropalaeontology, P153, DOI [10.1007/978-94-017-0763-35, DOI 10.1007/978-94-017-0763-35]; VANDERZWAN CJ, 1990, REV PALAEOBOT PALYNO, V62, P157, DOI 10.1016/0034-6667(90)90021-A; VANWAVEREN I, 1994, PALAEOGEOGR PALAEOCL, V112, P85, DOI 10.1016/0031-0182(94)90135-X; VOZZHENNIKOVA TF, 1960, AKAD NAUK SSSR SIBIR, V1, P7; Williams G.L., 1993, Geological Survey of Canada Paper, P1; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; Yepes Oscar, 2001, Palynology, V25, P217, DOI 10.2113/0250217	39	2	2	0	7	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	MAR	2016	9	3							207	10.1007/s12517-015-2111-1	http://dx.doi.org/10.1007/s12517-015-2111-1			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DG6CL					2025-03-11	WOS:000372169700041
J	Price, AM; Gurdebeke, PR; Mertens, KN; Pospelova, V				Price, Andrea Michelle; Gurdebeke, Pieter Roger; Mertens, Kenneth Neil; Pospelova, Vera			Determining the absolute abundance of dinoflagellate cysts in recent marine sediments III: Identifying the source of <i>Lycopodium</i> loss during palynological processing and further testing of the <i>Lycopodium</i> marker-grain method	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cyst; Palynological preparation; Lycopodium clavatum tablet; Spike; Reproducibility; Standardization	ASSEMBLAGES; SYSTEM; BASIN; WATER	Lycopodium clavatum marker-grain tablets are often added before palynological processing to calculate the absolute abundance of organic-walled microfossils in sediments. In this study we investigate the reproducibility of dinoflagellate cyst concentrations by performing nine different tests: varying dinoflagellate cyst/Lycopodium spore ratios, sample weights, centrifuge speeds and times, sonication times, and mesh sizes; manually powdering the sediment using a mortar and pestle prior to processing, using a water jug instead of squirt bottles during sieving, decanting over a 6 pm sieve and adding Lycopodium tablets at the end. Previous studies have reported loss of Lycopodium spores during processing. In this study we investigate sources of this loss by microscopically analyzing residue on stir sticks and sieves, and what is lost through the sieves and decanting. We document an average loss of 8.2 % of Lycopodium spores during processing, with the greatest loss occurring through the fine sieve and resulting in only a 4.8% overestimation of the cyst concentration. Results using powdered sediment and sonicating for more than 5 min are less reproducible. Large cyst/Lycopodium spore ratios were found to have higher cyst concentrations and standard deviations, thus we recommend ratios of less than five, and ideally ratios between 0.5 and 2 to facilitate counting. (C) 2016 Elsevier B.V. All rights reserved.	[Price, Andrea Michelle] McGill Univ, Dept Geog, 805 Sherbrooke St W, Montreal, PQ H3A 0B9, Canada; [Gurdebeke, Pieter Roger; Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium; [Mertens, Kenneth Neil] IFREMER, LER BO, Biol Stn, Pl Croix,BP40537, F-29185 Concameau, France; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB A405,POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada	Ghent University; Ifremer; University of Victoria	Price, AM (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St W, Montreal, PQ H3A 0B9, Canada.	andrea.price@mail.mcgill.ca	Gurdebeke, Pieter/AAY-7059-2020; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Price, Andrea/0000-0002-5359-053X; Mertens, Kenneth/0000-0003-2005-9483; Pospelova, Vera/0000-0003-4049-8133; Gurdebeke, Pieter R./0000-0003-1425-8515	Natural Sciences and Engineering Research Council of Canada (NSERC) [312305]	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	We are grateful to Captain Brown and crew of the MSV Strickland with their help with the sediment collection. Jasmin Chana and Christina Price (UVic) are thanked for their help sieving the samples and Lee Van Ardenne (McGill) for helpful discussions about ANOVA. Kenneth N. Mertens was a postdoctoral fellow of FWO Belgium. This research was partly supported by the Natural Sciences and Engineering Research Council of Canada (NSERC) through a Discovery grant (312305) to Vera Pospelova and a graduate scholarship to Andrea M. Price. We thank Dr. Martin J. Head and a second reviewer for their thoughtful comments which helped improve this manuscript.	[Anonymous], J PALEONTOL MEMOIR; [Anonymous], NOVA HEDWIGIA; BENNINGHOFF W. 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Palaeobot. Palynology	MAR	2016	226						78	90		10.1016/j.revpalbo.2015.12.009	http://dx.doi.org/10.1016/j.revpalbo.2015.12.009			13	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	DF5CP					2025-03-11	WOS:000371369700008
J	Triki, HZ; Laabir, M; Moeller, P; Chomérat, N; Daly-Yahia, OK				Triki, Habiba Zmerli; Laabir, Mohamed; Moeller, Peter; Chomerat, Nicolas; Daly-Yahia, Ons Kefi			First report of goniodomin A production by the dinoflagellate <i>Alexandrium pseudogonyaulax</i> developing in southern Mediterranean (Bizerte Lagoon, Tunisia)	TOXICON			English	Article						Alexandrium pseudogonyaulax; Goniodomin A; Mediterranean sea; Morphology; Phylogeny	POTENTIALLY TOXIC DINOFLAGELLATE; LIFE-HISTORY; POLYETHER MACROLIDE; GENUS ALEXANDRIUM; UNITED-STATES; RESTING CYSTS; COAST; PSEUDOGONIAULAX; DINOPHYCEAE; MONILATUM	The dinoflagellate Alexandrium pseudogonyaulax is widely distributed around the world including the Mediterranean waters. The objectives of this study were to determine the morphology and phylogenic affiliation of A. pseudogonyaulax strain isolated from Bizerte Lagoon (Mediterranean waters, Tunisia) and investigate its toxicity. Molecular analyses confirmed the morphological identification of the isolated strain (APBZ12) as A. pseudogonyaulax. Moreover, it showed that it is 100% identical with strains of this species found in New Zealand, Japan, China and North Sea (Norway and Denmark) suggesting that this species is cosmopolitan. Until now, no toxin studies have been conducted on fully characterized (morphologically and molecularly) A. pseudogonyaulax. Cellular toxin production was determined using high pressure liquid chromatography coupled to mass spectrometry (HPLC/MS). Results showed for the first time that A. pseudogonyaulax contains goniodomin A (GDA), a highly toxic. macrolide polyether previously shown to be produced by two other dinoflagellate species Alexandrium monilatum (Hsia et al., 2006) and Alexandrium hiranoi (erroneously identified as A. pseudogonyaulax in Murakami et al., 1988) in American and Japanese waters, respectively. This biologically active toxin has been associated over decades with fish mortality. Our study showed that the cell extracts of APBZ12 showed an important bioactivity using GH4C1 rat pituitary cytotoxicity bioassay. (C) 2016 Elsevier Ltd. All rights reserved.	[Triki, Habiba Zmerli; Daly-Yahia, Ons Kefi] Carthage Univ, IRESA, INAT, UR Marine Biol FST El Manar I, 43 Ave Charles Nicolle, Tunis 1082, Tunisia; [Laabir, Mohamed] Univ Montpellier, IRD, IFREMER, UMR 9190,MARBEC,CNRS, Pl Eugene Bataillon,Case 093, F-34095 Montpellier 5, France; [Moeller, Peter] NOAA, Toxin Nat Prod Chem Program, Natl Ocean Serv, Hollings Marine Lab, 331 Ft Johnson Rd, Charleston, SC 29412 USA; [Chomerat, Nicolas] IFREMER, Stn Biol Marine, Lab Environm & Ressources Bretagne Occidentale, Pl Croix, F-29900 Concarneau, France	Universite de Carthage; Ifremer; Centre National de la Recherche Scientifique (CNRS); Universite de Montpellier; Institut de Recherche pour le Developpement (IRD); National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; Ifremer	Triki, HZ (通讯作者)，Carthage Univ, IRESA, INAT, UR Marine Biol FST El Manar I, 43 Ave Charles Nicolle, Tunis 1082, Tunisia.	bibarouma@hotmail.fr		Chomerat, Nicolas/0000-0001-9691-6344; Kefi Daly Yahia, Ons/0000-0001-9532-8989	JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program; LMI COSYS-MED - IRD (Institut Francais pour la Recherche et le Developpement); LAGUNTOX project - TOTAL Foundation; IRD; Toxin/Natural Products Chemistry Program (NOAA, USA)	JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program; LMI COSYS-MED - IRD (Institut Francais pour la Recherche et le Developpement); LAGUNTOX project - TOTAL Foundation; IRD; Toxin/Natural Products Chemistry Program (NOAA, USA)	This work benefitted from financial supports of the JEAI ECOBIZ (Jeune Equipe Associee, Ecologie de la lagune de Bizerte) program and LMI COSYS-MED funded by IRD (Institut Francais pour la Recherche et le Developpement) and from LAGUNTOX project funded by TOTAL Foundation. Thanks to IRD for funding M. LAABIR stay in Tunisia. The Toxin/Natural Products Chemistry Program (NOAA, USA) provided support and analysis of toxins. The authors wish to thank G. Bilien for DNA amplification and sequencing.	Abe M, 2002, J CELL PHYSIOL, V190, P109, DOI 10.1002/jcp.10040; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; [Anonymous], 2004, B I NATN SCI TECH ME; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BASS EL, 1983, AQUAT TOXICOL, V3, P15, DOI 10.1016/0166-445X(83)90003-6; Biecheler B., 1952, Bull. Biol. Fr. 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J	Ied, IM; Lashin, GMA				Ied, Ibrahim M.; Lashin, Gamal M. A.			Palynostratigraphy and paleobiogeography of the Jurassic - Lower Cretaceous succession in Kabrit-1 well, northeastern Egypt	CRETACEOUS RESEARCH			English	Article						Jurassic; Cretaceous; Palynostratigraphy; Paleoecology; Paleobiogeography; Egypt	NORTH-WESTERN DESERT; DINOFLAGELLATE CYSTS; EASTERN DESERT; PALYNOLOGY; STRATIGRAPHY; PALYNOFACIES; PALYNOMORPHS; SEDIMENTS; SUDAN; FIELD	Well-preserved and abundant Jurassic Early Cretaceous palynomorph assemblages were recorded from the Kabrit-1 well, north Eastern Desert, Egypt. Thirty-one rock-cutting samples were analyzed and six rock units were differentiated. Seventy-one palynomorph species were identified from the productive samples. Six palynozones were differentiated, and they covered all the studied succession except for a palynomorph barren interval present in the uppermost part. These palynozones arranged in ascending order are as follows: two palynozones were recorded from the Middle-Upper Jurassic (Gonyaulacysta jurassica - Lithodinia jurassica Assemblage Zone and Klukisporites pseudoredculatus-Systematophora penicillata - Escharisphaeridia pocockii Assemblage Zone) and the other four palynozones characterize the Lower Cretaceous deposits (Pilosisporites trichopapillosus - Cribroperidinium orthoceras Assemblage Zone; Dicheiropollis etruscus Interval Zone; Murospora florida - Afropollis operculatus Assemblage Zone and Afropollis jardinus Range Zone). We infer open marine conditions during deposition of the lower part of the Khalig El Ayoun Formation (Oxfordian-Kimmeridgian) and within the Kharita Formation (Albian), and shallow marine or coastal environments during deposition of the remainder of the studied succession. Paleobiogeographically, Late Jurassic index terrestrial palynomorph species documented here are in common with those previously recorded from North Africa, while marine dinocyst species are common to those documented from the West European and North American province. During the Early Cretaceous, the recorded terrestrial microfloral species were similar to those previously recorded from the West African-South American Province, while the marine dinocyst species were still related to the West European and North American marine palynofloral province. (C) 2015 Elsevier Ltd. All rights reserved.	[Ied, Ibrahim M.] Zagazig Univ, Fac Sci, Dept Geol, Zagazig, Egypt; [Lashin, Gamal M. A.] Zagazig Univ, Fac Sci, Dept Bot, Zagazig, Egypt	Egyptian Knowledge Bank (EKB); Zagazig University; Egyptian Knowledge Bank (EKB); Zagazig University	Ied, IM (通讯作者)，Zagazig Univ, Fac Sci, Dept Geol, Zagazig, Egypt.	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J	Nehyba, S; Holcová, K; Gedl, P; Doláková, N				Nehyba, Slavomir; Holcova, Katarina; Gedl, Przemyslaw; Dolakova, Nela			The Lower Badenian transgressive-regressive cycles - a case study from Oslavany (Carpathian Foredeep, Czech Republic)	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article						Facies analyses; provenance; foraminifera; calcareous nannoplankton; dinoflagellate cysts; shoreline position	BENTHIC FORAMINIFERAL MORPHOGROUPS; DINOFLAGELLATE CYSTS; CENTRAL PARATETHYS; GLOBIGERINA-BULLOIDES; DISTRIBUTION PATTERNS; SURFACE SEDIMENTS; BASIN DEVELOPMENT; MIOCENE DEPOSITS; MARINE-SEDIMENTS; FORELAND BASINS	Two newly drilled boreholes (OSL-1 and OSL-2) at Oslavany (Carpathian Foredeep, Czech Republic, a holostratotype of the Moravian/Lower Badenian) provide data documenting the processes of the Lower Badenian marine transgression and regression along the passive margin of the peripheral foreland basin (south-eastern margin of the Bohemian Massif). Three facies associations show the evolution of the deposition and distinct basin margin paleogeography. Deposits of marine transgression (transgressive lag) are followed by open-marine (outer to inner shelf) deposits interpreted as transgressive and highstand systems tract. They reflect a cratonward shift of the coastline. The topmost foreshore and upper shoreface deposits (falling stage systems tract) recorded forced regression and basinward shift of the shoreline. The recorded transgressive-regressive cycle was induced by the coincidence of global TB 2.4. sea-level cycle and forebulge subsidence. The identified higher-frequency cycles were interpreted as climatically controlled.	[Nehyba, Slavomir; Dolakova, Nela] Masaryk Univ, Fac Sci, Inst Geol Sci, Kotlarska 2, CS-61137 Brno, Czech Republic; [Holcova, Katarina] Charles Univ Prague, Fac Sci, Inst Geol & Paleontol, CZ-12843 Prague 2, Czech Republic; [Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland	Masaryk University Brno; Charles University Prague; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Nehyba, S; Doláková, N (通讯作者)，Masaryk Univ, Fac Sci, Inst Geol Sci, Kotlarska 2, CS-61137 Brno, Czech Republic.; Holcová, K (通讯作者)，Charles Univ Prague, Fac Sci, Inst Geol & Paleontol, CZ-12843 Prague 2, Czech Republic.; Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	slavek@sci.muni.cz; holcova@natur.cuni.cz; ndgedl@cyf-kr.edu.pl; nela@sci.muni.cz	Dolakova, Nela/KDO-6495-2024; Holcova, Katarina/I-6992-2017	Dolakova, Nela/0000-0001-6590-2695; Holcova, Katarina/0000-0002-8371-3510	 [PRVOUK P44]		The study is the result of specific research at Institute of Geological Sciences of Masaryk University and was also supported by the projects PRVOUK P44. 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Jahrb. Geol. Palaontol.-Abh.	FEB	2016	279	2					209	238		10.1127/njgpa/2016/0548	http://dx.doi.org/10.1127/njgpa/2016/0548			30	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	DE4MC					2025-03-11	WOS:000370602600006
J	Persson, A; Smith, BC; Cyronak, T; Cooper, E; DiTullio, GR				Persson, Agneta; Smith, Barry C.; Cyronak, Tyler; Cooper, Emily; DiTullio, Giacomo R.			Differences in pigmentation between life cycle stages in <i>Scrippsiella lachrymosa</i> (dinophyceae)	JOURNAL OF PHYCOLOGY			English	Article						accumulation body; dinoflagellate; gamete; life stage; pellicle cyst; pigment; resting cyst; Scrippsiella lachrymosa; zygote	DINOFLAGELLATE RESTING CYSTS; GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; MARINE-PHYTOPLANKTON; COMMUNITY STRUCTURE; CLASS ABUNDANCES; RECENT SEDIMENTS; BENTHIC CYSTS; DIMETHYLSULFONIOPROPIONATE; CAROTENOIDS	Various life cycle stages of cyst-producing dinoflagellates often appear differently colored under the microscope; gametes appear paler while zygotes are darker in comparison to vegetative cells. To compare physiological and photochemical competency, the pigment composition of discrete life cycle stages was determined for the common resting cyst-producing dinoflagellate Scrippsiella lachrymosa. Vegetative cells had the highest cellular pigment content ( 25.2 +/- 0.5 pg cell-1), whereas gamete pigment content was 22% lower. The pigment content of zygotes was 82% lower than vegetative cells, even though they appeared darker under the microscope. Zygotes of S. lachrymosa contained significantly higher cellular concentrations of beta- carotene ( 0.65 +/- 0.15 pg cell -1) than all other life stages. Photoprotective pigments and the de- epoxidation ratio of xanthophylls- cycle pigments in S. lachrymosa were significantly elevated in zygotes and cysts compared to other stages. This suggests a role for accessory pigments in combating intracellular oxidative stress during sexual reproduction or encystment. Resting cysts contained some pigments even though chloroplasts were not visible, suggesting that the brightly colored accumulation body contained photosynthetic pigments. The differences in pigmentation between life stages have implications for interpretation of pigment data from field samples when sampled during dinoflagellate blooms.	[Persson, Agneta] Univ Gothenburg, Dept Biol & Environm Sci, Box 461, SE-40530 Gothenburg, Sweden; [Smith, Barry C.] NOAA, Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, Milford Lab, 212 Rogers Ave, Milford, CT 06460 USA; [Cyronak, Tyler; Cooper, Emily; DiTullio, Giacomo R.] Coll Charleston, Hollings Marine Lab, 331 Ft Johnson Rd, Charleston, SC 29412 USA; [Persson, Agneta] Smedjebacksvagen 13, SE-77190 Ludvika, Sweden	University of Gothenburg; National Oceanic Atmospheric Admin (NOAA) - USA; College of Charleston	Persson, A (通讯作者)，Univ Gothenburg, Dept Biol & Environm Sci, Box 461, SE-40530 Gothenburg, Sweden.; Persson, A (通讯作者)，Smedjebacksvagen 13, SE-77190 Ludvika, Sweden.	agnetapersson77@gmail.com		Persson, Agneta/0000-0003-0202-6514; Cyronak, Tyler/0000-0003-3556-7616	Signe och Olof Wallenius Foundation	Signe och Olof Wallenius Foundation	The Signe och Olof Wallenius Foundation provided financial support. We are grateful to Jennifer Alix for assistance with culturing as well as two anonymous reviewers and Dr. Gary H. Wikfors for manuscript advice. Mention of trade names does not imply endorsement.	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Phycol.	FEB	2016	52	1					64	74		10.1111/jpy.12364	http://dx.doi.org/10.1111/jpy.12364			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	DD6AB	26987089				2025-03-11	WOS:000370005000006
J	Hattenrath-Lehmann, TK; Zhen, Y; Wallace, RB; Tang, YZ; Gobler, CJ				Hattenrath-Lehmann, Theresa K.; Zhen, Yu; Wallace, Ryan B.; Tang, Ying-Zhong; Gobler, Christopher J.			Mapping the Distribution of Cysts from the Toxic Dinoflagellate <i>Cochlodinium polykrikoides</i> in Bloom-Prone Estuaries by a Novel Fluorescence <i>In Situ</i> Hybridization Assay	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							HARMFUL ALGAL BLOOMS; KOREAN COASTAL WATERS; RED TIDE BLOOMS; RIBOSOMAL-RNA; NEW-YORK; PHYLOGENETIC-RELATIONSHIPS; GONYAULAX-TAMARENSIS; SURFACE SEDIMENTS; ESCHERICHIA-COLI; CHESAPEAKE BAY	Cochlodinium polykrikoides is a cosmopolitan dinoflagellate that is notorious for causing fish-killing harmful algal blooms (HABs) across North America and Asia. While recent laboratory and ecosystem studies have definitively demonstrated that Cochlodinium forms resting cysts that may play a key role in the dynamics of its HABs, uncertainties regarding cyst morphology and detection have prohibited even a rudimentary understanding of the distribution of C. polykrikoides cysts in coastal ecosystems. Here, we report on the development of a fluorescence in situ hybridization (FISH) assay using oligonucleotide probes specific for the large subunit (LSU) ribosomal DNA (rDNA) of C. polykrikoides. The LSU rDNA-targeted FISH assay was used with epifluorescence microscopy and was iteratively refined to maximize the fluorescent reaction with C. polykrikoides and minimize cross-reactivity. The final LSU rDNA-targeted FISH assay was found to quantitatively recover cysts made by North American isolates of C. polykrikoides but not cysts formed by other common cyst-forming dinoflagellates. The method was then applied to identify and map C. polykrikoides cysts across bloom-prone estuaries. Annual cyst and vegetative cell surveys revealed that elevated densities of C. polykrikoides cysts (> 100 cm(-3)) during the spring of a given year were spatially consistent with regions of dense blooms the prior summer. The identity of cysts in sediments was confirmed via independent amplification of C. polykrikoides rDNA. This study mapped C. polykrikoides cysts in a natural marine setting and indicates that the excystment of cysts formed by this harmful alga may play a key role in the development of HABs of this species.	[Hattenrath-Lehmann, Theresa K.; Wallace, Ryan B.; Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Southampton, NY USA; [Zhen, Yu] Ocean Univ China, Coll Environm Sci & Engn, Qingdao, Peoples R China; [Zhen, Yu] Ocean Univ China, Minist Educ, Key Lab Marine Environm & Ecol, Qingdao, Peoples R China; [Tang, Ying-Zhong] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China	State University of New York (SUNY) System; Stony Brook University; Ocean University of China; Ocean University of China; Chinese Academy of Sciences; Institute of Oceanology, CAS	Gobler, CJ (通讯作者)，SUNY Stony Brook, Sch Marine & Atmospher Sci, Southampton, NY USA.; Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China.	yingzhong.tang@qdio.ac.cn; christopher.gobler@stonybrook.edu	Wallace, Ryan/AGW-6884-2022; ZHEN, YU/E-3247-2014; Gobler, Christopher/JOZ-2924-2023		New York Sea Grant, State University of New York [R/CMB-40]; New York Sea Grant [R/CMB-40]; Laurie Landeau Foundation; Simons Foundation	New York Sea Grant, State University of New York; New York Sea Grant; Laurie Landeau Foundation; Simons Foundation	New York Sea Grant, State University of New York provided funding to Christopher Gobler under grant number R/CMB-40. Laurie Landeau Foundation provided funding to Christopher Gobler. Simons Foundation provided funding to Christopher Gobler.r This research was supported by New York Sea Grant Award R/CMB-40 to C.J.G. We also acknowledge the continued and generous support of the Laurie Landeau Foundation and Simons Foundation. The funders had no role in study design, data collection and interpretation, or the decision to submit the work for publication.	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Environ. Microbiol.	FEB	2016	82	4					1114	1125		10.1128/AEM.03457-15	http://dx.doi.org/10.1128/AEM.03457-15			12	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	DC7CJ	26637596	Green Published, Bronze			2025-03-11	WOS:000369375900014
J	Kremp, A; Oja, J; LeTortorec, AH; Hakanen, P; Tahvanainen, P; Tuimala, J; Suikkanen, S				Kremp, Anke; Oja, Johanna; LeTortorec, Anniina H.; Hakanen, Paivi; Tahvanainen, Pia; Tuimala, Jarno; Suikkanen, Sanna			Diverse seed banks favour adaptation of microalgal populations to future climate conditions	ENVIRONMENTAL MICROBIOLOGY			English	Article							ALEXANDRIUM-OSTENFELDII DINOPHYCEAE; GENETIC DIVERSITY; TOXIN PRODUCTION; TEMPERATURE; EVOLUTIONARY; GROWTH; BLOOM; BIOLUMINESCENCE; VARIABILITY; RESPONSES	Selection of suitable genotypes from diverse seed banks may help phytoplankton populations to cope with environmental changes. This study examines whether the high genotypic diversity found in the Baltic cyst pool of the toxic dinoflagellate Alexandrium ostenfeldii is coupled to phenotypic variability that could aid short-term adaptation. Growth rates, cellular toxicities and bioluminescence of 34 genetically different clones isolated from cyst beds of four Baltic bloom sites were determined in batch culture experiments along temperature and salinity gradients covering present and future conditions in the Baltic Sea. For all parameters a significant effect of genotype on the response to temperature and salinity changes was identified. General or site-specific effects of the two factors remained minor. Clones thriving at future conditions were different from the best performing at present conditions, suggesting that genotypic shifts may be expected in the future. Increased proportions of highly potent saxitoxin were observed as a plastic response to temperature increase, indicating a potential for higher toxicity of future blooms. The observed standing variation in Baltic seed banks of A.ostenfeldii suggests that the population is likely to persist under environmental change.	[Kremp, Anke; Oja, Johanna; LeTortorec, Anniina H.; Hakanen, Paivi; Tahvanainen, Pia; Suikkanen, Sanna] Finnish Environm Inst, Marine Res Ctr, Helsinki 00251, Finland; [LeTortorec, Anniina H.; Tahvanainen, Pia] Univ Helsinki, Tvarminne Zool Stn, Hango 10900, Finland; [Tuimala, Jarno] Finnish Tax Adm, Haapaniemenkatu 4, Vero 00052, Finland	Finnish Environment Institute; University of Helsinki	Kremp, A (通讯作者)，Finnish Environm Inst, Marine Res Ctr, Helsinki 00251, Finland.	anke.kremp@ymparisto.fi		Le Tortorec, Anniina/0000-0002-9397-8328; Suikkanen, Sanna/0000-0002-0768-8149	Academy of Finland [128833, 251564, 259357, 132409]; Walter and Andree de Nottbeck Foundation; Finnish Cultural Foundation; Academy of Finland (AKA) [251564, 259357, 132409] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); Walter and Andree de Nottbeck Foundation; Finnish Cultural Foundation(Finnish Cultural FoundationFinnish IT center for science); Academy of Finland (AKA)(Research Council of Finland)	This study was financially supported by the Academy of Finland (grants #128833 and 251564 to AK, #259357 to SS, #132409 to AHL), the Walter and Andree de Nottbeck Foundation (PT) and the Finnish Cultural Foundation (PH).	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J	Marx, FG; Bosselaers, MEJ; Louwye, S				Marx, Felix Georg; Bosselaers, Mark E. J.; Louwye, Stephen			A new species of <i>Metopocetus</i> (Cetacea, Mysticeti, Cetotheriidae) from the Late Miocene of the Netherlands	PEERJ			English	Article						Mysticeti; Baleen whales; Cetotheriidae; Metopocetus; Phylogenetics; Paroccipital concavity; Late Miocene; Primary dorsal infraorbital foramen	BASIN NORTHERN BELGIUM; DINOFLAGELLATE CYST; BALEEN WHALE; MIDDLE MIOCENE; STRATIGRAPHY; EVOLUTION; PLIOCENE; MORPHOLOGY; PHYLOGENY; MAMMALIA	The family Cetotheriidae has played a major role in recent discussions of baleen whale phylogenetics. Within this group, the enigmatic, monotypic Metopocetus durinasus has been interpreted as transitional between herpetocetines and other members of the family, but so far Ihas been restricted to a single, fragmentary cranium of uncertain provenance and age. Here, we expand the genus and shed new light on its phylogenetic affinities and functional morphology by describing Metopocetus hunteri sp. nov. from the Late Miocene of the Netherlands. Unlike the holotype of M. durthasus, the material described here is confidently dated and preserves both the tympanic bufia and additional details of the basicranium. M. hurtteri closely resembles M. durthasus, differing primarily in its somewhat less distally expanded compound posterior process of the tympanoperiotic. Both species are characterised by the development of an unusually large fossa on the ventral surface of the paroccipital process, which extends anteriorly on to the compound posterior process and completely floors the facial sulcus. In life, this enlarged fossa may have housed the posterior sinus and/or the articulation of the stylohyal. Like other cetotheriids, Metopocetus also bears a well-developed, posteriorly-pointing dorsal infraorbital foramen near the base of the ascending process of the maxilla, the precise function of which remains unclear.	[Marx, Felix Georg] Natl Museum Nat & Sci, Dept Geol & Palaeontol, Tsukuba, Ibaraki, Japan; [Bosselaers, Mark E. J.] Royal Belgian Inst Nat Sci, Directorate Earth & Hist Life, Brussels, Belgium; [Bosselaers, Mark E. J.] Koninklijk Zeeuwsch Genootschap Wetenschappen, Marine Vertebrates, Middelburg, Netherlands; [Louwye, Stephen] Univ Ghent, Dept Geol, Res Unit Palaeontol, B-9000 Ghent, Belgium	National Museum of Nature and Science; Royal Belgian Institute of Natural Sciences; Ghent University	Marx, FG (通讯作者)，Natl Museum Nat & Sci, Dept Geol & Palaeontol, Tsukuba, Ibaraki, Japan.	felix.marx@otago.ac.nz	Marx, Felix/AAI-3480-2021; Louwye, Stephen/D-3856-2012	Marx, Felix Georg/0000-0002-1029-4001; Louwye, Stephen/0000-0003-4814-4313	Japan Society for the Promotion of Science; Grants-in-Aid for Scientific Research [13F03503] Funding Source: KAKEN	Japan Society for the Promotion of Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	FGM was supported by a Japan Society for the Promotion of Science Postdoctoral Fellowship for Foreign Researchers. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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Jr, 2008, Virginia Museum of Natural History Special Publication, V14, P141	49	22	23	0	11	PEERJ INC	LONDON	341-345 OLD ST, THIRD FLR, LONDON, EC1V 9LL, ENGLAND	2167-8359			PEERJ	PeerJ	JAN 28	2016	4								e1572	10.7717/peerj.1572	http://dx.doi.org/10.7717/peerj.1572			31	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	DC7NM	26835183	Green Published, gold, Green Submitted			2025-03-11	WOS:000369407200002
J	Deaf, AS; Harding, IC; Marshall, JEA				Deaf, Amr S.; Harding, Ian C.; Marshall, John E. A.			Early Cretaceous palynostratigraphy of the Abu Tunis 1x borehole, northern Western Desert, Egypt, with emphasis on the possible palaeoclimatic effect upon the range of <i>Dicheiropollis etruscus</i> in North Africa	PALYNOLOGY			English	Article						palynostratigraphy; Cretaceous; Western Desert; Egypt; Dicheiropollis etruscus; North Africa	DINOFLAGELLATE CYST STRATIGRAPHY; APTICORE SOUTHERN ALPS; ANGIOSPERM POLLEN; DAKHLA OASIS; PALYNOLOGY; BIOSTRATIGRAPHY; SPORES; PALYNOMORPHS; SEDIMENTS; SEQUENCE	Recent hydrocarbon exploration in the northern sector of the Western Desert in Egypt has revealed relatively rich hydrocarbon accumulations, mainly of gas, and demonstrate promising future prospects. In order to improve our understanding of this area and to provide a biostratigraphical framework for the hitherto poorly dated Lower Cretaceous successions, a palynological analysis was carried out on 57 ditch cutting samples from the Abu Tunis 1x borehole. Palynostratigraphic investigation on these samples has enabled the identification of three new palynostratigraphically defined age divisions with three corresponding palynozones defined by first uphole occurrences of gymnosperm and angiosperm pollen and dinoflagellate cysts. Spore and pollen grains recovered from the Abu Tunis 1x borehole show the characteristics of the pre-Albian Dicheiropollis/Afropollis Phytogeographical Province. Discrepancies in the reported range of Dicheiropollis etruscus, when compared with earlier (Berriasian) appearances in West Africa and later (late Hauterivian) appearances in East Africa, may be attributed to palaeoecological factors. Dicheiropollis etruscus is accepted as having a cheirolepidiacean conifer affinity and is regarded as having been produced by a thermophilous plant. Here, we suggest that Dicheiropollis etruscus was adapted to arid conditions. Dicheiropollis etruscus thus first appeared in hot, dry palaeo-subtropical African regions, but as Western Gondwana broke up and the African Plate moved northeast during/after the Late Jurassic, the region that is now present-day Egypt, Libya and Sudan had moved by the late Hauterivian into a subtropical position; the ensuing increased aridity thus allowed Dicheiropollis etruscus to migrate into these areas.	[Deaf, Amr S.; Harding, Ian C.; Marshall, John E. A.] Univ Southampton, Natl Oceanog Ctr, Sch Ocean & Earth Sci, European Way, Southampton SO14 3ZH, Hants, England; [Deaf, Amr S.] Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt	NERC National Oceanography Centre; University of Southampton; Egyptian Knowledge Bank (EKB); Assiut University	Deaf, AS (通讯作者)，Univ Southampton, Natl Oceanog Ctr, Sch Ocean & Earth Sci, European Way, Southampton SO14 3ZH, Hants, England.; Deaf, AS (通讯作者)，Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt.	amr.daif@science.au.edu.eg	Harding, Ian/K-3320-2012; Deaf, Amr/AAF-6269-2020; Marshall, John/M-9154-2018	Deaf, Amr/0000-0002-5073-7911; Marshall, John/0000-0002-9242-3646; Harding, Ian/0000-0003-4281-0581				[Anonymous], 1962, GEOLOGY EGYPT NEW YO; [Anonymous], 1971, POLLEN SPORES; Awad M.Z., 1994, Berliner geowissenschaftlische Abhandlungen A, V161, P1; Barakat MG, 1982, 20 ANN M GEOL SOC EG; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; Beck CB, 1988, Origin and evolution of gymnosperms, P382; Brenner Gilbert J., 1996, P91, DOI 10.1007/978-0-585-23095-5_5; Bumby AJ, 2005, J AFR EARTH SCI, V43, P1, DOI 10.1016/j.jafrearsci.2005.07.016; DAVEY R J, 1974, Palaeontology (Oxford), V17, P623; Davey R.J., 1973, REV ESP MICROPALEONT, V5, P173; Deaf AS, 2014, PALYNOLOGY, V38, P51, DOI 10.1080/01916122.2013.828662; DOYLE J A, 1975, Pollen et Spores, V17, P429; Doyle J.A., 1982, B CENT RECH EXPL, V6, P39; Doyle J.A., 1977, Bull. 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J	Moczydlowska, M				Moczydlowska, Malgorzata			Algal affinities of Ediacaran and Cambrian organic-walled microfossils with internal reproductive bodies: <i>Tanarium</i> and other morphotypes	PALYNOLOGY			English	Article						organic-walled microfossils; Ediacaran; Cambrian; zygotic cysts; phycoma; Chlorophyceae; Prasinophyceae	HORIZONTAL GENE-TRANSFER; CELL-WALL; ACANTHOMORPHIC ACRITARCHS; DOUSHANTUO FORMATION; MOLECULAR FOSSILS; OFFICER-BASIN; CHUAR GROUP; BIOLOGICAL AFFINITIES; LEVEL CLASSIFICATION; EVOLUTIONARY HISTORY	Organically preserved, unicellular microfossils of Ediacaran and Cambrian age, which comprise single and multiple internal bodies within the vesicle, have been studied with a view towards explaining the origin and function of these structures. Assessed by body plan, ornamentation, excystment structure, cell wall resistance and ultrastructure (where available), and newly observed internal bodies defined by their own, robust wall, these microfossils are recognised as algal zygotic cysts and phycomata by comparison with extant green algae. Although rare, these internal bodies are a persistent feature of specific morphotypes regardless of geological age, and are reviewed. Internal bodies are a part of reproductive cysts, resembling those known in different clades of green algae: prasinophytes, chlorophytes and streptophytes, as well as alveolates (including dinoflagellates). They are inferred to be endocysts containing zygotes and/or sacs of swarmers, if single, or offspring cells (spores), if multiple, in sexual and asexual generations of ancient taxa of the classes Prasinophyceae and Chlorophyceae. It may not be excluded, however, that they represent the earliest, stem-group streptophytes or alveolates. The diagnoses of the Ediacaran taxa Ancorosphaeridium, A. magnum, Densisphaera, D. arista, D. fistulosa, Multifronsphaeridium ramosum and Tanarium tuberosum are emended to include the internal bodies as integral morphological structures of microfossils, and to abandon the erroneous identification of the double wall of the vesicle. Based on the earliest occurrence of microfossils with an internal body in the Dictyosphaera-Shuiyousphaeridium plexus, sexual reproduction among photosynthesising microbiota is interpreted at c. 1.6-1.4 Ga, a common phenomenon in the Ediacaran (Tanarium, Ancorosphaeridium, Densisphaera), and dominant in the Cambrian (Skiagia, Polygonium and many others) periods.	[Moczydlowska, Malgorzata] Uppsala Univ, Dept Earth Sci, Palaeobiol, Villavagen 16, SE-75236 Uppsala, Sweden	Uppsala University	Moczydlowska, M (通讯作者)，Uppsala Univ, Dept Earth Sci, Palaeobiol, Villavagen 16, SE-75236 Uppsala, Sweden.	malgo.vidal@pal.uu.se			Swedish Research Council (VR) [621-2012-1669]	Swedish Research Council (VR)(Swedish Research Council)	The study was supported by research grant no. 621-2012-1669 from the Swedish Research Council (VR). I greatly appreciated discussions on phytoplankton diversity and origins with Kath Grey (Perth), Konstantin Nagovitsin (Novosibirsk), Sebastian Willman and Heda Agic (Uppsala); however, the views expressed here are my own responsibility. Marien van Westen (Groningen), Pavel Skaloud (Praha) and Vera Pospelova (Victoria) kindly provided images of modern algae from their collections. I especially thank Reed Wicander for his comments and thorough reading of the manuscript, and the anonymous reviewer for useful suggestions. I acknowledge discussions with the Editor Jim Riding on various aspects of fossil algae, and his editorial work.	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J	Akyuz, I; Warny, S; Famubode, O; Bhattacharya, JP				Akyuz, Isil; Warny, Sophie; Famubode, Oyebode; Bhattacharya, Janok P.			Palynology of the Upper Cretaceous (Turonian) Ferron Sandstone Member, Utah, USA: identification of marine flooding surfaces and Milankovitch cycles in subtropical, ever-wet, paralic to non-marine palaeoenvironments	PALYNOLOGY			English	Article						palynology; Upper Cretaceous (Turonian); Ferron Notom; Cretaceous Western Interior Seaway; sequence stratigraphy	HENRY MOUNTAINS REGION; SOUTH-CENTRAL UTAH; SEQUENCE STRATIGRAPHY; NOTOM DELTA; PALEOECOLOGY; WESTERN; SPORES	The Upper Cretaceous Ferron Sandstone Member of the Mancos Shale Formation in Utah includes coal and gas deposits and is an important outcrop analogue to study reservoir characterisation of fluvial-deltaic petroleum systems. Numerous sedimentological and sequence stratigraphic studies of the Notom fluvial-deltaic wedge have been conducted recently; however, palynological analyses had not previously been undertaken. Here, we present palynological data from 128 samples collected in the Notom wedge of the Ferron Sandstone Member outcropping in south-central Utah. The purpose of this study is to use palynological analysis to refine the broader depositional environments, evaluate the climatic setting, and to build a biostratigraphic palynological framework. The dominance of terrestrial palynomorphs, especially the high yield of moisture-loving cryptogam spores, indicates a primarily ever-wet depositional environment characteristic of hydromorphic floodplain palaeosols formed in subtropical to tropical climates. Although dinoflagellates are rare, four intervals with occurrences of marine cysts indicate periods of increased marine/tidal influence associated with previously identified flooding surfaces within Milankovitch-scale parasequences of the largely non-marine stratal succession. These flooding surfaces confirm correlations from regional high-resolution sequence stratigraphic studies and allow correlative marine parasequences and systems tracts to be extended within floodplain-dominated stratal successions. The presence of Nyssapollenites albertensis pollen places the interval studied within the Nyssapollenites albertensis Interval Zone (Nichols 1994), constraining the age of the Ferron Sandstone Member to the latter part of the Cenomanian and the early Coniacian. This largely agrees with the bentonite- and ammonite-derived Turonian age proposed in previous studies.	[Akyuz, Isil; Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA; [Akyuz, Isil; Warny, Sophie] Louisiana State Univ, Museum Nat Sci, E-235 Howe Russell, Baton Rouge, LA 70803 USA; [Famubode, Oyebode] Univ Houston Sci & Res, Dept Earth & Atmospher Sci, Bldg 1,Rm 312, Houston, TX 77204 USA; [Bhattacharya, Janok P.] McMaster Univ, Sch Geog & Earth Sci, 1280 Main St W, Hamilton, ON L8S 4L8, Canada	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University; McMaster University	Akyuz, I; Warny, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell, Baton Rouge, LA 70803 USA.; Akyuz, I; Warny, S (通讯作者)，Louisiana State Univ, Museum Nat Sci, E-235 Howe Russell, Baton Rouge, LA 70803 USA.	iyildi1@lsu.edu; swarny@lsu.edu	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X; Famubode, Oyebode/0000-0001-7857-5523	HESS Corporation; University of Houston (UH)-McMaster Quantitative Sedimentology Laboratories; Anadarko; BP; BHP-Billiton; Chevron; Ecopetrol; ExxonMobil; Inpex; Pioneer; Shell	HESS Corporation; University of Houston (UH)-McMaster Quantitative Sedimentology Laboratories; Anadarko; BP; BHP-Billiton; Chevron; Ecopetrol; ExxonMobil(Exxon Mobil Corporation); Inpex; Pioneer; Shell(Royal Dutch Shell)	We are grateful to HESS Corporation for funding the StrataBugs (R) licence to Louisiana State University (LSU). We thank the University of Houston (UH)-McMaster Quantitative Sedimentology Laboratories who helped fund this work through support from Anadarko, BP, BHP-Billiton, Chevron, Ecopetrol, ExxonMobil, Inpex, Pioneer and Shell.	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J	Williams, GL; Fensome, RA				Williams, Graham L.; Fensome, Robert A.			Fossil dinoflagellates: nomenclatural proposals in anticipation of a revised DINOFLAJ database	PALYNOLOGY			English	Article						dinoflagellate cysts; fossils; nomenclature; taxonomy	STRATIGRAPHY	The Lentin & Williams Index', of which the first version was published in 1973, was intended to keep those involved in fossil dinoflagellate research abreast of the burgeoning taxonomic literature. An additional role has been to tidy up' nomenclatural issues that have been left unresolved in publications. The printed Index has moved to an online database, DINOFLAJ, a new version of which is projected for 2016. Although since 2012 the International Code of Nomenclature makes allowance for nomenclatural novelties to be proposed online, these digital sources need to be in PDF format in a recognised online publication. As DINOFLAJ3 will arguably not meet formal rules of nomenclature, this brief communication is intended to formalise nomenclatural changes that are needed before the database is released. Thus, the following names are herein validated: Alterbidinium compactum, Alterbidinium nuculum, Alterbidinium nummiliforme, Alterbidinium pentangulare, Alterbidinium prominense, Alterbidinium pseudocirculum, Alterbidinium saltanovae, Alterbidinium simplex; and Palaecysta palmula subspecies ankamotraensis. Also proposed herein are the following new combinations: Amphorulacysta delicata, Amphorulacysta? dodekovae, Amphorulacysta? expirata, Amphorulacysta metaelliptica, Amphorulacysta? monteilii; Bonetocardiella peregrinaensis; Cordosphaeridium gracile forma areolatum; Cribroperidinium graemei subspecies trabeculosum; Dinopterygium asteriforme; Nyktericysta granorugosa, Nyktericysta pentaradiata; Palaecysta complicata, Palaecysta palmula, Palaecysta silyba; and Pithonella melloi.	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L., 1998, AM ASS STRATIGRAPHIC, V34; ZOTTO M, 1987, MICROPALEONTOLOGY, V33, P193, DOI 10.2307/1485637	49	5	5	0	4	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	JAN 2	2016	40	1					137	143		10.1080/01916122.2015.1113209	http://dx.doi.org/10.1080/01916122.2015.1113209			7	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	DD3UC					2025-03-11	WOS:000369847500008
J	Krueger, AM; McCarthy, FMG				Krueger, Andrea M.; McCarthy, Francine M. G.			Great Canadian <i>Lagerstatten</i> 5. Crawford Lake - A Canadian Holocene Lacustrine <i>Konservat</i>-<i>Lagerstatte</i> with Two-Century-Old Viable Dinoflagellate Cysts	GEOSCIENCE CANADA			English	Article							CULTURAL EUTROPHICATION; SEDIMENTS; ONTARIO; PHYTOPLANKTON; RECORD; ASSEMBLAGE; ROTIFERS; TAXONOMY	In addition to commonly preserved microfossils like pollen and diatoms, the varved sediments of Crawford Lake, Ontario, contain the fossilized remains of otherwise rare microfossils. Bottom water anoxia resulted from the physiography of this small, deep lake and enhanced biochemical oxygen demand (BOD) during two distinct phases of human settlement: prehistoric Iroquoians (approximately 1268-1486 CE) and historic Euro-Canadians (since 1822 CE). The exceptional preservation of delicate organic-walled microfossils like rotifer loricae and cellulosic dinoflagellate thecae provides unparalleled insights into a Holocene freshwater lake ecosystem and allows the biological and taphonomic components of the fossil assemblage to be isolated. Bottom water anoxia may also have increased the longevity of cell contents: resting cysts of Parvodinium [Peridinium] inconspicuum (Lemmermann) Carty and Peridinium volzii Lemmermann. These were germinated from varves deposited nearly two centuries ago, extending the known span of viability of dinoflagellates.	[Krueger, Andrea M.; McCarthy, Francine M. G.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Brock University	Krueger, AM (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	akrueger@brocku.ca						ALLISON PA, 1993, GEOLOGY, V21, P527, DOI 10.1130/0091-7613(1993)021<0527:EFRDOS>2.3.CO;2; [Anonymous], 1990, SUSSWASSERFLORA MITT; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; BELL M A, 1987, Palaios, V2, P455, DOI 10.2307/3514617; Boyko M., 1973, THESIS U TORONTO ON; Bradley W.H., 1931, US GEOLOGICAL SURVEY, V168, P1; Bravo Isabel, 2014, Microorganisms, V2, P11; Buchheim H. 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Can.		2016	43						123	132		10.12789/geocanj.2016.43.086	http://dx.doi.org/10.12789/geocanj.2016.43.086			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EW5WO		Bronze			2025-03-11	WOS:000402577400003
J	Nohr-Hansen, H; Williams, GL; Fensome, RA				Nohr-Hansen, H.; Williams, G. L.; Fensome, R. A.			Biostratigraphic correlation of the western and eastern margins of the Labrador-Baffin Seaway and implications for the regional geology	GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN			English	Article						Baffin Margin; Labrador Margin; offshore West Greenland; Cretaceous; Cenozoic; biostratigraphy; palynology; dinocysts; palaeoenvironments	EOCENE THERMAL MAXIMUM; DINOFLAGELLATE CYST STRATIGRAPHY; LOWER PALEOGENE; NUUSSUAQ BASIN; DAVIS STRAIT; NORTH-SEA; MAGNETOSTRATIGRAPHIC CALIBRATION; BOUNDARY SECTION; ATANE FORMATION; OCEANIC-CRUST	New analyses of the palynological assemblages in 13 offshore wells on the Canadian margin and six on the West Greenland Margin, in conjunction with onshore data, have led to a new biostratigraphic framework for the Cretaceous-Cenozoic strata of the Labrador Sea-Davis Strait-Baffin Bay (Labrador-Baffin Seaway) region and the first broad biostratigraphic correlation of the Canadian and Greenland margins. This framework is based on 167 last occurrences and 18 local/regional peak/ common-occurrence events for dinocysts, miospores, fungal spores and Azolla. Detailed biostratigraphic evidence has confirmed the following hiatuses: pre-Aptian in the Hopedale Basin; pre-Albian in the Saglek Basin; Albian-Turonian in some wells of the Hopedale Basin; Turonian-Santonian/Campanian in some areas; pre-Campanian and late Campanian-Thanetian on the Greenland Margin; late Maastrichtian and Danian in some wells of the Hopedale Basin and in the Saglek Basin; Selandian in part of the Hopedale Basin, in all the Saglek Basin wells and in two wells on the West Greenland Margin; late Ypresian and/or Lutetian on both sides; Oligocene to middle Miocene of considerable variability on both margins, with all of the Oligocene and the lower Miocene missing in all the West Greenland Margin wells; and middle to late Miocene on the western side. On the Canadian margin, the hiatuses can be partially matched with the five previously recognised regional unconformities; on the Greenland margin, however, the relationship to the five unconformities is more tenuous. Palyno morph assemblages show that most Aptian to Albian sediments were deposited in generally non-marine to marginal marine settings, interrupted by a short-lived shallow marine episode in the Aptian. A marine transgression started in the Cenomanian-Turonian and led to the most open-marine, oceanic conditions in the Campanian-Lutetian; shallowing probably started in the late Lutetian and continued into the Rupelian, when inner neritic and marginal marine palaeoenvironments predominated. Throughout the rest of the Cenozoic, inner neritic palaeoenvironments alternated with marginal marine conditions on the margins of the Labrador-Baffin Seaway. These observations broadly reflect the tectonic evolution of the seaway, with rift conditions prevailing from Aptian to Danian times, followed by drift through much of the Paleocene and Eocene, and post-drift from Oligocene to the present. Dinocysts indicate that climatic conditions in the Labrador-Baffin Seaway region were relatively temperate in the Cretaceous, but varied dramatically through the Cenozoic. The Danian was a time of increasingly warmer climate, a thermal maximum being reached around the Paleocene-Eocene boundary reflecting the global thermal event at this time. Warm to hot conditions prevailed throughout the Ypresian, but the climate began to cool in the Lutetian, a trend that accelerated through the Priabonian and Rupelian. Throughout the Neogene, temperatures generally declined, culminating in the Quaternary.	[Nohr-Hansen, H.] Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Williams, G. L.; Fensome, R. 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J	Gedl, P; Worobiec, E; Slodkowska, B				Gedl, Przemyslaw; Worobiec, Elzbieta; Slodkowska, Barbara			Palynology of Lower Oligocene brown coal and lowermost Middle Miocene sand deposits from the Lukowa-4 borehole (Carpathian Foredeep, SE Poland) - implications for palaeogeographical reconstructions	GEOLOGICAL QUARTERLY			English	Article						sporomorphs; dinoflagellate cysts; palynostratigraphy; palaeoenvironment; Oligocene-Miocene; Carpathian Foredeep	DINOFLAGELLATE CYST ZONATION; BASIN; PALEOGENE	Brown coal and overlying sand strata from the Lukowa-4 borehole, located in the northeastern sector of the Carpathian Foredeep in Poland, were studied for palynology. These strata are underlain by Upper Eocene sands, and covered by Middle Miocene rocks. Coal beds yielded infrequent sporomorphs and freshwater algae Botryococcus. The presence of the latter indicates that these deposits accumulated in a freshwater environment whereas sporomorph assemblages point to the presence of mixed forests with a significant portion of thermophilous taxa. Age of the coal beds has been established based both on the presence of species that appear for the last time in the Early Oligocene, and on the similarity with sporomorph spectra from the Lower Oligocene of the Polish Lowlands. Overlying sands yielded marine dinoflagellate cysts, which point to a marine sedimentary setting, and frequent sporomorphs. The latter indicate the presence of mixed mesophytic forests, bush swamps, swamp forests, and riparian forests in the vicinity of lacustrine environments. Stratigraphic analysis of dinoflagellate cyst and sporomorph assemblages suggests that the sands accumulated in early stages of Miocene transgression in the Carpathian Foredeep in the latest Early early Middle Miocene. Our climatic interpretation of the sporomorph spectra suggests that the climate during deposition of the strata was relatively warm, although less frequent thermophilous taxa recorded in the Miocene sands suggest a slightly cooler climate than that deducted from the spectra yielded by the underlying Lower Oligocene coal beds. Correlation of Lower Oligocene coal beds with neighbouring coeval marine sands suggests diverse morphological conditions in the Carpathian foreland at that time, partly covered by a sea, and partly emerged. A similar, morphologically diverse basement in the Carpathian foreland favoured accumulation of Lower Miocene phytogenic deposits. A similar stratigraphic position of both Lower Oligocene and Lower Miocene coal beds in the Carpathian Foredeep may result in a false correlation of these strata devoid of fossils, which are commonly regarded as Miocene.	[Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, Senacka 1, PL-31002 Krakow, Poland; [Worobiec, Elzbieta] Polish Acad Sci, W Szafer Inst Bot, Lubicz 46, PL-31512 Krakow, Poland; [Slodkowska, Barbara] 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; W. Szafer Institute of Botany 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		Worobiec, Elzbieta/0000-0001-5997-9602; Slodkowska, Barbara/0000-0003-3760-4935	W. Szafer Institute of Botany, Polish Academy of Sciences, Krakow	W. Szafer Institute of Botany, Polish Academy of Sciences, Krakow	The Management of Polskie Gornictwo Naftowe i Gazownictwo SA (PGNiG) is kindly acknowledged for granting permission to use their samples and to publish research results. The study was partly supported by the W. Szafer Institute of Botany, Polish Academy of Sciences, Krakow, through statutory funds for E. Worobiec. We also thank G. Worobiec (W. Szafer Institute of Botany, Polish Academy of Sciences, Krakow) for his help in taking photographs of pollen grains. M. Ziembinska-Tworzydlo and an anonymous reviewer are kindly acknowledged for reading the manuscript and critical comments.	Alexandrowicz S. W., 1963, Prace Instytutu Geologicznego Warszawa, V39, P1; Alexandrowicz S.W., 1970, SPRAWOZDANIA POSIEDZ, V13, P573; Alexandrowicz S.W., 1982, Geol. 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J	Kumar, A				Kumar, Arun			New palynological evidence for the age of the Beda Formation, Sirte Basin, Libya	PALAEONTOLOGIA ELECTRONICA			English	Article						Beda Formation; Sirte Basin Libya; Dinoflagellate cysts; Palaeocene-Eocene Palynology; Foraminifera; Palynology		The Beda Formation represents the subsurface sequence of interbedded limestone with subordinate dolomites, which are major hydrocarbon reservoirs in the western Sirte Basin of Libya. Middle Paleocene (Montian) age has been assigned to this formation based on foraminifera, but the list of those age diagnostic foraminifera could not be found in the published literature, thus the age of this formation is questionable. Thick Paleocene-Early to Middle Eocene limestones and calcareous claystones also occur in this basin. Palynological study of 32 core samples of the Beda Formation from four different wells was carried out; but only four samples of Core # 1 (6854'-6884') in the Well # X43 yielded low diversity yet workable assemblages of palynomorphs. The pollen grains and spores indicate a Paleogene age. However, the dinoflagellate cyst assemblages provide several stratigraphically significant forms that indicate an Early-Middle Eocene age. The results of the present study suggest that either the studied samples do not belong to the Beda Formation or the age of the Beda Formation ranges from Middle Palaeocene to Early-Middle Eocene. An extensive study of large numbers of core samples from several well sections is suggested to generate new micropaleontological and palynological data that could conclusively define age of the Beda Formation.	[Kumar, Arun] Carleton Univ, Dept Earth Sci, 1125 Colonel By Dr, Ottawa, ON K1S 5B6, Canada	Carleton University	Kumar, A (通讯作者)，Carleton Univ, Dept Earth Sci, 1125 Colonel By Dr, Ottawa, ON K1S 5B6, Canada.	arunkumarlko@hotmail.com						Ahlbrandt T.S., 2001, U. S. Geological Survey Bulletin, V2, P1; [Anonymous], 1972, P SEM PAL IND STRAT; [Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1996, GEOLOGY SIRT BASIN; Barr F., 1972, Stratigraphic Nomenclature of the Sirte Basin, Libya; Berggren W. A., 1969, P104; BERGGREN W A, 1974, Micropaleontology (New York), V20, P449, DOI 10.2307/1485130; Bezan A.M., 1996, First Symposium on the Sedimentary Basins of Libya, Geology of the Sirt Basin, V1, P97; Bezan A.M., 1996, GEOLOGY SIRT BASIN, V2, P135; Bronnimann P., 1962, BIOSTRATIGRAPHY W SI; Brosius M., 1963, Z DTSCH GEOLOGISCHEN, V114, P32; Burwood R, 2003, GEOL SOC SPEC PUBL, V207, P203, DOI 10.1144/GSL.SP.2003.207.11; Cookson I. 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J	Fensome, RA; Nohr-Hansen, H; Williams, GL				Fensome, Robert A.; Nohr-Hansen, Henrik; Williams, Graham L.			Cretaceous and Cenozoic dinoflagellate cysts and other palynomorphs from the western and eastern margins of the Labrador-Baffin Seaway	GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN			English	Article							TAXONOMIC NOTE; MICRO-FOSSILS; GREENLAND; PALEOCENE; STRATIGRAPHY; GENERA; NOV; EVOLUTION; REVISION; BIOSTRATIGRAPHY	New palynological analysis of samples from 13 offshore wells on the Canadian Margin and six wells on the West Greenland Margin has led to a new event biostratigraphic framework for Cretaceous-Cenozoic strata of the Labrador Sea - Davis Strait - Baffin Bay (Labrador-Baffin Seaway) region. This framework is based on about 150 dinoflagellate cyst taxa and 30 acritarch, algal, fungal and plant microfossil (mostly miospore) taxa. In the systematics we include three new genera of dinocysts (Scalenodinium, Simplicidinium and Taurodinium), 16 new species of dinocysts (Chirop teridium gilbertii, Chytroeisphaeridia hadra, Cleistosphaeridium elegantulum, Cleistosphaeridium palmatum, Dapsilidinium pseudoinsertum, De flan drea borealis, Evittosphaerula? foraminosa, Gingi nodinium? flexidentatum, Hystrichosphaeridium quadratum, Hystrichostrogylon digitus, Impletosphaeridium apodastum, Scalenodinium scalenum, Surculosphaeridium convocatum, Talladinium pellis, Taurodinium granulatum and Trithyrodinium? conservatum), four emendations of dinocyst genera (Alterbidinium, Chatangiella, Chiropteridium and Surculosphaeridium), six new combinations for dinocyst species (Alterbidinium biaperturum, Deflandrea majae, Kleithriasphaeridium mantellii, Simplicidinium insolitum, Spongodinium grossum, Spongodinium obscurum), one new acritarch species (Fromea quadrangularis), one new miospore species (Baculatisporites crenulatus) and one new combination for miospores (Tiliaepollenites crassipites). Most of the taxa included provide age information, almost exclusively last occurrences (range 'tops'), but some are useful mainly for environmental interpretations. Collectively, they provide a powerful tool for helping to establish the geological history of the Labrador-Baffin Seaway.	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J	Steurbaut, E; De Coninck, J; Van Simaeys, S				Steurbaut, Etienne; De Coninck, Jan; Van Simaeys, Stefaan			Micropalaeontological dating of the Premontre mammal fauna (MP10, Premontre Sands, EECO, early late Ypresian, Paris Basin)	GEOLOGICA BELGICA			English	Article						Organic-walled microfossils; calcareous nannofossils; Prrmontre Sands; MP10; palaeoenvironment; Paris Basin; EECO; early late Ypresian	DINOFLAGELLATE CYST; FOSSIL RECORD; EARLY EOCENE; BIOSTRATIGRAPHY	At their type locality the Premontre Sands contain fairly well-diversified organic-walled microfossil assemblages attributable to the lower part of dinoflagellate cyst Zone D9 and indicating a transition from an estuarine to a lagoonal depositional regime, up-section as well as laterally. Identical assemblages have been recorded in the inner to mid-neritic Merelbeke Clay Member in Belgium, allowing the Premontre Sands to be positioned within lower NP13 and early Chron C22r. The deposition of the MP10 Premontre mammal fauna is estimated to postdate the onset of both NP13 and Chron C22r, which are nearly coincident, by about 200 to 300 kyr. The biostratigraphic dating refers this deposit to the early late Ypresian and to the final phase of the Early Eocene Climatic Optimum (EECO) at about 50.4 to 50.3 million years ago. The Premontre Sands, as well as their distal equivalent the Merelbeke Clay Member, were deposited following a major sea-level rise, the highest of the late Ypresian in the southern North Sea Basin s.l. (including the Paris Basin). They are separated from the overlying "Glauconie grossiere" (zone NP14; middle part of zone D9) by a hiatus of approximately 2.5 myr.	[Steurbaut, Etienne] RBINS, OD Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium; [Steurbaut, Etienne] Katholieke Univ Leuven, Leuven, Belgium; [De Coninck, Jan] Univ Ghent, Res Unit Palaeontol WE13, Krijgslaan 281-S8, B-9000 Ghent, Belgium; [Van Simaeys, Stefaan] ExxonMobil Upstream Res Co, 22777 Springwoods Village Pkwy, Houston, TX 77389 USA	KU Leuven; Ghent University; Exxon Mobil Corporation	Steurbaut, E (通讯作者)，RBINS, OD Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium.; Steurbaut, E (通讯作者)，Katholieke Univ Leuven, Leuven, Belgium.	etienne.steurbaut@naturalsciences.be; svansimaeys@yahoo.com						Adnet S, 2008, ACTA PALAEONTOL POL, V53, P433, DOI 10.4202/app.2008.0306; Agnini C, 2006, EARTH PLANET SC LETT, V241, P815, DOI 10.1016/j.epsl.2005.11.005; [Anonymous], 1988, Geol. 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J	Gedl, P				Gedl, Przemyslaw			DINOFLAGELLATE CYSTS AND PALYNOFACIES FROM THE UPPER BADENIAN (MIDDLE MIOCENE) OF THE ROZTOCZE AREA AT JOZEFOW AND ZELEBSKO (CARPATHIAN FOREDEEP BASIN, POLAND): PALAEOENVIRONMENTAL IMPLICATIONS	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						Dinoflagellate cysts; palynofacies; palaeoenvironment; Miocene; Palaeogene substratum; Roztocze; Carpathian Foredeep Basin	SE POLAND; WESTERN UKRAINE; ADJACENT SEAS; NORTH; EOCENE; BIOSTRATIGRAPHY; ASSEMBLAGES; SEDIMENTS; PALEOGENE; SALINITY	The post-evaporitic upper Badenian (Middle Miocene) succession of the Roztocze (marginal zone of the Carpathian Foredeep Basin) consists of shallow-marine sands and organodetrital deposits. The latter, although predominantly coarse-grained, include very rare and usually very thin intercalations of fine-grained, loamy material. A few such clay layers were sampled for their palynological content in quarries at Jozefow (Jozefow and Pardysowka) and Zelebsko. The clay samples yielded palynological organic matter, in contrast to organodetrital limestone samples, which were barren. The palynofacies composition, both presence/absence of land-derived material and the specific composition of aquatic material, are useful for the palaeoenvironmental reconstructions of sedimentary settings. During late Badenian time, the sedimentary setting of the deposits studied was characterized by proximity to the shoreline, which, however, supplied limited input of terrestrial matter, and by restricted marine conditions caused by increased salinity. During the latest Badenian, water salinity presumably underwent a further increase, leading to the collapse of the dinoflagellate floras. The frequent occurrence of reworked Palaeogene dinoflagellate cysts in upper Badenian samples and their absence from the uppermost Badenian indicate variable intensity of erosion of the epicontinental Palaeogene strata during the Middle Miocene at Roztocze.	[Gedl, Przemyslaw] Polish Acad Sci, Res Ctr Krakow, 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, Res Ctr Krakow, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl						Andreychouk V, 2014, ANN SOC GEOL POL, V84, P297; [Anonymous], 1996, Palynology: principles and applications; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brugman W. 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J	Dalseg, TS; Nakrem, HA; Smelror, M				Dalseg, Thine Sanne; Nakrem, Hans Arne; Smelror, Morten			Dinoflagellate cyst biostratigraphy, palynofacies, depositional environment and sequence stratigraphy of the Agardhfjellet Formation (Upper Jurassic-Lower Cretaceous) in central Spitsbergen (Arctic Norway)	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Mesozoic; stratigraphy; dinoflagellate cysts; palynofacies; Svalbard; Arctic	HYDROCARBON SEEP CARBONATES; JANUSFJELLET SUBGROUP; LAGERSTATTE; SEA	The Upper Jurassic-Lower Cretaceous in the Isfjorden area (central Spitsbergen), consisting mostly of dark shales, with local carbonate-seep deposits, have been analysed for marine palynomorphs and palynofacies. Two dinoflagellate cyst assemblage zones have been defined in the Slottsmoya Member (Agardhfjellet Formation). The palynostratigraphic zones are established with reference to delta C-13(org) curves, and are correlated with Early Volgian to Late Ryazanian foraminiferal zones and ammonite zones from the same area. A Leiosphaeridia bloom at 45.62 m in the Janufjellet profile is correlated with a comparable bloom recovered from several locations on the western Barents shelf. Palynofacies analysis is used to interpret relative sea-level changes and is also used to constrain the sequence stratigraphy of the studied sections at Janufjellet and Knorrinfjellet.	[Dalseg, Thine Sanne] BakerHughes, Tanangerveien 501, N-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, N-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 [EC0425-09, EC0435-09]	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)	The sample material used in this study was collected by Oyvind Hammer and Hans Arne Nakrem during the palaeontological expeditions organised by the Natural History Museum, University of Oslo in 2008 and 2009. Fieldwork in Svalbard (2007-2010) was financed by the Norwegian Research Council, Norwegian Petroleum Directorate, Spitsbergen Travel, ExxonMobil, Fugro, Statoil, OMV, Powercontrols and Hydro, and by grants nos. EC0425-09 and EC0435-09 from the National Geographic Society. The authors are grateful to all the volunteers and students who have contributed weeks of fieldwork for free on the project.	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Geol.		2016	96	2					119	133		10.17850/njg96-2-04	http://dx.doi.org/10.17850/njg96-2-04			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EA3ZD		gold			2025-03-11	WOS:000386546900004
